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- W2021231411 abstract "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 14 C yr B.P. by scavenging owls. The 87 Sr/ 86 Sr ratio of Lake Bonneville varied with its elevation; 87 Sr/ 86 Sr 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 14 C 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 14 C yr B.P. This evidence is inconsistent with previous inferences of a near desiccation of Lake Bonneville between 13,000 and 12,000 14 C yr B.P. Peaks in Gila atraria frequencies in the upper strata suggest the Great Salt Lake had highstands at ∼3400 and ∼1000 14 C yr B.P." @default.
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- W2021231411 date "2000-05-01" @default.
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- W2021231411 title "Fish Remains from Homestead Cave and Lake Levels of the Past 13,000 Years in the Bonneville Basin" @default.
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- W2021231411 doi "https://doi.org/10.1006/qres.2000.2133" @default.
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