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 Terrigenious 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).
• bed-level stratigraphic resolution
Environment/lithology: marine; conglomeratic sandstone and conglomeratic mudstone
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 25969: authorized by Cindy Looy, entered by Cindy Looy on 30.09.2002
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Sporites | |
Sporites indet. PotoniƩ 1893 | |
Klausipollenites | |
| |
| |
Triadispora | |
| |
Lunatisporites | |
Lunatisporites sp. Leschik | |
Falcisporites | |
| |
Cycadopites | |
Cycadopites sp. Wodehouse 1933 | |
Limitisporites | |
Limitisporites sp. Leschik 1956 |