Edge Rewrite
// HTMLRewriter · presentation

This page was redesigned at the edge.

Cloudflare fetched the original article and streamed it through HTMLRewriter to apply an entirely new visual system without rebuilding the source page.

// request.cf · coarse context

A page that knows where it met you.

Only coarse request metadata is shown. This demo does not display or persist visitor IP addresses.

Country
US
Cloudflare location
CMH
Connection
HTTP/2
Language
Not provided

Ray ID: a2725370fe025645

Jump to content

// Workers AI · dad joke modeWhat did Studenicia say to its date? "You're a grade above

From Wikipedia, the free encyclopedia

Studenicia
Temporal range: Ediacaran
Scientific classification Edit this classification
Domain: incertae sedis
Genus: Studenicia
Gureev, 1983
Species:
S. galeiforma
Binomial name
Studenicia galeiforma
Gureev, 1983

Studenicia is a genus of Ediacaran fauna which is approximately 635-545 million years old. All Ediacaran fauna are considered to be invertebrate Metazoans or multicellular organisms with no backbone.

Description

[edit]

The fossils are made of small casts of the body. Studenicia is a small round organism (plan view) approximately 1-2 centimeters in diameter, and flat (side view). It is distinguished from other Ediacaran genera such as Nemiana by the presence of the central tubercle and Studenicia has a simpler structure (lacking rings) than Tirasiana.[1]

Diversity

[edit]

Gureev only documented one species of Studenicia which is known as Studenicia galeiforma.[1]

Discovery

[edit]
Location of the discovery in Ukraine of the genus Studenicia

Studenicia was discovered in the Studenitsa formation of the Dniester river, near Studenitsa village, Podolia, Ukraine. The fossil was discovered by Y. Gureev and first cataloged in 1983.[2][3]

Distribution

[edit]

Studenicia has only been found in the Studenitsa formation of the Dniester river, near Studenitsa village, Podolia, Ukraine.

Ecology

[edit]

Studenecia was a sedentary organism that lived on lower plane stratification.[1] The Studenitsa Formation outcrops are composed of grey sandstones, siltstones, and mudstones, with units of multi-grained sandstones. The outcrops have a total thickness of up to 60m in certain areas.[1]

See also

[edit]

References

[edit]
  1. 1 2 3 4 Ivantsov, A. (2015). Upper Vendian macrofossils of Eastern Europe Middle Dniester area and Volhynia. Gritsenko, V. P.; Paliy, V.M.; Velikanov, V.A.; Konstantinenko, L. I. Moscow: Russian Academy of Sciences. ISBN 9785903825325. OCLC 949268086.
  2. Gureev, Y. A. (1983). "Faunistic remains and fossil traces of invertebrates, their stratigraphic relation to the Upper Precambrian-Lower Cambrian section of the Middle Dneister area". Fossil Fauna and Flora of the Ukraine (in Russian). 43. Kyiv, Ukraine: Naukova Dumka: 34–39.
  3. Glaessner, Martin F. (1971). "Geographic Distribution and Time Range of the Ediacara Precambrian Fauna". Geological Society of America Bulletin. 82 (2): 509. Bibcode:1971GSAB...82..509G. doi:10.1130/0016-7606(1971)82[509:gdatro]2.0.co;2.
[edit]