Massive corals in Paleocene siliciclastic sediments of Chubut (Argentina)
A horizon with large, massive corals in growth position was discovered in the Paleocene, probably upper Danian, part of the Maastrichtian-Paleocene Lefipán Formation of Chubut (Patagonia, Argentina). All corals belong to one species, the cosmopolitan Haimesiastraea conferta Vaughan, which survived t...
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2005
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| LEADER | 12662caa a22011057a 4500 | ||
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| 001 | PAPER-3887 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518203321.0 | ||
| 008 | 190411s2005 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-29944434210 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Kiessling, W. | |
| 245 | 1 | 0 | |a Massive corals in Paleocene siliciclastic sediments of Chubut (Argentina) |
| 260 | |c 2005 | ||
| 270 | 1 | 0 | |m Kiessling, W.; Institut für Paläontologie, Museum für Naturkunde, Humboldt-Universität Berlin, Invalidenstr. 43, D-10115 Berlin, Germany; email: wolfgang.kiessling@museum.hu-berlin.de |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a A horizon with large, massive corals in growth position was discovered in the Paleocene, probably upper Danian, part of the Maastrichtian-Paleocene Lefipán Formation of Chubut (Patagonia, Argentina). All corals belong to one species, the cosmopolitan Haimesiastraea conferta Vaughan, which survived the end-Cretaceous mass extinction. The occurrence of massive corals at this site is exceptional both because of the siliciclastic depositional regime and because of the high palaeolatitude setting. An unusual autecology of this coral and strongly reduced sedimentation rates, were probably the prerequisites for coral growth, but a link to palaeoclimate is less likely. © Springer-Verlag 2005. |l eng | |
| 536 | |a Detalles de la financiación: Deutsche Forschungsgemeinschaft, Ki 806-1 | ||
| 536 | |a Detalles de la financiación: Fundación Antorchas | ||
| 536 | |a Detalles de la financiación: Acknowledgments Research on the KT boundary in Patagonia is supported by the Deutsche Forschungsgemeinschaft (DFG, Ki 806-1), the Antorchas Foundation (República Argentina) and the European Community program “Improving Human Research Potential and the Socio-Economic Knowledge Base”. We thank Rosemarie Baron-Szabo for advice regarding the taxonomic status of H. con-ferta, and Lucas Ruiz and Sven Weidemeyer for assistance in the field. | ||
| 593 | |a Institut für Paläontologie, Museum für Naturkunde, Humboldt-Universität Berlin, Invalidenstr. 43, D-10115 Berlin, Germany | ||
| 593 | |a Centro de Investigaciones Geológicas, Universidad Nacional de La Plata 1 No 644, 1900 La Plata, Argentina | ||
| 593 | |a Departamento de Ciencias Geológicas, FCEN, Universidad de Buenos Aires, Pab. 2, 1o Piso, 1428 Buenos Aires, Argentina | ||
| 593 | |a Department für Geo-und Umweltwissenschaften, Ludwig-Maximilians-Universität München, Richard-Wagner-Str. 10, D-80333 München, Germany | ||
| 593 | |a Instituto de Geologïa y Mineria, Universidad Nacional de Jujuy, C. Correo 258, 4600 S.S. de Jujuy, Argentina | ||
| 690 | 1 | 0 | |a BIOEROSION |
| 690 | 1 | 0 | |a CORALS |
| 690 | 1 | 0 | |a ECOLOGY |
| 690 | 1 | 0 | |a MASS EXTINCTION |
| 690 | 1 | 0 | |a PALEOCENE |
| 690 | 1 | 0 | |a SILICICLASTICS |
| 690 | 1 | 0 | |a CORAL REEF |
| 690 | 1 | 0 | |a MASS EXTINCTION |
| 690 | 1 | 0 | |a PALEOCENE |
| 690 | 1 | 0 | |a SILICICLASTIC DEPOSIT |
| 690 | 1 | 0 | |a ANTHOZOA |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a CHUBUT | |
| 651 | 4 | |a SOUTH AMERICA | |
| 700 | 1 | |a Aragón, E. | |
| 700 | 1 | |a Scasso, R. | |
| 700 | 1 | |a Aberhan, M. | |
| 700 | 1 | |a Kriwet, J. | |
| 700 | 1 | |a Medina, F. | |
| 700 | 1 | |a Fracchia, D. | |
| 773 | 0 | |d 2005 |g v. 51 |h pp. 233-241 |k n. 1-4 |p Facies |x 01729179 |t Facies | |
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