@article{oai:kanazawa-u.repo.nii.ac.jp:00046663,
 author = {藤, 則雄 and Fuji, Norio},
 issue = {9},
 journal = {Proceedings of the Japan Academy Series B: Physical and Biological Sciences},
 month = {},
 note = {The present writer reported on the outline of the palaeoenvironmental, especially palaeovegetational and palaeoclimatic, changes around Lake Biwa during the last 600,000 years on the basis of the palynological analysis of samples taken at intervals of 5 m on a 200-meter core (Fuji and Hone, 1972; Fuji and Hone, 1977) drilled in 1971 at the bottom of 65 m below the
present lake water level of Lake Biwa. In addition, the writer stated on the detailed palaeovegetation and palaeoclimate during the present -100 ,000 years B.P. on the basis of the palynological analysis of samples taken at intervals of 25 cm over the upper 55 m of the same core (Fuji, 1976a).
 In this article, the writer will debate minutely on the palaeoclimatic change during an age from 100,000-300,000 years B.P, from the view point of a palynology. The samples analysed for this investigation were used about 200 samples which were taken at intervals of about 25 cm throughout the middle part from 55-110 m of the 200-meter core., 金沢大学教育学部理科教育},
 pages = {275--278},
 title = {Palynological Study of a 200-meter Core Sample from Lake Biwa, Central Japan. II Palaeoclimate during the 100,000-300,000 Years BJP},
 volume = {58},
 year = {1982}
}