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  4. Pliocene mixed-layer oceanography for site 1241, using combined Mg/Ca and δ18O analyses of Globigerinoides sacculifer
 
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Pliocene mixed-layer oceanography for site 1241, using combined Mg/Ca and δ18O analyses of Globigerinoides sacculifer

Journal
Proceedings of the Ocean Drilling Program: Scientific Results
Journal Volume
202
Date Issued
2006
Author(s)
JEROEN GROENEVELD  
Steph S
Tiedemann R
Garbe-Schönberg D
Nürnberg D
Sturm A.
DOI
10.2973/odp.proc.sr.202.209.2006
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-67849111583&doi=10.2973%2fodp.proc.sr.202.209.2006&partnerID=40&md5=dc04f6ab9cc03fc409c01cc247cea0e5
https://scholars.lib.ntu.edu.tw/handle/123456789/624813
Abstract
To reconstruct changes in tropical Pacific surface hydrography, we used samples from Site 1241 (5°50'N, 86°26'W; 2027-m water depth) to establish high-resolution records of Mg/Ca and δ18O for the mixed-layer dwelling planktonic foraminifer Globigerinoides sacculifer for the Pliocene time interval from 4.8 to 2.4 Ma. An increase in average sea-surface temperatures (SSTs) (24.5°-25.5°C) between 4.8 and 3.7 Ma can probably be explained by a southward shift of the Intertropical Convergence Zone, thereby increasing the influence of the warmer North Equatorial Countercurrent. The general global cooling trend, a response to intensification of Northern Hemisphere glaciation (NHG), started at ~3.2 Ma (shown by the δ18Obenthic record) and is paralleled by tropical east Pacific cooling (indicated by SSTMg/Ca). Tropical east Pacific cooling, however, had already commenced by ~3.7 Ma, suggesting that global cooling, probably related to decreasing atmospheric CO2 concentrations, might have started well before intensification of NHG. Relative changes in local sea-surface salinity (indicated by δ18Osalinity) show a decoupling from global high-latitude processes (shown by the δ18Obenthic record). Long-term regional freshening started with decreasing SSTMg/Ca at ~3.7 Ma, suggesting that changes in the tropical wind field combined with latitudinal shifts of the tropical rainbelt were related to general decreases in tropical east Pacific SST-controlled δ18Osalinity. The similarity of Pliocene SSTMg/Ca for G. sacculifer with modern SSTs in the east Pacific, in combination with the early development of a shallow thermocline at Site 1241, gives no direct support to the idea that a permanent El Niño-like Pliocene climate might have existed during the early Pliocene.
Other Subjects
Foraminifera; Globigerinoides sacculifer
Type
journal article

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