Seasonal abundance and vertical distribution of capelin (Mallotus villosus) in relation to water temperature at a coastal site off eastern Newfoundland
David A. Methven, John F. Piatt
1991, ICES Journal of Marine Science (48) 187-193
The seasonal abundance and vertical distribution of capelin in relation to water temperature have been investigated by conducting repeated hydroacoustic surveys at a coastal site off eastern Newfoundland. Water temperatures were warmer in 1983 than in 1984 as indicated by the earlier appearance and greater depth of the seasonal thermocline....
Variable first prebasic molt in Rio Grande and Merriam's wild turkeys
Joel A. Schmutz, Richard W. Hoffman
1991, The Wilson Bulletin (103) 295-300
Gallinaceous birds typically retain the juvenal ninth (JIX) and tenth (JX) primary wing feathers during the first prebasic molt (Petrides 1945, terminology follows Humphrey and Parkes 1959). However, not all Wild Turkeys (Meleagris gallopavo) retain JIX and JX during this molt. Some retain only JX (reviewed by Lewis 1967),...
Geological and seismological evidence of increased explosivity during the 1986 eruptions of Pavlof volcano, Alaska
S.R. McNutt, T. P. Miller, J.J. Taber
1991, Bulletin of Volcanology (53) 86-98
We present results of study of the best-documented eruptions of Pavlof volcano in historic time. The 1986 eruptions were mostly Strombolian in character; a strong initial phase may have been Vulcanian. The 1986 activity erupted at least 8??106 m3 of feldspar-phyric basaltic andesite lava (SiO2=53-54%), and a comparable volume of...
The first Tertiary (Paleocene) marine mollusks from the Eureka Sound Group, Ellesmere Island, Canada
L. Marincovich Jr., W.J. Zinsmeister
1991, Journal of Paleontology (65) 242-248
The gastropod Drepanochilus pervetus (Stanton) and the bivalve Cytrodaria rutupiensis (Morris) occur in the Mount Moore Formation at Strathcona Fiord, west-central Ellesmere Island, northern Canada. They are the first marine mollusks identified from the Eureka Sound Group of the Canadian arctic islands. These mollusks correlate with Paleocene faunas of...
Isotopic and chemical constraints on the petrogenesis of Blackburn Hills volcanic field, western Alaska
E. J. Moll-Stalcup, Joseph G. Arth
1991, Geochimica et Cosmochimica Acta (55) 3753-3776
The Blackburn Hills volcanic field is one of several Late Cretaceous and early Tertiary (75–50 Ma) volcanic fields in western Alaska that comprise a vast magmatic province extending from the Arctic Circle to Bristol Bay. It consists of andesite flows, rhyolite domes, a central granodiorite to quartz monzonite pluton, and...
Oxygen, hydrogen, and sulfur isotope studies in the Juneau gold belt, southeastern Alaska: Constraints on the origin of hydrothermal fluids
R.J. Goldfarb, R.J. Newberry, W.J. Pickthorn, C. A. Gent
1991, Economic Geology (86) 66-80
The delta 18 O values of gold-bearing quartz from the Juneau gold belt range from 15.2 to 20.8 per mil, indicating that ore fluid values ranged from 7.2 to 12.8 per mil at an estimated temperature of 300 degrees C. Hydrothermal micas from many of the deposits are characterized by delta D...
Mitochondrial and nuclear genetic relationships of deer (Odocoileus spp.) in western North America
Matthew A. Cronin
1991, Canadian Journal of Zoology (69) 1270-1279
Odocoileus hemionus (mule deer and black-tailed deer) and Odocoileus virginanus (white-tailed deer) are sympatric in western North America and are characterized by distinct morphology, behavior, and allozyme allele frequencies. However, there is discordance among nuclear and mitochondrial genetic relationships, as mule deer (O. h. hemionus) and white-tailed deer have similar...
Evolution of deep structure along the trans-Alaska crustal transect, Chugach Mountains and Copper River Basin, southern Alaska
G. S. Fuis, George Plafker
1991, Journal of Geophysical Research (96) 4229-4253
One of the most important results of the Trans-Alaska Crustal Transect investigations is the discovery that more than one third of the North American plate in southern Alaska (Chugach Mountains and Copper River basin) consists of tectonically underplated oceanic lithosphere. In southern Alaska, exposed accreted...
Patterns of seabird and marine mammal carcass deposition along the central California coast, 1980-1986
James L. Bodkin, Ronald J. Jameson
1991, Canadian Journal of Zoology (69) 1149-1155
At monthly intervals from February 1980 through December 1986, a 14.5-km section of central California coastline was systematically surveyed for beach-cast carcasses of marine birds and mammals. Five hundred and fifty-four bird carcasses and 194 marine mammal carcasses were found. Common murres, western grebes, and Brandt's cormorants composed 45% of...
Effects of wind-hardened snow on foraging by reindeer (Rangifer tarandus)
W. B. Collins, T. S. Smith
1991, Arctic (44) 217-222
Various methods were investigated for assessing the relationship between wind-hardened snow (upsik) and forage availability to reindeer. Mean bottom area of individual craters was not a function of depth, hardness or integrated hardness. Individual crater area was partially dependent on specific cratering time (r2 = .60). Cratering time per active...
Apparatus for precise regulation and chilling of water temperatures in laboratory studies
D.B. Wangaard, John P. McDonell, Carl V. Burger, R.L. Wilmot
1991, Progressive Fish-Culturist (53) 251-255
Laboratory simulation of water temperature regimes that occur in subarctic rivers through winter necessitates the ability to maintain near‐freezing conditions. A heat‐exchanging apparatus is described that provided a convenient means of simulating the range of temperatures (0.5–12°C) that incubating eggs of salmon (Oncorhynchus spp.) typically experience in south‐central Alaskan watersheds. The...
Fluid inclusion gas chemistry as a potential minerals exploration tool: Case studies from Creede, CO, Jerritt Canyon, NV, Coeur d'Alene district, ID and MT, southern Alaska mesothermal veins, and mid-continent MVT's
G. P. Landis, A. H. Hofstra
1991, Journal of Geochemical Exploration (42) 25-59
Recent advances in instrumentation now permit quantitative analysis of gas species from individual fluid inclusions. Fluid inclusion gas data can be applied to minerals exploration empirically to establish chemical (gas composition) signatures of the ore fluids, and conceptually through the development...
Crustal structure of accreted terranes in southern Alaska, Chugach Mountains and Copper River Basin, from seismic refraction results
G. S. Fuis, E. L. Ambos, Walter D. Mooney, N.I. Christensen, E. Geist
1991, Journal of Geophysical Research (96) 4187-4227
Seismic refraction data were collected along a 320-km-long "transect' line in southern Alaska, crossing the Prince William, Chugach, Peninsular, and Wrangellia terranes, and along several shorter lines within individual terranes. Velocity structure in the upper crust (less than 9-km depth) differs among the four terranes. In contrast, layers in the...
Development of inverted metamorphic isograds in the western metamorphic belt, Juneau, Alaska
G. R. Himmelberg, D. A. Brew, A. B. Ford
1991, Journal of Metamorphic Geology (9) 165-180
An inverted metamorphic gradient is preserved in the western metamorphic belt near Juneau, Alaska. The western metamorphic belt is part of the Coast plutonic–metamorphic complex of western Canada and southeastern Alaska that developed as a result of tectonic overlap and/or compressional thickening of crustal rocks during collision of the Alexander...
Geochemistry and exploration criteria for epithermal cinnabar and stibnite vein deposits in the Kuskokwim River region, southwestern Alaska
J. E. Gray, R.J. Goldfarb, D.E. Detra, K. E. Slaughter
1991, Journal of Geochemical Exploration (41) 363-386
Cinnabar- and stibnite-bearing epithermal vein deposits are found throughout the Kuskokwim River region of southwestern Alaska. A geochemical orientation survey was carried out around several of these epithermal lodes to obtain information for planning regional geochemical surveys and to develop procedures which maximize the anomaly: threshold contrast of the deposits....
Arctic fox control improves nest success of black brant
R. Michael Anthony, Paul L. Flint, J.S. Sedinger
1991, Wildlife Society Bulletin (19) 176-184
A geodetic network in the Novarupta area, Katmai National Park, Alaska
J.W. Kleinman, E.Y. Iwatsubo
1991, Geophysical Research Letters (18) 1517-1519
A small geodetic network was established in 1989 and 1990 to monitor ground deformation in the Novarupta area, Katmai National Park, Alaska. Slope distances and zenith angles for three lines were repeated in 1990. A comparison of the two surveys indicates changes that are within the...
Erosion and accretion along the arctic coast of Alaska. The influence of ice and climate
Peter W. Barnes, Bonnie P. Rollyson
1991, Conference Paper, Coastal Sediments '91; Volume 2
Coastline comparison on 1951 and 1981 charts to determine erosion and accretion showed that ocean-facing coastal bluffs were retreating while deltas were rapidly expanding. Where the coast is fronted by a lagoon, and coast-parallel sand and gravel islands, bluff retreat was reduced. The extensive bluff erosion was volumetrically balanced by...
Mass sediment failure and transport features revealed by acoustic techniques, Beringian Margin, Bering Sea, Alaska
P.R. Carlson, Herman A. Karl, B. D. Edwards
1991, Marine Geotechnology (10) 33-51
Some of the largest single slide masses, including huge blocks tens of kilometers wide, occur on the rise of the central margin. Sliding of these blocks may have initiated the incision of some of the world's largest submarine canyons. One mass failure, particularly well defined by GLORIA, is 55 km...
Mitochondrial DNA in wildlife forensic science: Species identification of tissues
Matthew A. Cronin, Daniel A. Palmisciano, Ernest R. Vyse, David G. Cameron
1991, Wildlife Society Bulletin (19) 94-105
A common problem in wildlife law enforcement is identifying the species of origin of carcasses, meat, or blood when morphological characters such as hair or bones are not available. Immunological and protein electrophoretic (allozyme or general protein) procedures have been used in species identification with considerable success (Bunch et al....
Mitochondrial-DNA phylogeny of deer (Cervidae)
M. A. Cronin
1991, Journal of Mammalogy (72) 553-556
Mitochondrial-DNA restriction-site maps were constructed for several cervid taxa in the subfamilies Cervinae and Odocoileinae. Parsimony analyses of restriction sites and pair-wise analyses of genetic distances resulted in dendrograms congruent with the subfamily designations. Relationships within the Odocoileinae determined from genetic distances generally were concordant with those for nuclear-encoded...
Sources of aeromagnetic anomalies over Cement oil field (Oklahoma), Simpson oil field (Alaska), and the Wyoming-Idaho-Utah thrust belt
R. L. Reynolds, N.S. Fishman, M.R. Hudson
1991, Geophysics (56) 606-617
Geochemical and rock magnetic studies, undertaken to determine the causes of magnetic anomalies over Cement oil field (Anadarko basin, Oklahoma), Simpson oil field (North Slope basin, Alaska), and the Wyoming-Idaho-Utah thrust belt, have revealed different magnetic sources developed under different sedimentologic, geochemical, and structural settings.At Cement, ferrimagnetic pyrrhotite (Fe 7 S 8 ), typically...
Isotopic evidence for early Proterozoic age of the Idono Complex, west-central Alaska
Marti L. Miller, J.Y. Bradshaw, D.L. Kimbrough, T. W. Stern, T. K. Bundtzen
1991, Journal of Geology (99) 209-223
The Idono Complex of west-central Alaska is a fault-bounded, fragment of Early Proterozoic continental crust surrounded by overlap assemblages and younger terranes accreted in Mesozoic time. It is composed of granitic to dioritic orthogneiss, amphibolite, and metasedimentary rocks. Trace...
Energy dynamics, foraging ecology, and behavior of prenesting greater white-fronted geese
D.A. Budeau, John T. Ratti, Craig R. Ely
1991, Journal of Wildlife Management (55) 556-563
We collected greater white-fronted geese (Anser albifrons frontalis) on their nesting grounds on the Yukon-Kuskokwim Delta, Alaska, when they arrived and again before incubation during 1986 and 1987. Body mass, water content, crude fat, and crude protein increased in female geese between arrival and incubation onset in 1986 and 1987...
The last interglaciation in Alaska: Stratigraphy and paleoecology of potential sites
T. D. Hamilton, J. Brigham-Grette
1991, Quaternary International (10-12) 49-71
At least 20 localities in Alaska contain deposits that may provide information on the last interglaciation (Oxygen-Isotope Substage 5e). These widely dispersed localities include river bluffs, coastal bluffs and terraces, elevated marine shorelines, lake basins, and artificial excavations. Most of the inferred interglacial deposits contain macrofossils or pollen that are...