Sulphate‐reducing bacteria induce low‐temperature Ca‐dolomite and high Mg‐calcite formation
By Y. Van Lith, R. Warthmann, C. Vasconcelos, J. Mckenzie. 2003
301 citations recorded by the source corpus.
Subfields: Ecology, Oceanography, Paleontology
View Paper: https://www.semanticscholar.org/paper/236884bca4fef66bb9ced6a5103113b1f237cbf2
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Citations in the corpus
- Processes of carbonate precipitation in modern microbial mats (2009, background): “…in hypersaline lakes have been reported (e.g., Neumann et al., 1988; Mann and Nelson, 1989; Gerdes et al., 1994; Reitner et al., 1997; Arp et al., 1999a,b; van Lith et al., 2003; Jonkers et al., 2003; Burns et al., 2004; Wright and Wacey, 2005; Ludwig et al., 2005; Dupraz and Visscher, 2005).”
- Microbial biomineralization processes forming modern Ca:Mg carbonate stromatolites (2010, background): “It has been shown that nanospheres with a high organic matter content replace both the EPS structure (Dupraz et al., 2004) and bacterial bodies (Sprachta et al., 2001; van Lith et al., 2003b).”
- Microbially influenced formation of Mg‐calcite and Ca‐dolomite in the presence of exopolymeric substances produced by sulphate‐reducing bacteria (2014, methodology): “In recent years, experiments conducted with SRB (Vasconcelos et al., 1995; Warthmann et al., 2000, 2005; van Lith et al., 2003; Wright and Wacey, 2005; Deng et al., 2010; Bontognali et al., 2012; Krause et al., 2012), methanogenic archea (Kenward et al., 2009) and aerobic bacteria (Rivadeneyra et…”
- Ureolytic Bacteria and Calcium Carbonate Formation as a Mechanism of Strength Enhancement of Sand (2011, methodology): “To avoid the formation of ammonium ions during biocementation reaction, van Paassen and his colleagues (Van Paassen et al., 2008) have used organic acids (acetate, lactate, succinate and malate) as carbon sources, an electron acceptor and a counter ion.”