Ocean Science for Everyone

Cold Seeps

Learn About Cold Seeps

Cold seeps are locations where hydrocarbon-rich fluid seeps up from below the seafloor, often as methane or hydrogen sulfide. Cold seeps have been found to support significant chemosynthetic communities, which produce food using chemical energy.

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Cold Seeps

Tubeworms
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During the Seascape Alaska 3 expedition, the team encountered dense “fields” of Lamellibranchia sp. tubeworms, like those pictured here from a depth of 2,018 meters (1.25 miles). The field extended at least 200 meters (656 feet) wide, but is likely even larger based on the bubble trail discovered during expedition mapping operations.

Although no active gas bubbling was observed during Dive 19, the dense patches of live Bathymodiolus childressi mussels and associated bacterial mats are indicators of fluid seepage. Such ecosystems rely on methane or hydrogen sulfide produced during the bacterial breakdown of methane for their metabolic processes, meaning that an active methane system must be present below the seafloor. Red laser dots are separated by 10 centimeters (3.94 inches).
Mussel Community
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In 2013, scientists discovered a previously unknown methane seep off the coast of Virginia. At the seep site, they found this vast mussel community on flat bottom as well as on rocks rising a meter or more off the seafloor.

This octopus was seen at our dive at Blake Ridge Seep.
Octopus
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This octopus was seen during a DEEP SEARCH 2019: DEEP Sea Exploration to Advance Research on Coral/Canyon/Cold seep Habitats expedition dive at Blake Ridge Seep off the coast of North Carolina.

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This octopus was seen at our dive at Blake Ridge Seep.

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