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Changes in the source of nutrients associated with oceanographic dynamics offshore southern Chile (41°S) over the last 25,000 years

Published online by Cambridge University Press:  20 January 2017

Thomas J. Verleye ,
Philippe Martinez ,
Rebecca S. Robinson  and
Stephen Louwye
Thomas J. Verleye*
Affiliation:
Research Unit Palaeontology, Department of Geology and Soil Science, Ghent University, Krijgslaan 281 S8/WE13, 9000 Ghent, Belgium Flanders Marine Institute (VLIZ), Wandelaarkaai 7, 8200 Oostende, Belgium
Philippe Martinez
Affiliation:
Université Bordeaux 1, UMR 5805 EPOC, avenue des facultés, 33405 Talence cedex, France
Rebecca S. Robinson
Affiliation:
Graduate School of Oceanography, University of Rhode Island, Narragansett, RI 02882, USA
Stephen Louwye
Affiliation:
Research Unit Palaeontology, Department of Geology and Soil Science, Ghent University, Krijgslaan 281 S8/WE13, 9000 Ghent, Belgium
*
*Corresponding author at: Research Unit Palaeontology, Department of Geology and Soil Science, Ghent University, Krijgslaan 281 S8/WE13, 9000 Ghent, Belgium. Fax: + 32 59 34 21 31. E-mail address:thomas.verleye@vliz.be (T.J. Verleye).
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Abstract

In order to obtain a better knowledge of past oceanographic variability offshore southern Chile, this study reappraises the changes in the sources of nutrients over the last 25 ka based on a detailed comparison of previously published nitrogen isotope and microfossil records (dinoflagellate cysts, coccoliths and diatoms) from ODP Site 1233 (41°S). Our findings support the main conclusions of Martinez et al. (2006) in the sense that both the Subantarctic Surface Water and the Gunther Undercurrent are potential sources for the recorded late Quaternary sedimentary δ15N signatures at Site 1233, with variable contributions of both sources during different time periods. This study indicates that Subantarctic Surface Water forms the main source for nutrients during the last glacial maximum (25–18.6 cal ka BP), the first part of the deglaciation (18.6–15.7 cal ka BP) and the Holocene (9.8 cal ka BP until present). An increased contribution of Equatorial Subsurface Water as a source of nutrients to the photic zone offshore southern Chile is observed between 14.4 and 9.8 cal ka BP, which is indicative for upwelling conditions at least after 13.2 cal ka BP as indicated by the microfossil data.

Keywords

δ15NMicrofossilsOceanographySoutheast PacificLate Quaternary
Type
Original Articles
Information
Quaternary Research , Volume 80 , Issue 3 , November 2013 , pp. 495 - 501
Copyright
University of Washington

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