Specialised emission pattern of leaf trace in a late Permian (253 million-years old) conifer.
Specialised emission pattern of leaf trace in a late Permian (253 million-years old) conifer.
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二叠纪晚期(2.53 亿年)针叶树叶迹的特殊发射模式
DOI:
10.1038/srep12405
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发表时间:
2015-07-22
影响因子:
4.6
通讯作者:
He XY
中科院分区:
文献类型:
--
作者:
Wei HB;Feng Z;Yang JY;Chen YX;Shen JJ;He XY
Leaf traces are important structures in higher plants that connect leaves and the stem vascular system. The anatomy and emission pattern of leaf traces are well studied in extant vascular plants, but remain poorly understood in fossil lineages. We quantitatively analysed the leaf traces in the late Permian coniferNingxiaites specialisfrom Northwest China based on serial sections through pith, primary and secondary xylems. A complete leaf traces emission pattern of a conifer is presented for the first time from the late Palaeozoic. Three to five monarch leaf traces are grouped in clusters, arranged in a helical phyllotaxis. The leaf traces in each cluster can be divided into upper, middle and lower portions and initiate at the pith periphery and cross the wood horizontally. The upper leaf trace increases its diameter during the first growth increment and then diminishes completely, which indicates leaf abscission at the end of the first year. The middle trace immediately bifurcates once or twice to form two or three vascular bundles. The lower trace persists as a single bundle during its entire length. The intricate leaf trace dynamics indicates this fossil plant had a novel evolutionary habit by promoting photosynthetic capability for the matured plant.