Thermodynamic air-sea equilibration controls carbon isotopic composition of the South Atlantic thermocline during the last glacial period-Reference-Cited by-同舟云学术

Thermodynamic air-sea equilibration controls carbon isotopic composition of the South Atlantic thermocline during the last glacial period

Published:2023-10 Issue: Volume:229 Page:104223
ISSN:0921-8181
Container-title:Global and Planetary Change
language:en
Short-container-title:Global and Planetary Change

Author:

Pinho Tainã M.L.,Chiessi Cristiano M.,Campos Marília C.,Portilho-Ramos Rodrigo C.,Martínez-Méndez Gema,Venancio Igor M.,Nascimento Rodrigo A.,Crivellari Stefano,Albuquerque Ana L.S.,Arz Helge W.,Tiedemann Ralf,Bahr André,Mulitza Stefan

Funder

Fundação de Amparo à Pesquisa do Estado de São Paulo

CAPES

CNPq

FAPERJ

Alfred Wegener Institute for Marine and Polar Research

Publisher

Elsevier BV

Subject

Oceanography,Global and Planetary Change

Reference118 articles.

1. Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series;Anand;Paleoceanography,2003

2. Wind-driven upwelling in the southern ocean and the deglacial rise in atmospheric CO2;Anderson;Science,2009

3. Source waters contribution to the tropical Atlantic central layer: new insights on the Indo-Atlantic exchanges;Azar;Deep Sea Res. I Oceanogr. Res. Pap.,2021

4. A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry;Barker;Geochem. Geophys. Geosyst.,2003

5. Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation;Bauska;Proc. Natl. Acad. Sci.,2016

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