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Miocene carpological floras of the Konin region (Central Poland)

机译:Konin地区(波兰中部)的中新世鲤科植物区系

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Carbonaceous, three-dimensionally preserved macroscopic plant remains from the Lubstów, Gos?awice and P?tnów brown coal open-pit mines are described and illustrated, providing a comprehensive elaboration of the middle Miocene carpological floras of the Konin region. The diaspores represent the following families: Pinaceae, Sciadopityaceae, Cupressaceae, Annonaceae, Cabombaceae, Nymphaeaceae, Araceae, Typhaceae, Cyperaceae, Vitaceae, Rosaceae, Rhamnaceae, Fagaceae, Myricaceae, Cornaceae, Nyssaceae, Symplocaceae, Ericaceae, Araliaceae, and Adoxaceae. Forty-two species were recognised or documented for the first time in the Konin region. Two genera, three species and three morphotypes are described as new taxa. Most of these plant remains represent azonal vegetation. Ericaceous bogs, pine bogs and mixed coniferous bogs, accompanied by Gyptostrobus swamp forests and various aquatic plant communities, are suggested as the most widespread vegetation types. Remains representing mesophytic, zonal vegetation, resembling extant evergreen broad-leaved and mixed mesophytic forests, are sparse. A Sciadopitys raised bog, a mixed coniferous bog subtype, was one of the important biomass sources forming the brown coal of the I-Middle Polish seam group. Other bog types recognised in Lubstów presumably also played a part in this process. Wildfire is suggested as an important factor controlling the Miocene vegetation of the Konin region. The floristic composition and lithostratigraphy indicate the Badenian age (16.3–12.8 Ma) for the studied floras, but radiometric data suggest that two Lubstów floras are older and one is younger than 13.6 Ma. Biostrati-graphically, Lubstów floras were correlated with the Klettwitz – Salzhausen floristic complex. Based on several climatic indicators and biostratigraphic correlation, the climate is estimated to have been humid, warm-temperate or subtropical. The upper Miocene lower Rhenish Basin floras are the most comparable in floristic and plant communities’ composition. Tropical – subtropical, Mediterranean and extinct genera represent approximately 40% of the genera identified in Lubstów.
机译:描述并举例说明了从Lubstów,Gos?awice和P?tnów褐煤露天矿得到的碳质三维保存的宏观植物残骸,对科宁地区中新世中古植物区系进行了全面阐述。硬生孢子代表以下科:松科,桔梗科,柏科,番荔枝科,Cabombaceae,Nymphaeaceae,天南星科,香蒲科,莎草科,葡萄科,蔷薇科,鼠李科,山毛菜科,杨梅科,山茱ace科,菊科,交科,莎草科,交科。在科宁地区首次识别或记录了42种。两个属,三个物种和三个形态型被描述为新的分类单元。这些植物残骸大部分代表了地带性植被。建议将云杉沼泽,松树沼泽和针叶混交沼泽,以及短尾蛇沼泽森林和各种水生植物群落作为最广泛的植被类型。剩余的代表中生的,地带性的植被稀疏,类似于现存的常绿阔叶混交林。 Sciadopitys凸起的沼泽是一种混合的针叶沼泽亚型,是形成I-中波兰煤层组褐煤的重要生物量来源之一。大概在拉布斯托(Lubstów)中发现的其他沼泽类型也参与了这一过程。建议将野火作为控制Konin地区中新世植被的重要因素。植物区系组成和岩石地层学特征表明所研究的植物区系的巴登尼亚年龄(16.3-12.8 Ma),但放射线数据显示,两个Lubstów植物区系年龄较大,其中一个比13.6 Ma还年轻。从地层学上讲,Lubstów植物区系与Klettwitz-Salzhausen植物区系相关。根据一些气候指标和生物地层学相关性,估计气候为潮湿,温带或亚热带。中新世上层Rhenish盆地下部植物区系在植物区系和植物群落组成方面可比性最高。热带–亚热带,地中海和绝种属约占Lubstów属的40%。

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