A microbial driver of chemical weathering in glaciated systems
By S. Montross, M. Skidmore, M. Tranter, A. Kivimäki, R. Parkes. 2013
102 citations recorded by the source corpus.
Subfields: Ecology, Paleontology
View Paper: https://www.semanticscholar.org/paper/33ffdff31440bec8ec7a02195e0a45ecd1c18339
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In Ecology
In Paleontology
Citations in the corpus
- A review of prokaryotic populations and processes in sub-seafloor sediments, including biosphere:geosphere interactions (2014, background): “Middle panel: gas concentrationsinppm (Moore et al., 2001) — methane (diamonds) and ethane (circles), and total cell counts inlog 10 cm − 3 (triangles), light arrows mark depths where intact phospholipids (PL) were detected (Zink et al., 2003) and dark arrows the depths where ampli fi able DNA was…”
- Reviews and syntheses: Biological weathering and its consequences at different spatial levels – from nanoscale to global scale (2020, background): “Studies by Montross et al. (2013) demonstrated an up to 8-fold increase in dissolved cations in biotic systems containing glacial sediments and meltwater compared with abiotic systems, suggesting that microbial processes can maintain terrestrial chemical weathering rates in cooling climates during…”