Barium isotope cycling in the marine environment: Pathways of fractionation and implications for paleoceanographic applications
Removal of particulate organic carbon (POC) from sunlit surface waters into the deep ocean represents a climatically important sink of atmospheric carbon dioxide (CO₂), linking the biogeochemical cycling of POC to CO₂-driven climate change. As POC is not well preserved in the sediment record, other...
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Massachusetts Institute of Technology
2022
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| Online Access: | https://hdl.handle.net/1721.1/144900 |