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Facies analysis and depositional evolution of Lower–Middle Ordovician carbonates in the Shuntuoguole Low Uplift of Tarim Basin (NW China) 塔里木盆地顺图郭勒低隆起带(中国西北部)下-中奥陶统碳酸盐岩的岩相分析与沉积演化
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2023-12-10 DOI: 10.1007/s10347-023-00676-5
Jun Han, Daizhao Chen, Zicheng Cao, Chongyang Xiao, Cheng Huang, Shi Wang, Jingping Chen, Chuan Guo

As a result of a deep burial depth (> 6.5 km), the depositional history of the Early to Middle Ordovician carbonate platform in the Shuntuoguole Low Uplift (Tarim Basin, NW China) has been difficult to unravel, leading to problems in understanding the controls of the facies distribution, particularly in terms of petroleum exploration. Integrated with geophysical surveys, detailed sedimentological observations document the platform evolution and show that a carbonate ramp system developed in the Shuntuoguole Low Uplift during the Early-Middle Ordovician, with twelve lithofacies types arranged into two facies associations, including peritidal to semi-restricted subtidal and open-marine subtidal facies. Based on the tempo-spatial distribution of lithofacies, seven third-order depositional sequences are identified, each composed of a transgressive lower package and a regressive upper part. Their sequence boundaries are commonly characterised by a transitional zone with no obvious subaerial exposure features. The correlation of relative sea-level (or accommodation space) changes derived from the vertical stacking pattern of facies with the global sea-level curve of Haq and Schutter (2008) and sea-level oscillations of coeval successions worldwide suggests that eustatic sea-level fluctuations were the overriding factor controlling the development and evolution of this carbonate ramp during the Early-Middle Ordovician. Meanwhile, regional or local tectonic subsidence and environmental factors (e.g. palaeoclimate and prevailing wind) also exerted an influence on the depositional processes of the Shuntuoguole Low Uplift over this time interval.

由于埋藏深度较深(6.5 千米),顺图郭勒低隆起(中国西北部塔里木盆地)早中奥陶世碳酸盐岩平台的沉积历史一直难以揭示,导致在了解岩相分布的控制因素方面存在问题,特别是在石油勘探方面。结合地球物理勘探,详细的沉积学观察记录了平台的演化过程,并表明在早-中奥陶世期间,顺图郭勒低隆起发育了碳酸盐岩斜坡系统,有十二种岩性类型,分为两个面系,包括潮下带至半限制潮下带和开放海相潮下带。根据岩性的时间-空间分布,确定了七个三阶沉积序列,每个序列都由下部的横向组合和上部的回归组合组成。它们的序列边界通常是一个过渡带,没有明显的次海相暴露特征。根据面层垂直堆积模式得出的相对海平面(或容纳空间)变化与 Haq 和 Schutter(2008 年)的全球海平面曲线以及全球共生演替的海平面振荡的相关性表明,在早奥陶世-中奥陶世期间,侵蚀性海平面波动是控制该碳酸盐斜坡发育和演化的首要因素。同时,区域或地方构造沉降和环境因素(如古气候和盛行风)也对这一时期的顺图郭勒低隆起沉积过程产生了影响。
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引用次数: 0
The colourful optical appearance of centric diatom fossil frustules with diagenetic nanocrystalline calcite fill 具有成岩作用的纳米晶方解石充填的中心硅藻化石块状体的彩色光学外观
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2023-11-30 DOI: 10.1007/s10347-023-00675-6
Moritz Liesegang, Mohamed Ghobara, Sabine Matting, Richard Wirth

Biophotonic nanostructures rarely withstand fossilization processes occurring after burial over geologic time. Even more distinctive is a change introduced to the optical properties during diagenetic processes resulting in a different optical appearance. Here, we report and explain the optical appearance of centric diatom frustules obtained from ash-bearing carbonate-cemented concretions on the Greifswalder Oie island (Pomeranian Bay, Germany, southern Baltic Sea). The ultrastructural and mineralogical analysis of the fossil frustules were carried out using electron microscopy techniques and were correlated to the macroscopic and microscopic optical appearance of the frustules before and after acid etching. The unique optical properties of the fossil diatoms were associated with diagenetic nanocrystalline calcite filling the frustules’ areolae. This fill created the macroscopic pale-yellow colour of many frustules, a microscopic iridescence probably associated with diffraction grating behaviour, and microscopic colour rings. The results highlight the unique permineralization process of diatom frustules and might be an addition to the emerging studies on frustule optics and photonics.

生物光子纳米结构很少经受住地质时期埋藏后发生的石化过程。更独特的是在成岩过程中引入的光学性质的变化,导致不同的光学外观。在这里,我们报告并解释了在Greifswalder Oie岛(德国波美拉尼亚湾,波罗的海南部)的含灰碳酸盐胶结物中获得的中心硅藻晶体的光学外观。利用电子显微镜技术对化石结晶体进行了超微结构和矿物学分析,并与酸蚀前后结晶体的宏观和微观光学形貌进行了对比。硅藻化石独特的光学特性与成岩作用下的纳米晶方解石填充了硅藻的乳晕有关。这种填充产生了许多晶体的宏观淡黄色,一种可能与衍射光栅行为有关的微观虹彩,以及微观色环。该结果突出了硅藻晶体独特的过矿化过程,并可能为晶体光学和光子学的新兴研究提供新的补充。
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引用次数: 0
Evolution of eastern passive margin of Adria recorded in shallow- to deep-water successions of the transition zone between the Alps and the Dinarides (Ivanščica Mt., NW Croatia) 亚德里亚东部被动边缘的演化记录在阿尔卑斯山脉和迪纳里德斯山脉过渡带的浅-深水序列中(Ivanščica Mt., NW Croatia)
3区 地球科学 Q1 GEOLOGY Pub Date : 2023-10-01 DOI: 10.1007/s10347-023-00674-7
Matija Vukovski, Duje Kukoč, Tonći Grgasović, Ladislav Fuček, Damir Slovenec
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引用次数: 0
Biohermal complex dominated by microbial carbonates from the early Miaolingian (lower Cambrian) Maozhuang Formation, North China 华北早苗岭期(下寒武统)毛庄组以微生物碳酸盐岩为主的生物热液杂岩
3区 地球科学 Q1 GEOLOGY Pub Date : 2023-09-14 DOI: 10.1007/s10347-023-00673-8
Mingxiang Mei, Muhammad Riaz, Khalid Latif, Ziliang Liu, Mohamed S. Ahmed, Douaa Fathy
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引用次数: 1
Early Cretaceous marine microbiofacies from the South Atlantic Ocean (Sergipe–Alagoas Basin, Brazil): palaeobiogeographical and palaeoceanographical inferences 南大西洋(巴西Sergipe-Alagoas盆地)早白垩世海洋微生物相:古地理和古海洋学推论
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2023-08-21 DOI: 10.1007/s10347-023-00672-9
Fernanda Luft-Souza, G. J. S. Terra, G. Fauth
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引用次数: 1
Modularity explains large-scale reef booms in Earth’s history 模块性解释了地球历史上大规模的珊瑚礁繁荣
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2023-06-22 DOI: 10.1007/s10347-023-00671-w
N. Raja, J. Pandolfi, W. Kiessling
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引用次数: 1
A “cool-water”, non-tropical, mixed volcaniclastic–carbonate ramp from the Early Cretaceous of southern Chile (45°40’S) 智利南部早白垩纪(45°40'S)的“冷水”、非热带、混合火山碎屑-碳酸盐岩斜坡
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2023-06-16 DOI: 10.1007/s10347-023-00669-4
Hermann Rivas, Christian Salazar, W. Stinnesbeck
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引用次数: 0
Palaeoenvironments of an Upper Cretaceous mixed carbonate-siliciclastic shelf of the external Prebetic domain (Valencia, SE Spain) 西班牙东南部巴伦西亚外前世域上白垩统碳酸盐-硅质混合陆架的古环境
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2023-06-13 DOI: 10.1007/s10347-023-00670-x
R. Robles‐Salcedo, V. Vicedo
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引用次数: 0
Paleoenvironmental reconstruction of the Middle Jurassic rocks in western India using benthic foraminifera 利用海底有孔虫重建印度西部中侏罗世岩石的古环境
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2023-06-12 DOI: 10.1007/s10347-023-00668-5
Sreepat Jain, Mohamad Alhussein, M. Ahmed, A. Abdelhady
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引用次数: 0
Facies character and evolution of a mixed carbonate–siliciclastic shelf: Upper Triassic–Lower Jurassic succession in the eastern Northern Calcareous Alps (Stumpfmauer, Austria) 北钙质阿尔卑斯山脉东部上三叠统-下侏罗统混合碳酸盐-硅质陆架的相特征与演化
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2023-06-01 DOI: 10.1007/s10347-023-00662-x
G. Della Porta, Alessandro Mancini, F. Berra
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引用次数: 0
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