Article ID Journal Published Year Pages File Type
4465602 Palaeogeography, Palaeoclimatology, Palaeoecology 2016 12 Pages PDF
Abstract

•Lower Devonian assemblage of vertebrate and invertebrate trace fossils is described.•Two trace-bearing horizons occur in the shallow-marine deposits.•Osculichnus tarnowskae is interpreted as a unique example of fish praedichnia.•Morphology of the trace suggests that they were made by a hunting lungfish.•The trace fossil provides the first evidence for Devonian lungfish feeding behaviour.

An exceptionally well-preserved assemblage of numerous invertebrate and vertebrate trace fossils is described from the Lower Devonian of the Holy Cross Mountains, southern Poland. Two trace-bearing horizons occur in the shallow-marine sequence that is exposed in a small outcrop near Ujazd village. One of the trace fossils is preserved as a bilobate, generally elliptical, epichnial pit is described as Osculichnus tarnowskae isp. nov. and interpreted as a unique example of praedichnia. Neoichnologic experiments and observations indicate that the ichnogenus Osculichnus was produced by feeding fish. The fish producing O. tarnowskae probably hunted bivalves, polychaetes and arthropods, which are represented by invertebrate trace fossils in the same horizons. The overall shape and morphological details of O. tarnowskae suggest that it was made by a lungfish broadly similar to Dipnorhynchus. The trace provides the first direct evidence for Devonian lungfish feeding behaviour, as well as the first record of three-dimensional soft-tissue morphology of the snout area of an Emsian representative of this group. The trace fossils from Ujazd provide new insight into the palaeoecology and taphonomy of the Lower Devonian of the Holy Cross Mountains.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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