Cited by 7Methane Hydrates and Related PhenomenaPaleontology and Stratigraphy of FossilsGeochemistry and Elemental Analysis

Data report: dolomite in Neogene sediments of the Belgica carbonate mound province, Porcupine Seabight, North Atlantic

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Gregg, J.M., Frank, T.D.·2009·Proceedings of the IODP

Abstract

Dolomite was observed, using petrography, X-ray diffraction (XRD), and scanning electron microscopy (SEM), in cored Neogene sediments from the Porcupine Seabight in the north Atlantic Ocean, Integrated Ocean Drilling Program Expedition 307 Sites U1316, U1317, and U1318, ~100 km off the west coast of Ireland.Trace amounts (<10% of total carbonate component) of dolomite were observed in Challenger Mound, a deep coldwater mixed silicaclastic-carbonate mud mound located in the Porcupine Seabight.Significant dolomitization (>50% of total carbonate component) was observed primarily in Miocene strata in submound and off-mound sediments.Petrographic examination of smear slides indicates that dolomite is composed of micrometer-to decimicron-sized, limpid, rhombic crystals.XRD analysis indicates that the dolomite is calcium rich and poorly ordered.SEM confirms light petrographic analysis of size and morphology of dolomite crystals, and electron microprobe analysis indicates that the dolomite is ferroan and displays distinct compositional zoning.Microbes and associated microbial filamentous structures were observed associated with dolomite crystals.Saturation indexes of carbonate minerals calculated for interstitial waters collected from the three sites are consistent with the petrographic and XRD observation of dolomite.

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  1. [9]9. Lees, A., and Miller, J., 1995. Waulsortian banks. In Monty, C.L.V., Bosence, D.W.J., Bridges, P.H., and Pratt, B.R. (Eds.), Carbonate Mud-Mounds: Their Origin and Evolution. Spec. Publ. Int. Assoc. Sedimentol., 23:191-271.
  2. [10]10. Lumsden, D.N., and Chimahusky, J.S., 1980. Relationship between dolomite nonstoichiometry and carbonate facies parameters. In Zenger, D.H., Dunham, J.B., and Ethington, R.L. (Eds.), Concepts and Models of Dolomiti- zation. Spec. Publ.-Soc. Econ. Paleontol. Mineral., 28:123-137.
  3. [12]12. Ntarlagiannis, D., Atekwana, E., Hill, E., and Gorby, Y., 2006. Bacterial nanowires facilitate electron transfer in saturated porous media. Eos, Trans. Am. Geophys. Union, 87(52)(Suppl.):NS21A-05. (Abstract) http:// www.agu.org/meetings/fm06/waisfm06.html Initial receipt: 21 July 2008 Acceptance: 14 April 2009 Publication: 3 July 2009 MS 307-207

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Authors
Gregg, J. M., & Frank, T. D.
Affiliations
  • Oklahoma State University (US)
  • University of Nebraska–Lincoln (US)
Corresponding author
Gregg, J.M.
Venue
Proceedings of the IODP
Published
2009
ISSN
1930-1014 (ISSN-L)
OpenAlex
W2484096918
Cited by
7
References
5
Citations by year
2026: 1 · 2023: 1 · 2022: 1 · 2021: 3 · 2017: 1
FWCI
0.00
Type
book chapter
Language
en
Open access
Locations
Proceedings of the Integrated Ocean Drilling Program. Expedition reports/Proceedings of the Integrated Ocean Drilling Program (publishedVersion)
Funders
  • Consortium for Ocean Leadership
  • Oklahoma State University
  • United States Science Support Program
Topics
  • Physical Sciences › Environmental Science › Environmental Chemistry › Methane Hydrates and Related Phenomena
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
Keywords
dolomite, dolomitization, Neogene sediments, carbonate mounds, Porcupine Seabight, ferroan dolomite, microbial filaments, carbonate saturation state, Miocene strata

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