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首页> 外文期刊>Palaeobotanist >Vegetation vis á vis climate change around Bhogdoi swamp in lower Brahmaputra flood plain of Assam, Northeast India since Late Holocene
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Vegetation vis á vis climate change around Bhogdoi swamp in lower Brahmaputra flood plain of Assam, Northeast India since Late Holocene

机译:自新世晚期以来印度东北部阿萨姆邦布拉马普特拉河下游平原博格多沼泽附近的植被与气候变化

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Dixit S & Bera SK 2013. Vegetation vis á vis climate change around Bhogdoi swamp in lower Brahmaputra flood plain of Assam, Northeast India since Late Holocene. The Palaeobotanist 62(1): 19-27. Pollen records from 1.8 m deep sedimentary profile cored from Bhogdoi swamp, Kamrup District, lower Brahmaputra flood plain of Assam, Northeast India have revealed enrichment of tropical mixed deciduous forest elements including Shorea robusta, Syzygium cumini, Dillenia pentagyna and Acacia catechu indicating warm and humid climatic regime during 3,795-2,530 years BP. Subsequently during 2,530-680 years BP relative increment in proliferation of tropical mixed deciduous elements namely Lagerstroemia parviflora, Lannea coromandelica, Terminalia bellirica, Sapotaceae and Emblica officinalis occurred resulting into final settlement of tropical mixed deciduous forest under increased warm and humid climatic regime attributable to active Southwest Monsoon. However, from 680 years BP onward gradual deterioration of mixed deciduous forest occurred as evidenced by sudden decline in Sal and its associates under warm and relatively drier climate. Drastic increment in Melastoma, Ziziphus and Areca implying forest clearance at this phase. The occurrence of degraded pollen-spore along with adequate fungal remains especially Xylaria, Diplodia, Nigrospora and Microthyriaceous fruiting body is suggestive of aerobic microbial digenesis of rich organic debris during sedimentation.
机译:Dixit S&Bera SK2013。植被自气候变化以来在印度新罕布什尔州阿萨姆邦较低的雅鲁藏布江泛洪平原博格伊沼泽附近。古植物学家62(1):19-27。来自印度东北部阿萨姆邦下部阿布萨姆邦布拉马普特拉洪水泛滥区博格多伊沼泽的1.8 m深沉积剖面的花粉记录显示,热带混合落叶林元素的富集,包括浓香木,Syzygium cumini,Dillenia pentagyna和相思树(Acacia catechu),表明温暖湿润BP 3,795-2,530年间的气候状况。随后,在2,530-680年间,BP混合热带落叶植物,即小花紫薇,兰香,甜菜,榄仁科和Emblica officinalis的增殖相对增加,导致热带混合落叶林最终定居,这归因于活跃和温暖的气候条件西南季风。但是,从680年开始,BP逐渐发生了混合落叶林的逐渐恶化,这在温暖和相对干燥的气候下,Sal及其伴生的突然下降就证明了这一点。 Melastoma,Zipziphus和Areca的急剧增加意味着在此阶段清除了森林。花粉孢子的降解以及适当的真菌残留物的出现,尤其是木屑,Diplodia,Nigrospora和Microthyriaceous的子实体,表明在沉积过程中富含有机物碎片的好氧微生物成生。

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