FN Archimer Export Format
PT J
TI Organic carbon accumulation in modern sediments of the Angola basin influenced by the Congo deep sea fan
BT 
AF BAUDIN, Francois
   MARTINEZ, Philippe
   DENNIELOU, Bernard
   CHARLIER, Karine
   MARSSET, Tania
   DROZ, Laurence
   RABOUILLE, Christophe
AS 1:1;2:2;3:3;4:2;5:3;6:4;7:5,6;
FF 1:;2:;3:PDG-REM-GM-LGS;4:;5:PDG-REM-GM-LGS;6:;7:;
C1 Sorbonne Univ, UPMC Univ Paris 06, CNRS, Inst Sci Terre ISTeP,UMR 7193, 4 Pl Jussieu, F-75005 Paris, France.
   Univ Bordeaux, CNRS, UMR 5805, EPOC, Allee Geoffroy St Hilaire, F-33615 Pessac, France.
   IFREMER, Unite Geosci Marines, Dept REM, F-29280 Plouzane, France.
   Inst Univ Europeen Mer, CNRS, UMR 6538, Lab Domaines Ocean, Rue Dumont dUrville, F-29280 Plouzane, France.
   Univ Paris Saclay, UMR CEA CNRS UVSQ 8212, LSCE, Bat 12,Ave Terrasse, F-91198 Gif Sur Yvette, France.
   Univ Paris Saclay, IPSL, Bat 12,Ave Terrasse, F-91198 Gif Sur Yvette, France.
C2 UNIV PARIS 06, FRANCE
   UNIV BORDEAUX, FRANCE
   IFREMER, FRANCE
   UBO, FRANCE
   UNIV PARIS SACLAY, FRANCE
   UNIV PARIS SACLAY, FRANCE
SI BREST
SE PDG-REM-GM-LGS
UM LGO
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-univ-france
IF 2.451
TC 20
UR https://archimer.ifremer.fr/doc/00369/47974/47999.pdf
LA English
DT Article
CR CONGOLOBE
   GUINESS 2
   GUINESS I
   REPREZAI_LEG2
   WACS
   ZAIANGO1
   ZAIANGO2
BO Pourquoi pas ?
   Le Suroît
   L'Atalante
DE ;Organic matter;Recent sediments;South Atlantic Ocean;Turbidites
AB Geochemical data (total organic carbon-TOC content, δ13Corg, C:N, Rock-Eval analyses) were obtained on 150 core tops from the Angola basin, with a special focus on the Congo deep sea fan. Combined with the previously published data, the resulting dataset (322 stations) shows a good spatial and bathymetric representativeness. TOC content and δ13Corg maps of the Angola basin were generated using this enhanced dataset. The main difference in our map with previously published ones is the high terrestrial organic matter content observed downslope along the active turbidite channel of the Congo deep sea fan till the distal lobe complex near 5,000 m of water-depth. Interpretation of downslope trends in TOC content and organic matter composition indicates that lateral particle transport by turbidity currents is the primary mechanism controlling supply and burial of organic matter in the bathypelagic depths.
PY 2017
PD AUG
SO Deep-sea Research Part Ii-topical Studies In Oceanography
SN 0967-0645
PU Pergamon-elsevier Science Ltd
VL 142
UT 000408783500005
BP 64
EP 74
DI 10.1016/j.dsr2.2017.01.009
ID 47974
ER

EF