D
David A. Osleger
Researcher at University of California, Davis
Publications - 27
Citations - 1981
David A. Osleger is an academic researcher from University of California, Davis. The author has contributed to research in topics: Sedimentary depositional environment & Sequence stratigraphy. The author has an hindex of 17, co-authored 27 publications receiving 1830 citations. Previous affiliations of David A. Osleger include University of California & University of California, Riverside.
Papers
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Journal Article
Evolution of the Sr and C Isotope Composition of Cambrian Oceans
TL;DR: In this paper, the authors present a set of high-resolution, seawater Sr and C isotope curves for the late Early through early Late Cambrian, defined in continuous exposures of marine carbonates in the Great Basin and southern Canadian Rockies, and used to better constrain primary variations in ocean chemistry during this time period.
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Relation of eustasy to stacking patterns of meter-scale carbonate cycles, Late Cambrian, U.S.A.
David A. Osleger,J. Fred Read +1 more
TL;DR: In this paper, an interbasinal study of Late Cambrian cyclic carbonate successions in the Appalachian and Cordilleran passive margins suggests that superimposed orders of eustasy controlled the development of large-scale depositional sequences and the component peritidal to subtidal meter-scale cycles that comprise them.
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Sequence Stratigraphy and Onlap History of the Donets Basin, Ukraine: Insight into Carboniferous Icehouse Dynamics
J. M. Eros,Isabel P. Montañez,David A. Osleger,Vladimir I. Davydov,Tamara I. Nemyrovska,Vladislav I. Poletaev,M. V. Zhykalyak +6 more
TL;DR: This paper developed the sequence stratigraphy and onlap-offlap history for a 33my interval of the Carboniferous using the U-Pb calibrated succession of the Donets Basin, Ukraine, in order to assess the relationship between sea-level, high-latitude changes in glacial extent, and climate.
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Toward an orbital chronology for the early Aptian Oceanic Anoxic Event (OAE1a, ~ 120 Ma)
Yongxiang Li,Timothy J. Bralower,Isabel P. Montañez,David A. Osleger,Michael A. Arthur,David M. Bice,Timothy D Herbert,Elisabetta Erba,Isabella Premoli Silva +8 more
TL;DR: The early Aptian Oceanic Anoxic Event (OAE1a, 120 Ma) represents a geologically brief time interval in the mid-Cretaceous greenhouse world that is characterized by increased organic carbon accumulation in marine sediments, sudden biotic changes, and abrupt carbon-isotope excursions indicative of significant perturbations to global carbon cycling.
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Dynamic carboniferous climate change, Arrow Canyon, Nevada
TL;DR: The history of the late Paleozoic ice age is archived within the biostratigraphically well-constrained, carbonate-dominated succession of Arrow Canyon, Nevada, United States as mentioned in this paper.