Cryogenic cave carbonates from the Ural Mountains (Russia)
Coarsely crystalline cryogenic cave carbonates (CCCcoarse) are widely used indicators of past permafrost conditions. Nevertheless, details of their formation with respect to macroscopic morphology, stable isotope evolution and potential metastable precursor phases are poorly understood. CCCcoarse we...
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ftdatacite:10.5281/zenodo.5807542 2023-05-15T16:37:42+02:00 Cryogenic cave carbonates from the Ural Mountains (Russia) Töchterle, Paul 2018 https://dx.doi.org/10.5281/zenodo.5807542 https://zenodo.org/record/5807542 en eng Zenodo https://dx.doi.org/10.5281/zenodo.5807541 Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess CC-BY Cave Permafrost Cryogenic Calcite Ural Mountains article-journal Text ScholarlyArticle Thesis 2018 ftdatacite https://doi.org/10.5281/zenodo.5807542 https://doi.org/10.5281/zenodo.5807541 2022-02-08T18:10:54Z Coarsely crystalline cryogenic cave carbonates (CCCcoarse) are widely used indicators of past permafrost conditions. Nevertheless, details of their formation with respect to macroscopic morphology, stable isotope evolution and potential metastable precursor phases are poorly understood. CCCcoarse were found in 5 caves located along a north-south transect of the Ural Mountains, Russia. A comprehensive data set was generated including results of carbonate stable isotope composition, stable isotopic composition of fluid inclusion water, stable oxygen isotope thermometry, trace element composition, X-ray diffraction and transmission properties and U/Th disequilibrium dating. Detailed petrographic characterization of the samples allows for the proposal of a morphological classification scheme for CCCcoarse. Non-crystallographic branching of crystallites, also referred to as crystal splitting, is identified as the mechanism enabling morphological variety in CCCcoarse. Splitting propensity is likely related to physico-chemical properties of the mineral forming solution such as Mg++ concentration and supersaturation with respect to carbonate minerals. Numerical modelling of C and O stable isotope evolution shows that open system style degassing of CO2 during CCCcoarse formation accounts for 10 – 20% of the observed isotopic trends. These results support a model of slow and continuous degassing of CO2 via nucleation of gas bubbles in co-precipitating ice in compliance to freezing experiments. Fluid inclusion analyses suggest that early stages of CCCcoarse formation take place at isotopic equilibrium between carbonate minerals and the parent solution. However, oxygen isotope fractionation ( ????????????−???????????????????? 18 = 1.0318 ±0.0005) appears to be smaller than expected from literature values extrapolated to 0°C. Diffraction properties of a CCCcoarse specimen indicate that it formed via non-classical crystallisation pathways. Crystallisation by particle attachment (CPA) of poorly crystalline, or even amorphous precursor phases can explain diffraction data. Text Ice permafrost DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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English |
topic |
Cave Permafrost Cryogenic Calcite Ural Mountains |
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Cave Permafrost Cryogenic Calcite Ural Mountains Töchterle, Paul Cryogenic cave carbonates from the Ural Mountains (Russia) |
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Cave Permafrost Cryogenic Calcite Ural Mountains |
description |
Coarsely crystalline cryogenic cave carbonates (CCCcoarse) are widely used indicators of past permafrost conditions. Nevertheless, details of their formation with respect to macroscopic morphology, stable isotope evolution and potential metastable precursor phases are poorly understood. CCCcoarse were found in 5 caves located along a north-south transect of the Ural Mountains, Russia. A comprehensive data set was generated including results of carbonate stable isotope composition, stable isotopic composition of fluid inclusion water, stable oxygen isotope thermometry, trace element composition, X-ray diffraction and transmission properties and U/Th disequilibrium dating. Detailed petrographic characterization of the samples allows for the proposal of a morphological classification scheme for CCCcoarse. Non-crystallographic branching of crystallites, also referred to as crystal splitting, is identified as the mechanism enabling morphological variety in CCCcoarse. Splitting propensity is likely related to physico-chemical properties of the mineral forming solution such as Mg++ concentration and supersaturation with respect to carbonate minerals. Numerical modelling of C and O stable isotope evolution shows that open system style degassing of CO2 during CCCcoarse formation accounts for 10 – 20% of the observed isotopic trends. These results support a model of slow and continuous degassing of CO2 via nucleation of gas bubbles in co-precipitating ice in compliance to freezing experiments. Fluid inclusion analyses suggest that early stages of CCCcoarse formation take place at isotopic equilibrium between carbonate minerals and the parent solution. However, oxygen isotope fractionation ( ????????????−???????????????????? 18 = 1.0318 ±0.0005) appears to be smaller than expected from literature values extrapolated to 0°C. Diffraction properties of a CCCcoarse specimen indicate that it formed via non-classical crystallisation pathways. Crystallisation by particle attachment (CPA) of poorly crystalline, or even amorphous precursor phases can explain diffraction data. |
format |
Text |
author |
Töchterle, Paul |
author_facet |
Töchterle, Paul |
author_sort |
Töchterle, Paul |
title |
Cryogenic cave carbonates from the Ural Mountains (Russia) |
title_short |
Cryogenic cave carbonates from the Ural Mountains (Russia) |
title_full |
Cryogenic cave carbonates from the Ural Mountains (Russia) |
title_fullStr |
Cryogenic cave carbonates from the Ural Mountains (Russia) |
title_full_unstemmed |
Cryogenic cave carbonates from the Ural Mountains (Russia) |
title_sort |
cryogenic cave carbonates from the ural mountains (russia) |
publisher |
Zenodo |
publishDate |
2018 |
url |
https://dx.doi.org/10.5281/zenodo.5807542 https://zenodo.org/record/5807542 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_relation |
https://dx.doi.org/10.5281/zenodo.5807541 |
op_rights |
Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5281/zenodo.5807542 https://doi.org/10.5281/zenodo.5807541 |
_version_ |
1766028013464453120 |