FN Archimer Export Format
PT J
TI Mediterranean faunal evolution and biochronological events during the last 24 kyr
BT 
AF Zouari, Sonda
   Boussetta, Soumaya
   Siani, Giuseppe
   Tisnerat-Laborde, Nadine
   Thil, François
   Kallel, Abdelaziz
   Michel, Elisabeth
   Kallel, Nejib
AS 1:1,2;2:1;3:2;4:3;5:3;6:4;7:3;8:1;
FF 1:;2:;3:;4:;5:;6:;7:;8:;
C1 Laboratoire Géoressources, Matériaux, Environnement et changements Globaux (GEOGLOB), Faculté des Sciences de Sfax, Université de Sfax, BP802, 3038 Sfax, Tunisia
   Laboratoire Géosciences Paris-Sud (GEOPS), Université Paris-Saclay, 91405 ORSAY, France
   Laboratoire des Sciences du Climat et de l'Environnement (LSCE), Gif-sur-Yvette, France
   Digital Research Centre of Sfax, Technopark of Sfax, Sfax, Tunisia
C2 UNIV SFAX, TUNISIA
   UNIV PARIS SACLAY, FRANCE
   LSCE, FRANCE
   CRNS, TUNISIA
IF 2.102
TC 3
UR https://archimer.ifremer.fr/doc/00691/80342/83427.pdf
LA English
DT Article
CR ETNA 80
   MD NOE / MARMED
BO Le Noroit
   Marion Dufresne
DE ;Mediterranean Sea;Planktonic foraminifera;SST;LGM;Bio-event;AMS(14)C
AB We generated high-resolution biochronological records in the Mediterranean Sea covering the period extending to the Late-glacial. The present study is based on micropaleontological, sea-surface temperature (SST) and oxygen isotopic analyses performed along three well-dated deep-sea cores: REC13–53, KET80–19 and MD84–641 recovered in the Siculo-Tunisian Strait, Tyrrhenian Sea and Levantine Basin, respectively. The quantitative distributional patterns of planktic foraminifera permitted to identify seven biozones based on the apparition and/or disappearance of the main specific taxa or by their noticeable abundance peaks. Abundance records display that major changes in planktic foraminiferal assemblages have a similar pattern mainly in central and western basins. In particular, four recognized bio-events can be used to establish or to improve the chronology of Mediterranean deep-sea cores. The comparison of the SST estimates and foraminiferal records with those of NGRIP ice-core shows a similarity between the Greenland climate and the Mediterranean hydrology. This indicates that the main climate changes recorded in the North Atlantic are globally in phase with those observed in the Mediterranean region. 
PY 2021
PD MAY
SO Marine Micropaleontology
SN 0377-8398
PU Elsevier BV
VL 165
UT 000659164000006
DI 10.1016/j.marmicro.2021.101997
ID 80342
ER

EF