FN Archimer Export Format
PT J
TI What caused G. truncatulinoides to calcify in shallower water during the early Holocene in the western Atlantic/Gulf of Mexico?
BT 
AF CLEROUX, Caroline
   LYNCH-STIEGLITZ, Jean
AS 1:1;2:;
FF 1:;2:;
C1 School of Earth and Environmental Sciences, Georgia Institute of Technology, Atlanta, GA, USA
C2 GEORGIA INST TECHNOL, USA
TC 2
UR https://archimer.ifremer.fr/doc/00496/60752/65139.pdf
LA English
DT Article
CR IMAGES V LEG 1-MD114
   IMAGES V LEG 4-MD114
BO Marion Dufresne
AB In a recent paper we reconstructed the calcification depth of G. truncatulinoides since the last deglaciation in the Florida Straits. We highlighted a significantly different calcification depth between 8-10 ka and the late Holocene. This migration was found in three different cores over the western North Atlantic American continental margin. This paper presents new Mg/Ca ratio data on G. truncatulinoides in the Florida Strait and new stable isotopic measurements on G. crassaformis in the Gulf of Mexico. Preliminary interpretation to understand the cause of G. truncatulinoides migration in the water column at the beginning of the Holocene is given. 
PY 2010
SO IOP Conference Series: Earth and Environmental Science
SN 1755-1307
PU Iop Publishing Ltd
VL 9
IS 1
UT 000327134700020
DI 10.1088/1755-1315/9/1/012020
ID 60752
ER

EF