ASGP (2022), vol. 92: 323–379


Adam T. HALAMSKI (1*), Andrzej BALIŃSKI (1), Grzegorz RACKI (2), Michael R. W. AMLER (3), Martin BASSE (4), Julien DENAYER (5), Zofia DUBICKA (6), Paweł FILIPIAK (2), Marcelina KONDAS (2), Wojciech KRAWCZYŃSKI (2), Radosław MIESZKOWSKI (6), Katarzyna NARKIEWICZ (8), Ewa OLEMPSKA (1), Tomasz WRZOŁEK (2), Patrick N. WYSE JACKSON (7), Mikołaj K. ZAPALSKI (6), Michał ZATOŃ (2), Wojciech KOZŁOWSKI (6)

1) Institute of Paleobiology, Polish Academy of Sciences, ul. Twarda 51/55, 00-818 Warszawa, Poland; e-mail:
2) Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia in Katowice, Będzińska 60, 41-200 Sosnowiec, Poland
3) Universität zu Köln, Institut für Geologie und Mineralogie, Abt. Paläontologie und Historische Geologie, Zülpicher Str. 49a, 50674 Köln, Germany
4) Senckenberg Research Institute and Natural History Museum, Senckenberganlage 25, 60325 Frankfurt am Main, Germany
5) Evolution & Diversity Dynamics Lab, University of Liège, Allée du Six-Août, B18, Sart Tilman, Liège, Belgium
6) Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warszawa, Poland
7) Department of Geology, Trinity College, Dublin 2, Ireland
8) Polish Geological Institute – National Research Institute, Rakowiecka 4, 00-975 Warszawa, Poland
*) Corresponding author

Halamski, A. T., Baliński, A., Racki, G., Amler, M. R. W., Basse, M., Denayer, J., Dubicka, Z., Filipiak, P., Kondas, M., Krawczyński, W., Mieszkowski, R., Narkiewicz, K., Olempska, E., Wrzołek, T., Wyse Jackson, P. N., Zapalski, M. K., Zatoń, M. & Kozłowski, W., 2022. The pre-Taghanic (Givetian, Middle Devonian) ecosystems of Miłoszów (Holy Cross Mts, Poland). Annales Societatis Geologorum Poloniae, 92: 323–379.

Abstract: The middle and upper parts of the Skały Fm, Early to Middle Givetian in age, were investigated in four sections at Miłoszów Wood in the Łysogóry Region (northern region of the Holy Cross Mountains, central Poland). The dating is based on conodonts (Polygnathus timorensis Zone to the later part of the Polygnathus varcus/Polygnathus rhenanus Zone; early Polygnathus ansatus Zone cannot be excluded) and spores (Ex1–2 subzones) and, coupled with cartographic analysis and geophysical investigation, allows correlation within the strongly faulted succession. Significant lateral facies variations within the carbonate ramp depositional system in comparison with the better studied Grzegorzowice–Skały section, about 3 km distant, are documented, thanks to conodont-based correlation of both successions. Foraminifers, fungi, sponges, rugose and tabulate corals, medusozoans, microconchids and cornulitids, polychaetes (scolecodonts), molluscs (bivalves, rostroconchs, and gastropods), arthropods (trilobites and ostracods), bryozoans, hederelloids, ascodictyids, brachiopods, echinoderms (mostly crinoids, rare echinoids, holuthurians, and ophiocistoids), conodonts, fish, plants (prasinophytes, chlorophycophytes, and land plant spores), and acritarchs are present. Brachiopods are the most diverse phylum present (68 species), other richly represented groups are bryozoans and echinoderms; in contrast, cephalopods and trilobites are low in diversity and abundance. The muddy, middle to outer ramp biota (200 marine taxa, including 170 species of marine animals, 22 photoautotrophs, 6 forams) represents a mixture of allochthonous shallower-water communities (upper BA3), including storm- and possibly tsunami-affected coral mounds, and autochthonous deep-water soft-bottom brachiopod (e.g., Bifida–Echinocoelia) communities (BA 4–5). The richness and diversity of the Miłoszów biota is relatively high, comparable with other approximately coeval pre-Taghanic ecosystems during the Devonian climatic deterioration (cooling). Preliminary data indicate that in the Holy Cross Mountains, no large-scale replacement of brachiopod (and probably many other benthic ones, like crinoids) communities took place between the Early–Middle Givetian and the Early Frasnian, in contrast to the demise of the Hamilton/Upper Tully fauna in the Appalachian Basin. Such a similarity of pre- and post-Taghanic faunas does not exclude the occurrence of environmental perturbations and transient community turnovers, caused by immigrations during the Taghanic Biocrisis, but evidences the successful recovery of the indigenous biota.

Manuscript received 11 June 2022, accepted 16 December 2022