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Evidence for isolated evolution of deep-sea ciliate communities through geological separation and environmental selection
BACKGROUND: Deep hypersaline anoxic basins (DHABs) are isolated habitats at the bottom of the eastern Mediterranean Sea, which originate from the ancient dissolution of Messinian evaporites. The different basins have recruited their original biota from the same source, but their geological evolution...
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| Hoofdauteurs: | , , , , , , |
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| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
BioMed Central
2013
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| Onderwerpen: | |
| Online toegang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3707832/ https://ncbi.nlm.nih.gov/pubmed/23834625 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1186/1471-2180-13-150 |
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