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ISME Commun
January 2024
GFZ German Research Centre for Geosciences, Section Geomicrobiology, Telegrafenberg, 14473 Potsdam, Germany.
Ferruginous conditions prevailed through Earth's early oceans history, yet our understanding of biogeochemical cycles in anoxic iron-rich, sulfate-poor sediments remains elusive in terms of redox processes and organic matter remineralization. Using comprehensive geochemistry, cell counts, and metagenomic data, we investigated the taxonomic and functional distribution of the microbial subsurface biosphere in Lake Towuti, a stratified ferruginous analogue. Below the zone in which pore water becomes depleted in electron acceptors, cell densities exponentially decreased while microbial assemblages shifted from iron- and sulfate-reducing bacterial populations to fermentative anaerobes and methanogens, mostly selecting Bathyarchaeia below the sulfate reduction zone.
View Article and Find Full Text PDFEcotoxicol Environ Saf
December 2024
Environmental Health Division, Graduate School of Global Environmental Studies, Kyoto University, Kyoto, Japan; Institute for International Academic Research, Kyoto University of Advanced Science, Kyoto, Japan; Research Institute for Coexistence and Health Science, Kyoto University of Advanced Science, Kyoto, Japan.
Environ Pollut
August 2024
Graduate School of Global Environmental Studies, Kyoto University, Kyoto, 606-8501, Japan; Institute for International Academic Research, Kyoto University of Advanced Science, Kyoto, 615-8577, Japan.
The respiratory effects of particulate matter (PM) in subway station platforms or tunnels have attracted considerable research attention. However, no studies have characterized the effects of subway PM on allergic immune responses. In this study, iron oxide (α-FeO and FeO) particles-the main components of subway PM-were intratracheally administered to BALB/c mice where ovalbumin (OVA) induced allergic pulmonary inflammation.
View Article and Find Full Text PDFRedox Biol
May 2024
Department of Earth Sciences, The University of Hong Kong, Hong Kong, 999077, China. Electronic address:
Recent research has hypothesized that hydrogen peroxide (HO) may have emerged from abiotic geochemical processes during the Archean eon (4.0-2.5 Ga), stimulating the evolution of an enzymatic antioxidant system in early life.
View Article and Find Full Text PDFGeobiology
February 2024
Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, Michigan, USA.
Chemical sedimentary deposits called Banded Iron Formations (BIFs) are one of the best surviving records of ancient marine (bio)geochemistry. Many BIF precursor sediments precipitated from ferruginous, silica-rich waters prior to the Great Oxidation Event at ~2.43 Ga.
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