Last Glacial Maximum and deglacial abyssal seawater oxygen isotopic ratios
An earlier analysis of pore-water salinity (chlorinity) in two deep-sea cores, using terminal constraint methods of control theory, concluded that although a salinity amplification in the abyss was possible during the LGM, it was not required by the data. Here the same methodology is applied to <...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2016-06-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/12/1281/2016/cp-12-1281-2016.pdf |