SCLEROSPONGES AS A NEW POTENTIAL RECORDER OF ENVIRONMENTAL CHANGES: LEAD IN CERATOPORELLA NICHOLSONI

dc.contributor.authorLazareth C.E.
dc.contributor.authorWillenz P.
dc.contributor.authorNavez J.
dc.contributor.authorKeppens E.
dc.contributor.authorDehairs F.
dc.contributor.authorAndré L.
dc.date.accessioned2021-02-03T02:18:28Z
dc.date.available2021-02-03T02:18:28Z
dc.date.issued2000
dc.description.abstractLead concentrations have been analyzed on a 223 yr profile through the aragonitic skeleton of the reef-building Caribbean sclerosponge Ceratoporella nicholsoni by using laser-ablation inductively coupled plasma-mass spectrometry. A parallel study of the δ13C distribution in the skeleton validates the previously established mean annual growth rate of 230 μm/yr, at least for long-term important environmental changes. The Pb trend in the specimen displays a general increase from 0.30 ppm ca. A.D. 1760 to 2.15 ppm ca. A.D. 1984; a major threefold increase occurred after 1930. This Pb profile is analogous to results acquired from ice or coral cores and clearly highlights the potential of sclerosponges as a new proxy of environmental changes for time series extending over several centuries.
dc.identifierhttps://elibrary.ru/item.asp?id=31874807
dc.identifier.citationGeology, 2000, 28, 6, 515-518
dc.identifier.issn0091-7613
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/24447
dc.titleSCLEROSPONGES AS A NEW POTENTIAL RECORDER OF ENVIRONMENTAL CHANGES: LEAD IN CERATOPORELLA NICHOLSONI
dc.typeСтатья

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