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Cold Seeps

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Cold seeps and hydrothermal vents are localities where subsurface fluid leak from the seafloor. The main difference between cold seeps and hydrothermal vents is the temperature of the emanating fluid. The seepage emitted from cold seeps is the same temperature as the surrounding seawater, whereas hydrothermal vents radiate much hotter water. The hydrocarbons that emanate from cold seeps are usually methane, but could also be ethane, propane, or oil. Cold seeps and hydrothermal vents have a community of organisms that surround them, which can be restricted to the area. The cold seeps are known to house communities of invertebrates that have created a relationship with chemoautotrophic bacteria. This relationship gives the bacteria a protected …show more content…
Both, bacteria and the host, benefit from this relationship, which is why the communities are so successful. These dependent invertebrates survive by using the chemosynthetic bacteria’s by-products as most or all food that they consume. In order to maximize the nutrients collected, many invertebrates house the bacteria in their tissues. Some brachiopods, bivalves, and molluscs have been recorded to have this relationship (Barry et al., 2002, Campbell and Bottjer, 1995, Kiel, 2006, Kiel el al., 2008, Sandy and Campbell. 1994). The chemosynthetic bacteria living in organisms have a strong and secure home for carbon fixation. A species known for housing large numbers of chemosynthetic bacteria was the Bathymodiolus platifrons, a bivalve. Scientists discovered this after using a transmission electron microscopy to viewing bacterium in parts of the B, platifrons’ tissue (Barry et al., 2002). The invertebrates that do not house the bacteria in their tissues still use the by-products, but in a less efficient …show more content…
For example, Peregrinella is a brachiopod that was restricted to cold seeps because of their mutualistic relationship with chemosynthetic bacteria. They even adapted ways to better obtain the nutrients produced, by housing the bacteria in their tissue (Campbell and Bottjer, 1995). Trace fossils of worms have also been discovered in multiple fossilized cold seeps. These worm burrows suggest that they were not only an inhabitant of cold seeps, but could also be the dominant organism. One cold seep fossil was completely comprised of burrows in varying sizes, with barely any traces of other organisms in the surrounding area (Goedert et al., 2000). Regional species, such as crabs, have been known to feed on the invertebrates at cold seeps. Although there have been cold seeps with remnants of species most are not restricted to the seeps (Bishop and Williams, 2000). Fossilized sponges have recently been discovered that are found near the peripheral of cold seep communities. There are very few sponges species identified at modern or fossilized sites and those that are do not seem to be dependent on the chemosynthetic community (Rigby and Goedert, 1996). The organisms that inhabit cold seep communities are what make the sites so unique and easier to

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