首页> 外文期刊>Palaeobotanist >Middle Miocene flora from Siwalik foreland basin of Uttarakhand, India and its phytogeographic and palaeoclimatic implications
【24h】

Middle Miocene flora from Siwalik foreland basin of Uttarakhand, India and its phytogeographic and palaeoclimatic implications

机译:来自乌塔瓦尔赫,印度北尔米克前院盆地的中部内科植物植物及其植物地图和古网植物的影响

获取原文
       

摘要

Morphotaxonomical study on the plant fossils (leaf and fruit impressions) collected from Lower Siwalik sediments of Tanakpur area, Uttarakhand revealed the occurrence of 57 species of 25 angiospermous families. Of these, 39 species have been recorded new to the fossil flora of Himalayan foot hills and remaining 18 species are reported already from different Siwalik fossil localities of India, Nepal and Bhutan. The family Fabaceae (Legume family) represented by 15 species is the most dominant family in present assemblage followed by Annonaceae (8 species), Sapindaceae (5 species), Lauraceae and Euphorbiaceae (4 species) and Dipterocarpaceae and Rutaceae (3 species). The family Fabaceae which appeared in Upper Palaeocene became a major component of the evergreen forest during Middle Miocene times all along the Himalayan foot hills. In the present assemblage the evergreen floral taxa (54%) are dominant in contrast to mixed deciduous taxa at present. The predominance of evergreen elements in the Siwalik fossil assemblage indicates the prevalence of warm and humid climate with plenty of rain fall during the deposition of Siwalik sediments. The analysis of present day distribution of all the recovered species from the Siwalik foreland basins of Tanakpur area shows that they are mostly known to occur in North-east India, Bangladesh, Myanmar and Malaysia wherever favourable climatic conditions exist. Only about 14% taxa of the total assemblage are found to grow presently in the Himalayan foot hills and the remaining 86% taxa are locally extinct, suggesting changes in the climatic condition. Nearest Living Relative (NLR) suggests that the Tanakpur area enjoyed a tropical climate having Mean Annual Temperature (MAT) 24-28°C and Mean Annual Precipitation (MAP) 2100-2800 mm during the deposition of the sediments.
机译:从塔卡普尔地区的下斯瓦尔克沉积物收集的植物化石(叶子和水果印象)的MorphotoxoroMical研究,北方人揭示了57种缓神友家庭的发生。其中,39种已经为喜马拉雅脚山的化石群群体录制了新的,并且报告了来自印度,尼泊尔和不丹的不同Siwalik化石地区的18种。由15种所代表的家庭Fabaceae(豆科家族)是当前组合中最多的家庭,其次是Annonaceae(8种),Sapindaceae(5种),Lauraceae和Euphorbiaceae(4种)和Dipterocarpaceae和Ruticae(3种)。在Himalayan脚山上的中间内科时代,在上部古世教中出现的家族Fabaceae成为常绿森林的主要组成部分。在目前的组合中,与目前混合落叶征纳米的常绿花卉分类群(54%)是显着的。赤瓦石化术中常绿元素的优势表明,在塞瓦里克沉积物沉积期间,在塞瓦里克沉积期间,雨水落下的温暖和潮湿的气候普遍存在。从塔卡普尔地区斯瓦尔里克前陆盆地的所有回收物种的现今分布的分析表明,他们大多数人在印度东北,孟加拉国,缅甸和马来西亚存在,无论存在良好的气候条件。只有大约14%的总组合的分类群将在喜马拉雅脚山上目前增长,其余86%的分类群在局部灭绝,暗示气候条件的变化。最近的生活相对(NLR)表明,Tanakpur地区在沉积沉积期间享有24-28°C的平均温度(MAT)24-28°C和平均年降水量(地图)2100-2800mm。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号