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- W45211871 abstract "Abstract As important palaeoenvironmental proxies, non-marine ostracods provide several independent lines of evidence of palaeoclimatic and hydrological change in Quaternary records. Species diversity, biogeography, ecology and shell geochemistry (δ18O, δ13C, Mg/Ca, Sr/Ca and 87Sr/86Sr) are all potential sources of information concerning past environmental conditions. However, often there is not a strong covariance between changes in species assemblages and their corresponding suite of geochemical measurements; that is, in some records, there is little change in the shell geochemistry, whereas the species assemblages show significant change, and vice versa. Thus, multivariate statistical analyses used to develop transfer functions or modern analogues, based upon species assemblages, may or may not correspond to changes in the shell geochemistry. However, this lack of covariance is in itself informative and by examining the observed changes in ostracod shell geochemical measurements and species assemblages, it is possible to identify and track process dynamics in palaeolimnological records." @default.
- W45211871 created "2016-06-24" @default.
- W45211871 creator A5069961351 @default.
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- W45211871 date "2012-01-01" @default.
- W45211871 modified "2023-10-01" @default.
- W45211871 title "The Versatility of Quaternary Ostracods as Palaeoclimate Proxies" @default.
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- W45211871 doi "https://doi.org/10.1016/b978-0-444-53636-5.00011-1" @default.
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