FN Archimer Export Format
PT J
TI Organic, Gas, and Element Geochemistry of Hydrothermal Fluids of the Newly Discovered Extensive Hydrothermal Area in the Wallis and Futuna Region (SW Pacific)
BT 
AF KONN, Cecile
   DONVAL, Jean-Pierre
   GUYADER, Vivien
   ROUSSEL, Erwan
   FOURRE, E.
   JEAN-BAPTISTE, P.
   PELLETER, Ewan
   CHARLOU, Jean-Luc
   FOUQUET, Yves
AS 1:1;2:1;3:1;4:2;5:3;6:3;7:1;8:1;9:1;
FF 1:PDG-REM-GM-LCG;2:PDG-REM-GM-LCG;3:PDG-REM-GM-LCG;4:PDG-REM-EEP-LMEE;5:;6:;7:PDG-REM-GM-LCG;8:PDG-REM-GM-LCG;9:PDG-REM-GM-LCG;
C1 IFREMER, Lab Cycles Geochim & Ressources, CS10070, F-29280 Plouzane, France.
   IFREMER, Lab Microbiol Environm Extremes, F-29280 Plouzane, France.
   CNRS, UMR 8212, CEA, LSCE,UVSQ, F-91191 Gif Sur Yvette, France.
C2 IFREMER, FRANCE
   IFREMER, FRANCE
   CNRS, FRANCE
SI BREST
SE PDG-REM-GM-LCG
   PDG-REM-EEP-LMEE
UM BEEP-LM2E
IN WOS Ifremer jusqu'en 2018
   DOAJ
   copubli-france
IF 1.437
TC 12
UR https://archimer.ifremer.fr/doc/00431/54245/55571.pdf
   https://archimer.ifremer.fr/doc/00431/54245/55572.pdf
   https://archimer.ifremer.fr/doc/00431/54245/55573.mov
   https://archimer.ifremer.fr/doc/00431/54245/55574.mov
   https://archimer.ifremer.fr/doc/00431/54245/55575.mov
   https://archimer.ifremer.fr/doc/00431/54245/57511.pdf
LA English
DT Article
CR FUTUNA
   FUTUNA 2 LEG1
   FUTUNA 2 LEG2
   FUTUNA 3
BO L'Atalante
AB Two newly discovered hydrothermal vent fields of the Wallis and Futuna region, Kulo Lasi and Fatu Kapa, were sampled for fluid geochemistry. A great geochemical diversity was observed and assigned to the diversity of lithologies as well as the occurrence of various processes. Kulo Lasi fluids likely formed by interaction with fresh volcanic rocks, phase separation, and mixing with magmatic fluid. Conversely, the geochemistry of the Fatu Kapa fluids would be mostly due to water/felsic lavas reactions. In terms of organic geochemistry, fluids from both fields were found to be enriched in formate, acetate, and semivolatile organic compounds (SVOCs): n-alkanes, n-fatty acids, and polyaromatic hydrocarbons (PAHs). Concentrations of SVOCs reached a few ppb at most. The distribution patterns of SVOCs indicated that several processes and sources, at once of biogenic, thermogenic, and abiogenic types, likely controlled organic geochemistry. Although the contribution of each process remains unknown, the mere presence of organics at the μM level has strong implications for metal dispersion (cycles), deposition (ore-forming), and bioavailability (ecosystems), especially as our fluxes estimations suggest that back-arc hosted vent fields could contribute as much as MOR to the global ocean heat and mass budget. 
PY 2018
SO Geofluids
SN 1468-8115
PU Wiley-hindawi
IS 7692839
UT 000428401400001
DI 10.1155/2018/7692839
ID 54245
ER

EF