The Southwest Pacific during the Pliocene: a reply to Dickens and Backman, 2011.

Karas, Cyrus, Nürnberg, Dirk and Tiedemann, Ralf (2012) The Southwest Pacific during the Pliocene: a reply to Dickens and Backman, 2011. Earth and Planetary Science Letters, 331-332 . pp. 360-363. DOI 10.1016/j.epsl.2012.03.006.

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Abstract

Introduction
In a comment on our recent paper (Karas et al., 2011a) Dickens and Backman argue that our interpretation of planktonic δ18O and Mg/Ca data from the southwestern Pacific DSDP Site 590B for the time period 5.0 to 4.3 Ma is difficult to reconcile with previous notions on early Pliocene upwelling phenomena and subsequent surface warming at the same site. Our study for the first time presented Pliocene Mg/Ca-derived temperatures and δ18Oivc-seawater values approximating changes in salinities at Site 590B for both surface and subsurface levels. It is hitherto the only study, which reconstructs absolute temperatures for the Pliocene with a substantially higher time resolution (~ 9 kyrs) than previous geochemical and faunal records from Site 590 (e.g., ~ 250 kyrs in Elmstrom and Kennett, 1986; [Grant and Dickens, 2002] and [Kennett and von der Borch, 1986]). Here, we attempt to address the issues raised by Dickens and Backman and synthesize the so far diverging interpretations in order to support the reliability of our study.

Document Type: Article
Keywords: Paleoceanography; Southwest Pacific; Pliocene; Foraminiferal Mg/Ca; Ocean gateways
Research affiliation: AWI
OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-P-OZ Paleo-Oceanography
OceanRep > The Future Ocean - Cluster of Excellence
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1016/j.epsl.2012.03.006
ISSN: 0012-821X
Projects: Future Ocean
Date Deposited: 18 Apr 2012 10:15
Last Modified: 06 Mar 2017 12:36
URI: http://oceanrep.geomar.de/id/eprint/14225

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