Record of methane emissions from the West Svalbard continental margin during the last 23.500 yrs revealed by delta C-13 of benthic foraminifera

• Published in: Global and Planetary Change
• Main Authors: Panieri, Giuliana, James, Rachael H., Camerlenghi, Angelo, Westbrook, Graham, Consolaro, Chiara, Cacho, Isabel, Cesari, Valentina, Sanchez Cervera, Cristina
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier Science Bv 2014
• Subjects: Methane emission; Vestnesa Ridge; West Svalbard; Stable isotope; delta C-13; Benthic foraminifera; Greenland; Svalbard; Greenland ice core; ice core
• Online Access: https://archimer.ifremer.fr/doc/00245/35605/88200.pdf; https://doi.org/10.1016/j.gloplacha.2014.08.014; https://archimer.ifremer.fr/doc/00245/35605/

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.