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• W2090670637 abstract "Coenocorrelation is the correlation of positions in a stratigraphic sequence with corresponding positions along a paleoenvironmental gradient through gradient analysis of fossil communities. By ordination of community samples, the distribution and abundance of taxa along a depth gradient can be translated into a continuous scale that accurately measures the gradient and thus makes possible analysis of facies change on a continuum. The procedure is tested using data on marine benthic invertebrates along ten time-parallel transects down an Ordovician basin slope (Trenton Group, New York). Reversals between transgression and regression revealed in coenocorrelation curves served nearly as well as bentonite beds in time-correlation of sections. Ordinations gave estimates of depositional strike in close agreement with estimates from physical indicators. Walther's Law of Facies is evidently a more rigorous, quantifiable generalization than it has been revealed to be through classificatory approaches to communities and environments." @default.
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• W2090670637 date "1978-10-01" @default.
• W2090670637 modified "2023-09-23" @default.
• W2090670637 title "Coenocorrelation: gradient analysis of fossil communities and its applications in stratigraphy" @default.
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• W2090670637 doi "https://doi.org/10.1111/j.1502-3931.1978.tb01893.x" @default.
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