Reference Type | Journal (article/letter/editorial) |
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Title | Evidence for temperate soil development during the Early Devensian in Gower, South Wales |
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Journal | Geological Magazine |
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Authors | Case, D. J. | Author |
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Year | 1993 (January) | Volume | 130 |
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Issue | 1 |
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Publisher | Cambridge University Press (CUP) |
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DOI | doi:10.1017/s0016756800023773Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 255616 | Long-form Identifier | mindat:1:5:255616:5 |
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GUID | 0 |
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Full Reference | Case, D. J. (1993) Evidence for temperate soil development during the Early Devensian in Gower, South Wales. Geological Magazine, 130 (1) 113-115 doi:10.1017/s0016756800023773 |
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Plain Text | Case, D. J. (1993) Evidence for temperate soil development during the Early Devensian in Gower, South Wales. Geological Magazine, 130 (1) 113-115 doi:10.1017/s0016756800023773 |
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In | (1993, January) Geological Magazine Vol. 130 (1) Cambridge University Press (CUP) |
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Abstract/Notes | AbstractInvestigations into the micromorphology of the Pwll Du Red Beds in Gower, South Wales, have revealed pedo-features in the form of compound void coatings. Overlying marine deposits dated to the Ipswichian (Oxygen Isotope Substage 5e), the Red Beds are interpreted as the product of sedimentation and pedogenesis during Early Devensian time. |
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