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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

Michael E. Weber

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

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.

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