Cypriniden-Schlundzähne west- und südosteuropäischer Tertiär-Lokalitäten

Rutte, Erwin; Weerd, A. van de

doi:10.1127/nos/8/1980/223

Cited by 7 publications

(7 citation statements)

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“…The material from the early Pleistocene of Altai contains a left pharyngeal bone with pharyngeal teeth, the second tooth of the first row bearing two grooves, the third tooth of the first row and a tooth from the second row bearing two grooves on the grinding surface. In Europe, the earliest Cyprinus (C. priscus Meyer) was described from the early Miocene of Würtemberg, Germany [67], but Rutte [68] did not think it was Cyprinus, whereas Obrhelová [69) and Gaudant [70) considered it closer to †Paleocarassius than to Cyprinus. c. scapularis, along with members from the tribe Oreinini in a list of vertebrate fossils found from the Plio-Pleistocene deposits of Karewa intermontane basin, Kashmir Valley, India.…”

Section: Distribution Of Cyprinus and Cyprinus-like Fishesmentioning

confidence: 99%

A new early cyprinin from Oligocene of South China

Chen

2011

Sci. China Earth Sci.

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Here we describe †Huashancyprinus robustispinus, gen. et sp. nov, a fossil cyprinin fish from the Oligocene of Ningming Basin, Guangxi, South China. It differs from all other cyprinin fishes in the following apomorphic characters: extremely robust last unbranched dorsal and anal fin rays with very fine serrations along posterior edge, the crowns of pharyngeal teeth A2 and A3 with a number of deep grooves on the lateral wall, rather large A3, and relatively deep infraorbital 2. Among the members of the Tribe Cyprinini sensu stricto, it mostly resembles the extant genus Cyprinus, particularly to species Cyprinus micristius and C. fuxianensis, which are restricted to Yunnan, southwestern China. The discovery of the cyprinin †Huashancyprinus from southern China, along with the previously known late Eocene †Cyprinus maomingensis, indicates an early branching of the Cyprininae (Cyprinidae) in this area. new early cyprinin, Oligocene, South China Citation:Chen G J, Chang M M. A new early cyprinin from Oligocene

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Section: Distribution Of Cyprinus and Cyprinus-like Fishesmentioning

confidence: 99%

A new early cyprinin from Oligocene of South China

Chen

2011

Sci. China Earth Sci.

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“…Fossils in the Mediterranean Sea during the Late Miocene and Early Pliocene belong to marine organisms or euryhalines such as the genus Lebias (Bianucci & Landini, 1992). Therefore, the presence of the genus Leuciscus in the fossil register of the southern part of the Iberian Peninsula is widely represented since the Middle Miocene to Early Pliocene (Gaudant, 1977;Rutte & van de Weerd, 1980;Doadrio & Casado, 1989). Bianco's hypothesis is supported by Hsü 's (1978) paleogeographical interpretations, which have been criticized extensively (Steininger & Rö gl, 1984).…”

Section: Biogeographical Implications and Paleogeographical Backgroundmentioning

confidence: 99%

Genetic divergence in Greek populations of the genus Leuciscus and its evolutionary and biogeographical implications

Doadrio

Carmona

1998

Journal of Fish Biology

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In 23 populations of Greek Leuciscus (Squalius), the percentage of polymorphic allozyme loci ranged between 0·034 and 0·379 (P=0·19) and expected heterozygosity was 0·011–0·166 (He=0·067). Current taxonomy is confusing and does not correspond to genetic data that support the presence in Greece of at least seven different species: L. cephalus, L. peloponnensis, L. prespensis, L. moreoticus, L. borysthenicus, L. keadicus and Leuciscus sp. from Euboea Island. The maximum Nei modified genetic distance was found among L. keadicus and the rest of subgenus Squalius populations D* Nei=0·446–0·705). Accepting the molecular clock hypothesis, speciation for the genus Leuciscus in Greece must have occurred during the Cenozoic period (between the Middle Miocene and the Later Pliocene). The two main biogeographical events causing speciation on mainland Greece were the Uplift of the Pindic cordillera and the isolation of the southern part of Peloponnesus. The faunistic composition of the lakes studied, in which new taxa are reconsidered, suggests the same faunistic origin in the Early Pliocene for Lakes Prespa and Stymphalia and a younger one in the Late Pliocene for Lake Trichonis. Euboea Island was not a zoogeographical unit during the Cenozoic. The isolation of all the freshwater fish fauna of Euboea has occurred since the Pliocene. The biogeographical model proposed here differs from classical hypotheses in considering of lesser importance the dispersion of L. cephalus on the Greek mainland during the Neogene and Quaternary.

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“…Для кількісних характеристик морфології глоткових зубів використана схема промірів, наведена у праці О.М. Касьянова зі співавторами [4] з урахуванням термінології Е. Рутте [25]: вимірювали висоту зуба і ширину основи коронки (рис. Рисунки зроблені з використанням рисувального апарату "Wild TYP 308700" до стереомікроскопа "Wild M3C".…”

Section: матеріали та методи дослідженняunclassified

“…Рештки риб роду Silurus є звичайними у пізньоміоценових і пліоценових відкладах півдня України. Кістки Silurus glanis fossilis знайдені у прибережно-морських вапняках понтичного віку в околицях м. Одеса[25], рештки S. glanis зібрані Т.Г. Грицаєм у 1957 р. на місцезнаходженні Шкодова гора Одеської області[2].…”

unclassified

Late Maeotian bony fish fauna in the North-Western Black Sea region

Kovalchuk

2013

Biol. Stud.

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Cypriniden-Schlundzähne west- und südosteuropäischer Tertiär-Lokalitäten

Cited by 7 publications

References 0 publications

A new early cyprinin from Oligocene of South China

A new early cyprinin from Oligocene of South China

Genetic divergence in Greek populations of the genus Leuciscus and its evolutionary and biogeographical implications

Late Maeotian bony fish fauna in the North-Western Black Sea region

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