Methane seeps are places in the ocean where methane from deep sediment layers escapes the seabed. Specific microorganisms use the potential greenhouse gas as an energy source and thus form the basis for complex ecosystems. Now, an international team of researchers led by the Max Planck Institute for Marine Microbiology has investigated the microbial communities of selected methane seeps from all oceans, and compared those to communities of other marine ecosystems. In the current issue of Proceedings of the National Academy of Sciences (USA), the researchers report that methane seeps contain many endemic microorganisms and therefore are hotspots of biodiversity in the deep sea . In general, the seep communities are very different from those of other ecosystems. Only a few species of methanotrophs occur at all seeps worldwide, but these microorganisms seem to greatly influence the methane budget of the ocean.
Seafloor ecosystems have unique inhabitants
Each ecosystem in the deep sea is inhabited by certain microorganisms that can be assigned to the three domains of the tree of life: eukaryotes, archaea and bacteria. Eukaryotes have a nucleus and include all plants, fungi, and animals. Archaea and bacteria are single cells without a nucleus. The researchers studied the composition and relative abundance of archaea and bacteria at 77 locations of different marine ecosystems, including coastal sediments, deep-sea sediments, black smokers, and methane seeps. They extracted the DNA of these organisms from the seabed samples and analyzed it using modern DNA sequencing techniques and mathematical algorithms.
Emil Ruff, scientist at the Max Planck Institute, summarizes: "Almost all of the major groups of archaea and bacteria were present at all examined sites. With increasing resolution, however, the differences between the ecosystems became clearer. At the level of individual species, which are the smallest branches of the tree of life, we found communities that are characteristic for each ecosystem and have a very specific task." These characteristic communities were defined as the methane seep microbiome. The term microbiome is used to describe all microorganisms of a particular ecosystem and their genetic diversity. Such an ecosystem may be a methane seep, or soil or even the human intestine. The head of the research group and DCO Deep Life Scientific Steering Committee member, Prof. Dr. Antje Boetius, adds: "This study represents the first global view on microbes inhabiting methane seeps. It was enabled by a large international effort, the International Census of Marine Microbes.”
Methane seeps accommodate many specialists
Natural methane seeps (cold seeps) are found worldwide at continental margins. The gas is formed by decomposition processes in the anoxic layers deep down in the sediment, moves upwards, and escapes at the seafloor. The uppermost sediment layers harbor methane oxidizers, which consume about three-quarters of the escaping methane. This is equivalent to 60 million tons of carbon per year. At methane seeps, the primary energy source is completely different from those of the surrounding seabed. Thus, like oases in the desert methane sources attract particular organisms. These include groups with known function, such as anaerobic methane-oxidizing archaea (ANME) and sulfate-reducing bacteria (SRB). However, the researchers also found microbial groups on the methane sources with unknown function.
Emil Ruff, first author of the study, said: "It was surprising that microorganisms from seeps that are thousands of miles away in different oceans, are so closely related. Many methane oxidizers and sulfate reducers are sensitive to oxygen. Therefore, it is a mystery how they survive the great distances between the methane seeps." These new findings suggest that only a few worldwide populations are responsible for the bulk of methane consumption. The vast diversity of species and the evolution of new species, however, is limited to and can only be found at certain sites. Methane seeps thus contribute greatly to the biodiversity of the deep sea.
Image: Micrographs of aerobic methanotrophic bacteria (white), anaerobic methanotrophic archaea (ANME – red) and sulfate-reducing bacteria (SRB – green) visualized by fluorescence in situ hybridization. Anaerobic oxidation of methane is a globally relevant process removing 60 million tons, the mass of ten pyramids of Giza, of the greenhouse gas methane from seafloor sediments each year. Courtesy of Katrin Knittel/Emil Ruff, MPI Bremen.
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