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大孢子拉格诺孢(拉格诺孢属 大孢种,池和希尔斯,1976年)的形态学,坎迪利耶等人(1982年),来自玻利维亚石炭纪(密西西比纪早期:杜内阶中上部)。

Morphology of the megaspore Lagenoisporites magnus (Chi and Hills 1976) Candilier et al. (1982), from the Carboniferous (lower Mississippian: mid-upper Tournaisian) of Bolivia.

作者信息

Quetglas Marcela, Macluf Cecilia, Pasquo Mercedes DI

机构信息

Cátedra de Palinología, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Calle 64, 3, B1904DZA La Plata, Buenos Aires, Argentina.

Laboratorio de Palinoestratigrafía y Paleobotánica, Centro de Investigaciones Científicas y Transferencia de Tecnología a la Producción (CONICET-Entre Ríos-UADER), Matteri y España s/n, E3105BWA Diamante, Entre Ríos, Argentina.

出版信息

An Acad Bras Cienc. 2019 Jul 22;91(supp 2):e20180750. doi: 10.1590/0001-3765201920180750.

DOI:10.1590/0001-3765201920180750
PMID:31340218
Abstract

The morphology and structure of megaspores assigned to Lagenoisporites magnus from the Toregua Formation, Retama Group, mid-upper Tournaisian of Bolivia were studied. The analysis was performed with light, fluorescence and scanning electron microscopy. Megaspores were laterally compressed and presented a spherical body with a proximal gula, of the hologula type. Gula had verrucae ornamentation and the spore body presented complex processes consisting of a bulbous base and an internally partitioned projection with sharp apex. In addition to this main ornamentation, perforations were present throughout the spore surface. Megaspores showed well marked curvaturae perfectae due to the abrupt transition existing between the gula ornamentation and the spore body processes. These megaspores were assigned to heterosporous arborescent lycopsids of the Lepidocarpaceae family, as in section view, exospore structure presented a three-dimensional network of fused elements. Likewise, due to a similarity found between sporoderm and Isoetes L. structure, it is evident that megaspores structure has remained intact inside the heterosporous lycopsids. Therefore; the L. magnus structure not only would confirm its affinity with the Lycophyta fossils but also with the living ones.

摘要

对来自玻利维亚杜内阶中上部雷塔马群托雷瓜组的大孢子进行了研究,这些大孢子被归类为大孢叶菌属。分析采用了光学显微镜、荧光显微镜和扫描电子显微镜。大孢子侧向压缩,呈球体,具近端唇,属于全唇型。唇具疣状纹饰,孢子体具复杂的突起,由球状基部和顶端尖锐的内部有隔板的突起组成。除了这种主要纹饰外,孢子表面还布满穿孔。由于唇纹饰和孢子体突起之间存在突然过渡,大孢子呈现出明显的完美曲率。这些大孢子被归类为鳞木科的异孢树状石松类,因为在横切面上,外壁结构呈现出融合元素的三维网络。同样,由于在孢子壁和水韭属结构之间发现了相似性,很明显大孢子结构在异孢石松类植物内部保持完整。因此,大孢叶菌属的结构不仅可以证实其与石松类化石的亲缘关系,也可以证实其与现存石松类植物的亲缘关系。

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