Impact of diagenetic alteration on brachiopod shell magnesium isotope (δ²⁶Mg) signatures: Experimental versus field data

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• 作者：Sylvia Riechelmann^a ; ^{Sylvia.Riechelmann@rub.de" class="auth_mail" title="E-mail the corresponding author} ; Vasileios Mavromatis^b ; ^c ; Dieter Buhl^a ; Martin Dietzel^b ; Anton Eisenhauer^d ; Adrian Immenhauser^a
• 关键词：Magnesium isotopes ; Diagenesis ; Brachiopods ; Carbon and oxygen isotopes
• 刊名：Chemical Geology
• 出版年：2016
• 出版时间：15 November 2016
• 年：2016
• 卷：440
• 期：Complete
• 页码：191-206
• 全文大小：2309 K

文摘

Due to their thermodynamically stable low-Mg calcite mineralogy, the shells of brachiopods are often counted among the most reliable archives of the physicochemical conditions that occurred during the Phanerozoic in marine waters. Consequently, traditional and non-traditional isotope and elemental proxy data from brachiopod valves have been analyzed in numerous studies and results obtained have been placed in context with ancient seawater properties. This paper tests the sensitivity of brachiopod shell magnesium isotope (δ²⁶Mg) data to diagenetic alteration. We apply a dual approach by: (i) performing hydrothermal alteration experiments using meteoric, marine, and burial reactive fluids; and (ii) comparing these data to naturally altered, ancient brachiopod shells. The degree of alteration of individual shells is assessed by a combination of fluorescence and cathodoluminescence microscopy. The absence of luminescence might indicate both well-preserved shell material, but also the secondary enrichment of quenching elements such as iron along diagenetic pathways. Complementary oxygen isotope data provide insight into the question of open versus closed system behavior of brachiopod shells. Brachiopod shell magnesium isotope values respond to differential fluid temperature, chemistry, and experiment durations. The patterns observed are complicated by the interplay of kinetic and thermodynamic patterns and the presence of variable amounts of water soluble and water insoluble organic matter within these biominerals. Generally, the range in bulk δ²⁶Mg from experimentally altered (1.52‰) and that of bulk samples from ancient, diagenetically altered brachiopod valves (1.53‰) exceed the geochemical variability of δ²⁶Mg_brachiopod bulk values of most recent specimens (1.26‰) in the lower and upper range. More ²⁶Mg enriched (0.8‰) and more ²⁶Mg depleted (0.7‰) values, respectively, are found in altered shells in comparison to unaltered ones. The data shown here are considered significant for those aiming to reconstruct palaeoenvironmental parameters based on brachiopod archives. Consequently, we propose tentative guidelines for magnesium isotope research applied to ancient carbonates.