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Biological influences on seafloor carbonate precipitation

Bergmann, Kristin D. and Grotzinger, John P. and Fischer, Woodward W. (2013) Biological influences on seafloor carbonate precipitation. Palaios, 28 (2). pp. 99-115. ISSN 0883-1351. doi:10.2110/palo.2012.p12-088r. https://resolver.caltech.edu/CaltechAUTHORS:20130509-105315509

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Abstract

The sedimentary record reveals first-order changes in the locus of carbonate precipitation through time, documented in the decreasing abundance of carbonate precipitation on the seafloor. This pattern is most clearly recorded by the occurrence of seafloor carbonate crystal fans (bladed aragonite pseudomorphs neomorphosed to calcite or dolomite), which have a distinct temporal distribution, ubiquitous in Archean carbonate platforms, but declining through Proterozoic time and extremely rare in Phanerozoic basins. To understand better the potential influences on this pattern, we built a mathematical framework detailing the effects of organic matter delivery and microbial respiratory metabolisms on the carbonate chemistry of shallow sediments. Two nonunique end-member solutions emerge in which seafloor precipitation is favorable: enhanced anaerobic respiration of organic matter, and low organic matter delivery to the sediment-water interface. This analysis suggests that not all crystal fans reflect a unique set of circumstances; rather there may have been several different geobiological and sedimentary mechanisms that led to their deposition. We then applied this logical framework to better understand the petrogenesis of two distinct crystal fan occurrences—the Paleoproterozoic Beechey Formation, Northwest Territories, Canada, and the middle Ediacaran Rainstorm Member of the Johnnie Formation, Basin and Range, United States—using a combination of high-resolution petrography, micro X-ray fluorescence and wavelength dispersive spectroscopy, C isotopes, and sedimentary context to provide information on geobiological processes occurring at the sediment-water interface. Interestingly, both of these Proterozoic examples are associated with iron-rich secondary mineral assemblages, have elevated trace metal signatures, and sit within maximum flooding intervals, highlighting key commonalities in synsedimentary geobiological processes that led to seafloor carbonate precipitation.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.2110/palo.2012.p12-088rDOIArticle
http://palaios.sepmonline.org/content/28/2/99PublisherArticle
ORCID:
AuthorORCID
Grotzinger, John P.0000-0001-9324-1257
Fischer, Woodward W.0000-0002-8836-3054
Additional Information:© 2013 SEPM. Published Online: February 2013. We thank Jena Johnson, Sara Pruss, and an anonymous reviewer for insightful comments. Most analytical work was completed using facilities available in the Division of Geological and Planetary Sciences (GPS) at California Institute of Technology with assistance from Chi Ma, George Rossman, and Andrew Matzen. µXRF analysis was completed at the Jet Propulsion Laboratory with assistance from Mark Anderson. Support from a Henshaw Fellowship (GPS) and a National Science Foundation Graduate Research Fellowship was provided to K. Bergmann. W. Fischer acknowledges support from the Agouron Institute and a David and Lucile Packard Fellowship for Science and Engineering.
Funders:
Funding AgencyGrant Number
Henshaw FellowshipUNSPECIFIED
NSF Graduate Research FellowshipUNSPECIFIED
Agouron InstituteUNSPECIFIED
David and Lucile Packard FoundationUNSPECIFIED
Issue or Number:2
DOI:10.2110/palo.2012.p12-088r
Record Number:CaltechAUTHORS:20130509-105315509
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20130509-105315509
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:38387
Collection:CaltechAUTHORS
Deposited By: Jason Perez
Deposited On:09 May 2013 18:13
Last Modified:09 Nov 2021 23:37

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