Stable carbon and oxygen isotope ratios of foraminifera from North Atlantic sediments
Oxygen-18 records of benthic foraminifera from the Atlantic Ocean are significantly different from those of the Pacific and Indian Oceans indicating that the Glacial North Atlantic Deep Water was about 1.3°C cooler than today because different deep water sources appeared in the North Atlantic Ocean...
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Format: | Dataset |
Language: | English |
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PANGAEA
1982
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.726217 https://doi.org/10.1594/PANGAEA.726217 |