Occurrence of the earliest gigantopterid from the basal Permian of the North China Block and its bearing on evolution
Occurrence of the earliest gigantopterid from the basal Permian of the North China Block and its bearing on evolution
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华北地块基底二叠系最早的巨蕨类植物的出现及其对演化的影响
DOI:
10.1002/gj.2907
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发表时间:
--
影响因子:
1.8
通讯作者:
Jun Wang
中科院分区:
文献类型:
--
作者:
Weiming Zhou;Mingli Wan;Rebecca A. Koll;Jun Wang
Gigantopterids are a morphological group consisting of a number of enigmatic fossil plants with angiosperm‐like leaves and reticulate venation that are of uncertain systematic affinity. Gigantopterid plants were abundant and a characteristic floral element in the Late Palaeozoic Cathaysian floras. However, in China, their oldest occurrence was much later than that in North America (Artinskian) and Indonesia (Asselian to Sakmarian). Here, we document the gigantopteridGigantonocleacf.mirafrom basal Permian (Asselian) strata in the North China Block that represents the oldest unequivocal evidence for the gigantopterids. The foliage is characterized by complex venation composed of four orders, small isodiametric meshes, and intercalary subsidiary veins arising directly from the rachis, being a distinctive morphological type of leaf venation. In addition, a nonmarginal feeding trace is detected on the lamina, extending the earliest record of plant–animal interaction between gigantopterid plants and arthropods to the earliest Permian. Our new observations show that the venation characters ofGigantonoclea miraandGigantonocleacf.miramore closely resembleGigantopteris dictyophylloidesthan other members of gigantopterids including the evolutionaryCallipteridiumsequence to which it was previously assigned.