Introduction to geomicrobiology
By K. Konhauser. 2006
505 citations recorded by the source corpus.
Subfields: Biomedical Engineering, Ecology, Environmental Engineering
View Paper: https://www.semanticscholar.org/paper/738a1870dfeff39399bf984a8964ad7aa6cf8dd2
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Citations in the corpus
- Biogeochemical processes and geotechnical applications: progress, opportunities and challenges (2013, background): “A permanent biological presence (microbes have been active geotechnical engineers for 3+ billion years, much longer than the 0.0002 billion years for humans; Kohnhauser, 2007) in soil provides opportunities for geotechnical engineering to consider soil as a living ecosystem rather than as an inert c”
- Cyanobacterial evolution during the Precambrian (2016, background): “Sheaths have also been shown to contain functional groups (e.g. carboxyl) that help mediate rapid mineralization (Konhauser 2007).”
- Microbiological processes in banded iron formation deposition (2013, methodology): “…Fe(II) into the photic zone by hydrothermal plumes associated with shallow seamount-type systems (Isley, 1995; Isley & Abbot, 1999) would curtail the difficulties introduced by the high upwelling rates needed to bring sufficient iron from the deep sea onto the continental shelf (Konhauser, 2007b).”
- Carbonate and silicate biomineralization in a hypersaline microbial mat (Mesaieed sabkha, Qatar): Roles of bacteria, extracellular polymeric substances and viruses (2018, background): “The most frequent observation of biogenic clay phases comes from biofilms in freshwater lakes and rivers where Fe/Al silicates are the most common (Konhauser, 1997, 2007).”
- Metals, minerals and microbes: geomicrobiology and bioremediation. (2010, unknown): “Geomicrobiology can simply be defined as the roles of microbes in geological processes (Banfield & Nealson, 1997; Banfield et al., 2005; Konhauser, 2007; Ehrlich & Newman, 2009).”
- Modes of Biomineralization of Magnetite by Microbes (2007, background): “It should be noted however that Schüler and Baeuerlein (1998) showed that, in Magnetospirillum gryphiswaldense, Fe(III) is taken up and rapidly converted to Fe3O4 without delay, indicating that no significant accumulation of an Fe3O4 precur sor occurs inside the cell, at least under the microaerobi”