Authigenic uranium, mass accumulation rates, benthic δ¹³C and SST during the last interglacial period of ODP Site 177-1094
Southern Ocean sediments reveal a spike in authigenic uranium 127,000 years ago, within the last interglacial, reflecting decreased oxygenation of deep water by Antarctic Bottom Water (AABW). Unlike ice age reductions in AABW, the interglacial stagnation event appears decoupled from open ocean condi...
Main Authors: | , , , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2014
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.839454 https://doi.org/10.1594/PANGAEA.839454 |