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亚特兰提化的赢家和输家:海洋变暖的程度影响北极微生物群落的结构。

Winners and Losers of Atlantification: The Degree of Ocean Warming Affects the Structure of Arctic Microbial Communities.

机构信息

Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, 27570 Bremerhaven, Germany.

UMR7621 Laboratoire d'Océanographie Microbienne, CNRS/Sorbonne Université, 66650 Banyuls-sur-Mer, France.

出版信息

Genes (Basel). 2023 Mar 1;14(3):623. doi: 10.3390/genes14030623.

DOI:10.3390/genes14030623
PMID:36980894
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10048660/
Abstract

Arctic microbial communities (i.e., protists and bacteria) are increasingly subjected to an intrusion of new species via Atlantification and an uncertain degree of ocean warming. As species differ in adaptive traits, these oceanic conditions may lead to compositional changes with functional implications for the ecosystem. In June 2021, we incubated water from the western Fram Strait at three temperatures (2 °C, 6 °C, and 9 °C), mimicking the current and potential future properties of the Arctic Ocean. Our results show that increasing the temperature to 6 °C only minorly affects the community, while an increase to 9 °C significantly lowers the diversity and shifts the composition. A higher relative abundance of large hetero- and mixotrophic protists was observed at 2 °C and 6 °C compared to a higher abundance of intermediate-sized temperate diatoms at 9 °C. The compositional differences at 9 °C led to a higher chlorophyll a:POC ratio, but the C:N ratio remained similar. Our results contradict the common assumption that smaller organisms and heterotrophs are favored under warming and strongly indicate a thermal limit between 6 °C and 9 °C for many Arctic species. Consequently, the magnitude of temperature increase is a crucial factor for microbial community reorganization and the ensuing ecological consequences in the future Arctic Ocean.

摘要

北极微生物群落(即原生生物和细菌)越来越多地受到新物种通过大西洋化的入侵和海洋变暖的不确定程度的影响。由于物种在适应特征上存在差异,这些海洋条件可能导致具有生态系统功能意义的组成变化。2021 年 6 月,我们在三个温度(2°C、6°C 和 9°C)下培养了来自西弗拉姆海峡的水,模拟了当前和未来北极海洋的特性。我们的结果表明,将温度升高到 6°C 只会对群落产生轻微影响,而升高到 9°C 会显著降低多样性并改变组成。与 9°C 时中温硅藻丰度较高相比,在 2°C 和 6°C 时观察到大的异养和混合营养原生生物的相对丰度较高。9°C 时的组成差异导致叶绿素 a:POC 比值升高,但 C:N 比值保持相似。我们的结果与普遍假设相矛盾,即变暖有利于较小的生物和异养生物,并强烈表明许多北极物种在 6°C 和 9°C 之间存在一个热限制。因此,温度升高的幅度是未来北极海洋中微生物群落重组和随之而来的生态后果的关键因素。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b8f3/10048660/e2dfae563c4e/genes-14-00623-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b8f3/10048660/35192d63b491/genes-14-00623-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b8f3/10048660/e9e3c9f44d2e/genes-14-00623-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b8f3/10048660/49f0a9b6cfac/genes-14-00623-g003a.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b8f3/10048660/ac466516b460/genes-14-00623-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b8f3/10048660/e2dfae563c4e/genes-14-00623-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b8f3/10048660/35192d63b491/genes-14-00623-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b8f3/10048660/e9e3c9f44d2e/genes-14-00623-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b8f3/10048660/49f0a9b6cfac/genes-14-00623-g003a.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b8f3/10048660/ac466516b460/genes-14-00623-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b8f3/10048660/e2dfae563c4e/genes-14-00623-g005.jpg

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