Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.palaeo.2010.01.025 |
Vegetation response to glacial-interglacial climate variability near Lake Malawi in the southern African tropics | |
Beuning, Kristina R. M.1; Zimmerman, Kurt A.1; Ivory, Sarah J.1; Cohen, Andrew S.2 | |
通讯作者 | Beuning, Kristina R. M. |
来源期刊 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
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ISSN | 0031-0182 |
EISSN | 1872-616X |
出版年 | 2011 |
卷号 | 303期号:1-4页码:81-92 |
英文摘要 | Pollen records from Lake Malawi, Africa spanning the last 135 kyr show substantial and abrupt vegetation response to multiple episodes of extreme aridity between 135 and 75 ka. Peaks in both the relative abundance and total production of Podocarpus pollen define the first two of these drought episodes. From 135 to 127 and again from 117 to 105 kyr BP. Podocarpus percentages remain above 16% with peak values as high as 38% indicating a period marked by a cool climate resulting in expansion of montane forest taxa to lower elevations. Marine palynological records from the Angola Margin and Congo Fan show similar peak Podocarpus percentages at this time (oxygen isotope stage 5d) indicating a similar climate across the African continent at this latitude. From 105 to 90 ka, continuing drought resulted in total pollen accumulation rates in Lake Malawi to fall to less than 300 grains/cm(2)/yr of predominately grass pollen. This episode in African history was severe enough to cause the disappearance of pteridophytes and forest taxa such as Uapaca and Brachystegia as well as montane taxa (Podocarpus, Olea spp. and Ericaceae) within the pollen source area of Lake Malawi. These taxa all remain nearly absent from the surrounding vegetation for the next 18,000 years. The resultant semi-desert vegetation would have been inhospitable for early humans living within or traveling through the Lake Malawi region. Increasing moisture following these arid intervals allowed expansion, creation and maintenance of a more diverse landscape vegetation mosaic around Lake Malawi including Zambezian miombo woodland, humid evergreen woodland and afromontane forests. The relative abundance of each fluctuated in response to either cooling (i.e. afromontane expansion from 60 to 56 ka) or moisture balance (i.e. increasing humid evergreen woodland between 75 and 65 ka). Notably there was no significant change in vegetation composition during the Last Glacial Maximum (LGM) (30-15 ka) as compared to the previous 20,000 years. (C) 2010 Elsevier B.V. All rights reserved. |
英文关键词 | Pollen Vegetation Pleistocene East Africa Paleoclimate |
类型 | Article |
语种 | 英语 |
国家 | USA |
收录类别 | SCI-E |
WOS记录号 | WOS:000289825900007 |
WOS关键词 | LATE PLEISTOCENE ; LATE QUATERNARY ; EAST-AFRICA ; EQUATORIAL AFRICA ; POLLEN ; HISTORY ; TEMPERATURE ; HOLOCENE ; RECORD ; MEGADROUGHTS |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology |
WOS研究方向 | Physical Geography ; Geology ; Paleontology |
来源机构 | University of Arizona |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/169889 |
作者单位 | 1.Univ Wisconsin, Dept Biol, Eau Claire, WI 54701 USA; 2.Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA |
推荐引用方式 GB/T 7714 | Beuning, Kristina R. M.,Zimmerman, Kurt A.,Ivory, Sarah J.,et al. Vegetation response to glacial-interglacial climate variability near Lake Malawi in the southern African tropics[J]. University of Arizona,2011,303(1-4):81-92. |
APA | Beuning, Kristina R. M.,Zimmerman, Kurt A.,Ivory, Sarah J.,&Cohen, Andrew S..(2011).Vegetation response to glacial-interglacial climate variability near Lake Malawi in the southern African tropics.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,303(1-4),81-92. |
MLA | Beuning, Kristina R. M.,et al."Vegetation response to glacial-interglacial climate variability near Lake Malawi in the southern African tropics".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 303.1-4(2011):81-92. |
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