印度纳尔马达河谷中部脊椎动物化石的晶体学研究

Sakina Abdeali Halvadwala, Prateek Chakraborty
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摘要

纳尔马达河发源于中央邦东部的阿马尔坎塔克附近(北纬 200 40′,东经 81 46′),流经中央邦、马哈拉施特拉邦和古吉拉特邦,在古吉拉特邦的巴鲁克附近注入阿拉伯海的坎拜湾。该地区发现的大量化石包括各种哺乳动物、爬行动物、鱼类、两栖动物和软体动物贝壳。纳尔马达河谷不仅是旧大陆罕见的中间位置,而且历来是划分印度北部和南部的分界线。该河谷出土了无数动物化石和少量人类化石。这里是动物从北方向南方迁徙和季风从东南向西北传播的重要通道。本研究对位于中央邦纳尔马达河谷的三个地方(巴曼加特、塔拉亚加特和德瓦卡查尔)的动物化石的结晶指数进行了研究。对化石样本进行了 X 射线衍射,以计算作为化石化程度直接指标的结晶指数。之前的学者已经对纳尔马达河流域的材料进行了广泛的研究,但本研究是首次尝试使用 X 射线衍射等科学技术来研究化石。
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Crystallographic study of vertebrate fossils from the Central Narmada valley, India

The Narmada River originates in eastern Madhya Pradesh near Amarkantak (200 40′ N, 81 46′ E), travels through Madhya Pradesh, Maharashtra, and Gujarat before emptying into the Gulf of Cambay in the Arabian Sea, close to Baruch in Gujarat. Numerous fossil discoveries in the region include various mammals, reptiles, fishes, amphibians, and molluscan shells. In addition to being a rare mid-continental location in the Old World, the Narmada Valley has traditionally served as a line delineating Northern and Southern India. This valley has produced countless animal fossils as well as a few human fossils. This has been a crucial route for the movement of both faunal migrations from the north to the south and the transmission of the monsoons from the southeast to the northwest. The present work examines the crystallization index of the faunal fossils from three (Barmanghat,Talayyaghat,Devakachar) localities in the Central Narmada valley falling within the region of Madhya Pradesh. Fossil samples were subjected to X-Ray diffraction in order to calculate the Crystallization index as a direct indicator of the degree of fossilization. The materials of Narmada river valley have been studied extensively by previous scholars; however, this study is first attempt to study the fossils using scientific technique such as XRD.

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