4.3 Article

A glimpse into ancient food storage: Sequestrichnia and associated nucleocave Chondrites from Eocene deep-sea deposits

Journal

ACTA PALAEONTOLOGICA POLONICA
Volume 67, Issue 3, Pages 767-779

Publisher

INST PALEOBIOLOGII PAN
DOI: 10.4202/app.00965.2021

Keywords

Zoophycos; trace fossils; deep-marine; flysch; Bile Karpaty Unit; Outer Western Carpathians; Czech Republic

Categories

Funding

  1. Institute of Geology of the Czech Academy of Sciences [RVO 679 858 31]
  2. Czech Science Foundation [18-05935S]
  3. [MUNI/A/1394/2021]

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The old brickyard Velka nad Velickou in the Czech Republic provides a unique insight into a Eocene deep-sea ichno-assemblage dominated by sequestrichnia. The tracemaker Chondrites intricatus is seen frequently penetrating the Zoophycos brianteus trace fossil and occurring preferentially on the surface of Zoophycos spreiten, indicating the secondary use of food-stowing. This close relationship between Chondrites and Zoophycos supports the hypothesis of sequestrichnial behavior of Zoophycos producer. Other fossils such as Helminthopsis tenuis, Tubulichnium mediterranensis, Scolicia strozzii, ?Dactyloidites isp., Megagrapton irregulare, and Planolites isp. are also found in this studied locality.
The old brickyard Velka nad Velickou in the Czech Republic offers a unique insight into an Eocene deep-sea ichno-assemblage that is dominated by sequestrichnia. Secondary use of such food-stowing was made by the tracemaker of Chondrites intricatus as evidenced by its frequent penetration of the trace fossil Zoophycos brianteus and its occurrence preferentially on the surface of Zoophycos spreiten. Here, the Chondrites tracemaker presumably exploited the nutrient-enriched micro-environment (nucleocave). This close interrelations between Chondrites and Zoophycos support the hypothesis of a sequestrichnial behaviour of the Zoophycos producer. The studied locality also yields Helminthopsis tenuis, Tubulichnium mediterranensis, Scolicia strozzii, ?Dactyloidites isp., Megagrapton irregulare, and Planolites isp.

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