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Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12128/538
Title: Palynology and microfacies of Lower Devonian mixed carbonate-siliciclastic deposits in Podolia, Ukraine
Authors: Filipiak, Paweł
Zatoń, Michał
Szaniawski, Hubert
Wrona, Ryszard
Racki, Grzegorz
Keywords: Carbonate Microfacies; Cuticles; Eurypterids; Lower Devonian; Palynofacies; Podolia; Palynostratigraphy
Issue Date: 2012
Citation: Acta Palaeontologica Polonica" (2012, vol. 57, no. 4, p. 863-877
Abstract: Investigation of mixed carbonate-siliciclastic Lower Devonian deposits have been carried out in the Ivanye Zolote and Ustechko sections in Podolia, Ukraine. Based on palynomorph evidence, the age of the samples studied is late Lochkovian, not older than the NM Oppel Miospore Zone, specifically the Si Lineage Zone. The presence of acritarchs and chitinozoans points to dominantly marine depositional conditions. However, a regressive environmental change to-ward more brackish conditions is indicated by a decrease in the taxonomic diversity of acritarchs in the topmost samples, the simultaneous disappearance of chitinozoans, and an increase in leiosphaerid frequency. Furthermore, evolution of limestone microfacies demonstrates a progressive transition from a shrinking marine basin toward a brackish, storm-af-fected muddy lagoon, manifested by recurrent profusion of impoverished, mostly opportunistic and euryhaline shelly benthos (nuculanid bivalves, leperditicopids and other ostracods, terebratulid brachiopods), chaetetid demosponges and diverse ichthyofauna. The association of plant (mainly nematophytes and some tracheids) and animal (eurypterid, ?scor-pion, and possibly other arthropod) remains points to the presence of nearby Early Devonian wetland vegetation, provid-ing food and shelter for various semi-aquatic and other terrestrial arthropods. Copyright © 2012.
URI: http://hdl.handle.net/20.500.12128/538
DOI: 10.4202/app.2011.0184
ISSN: 0567-7920
1732-2421
Appears in Collections:Artykuły (WNP)

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