| Reference Type | Journal (article/letter/editorial) |
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| Title | Aliphatic carboxylic acids in buried Ah horizons in Alberta, Canada as paleoenvironmental indicators |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Dormaar, J. F. | Author |
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| Year | 1983 (May 1) | Volume | 20 |
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| Issue | 5 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e83-075Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 477907 | Long-form Identifier | mindat:1:5:477907:4 |
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| GUID | 0 |
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| Full Reference | Dormaar, J. F. (1983) Aliphatic carboxylic acids in buried Ah horizons in Alberta, Canada as paleoenvironmental indicators. Canadian Journal of Earth Sciences, 20 (5) 859-866 doi:10.1139/e83-075 |
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| Plain Text | Dormaar, J. F. (1983) Aliphatic carboxylic acids in buried Ah horizons in Alberta, Canada as paleoenvironmental indicators. Canadian Journal of Earth Sciences, 20 (5) 859-866 doi:10.1139/e83-075 |
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| In | (1983, May) Canadian Journal of Earth Sciences Vol. 20 (5) Canadian Science Publishing |
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| Abstract/Notes | In southern Alberta, a buried Ah horizon is frequently present beneath Mazama tephra (ca. 6600 years BP). Drainage conditions during the formation of such buried Ah horizons may determine the quality of the aliphatic carboxylic acids in the soil organic matter. The spectrum of aliphatic acids extracted from a number of buried Ah horizons indeed suggests either well drained or poorly drained conditions during soil formation regardless of the mode of deposition of materials before or after the soil-forming interval. The climate required for development of the well drained paleosols was inferred to be similar to the climate under which surficial Black Chernozemic Ah horizons were formed. |
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