Zoophycos

Zoophycos
Trace fossil classification
Ichnogenus: Zoophycos
Massalongo, 1855
Zoophycos from turbidites of Farmers Member of Borden Formation at mile marker 135, I-64, Kentucky.

Zoophycos is a somewhat cosmopolitan ichnogenus thought to be produced by moving and feeding polychaete worms.[1]

Appearance

Zoophycos occurs in two forms, one planar, and one which resembles a corkscrew.[2] 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.[3]

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.[3](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.[3] An alternative is that it is simply a deposit feeding trace.[4]

Occurrence

The ichnogenus gives its name to an ichnofacies associated with the shelf break.[5] Nevertheless, it is now appreciated that it has a somewhat more cosmopolitan occurrence that has changed through time.[5] 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.[6] However, it can also occur in shallow-marine storm deposits.[7]

It occurs from the early Ordovician until the present.[2] It is restricted to deep waters in the Silurian, but occurs in nearshore settings from the Devonian until the end of the Permian.[2]

See also

References

  1. ↑ Zhang, Li-Jun; Zhao, Zhao (2015). "Complex behavioural patterns and ethological analysis of the trace fossil Zoophycos: Evidence from the Lower Devonian of South China". Lethaia. 49 (2): n/a. doi:10.1111/let.12146.
  2. 1 2 3 Donovan (ed.). "Bottjer & Droser, THe history of Phanerozoic bioturbation". the palaeobiology of trace fossils.
  3. 1 2 3 "A test of the gardening hypothesis for the trace fossil Zoophyco". doi:10.2110/pec.07.88.0079 (inactive 2016-10-28).
  4. ↑ McIlroy, Duncan; Logan, Graham A. (1999). "The Impact of Bioturbation on Infaunal Ecology and Evolution during the Proterozoic-Cambrian Transition". PALAIOS. 14: 58. doi:10.2307/3515361. JSTOR 3515361.
  5. 1 2 MacEachern JA, Bann KL, Pemberton SG, Gingras MK. 2009. The Ichnofacies Paradigm: High-Resolution Paleoenvironmental Interpretation of the Rock Record. In: MacEachern JA,, In: Bann KL,, In: Gingras MK,, In: Pemberton SG, eds. Applied Ichnology: SEPM Short Course Notes.27–64.
  6. ↑ Seilacher, A. (1967). "Bathymetry of trace fossils". Marine Geology. 5 (5–6): 413–428. doi:10.1016/0025-3227(67)90051-5.
  7. ↑ Zhang, Li-Jun; Zhao, Zhao (2015). "Complex behavioural patterns and ethological analysis of the trace fossil Zoophycos: Evidence from the Lower Devonian of South China". Lethaia. 49 (2): n/a. doi:10.1111/let.12146.

Further reading

The Paleontology Portal. "Trace Fossils from North America" (Web – photos). The Paleontology Portal. Retrieved 2008-08-19.  "Zoophycos : Massalongo, 1855". 

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