Abstract
The time interval between the Emsian (Early Devonian) and the end of the Permian is characterized by the rapid evolution of the Ammonoidea, and this evolution is reflected by the establishment of a detailed biostratigraphical scheme. Ammonoids are, together with the conodonts, the most important stratigraphical tools for this interval. The present time resolution in terms of ammonoid biostratigraphy is highest in the Devonian (one zone has a mean of 0.9 Ma) and in the Carboniferous (about 1 Ma), while the subdivision of the Permian is much coarser (about 2.5 Ma per ammonoid zone on average).
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Acknowledgments
We are indebted to Sonny A. Walton and Dieter Weyer (Berlin) for reading earlier versions of the manuscript. We thank Royal H. Mapes (Athens, Ohio) and M. Rakociński (Katowice) for reviewing the manuscript.
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Korn, D., Klug, C. (2015). Paleozoic Ammonoid Biostratigraphy. In: Klug, C., Korn, D., De Baets, K., Kruta, I., Mapes, R. (eds) Ammonoid Paleobiology: From macroevolution to paleogeography. Topics in Geobiology, vol 44. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-9633-0_12
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