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Climate and Biota of the Early Paleogene: recent advances and new perspectives |
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V. PUJALTE, A. PAYROS and E. APELLANIZ
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DOI: 10.1344/105.000000283
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Late Maastrichtian-Early Paleocene sea level and climate changes in the Antioch Church Core (Alabama, Gulf of Mexico margin, USA): A multi-proxy approach |
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PETER SCHULTE and ROBERT P. SPEIJER
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DOI: 10.1344/105.000000279
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A Danian subtropical lacustrine palynobiota from South America (Bororó Formation, San Jorge Basin, Patagonia - Argentina) |
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L. SCAFATI, D.L. MELENDI and W. VOLKHEIMER
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DOI: 10.1344/105.000000270
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Biostratigraphy of the Danian/Selandian transition in the southern Tethys. Special reference to the Lowest Occurrence of planktic foraminifera Igorina albeari |
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J. SPRONG, R.P. SPEIJER and E. STEURBAUT
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DOI: 10.1344/105.000000271
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New high resolution calcareous nannofossil analysis across the Danian/Selandian transition at the Zumaia section: comparison with South Tethys and Danish sections |
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G. BERNAOLA, M. MARTÍN-RUBIO and J.I. BACETA
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DOI: 10.1344/105.000000272
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Reconstruction of a latest Paleocene shallow-marine eutrophic paleoenvironment at Sidi Nasseur (Central Tunisia) based on foraminifera, ostracoda, calcareous nannofossils and stable isotopes (d13C, d18O) |
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P. STASSEN, C. DUPUIS, A.M. MORSI, E. STEURBAUT and R.P. SPEIJER
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DOI: 10.1344/105.000000273
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An anachronistic Clarkforkian mammal fauna from the Paleocene Fort Union Formation (Great Divide Basin, Wyoming, USA) |
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ROBERT L. ANEMONE and WENDY DIRKS
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DOI: 10.1344/105.000000274
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Early Paleogene climate at mid latitude in South America: Mineralogical and paleobotanical proxies from continental sequences in Golfo San Jorge basin (Patagonia, Argentina) |
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M. RAIGEMBORN, M. BREA, A. ZUCOL and S. MATHEOS
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DOI: 10.1344/105.000000269
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Palynology of Lower Palaeogene (Thanetian-Ypresian) coastal deposits from the Barmer Basin (Akli Formation, Western Rajasthan, India): Palaeoenvironmental and palaeoclimatic implications |
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S.K.M. TRIPATHI, M. KUMAR and D. SRIVASTAVA
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DOI: 10.1344/105.000000275
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Correlation of the Thanetian-Ilerdian turnover of larger foraminifera and the Paleocene-Eocene thermal maximum: confirming evidence from the Campo area (Pyrenees, Spain) |
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V. PUJALTE, B. SCHMITZ, J. I. BACETA, X. ORUE-ETXEBARRIA, G. BERNAOLA, J. DINARÈS-TURELL, A. PAYROS, E. APELLANIZ and F. CABALLERO
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DOI: 10.1344/105.000000276
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Redefinition of the Ilerdian Stage (early Eocene) |
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V. PUJALTE, J.I. BACETA, B. SCHMITZ, X. ORUE-ETXEBARRIA, A. PAYROS, G. BERNAOLA, E. APELLANIZ, F. CABALLERO, A. ROBADOR, J. SERRA-KIEL and J. TOSQUELLA
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DOI: 10.1344/105.000000268
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Recalibration of the Tethyan shallow-benthic zonation across the Paleocene-Eocene boundary: the Egyptian record |
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CHRISTIAN SCHEIBNER and ROBERT P. SPEIJER
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DOI: 10.1344/105.000000267
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From shelf to abyss: Record of the Paleocene/Eocene-boundary in the Eastern Alps (Austria) |
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H. EGGER, C. HEILMANN-CLAUSEN and B. SCHMITZ
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DOI: 10.1344/105.000000266
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Rock magnetic properties across the Paleocene-Eocene Thermal Maximum in Marlborough, New Zealand |
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V. VILLASANTE-MARCOS, C.J. HOLLIS, G.R. DICKENS and M.J. NICOLO
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DOI: 10.1344/105.000000280
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The role of new Iberian finds in understanding European Eocene mammalian paleobiogeography |
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A. BADIOLA, L. CHECA, M.A. CUESTA, R. QUER, J.J. HOOKER and H. ASTIBIA
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DOI: 10.1344/105.000000281
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Biostratigraphy of larger foraminifera in the Eocene (upper Ypresianlower Bartonian) sequences of the Southern Slope of the Western Caucasus (Russia, NE Black Sea). Correlation with regional and standard planktonic foraminiferal zones |
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E. ZAKREVSKAYA S. STUPIN and E. BUGROVA
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DOI: 10.1344/105.000000277
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Integrated calcareous nannofossil biostratigraphy and magnetostratigraphy from the uppermost marine Eocene deposits of the southeastern Pyrenean foreland basin: evidences for marine Priabonian deposition) |
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ANTONIO CASCELLA and JAUME DINARÈS-TURELL
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DOI: 10.1344/105.000000282
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Paleogene floral assemblages around epicontinental seas and straits in Northern Central Eurasia: proxies for climatic and paleogeographic evolution |
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MIKHAIL A. AKHMETIEV and VLADIMIR N. BENIAMOVSKI
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DOI: 10.1344/105.000000278
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