Where: Poland (50.8° N, 20.7° E: paleocoordinates 17.7° N, 28.9° E)
• coordinate based on nearby landmark
• small collection-level geographic resolution
When: Top Terrigenous Series Formation, Wuchiapingian to Wuchiapingian (259.9 - 252.2 Ma)
• The following lithological complexes are currently distinguished within the Zechstein on the so-called "near" Permian-Mesozoic edge of the Holy Cross Paleozoic core: Zechstein Limestone (Ca1) locally underlaying by the Copper-Bearing Shale (in German Kupfer schiefer; T1), Lower Anhydrite (Ald) in some sections, Terrigenious Series (T1r) and Upper Anhydrite (A1g) which all form the Werra Cycle (PZ1); the Strassfort Cycle (PZ2) is developed as the Terrigenous Series (T2r), the Grey Pelite (T3), Platy Dolomite (Ca3) and only locally Main Anhydrite (A3) represents the Leine Cycle (PZ3). The uppermost Zechstein deposits consist of the Top Terrigenous Series (Pzt).
• group of beds-level stratigraphic resolution
Environment/lithology: marine; conglomeratic mudstone and conglomeratic sandstone
•In log: sandstones and mustones with conglomerate intercalations
Size class: microfossils
Preservation: original sporopollenin
Collection methods: core, chemical, mechanical,
Primary reference: A. Fijalkowska. 1994. Palynological aspects of the Permo-Triassic succession in the Holy Cross Mountains, Poland. Documenta Naturae 87:1-76 [C. Looy/C. Looy/C. Looy]more details
Purpose of describing collection: biostratigraphic analysis
PaleoDB collection 24958: authorized by Cindy Looy, entered by Cindy Looy on 23.08.2002
Creative Commons license: CC BY (attribution)
Taxonomic list