Where: Hungary (46.1° N, 18.1° E: paleocoordinates 7.9° S, 30.8° E)
• coordinate based on nearby landmark
• small collection-level geographic resolution
When: Permian (298.9 - 251.9 Ma)
• The sequence of the Kovagoszolos formation consists of a rhythmic alternation of coarser and finer grained beds, beginning with conglomerates. Its middle part consists of relatively finer grained sandstone beds. Higer up the profile grains become coarser again and the upper part ends with a pebbled sandstone. Lower Varied Sandstone member, middle Gray Sandstone member, and upper Red Sandstone member.
• group of beds-level stratigraphic resolution
Environment/lithology: fluvial; gray, green sandstone
Size class: microfossils
Preservation: original sporopollenin
Collection methods: core, chemical,
Primary reference: A. Barabas-Stuhl. 1981. Microflora of the Permian and Lower Triassic sediments of the Mecsek Mountains (south Hungary). Acta Geologica Academiae Scientarum Hungaricae 24(1):49-97 [C. Looy/C. Looy/C. Looy]more details
Purpose of describing collection: biostratigraphic analysis
PaleoDB collection 24462: authorized by Cindy Looy, entered by Cindy Looy on 08.08.2002
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Taeniasporites labdacus, Jugasporites schaubergeroides, Gardenasporites heisseli, Nuskoissporites dulhuntyi
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Converrucosisporites | |
Converrucosisporites sp. Potonié and Kremp 1954 | |
Striatites | |
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Endosporites | |
Endosporites sp. Wilson and Coe | |
Taeniaesporites | |
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Guttulapollenites | |
Guttulapollenites sp. Goubin | |
Strotersporites | |
Strotersporites sp. Wilson | |
Monosaccites | |
Monosaccites "I" Potonié and Kemp 1954
Monosaccites "II" Potonié and Kemp 1954 | |
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Klausipollenites | |
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Falcisporites | |
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Alisporites | |
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Sphenopsida | |
Calamospora sp. Schopf et al. | |
Lueckisporites | |
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