Multiproxy record of abrupt sea-surface cooling across the Eocene-Oligocene transition in the Gulf of Mexico

• Published in: Geology
• Main Authors: Wade, Bridget S, Houben, Alexander JP, Quaijtaal, Willemijn, Schouten, Stefan, Rosenthal, Yair, Miller, Kenneth G, Katz, Miriam E, Wright, James D, Brinkhuis, Henk
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2012
• Subjects: Earth and Environmental Sciences; CLIMATE TRANSITION; ISOPRENOID TETRAETHER LIPIDS; TEMPERATURE; ICE; BOUNDARY; FORAMINIFERA; GLACIATION; ISOTOPES; ALABAMA; NORTH; Antarctic; Alabama; Antarc*
• Online Access: https://biblio.ugent.be/publication/3098187; http://hdl.handle.net/1854/LU-3098187; https://doi.org/10.1130/G32577.1; https://biblio.ugent.be/publication/3098187/file/3106134

The Eocene-Oligocene transition (EOT; ca. 33-34 Ma) was a time of pronounced climatic change, marked by the establishment of continental-scale Antarctic ice sheets. The timing and extent of temperature change associated with the EOT is controversial. Here we present multiproxy EOT climate records (similar to 15-34 k.y. resolution) from St. Stephens Quarry, Alabama, USA, derived from foraminiferal Mg/Ca, delta O-18, and TEX86. We constrain sea-surface temperatures (SSTs) in the latest Eocene and early Oligocene and address the issue of climatic cooling during the EOT. Paleotemperatures derived from planktic foraminifera Mg/Ca and TEX86 are remarkably consistent and indicate late Eocene subtropical SSTs of >28 degrees C. There was substantial and accelerated cooling of SSTs (3-4 degrees C) through the latest Eocene "precursor" delta O-18 shift (EOT-1), prior to Oligocene Isotope-1 (Oi-1). Our multispecies planktic foraminiferal delta O-18 records diverge at the E/O boundary (33.7 Ma), signifying enhanced seasonality in the earliest Oligocene in the Gulf of Mexico.