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Carl N. Drummond
Researcher at Indiana University – Purdue University Fort Wayne
Publications - 44
Citations - 951
Carl N. Drummond is an academic researcher from Indiana University – Purdue University Fort Wayne. The author has contributed to research in topics: Carbonate & Sedimentary depositional environment. The author has an hindex of 17, co-authored 42 publications receiving 908 citations. Previous affiliations of Carl N. Drummond include University of Michigan & Indiana University – Purdue University Indianapolis.
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Climatic forcing of carbon-oxygen isotopic covariance in temperate-region marl lakes
TL;DR: Isotopic covariance observed in the Michigan marl lake cores is interpreted to reflect postglacial warming from 10 to 3 ka followed by cooler mean annual temperature, a shift toward greater proportions of seasonal summer precipitation, a shortening of the winter season, or some combination of these three factors.
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Poisson processes of carbonate accumulation on Paleozoic and Holocene platforms
TL;DR: In this paper, the authors show that the horizontal extent of individual facies units (lithotopes) are described by a frequency distribution in agreement with that anticipated for a population of equidimensional facies elements whose diameter distribution follows an exponential frequency distribution.
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Stratal Order in Peritidal Carbonate Sequences
TL;DR: In this article, the authors examined several long sections of peritidal carbonate both with respect to the presence or absence of Markovian lithologic transitions and with the "upward-shallowing" character of lithofacies associations.
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Stratal Thickness Frequencies and the Prevalence of Orderedness in Stratigraphic Sequences
TL;DR: The existence of discernable hierarchies in the thickness and/or temporal recurrence of stratal units within sedimentary sequences has become an increasingly important axiom of sequence and cyclostratigraphic studies, and multiple orders of stratigraphic cyclicity are now commonly associated with inferred durations and magnitudes of rhythmic variation in global sea level as mentioned in this paper.
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Carbonate Cycle Stacking Patterns and Hierarchies of Orbitally Forced Eustatic Sealevel Change
TL;DR: In this article, the authors consider the assumption that each individual cycle represents a single sealevel rise and show that multiple upward-shallowing cycles may originate during any single rise in sea-ice.