Western Mediterranean Sea Paleothermometry Over the Last Glacial Cycle Based on the Novel RI‐OH Index

Type Article
Date 2019-04
Language English
Author(s) Davtian Nina1, Ménot Guillemette2, Fagault Yoann1, Bard Edouard1
Affiliation(s) 1 : CEREGE, Aix Marseille Univ, CNRS, IRD, INRA, Collège de France Aix‐en‐Provence ,France
2 : Univ Lyon, ENS de Lyon, Université Lyon 1, CNRS, UMR 5276 LGL‐TPE Lyon ,France
Source Paleoceanography And Paleoclimatology (2572-4517) (American Geophysical Union (AGU)), 2019-04 , Vol. 34 , N. 4 , P. 616-634
DOI 10.1029/2018PA003452
WOS© Times Cited 5
Abstract

RI‐OH (Ring Index of hydroxylated tetraethers) has recently been proposed to reconstruct paleotemperatures in mid‐to‐low latitude marginal seas. However, RI‐OH has barely been tested in marginal seas under substantial terrigenous inputs. Here, we analyze tetraether lipids in two adjacent marine cores from the Gulf of Lions. We then test for the first time the RI‐OH paleothermometer from 160 to 9 ka BP in the western Mediterranean Sea. While terrigenous inputs prevent TEX86 from behaving as a paleothermometer, RI‐OH is generally consistent with other paleothermometric proxies. RI‐OH also responds systematically and coherently to glacial‐interglacial transitions as well as to abrupt climatic events. The average difference between RI‐OH‐temperatures and November–May UK′37‐temperatures is –2.0 °C with a standard error of 0.4 °C based on 249 RI‐OH‐UK′37 comparisons. This systematic difference suggests that hydroxylated tetraethers and alkenones record different temperatures, for instance winter and/or subsurface temperatures for RI‐OH. Another source of bias could be linked to the available RI‐OH‐temperature calibration, which clearly needs more work at the global and regional scales, notably for semienclosed basins such as the Mediterranean Sea. Nevertheless, our RI‐OH‐based interglacial – glacial anomalies are of 10 °C, a value within the high end of anomalies from previously published temperature records in the western Mediterranean Sea (from 3 to 13 °C). The RI‐OH‐based temperature anomalies also confirm the regional differences and seasonal contrasts in interglacial – glacial anomalies produced by models.

Key Points

RI‐OH consistently records glacial‐interglacial transitions and abrupt climatic events despite substantial terrigenous inputs

RI‐OH could reflect winter and/or subsurface temperatures rather than annual sea surface temperatures in the Gulf of Lions

RI‐OH‐based interglacial – glacial anomalies are high but plausible compared to reported anomalies in the western Mediterranean Sea

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