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            <gco:CharacterString>2005 Strategic Environmental Assessment SEA6 Technical Report - The Distribution and extent of methane-derived authigenic carbonate (Irish Sea)</gco:CharacterString>
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        <gco:CharacterString>This report is a contribution to the Strategic Environmental Assessment (SEA6) conducted by the Department of Trade and Industry (now Department of Energy and Climate Change). Methane-derived authigenic carbonate (MDAC) is formed as a consequence of the anaerobic oxidation of methane by consortia of bacteria. MDAC develops as a rock-like concretion when a carbonate precipitate cements normal seabed sediment; the carbon of this carbonate is derived from methane. It occurs as crusts or slabs at the seabed, or as exposed lumps. The occurrence of MDAC is evidence of methane seepage, although the seepage is not necessarily going on at the present time. Large quantities of MDAC indicate that methane seepage has occurred over a prolonged period of time. 'Submarine structures formed by leaking gas' have been identified by the European Commission's Habitats Directive as habitats worthy of protection.

The distribution of MDAC in UK waters is poorly known. This report summarises the available information relevant to MDAC in the SEA6 area, including data acquired by surveys specifically conducted in support of this SEA in 2004. Carbon isotope data for samples recovered in 2004 have confirmed that the cemented hard grounds from two of the areas studied, Texel 11 and Holden's Reef, are composed of MDAC.</gco:CharacterString>
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            <gco:CharacterString>The report was prepared by Dr A. G. Judd  as part of the UK Department of Energy and Climate Change's Offshore Energy Strategic Environmental Assessment programme. There are no published reports of methane-derived authigenic carbonate (MDAC) in the SEA6 area, but carbon isotope data have confirmed that the cemented hard grounds of two areas studied for the SEA6 project, Texel 11, and Holden's Reef, are composed of MDAC. Geophysical surveys, sampling and photographic surveys of other parts of the SEA6 area have confirmed that indicators of gas seepage (seep plumes, and pockmarks) are present in several other areas, and that acoustic turbidity (shallow gas) is widespread. 

A specific objective of the SEA6 surveys was to investigate possible occurrences of MDAC in examples of a range of the geological contexts present in the SEA6 area. To that end 12 study areas were identified. Two surveys were undertaken during the period 24th August to 31st October 2004 geophysical surveys (S/V Meridian): single-beam echo sounder (SBES), multi-beam echo sounder (MBES), side-scan sonar (SSS), and chirp sub-bottom profiler (SBP); photography, seabed sediment sampling, and water sampling (S/V Kommandor Jack).</gco:CharacterString>
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