Planktonic foraminifera, nannofossils and stable isotope record across tghe Paleocene-Eocene thermal maximum of ODP Hole 113-690B, supplement to: Kelly, Daniel Clay; Zachos, James C; Bralower, Timothy J; Schellenberg, Stephen A (2005): Enhanced terrestrial weathering/runoff and surface ocean carbonate production during the recovery stages of the Paleocene-Eocene thermal maximum. Paleoceanography, 20(4), PA4023

• Main Authors: Kelly, Daniel Clay, Zachos, James C, Bralower, Timothy J, Schellenberg, Stephen A
• Format: Article in Journal/Newspaper
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2005
• Subjects: Drilling/drill rig; Leg113; Joides Resolution; Ocean Drilling Program ODP; Weddell Sea; Weddell; Kennett; Dickens; Planktonic foraminifera
• Online Access: https://dx.doi.org/10.1594/pangaea.836317; https://doi.pangaea.de/10.1594/PANGAEA.836317

The carbonate saturation profile of the oceans shoaled markedly during a transient global warming event known as the Paleocene-Eocene thermal maximum (PETM) (circa 55 Ma). The rapid release of large quantities of carbon into the ocean-atmosphere system is believed to have triggered this intense epis...