Stable oxygen and carbon isotopic composition of foraminifera and sea water from the Arctic Ocean
O18/O16 data on a depth profile of water samples from the Arctic Ocean reveal that near surface water is depleted in O18 by about 4 per mil, but water at depths greater than 350 meters reaches near normal open ocean water composition. The O18 profile very closely follows the salinity profile, with d...
| Main Authors: | , |
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| Format: | Dataset |
| Language: | English |
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PANGAEA
1969
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| Subjects: | |
| Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.730373 https://doi.org/10.1594/PANGAEA.730373 |