FN Archimer Export Format
PT J
TI Record of methane emissions from the West Svalbard continental margin during the last 23.500 yrs revealed by delta C-13 of benthic foraminifera
BT 
AF PANIERI, Giuliana
   JAMES, Rachael H.
   CAMERLENGHI, Angelo
   WESTBROOK, Graham
   CONSOLARO, Chiara
   CACHO, Isabel
   CESARI, Valentina
   SANCHEZ CERVERA, Cristina
AS 1:1,2;2:3;3:4;4:3,5,6;5:1,7;6:8;7:2;8:8;
FF 1:;2:;3:;4:;5:;6:;7:;8:;
C1 UiT Arctic Univ Norway, CAGE Ctr Arctic Gas Hydrate Environm & Climate, N-9037 Tromso, Norway.
   CNR ISMAR, I-40129 Bologna, Italy.
   Univ Southampton, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England.
   OGS Ist Nazl Oceanog & Geofis Sperimentale, I-34010 Trieste, Italy.
   Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham B15 2TT, W Midlands, England.
   IFREMER, Ctr Brest, F-29280 Plouzane, France.
   Univ Plymouth, Sch Geog Earth & Environm Sci, Plymouth PL4 8AA, Devon, England.
   Univ Barcelona, Fac Geol, Dept Estratig Paleontol & Geociencies Marines, GRC Geociencies Marines, E-08028 Barcelona, Spain.
C2 UNIV ARCTIC NORWAY, NORWAY
   ISMAR, ITALY
   NOC, UK
   OGS, ITALY
   UNIV BIRMINGHAM, UK
   IFREMER, Ctr Brest, F-29280 Plouzane, France.
   UNIV PLYMOUTH, UK
   UNIV BARCELONA, SPAIN
IF 2.766
TC 50
UR https://archimer.ifremer.fr/doc/00245/35605/88200.pdf
LA English
DT Article
DE ;Methane emission;Vestnesa Ridge;West Svalbard;Stable isotope;delta C-13;Benthic foraminifera
AB The values of delta C-13 in benthic foraminifera have been measured in a gas-hydrate-bearing sediment core collected from an area of active methane venting on the Vestnesa Ridge (West Svalbard continental margin) to reconstruct the local history of methane emissions over the past 23.500 yrs BP. The chronostratigraphic framework of the core has been derived from AMS C-14 dates and biostratigraphic analysis. While foraminifera from some intervals have delta C-13 within the normal marine range (0 to-1%.), five intervals are characterized by a much lower delta C-13, as low as -17.4%.. These intervals are interpreted to record the incorporation of C-13-depleted carbon in the presence of methane emissions at the seafloor during biomineralization of the carbonate foraminiferal tests and subsequent secondary mineralization. Methane emission events (MEE) occur from the Last Glacial Maximum (LGM) to the Holocene, with the most prominent one, in terms of delta C-13 depletion, predating the Bolling-Allerod Interstadial (GI-1 in the Greenland ice core record). The lack of correlation between the values of delta C-13 and delta O-18, however, appears to preclude warming of bottom waters as the principal control on methane release. Rather, it seems likely that methane release is a consequence of episodicity in the supply of gas to the hydrate system and in the processes that enable methane gas to migrate through the hydrate stability field to the seabed, or of other geological processes still under debate.
PY 2014
PD NOV
SO Global And Planetary Change
SN 0921-8181
PU Elsevier Science Bv
VL 122
UT 000345488600013
BP 151
EP 160
DI 10.1016/j.gloplacha.2014.08.014
ID 35605
ER

EF