{"pageNumber":"807","pageRowStart":"20150","pageSize":"25","recordCount":184618,"records":[{"id":70200943,"text":"70200943 - 2018 - Currents, waves and sediment transport around the headland of Pt. Dume, California","interactions":[],"lastModifiedDate":"2018-11-16T16:54:43","indexId":"70200943","displayToPublicDate":"2018-11-16T16:54:41","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1333,"text":"Continental Shelf Research","active":true,"publicationSubtype":{"id":10}},"title":"Currents, waves and sediment transport around the headland of Pt. Dume, California","docAbstract":"<p><span>Sediment transport&nbsp;past rocky headlands has received less attention compared to transport along beaches. Here we explore, in a field-based study, possible pathways for sediment movement adjacent to Point Dume, a headland in Santa Monica&nbsp;Bay, California. This prominent&nbsp;shoreline feature&nbsp;is a nearly symmetrical, triangular-shaped promontory interior to the Santa Monica&nbsp;</span>Littoral<span>&nbsp;Cell. We collected current, wave, and&nbsp;turbidity&nbsp;data for 74 days during which several wave events occurred, including one associated with a remote&nbsp;hurricane&nbsp;and another generated by the first winter storm of 2014. We also acquired sediment samples to quantify&nbsp;seabed&nbsp;grain-size&nbsp;distributions. Near-bottom currents towards the headland dominated on both of its sides and wave-driven&nbsp;longshore currents&nbsp;in the&nbsp;surf zone&nbsp;were faster on the exposed side. Bed&nbsp;shear stresseswere generated mostly by waves with minor contributions from currents, but both wave-driven and other currents contributed to sediment flux. On the wave-exposed west side of the headland,&nbsp;suspended sediment&nbsp;concentrations correlated with bed stress suggesting local&nbsp;resuspension&nbsp;whereas turbidity levels on the sheltered east side of the headland are more easily explained by advective delivery. Most of the suspended sediment appears to be exported offshore due to flow separation at the apex of the headland but may not move far given that sediment fluxes at moorings offshore of the apex were small. Further, wave-driven sediment flux in the surf zone is unlikely to pass the headland due to the discontinuity in wave forcing that causes longshore transport in different directions on each side of the headland. It is thus unlikely that sand is transported past the headland (specifically in a westerly direction), although some transport of finer fractions may occur offshore in deep water. These findings of minimal sediment flux past Point Dume are consistent with its role as a littoral cell boundary, although more complex multi-stage processes and unusual events may account for some transport at times.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.csr.2018.10.011","usgsCitation":"George, D.A., Largier, J.L., Storlazzi, C.D., Robart, M.J., and Gaylord, B., 2018, Currents, waves and sediment transport around the headland of Pt. Dume, California: Continental Shelf Research, v. 171, p. 63-76, https://doi.org/10.1016/j.csr.2018.10.011.","productDescription":"14 p.","startPage":"63","endPage":"76","ipdsId":"IP-091841","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":468242,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.csr.2018.10.011","text":"Publisher Index Page"},{"id":359531,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Pt. Dume","volume":"171","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5befe5b9e4b045bfcadf7f26","contributors":{"authors":[{"text":"George, Douglas A.","contributorId":60328,"corporation":false,"usgs":true,"family":"George","given":"Douglas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":751417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Largier, John L.","contributorId":175121,"corporation":false,"usgs":false,"family":"Largier","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":751418,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Storlazzi, Curt D. 0000-0001-8057-4490 cstorlazzi@usgs.gov","orcid":"https://orcid.org/0000-0001-8057-4490","contributorId":140584,"corporation":false,"usgs":true,"family":"Storlazzi","given":"Curt","email":"cstorlazzi@usgs.gov","middleInitial":"D.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":751416,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robart, Matthew J.","contributorId":210665,"corporation":false,"usgs":false,"family":"Robart","given":"Matthew","email":"","middleInitial":"J.","affiliations":[{"id":38129,"text":"UCD/BML","active":true,"usgs":false}],"preferred":false,"id":751419,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gaylord, Brian","contributorId":210666,"corporation":false,"usgs":false,"family":"Gaylord","given":"Brian","email":"","affiliations":[{"id":38129,"text":"UCD/BML","active":true,"usgs":false}],"preferred":false,"id":751420,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70198512,"text":"sir20185097 - 2018 - Chemical and isotopic characteristics of methane in groundwater of Ohio, 2016","interactions":[],"lastModifiedDate":"2018-11-19T14:13:05","indexId":"sir20185097","displayToPublicDate":"2018-11-16T16:00:00","publicationYear":"2018","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2018-5097","displayTitle":"Chemical and Isotopic Characteristics of Methane in Groundwater of Ohio, 2016","title":"Chemical and isotopic characteristics of methane in groundwater of Ohio, 2016","docAbstract":"<p>In 2016, the U.S. Geological Survey, in cooperation with the Ohio Water Development Authority, investigated the hydrogeologic setting, chemical and isotopic characteristics, and origin of methane in groundwater of Ohio. Understanding the occurrence and distribution of methane in groundwater is important in terms of public safety because methane in water wells can pose a risk of explosion. In addition, documenting the chemical and isotopic characteristics of methane in groundwater can make an important contribution to future stray gas investigations.</p><p>Water samples were collected from 15 domestic water wells known to produce methane, which were in 12 counties in diverse parts of Ohio. The wells were 75–345 feet deep and tapped a range of aquifer types, including glacial deposits and bedrock of Upper Ordovician, Upper Devonian, Lower Mississippian, and Pennsylvanian ages. Although the hydrogeologic settings were varied, there was a broad similarity among the well sites in that the bedrock was predominantly shale and the glacial deposits were predominantly clay.</p><p>The wells were sampled for dissolved inorganic constituents; dissolved organic carbon; methane and other dissolved gases; stable isotopes (carbon, hydrogen, and oxygen) of methane, water, and dissolved inorganic carbon; and carbon-14 of methane. Gas composition and stable isotopes of methane were used to differentiate thermogenic and microbial methane. The degree of fractionation of hydrogen and carbon isotopes was used to evaluate the pathway of microbial methanogenesis (carbon dioxide [CO<sub>2</sub>] reduction or acetate fermentation) and the effects of secondary processes such as oxidation, mixing, and migration. The concentration of carbon-14 of methane was used to evaluate the relative age of the carbon source.</p><p>The quality of water from the 15 wells differed greatly; water types ranged from CaMgHCO<sub>3</sub> to NaCl, and total dissolved solids concentrations ranged from 318 to 2,940 milligrams per liter (mg/L). Methane concentrations ranged from 1.2 to 120 mg/L. Of the 15 samples, 12 had methane concentrations greater than 28 mg/L, the level that can pose a risk of explosion.</p><p>Of the 15 samples, 12 had chemical and isotopic characteristics or \"signatures\" consistent with microbial methane formed by CO<sub>2</sub> reduction. CO<sub>2</sub> reduction is commonly associated with microbial degradation of organic matter in anaerobic aquifers and with the formation of microbial shale gas and coalbed methane along margins of sedimentary basins. Two of 15 samples were interpreted as having a component of thermogenic methane based on the δ<sup>13</sup>C of methane (−50.96 and −47.74 parts per thousand [per mil]) and gas dryness (28 and 5). One of 15 samples (from the shallowest well) had chemical and isotopic characteristics consistent with methane oxidation by sulfate reduction based on light δ<sup>13</sup>C of dissolved inorganic carbon (−31.6 per mil) and evidence of sulfate reduction in terms of the odor and appearance of the water.</p><p>For the 12 samples interpreted as microbial methane formed by CO<sub>2</sub> reduction, the δ<sup>13</sup>C of methane varied from −75 to −56 per mil. Multiple samples from the same aquifer demonstrated a general trend of increasing δ<sup>13</sup>C of methane with depth. Samples with lighter δ<sup>13</sup>C of methane (−75 to −62 per mil) were from shallower wells (or wells with shallow open intervals), and the isotopic signature of the water was consistent with modern or postglacial groundwater recharge. Three samples with heavier δ<sup>13</sup>C of methane (−61 to −56 per mil) were from deeper wells or more confined aquifers where the isotopic signature of water was consistent with older (glacial) recharge. In addition, δ<sup>13</sup>C of dissolved inorganic carbon was enriched (+12 to +18.9 per mil), and carbon-14 of methane was consistent with carbon associated with Paleozoic bedrock or older glacial deposits. These observations are generally consistent with increased Rayleigh-type fractionation at greater depths; however, other interpretations are possible. Isotopic signatures can be ambiguous, especially in areas with complex geologic histories that include multiple episodes of migration, mixing, and (or) oxidation.</p><p>Many of the wells were in proximity to multiple potential natural and anthropogenic pathways of methane migration; however, it is not possible to determine if the methane in any of the wells is related to human activities based on the chemical and isotopic data collected for this study.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20185097","collaboration":"Prepared in cooperation with the Ohio Water Development Authority","usgsCitation":"Thomas, M.A., 2018, Chemical and isotopic characteristics of methane in groundwater of Ohio, 2016: U.S. Geological Survey Scientific Investigations Report 2018–5097, 42 p., https://doi.org/10.3133/sir20185097.","productDescription":"vi, 42 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 \"}}]}","contact":"<p><a href=\"mailto:dc_oh@usgs.gov\" data-mce-href=\"mailto:dc_oh@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/oki-water\" data-mce-href=\"https://www.usgs.gov/centers/oki-water\">Ohio-Kentucky-Indiana Water Science Center</a><br>U.S. Geological Survey<br>6460 Busch Boulevard Ste. 100<br>Columbus, OH 43229-1737</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Methods of Study&nbsp;</li><li>Characteristics of the Well Network</li><li>Groundwater Quality</li><li>Chemical and Isotopic Characteristics of Methane and Related Constituents</li><li>Interpretation of Methane Origin</li><li>Summary and Conclusions</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":15,"text":"Madison PSC"},"publishedDate":"2018-11-16","noUsgsAuthors":false,"publicationDate":"2018-11-16","publicationStatus":"PW","scienceBaseUri":"5befe5b9e4b045bfcadf7f28","contributors":{"authors":[{"text":"Thomas, Mary Ann 0000-0001-8681-1370 mathomas@usgs.gov","orcid":"https://orcid.org/0000-0001-8681-1370","contributorId":206777,"corporation":false,"usgs":true,"family":"Thomas","given":"Mary Ann","email":"mathomas@usgs.gov","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":741734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207058,"text":"70207058 - 2018 - Construction of a compact low-cost radiation shield for air-temperature sensors in ecological field studies","interactions":[],"lastModifiedDate":"2019-12-04T15:32:41","indexId":"70207058","displayToPublicDate":"2018-11-16T15:28:11","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2498,"text":"Journal of Visualized Experiments","active":true,"publicationSubtype":{"id":10}},"title":"Construction of a compact low-cost radiation shield for air-temperature sensors in ecological field studies","docAbstract":"<p><span>With the advent of small, low-cost environmental sensors, it is now possible to deploy high-density networks of sensors to measure hyper localized temperature variation. Here, we provide a detailed methodology for constructing a compact version of a previously described custom-fabricated radiation shield for use with inexpensive thermochrons.</span></p>","language":"English","publisher":"JoVE","doi":"10.3791/58273","usgsCitation":"Terando, A.J., Prado, S.G., and Youngsteadt, E., 2018, Construction of a compact low-cost radiation shield for air-temperature sensors in ecological field studies: Journal of Visualized Experiments, no. 141, e58273, https://doi.org/10.3791/58273.","productDescription":"e58273","ipdsId":"IP-098717","costCenters":[{"id":36940,"text":"National Climate Adaptation Science Center","active":true,"usgs":true}],"links":[{"id":369920,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"141","noUsgsAuthors":false,"publicationDate":"2018-11-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Terando, Adam J. 0000-0002-9280-043X aterando@usgs.gov","orcid":"https://orcid.org/0000-0002-9280-043X","contributorId":173447,"corporation":false,"usgs":true,"family":"Terando","given":"Adam","email":"aterando@usgs.gov","middleInitial":"J.","affiliations":[{"id":565,"text":"Southeast Climate Science Center","active":true,"usgs":true}],"preferred":true,"id":776664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prado, Sara G.","contributorId":204504,"corporation":false,"usgs":false,"family":"Prado","given":"Sara","email":"","middleInitial":"G.","affiliations":[{"id":7091,"text":"North Carolina State University","active":true,"usgs":false}],"preferred":false,"id":776665,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Youngsteadt, Elsa","contributorId":205500,"corporation":false,"usgs":false,"family":"Youngsteadt","given":"Elsa","email":"","affiliations":[{"id":7091,"text":"North Carolina State University","active":true,"usgs":false}],"preferred":false,"id":776666,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70204266,"text":"70204266 - 2018 - Defining blue carbon: The emergence of a climate context for coastal carbon dynamics","interactions":[],"lastModifiedDate":"2019-07-17T12:57:23","indexId":"70204266","displayToPublicDate":"2018-11-16T14:57:39","publicationYear":"2018","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"chapter":"1","title":"Defining blue carbon: The emergence of a climate context for coastal carbon dynamics","docAbstract":"<div class=\"product-details\"><div class=\"chapter-detail-container\"><div class=\"container\"><div class=\"flex-container\"><div class=\"chapter-description-container\"><div class=\"abstract-content\"><p>Blue Carbon Ecosystems (BCEs) are defined as coastal wetland ecosystems with manageable and atmospherically significant carbon stocks and fluxes.</p><p>Policy and management opportunities have promoted the emergence of blue carbon as a concept and spurred scientific interest to reduce uncertainties in coastal carbon budgets.</p><p>The four major BCEs are generally classified by their plant communities: tidal marshes, tidal freshwater forests, mangroves, and seagrass meadows.</p><p><br data-mce-bogus=\"1\"></p></div></div></div></div></div></div>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"A blue carbon primer: The state of coastal wetland carbon science, practice and policy","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Taylor & Francis","doi":"10.1201/9780429435362","usgsCitation":"Crooks, S., Windham-Myers, L., and Tiffany Troxler, 2018, Defining blue carbon: The emergence of a climate context for coastal carbon dynamics, chap. 1 <i>of</i> A blue carbon primer: The state of coastal wetland carbon science, practice and policy, p. 1-8, https://doi.org/10.1201/9780429435362.","productDescription":"8 p.","startPage":"1","endPage":"8","ipdsId":"IP-099272","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":365632,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Crooks, Stephen","contributorId":217032,"corporation":false,"usgs":false,"family":"Crooks","given":"Stephen","email":"","affiliations":[{"id":38182,"text":"Silvestrum Climate Associates","active":true,"usgs":false}],"preferred":false,"id":766271,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Windham-Myers, Lisamarie","contributorId":217031,"corporation":false,"usgs":true,"family":"Windham-Myers","given":"Lisamarie","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":766270,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tiffany Troxler","contributorId":217029,"corporation":false,"usgs":false,"family":"Tiffany Troxler","affiliations":[{"id":7017,"text":"Florida International University","active":true,"usgs":false}],"preferred":false,"id":766272,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70204267,"text":"70204267 - 2018 - Blue Carbon Futures: moving forward on terra firma","interactions":[],"lastModifiedDate":"2019-07-16T14:54:15","indexId":"70204267","displayToPublicDate":"2018-11-16T14:51:00","publicationYear":"2018","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"chapter":"28","title":"Blue Carbon Futures: moving forward on terra firma","docAbstract":"<p>Maintaining coastal carbon sequestration and storage services is economically valuable in providing a potentially long-term contribution toward climate resilience, both in terms of adaptation and mitigation.</p><p>392The volumetric accumulation of coastal carbon stocks is unique from other terrestrial and aquatic processes, and inconsistent use of terminology is holding back understanding of the range, magnitude, and processes critical to this carbon sink.</p><p>Documenting net greenhouse gas (GHG) benefits of coastal ecosystem management needs integrated models that quantitatively incorporate geomorphic, biogeochemical, atmospheric, and hydrologic exchanges to account for both carbon accumulation and loss, across a range of timescales.</p><p>A community effort is necessary to explore similarities among coastal ecosystems to determine the drivers and scale of true variability, to prioritize specific wetland management options, and develop the most effective monitoring approaches.</p><p>While there are further scientific aspects of blue carbon to be explored, there is sufficient knowledge and experience to advance demonstration projects across a range of systems and conditions, which can inform policy development and scaled implementation.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"A blue carbon primer: The state of coastal wetland carbon science, practice and policy","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Taylor & Francis","doi":"10.1201/9780429435362","usgsCitation":"Windham-Myers, L., Crooks, S., and Tiffany Troxler, 2018, Blue Carbon Futures: moving forward on terra firma, chap. 28 <i>of</i> A blue carbon primer: The state of coastal wetland carbon science, practice and policy, p. 391-402, https://doi.org/10.1201/9780429435362.","productDescription":"11 p.","startPage":"391","endPage":"402","ipdsId":"IP-099273","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":365629,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Windham-Myers, Lisamarie","contributorId":217033,"corporation":false,"usgs":true,"family":"Windham-Myers","given":"Lisamarie","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":766273,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crooks, Stephen","contributorId":217032,"corporation":false,"usgs":false,"family":"Crooks","given":"Stephen","email":"","affiliations":[{"id":38182,"text":"Silvestrum Climate Associates","active":true,"usgs":false}],"preferred":false,"id":766274,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tiffany Troxler","contributorId":217029,"corporation":false,"usgs":false,"family":"Tiffany Troxler","affiliations":[{"id":7017,"text":"Florida International University","active":true,"usgs":false}],"preferred":false,"id":766275,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70204497,"text":"70204497 - 2018 - Identification of storm events and contiguous coastal sections for deterministic modeling of extreme coastal flood events in response to climate change","interactions":[],"lastModifiedDate":"2020-12-15T22:35:31.045435","indexId":"70204497","displayToPublicDate":"2018-11-16T14:27:18","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1262,"text":"Coastal Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Identification of storm events and contiguous coastal sections for deterministic modeling of extreme coastal flood events in response to climate change","docAbstract":"<p>Deterministic dynamical modeling of future climate conditions and associated hazards, such as flooding, can be computationally-expensive if century-long time-series of waves, sea level variations, and overland flow patterns are simulated. To alleviate some of the computational costs, local impacts of individual coastal storms can be explored by first identifying particular events or scenarios of interest and dynamically modeling those events in detail. In this study, an efficient approach to selecting storm events for subsequent deterministic detailed modeling of coastal flooding is presented. The approach identifies locally relevant scenarios derived from regional datasets spanning long time-periods and covering large geographic areas. This is done by identifying storm events from global climate models using a robust, yet computationally simple approach for calculating total water level proxies at the shore, assuming a linear superposition of the important processes contributing to the overall total water level. Clustering of the total water level time-series is used to define coherent coastal cells where similar return period water level extrema occur in response to region-wide storms. Results show that the more severe but rare coastal flood events (e.g., the 100-year (yr) event) typically occur from the same storm across the region, but that a number of different storms are responsible for the less severe but more frequent local extreme water levels (e.g., the 1-yr event). This new ‘storm selection’ approach is applied to the Southern California Bight, a region of varying shoreline orientations that is subject to wave refraction across complex bathymetry, and shadowing, focusing, diffraction, and dissipation of wave energy by islands. Results indicate that wave runup dominates total water level extremes at this study site, highlighting the importance of downscaling global-scale models to nearshore waves when seeking accurate projections of local coastal hazards in response to climate change.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.coastaleng.2018.08.003","usgsCitation":"Erikson, L.H., Espejo, A., Barnard, P., Katherine A. Serafin, Hegermiller, C., O'Neill, A., Ruggerio, P., Limber, P.W., and Mendez, F.J., 2018, Identification of storm events and contiguous coastal sections for deterministic modeling of extreme coastal flood events in response to climate change: Coastal Engineering, v. 140, p. 316-330, https://doi.org/10.1016/j.coastaleng.2018.08.003.","productDescription":"15 p.","startPage":"316","endPage":"330","ipdsId":"IP-077289","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":468243,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1016/j.coastaleng.2018.08.003","text":"External Repository"},{"id":366001,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Southern California Bight","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.2451171875,\n              32.63937487360669\n            ],\n            [\n              -116.5869140625,\n              32.63937487360669\n            ],\n            [\n              -116.5869140625,\n              35.10193405724606\n            ],\n            [\n              -121.2451171875,\n              35.10193405724606\n            ],\n            [\n              -121.2451171875,\n              32.63937487360669\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"140","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Erikson, Li H. 0000-0002-8607-7695 lerikson@usgs.gov","orcid":"https://orcid.org/0000-0002-8607-7695","contributorId":149963,"corporation":false,"usgs":true,"family":"Erikson","given":"Li","email":"lerikson@usgs.gov","middleInitial":"H.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":767253,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Espejo, Antonio","contributorId":217673,"corporation":false,"usgs":false,"family":"Espejo","given":"Antonio","email":"","affiliations":[],"preferred":false,"id":767254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barnard, Patrick L. 0000-0003-1414-6476 pbarnard@usgs.gov","orcid":"https://orcid.org/0000-0003-1414-6476","contributorId":147147,"corporation":false,"usgs":true,"family":"Barnard","given":"Patrick L.","email":"pbarnard@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":767255,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Katherine A. Serafin","contributorId":187534,"corporation":false,"usgs":false,"family":"Katherine A. Serafin","affiliations":[],"preferred":false,"id":767256,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hegermiller, Christie 0000-0002-6383-7508 chegermiller@usgs.gov","orcid":"https://orcid.org/0000-0002-6383-7508","contributorId":149010,"corporation":false,"usgs":true,"family":"Hegermiller","given":"Christie","email":"chegermiller@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":767257,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"O'Neill, Andrea C. 0000-0003-1656-4372 aoneill@usgs.gov","orcid":"https://orcid.org/0000-0003-1656-4372","contributorId":5351,"corporation":false,"usgs":true,"family":"O'Neill","given":"Andrea C.","email":"aoneill@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":767258,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ruggerio, Peter","contributorId":67403,"corporation":false,"usgs":true,"family":"Ruggerio","given":"Peter","email":"","affiliations":[],"preferred":false,"id":767259,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Limber, Patrick W. 0000-0002-8207-3750 plimber@usgs.gov","orcid":"https://orcid.org/0000-0002-8207-3750","contributorId":196794,"corporation":false,"usgs":true,"family":"Limber","given":"Patrick","email":"plimber@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":767260,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Mendez, Fernando J.","contributorId":140322,"corporation":false,"usgs":false,"family":"Mendez","given":"Fernando","email":"","middleInitial":"J.","affiliations":[{"id":13456,"text":"IH Cantrabria","active":true,"usgs":false}],"preferred":false,"id":767261,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70200699,"text":"70200699 - 2018 - Subsurface controls on the development of the Cape Fear Slide Complex, central US Atlantic Margin","interactions":[],"lastModifiedDate":"2019-10-09T08:37:04","indexId":"70200699","displayToPublicDate":"2018-11-16T13:02:32","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5011,"text":"Geological Society of London Special Publications","active":true,"publicationSubtype":{"id":10}},"title":"Subsurface controls on the development of the Cape Fear Slide Complex, central US Atlantic Margin","docAbstract":"<p><span>The Cape Fear Slide is one of the largest (&gt;25 000 km</span><sup>3</sup><span>) submarine slope failure complexes on the US Atlantic margin. Here we use a combination of new high-resolution multichannel seismic data (MCS) from the National Science Foundation Geodynamic Processes at Rifting and Subducting Margins (NSF GeoPRISMS) Community Seismic Experiment and legacy industry MCS to derive detailed stratigraphy of this slide and constrain the conditions that lead to slope instability. Limited outer-shelf and upper-slope accommodation space during the Neogene, combined with lowstand fluvial inputs and northwards Gulf Stream sediment transport, appears to have contributed to thick Miocene and Pliocene deposits that onlapped the lower slope. This resulted in burial of an upper-slope bypass zone developed from earlier erosional truncation of Paleogene strata. These deposits created a broad ramp that allowed accumulation of thick Quaternary strata across a low-gradient (&lt;3.5°) upper slope. Upslope of one of the larger headwalls, undulating Quaternary strata appear to downlap onto a buried failure plane. Many of the nested headwalls of the upper-slope portion of slide complex are underlain by deformed strata, which may be the result of fluid migration associated with localized subsidence from salt migration. These new data and observations suggest that antecedent margin physiography, sediment loading and substrate fluid flow were key factors in preconditioning the Cape Fear slope for failure.</span></p>","language":"English","publisher":"Geological Society of London","doi":"10.1144/SP477.17","usgsCitation":"Hill, J.C., Brothers, D., Hornbach, M.J., Sawyer, D.E., Shillington, D.J., and Becel, A., 2018, Subsurface controls on the development of the Cape Fear Slide Complex, central US Atlantic Margin: Geological Society of London Special Publications, v. 477, p. 169-182, https://doi.org/10.1144/SP477.17.","productDescription":"14 p.","startPage":"169","endPage":"182","ipdsId":"IP-089531","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":359515,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"477","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2018-03-28","publicationStatus":"PW","scienceBaseUri":"5befe5bae4b045bfcadf7f2a","contributors":{"authors":[{"text":"Hill, Jenna C. 0000-0002-7475-357X","orcid":"https://orcid.org/0000-0002-7475-357X","contributorId":21987,"corporation":false,"usgs":true,"family":"Hill","given":"Jenna","email":"","middleInitial":"C.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":750155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brothers, Daniel S. 0000-0001-7702-157X","orcid":"https://orcid.org/0000-0001-7702-157X","contributorId":210199,"corporation":false,"usgs":true,"family":"Brothers","given":"Daniel S.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":750156,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hornbach, Matthew J.","contributorId":210200,"corporation":false,"usgs":false,"family":"Hornbach","given":"Matthew","email":"","middleInitial":"J.","affiliations":[{"id":20300,"text":"Southern Methodist University","active":true,"usgs":false}],"preferred":false,"id":750157,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sawyer, Derek E.","contributorId":210201,"corporation":false,"usgs":false,"family":"Sawyer","given":"Derek","email":"","middleInitial":"E.","affiliations":[{"id":18155,"text":"The Ohio State University","active":true,"usgs":false}],"preferred":false,"id":750158,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Shillington, Donna J.","contributorId":210202,"corporation":false,"usgs":false,"family":"Shillington","given":"Donna","email":"","middleInitial":"J.","affiliations":[{"id":38091,"text":"Lamont Doherty Earth Observatory, Columbia University","active":true,"usgs":false}],"preferred":false,"id":750159,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Becel, Anne","contributorId":210203,"corporation":false,"usgs":false,"family":"Becel","given":"Anne","email":"","affiliations":[{"id":38091,"text":"Lamont Doherty Earth Observatory, Columbia University","active":true,"usgs":false}],"preferred":false,"id":750160,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70201041,"text":"70201041 - 2018 - American Recent Eulipotyphla: Nesophontids, Solenodons, Moles, and Shrews in the New World","interactions":[],"lastModifiedDate":"2018-11-26T11:50:23","indexId":"70201041","displayToPublicDate":"2018-11-16T11:50:13","publicationYear":"2018","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"American Recent Eulipotyphla: Nesophontids, Solenodons, Moles, and Shrews in the New World","docAbstract":"The mammalian taxonomic order Eulipotyphla is comprised of the living taxonomic families Erinaceidae (gymnures, hedgehogs, and moonrats), Solenodontidae (solenodonts), Soricidae (shrews), and Talpidae (desmans and moles).  Morphological and molecular studies continue to alter our view of relationships within and among these families, and this research has added considerably to our understanding of the diversity, distributions, and relationships of many of the New World species that belong to them. Currently, there are more than 450 recognized living species worldwide, making the Eulipotyphla the third most speciose order of mammals. New World (North and South America and associated islands) eulipotyphlans currently include 110 recognized species of shrews, seven species of moles, and both living species of solenodons.  In this work, I attempt to summarize the taxonomic results of recent studies and provide a guide to the most appropriate current applications of taxonomic names in this region.","language":"English","publisher":"Smithsonian Institute Scholarly Press","doi":"10.5479/si.1943-6696.650","usgsCitation":"Woodman, N., 2018, American Recent Eulipotyphla: Nesophontids, Solenodons, Moles, and Shrews in the New World, v. 650, vi, 107 p., https://doi.org/10.5479/si.1943-6696.650.","productDescription":"vi, 107 p.","ipdsId":"IP-097553","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":359655,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"650","publishingServiceCenter":{"id":10,"text":"Baltimore PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5bfd146ee4b0815414ca38f0","contributors":{"authors":[{"text":"Woodman, Neal 0000-0003-2689-7373 nwoodman@usgs.gov","orcid":"https://orcid.org/0000-0003-2689-7373","contributorId":3547,"corporation":false,"usgs":true,"family":"Woodman","given":"Neal","email":"nwoodman@usgs.gov","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":751971,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70200934,"text":"70200934 - 2018 - The influence of seep habitats on sediment macrofaunal biodiversity and functional traits","interactions":[],"lastModifiedDate":"2018-12-05T14:05:19","indexId":"70200934","displayToPublicDate":"2018-11-16T11:21:28","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1370,"text":"Deep-Sea Research Part I: Oceanographic Research Papers","active":true,"publicationSubtype":{"id":10}},"title":"The influence of seep habitats on sediment macrofaunal biodiversity and functional traits","docAbstract":"<p><span>Chemosynthetic ecosystems in the Gulf of Mexico (GOM) support dense communities of seep megafaunal&nbsp;invertebrates&nbsp;that rely on endosymbiotic bacteria for nutrition. Distinct infaunal communities are associated with the&nbsp;biogenic&nbsp;habitats created by seep biota, where habitat heterogeneity and sediment&nbsp;geochemistry&nbsp;influence local macrofaunal community structure. Here we examine the community structure and function of seep infaunal communities in the GOM in relation to environmental drivers and estimated proximity to seeps. We modeled seep distribution within 3 major seep fields (AC601, GC852, and AT340), and examined the influence of proximity to seep and associated sediment environment on infaunal community structure and function. To model seep habitat distribution, we used known seep occurrence data from&nbsp;ROV&nbsp;and towed camera images, terrain variables derived from high resolution multibeam&nbsp;bathymetry&nbsp;(gridded to 3 m resolution), and a maximum&nbsp;entropy&nbsp;(Maxent) approach. Model performance was high, with mean area under the curve for each habitat ranging from 0.851 for mussel to 0.908 for&nbsp;</span>tubeworm<span>&nbsp;habitat, with the models highly influenced by terrain&nbsp;rugosity. Replicate&nbsp;sediment cores&nbsp;were collected from the three sites in 2007 and processed for&nbsp;macrofauna&nbsp;and environmental characteristics. A majority of the taxa (86%) occurred within 16 m of modeled seep habitat and increased distance from modeled seeps was generally associated with lower calculated seep index coupled with decreased macrofaunal densities. Distance-based linear regression indicated that patterns in macrofaunal communities were driven by proximity to modeled seep habitat and profile curvature, a metric for the shape of the maximum slope. Similarly, variance in infaunal functional traits was best explained by proximity to seep, but also sediment C:N, reflecting the relative influence of&nbsp;sediment chemistry, including organic content, on infaunal communities. Results suggest that northern GOM seep infaunal community assemblages and their function are structured by factors that influence&nbsp;food availability&nbsp;and habitat heterogeneity. Given the abundance of seeps in the GOM and in the world’s oceans, this study supports the premise that the sphere of influence of seeps is spatially extensive.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.dsr.2018.10.004","usgsCitation":"Demopoulos, A.W., Bourque, J.R., Durkin, A., and Cordes, E.E., 2018, The influence of seep habitats on sediment macrofaunal biodiversity and functional traits: Deep-Sea Research Part I: Oceanographic Research Papers, v. 142, p. 77-93, https://doi.org/10.1016/j.dsr.2018.10.004.","productDescription":"17 p.","startPage":"77","endPage":"93","ipdsId":"IP-092914","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":468244,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.dsr.2018.10.004","text":"Publisher Index Page"},{"id":437683,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/F7FB524M","text":"USGS data release","linkHelpText":"The influence of hydrocarbon seeps on sediment macrofaunal biodiversity and functional traits"},{"id":359513,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Gulf of Mexico","volume":"142","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5befe5bae4b045bfcadf7f2c","contributors":{"authors":[{"text":"Demopoulos, Amanda W. J. 0000-0003-2096-4694","orcid":"https://orcid.org/0000-0003-2096-4694","contributorId":206536,"corporation":false,"usgs":true,"family":"Demopoulos","given":"Amanda","email":"","middleInitial":"W. J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":751380,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bourque, Jill R. 0000-0003-3809-2601 jbourque@usgs.gov","orcid":"https://orcid.org/0000-0003-3809-2601","contributorId":5452,"corporation":false,"usgs":true,"family":"Bourque","given":"Jill","email":"jbourque@usgs.gov","middleInitial":"R.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":751381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Durkin, Alanna","contributorId":210654,"corporation":false,"usgs":false,"family":"Durkin","given":"Alanna","email":"","affiliations":[{"id":12547,"text":"Temple University","active":true,"usgs":false}],"preferred":false,"id":751382,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cordes, Erik E.","contributorId":37623,"corporation":false,"usgs":false,"family":"Cordes","given":"Erik","email":"","middleInitial":"E.","affiliations":[{"id":16710,"text":"Temple University, Department of Biology","active":true,"usgs":false}],"preferred":false,"id":751383,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70204947,"text":"70204947 - 2018 - Integrated observations and informatics improve understanding of changing marine ecosystems","interactions":[],"lastModifiedDate":"2019-08-26T10:55:19","indexId":"70204947","displayToPublicDate":"2018-11-16T10:45:09","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3912,"text":"Frontiers in Marine Science","onlineIssn":"2296-7745","active":true,"publicationSubtype":{"id":10}},"title":"Integrated observations and informatics improve understanding of changing marine ecosystems","docAbstract":"<p><span>Marine ecosystems have numerous benefits for human societies around the world and many policy initiatives now seek to maintain the health of these ecosystems. To enable wise decisions, up to date and accurate information on marine species and the state of the environment they live in is required. Moreover, this information needs to be openly accessible to build indicators and conduct timely assessments that decision makers can use. The questions and problems being addressed demand global-scale investigations, transdisciplinary science, and mechanisms to integrate and distribute data that otherwise would appear to be disparate. Essential Ocean Variables (EOVs) and marine Essential Biodiversity Variables (EBVs), conceptualized by the Global Ocean Observing System (GOOS) and the Marine Biodiversity Observation Network (MBON), respectively, guide observation of the ocean. Additionally, significant progress has been made to coordinate efforts between existing programs, such as the GOOS, MBON, and Ocean Biogeographic Information System collaboration agreement. Globally and nationally relevant indicators and assessments require increased sharing of data and analytical methods, sustained long-term and large-scale observations, and resources to dedicated to these tasks. We propose a vision and key tenets as a guiding framework for building a global integrated system for understanding marine biological diversity and processes to address policy and resource management needs. This framework includes: using EOVs and EBVs and implementing the guiding principles of Findable, Accessible, Interoperable, Reusable (FAIR) data and action ecology. In doing so, we can encourage relevant, rapid, and integrative scientific advancement that can be implemented by decision makers to maintain marine ecosystem health.</span></p>","language":"English","publisher":"Frontiers Media","doi":"10.3389/fmars.2018.00428","usgsCitation":"Benson, A.L., Brooks, C.M., Canonico, G., Duffy, J.E., Muller-Karger, F., Sosik, H.M., Miloslavich, P., and Klein, E., 2018, Integrated observations and informatics improve understanding of changing marine ecosystems: Frontiers in Marine Science, v. 5, 428, 8 p., https://doi.org/10.3389/fmars.2018.00428.","productDescription":"428, 8 p.","ipdsId":"IP-100471","costCenters":[{"id":208,"text":"Core Science Analytics and Synthesis","active":true,"usgs":true}],"links":[{"id":468245,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3389/fmars.2018.00428","text":"Publisher Index Page"},{"id":366906,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","noUsgsAuthors":false,"publicationDate":"2018-11-16","publicationStatus":"PW","contributors":{"authors":[{"text":"Benson, Abigail L. 0000-0002-4391-107X albenson@usgs.gov","orcid":"https://orcid.org/0000-0002-4391-107X","contributorId":4562,"corporation":false,"usgs":true,"family":"Benson","given":"Abigail","email":"albenson@usgs.gov","middleInitial":"L.","affiliations":[{"id":208,"text":"Core Science Analytics and Synthesis","active":true,"usgs":true}],"preferred":true,"id":769213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooks, Cassandra M.","contributorId":218423,"corporation":false,"usgs":false,"family":"Brooks","given":"Cassandra","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":769214,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Canonico, Gabrielle","contributorId":217563,"corporation":false,"usgs":false,"family":"Canonico","given":"Gabrielle","email":"","affiliations":[{"id":39659,"text":"National Oceanographic and Atmospheric Administration, US Integrated Ocean Observing System, Silver Spring, MD, USA","active":true,"usgs":false}],"preferred":false,"id":769215,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Duffy, J. Emmett","contributorId":78186,"corporation":false,"usgs":true,"family":"Duffy","given":"J.","email":"","middleInitial":"Emmett","affiliations":[],"preferred":false,"id":769216,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Muller-Karger, Frank","contributorId":218424,"corporation":false,"usgs":false,"family":"Muller-Karger","given":"Frank","affiliations":[],"preferred":false,"id":769217,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sosik, Heidi M.","contributorId":218425,"corporation":false,"usgs":false,"family":"Sosik","given":"Heidi","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":769218,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Miloslavich, Patricia","contributorId":206627,"corporation":false,"usgs":false,"family":"Miloslavich","given":"Patricia","email":"","affiliations":[{"id":37357,"text":"University of Tasmania, Hobart, Tasmania, Australia","active":true,"usgs":false}],"preferred":false,"id":769219,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Klein, Eduardo","contributorId":206675,"corporation":false,"usgs":false,"family":"Klein","given":"Eduardo","email":"","affiliations":[],"preferred":false,"id":769220,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70216314,"text":"70216314 - 2018 - Degradation of 100‐m‐scale rocky ejecta craters at the InSight Landing Site on Mars and implications for surface processes and erosion rates in the hesperian and amazonian","interactions":[],"lastModifiedDate":"2020-11-11T15:38:23.698218","indexId":"70216314","displayToPublicDate":"2018-11-16T09:36:39","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7353,"text":"Journal of Geophysical Research - Planets","active":true,"publicationSubtype":{"id":10}},"title":"Degradation of 100‐m‐scale rocky ejecta craters at the InSight Landing Site on Mars and implications for surface processes and erosion rates in the hesperian and amazonian","docAbstract":"<div class=\"article-section__content en main\"><p>Rocky ejecta craters (RECs) at the Interior Exploration using Seismic Investigations, Geodesy and Heat Transport (InSight) landing site on Elysium Planitia, Mars, provide constraints on crater modification and rates for the Hesperian and Amazonian. The RECs are between 10&nbsp;m and 1.2&nbsp;km in diameter and exhibit five classes of preservation. Class 1 represents pristine craters with sharp rims and abundant ejected rocks. From Classes 2 to 5, rims become more subdued, craters are infilled, and the ejecta become discontinuously distributed. High‐Resolution Imaging Science Experiment digital elevation models indicate a maximum depth to diameter ratio of ~0.15, which is lower than pristine models for craters of similar size. The low ratio is related to the presence of a loosely consolidated regolith and early‐stage eolian infill. Rim heights have an average height to diameter ratio of ~0.03 for the most pristine class. The size‐frequency distribution of RECs, plotted using cumulative and differential methods, indicates that crater classes within the diameter range of 200&nbsp;m to 1.2&nbsp;km are separated by ~100 to 200&nbsp;Myr. Smaller craters degrade faster, with classes separated by &lt;100&nbsp;Myr. Rim erosion can be entirely modeled by nonlinear diffusional processes using the calculated timescales and a constant diffusivity of 8&nbsp;×&nbsp;10<sup>−7</sup>&nbsp;m<sup>2</sup>/year for craters 200 to 500&nbsp;m in diameter. Diffusion models only partly capture depth‐related degradation, which requires eolian infill. Depth degradation and rim erosion rates are 10<sup>−2</sup><span>&nbsp;</span>to 10<sup>−3</sup>&nbsp;m/Myr, respectively. The rates are consistent with relatively slow modification that is typical of the last two epochs of Martian history.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2018JE005618","usgsCitation":"Sweeney, J., Warner, N.H., Ganti, V., Golombek, M.P., Lamb, M.P., Fergason, R.L., and Kirk, R.L., 2018, Degradation of 100‐m‐scale rocky ejecta craters at the InSight Landing Site on Mars and implications for surface processes and erosion rates in the hesperian and amazonian: Journal of Geophysical Research - Planets, v. 123, no. 10, p. 2732-2759, https://doi.org/10.1029/2018JE005618.","productDescription":"28 p.","startPage":"2732","endPage":"2759","ipdsId":"IP-097429","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":468246,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1029/2018je005618","text":"External Repository"},{"id":380417,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"123","issue":"10","noUsgsAuthors":false,"publicationDate":"2018-10-23","publicationStatus":"PW","contributors":{"authors":[{"text":"Sweeney, J.","contributorId":196344,"corporation":false,"usgs":false,"family":"Sweeney","given":"J.","email":"","affiliations":[],"preferred":false,"id":804642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warner, N. H","contributorId":244804,"corporation":false,"usgs":false,"family":"Warner","given":"N.","email":"","middleInitial":"H","affiliations":[{"id":48982,"text":"Department of Geological Sciences, State University of New York at Geneseo","active":true,"usgs":false}],"preferred":false,"id":804643,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ganti, V.","contributorId":167364,"corporation":false,"usgs":false,"family":"Ganti","given":"V.","email":"","affiliations":[{"id":13711,"text":"Caltech","active":true,"usgs":false}],"preferred":false,"id":804644,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Golombek, Matthew P.","contributorId":175450,"corporation":false,"usgs":false,"family":"Golombek","given":"Matthew","email":"","middleInitial":"P.","affiliations":[{"id":7023,"text":"Jet Propulsion Laboratory, California Institute of Technology","active":true,"usgs":false}],"preferred":false,"id":804645,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lamb, M. P.","contributorId":172652,"corporation":false,"usgs":false,"family":"Lamb","given":"M.","email":"","middleInitial":"P.","affiliations":[{"id":13711,"text":"Caltech","active":true,"usgs":false}],"preferred":false,"id":804646,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fergason, Robin L. 0000-0002-2044-1714","orcid":"https://orcid.org/0000-0002-2044-1714","contributorId":206167,"corporation":false,"usgs":true,"family":"Fergason","given":"Robin","email":"","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":804648,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kirk, Randolph L. 0000-0003-0842-9226 rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":804647,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70212526,"text":"70212526 - 2018 - Inhibition of grain boundary sliding creep in fine-grained ice by inter-granular particles: Implications for planetary ice masses","interactions":[],"lastModifiedDate":"2020-08-19T14:04:04.15164","indexId":"70212526","displayToPublicDate":"2018-11-16T09:00:20","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Inhibition of grain boundary sliding creep in fine-grained ice by inter-granular particles: Implications for planetary ice masses","docAbstract":"<div class=\"article-section__content en main\"><p>Ice in both terrestrial and planetary settings often contains rock particles. Here we present an experimental investigation of the influence of intergranular particles on the rheological behavior of ice. Experiments were performed on samples fabricated from 10‐μm ice powders +1‐μm graphite or 0.8‐μm alumina particles and subjected to elevated confining pressures. A critical particle fraction, ∼6%, was observed, below which samples behave like pure ice and deform by both grain boundary sliding (GBS) and dislocation creep, and above which GBS creep is impeded. Above this critical fraction, ice grains occur in particle‐free clusters surrounded by bands of particles mixed with fine‐grained ice, resulting in the impedance of GBS in the bands as well as sliding between the ice clusters. Our results imply that South Polar Layered Deposits and midlatitude lobate debris aprons on Mars must contain &gt;94% ice and that the shallow subsurface of Ceres could contain &gt;90% ice.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2018GL080228","usgsCitation":"Qi, C., Stern, L.A., Pathare, A., Durham, W.B., and Goldsby, D.L., 2018, Inhibition of grain boundary sliding creep in fine-grained ice by inter-granular particles: Implications for planetary ice masses: Geophysical Research Letters, v. 45, no. 23, p. 12757-12765, https://doi.org/10.1029/2018GL080228.","productDescription":"9 p.","startPage":"12757","endPage":"12765","ipdsId":"IP-098726","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":499885,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doaj.org/article/5ff1247bc62a42ba985589f6597880f6","text":"External Repository"},{"id":377646,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"23","noUsgsAuthors":false,"publicationDate":"2018-12-03","publicationStatus":"PW","contributors":{"authors":[{"text":"Qi, Chao","contributorId":238837,"corporation":false,"usgs":false,"family":"Qi","given":"Chao","email":"","affiliations":[{"id":16979,"text":"University of Pennsylvania","active":true,"usgs":false}],"preferred":false,"id":796695,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stern, Laura A. 0000-0003-3440-5674","orcid":"https://orcid.org/0000-0003-3440-5674","contributorId":212238,"corporation":false,"usgs":true,"family":"Stern","given":"Laura","email":"","middleInitial":"A.","affiliations":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":796696,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pathare, Asmin","contributorId":238838,"corporation":false,"usgs":false,"family":"Pathare","given":"Asmin","affiliations":[{"id":12445,"text":"Lunar and Planetary Institute","active":true,"usgs":false}],"preferred":false,"id":796697,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Durham, William B.","contributorId":238839,"corporation":false,"usgs":false,"family":"Durham","given":"William","email":"","middleInitial":"B.","affiliations":[{"id":47799,"text":"MIT","active":true,"usgs":false}],"preferred":false,"id":796698,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Goldsby, David L.","contributorId":194803,"corporation":false,"usgs":false,"family":"Goldsby","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":796699,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70254571,"text":"70254571 - 2018 - Calibration of regional hydraulic and transport properties of an arid-region aquifer under modern and paleorecharge conditions using water levels and environmental tracers","interactions":[],"lastModifiedDate":"2024-06-03T11:44:55.821178","indexId":"70254571","displayToPublicDate":"2018-11-16T06:41:59","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1923,"text":"Hydrogeology Journal","active":true,"publicationSubtype":{"id":10}},"title":"Calibration of regional hydraulic and transport properties of an arid-region aquifer under modern and paleorecharge conditions using water levels and environmental tracers","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>A two-dimensional numerical groundwater flow model was established and calibrated for the hyperarid Najd region in southern Oman. The results indicate that recent recharge rates are required to sustain the observed groundwater heads in the Najd. The model was also used to estimate possible ranges of past recharge rates and the effective porosity of the main aquifer unit. Recharge rates during past humid periods were estimated to be no more than 1–3 times modern rates. The effective porosity was estimated to be between 0.06 and 0.093. Insight into the nature of the long-term transport within the aquifer was gained by using transient model runs over the last 350&nbsp;ka and (1) varying the recharge intensity (from 0.1 to 2.5 times modern), and (2) the timing and duration of humid and dry periods. Finally, results indicate that although recharge rates and the flow conditions have likely changed over time, a steady-state model is capable of reproducing the observed groundwater residence times in the Najd based on carbon-14, helium and chlorine-36 dating.</p></div></div><div id=\"Abs2-section\" class=\"c-article-section\"><br></div>","language":"English","publisher":"Springer","doi":"10.1007/s10040-018-1894-z","usgsCitation":"Muller, T., and Sanford, W.E., 2018, Calibration of regional hydraulic and transport properties of an arid-region aquifer under modern and paleorecharge conditions using water levels and environmental tracers: Hydrogeology Journal, v. 27, no. 2, p. 685-701, https://doi.org/10.1007/s10040-018-1894-z.","productDescription":"17 p.","startPage":"685","endPage":"701","ipdsId":"IP-099686","costCenters":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"links":[{"id":429442,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Oman","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[58.86114,21.11403],[58.48799,20.42899],[58.03432,20.48144],[57.82637,20.243],[57.66576,19.736],[57.7887,19.06757],[57.69439,18.94471],[57.23426,18.94799],[56.60965,18.57427],[56.51219,18.08711],[56.28352,17.87607],[55.66149,17.88413],[55.26994,17.63231],[55.2749,17.22835],[54.791,16.9507],[54.23925,17.04498],[53.57051,16.70766],[53.10857,16.65105],[52.78218,17.34974],[52.00001,19],[54.99998,19.99999],[55.66666,22],[55.20834,22.70833],[55.23449,23.11099],[55.52584,23.52487],[55.52863,23.9336],[55.98121,24.13054],[55.80412,24.2696],[55.88623,24.92083],[56.39685,24.92473],[56.84514,24.24167],[57.40345,23.87859],[58.13695,23.74793],[58.72921,23.56567],[59.1805,22.9924],[59.4501,22.66027],[59.80806,22.53361],[59.80615,22.31052],[59.44219,21.71454],[59.28241,21.43389],[58.86114,21.11403]]],[[[56.39142,25.89599],[56.26104,25.71461],[56.07082,26.05546],[56.36202,26.39593],[56.48568,26.30912],[56.39142,25.89599]]]]},\"properties\":{\"name\":\"Oman\"}}]}","volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2018-11-16","publicationStatus":"PW","contributors":{"authors":[{"text":"Muller, Thomas","contributorId":337080,"corporation":false,"usgs":false,"family":"Muller","given":"Thomas","email":"","affiliations":[{"id":80964,"text":"Department of Hydrogeology, Helmhoz-Centre for Environmental Research","active":true,"usgs":false}],"preferred":false,"id":901928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanford, Ward E. 0000-0002-6624-0280 wsanford@usgs.gov","orcid":"https://orcid.org/0000-0002-6624-0280","contributorId":2268,"corporation":false,"usgs":true,"family":"Sanford","given":"Ward","email":"wsanford@usgs.gov","middleInitial":"E.","affiliations":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":901929,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70202341,"text":"70202341 - 2018 - Do we know how much fluvial sediment reaches the sea? Decreased river monitoring of U.S. coastal rivers","interactions":[],"lastModifiedDate":"2019-02-22T16:53:40","indexId":"70202341","displayToPublicDate":"2018-11-15T16:53:35","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"Do we know how much fluvial sediment reaches the sea? Decreased river monitoring of U.S. coastal rivers","docAbstract":"Given the present and future changing climate and human changes to land use and river control, river sediment fluxes to coastal systems are changing and will continue to change in the future.  To delineate these changes and their effects, it is increasingly important to document the fluxes of river-borne sediment discharged to the sea.  Unfortunately, broad-scale river sediment monitoring programs established more than 50 years ago in the U.S. have diminished substantially and now focus principally on the largest rivers and estuaries.  Unless addressed, these data gaps will provide significant challenges in addressing fundamental scientific and management questions about the effects of climate change and sea-level rise in our estuaries and on our coasts.","language":"English","publisher":"Wiley","doi":"10.1002/hyp.13276","usgsCitation":"Warrick, J.A., and Milliman, J.D., 2018, Do we know how much fluvial sediment reaches the sea? Decreased river monitoring of U.S. coastal rivers: Hydrological Processes, v. 32, no. 23, p. 3561-3567, https://doi.org/10.1002/hyp.13276.","productDescription":"7 p.","startPage":"3561","endPage":"3567","ipdsId":"IP-092050","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":468247,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/hyp.13276","text":"Publisher Index Page"},{"id":361482,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"23","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2018-10-11","publicationStatus":"PW","contributors":{"authors":[{"text":"Warrick, Jonathan A. 0000-0002-0205-3814 jwarrick@usgs.gov","orcid":"https://orcid.org/0000-0002-0205-3814","contributorId":167736,"corporation":false,"usgs":true,"family":"Warrick","given":"Jonathan","email":"jwarrick@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":757911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Milliman, John D.","contributorId":213518,"corporation":false,"usgs":false,"family":"Milliman","given":"John","email":"","middleInitial":"D.","affiliations":[{"id":38770,"text":"College of William and Mary, Virginia Institute of Marine Science","active":true,"usgs":false}],"preferred":false,"id":757912,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70202368,"text":"70202368 - 2018 - Effect of heat and singeing on stable hydrogen isotope ratios of bird feathers and implications for their use in determining geographic origin","interactions":[],"lastModifiedDate":"2019-02-26T14:44:31","indexId":"70202368","displayToPublicDate":"2018-11-15T14:44:24","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3233,"text":"Rapid Communications in Mass Spectrometry","active":true,"publicationSubtype":{"id":10}},"title":"Effect of heat and singeing on stable hydrogen isotope ratios of bird feathers and implications for their use in determining geographic origin","docAbstract":"<div id=\"rcm8253-sec-0001\" class=\"article-section__content\"><p class=\"article-section__sub-title section1\"><strong>Rationale</strong></p><p>Stable hydrogen isotope (<i>δ</i><sup>2</sup>H) ratios of animal tissues are useful for assessing movement and geographic origin of mobile organisms. However, it is uncertain whether heat and singeing affects feather<span>&nbsp;</span><i>δ</i><sup>2</sup>H values and thus subsequent geographic assignments. This is relevant for birds of conservation interest that are burned and killed at concentrating solar‐energy facilities that reflect sunlight to a receiving tower and generate a solar flux field.</p></div><div id=\"rcm8253-sec-0002\" class=\"article-section__content\"><p class=\"article-section__sub-title section1\"><strong>Methods</strong></p><p>We used a controlled experiment to test the effect of known heat loads (exposure to 200, 250 or 300°C for 1 min) on the morphology and<span>&nbsp;</span><i>δ</i><sup>2</sup>H values of feathers from two songbird species. Subsequently, we examined the effects of singeing on<span>&nbsp;</span><i>δ</i><sup>2</sup>H values of feathers from three other songbird species that were found dead in the field at a concentrating solar‐energy facility.</p></div><div id=\"rcm8253-sec-0003\" class=\"article-section__content\"><p class=\"article-section__sub-title section1\"><strong>Results</strong></p><p>Relative to control samples, heating caused visual morphological changes to feathers, including shriveling at 250°C and charring at 300°C. The<span>&nbsp;</span><i>δ</i><sup>2</sup>H values significantly declined by a mean of 27.8‰ in experimental samples exposed to 300°C. There was no statistically detectable difference between<span>&nbsp;</span><i>δ</i><sup>2</sup>H values of the singed and unsinged portions of field‐collected feathers from the same bird.</p></div><div id=\"rcm8253-sec-0004\" class=\"article-section__content\"><p class=\"article-section__sub-title section1\"><strong>Conclusions</strong></p><p>Limited singeing that did not dramatically alter the feather morphology did not substantially affect<span>&nbsp;</span><i>δ</i><sup>2</sup>H values of feathers from these songbirds. However, higher temperatures induced charring and reduced<span>&nbsp;</span><i>δ</i><sup>2</sup>H values. Therefore, severely charred feathers should be avoided when selecting feathers for<span>&nbsp;</span><i>δ</i><sup>2</sup>H‐based assessment of geographic origin.</p></div>","language":"English","publisher":"Wiley","doi":"10.1002/rcm.8253","usgsCitation":"Vander Zanden, H.B., Reid, A., Katzner, T., and Nelson, D.M., 2018, Effect of heat and singeing on stable hydrogen isotope ratios of bird feathers and implications for their use in determining geographic origin: Rapid Communications in Mass Spectrometry, v. 32, no. 21, p. 1859-1866, https://doi.org/10.1002/rcm.8253.","productDescription":"8 p.","startPage":"1859","endPage":"1866","ipdsId":"IP-097643","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":361557,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"21","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2018-09-25","publicationStatus":"PW","contributors":{"authors":[{"text":"Vander Zanden, Hannah B.","contributorId":138885,"corporation":false,"usgs":false,"family":"Vander Zanden","given":"Hannah","email":"","middleInitial":"B.","affiliations":[{"id":12562,"text":"Department of Geology and Geophysics, University of Utah; Archie Carr Center for Sea Turtle Research, University of Florida","active":true,"usgs":false}],"preferred":false,"id":758044,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reid, Abigail","contributorId":213574,"corporation":false,"usgs":false,"family":"Reid","given":"Abigail","email":"","affiliations":[{"id":38801,"text":"Pawling High School","active":true,"usgs":false}],"preferred":false,"id":758045,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Katzner, Todd E. 0000-0003-4503-8435 tkatzner@usgs.gov","orcid":"https://orcid.org/0000-0003-4503-8435","contributorId":191353,"corporation":false,"usgs":true,"family":"Katzner","given":"Todd E.","email":"tkatzner@usgs.gov","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":758043,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nelson, David M.","contributorId":175098,"corporation":false,"usgs":false,"family":"Nelson","given":"David","email":"","middleInitial":"M.","affiliations":[{"id":13479,"text":"University of Maryland Center for Environmental Science, Appalachian Laboratory,  301 Braddock Road, Frostburg, Maryland","active":true,"usgs":false}],"preferred":false,"id":758046,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70200816,"text":"fs20183061 - 2018 - Unmanned aerial systems capabilities of the U.S. Geological Survey Woods Hole Coastal and Marine Science Center","interactions":[],"lastModifiedDate":"2018-11-20T11:18:54","indexId":"fs20183061","displayToPublicDate":"2018-11-15T14:30:00","publicationYear":"2018","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2018-3061","displayTitle":"Unmanned Aerial Systems Capabilities of the U.S. Geological Survey Woods Hole Coastal and Marine Science Center","title":"Unmanned aerial systems capabilities of the U.S. Geological Survey Woods Hole Coastal and Marine Science Center","docAbstract":"<p>Unmanned aerial system (UAS) technology provides a rapid and low-cost solution for mapping coastal environments and assessing short- and long-term changes. The interdisciplinary nature of the data collected and the breadth of applications make UAS technology applicable to multiple scientific investigations. The Aerial Imaging and Mapping (AIM) group at the U.S. Geological Survey (USGS) Woods Hole Coastal and Marine Science Center provides UAS services to scientists to advance the science mission of the Coastal-Marine Hazards and Resources Program. Scientists at the Woods Hole Coastal and Marine Science Center use UASs to acquire imagery of coastal and wetland environments, which is then used to produce detailed topographic and visual reflectance datasets. UAS technology supports the work of geologists, engineers, physical scientists, geographers, and geochemists who study coastal erosion, sediment transport, storm impacts, habitats, biomass, and marsh stability.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20183061","usgsCitation":"Brosnahan, S., and Sherwood, C., 2018, Unmanned aerial systems capabilities of the U.S. Geological Survey Woods Hole Coastal and Marine Science Center: U.S. Geological Survey Fact Sheet 2018–3061, 2 p., https://doi.org/10.3133/fs20183061.","productDescription":"2 p.","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-098218","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":359425,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2018/3061/fs20183061.pdf","text":"Report","size":"926 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 2018-3061"},{"id":359424,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2018/3061/coverthb.jpg"}],"contact":"<p><a href=\"https://www.usgs.gov/centers/whcmsc\" data-mce-href=\"https://www.usgs.gov/centers/whcmsc\">Woods Hole Coastal and Marine Science Center</a><br><a href=\"https://www.usgs.gov/centers/whcmsc/science/aerial-imaging-and-mapping\" data-mce-href=\"https://www.usgs.gov/centers/whcmsc/science/aerial-imaging-and-mapping\">Aerial Imaging and Mapping</a> Group<br>U.S. Geological Survey<br>384 Woods Hole Road<br>Quissett Campus<br>Woods Hole, MA 02543</p>","tableOfContents":"<ul><li>Science Applications</li><li>UAS Capabilities</li></ul>","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"publishedDate":"2018-11-19","noUsgsAuthors":false,"publicationDate":"2018-11-19","publicationStatus":"PW","scienceBaseUri":"5bf3d9f0e4b045bfcae0c9b1","contributors":{"authors":[{"text":"Brosnahan, Sandra 0000-0003-3797-4207 sbrosnahan@usgs.gov","orcid":"https://orcid.org/0000-0003-3797-4207","contributorId":192274,"corporation":false,"usgs":true,"family":"Brosnahan","given":"Sandra","email":"sbrosnahan@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":750756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sherwood, Christopher R. 0000-0001-6135-3553 csherwood@usgs.gov","orcid":"https://orcid.org/0000-0001-6135-3553","contributorId":2866,"corporation":false,"usgs":true,"family":"Sherwood","given":"Christopher","email":"csherwood@usgs.gov","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":750757,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70200528,"text":"sir20185148 - 2018 - Flood frequency of rural streams in Mississippi, 2013","interactions":[{"subject":{"id":28223,"text":"wri914037 - 1991 - Flood characteristics of Mississippi streams","indexId":"wri914037","publicationYear":"1991","noYear":false,"title":"Flood characteristics of Mississippi streams"},"predicate":"SUPERSEDED_BY","object":{"id":70200528,"text":"sir20185148 - 2018 - Flood frequency of rural streams in Mississippi, 2013","indexId":"sir20185148","publicationYear":"2018","noYear":false,"title":"Flood frequency of rural streams in Mississippi, 2013"},"id":1}],"lastModifiedDate":"2018-11-26T09:50:24","indexId":"sir20185148","displayToPublicDate":"2018-11-15T13:33:02","publicationYear":"2018","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2018-5148","displayTitle":"Flood Frequency of Rural Streams in Mississippi, 2013","title":"Flood frequency of rural streams in Mississippi, 2013","docAbstract":"<p>To improve flood-frequency estimates at rural streams in Mississippi, annual exceedance probability flows at gaged streams and regional regression equations used to estimate annual exceedance probability flows for ungaged streams were developed by using current geospatial data, new analytical methods, and annual peak-flow data through the 2013 water year. The regional regression equations were derived from statistical analyses of peak-flow data and basin characteristics for 281 streamgages and incorporated a newly developed study-specific skew coefficient at streamgages located in five subregional watersheds (Middle Tennessee-Elk, Mobile-Tombigbee, Lower Mississippi-Big Black, Pearl, and Pascagoula) in Mississippi. Three flood regions—A, B, and C—were identified based on residuals from the regional regression analyses and contain sites with similar basin characteristics. Analysis was not conducted for the fourth flood region, the Mississippi Alluvial Plain, because of insufficient long-term streamflow data and poorly defined basin characteristics.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20185148","collaboration":"Prepared in cooperation with the Mississippi Department of Transportation","usgsCitation":"Anderson, B.T., 2018, Flood frequency of rural streams in Mississippi, 2013: U.S. Geological Survey Scientific Investigations Report 2018–5148, 12 p., https://doi.org/10.3133/sir20185148. [Supersedes USGS Water-Resources Investigations Report 91–4037.]","productDescription":"Report: vii, 12 p.; Data Release","numberOfPages":"24","onlineOnly":"N","ipdsId":"IP-079995","costCenters":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"links":[{"id":359439,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/F7ZP45B8","text":"USGS data release","description":"USGS Data Release","linkHelpText":"Regions and Tables for Mississippi Flood Frequency, Data through 2013"},{"id":359438,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2018/5148/sir20185148.pdf","text":"Report","size":"1.96 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2018–5148"},{"id":359437,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2018/5148/coverthb.jpg"}],"country":"United 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 \"}}]}","contact":"<p><a data-mce-href=\"mailto:%20dc_tn@usgs.gov\" href=\"mailto:%20dc_tn@usgs.gov\">Director</a>, <a data-mce-href=\"https://www.usgs.gov/centers/lmg-water\" href=\"https://www.usgs.gov/centers/lmg-water\">Lower Mississippi-Gulf Water Science Center</a><br>U.S. Geological Survey<br>640 Grassmere Park, Suite 100<br>Nashville, Tennessee 37211 </p>","tableOfContents":"<ul><li>Acknowledgments</li><li>Abstract</li><li>Introduction</li><li>Data Compilation</li><li>Application of Methods</li><li>Summary and Conclusions</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"publishedDate":"2018-11-15","noUsgsAuthors":false,"publicationDate":"2018-11-15","publicationStatus":"PW","scienceBaseUri":"5bee93e3e4b08f163c24a1b5","contributors":{"authors":[{"text":"Anderson, Brandon T. 0000-0001-6698-0791","orcid":"https://orcid.org/0000-0001-6698-0791","contributorId":209976,"corporation":false,"usgs":true,"family":"Anderson","given":"Brandon","email":"","middleInitial":"T.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"preferred":true,"id":749375,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70199131,"text":"70199131 - 2018 - Filtering of periodic infiltration in a layered vadose zone: 2. Applications and a freeware screening tool","interactions":[],"lastModifiedDate":"2018-11-20T12:05:24","indexId":"70199131","displayToPublicDate":"2018-11-15T12:05:18","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3674,"text":"Vadose Zone Journal","active":true,"publicationSubtype":{"id":10}},"title":"Filtering of periodic infiltration in a layered vadose zone: 2. Applications and a freeware screening tool","docAbstract":"<p><span>We have developed a screening tool to visualize and conceptualize the filtering properties of a layered vadose zone. Climate projections indicate that rainfall timing and magnitude may change and impact groundwater resources. This increases the importance of understanding how the vadose zone filters infiltration variability and ultimately affects recharge and groundwater resources. An approximate solution for the filtering of surface forcings through soil layers was developed previously, and the soil and conditions where its approximations are appropriate was evaluated. Here we present a screening tool based on the solution for estimating how periodic infiltration forcings filter in a layered vadose zone for different soil properties and surface flux conditions. The solutions identify time-varying elements of surface forcings that persist to the depth of the water table, leading to transient recharge. We investigated the filtering properties of the vadose zone in Central Valley, California, and identified areas where surface forcings are essentially damped and recharge can be approximated as steady. We also determined the travel time for infiltration pulses to reach the depth of the water table.</span></p>","language":"English","publisher":"ACSESS","doi":"10.2136/vzj2018.03.0048","usgsCitation":"Dickinson, J.E., and Ferre, T.P., 2018, Filtering of periodic infiltration in a layered vadose zone: 2. Applications and a freeware screening tool: Vadose Zone Journal, v. 17, no. 1, p. 1-12, https://doi.org/10.2136/vzj2018.03.0048.","productDescription":"Article 180048; 12 p.","startPage":"1","endPage":"12","ipdsId":"IP-096156","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":468248,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2136/vzj2018.03.0048","text":"Publisher Index Page"},{"id":437684,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9BHD74M","text":"USGS data release","linkHelpText":"Code for computing the responses to cyclical infiltration in a layered vadose zone in Central Valley, California"},{"id":359606,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2018-11-15","publicationStatus":"PW","scienceBaseUri":"5bf52b68e4b045bfcae28006","contributors":{"authors":[{"text":"Dickinson, Jesse E. 0000-0002-0048-0839 jdickins@usgs.gov","orcid":"https://orcid.org/0000-0002-0048-0839","contributorId":152545,"corporation":false,"usgs":true,"family":"Dickinson","given":"Jesse","email":"jdickins@usgs.gov","middleInitial":"E.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":744269,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ferre, T. P. A","contributorId":206539,"corporation":false,"usgs":false,"family":"Ferre","given":"T.","email":"","middleInitial":"P. A","affiliations":[{"id":7042,"text":"University of Arizona","active":true,"usgs":false}],"preferred":false,"id":744270,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70199133,"text":"70199133 - 2018 - Filtering of cyclic period infiltration in a layered vadose zone: 1. Approximation of damping and time lags","interactions":[],"lastModifiedDate":"2021-02-01T17:54:29.16291","indexId":"70199133","displayToPublicDate":"2018-11-15T11:53:24","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3674,"text":"Vadose Zone Journal","active":true,"publicationSubtype":{"id":10}},"title":"Filtering of cyclic period infiltration in a layered vadose zone: 1. Approximation of damping and time lags","docAbstract":"<h3 id=\"vzj2vzj2018030047-sec-0001-title\" class=\"article-section__sub-title section1\">Core Ideas</h3><div class=\"paragraph-element\"><ul class=\"unordered-list\"><li>We describe an approximation for filtering of periodic infiltration in layered soil.</li><li>Transitions in soil‐water properties between soil layers affect the filtering.</li><li>Errors are smaller in soils where changes in soil‐water properties are small.</li></ul></div><p>Infiltration and downward percolation of water in the vadose zone are important processes that can define the availability of water resources. We present an approach that provides insight into how periodic infiltration forcings at the land surface filter in a layered vadose zone in terms of changes in the timing and magnitude of hydrologic responses. To represent geologically realistic systems, we used vertical sequences of one‐dimensional periodic solutions, where each solution represents a single soil in a layered profile. The overall approach is based on a linearized Richards equation and assumes that the effects on flow of continuous pressure head changes at soil interfaces are negligible. We evaluated the limit of these approximations by comparison with results from the numerical model HYDRUS‐1D, which uses the full Richards equation. We compared (i) the depth at which flux variations became steady, and (ii) the travel time of wetting fronts to reach a depth of 3 m. The solution was reasonably accurate (error less than a factor of 2) for infiltration cycles with periods from 30 to 365 d and for fluxes common in arid and semiarid environments (0–2 mm d<sup>−1</sup>). Lag times between a surface forcing and response at any depth were accurate (error less than a factor of 1.1). The approximation generally provided consistent estimates of the damping and time lag, such that it overestimated the depths where fluxes were steady and underestimated the time for a forcing to reach a specific depth.</p>","language":"English","publisher":"ACSESS","doi":"10.2136/vzj2018.03.0047","usgsCitation":"Dickinson, J.E., and Ferre, T.P., 2018, Filtering of cyclic period infiltration in a layered vadose zone: 1. Approximation of damping and time lags: Vadose Zone Journal, v. 17, no. 1, p. 1-16, https://doi.org/10.2136/vzj2018.03.0047.","productDescription":"16 p.","startPage":"1","endPage":"16","ipdsId":"IP-077789","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":468249,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2136/vzj2018.03.0047","text":"Publisher Index Page"},{"id":382854,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2018-11-15","publicationStatus":"PW","contributors":{"authors":[{"text":"Dickinson, Jesse E. 0000-0002-0048-0839 jdickins@usgs.gov","orcid":"https://orcid.org/0000-0002-0048-0839","contributorId":152545,"corporation":false,"usgs":true,"family":"Dickinson","given":"Jesse","email":"jdickins@usgs.gov","middleInitial":"E.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":744271,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ferre, T. P. A","contributorId":206539,"corporation":false,"usgs":false,"family":"Ferre","given":"T.","email":"","middleInitial":"P. A","affiliations":[{"id":7042,"text":"University of Arizona","active":true,"usgs":false}],"preferred":false,"id":744272,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211496,"text":"70211496 - 2018 - New England and northern New York forest ecosystem vulnerability assessment and synthesis: A report from the New England Climate Change Response Framework project","interactions":[],"lastModifiedDate":"2020-08-04T21:01:51.925161","indexId":"70211496","displayToPublicDate":"2018-11-15T10:42:41","publicationYear":"2018","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":32,"text":"General Technical Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"NRS-173","title":"New England and northern New York forest ecosystem vulnerability assessment and synthesis: A report from the New England Climate Change Response Framework project","docAbstract":"<p><span>Forest ecosystems will face direct and indirect impacts from a changing climate over the 21st century. This assessment evaluates the vulnerability of forest ecosystems across the New England region (Connecticut, Maine, Massachusetts, New Hampshire, northern New York, Rhode Island, and Vermont) under a range of future climates. We synthesized and summarized information on the contemporary landscape, provided information on past climate trends, and described a range of projected future climates. This information was used to parameterize and run multiple vegetation impact models, which provided a range of potential vegetative responses to climate. Finally, we brought these results before a multidisciplinary panel of scientists and natural resource professionals familiar with the forests of this region to assess ecosystem vulnerability through a formal consensus-based expert elicitation process. Observed trends in climate over the historical record from 1901 through 2011 show that the mean annual temperature has increased across the region by 2.4 °F, with even greater warming during winter. Precipitation patterns also changed during this time, with a slight trend toward greater annual precipitation and a substantial increase in extreme precipitation events. Projected climate trends using downscaled global climate model data indicate a potential increase in mean annual temperature of 3 to 8 °F for the assessment area by 2100. Projections for precipitation indicate an increase in fall and winter precipitation, and spring and summer precipitation projections vary by scenario. We identified potential impacts on forests by incorporating these future climate projections into three forest impact models (DISTRIB, LINKAGES, and LANDIS PRO). Model projections suggest that many northern and boreal species, including balsam fir, red spruce, and black spruce, may fare worse under future conditions, but other species may benefit from projected changes in climate. Published literature on climate impacts related to wildfire, invasive species, and forest pests and diseases also contributed to the overall determination of climate change vulnerability. We assessed vulnerability for eight forest communities in the assessment area. The assessment was conducted through a formal elicitation process with 20 scientists and resource managers from across the area, who considered vulnerability in terms of the potential impacts and the adaptive capacity for an individual community. Montane spruce-fir, low-elevation spruce-fir, and lowland mixed conifer forests were determined to be the most vulnerable communities. Central hardwoods, transition hardwoods, and pitch pine-scrub oak forests were perceived as having lower vulnerability to projected changes in climate. These projected changes in climate and the associated impacts and vulnerabilities will have important implications for economically valuable timber species, forest-dependent animals and plants, recreation, and long-term natural resource planning.</span></p>","language":"English","publisher":"Northern Research Station","doi":"10.2737/NRS-GTR-173","usgsCitation":"Janowiak, M., D’Amato, A., Swanston, C., Iverson, L.R., Thompson, F., Dijak, W.D., Matthews, S., Peters, M.P., Prasad, A., Fraser, J.S., Brandt, L.A., Butler-Leopold, P.R., Handler, S.D., Shannon, P.D., Burbank, D., Campbell, J., Cogbill, C., Duveneck, M.J., Emery, M.R., Fisichelli, N., Foster, J., Hushaw, J., Kenefic, L., Mahaffey, A., Morelli, T.L., Reo, N., Schaberg, P.G., Simmons, K.R., Weiskittel, A., Wilmot, S., Hollinger, D., Lane, E., Rustad, L., and Templar, P.H., 2018, New England and northern New York forest ecosystem vulnerability assessment and synthesis: A report from the New England Climate Change Response 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,{"id":70201370,"text":"70201370 - 2018 - Shared habitat use by juveniles of three sea turtle species","interactions":[],"lastModifiedDate":"2018-12-12T09:53:13","indexId":"70201370","displayToPublicDate":"2018-11-15T09:53:04","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2663,"text":"Marine Ecology Progress Series","active":true,"publicationSubtype":{"id":10}},"title":"Shared habitat use by juveniles of three sea turtle species","docAbstract":"<p><span>The first step in understanding how sympatric species share habitat is defining spatial boundaries. While home range data for juvenile sea turtles exists, few studies have examined spatial overlap of multiple species in foraging habitat. Using satellite tracking technology, we define home ranges for juveniles of 3 sea turtle species (loggerhead, Kemp’s ridley, and green; n = 21) captured at 2 adjacent foraging sites in the northern Gulf of Mexico. In these areas, green turtles are known to be primarily herbivorous, whereas Kemp’s ridley turtles forage predominately on crabs, and loggerhead turtles on various hard-shelled benthic invertebrates. No differences in home range size or characteristics, such as water depth and distance to shore, were observed among species, although fine-scale foraging patches were not examined in this study. A high degree of overlap in habitat-use among all 3 species was documented in summer at both sites. Seasonal movements, triggered by colder winter temperatures, were documented and appeared to differ among species, with Kemp’s ridley and loggerhead turtles leaving bays, and green turtles overwintering inside bays. By identifying shared habitat-use by juvenile sea turtles, we have created a foundation for further fine-scale studies on resource partitioning that will aid in habitat management and conservation of these threatened and endangered species.</span></p>","language":"English","publisher":"Inter-Research","doi":"10.3354/meps12748","usgsCitation":"Lamont, M.M., and Iverson, A., 2018, Shared habitat use by juveniles of three sea turtle species: Marine Ecology Progress Series, v. 606, p. 187-200, https://doi.org/10.3354/meps12748.","productDescription":"14 p.","startPage":"187","endPage":"200","ipdsId":"IP-098002","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":360185,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"606","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c122c55e4b034bf6a8569df","contributors":{"authors":[{"text":"Lamont, Margaret M. 0000-0001-7520-6669 mlamont@usgs.gov","orcid":"https://orcid.org/0000-0001-7520-6669","contributorId":4525,"corporation":false,"usgs":true,"family":"Lamont","given":"Margaret","email":"mlamont@usgs.gov","middleInitial":"M.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":753832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Iverson, Autumn R. 0000-0002-8353-6745","orcid":"https://orcid.org/0000-0002-8353-6745","contributorId":173555,"corporation":false,"usgs":false,"family":"Iverson","given":"Autumn R.","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":753833,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70216309,"text":"70216309 - 2018 - Fire and tree death: Understanding and improving modeling of fire-induced tree mortality","interactions":[],"lastModifiedDate":"2020-11-11T14:42:14.27702","indexId":"70216309","displayToPublicDate":"2018-11-15T08:36:33","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1562,"text":"Environmental Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Fire and tree death: Understanding and improving modeling of fire-induced tree mortality","docAbstract":"<div class=\"article-text wd-jnl-art-abstract cf\"><p>Each year wildland fires kill and injure trees on millions of forested hectares globally, affecting plant and animal biodiversity, carbon storage, hydrologic processes, and ecosystem services. The underlying mechanisms of fire-caused tree mortality remain poorly understood, however, limiting the ability to accurately predict mortality and develop robust modeling applications, especially under novel future climates. Virtually all post-fire tree mortality prediction systems are based on the same underlying empirical model described in Ryan and Reinhardt (1988&nbsp;<i>Can. J. For. Res.</i>&nbsp;18&nbsp;1291–7), which was developed from a limited number of species, stretching model assumptions beyond intended limits. We review the current understanding of the mechanisms of fire-induced tree mortality, provide recommended standardized terminology, describe model applications and limitations, and conclude with key knowledge gaps and future directions for research. We suggest a two-pronged approach to future research: (1) continued improvements and evaluations of empirical models to quantify uncertainty and incorporate new regions and species and (2) acceleration of basic, physiological research on the proximate and ultimate causes of fire-induced tree mortality to incorporate processes of tree death into models. Advances in both empirical and process fire-induced tree modeling will allow creation of hybrid models that could advance understanding of how fire injures and kills trees, while improving prediction accuracy of fire-driven feedbacks on ecosystems and landscapes, particularly under novel future conditions.</p></div>","language":"English","publisher":"IOP Publishing","doi":"10.1088/1748-9326/aae934","usgsCitation":"Hood, S.M., Varner, J.M., van Mantgem, P., and Cansler, C.A., 2018, Fire and tree death: Understanding and improving modeling of fire-induced tree mortality: Environmental Research Letters, v. 13, no. 11, 113004, 17 p., https://doi.org/10.1088/1748-9326/aae934.","productDescription":"113004, 17 p.","ipdsId":"IP-091982","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":468250,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1088/1748-9326/aae934","text":"Publisher Index Page"},{"id":380408,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"11","noUsgsAuthors":false,"publicationDate":"2018-11-15","publicationStatus":"PW","contributors":{"authors":[{"text":"Hood, Sharon M.","contributorId":221183,"corporation":false,"usgs":false,"family":"Hood","given":"Sharon","email":"","middleInitial":"M.","affiliations":[{"id":37389,"text":"U.S. Forest Service","active":true,"usgs":false}],"preferred":false,"id":804622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Varner, J. Morgan 0000-0003-3781-5839","orcid":"https://orcid.org/0000-0003-3781-5839","contributorId":244802,"corporation":false,"usgs":false,"family":"Varner","given":"J.","email":"","middleInitial":"Morgan","affiliations":[{"id":36493,"text":"USDA Forest Service","active":true,"usgs":false}],"preferred":false,"id":804623,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"van Mantgem, Phillip J. 0000-0002-3068-9422","orcid":"https://orcid.org/0000-0002-3068-9422","contributorId":204320,"corporation":false,"usgs":true,"family":"van Mantgem","given":"Phillip J.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":804624,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cansler, C. Alina 0000-0002-2155-4438","orcid":"https://orcid.org/0000-0002-2155-4438","contributorId":225029,"corporation":false,"usgs":false,"family":"Cansler","given":"C.","email":"","middleInitial":"Alina","affiliations":[{"id":41022,"text":"Missoula Fire Science Lab","active":true,"usgs":false}],"preferred":false,"id":804625,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70200388,"text":"ofr20181166 - 2018 - Overview and progress of the pallid sturgeon assessment framework redesign process","interactions":[],"lastModifiedDate":"2018-11-15T15:58:21","indexId":"ofr20181166","displayToPublicDate":"2018-11-14T16:01:52","publicationYear":"2018","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2018-1166","displayTitle":"Overview and Progress of the Pallid Sturgeon Assessment Framework Redesign Process","title":"Overview and progress of the pallid sturgeon assessment framework redesign process","docAbstract":"<p>The Pallid Sturgeon Population Assessment Program (PSPAP) was initiated in 2003, and full implementation began in 2006, to monitor the trend of <i>Scaphirhynchus albus</i> (pallid sturgeon) and native fish communities in the Upper and Lower Missouri River Basins. The original PSPAP (v. 1.0) was a catch-effort based monitoring program where population abundance and trend were monitored using a relative index, catch per unit effort. In 2013, the Missouri River Recovery Program (MRRP), led by the U.S. Army Corps of Engineers (USACE) and the U.S. Fish and Wildlife Service (USFWS), began a reassessment of science and monitoring approaches to support a new river management plan. The need to redesign the PSPAP was triggered by the recognition that the PSPAP v. 1.0 would not be optimally effective in contributing information needed to make decisions about the pallid sturgeon fundamental management objective—to avoid jeopardizing the continued existence of the pallid sturgeon from USACE actions in the Missouri River—identified in the Missouri River Science and Adaptive Management Plan. The fundamental management objective includes two management subobjectives: (1) increase pallid sturgeon recruitment to age 1 and (2) maintain or increase numbers of pallid sturgeon as an interim measure until sufficient and sustained natural recruitment occurs. These two management subobjectives motivated the development of two fundamental information objectives for PSPAP v. 2.0: (1) to provide information needed to quantify recruitment to age 1 and (2) to quantify pallid sturgeon population abundance and trend. The charge to the authors of this report was to develop an approach to monitoring the pallid sturgeon population in the Missouri River that would contribute information toward gauging overall performance of management actions to achieve the fundamental objectives of the MRRP and to potentially improve understanding of linkages from the management activities to population responses. We used transparent and robust processes to identify alternative monitoring designs that meet the fundamental objectives for managing pallid sturgeon in the MRRP, with a focus on simulation models to evaluate the performance of varying monitoring. This report documents the process of comparing potential alternative monitoring design abilities to provide decision-relevant information for management of the species. The process includes&nbsp; evaluation of information content and attendant uncertainties and considers tradeoffs in types of information valued by stakeholders. The anticipated end product of this process will be synthesized in a decision-support tool that can be used to facilitate learning and iterative revisions of the monitoring roadmap.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20181166","collaboration":"Prepared in cooperation with the Missouri River Recovery Program","usgsCitation":"Colvin, M.E., Reynolds, S., Jacobson, R.B., Pierce, L.L., Steffensen, K.D., and Welker, T.L., 2018, Overview and progress of the pallid sturgeon assessment framework redesign process: U.S. Geological Survey Open-File Report 2018–1166, 87 p., https://doi.org/10.3133/ofr20181166.","productDescription":"vii, 87 p.","numberOfPages":"96","onlineOnly":"Y","ipdsId":"IP-097824","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":359394,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2018/1166/ofr20181166.pdf","text":"Report","size":"5.31 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2018–1166"},{"id":359393,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2018/1166/coverthb.jpg"}],"contact":"<p>Director, <a data-mce-href=\"https://www.usgs.gov/centers/cerc\" href=\"https://www.usgs.gov/centers/cerc\">Columbia Environmental Research Center</a> <br>U.S. Geological Survey <br>4200 New Haven Road <br>Columbia, MO 65201</p>","tableOfContents":"<ul><li>Acknowledgments</li><li>Abstract</li><li>Introduction</li><li>Context of the Pallid Sturgeon Population Assessment Program in the Adaptive Management Program</li><li>The Need to Initiate a Pallid Sturgeon Population Assessment Program Redesign Geographic Context</li><li>Redesign Process Overview</li><li>Identify Stakeholder Views on Objectives for the Monitoring Program</li><li>Calculate Performance Metrics Given Alternative Monitoring Designs</li><li>Synthesize Outputs and Develop a Decision-Support Tool to Compare Alternative Monitoring Designs</li><li>Refine Preliminary Outputs with Pilot Studies</li><li>Summary</li><li>References Cited</li><li>Appendix 1. Recruitment-Detection Simulation Parameters</li><li>Appendix 2. Arithmetic Mean Compared to Weighted Mean Aggregation Approaches</li><li>Appendix 3. Reference Population and Catch-Data Simulation Parameters</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"publishedDate":"2018-11-14","noUsgsAuthors":false,"publicationDate":"2018-11-14","publicationStatus":"PW","scienceBaseUri":"5bed426fe4b0b3fc5cf91c6e","contributors":{"authors":[{"text":"Colvin, Michael E. 0000-0002-6581-4764","orcid":"https://orcid.org/0000-0002-6581-4764","contributorId":171431,"corporation":false,"usgs":false,"family":"Colvin","given":"Michael E.","affiliations":[{"id":26913,"text":"Iowa State University, Ames, Iowa","active":true,"usgs":false}],"preferred":false,"id":748693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Sara","contributorId":209740,"corporation":false,"usgs":false,"family":"Reynolds","given":"Sara","email":"","affiliations":[{"id":17848,"text":"Mississippi State University","active":true,"usgs":false}],"preferred":false,"id":748694,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jacobson, Robert B. 0000-0002-8368-2064 rjacobson@usgs.gov","orcid":"https://orcid.org/0000-0002-8368-2064","contributorId":1289,"corporation":false,"usgs":true,"family":"Jacobson","given":"Robert","email":"rjacobson@usgs.gov","middleInitial":"B.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":748692,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pierce, Landon L.","contributorId":196925,"corporation":false,"usgs":false,"family":"Pierce","given":"Landon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":748695,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Steffensen, Kirk D.","contributorId":196924,"corporation":false,"usgs":false,"family":"Steffensen","given":"Kirk","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":748696,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Welker, Timothy L.","contributorId":140976,"corporation":false,"usgs":false,"family":"Welker","given":"Timothy","email":"","middleInitial":"L.","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":748697,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70200902,"text":"70200902 - 2018 - Two-event lode-ore deposition at Butte, USA: 40Ar/39Ar and U-Pb documentation of Ag-Au-polymetallic lodes overprinted by younger stockwork Cu-Mo ores and penecontemporaneous Cu lodes","interactions":[],"lastModifiedDate":"2018-11-14T15:13:05","indexId":"70200902","displayToPublicDate":"2018-11-14T15:12:47","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2954,"text":"Ore Geology Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Two-event lode-ore deposition at Butte, USA: 40Ar/39Ar and U-Pb documentation of Ag-Au-polymetallic lodes overprinted by younger stockwork Cu-Mo ores and penecontemporaneous Cu lodes","docAbstract":"<p id=\"sp0015\">The ore-genesis model for world-class deposits of the Butte mining district, Montana, USA, is deep pre-Main Stage porphyry Cu-Mo and overlying Main Stage Ag-Zn-Cu zoned-lode deposits, both of which formed from hydrothermal fluids driven by minor volumes of rhyolitic magma. The lode-specific model is that hydrothermal processes diminished in intensity outward from district center along lode veins, synchronously forming metal zones. The accepted models are controverted by new geologic and multi-method geochronologic studies.</p><p id=\"sp0020\">The new data reveal the following sequence of events: (1) Thermal study of country rock indicates that the 76.9-Ma Butte Granite cooled to 350–400 °C by 4 m.y. after emplacement. (2) Five quartz porphyry rhyolite dikes were emplaced at 67–65 Ma and another at 60 Ma (SHRIMP U-Pb) into the cooled Butte Granite without resetting<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar ages in country rock. (3) Fifty-eight white mica and K-feldspar samples from alteration envelopes adjacent to Ag-Au-polymetallic lodes in outer parts of the district, Zn-rich lodes in intermediate parts, and Cu-rich lodes in the district center yield<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar ages of 73–70 Ma for Ag-rich lodes, 65–64 Ma for Cu-rich lodes, and complex age spectra of 69–65 Ma for Zn-rich lodes.</p><p id=\"sp0025\">The data show that Ag-Au-polymetallic lodes occupied cross-district fractures by about 73 Ma, forming the greater Butte mining district. At 67–65 Ma, minor quartz porphyry dikes were emplaced into central and eastern parts of the rejuvenated fracture system but without evidence of related cupola or volcanic rocks or of thermal disturbance in the country rock. At 64.5 Ma, overlapping hydrothermal cells formed two stockwork Cu-Mo domes in deep parts of the fracture system. At 65–64 Ma and closely related to late-stage stockwork Cu-Mo activity, a penecontemporaneous hydrothermal pulse formed a high-sulfidation hydrothermal plume that (1) utilized the large re-opened fractures to cannibalize and remobilize Cu from autologous, stockwork, and older Ag-Au-polymetallic lodes, (2) deposited the rich, high-sulfidation Cu lodes, and (3) mobilized metals from early Ag-Au-polymetallic veins in middle parts of the district, transported the metals outward and redeposited them, enriching early veins, especially in the intermediate Zn plus Cu areas.</p><p id=\"sp0030\">Metals zones in lodes of the Butte district are the result of an intensely focused, Cu-rich hydrothermal plume that variably reworked the center of significantly larger, 10 m.y. older, Ag-Au-polymetallic lodes.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.oregeorev.2018.05.018","usgsCitation":"Lund, K., McAleer, R., Aleinikoff, J.N., Cosca, M.A., and Kunk, M.J., 2018, Two-event lode-ore deposition at Butte, USA: 40Ar/39Ar and U-Pb documentation of Ag-Au-polymetallic lodes overprinted by younger stockwork Cu-Mo ores and penecontemporaneous Cu lodes: Ore Geology Reviews, v. 102, p. 666-700, https://doi.org/10.1016/j.oregeorev.2018.05.018.","productDescription":"35 p.","startPage":"666","endPage":"700","ipdsId":"IP-087572","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":359430,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","city":"Butte","volume":"102","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5bed4270e4b0b3fc5cf91c70","contributors":{"authors":[{"text":"Lund, Karen 0000-0002-4249-3582 klund@usgs.gov","orcid":"https://orcid.org/0000-0002-4249-3582","contributorId":1235,"corporation":false,"usgs":true,"family":"Lund","given":"Karen","email":"klund@usgs.gov","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":true,"id":751253,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McAleer, Ryan J. 0000-0003-3801-7441 rmcaleer@usgs.gov","orcid":"https://orcid.org/0000-0003-3801-7441","contributorId":5301,"corporation":false,"usgs":true,"family":"McAleer","given":"Ryan J.","email":"rmcaleer@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":751254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Aleinikoff, John N. 0000-0003-3494-6841 jaleinikoff@usgs.gov","orcid":"https://orcid.org/0000-0003-3494-6841","contributorId":1478,"corporation":false,"usgs":true,"family":"Aleinikoff","given":"John","email":"jaleinikoff@usgs.gov","middleInitial":"N.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":751255,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cosca, Michael A. 0000-0002-0600-7663 mcosca@usgs.gov","orcid":"https://orcid.org/0000-0002-0600-7663","contributorId":1000,"corporation":false,"usgs":true,"family":"Cosca","given":"Michael","email":"mcosca@usgs.gov","middleInitial":"A.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":751256,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kunk, Michael J. 0000-0003-4424-7825 mkunk@usgs.gov","orcid":"https://orcid.org/0000-0003-4424-7825","contributorId":200968,"corporation":false,"usgs":true,"family":"Kunk","given":"Michael","email":"mkunk@usgs.gov","middleInitial":"J.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":751257,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70200903,"text":"70200903 - 2018 - Multi-scale effects of land cover and urbanization on the habitat suitability of an endangered toad","interactions":[],"lastModifiedDate":"2018-11-14T15:08:37","indexId":"70200903","displayToPublicDate":"2018-11-14T15:08:33","publicationYear":"2018","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1015,"text":"Biological Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Multi-scale effects of land cover and urbanization on the habitat suitability of an endangered toad","docAbstract":"<p><span>Habitat degradation, entwined with&nbsp;land cover change, is a major driver of&nbsp;biodiversity loss. Effects of land cover change on species can be direct (when habitat is converted to alternative land cover types) or indirect (when land outside of the species habitat is altered). Hydrologic and ecological connections between terrestrial and aquatic systems are well understood, exemplifying how spatially disparate land cover conditions may influence aquatic habitats, but are rarely examined. We sought to quantify relative effects of land cover at two different but interacting scales on habitat suitability for the endangered arroyo toad (</span><span><i>Anaxyrus</i>&nbsp;californicus</span><span>). Based on an existing distribution model for the arroyo toad and available land cover data, we estimated effects of land cover along streams and within entire watersheds on habitat suitability using structural equation modeling. Relationships between land cover and habitat suitability differed between scales, and broader, watershed-scale conditions influenced land cover along the embedded stream networks. We found anthropogenic development and&nbsp;forest cover&nbsp;at the watershed-scale negatively impacted habitat suitability, but development along stream networks was positively associated with suitability. The positive association between development along streams and habitat suitability may be attributable to increased spatial heterogeneity along urbanized streams, or related factors including policies designed to conserve riparian habitats amidst development. These findings show arroyo toad habitat is influenced by land cover across multiple scales, and can inform conservation of the species. Furthermore, our methodology can help elucidate similar dynamics with other taxa, particularly those reliant on both&nbsp;terrestrial and aquatic environments.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.biocon.2018.10.032","usgsCitation":"Treglia, M.L., Landon, A.C., Fisher, R.N., Kyle, G., and Fitzgerald, L.A., 2018, Multi-scale effects of land cover and urbanization on the habitat suitability of an endangered toad: Biological Conservation, v. 228, p. 310-318, https://doi.org/10.1016/j.biocon.2018.10.032.","productDescription":"9 p.","startPage":"310","endPage":"318","ipdsId":"IP-094043","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":359429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","volume":"228","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5bed4270e4b0b3fc5cf91c72","contributors":{"authors":[{"text":"Treglia, Michael L.","contributorId":145921,"corporation":false,"usgs":false,"family":"Treglia","given":"Michael","email":"","middleInitial":"L.","affiliations":[{"id":16299,"text":"Dep't Wildlife and Fisheries, Texas A&M U, College Station, Texas","active":true,"usgs":false}],"preferred":false,"id":751170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landon, Adam C","contributorId":210605,"corporation":false,"usgs":false,"family":"Landon","given":"Adam","email":"","middleInitial":"C","affiliations":[{"id":6747,"text":"Texas A&M University","active":true,"usgs":false}],"preferred":false,"id":751171,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fisher, Robert N. 0000-0002-2956-3240 rfisher@usgs.gov","orcid":"https://orcid.org/0000-0002-2956-3240","contributorId":1529,"corporation":false,"usgs":true,"family":"Fisher","given":"Robert","email":"rfisher@usgs.gov","middleInitial":"N.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":751169,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kyle, Gerard","contributorId":210606,"corporation":false,"usgs":false,"family":"Kyle","given":"Gerard","affiliations":[{"id":6747,"text":"Texas A&M University","active":true,"usgs":false}],"preferred":false,"id":751172,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fitzgerald, Lee A.","contributorId":141035,"corporation":false,"usgs":false,"family":"Fitzgerald","given":"Lee","email":"","middleInitial":"A.","affiliations":[{"id":6747,"text":"Texas A&M University","active":true,"usgs":false}],"preferred":false,"id":751173,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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