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Original article

14C ages and δ13C of sclerotium grains found in forest soils

, , , , , , , & show all
Pages 125-131 | Received 26 Feb 2006, Accepted 11 Dec 2006, Published online: 17 Dec 2010

Figures & data

Figure 1  Sclerotium grains collected from Myoko Asadaira soil.

Figure 1  Sclerotium grains collected from Myoko Asadaira soil.

Figure 2  Profile of Myoko Asadaira soil. KG-b, Koyaike ash-b; KG-c, Koyaike ash-c.

Figure 2  Profile of Myoko Asadaira soil. KG-b, Koyaike ash-b; KG-c, Koyaike ash-c.

Table 1 14C ages determined using accelerator mass spectrometry

Figure 3  Distribution of 14C ages of sclerotium in the profile of Myoko Asadaira soil. KG-b, Koyaike ash-b; KG-c, Koyaike ash-c.

Figure 3  Distribution of 14C ages of sclerotium in the profile of Myoko Asadaira soil. KG-b, Koyaike ash-b; KG-c, Koyaike ash-c.

Figure 4  The relationship between 14C age and grain size obtained for the Myoko Asadaira profile.

Figure 4  The relationship between 14C age and grain size obtained for the Myoko Asadaira profile.

Figure 5  The relationship between 14C ages of sclerotium grains and carbon content (%) measured using a CO2 pressure gauge in the process of graphite preparation.

Figure 5  The relationship between 14C ages of sclerotium grains and carbon content (%) measured using a CO2 pressure gauge in the process of graphite preparation.

Figure 6  (a) δ13C and (b) carbon content for Myoko Asadaira sclerotium grains measured using an isotopic ratio mass spectrometer.

Figure 6  (a) δ13C and (b) carbon content for Myoko Asadaira sclerotium grains measured using an isotopic ratio mass spectrometer.

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