Temporal succession of bacterial and archaeal communities in a Mediterranean high-mountain lake over the last 430 years using sedimentary DNA.

IF 4 3区 生物学 Q2 ECOLOGY
Antonio Castellano-Hinojosa, Joana Llodrà-Llabrés, Eloísa Ramos-Rodríguez, John P Smol, Carsten Meyer-Jacob, Javier Sigro, Carmen Pérez-Martínez
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Abstract

Despite the known influence of climate change on high-altitude ecosystems, the long-term response of prokaryotic communities in Mediterranean high-mountain lakes remains poorly understood. Here, we investigate the temporal dynamics of prokaryotic communities over the past ~ 430 years in a Mediterranean high-mountain lake, utilizing sedimentary ancient DNA (sedDNA). By examining a sediment core from Borreguil Lake in the Sierra Nevada (Spain), we evaluated bacterial and archaeal abundance, diversity, and community composition (β-diversity) in relation to paleoenvironmental and climate data. Our findings revealed a significant restructuring of prokaryotic communities, particularly since ca. 1960. A Random Forest model identified dissolved organic carbon, organic nitrogen, Saharan atmospheric dust inputs, and temperature as key drivers of the abundance, diversity, and composition of prokaryotic communities, particularly in the modern era. Notably, the abundance and diversity of bacterial communities increased in response to increased dissolved organic carbon, elevated temperatures, and dust deposition, while archaea demonstrated a more nuanced response linked to organic nitrogen availability and dust inputs. The temporal shifts in microbial community composition point to broader ecological changes within the lake, shaped by climate-driven environmental variations. For example, the increased relative abundance of Cyanobacteria and other taxa linked to higher nutrient availability indicates ongoing eutrophication processes, likely intensified by climate warming. This study highlights the importance of high-mountain lakes as indicators of climate change, contributing valuable insights into microbial ecology's response to long-term environmental change. Our findings offer a foundational understanding for predicting microbial responses in sensitive ecosystems under future climate scenarios.

利用沉积DNA对地中海高山湖泊中细菌和古细菌群落在过去430年的时间演替进行研究。
尽管已知气候变化对高海拔生态系统的影响,但对地中海高山湖泊原核生物群落的长期响应仍知之甚少。本文利用沉积古DNA (sedDNA)研究了地中海高山湖泊近430年来原核生物群落的时间动态。通过研究内华达山脉(西班牙)Borreguil湖的沉积物岩心,我们评估了细菌和古细菌的丰度、多样性和群落组成(β-多样性)与古环境和气候数据的关系。我们的发现揭示了原核生物群落的重大重组,特别是自1960年以来。随机森林模型发现,溶解有机碳、有机氮、撒哈拉大气粉尘输入和温度是原核生物群落丰度、多样性和组成的关键驱动因素,尤其是在现代。值得注意的是,细菌群落的丰度和多样性随着溶解有机碳的增加、温度升高和灰尘沉积而增加,而古细菌则表现出与有机氮可用性和灰尘输入有关的更细微的反应。微生物群落组成的时间变化表明湖泊内更广泛的生态变化,由气候驱动的环境变化形成。例如,蓝藻和其他类群相对丰度的增加与更高的养分可用性有关,表明正在进行的富营养化过程,可能因气候变暖而加剧。这项研究强调了高山湖泊作为气候变化指标的重要性,为微生物生态对长期环境变化的响应提供了有价值的见解。我们的发现为预测敏感生态系统在未来气候情景下的微生物反应提供了基础认识。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Microbial Ecology
Microbial Ecology 生物-海洋与淡水生物学
CiteScore
6.90
自引率
2.80%
发文量
212
审稿时长
3-8 weeks
期刊介绍: The journal Microbial Ecology was founded more than 50 years ago by Dr. Ralph Mitchell, Gordon McKay Professor of Applied Biology at Harvard University in Cambridge, MA. The journal has evolved to become a premier location for the presentation of manuscripts that represent advances in the field of microbial ecology. The journal has become a dedicated international forum for the presentation of high-quality scientific investigations of how microorganisms interact with their environment, with each other and with their hosts. Microbial Ecology offers articles of original research in full paper and note formats, as well as brief reviews and topical position papers.
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