J 2021

First remains of Diplocynodon cf. ratelii from the early Miocene sites of Ahnikov (Most Basin, Czech Republic)

CHROUST, Milan; Martin MAZUCH; Martin IVANOV; Boric EKRT; Ángel HERNÁNDEZ LUJÁN et. al.

Základní údaje

Originální název

First remains of Diplocynodon cf. ratelii from the early Miocene sites of Ahnikov (Most Basin, Czech Republic)

Autoři

CHROUST, Milan; Martin MAZUCH; Martin IVANOV; Boric EKRT a Ángel HERNÁNDEZ LUJÁN

Vydání

Bulletin of Geosciences, Czech Geological Survey, 2021, 1214-1119

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10506 Paleontology

Stát vydavatele

Česká republika

Utajení

není předmětem státního či obchodního tajemství

Odkazy

Impakt faktor

Impact factor: 1.404

Kód RIV

RIV/00216224:14310/21:00122266

Organizační jednotka

Přírodovědecká fakulta

UT WoS

000678008500001

EID Scopus

2-s2.0-85107424088

Klíčová slova anglicky

fossil crocodiles; alligatoroid; Ahnikov; Ohre/Eger Graben; Eggenburgian

Štítky

Příznaky

Mezinárodní význam, Recenzováno
Změněno: 6. 9. 2021 14:41, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

Fossil crocodylians from the early Miocene (Eggenburgian, MN3a) sites of Ahnikov (Most Basin, Czech Republic) are described in this paper. The new material presented here includes over 200 remains (bones, teeth and osteoderms), and therefore constitutes the largest crocodylian sample known from the fossil record of the Czech Republic. Assignment of the specimens to the fossil alligatoroid taxon Diplocynodon cf. ratelii Pomel, 1847 (family Diplocynodontidae) is justified by the presence of several cranial and postcranial features. In the Czech Republic, this species has been previously reported only from the Tusimice site (MN3, Most Basin, Ohre/Eger Graben). The majority of the material reported from Ahnikov is composed of disarticulated juvenile individuals. Both sites are most likely attributable to the specific environment of swampy areas, where crocodile hatchlings would hide from predators. The presence of the genus Diplocynodon supports the assumption of rather warm climatic conditions in Central Europe during the early to middle Miocene, as well as a swampy depositional environment previously inferred for Ahnikov. However, some squamate taxa suggest the existence of additional, surrounding palaeoenvironment characterised by a more open landscape with slightly drier conditions.

Návaznosti

EF16_027/0008360, projekt VaV
Název: Postdoc@MUNI