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原生微生物在潮间带生态系统中的演替。

Primary Microbial Succession in the Anchialine Ecosystem.

机构信息

Dept. of Integrative Biology, The University of Texas at Austin, Austin, TX 78712, USA.

Division of Aquatic Resources, Department of Land and Natural Resources, State of Hawaii, Hilo, HI 96720, USA.

出版信息

Integr Comp Biol. 2022 Aug 25;62(2):275-287. doi: 10.1093/icb/icac087.

Abstract

When new land is created, initial microbial colonization lays the foundation for further ecological succession of plant and animal communities. Primary microbial succession of new aquatic habitats formed during volcanic activity has received little attention. The anchialine ecosystem, which includes coastal ponds in young lava flows, offers an opportunity to examine this process. Here, we characterized microbial communities of anchialine habitats in Hawaii that were created during volcanic eruptions in 2018. Benthic samples from three habitats were collected ∼2 years after their formation and at later time points spanning ∼1 year. Sequence profiling (16S and 18S) of prokaryotic and eukaryotic communities was used to test whether communities were similar to those from older, established anchialine habitats, and if community structure changed over time. Results show that microbial communities from the new habitats were unlike any from established anchialine microbial communities, having higher proportions of Planctomycetota and Chloroflexi but lower proportions of green algae. Each new habitat also harbored its own unique community relative to other habitats. While community composition in each habitat underwent statistically significant changes over time, they remained distinctive from established anchialine habitats. New habitats also had highly elevated temperatures compared to other habitats. These results suggest that idiosyncratic microbial consortia form during early succession of Hawaiian anchialine habitats. Future monitoring will reveal whether the early communities described here remain stable after temperatures decline and macro-organisms become more abundant, or if microbial communities will continue to change and eventually resemble those of established habitats. This work is a key first step in examining primary volcanic succession in aquatic habitats and suggests young anchialine habitats may warrant special conservation status.

摘要

当新的土地形成时,初始的微生物定殖为植物和动物群落的进一步生态演替奠定了基础。火山活动形成的新水生栖息地的主要微生物演替受到的关注较少。包括年轻熔岩流中的沿海池塘在内的向海生态系统为研究这一过程提供了机会。在这里,我们对 2018 年火山喷发形成的夏威夷向海栖息地的微生物群落进行了特征描述。在形成后约 2 年和之后约 1 年的时间跨度内,从三个栖息地采集了底栖样本。对原核生物和真核生物群落的序列分析(16S 和 18S)用于测试这些群落是否与较老的、已建立的向海微生物群落相似,以及群落结构是否随时间而变化。结果表明,新栖息地的微生物群落与任何已建立的向海微生物群落都不相似,具有更高比例的浮霉菌和绿弯菌,但更低比例的绿藻。每个新栖息地相对于其他栖息地也拥有自己独特的群落。虽然每个栖息地的群落组成随时间发生了显著变化,但它们仍然与已建立的向海栖息地不同。新栖息地的温度也比其他栖息地高得多。这些结果表明,在夏威夷向海栖息地早期演替过程中形成了独特的微生物共生体。未来的监测将揭示这里描述的早期群落在温度下降和大型生物变得更加丰富后是否保持稳定,或者微生物群落是否会继续变化并最终类似于已建立的栖息地。这项工作是研究水生栖息地主要火山演替的关键第一步,并表明年轻的向海栖息地可能需要特殊的保护地位。

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