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Mineralogical Transformation of Bioweathered Granitic Biotite, Studied by HRTEM: Evidence for a New Pathway in Lichen Activity

Published online by Cambridge University Press:  28 February 2024

Jacek Wierzchos  and
Carmen Ascaso
Jacek Wierzchos
Affiliation:
Servei de Microscòpia Electrònica, Universitat de Lleida, Rovira Roure 44, 25196 Lleida, Spain
Carmen Ascaso
Affiliation:
Centro de Ciencias Medioambientales, CSIC, Serrano 115 dpdo., 28006 Madrid, Spain
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Abstract

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The question of whether clay minerals can be biogenically transformed as a result of lichen activity at the lichen-rock interface remains unresolved. We applied several microscopical and analytical techniques—scanning electron microscopy-back-scattered electron (SEM-BSE), energy dispersive spectroscopy (EDS) and high-resolution transmission electron microscopy (HRTEM)—in an attempt to address this issue. Unaffected granitic biotite and bioweathered material from the granitic biotite and Parmelia conspersa lichen thalli interface were examined using HRTEM after ultrathin sectioning. The n-alkylammonium treatment of ultrathin sections was carried out in order to study the biogenous mineralogical transformation of the biotite. Microsamples proceeding from unaffected biotite zones demonstrated homogenous 10-Å d(001)-value biotite phase. HRTEM images of lattice fringes of samples taken from the lichen-biotite contact zone reveal large areas of both unexpanded (10-A) and randomly and R = 3 distributed expanded (from 14- to 30-Å) layers of phyllosilicates identified as interstratified biotite-vermiculite. Results of artificial biotite weathering (replacement of K by Ca ion) also revealed the biotite-vermiculite phase formation, indicating that K release in biotite is one of the mechanisms responsible for interstratified mineral phase formation. Two parallel processes, physical exfoliation of biotite and inter-layer ionic exchange of K and subsequent vermiculite formation, are the mechanisms for biotite bioweathering induced by lichens.

Keywords

Back-scattered ElectronsBiotiteBioweatheringGraniteHigh-Resolution Transmission Electron Microscopy (HRTEM)Lattice-Fringe ImagesLichensVermiculite
Type
Research Article
Information
Clays and Clay Minerals , Volume 46 , Issue 4 , August 1998 , pp. 446 - 452
Copyright
Copyright © 1998, The Clay Minerals Society

References

Adamo, P. and Violante, P., 1991 Weathering of volcanic rocks from Mt Vesuvius associated with the lichen Stereocaulon vesuvianum Pedobiol 35 35–217.CrossRefGoogle Scholar
Ahn, J.H. and Peacor, D.R., 1987 Kaolinization of biotite: TEM data and implications for an alteration mechanism Am Mineral 72 72–356.Google Scholar
Ascaso, C., Vicente, C. Brown, D.H. and Legaz, M.E., 1985 Structural aspects of lichens invading their substrata Surface physiology of lichens Madrid Univ Complutense 87–113.Google Scholar
Ascaso, C. Brown, D. and Rapsch, S., 1988 The effect of desiccation on pyrenoid structure of the oceanic lichen Parmelia leavigata Lichenologist 20 20–40 10.1017/S0024282988000076.CrossRefGoogle Scholar
Ascaso, C. Galvan, J. and Ortega, C., 1976 The pedogenic action of Parmelia conspersa, Rhizocarpon geographicum and Umbilicaria postulata Lichenologist 8 151–171 10.1017/S0024282976000236.CrossRefGoogle Scholar
Ascaso, C. and Wierzchos, J., 1994 Structural aspects of the lichenrock interface using back-scattered electron imaging Bot Acta 107 107–256 10.1111/j.1438-8677.1994.tb00793.x.CrossRefGoogle Scholar
Banfield, J.F. and Eggleton, R.A., 1988 Transmission electron microscope study of biotite weathering Clays Clay Miner 36 36–60 10.1346/CCMN.1988.0360107.CrossRefGoogle Scholar
Berthelin, J. and Belgy, G., 1979 Microbial degradation of phyllosilicates during simulated podzolization Geoderma 21 21–310 10.1016/0016-7061(79)90004-1.CrossRefGoogle Scholar
Douglas, L.A. and Fiessinger, F., 1971 Degradation of clay minerals by H2O2 treatments to oxidise organic matter Clays Clay Miner 19 19–68 10.1346/CCMN.1971.0190108.CrossRefGoogle Scholar
Eggleton, R.A. and Banfield, J.F., 1985 The alteration of granitic biotite to chlorite Am Mineral 70 70–910.Google Scholar
Ghabru, S.K. Mermut, A.R. and St. Arnaud, R.J., 1989 Layer-charge and cation-exchange characteristics of vermiculite (weathered biotite) isolated from a grey luvisol in north-eastern Saskatchewan Clays Clay Miner 37 37–172 10.1346/CCMN.1989.0370208.CrossRefGoogle Scholar
von Graf Reichenbach, H. Wachsmuth, H. and Marcks, C., 1988 Observations at the mica-vermiculite interface with HRTEM Coll Polym Sci 266 266–656.Google Scholar
Hinsinger, P. Elsass, F. Jaillard, B. and Robert, M., 1993 Root-induced irreversible transformation of a trioctahedral mica in the rhizosphere of rape J Soil Sci 44 44–545.CrossRefGoogle Scholar
Hinsinger, P. and Jaillard, B., 1993 Root-induced release of interlayer potassium and vermiculization of phlogopite as related to potassium depletion in the rhizosphere of rye-grass J Soil Sci 44 44–534.CrossRefGoogle Scholar
Hinsinger, P. Jaillard, B. and Dufey, J.E., 1992 Rapid weathering of a trioctahedral mica by the roots of ryegrass Soil Sci Soc Am J 56 56–982 10.2136/sssaj1992.03615995005600030049x.CrossRefGoogle Scholar
Jones, D. Wilson, M.J., Leadbeater, B.S.C. and Riding, R., 1985 Biomineralization in crustose lichens Biomineralization in lower plants and animals Oxford Clarendon Pr. 91–101.Google Scholar
Jones, D. Wilson, M.J. McHardy, W.J., Houghton, D.R. and Smith, E., 1987 Effects of lichens on mineral surfaces Biodeterioration 7. Proc 7th Int Biodeterioration Symp Amsterdam Elsevier 129–134.Google Scholar
Kodama, H. Nelson, S. F. Yang, A. and Kohyama, N., 1994 Mineralogy of rhizospheric and non-rhizospheric soils in corn fields Clays Clay Miner 42 42–763 10.1346/CCMN.1994.0420612.CrossRefGoogle Scholar
Lagaly, G., 1982 Layer charge heterogeneity in vermiculites Clays Clay Miner 30 30–222 10.1346/CCMN.1982.0300308.CrossRefGoogle Scholar
Laird, D.A. Scott, A.D. and Fenton, T.E., 1987 Interpretation of alkylammonium characterisation of soil clays Soil Sci Soc Am J 51 51–1663 10.2136/sssaj1987.03615995005100060046x.CrossRefGoogle Scholar
Lakvulich, L.M. and Wiens, J.H., 1970 Comparison of organic matter destruction by hydrogen peroxide and sodium hypochlorite and its effect on selected mineral constituents Soil Sci Soc Am Proc 34 34–758.Google Scholar
Leyval, C. and Berthelin, J., 1991 Weathering of mica by roots and rhizospheric microorganisms of pine Soil Sci Soc Am J 55 55–1016 10.2136/sssaj1991.03615995005500040020x.CrossRefGoogle Scholar
Leyval, C. Lahuerte, F. Belgy, G. and Berthelin, J., 1990 Weathering of micas in the rhizospheres of maize, pine and beech seedling influenced by mycorrhizal and bacterial inoculation Symbiosis 9 105–109.Google Scholar
Marcks, C. Wachsmuth, H. and von Graf Reichenbach, H., 1989 Preparation of vermiculites for HRTEM Clay Miner 24 24–32 10.1180/claymin.1989.024.1.02.CrossRefGoogle Scholar
Mortland, M.M. Lawton, K. and Uehara, G., 1956 Alteration of biotite to vermiculite by plant growth Soil Sci 82 82–481 10.1097/00010694-195612000-00004.CrossRefGoogle Scholar
van Oort, F. Jongmans, A.G. and Jaunet, A.M., 1994 The progression from optical light microscopy to transmission electron microscopy in the study of soils Clay Miner 29 29–254.CrossRefGoogle Scholar
Plervittori, R. Salvadori, O. and Laccisaglia, A., 1994 Literature on lichens and biodeterioration of stonework Lichenologist 26 26–192.Google Scholar
Purvis, O.W. Elix, J.A. Broomhead, J.A. and Jones, G.C., 1987 The occurrence of copper-norstictic acid in lichens from cupriferous substrata Lichenologist 19 19–203 10.1017/S0024282987000161.CrossRefGoogle Scholar
Purvis, O.W. Elix, J.A. and Gaul, K.A., 1990 The occurrence of copper-psoromic acid from cupriferous substrata Lichenologist 22 22–354 10.1017/S002428299000038X.CrossRefGoogle Scholar
Schatz, A., 1963 Soil microorganisms and soil chelation. The pedogenic action of lichens and lichens acids J Agric Food Chem 11 11–118 10.1021/jf60126a004.CrossRefGoogle Scholar
Seriña, E., 1993 Estudio quimiotaxonómico en líquenes de la Provincia de Madrid [Ph.D. thesis] Madrid, Spain Univ Complutense.Google Scholar
Środorí, J. Andreoli, C. Elsass, F. and Robert, M., 1990 Direct high-resolution transmission electron microscopic measurement of expandability of mixed-layer illite/smectite in bentonite rock Clays Clay Miner 38 38–379.Google Scholar
Syers, J.K. Iskandar, I.K., Ahmadjian, V. and Hale, M.E., 1973 Pedogenic significance of lichens The lichens New York Academic Pr. 225–248 10.1016/B978-0-12-044950-7.50012-X.CrossRefGoogle Scholar
Vali, H. and Hesse, R., 1990 Alkylammonium ion treatment of clay minerals in ultrathin section: A new method for HRTEM examination of expandable layers Am Mineral 75 75–1446.Google Scholar
Vali, H. and Hesse, R., 1992 Identification of vermiculite by transmission electron microscopy and X-ray diffraction Clay Miner 27 27–192 10.1180/claymin.1992.027.2.04.CrossRefGoogle Scholar
Vali, H. Hesse, R. and Kodama, H., 1992 Arrangement of n-alkylammonium ions in phlogopite and vermiculite: An XRD and TEM study Clays Clay Miner 40 40–245 10.1346/CCMN.1992.0400106.CrossRefGoogle Scholar
Vali, H. Hesse, R. and Kohler, E.E., 1991 Combined freeze-etched replicas and HRTEM images as tools to study fundamental-particles and multi-phase nature of 2:1 layer silicates Am Mineral 76 76–1964.Google Scholar
Vali, H. Hesse, R. and Martin, R.F., 1994 A TEM-based definition of 2:1 layer silicates and their interstratified constituents Am Mineral 79 79–653.Google Scholar
Weed, S.B. Davey, C.B. and Cook, M.G., 1969 Weathering of mica by fungi Soil Sci Soc Am Proc 33 33–706.CrossRefGoogle Scholar
Wilson, M.J., 1995 Interactions between lichens and rock; A review Crypt Bot 5 5–305.Google Scholar
Wilson, M.J. Jones, D. and Wilson, R.C.L., 1983 Lichen weathering of minerals and implication for pedogenesis Residual deposits: Surface related weathering processes and materials. Special Publ Geol Soc London Blackwell 5–12.Google Scholar
Wierzchos, J. and Ascaso, C., 1994 Application of back-scattered electron imaging to the study of the lichen-rock interface J Microsc 175 175 59 10.1111/j.1365-2818.1994.tb04787.x.CrossRefGoogle Scholar
Wierzchos, J. and Ascaso, C., 1996 Morphological and chemical features of bioweathered granitic biotite induced by lichen activity Clays Clay Miner 44 44–657 10.1346/CCMN.1996.0440507.CrossRefGoogle Scholar