Courier Forschungsinstitut Senckenberg gy and Stratigraphy. Part II: Various Devonian Topics. E. Otto H. Walliser; Willi Ziegler.
Courier Forschungsinstitut Senckenberg gy and Stratigraphy. DeutschDE EnglishEN FrançaisFR. Contributions to Devonian Palaeontology and Stratigraphy. Part I: Chinese - German Collaboration. Courier Forschungsinstitut Senckenberg, Band 110). ISBN 978-3-510-61155-3, paperback, price: 3. 0 €. in stock and ready to ship.
ed. Contributions to Devonian Palaeontology and Stratigraphy: Part I, Chinese - German Collaboration, Part II: Various Devonian Topics: Courier Forschungsinstitut Senckenberg, v. 110, p. 195–230.
Ziegler, . and Bultynck, . 1989, New standard conodont zones and early Ancyrodella phylogeny across Middle-Upper Devonian boundary, in Walliser, . and Ziegler, . ed.
Courier Forschungsinstitut Senckenberg, 242, 141–156. Nandan typical stratigraphy and paleontology of the Devonian in South China (pp. 1–161). Baird, G. & Brett, C. (2008). Givetian Taghanic bioevents in New York State: new discoveries and questions. Basinwide stratigraphic synthesis and sequence stratigraphy, Upper Pragian, Emsian, and Eifelian stages (Lower to Middle Devonian), Appalachian Basin. In R. T. Becker, & W. Kirchgasser (Ed. Devonian events and correlations. Guyang: Guizhou People’s Publishing House + pls 1–48. Zambito, IV, J. Brett, C. & Baird, G. C. (2012a).
n in der Grube Messel bei Darmstadt - 3. Ergebnisse 1979-1981.
Botany and Molecular Evolution. Biodiversity Mapping. Sixteen contributions describe the geological and palaeontological evolution of Thuringia during the Tertiary and Quaternary – particularly the Neogene and Pleistocene development of the landscape, Palaeogene stratigraphy, the Tertiary between Leipzig and Altenburg, and the basalt deposits in the Thuringian Rhön mountains.
CFS Courier Forschungsinstitut Senckenberg. Stratigraphic ranges of these species confirm that the representatives of Protacrodontoidea and Stethacanthidae were resistant to changes in the biosphere close to the Frasnian - Famennian and Devonian - Carboniferous boundaries, contrary to most phoebodontid species. KW - Biostratigraphy.
Courier Forschungs-Institut Senckenberg 157, 1-183. SZULCZEWSKI, M. 1971. Upper Devonian conodonts, stratigraphy and facial development in the Holy Cross Mts. Belief and reality in biostratigraphic zonation. Acta Geologica Polonica 21(1), 1-130.
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