美国亚利桑那州上三叠统Chinle组苏铁新羽状叶

Botanical Gazette Pub Date : 1991-03-01 DOI:10.1086/337871
S. Ash
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引用次数: 10

摘要

最近发现的一片上三叠世的树叶显示了许多现存苏铁树叶的特征,并被归入苏铁科。然而,这片叶子的所有特征都与之前描述的任何化石或现存苏铁叶子不匹配,并被分配到一个新的属和种,Aricycas paulae。叶生相反排列的线状披针形羽状花序,顶端尖,基部收缩,羽状花序有突出的中脉和吻合的侧脉,近边缘自由结束。普通表皮细胞呈矩形,侧壁直至略弯曲,有单倍体气孔。这片叶子上的羽片明显是皱巴巴的,在某些情况下,在母叶脱落之前就脱落了,这是现存苏铁的典型特征。这一特征似乎从未在苏铁叶化石中报道过。由于A. paulae是卡尼晚期的,它是已知最古老的苏铁树叶之一,因此支持了Delevoryas(1982)的建议,即有足够的证据表明,具有复叶的植物可能与具有整叶的植物一样产生了苏铁。
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A New Pinnate Cycad Leaf from the Upper Triassic Chinle Formation of Arizona
A recently discovered Upper Triassic leaf shows many of the characters of the leaves of the living cycads and is assigned to the Cycadales. The leaf, however, does not match any previously described fossil or living cycad leaf in all features and is assigned to a new genus and species, Aricycas paulae. The leaf bears oppositely arranged linear-lanceolate pinnae with pointed apices and contracted bases Pinnae contain prominent midribs and anastomosing lateral veins which end freely near the margins. The ordinary epidermal cells are rectangular with straight to slightly curving side walls and haplocheilic stomata. Pinnae in this leaf are apparently wrinkled and shriveled and in some cases fell before the parent leaves were shed, as is typical of the living cycads. It appears that this character has never been reported in fossil cycad leaves. Since A. paulae is Late Carnian age, it is one of the oldest known cycad leaves and thus supports the suggestion by Delevoryas (1982) that there is as much evidence that plants with compound leaves could have given rise to the Cycadales as plants with entire leaves have.
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