TY - JOUR
T1 - Rhythmic bedding in Mesozoic- Cenozoic pelagic carbonate sequences
T2 - the primary and diagenetic origin of Milankovitch-like cycles.
AU - Arthur, M. A.
AU - Dean, W. E.
AU - Bottjer, D.
AU - Scholle, P. A.
PY - 1984/1/1
Y1 - 1984/1/1
N2 - Rhythmicity is a pronounced characteristic of nearly all Cretaceous and Cenozoic pelagic carbonate sequences whether deposited in shallow or deep-water environments. Proposes that periodic changes in insolation, evaporation, wind stress, and/or rainfall in a wide variety of environments caused changes in input of terrigenous detritus, water mass stratification, surface productivity, deepwater oxygen content, and rates of carbonate dissolution. A number of lines of evidence, including stable isotope and geochemical profiles across individual cycles support these inferences. -from Authors
AB - Rhythmicity is a pronounced characteristic of nearly all Cretaceous and Cenozoic pelagic carbonate sequences whether deposited in shallow or deep-water environments. Proposes that periodic changes in insolation, evaporation, wind stress, and/or rainfall in a wide variety of environments caused changes in input of terrigenous detritus, water mass stratification, surface productivity, deepwater oxygen content, and rates of carbonate dissolution. A number of lines of evidence, including stable isotope and geochemical profiles across individual cycles support these inferences. -from Authors
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M3 - Article
AN - SCOPUS:0021627038
SP - 191
EP - 222
JO - [No source information available]
JF - [No source information available]
SN - 0042-1215
ER -