Journal Article

Holocene water level changes of Lake Ogawara presumed by diatom analysis, eastern part of Aomori Prefecture, north Japan.

Geographical Review of Japan, Series A (1986) 59(4) 205-212
DOI: 10.4157/grj1984a.59.4_205
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Abstract

On the basis of the result of diatom analysis, 14C date and tephrochronology, water level of Lake Ogawara was 2 m higher than that of present about 4500-5000 y BP, and it had lowered to the same level as present till 3500 y BP. Since then water level has been stable. -from English summary

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APA

Ishizuka, T., & Kashima, K. (1986). Holocene water level changes of Lake Ogawara presumed by diatom analysis, eastern part of Aomori Prefecture, north Japan. Geographical Review of Japan, Series A, 59(4), 205–212. https://doi.org/10.4157/grj1984a.59.4_205

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