ArticleMicrobial ecology2025
Temporal succession of bacterial and archaeal communities in a Mediterranean high-mountain lake over the last 430 years using sedimentary DNA.
Article in Microbial ecology, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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1 citing paper in PubMed.
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7 authors.
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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.
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