Proarticulata

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Proarticulata
Temporal range: Late
Ma
Fossil of Dickinsonia costata
Fossil of Spriggina
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Stem group: Bilateria
Phylum: Proarticulata
Fedonkin, 1985
Class / Family

For more taxa, see text

Proarticulata is a proposed

Mikhail A. Fedonkin in 1985 for such animals as Dickinsonia, Vendia, Cephalonega, Praecambridium[3] and currently many other Proarticulata are described (see list).[4][5]

Due to their simplistic morphology, their affinities and mode of life are subject to debate. They are almost universally considered to be

Morphology

Examples of the classes Proarticulata, including reconstructions of Vendia sokolovi, Dickinsonia costata and Yorgia waggoneri.

Vendiamorpha

The body is completely segmented, with all isomers curved towards the posterior, and the first isomer is normally much larger than the rest. The first two isomers at the anterior dorsal end are partly fused. (e.g., Vendia, Paravendia and Karakhtia).[6][13][14][15]

Cephalozoa

These proarticulatans are incompletely segmented, as the anterior zone is free of isomers, often making a "hairband" like appearance (example cephalozoans include

Tamga, Spriggina, Marywadea and Cyanorus).[6][13][15][16] Some cephalozoans from the family Yorgiidae demonstrate pronounced asymmetry of the left and right parts of the body. For instance, Yorgia’s initial right isomer is the only one which spreads far towards the left side of the body. Archaeaspinus has an unpaired anterior lobe confined by the furrow to the left side only.[6][7][15]

Artist's reconstruction of Cephalonega stepanovi.[17]
Artist's reconstruction of Lossinia feeding on surface algae.

In Cephalonega stepanovi and Tamga hamulifera the zone containing the isomers is encircled by a peripheral, undivided zone.[16] The Cephalonega's isomers are connected to each other, forming a body resembling a rubber raft; the Tamga's isomers are separated from each other, and do not touch.

In Lossinia, the center undivided region has no visible isomers, instead having the lobe-like isomers emanate from the periphery of the undivided region as "transverse articulations."[16]

Dipleurozoa

The dipleurozoan body is subradial, divided by isomers entirely (e.g., Dickinsonia and Phyllozoon). Dickinsonia juveniles show undivided anterior areas but these regions were reduced in the course of ontogeny, and in the adult stages Dickinsonia-like proarticulates changed so radically that they became almost indistinguishable from isomers.[13][16][18]

List of Proarticulata

Andiva ivantsovi
Andiva ivantsovi
Dickinsonia costata
Dickinsonia costata
Spriggina floundersi
Spriggina floundersi
Ovatoscutum concentricum
Ovatoscutum concentricum
Yorgia waggoneri
Yorgia waggoneri
Tamga hamulifera
Tamga hamulifera

Body fossils

A. parva Fedonkin, 1980
A. ivantsovi Fedonkin, 2002
  • Archaeaspinus Ivantsov, 2007[6] (=Archaeaspis Ivantsov, 2001)[16]
A. fedonkini Ivantsov, 2001
C. stepanovi (Fedonkin, 1976)[16][22]
C. bilobatum Wade, 1971
C. singularis Ivantsov, 2004
D. costata Sprigg, 1947
D. menneri Keller 1976[16] (=Vendomia menneri Keller 1976[22])
D. tenuis Glaessner & Wade, 1966
I. rugulosa Ivantsov, 2007
K. nessovi Ivantsov, 2004
L. lissetskii Ivantsov, 2007
M. ovata Glaessner & Wade, 1966
O. concentricum Glaessner & Wade, 1966
P. janae Ivantsov, 2001 (=Vendia janae Ivantsov, 2001)
P. mirus Fedonkin, 1983 (Valdainia plumosa Fedonkin, 1983)
P. siggilum Glaessner & Wade, 1966
S. floundersi Glaessner, 1958
  • Tamga Ivantsov, 2007[16]
T. hamulifera Ivantsov, 2007
V. sokolovi Keller, 1969
V. rachiata Ivantsov, 2004
W. aitkeni Narbonne, 1994[24]
Y. waggoneri Ivantsov, 1999

Trace fossils

E. axiferus Ivantsov, 2002.
E. waggoneris Ivantsov, 2011. This is a trace of Yorgia waggoneri
E. costatus Ivantsov, 2011. This is a trace of Dickinsonia costata
P. hanseni Jenkins & Gehling, 1978

See also

References

  1. .
  2. .
  3. ^ Fedonkin MA (1985). "Systematic Description of Vendian Metazoa". In Sokolov BS, Iwanowski AB (eds.). Vendian System: Historical–Geological and Paleontological Foundation. Vol. 1: Paleontology. Moscow: Nauka. pp. 70–106.
  4. S2CID 55178329
    .
  5. ^ .
  6. ^ a b c d e f g Ivantsov, A.Yu. (2001). "Vendia and other precambrian "Arthropods"". Paleontological Journal. 35 (4): 335–343.
  7. ^ a b c Ivantsov, A.Yu. (1999). "A new Dickinsoniid from the upper Vendian of the White Sea Winter Coast (Russia, Arkhangelsk region)". Paleontological Journal. 33 (3): 233–241.
  8. PMID 29105292
    .
  9. .
  10. .
  11. .
  12. .
  13. ^ a b c d e f Ivantsov, A.Yu. (2004). "New Proarticulata from the Vendian of the Arkhangel'sk Region" (PDF). Paleontological Journal. 38 (3): 247–253. Archived from the original (PDF) on 2007-09-27.
  14. ^ Ivantsov, A.Yu.; Malakhovskaya, Y.E.; Serezhnikova, E.A. (2004). "Some problematic fossils from the Vendian of the south-eastern White Sea region" (PDF). Paleontological Journal. 38 (1): 1–9. Archived from the original (PDF) on 2007-07-04.
  15. ^ a b c Ivantsov, A.Yu. (2004). Vendian animals in the phylum Proarticulata (PDF). The Rise and Fall of the Vendian Biota. Prato, Italy. p. 52. IGSP Project 493.
  16. ^ a b c d e f g h i j Ivantsov, A.Yu. (April 2007). "Small Vendian transversely articulated fossils". Paleontological Journal. 41 (2): 113–122.
    S2CID 86636748
    .
  17. ^ illustration (c) Stanton F. Fink
  18. ^ a b Ivantsov, A.Yu.; Malakhovskaya, Y.E. (2002). "Giant traces of Vendian animals" (PDF). Doklady Earth Sciences. 385 (6): 618–622. Archived from the original (PDF) on 2007-07-04.
  19. S2CID 86523806
    .
  20. .
  21. .
  22. ^ a b Keller BM, Fedonkin MA (1976). "New Records of Fossils in the Valdaian Group of the Precambrian on the Syuz'ma River" (PDF). Izvestiya Akademii Nauk SSR. Seriya Geologicheskaya (in Russian). 3: 38–44. Archived from the original (PDF) on 2007-09-27.
  23. ^ Dzik, J.; Martyshyn, A. (2015). "Taphonomy of the Ediacaran Podolimirus and associated dipleurozoans from the Vendian of Ukraine". Precambrian Research. 269: 139–146. .
  24. .
  25. .

External links