Abstract
The recent find of an ethmosphenoid of Glyptopomus bystrowi (Gross 1941), a “glyptopomid” tetrapodomorph, in the Ketleri Formation (Upper Famennian, Upper Devonian) in western Latvia induced the description of historical material from this site and almost coeval localities in Central Russia (Orel-Saburovo Beds, Plavskian Regional Stage). Detailed morphological studies allowed recognition of new characters which support the taxonomic position of this species. Three-dimensional preservation of isolated elements enable the description of internal cranial structures, like the posterodorsolateral expansion of prenasal pits, the passage of some nerves and blood vessels, unknown in the previously described species of this genus. Despite minor differences, the vertebrate assemblages from these areas fit within the placoderm B. ciecere Zone (VII), which corresponds to the ?Upper postera–Lower expansa conodont Zone interval. These assemblages are virtually the same in their composition, except that durophagous placoderms and dipnoans are present in the Central Russian sites, in contrast to the Latvian ones. This could be explained by more significant marine influences.
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Acknowledgements
Our thanks go to Ģirts Stinkulis (University of Latvia) for valuable discussions and advice in interpretation of sedimentary environment, and Kārlis Linde (University of Latvia) for fast and perfect preparation work on the Ketleri fossils. The anonymous referee and Gaël Clément (Muséum National d’Histoire Naturelle, Paris) are thanked for scrupulous corrections and their valuable comments on an earlier version of this paper. We are grateful to all members of the Ketleri excavation team in 2014. Costs of the Ketleri excavations in 2014 were partly covered from the State base financing of scientific research for University of Latvia given to E.L. From the Russian side this work was supported by the programme of fundamental scientific research of the Presidium of the Russian Academy of Sciences No. 30 “Organic World and Planetary Processes Evolution,” project “Renovation of Palaeozoic and Mesozoic Vertebrate communities after Ecological Crises.” This is a contribution to the IGCP 596 project “Climate change and Biodiversity patterns in the Mid-Palaeozoic.”
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This article is a contribution to the special issue “Climate change and biodiversity patterns in the mid-Palaeozoic”
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Lebedev, O.A., Lukševičs, E. Glyptopomus bystrowi (Gross, 1941), an “osteolepidid” tetrapodomorph from the Upper Famennian (Upper Devonian) of Latvia and Central Russia. Palaeobio Palaeoenv 97, 615–632 (2017). https://doi.org/10.1007/s12549-016-0249-9
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DOI: https://doi.org/10.1007/s12549-016-0249-9