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- W2593205435 abstract "Glendonites, pseudomorphs after ikaite (CaCO The results are consistent with observations from the modern, whic h suggest that ikaite is an early diagenetic phase that forms in the zone of suboxic diagenesis in organic matter (OM) rich sediment s. Given ikaite's proclivity for forming in OM-rich sediments, glendonites may be considered useful indicators of paleopr oductivity, paleo-upwelling, and potential hydrocarbon source rocks. In addition, the δ" @default.
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- W2593205435 date "2008-01-01" @default.
- W2593205435 modified "2023-09-27" @default.
- W2593205435 title "Glendonites as Paleoclimatic and Paleoceanographic I ndicators: A Case Study from the Glacially Influenced Permian System of Eastern Australia*" @default.
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