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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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 |