Yorgia

Short description: Extinct proarticulate of Russia

Yorgia waggoneri

Temporal range: Ediacaran

Fossil of Yorgia waggoneri
Scientific classification
Domain:  | Eukaryota
Kingdom:  | Animalia
Phylum:  | †Proarticulata
Class:  | †Cephalozoa
Family:  | †Yorgiidae
Genus:  | †Yorgia
Ivantsov, 1999
Species:  |

†Y. waggoneri

Binomial name
†Yorgia waggoneri

Ivantsov, 1999[1]

Yorgia waggoneri is a discoid Ediacaran organism. It has a low, segmented body consisting of a short wide "head", no appendages, and a long body region, reaching a maximum length of 25 cm (9.8 in). It is classified within the extinct animal phylum Proarticulata.[2]

## Contents

* 1 Etymology
* 2 Morphology
* 3 Fossil record
* 3.1 Trace fossils
* 4 See also
* 5 References

## Etymology

The generic name Yorgia comes from the Yorga river on the Zimnii Bereg (Winter Coast) of the White Sea, where the first specimens were found. The specific name Yorgia waggoneri honors the American paleontologist Ben Waggoner, who found the first specimen.

## Morphology

Sketch reconstruction of the anatomy of Yorgia waggoneri and its ontogeny

The body plan of the Yorgia and other proarticulates is unusual for solitary (non-colonial) metazoans. These bilateral organisms have segmented metameric bodies, but left and right transverse elements (isomers) are organized in an alternating pattern relatively to the axis of the body – they are not direct mirror images. This phenomenon is described as the symmetry of glide reflection, which is a characteristic also found in the similar Spriggina. Some proarticulates (Yorgia, Archaeaspinus) demonstrate obvious asymmetry of left and right parts of the body. Yorgia’s initial isomer (on the right side, nearest the head) is the only one that extends across the median dividing left and right sides.[2][3] This lack of true bilateral symmetry, along with other considerations, has led some scientists to suspect that the organism falls in a sister group to the eumetazoa (i.e. all animals except Parazoa).[4]

The integument of the dorsal side were unsegmented and covered with small tubercles, same as with Cephalonega, Lossinia, Archaeaspinus and some Dickinsonia.[5] [6]

## Fossil record

Imprints of the species Yorgia waggoneri have been found in the rocks of Vendian period (Ediacaran) White sea region of Russia ,[7] dated around 555.5 Ma, and Yorgia sp. has been found in the Central Urals of Russia [8] and Flinders Ranges, Australia .[9] Most body imprints of Yorgia have in the past been primarily preserved on the sole of sandstone beds in negative relief. Other Yorgia fossils show internal structure in the original organism, showing two symmetrical rows of nodules, a central tube, rib-like tubes, and a semicircular shape with a hole in the circle centre positioned towards the head end. This structure has been interpreted as the impression of gonads, intestine and mouth.[10]

### Trace fossils

Epibaion waggoneris, chain of trace platforms and the imprint of the body of Yorgia waggoneri (right), which created these traces.

Some fossils appear as chains of positive imprints (the ichnospecies Epibaion waggoneris), terminated by the negative imprint of the animal. Such positive imprints are confined to the "elephant skin" surface texture that is interpreted as the remains of a microbial film. They have been interpreted as the feeding tracks produced as Yorgia fed on the surface of the microbial mat that lined the sea floor. Grazing of that bacterial film could have been accomplished by the work of numerous hair-like organs, cilia, located on the ventral side of the body, which caught and transported particles of the food substrate into the special elongated pockets arranged on the borders between the isomers.[11] Chevron-like marks on the positive imprints have been taken as evidence of this cilia activity.[3][12] This feeding habit is unknown in post-Ediacaran deposits.[13]

Taphonomic details revealed in Yorgia allow interpretation of the chains of positive imprints of other proarticulates as grazing traces, as opposed to trails created as organisms were swept along the sea floor by currents. In addition to Yorgia, two fossil taxa, Epibaion and Phyllozoon, seem to have produced similar grazing traces. Small groups of positive body imprints are documented for Dickinsonia costata as well and Dickinsonia cf. tenuis.[12][14]

## See also

* List of Ediacaran genera

## References

1. ↑ Ivantsov, A.Y. (1999). "A New Dickinsonid from the Upper Vendian of the White Sea Winter Coast (Russia, Arkhangelsk Region)". Paleontological Journal 33 (3): 233–241. https://www.academia.edu/2604893.
2. ↑ 2.0 2.1 Ivantsov, A.Y. (2001). "Vendia and Other Precambrian "Arthropods"". Paleontological Journal 35 (4): 335–343. https://www.academia.edu/2605872.
3. ↑ 3.0 3.1 Ivantsov, A.Y. (2004) "Vendian Animals in the Phylum Proarticulata". The Rise and Fall of the Vendian Biota. IGSP Project 493. Abstracts. Prato, Italy, p. 52.
4. ↑ Buss, L.W.; Seilacher, A. (1994). "The Phylum Vendobionta: A Sister Group of the Eumetazoa?". Paleobiology 20 (1): 1–4. doi:10.1017/S0094837300011088. ISSN 0094-8373.
5. ↑ Ivantsov, A. Yu.; Zakrevskaya, M. A.; Nagovitsyn, A. L. (2018). "Morphology of the covers of Proarticulata (Ediacaran Metazoa)". Ist Palaeontological Virtual Congress. Book of Abstracts.: 65. https://www.uv.es/everlab/PUBLICACIONES/1stSVP BOOK OF ABTRACTS.pdf.
6. ↑ Ivantsov, Yu. A.; Zakrevskaya, M.A.; Nagovitsyn, A.L. (2019). "Morphology of integuments of the Precambrian animals, Proarticulata". Invertebrate Zoology 16 (1): 19–26. doi:10.15298/invertzool.16.1.03. https://www.researchgate.net/publication/332098715.
7. ↑ Dzik, Jerzy; Ivantsov, Andrey Yu. (January 1999). "An asymmetric segmented organism from the Vendian of Russia and the status of the dipleurozoa". Historical Biology 13 (4): 255–268. doi:10.1080/08912969909386585. https://www.researchgate.net/publication/232955027. Retrieved 29 January 2023.
8. ↑ Grazhdankin, D. V.; Maslov, A. V., Mustill, T. M. R.; Krupenin, M. T. (2005). "The Ediacaran White Sea Biota in the Central Urals". Doklady Earth Sciences 401 (6): 784–788.
9. ↑ Droser, M.; Gehling, J.; Jensen, S. (2006). "Assemblage palaeoecology of the Ediacara biota: The unabridged edition?". Palaeogeography, Palaeoclimatology, Palaeoecology 232 (2–4): 131–147. doi:10.1016/j.palaeo.2005.12.015. Bibcode: 2006PPP...232..131D. http://earthscience.ucr.edu/docs/Droser_et_2006.pdf.
10. ↑ Dzik, Jerzy (2003). "Anatomical Information Content in the Ediacaran Fossils and Their Possible Zoological Affinities". Integrative and Comparative Biology 43 (1): 114–126. doi:10.1093/icb/43.1.114. PMID 21680416. http://icb.oxfordjournals.org/cgi/reprint/43/1/114.pdf.
11. ↑ Fedonkin, Mikhail A. (31 March 2003). "The origin of the Metazoa in the light of the Proterozoic fossil record". Paleontological Research 7 (1): 9–41. doi:10.2517/prpsj.7.9.
12. ↑ 12.0 12.1 Ivantsov, A.Y.; Malakhovskaya, Y.E. (2002). "Giant Traces of Vendian Animals". Doklady Earth Sciences 385 (6): 618–622. http://vend.paleo.ru/pub/Ivantsov_et_Malakhovskaya_2002-e.pdf.
13. ↑ Ivantsov, A. Yu. (2011). "Feeding traces of proarticulata—the Vendian metazoa". Paleontological Journal 45 (3): 237–248. doi:10.1134/S0031030111030063. ISSN 0031-0301.
14. ↑ Retallack, G.J. (2007). "Growth, decay and burial compaction of Dickinsonia, an iconic Ediacaran fossil". Alcheringa: An Australasian Journal of Palaeontology 31 (3): 215–240. doi:10.1080/03115510701484705. http://www.informaworld.com/index/781217204.pdf.

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