@article{oai:rekihaku.repo.nii.ac.jp:00000344,
 author = {辻, 誠一郎 and Tsuji, Sei-ichiro},
 journal = {国立歴史民俗博物館研究報告, Bulletin of the National Museum of Japanese History},
 month = {Mar},
 note = {application/pdf, Pollen assemblages from the Late Pleistocene Nishiyagi Formation at the excavation site studied to confirm and reveal the evidence of paleolithic man and the paleoenvironment are described. Both beds, namely the V and the IV at this site, yields abundant pollen fossils. The lower part of the V bed contains arboreal pollen with high frequencies (59%), and is characterized by a dominance of Alnus and concomitant Quercus subgen. Lepidobalanus pollen. On the contrary, in the upper part of the V bed and the IV bed, the frequencies of arboreal pollen are generally low (24 to 36%), and Quercus subgen. Lepidobalanus, Pinus, Carpinus-Ostrya, Ulmus-Zelkova-Hemiptelea and Lagerstroemia are the major arboreal pollen. The former differs from the latter in containing no pollen of the warm-temperate element such as Lagerstroemia, Sapium and Melia, and the temperate conifer including Abies and Tsuga. The pollen assemblages of both beds are very similar to those of the lower part of the Ma12 bed, namely D1 subzone based on the pollen stratigraphy, deposited under the Uemachi transgression in the Osaka district.},
 pages = {135--142},
 title = {10. 西八木層の花粉化石群集（前篇　発掘調査の成果 / 第Ⅱ部　古環境の復元）},
 volume = {13},
 year = {1987},
 yomi = {ツジ, セイイチロウ}
}