Latitudinal gradient of C4 grass contribution to Black Soil organic carbon and correlation between δ13C and the melanic index in Japanese forest stands
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Balesdent J, Girardin C, Mariotti A (1993) Site-related δ13C of tree leaves and soil organic matter in a temperate forest. Ecology 74(6):1713–1721. doi: 10.2307/1939930
Edwards EJ, Smith SA (2010) Phylogenetic analyses reveal the shady history of C4 grasses. Proc Natl Acad Sci USA 107(6):2532–2537. doi: 10.1073/pnas.0909672107
Edwards EJ, Osborne CP, Stromberg CAE, Smith SA, Consortium CG (2010) The origins of C4 grasslands: integrating evolutionary and ecosystem science. Science 328(5978):587–591. doi: 10.1126/science.1177216
Ehleringer JR, Cerling TE, Helliker BR (1997) C4 photosynthesis, atmospheric CO2 and climate. Oecologia 112(3):285–299. doi: 10.1007/s004420050311
Epstein HE, Lauenroth WK, Burke IC, Coffin DP (1997) Productivity patterns of C3 and C4 functional types in the US Great Plains. Ecology 78(3):722–731. doi: 10.2307/2266052
Forest Soil Division (1976) Classification of forest soils in Japan. Bull Gov For Exp Stn 280:1–28
Gerhart LM, Ward JK (2010) Plant responses to low CO2 of the past. New Phytol 188(3):674–695. doi: 10.1111/j.1469-8137.2010.03441.x
Hattersley PW (1983) The distribution of C3 and C4 grasses in Australia in relation to climate. Oecologia 57(1/2):113–128. doi: 10.2307/4216935
Higashi T, Baba H (1995) Plant opal and the nature of humus in volcanic ash soils, Java Island, Indonesia. Pedologist 39:58–66
Higashi T, Suzuki W (1996) Studies on the phytolith from some volcanic ash soils distributed in Luzon Island, the Philippines. Pedologist 40:11–25
Hiradate S, Nakadai T, Shindo H, Yoneyama T (2004) Carbon source of humic substances in some Japanese volcanic ash soils determined by carbon stable isotopic ratio, delta C-13. Geoderma 119(1–2):133–141. doi: 10.1016/s0016-7061(03)00257-x
Hiradate S, Hirai H, Hashimoto H (2006) Characterization of allophanic Andisols by solid-state C-13, Al-27, and Si-29 NMR and by C stable isotopic ratio, delta C-13. Geoderma 136(3–4):696–707. doi: 10.1016/j.geoderma.2006.05.007
Honma H, Marumoto T, Nishiyama M, Shindo H (1998) Changes in elementary composition and humus composition in the burning process of Susuki (Miscanthus sinensis A.) plants at various temperatures. Jpn J Soil Sci Plant Nutr 69:429–434
Honna T, Yamamoto S, Matsui K (1988) A simple procedure to determine melanic index that is useful for differentiating melanic from Fulvic Andisols. Pedologist 32(1):69–78
Huang Y, Street-Perrott FA, Metcalfe SE, Brenner M, Moreland M, Freeman KH (2001) Climate change as the dominant control on glacial-interglacial variations in C3 and C4 plant abundance. Science 293(5535):1647–1651. doi: 10.1126/science.1060143
Iimura Y, Fujimoto M, Hirota M, Tamura K, Higashi T, Yonebayashi K, Fujitake N (2010) Effects of ecological succession on surface mineral horizons in Japanese volcanic ash soil. Geoderma 159(1–2):122–130. doi: 10.1016/j.geoderma.2010.07.003
Inoue Y, Yoneyama T, Sugiyama S, Okada H, Nagatomo Y (2001) Variations in natural abundance of stable carbon and nitrogen isotopes in a cumulative Andisol in Miyakonojo Basin, Southern Kyushu, with reference to vegetation changes from phytolith. Quat Res 40:307–318
Inoue Y, Nagaoka S, Sugiyama S (2006) The genesis of humic soil with interlayered Aira—an tephra in the southeast part of Shimabara Peninsula, Japan. Quat Res 45:303–311
Ishizuka S, Kawamuro K, Minami H (1999) Contribution of past C4 plants estimated from. δ13C values of soil organic matter to the black soil genesis in Hakkoda Mountain, Northeast Japan. Quat Res 38(2):85–92
Kawamuro K, Torii A (1986a) Difference in past vegetation between Black Soils and Brown Forest Soils derived from volcanic ash at Mt. Kurohime, Nagano Pref. Japan. Quat Res 25:81–98
Kawamuro K, Torii A (1986b) Past vegetation on volcanic ash forest soil I—pollen analysis of the black soils, brown forest soils and podozolic soil in Hakkoda Mountain. Bull For For Prod Res Inst 337:69–89
Kubotera H, Yamada I (1995) Characteristics of induration of tephra-derived soils in Kyushu (1) Morphological, physical, chemical and mineralogical properties of “Nigatsuchi” in the western foot area of Aso Volcano in Kumamoto prefecture. Pedologist 39:84–98
Kudo T, Sasaki H (2007) High-precision chronology of eruptive products during the post-caldera stage of Towada volcano, northeast Japan. J Geogr 116:653–663
Kumada K (1965) Studies on the colour of humic acids—part 1 on the concepts of humic substances and humification. Soil Sci Plant Nutr 11(4):11–16
Machida H, Arai F, Moriwaki H (1981) Tephra across the Japanese sea. Kagaku 51:562–569 The title is translated from the original Japanese
Mo W, Nishimura N, Soga Y, Yamada K, Yoneyama T (2004) Distribution of C3 and C4 plants and changes in plant and soil carbon isotope ratios with altitude in the Kirigamine Grassland, Japan. Grassland Sci 50:243–254
Nadelhoffer KJ, Fry B (1988) Controls on natural nitrogen-15 and carbon-13 abundances in forest soil organic matter. Soil Sci Soc Am J 52(6):1633–1640. doi: 10.2136/sssaj1988.03615995005200060024x
Ogura J (2006) The transition of grassland area in Japan. J Kyoto Seika Univ 30:160–172
Otsuka H, Kimiwada K, Uehara Y (1994) Genesis of humic acid derived from each plant residue of Susuki (Miscanthus sinensis), Sasa (Sasa nipponica), or Kashiwa (Quercus dentata) in fresh volcanic ash. Jpn J Soil Sci Plant Nutr 65:629–636
Sakaguchi Y (1987) Culture on the Black Soils. Kagaku 57:352–361
Sase T (1986) Plant opal analysis of Andisols in North Island, New Zealand. Pedologist 30:2–12
Sase T, Katoh Y, Makino S (1985) Plant opal analysis of volcanic ash soils at the foots of Mt Fuji and Mt. Amagi. Pedologist 29:44–59
Shindo H, Yoshida M, Yamamoto A, Honma H, Hiradate S (2005) δ13C values of organic constituents and possible source of humic substances in Japanese volcanic ash soils. Soil Sci 170(3):175–182
Soil Survey Staff (1999) Soil taxonomy. a basic system of soil classification for making and interpreting soil surveys, agriculture handbook, 2nd edn. vol 436. US Government Printing Office, Washington. http://www.nrcs.usda.gov/Internet/FSE_DOCUMENTS/nrcs142p2_051232.pdf
Tieszen LL, Reed BC, Bliss NB, Wylie BK, DeJong DD (1997) NDVI, C-3 and C-4 production, and distributions in great plains grassland land cover classes. Ecol Appl 7(1):59–78. doi: 10.1890/1051-07611997007
Wada K (1986) Ando Soils in Japan. Kyushu Univ Press, Fukuoka
Watanabe A, Takada H (2006) Structural stability and natural 13C abundance of humic acids in buried volcanic ash soils. Soil Sci Plant Nutr 52(2):145–152. doi: 10.1111/j.1747-0765.2006.00029.x
Wittmer MHOM, Auerswald K, Bai Y, Schäufele R, Schnyder H (2010) Changes in the abundance of C3/C4 species of Inner Mongolia grassland: evidence from isotopic composition of soil and vegetation. Glob Change Biol 16(2):605–616. doi: 10.1111/j.1365-2486.2009.02033.x
Yoneyama T (1996) Clarify the vegetation change using δ13C values of organic carbon. Radioisotopes 45:659–660 The title is translated from the original Japanese
Yoneyama T, Yoshida M (2000) δ13C and δ15N values of tephra profiles at three sites in Southern Kyushu, Japan. Jpn J Soil Sci Plant Nutr 71(6):834–838