The Crystallization of Calcium Oxalate Hydrates Formed by Interaction Between Microorganisms and Minerals

The Crystallization of Calcium Oxalate Hydrates Formed by Interaction Between Microorganisms and Minerals is …
instance of (P31):
scholarly articleQ13442814

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P356DOI10.1007/978-3-319-24987-2_28

P50authorDmitry VlasovQ86270250
P2093author name stringDmitry Yu. Vlasov
Olga V. Frank-Kamenetskaya
Aleksei D. Vlasov
Aleksei V. Rusakov
Marina S. Zelenskaya
P2860cites workOxalotrophic bacteria.Q30973874
Fungi, bacteria and soil pH: the oxalate-carbonate pathway as a model for metabolic interaction.Q34296424
Biodegradation of ivory (natural apatite): possible involvement of fungal activity in biodeterioration of the Lewis ChessmenQ46289422
Mimicking the growth of a pathologic biomineral: shape development and structures of calcium oxalate dihydrate in the presence of polyacrylic acidQ46291574
Fungal degradation of calcium-, lead- and silicon-bearing minerals.Q46571793
Geomycology: biogeochemical transformations of rocks, minerals, metals and radionuclides by fungi, bioweathering and bioremediation.Q55043258
Influence ofBacillus subtilis on the growth of calcium oxalateQ57351031
Crystallization of calcium oxalate hydrates by interaction of calcite marble with fungusAspergillus nigerQ57382320
An integrated approach to assess the origins of black films on a granite monumentQ57613135
The oxalate–carbonate pathway in soil carbon storage: the role of fungi and oxalotrophic bacteriaQ58867001
Biomineralization of Fungal Hyphae with Calcite (CaCO3) and Calcium Oxalate Mono- and Dihydrate in Carboniferous Limestone MicrocosmsQ59150654
Experimental observations on fungal diagenesis of carbonate substratesQ59791464
P921main subjectcalcium oxalateQ412399
P304page(s)357-377
P577publication date2015-12-25
P1476titleThe Crystallization of Calcium Oxalate Hydrates Formed by Interaction Between Microorganisms and Minerals

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Q57859123Oxalate formation under the hyperarid conditions of the Atacama desert as a mineral marker to provide clues to the source of organic carbon on Marscites workP2860
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