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- W2109362435 abstract "Geographical variations of radiogenic isotopes in seawater, through time, have the potential to provide information on changes in erosional input and ocean circulation patterns, and their relation to tectonic and climatic events. For those elements which have a long residence time, such as Sr, the oceans are isotopically uniform on a global scale, and the geographical source of any chemical or isotopic variations can not be easily identified. By comparison, the residence times of Nd and Os are sufficiently short that both systems have the capability to respond, in phase, to short term fluctuations in input (Richter and Turekian, 1993). Foraminifera potentially offer a high-resolution radiogenic isotope record, amenable to precise biostratigraphic or isotopic dating, that can be directly related to the stable isotope, trace metal, and palaeoenvironmental information from the same material. This study presents Sr-Os-Nd isotopic variations recorded by foraminifera for the past 150 ka from ODP site 758 in the North East Indian ocean. This locality is of particular interest because it potentially preserves not only a record of the composition of seawater accompanying climate change, but also the local effects of continental erosion from the Himalaya-Tibet region." @default.
- W2109362435 created "2016-06-24" @default.
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- W2109362435 date "1998-01-01" @default.
- W2109362435 modified "2023-10-18" @default.
- W2109362435 title "Seawater Sr-Nd-Os Isotope Variations Recorded by Foraminifera Over the Last 150 Kyrs" @default.
- W2109362435 cites W2023333296 @default.
- W2109362435 cites W2060463021 @default.
- W2109362435 doi "https://doi.org/10.1180/minmag.1998.62a.1.140" @default.
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