FN Archimer Export Format PT J TI Deep-dwelling foraminifera as thermocline temperature recorders BT AF CLEROUX, Caroline CORTIJO, Elsa DUPLESSY, Jean-Claude ZAHN, Rainer AS 1:1;2:1;3:1;4:2,3; FF 1:;2:;3:;4:; C1 IPSL, Lab Sci Climat & Environm, Lab Mixte, CEA CNRS UVSQ, F-91198 Gif Sur Yvette, France. ICREA, E-08193 Bellaterra, Cerdanyola, Spain. Univ Autonoma Barcelona, Inst Ciencia & Tecnol Ambientals, E-08193 Bellaterra, Cerdanyola, Spain. C2 IPSL, FRANCE ICREA, SPAIN UNIV AUTONOMA BARCELONA, SPAIN IF 2.354 TC 82 UR https://archimer.ifremer.fr/doc/00236/34727/33178.pdf LA English DT Article CR IMAGES 1-MD101 IMAGES V LEG 1-MD114 IMAGES V LEG 4-MD114 MD 126 / MONA MD 127 / PAGE BO Marion Dufresne DE ;deep-dwelling foraminifera;depth habitat;isotopic temperature;thermocline;North Atlantic;Mauritanian upwelling;ecological prediction;stable isotopes;micropaleontology AB We measured the oxygen isotopic composition of the deep-dwelling foraminiferal species G. inflata, G. truncatulinoides dextral and sinistral, and P. obliquiloculata in 29 modern core tops raised from the North Atlantic Ocean. We compared calculated isotopic temperatures with atlas temperatures and defined ecological models for each species. G. inflata and G. truncatulinoides live preferentially at the base of the seasonal thermocline. Under temperature stress, i.e., when the base of the seasonal thermocline is warmer than 16 degrees C, G. inflata and G. truncatulinoides live deeper in the main thermocline. P. obliquiloculata inhabits the seasonal thermocline in warm regions. We tested our model using 10 cores along the Mauritanian upwelling and show that the comparison of delta(18)O variations registered by the surficial species G. ruber and G. bulloides and the deep-dwelling species G. inflata evidences significant glacial-interglacial shifts of the Mauritanian upwelling cells. PY 2007 PD APR SO Geochemistry Geophysics Geosystems SN 1525-2027 PU Amer Geophysical Union VL 8 IS 4 UT 000246140300002 BP 1 EP 19 DI 10.1029/2006GC001474 ID 34727 ER EF