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Millennial‐Scale Carbon Flux Variability in the Subantarctic Pacific During Marine Isotope Stage 3 (57–29 Ka)

H. J. Anderson,Z. Chase,H. C. Bostock,T. L. Noble, R. Shuttleworth, B. Taiapa, W. H. Chen,H. Ren,G. E. Jacobsen

PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY(2024)

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Key words
Marine Isotope Stage 3,carbon cycle,biogeochemistry,paleoceanography,iron limitation,AMOC
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