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首页> 外文期刊>Sbornik Narodniho Muzea v Praze, Rada B. Prirodovedecka >FIMMENITE AUS DEM MITTELEOZAN DES GEISELTALES
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FIMMENITE AUS DEM MITTELEOZAN DES GEISELTALES

机译：辉石中欧亚岩中的铁矾

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摘要

Fimmenits from the Middle Eocene of Geiseltal. Pollen agglomerates called fimmenits collected during previous micropaleobota-nical research in 1930s from the Middle Eocene coal deposits of Geiseltal are discussed. They may have originated as remains of flowers(pollen sacs), or accumulations by insects, but not by currents or wind transport during the deposition. Various kinds of pollen agglomera-tes differ by prevailing types of plant groups they are constituted - Ericaceae-, Spotaceae-, T. willrathae-, and Myrtaceae-dominated as wellas mixed agglomerates have been distinguished as main types. Some include masses of otherwise rare or extremely rare pollen, e.g. of thewillrathae or abbreviatus groups. Some pollen forms have not been so far known in Geiseltal at all. The microfossils in fimmenits have beenembedded into preparations without maceration and consequently they preserved in some cases very fine structures, namely intine. Mostsamples come from the upper Middle Coal (pollen subzone SPP 15C) of the former mines Cecilie and Leonhard. The fimmenit agglomera-tes yielded much more differentiated pollen assemblages than the so far known flora of Geiseltal attests. A more detailed taxonomical ana-lysis of the material will be incorporated in a monograph of the Geiseltal microflora in the future.
机译：来自盖世塔尔中始新世的影像。讨论了在1930年代以前的微古植物学研究中从Geiseltal中始新世煤矿床中收集的花粉团聚体。它们可能起源于花的残留物（花粉囊），或者是由昆虫积累的，而不是沉积过程中的洋流或风的传播。不同种类的花粉团聚体因其构成的主要植物群而异-蓖麻科，斑点科，柳枝T和桃金娘科为主以及混合团聚体已被区分为主要类型。一些包括其他稀有或极其稀少的花粉，例如大块的花粉。 willrathae或abbreviatus组中的一个。到目前为止，Geiseltal尚不了解某些花粉形式。芬尼特中的微化石已被嵌入制剂中而没有浸软，因此在某些情况下它们保留了非常精细的结构，即intine。大多数样品来自前矿Cecilie和Leonhard的上部中煤层（花粉分区SPP 15C）。与迄今已知的盖瑟尔特尔证明的菌群相比，纤细的团聚体产生了分化得多的花粉组合。将来，该材料的更详细的分类学分析将纳入Geiseltal菌群专论中。

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