The trace fossil Circulichnis as a record of feeding exploration: New data from deep-sea Oligocene–Miocene deposits of northern Italy
DOI | 10.1016/j.crpv.2018.05.002 |
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Aasta | 2019 |
Kirjastus | Elsevier BV |
Ajakiri | Comptes Rendus Palevol |
Köide | 18 |
Number | 1 |
Leheküljed | 1-12 |
Tüüp | artikkel ajakirjas |
Keel | inglise |
Id | 7984 |
Abstrakt
Circulichnis is a puzzling, ring-like trace fossil preserved on bedding planes. It is represented mostly by its type ichnospecies C. montanus, which is characterized by an evenly circular or elliptical course. A new ichnospecies, C. ligusticus, is distinguished based on material from deep-sea Oligocene–Miocene deposits of the Tertiary Piemonte Basin, NW Italy. It shows a winding or irregular course. A new model of Circulichnis is proposed as an exploration burrow produced mostly by the trace makers of Helminthoidichnites, Gordia, or Helminthopsis, as it moved to a different sediment layer to checking its feeding utility. This type of behaviour occurred already by the Ediacaran and is common in marine, mostly deep-sea bedded sediments. The trace makers belong mostly to polychaetes in marine sediments and to oligochaetes in continental sediments.