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Microbial communities of ultramafic soils in maquis and rainforest at Mont Do, New Caledonia

Authors :
Tanguy Jaffré
Lesley S. Rigg
Neal J. Enright
Melissa Lenczewski
Heidi Kelly
Geology and Environmental Geosciences
Northern Illinois University
Biological Sciences & Geography
Botanique et Modélisation de l'Architecture des Plantes et des Végétations (UMR AMAP)
Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Institut National de la Recherche Agronomique (INRA)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])
Laboratoire de Botanique et d'Écologie Végétale Appliquée
School of Environmental Science
Murdoch University
Centre National de la Recherche Scientifique (CNRS)-Université de Montpellier (UM)-Institut National de la Recherche Agronomique (INRA)-Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Institut de Recherche pour le Développement (IRD [France-Sud])
Source :
Austral Ecology, Austral Ecology, Wiley, 2009, 34 (5), pp.567-576. ⟨10.1111/j.1442-9993.2009.01962.x⟩
Publication Year :
2009
Publisher :
Wiley, 2009.

Abstract

A-09-41; International audience; We analysed variation in microbial community richness and function in soils associated with a fire-induced vegetation successional gradient from low maquis (shrubland) through tall maquis to rainforest on metal-rich ultramafic soils at Mt Do, New Caledonia. Random amplified polymorphic DNA fingerprinting was used to determine the extent of genetic relatedness among the microbial communities and indicated that the open and tall maquis microbial communities were more similar to each other than they were to the rainforest community. Sole-source carbon utilization indicated variation in the microbial communities, again with greater diversity in rainforest soils. Plate counts showed that both rainforest and maquis soils contained bacteria that can grow in the presence of up to 20 mmol L−1 nickel and 10 mmol L−1 chromium. Understanding microbial community composition and dynamics in these ultramafic soils may lead to a better understanding of the processes facilitating vegetation succession from shrubland to forest on these high-metal substrates, and of approaches to successful revegetation following mining for metals including nickel, chromium and cobalt.

Details

ISSN :
14429993 and 14429985
Volume :
34
Database :
OpenAIRE
Journal :
Austral Ecology
Accession number :
edsair.doi.dedup.....2d7122742eecfc28b8b6d59392cbe199
Full Text :
https://doi.org/10.1111/j.1442-9993.2009.01962.x