40Ar/39Ar whole-rock data constraints on Acadian diagenesis and Alleghanian cleavage in the Martinsburg formation, eastern Pennsylvania
R. P. Wintsch, Michael J. Kunk, Jack B. Epstein
1996, American Journal of Science (296) 766-788
A comparison of 40Ar/39Ar age spectra of whole-rock mudstone and slate samples from the Ordovician Martinsburg Formation at Lehigh Gap, Pennsylvania and stratigraphic and thermal constraints support Alleghanian age for regional slaty cleavage and a late Acadian age for diagenesis in these rocks. Age spectra from mud-stones have a sigmodal shape,...
Using landscape ecology to test hypotheses about large-scale abundance patterns in migratory birds
Curtis H. Flather, John R. Sauer
1996, Ecology (77) 28-35
The hypothesis that Neotropical migrant birds may be undergoing widespread declines due to land use activities on the breeding grounds has been examined primarily by synthesizing results from local studies. Growing concern for the cumulative influence of land use activities on ecological systems has heightened the need for large—scale studies...
Climatic control of nitrate loss from forested watersheds in the northeast United States
M.J. Mitchell, C. T. Driscoll, J. S. Kahl, G.E. Likens, Peter S. Murdoch, L.H. Pardo
1996, Environmental Science & Technology (30) 2609-2612
Increased losses of nitrate from watersheds may accelerate the depletion of nutrient cations and affect the acidification and trophic status of surface waters. Patterns of nitrate concentrations and losses were evaluated in four forested watersheds (East Bear Brook Watershed, Lead Mountain, ME; Watershed 6, Hubbard Brook Experimental Forest, White Mountains,...
Holocene paleoenvironments of Northeast Iowa
R. G. Baker, E. Arthur Bettis III, D. R. Schwert, D. G. Horton, C. A. Chumbley, Luis A. Gonzalez, M. K. Reagan
1996, Ecological Monographs (66) 203-234
This paper presents the biotic, sedimentary, geomorphic, and climatic history of the upper part of the Roberts Creek Basin, northeastern Iowa for the late—glacial and Holocene, and compares these records with a C—O isotopic sequence from Coldwater Cave, 60 km northwest of Roberts Creek. The biotic record (pollen, vascular plant...
Magnetic properties and emplacement of the Bishop tuff, California
H.C. Palmer, W.D. MacDonald, C. S. Grommé, B.B. Ellwood
1996, Bulletin of Volcanology (58) 101-116
Anisotropy of magnetic susceptibility (AMS) and characteristic remanence were measured for 45 sites in the 0.76 Ma Bishop tuff, eastern California. Thirty-three sites were sampled in three stratigraphic sections, two in Owens gorge south of Long Valley caldera, and the third in the Adobe lobe north of...
Taxonomic reassessment of the ichnogenus Beaconichnus and additional examples from the Carboniferous of Kansas, U.S.A.
Luis A. Buatois, M. Gabriela Mángano, Christopher G. Maples, William P. Lanier
1996, Ichnos: An International Journal for Plant and Animal Traces (5) 287-302
The ichnogenus Beaconichnus (Gevers 1973), an arthropod trace fossil, includes very different forms that comprise five ichnospecies, namely B. darwi‐nunt (Gevers 1971), B. gouldi (Gevers 1971), B. ahtarcticum(Gevers 1971), B. giganteum Gevers and Twomey 1982, and B. wrrighti Gevers and Twomey 1982. The original diagnosis of Beaconichnus is rather vague and potentially may accommodate virtually every arthropod trackway described from the fossil record. In...
Transition from slab to slabless: Results from the 1993 Mendocino triple junction seismic experiment
B. C. Beaudoin, N. J. Godfrey, S.L. Klemperer, C. Lendl, A.M. Trehu, T.J. Henstock, A. Levander, J.E. Holl, A.S. Meltzer, James H. Luetgert, Walter D. Mooney
1996, Geology (24) 195-199
Three seismic refraction-reflection profiles, part of the Mendocino triple junction seismic experiment, allow us to compare and contrast crust and upper mantle of the North American margin before and after it is modified by passage of the Mendocino triple junction. Upper crustal velocity models reveal an asymmetric Great Valley basin...
Using hydrogeochemical methods to evaluate complex quaternary subsurface stratigraphy Block Island, Rhode Island, USA
A.I. Veeger, B. D. Stone
1996, Hydrogeology Journal (4) 69-82
One of the major problems in hydrogeologic investigations of glaciated regions is the determination of complex stratigraphic relationships in the subsurface where insufficient information is available from drilling and geophysical records. In this paper, chemical characteristics of groundwater were used to identify stratigraphic changes in glacial deposits that were previously...
Late Stage 5 Glacio-isostatic Sea in the St. Lawrence Valley, Canada and United States
S. Occhietti, S. Balescu, M. Lamothe, M. Clet, T. Cronin, P. Ferland, P. Pichet
1996, Quaternary Research (45) 128-137
Although post-glacial marine sediments of late Wisconsinan and early Holocene age are common in eastern Canada and the northeastern United States, remnants of older Pleistocene marine sediments are scarce. A fossiliferous marine clay that predates the classical Wisconsinan was recently discovered in the St. Lawrence Valley. A dominantly estuarine environment...
Late Pennsylvanian climate changes and palynomorph extinctions
R.M. Kosanke, C. B. Cecil
1996, Review of Palaeobotany and Palynology (90) 113-140
A major floral change occurs in the Upper Pennsylvanian strata in the Midcontinent, Illinois basin, and in the northern Appalachian basin of eastern United States. Lycospora spp. (derived from arborescent lycopsids) became extinct along with some other palynomorph taxa. This investigation is concerned with the importance of this major floral...
Block and shear-zone architecture of the Minnesota River Valley subprovince: Implications for late Archean accretionary tectonics
D. L. Southwick, V.W. Chandler
1996, Canadian Journal of Earth Sciences (33) 831-847
The Minnesota River Valley subprovince of the Superior Province is an Archean gneiss terrane composed internally of four crustal blocks bounded by three zones of east-northeast-trending linear geophysical anomalies. Two of the block-bounding zones are verified regional-scale shears. The geological nature of the third boundary has not been established. Potential-field...
Shear wave velocity structure in North America from large-scale waveform inversions of surface waves
D. Alsina, R.L. Woodward, R.K. Snieder
1996, Journal of Geophysical Research B: Solid Earth (101) 15969-15986
A two-step nonlinear and linear inversion is carried out to map the lateral heterogeneity beneath North America using surface wave data. The lateral resolution for most areas of the model is of the order of several hundred kilometers. The most obvious feature in the tomographic images is the rapid transition...
The contribution of wetlands to stream nitrogen load in the Loch Vale Watershed, Colorado, USA
Huang Jian-hui, Jill Baron, Dan Binkley
1996, Chinese Journal of Plant Ecology (20) 289-302
We explored the difference between the concentrations of different N forms and other chemical properties between stream water and riparian zone wetland soil water in the Loch Vale Watershed which is located on the eastern slope of the Continental Divide in Rocky Mountain National Park, Colorado, USA. The nitrate N...
Serological evidence of morbillivirus infection in polar bears (Ursus maritimus) from Alaska and Russia
Erich H. Follmann, G.W. Garner, Jim F. Evermann, McKeirnan
1996, Veterinary Record (138) 615-618
One-hundred-and-ninety-one samples of blood serum collected from 186 polar bears (Ursus maritimus) between 1987 and 1992 were analysed for morbillivirus antibodies. The samples were collected in the Bering, Chukchi and East Siberian seas. Sixty-eight samples (35.6 per cent) had morbillivirus antibody titres > 5; the percentage of positive samples ranged...
The stable oxygen and carbon isotopic record from a coral growing in Florida Bay: a 160 year record of climatic and anthropogenic influence
Peter K. Swart, Genevieve F. Healy, Richard E. Dodge, Philip Kramer, J. Harold Hudson, Robert B. Halley, Michael B. Robblee
1996, Palaeogeography, Palaeoclimatology, Palaeoecology (123) 219-237
A 160 year record of skeletal δ13C and δ18O was examined in a specimen of the coral Solenastrea bournonigrowing in Florida Bay. Variations in the δ18O of the skeleton can be correlated to changes in salinity while changes in the δ13C reflect cycling of organic material within the Bay. Based on...
Geographic variation in migratory behavior of greater white-fronted geese (Anser albifrons)
Craig R. Ely, John Y. Takekawa
1996, The Auk (113) 889-901
We studied the migration and winter distribution of adult Greater White-fronted Geese (Anser albifrons frontalis) radio-marked on the Yukon-Kuskokwim Delta (YKD) and Bristol Bay Lowlands (BBL) of Alaska from 1987 to 1992. The major autumn staging site for geese from both breeding areas was the Klamath Basin on the California/Oregon...
Middle Proterozoic age for the Montpelier Anorthosite, Goochland terrane, eastern Piedmont, Virginia
J. N. Aleinikoff, J. Wright Horton Jr., M. Walters
1996, Geological Society of America Bulletin (108) 1481-1491
Uranium-lead dating of zircons from the Montpelier Anorthosite confirms previous interpretations, based on equivocal evidence, that the Goochland terrane in the eastern Piedmont of Virginia contains Grenvillian basement rocks of Middle Proterozoic age. A very few prismatic, elongate, euhedral zircons, which contain 12–29...
Record of middle Pleistocene climate change from Buck Lake, Cascade Range, southern Oregon - Evidence from sediment magnetism, trace-element geochemistry, and pollen
J. G. Rosenbaum, R. L. Reynolds, D.P. Adam, J. Drexler, A.M. Sarna-Wojcicki, G.C. Whitney
1996, Geological Society of America Bulletin (108) 1328-1341
Comparison of systematic variations in sediment magnetic properties to changes in pollen assemblages in middle Pleistocene lake sediments from Buck Lake indicates that the magnetic properties are sensitive to changes in climate. Buck Lake is located in southern Oregon just east of the...
The southern Whidbey Island fault: An active structure in the Puget Lowland, Washington
S. Y. Johnson, C. J. Potter, J.M. Armentrout, J. J. Miller, Carol A. Finn, C.S. Weaver
1996, Geological Society of America Bulletin (108) 334-354
Information from seismic-reflection profiles, outcrops, boreholes, and potential field surveys is used to interpret the structure and history of the southern Whidbey Island fault in the Puget Lowland of western Washington. This northwest-trending fault comprises a broad (as wide as 6–11 km), steep, northeast-dipping zone that includes several splays with...
Effects of winter atmospheric circulation on temporal and spatial variability in annual streamflow in the western United States
G. J. McCabe Jr.
1996, Hydrological Sciences Journal (41) 873-887
Winter mean 700-hectoPascal (hPa) height anomalies, representing the average atmospheric circulation during the snow season, are compared with annual streamflow measured at 140 streamgauges in the western United States. Correlation and anomaly pattern analyses are used to identify relationships between winter mean atmospheric circulation and temporal and spatial variability in...
Origin of high mountains in the continents: The Southern Sierra Nevada
B. Wernicke, R. Clayton, Mihai N. Ducea, C.H. Jones, S. Park, S. Ruppert, J. Saleeby, J.K. Snow, L. Squires, M. Fliedner, G. Jiracek, Rebecca Hylton Keller, S. Klemperer, J. Luetgert, P. Malin, K. Miller, Walter D. Mooney, H. Oliver, R. Phinney
1996, Science (271) 190-193
Active and passive seismic experiments show that the southern Sierra, despite standing 1.8 to 2.8 kilometers above its surroundings, is underlain by crust of similar seismic thickness, about 30 to 40 kilometers. Thermobarometry of xenolith suites and magnetotelluric profiles indicate that the upper mantle is eclogitic to depths of 60...
Riparian vegetation and fluvial geomorphic processes
C.R. Hupp, W. R. Osterkamp
1996, Geomorphology (14) 277-295
Riparian vegetation and fluvial-geomorphic processes and landforms are intimately connected parts of the bottomland landscape. Relations among vegetation, processes, and landforms are described here for representative streams of four areas of the United States: high-gradient streams of the humid east, coastal-plain streams. Great Plains streams, and stream channels of the...
Directional topographic site response at Tarzana observed in aftershocks of the 1994 Northridge, California, earthquake: Implications for mainshock motions
P. Spudich, M. Hellweg, W.H.K. Lee
1996, Bulletin of the Seismological Society of America (86) S193-S208
The Northridge earthquake caused 1.78 g acceleration in the east-west direction at a site in Tarzana, California, located about 6 km south of the mainshock epicenter. The accelerograph was located atop a hill about 15-m high, 500-m long, and 130-m wide, striking about N78°E. During...
Exposure of wild waterfowl to Mycoplasma anatis
M.D. Samuel, Diana R. Goldberg, C. B. Thomas, P. Sharp, J.R. Robb, Gary L. Krapu, B.N. Nersessian, K.P. Kenow, C. E. Korschgen, W.H. Chipley, M.J. Conroy
1996, Journal of Wildlife Diseases (32) 331-337
We developed an ELISA procedure to assess the presence of M. Anatis-specific serum antibody in ducks. Sera from exposed and unexposed Pekin ducks (Anas platyrhynchos) were used to standardize tile ELISA and to establish reference ranges to classify ELISA results as exposed or not exposed. We conducted serological surveys of...
Sea birds as proxies of marine habitats and food webs in the western Aleutian Arc
Alan M. Springer, John F. Piatt, Gus B. Van Vliet
1996, Fisheries Oceanography (5) 45-55
We propose that ocean conditions of the Near Islands in the western Aleutian Arc mimic those of the shallow continental shelf of the eastern Bering Sea to the extent that the marine community, including assemblages of forage fishes and their avian predators, has distinctly coastal characteristics. In contrast, marine avifauna...