ArticleMicrobial ecology2025
The Deep Subsurface Biosphere and its Substrates Along a One-Million-Year Ferruginous Lake Archive.
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 2 papers, 1 of them a synthesis that pooled it.
What it found
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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.
The trial behind it
Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.
Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.
Who cites it
2 citing papers in PubMed, 1 synthesis or guideline pooled it.
- Pooled it
- Cryptic sulfur cycling in the deep biosphere of ferruginous Lake Towuti, Indonesia.Frontiers in microbiology · 2025Article
Corrections and comments
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Authors and funding
7 authors.
Funding
Abstract
Lake Towuti, Indonesia, is an ancient stratified lake with ferruginous (iron-rich, sulfate-poor) anoxic bottom water conditions and a long depositional record affected by redox changes in the water column and sediments. As modern analogue of Earth's early ferruginous oceans, it enables the study of an active microbial subsurface biosphere and its role in organic matter and iron mineralization. Combining 16S rRNA genes, cell counts, pore water geochemistry, and bulk sediment profiles from a 100-m-long core, we present the first comprehensive characterization of the deep subsurface biosphere along a one-million-year lacustrine archive. Electron acceptors in the pore water became depleted at shallow depths, resulting in a drastic decrease in cell densities in the fermentative zone, where Bathyarchaeia dominate the microbial community composition. Although alpha and beta diversity reflected initial depletion of substrates during burial, they also varied across successive lithologies, indicating that sediment composition subsequent to deposition also affects diversity. The upper sediments (0-20 mblf) sheltered a dense and diverse microbial community involved in organic matter remineralization, actively producing and converting volatile fatty acids into carbon dioxide and methane. Deeper sediments (20-70 mblf) contained low-diversity microbial communities adapted to nutrient scarcity. In contrast, deepest lacustrine sediments (70-100 mblf) contained an increased microbial diversity reflecting greater availability of organic matter of terrestrial origin. Despite Bathyarchaeia being prime constituents of the deep subsurface biosphere, increased diversity in 16S rRNA gene composition was observed in discrete sediment layers (tephra, diatom ooze, peat). This demonstrated that depositional conditions remained traceable, while stratified microbial communities drove reductive diagenesis.
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Registered trials
Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.