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Paleoceanographic changes in the Eastern Equatorial Pacific over the last 10 Myr

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Please use this identifier to cite or link to this item:http://hdl.handle.net/2115/52111

Title: Paleoceanographic changes in the Eastern Equatorial Pacific over the last 10 Myr
Authors: Seki, Osamu Browse this author →KAKEN DB
Schmidt, Daniela N. Browse this author
Schouten, Stefan Browse this author
Hopmans, Ellen C. Browse this author
Damsté, Jaap S. Sinninghe Browse this author
Pancost, Richard D. Browse this author
Keywords: TEX86
Tropical Pacific
alkenone
diol index
Issue Date: 1-Sep-2012
Publisher: American Geophysical Union
Journal Title: Paleoceanography
Volume: 27
Issue: 3
Start Page: PA3224
Publisher DOI: 10.1029/2011PA002158
Abstract: To examine the Late Neogene evolution of tropical Pacific oceanography, we determined multiple geochemical proxy records for temperature (U37^[K'] and TEX86^[H] indices) and primary productivity (algal biomarkers and diol indices) in sediments recovered at ODP Site 1241 in the East Equatorial Pacific (EEP) spanning a record of the last 10 Myr. The TEX86^[H] temperatures are lower than those recorded by U37^[K'] indices, exhibiting large fluctuations and suggesting strong warming during the Mid Pliocene Warm Period (MPWP; 4.5-3.2 Ma) and significantly colder temperature during the Late Miocene cooling period (7-5 Ma) and after the Middle Pliocene Warm Period (MPWP). Such variations could reflect changes in the EEP thermocline temperatures, but we suggest that they instead reflect changes in the depth of export production of glycerol dialkyl glycerol tetraether lipids in response to changes in the upper ocean structure. A combination of temperature records, inferred to represent different and likely varying depths in the water column, as well as algal biomarker records for export production and ecosystem structure, suggest that both productivity and inference upwelling were reduced in the EEP during warmer periods, such as the MPWP and prior to 7 Ma. In contrast, stronger upwelling conditions and associated increased productivity likely prevailed from 7 to 5 Ma and for the past 3 Myr, both corresponding to globally cool intervals. A further increase in EEP productivity occurred at ca 1.8 Ma, coincident with the development of the E-W Pacific SST gradient. These results confirm previous work that protracted El Niño-like conditions prevailed during warmer intervals of the Pliocene before ultimately descending into the current climate state.
Rights: ©2012 American Geophysical Union
Type: article
URI: http://hdl.handle.net/2115/52111
Appears in Collections:低温科学研究所 (Institute of Low Temperature Science) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

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