Microbial community changes along the active seepage site of one cold seep in the Red Sea.

Huiluo Cao, Weipeng Zhang, Yong Wang, Pei-Yuan Qian

Research output: Contribution to journalArticlepeer-review

12 Scopus citations


The active seepage of the marine cold seeps could be a critical process for the exchange of energy between the submerged geosphere and the sea floor environment through organic-rich fluids, potentially even affecting surrounding microbial habitats. However, few studies have investigated the associated microbial community changes. In the present study, 16S rRNA genes were pyrosequenced to decipher changes in the microbial communities from the Thuwal seepage point in the Red Sea to nearby marine sediments in the brine pool, normal marine sediments and water, and benthic microbial mats. An unexpected number of reads from unclassified groups were detected in these habitats; however, the ecological functions of these groups remain unresolved. Furthermore, ammonia-oxidizing archaeal community structures were investigated using the ammonia monooxygenase subunit A (amoA) gene. Analysis of amoA showed that planktonic marine habitats, including seeps and marine water, hosted archaeal ammonia oxidizers that differed from those in microbial mats and marine sediments, suggesting modifications of the ammonia oxidizing archaeal (AOA) communities along the environmental gradient from active seepage sites to peripheral areas. Changes in the microbial community structure of AOA in different habitats (water vs. sediment) potentially correlated with changes in salinity and oxygen concentrations. Overall, the present results revealed for the first time unanticipated novel microbial groups and changes in the ammonia-oxidizing archaea in response to environmental gradients near the active seepages of a cold seep.
Original languageEnglish (US)
JournalFrontiers in Microbiology
Issue numberJUL
StatePublished - Jul 21 2015
Externally publishedYes

Bibliographical note

KAUST Repository Item: Exported on 2020-10-01
Acknowledged KAUST grant number(s): SA-C0040, UK-C0016
Acknowledgements: This study was supported by the National Basic Research Program of China (973 Program, No: 2012CB417304), the Strategic Priority Research Program of the Chinese Academy of Sciences (XDB06010100 and XDB06010200), Exploration and Evaluation of Potential Resources from Deep-sea Microorganisms (DY125-15-R-02) from China Ocean Mineral Resources R&D Association (COMRRDA12SC02), and an award (SA-C0040/UK-C0016) from the King Abdullah University of Science and Technology in Saudi Arabia to P-YQ. The authors are grateful to Alex Shek for his technical assistance. We thank Dr. Abdulaziz M Al-Suwailem and his team from the King Abdullah University of Science and Technology for organizing research cruise and assistance in collecting samples.
This publication acknowledges KAUST support, but has no KAUST affiliated authors.


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