Rhinocerotidae from the Upper Miocene deposits of the Western Pannonian Basin (Hungary): implications for migration routes and biogeography

Pandolfi, Luca; Gasparik, Mihály; Magyar, Imre

doi:10.1515/geoca-2016-0004

Cited by 16 publications

(9 citation statements)

References 31 publications

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“…The two first localities are referred to MN14, whilst Venta del Moro is biochronologically placed between the latest Turolian and the early Ruscinian (Table 3). The occurrence of P. megarhinus during that time agrees with the records of this species in France, Italy and Hungary (Pandolfi et al 2015(Pandolfi et al , 2016Pandolfi and Rook 2017). A dispersal of this taxon from East to West Europe during the latest Miocene has been Fig.…”

Section: The Spanish Pliocene Records Revised: Biochronology and Paleobiogeographysupporting

confidence: 87%

“…A dispersal of this taxon from East to West Europe during the latest Miocene has been Fig. 6 New biochronological scheme for the Spanish Pliocene rhinocerotines (Table 1 for references) indeed proposed by Pandolfi et al (2015Pandolfi et al ( , 2016 and Pandolfi and Rook (2017) who recorded P. megarhinus in several MN13 localities. The species probably reached the Iberian Peninsula at the Turolian-Ruscinian transition and occurred there till the mid-Pliocene (MN14-15 transition) (Fig.…”

Section: The Spanish Pliocene Records Revised: Biochronology and Paleobiogeographymentioning

confidence: 74%

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New Pliocene Rhinocerotidae findings from the Iberian Peninsula and the revision of the Spanish Pliocene records

Pandolfi

Sendra

Reolid

et al. 2022

PalZ

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A fragmentary mandible from the early Pliocene of the Vera Basin is here investigated to clarify its taxonomic position. The studied specimen is here assigned to Pliorhinus megarhinus, documented in Europe from the latest Miocene to the mid-Pliocene. The morphometrical comparison reveals that this taxon is larger than Stephanorhinus etruscus and S. jeanvireti but overlaps with Dihoplus schleiermacheri. P. megarhinus and D. schleiermacheri differ in some characters of the lower molars, such as the length of the metalophid and the shape of the trigonid in occlusal view, thus allowing new considerations on the Pliocene Spanish rhinocerotine record. According to the results here obtained, three species are at least documented in Span during the Pliocene: P. megarhinus, P. miguelcrusafonti, and S. etruscus. The presence of S. jeanvireti has to be verified and confirmed by further evidence. The presence of Dihoplus schleiermacheri as a relict taxon in the Pliocene of Spain is here discarded.

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Section: The Spanish Pliocene Records Revised: Biochronology and Paleobiogeographysupporting

confidence: 87%

Section: The Spanish Pliocene Records Revised: Biochronology and Paleobiogeographymentioning

confidence: 74%

New Pliocene Rhinocerotidae findings from the Iberian Peninsula and the revision of the Spanish Pliocene records

Pandolfi

Sendra

Reolid

et al. 2022

PalZ

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“…(Halaváts, 1925). Mammal remnants representing MN11 to MN14 are relatively common (Gasparik 2001;Kováč et al 2006Kováč et al , 2010Tóth 2010;Pandolfi et al 2016). Authigenic 10 Be / 9 Be ages obtained from the Volkovce Fm.…”

Section: Zagyva Formation / Volkovce Formationmentioning

confidence: 99%

Late Miocene sedimentary record of the Danube/Kisalföld Basin: interregional correlation of depositional systems, stratigraphy and structural evolution

Sztanó¹,

Kováč²,

Magyar³

et al. 2016

Geologica Carpathica

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Abstract:The Danube / Kisalföld Basin is the north-western sub-basin of the Pannonian Basin System. The lithostratigraphic subdivision of the several-km-thick Upper Miocene to Pliocene sedimentary succession related to Lake Pannon has been developed independently in Slovakia and Hungary. A study of the sedimentary formations across the entire basin led us to claim that these formations are identical or similar between the two basin parts to such an extent that their correlation is indeed a matter of nomenclature only. Nemčiňany corresponds to the Kálla Formation, representing locally derived coarse clastics along the basin margins (11-9.5 Ma). The deep lacustrine sediments are collectively designated the Ivanka Formation in Slovakia, while in Hungary they are subdivided into Szák (fine-grained transgressive deposits above basement highs, 10.5 -8.9 Ma), Endrőd (deep lacustrine marls, 11.6 -10 Ma), Szolnok (turbidites, 10.5 -9.2 Ma) and Algyő Formations (fine-grained slope deposits, 10 -9 Ma). The Beladice Formation represents shallow lacustrine deltaic deposits, fully corresponding to Újfalu (10.5 -8.7 Ma). The overlying fluvial deposits are the Volkovce and Zagyva Formations (10 -6 Ma). The synoptic description and characterization of these sediments offer a basin-wide insight into the development of the basin during the Late Miocene. The turbidite systems, the slope, the overlying deltaic and fluvial systems are all genetically related and are coeval at any time slice after the regression of Lake Pannon initiated about 10 Ma ago. All these formations get younger towards the S, SE as the progradation of the shelf-slope went on. The basin got filled up to lake level by 8.7 Ma, since then fluvial deposition dominated.

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“…The evolutionary origin of the Hundsheim rhinoceros remains unresolved, as does the more general issue of the phylogenetic relationships within the genus Stephanorhinus. Moreover, the genus Stephanorhinus is probably paraphyletic as currently defined, which is indicated both by the morphological (Pandolfi et al, , 2016 and molecular (Cappellini et al, 2019) data. The analysis of dental enamel proteome of an isolated lower molar classified as Stephanorhinus ex gr.…”

Section: Discussionmentioning

confidence: 87%

Pleistocene rhinoceros from Bogovina Cave: the first report of Stephanorhinus hundsheimensis Toula, 1902 (Mammalia, Rhinocerotidae) from Serbia

Radović

Radonjić

Billia

2020

Palaeontol Electron

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Finds of Pleistocene rhinoceros are rare in Serbia, and only one species (the woolly rhinoceros Coelodonta antiquitatis Blumenbach, 1799) has been reported so far. The current paper presents the dental material of an extinct so-called Hundsheim rhinoceros, Stephanorhinus hundsheimensis Toula, 1902 from Bogovina Cave (Eastern Serbia). Both the morphological and metric characteristics of the teeth are consistent with the attribution to S. hundsheimensis. Unfortunately, the rhinoceros material originated from an uncertain geological context, so there is no firm basis for dating. However, a potential association with a caballoid horse tooth could hint at an age of 600 ka or less for the assemblage, which would indicate a relatively late date for the Hundsheim rhinoceros from Bogovina Cave.

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Rhinocerotidae from the Upper Miocene deposits of the Western Pannonian Basin (Hungary): implications for migration routes and biogeography

Cited by 16 publications

References 31 publications

New Pliocene Rhinocerotidae findings from the Iberian Peninsula and the revision of the Spanish Pliocene records

New Pliocene Rhinocerotidae findings from the Iberian Peninsula and the revision of the Spanish Pliocene records

Late Miocene sedimentary record of the Danube/Kisalföld Basin: interregional correlation of depositional systems, stratigraphy and structural evolution

Pleistocene rhinoceros from Bogovina Cave: the first report of Stephanorhinus hundsheimensis Toula, 1902 (Mammalia, Rhinocerotidae) from Serbia

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