T. Kotsakis, L. Pandolfi, L. Maiorino, C. Petronio, G. Sansalone, L. Salari
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引用次数: 2
摘要
拉格雷夫(La Grave)的化石矿床(喀斯特洞穴)位于意大利南部塔兰托(Taranto)小镇avetraa附近,已经发现了许多脊椎动物的化石。大型哺乳动物的遗骸一直是几项研究的主题。本文通过对小型脊椎动物遗骸的研究,鉴定出两栖动物4个分类群(Bufo Bufo, Bufotes gr. b.v irridis, Hyla gr. H. Arborea和Rana (s.l.) sp.),爬行动物4个分类群(Testudo hermanni, Podarcis sp., Zamenis gr. Z. longissimus, Natrix Natrix),小型哺乳动物9个分类群(Erinaceus europaeus, Crocidura suaveolens, Arvicola italicus, Microtus (Terricola) savii, Microtus (Microtus) arvalis, Apodemus gr. A. sylvaticus - A. flavicollis,棘毛猴、小黄猴、小黄猴。从生物年代学的角度来看,小型和大型脊椎动物的数据表明其年龄介于晚更新世(MIS 5e)开始和MIS 3的中心部分之间。与前几层相比,最近的化石层(8层)可能是在较冷的时期沉积的。从小型脊椎动物化石和从大型哺乳动物和鸟类化石中得到的数据表明,在喀斯特洞穴附近,存在着带有水池的开放空间(草原),周围是树木繁茂的地区,不远的地方还有岩石海岸线。
Pequeños vertebrados del relleno kárstico del Pleistoceno Superior de Avetrana (Apulia, Sur de Italia)
The fossiliferous deposit (karst cavity) in La Grave, a locality near the small town of Avetrana (Taranto, southern Italy), has yielded numerous fossils of vertebrates. The remains of large mammals have been the subject of several studies. This paper examines the remains of small vertebrates and identifies four taxa of amphibians ( Bufo bufo, Bufotes gr. B. viridis, Hyla gr. H. Arborea and Rana (s.l.) sp.), four taxa of reptiles ( Testudo hermanni, Podarcis sp., Zamenis gr. Z. longissimus, Natrix natrix ), and nine taxa of small mammals ( Erinaceus europaeus, Crocidura suaveolens, Arvicola italicus, Microtus (Terricola) savii, Microtus (Microtus) arvalis, Apodemus gr. A. sylvaticus - A. flavicollis, Hystrix (Acanthion) vinogradovi, Oryctolagus cuniculus and Lepus corsicanus ). From a biochronological point of view, the data on small and large vertebrates indicate an age between the beginning of the Late Pleistocene (MIS 5e) and the central part of MIS 3. The most recent fossiliferous layer (bed 8) is likely to have been deposited during a cooler period when compared to the previous layers.The data from small fossil vertebrates combined with those emerging from the large mammals and birds evidence the presence, near the karstic cavity, of open spaces (prairies) with pools of water, bordered by wooded areas and, not far, the presence of a rocky coastline.
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