Geochemical evidence for a large methane release during the last deglaciation from Marmara Sea sediments

• Published in: Geochimica et cosmochimica acta Vol. 74; no. 5; pp. 1537 - 1550
• Main Authors: Ménot, Guillemette, Bard, Edouard
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.03.2010; Elsevier
• Subjects: Basins; Bioclimatology; Concentration (composition); Deglaciation; Ecology, environment; Expulsion; Gas hydrates; Geochemistry; Hydrates; Life Sciences; Maxima; Methane; MED, Black Sea; MED, Marmara Sea; BARD Édouard; Chaires; Document sous DOI (Digital Object Identifier); traité; web-evolution-climat-ocean; 2HAL
• ISSN: 0016-7037; 1872-9533
• DOI: 10.1016/j.gca.2009.11.022

Recent methane inventories have revealed the potential impact of gas hydrates on the global carbon cycle, and hence in climate change ( Milkov, 2004). However, only a few studies have traced methane release in the geologic record. Here, we show geochemical evidence for a large scale methane release at mid-latitudes during the last deglaciation. The Sea of Marmara, an enclosed sea between the Mediterranean and Black Seas, is located in a tectonically active basin with gas hydrate expulsion and the formation of shallow gas hydrates. Since depths in the basin are shallower than 1100 m, future global temperatures are expected to have a great influence in destabilizing methane clathrates. Among the suite of biomarkers, we have focused on diplopterol and diploptene profiles in core MD012430, retrieved from the central basin in the Marmara Sea. Our results indicate that during the last 15,000 years, hopanoids showed important concentration variations with a pronounced peak during the deglaciation. The lack of a relationship between diplopterol/diploptene and phytoplanktonic biomarker concentrations, as well as a depleted isotopic composition, have linked the hopanoid maxima to methanotrophic activity, suggesting that an intense methane release occurred at the onset of deglaciation in the Marmara Sea. The vulnerability of the hydrate stability zone to changes in temperature and pressure under this range of shallow water depths, as well as the relative timing of the hopanoid maxima and sea surface temperature rise, points to thermal destabilization of hydrates as a trigger for methane release in the water column.