The weathering action of saxicolous lichens in maritime Antarctica

7 pages, figures and tables statistics. Xanthoria elegans (Link) Th Fr. and Lecidea lapicida (Ach.) were studied on volcanic andesite, and Rhizocarpon geooraphicum (L.) DC. and Bacidia stipata Lamb on a volcanigenic sediment, using light microscopy, infrared spectroscopy, X-ray diffraction and trans...

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Main Authors: Ascaso, Carmen, Sancho, Leopoldo G., Rodríguez Pascual, C.
Format: Article in Journal/Newspaper
Language:English
Published: 1990
Subjects:
Online Access:http://hdl.handle.net/10261/31464
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spelling ftcsic:oai:digital.csic.es:10261/31464 2024-02-11T09:57:19+01:00 The weathering action of saxicolous lichens in maritime Antarctica Ascaso, Carmen Sancho, Leopoldo G. Rodríguez Pascual, C. 1990 http://hdl.handle.net/10261/31464 en eng Polar Biology (11): 33-39 (1990) 0722-4060 http://hdl.handle.net/10261/31464 open Lichens in maritime Antarctica Xanthoria elegans Lecidea lapicida Rhizocarpon geographicum Bacidia stipata artículo http://purl.org/coar/resource_type/c_6501 1990 ftcsic 2024-01-16T09:29:52Z 7 pages, figures and tables statistics. Xanthoria elegans (Link) Th Fr. and Lecidea lapicida (Ach.) were studied on volcanic andesite, and Rhizocarpon geooraphicum (L.) DC. and Bacidia stipata Lamb on a volcanigenic sediment, using light microscopy, infrared spectroscopy, X-ray diffraction and transmission electron microscopy. Feldspars were present in the rocklichen interface to a lesser extent than in the underlying rock. R. geographicum was found to alter the minerals in the rock on which it grew without producing any new minerals in the rock/lichen interface, in contrast to the observations for this species on granite in temperate regions. Beneath of the thallus of L. lapicida there was calcium oxalate and some micas of the illite type, which may have been degradation products of various phyllosilicates in the rock. B. stipata, an endemic Antarctic lichen, had the greatest capacity to weather the rock and had weddellite (dihydrate calcium oxalate) and calcite in the contact area as well as many bacteria. The presence of crystalline oxalate, imogolite, allophane, carbonates (calcite) and amorphous material not found in the parent rock indicates biomineralization processes attributable to the lichens. We are pleased to acknowledge that this work was supported by a grant number PB87 0229 from the Comisi6n Asesora de Ciencia y Tecnologia. We are grateful to Mr. F. Pinto and M. T. Carnota for technical assistance, and to Prof. Kappen and William Sanders for help with the English manuscript. Peer reviewed Article in Journal/Newspaper Antarc* Antarctic Antarctica Polar Biology Digital.CSIC (Spanish National Research Council) Antarctic
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
topic Lichens in maritime Antarctica
Xanthoria elegans
Lecidea lapicida
Rhizocarpon geographicum
Bacidia stipata
spellingShingle Lichens in maritime Antarctica
Xanthoria elegans
Lecidea lapicida
Rhizocarpon geographicum
Bacidia stipata
Ascaso, Carmen
Sancho, Leopoldo G.
Rodríguez Pascual, C.
The weathering action of saxicolous lichens in maritime Antarctica
topic_facet Lichens in maritime Antarctica
Xanthoria elegans
Lecidea lapicida
Rhizocarpon geographicum
Bacidia stipata
description 7 pages, figures and tables statistics. Xanthoria elegans (Link) Th Fr. and Lecidea lapicida (Ach.) were studied on volcanic andesite, and Rhizocarpon geooraphicum (L.) DC. and Bacidia stipata Lamb on a volcanigenic sediment, using light microscopy, infrared spectroscopy, X-ray diffraction and transmission electron microscopy. Feldspars were present in the rocklichen interface to a lesser extent than in the underlying rock. R. geographicum was found to alter the minerals in the rock on which it grew without producing any new minerals in the rock/lichen interface, in contrast to the observations for this species on granite in temperate regions. Beneath of the thallus of L. lapicida there was calcium oxalate and some micas of the illite type, which may have been degradation products of various phyllosilicates in the rock. B. stipata, an endemic Antarctic lichen, had the greatest capacity to weather the rock and had weddellite (dihydrate calcium oxalate) and calcite in the contact area as well as many bacteria. The presence of crystalline oxalate, imogolite, allophane, carbonates (calcite) and amorphous material not found in the parent rock indicates biomineralization processes attributable to the lichens. We are pleased to acknowledge that this work was supported by a grant number PB87 0229 from the Comisi6n Asesora de Ciencia y Tecnologia. We are grateful to Mr. F. Pinto and M. T. Carnota for technical assistance, and to Prof. Kappen and William Sanders for help with the English manuscript. Peer reviewed
format Article in Journal/Newspaper
author Ascaso, Carmen
Sancho, Leopoldo G.
Rodríguez Pascual, C.
author_facet Ascaso, Carmen
Sancho, Leopoldo G.
Rodríguez Pascual, C.
author_sort Ascaso, Carmen
title The weathering action of saxicolous lichens in maritime Antarctica
title_short The weathering action of saxicolous lichens in maritime Antarctica
title_full The weathering action of saxicolous lichens in maritime Antarctica
title_fullStr The weathering action of saxicolous lichens in maritime Antarctica
title_full_unstemmed The weathering action of saxicolous lichens in maritime Antarctica
title_sort weathering action of saxicolous lichens in maritime antarctica
publishDate 1990
url http://hdl.handle.net/10261/31464
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Antarctica
Polar Biology
genre_facet Antarc*
Antarctic
Antarctica
Polar Biology
op_relation Polar Biology (11): 33-39 (1990)
0722-4060
http://hdl.handle.net/10261/31464
op_rights open
_version_ 1790609607271383040