埼玉県立自然史博物館研究報告 第16号 (1998)

関東平野西縁,埼玉県玉川村田黒における
後期更新世の花粉および昆虫化石群集

楡井 尊
埼玉県立自然史博物館.〒369-1305埼玉県秩父郡長瀞町長瀞1417-1
林 成多
新潟大学大学院自然科学研究科.〒950-2181新潟県新潟市五十嵐2の町8050

要 旨 関東平野西縁の玉川村田黒の上部更新統,田黒含植物化石層について花粉化石と昆虫化石の検 討を行った.花粉化石群集の変遷から2つの地域花粉帯に区分した.下位のTG-A帯はCryotomeriaPiceaが高率でFagusAcerを伴い,温帯針葉樹の多い針広混交林で,古気候はやや冷涼. TG-B帯はPiceaが高率でLarixを伴い古気候は冷涼である.上位に向かって古気候は寒冷化した.関東および周辺の花粉分析資料と比較すると,酸素同位対比ステージ3ないしは5に相当すると推定された.昆虫化石から推定される田黒含植物化石層の古環境はヨシやスゲなどの生える低湿地であったと推定される.

キーワード:関東平野西縁,花粉分析,昆虫化石,後期更新世, Cryptomeria,酸素同位対比ステージ



Fossil Pollen and Insect Assemblages from Late Pleistocene Peat Deposits
at Taguro, Tamagawa Village, Western Margin of Kanto Plain, Central Japan

NIREI Takashi
Saitama Museum of Natural History. Nagatoro, Chichibu-gun, Saitama 369-l305
and
HAYASHI Masakazu
Graduate School of Science and Technology, Niigata University, Ikarashi 2-8050, Niigata 950-2181

Abstract
  In the Late Pleistocene Taguro peaty bed of the western margin of Kanto Plain, fossil of pollen, macroplants and insects occur in relative abundance. Fossil pollen assemblage was divided into two zones based on pollen analysis. From the lower one to zone TG-A , recognized were the coniferous to deciduous forests of the Cool Temperate Zone containing many of Picea, Cryptomeria, Fagus, Acer; and the climatic condition was slightly cooler than the present. In the Zone TG-B, recognized were the coniferous forests of the Cool Temperate Zone containing many of Picea with Larix; and the climatic condition was cooler than the lower zone. Cryptomeria was decrease in this zone.
  The age of this Pollen zone has been considered to be about the age of 38,000 years ago. The Pollen assemblage of the Taguro peaty bed is correlative to the δ18 Stage 3 or 5.
  The insect assemblage of the bed includes aquatic beetles mainly, such as Elaphrus japonicus, Agabus conspicuus, Donacia hiurai, Plateumaris sericea, and P. constricticollis. This assemblage indicates the paleoenvironment of the bed that there were mainly marsh of reeds and sedges accompanied with areas of still water.


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