User:Yewtharaptor/sandbox: Difference between revisions
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* Bivalves |
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* Crustaceans |
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|style="background:#FEF6E4;" |''[[Ptychoplasma]]''<ref>{{Cite journal |last=Pieńkowski |first=G. |last2=Uchman |first2=A. |date=2009 |title=Ptychoplasma conica isp. nov.: a new bivalve locomotion trace fossil from the Lower Jurassic (Hettangian) alluvial sediments of Sołtyków, Holy Cross Mountains, Poland |url=https://ruj.uj.edu.pl/entities/publication/e7dbe0c3-20e3-4de3-b4dc-543fe5005ea0 |journal=Geological Quarterly |volume=53 |issue=4 |pages=397-406}}</ref> |
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* ''P. conica'' |
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* Soltyków |
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|style="background:#FEF6E4;" |Locomotion trace |
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* Repichnia |
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* Gastropods |
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Revision as of 21:18, 27 November 2024
 | This page is currently being created It is a new Wikipedia article developing through collaboration and successive edits.To help avoid edit conflicts and other confusion, the creator asks that for a short time this page not be edited unnecessarily, or nominated for deletion during this early stage of development.
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| Zagaje Formation | |
|---|---|
| Stratigraphic range: Lower Hettangian-Lower Sinemurian~[1] | |
_-_http-pl.wikipedia.org-wiki-Rezerwat_przyrody_Gagaty_So%5EC5%5E82tykowskie_-_panoramio_(1).jpg) Exposed Layers at Sołtyków | |
| Type | Geological formation |
| Unit of | Kamienna Group |
| Sub-units | Huta Mudstone Member |
| Underlies | |
| Overlies | Unnamed Rhaetian Beds |
| Area | Polish epicontinental basin except of the Mazury region and Czêstochowa region. Reaches also into north Germany |
| Thickness | 157.5 m |
| Lithology | |
| Primary | Sandstone |
| Other | Mudstone |
| Location | |
| Coordinates | 51°06′N 20°30′E / 51.1°N 20.5°E |
| Approximate paleocoordinates | 43°06′N 18°48′E / 43.1°N 18.8°E |
| Region | Swietokrzyskie |
| Country | |
| Type section | |
| Named for | The Town of Zagaje near Gromadzice |
| Named by | Karaszewski (as an informal unit)[3] |
  Yewtharaptor/sandbox (Poland) | |
The Zagaje Formation is an Early Jurassic Epoch (Hettangian-Sinemurian) geologic formation located mostly in Poland with layers also exposed in north Germany. This unit is known for its diverse Ichnofossil assemblages, with traces of invertebrates along vertebrate footprints. Indeterminate fossil ornithischian tracks, of the Hettangian Stage, have been reported from the formation.[4] The Zagaje Formation correlates with The lower part of the Höganäs Formation in Scania, as well the Munkerup Member and the Gassum Formation in Denmark.[1]
Biota
Ichnofossils
Several unname Ichnofossils are recovered at Soltyków, including conical domichnia (Conichnus?), bivalve straight to winding linear trails, smooth vertical and subvertical branching tunnels, knob-walled tunnels, mace-shaped or irregular ellipsoid chambers, etc.[5][6]
| Genus | Species | Location | Material | Type | Made By | Images |
|---|---|---|---|---|---|---|
| Calceoformites[5][6] |
|
|
Clog-shaped protrusions |
|
|
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| Cruziana[5][6] |
|
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Dwelling structures |
|
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| Cochlichnus[1][5] |
|
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Traces |
|
|
 |
| Conichnus[1][5][6] |
|
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Subcylindrical burrows |
|
|
|
| Diplichnites[5][6] |
|
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Hypichnial trackway |
|
|
|
| Diplocraterion[1][5] |
|
|
U-Shaped Burrows |
|
|
 |
| Imbrichnus[1][5] |
|
|
Burrows |
|
|
|
| Isopodichnus[1][5] |
|
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Hypichnial marks |
|
|
 |
| Kouphichnium[5][6] |
|
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V-shaped hypichnial marks |
|
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|
| Lockeia[1][5] |
|
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Dwelling traces |
|
|
 |
| Palaeophycus[6] |
|
|
Straight or slightly curved burrows |
|
|
|
| Planolites[6] |
|
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Tubular unbranched, usually horizontal burrows |
|
|
|
| Ptychoplasma[7] |
|
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Locomotion trace |
|
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| Rusophycus[6] |
|
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Resting Traces |
|
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| Scalichnus[1][5][6] |
|
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Sac/Bottle shaped burrows |
|
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| Scolicia[1][5] |
|
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Traces |
|
|
 |
| Scoyenia[5][6] |
|
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Linear slender burrows |
|
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| Skolithos[1][5][6] |
|
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Sac/Bottle shaped burrows |
|
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| Spongeliomorpha[1][5][6] |
|
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Sac/Bottle shaped burrows |
|
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Insects
Radial chambers around large tunnels have been recovered, they may be arthropod burrows or traces of roots.[5][6] Large nest structures with septa, similar to nesting behaviour of insects like Cicadas are know.[6]
| Genus | Species | Location | Material | Notes | Images |
|---|---|---|---|---|---|
| Artematopodites[8] | A. ssp. |
|
MPK 5/36, 39, 40 | A Coleopteran, member of the family Permosynidae | |
| Blattodea[8] | Indeterminate |
|
MPK 5/54 | Indeterminate Blattodean remains | |
| Blattulidae[8] | Indeterminate |
|
MPK 5/1 | Indeterminate Cockroach remains | |
| Caraboidea[8] | Indeterminate |
|
MPK 5/12, 15 | Indeterminate Beetle remains | |
| Coleoptera[8] | Indeterminate |
|
Isolated Wings | Indeterminate Beetle remains | |
| Helminthoidichnites[6] | cf. H. isp. |
|
Gnawing traces | surficial gnawing traces made by insects | |
| Hydrobiites[8] | H. sp. |
|
MPK 5/10, 13, 17, 22, 25, 33 | A Coleopteran, member of the family Permosynidae | |
| Linckichnus[6] | L. terebrans |
|
Boring Traces | Detritivorous habitation dwellings or oviposition structures of insects in dead wood | |
| Memptus[8] | M. sp. |
|
MPK 5/44 | A Coleopteran, Incertade sedis | |
| Notocupes[8] | N. sp. |
|
MPK 5/6 | A Coleopteran, Incertade sedis | |
| Odrowazicoris[9] | O. polonicus |
|
MPK 5/2 | An Hemipteran, member of the family Belostomatidae | |
| Polysitum[8] | P.? sp. |
|
MPK 5/14, 29 | A Coleopteran, Incertade sedis | |
| Phoroschizidae[8] | Indeterminate |
|
MPK 5/4,5, 8, 20, 35 | Indeterminate Beetle remains | |
| Xylonichnus[6] | Cf.Xylonichnus isp. |
|
Boring Traces | Borings in the wood made probably by insect larvae |
See also
References
- ^ a b c d e f g h i j k l Pieñkowski, G. (2004). "The epicontinental Lower Jurassic of Poland". Polish Geological Institute Special Papers. 12 (1): 1–154. S2CID 128922070.
- ^ Deutsche Stratigraphische Kommission (2016). "Stratigraphische Tabelle von Deutschland" (PDF). GeoForschungsZentrum. 1 (1): 1. Retrieved 22 December 2021.
- ^ Karaszewski, W. (1962). "The stratigraphy of the Lias in the Northern Mesozoic Zone surrounding the Święty Krzyż Mountains (Central Poland) [Eng. Sum.]". Pr. Inst. Geol. 30 (3): 333–416.
- ^ Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
- ^ a b c d e f g h i j k l m n o p q PIEŃKOWSKI, GRZEGORZ (1985), "Early Liassic Trace Fossil Assemblages from the Holy Cross Mountains, Poland: Their Distribution in Continental and Marginal Marine Environments", Biogenic Structures, SEPM (Society for Sedimentary Geology), pp. 37–51, ISBN 0-918985-15-3, retrieved 2024-11-27
- ^ a b c d e f g h i j k l m n o p q r Pieńkowski, G.; Niedźwiedzki, G. (2008). "Invertebrate trace fossil assemblages from the lower Hettangian of Sołtyków, Holy Cross Mountains, Poland". Volumina Jurassica. 6 (1): 109–132.
- ^ Pieńkowski, G.; Uchman, A. (2009). "Ptychoplasma conica isp. nov.: a new bivalve locomotion trace fossil from the Lower Jurassic (Hettangian) alluvial sediments of Sołtyków, Holy Cross Mountains, Poland". Geological Quarterly. 53 (4): 397–406.
- ^ a b c d e f g h i j Wegierek, P.; Zherikhin, V. V. (1997). "An Early Jurassic insect fauna in the Holy Cross Mountains" (PDF). Acta Palaeontologica Polonica. 42 (4): 539–543.
- ^ Popov, Y. A. (1996). "The first record of a fossil water bug from the Lower Jurassic of Poland (Heteroptera: Nepomoprha: Belostomatidae)". Polskie Pismo Entomologiczne. 65 (1): 101–105.
Bibliography
- Weishampel, David B.; Dodson, Peter; Osmólska, Halszka (2004), The Dinosauria, 2nd edition, Berkeley: University of California Press, pp. 1–880, ISBN 0-520-24209-2, retrieved 2019-02-21