不同的微生物群落内和渗漏碳酸盐支持长期厌氧氧化甲烷和不同的pMMO多样性。

IF 10 1区 环境科学与生态学 Q1 ECOLOGY
Magdalena J Mayr, Sergio A Parra, Stephanie A Connon, Aditi K Narayanan, Ranjani Murali, Antoine Crémière, Victoria J Orphan
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引用次数: 0

摘要

在世界各地的甲烷渗漏中,合成厌氧甲烷氧化古菌和硫酸盐还原细菌促进碳酸盐沉淀和岩石形成,起到甲烷和碳汇的作用。虽然甲烷厌氧氧化(AOM)在渗碳酸盐中的维持已被记录,但其在甲烷暴露后的再激活仍然不确定。表面相关微生物可能代谢AOM中的硫化物,维持碳酸盐缺氧,促进碳酸盐溶解,并支持更高的营养水平;然而,对这些社区的描述却很少。我们通过扩增子和宏基因组测序、孵育和结合荧光原位杂交(BONCAT-FISH)的非规范氨基酸标记,提供微生物多样性、代谢、活性和弹性在渗碳酸盐内部和上的见解。在活性和低活性渗漏中,Ca. Methanophaga (ANME-1)在碳酸盐岩内部占主导地位,与Ca. desultatia共同发生,是主要的硫酸盐还原剂,可能是AOM中新的协同伙伴。单细胞BONCAT-FISH揭示了ANME-1活性的可变性,表明低活性渗漏部位的碳酸盐可能处于休眠状态。然而,与低活性渗漏(≥24个月)的碳酸盐孵卵后,AOM恢复呈指数型(约44天加倍),表明这些碳酸盐在动态渗流条件下仍具有长期甲烷汇的潜力。表面相关微生物群落是不均匀的,与碳酸盐内部和其他渗漏栖息地不同。厌氧甲烷氧化生物膜和硫化物氧化垫与具有高和中等AOM速率的碳酸盐相关,可能影响碳酸盐的沉淀/溶解。碳酸盐岩表面和无脊椎动物之间共享的好氧甲烷氧化菌表明,碳酸盐岩表面可能是动物表面生物的储集层。回收的颗粒甲烷单加氧酶既包括需氧甲烷氧化菌,也包括与甲基噬菌科相关的不同形式,这表明该组具有新的功能。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Distinct microbial communities within and on seep carbonates support long-term anaerobic oxidation of methane and divergent pMMO diversity.

At methane seeps worldwide, syntrophic anaerobic methane-oxidizing archaea and sulfate-reducing bacteria promote carbonate precipitation and rock formation, acting as methane and carbon sinks. Although maintenance of anaerobic oxidation of methane (AOM) within seep carbonates has been documented, its reactivation upon methane exposure remains uncertain. Surface-associated microbes may metabolize sulfide from AOM, maintain carbonate anoxia, contribute to carbonate dissolution, and support higher trophic levels; however, these communities are poorly described. We provide insights into microbial diversity, metabolism, activity, and resiliency within and on seep carbonates through amplicon and metagenomic sequencing, incubations, and non-canonical amino acid tagging combined with fluorescence in situ hybridization (BONCAT-FISH). Ca. Methanophaga (ANME-1) dominated the carbonate interiors in active and low activity seeps, co-occurring with Ca. Desulfaltia as main sulfate reducer, potentially a new syntrophic partner in AOM. Single-cell BONCAT-FISH revealed variability in ANME-1 activity, suggesting potential dormancy in carbonates from low activity seep sites. However, incubations with carbonates from low activity seeps (≥24 months) showed exponential AOM reactivation (~44-day doubling), suggesting these carbonates retain the potential as long-term methane sinks under dynamic seepage conditions. Surface-associated microbial communities were heterogeneous and distinct from the carbonate interior and other seep habitats. Anaerobic methane-oxidizing biofilms and sulfide-oxidizing mats were associated with carbonates with high and intermediate AOM rates potentially influencing carbonate precipitation/dissolution. Shared aerobic methanotrophs between carbonate surfaces and invertebrates indicated carbonate surfaces may represent animal epibiont reservoirs. Recovered particulate methane monooxygenases included both aerobic methanotrophs and divergent forms associated with the Methylophagaceae, suggesting a new function in this group.

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来源期刊
ISME Journal
ISME Journal 环境科学-生态学
CiteScore
22.10
自引率
2.70%
发文量
171
审稿时长
2.6 months
期刊介绍: The ISME Journal covers the diverse and integrated areas of microbial ecology. We encourage contributions that represent major advances for the study of microbial ecosystems, communities, and interactions of microorganisms in the environment. Articles in The ISME Journal describe pioneering discoveries of wide appeal that enhance our understanding of functional and mechanistic relationships among microorganisms, their communities, and their habitats.
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