アクセス数 : 1202 件
ダウンロード数 : 86 件
この文献の参照には次のURLをご利用ください : https://doi.org/10.24568/6365
島根大学地球資源環境学研究報告 Volume 12
published_at 1993-08-30
中海南部における最上部完新統の花粉群
Pollen flora of the uppermost Holocene from southem part of Lake Nakaumi
Onishi Ikuo
Kidera Masahito
Senda Nobuo
full_text_file
c006012007.pdf
( 617 KB )
Descriptions
Pollen flora of the latest Holocene at NU9007 core and Mudlump from southem part of Lake Nakaumi have been studied and correlated to pollen zones and subzones of Lake Shinji（Onishi et al．1990）．
In NU9007 core，Cryptomeria subzone，Cyclobalanopsis-Quercus subzone and Pinus subzone of Gramineae pollen zone are recognized and sedimentation rate is estimated to be 2.0 to 2.3 mm／year．
At Mudlump，Podocarpus subzone of Cyclobalanopsis-Castanopsis pollen zone and all subzones of Gramineae pollen zone are recognized and sedimentation rate is estimated to be 1.3 mm／year．
Sedimentation rate of NU8806（Watanabe et a1，1988）is also estimated to be 0.95 mm／year．
Pollen zoning of NB12 （Onishi，1977）has been reexamined and the subzones from
Apananthe-Celtis subzone of Fagus-Tsuga pollen zone to Pinus subzone of Gramineae pollen zone are recognized．Sedimentation rate is estimated to be 0.6 mm／year．
In NU9007 core，Cryptomeria subzone，Cyclobalanopsis-Quercus subzone and Pinus subzone of Gramineae pollen zone are recognized and sedimentation rate is estimated to be 2.0 to 2.3 mm／year．
At Mudlump，Podocarpus subzone of Cyclobalanopsis-Castanopsis pollen zone and all subzones of Gramineae pollen zone are recognized and sedimentation rate is estimated to be 1.3 mm／year．
Sedimentation rate of NU8806（Watanabe et a1，1988）is also estimated to be 0.95 mm／year．
Pollen zoning of NB12 （Onishi，1977）has been reexamined and the subzones from
Apananthe-Celtis subzone of Fagus-Tsuga pollen zone to Pinus subzone of Gramineae pollen zone are recognized．Sedimentation rate is estimated to be 0.6 mm／year．
About This Article
Doi
https://doi.org/10.24568/6365
Pages
Other Article