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A contribution to the Holocene vegetation history of Nigeria: Pollen from Ohe Pond Nsukka, southeastern Nigeria

机译:对尼日利亚全新世植被历史的贡献:来自尼日利亚东南部Ohe Pond Nsukka的花粉

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摘要

The pollen record from Ohe Pond (N 06° 50.156, E 007° 21.837) in Nsukka, Enugu State, southeastern Nigeria, provided strong evidence of existence of a Southern Guinea savanna in the mid-Holocene. Prior to 6417 ± 67 BP, there was a closed forest with strong Guinea savanna affinities with a more humid condition. However, after 6417 ± 67 BP, Southern Guinea savanna woodland became well established in the area. Considerable periods of high precipitation alternating with warm and dry climatic phases may have favoured the establishment and maintenance of this complex heterogeneous vegetation structure after 6388 ± 71 BP. Frequent natural fires, indicated by charred plant tissues throughout the mid Holocene, probably were important in promoting the expansion of savanna species in the vegetation. Furthermore, human impact associated with iron smelting from about 4005 ± 40 BP in the area may have contributed to depletion of the forest vegetation. The transition from the Southern Guinea savanna to derived forest-savanna mosaic vegetation became apparent at a latter part of the late Holocene around 1470 ± 79 BP. Although climate may have played a significant role in shaping the structure of the vegetation, human activities certainly played an important role in the late Holocene vegetation transformation.
机译:尼日利亚东南部Enugu州Nsukka的Ohe Pond(N 06°50.156,E 007°21.837)的花粉记录提供了强烈的证据,表明全新世中存在南部几内亚热带稀树草原。在6417±67 BP之前,有一个封闭的森林,其几内亚热带稀树草原亲和力强,湿度更高。但是,在6417±67 BP之后,几内亚南部大草原林地在该地区已经建立。在6388±71 BP之后,相当长的高降水期与温暖和干燥的气候阶段交替可能有利于这种复杂的非均质植被结构的建立和维持。在整个全新世中期,频频发生的自然火灾以烧焦的植物组织为标志,这可能对促进植被中热带稀树草原物种的扩散很重要。此外,与该地区约4005±40 BP的铁熔炼相关的人为影响可能导致森林植被枯竭。从新几内亚热带稀树草原到衍生的森林热带稀树草原马赛克植被的转变在全新世晚期大约1470±79 BP的后期很明显。尽管气候可能在塑造植被结构中发挥了重要作用,但人类活动无疑在晚新世植被转变中起了重要作用。

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  • 来源
    《Quaternary International》 |2014年第4期|28-34|共7页
  • 作者单位

    Department of Plant Science and Biotechnology, University of Nigeria, Nsukka, Enugu State, Nigeria;

    Department of Geology, University of Ibadan, Ibadan, Oyo State, Nigeria;

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