Resumé
A large, well-preserved vertebrate coprolite found in the clay pit
Sofienlund Lergrav, Jylland, is identified as crocodilian due to its
size and morphology. The coprolite consists of several concentric layers
wrapped around a more homogeneous core. Weak constriction marks are
present on the surface. Dinoflagellate cyst contents of the coprolite
indicate a mid-Lutetian to earliest Rupelian (middle Eocene to earliest
Oligocene) age, which at Sofienlund Lergrav places it within the lower
Oligocene Viborg Formation. The coprolite can thus be dated as
approximately 33–34 Ma old. The Viborg Formation in Denmark represents a
period with deposition of hemipelagic marine clay and formation of
glaucony.
The nearest shoreline was located c. 200 km north of the location of the present day Sofienlund Lergrav, and the climate was humid, warm-temperate to sub-tropical. The presence of a crocodilian coprolite is an important addition to the sparse Oligocene vertebrate fauna of Denmark, which previously only consisted of sharks and cetaceans.
The nearest shoreline was located c. 200 km north of the location of the present day Sofienlund Lergrav, and the climate was humid, warm-temperate to sub-tropical. The presence of a crocodilian coprolite is an important addition to the sparse Oligocene vertebrate fauna of Denmark, which previously only consisted of sharks and cetaceans.
Originalsprog | Engelsk |
---|---|
Sider (fra-til) | 181–187 |
Antal sider | 7 |
Tidsskrift | Bulletin of the Geological Society of Denmark |
Vol/bind | 66 |
DOI | |
Status | Udgivet - 2018 |
Programområde
- Programområde 3: Energiressourcer