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

• Published in: Antarctic Science
• Main Authors: BARGAGLI, R., SMITH, R. I. L., MARTELLA, L., MONACI, F., SANCHEZ-HERNANDEZ, J. C., UGOLINI, F. C.
• Other Authors: Bargagli, R., Smith, R. I. L., Martella, L., Monaci, F., Ugolini, F. C.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 1999
• Subjects: Edmonson Point; major and trace element; moss community; solution geochemistry; Victoria Land; Antarctic; Antarc*; Antarctic Science; Antarctica
• Online Access: http://hdl.handle.net/11365/10641; https://doi.org/10.1017/S0954102099000024; https://www.cambridge.org/core/journals/antarctic-science/article/solution-geochemistry-and-behaviour-of-major-and-trace-elements-during-summer-in-a-moss-community-at-edmonson-point-victoria-land-antarctica/916D99A9A8174780EC916ADD6A326999

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 mosses were less affected by salt encrustations and there was evidence of Ca2+ uptake and an active cycling of nutrients.