2025
Early Permian Freshwater Silicified Stromatolites and Oolites from the Krkonoše Piedmont Basin (Bohemian Massif): Paleobiology, Environmental Setting and Early Diagenesis
VODRAZKOVA, Stanislava; Radek VODRAZKA; Tomáš KUMPAN; Juraj FRANCU; Markéta HOLÁ et. al.Základní údaje
Originální název
Early Permian Freshwater Silicified Stromatolites and Oolites from the Krkonoše Piedmont Basin (Bohemian Massif): Paleobiology, Environmental Setting and Early Diagenesis
Autoři
VODRAZKOVA, Stanislava; Radek VODRAZKA; Tomáš KUMPAN (203 Česká republika, domácí); Juraj FRANCU; Markéta HOLÁ (203 Česká republika, domácí) a Karel SLAVÍČEK (203 Česká republika, domácí)
Vydání
Bulletin of Geosciences, Czech Geological Survey, 2025, 1214-1119
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10505 Geology
Stát vydavatele
Česká republika
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 1.500 v roce 2024
Organizační jednotka
Přírodovědecká fakulta
UT WoS
001538882700004
EID Scopus
2-s2.0-105011740457
Klíčová slova anglicky
early Permian; Krkonoše Piedmont Basin; stromatolites; oolites; cyanobacteria; silicification
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 2. 9. 2025 15:52, Mgr. Marie Novosadová Šípková, DiS.
Anotace
V originále
Late Palaeozoic non-marine microbialites remain poorly documented despite their potential significance for understanding terrestrial ecosystems during this period of profound climatic and environmental change. Here we report exceptionally preserved lower Permian (Autunian regional stage ˜ Asselian-Sakmarian) silicified stromatolites and oolites from the Krkonoše Piedmont Basin (Bohemian Massif, Czech Republic). Despite their occurrence in Quaternary eluvial and colluvial deposits, multiple lines of evidence suggest formation in a shallow, ephemeral fluviolacustrine setting. The stromatolites display a vertical succession of different growth forms, including structures similar to modern sheath-forming cyanobacterial taxa that form fan-like and hemispheroidal colonies with characteristic upright growth, features especially common in modern streams and rivers. Early diagenetic silicification preserved not only delicate stromatolitic architectures but also microbial organic matter. The presence of volcaniclastic material within ooidal cortices and cores, as well as within the rock matrix, indicates contemporaneous volcanic input, which likely provided silica for early replacement of the primary carbonate fabric. This exceptional preservation, facilitated by rapid CaCO3 encrustations of microbial structures and subsequent early silicification, provides rare insights into early Permian terrestrial ecosystems.
Návaznosti
GC20-20785J, projekt VaV |
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