首页> 外文期刊>Journal of earth system science >Lagerstroemia L. from the middle Miocene Siwalik deposits, northern India: Implication for Cenozoic range shifts of the genus and the family Lythraceae
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Lagerstroemia L. from the middle Miocene Siwalik deposits, northern India: Implication for Cenozoic range shifts of the genus and the family Lythraceae

机译:来自印度北部中新世中部西瓦里克矿床的紫薇:属和千屈菜科的新生代范围变化的含义

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Fossil leaves of Lagerstroemia (Lythraceae) are described from the Siwalik deposits (middle Miocene) of Kathgodam, Uttarakhand, India. The fossil records of the Lythraceae indicate its worldwide distribution in the Cenozoic. The family had its widest distribution during the Miocene but became less widespread during the Pliocene, followed by range expansion during the Quaternary. The present leaf fossil, along with the previous fossil records of Lagerstroemia, indicates that the genus followed the same pattern of expansion and retraction as the entire family Lythraceae suggesting that both the genus and the family adapted in similar ways. The fossil plant assemblage from the Lower Siwalik deposits indicates warm and humid climate with plenty of rainfall in the region during the depositional period.
机译:紫薇(化石科)的化石叶片是从印度北阿坎德邦加德哥丹的西瓦里克矿床(中新世中期)描述的。千屈菜科的化石记录表明其在新生代分布。该家族在中新世时期分布最广,但在上新世时期分布不大,随后在第四纪世代扩展。目前的叶化石以及紫薇的先前化石记录表明,该属与整个千屈菜科遵循相同的扩展和收缩模式,这表明该属和该科都以相似的方式进行了适应。下西瓦里克沉积物的化石植物组合表明该地区气候温暖湿润,在沉积期间该地区降雨充沛。

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