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Solution geochemistry and behaviour of major and trace elements during summer in a moss community at Edmonson Point, Victoria Land, Antarctica

Bargagli, R.; Smith, R.I.L.; Martella, L.; Monaci, F.; Sanchez-Hernandez, J.C.; Ugolini, F.C.. 1999 Solution geochemistry and behaviour of major and trace elements during summer in a moss community at Edmonson Point, Victoria Land, Antarctica. Antarctic Science, 11 (01). 3-12. 10.1017/S0954102099000024

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Text (This article has been accepted for publication and will appear in a revised form in Antarctic Science, published by Cambridge University Press. Copyright Antarctic Science Ltd.)
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Abstract/Summary

Physical and chemical characteristics and solution geochemistry of major and trace elements were investigated in an area of volcanic soil colonized by mosses at Edmonson Point (central Victoria Land) during the international BIOTAS (Biological Investigations of Terrestrial Antarctic Systems) expedition (BIOTEX) in the 1995–96 summer. The broad objective was to study the environmental factors involved in plant colonisation and survival in terrestrial continental Antarctic ecosystems. The results showed that moss distribution and survival throughout the summer was closely dependent on water supply. In Antarctic coastal ecosystems the environmental biogeochemistry is largely dominated by ions of marine origin. At the drier end of a hydrological gradient the dry cushions of Hennediella heimii were encrusted with salts and showed much higher concentrations of soluble ions (Na+, Cl−, K+, Ca2+, Mg2+, SO42−, NO3−) than those in adhering soil particles or in other moss species from wetter parts of the transect. Although salt encrustations may partly derive from sublimation of surface snow, comparisons between concentrations of soluble ions in the dry moss and those in the < 2 mm fraction of surface and deep soil showed an upward migration along the soil profile of soluble ions as the substratum dried out, between December and January, and their accumulation mostly on mosses. At the wet end of the transect messes were less affected by salt encrustations and there was evidence of Ca2+ uptake and an active cycling of nutrients.

Item Type: Publication - Article
Digital Object Identifier (DOI): 10.1017/S0954102099000024
Programmes: BAS Programmes > Pre 2000 programme
ISSN: 0954-1020
Additional Keywords: Edmonson Point, major and trace elements, moss community, solution geochemistry, Victoria Land
Date made live: 20 Aug 2013 09:25 +0 (UTC)
URI: http://nora.nerc.ac.uk/id/eprint/503003

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