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Wyświetlanie 1-6 z 6
Tytuł:
Znalezisko kości ssaków plejstoceńskich w Garwolinie (Nizina Mazowiecka)
Bones of Pleistocene Mammals find in Garwolin (Mazovian Lowland)
Autorzy:
Żarski, M.
Jakubowski, G.
Ploch, I.
Powiązania:
https://bibliotekanauki.pl/articles/2075105.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Garwolin
mammoth
Vistulian
mamut
Wisła
Opis:
Remains of woolly mammoth, woolly rhinoceros, bison, reindeer and horse bones were found in 2006 y in gravel pit in Wilga Valley near Garwolin. The most numerous represent the mammoth bones: fragments of skull, teeth, and pelvis with biting trace by predators. The bones were found in the fluvial sands and gravels at the depth of 5–6 m below the ground surface. Geological studies have identified the origin and age of the deposits for the period of Vistulian. The age of mammoth bones in two analysis used 14C method is between 38 and 46 ka and is correlated with the Grudziadz Interstadial. Below the Vistululian sands and gravels are located tills of the Wartanian Glaciation, and above Holocene peat.
Źródło:
Przegląd Geologiczny; 2014, 62, 10/1; 525--531
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A new find of mammoth tusk in loess-like sediments of the Zakliczyn Basin (Outer Western Carpathians, Poland)
Autorzy:
Cieszkowski, M.
Zuchiewicz, W.
Alexandrowicz, W. P.
Wojtal, P.
Powiązania:
https://bibliotekanauki.pl/articles/191972.pdf
Data publikacji:
2010
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
loesses
mammoth remains
malacofauna
Upper Pleistocene
Polish Outer Carpathians
Opis:
In June 2007, in a valley side of a small stream close to Janowice in the Western Outer Carpathians of Poland, a 1.8 m long mammoth tusk was found within loamy-debris solifluction sediments, ca. 1 m thick. These discordantly overlie a 4-m-high strath built up of steeply dipping sandstones of the Krosno beds of the Skole Nappe, being in turn covered by 7.5-m-hick loessial silts and loess-like slopewash sediments. The latter are overlain at the top by another solifluction cover, ca. 1.5 m thick. The mammoth tusk belonged to an adult animal, probably 30-60 years old. The succession of malacofaunistic assemblages within loess-like sediments indicates a cold, polar climate, and an environment resembling tundra developed upon moderately moist substratum during the last glacial stage. The lower part of malacological sequence enriched in mesophile species probably refers to the Vistulian (Weichselian) interpleniglacial period. The middle part, indicative of more dry habitats, can be associated with the younger Pleniglacial, whereas the top part should represent the terminal phase of the latter. Sediments bearing the mammoth tusk were probably deposited at the turn of the Vistulian older Pleniglacial and Interpleniglacial time.
Źródło:
Annales Societatis Geologorum Poloniae; 2010, 80, No 1; 89-99
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rhinoceros exploitation at Érd (Hungary). What a place for the megaherbivores in the Neanderthal diet in Hungary?
Autorzy:
Daschek, Éva J.
Powiązania:
https://bibliotekanauki.pl/articles/2035494.pdf
Data publikacji:
2021
Wydawca:
Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego
Tematy:
Middle Palaeolithic
Rhinocerotidae
Proboscidea
rhinoceros exploitation
mammoth exploitation
Carpathian Basin
Opis:
The Hungarian Transdanubian site of Érd, where a Mousterian industry and abundant osteological material were discovered in the early 1960s is well known to prehistorians. The remains of megaherbivores (Mammuthus primigenius, Coelodonta antiquitatis) are re-examined here under the taphonomic and archaeozoological components in order to complete the Hungarian and European s.l. data and reassess the potential exploitation of these two pachyderms in the Neanderthal diet and economy. The cut marks, the intense activity of carnivores/hyenas and the skeletal profiles indicate a mixed origin of the carcasses. Mortality patterns of rhinoceros are characterized by the presence of young, subadult and adults, and suggest multiple acquisition by active scavenging and/or hunting with quick access. Skeletal profiles suggest a selective transport of rich/nutritive elements by humans to the site. The cut marks and fracturing of some elements (in situ butchery treatment) confirm that Neanderthals consumed these species on site and that they had at least partial primary access. The mode of acquisition seems active with rapid access for a young mammoth. Érd confirms the Neanderthal exploitation of rhinos and mammoths in their steppic environment during the Middle Palaeolithic. Érd is currently the only Hungarian Middle Palaeolithic site with a proven exploitation and consumption of these megaherbivores.
Źródło:
Acta Archaeologica Carpathica; 2021, 56; 13-66
0001-5229
2719-4841
Pojawia się w:
Acta Archaeologica Carpathica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Unikalne stanowisko szczątków mamuta na Dolnym Śląsku
Unique site of the mammoth remains in the Lower Silesia
Autorzy:
Wiśniewski, A.
Wojtal, P.
Krzemińska, A.
Zych, J.
Przybylski, B.
Badura, J.
Ciszek, D.
Powiązania:
https://bibliotekanauki.pl/articles/2074685.pdf
Data publikacji:
2009
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
mamut
vistulian
środowisko peryglacjalne
Dolny Śląsk
mammoth
Weichselian glaciation
periglacial environment
Lower Silesia
Opis:
Aunique set of mammoth bones and tusk was found in active gravel pit in vicinities of Zastruże near Żarów, Lower Silesia. The use of archaeological methods made it possible to uncover 17 bones belonging to a single individual (Mammuthus primigenius). This is the first record of so complete set of mammoth bones in the Lower Silesian region. Mammoth remains were found to be accompanied by some bones of a horse and a flint artifact. The mammoth bones were dated radiocarbon method at 23 790 š 160 years, that is at the beginning of the last Pleniglacial of the Weichselian Glaciation. The mammoth remains were embedded in slope sediments of a small valley so they did not occurin anatomical order.
Źródło:
Przegląd Geologiczny; 2009, 57, 3; 234-242
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Stanowisko mamuta – Mammuthus primigenius (Blumenbach, 1799) w górnym plejstocenie Kopalni Węgla Brunatnego Bełchatów
Mammuthus primigenius (Blumenbach, 1799) fromUpper Pleistocene deposits of the Be³chatów Coal Mine
Autorzy:
Błażejowski, B.
Jakubowski, G.
Gieszcz, P.
Kowalski, R.
Hołda-Michalska, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075107.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
mamut włochaty
izotopy stabilne w zębach
Bełchatów
woolly mammoth
stable isotope composition of teeth
Opis:
The fossil remains of juvenile woolly mammoth (Mammuthus primigenius) from Pleistocene deposits of the Be³chatów coal mine are described. Precise measurements of the excavated bones allowed for approximate reconstruction of the specimen, which turned out to be in the estimated age of 10 years. Serial samples for isotope analysis of carbon and oxygen were taken from a tooth, and the isotope record has revealed a probable change of diet due to switching from milk-based to plant-based food.
Źródło:
Przegląd Geologiczny; 2014, 62, 11; 755--760
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Structure and evolution of mammoth molar enamel
Autorzy:
Ferretti, M P
Powiązania:
https://bibliotekanauki.pl/articles/22594.pdf
Data publikacji:
2003
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
systematics
structure
Proboscidea
Middle Pliocene
Mammalia
mammoth
terminology
evolution
Pleistocene
Mammuthus
Mammuthus meridionalis
paleontology
Opis:
This work investigates the structure of Eurasian Plio–Pleistocene Mammuthus enamel, with attention to diagenesis and individual variability. A focal point of this study was to determine whether morphological trends in Mammuthus molars were accompanied by correlated enamel microstructure changes. In the examined four taxa the enamel of the cheek teeth consists of three layers delimited by two major discontinuities in enamel prism direction. Noticeably, the enamel capping the occlusal end of the unworn molar plates retains a less derived two−layered structure, similar to that found in the basal proboscidean Moeritherium. In Mammuthus meridionalis the third deciduous premolar is differentiated from all other teeth in having more strongly decussating Hunter−Schreger bands in the middle layer, as a possible reinforcement of the very thin enamel. Evidence from this analysis shows that, in the transition from late Middle Pliocene M. rumanus to Late Pleistocene M. primigenius, the middle enamel layer, which is made up of prisms at an angle to the occlusal surface, providing greater resistance against wear, increased its relative thickness. This is consistent with the hypothesis that Mammuthus adapted to a more abrasive diet. Comparison with other proboscidean taxa indicates that the schmelzmuster (enamel pattern) found in Mammuthus is a synapomorphy of the Elephantoidea.
Źródło:
Acta Palaeontologica Polonica; 2003, 48, 3
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-6 z 6

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