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Fossil leaf-impressions from the Late Tertiary sediments of Mahuadanr Valley, Latehar District, Jharkhand, India

机译:印度贾坎德邦拉哈尔地区Mahuadanr谷地第三纪沉积物的化石叶片印象

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Morphotaxonomical study of the leaf impressions collected from the Late Tertiary sediments of Mahuadanr Valley,Jharkhand, India has been done. The comparison of morphological features between the fossils and extant taxa revealedthe occurrence of 13 species of 5 dicotyledonous families. On the basis of present assemblage the palaeoclimate andphytogeography of Mahuadanr area during the Late Tertiary have been deduced. Present distribution of all the moderncomparable species of the fossils indicates that these are presently found to grow in the tropical forests of the Himalayanfoot hills, central India, south India and adjoining area of the Mahuadanr Valley, suggesting a mixed, mesophytic type offorest was flourishing in and around the fossil locality during the sedimentation. As most of the comparable species arefound now-a-days in the vicinity of fossil locality of Mahuadanr it indicates that same flora has continued till now whichsuggests that there has been no marked climatic change in the area since the Late Tertiary time.
机译:对从印度贾坎德邦马瓦丹尔河谷第三纪晚期沉积物中收集的叶片印象进行形态分类学研究。化石和现存的分类单元之间形态特征的比较揭示了5个双子叶植物科中有13种。根据目前的组合,推导了第三纪晚期Mahuadanr地区的古气候和植物地理。目前所有现代可比化石物种的分布情况表明,目前发现这些化石生长在喜马拉雅山丘陵地带,印度中部,印度南部和马瓦丹尔河谷毗连地区的热带森林中,这表明混合的中生类型森林正在蓬勃发展。以及沉积过程中化石的周围。由于如今大多数可比物种都在马化丹省化石所在地附近发现,这表明同一植物群一直持续到现在,这表明该地区自第三纪晚期以来一直没有明显的气候变化。

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