Millennial-scale Iron Flux and Ocean Circulation Change Affects Subantarctic Pacific Carbon Cycling During Marine Isotope Stage 3 (57-29 ka)-Reference-Cited by-同舟云学术

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Millennial-scale Iron Flux and Ocean Circulation Change Affects Subantarctic Pacific Carbon Cycling During Marine Isotope Stage 3 (57-29 ka)

Published:2022-07-24 Issue: Volume: Page:
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Author:

Anderson Harris John¹^ORCID,Chase Zanna¹,Bostock Helen²^ORCID,Noble Taryn¹^ORCID,Shuttleworth Rachel³,Taiapa Bryn⁴,Chen Wen-Hui⁵^ORCID,Ren Haojia⁵,Jacobsen Geraldine E⁶^ORCID

Affiliation:

1. University of Tasmania

2. University of Queensland

3. University of Southampton

4. Victoria University

5. National Taiwan University

6. Australian Nuclear Science and Technology Organisation

Funder

Australian Research Council

Australian Nuclear Science and Technology Organisation

Publisher

Wiley

Reference264 articles.

1. Ahn J. & Brook E.J. 2008. "Atmospheric CO2 and Climate on Millennial

2. Time Scales During the Last Glacial Period." Science 322: 83-85.

3. Anderson H.J. Pedro J.B. Bostock H.C. Chase Z. & Noble T.L.

4. 2021. "Compiled Southern Ocean Sea Surface Temperatures Correlate

5. with Antarctic Isotope Maxima." Quaternary Science Reviews 255: 106821.

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