http://www.cnr.it/ontology/cnr/individuo/prodotto/ID20027
Variations in atmospheric trace elements in Dome C (East Antarctica) ice over the last two climatic cycles (Articolo in rivista)
- Type
- Label
- Variations in atmospheric trace elements in Dome C (East Antarctica) ice over the last two climatic cycles (Articolo in rivista) (literal)
- Anno
- 2005-01-01T00:00:00+01:00 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Gabrielli P.; Barbante C.; Boutron C.; Cozzi G.; Gaspari V.; Planchon F.; Ferrari C.; Turetta C.; Hong S.; Cescon P. (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#altreInformazioni
- Il lavoro si propone di ricostruire le sorgenti e le origini degli
elementi in traccia con particolare riferimento allapporto di polveri
crostali, aerosol vulcanico e marino. (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
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- Larticolo illustra landamento delle concentrazioni di vari
elementi in tracce nella carota di ghiaccio antartica denominata EPICA
durante i due ultimi cicli climatici
(literal)
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Laboratoire de Glaciologie et Geophysique de l'Environnement du CNRS, St Martin d'Heres Cedex, France e Department of Environmental Sciences, University of Venice, Ca' Foscari, Venice, Italy;
Department of Environmental Sciences, University of Venice, Ca' Foscari, Venice, Italy e Institute for the Dynamics of Environmental Processes-CNR, Venice, Italy;
Laboratoire de Glaciologie et Ge´ophysique de l'Environnement du CNRS, St Martin d'Heres Cedex, France e Observatoire des Sciences de l'Univers et Unite´ de Formation et de Recherche de Physique (Institut Universitaire de France), Universite´ Joseph Fourier, Domaine Universitaire, Grenoble, France;
Department of Environmental Sciences, University of Venice, Ca' Foscari, 30123 Venice, Italy;
Department of Environmental Sciences, University of Venice, Ca' Foscari, 30123 Venice, Italy;
Department of Environmental Sciences, University of Venice, Ca' Foscari, 30123 Venice, Italy;
Laboratoire de Glaciologie et Ge´ophysique de l'Environnement du CNRS, St Martin d'Heres Cedex, France e Polytech Grenoble (Institut Universitaire de France), Universite´ Joseph Fourier, 28 avenue Beno?^t Frachon, B.P. 53, 38041 Grenoble, France;
Institute for the Dynamics of Environmental Processes-CNR, 30123 Venice, Italy;
Korea Polar Research Institute, KORDI, Ansan, PO Box 29, Seoul 426-744, Republic of Korea;
Department of Environmental Sciences, University of Venice, Ca' Foscari, Venice, Italy e Institute for the Dynamics of Environmental Processes-CNR, Venice, Italy. (literal)
- Titolo
- Variations in atmospheric trace elements in Dome C (East Antarctica) ice over the last two climatic cycles (literal)
- Abstract
- Concentrations of Li, Mg, Cr, Mn, Co, Cu, As, Rb, Cd, Ba and Bi have been determined by inductively coupled
plasma sector field mass spectrometry (ICP-SFMS) in various sections of the new Dome C EPICA Antarctic ice core,
down to the depth of 2193 m, covering a time period of two climatic cycles. The time resolution of these records is at
least twice as good as previously published ultra trace elements profiles obtained from the Vostok ice core. During the
~217 kyr period spanned by this record, a high variability in concentrations is observed for most elements, with low
values during warm periods and high values during cold periods. The highest concentrations are recorded at the times
of the last two glacial maxima (~20 and ~140 kyr BP). The timing and the amplitude of the main concentration peaks
match remarkably well the insoluble dust concentration profile. It confirms that dust was the main carrier of
atmospheric trace elements to East Antarctica during the cold periods. For Ba, Co, Cu and Rb the crustal contribution
was also dominant during warm periods. For other elements the situation is more complex during interglacial periods,
when other sources such as volcanic quiescent emissions, became possibly significant for several trace elements such as
Cd and Bi. Peculiarly high concentration values are observed for Cd and Bi for a short depth interval dated at ~18 kyr
BP. It is the same depth interval in which elevated F- values were previously observed. These very high concentrations
are attributed to fallout from major local volcanic emissions at that time. (literal)
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