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The stratigraphic expression of a large negative carbon isotope excursion from the Ediacaran Johnnie Formation, Death Valley

Bergmann, Kristin D. and Zentmyer, Rebecca A. and Fischer, Woodward W. (2011) The stratigraphic expression of a large negative carbon isotope excursion from the Ediacaran Johnnie Formation, Death Valley. Precambrian Research, 188 (1-4). pp. 45-56. ISSN 0301-9268. https://resolver.caltech.edu/CaltechAUTHORS:20110725-113149209

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Abstract

The Rainstorm Member of the Ediacaran Johnnie Formation of the southern Basin and Range, US, records a large negative excursion in carbon isotope ratios of carbonate strata (δ^(13)C_VPDB > −6‰). The character of the excursion raises fundamental questions about whether this isotopic pattern is accurately capturing the time-series behavior of marine dissolved inorganic carbon (DIC) or is a product of diagenesis. To explore this issue, we examined the expression of this isotopic excursion within the Johnnie oolite, a ~2 m thick marker bed, which records the highest rate of change in δ^(13)C. Sedimentologically, the oolite unit is thought to be time-transgressive; if the isotopic excursion reflects time-series behavior of the carbon cycle, its expression in the oolite across the basin should systematically align the sections according to their slight diachroneity. Detailed carbon and oxygen isotopic stratigraphy of the oolite at seven different locations indicates the magnitude of the excursion at the base of the oolite is spatially variable such that after a palinspastic reconstruction the sections align along a systematic north to south gradient in the isotopic data. The oolite preserved in the Old Dad Mountains, the most southerly section measured, is an outlier to this trend (and the most difficult to ordinate accurately in the reconstruction), showing the largest isotopic range between the onset of carbonate deposition and top of the oolite. Several hypotheses are congruent with these data, but the sum of observations is best explained by a scenario wherein the oolite is time-transgressive and deposited in a north to south manner throughout the onset of the isotopic excursion. If correct, this implies that the stratigraphic δ^(13)C pattern reflects time series behavior of marine DIC.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1016/j.precamres.2011.03.014DOIArticle
http://www.sciencedirect.com/science/article/pii/S0301926811000775PublisherArticle
ORCID:
AuthorORCID
Fischer, Woodward W.0000-0002-8836-3054
Additional Information:© 2011 Elsevier B.V. Received 5 October 2010; revised 25 February 2011; accepted 23 March 2011. Available online 7 April 2011. The authors would like to acknowledge Frank Corsetti and Alex Brasier for providing useful reviews. We thank E. Trower, S. Finnegan, N. Boekelheide and E. Niedermeyer for assistance in the field. We also thank B. Wernicke, J. Grotzinger and M. Osburn for helpful discussions. Support was provided by the National Science Foundation through a Graduate Research Fellowship to K. Bergmann and by the Agouron Institute to W. Fischer for analytical support.
Funders:
Funding AgencyGrant Number
NSF Graduate Research FellowshipUNSPECIFIED
Agouron InstituteUNSPECIFIED
Subject Keywords:Oolite; Neoproterozoic; Carbon cycle; Chemostratigraphy; Diagenesis; Johnnie Formation
Issue or Number:1-4
Record Number:CaltechAUTHORS:20110725-113149209
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20110725-113149209
Official Citation:Kristin D. Bergmann, Rebecca A. Zentmyer, Woodward W. Fischer, The stratigraphic expression of a large negative carbon isotope excursion from the Ediacaran Johnnie Formation, Death Valley, Precambrian Research, Volume 188, Issues 1-4, July 2011, Pages 45-56, ISSN 0301-9268, DOI: 10.1016/j.precamres.2011.03.014.
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:24527
Collection:CaltechAUTHORS
Deposited By: Jason Perez
Deposited On:25 Jul 2011 20:40
Last Modified:03 Oct 2019 02:57

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