Abstract
Eight anatomically and taxonomically different finds are presented in this paper, and they belong to four taxa: woolly mammoth (Mammuthus primigenius), giant deer (Megaloceros giganteus), red deer (Cervus elaphus), and dog (Canis familiaris). All specimens represent allochthonous Late Pleistocene and Holocene animal remains, and all were dredged during the gravel exploitation at the Sekuline site near Molve (Podravina region, SW Pannonian basin, NE Croatia). Mammoth remains (bone and tusk fragments) were radiocarbon dated, and these are the first absolute dates on mammoths in Croatia. One upper last left deciduous premolar (dP4 sin.) also belongs to the same species. Ascribed to a dog is one well-preserved skull with a peculiar abscess scar on the maxillary bone as the result of an inflammatory process on the carnassial (P4) premolar. The Late Pleistocene cervid remains are giant deer, while the other cervid finds were determined to be red deer of the Holocene age. Morphometrical and taphonomical data are presented for each specimen. Such fossil and recent bone/tooth aggregates are characteristic of fluvial deposits and selective collecting. Although lacking stratigraphic provenance, these finds help to fulfil the gaps in palaeoenvironmental, palaeoecological, and palaeoclimate reconstructions of Podravina and its neighbouring areas.
Highlights
Gravel pits in Sekuline (46◦ 70 N, 17◦ 40 E, 120 m a.s.l.) are situated near the town of Molve (NE Croatia; Figure 1) in Podravina region, which is located in the southwestern part of the Pannonian basin
The bones, antlers, and teeth belong to the following species: Mammuthus primigenius, Megaloceros giganteus, Cervus elaphus, and Canis familiaris
The fossil/subfossil/recent remains were prepared with polyvinyl butyral (PVB) solution, in which the bones/teeth and antlers were submerged for 1 week, after which they were dried at room temperature
Summary
Gravel pits in Sekuline (46◦ 70 N, 17◦ 40 E, 120 m a.s.l.) are situated near the town of Molve (NE Croatia; Figure 1) in Podravina region, which is located in the southwestern part of the Pannonian basin. This central-eastern European basin is bounded by the Carpathian, Alpine, Rhodope and Dinaric mountain belts [1]. Alluvial depressions of the Danube, Tisa, Drava, and Sava rivers are Quaternary 2018, 1, 11; doi:10.3390/quat1020011 www.mdpi.com/journal/quaternary. Alluvial depressions of the Danube, Tisa, Drava, and Sava rivers. 2 of Dinaric are indicative of the Pannonian basin. Sekuline is oneare of the most recently sites indicative of the Pannonian
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