Trace metal evidence for a poorly ventilated glacial Southern Ocean
Glacial benthic δ 13 C and Δ 14 C measurements from the Atlantic Ocean have been interpreted to indicate the existence of a poorly ventilated Southern Ocean with greater CO 2 and nutrient contents compared to present. Enhanced storage of CO 2 in the deep ocean predicts that oxygen concentrations sho...
| Main Authors: | , |
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| Format: | Text |
| Language: | English |
| Published: |
2018
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| Subjects: | |
| Online Access: | https://doi.org/10.5194/cpd-11-637-2015 https://cp.copernicus.org/preprints/cp-2014-148/ |
| Summary: | Glacial benthic δ 13 C and Δ 14 C measurements from the Atlantic Ocean have been interpreted to indicate the existence of a poorly ventilated Southern Ocean with greater CO 2 and nutrient contents compared to present. Enhanced storage of CO 2 in the deep ocean predicts that oxygen concentrations should have declined at the same time, although no unequivocal evidence for glacial Southern Ocean suboxia has yet been found. Here we take a novel approach by using concentrations of redox-sensitive trace metals to show that Southern Ocean sediments from two cores in the Atlantic sector were suboxic during deglaciation and the last glacial period, implying reduced ventilation and/or elevated export production that significantly altered deep water chemistry. In the Cape Basin, high concentrations of the authigenically deposited trace metal Re coincide with oldest Δ 14 C values at 3.8 km water depth in the Subantarctic Zone, indicating that poorest Southern Ocean ventilation occurred during the Last Glacial Maximum (~ 23–19 ka). Furthermore, trace metal results suggest that the vertical structure of the glacial Southern Ocean differed from modern deep water mass arrangement such that Lower Circumpolar Deep Water had lower O 2 concentrations, and therefore was the likely reservoir of glacial CO 2 . |
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