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- W332981736 abstract "There are several different approaches that can be utilized to reconstruct past variations in salinity. These can be grossly classified as ‘biological’ and ‘chemical.’ In the purely biological approach, one relates the distribution and relative abundance of certain species to salinity and makes an assumption that this empirical relationship has been the same in the past. The salinity gradients in the deep ocean are very small, so this approach has been mainly used to attempt to reconstruct surface salinity variations in the open ocean and changes in estuarine or coastal environments. Current methods of reconstructing past ocean salinity focus on using either direct measurements of past δ18O water (e.g., glacial pore-water δ18O) or independent paleotemperature proxies (e.g., alkenones, foraminiferal Mg/Ca, coral Sr/Ca, and faunal assemblages) to extract the past δ18O water signal from the δ18O carbonate record. Pore-water chlorinity measurements can be used to directly estimate glacial salinity. The indirect methods using biogeochemical proxies have the advantage over the direct pore-water estimates by facilitating time series and having the potential to document so-called abrupt climate change events at the submillennial to seasonal timescale. The reconstructed δ18O water record can then be deconvolved into its ice volume and salinity components." @default.
- W332981736 created "2016-06-24" @default.
- W332981736 creator A5036554035 @default.
- W332981736 date "2013-01-01" @default.
- W332981736 modified "2023-10-16" @default.
- W332981736 title "PALEOCEANOGRAPHY, PHYSICAL AND CHEMICAL PROXIES | Salinity Proxies δ18O" @default.
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- W332981736 doi "https://doi.org/10.1016/b978-0-444-53643-3.00295-8" @default.
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