δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2
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...
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| Autores principales: | Campos, M.C., Chiessi, C.M., Voigt, I., Piola, A.R., Kuhnert, H., Mulitza, S. |
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| Formato: | JOUR |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_18149324_v13_n4_p345_Campos |
| Aporte de: |
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