Luterbacher | Contributions to the Stratigraphy of the Paleogene | Buch | 978-3-510-66042-1 | sack.de

Buch, Englisch, Band 234, 440 Seiten, Format (B × H): 160 mm x 240 mm, Gewicht: 820 g

Reihe: Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen

Luterbacher

Contributions to the Stratigraphy of the Paleogene

Symposium on the Paleogene 25-30 August 2003, Leuven, Belgium

Buch, Englisch, Band 234, 440 Seiten, Format (B × H): 160 mm x 240 mm, Gewicht: 820 g

Reihe: Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen

ISBN: 978-3-510-66042-1
Verlag: E. Schweizerbart


This volume contains 15 English-language contributions to the?Symposium on the Paleogene? organized by Noël Vandenberghe in Leuven (Belgium) in August 2003 under the auspices of the International Subcommission on Paleogene Stratigraphy which is part of the International Commission on Stratigraphy of the International Commission of Geological Sciences. The objective of this subcommission is to encourage research into the Paleogene by establishing working groups dealing with specific problems, in particular the agreement on an international set of stages and series defined by boundary stratotypes, and organizing general symposia and thematic meetings. Ph.D.Gingerich demonstrates that the increase in diversity of the vertebrates is greatest during the late Paleocene and early Eocene and stresses the importance of the Paleogene for the understanding both vertebrate history back to the deeper past and forward to the present Two papers are dedicated to the evolution of the foraminiferal faunas at the Cretaceous/Paleogene boundary. Alegret et al. establish a succession of events affecting the foraminiferal faunas in the Tethyan and Gulf of Mexico across the boundary interval. The planktonic foraminiferal extinction patterns during the Campanian-Maastrichtian and at the Cretaceous/Paleogene boundary studied in detail by El-Sabbagh et al. in two sections of the Western Central Sinai represent?normal? background extinctions below the Cretaceous/Paleogene boundary, whereas the extinction of 45 species at the boundary level is compatible with the effects of a large meteorite impact. The study of the larger foraminifera of the Paleogene succession of the Island of Masirah (Oman) allows to recognize early to middle Lutetian and early Oligocene shallow-marine carbonates (Menkfeld-Gfeller Decrouez). The critical species are discussed and illustrated. The biostratigraphy of the middle to late Eocene part of the Valle della Contessa and the Monte Gagnero sections in Central Italy is revised by Verducci Nocchi based on planktonic foraminifera determined mainly in thin section. Problems in the correlation with the magnetostratigraphy and the boundaries of the Paleogene stages are discussed. The numerous illustration of the planktonic foraminiferal species are very useful for studies of Paleogene carbonates restricted to thin sections.
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Gingerich, P. D.: Paleogene vertebrates and their response to environmental change. (With 7 figures and 1 table) 1-23

Alegret, L., Arenillas, I., Arz, J. A. & Molina, E.: Foraminiferal event-stratigraphy across the Cretaceous/Paleogene boundary. (With 10 figures) 25-50

El-Sabbagh, A. M., Ibrahim, M. I. A. & Luterbacher, H. P.: Planktic foraminiferal biostratigraphy, extinction patterns and turnover during the Campanian-Maastrichtian and at the Cretaceous/Paleogene (K/Pg) boundary in the Western Central Sinai, Egypt. (With 26 figures) 51-120

Fluegeman, R. H.: Preliminary study of the Paleocene Planktonic Foraminifera from the John Crow Mountains Belt, Portland, Eastern Jamaica. (With 7 figures and 2 tables) 121-136

Akhmetiev, M. A. & Beniamovski, V. N.: Paleocene and Eocene of Western Eurasia (Russian sector) stratigraphy, palaeogeography, climate. (With 18 figures) 137-181

Beniamovski, V. N.: Paleocene benthic foraminiferal ecozones of the northern Peri-Tethys. (With 9 figures) 183-199

Oreshkina, T. V., Aleksandrova, G. N. & Kozlova, G. E.: Early Eocene marine planktonic record of the East Urals margin (Sverdlovsk region): biostratigraphy and paleoenvironments. (With 6 figures) 201-222

Orue-Etxebar ria, X., Bernaola, G., Baceta, J. I., Angori, E., Caballero, F., Monechi, S., Pujalte, V., Dinarès-Tutrell, J., Apellaniz, E. & Payros, A.: New constraints on the evolution of planktic foraminifers and calcareous nannofossils across the Paleocene-Eocene boundary interval: the Zumaia section revisited. (With 12 figures) 234-259

Aref, M. & Youssef, M.: The benthonic foraminifera turnover at the Paleocene/Eocene Thermal Maximum Event (PETM) in the southwestern Nile Valley, Egypt. (With 12 figures) 261-289

Youssef, M. & Mutterlose, J.: The calcareous nannofossil turnover across the Paleocene-Eocene Thermal Maximum event (PETM) in the southwestern Nile Valley, Egypt. (With 7 figures) 291-309

Menkveld-Gfeller, U. & Decrouez, D.: The Paleogene of Masirah Island (Sultanate of Oman). (With 9 figures) 311-333

Zakrevskaya, E. Yu.: Distribution of larger foraminifera near the Lower-Middle Eocene boundary in the northeastern Peritethys. (With 7 figures and 1 table) 335-360

Verducci, M. & Nocchi, M.: Middle to Late Eocene main planktonic foraminiferal events in the Central Mediterranean area (Umbria-Marche Basin) related to paleoclimatic changes. (With 22 figures and 2 tables) 361-413

Podobina, V. M.: The Latdorfian stage and the lower Oligocene foraminiferal zones of the West-Siberian Plain. (With 1 table) 415-431 Gladenkov, Yu. B.: The Oligocene of Sakhalin. (With 2 figures) 433-440


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