Where: Kaliningrad, Russian Federation (54.9° N, 19.9° E: paleocoordinates 53.9° N, 15.2° E)
When: Priabonian (38.0 - 33.9 Ma)
• According to Aleksandrova and Zaporozhets (2008), the higher parts of the Prussian Formation (including the Blaue Erde or Blue Earth) belong to the Charlesdowniea clathrata angulosa dinocyst Zone. Based on its index species, this zone is concurrent to Zone W13 established in the Parisian basin (Châteauneuf and Gruas-Cavagnetto 1978), where it is correlated with nannoplankton zones NP18–NP21 (Powell, 1992) of the Priabonian. In the Paleogene zonation of northwestern Europe, the first occurrence of Thalassiphora fenestrata is designated at the base of the dinocyst Subzone D12b (36.20 +/- 0.1 Ma), which is correlated with zones NP18 (terminal part)–NP20 of the Priabonian (Luterbacher et al., 2004).
Environment/lithology: terrestrial; amber
Size classes: macrofossils, mesofossils, microfossils
Preservation: amber
Collection methods: Repository: Dresden Museum
Primary reference: G. L. Mayr. 1868. Die Ameisen des baltischen Bernsteins. Beiträge zur Naturkunde Preussens 1:1-102 [M. Clapham/M. Clapham/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 138659: authorized by Matthew Clapham, entered by Matthew Clapham on 24.01.2013
Creative Commons license: CC BY (attribution)
Taxonomic list
Myriapoda | |
Craspedosoma angulatum n. sp.
Craspedosoma angulatum n. sp. Koch and Berendt 1854 millipede | |
Insecta | |
"Hypoclinea geinitzi" = Yantaromyrmex geinitzi, "Hypoclinea goepperti" = Ctenobethylus goepperti
"Hypoclinea geinitzi" = Yantaromyrmex geinitzi Mayr 1868 ant
"Hypoclinea goepperti" = Ctenobethylus goepperti Mayr 1868 ant |