Extreme warming of mid-latitude coastal ocean during the Paleocene-Eocene Thermal Maximum; inferences from TEX86 and isotope data

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doi: 10.1130/G22522.1
Author(s): Zachos, J. C.; Schouten, S.; Bohaty, S.; Quattlebaum, T.; Sluijs, A.; Brinkhuis, H.; Gibbs, S. J.; Bralower, T. J.
Author Affiliation(s): Primary:
University of California at Santa Cruz, Earth Sciences Department, Santa Cruz, CA, United States
Other:
Royal Netherlands Institute for Sea Research, Netherlands
Utrecht University, Netherlands
Pennsylvania State University, United States
Volume Title: Geology (Boulder)
Source: Geology (Boulder), 34(9), p.737-740. Publisher: Geological Society of America (GSA), Boulder, CO, United States. ISSN: 0091-7613 CODEN: GLGYBA
Note: In English. With GSA Data Repository Item 2006155. 27 refs.; illus., incl. strat. cols., sketch map
Summary: Changes in sea surface temperature (SST) during the Paleocene-Eocene Thermal Maximum (PETM) have been estimated primarily from oxygen isotope and Mg/Ca records generated from deep-sea cores. Here we present a record of sea surface temperature change across the Paleocene-Eocene boundary for a nearshore, shallow marine section located on the eastern margin of North America. The SST record, as inferred from TEX86 data, indicates a minimum of 8°C of warming, with peak temperatures in excess of 33°C. Similar SSTs are estimated from planktonic foraminifer oxygen isotope records, although the excursion is slightly larger. The slight offset in the oxygen isotope record may reflect on seasonally higher runoff and lower salinity.
Year of Publication: 2006
Research Program: ODP Ocean Drilling Program
Key Words: 12 Stratigraphy, Historical Geology and Paleoecology; Algae; Atlantic Coastal Plain; Case studies; Cenozoic; Climate change; Cores; Dinoflagellata; Eocene; Foraminifera; Gloucester County New Jersey; Greenhouse effect; Invertebrata; Isotope ratios; Isotopes; Lacustrine environment; Lake sediments; Leg 150X; Leg 174AX; Lower Eocene; Marine sediments; Microfossils; Nannofossils; New Jersey; O-18/O-16; Ocean Drilling Program; Oxygen; PETM; Paleocene; Paleocene-Eocene Thermal Maximum; Paleoclimatology; Paleogene; Paleotemperature; Palynomorphs; Planktonic taxa; Plantae; Protista; SEM data; Sea-surface temperature; Sediments; Stable isotopes; Tertiary; United States; Upper Paleocene; Wilson Lake
Coordinates: N393900 N393900 W0750300 W0750300
Record ID: 2006071520
Copyright Information: GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data supplied by the Geological Society of America, Boulder, CO, United States