Proliferation of hydrocarbon-degrading microbes at the bottom of the Mariana Trench

Jiwen Liu, Yanfen Zheng, Heyu Lin, Xuchen Wang, Meng Li, Yang Liu, Meng Yu, Meixun Zhao, Nikolai Pedentchouk, David J. Lea-Smith, Jonathan D. Todd, Clayton R. Magill, Wei-Jia Zhang, Shun Zhou, Delei Song, Haohui Zhong, Yu Xin, Min Yu, Jiwei Tian, Xiao-Hua Zhang

Research output: Contribution to journalArticle

22 Citations (Scopus)
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Abstract

Background The Mariana Trench is the deepest known site in the Earth's oceans, reaching a depth of ~ 11,000 m at the Challenger Deep. Recent studies reveal that hadal waters harbor distinctive microbial planktonic communities. However, the genetic potential of microbial communities within the hadal zone is poorly understood. Results Here, implementing both culture-dependent and culture-independent methods, we perform extensive analysis of microbial populations and their genetic potential at different depths in the Mariana Trench. Unexpectedly, we observed an abrupt increase in the abundance of hydrocarbon-degrading bacteria at depths > 10,400 m in the Challenger Deep. Indeed, the proportion of hydrocarbon-degrading bacteria at > 10,400 m is the highest observed in any natural environment on Earth. These bacteria were mainly Oleibacter, Thalassolituus, and Alcanivorax genera, all of which include species known to consume aliphatic hydrocarbons. This community shift towards hydrocarbon degraders was accompanied by increased abundance and transcription of genes involved in alkane degradation. Correspondingly, three Alcanivorax species that were isolated from 10,400 m water supplemented with hexadecane were able to efficiently degrade n-alkanes under conditions simulating the deep sea, as did a reference Oleibacter strain cultured at atmospheric pressure. Abundant n-alkanes were observed in sinking particles at 2000, 4000, and 6000 m (averaged 23.5 μg/gdw) and hadal surface sediments at depths of 10,908, 10,909, and 10,911 m (averaged 2.3 μg/gdw). The δ2H values of n-C16/18 alkanes that dominated surface sediments at near 11,000-m depths ranged from - 79 to - 93‰, suggesting that these sedimentary alkanes may have been derived from an unknown heterotrophic source. Conclusions These results reveal that hydrocarbon-degrading microorganisms are present in great abundance in the deepest seawater on Earth and shed a new light on potential biological processes in this extreme environment.
Original languageEnglish
Article number47
JournalMicrobiome
Volume7
DOIs
Publication statusPublished - 12 Apr 2019

Keywords

  • Challenger Deep
  • Hadal water
  • Hydrocarbon biosynthesis
  • Hydrocarbon degradation
  • Mariana Trench
  • Metagenomics
  • Microbial community

ASJC Scopus subject areas

  • Microbiology
  • Microbiology (medical)

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