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Lookup NU author(s): Benjamin Petrick, Dr Erin McClymont, Sonja Felder, Dr Antoni Rosell-Mele
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The Late Pliocene has been proposed as a possible analogue for understanding future climate change and for testing climate models. Previous work has shown that during the Pliocene the major upwelling systems were relatively warm, and that this meant they were either inactive, contracted, or were upwelling warmer waters than present. Here, we examine evidence from a site located on the margins of the modem Benguela Upwelling system to test whether the upwelling cells had migrated or contracted relative to present during the Pliocene. We applied several organic geochemistry proxies and foraminiferal analyses to reconstruct the Pliocene history of ODP Site 1087 (31 degrees 28'S, 15 degrees 19'E, 1374 m water depth), including the U-37(K)' and TEX86 indices (for reconstructing sea surface temperatures), phytoplankton biomarker concentrations and stable isotope ratios (for estimating export primary productivity, and for oxygen isotope statigraphy), and planktonic foraminifera assemblage abundances (for inferring water mass changes). These proxies show that, between 3.5 and 3.0 Ma, the southern Benguela region was cooler than the northern Benguela region by 5 degrees C, the latter being where the main upwelling cells are found today. From the multiproxy data obtained, we also infer that more extensive upwelling was present in the southern Benguela region during the Pliocene than at present, and that the Benguela Upwelling cells shifted northwards after the Pliocene epoch as a result of changes in the local wind field. We also find evidence that the Benguela Upwelling was sensitive to the pronounced cooling during the M2 and KM2 glacial stages, potentially associated with the expansion of sea ice and cooling in Antarctica in the Late Pliocene. (C) 2015 Elsevier B.V. All rights reserved.
Author(s): Petrick B, McClymont EL, Felder S, Rueda G, Leng MJ, Rosell-Mele A
Publication type: Article
Publication status: Published
Journal: Palaeogeography, Palaeoclimatology, Palaeoecology
Year: 2015
Volume: 429
Pages: 62-71
Print publication date: 01/07/2015
Online publication date: 08/04/2015
Acceptance date: 29/03/2015
ISSN (print): 0031-0182
ISSN (electronic): 1872-616X
Publisher: Elsevier BV
URL: http://dx.doi.org/10.1016/j.palaeo.2015.03.042
DOI: 10.1016/j.palaeo.2015.03.042
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