首页> 外文期刊>Quaternary International >Vegetation history during the last 17,000 years around Sonenuma Swamp in the eastern shore area of Lake Biwa, western Japan: With special reference to changes in species composition of Quercus subgenus Lepidobalanus trees based on SEM pollen morphology
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Vegetation history during the last 17,000 years around Sonenuma Swamp in the eastern shore area of Lake Biwa, western Japan: With special reference to changes in species composition of Quercus subgenus Lepidobalanus trees based on SEM pollen morphology

机译:日本西部琵琶湖东岸地区Sonenuma沼泽周围近17,000年的植被历史:基于SEM花粉形态,特别参考了栎属鳞翅目栎属树种的物种变化

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摘要

A pollen record of Sonenuma Swamp provides vegetation history for the last 17,000 years around the eastern shore area of Lake Biwa, western Japan. Identification of Quercus subgenus Lepidobalanus pollen by using scanning electron microscope shows composition changes of deciduous oaks at the species level. During 17,000 to 15,000 cal BP, deciduous broadleaved forest mainly consisted of Q, sect. Prinus developed around Sonenuma Swamp associated with pinaceous conifers and birch trees. Q, sect. Prinus and Q, dentata became dominant in the forests from 15,000 to 10,000 cal BP. The increase of Q. dentata in this period was possibly related to fire events around Sonenuma Swamp, as indicated by the charcoal record. From 10,000 to 6000 cal BP, CeltisjAphananthe trees became dominant in forests around Sonenuma Swamp. Temperate evergreen broadleaved forest composed of Q, subgenus Cyclobalanopsis trees along with Q. sect. Cerris trees developed during the period 6000 to 2500 cal BP. After 2500 cal BP, pine forests and grassland increased, with charcoal abundance likely affected by human activity around Sonenuma Swamp.
机译:Sonenuma沼泽的花粉记录提供了日本西部琵琶湖东岸地区过去17,000年的植被历史。通过扫描电子显微镜鉴定栎属鳞翅目花粉,显示了在物种水平上落叶栎的组成变化。在17,000至15,000 cal BP期间,落叶阔叶林主要由Q属组成。普里努斯在松嫩沼沼泽附近生长,与松树针叶树和桦树相关。 Q,教派从15,000到10,000 cal BP,Prinus和Q,dentata在森林中占主导地位。如木炭记录所示,此期间齿牙dent的增加可能与Sonenuma沼泽周围的火灾有关。从10,000到6000 cal BP,CeltisjAphananthe树在Sonenuma沼泽附近的森林中占主导地位。温带常绿阔叶林,由Q,Cyclobalanopsis属亚种和Q.属组成。紫杉树在6000到2500 cal BP期间发育。在2500 cal BP之后,松树林和草地增加,木炭的丰度很可能受到Sonenuma沼泽周围人类活动的影响。

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  • 来源
    《Quaternary International》 |2012年第16期|p.99-106|共8页
  • 作者单位

    Graduate School of Life and Environmental Sciences, Kyoto Prefecturat University, 1-5, Hangi-cho, Shimogamo, Sakyo-ku, Kyoto 606-8522, Japan;

    Graduate School of Science, Osaka City University, 3-3-138, Sugimoto-cho, Sumiyoshi-ku, Osaka, 558-8585, Japan;

    Graduate School of Agriculture, Kyoto Prefectural University, 1-5, Hangi-cho, Shimogamo, Sakyo-ku, Kyoto, 606-8522, Japan,Hokkaido Oshimaseibu Forestry Center, 495-9 Asahi, Matsumae-cho, Matsumae-gun, Hokkaido, 049-1517, Japan;

    Graduate School of Life and Environmental Sciences, Kyoto Prefecturat University, 1-5, Hangi-cho, Shimogamo, Sakyo-ku, Kyoto 606-8522, Japan;

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