Biogeochemical cycling of Pb in the coastal marine environment at Terra Nova Bay, Ross Sea

The biogeochemical cycle of lead in the marine coastal environment of Terra Nova Bay has been investigated by determining the lead concentration in a large number of matrices: marine sediments, pack ice, snow, seawater, marine microlayer, aerosol and eight species of marine organisms (the bivalve mo...

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Published in:Antarctic Science
Main Authors: RIVA, S. DALLA, ABELMOSCHI, M.L., CHIANTORE, M., GROTTI, M., MAGI, E., SOGGIA, F.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2003
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102003001524
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102003001524
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spelling crcambridgeupr:10.1017/s0954102003001524 2024-09-09T19:05:49+00:00 Biogeochemical cycling of Pb in the coastal marine environment at Terra Nova Bay, Ross Sea RIVA, S. DALLA ABELMOSCHI, M.L. CHIANTORE, M. GROTTI, M. MAGI, E. SOGGIA, F. 2003 http://dx.doi.org/10.1017/s0954102003001524 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102003001524 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 15, issue 4, page 425-432 ISSN 0954-1020 1365-2079 journal-article 2003 crcambridgeupr https://doi.org/10.1017/s0954102003001524 2024-07-17T04:03:47Z The biogeochemical cycle of lead in the marine coastal environment of Terra Nova Bay has been investigated by determining the lead concentration in a large number of matrices: marine sediments, pack ice, snow, seawater, marine microlayer, aerosol and eight species of marine organisms (the bivalve molluscs Adamussium colbecki and Laternula elliptica , the seastar Odontaster validus , the sea urchin Sterechinus neumayeri , the fish Trematomus bernacchii , the seaweeds Iridaea cordata and Phyllophora antarctica , and the nemertine worm Parborlasia corrugatus ). The study of solid speciation of sediment showed that the site is not influenced by human activity and is hence suitable to examine natural processes. The concentration values found in the suspended paniculate matter (SPM) of pack ice core, aerosol, marine microlayer and seawater as well as the particulate morphology, investigated by SEM, seem to support the hypothesis that particulate lead is transferred from the atmosphere to the water column through three different mechanisms: (i) release of SPM from the pack ice during its melting, (ii) input from the continental land through wet deposition, (iii) transport by aerosol and marine microlayer. Concentration data both in the whole organism and in some target organs indicated two suitable biomonitor organisms: the bivalva Laternula elliptica (particularly its digestive gland) and the fish Trematomus bernacchii (particularly its bones). Article in Journal/Newspaper Antarc* Antarctic Science Antarctica ice core Ross Sea Cambridge University Press Ross Sea Terra Nova Bay Antarctic Science 15 4 425 432
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description The biogeochemical cycle of lead in the marine coastal environment of Terra Nova Bay has been investigated by determining the lead concentration in a large number of matrices: marine sediments, pack ice, snow, seawater, marine microlayer, aerosol and eight species of marine organisms (the bivalve molluscs Adamussium colbecki and Laternula elliptica , the seastar Odontaster validus , the sea urchin Sterechinus neumayeri , the fish Trematomus bernacchii , the seaweeds Iridaea cordata and Phyllophora antarctica , and the nemertine worm Parborlasia corrugatus ). The study of solid speciation of sediment showed that the site is not influenced by human activity and is hence suitable to examine natural processes. The concentration values found in the suspended paniculate matter (SPM) of pack ice core, aerosol, marine microlayer and seawater as well as the particulate morphology, investigated by SEM, seem to support the hypothesis that particulate lead is transferred from the atmosphere to the water column through three different mechanisms: (i) release of SPM from the pack ice during its melting, (ii) input from the continental land through wet deposition, (iii) transport by aerosol and marine microlayer. Concentration data both in the whole organism and in some target organs indicated two suitable biomonitor organisms: the bivalva Laternula elliptica (particularly its digestive gland) and the fish Trematomus bernacchii (particularly its bones).
format Article in Journal/Newspaper
author RIVA, S. DALLA
ABELMOSCHI, M.L.
CHIANTORE, M.
GROTTI, M.
MAGI, E.
SOGGIA, F.
spellingShingle RIVA, S. DALLA
ABELMOSCHI, M.L.
CHIANTORE, M.
GROTTI, M.
MAGI, E.
SOGGIA, F.
Biogeochemical cycling of Pb in the coastal marine environment at Terra Nova Bay, Ross Sea
author_facet RIVA, S. DALLA
ABELMOSCHI, M.L.
CHIANTORE, M.
GROTTI, M.
MAGI, E.
SOGGIA, F.
author_sort RIVA, S. DALLA
title Biogeochemical cycling of Pb in the coastal marine environment at Terra Nova Bay, Ross Sea
title_short Biogeochemical cycling of Pb in the coastal marine environment at Terra Nova Bay, Ross Sea
title_full Biogeochemical cycling of Pb in the coastal marine environment at Terra Nova Bay, Ross Sea
title_fullStr Biogeochemical cycling of Pb in the coastal marine environment at Terra Nova Bay, Ross Sea
title_full_unstemmed Biogeochemical cycling of Pb in the coastal marine environment at Terra Nova Bay, Ross Sea
title_sort biogeochemical cycling of pb in the coastal marine environment at terra nova bay, ross sea
publisher Cambridge University Press (CUP)
publishDate 2003
url http://dx.doi.org/10.1017/s0954102003001524
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102003001524
geographic Ross Sea
Terra Nova Bay
geographic_facet Ross Sea
Terra Nova Bay
genre Antarc*
Antarctic Science
Antarctica
ice core
Ross Sea
genre_facet Antarc*
Antarctic Science
Antarctica
ice core
Ross Sea
op_source Antarctic Science
volume 15, issue 4, page 425-432
ISSN 0954-1020 1365-2079
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0954102003001524
container_title Antarctic Science
container_volume 15
container_issue 4
container_start_page 425
op_container_end_page 432
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