2015
DOI: 10.1016/j.coal.2014.12.009
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Paleoclimate reconstruction from petrography and biomarker geochemistry from Permian humic coals in Sydney Coal Basin (Australia)

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Cited by 31 publications
(16 citation statements)
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“…Obtained CPI value > 1, which is 7.82 (Table 2) in this study, indicates the sample of immature coal n-alkane has not experienced thermal degradation. This result is also supported by several previous studies which gave CPI values > 1 as an indicator of immature coal [21][22][23][24] and confirmed the terrestrial origin of the organic matter [36].…”
Section: N-alkane Biomarkerssupporting
confidence: 89%
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“…Obtained CPI value > 1, which is 7.82 (Table 2) in this study, indicates the sample of immature coal n-alkane has not experienced thermal degradation. This result is also supported by several previous studies which gave CPI values > 1 as an indicator of immature coal [21][22][23][24] and confirmed the terrestrial origin of the organic matter [36].…”
Section: N-alkane Biomarkerssupporting
confidence: 89%
“…In this study, the presence of pristane and phytane compounds in Wondama coal are shown by the Pr/Ph ratio > 3, which is 3.74 as seen in Table 2. The high Pr/Ph ratio values of the samples used indicate that terrigenous organic matter was deposited under relatively oxic conditions [19][20][21][22][23][24]41]. This result is also supported by the Hunt diagram (Pr/n-C17 ratio versus Ph/n-C18) as seen in Figure 4 which shows that the Wondama coal organic compound is produced by terrestrial higher plants which undergo deposition in an oxic environment.…”
Section: Acyclic Isoprenoid Biomarkerssupporting
confidence: 56%
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