δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2

• Published in: Climate of the Past
• Main Authors: Campos, Marília C., Mazur Chiessi, Cristiano, Voigt, Ines, Piola, Alberto Ricardo, Kuhnert, Henning, Mulitza, Stefan
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications
• Subjects: Planktonic Foraminifera; Stable Carbon Isotopes; Heinrich Stadials; Southern Ocean; https://purl.org/becyt/ford/1.5; https://purl.org/becyt/ford/1; Ricardo; North Atlantic; Planktonic foraminifera
• Online Access: http://hdl.handle.net/11336/72736

Abrupt millennial-scale climate change events of the last deglaciation (i.e. Heinrich Stadial 1 and the Younger Dryas) were accompanied by marked increases in atmospheric CO2 (CO2atm) and decreases in its stable carbon isotopic ratios (δ13C), i.e. δ13CO2atm, presumably due to outgassing from the oce...