2021
The Record of Prodeinotherium in the Iberian Peninsula: New Data from the Vallès-Penedès Basin
GASAMANS, Natalia; Ángel HERNÁNDEZ LUJÁN; Guillem PONS-MONJO; Pau OBRADÓ; Isaac CASANOVAS-VILAR et. al.Základní údaje
Originální název
The Record of Prodeinotherium in the Iberian Peninsula: New Data from the Vallès-Penedès Basin
Autoři
GASAMANS, Natalia; Ángel HERNÁNDEZ LUJÁN; Guillem PONS-MONJO; Pau OBRADÓ; Isaac CASANOVAS-VILAR a David M. ALBA
Vydání
Journal of Mammalian Evolution, Springer, 2021, 1064-7554
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10500 1.5. Earth and related environmental sciences
Stát vydavatele
Spojené státy
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 2.412
Kód RIV
RIV/00216224:14310/21:00123670
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000639731300001
EID Scopus
2-s2.0-85104501750
Klíčová slova anglicky
Proboscidea; Deinotheriidae; Prodeinotherium cuvieri; Prodeinotherium bavaricum; Miocene; Europe
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 12. 1. 2022 12:24, Mgr. Marie Novosadová Šípková, DiS.
Anotace
V originále
Deinotheres (Proboscidea, Deinotheriidae) are a clade of non-elephantiform proboscideans that originated in Africa and dispersed into Eurasia by the early Miocene. In Europe, deinotheres are first recorded in Greece during MN3, although they did not become a common faunal element throughout Europe until MN4. Early Miocene (MN3–MN4) deinothere remains from Europe are generally assigned to a different species (Prodeinotherium cuvieri) than those from the early middle Miocene (Prodeinotherium bavaricum; MN5–MN6). In the Vallès-Penedès Basin (NE Iberian Peninsula), Prodeinotherium remains are very scarce and largely remain unpublished. To clarify their taxonomic assignment, we describe the available material and compare it with that from elsewhere in Europe. Based on size and a few diagnostic occlusal details, we tentatively recognize both Prodeinotherium cf. P. cuvieri and Prodeinotherium cf. P. bavaricum in the basin. Although all the studied sites had previously been correlated to MN4, the recognition of P. cf. P. bavaricum at els Casots and les Escletxes is consistent with ongoing litho- and magnetostratigraphic studies suggesting a slightly younger age for these sites. The lack of Prodeinotherium remains in older (MN3) localities from the Vallès-Penedès Basin, where Gomphotherium is already recorded, further supports the view that deinotheres dispersed into Western Europe somewhat later than gomphotheres.
Návaznosti
| EF16_027/0008360, projekt VaV |
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