Articles | Volume 19, issue 16
https://doi.org/10.5194/bg-19-3791-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-19-3791-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Experimental burial diagenesis of aragonitic biocarbonates: from organic matter loss to abiogenic calcite formation
Department of Mineralogy and Petrology, Universidad Complutense de Madrid, Madrid, 28040, Spain
María Simonet Roda
Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universität, Munich, 80333, Germany
Martina Greiner
Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universität, Munich, 80333, Germany
Erika Griesshaber
Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universität, Munich, 80333, Germany
Nelson A. Lagos
Centro de Investigación e Innovación para el Cambio Climático, Universidad Santo Tomás, Santiago, Chile
Sabino Veintemillas-Verdaguer
CORRESPONDING AUTHOR
Instituto de Ciencia de Materiales de Madrid (ICMM, CSIC), Madrid, 28049, Spain
José Manuel Astilleros
Department of Mineralogy and Petrology, Universidad Complutense de Madrid, Madrid, 28040, Spain
Instituto de Geociencias (IGEO), (UCM, CSIC), Madrid, 28040, Spain
Lurdes Fernández-Díaz
CORRESPONDING AUTHOR
Department of Mineralogy and Petrology, Universidad Complutense de Madrid, Madrid, 28040, Spain
Instituto de Geociencias (IGEO), (UCM, CSIC), Madrid, 28040, Spain
Wolfgang W. Schmahl
Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universität, Munich, 80333, Germany
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Cited
10 citations as recorded by crossref.
- Pleistocene aragonite crust diagenesis mimics microbialite fabrics (Danakil Depression, Ethiopia) D. Jaramillo-Vogel et al. 10.1016/j.sedgeo.2023.106341
- The role of sulfate in the hydrothermal replacement of aragonite single crystals by calcite P. Forjanes et al. 10.1016/j.epsl.2024.118771
- Pb Removal Efficiency by Calcium Carbonates: Biogenic versus Abiogenic Materials A. Roza-Llera et al. 10.1021/acs.cgd.3c00517
- Melanoides tuberculata and Zootecus insularis gastropod shells provide a snapshot into past hydroclimatic conditions of arid environments: New perspectives from Oman K. Schmitt et al. 10.1016/j.palaeo.2024.112542
- Fossil biocalcite remains open to isotopic exchange with seawater for tens of millions of years D. Cisneros-Lazaro et al. 10.1038/s41598-024-75588-7
- Increasing control over biomineralization in conodont evolution B. Shirley et al. 10.1038/s41467-024-49526-0
- Ca isotopic gradients in epeiric marine carbonates: Diagenetic origins of and significance for Ca cycle reconstructions C. Holmden et al. 10.1016/j.gca.2024.03.017
- Exploring electron backscatter diffraction analysis as a tool for understanding stromatolite: Quantitative description of Cretaceous lacustrine stromatolite reveals formative processes and high‐resolution climatic cycles M. Simonet Roda et al. 10.1111/sed.13222
- Formation of Strontianite and Witherite Cohesive Layers on Calcite Surfaces for Building Stone Conservation P. Forjanes et al. 10.1021/acs.cgd.2c00383
- Thermal-induced crystallographic transformation in shells of Mytilus galloprovincialis Lamarck, 1819 L. Hu et al. 10.1016/j.palaeo.2024.112523
10 citations as recorded by crossref.
- Pleistocene aragonite crust diagenesis mimics microbialite fabrics (Danakil Depression, Ethiopia) D. Jaramillo-Vogel et al. 10.1016/j.sedgeo.2023.106341
- The role of sulfate in the hydrothermal replacement of aragonite single crystals by calcite P. Forjanes et al. 10.1016/j.epsl.2024.118771
- Pb Removal Efficiency by Calcium Carbonates: Biogenic versus Abiogenic Materials A. Roza-Llera et al. 10.1021/acs.cgd.3c00517
- Melanoides tuberculata and Zootecus insularis gastropod shells provide a snapshot into past hydroclimatic conditions of arid environments: New perspectives from Oman K. Schmitt et al. 10.1016/j.palaeo.2024.112542
- Fossil biocalcite remains open to isotopic exchange with seawater for tens of millions of years D. Cisneros-Lazaro et al. 10.1038/s41598-024-75588-7
- Increasing control over biomineralization in conodont evolution B. Shirley et al. 10.1038/s41467-024-49526-0
- Ca isotopic gradients in epeiric marine carbonates: Diagenetic origins of and significance for Ca cycle reconstructions C. Holmden et al. 10.1016/j.gca.2024.03.017
- Exploring electron backscatter diffraction analysis as a tool for understanding stromatolite: Quantitative description of Cretaceous lacustrine stromatolite reveals formative processes and high‐resolution climatic cycles M. Simonet Roda et al. 10.1111/sed.13222
- Formation of Strontianite and Witherite Cohesive Layers on Calcite Surfaces for Building Stone Conservation P. Forjanes et al. 10.1021/acs.cgd.2c00383
- Thermal-induced crystallographic transformation in shells of Mytilus galloprovincialis Lamarck, 1819 L. Hu et al. 10.1016/j.palaeo.2024.112523
Latest update: 13 Dec 2024
Short summary
Aragonitic skeletons are employed to decipher past climate dynamics and environmental change. Unfortunately, the information that these skeletons keep can be destroyed during diagenesis. In this work, we study the first changes undergone by aragonitic skeletons upon hydrothermal alteration. We observe that major changes occur from the very beginning of the alteration, even without mineralogical changes. These results have major implications for the use of these archives to understand the past.
Aragonitic skeletons are employed to decipher past climate dynamics and environmental change....
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