Middle Pleistocene (Early Toringian) Carnivore Remains from Northern Israel
Seventy well-preserved fossil remains from deposits of an eroded karstic cave in the Upper Galilee of northern Israel includeUrsus deningeri(Ursidae),Canis lupus cf.mosbachensis (Canidae),Crocuta crocuta cf. praespelaea (Hyaenidae), Panthera leo cf. spelaea (Felidae), and Dama sp. (Cervidae). This a...
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Veröffentlicht in: | Quaternary research 1997-07, Vol.48 (1), p.122-136 |
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description | Seventy well-preserved fossil remains from deposits of an eroded karstic cave in the Upper Galilee of northern Israel includeUrsus deningeri(Ursidae),Canis lupus cf.mosbachensis (Canidae),Crocuta crocuta cf. praespelaea (Hyaenidae), Panthera leo cf. spelaea (Felidae), and Dama sp. (Cervidae). This assemblage probably dates to the Early Toringian (MQ2, Middle Pleistocene). Ursus deningeri and Panthera leo cf. spelaeahave never before been recorded south of the Taurus–Zagros mountain chain. We correlate the carnivore faunule with some Near Eastern and southern Levantine sites and assume that only a severe cold phase could have shifted these species over the Taurus–Zagros mountain chain this far to the south. Due to the relative scarcity of Middle Pleistocene assemblages, especially carnivores, in the southern Levant, the biogeographic connection between the southern Levant and the Near East is still not well known. This faunule elucidates Pleistocene biotic exchanges between Europe and the Levant during this period. |
doi_str_mv | 10.1006/qres.1997.1901 |
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(Cervidae). This assemblage probably dates to the Early Toringian (MQ2, Middle Pleistocene). Ursus deningeri and Panthera leo cf. spelaeahave never before been recorded south of the Taurus–Zagros mountain chain. We correlate the carnivore faunule with some Near Eastern and southern Levantine sites and assume that only a severe cold phase could have shifted these species over the Taurus–Zagros mountain chain this far to the south. Due to the relative scarcity of Middle Pleistocene assemblages, especially carnivores, in the southern Levant, the biogeographic connection between the southern Levant and the Near East is still not well known. 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(Cervidae). This assemblage probably dates to the Early Toringian (MQ2, Middle Pleistocene). Ursus deningeri and Panthera leo cf. spelaeahave never before been recorded south of the Taurus–Zagros mountain chain. We correlate the carnivore faunule with some Near Eastern and southern Levantine sites and assume that only a severe cold phase could have shifted these species over the Taurus–Zagros mountain chain this far to the south. Due to the relative scarcity of Middle Pleistocene assemblages, especially carnivores, in the southern Levant, the biogeographic connection between the southern Levant and the Near East is still not well known. 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(Cervidae). This assemblage probably dates to the Early Toringian (MQ2, Middle Pleistocene). Ursus deningeri and Panthera leo cf. spelaeahave never before been recorded south of the Taurus–Zagros mountain chain. We correlate the carnivore faunule with some Near Eastern and southern Levantine sites and assume that only a severe cold phase could have shifted these species over the Taurus–Zagros mountain chain this far to the south. Due to the relative scarcity of Middle Pleistocene assemblages, especially carnivores, in the southern Levant, the biogeographic connection between the southern Levant and the Near East is still not well known. This faunule elucidates Pleistocene biotic exchanges between Europe and the Levant during this period.</abstract><cop>New York, USA</cop><pub>Cambridge University Press</pub><doi>10.1006/qres.1997.1901</doi><tpages>15</tpages></addata></record> |
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source | ScienceDirect Journals (5 years ago - present) |
subjects | Asia Bgi / Prodig Israel Southwest Asia |
title | Middle Pleistocene (Early Toringian) Carnivore Remains from Northern Israel |
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