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首页> 外文期刊>Quaternary International >First finding of a partially articulated elephant skeleton from a Late Pleistocene hyena den in Sicily (San Teodoro Cave, North Eastern Sicily, Italy)
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First finding of a partially articulated elephant skeleton from a Late Pleistocene hyena den in Sicily (San Teodoro Cave, North Eastern Sicily, Italy)

机译:在西西里岛(意大利西西里岛东北部的圣特奥多罗洞穴)的晚更新世鬣狗窝中首次发现部分铰接的大象骨骼

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摘要

Associated and partially articulated fossil remains of the endemic reduced size elephant Palaeoloxodon mnaidriensis have been recently discovered at San Teodoro Cave, a large Late Pleistocene hyena den in Sicily. The skeletal elements belong to both cranial and post-cranial portions, and are represented by a semi-complete mandible, a tusk fragment, a cervical vertebra, three thoracic vertebrae, a rib fragment, a scapula, a distal epiphysis of radius, a pyramidal bone, a Ⅲ metacarpal bone, a coxal bone fragment, a femur shaft, two symmetrical pairs of tibias and fibulas, a patella and an astragalus. The bones were recovered mixed with remains belonging to other taxa, numerous hyena coprolites and with a juvenile elephant mandible in the perinatal stage. On the basis of anatomical representation, spatial distribution and development stages, the partially articulated elephant bones from the San Teodoro Cave belong to a single adult individual, perhaps a female, which probably entered the cave before its death, and was afterwards scavenged and disarticulated by hyenas. This is the first finding of a partially articulated elephant skeleton from a fossil hyena den, and may attest to the intermittent use of the cave by hyenas and elephants.
机译:最近在西西里岛的一个大型晚更新世鬣狗洞穴San Teodoro Cave中发现了地方性缩小大小的大象Palaeoloxodon mnaidriensis的相关的和部分铰接的化石遗址。骨骼元素既属于颅骨部分,又属于颅骨后部分,由半完整的下颌骨,象牙碎片,颈椎骨,三个胸椎骨,肋骨碎片,肩骨,of骨远端骨,、锥体状骨组成。骨,Ⅲ掌骨,髋骨碎片,股骨干,两对对称的胫骨和腓骨,a骨和黄芪。在围生期,这些骨头与其他类群的残留物,许多鬣狗共生遗骸以及下颌的幼年象混合在一起。根据解剖学表现,空间分布和发育阶段,来自圣特奥多罗山洞的部分铰接的大象骨头属于一个成年个体,也许是一头雌性,它们很可能在死前进入了该山洞,随后被清扫和分离。鬣狗。这是从化石鬣狗窝中发现部分铰接的大象骨骼的首次发现,并且可以证明鬣狗和大象对洞穴的间歇性使用。

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  • 来源
    《Quaternary International》 |2012年第25期|p.53-60|共8页
  • 作者单位

    Department of Earth Sciences, University of Messina, Viale Ferdinando Stagno d'Alcontres 31,1-98166, Messina-S. Agata, Italy;

    Department of Earth Sciences, University of Messina, Viale Ferdinando Stagno d'Alcontres 31,1-98166, Messina-S. Agata, Italy;

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