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Palaeozoic stromatoporoids and chaetetids analysed using electron backscatter diffraction (EBSD); implications for original mineralogy and microstructure 利用电子背散射衍射(EBSD)分析古生代叠孔虫和毛纲对原始矿物学和微观结构的影响
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2021-01-01 DOI: 10.1007/s10347-020-00618-5
U. Balthasar, S. Kershaw, A. Silva, Barbara Seuss, M. Cusack, Kilian Eichenseer, P. Chung
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引用次数: 2
Late Pennsylvanian carbonate platform facies and coral reef: new insights from southern China (Guizhou Province). 晚宾夕法尼亚期碳酸盐岩台地相与珊瑚礁:中国南方(贵州)的新认识。
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2021-01-01 Epub Date: 2020-11-10 DOI: 10.1007/s10347-020-00613-w
Marine Maillet, Wen-Tao Huang, Xiao Li, Zhen-Yuan Yang, Chang-Qing Guan, Yong-Li Zhang, En-Pu Gong, Katsumi Ueno, Elias Samankassou

The Pennsylvanian is characterized by intense paleoenvironmental changes related to glacio-eustatic sea-level fluctuations and major tectonic events, which affected the evolution of biocommunities. Most known Pennsylvanian tropical reefs and mounds are predominantly composed of calcareous algae (e.g. phylloid algae, Archaeolithophyllum), calcareous sponges, fenestrate bryozoans, Tubiphytes, and microbialites. However, in Houchang (southern China), the Late Pennsylvanian carbonate platform records a large coral reef lacking any analogs in age (Gzhelian), size (80-100 m thick) and composition (high biodiversity). The large coral reef developed at the border of the Luodian intraplatform basin. The intraplatform basin is characterized by the deposition of green algal grainstone, coated grain grainstone and bioclastic packstone, grainstone, floatstone and rudstone in shallow-waters. In the deep-water shelf, lithofacies are composed of burrowed bioclastic wackestone, microbioclastic peloidal packstone, grainstone, and fine-grained burrowed wackestone and packstone. In this context, the coral reef developed on a deep-shelf margin, in a moderate to low energy depositional environment, below the FWWB. The scarcity of Pennsylvanian coral reefs suggests global unfavorable conditions, which can be attributed to a complex pattern of several environmental factors, including seawater chemistry (aragonite seas), paleoclimatic cooling related to continental glaciation, and the biological competition with the more opportunistic and adaptive phylloid algal community that occupied similar platform margin paleoenvironments. The existence of the large Bianping coral reef in southern China, as well as a few additional examples of Pennsylvanian coralliferous bioconstructions, provides evidence that coral communities were able to endure the Late Paleozoic fluctuating paleoenvironmental conditions in specific settings. One of such settings appears to have been the deep shelf margin, where low light levels decreased competition with the phylloid algal community.

宾夕法尼亚纪具有强烈的古环境变化特征,这些变化与冰川-海平面上升和重大构造事件有关,影响了生物群落的演化。大多数已知的宾夕法尼亚热带珊瑚礁和土丘主要由钙质藻类(如phylloid藻类,Archaeolithophyllum),钙质海绵,窗状苔藓虫,管生动物和微生物组成。然而,在中国南方的后昌,晚宾夕法尼亚期碳酸盐岩台地记录了一个在年龄(Gzhelian)、大小(80-100 m厚)和组成(高生物多样性)上没有任何类似的大型珊瑚礁。罗甸地台内盆地边缘发育大型珊瑚礁。台内盆地以绿藻纹岩、包覆纹岩、生物碎屑包覆岩、浅水纹岩、浮石、硬砂岩沉积为特征。在深水陆架中,岩相主要由穴形生物碎屑碎屑岩、微生物碎屑碎屑碎屑碎屑岩、颗粒岩、细粒穴形碎屑岩和碎屑岩组成。在此背景下,珊瑚礁发育在深水陆架边缘,处于中低能沉积环境中。宾夕法尼亚珊瑚礁的稀缺表明全球不利条件,这可归因于多种环境因素的复杂模式,包括海水化学(文石海),与大陆冰川相关的古气候冷却,以及与占据类似台地边缘古环境的更具机会主义和适应性的叶状藻类群落的生物竞争。中国南方大型汴平珊瑚礁的存在,以及宾夕法尼亚珊瑚系生物构造的一些例子,提供了珊瑚群落在特定环境下能够承受晚古生代波动的古环境条件的证据。其中一种环境似乎是深陆架边缘,那里的低光照水平减少了与叶状藻类群落的竞争。
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引用次数: 6
Palaeoecological analysis of maximum flooding zones from the Tithonian (Upper Jurassic) of the Kachchh Basin, western India 印度西部Kachchh盆地Tithonian(上侏罗纪)最大洪水带的古生态分析
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2020-12-24 DOI: 10.1007/s10347-020-00617-6
F. Fürsich, Matthias Alberti, D. Pandey
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引用次数: 6
Development of coral–sponge–microbialite reefs in a coated grain-dominated carbonate ramp (Upper Jurassic, eastern Sardinia, Italy) 意大利撒丁岛东部上侏罗统包覆颗粒为主的碳酸盐斜坡中珊瑚-海绵-微生物岩礁的发育
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2020-12-24 DOI: 10.1007/s10347-020-00616-7
M. Nembrini, G. Della Porta, F. Berra
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引用次数: 3
A wet climatic terrestrial carbonate record in the middle-upper Pleistocene, north Tunisia 突尼斯北部更新世中上段陆相碳酸盐岩湿气候记录
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2020-11-12 DOI: 10.1007/s10347-020-00612-x
I. Armenteros, Naoufel Ghannem
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引用次数: 3
Petrofacies and taphofacies analyses of coquinas as a tool for the establishment of a stratigraphic evolution model of the Morro do Chaves Formation (Sergipe-Alagoas Basin, NE Brazil) 作为建立Morro do Chaves组(Sergipe-Alagoas盆地,巴西东北部)地层演化模型的工具,coquinas的岩相和分相分析
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2020-11-12 DOI: 10.1007/s10347-020-00614-9
G. Garcia, M. Henriques, Antônio Jorge Vasconcellos Garcia, M. Dantas
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引用次数: 3
Early Miocene (Burdigalian) marine rocky shores in the French Jura Massif: a palaeoecological and palaeoenvironmental analysis 法国侏罗地块早中新世海相岩岸:古生态和古环境分析
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2020-10-29 DOI: 10.1007/s10347-020-00610-z
J. Martinell, J. Juilleret, R. Domènech
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引用次数: 1
The “Rzehakia beds” on the northern shelf of the Pannonian Basin: biostratigraphic and palaeoenvironmental implications 潘诺尼亚盆地北部陆架上的“Rzehakia层”:生物地层学和古环境意义
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2020-10-24 DOI: 10.1007/s10347-020-00609-6
Andrej Ruman, S. Ćorić, E. Halásová, M. Harzhauser, N. Hudáčková, Michal Jamrich, Marcus Palzer-Khomenko, Mathias Kranner, O. Mandic, S. Rybár, V. Šimo, Michal Šujan, M. Kováč
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引用次数: 3
Diagenesis and reservoir characteristics of the Lithocodium–Bacinella facies in a Lower Cretaceous reservoir, eastern Persian Gulf Basin 波斯湾盆地东部下白垩统储层岩性-Bacinella相成岩作用及储层特征
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2020-09-03 DOI: 10.1007/s10347-020-00608-7
B. Esrafili-Dizaji, E. Hajikazemi, M. Dalvand, Morteza Hassanzadeh Nemati, R. Swennen
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引用次数: 3
New contributions to the palaeoenvironmental framework of the Los Molles Formation (Early-to-Middle Jurassic), Neuquén Basin, based on palynological data 基于孢粉学资料对neuquimassn盆地早-中侏罗世Los Molles组古环境格架的新贡献
IF 1.8 3区 地球科学 Q1 GEOLOGY Pub Date : 2020-08-12 DOI: 10.1007/s10347-020-00607-8
D. Olivera, M. Martínez, C. Zavala, J. E. Di Nardo, Germán Otharán
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引用次数: 5
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