Michael E. Weber
Decoupled dust deposition and ocean productivity in the Antarctic Zone of the Southern Ocean
Weber, Michael E.; Bailey, Ian; Hemming, Sidney; Martos, Yasmina M.; Reilly, Brendan; Ronge, Thomas A.; Brachfeld, Stefanie; Williams, Trevor; Raymo, Maureen; Belt, Simon T.; Smik, Lukas; Vogel, Hendrik; Peck, Victoria; Armbrecht, Linda; Cage, Alix; Bardillo, Fabricio G.; Du, Zhiheng; Fauth, Gerson; Fogwill, C.J.; García, Marga; Garnsworthy, Marlo; Glueder, Anna; Guitard, Michelle; Gutjahr, Marcus; Hernández-Almeida, Iván; Hoem, Frida; Hwang, Ji-Hwan; Iizuka, Mutsumi; Kato, Yuji; Kenlee, Bridget; Oconnell, Suzanne; Pérez, Lara F.; Seki, Osamu; Stevens, Lee; Tauxe, Lisa; Tripathi, Shubham; Warnock, Jonathan P; Zheng, Xufeng
Authors
Ian Bailey
Sidney Hemming
Yasmina M. Martos
Brendan Reilly
Thomas A. Ronge
Stefanie Brachfeld
Trevor Williams
Maureen Raymo
Simon T. Belt
Lukas Smik
Hendrik Vogel
Victoria Peck
Linda Armbrecht
Alix Cage a.g.cage@keele.ac.uk
Fabricio G. Bardillo
Zhiheng Du
Gerson Fauth
C.J. Fogwill
Marga García
Marlo Garnsworthy
Anna Glueder
Michelle Guitard
Marcus Gutjahr
Iván Hernández-Almeida
Frida Hoem
Ji-Hwan Hwang
Mutsumi Iizuka
Yuji Kato
Bridget Kenlee
Suzanne Oconnell
Lara F. Pérez
Osamu Seki
Lee Stevens
Lisa Tauxe
Shubham Tripathi
Jonathan P Warnock
Xufeng Zheng
Abstract
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 the first 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 ≥10-fold increase in dust deposition during glacials and a ≤5-fold increase in ocean productivity during interglacials. This antiphasing persisted throughout the last 25 glacial cycles. Dust deposition became more widespread across the Mid-Pleistocene Transition (MPT) and, at ~0.9 Ma, dominant ice-age cycles changed from 40,000 to 100,000-years, suggesting more severe glaciations thereafter. Productivity was intermediate pre-MPT, lowest during the MPT and highest since 0.4 Ma. Glacials experienced extended sea-ice cover, reduced bottom-water export and Weddell Gyre dynamics, which helped lower atmospheric CO2 levels.
Citation
Weber, M. E., Bailey, I., Hemming, S., Martos, Y. M., Reilly, B., Ronge, T. A., …Zheng, X. (2021). Decoupled dust deposition and ocean productivity in the Antarctic Zone of the Southern Ocean.
Conference Name | GeoKarlsruhe |
---|---|
Conference Location | Karlsruhe, Germany |
Start Date | Sep 19, 2021 |
End Date | Sep 24, 2021 |
Acceptance Date | Sep 19, 2021 |
Online Publication Date | Sep 19, 2021 |
Publication Date | Sep 19, 2021 |
Deposit Date | May 30, 2023 |
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