A tsunami deposit at the Cretaceous/Paleogene boundary in the Neuquén Basin of Argentina
A coarse-grained sandstone bed of Cretaceous/Paleogene (K/Pg) boundary age occurs in a homogeneous neritic shelf mudstone sequence (Jagüel Formation) in the Neuquén Basin of Argentina. This bed, 15 - 25 cm thick, contains abundant plagioclase, broken shells and sharks' teeth. Sedimentological f...
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2005
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| 005 | 20230518203341.0 | ||
| 008 | 190411s2005 xx ||||fo|||| 00| 0 eng|d | ||
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| 100 | 1 | |a Scasso, R.A. | |
| 245 | 1 | 2 | |a A tsunami deposit at the Cretaceous/Paleogene boundary in the Neuquén Basin of Argentina |
| 260 | |c 2005 | ||
| 270 | 1 | 0 | |m Kiessling, W.; Museum für Naturkunde, Institut für Paläontologie, 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 coarse-grained sandstone bed of Cretaceous/Paleogene (K/Pg) boundary age occurs in a homogeneous neritic shelf mudstone sequence (Jagüel Formation) in the Neuquén Basin of Argentina. This bed, 15 - 25 cm thick, contains abundant plagioclase, broken shells and sharks' teeth. Sedimentological features include an erosive base, abundant rip-up clasts, normal grading and hummocky cross-bedding. The K/Pg boundary age of the bed was confirmed by calcareous nannofossils. Similar to other sections in the Gulf Coast region and the Danish Basin, a "dead zone" significantly depleted in macrofossils is evident in the basal 1 m above the clastic layer. In combination, these features suggest that the clastic layer represents a tsunami deposit that was related to the Chicxulub impact event in Yucatan/Mexico. Mechanisms of tsunami wave amplification in this extremely distal and somewhat protected setting are poorly understood but the funnel-shape of the basin may have promoted the unusually strong sedimentological response. © 2005 Elsevier Ltd. All rights reserved. |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: We thank the reviewers J.R. Ineson and E. Koutsoukos, whose comments led to a significantly improved manuscript. This study is funded by the Deutsche Forschungsgemeinschaft (DFG, Ki 806-1) and the Antorchas Foundation. We thank Ralf Schmitt for XRF analyses, Henning Scholz, Lucas Ruiz and Natalia Scaricabarozzi for assistance in the field, and D.J. Batten for his editorial work. | ||
| 593 | |a Departamento de Ciencias Geologicas, FCEN, Universidad de Buenos Aires, 1428 Buenos Aires, Argentina | ||
| 593 | |a Museum für Naturkunde, Institut für Paläontologie, Humboldt-Universität Berlin, Invalidenstr. 43, D-10115 Berlin, Germany | ||
| 593 | |a Museum für Naturkunde, Institut für Mineralogie, Humboldt-Universität Berlin, Invalidenstr. 43, D-10115 Berlin, Germany | ||
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a NEUQUEN BASIN | |
| 651 | 4 | |a SOUTH AMERICA | |
| 690 | 1 | 0 | |a CRETACEOUS/PALEOGENE BOUNDARY |
| 690 | 1 | 0 | |a MASS EXTINCTION |
| 690 | 1 | 0 | |a PATAGONIA |
| 690 | 1 | 0 | |a TSUNAMI |
| 690 | 1 | 0 | |a CRETACEOUS-TERTIARY BOUNDARY |
| 690 | 1 | 0 | |a MASS EXTINCTION |
| 690 | 1 | 0 | |a METEORITE |
| 690 | 1 | 0 | |a STORM DEPOSIT |
| 690 | 1 | 0 | |a TSUNAMI |
| 690 | 1 | 0 | |a WESTERN HEMISPHERE |
| 690 | 1 | 0 | |a WORLD |
| 690 | 1 | 0 | |a CHONDRICHTHYES |
| 700 | 1 | |a Concheyro, A. | |
| 700 | 1 | |a Aberhan, M. | |
| 700 | 1 | |a Hecht, L. | |
| 700 | 1 | |a Medina, F.A. | |
| 700 | 1 | |a Tagle, R. | |
| 773 | 0 | |d 2005 |g v. 26 |h pp. 283-297 |k n. 2 |p Cretaceous Res. |x 01956671 |w (AR-BaUEN)CENRE-4335 |t Cretaceous Research | |
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