The age and paleoenvironment of a late Miocene floodplain alongside Lake Pannon: Rodent and mollusk biostratigraphy coupled with authigenic 10Be/9Be dating in the northern Danube Basin of Slovakia

Joniak, Peter; Šujan, Michal; Fordinál, Klement; Braucher, Régis; Rybár, Samuel; Kováčová, Marianna; Kováč, Michal; Aumaître, Georges; Bourlès, Didier; Keddadouche, Karim

doi:10.1016/j.palaeo.2019.109482

Cited by 15 publications

(9 citation statements)

References 54 publications

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“…The success of the water-moles in Šalgovce 5 (MN12) supports a change towards more homogeneous environments with a prevalence of lakes, low-energy rivers, and floodplains. Such interpretation matches the paleoenvironmental reconstruction of Joniak et al (2020).…”

Section: Discussionsupporting

confidence: 91%

“…Typically, the Vallesian-aged P2 and P3 are double-rooted, whereas Turolian-aged P2 and P3 are triple-rooted (Ziegler, 2006a). Triblavina is an exception as the P2 and P3 still display two roots, whereas this locality is correlated to the lowermost MN11 (Joniak and Šujan, 2020; Joniak et al, 2020). The presence of two roots in A .…”

Section: Systematic Paleontologymentioning

confidence: 99%

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The Late Miocene Talpidae (Eulipotyphla, Mammalia) from the Pannonian Region, Slovakia

Cailleux,

van den Hoek Ostende,

Joniak

2024

J. Paleontol.

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Central Europe is an area of high diversity for the Talpidae (Eulipotyphla, Mammalia) during the Late Miocene. The assemblages from Slovakia (Borský Svätý Jur, Krásno, Pezinok, Šalgovce, Studienka, Triblavina) are no exception with their abundant material representing eleven species. The uropsiline Desmanella is represented by D. rietscheli and D. dubia. Desmanini fossils are attributed to Archaeodesmana vinea, Archaeodesmana dissona new species, Gerhardstorchia biradicata, and Gerhardstorchia sp. The scalopines Proscapanus minor and P. austriacus are well recorded in the Vallesian localities and support the emergence of P. austriacus before the MN9/10 transition. Talpini and Urotrichini are especially rare and only represented by Talpa cf. T. minuta and Urotrichini gen. sp. indet. Finally, we identified the youngest occurrence of Desmanodon in Europe, D. cf. D. fluegeli, at the MN9 locality of Borský Svätý Jur. The high diversity in the Late Miocene Central European is partly explained by the co-occurrence of the competing Scalopini and Talpini during the Vallesian, indicating high resource environments. The decline of these tribes, followed by the success of the desmans during the Turolian, appears as a consequence of regional environmental changes.UUID: http://zoobank.org/a3eb532b-c341-489a-b0ff-ecf3f9466a76

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Section: Discussionsupporting

confidence: 91%

Section: Systematic Paleontologymentioning

confidence: 99%

The Late Miocene Talpidae (Eulipotyphla, Mammalia) from the Pannonian Region, Slovakia

Cailleux,

van den Hoek Ostende,

Joniak

2024

J. Paleontol.

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“…Pollen Zone KM19-1 is entirely in the clay layer with large fragments of wood, and alternates between silty-clay and clayey-silt grain sizes (Figure 4; Figure 7: Stages A-C). In sedimentological terms, this could be indicative of a floodplain setting, given the implied decrease in fluvial transport capacity associated with plant fragments and lignite, as described by Joniak et al (2020). The pollen assemblages show that the hinterland of the lake was covered by a conifer-dominated mixed forest (Schneider, 1992;Figure 7: Stages A-B).…”

Section: Figurementioning

confidence: 92%

Middle Miocene (Serravallian) wetland development on the northwest edge of Europe based on palynological analysis of the uppermost Brassington Formation of Derbyshire, United Kingdom

McCoy¹,

Barrass-Barker²,

Hocking³

et al. 2022

Preprint

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The Middle Miocene was a warmer and wetter interval than present-day (Steinthorsdottir et al., 2021). In the UK, the most extensive Middle Miocene deposit is the Serravallian Kenslow Member of the Brassington Formation as exposed at Bees Nest Pit, near Brassington, Derbyshire, UK. While known to contain a diverse palynological and palaeobotanical record, the stratigraphical distribution of these fossils has not been studied in detail, thus biome variations through a most important proxy period are very poorly understood. This important unit has never been the subject of a detailed, multi-sample study. Here we present a 58-sample record covering 133 cm of clay and lignite. The results comprise the first reconstruction of a bog succession in the Miocene palaeobotanical record of the UK. A predominant warm-temperate and mixed mesophytic forest biome was present. Within this forest, the local wetland developed in response to environmental changes that were not related to any major climatic shift. This wetland development produced a relatively open shrub and reed-dominated mire which produced the lignite-precursor peat. The limited extent of the lignite lentil and its position adjacent to a preserved fallen tree suggests that the peat was deposited in a tree throw, although it is not possible to rule out a slightly deeper stagnant pond within the overall wetland environment.

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“…The artificial temporal outcrop was accessible during construction of the road near Triblavina [1] in June 2017. At least 2.5 tons of sediment from the fossiliferous layer was dried, soaked and washed on a set of stable sieves [11].…”

Section: Experimental Design Materials and Methodsmentioning

confidence: 99%

Systematic and morphometric data of late Miocene rodent assemblage from Triblavina (Danube Basin, Slovakia)

Joniak

Šujan

2020

Data in Brief

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The lower Turolian (MN11) assemblage of rodents collected from new temporal outcrop near Triblavina (Danube Basin, Western Slovakia) is described. Fossils were collected from at least 2.5 tons of sediment that was wet sieved on a set of stable sieves. The mesh size of the lower sieve was 0.5 mm and the residue was not treated with acids for the sake of preserving mollusk shells. Fossil remains were picked manually from residue under the stereo-microscope. More than 170 teeth of small mammals were recovered. The rodent assemblage consists of 87 identifiable teeth belonging to ten taxa: Apodemus lugdunensis, Kowalskia sp., Epimeriones austriacus, Eozapus intermedius, Spermophilinus sp., Myomimus dehmi, Vasseuromys pannonicus, Keramidomys ermannorum, Keramidomys sp. and Eomyops sp. Fauna of rodents from Triblavina is described in detail here and these data are associated with recent article [1].

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The age and paleoenvironment of a late Miocene floodplain alongside Lake Pannon: Rodent and mollusk biostratigraphy coupled with authigenic 10Be/9Be dating in the northern Danube Basin of Slovakia

Cited by 15 publications

References 54 publications

The Late Miocene Talpidae (Eulipotyphla, Mammalia) from the Pannonian Region, Slovakia

The Late Miocene Talpidae (Eulipotyphla, Mammalia) from the Pannonian Region, Slovakia

Middle Miocene (Serravallian) wetland development on the northwest edge of Europe based on palynological analysis of the uppermost Brassington Formation of Derbyshire, United Kingdom

Systematic and morphometric data of late Miocene rodent assemblage from Triblavina (Danube Basin, Slovakia)

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