Where: Poland (51.0° N, 23.7° E)
• Paleocoordinates: 2.5° N, 34.6° W (Wright 2013)
• coordinate estimated from map
• outcrop-level geographic resolution
When: Pridoli (423.0 - 419.2 Ma)
• Upper part of the Siedlce series. Ludlovian through Siegenian
Environment/lithology: deep subtidal; siltstone
•marine fauna. The siltstones become upwards more and more sandy and comprise commonly layers of fine-grained quartz sandstones; they are often mottled and display commonly mud cracks. This is a typical Oldred fades; it is attributed to the Siegenian to Emsian. Thus, the marine sedimentation persisted in the investigated area continuously all through the Silurian and Lower Devonian. The earliest regression is marked in the Lower Siegenian deposits, while the
•terrestrial oldred-type sedimentation became prevalent in the Upper Siegenian.
Size classes: macrofossils, mesofossils, microfossils
Primary reference: R. Wrona. 1980. Upper SiIurian-Lower Devonian Chitinozoa from the subsurface of southeastern Poland. Palaeontologia Polonica 41:103-165 [W. Kiessling/M. Krause]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 145674: authorized by Wolfgang Kiessling, entered by Mihaela Krause on 08.06.2013
Creative Commons license: CC0 (CC0)
Taxonomic list
Cephalopoda | |
Cephalopoda indet. Cuvier 1797 | |
Bivalvia | |
Bivalvia indet. Linnaeus 1758 clam | |
Pterobranchia | |
Monograptus formosus graptolite
Pristiograptus cf. dubius graptolite | |
Linograptus posthumus graptolite | |
"Monograptus ultimus" = Neocolonograptus ultimus
"Monograptus ultimus" = Neocolonograptus ultimus Perner 1899 graptolite |