Paleo-redox conditions during the demise of a carbonate platform in the Tethyan ocean: Evidence from phosphatized and metals (Mn and Fe) rich hardgrounds

IF 3.7 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Luca Basilone , Simone Bernardini , Fausto Grassa , Attilio Sulli , Luis M. Nieto , Anas Abbassi , Luigi Jovane
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Abstract

Phosphatized Mn and Fe rich hardgrounds and condensed pelagic deposits in carbonate platform successions are precious archives of abrupt climate and environmental changes (redox conditions and phosphorous availability) in the past shallow-water marine environment. While numerous examples have been documented in the Cretaceous successions of the Northern Tethys, the scarcity of similar descriptions from the southern margins suggests differences in sedimentary processes or preservation conditions.
In this work we study three phosphatized Mn and Fe rich hardgrounds and pelagic condensed deposits that mark the repetitive demise of the Panormide carbonate platform developed in the Southern Tethyan margin during the Cretaceous. The integration of SEM-EDS, PXRD, and Micro-Raman spectroscopy data shows that these hardgrounds consist of fine-grained Fe (goethite and hematite) and Mn (birnessite and/or vernadite) oxides dispersed in a calcite and apatite matrix. Micro-Raman spectroscopy shows the presence of oxidized Mn species: Mn3+ and Mn4+. The oxidation of Mn2+ → Mn3+/4+ and/or Fe2+ → Fe3+ occurred at the sediment-seawater interface under oxic conditions (where both Mn and Fe oxidize) or suboxic conditions (where only Fe oxidizes). The paleoenvironmental perturbations that triggered the formation of both hardgrounds and condensed pelagic deposits were likely related to pCO2 cycle, upwelling of P-Mn-Fe-rich water masses, eutrophication and phosphatization related to the Cretaceous climate oscillations during the main Oceanic Anoxic Events. These perturbations were likely enhanced by tectonic activity. Moreover, we show that the formation of the phosphatized metals-rich hardgrounds and the recovery of shallow-water sedimentation occurred after long-term periods (6–12 Ma). Thus, the Panormide serves as a remarkable example of resilience amidst significant climatic changes.
泰特洋碳酸盐平台消亡期间的古氧化还原条件:磷化和富含金属(锰和铁)的硬地提供的证据
碳酸盐平台演替中富含磷化锰和铁的硬地和凝聚沉积物是过去浅水海洋环境中气候和环境(氧化还原条件和磷的可用性)骤变的珍贵档案。在这项工作中,我们研究了三个富含磷化锰和铁的硬地和浮游凝聚沉积物,它们标志着白垩纪期间在南特提斯洋边缘发育的 Panormide 碳酸盐平台的重复消亡。SEM-EDS, PXRD 和显微拉曼光谱数据的整合表明,这些硬地由分散在方解石和磷灰石基质中的细粒铁(鹅铁矿和赤铁矿)和锰(桦锰矿和/或蛭锰矿)氧化物组成。显微拉曼光谱显示存在氧化锰物种:Mn3+ 和 Mn4+。Mn2+ → Mn3+/4+ 和/或 Fe2+ → Fe3+ 的氧化发生在沉积物-海水界面的氧化条件下(锰和铁都氧化)或亚氧化条件下(只有铁氧化)。引发硬地和凝聚沉积物形成的古环境扰动可能与 pCO2 循环、富含 P-Mn-Fe 的水团上涌、富营养化以及主要大洋缺氧事件期间与白垩纪气候振荡有关的磷化有关。这些扰动很可能因构造活动而加剧。此外,我们还表明,富含金属的磷化硬地的形成和浅水沉积的恢复发生在长期时期(6-12Ma)之后。因此,Panormide 是在重大气候变化中恢复能力的杰出范例。
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来源期刊
Marine and Petroleum Geology
Marine and Petroleum Geology 地学-地球科学综合
CiteScore
8.80
自引率
14.30%
发文量
475
审稿时长
63 days
期刊介绍: Marine and Petroleum Geology is the pre-eminent international forum for the exchange of multidisciplinary concepts, interpretations and techniques for all concerned with marine and petroleum geology in industry, government and academia. Rapid bimonthly publication allows early communications of papers or short communications to the geoscience community. Marine and Petroleum Geology is essential reading for geologists, geophysicists and explorationists in industry, government and academia working in the following areas: marine geology; basin analysis and evaluation; organic geochemistry; reserve/resource estimation; seismic stratigraphy; thermal models of basic evolution; sedimentary geology; continental margins; geophysical interpretation; structural geology/tectonics; formation evaluation techniques; well logging.
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