Diatom isotope data and salinity reconstructions from ODP Site 887, subarctic northeast Pacific Ocean
Understanding the response of the climate to abrupt changes in the Earth system represents a key objective in paleoclimatology. Heinrich events in the last glacial, during which significant amounts of glacial discharge entered the North Atlantic Ocean, triggered the development of colder conditions...
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2020
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.925157 https://doi.org/10.1594/PANGAEA.925157 |