Where: Lithuania (55.9° N, 21.1° E: paleocoordinates 55.0° N, 16.1° E)
• coordinate based on nearby landmark
• outcrop-level geographic resolution
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
Preservation: soft parts, original chitin, amber
Collection methods: University of Warszawa (IGAW) collection
Primary reference: A. W. Skalski. 1973. Studies on the Lepidoptera from fossil resins. Part II. Epiborkausenites obscurotrimaculatus gen. et sp. nov. (Oecophoridae) and a tineid-moth discovered in the Baltic amber. Acta Palaeontologica Polonica 18:153-160 [M. Clapham/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 122983: authorized by Matthew Clapham, entered by Matthew Clapham on 08.01.2012
Creative Commons license: CC BY (attribution)
Taxonomic list
Insecta | |
Epiborkhausenites obscurotrimaculatus n. gen. n. sp.
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