Dating monospecific and single-shell benthic foraminifera samples with a gas ion source: implications for the hypothetic release of ¹⁴C-depleted CO₂ from ocean midwaters into the atmosphere
Résumé
The evidence for very old intermediate waters during the glacial and deglaciation periods and their relationship with the evolution of atmospheric pCO₂ are still debated issues. The ¹⁴C-depletion of intermediate waters may be linked to the Dansgaard-Oeschger (DO) and Heinrich (H) events abrupt climatic changes, which affected the stratification and dynamics of the global ocean during the last glacial period.
Domaines
Sciences de la Terre
Format : Autre
Origine : Fichiers produits par l'(les) auteur(s)
Commentaire : Résumé
Origine : Fichiers produits par l'(les) auteur(s)
Commentaire : Résumé