FN Archimer Export Format
PT J
TI Freshwater lake to salt-water sea causing widespread hydrate dissociation in the Black Sea
BT 
AF RIBOULOT, Vincent
   KER, Stephan
   SULTAN, Nabil
   THOMAS, Yannick
   MARSSET, Bruno
   SCALABRIN, Carla
   RUFFINE, Livio
   BOULART, Cedric
   ION, Gabriel
AS 1:1;2:1;3:1;4:1;5:1;6:1;7:1;8:1;9:2;
FF 1:PDG-REM-GM-LAD;2:PDG-REM-GM-LAD;3:PDG-REM-GM;4:PDG-REM-GM-LAD;5:PDG-REM-GM-LAD;6:PDG-REM-GM-LCG;7:PDG-REM-GM-LCG;8:PDG-REM-GM-LCG;9:;
C1 IFREMER, REM GM, BP70, F-29280 Plouzane, France.
   Natl Inst Marine Geol & Geoecol, RO-024053 Bucharest, Romania.
C2 IFREMER, FRANCE
   NIRD GEOECOMAR, ROMANIA
SI BREST
SE PDG-REM-GM-LAD
   PDG-REM-GM
   PDG-REM-GM-LCG
IN WOS Ifremer jusqu'en 2018
   DOAJ
   copubli-europe
IF 11.878
TC 58
UR https://archimer.ifremer.fr/doc/00418/52981/53916.pdf
   https://archimer.ifremer.fr/doc/00418/52981/53917.pdf
   https://archimer.ifremer.fr/doc/00418/52981/53918.pdf
LA English
DT Article
CR GHASS
BO Pourquoi pas ?
AB Gas hydrates, a solid established by water and gas molecules, are widespread along the continental margins of the world. Their dynamics have mainly been regarded through the lens of temperature-pressure conditions. A fluctuation in one of these parameters may cause destabilization of gas hydrate-bearing sediments below the seafloor with implications in ocean acidification and eventually in global warming. Here we show throughout an example of the Black Sea, the world’s most isolated sea, evidence that extensive gas hydrate dissociation may occur in the future due to recent salinity changes of the sea water. Recent and forthcoming salt diffusion within the sediment will destabilize gas hydrates by reducing the extension and thickness of their thermodynamic stability zone in a region covering at least 2800 square kilometers which focus seepages at the observed sites. We suspect this process to occur in other world regions (e.g., Caspian Sea, Sea of Marmara). 
PY 2018
PD JAN
SO Nature Communications
SN 2041-1723
PU Nature Publishing Group
VL 9
IS 117
UT 000419658100016
BP 1
EP 8
DI 10.1038/s41467-017-02271-z
ID 52981
ER

EF