Middle Jurassic Flora and palaeoenvironmental reconstruction of the Kamala Formation in Rybinsk Formational Zone, the Kansk Coal Basin, Siberia

IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Review of Palaeobotany and Palynology Pub Date : 2024-04-16 DOI:10.1016/j.revpalbo.2024.105113
Anatolii Muraviev , Jiří Kvaček
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Abstract

The Kansk Basin is one of the biggest reserves of brown coal in Russia. Jurassic coal-containing terrestrial deposits bearing plant remains crop out in several localities. This work is focused on five fossil-plant-containing localities in the Middle Jurassic Kamala Formation of the Kansk Basin within the Rybinsk Formational Zone. The studied material comprises 29 plant morphospecies. They are assigned to: Pteridophytes (Equisetites, Coniopteris, Cladophlebis and Raphaelia), Bennettitales (cf. Pterophyllum), Ginkgoales (Ginkgoites, Sphenobaiera and Eretmophyllum), Leptostrobales (Czekanowskia and Phoenicopsis) and Coniferales (Pityophyllum). There are several plants remains of uncertain systematic position, such as roots (Radicites sp.), cones and fossil wood. As a result, palaeoenvironmental interpretation was implemented; three taphonomic units were distinguished utilising complex palaeobotanical, lithofacial analyses, and literature-based data. Palaeoecological analysis identified three depositional environments with corresponding type of vegetation: a) periodically flooded alluvial plain dominated by Czekanowskia-Phoenicopsis; b) swamp-semiaquatic dominated by Equisetites, Coniopteris, Cladophlebis and Phoenicopsis; c) slope and upland vegetation dominated by Sphenobaiera, Ginkgoites, Eretmophyllum and Pityophyllum.

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西伯利亚坎斯克煤炭盆地雷宾斯克构造带卡马拉地层中侏罗纪植物区系和古环境重建
坎斯克盆地是俄罗斯褐煤储量最大的地区之一。侏罗纪含煤陆相沉积中有多处植物遗迹。这项研究的重点是雷宾斯克地层区内坎斯克盆地中侏罗世卡马拉地层中的五个含有植物化石的地点。所研究的材料包括 29 个植物形态种。它们被归入翼手目(Equisetites、Coniopteris、Cladophlebis 和 Raphaelia)、Bennettitales(参见 Pterophyllum)、Ginkgoales(Ginkgoites、Sphenobaiera 和 Eretmophyllum)、Leptostrobales(Czekanowskia 和 Phoenicopsis)和 Coniferales(Pityophyllum)。还有一些植物遗迹的系统位置不确定,如根(Radicites sp.)、球果和木化石。因此,对其进行了古环境解释;利用复杂的古植物学、岩相分析和基于文献的数据,区分出三个岩石学单元。古生态学分析确定了三种沉积环境以及相应的植被类型:a) 周期性泛滥的冲积平原,以 Czekanowskia-Phoenicopsis 为主;b) 沼泽-半沼泽,以 Equisetites、Coniopteris、Cladophlebis 和 Phoenicopsis 为主;c) 斜坡和高地植被,以 Sphenobaiera、Ginkgoites、Eretmophyllum 和 Pityophyllum 为主。
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来源期刊
CiteScore
3.50
自引率
21.10%
发文量
149
审稿时长
6 months
期刊介绍: The Review of Palaeobotany and Palynology is an international journal for articles in all fields of palaeobotany and palynology dealing with all groups, ranging from marine palynomorphs to higher land plants. Original contributions and comprehensive review papers should appeal to an international audience. Typical topics include but are not restricted to systematics, evolution, palaeobiology, palaeoecology, biostratigraphy, biochronology, palaeoclimatology, paleogeography, taphonomy, palaeoenvironmental reconstructions, vegetation history, and practical applications of palaeobotany and palynology, e.g. in coal and petroleum geology and archaeology. The journal especially encourages the publication of articles in which palaeobotany and palynology are applied for solving fundamental geological and biological problems as well as innovative and interdisciplinary approaches.
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