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Reassessment of historical sections from the Paleogene marine margin of the Congo Basin reveals an almost complete absence of Danian deposits

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Geoscience Frontiers 2019年第3期10卷 1039-1063页

作者： Floréal Solé Corentin Noiret Delphine Desmares Sylvain Adnet louis taverne Thierry De Putter Florias Mees Johan Yans Thomas Steeman Stephen Louwye Annelise Folie Nancy J.Stevens Gregg F.Gunnell Daniel Baudet Nicole Kitambala Yaya Thierry Smith Royal Belgian Institute of Natural Sciences (RBINS) Operational Directorate Earth and History of Life University of Namur (UNamur) Department of Geology Rue de Bruxelles 61 Sorbonne Université UPMC Paris 06 UMR 7207 (CR2P) UMR 5554-Institut des Sciences de l'Evolution Université Montpellier Place E.Bataillon Royal Museum for Central Africa (RMCA) Geodynamics and Mineral Resources Leuvensesteenweg 13 Ghent University (UGent) Department of Geology Royal Belgian Institute of Natural Sciences (RBINS) Heritage Scientific Survey Ohio University Department of Biomedical Sciences Heritage College of Osteopathic Medicine Duke University Lemur Center Division of Fossil Primates (DFP) Centre de Recherches Géologiques et Minières (CRGM) 44 av.de la Démocratie Kinshasa Gombe

The early Paleogene is critical for understanding global biodiversity patterns in modern ecosystems. During this interval, Southern Hemisphere continents were largely characterized by isolation and faunal endemism following the breakup of Gondwana. Africa has been proposed as an important source area for the origin of several marine vertebrate groups but its Paleogene record is poorly sampled, especially from sub-Saharan Africa. To document the early Paleogene marine ecosystems of Central Africa, we revised the stratigraphic context of sedimentary deposits from three fossil-rich vertebrate localities: the Landana section in the Cabinda exclave(Angola), and the Manzadi and Bololo localities in western Democratic Republic of *** provide more refined age constraints for these three localities based on invertebrate and vertebrate faunas, foraminiferal and dinoflagellate cyst assemblages, and carbon isotope records. We find an almost complete absence of Danian-aged rocks in the Landana section, contrary to prevailing interpretations over the last half a century(only the layer 1, at the base of the section, seems to be Danian). Refining the age of these Paleocene layers is crucial for analyzing fish evolution in a global framework, with implications for the early appearance of Scombridae(tunas and mackerels) and Tetraodontiformes(puffer fishes). The combination of vertebrate fossil records from Manzadi and Landana sections suggests important environmental changes around the K/Pg transition characterized by an important modification of the ichthyofauna. A small faunal shift may have occurred during the Selandian. More dramatic is the distinct decrease in overall richness that lasts from the Selandian to the Ypresian. The Lutetian of West Central Africa is characterized by the first appearance of numerous cartilaginous and bony fishes. Our analysis of the ichthyofauna moreover indicates two periods of faunal exchanges: one during the Paleocene, where Central Africa app

关键词： Central Africa Paleogene Stratigraphy Carbon isotope Planktonic foraminifera Vertebrates

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