Chemical measurements from the EPICA Dome C core
Sea ice and dust flux increased greatly in the Southern Ocean during the last glacial period. Palaeorecords provide contradictory evidence about marine productivity in this region, but beyond one glacial cycle, data were sparse. Here we present continuous chemical proxy data spanning the last eight...
Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2006
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.728218 https://doi.org/10.1594/PANGAEA.728218 |