Chromium isotope stratigraphy of Ediacaran cap dolostones, Doushantuo Formation, South China

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• 作者：A.S. Rodler^a ; ^b ; ^{alexandra.rodler@reflex.at" class="auth_mail" title="E-mail the corresponding author} ; S.V. Hohl^c ; Q. Guo^d ; R. Frei^a ; ^b
• 关键词：Yangtze Platform ; Detrital contamination ; Al-corrected Cr signals ; Diagenetic alteration ; Coeval oxygenated seawater Cr composition
• 刊名：Chemical Geology
• 出版年：2016
• 出版时间：15 October 2016
• 年：2016
• 卷：436
• 期：Complete
• 页码：24-34
• 全文大小：817 K

文摘

The Yangtze Platform in South China is considered a key site for studying Neoproterozoic ocean oxygenation. Comprehensive Cr concentration and isotopic signatures are presented from cap dolostones of the Doushantuo Formation from a deep water and a shallow marine carbonate section, that have previously been used to constrain the redox evolution of Ediacaran seawater in space and time employing major and trace element abundances as well as Sr-, O- and C-isotope compositions. The majority of the studied samples yield elevated Cr concentrations and negatively fractionated δ⁵³Cr signals due to (i) detrital contamination consistent with Cr signatures of other post-Marinoan cap dolostones, (ii) diagenetic carbonate alteration and post-depositional remobilization of Cr. Al concentrations were used as indicator of detrital contamination and to calculate authigenic Cr concentration and isotope signatures when the detrital contribution of Cr was < 40%, which generally resulted in slightly lower Cr concentrations and slightly higher Cr isotopic signals in these samples. Diagenetic alteration of a majority of the studied cap dolostones is evident from low Sr concentrations and light δ¹⁸O_carb signals that correlate with low Cr concentrations and negatively fractionated δ⁵³Cr values. Post-depositional remobilization of Cr results in the loss of heavy Cr isotopes and consequently light Cr isotopes are retained during precipitation of secondary carbonates. However, some samples might still show pristine Ediacaran seawater signals. Two samples pertaining to the deep water cap dolostone section at Yanwutan and one sample pertaining to the shallow water section at Jijiawan yield slightly positively fractionated δ⁵³Cr signals, particularly when corrected to presumably authigenic signals (δ⁵³Cr_auth). These values are consistent with those from other Neoproterozoic carbonate sections deposited in an oxygenated environment. This short sequence of positively fractionated δ⁵³Cr_auth is concurrent with a cap dolostone ⁸⁷Sr/⁸⁶Sr signal close to Ediacaran seawater values with relatively high Sr and Cr concentrations, with decreased detrital contamination and with a pronounced negative Ce anomaly. They indicate either light pulses of enhanced oxidative weathering or, inferred from a few least-altered samples, prevailing oxic conditions during cap dolostone deposition. The Cr isotopic composition of Ediacaran cap dolostones pertaining to the Doushantuo Formation reveals fine-scale fluctuations in post-glacial detrital contamination and diagenesis balanced against a clear signal of oxidative weathering. Cr isotopes have the potential to further enhance our understanding of Neoproterozoic weathering regimes and past ocean oxygenation, however, before the Cr isotope system can be faithfully applied to delineate changes in redox conditions recorded in ancient marine carbonates, possible diagenetic alteration of the Cr signal as well as Cr contribution from detrital contamination need to be taken into consideration.