Arid
DOI10.1016/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
ISSN0031-0182
EISSN1872-616X
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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