Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Geology Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Geology; May 1998; v. 26; no. 5; p. 403-406; DOI: 10.1130/0091-7613(1998)026<0403:UPDOPC>2.3.CO;2
© 1998 Geological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Rasbury, E. T.
Right arrow Articles by Saller, A. H.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

U-Pb dates of paleosols: Constraints on late Paleozoic cycle durations and boundary ages

E. T. Rasbury1, G. N. Hanson1, W. J. Meyers1, W. E. Holt1, R. H. Goldstein2 and A. H. Saller3

1 Department of Geosciences, State University of New York at Stony Brook, Stony Brook, New York 11794-2100
2 Department of Geology, University of Kansas, Lawrence, Kansas 66045
3 Unocal Corporation, Sugar Land, Texas 77210-4551

U-Pb ages of paleosol samples from cyclothemic sections in the Sacramento Mountains of New Mexico and the Permian basin of West Texas bracket the Pennsylvanian-Permian and Carboniferous-Permian boundaries. Linear interpolation and extrapolation to boundaries are accomplished by using cyclothems as periodic subdivisions. The Carboniferous-Permian boundary is 301 ± 2 Ma (2 {sigma}), the Pennsylvanian-Permian boundary is 302 ± 2.4 (2 {sigma}), and the Missourian-Virgilian boundary is 307 ± 3 Ma (2 {sigma}). These ages are within the uncertainties of recent estimates for the boundaries but are significantly more precise. The average cycle duration for this Upper Pennsylvanian and Lower Permian interval is 143 ± 64 ka (2 {sigma}), within the uncertainty of the ~100 k.y. cycle that dominated Pleistocene sea-level history. This new estimate, which is much shorter than those published previously, suggests that the Pennsylvanian and Early Permian cyclothems may have been driven in a manner similar to that which caused glacio-eustatic cycles of the Pleistocene.




This article has been cited by other articles:


Home page
Geological Society of America BulletinHome page
G. J. Retallack
Greenhouse crises of the past 300 million years
Geological Society of America Bulletin, September 1, 2009; 121(9-10): 1441 - 1455.
[Abstract] [Full Text] [PDF]


Home page
Journal of Sedimentary ResearchHome page
S. Leleu, A. J. Hartley, and B. P.J. Williams
Large-Scale Alluvial Architecture and Correlation in a Triassic Pebbly Braided River System, Lower Wolfville Formation (Fundy Basin, Nova Scotia, Canada)
Journal of Sedimentary Research, May 1, 2009; 79(5): 265 - 286.
[Abstract] [Full Text] [PDF]


Home page
Geological Society of America Special PapersHome page
E. T. Rasbury, E. H. Gierlowski-Kordesch, J. M. Cole, C. Sookdeo, G. Spataro, and J. Nienstedt
Calcite cement stratigraphy of a nonpedogenic calcrete in the Triassic New Haven Arkose (Newark Supergroup)
Geological Society of America Special Papers, January 1, 2006; 416(0): 203 - 221.
[Abstract] [Full Text] [PDF]


Home page
Journal of Sedimentary ResearchHome page
H. R. Feldman, E. K. Franseen, R.M. Joeckel, and P. H. Heckel
Impact of Longer-Term Modest Climate Shifts on Architecture of High-Frequency Sequences (Cyclothems), Pennsylvanian of Midcontinent U.S.A.
Journal of Sedimentary Research, May 1, 2005; 75(3): 350 - 368.
[Abstract] [Full Text] [PDF]


Home page
Geological Society of America BulletinHome page
J. M. Cole, E. T. Rasbury, G. N. Hanson, I. P. Montanez, and V. A. Pedone
Using U-Pb ages of Miocene tufa for correlation in a terrestrial succession, Barstow Formation, California
Geological Society of America Bulletin, March 1, 2005; 117(3-4): 276 - 287.
[Abstract] [Full Text] [PDF]


Home page
Journal of PaleontologyHome page
A LATE PERMIAN CHINESE GASTROPOD SPECIES, POSSIBLY LARVAL, IN THE MIDDLE PENNSYLVANIAN OF NEW MEXICO
Journal of Paleontology, February 1, 2004; 78(2): 420 - 423.



Home page
PALAIOSHome page
It's All About Dating: From Nexters to Climate Change
Palaios, October 1, 2003; 18(4-5): 299 - 300.



Home page
Journal of Sedimentary ResearchHome page
From Cyclothems to Sequences: The Record of Eustasy and Climate on an Icehouse Epeiric Platform (Pennsylvanian-Permian, North American Midcontinent)
Journal of Sedimentary Research, January 1, 2003; 73(1): 15 - 30.



Home page
PaleobiologyHome page
Evaluating taxonomic turnover: Pennsylvanian-Permian brachiopods and bivalves of the North American Midcontinent
Paleobiology, December 1, 2001; 27(4): 646 - 668.



Home page
Journal of Sedimentary ResearchHome page
Hypersaline Burial Diagenesis Delineated by Component Isotopic Analysis, Late Paleozoic Limestones, West Texas
Journal of Sedimentary Research, May 1, 2001; 71(3): 372 - 379.



Home page
Proc. Natl. Acad. Sci. USAHome page
D. H. Rothman
From the Cover: Global biodiversity and the ancient carbon cycle
PNAS, April 10, 2001; 98(8): 4305 - 4310.
[Abstract] [Full Text] [PDF]


Home page
GeologyHome page
M. L. Becker, J. M. Cole, E. T. Rasbury, V. A. Pedone, I. P. Montanez, and G. N. Hanson
Cyclic variations of uranium concentrations and oxygen isotopes in tufa from the middle Miocene Barstow Formation, Mojave Desert, California
Geology, February 1, 2001; 29(2): 139 - 142.
[Abstract] [Full Text] [PDF]


Home page
Journal of Sedimentary ResearchHome page
Relationship of Uranium to Petrography of Caliche Paleosols with Application to Precisely Dating the Time of Sedimentation
Journal of Sedimentary Research, May 1, 2000; 70(3): 604 - 618.



Home page
Journal of Sedimentary ResearchHome page
Diagenesis of the Lower Permian Krider Member, Southwest Kansas, U.S.A.: Fluid-Inclusion, U-Pb, and Fission-Track Evidence for Reflux Dolomitization During Latest Permian Time
Journal of Sedimentary Research, May 1, 2000; 70(3): 762 - 773.





JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Geological Society of America