1,721,000 research outputs found

    Biomagnification of mercury in an Antarctic marine coastal food web

    No full text
    Total Hg concentrations were determined in marine sediments and biota from the inner shelf of Terra Nova Bay (Antarctica). Like published data on air, snow and soils from the same region, Hg levels in the finest fraction of marine sediments were among the lowest ever reported for coastal marine environments (0.012 ± 0.007 μg g-1 dry wt). A progressive increase in Hg concentrations was found in organisms at different levels of the marine food web (phytoplankton < zooplankton and benthic primary consumers < detritivorous and opportunistic benthic invertebrates < epipelagic fish < demersal fish and plankton-feeding seabirds < fish-eating penguins < predatory birds and Weddell seal). In general, primary producers and consumers showed slightly lower Hg concentrations (0.076 ± 0.023 μg g-1 dry wt) than organisms of related species from other seas, but values in feathers (2.91 ± 1.93 μg g-1 dry wt) of the Antarctic skua and in tissues of a Weddell seal (44.0 and 24.0 μg g-1 dry wt in the liver and spleen, respectively) were similar to those in skuas and seals from the northern hemisphere. Trophic connections between organisms in well developed benthic communities, phytoplankton and fish and environmental factors such as enhanced upwelling of cold water, sea ice and low light are deemed to enhance natural biomagnification processes of Hg in the pristine Antarctic coastal environment

    Mercury, cadmium and lead accumulation in Antarctic mosses growing along nutrient and moisture gradients

    No full text
    Accumulation of Hg, Cd and Pb by moss was studied in a coastal ice-free area (Edmonson Point, northern Victoria Land) in relation to the water and nutrient availability and substratum characteristics. Although metal concentrations in surface soils were among the lowest ever reported from remote areas, those of Hg and Cd in mosses were higher, being in the same range as those usually reported in regional surveys in the northern hemisphere. By contrast, Antarctic mosses showed very low Pb concentrations, and no impact from local human activities was detected. Marine aerosols, seabird guano and volcanic emissions appeared to be the more probable sources of Cd and Hg. Besides atmospheric deposition, the main pathway of metals to mosses was probably through evapo-transpiration at their surface which determines an upward migration of ions and their bioaccumulation

    Baseline concentrations of elements in the Antarctic macrolichen Umbilicaria decussata

    No full text
    Total concentrations of major and trace elements were determined in samples of the epilithic lichen Umbilicaria decussata from 24 ice-free areas in coastal Victoria Land (Antarctica). Overall average concentrations of trace elements except Cd were the lowest ever reported for lichens of the genus Umbilicaria. Specifically, the mean level of Pb in lichens from granitic rocks (0.46 ± 0.18 μg g-1 dry wt) was more than four times lower than the lowest record in Arctic lichens. No impact of local human activities was detected, but the elemental composition of U. decussata was affected by entrapment of soil or rock dust particles and probably by uptake of soluble elements from substrate. Relationships between elements and their distribution patterns in the study area indicated that the marine environment is the main source of major ions and perhaps of Cd in lichens. Accumulation of P was detected in samples from coastal sites frequented by seabirds. Although the present results can be taken as baseline levels of major and trace elements in Antarctic U. decussata from substrates with very different geochemical features, further research is necessary to evaluate the relative element contribution from each substrate with respect to those from snow, marine aerosol, salt encrustations and guano

    Environmental factors promoting bioaccumulation of Hg and Cd in Antarctic marine and terrestrial organisms

    No full text
    Continental Antarctica is almost unaffected by long-range atmospheric transport ofheavy metals and contlIDination due te human activities has only been detected in very localised areas. Concentrations ofmetals in most abiotic environmental matrices are therefore among the lowest in the world. Despite these pristine environmental conditions, lichens, mosses and several anitnal taxa dominating coastal marine ecosystems of northern Victoria Land (continentaf Antarctica) .show surprisingly high concentrations of cadmium and mercury (i.e. similar to or higher than those measured in related . species in the northern hemisphere). Besides the slow growth rate (Le. long exposure time) and other ecophysiological characteristics ofAntarctic organisms, environmental factors such as upwelling of deep marine waters and ice-cover are presumably involved in the bioaccumulation of cadmium and mercury. These metals from the marine environment also reach cryptogarns in coastal ice-free areas through marine aerosol, seabird guano and snow precipitation. In coastal marine ecosystems, food webs are much more complex than the krill system in oceano waters. The involvement of benthic organisrns lengthens the chains and enhances the biomagnification of mercury (plankton &lt; benthic invertebrates &lt; demersal fish &lt; fish-eating birds and mammals)

    Organochlorine pollutants in soils and mosses from Victoria Land (Antarctica)

    No full text
    The major organochlorine (OC) pollutants, i.e. pentachlorobenzene (PCBz), hexachlorobenzene (HCB), hexachlorocyclohexanes (HCHs), polychlorobiphenyls (PCBs) and DDTs have been analyzed in soils and mosses from coastal areas of Victoria Land (70-80degreesS, 160-170degreesE). PCBs (23-34 ng g(-1) dry wt.) and PCBz (0.38-1.3 ng g(-1) dry wt.) were the dominant OCs in mosses and soils, respectively. In general, the concentrations of OC in soils, i.e. HCB (0.034-0.17 ng g(-1) dry wt.), PCBs (0.36-0.59 ng g(-1) dry wt.) and 4,4'-DDE (0.053-0.086 ng g(-1) dry wt.), range among the lowest reported in remote regions. These concentrations exhibited high correlation coefficients when represented vs. total organic carbon (TOC) which is consistent with the general correlation between OC and TOC in soils from remote areas recently observed (Meijer, S.N., Ockenden, W.A., Seetman, A., Breivik, K., Grimalt, J.O., Jones, K.C., 2003. Global distribution and budget of PCBs and HCB in background surface soils: implications for sources and environmental processes. Environ. Sci. Technol. 37, 667-672). Statistically significant dependences between reciprocal of temperature and log-transformed concentrations of HCB and 4,4'-DDE in mosses and alpha-HCH in soils have been found. These observations provide further data illustrating that temperature is a major factor determining the planetary scale distribution and accumulation of OCs giving additional ground to the general validity of the global distillation effect for description of planetary OC distribution. (C) 2004 Elsevier Ltd. All rights reserved
    corecore