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Study on Analysis of the Fossil Pollen from the Izumiyatsu Formation Northern Part of Boso Peninsula, Chiba Prefecture

机译:千叶县房总半岛北部泉支组化石花粉的分析研究

摘要

The Izumiyatsu Formation which is between the Kongoji Formation and the Jizodo Formation in the Shimousa Group chiefly consists of mud and it is a few meters in thickness. It spreads from the type locality of the Izumiyatsu (Kisarazu City) toward the Northeast and is distributed to Kanazawa (Ichihara City), Ooshii (Chiba City), Tannoo (Togane City), Yabe (Sanbu-Gun) and to Henda (Matsuo Town). We can find a sheet to five sheets of the peat in the formation. Among these fossil pollen gathered in the area, Alnus is most abundant. And every sample involves Tsuga. These facts indicate the possibility of relatively cool clmate and moist ground condition.
机译:Shimousa组中的Kongoji组和Jizodo组之间的Izumiyatsu组主要由泥浆组成,厚度为几米。它从泉轻(木更津市)的类型地区向东北传播,并分布到金泽(市原市),大石市(千叶市),天王野(To金市),矢部(三部郡)和Henda(松尾镇) )。我们可以在地层中找到一片到五片泥炭。在该地区聚集的这些化石花粉中,阿尔努斯最为丰富。每个样本都涉及Tsuga。这些事实表明相对凉爽的气候和潮湿的地面条件的可能性。

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