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Morphology and structure of the pollen cone and pollen grain of the Araucaria species from Argentina

机译:阿根廷南洋杉物种花粉锥和花粉粒的形态结构

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The pollen cone and the pollen grain of the two Argentinean species of Araucaria are described with LM, SEM and TEM. Primordia of pollen cones are formed in April and May and reach maturity by mid-October in A. angustifolia (Bert.) O. Kuntze and by mid-November in A. araucana. (Mol.) K. Koch. Characters of the mature pollen cones and microsporophylls between both taxa are clearly differentiated. Pollen grains are spheroidal-subspberoidal, inaperturate, and asaccate with granulate exine and a subequatorial annular area that corresponds to the sexine thickness. Sculpturing consists of irregularly dispersed granules that are sometimes fused to each other (A. angustifolia) or forming microrugulae (A. araucana). Microgranules and microspinules are also present. The pollen wall ultrastructure is formed by a granular ectexine and lamellated endexine. Granular elements in A. angustifolia are more loosely disposed, form more interstices, and are gradually smaller towards the endexine than in A. araucana. To asses the probable relationships within the family, we compared the pollen grains of the two Araucaria species with those of other extant genera (Agathis, Wollemia) and also with fossil pollen {Araucariacites, Balmeiopsis, Cyclusphaera, Dilwynites) attributed to Araucariaceae.
机译:用LM,SEM和TEM描述了两种南洋杉的花粉锥和花粉粒。花粉锥的原基在四月和五月形成,并在十月中旬在A. angustifolia(Bert。)O. Kuntze中成熟,并在十一月中旬在A. araucana中成熟。 (分子)K。科赫两种类群之间成熟的花粉视锥细胞和微孢子叶素的特征明显不同。花粉粒为球状-亚近孢子状,无孔,不具颗粒状外and和与六边形厚度相对应的赤道以下环形区域。雕刻由不规则分散的颗粒组成,这些颗粒有时会相互融合(A. angustifolia)或形成微皱皮(A. araucana)。也存在微粒和微纺锤体。花粉壁的超微结构是由粒状的艾克西汀和层状的艾迪西恩形成的。相较于A. araucana,A。angustifolia中的颗粒元素更疏松地排列,形成更多的间隙,并且向着内啡肽逐渐变小。为了评估该家族中可能的亲缘关系,我们将两种南洋杉属的花粉粒与其他现存属(Agathis,Wollemia)的花粉粒以及南洋杉科的化石花粉(南洋杉属,Balmeiopsis,Cyclusphaera,Dilwynites)进行了比较。

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