Synsedimentary diagenesis in a Cryogenian reef complex: Ubiquitous marine dolomite precipitation
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A similar direct formation mechanism producing radial growth morphology has been suggested for dolomite cements in Cryogenian reef carbonates.
“A similar 'direct' formation mechanism, which also produces a radial growth morphology, has been suggested for dolomite cements in Cryogenian ( ~ 850 to ~ 650 Mya) reef carbonates (Hood et al. 2011; Hood and Wallace 2012).”
From A route for the direct crystallization of dolomite (2015) · cites this paper as Hood and Wallace 2012
The radial growth morphology of direct dolomite cements in Neoproterozoic cap carbonates may also be a product of spherulitic growth, indicating they may have formed from an amorphous precursor.
“Furthermore, the radial growth morphology of the 'direct' dolomite cements in the Neoproterozoic cap carbonates may also be a product of spherulitic growth indicating that they also may have formed from an amorphous precursor (Hood et al. 2011; Hood and Wallace 2012).”
From A route for the direct crystallization of dolomite (2015) · cites this paper as Hood and Wallace 2012
Environmental conditions that promoted direct precipitation of dolomite in Neoproterozoic seas were characterized by high alkalinities, elevated Mg:Ca ratios (>7), and high supersaturations.
“Hood et al. (2011) and Hood and Wallace (2012) suggest that the environmental conditions that dominated and promoted the 'direct precipitation' of dolomite from solution in the Neoproterozoic seas were characterized by high alkalinities, elevated Mg:Ca ratios (>7) and high supersaturations.”
From A route for the direct crystallization of dolomite (2015) · cites this paper as Hood and Wallace 2012
Cites
Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry
Canfield, D. E., Poulton, S. W., Knoll, A. H., Narbonne, G. M., Ross, G., Goldberg, T., & Strauss, H. (2008) · Science · doi:10.1126/science.1154499 · Cited by 789 · see citing works
Microbial mediation as a possible mechanism for natural dolomite formation at low temperatures
Vasconcelos, C., McKenzie, J. A., Bernasconi, S., Grujic, D., & Tiens, A. J. (1995) · Nature · doi:10.1038/377220a0 · Cited by 745 · cited 1× · see citing works
“Microbial metabolic processes, particularly those of sulphate-reducing and methanogenic bacteria, have been suggested to induce dolomite precipitation in modern and ancient marine settings (Vasconcelos et al., 1995; Font et al., 2010).”
BackgroundThe Isotopic and Trace Element Geochemistry of Dolomite: The State of the Art
Land, L. S. (1980) · Concepts and Models of Dolomitization · doi:10.2110/pec.80.28.0087 · Cited by 664 · cited 1× · see citing works
“While dolomite has not been experimentally, inorganically precipitated under standard Earth surface conditions (Land, 1980, 1998), experimental work implicates several chemical and physical factors that influence dolomite precipitation.”
BackgroundVasconcelos, C., & McKenzie, J. A. (1997) · Journal of Sedimentary Research · doi:10.1306/d4268577-2b26-11d7-8648000102c1865d · Cited by 620 · see citing works
Low marine sulphate and protracted oxygenation of the Proterozoic biosphere
Kah, L. C., Lyons, T. W., & Frank, T. D. (2004) · Nature · doi:10.1038/nature02974 · Cited by 482 · see citing works
The dolomite problem; control of precipitation kinetics by temperature and saturation state
Arvidson, R. S. (1999) · American Journal of Science · doi:10.2475/ajs.299.4.257 · Cited by 447 · cited 1× · see citing works
“…of these factors include the solubility of the reactant (Katz and Mathews, 1977), the Mg2+/Ca2+ ratio of the fluid (Sibley et al., 1987), the presence of dissolved sulphate (Baker and Kastner, 1981), as well as the temperature and saturation state of the solution (Arvidson and MacKenzie, 1999).”
BackgroundLand, L. S. (1998) · Aquatic Geochemistry · doi:10.1023/a:1009688315854 · Cited by 396 · see citing works
Vasconcelos, C., McKenzie, J. A., Warthmann, R., & Bernasconi, S. M. (2005) · Geology · doi:10.1130/g20992.1 · Cited by 354 · cited 1× · see citing works
“This variation is significantly greater than the recently calculated fractionation factor between dolomite and calcite of 2.6‰ (Vasconcelos et al., 2005), suggesting dolomite precipitation and the aragonite-calcite conversion occurred at different times.”
BackgroundInfluentialDolomite formation and biogeochemical cycles in the Phanerozoic
Burns, S. J., Mckenzie, J. A., & Vasconcelos, C. (2000) · Sedimentology · doi:10.1046/j.1365-3091.2000.00004.x · Cited by 201 · see citing works
Hood, A. V. S., Wallace, M. W., & Drysdale, R. N. (2011) · Geology · doi:10.1130/g32119.1 · Cited by 133 · cited 15× · see citing works
“Twenty four samples were chosen for stable isotope (δ18O and δ13C) measurements based on their quality of preservation, according to thin section petrography and cathodoluminescence (Hood et al. (2011): Supplementary Data).”
BackgroundMethodInfluentialSelf-citation
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A route for the direct crystallization of dolomite
Rodriguez-Blanco, J. D., Shaw, S., & Benning, L. G. (2015) · American Mineralogist · doi:10.2138/am-2015-4963 · Cited by 161 · see citing works
“Furthermore, the radial growth morphology of the “direct” dolomite cements in the Neoproterozoic cap carbonates may also be a product of spherulitic growth indicating that they also may have formed from an amorphous precursor (Hood et al. 2011; Hood and Wallace 2012).”
BackgroundThe Tonian Beck Spring Dolomite: Marine dolomitization in a shallow, anoxic sea
Shuster, A. M., Wallace, M. W., van Smeerdijk Hood, A., & Jiang, G. (2018) · Sedimentary Geology · doi:10.1016/j.sedgeo.2018.03.003 · Cited by 89 · see citing works
Self-citationMüller, I. A., Rodriguez-Blanco, J. D., Storck, J.-C., do Nascimento, G. S., Bontognali, T. R. R., Vasconcelos, C., Benning, L. G., & Bernasconi, S. M. (2019) · Chemical Geology · doi:10.1016/j.chemgeo.2019.07.014 · Cited by 77 · see citing works
Structure, genesis and resources efficiency of dolomite: New insights and remaining enigmas
Cai, W. K., Liu, J. H., Zhou, C. H., Keeling, J., & Glasmacher, U. A. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120191 · Cited by 61 · see citing works
Enigmatic chambered structures in Cryogenian reefs: The oldest sponge-grade organisms?
Wallace, M. W., Hood, A. V. S., Woon, E. M. S., Hoffmann, K.-H., & Reed, C. P. (2014) · Precambrian Research · doi:10.1016/j.precamres.2014.09.020 · Cited by 30 · see citing works
Self-citationRaudsepp, M. J., Wilson, S., Morgan, B., Patel, A., Johnston, S. G., Gagen, E. J., & Fallon, S. J. (2022) · Sedimentology · doi:10.1111/sed.12991 · Cited by 29 · see citing works
- Authors
- Hood, A. V. S., & Wallace, M. W.
- Affiliations
- The University of Melbourne (AU)
- Corresponding author
- Hood, Ashleigh van Smeerdijk
- Venue
- Sedimentary Geology
- Publisher
- Elsevier BV
- Published
- 2012-05
- Volume
- 255-256
- Pages
- 56-71
- ISSN
- 0037-0738 (ISSN-L)
- OpenAlex
- W2008149897
- Cited by
- 112
- References
- 10
- Citations by year
- 2026: 9 · 2025: 9 · 2024: 9 · 2023: 15 · 2022: 15 · 2021: 11 · 2020: 8 · 2019: 8 · 2018: 4 · 2017: 5 · 2016: 4 · 2015: 7 · 2014: 6 · 2013: 1 · 2012: 1
- FWCI
- 3.58
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Sedimentary Geology (publishedVersion)
- Funders
- Monash University
- Topics
- 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
- Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
- Keywords
- Cryogenian, high-Mg calcite, aragonite, calcite, Precambrian carbonates, cathodoluminescence, crystallographic fabric
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