Römer, Miriam; Sahling, Heiko; Pape, Thomas; dos Santos Ferreira, Christian; Wenzhöfer, Frank; Boetius, Antje; Bohrmann, Gerhard (2013): Methane fluxes and carbonate deposits at eastern Mediterranean cold seeps. PANGAEA, https://doi.org/10.1594/PANGAEA.823759, Supplement to: Römer, M et al. (2013): Methane fluxes and carbonate deposits at a cold seep area of the Central Nile Deep Sea Fan, Eastern Mediterranean Sea. Marine Geology, 27-42, https://doi.org/10.1016/j.margeo.2013.10.011
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High acoustic seafloor-backscatter signals characterize hundreds of patches of methane-derived authigenic carbonates and chemosynthetic communities associated with hydrocarbon seepage on the Nile Deep Sea Fan (NDSF) in the Eastern Mediterranean Sea. During a high-resolution ship-based multibeam survey covering a ~ 225 km**2 large seafloor area in the Central Province of the NDSF we identified 163 high-backscatter patches at water depths between 1500 and 1800 m, and investigated the source, composition, turnover, flux and fate of emitted hydrocarbons. Systematic Parasound single beam echosounder surveys of the water column showed hydroacoustic anomalies (flares), indicative of gas bubble streams, above 8% of the high-backscatter patches. In echosounder records flares disappeared in the water column close to the upper limit of the gas hydrate stability zone located at about 1350 m water depth due to decomposition of gas hydrate skins and subsequent gas dissolution. Visual inspection of three high-backscatter patches demonstrated that sediment cementation has led to the formation of continuous flat pavements of authigenic carbonates typically 100 to 300 m in diameter. Volume estimates, considering results from high-resolution autonomous underwater vehicle (AUV)-based multibeam mapping, were used to calculate the amount of carbonate-bound carbon stored in these slabs. Additionally, the flux of methane bubbles emitted at one high-backscatter patch was estimated (0.23 to 2.3 × 10**6 mol a**-1) by combined AUV flare mapping with visual observations by remotely operated vehicle (ROV). Another high-backscatter patch characterized by single carbonate pieces, which were widely distributed and interspaced with sediments inhabited by thiotrophic, chemosynthetic organisms, was investigated using in situ measurements with a benthic chamber and ex situ sediment core incubation and allowed for estimates of the methane consumption (0.1 to 1 × 10**6 mol a**-1) and dissolved methane flux (2 to 48 × 10**6 mol a**-1). Our comparison of dissolved and gaseous methane fluxes as well as methane-derived carbonate reservoirs demonstrates the need for quantitative assessment of these different methane escape routes and their interaction with the geo-, bio-, and hydrosphere at cold seeps.
Boetius, Antje (2010): Profile of sediment echo sounding during Maria S. Merian cruise MSM13/3 with links to ParaSound data files. PANGAEA, https://doi.org/10.1594/PANGAEA.736831
Median Latitude: 32.508722 * Median Longitude: 30.282635 * South-bound Latitude: 32.500000 * West-bound Longitude: 30.258333 * North-bound Latitude: 32.533470 * East-bound Longitude: 30.352500
Date/Time Start: 2006-10-29T21:42:00 * Date/Time End: 2009-12-11T09:41:00
Datasets listed in this publication series
- Römer, M; Sahling, H; Pape, T et al. (2013): (Appendix) Visually determined major and minor diameters of gas bubbles emanating from five sites at the high-backscatter patch C-1. https://doi.org/10.1594/PANGAEA.823758
- Boetius, A; Wenzhöfer, F (2013): (Table 1) Diffusive methane effluxes and AOM turnover rates at C-9. https://doi.org/10.1594/PANGAEA.823626
- Römer, M; Sahling, H; Pape, T et al. (2013): (Table 2) Volume estimation of the carbonate slabs distributed in an area of about 1.4 km2 and estimate of carbonate-bound carbon stored within the patches. https://doi.org/10.1594/PANGAEA.823789
- Römer, M; Sahling, H; Pape, T et al. (2013): (Table 3) Gas flux estimation for gas bubble streams at C-1. https://doi.org/10.1594/PANGAEA.823693