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Dynamics of a transgressive prodeltaic system: implications for geography and climate within a Pennsylvanian intracratonic basin, Colorado, USA

Myrow, P. M. and Lukens, C. and Lamb, M. P. and Houck, K. and Strauss, J. (2008) Dynamics of a transgressive prodeltaic system: implications for geography and climate within a Pennsylvanian intracratonic basin, Colorado, USA. Journal of Sedimentary Research, 78 (8). pp. 512-528. ISSN 1527-1404. http://resolver.caltech.edu/CaltechAUTHORS:MYRjsr08

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Abstract

Detailed sedimentological analysis of a prodeltaic turbidite unit within the Pennsylvanian Minturn Formation provides insight into the nature of fan-delta deposition, and allows reconstruction of paleogeographic and paleoclimatic conditions within a tectonically active cratonic basin. The formation, a thick succession of fan-delta deposits, exhibits a complex stratigraphic architecture of alluvial, fluvial, and deltaic fithofacies that were deposited in the Central Colorado Basin (CCB), U.S.A., a fault-bounded depression within the Ancestral Rockies. An ~ 20 to 35-m-thick, regionally extensive, unconformity-bounded prodelta unit was deposited during a large eustatic sea-level rise that temporarily interrupted coarsegrained fluvial-deltaic deposition. The unit consists of dark-green shale and sandstone event beds with tool marks produced by abundant plant debris. The sandstone event beds were previously interpreted as turbidites because they contain current ripples, parallel lamination, and sole marks consistent with deposition from turbidity currents in the absence of storm-generated surface gravity waves. We have found, however, that proximal prodeltaic deposits contain evidence for combined oscillatory and unidirectional flow (i.e., asymmetric hummocky cross stratification (HCS), quasi-planar lamination, and combined-flow ripple stratification), indicating deposition under large waves in relatively shallow water. Paleohydraulic calculations indicate that formation of the HCS beds requires a fetch of at least 75 km to generate the necessary wave periods. Given the position of the CCB in the lee of the ancestral Front Range relative to the prevailing trade winds, and the narrow seaway to the south, storms either tracked across the Cordilleran seaway from the west or formed in situ within the CCB. The former hypothesis is consistent with paleoclimate models that purport the development of summer monsoonal circulation patterns over western equatorial Pangea during the late Paleozoic, and regional observations of southeastward eolian bedform migration directions.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.2110/jsr.2008.061DOIArticle
http://jsedres.sepmonline.org/cgi/content/abstract/78/8/512PublisherArticle
ORCID:
AuthorORCID
Lamb, M. P.0000-0002-5701-0504
Additional Information:© 2008 SEPM Society for Sedimentary Geology. Received 11 September 2007; accepted 24 February 2008. This project was funded by National Science Foundation Grants to Paul Myrow (EAR-0309693) at Colorado College and Jeff Parsons (EAR-0309887), Dept. of Oceanography, University of Washington. M.P. Lamb thanks Jeff Parsons for financial support and advisement during the course of this study. We are grateful to John Southard and David Mohrig for helpful discussions and suggestions. We also thank associate editor Paul McCarthy, as well as Gary Hampson and an anonymous reviewer, for their keen insight and suggestions.
Funders:
Funding AgencyGrant Number
NSFEAR-0309693
NSFEAR-0309887
Subject Keywords:hummocky cross-stratification; western equatorial Pangea; upper Paleozoic loessite; turbidity currents; United-States; clinoform development; bed configurations; minturn formation; oscillatory-flow; Rocky-Mountains
Issue or Number:8
Record Number:CaltechAUTHORS:MYRjsr08
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:MYRjsr08
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:13331
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:21 Apr 2009 16:47
Last Modified:05 Oct 2017 20:44

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