Cold seeps arise in waters rich in methane and/or sulphides
which come from the geology of the ocean floor. Life exists in these deep sea
hot-spots due to the activity of two types of chemoautotrophic bacteria; Sulphur
oxidisers and Methane oxidisers. These bacteria are symbionts to tube worms and
mussels and can be found densely packed within specialised tissues. Many cold
seeps have been studied in the north of the Gulf of Mexico but not many in the
south. A new type of cold seep was discovered recently which is covered with
solid asphalt. Asphalt flows are formed by the seepage of hydrocarbons which
settle and remain on the sea floor. This study aimed to characterise symbiotic
fauna of this new site (Chapopote) using molecular methods and stable carbon
isotopes analysis and comparing the results to those found in cold seeps in the
north of the Gulf of Mexico.
They found that the symbiotic relationships are very similar
(if not identical) to those found in the north. An Escarpia sp. tube worm was identified with two species of Bathymodiolus mussels, all of which had
intracellular sulphur-oxidising symbionts that are found in association with
the same species in the northern cold seeps. Both mussel species contained methane
oxidising symbionts identical to those found in the north. Until now only
methane and reduced sulphur compounds have been shown to power cold seep chemosynthetic
symbioses. However, novel hydrocarbon-degrading bacteria belonging in the Cycloclasticus genus were found in close
relation to the mussel Bathymodiolus
hecherae which also had genes for the metabolism of aromatic compounds,
suggesting the utilisation of heavy aromatic hydrocarbons in addition to
sulphate oxidation.
This study was very interesting and links Grahams and Colins
lecturers. It reinforces the opportunistic nature of ‘nature’ and provides the
first evidence of hydrocarbon symbiosis in a cold seep environment.
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