Late Paleocene to Eocene paleoceanography of the Equatorial Pacific Ocean; stable isotopes recorded at Ocean Drilling Program Site 865, Allison Guyot

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doi: 10.1029/95PA01143
Author(s): Bralower, Timothy J.; Zachos, James C.; Thomas, Ellen; Parrow, Matthew; Paull, Charles K.; Kelly, D. Clay; Premoli Silva, Isabella; Sliter, William V.; Lohmann, Kyger C.
Author Affiliation(s): Primary:
University of North Carolina, Department of Geology, Chapel Hill, NC, United States
University of California at Santa Cruz, United States
Yale University, United States
Universita di Milano, Italy
U. S. Geological Survey, United States
University of Michigan, United States
Volume Title: Paleoceanography
Source: Paleoceanography, 10(4), p.841-865. Publisher: American Geophysical Union, Washington, DC, United States. ISSN: 0883-8305 CODEN: POCGEP
Note: In English. 91 refs.; illus., incl. 3 tables, sketch map
Summary: An expanded and largely complete upper Paleocene to upper Eocene section was recovered from the pelagic cap overlying Allison Guyot, Mid-Pacific Mountains at Ocean Drilling Program (ODP) Site 865 (18°26'N, 179°33'W; paleodepth 1300-1500 m). Reconstructions show that the site was within a few degrees of the equator during the Paleogene. Because no other Paleogene sections have been recovered in the Pacific Ocean at such a low latitude, Site 865 provides a unique record of equatorial Pacific paleoceanography. Detailed stable isotopic investigations were conducted on three planktonic foraminiferal taxa (species of Acarinina, Morozovella, and Subbotina). We studied benthic foraminiferal isotopes at much lower resolution on species of Cibicidoides and Lenticulina, Nuttallides truempyi and Gavelinella beccariiformis, because of their exceptional rarity. The δ18O and δ13C stratigraphies from Site 865 are generally similar to those derived from other Paleocene and Eocene sections. The planktonic foraminiferal records at Site 865, however, include significantly less short-term, single-sample variability than those from higher-latitude sites, indicating that this tropical, oligotrophic location had a comparatively stable water column structure with a deep mixed layer and less seasonal variability. Low-amplitude (0.1-0.8 per mil) oscillations on timescales of 250,000 to 300,000 years correlate between the δ13C records of all planktonic taxa and may represent fluctuations in the mixing intensity of surface waters. Peak sea surface temperatures of 24°-25°C occurred in the earliest Eocene, followed by a rapid cooling of 3-6°C in the late early Eocene. Temperatures remained cool and stable through the middle Eocene. In the late Eocene, surface water temperatures decreased further. Vertical temperature gradients decreased dramatically in the late Paleocene and were relatively constant through much of the Eocene but increased markedly in the late Eocene. Intermediate waters warmed through the late Paleocene, reaching a maximum temperature of 10°C in the early Eocene. Cooling in the middle and late Eocene paralleled that of surface waters, with latest Eocene temperatures below 5°C. Extinction patterns of benthic foraminifera in the latest Paleocene were similar to those observed at other Pacific sites and were coeval with a short-term, very rapid negative excursion in δ13C values in planktonic and benthic taxa as at other sites. During this excursion, benthic foraminiferal δ18O values decreased markedly, indicating warming of 4 to 6°C for tropical intermediate waters, while planktonic taxa show slight warming (1°C) followed by 2°C of cooling. Convergence of δ18O values of planktonic and benthic foraminifera suggests that thermal gradients in the water column in this tropical location collapsed during the excursion. These data are consistent with the hypothesis that equatorial Pacific surface waters were a potential source of warm, higher salinity waters which filled portions of the deep ocean in the latest Paleocene. Oxygen isotopic data indicate that equator to high southern latitude sea surface thermal gradients decreased to as little as 4°C at the peak of the excursion, suggesting some fundamental change in global heat transport. Copyright 1995 by the American Geophysical Union.
Year of Publication: 1995
Research Program: ODP Ocean Drilling Program
Key Words: 12 Stratigraphy, Historical Geology and Paleoecology; Allison Seamount; Benthic taxa; C-13/C-12; Carbon; Cenozoic; Eocene; Equatorial Pacific; Foraminifera; Geothermal gradient; Heat flow; Invertebrata; Isotope ratios; Isotopes; Leg 143; Microfossils; Mid-Pacific Mountains; North Pacific; O-18/O-16; ODP Site 865; Ocean Drilling Program; Oxygen; Pacific Ocean; Paleo-oceanography; Paleocene; Paleoclimatology; Paleogene; Paleotemperature; Planktonic taxa; Protista; Stable isotopes; Tertiary; Thermal history; Upper Paleocene
Coordinates: N182624 N182626 W1793320 W1793321
Record ID: 1997026650
Copyright Information: GeoRef, Copyright 2019 American Geosciences Institute.