2008
DOI: 10.4116/jaqua.47.1
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Fluctuations of opal phytolith assemblage in the Tachikawa and Musashino Loam formations in southwest Kanto, central Japan: Changes in vegetation, climate, terrace, and soil-facies since marine isotope stage 5.1

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Cited by 15 publications
(5 citation statements)
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“…Research in soil science has generated a hypothesis concerning land use in the EUP for the Mt. Ashitaka area (Sase et al 2006(Sase et al , 2008Hosono and Sase 2015). Researchers studied buried paleosol layers from the UP sites in the Mt.…”
Section: Implications Of Study Results On Trapezoids From the Doteue ...mentioning
confidence: 99%
“…Research in soil science has generated a hypothesis concerning land use in the EUP for the Mt. Ashitaka area (Sase et al 2006(Sase et al , 2008Hosono and Sase 2015). Researchers studied buried paleosol layers from the UP sites in the Mt.…”
Section: Implications Of Study Results On Trapezoids From the Doteue ...mentioning
confidence: 99%
“…Global climate changes in temperature and precipitation, including snow depth, are expected to cause species turnover among Sasa species (Tsuyama et al, 2011). When the timescale is extended to the Quaternary, it is confirmed that the genus Sasa is replaced by the genus Pleioblastus and vice versa in response to climate change, as revealed by the identification of leaf siliceous bodies (Sase et al, 2008; Sase et al, 2011).…”
Section: Discussionmentioning
confidence: 97%
“…This shift of forest types roughly corresponds with the transition from Period I to Period III. In addition, opal phytolith analysis shows that grassland vegetation was causal in creating the Black Band II (s trata VII-IX: buried paleosol) in the Tachikawa Loam (Sase et al 2008). The expansion of grassland vegetation from Stratum X to Black Band II (strata VII-IX) roughly corresponds with a decrease of adzes.…”
Section: Period IIImentioning
confidence: 93%