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Ichnogenus ZoophycosMassalongo, 1855 Similar Chondrites, Thalassinoides, Planolites, Rhizocorallium, Cruziana | ||
Zoophycos cuilfail sous le hg navigation mesnil val
Zoophycos is a somewhat cosmopolitan ichnogenus thought to be produced by moving and feeding polychaete worms.
Contents
Appearance
Zoophycos occurs in two forms, one planar, and one which resembles a corkscrew. In the latter helicoidal form, successive turns having larger or smaller radii. A marginal tube surrounds the perimeter of the corkscrew, linked to the vertical shaft that connects the burrow to the surface. Spreiten occur between the marginal tube and the corkscrew axis. The burrows can exceed a metre in vertical and horizontal dimension.
Ethology
One hypothesis proposes that Zoophycos represents gardening behaviour, in a similar fashion to Palaeodictyon. On this view there should be a fractionation of carbon isotopes between the burrow infills and the matrix – but such differentiation was not observed in Quaternary instances from deep-water cores off the Portuguese coast.(Variation in morphology between different zoophycos 'species' means that thes emany not be representative of all zoophycos instances.) Instead, increased concentration of organic carbon within burrows suggests that the burrows may be used to cache food resources. An alternative is that it is simply a deposit feeding trace.
Occurrence
The ichnogenus gives its name to an ichnofacies associated with the shelf break. Nevertheless, it is now appreciated that it has a somewhat more cosmopolitan occurrence that has changed through time. It is typically associated with deep marine muds and sands, often between turbidite beds. It is known from both the fossil record and deep sea sediment cores. However, it can also occur in shallow-marine storm deposits.
It occurs from the early Ordovician until the present. It is restricted to deep waters in the Silurian, but occurs in nearshore settings from the Devonian until the end of the Permian.
