Paleoenvironment and vegetational history of a Middle Pennsylvanian intramontane peat swamp: an example from the Lower Radnice Coal, Kladno coalfield (Czech Republic)

IF 1.8 3区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Stanislav Opluštil, Cortland Eble, Zbyněk Šimůnek, Jana Drábková
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Abstract

The depositional environment, hydrology and vegetational history of the Lower Radnice Coal (Duckmantian) in the Kladno coalfield was studied using sedimentary geology, coal petrology and paleobotanical/palynological methods. The peat accumulating wetland of the coal formed in a fluvial paleovalley approximately 15 km long and 2–5 km wide, bordered by basement paleohighs and landlocked in the interior of the central European Variscides. The peat swamp evolved on top of mud-dominated floodplain successions pedogenically modified to a vertic gleyed Protosol. Probably climatically controlled rising ground water table resulted in paludification that from downstream part gradually spread upstream. Most clastic load was deposited in the upper part of the valley, whereas only mud suspension was dispersed downstream throughout the vegetated swamp. The best conditions for peat accumulation were situated in the eastern part of the paleovalley, where up to 1.5 m thick coal with thin bands of impure coal and carbonaceous mudstone formed in an occasionally inundated rheotrophic system with peat accretion controlled by regional ground water table. The peat swamp was vegetated mainly by lepidodendrid lycopsids with Lepidodendron and Paralycopodites being dominant genera. Shrubby to ground cover vegetation was represented by medulosallean pteridosperms, small shrubby lycopsids, sphenopsids, and herbaceous ferns. Tree ferns were locally abundant, especially in mineral-rich substrates. The rheotrophic character of the peat swamp may indicate higher seasonality of the Variscan interior, compared to coastal areas in the North Variscan foreland with contemporaneous ombrotrophic peats. Modern equivalents of the Lower Radnice Coal swamp are inland planar tropical peat swamps in tributary paleovalleys of the Tasek Bera in peninsular Malaysia and central Congo basins.

Graphical abstract

Lower Radnice Coal peat swamp.

Abstract Image

宾夕法尼亚中期山内泥炭沼泽的古环境和植被史:以克拉德诺煤田(捷克共和国)下拉德尼采煤为例
研究人员采用沉积地质学、煤岩学和古植物学/古风化学方法,对克拉德诺煤田下拉德尼采煤(Duckmantian)的沉积环境、水文和植被历史进行了研究。该煤的泥炭堆积湿地形成于一个长约 15 公里、宽约 2-5 公里的河流古山谷中,与基底古高地接壤,位于中欧瓦里斯基德内陆地区。泥炭沼泽是在以泥浆为主的洪泛平原演替之上演化而成的,这些演替经过了垂直格理原岩的血统改造。可能是气候控制了地下水位的上升,导致泥炭化从下游逐渐向上游蔓延。大部分碎屑沉积在河谷的上游,而只有泥浆悬浮物散布在下游的植被沼泽中。泥炭堆积的最佳条件位于古河谷的东部,这里形成了厚达 1.5 米的煤炭,并带有薄薄的不纯煤带和碳质泥岩,是一个偶尔被淹没的流变系统,泥炭的堆积受区域地下水位的控制。泥炭沼泽的植被主要是鳞毛茄属植物,其中鳞毛茄属植物和鳞毛茄属植物是优势种属。灌木和地被植被主要是髓质翼手目、小灌木状茄科植物、鞘蕨类植物和草本蕨类植物。树蕨类植物在局部地区非常丰富,尤其是在富含矿物质的基质中。泥炭沼泽的流养特征可能表明,与北瓦里斯坦前陆沿海地区同时代的腐生泥炭相比,瓦里斯坦内陆地区的季节性更强。与下拉德尼采煤炭沼泽类似的现代泥炭沼泽是马来西亚半岛和刚果盆地中部塔塞克贝拉河支流古河谷中的内陆平面热带泥炭沼泽。
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来源期刊
International Journal of Earth Sciences
International Journal of Earth Sciences 地学-地球科学综合
CiteScore
4.60
自引率
4.30%
发文量
120
审稿时长
4-8 weeks
期刊介绍: The International Journal of Earth Sciences publishes process-oriented original and review papers on the history of the earth, including - Dynamics of the lithosphere - Tectonics and volcanology - Sedimentology - Evolution of life - Marine and continental ecosystems - Global dynamics of physicochemical cycles - Mineral deposits and hydrocarbons - Surface processes.
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