Changes in the active, dead, and dormant microbial community structure across a Pleistocene permafrost chronosequence
Alexander Burkert, Thomas A. Douglas, Mark Waldrop, Rachel Mackelprang
2019, Applied and Environmental Microbiology (85)
Permafrost hosts a community of microorganisms that survive and reproduce for millennia despite extreme environmental conditions such as water stress, subzero temperatures, high salinity, and low nutrient availability. Many studies focused on permafrost microbial community composition use DNA-based methods such as metagenomic and 16S rRNA gene sequencing. However, these methods...
Effect of permafrost thaw on plant and soil fungal community in the boreal forest: Does fungal community change mediate plant productivity response?
Ursel M.E Schütte, Jeremiah A. Henning, Yuzhen Ye, A. Bowling, James D. Ford, Helene Genet, Mark Waldrop, Merritt R. Turetsky, Jeffrey R. White, James D Bever
2019, Journal of Ecology (107) 1737-1752
Permafrost thaw is leading to rapid shifts in boreal ecosystem function. Permafrost thaw affects soil carbon turnover through changes in soil hydrology, however, the biotic mechanisms regulating plant community response remain elusive. Here, we measured the response of fungal community composition and soil nutrient content in an intact permafrost plateau...
Beneath the arctic greening: Will soils lose or gain carbon or perhaps a little of both?
Jennifer W. Harden, J.A. O’Donnell, K.A. Heckman, B.N. Sulman, C.D. Koven, C.L. Ping, G.J. Michaelson
2019, SOIL
Ecosystem shifts related to climate change are anticipated for the next decades to centuries based on a number of conceptual and experimentally derived models of plant structure and function. Belowground, the potential responses of soil systems are less well known. We used geochemical steady state models, soil density fractionation, and...
Development of perennial thaw zones in boreal hillslopes enhances potential mobilization of permafrost carbon
Michelle A. Walvoord, Clifford I. Voss, Brian A. Ebel, Burke J. Minsley
2019, Environmental Research Letters (14) 1-11
Permafrost thaw alters subsurface flow in boreal regions that in turn influences the magnitude, seasonality, and chemical composition of streamflow. Prediction of these changes is challenged by incomplete knowledge of timing, flowpath depth, and amount of groundwater discharge to streams in response to thaw. One important phenomenon that may affect...
Survival of Bristle-thighed Curlews equipped with externally mounted transmitters
Daniel R. Ruthrauff, T. Lee Tibbitts, Vijay P. Patil
2019, Wader Study (126) 109-115
Telemetry devices are widely used in avian research, but the degree to which the deployment of such devices affects the survival of study subjects is often not addressed. It is generally assumed that such effects are less pronounced in large-bodied species that conduct relatively short migrations and carry relatively light...
Main stem and off-channel habitat use by juvenile Chinook salmon in a sub-Arctic riverscape
Brock M. Huntsman, Jeffrey A. Falke
2019, Freshwater Biology (64) 433-446
Poor growth and survival in freshwater and marine environments have been implicated as responsible for Chinook salmon (Oncorhynchus tshawytscha) declines across Alaska.Lateral connectivity of river main stems with off-channel habitats may play an integral role in sustaining Alaskan salmonid populations because off-channel habitats commonly provide greater growth opportunities than...
Warming effects of spring rainfall increase methane emissions from thawing permafrost
Rebecca B. Neumann, C.J. Moorberg, J.D. Lundquist, J.C. Turner, Mark P. Waldrop, Jack W. McFarland, E.S. Euskirchen, C.W. Edgar, M. R. Turetsky
2019, Geophysical Research Letters (46) 1393-1401
Methane emissions regulate the near‐term global warming potential of permafrost thaw, particularly where loss of ice‐rich permafrost converts forest and tundra into wetlands. Northern latitudes are expected to get warmer and wetter, and while there is consensus that warming will increase thaw and methane emissions, effects of increased precipitation are...
Trophic plasticity and the invasion of a renowned piscivore: A diet synthesis of northern pike (Esox lucius) from the native and introduced ranges in Alaska, U.S.A.
C. Nathan Cathcart, Kristine J. Dunker, Thomas P. Quinn, Adam J. Sepulveda, Frank A. von Hippel, Andrew Wizik, Daniel B. Young, Peter A.H. Westley
2019, Biological Invasions (21) 1379-1392
The invasion of non-native fishes is a leading cause of extinction and imperilment of native freshwater fishes. Evidence suggests that introduced species with generalist diets have the potential for greatest impacts through competition and predation even though populations are often comprised of specialist individuals. The northern pike (Esox lucius), a...
Volcanic ash resuspension from the Katmai Region
Kristi L. Wallace, Hans Schwaiger
2019, Park Science
Volcanic ash is not only a hazard during an eruptive event; in strong winds, previously deposited loose volcanic ash can be picked up and reworked into dust clouds. Resuspension and transport of fine-grained volcanic ash from Katmai National Park and Preserve, Alaska has been observed and documented many times over...
Volcanic hazards in Alaska’s National Parks
Katherine Mulliken, Kristi L. Wallace, Cheryl Cameron, Christopher F. Waythomas
2019, Park Science
There are over 100 volcanoes in Alaska, 54 of which are considered historically active. A historically active volcano is one that fits one of the following criteria: a documented or strongly suspected eruption since the year 1700, persistent fumaroles near boiling point, significant deformation with a volcanic cause, or an...
Global sea-level contribution from Arctic land ice: 1971 to 2017
Jason E. Box, William T. Colgan, Bert Wouters, David O Burgess, Shad O’Neel, Laura Thomson, Sebastian H Mernild
2019, Environmental Research Letters (13)
The Arctic Monitoring and Assessment Program (AMAP) (AMAP, 2017) identifies the Arctic as the largest regional source of land ice to global sea-level rise in the 2003 to 2014 period. Yet, this contextualization ignores the longer perspective from in-situ records of glacier mass balance. Here, using 18 (> 55 °N latitude) glacier and...
Incorporating productivity as a measure of fitness into models of breeding area quality of Arctic peregrine falcons
David E. Andersen, Jason E. Bruggeman, Ted Swem, Patricia L. Kennedy, Debora Nigro
2019, Wildlife Biology
Using empirical location data from individuals to model habitat quality and species distributions is valuable towards understanding habitat use of wildlife, especially for conservation and management planning. Incorporating measures of reproductive success or survival into these models helps address the role of vital rates (a surrogate of fitness) in affecting...
Petroleum systems framework of significant new oil discoveries in a giant Cretaceous (Aptian–Cenomanian) clinothem in Arctic Alaska
David W. Houseknecht
2019, American Association of Petroleum Geologists Bulletin (103) 619-652
Recent oil discoveries in an Aptian–Cenomanian clinothem in Arctic Alaska demonstrate the potential for hundred-million- to billion-barrel oil accumulations in Nanushuk Formation topsets and Torok Formation foresets–bottomsets. Oil-prone source rocks and the clinothem are draped across the Barrow arch, a structural hinge between the Colville foreland basin and Beaufort Sea...
Interannual snow accumulation variability on glaciers derived from repeat spatially extensive ground-penetrating radar surveys
Daniel J McGrath, Louis Sass, Shad O’Neel, Christopher J. McNeil, Salvatore G Candela, Emily Baker, Hans P. Marshall
2019, The Cryosphere (12) 3617-3633
There is significant uncertainty regarding the spatiotemporal distribution of seasonal snow on glaciers, despite being a fundamental component of glacier mass balance. To address this knowledge gap, we collected repeat, spatially extensive high-frequency ground-penetrating radar (GPR) observations on two glaciers in Alaska for five consecutive years. GPR measurements showed steep...
New approach to assessing age uncertainties – The 2300-year varve chronology from Eklutna Lake, Alaska (USA)
David Fortin, Nore Praet, Nicholas P. McKay, Darrell S. Kaufman, Britta J.L. Jensen, Peter J. Haeussler, Casey Buchanan, Marc De Batist
2019, Quaternary Science Reviews (203) 90-101
Developing robust chronological frameworks of lacustrine sediment is central to reconstructing past environmental changes. We present varve chronologies from five sites extending back 2300 years from Eklutna Lake, in the Chugach Mountains of south-central Alaska. The chronologies are built from image analysis of high-resolution photographs...
Density‐dependent and phenological mismatch effects on growth and survival in lesser snow and Ross's goslings
Megan V. Ross, Ray T. Alisauskas, David C. Douglas, Dana K. Kellett, Kiel L. Drake
2019, Journal of Avian Biology (49)
Strong seasonality of high‐latitude environments imposes temporal constraints on forage availability and quality for keystone herbivores in terrestrial arctic ecosystems, including hyper‐abundant colonial geese. Changes in food quality due to intraspecific competition, or food availability relative to the breeding phenology of birds, may have consequences for growth and survival of...
Delayed herbivory by migratory geese increases summer‐long CO2 uptake in coastal western Alaska
A. Joshua Leffler, Karen H. Beard, Katharine C. Kelsey, Ryan T. Choi, Joel A. Schmutz, Jeffery M. Welker
2019, Global Change Biology (25) 277-289
The advancement of spring and the differential ability of organisms to respond to changes in plant phenology may lead to ‘phenological mismatches’ as a result of climate change. One potential for considerable mismatch is between migratory birds and food availability in northern breeding ranges and these mismatches may have consequences...
Changing station coverage impacts temperature trends in the Upper Colorado River Basin
Stephanie A. McAfee, Gregory J. McCabe, Stephen Gray, Gregory T. Pederson
2019, International Journal of Climatology (39) 1517-1538
Over the Upper Colorado River Basin (UCRB), temperatures in widely used gridded data products do not warm as much as mean temperatures from a stable set of U.S. Historical Climatology Network (USHCN) stations, located at generally lower elevations, in most months of the year. This is contrary to expectations of...
Overview of the oxygen isotope systematics of land snails from North America
Yurena Yanes, Nasser M. Al-Qattan, Jason A. Rech, Jeffrey S. Pigati, Justin P. Dodd, Jeffrey C. Nekola
2019, Quaternary Research (91) 329-344
Continental paleoclimate proxies with near-global coverage are rare. Land snail δ18O is one of the few proxies abundant in Quaternary sediments ranging from the tropics to the high Arctic tundra. However, its application in paleoclimatology remains difficult, attributable in part to limitations in published calibration studies. Here we present...
Nesting ecology of a naturalized population of Mallards Anas platyrhynchos in New Zealand
Jennifer L. Sheppard, Courtney L. Amundson, Todd W. Arnold, David Klee
2019, Ibis (161) 504-520
Investigating the reproductive ecology of naturalized species provides insights into the role of the source population's characteristics vs. post‐release adaptation that influence the success of introduction programmes. Introduced and naturalized Mallards Anas platyrhynchos are widely established in New Zealand (NZ), but little is known regarding their reproductive ecology. We evaluated the nesting...
Phenology of hatching, emergence, and end-of-season body size in young-of-year Coho Salmon in thermally contrasting streams draining the Copper River Delta, Alaska
Emily Y. Campbell, Jason B. Dunham, Gordon H. Reeves, Steve M. Wondzell
2019, Canadian Journal of Fisheries and Aquatic Sciences (76) 185-191
Phenology can be linked to individual fitness, particularly in strongly seasonal environments where the timing of events have important consequences for growth, condition, and survival. We studied the phenology of Coho Salmon hatching and emergence in streams with contrasting thermal variability, but in close geographic proximity. Following emergence, we tracked...
Capture versus tagging impacts on chum salmon freshwater spawning migration travel times
Suresh Sethi
2019, Fisheries Management and Ecology (25) 296-303
The spawning migration travel times of chum salmon, Oncorhynchus keta (Walbaum), fitted with gastrically implanted radio tags vs external spaghetti tags were tested for a short [≈60 river km (rkm)] and long migration route (≈730 rkm) on the Koyukuk River, Alaska, USA. Using a novel application of statistical arrival curve...
Development of on-shore behavior among polar bears (Ursus maritimus) in the southern Beaufort Sea: Inherited or learned?
K. M. Lillie, E. M. Gese, Todd C. Atwood, Sarah A. Sonsthagen
2019, Ecology and Evolution (8) 7790-7799
Polar bears (Ursus maritimus) are experiencing rapid and substantial changes to their environment due to global climate change. Polar bears of the southern Beaufort Sea (SB) have historically spent most of the year on the sea ice. However, recent reports from Alaska indicate that the proportion of the SB subpopulation...
A repeating event sequence alarm for monitoring volcanoes
Gabrielle Tepp
2019, Seismological Research Letters (89) 1863-1876
A major challenge in volcanology is forecasting eruptions. Repeating earthquake sequences may precede volcanic eruptions or lava dome growth and collapse, providing an opportunity for short-term eruption forecasting. I develop an automated repeating earthquake sequence detector and near real-time alarm to send alerts when an in-progress sequence is identified. The...
Slope failure and mass transport processes along the Queen Charlotte Fault, southeastern Alaska
Daniel Brothers, Brian D. Andrews, Maureen A. L. Walton, H. Gary Greene, J. Vaughn Barrie, Nathaniel C. Miller, Uri S. ten Brink, Amy E. East, Peter J. Haeussler, Jared W. Kluesner, James E. Conrad
2019, Geological Society Special Publication
The Queen Charlotte Fault defines the Pacific–North America transform plate boundary in western Canada and southeastern Alaska for c. 900 km. The entire length of the fault is submerged along a continental margin dominated by Quaternary glacial processes, yet the geomorphology along the margin has never been systematically examined due...