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Lithostratigraphy and biostratigraphy of the Campanian-Maastrichtian Toyajo Formation in Wakayama, southwestern Japan

机译:日本西南部和歌山的Campanian-Maastrichtian Toyajo组的岩石地层学和生物地层学

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摘要

The Upper Cretaceous Toyajo Formation is distributed around the Mt. Toyajo in the Aridagawa area, Wakayama, southwestern Japan. The formation is subdivided into three newly defined members, the Nakaibara Siltstone Member, Hasegawa Muddy Sandstone Member, and Buyo Sandstone Member, in ascending order. Close field observation elucidated the detailed biostratigraphy of the Toyajo Formation, and high-precision biostratigraphic correlation was made with the Yezo Group in Hokkaido (northern Japan) and Sakhalin and the Izumi Group in southwestern Japan. The Toyajo Formation contains diversified lower Campanian to upper Campanian heteromorph ammonoid assemblages, including Eubostrychoceras and Scaphites. Discovery of the heteromorph fauna demonstrates that scaphitid ammonoids survived until Campanian time in the northwestern Pacific region. Although Eubostrychoceras elongatum has been known in the northeastern Pacific region, the occurrence of this species in the northwestern Pacific region has been uncertain before. The rich occurrence of E elongatum in the Aridagawa area indicates that this species was distributed widely in the northern Pacific realm. The Toyajo Formation is similar to the Izumi Group in various geologic features, and may indicate that the Toyajo Formation was deposited in a strike-slip basin along the Chichibu Belt formed by the movement along the Kurosegawa Tectonic Zone in the latest Cretaceous, like the Izumi Group, along the Median Tectonic Line.
机译:上白垩统统屋组分布在山顶。日本西南部和歌山有田川地区的Toyajo。地层按升序细分为三个新定义的成员,中原砂岩成员,长谷川泥泞砂岩成员和不二砂岩成员。近距离观察证实了丰屋组的详细生物地层学,并与北海道的Yezo组(日本北部)以及萨哈林岛和日本西南部的Izumi组进行了高精度的生物地层学关联。洞爷组形成了从下坎帕尼阶到上坎帕尼阶的异形物氨类组合,包括Eubostrychoceras和Scaphites。异形动物群的发现表明,在西北太平洋地区,鳞片状的类人猿生存到Campanian时间。尽管在东北太平洋地区已经知道Eubostrychoceras elongatum,但是该物种在西北太平洋地区的发生以前还不确定。在有田川地区,E elongatum的大量出现表明该物种在北太平洋地区广泛分布。 ya谷组在各种地质特征上与泉组相似,可能表明the谷组沉积在千叶岩带的走滑盆地中,该盆地是由最近的白垩纪沿黑濑川构造带运动形成的,如泉沿中构造线分组。

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