Cornulitids from the Upper Ordovician of northwestern Russia
2017; Society for Sedimentary Geology; Volume: 17; Issue: 12 Linguagem: Inglês
10.4267/2042/64289
ISSN2108-5196
Autores Tópico(s)Geological Formations and Processes Exploration
ResumoFour cornulitid species occur in the Rakvere Regional Stage in NW Russia. The new species Conchicolites rossicus is here described; it is the earliest known Conchicolites from the Ordovician of Baltica. The new species has very small tubes with sharp, strong and regular annulations. The diversity of cornulitids in the Rakvere Regional Stage at the Pechurki quarry is usual for the Upper Ordovician of Baltica. The cornulitids of Pechurki quarry encrusted hard organic substrates in a mud bottom (clay and carbonate clay) environment. Cornulites sterlingensis occurs both in the Upper Ordovician of North America and Baltica, which suggest a short distance between these two paleocontinents and/or similar environmental conditions.
Referência(s)