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冷泉中参与生物地球化学循环的原核生物群落及其潜在功能的研究进展

Insights into prokaryotic communities and their potential functions in biogeochemical cycles in cold seep.

机构信息

South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China.

University of Chinese Academy of Sciences, Beijing, China.

出版信息

mSphere. 2024 Oct 29;9(10):e0054924. doi: 10.1128/msphere.00549-24. Epub 2024 Sep 13.

Abstract

UNLABELLED

Microorganisms are significant drivers of organic matter mineralization and are essential in marine biogeochemical cycles. However, the variations and influencing factors in prokaryotic communities from cold-seep sediments to the water column and the specific role of these microorganisms in biogeochemical cycles in the water column above cold seep remain unclear. Here, we investigated prokaryotic communities and their roles in nitrogen/sulfur cycling processes and conducted dissolved organic matter (DOM) enrichment experiments to explore the effects of diverse sources of DOM on prokaryotic communities. Field investigations showed that the prokaryotic communities in the near-bottom water were more similar to those in the deep layer of the euphotic zone (44.60%) and at a depth of 400 m (50.89%) than those in the sediment (18.00%). DOM enrichment experiments revealed that adding dissolved organic nitrogen (DON) and phosphorus DOP caused a notable increase in the relative abundances of Rhodobacterales and Vibrionales, respectively. A remarkable increase was observed in the relative abundance of Alteromonadales and Pseudomonadales after the addition of dissolved organic sulfur (DOS). The metagenomic results revealed that Proteobacteria served as the keystone taxa in mediating the biogeochemical cycles of nitrogen, phosphorus, and sulfur in the Haima cold seep. This study highlights the responses of prokaryotes to DOM with different components and the microbially driven elemental cycles in cold seeps, providing a foundational reference for further studies on material energy metabolism and the coupled cycling of essential elements mediated by deep-sea microorganisms.

IMPORTANCE

Deep-sea cold seeps are among the most productive ecosystems, sustaining unique fauna and microbial communities through the release of methane and other hydrocarbons. Our study revealed that the influence of seepage fluid on the prokaryotic community in the water column is surprisingly limited, which challenges conventional views regarding the impact of seepage fluids. In addition, we identified that different DOM compositions play a crucial role in shaping the prokaryotic community composition, providing new insights into the factors driving microbial diversity in cold seeps. Furthermore, the study highlighted Proteobacteria as key and multifaceted drivers of biogeochemical cycles in cold seeps, emphasizing their significant contribution to complex interactions and processes. These findings offer a fresh perspective on the dynamics of cold-seep environments and their microbial communities, advancing our understanding of the biogeochemical functions in deep-sea environments.

摘要

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微生物是有机质矿化的重要驱动因素,也是海洋生物地球化学循环的关键。然而,冷泉沉积物到水柱中的原核生物群落的变化和影响因素,以及这些微生物在冷泉上方水柱生物地球化学循环中的具体作用仍不清楚。在这里,我们研究了原核生物群落及其在氮/硫循环过程中的作用,并进行了溶解有机物质(DOM)富集实验,以探索不同来源的 DOM 对原核生物群落的影响。现场调查表明,近底层水中的原核生物群落与透光层深部(44.60%)和 400 米深处(50.89%)的原核生物群落更为相似,而与沉积物(18.00%)的相似性较低。DOM 富集实验表明,添加溶解有机氮(DON)和磷 DOP 分别导致红杆菌目和颤蚓目相对丰度的显著增加。添加溶解有机硫(DOS)后,交替单胞菌目和假单胞菌目的相对丰度显著增加。宏基因组学结果表明,变形菌门在介导海麻冷泉氮、磷和硫的生物地球化学循环中起关键作用。本研究强调了具有不同成分的 DOM 对原核生物的响应以及冷泉中微生物驱动的元素循环,为进一步研究深海微生物介导的物质能量代谢和关键元素的偶联循环提供了基础参考。

重要性

深海冷泉是生产力最高的生态系统之一,通过释放甲烷和其他碳氢化合物,维持着独特的动物群和微生物群落。我们的研究表明,渗流流体对水柱中原核生物群落的影响令人惊讶地有限,这对渗流流体影响的传统观点提出了挑战。此外,我们发现不同的 DOM 组成在塑造原核生物群落组成方面起着至关重要的作用,为冷泉中微生物多样性的驱动因素提供了新的见解。此外,该研究强调了变形菌门是冷泉生物地球化学循环的关键和多方面的驱动因素,强调了它们对复杂相互作用和过程的重要贡献。这些发现为冷泉环境及其微生物群落的动态提供了新的视角,提高了我们对深海环境生物地球化学功能的理解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f48e/11524163/c7a03c26f6fa/msphere.00549-24.f001.jpg

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