(Table 1) Age determination of western North Atlantic sediment cores
Foraminiferal abundance, 14C ventilation ages, and stable isotope ratios in cores from high deposition rate locations in the western subtropical North Atlantic are used to infer changes in ocean and climate during the Younger Dryas (YD) and Last Glacial Maximum (LGM). The d18O of the surface dwellin...
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Format: | Dataset |
Language: | English |
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PANGAEA
2004
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.837767 https://doi.org/10.1594/PANGAEA.837767 |