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椭圆斜羽叶的解剖研究及斜羽叶的系统分类位置 被引量:2

THE ANATOMICAL STUDY OF PLAGIOZAMITES OBLONGIFOLIUS AND THE SYSTEMATIC POSITION OF PLAGIOZAMITES
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摘要 本文根据对椭圆斜羽叶(Plagiozamites oblongifolius)钙质石化化石的研究,认为其主要特征如下:羽状复叶,叶肉无海绵组织和栅栏组织分化。羽片叶脉维管束外韧式,木质部外始式,与现代苏铁属叶脉特征相近。羽轴维管束为“U”形,外始式木质部、梯状纹孔管胞,与现代苏铁属的羽轴维管束相似。根据上述特征,目前可将斜羽叶属归入原始苏铁类植物。但是,如果斜羽叶的生殖器官同 Noeggerathia 一样,为异孢型孢子囊穗,则斜羽叶可能为一种与苏铁类起源有关的原裸子植物。 The specimens of petrified fossil plant,Plagiozamites oblongifolius,described here,were collected from the sandstone of Late Permian of Western Guizhou,China.Their morphological as well as the internal anatomical characters were preserved.All of the samples were treated with hydrochloric acid and made into peels and thin sections.The main internal anatomical ch- aracters are as follows:The mesophyll of pinna is not differentiated into spongy and palisade tissue.The phloem of the pinna vein is ectophloic and the xylem of which is exarch.The trach- eids are annular,helical and scalariform thickening.The vein is surrounded by the transfusion tissue which consists of parenchymous cells and short tracheids.In the transverse section of ra- chis,the vascular bundle is in“U”shape.It has amphiphloic siphonostele with exarch xylem. The protoxylem consists of small tracheids with spiral or annular thickened walls,and the me- taxylern,with scalariform or transitional type of scalariform and pitting thickening.The stru- cture of vascular bundles of the pinna and the rachis is similar to that of Cycas (Fig.I,2). The systematic position of Plagiozamites has been disputed for a long time.However, based on the morphological and anatomical characters of Plagiozarnites,they might be belonged to cycadophytes.If the fructifications of Plagiozamites are considered as the same type as that of Noeggerathia,Plagiozamites should be a kind of progymnosperms.
出处 《Acta Botanica Sinica》 CSCD 1990年第10期799-804,共6页 Acta Botanica Sinica(植物学报:英文版)
关键词 椭圆斜羽叶 解剖 分类 Plagiozamites oblongifolius Anatomical characters Systematic position
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参考文献4

  • 1杨关秀,广东晚二叠世含煤地层和古生物群.古植物部分,1980年
  • 2团体著者,黔西滇东晚二叠纪含煤地层和古生物群,1980年
  • 3团体著者,中国古生代植物,1974年
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同被引文献11

  • 1王士俊,田宝霖.太原西山煤田一种新的科达根及其生态意义[J].煤田地质与勘探,1993,21(6):7-11. 被引量:4
  • 2桑树勋,刘焕杰,施健.海南岛红树植物的解剖生态研究及其地质意义[J].煤田地质与勘探,1993,21(3):1-6. 被引量:4
  • 3姚兆奇 李成栋 等.龙潭组的定义和时代[J].地层学杂志,1984,8(3):199-214.
  • 4杨关秀.豫西禹县二叠纪大羽羊齿类的演化及其地质意义[J].现代地质,1987,1(2):173-195,1.
  • 5骆善胜.长广煤田C煤层海相成煤的初步认识[J].煤炭学报,1980,(1):26-36.
  • 6韩德馨 任德贻 等.浙江长广煤田树皮残植煤的成因及其沉积环境[J].沉积学报,1983,1(4):1-14.
  • 7李星学 姚兆奇.中国南部二叠纪含煤地层[J].地层学杂志,1980,4(4).
  • 8张正坤.中朝地块与扬子地块在古生代晚期是太平洋古陆的一部分[J].中国地质科学院院报,1984,(9):45-54.
  • 9谌建国 李有亮.广西上二叠统含煤建造和藻坪沼泽成煤模式[J].沉积学报,1983,1(1):86-93.
  • 10田宝霖,王士俊.山西煤核中科达茎Shanxioxylon sinense和Pennsylvanioxylon tianii的初生维管系统的研究[J]古生物学报,1988(01).

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