MICROBIAL COLONIZATION PROCESSES IN ANTARCTIC FELLFIELD SOILS : AN EXPERIMENTAL OVERVIEW (Eleventh Symposium on Polar Biology)

The process of colonization of Antarctic fellfield soils by micro-organisms has two phases: Firstly, the immigration, survival and establishment of microbial propagules themselves, and secondly the stabilization of the soil for subsequent colonization and establishment by mosses, lichens and inverte...

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Main Author: David D. WYNN-WILLIAMS
Format: Report
Language:English
Published: Proceeding 1990
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:00005098 2023-05-15T13:49:03+02:00 MICROBIAL COLONIZATION PROCESSES IN ANTARCTIC FELLFIELD SOILS : AN EXPERIMENTAL OVERVIEW (Eleventh Symposium on Polar Biology) David D. WYNN-WILLIAMS 1990-03 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=5098 http://id.nii.ac.jp/1291/00005098/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=5098&item_no=1&attribute_id=18&file_no=1 en eng Proceeding British Antarctic Survey, Natural Environment Research Council National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=5098 http://id.nii.ac.jp/1291/00005098/ AA10819561 Proceedings of the NIPR Symposium on Polar Biology, 3, 164-178(1990-03) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=5098&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1990 ftnipr 2023-02-11T20:10:44Z The process of colonization of Antarctic fellfield soils by micro-organisms has two phases: Firstly, the immigration, survival and establishment of microbial propagules themselves, and secondly the stabilization of the soil for subsequent colonization and establishment by mosses, lichens and invertebrates. Dominant amongst primary microbial colonizers are the phototrophic cyanobacteria and algae. Not only do they introduce organic nutrients into the microhabitat but they also have a structural function. Filaments of several dimensions frequently form a mesh over the surface of the soil. This mesh often has a canopy structure of fine filaments closely admixed with the mineral soil grains, overlain by a layer of broader, longer filaments. This structure may provide a rich grazing zone for micro-invertebrates such as protozoa and nematodes. Microbial filaments, clusters and unicells frequently have mucilaginous sheaths or capsules which may cement mineral grains together and improve soil crust stability. The combination of filaments and mucigel promotes the formation of microbial "rafts" which are dispersed by wind or water. The diverse microbiota of these compound propagules is likely to improve their chances of successful colonization of unpopulated soil surfaces. Phototrophic microbes can be distinguished in mixed natural communities of undisturbed soil crusts by selective filtration of their autofluorescence spectra. Heterotrophs can be distinguished after staining. The population can be selectively quantified by television image analysis (TVIA) using criteria of pigmentation, size and morphology. Report Antarc* Antarctic Polar Biology Proceedings of the NIPR Symposium on Polar Biology National Institute of Polar Research Repository, Japan Antarctic
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
description The process of colonization of Antarctic fellfield soils by micro-organisms has two phases: Firstly, the immigration, survival and establishment of microbial propagules themselves, and secondly the stabilization of the soil for subsequent colonization and establishment by mosses, lichens and invertebrates. Dominant amongst primary microbial colonizers are the phototrophic cyanobacteria and algae. Not only do they introduce organic nutrients into the microhabitat but they also have a structural function. Filaments of several dimensions frequently form a mesh over the surface of the soil. This mesh often has a canopy structure of fine filaments closely admixed with the mineral soil grains, overlain by a layer of broader, longer filaments. This structure may provide a rich grazing zone for micro-invertebrates such as protozoa and nematodes. Microbial filaments, clusters and unicells frequently have mucilaginous sheaths or capsules which may cement mineral grains together and improve soil crust stability. The combination of filaments and mucigel promotes the formation of microbial "rafts" which are dispersed by wind or water. The diverse microbiota of these compound propagules is likely to improve their chances of successful colonization of unpopulated soil surfaces. Phototrophic microbes can be distinguished in mixed natural communities of undisturbed soil crusts by selective filtration of their autofluorescence spectra. Heterotrophs can be distinguished after staining. The population can be selectively quantified by television image analysis (TVIA) using criteria of pigmentation, size and morphology.
format Report
author David D. WYNN-WILLIAMS
spellingShingle David D. WYNN-WILLIAMS
MICROBIAL COLONIZATION PROCESSES IN ANTARCTIC FELLFIELD SOILS : AN EXPERIMENTAL OVERVIEW (Eleventh Symposium on Polar Biology)
author_facet David D. WYNN-WILLIAMS
author_sort David D. WYNN-WILLIAMS
title MICROBIAL COLONIZATION PROCESSES IN ANTARCTIC FELLFIELD SOILS : AN EXPERIMENTAL OVERVIEW (Eleventh Symposium on Polar Biology)
title_short MICROBIAL COLONIZATION PROCESSES IN ANTARCTIC FELLFIELD SOILS : AN EXPERIMENTAL OVERVIEW (Eleventh Symposium on Polar Biology)
title_full MICROBIAL COLONIZATION PROCESSES IN ANTARCTIC FELLFIELD SOILS : AN EXPERIMENTAL OVERVIEW (Eleventh Symposium on Polar Biology)
title_fullStr MICROBIAL COLONIZATION PROCESSES IN ANTARCTIC FELLFIELD SOILS : AN EXPERIMENTAL OVERVIEW (Eleventh Symposium on Polar Biology)
title_full_unstemmed MICROBIAL COLONIZATION PROCESSES IN ANTARCTIC FELLFIELD SOILS : AN EXPERIMENTAL OVERVIEW (Eleventh Symposium on Polar Biology)
title_sort microbial colonization processes in antarctic fellfield soils : an experimental overview (eleventh symposium on polar biology)
publisher Proceeding
publishDate 1990
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=5098
http://id.nii.ac.jp/1291/00005098/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=5098&item_no=1&attribute_id=18&file_no=1
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Polar Biology
Proceedings of the NIPR Symposium on Polar Biology
genre_facet Antarc*
Antarctic
Polar Biology
Proceedings of the NIPR Symposium on Polar Biology
op_relation https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=5098
http://id.nii.ac.jp/1291/00005098/
AA10819561
Proceedings of the NIPR Symposium on Polar Biology, 3, 164-178(1990-03)
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=5098&item_no=1&attribute_id=18&file_no=1
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