Patrycja G. Dworczak’s scientific contributions

What is this page?


This page lists works of an author who doesn't have a ResearchGate profile or hasn't added the works to their profile yet. It is automatically generated from public (personal) data to further our legitimate goal of comprehensive and accurate scientific recordkeeping. If you are this author and want this page removed, please let us know.

Publications (1)


Bioerosion traces and borings in the Upper Devonian vertebrate remains from the Holy Cross Mountains, Poland Bioerosion in fish remains
  • Preprint
  • File available

July 2021

·

138 Reads

·

1 Citation

Piotr Szrek

·

Patrycja G. Dworczak

·

Among the hundreds of collected Devonian vertebrate macrofossils in the Holy Cross Mountains, placoderms dominate and provide data on their morphology, distribution and taphonomy. So far 17 out of more than 500 studied specimens have revealed bones with surfaces covered by sediment-filled trace fossils. The traces have been made on the vertebrate remains before their final burial. The borings, oval in cross-section, include dendroidal networks of shallow tunnels or short, straight or curved individual scratches and grooves, which frequently create groups on the both sides of the bones. ? Karethraichnus isp. from Kowala and ? Osteocallis isp. from Wietrznia are the oldest record of these ichnogenera. Sedimentological clues indicate a shallow water environment, probably from the slope below the storm wave base.

Download

Citations (1)


... Bioerosion marks serve as frequently encountered indicators of the dynamic interactions between organisms and their environment (Bromley 2004;Augustin et al. 2019). In the vertebrate fossil record, these structures are commonly inferred to signify instances of predation, scavenging, and are inferred to contribute to post-mortem degradation processes (Belaústegui et al. 2012;Higgs et al. 2014;Fernández-Jalvo and Andrews 2016;Ozeki et al. 2020;Szrek et al. 2021;Jamison-Todd et al. 2023). However, in the case of animals with dermal bone, such as turtles, their shells offer a distinctive substrate that is available for the development of bioerosional structure throughout the organism lifespan, unlike other vertebrate bone structures (e.g., Frick et al. 1998;Mader 2006;Pfaller et al. 2008;Zakhama-Sraieb et al. 2010). ...

Reference:

Bioerosional marks in the shells of two sea turtle taxa from the middle Eocene of Belgium
Bioerosion traces and borings in the Upper Devonian vertebrate remains from the Holy Cross Mountains, Poland Bioerosion in fish remains