来自捷克皮尔森盆地和加拿大悉尼煤田的宾夕法尼亚martialean蕨“Pecopteris”Polypodioides (C. Presl in Sternberg)的角质层

J. Pšenička, E. Zodrow
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引用次数: 2

摘要

宾夕法尼亚蕨类化石的角质层是众所周知的难以提取,在古植物学文献中很少发现,但它们可以提供重要的分类/系统、植物地层学和古环境信息。来自捷克共和国和加拿大煤盆地的“Pecopteris”polypodioides的角质层证明了这一点。“Pecopteris”polypodioides是一种武生树蕨,是泥炭形成植物群的一部分,生长在潮湿的环境中。由于这个事实,角质层通常很薄,我们认为它们的主要功能是减少真菌孢子发芽和细菌生长的能力,从而减少这些物质引起疾病的可能性。第二个功能是作为一个主要的屏障,以防止水分流失和降低小叶的润湿性。
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Cuticles from Pennsylvanan Marattialean Fern “Pecopteris” Polypodioides (C. Presl in Sternberg) Němejc from Pilsen Basin (Czech Republic) and Sydney Coalfield (Canada)
Abstract Pennsylvanian fossil-fern cuticles are notoriously difficult to extract, little can be found in the palaeobotanical literature, yet they can supply significant taxonomic/systematic, phytostratigragphic, and palaeoenvironment information. This is demonstrated for cuticles from “Pecopteris” polypodioides of the coal basins in the Czech Republic and Canada. “Pecopteris” polypodioides is a marattialean tree fern which was part of the peat-forming flora, growing in a wet environment. Due to this fact, cuticles are generally very thin, and we assume that their major function was to reduce the ability of fungal spores to germinate and bacterial to grow, thereby reducing the possibility of these agents to cause disease. The secondary function was to be a major barrier to water loss and reducing the wettability of pinnules.
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