Stratigraphy of the Lower Cretaceous Tetori Group and stratigraphic implication of plant assemblages in the border area between Ishikawa and Fukui Prefectures, central Japan

Y. Sakai, Shinji Sekido, A. Matsuoka
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引用次数: 6

Abstract

The stratigraphy of the Tetori Group in the Shiramine area of Ishikawa Prefecture and the Takinamigawa area of Fukui Prefecture has been reexamined, and the plant-bearing horizons stratigraphically compared. The Tetori Group in the study areas is divided into the Gomijima, Kuwajima, Akaiwa, and Kitadani Formations, in ascending stratigraphic order. Plant assemblages from the Akaiwa Formation around Mt. Oarashiyama in the Shiramine area comrise 23 species of 18 genera typified by the abundant occurrence of Tetoritype floral elements including ferns, ginkgoaleans, and conifers. The floral elements are associated with minor Zamites-like macrophyllous bennettitalean (or cycadalean) and microphyllous coniferous foliage represented by Brachyphyllum, indicating a climate with a dry season(s). Previously the occurrence of the Ryoseki-type floral elements was presumed to be consistent with floral change and a warming and drying climate during the deposition of the Kitadani Formation. However, this study suggests that such a trend started from the deposition of the Akaiwa Formation, earlier than previously thought.
日本中部石川和福井交界地区下白垩统鸟居群地层学及植物组合的地层意义
重新研究了石川县Shiramine地区和福井县Takinamigawa地区的Tetori群地层,并对植物层位进行了地层比较。研究区鸟鸟群按地层顺序由高到高分为高岛组、古岛组、赤洼组和北谷组。Shiramine地区原山地区的赤海组植物组合包括18属23种,以蕨类、银杏、针叶树等植物类型丰富为代表。植物成分与小的扎米特类大叶类贝尼特(或苏铁)和以短叶科为代表的小叶类针叶有关,表明气候为旱季。在此之前,ryoseki型花元素的出现被认为与北达谷组沉积时期的植物变化和气候变暖干燥相一致。然而,这项研究表明,这种趋势始于赤洼组的沉积,比以前认为的要早。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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