Repost: Deep-Sea Corals and Methane Seeps
This is a repost of KZ’s winning post for Open Laboratory 2009: The Best Science Writing on the Web. Congrats to KZ!
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This is a tale of cause and effect in the deep sea woven by threads of hypotheses held together by the loom of targeted sampling efforts and multiple lines of evidence. You see, dear readers, once upon a time existed an observation. Hovland (1989) noticed along the Norwegian coastline that carbonate reefs occurred in sediment laden with detectable concentrations of methane and oil. This led him to suggest that
“such reefs form at locations containing high concentrations of bacteria and other microorganisms suspended in the water column as a result of seeping fluids (solutions and gases) that provide some of the energy basis and carbon source for ecosystems independently of photosynthesis.”
Over the course of the last 20 years that hypothesis has been refined by several lines of evidence to suggest that
“the coral reef is located at this exact location due to sub-surface hydrogeologic properties, i.e. that there is an upward seepage of hydrocarbon-charged porewater on which bacteria and other micro-organisms thrive, thus providing suspension-feeders, including the corals, with a substantial and reliable food source.” (Hovland & Thomsen 1997)
This is known as the “hydraulic theory” for reef occurrence. My colleague and former labmate Erin Becker just published a study which sheds more light on the coral-seep relationship. (more…)
Comments (2) | Date Posted: January 18, 2010 at 4:25 PM






To counterpoint 
As a result, the gear worked perfectly the first time we deployed it at 1500 ft in the Gulf of Mexico and every time since. The only usable samples of deep-sea corals I have collected have come from the Johnson-Sea-Link. My luck with ROVs to date has been abysmal. ROV and AUV technology are great for a lot of things, but for delicate sample collection, in situ manipulation, and times when you just ‘have to be there’ there is no beating the Johnson-Sea-Link.







