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栖息在浅层热液喷口的微生物群落作为酸化过程的哨兵。

Microbial communities inhabiting shallow hydrothermal vents as sentinels of acidification processes.

作者信息

Arcadi Erika, Rizzo Carmen, Calogero Rosario, Sciutteri Valentina, Fabiano Francesco, Consoli Pierpaolo, Andaloro Franco, Romeo Teresa

机构信息

Department of Biology and Evolution of Marine Organism, Stazione Zoologica Anton Dohrn, Sicily Marine Centre, Messina, Italy.

Marine Biotechnology Department, Stazione Zoologica Anton Dohrn-, Sicily Marine Centre, Messina, Italy.

出版信息

Front Microbiol. 2023 Sep 1;14:1233893. doi: 10.3389/fmicb.2023.1233893. eCollection 2023.

DOI:10.3389/fmicb.2023.1233893
PMID:37727286
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10505797/
Abstract

INTRODUCTION

Shallow hydrothermal vents are considered natural laboratories to study the effects of acidification on biota, due to the consistent CO emissions with a consequent decrease in the local pH.

METHODS

Here the microbial communities of water and sediment samples from Levante Bay (Vulcano Island) with different pH and redox conditions were explored by Next Generation Sequencing techniques. The taxonomic structure was elucidated and compared with previous studies from the same area in the last decades.

RESULTS AND DISCUSSION

The results revealed substantial shifts in the taxonomic structure of both bacterial and archaeal communities, with special relevance in the sediment samples, where the effects of external parameters probably act for a long time. The study demonstrates that microbial communities could be used as indicators of acidification processes, by shaping the entire biogeochemical balance of the ecosystem in response to stress factors. The study contributes to understanding how much these communities can tell us about future changes in marine ecosystems.

摘要

引言

浅海热液喷口被视为研究酸化对生物群影响的天然实验室,因为其持续排放二氧化碳,导致局部pH值下降。

方法

本文采用下一代测序技术,对莱万特湾(武尔卡诺岛)不同pH值和氧化还原条件下的水和沉积物样本中的微生物群落进行了探索。阐明了分类结构,并与过去几十年该地区的先前研究进行了比较。

结果与讨论

结果显示,细菌和古菌群落的分类结构发生了显著变化,在沉积物样本中尤为明显,外部参数的影响可能在沉积物中持续很长时间。该研究表明,微生物群落可作为酸化过程的指标,通过响应压力因素塑造生态系统的整个生物地球化学平衡。该研究有助于理解这些群落能在多大程度上为我们揭示海洋生态系统的未来变化。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/ec04b610aefe/fmicb-14-1233893-g010.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/bdb28dc002e8/fmicb-14-1233893-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/f5ed9794aab8/fmicb-14-1233893-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/3891f0707968/fmicb-14-1233893-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/7955157e21d9/fmicb-14-1233893-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/3dfd79ac5a42/fmicb-14-1233893-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/8101cd64dcca/fmicb-14-1233893-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/b8e2cf7ec74e/fmicb-14-1233893-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/c0da52d754f2/fmicb-14-1233893-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/c606db7a01e3/fmicb-14-1233893-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/ec04b610aefe/fmicb-14-1233893-g010.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/bdb28dc002e8/fmicb-14-1233893-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/f5ed9794aab8/fmicb-14-1233893-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/3891f0707968/fmicb-14-1233893-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/7955157e21d9/fmicb-14-1233893-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/3dfd79ac5a42/fmicb-14-1233893-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/8101cd64dcca/fmicb-14-1233893-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/b8e2cf7ec74e/fmicb-14-1233893-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/c0da52d754f2/fmicb-14-1233893-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/c606db7a01e3/fmicb-14-1233893-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/48a7/10505797/ec04b610aefe/fmicb-14-1233893-g010.jpg

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