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Australia: The Land Where Time Began |
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Methane Leakage
over Widespread Areas of the Seafloor on the Atlantic Margin of Northern
US Methane inputs to the atmosphere (McGinnis et al.,
2006) are affected by methane emissions from the sea floor, as are
acidification and de-oxygenation (Biastoch et
al., 2011; Archer, Buffett &
Brovkin, 2009) of the ocean, distribution of chemosynthetic communities
and energy resources. Global methane flux derived from cold seeps has
only been estimated for continental shelves (Hovland, Judd & Burke,
1993), at 8-65 Tg CH4 yr-1, though methane is
being emitted by other parts of the marine continental margins. The
Atlantic margin of
the US has not previously been considered to be an area where widespread
seepage was occurring, with only 3 methane seeps being recognised
seaward of the shelf break. It has been predicted that there would be
massive upper-slope seepage related to
gas hydrate
degradation for the southern part of this margin (Phrampus & Hornbach,
2012), though previously this process has been recognised only in the
Arctic (Biastoch et
al.,
2011; Westbrook et al., 2009; ). In this study the authors1
used multibeam water-column backscatter data to cover 94,000 km2
of the sea floor, identifying about 570 gas plumes at water depths
between 50 and 1,700 m between Cape Hatteras and Georges Bank on the
passive margin of the northern US Atlantic coast. At water depths
bracketing the updip limit for methane hydrate stability there are about
440 seeps that originate there. At this location contemporary seepage
from the upper slope may be triggered by ongoing warming of intermediate
waters, though emissions are implied to have continued for more than
1,000 years at some seeps by authigenic carbonates observed. The authors1
suggest there could be 10s of thousands of seeps that have not yet been
discovered based on extrapolation of the upper slope density of this
margin to global passive margin systems.
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| Author: M.H.Monroe Email: admin@austhrutime.com Sources & Further reading | ||||||||||||||