Neoproterozoic aragonite-dolomite seas? Widespread marine dolomite precipitation in Cryogenian reef complexes
Abstract
Research Article| September 01, 2011 Neoproterozoic aragonite-dolomite seas? Widespread marine dolomite precipitation in Cryogenian reef complexes Ashleigh v.S. Hood; Ashleigh v.S. Hood 1School of Earth Sciences, University of Melbourne, Parkville, Victoria 3010, Australia Search for other works by this author on: GSW Google Scholar Malcolm W. Wallace; Malcolm W. Wallace 1School of Earth Sciences, University of Melbourne, Parkville, Victoria 3010, Australia Search for other works by this author on: GSW Google Scholar Russell N. Drysdale Russell N. Drysdale 2Department of Resource Management and Geography, University of Melbourne, Parkville, Victoria 3010, Australia Search for other works by this author on: GSW Google Scholar Author and Article Information Ashleigh v.S. Hood 1School of Earth Sciences, University of Melbourne, Parkville, Victoria 3010, Australia Malcolm W. Wallace 1School of Earth Sciences, University of Melbourne, Parkville, Victoria 3010, Australia Russell N. Drysdale 2Department of Resource Management and Geography, University of Melbourne, Parkville, Victoria 3010, Australia Publisher: Geological Society of America Received: 28 Jan 2011 Revision Received: 08 Apr 2011 Accepted: 19 Apr 2011 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2011 Geological Society of America Geology (2011) 39 (9): 871–874. https://doi.org/10.1130/G32119.1 Article history Received: 28 Jan 2011 Revision Received: 08 Apr 2011 Accepted: 19 Apr 2011 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Ashleigh v.S. Hood, Malcolm W. Wallace, Russell N. Drysdale; Neoproterozoic aragonite-dolomite seas? Widespread marine dolomite precipitation in Cryogenian reef complexes. Geology 2011;; 39 (9): 871–874. doi: https://doi.org/10.1130/G32119.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The extraordinary abundance of dolomite in the Proterozoic challenges our understanding of Precambrian marine environments. Here we show that synsedimentary marine dolomite precipitation was pervasive within Cryogenian reef complexes from the Adelaide Fold Belt, South Australia. Although these reefs are composed of dolomite, textural evidence indicates an originally aragonitic mineralogy for depositional components, in common with many other Neoproterozoic carbonates. Allochthonous slope debris from the reefs invariably contains both limestone and dolomite clasts, indicating synsedimentary dolomitization in the reefs. We describe several new forms of fibrous marine dolomite cement from the reefs that have a length-slow optical character. These fascicular slow, radial slow, and rhombic dolomite cements have finely preserved cathodoluminescent growth zones, and optical characteristics that indicate they originally precipitated as dolomite, rather than replacing calcite or aragonite cements. Abundant early marine dolomite precipitation implies a radically different seawater chemistry for the Cryogenian. Perhaps these aragonite-dolomite seas are associated with extreme Neoproterozoic glacial events and/or ocean anoxia. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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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 et al. 2011
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 et al. 2011
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 et al. 2011
If the assertion of a 'direct' dolomite cement formation scenario is correct, the spherulitic growth mechanism could have been the controlling pathway to produce the Cryogenian cap dolomites described by Hood et al. (2011), regardless of whether their formation occurred via microbially mediated processes.
“This leads us to infer that if the assertion of a 'direct' dolomite cement formation scenario is correct, the spherulitic growth mechanism could have been the controlling pathway to produce the Cryogenian cap dolomites described by Hood et al. (2011), regardless of whether their formation occurred via a microbially mediated processes as suggested by Font et al. (2010).”
From A route for the direct crystallization of dolomite (2015) · cites this paper as Hood et al. 2011
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“In particular, primary dolomite is hypothesized to have precipitated in the Precambrian (Tucker, 1982), perhaps from aragonite–dolomite seas (Hood et al., 2011; Hood & Wallace, 2012) and in the Triassic in the Dolomites of Northern Italy (Preto et al., 2015; Meister & Frisia, 2019).”
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Santos, R. F., Nogueira, A. C., da Costa, J. D., Sepeda, L. F., Okubo, J., Barros, I. S., Sodré, A. A. N., Oliveira, P. G. A., Barrera, I. A. R., & Sansjsofre, P. (2023) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2023.106496 · Cited by 11 · see citing works
The record of sea water chemistry evolution during the Ediacaran–Cambrian from early marine cements
Xiong, Y., Wood, R., & Pichevin, L. (2022) · The Depositional Record · doi:10.1002/dep2.211 · Cited by 11 · see citing works
“These so- called ‘aragonite– dolomite seas’ (Hood et al., 2011) were largely replaced by ‘aragonite seas’ with aragonitic cements and inferred lower Mg/Ca ratios by the early (Corsetti et al., 2006; Hardie, 2003) or late Ediacaran (Wood et al., 2017).”
BackgroundStromatolite framework builders: ecosystems in a Cryogenian interglacial reef
Corkeron, M., & Slezak, P. (2020) · doi:10.1080/08120099.2020.1732464 · Cited by 11
Resolving the Snowball Earth conundrum: the role of marine dissolved organic carbon pool.
Shen, B., Lang, X., Wang, R.-M., Liu, Y.-G., Zhang, S., Huang, T.-Z., Chu, X., Cui, Y., Ding, W., Du, Y., et al. (2025) · Science Bulletin · doi:10.1016/j.scib.2025.03.056 · Cited by 10 · see citing works
Virgo, G., Collins, A., Amos, K. J., Farkaš, J., Blades, M., & Subarkah, D. (2021) · Precambrian Research · doi:10.1016/j.precamres.2021.106449 · Cited by 10 · see citing works
Wang, L.-C., Hu, G., Zhao, D., Tan, X.-C., & Wang, H. (2021) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/j.palaeo.2021.110729 · Cited by 10 · see citing works
Li, F., Lang, X., Ma, H.-R., Cui, Y., Pei, H.-X., & Shen, B. (2020) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2019.109409 · Cited by 10 · see citing works
Li, C.-W., Liu, K.-Y., & Liu, J.-L. (2023) · Goldschmidt2022 abstracts · doi:10.46427/gold2022.13278 · Cited by 9
Zhang, X.-J., Zhou, G., Zhang, P., He, Y., Wei, Z.-F., Wang, G.-X., Zhang, T., He, W., Ma, H., Zhu, C.-X., et al. (2022) · Frontiers in Earth Science · doi:10.3389/feart.2022.865709 · Cited by 9 · see citing works
“Additionally, some studies have shown that the Ediacaran seawater was the “aragonite seawater” with Mg/Ca values over 2 (Hardie, 1996, Hardie, 2003), while others proposed that the characteristics of the Ediacaran seawater may provide the precipitation condition for dolomite, indicating an “aragonite–dolomite seawater…”
BackgroundCarbonate fabric diversity and environmental heterogeneity in the late Mesoproterozoic Era
Kah, L. C., & Bartley, J. (2021) · Geological Magazine · doi:10.1017/s0016756821000406 · Cited by 9 · see citing works
Lu, K., Bao, Z.-D., Sheng, M., Bao, Y., Dai, Q., Cao, Y., Liu, R., Zhang, S.-C., & Li, J. (2021) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2020.104877 · Cited by 9 · see citing works
Delpomdor, F., Bonneville, S., Baert, K., & Préat, A. (2018) · Journal of Petroleum Geology · doi:10.1111/jpg.12690 · Cited by 8 · see citing works
Liu, E.-T., Yan, D.-T., Zhao, J.-X., Wang, J., Feng, Y.-X., Zhong, L., Jiang, H., Shen, N., & Zhan, J. (2025) · Precambrian Research · doi:10.1016/j.precamres.2024.107636 · Cited by 7 · see citing works
More than an age: U-Pb dating constrains alteration of Precambrian carbonates
Neagu, N., Kylander-Clark, A., Fischer, W., & Ryb, U. (2025) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2024.119154 · Cited by 7 · see citing works
Zhao, Y., Gao, D., Ngia, N., Hu, M.-Y., & Zhao, S.-Q. (2025) · Journal of Petroleum Exploration and Production Technology · doi:10.1007/s13202-025-01996-8 · Cited by 6 · see citing works
“Previous studies have identified various types of fluids involved in early diagenetic dolomitization, including nor - mal seawater (Saller 1984; Hood et al. 2011 ), high-salinity seawater (Adams and Rhodes 1960; Jones et al. 2002; Melim and Scholle 2002 ), and mixed water (Humphrey 1988; Li et al.…”
Gómez-Peral, L., Arrouy, M., Ferreyra, C., Penzo, V., & Poiré, D. (2024) · Minerals · doi:10.3390/min14060529 · Cited by 6 · see citing works
Liu, H.-Y., Shi, K., Liu, B., Li, Y., Li, Y., Zheng, H., Peng, Y., & Fu, Y. (2023) · Sedimentology · doi:10.1111/sed.13139 · Cited by 6 · see citing works
“Extensive dolomite cement precipitation during syn-sedimentary diagenesis in the Precambrian was due to radically different seawater chemistry (Hood et al ., 2011; Hood & Wallace, 2012; Hu et al ., 2020, 2022).”
BackgroundDichotomous effects of oxidative metabolisms: A theoretical perspective on the dolomite problem
Shang, H. (2023) · Global and Planetary Change · doi:10.1016/j.gloplacha.2023.104041 · Cited by 6 · see citing works
A best-practices guide to X-ray diffraction studies of sedimentary carbonates
Lukoczki, G., Bish, D. L., & Gregg, J. (2026) · Sedimentary Geology · doi:10.1016/j.sedgeo.2026.107028 · Cited by 5 · see citing works
Fabbi, S., Borrelli, M., Innamorati, G., Aldega, L., Daëron, M., Perri, E., & Santantonio, M. (2024) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2024.107115 · Cited by 5 · see citing works
Palaeo-environmental significance of fibrous carbonate cement in Marinoan cap carbonates
Hu, Y.-J., Cai, C., Sun, P., Zhang, H., Liu, Z., Li, Y., Wang, Q., Tang, Y.-J., & Immenhauser, A. (2023) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2023.106392 · Cited by 5 · see citing works
Preservation of Soft-Bodied Organisms in Early Cambrian Carbonates
Marusin, V., & Bykova, N. (2023) · Russian Geology and Geophysics · doi:10.2113/rgg20234595 · Cited by 5 · see citing works
Chen, X., Kuang, H., Liu, Y.-Q., Heron, D. P. L., Wang, Y.-C., Bai, H., & Peng, N. (2022) · Sedimentology · doi:10.1111/sed.13051 · Cited by 5 · see citing works
“8F) dolomite cements had syntaxially replaced original calcite or aragonite, the dolomite would have a lengthfast character (Hood et al., 2011).”
BackgroundComposition and history of giant carbonate seep mounds, Mesoproterozoic Borden Basin, Arctic Canada
Hahn, K., & Turner, E. (2017) · Precambrian Research · doi:10.1016/j.precamres.2017.03.009 · Cited by 5 · see citing works
Han, Z.-Z., Dai, S.-R., Zhang, Y.-J., Han, C., Zhu, C., Zhao, Y.-Y., Zhang, Y.-T., & Li, Q. (2024) · Sedimentary Geology · doi:10.1016/j.sedgeo.2024.106653 · Cited by 4 · see citing works
Lu, Y., Mihailova, B., Malcherek, T., Paulmann, C., Smrzka, D., Zwicker, J. D., Lin, Z.-Y., Bohrmann, G., & Peckmann, J. (2023) · Sedimentology · doi:10.1111/sed.13170 · Cited by 4 · see citing works
“For instance, Neoprotero-zoic seawater corresponded to aragonite sea conditions (Hardie, 2003), but promoted the formation of fibrous dolomite (Hood et al ., 2011; Wood et al ., 2017; Shuster et al ., 2018; Ding et al ., 2019; Hu et al ., 2020).”
BackgroundSmrzka, D., Kuzel, K., Chiarella, D., Joachimski, M., Vandyk, T., Kettler, C., & Heron, D. P. L. (2022) · Sedimentology · doi:10.1111/sed.13003 · Cited by 4 · see citing works
Li, Y., Zhang, B., Zhou, G., Tang, R.-F., Long, H.-Y., Li, C., Chen, X., Chen, D., Liu, X.-H., Zhang, C., et al. (2024) · Frontiers in Earth Science · doi:10.3389/feart.2024.1407400 · Cited by 3 · see citing works
The evolution of Earth's marine carbonate factory
Tarhan, L., & Planavsky, N. (2026) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/j.palaeo.2026.113746 · Cited by 2 · see citing works
Neoproterozoic rocks of the Garvellachs, Scotland
Tyler, D. (2026) · Journal of Palaeogeography · doi:10.1016/j.jop.2026.100386 · Cited by 2
Carbonate sedimentology: An evolved discipline
James, N. P., & Pufahl, P. (2025) · The Depositional Record · doi:10.1002/dep2.70042 · Cited by 2 · see citing works
Liu, Y.-H., Lee, D.-C., Liang, M.-C., Iizuka, Y., Thiemens, M., Shen, Y., & Shang, H. (2025) · Chemical Geology · doi:10.1016/j.chemgeo.2025.122764 · Cited by 2 · see citing works
Bahri, J. A., Bankole, O., Muir, D., el Albani, A., Oldroyd, A., Contreras, D., Andersen, M., & Chi-Fru, E. (2024) · Precambrian Research · doi:10.1016/j.precamres.2024.107498 · Cited by 2 · see citing works
Nanoscale crystal fabric of primary Ediacaran dolomite
Wilcots, J., Gilbert, P., & Bergmann, K. (2021) · doi:10.1002/essoar.10507750.2 · Cited by 2
“These isopachous, length-slow dolomite crystals are arranged222 in bundles that fan outward, and are interpreted to represent primary dolomite cements pre-223 cipitated in pore space in the early diagenetic environment of the ca. 650 Ma Balcanoona224 Reef Complex (Hood et al., 2011; Hood & Wallace, 2012).”
BackgroundInfluential
- Authors
- Hood, A. V. S., Wallace, M. W., & Drysdale, R. N.
- Affiliations
- The University of Melbourne (AU)
- Venue
- Geology
- Publisher
- Geological Society of America
- Published
- 2011-09
- Volume
- 39
- Issue
- 9
- Pages
- 871-874
- ISSN
- 0091-7613 (ISSN-L)
- 1943-2682
- OpenAlex
- W1972822342
- Cited by
- 133
- References
- 0
- Citations by year
- 2026: 15 · 2025: 11 · 2024: 12 · 2023: 10 · 2022: 15 · 2021: 16 · 2020: 13 · 2019: 7 · 2018: 11 · 2017: 9 · 2016: 3 · 2015: 4 · 2014: 3 · 2013: 1 · 2012: 3
- FWCI
- 1.57
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geology (publishedVersion)
- 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 › Geophysics › Geological and Geochemical Analysis
- Keywords
- Neoproterozoic, Cryogenian, aragonite, dolomite, reef complexes, carbonate geochemistry, seawater chemistry, Neoproterozoic glaciation, paleoceanography, redox conditions, Snowball Earth, Permian-Triassic boundary, carbonate diagenesis
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