SCLEROSPONGES AS A NEW POTENTIAL RECORDER OF ENVIRONMENTAL CHANGES: LEAD IN CERATOPORELLA NICHOLSONI
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dc.contributor.author | Lazareth C.E. | |
dc.contributor.author | Willenz P. | |
dc.contributor.author | Navez J. | |
dc.contributor.author | Keppens E. | |
dc.contributor.author | Dehairs F. | |
dc.contributor.author | André L. | |
dc.date.accessioned | 2021-02-03T02:18:28Z | |
dc.date.available | 2021-02-03T02:18:28Z | |
dc.date.issued | 2000 | |
dc.identifier | https://elibrary.ru/item.asp?id=31874807 | |
dc.identifier.citation | Geology, 2000, 28, 6, 515-518 | |
dc.identifier.issn | 0091-7613 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/24447 | |
dc.description.abstract | Lead 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.title | SCLEROSPONGES AS A NEW POTENTIAL RECORDER OF ENVIRONMENTAL CHANGES: LEAD IN CERATOPORELLA NICHOLSONI | |
dc.type | Статья |
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