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Fish Remains from Homestead Cave and Lake Levels of the Past 13,000 Years in the Bonneville Basin

Published online by Cambridge University Press:  20 January 2017

Jack M. Broughton ,
David B. Madsen  and
Jay Quade
Jack M. Broughton
Affiliation:
Department of Anthropology, 270 S 1400 E RM 102, University of Utah, Salt Lake City, Utah 84112-0060
David B. Madsen
Affiliation:
Environmental Sciences, Utah Geological Survey, Salt Lake City, Utah 84114-6100
Jay Quade
Affiliation:
Department of Geosciences, Gould-Simpson Building, 1040 E 4th Street, University of Arizona, Tucson, Arizona 85721-0077
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Abstract

A late Quaternary ichthyofauna from Homestead Cave, Utah, provides a new source of information on lake history in the Bonneville basin. The fish, represented by 11 freshwater species, were accumulated between ∼11,200 and ∼1000 14C yr B.P. by scavenging owls. The 87Sr/86Sr ratio of Lake Bonneville varied with its elevation; 87Sr/86Sr values of fish from the lowest stratum of the cave suggest they grew in a lake near the terminal Pleistocene Gilbert shoreline. In the lowest deposits, a decrease in fish size and an increase in species tolerant of higher salinities or temperatures suggest multiple die-offs associated with declining lake levels. An initial, catastrophic, post-Provo die-off occurred at 11,300–11,200 14C yr B.P. and was followed by at least one rebound or recolonization of fish populations, but fish were gone from Lake Bonneville sometime before ∼10,400 14C yr B.P. This evidence is inconsistent with previous inferences of a near desiccation of Lake Bonneville between 13,000 and 12,000 14C yr B.P. Peaks in Gila atraria frequencies in the upper strata suggest the Great Salt Lake had highstands at ∼3400 and ∼1000 14C yr B.P.

Keywords

fish remainslake-level fluctuationsLake BonnevilleGreat Salt Laketerminal PleistoceneHolocene
Type
Research Article
Information
Quaternary Research , Volume 53 , Issue 3 , May 2000 , pp. 392 - 401
Copyright
University of Washington

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References

Bachhuber, F.W., (1989). The occurrence and paleolimnologic significance of cutthroat trout (Oncorhynchus clarki) in pluvial lakes of the Estancia Valley, central New Mexico. Geological Society of America Bulletin 101, 1543–1551.Google Scholar
Benson, L.V., Currey, D.R., Yong, L., Hostetler, S., (1992). Lake-size variations in the Lahontan and Bonneville basins between 13,000 and 9000 14C yr B.P. Palaeogeography, Palaeoclimatology, Palaeoecology 95, 19–32.Google Scholar
Bouchard, D.P., (1997). Quaternary Bear River Paleohydrogeography Reconstructed from the 87Sr/86Sr Composition of Lacustrine Fossils.Google Scholar
Bouchard, D.P., Kauffman, D.S., Hochberg, A., Quade, J., (1998). Quaternary history of the Thatcher Basin, Idaho, reconstructed from the 87Sr/86Sr and amino acid composition of lacustrine fossils: Implications for the diversion of the Bear River into the Bonneville Basin. Palaeogeography, Palaeoclimatology, Palaeoecology 141, 95–114.Google Scholar
Broughton, J.M., (2000). Terminal Pleistocene fish remains from Homestead Cave, Utah, and implications for fish biogeography in the Bonneville basin. Copeia.Google Scholar
Broughton, J.M., (2000). The Homestead Cave ichthyofauna. Madsen, D.B., Late Quaternary Paleoecology in the Bonneville Basin.Google Scholar
Charnov, E.L., (1993). Life History Invariants: Some Explorations of Symmetry in Evolutionary Ecology. Oxford University Press, Oxford.Google Scholar
Currey, D.R., (1990). Quaternary paleolakes in the evolution of semidesert basins, with emphasis on Lake Bonneville and the Great Basin, U.S.A. Palaeogeography, Palaeoclimatology Palaeoecology 76, 189–214.Google Scholar
Errington, P., Hammerstrom, F., Hammerstrom, F.N. Jr., (1940). The Great Horned Owl and its prey in north-central United States. Iowa Agricultural Experiment Station Research Bulletin 277, 757–850.Google Scholar
Gallup, F.N., (1949). Banding recoveries of Tyto alba . Bird-Banding 20, 150.Google Scholar
Gilbert, G.K., (1890). Lake Bonneville.Google Scholar
Grayson, D.K., (1998). Moisture history and small mammal community richness during the latest Pleistocene and Holocene, northern Bonneville Basin, Utah. Quaternary Research 49, 330–334.Google Scholar
Hubbs, C.L., Miller, R.R., (1948). Zoological evidence: Correlation between fish distribution and hydrographic history in the desert basins of the western United States. In The Great Basin, with Emphasis on Glacial and Postglacial Times. p. 17–144.Google Scholar
Jobling, M., (1981). Temperature tolerance and the final preferendum—Rapid methods for the assessment of optimum growth temperatures. Journal of Fish Biology 19, 439–455.Google Scholar
Jones, L.M., Faure, G., (1972). Strontium isotope geochemistry of Great Salt Lake, Utah. Geological Society of America Bulletin 83, 1875–1880.Google Scholar
Livingston, S., (2000). The Homestead Cave avifauna. Madsen, D.B., Late Quaternary Paleoecology in the Bonneville Basin Utah Geological Survey Bulletin, .Google Scholar
Madsen, D.B., (2000). Utah Geological Survey Bulletin. Late Quaternary Paleoecology in the Bonneville Basin.Google Scholar
Marti, C., (1992). Birds of North America. Barn Owl Philadelphia Academy of Sciences, .Google Scholar
McKenzie, J.A., Eberli, G.P., (1987). Indications for abrupt Holocene climatic change: Late Holocene oxygen isotope stratigraphy of the Great Salt Lake, Utah. Berger, H.W., Labeyrie, L.D., Abrupt Climate Change Reidel, Dordrecht.127–136.Google Scholar
Mehringer, P.J. Jr., (1985). In Pollen Records of Late-Quaternary North American Sediments Late-Quaternary pollen records from the interior Pacific Northwest and northern Great Basin of the United States. Bryant, V.M., American Association of Stratigraphic Palynologists Foundation, 167–189.Google Scholar
Murchison, S.B., (1989). Fluctuation History of the Great Salt Lake, Utah, During the Last 13,000 Years.Google Scholar
Oviatt, C.G., (1997). Lake Bonneville fluctuations and global climate change. Geology 25, 155–158.Google Scholar
Oviatt, C.G., Currey, D.R., Sack, D., (1992). Radiocarbon chronology of Lake Bonneville, eastern Great Basin, U.S.A. Palaeogeography, Palaeoclimatology, Palaeoecology 99, 225–241.Google Scholar
Quade, J., (2000). 87Sr/86Sr (strontium) and Lake Bonneville chronostratigraphy. Madsen, D.B., Late Quaternary Paleoecology in the Bonneville Basin.Google Scholar
Quade, J., (2000). Strontium ratios and the origin of the early Homestead Cave biota. In Late Quaternary Paleoecology in the Bonneville Basin. (Madsen, D.B., Ed.), Vol. 130, Utah Geological Survey Bulletin, in press.Google Scholar
Rhode, D., Madsen, D.B., (1995). Late Wisconsin/early Holocene vegetation in the Bonneville Basin. Quaternary Research 44, 246–256.Google Scholar
Robins, C.R., Bailey, R.M., Bond, C.E., Brooker, J.R., Lachner, E.A., Lea, R.N., Scott, W.B., (1991). Common and Scientific Names of Fishes from the United States and Canada.Google Scholar
Roff, D.A., (1984). The evolution of life history parameters in teleosts. Canadian Journal of Fisheries and Aquatic Sciences 41, 989–1000.Google Scholar
Rosenfeld, M.J., (1991). Systematic Studies of Members of the Genus Gila (Pisces: Cyprinidae) from the Great Basin and Colorado River: Protein Electrophoretic and Cytogenetic Variation.Google Scholar
Schmitz, B., Aberg, G., Werdilin, L., Forey, P., Bendix-Almgren, S.E., (1991). 87Sr/86Sr, Na, Na, F, Sr, and La in skeletal fish debris as a measure of the paleosalinity of fossil-fish habitats. Geological Society of America Bulletin 103, 786–794.Google Scholar
Sigler, W.F., Sigler, J.W., (1996). Fishes of Utah: A Natural History. University of Utah Press, Salt Lake City.Google Scholar
Smith, D.G., (1971). Population Dynamics, Habitat Selection, and Partitioning of Breeding Raptors in the Eastern Great Basin of Utah. Brigham Young University, Provo.Google Scholar
Smith, G.R., (1981). Effects of habitat size on species richness and adult body size of desert fishes. Naiman, R.J., Soltz, D.L., Fishes in North American Deserts Wiley, New York.125–171.Google Scholar
Smith, G.R., Stokes, W.L., Horn, K.F., (1968). Some late Pleistocene fishes of Lake Bonneville. Copeia 1968, 807–816.Google Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, G., van der Plicht, J., Spurk, M., (1998). INTCAL98 radiocarbon age calibration, 24,000–0 cal BP. Radiocarbon 40, 1041–1084.Google Scholar
Thompson, R.S., Toolin, L.J., Forester, R.M., Spencer, R.J., (1990). Accelerator-mass spectrometer (AMS) radiocarbon dating of Pleistocene lake sediments in the Great Basin. Palaeogeography, Palaeoclimatology, Palaeoecology 78, 301–313.Google Scholar
Vigg, S.C., Koch, D.L., (1980). Upper lethal temperature range of Lahontan cutthroat trout in waters of different ionic concentrations. Transactions of the American Fisheries Society 109, 336–339.Google Scholar
Westenfelder, C., Birch, F.M., Baranowski, R.L., Rosenfeld, M.J., Shiozawa, D.K., Kablitz, C., (1988). Atrial natriuretic factor and salt adaptation in the teleost fish Gila atraria . American Journal of Physiology 256, F1281–F1286.Google Scholar
Wydoski, R.S., Whitney, R.R., (1979). Inland Fishes of Washington. University of Washington Press, Seattle.Google Scholar
Zachary, C.G., Oviatt, C.G., (1999). Paleoenvironmental changes during the late-Pleistocene transition from Lake Bonneville to Great Salt Lake. Geological Society of America Abstracts with Programs 31, 55.Google Scholar