FN Archimer Export Format
PT J
TI Deglacial export of pre-aged terrigenous carbon to the Bay of Biscay
BT 
AF Queiroz Alves, Eduardo
   Wong, Wanyee
   Hefter, Jens
   Grotheer, Hendrik
   Tesi, Tommaso
   Gentz, Torben
   Zonneveld, Karin
   Mollenhauer, Gesine
AS 1:1;2:1,2;3:1;4:1;5:3;6:1;7:4;8:1,2,4;
FF 1:;2:;3:;4:;5:;6:;7:;8:;
C1 Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
   University of Bremen, Bremen, Germany
   Institute of Polar Sciences - National Research Council, 40129 Bologna, Italy
   MARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
C2 INST A WEGENER, GERMANY
   UNIV BREMEN, GERMANY
   CNR, ITALY
   UNIV BREMEN, GERMANY
IN DOAJ
IF 4.3
TC 0
UR https://archimer.ifremer.fr/doc/00825/93684/100478.pdf
   https://archimer.ifremer.fr/doc/00825/93684/107879.pdf
   https://archimer.ifremer.fr/doc/00825/93684/107880.pdf
   https://archimer.ifremer.fr/doc/00825/93684/107881.pdf
LA English
DT Article
CR IMAGES 1-MD101
BO Marion Dufresne
AB The last deglaciation is the most recent relatively well-documented period of pronounced and fast climate warming and, as such, it holds important information for our understanding of the climate system. Notably, while research into terrestrial organic carbon reservoirs has been instrumental in exploring the possible sources of atmospheric carbon dioxide during periods of rapid change, the underlying mechanisms are not fully understood. Here we investigate the mobilization of organic matter to the Bay of Biscay at the mouth of the Channel River, where an enhanced terrigenous input has been reported for the last glacial-interglacial transition. A suite of biomarker and isotopic analyses on a high-resolution sedimentary archive provided the first direct evidence for the fluvial supply of immature and ancient terrestrial organic matter to the core location. In the light of what has been reported for other regions with present or past permafrost conditions on land, this result points to the possibility of permafrost carbon export to the ocean, caused by processes that likely furthered the observed changes in atmospheric carbon dioxide. 
PY 2024
PD JAN
SO Climate Of The Past
SN 1814-9324
PU Copernicus GmbH
VL 20
IS 1
UT 001168885500001
BP 121
EP 136
DI 10.5194/cp-20-121-2024
ID 93684
ER

EF