Discerning biotic from abiotic carbonate cementations in Holocene beachrock: mineralogical and geochemical fingerprints for biosignatures

IF 2.9 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Xi-yang Zhang , Ming-zhuang Wang , Qi Shi , Fei Tan , Guo-tao Zhang , Si-qi Chen , Hong-qiang Yang
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引用次数: 0

Abstract

Beachrock cementation, mediated by physicochemical and biological processes, plays a pivotal role in the rapid lithification of coastal sediments. Distinguishing between biotic and abiotic carbonate cements is critical for quantitatively reconstructing diagenetic pathways and accurately evaluating paleoenvironmental conditions. We analyzed Holocene beachrocks from Hainan and the Xisha Islands to compare their cement types. Beachrocks from Hainan are characterized by isopachous high-Mg calcite (HMC) rinds, HMC-rich peloidal fabrics, and blocky–drusy low-Mg calcite (LMC), whereas those from the Xisha Islands are dominated by acicular aragonite. HMC rinds composed of equilong fibrous crystals represent marine phreatic cements with minimal diagenetic alteration, whereas LMC forms through meteoric vadose processes, as indicated by red cathodoluminescent rings. Acicular aragonite nucleates within organic-rich micrite envelopes, with its rapid growth governed primarily by inorganic mechanisms. Peloidal fabrics exhibit distinct fluorescence patterns, dull cathodoluminescence, and elevated Mn/Fe ratios, consistent with their interpretation as microbially mediated precipitates formed during organic matter degradation under intermittently reducing conditions. Notably, peloidal fabrics and aragonite are enriched in bioactive metals (V, Fe, Zn, Pb) relative to coral Porites, consistent with active microbial metabolism. Unlike HMC rinds and acicular aragonite, peloidal fabrics display high total rare earth element (REE) contents, uniform REE distributions, LREE depletion (low LREE/HREE), negative Ce anomalies, positive La anomalies, Y/Ho ratios (∼45), and REE partitioning patterns closely matching modern seawater. These distinctive geochemical signatures establish peloidal fabrics as high-fidelity, high-resolution archives of paleo-seawater chemistry, providing a robust tool for deciphering ancient marine environments.
全新世滩岩中生物与非生物碳酸盐胶结的识别:生物特征的矿物学和地球化学指纹图谱
滩岩胶结作用是由物理化学和生物过程介导的,在海岸沉积物的快速岩化过程中起着关键作用。区分生物和非生物碳酸盐胶结物对于定量重建成岩路径和准确评价古环境条件至关重要。我们分析了海南和西沙群岛的全新世滩岩,比较了它们的胶结类型。海南滩岩以等径高镁方解石(HMC)表层、富HMC的似球粒状组构和块状低镁方解石(LMC)为主,西沙滩岩以针状文石为主。HMC环由等长纤维晶体组成,代表海洋潜水胶结物,成岩蚀变最小,而LMC则通过大气渗透过程形成,如红色阴极发光环所示。针状文石在富有机质泥晶包壳内成核,其快速生长主要受无机机制支配。Peloidal织物表现出明显的荧光模式、暗淡的阴极发光和升高的Mn/Fe比率,这与它们的解释一致,即在间歇性还原条件下有机物降解过程中形成的微生物介导的沉淀。值得注意的是,相对于珊瑚孔隙岩,peloidal fabric和文石富含生物活性金属(V, Fe, Zn, Pb),与活跃的微生物代谢一致。与HMC和针状文石不同,peloidal织物显示出高总稀土元素(REE)含量,均匀的REE分布,LREE枯竭(低LREE/HREE),负Ce异常,正La异常,Y/Ho比(~ 45),以及与现代海水密切匹配的REE分配模式。这些独特的地球化学特征使peloidal织物成为高保真度,高分辨率的古海水化学档案,为破译古代海洋环境提供了强大的工具。
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来源期刊
CiteScore
5.90
自引率
10.00%
发文量
398
审稿时长
3.8 months
期刊介绍: Palaeogeography, Palaeoclimatology, Palaeoecology is an international medium for the publication of high quality and multidisciplinary, original studies and comprehensive reviews in the field of palaeo-environmental geology. The journal aims at bringing together data with global implications from research in the many different disciplines involved in palaeo-environmental investigations. By cutting across the boundaries of established sciences, it provides an interdisciplinary forum where issues of general interest can be discussed.
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