埼玉県立自然史博物館研究報告 第13号 (1995)

入間市元加治付近の仏子層下部の花粉化石

楡 井   尊
埼玉県立自然史博物館. 369-13 埼玉県秩父郡長瀞町長瀞1417-1

要 旨 入間市野田付近に分布する仏子層A部層の花粉分析をおこない次のような結果を得た.花粉化石群はPicea, Metasequoia-Glyptostrobus,Pseudolarix,Fagus,Quercus (Lepidobalanus)が多い.古植生は,冷温帯南部程度の針葉樹林および広葉樹林で,古気候はやや冷涼と推定でさる. FT地点の古環境は,海水域から淡水域に変化した.関東平野西縁部でもメタセコイア植物群の消滅過程が,大阪層群と同様であることが明らかになった.

キーワード:関東平野西縁,仏子層,花粉化石,鮮新-更新統.




Fossil Pollen Assemblages of Lower Part of Bushi Formatiom, Kazusa Group in Iruma City, Saitama in Central Japan

NIREI, Takashi
Saitama Museum of Natural History, Nagatoro, Chichibu-gun, Saitama 369-13

Abstract
    Pollen analytical studies were conducted on the first member of Bushi Formation in lruma City. The fossil pollen assemblages were characterized by Picea, Metasequoia-Glyptostrobus, Pseudolarix, Fagus and Quercus(Lepidobalanus). Paleovegetation can be presumed to be the coniferous forest and the deciduous broad-leaved forest of the cool temperate zone level. Climatic condition was cooler or slightly cooler than that of the present. Paleoenviroments of upper part of FT site was changed from marine condition into freshwater condition.
   This part of Bushi Formation corresponds to the lower part Metasequoia Zone of the Osaka Group in Kinki region, South-western Japan. It was clarified here that the disappearance process of the Metasequoia Flora was similar to the Osaka Group.


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