Articles | Volume 11, issue 7
https://doi.org/10.5194/cp-11-1009-2015
https://doi.org/10.5194/cp-11-1009-2015
Research article
 | 
31 Jul 2015
Research article |  | 31 Jul 2015

The Paleocene–Eocene Thermal Maximum at DSDP Site 277, Campbell Plateau, southern Pacific Ocean

C. J. Hollis, B. R. Hines, K. Littler, V. Villasante-Marcos, D. K. Kulhanek, C. P. Strong, J. C. Zachos, S. M. Eggins, L. Northcote, and A. Phillips

Viewed

Total article views: 4,676 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,664 1,827 185 4,676 508 206 237
  • HTML: 2,664
  • PDF: 1,827
  • XML: 185
  • Total: 4,676
  • Supplement: 508
  • BibTeX: 206
  • EndNote: 237
Views and downloads (calculated since 12 Feb 2015)
Cumulative views and downloads (calculated since 12 Feb 2015)
Latest update: 02 Dec 2025
Download
Short summary
Re-examination of a Deep Sea Drilling Project sediment core (DSDP Site 277) from the western Campbell Plateau has identified the initial phase of the Paleocene-Eocene Thermal Maximum (PETM) within nannofossil chalk, the first record of the PETM in an oceanic setting in the southern Pacific Ocean (paleolatitude of ~65°S). Geochemical proxies indicate that intermediate and surface waters warmed by ~6° at the onset of the PETM prior to the full development of the negative δ13C excursion.
Share