FN Archimer Export Format
PT J
TI Are Past Sea-Ice Reconstructions Based on Planktonic Foraminifera Realistic? Study of the Last 50 ka as a Test to Validate Reconstructed Paleohydrography Derived from Transfer Functions Applied to Their Fossil Assemblages
BT 
AF Eynaud, Frédérique
   Zaragosi, Sébastien
   Wary, Mélanie
   Woussen, Emilie
   Rossignol, Linda
   Voisin, Adrien
AS 1:1;2:1;3:1;4:1;5:1;6:1;
FF 1:;2:;3:;4:;5:;6:;
C1 EPOC (Environnements & Paléoenvironnements Océaniques et Continentaux) Laboratory, UMR 5805, Bordeaux University, Allée Geoffroy Saint Hilaire, 33615 Pessac, France
C2 UNIV BORDEAUX, FRANCE
IN DOAJ
TC 0
UR https://archimer.ifremer.fr/doc/00725/83687/88742.pdf
   https://archimer.ifremer.fr/doc/00725/83687/88743.zip
LA English
DT Article
CR IMAGES 1-MD101
   IMAGES V LEG 1-MD114
   IMAGES V LEG 4-MD114
   IMAGES V LEG 5
BO Marion Dufresne
DE ;sea surface paleohydrographical reconstructions;North Atlantic Ocean;foraminifera
AB Since its existence, paleoceanography has relied on fossilized populations of planktonic foraminifera. Except for some extreme environments, this calcareous protist group composes most of the silty-to-sandy fraction of the marine sediments, i.e., the foraminiferal oozes, and its extraction is probably the simplest among the currently existing set of marine fossil proxies. This tool has provided significant insights in the building of knowledge on past climates based on marine archives, especially with the quantification of past hydrographical variables, which have been a turning point for major comprehensive studies and a step towards the essential junction of modelling and paleodata . In this article, using the modern analog technique and a database compiling modern analogs (n = 1007), we test the reliability of this proxy in reconstructing paleohydrographical data other than the classical sea-surface temperatures, taking advantage of an update regarding a set of extractions from the World Ocean Atlas for transfer functions. Our study focuses on the last glacial period and its high climatic variability, using a set of cores distributed along the European margin, from temperate to subpolar sites. We discuss the significance of the reconstructed parameters regarding abrupt and extreme climate events, such as the well-known Heinrich events. We tested the robustness of the newly obtained paleodata by comparing them with older published reconstructions, especially those based on the complementary dinoflagellate cyst proxy. This study shows that the potential of planktonic foraminifera permits going further in reconstructions, with a good degree of confidence; however, this implies considering ecological forcings in a more holistic perspective, with the corollary to integrate the message of this fossil protist group, i.e., the obtained parameters, in light of a cohort of other data. This article constitutes a first step in this direction. 
PY 2021
PD OCT
SO Geosciences
SN 2076-3263
PU MDPI AG
VL 11
IS 10
UT 000711917500001
DI 10.3390/geosciences11100409
ID 83687
ER

EF