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5 mm (0.20 in) in diameter located slightly eccentrically towards one of the ends of the fossil. One of the aforementioned ends being more elongated, with the other end being more rounded in nature. The latter of the ends shows a short, protruding neck that becomes wider when reaching its termination. With the termination that ends the neck being rather unevenly lobate, with the terminations margins being sharp and even in appearance. The structures surface is generally smooth, except for the local grain-sized corrugations, the thin and short grooves and a longer, narrower groove that runs obliquely throughout three-quarters of the width that is closer to the wider end of the holotype's body.
403:
concentric rings around the terminations. These concentric rings are more continuous on one side than the opposite side, where on the latter only fragments of them are visible instead of the full ring. This structure also shows a multitude of small corrugations, although these corrugations do not form any pattern whatsoever. The edges of the structure are remarkably either elevated or depressed and more often than not show a double ridge which is 1.5β3 mm (0.059β0.118 in).
137:
336:. Often, a low or shallow circular protrusion/depression can be spotted in the convex or concave structure of the fossil. Smaller specimens of this species can be present without the protruding neck as well as the other multiple protrusions/depressions within the fossils. Specimens which are less than 25 mm (0.98 in) are thought of as being juveniles, with its
111:
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also shows six longitudinal, low grooves and ridges across its body that also manifest gentle slopes about 3β4 mm (0.12β0.16 in) wide that run parallel to the margin of its structure and turn accordingly when they reach the terminations in the fossil. And as a result of that, tend to form
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that shows winding margins across its body, alongside longitudinal furrows/ridges which tend to run parallel to the fossil's margin. The holotype of this form shows an elongated, cucumber-like structure that is 120 mm (4.7 in) long and 42 mm (1.7 in) wide which is visible as a
367:
is described as a convex oval-shaped form on the lower surface of a micaceous clayey, with very finely grained sandstone making up its slab. The holotype was measured as being 95 mm (3.7 in) long and up to 55 mm (2.2 in) wide, with there also being a round protrusion roughly
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379:
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283:. This fossil is also described from the Marwar Super Group of rocks of Sonia Sandstone at Jodhpur region in Sursagar area. The genus contains two species,
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340:
being selected from a number of adult individuals that have been completely developed and show signs of the best preservation of the organism.
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positive part (its convex) with its negative counterpart being visible in a horizontally split slab (its concave). The holotype for
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267:-like organism that was first described from a spot in Ukraine in 2021. In the same paper that described the genus
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Bobrovskiy, Ilya; Krasnova, Anna; Ivantsov, Andrey; Luzhnaya (Serezhnikova), Ekaterina; Brocks, Jochen J. (2019).
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specimens that also includes the paratype. Although these could simply just be rounded clay pebbles fossilised.
386:, showing the winding margins across its body. The fossil was found in the Mogilev formation within a quarry.
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to fossilised clay pebbles, that are also seen within the
Cambrian, that also showed up with the holotype of
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559:"Finkoella: a sack-like Ediacaran soft-bodied fossil from the Marwar Supergroup, western Rajasthan, India"
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577:
352:
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seems to be represented by oval- elliptical-shaped fossils, that rarely ever become the same shape as
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that was located inside a quarry near the DHPS. The slab showed in the image is a general view of
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The image above shows the upper surface of the finely grained sandstone slab from the
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415:, honours the amateur palaeontologist S.V. Finko who helped provide the holotype for
332:, which are thought to show a short, protruding neck-like structure and/or a shallow
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605:
515:"New Ediacaran fossils from the Ukraine, some with a putative tunicate relationship"
427:, refers to Ukraine, the country where both species are found. The specific epithet
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of this genus, with its name referring to where it was described from, Ukraine.
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meaning "elongate," refers to the elongated appearance of the second species,
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Parihar*, V. S.; Ram, Hukma; Kumar, Pawan; Harsh, Anshul (10 July 2024).
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606:"Simple sediment rheology explains the Ediacara biota preservation"
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656:"Late Neoproterozoic sedimentation in the Timan foreland"
419:, as well as the sandstone slab that had the paratype of
275:, being a reticulate, possibly being a fragment of the
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Small, Tunicate-like animal of the
Ediacaran Period
8:
582:: CS1 maint: multiple names: authors list (
298:It is also worth noting the similarities of
260:is a genus of sack-like body fossils of an
513:Martyshyn, Andrej; Uchman, Alfred (2021).
423:fossilised onto it. The specific epithet,
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20:
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306:. These double siphon tunicate organism
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271:, another organism was described named
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393:represents itself as a more elongated
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126:, scale bar 2 cm (0.79 in)
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720:Enigmatic prehistoric animal genera
660:Geological Society, London, Memoirs
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672:10.1144/gsl.mem.2004.030.01.04
610:Nature Ecology & Evolution
1:
715:Fossil taxa described in 2021
310:shows organic layer in MSG.
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532:10.1007/s12542-021-00596-1
710:Prehistoric animal genera
622:10.1038/s41559-019-0820-7
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132:Scientific classification
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654:Grazhdankin, D. (2004).
453:List of Ediacaran genera
431:, feminine form of the
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224:Andrej Martyshyn, 2021
566:Current Science India
411:The generic epithet,
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586:) CS1 maint: year (
357:Finkoella ukrainica
300:Finkoella ukrainica
705:Fossils of Ukraine
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363:The holotype for
353:Mogilev formation
277:pharyngeal basket
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29:Temporal range:
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700:Ediacaran life
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616:(4): 582β589.
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525:(4): 623β639.
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273:Pharyngomorpha
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417:F. ukrainica
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382:A fossil of
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365:F. ukrainica
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320:F. ukrainica
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293:type species
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285:F. ukrainica
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239:F. ukrainica
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124:F. ukrainica
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572:(1): 50β55.
314:Description
175:Subphylum:
694:Categories
469:References
441:F. oblonga
421:F. oblonga
400:F. oblonga
391:F. oblonga
384:F. oblonga
373:F. oblonga
330:F. oblonga
289:F. oblonga
246:F. oblonga
189:Ascidiacea
680:129144374
666:: 37β46.
541:244957825
425:ukrainica
413:Finkoella
407:Etymology
395:Finkoella
308:Finkoella
281:Finkoella
269:Finkoella
262:Ediacaran
257:Finkoella
219:Finkoella
191: (?)
155:Kingdom:
149:Eukaryota
31:Ediacaran
25:Finkoella
638:85495899
630:30911145
463:Yarnemia
458:Burykhia
447:See also
437:oblongus
338:holotype
265:tunicate
230:Species
205:Ausiidae
198:Family:
179:Tunicata
169:Chordata
165:Phylum:
159:Animalia
145:Domain:
120:holotype
429:oblonga
351:of the
211:Genus:
185:Class:
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676:S2CID
634:S2CID
562:(PDF)
537:S2CID
435:word
433:Latin
334:sinus
279:of a
626:PMID
588:link
584:link
519:PalZ
287:and
118:The
44:Preκ
668:doi
618:doi
570:127
527:doi
122:of
696::
674:.
664:30
662:.
658:.
646:^
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608:.
596:^
580:}}
576:{{
568:.
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549:^
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523:95
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477:^
443:.
94:Pg
38:Ma
33:,
682:.
670::
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620::
614:3
590:)
543:.
529::
244:β
237:β
215:β
202:β
99:N
89:K
84:J
79:T
74:P
69:C
64:D
59:S
54:O
49:κ
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