Authors

ORCID

Abstract

The Southern Ocean paleoceanography provides key insights into how iron fertilization and oceanic productivity developed through Pleistocene ice-ages and their role in influencing the carbon cycle. We report a high-resolution record of dust deposition and ocean productivity for the Antarctic Zone, close to the main dust source, Patagonia. Our deep-ocean records cover the last 1.5 Ma, thus doubling that from Antarctic ice-cores. We find a 5 to 15-fold increase in dust deposition during glacials and a 2 to 5-fold increase in biogenic silica deposition, reflecting higher ocean productivity during interglacials. This antiphasing persisted throughout the last 25 glacial cycles. Dust deposition became more pronounced across the Mid-Pleistocene Transition (MPT) in the Southern Hemisphere, with an abrupt shift suggesting more severe glaciations since ~0.9 Ma. Productivity was intermediate pre-MPT, lowest during the MPT and highest since 0.4 Ma. Generally, glacials experienced extended sea-ice cover, reduced bottom-water export and Weddell Gyre dynamics, which helped lower atmospheric CO2 levels.

Publication Date

2022-04-19

Publication Title

Nature Communications

Volume

13

Issue

1

ISSN

2041-1723

Acceptance Date

2022-03-25

Deposit Date

2022-04-27

Embargo Period

2022-04-29

Funding

We are very grateful to the captain, crew, and IODP staff that made IODP Expedition 382 (Iceberg Alley) and subsequent research successful. This research used samples and/ or data provided by the International Ocean Discovery Program (IODP). Funding for this research was provided by the Deutsche Forschungsgemeinschaft (DFG–Priority Programme 527, Grant We2039/17-1 (M.E.W.), a Natural Environmental Research Council (NERC) UK IODP grant NE/T006609/1 (I.B.), and the IODP U.S. Science Support Program (National Science Foundation prime award OCE-1450528) through Columbia University for all U.S.-based participants via subaward 97(GG009393).

Creative Commons License

Creative Commons Attribution 4.0 International License
This work is licensed under a Creative Commons Attribution 4.0 International License.

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