http://www.cnr.it/ontology/cnr/individuo/prodotto/ID20041
A 220 ky record of Pb isotopes at Dome C Antarctica from analyses of the EPICA ice core. (Articolo in rivista)
- Type
- Label
- A 220 ky record of Pb isotopes at Dome C Antarctica from analyses of the EPICA ice core. (Articolo in rivista) (literal)
- Anno
- 2005-01-01T00:00:00+01:00 (literal)
- Alternative label
Vallelonga P., Gabrielli P., Rosman K.J.R., Barbante C., Boutron C.F. (2005)
A 220 ky record of Pb isotopes at Dome C Antarctica from analyses of the EPICA ice core.
in Geophysical research letters
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Vallelonga P., Gabrielli P., Rosman K.J.R., Barbante C., Boutron C.F. (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#altreInformazioni
- Il lavoro si propone di ricostruire le sorgenti e le origini del
piombo con particolare riferimento allapporto di polveri crostali ed
aerosol vulcanici.
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#descrizioneSinteticaDelProdotto
- Larticolo illustra landamento delle concentrazioni del piombo
ed i suoi isotopi nella carota di ghiaccio antartica denominata EPICA
durante i due ultimi cicli climatici.
(literal)
- Note
- ISI Web of Science (WOS) (literal)
- Titolo
- A 220 ky record of Pb isotopes at Dome C Antarctica from analyses of the EPICA ice core. (literal)
- Abstract
- Pb isotopic compositions and Pb and Ba concentrations
are reported in EPICA Dome C ice core samples dating to
220 kyr BP, indicating that Pb isotopic compositions in
Antarctic ice vary with changing climate. 206Pb/207Pb ratios
decrease during glacial periods, with the lowest values
occurring during colder climatic periods (stages 2, 4 and 6)
and the Holocene. Low Pb concentrations (<1 pg/g) were
found during the Holocene and the last interglacial (climate
stage 5.5) while higher Pb concentrations (>10 pg/g) were
found during cold climatic periods. Ba, a proxy for mineral
dust, was used to determine that dust usually accounts for
~70% of Pb in Dome C ice, while the remaining ~30% was
attributed to volcanic emissions. Pb isotopic compositions at
Dome C differ from those reported in pre-industrial ice from
other Antarctic locations, due to greater proportions
of dust Pb at Dome C. (literal)
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