Anomozamites (Bennettitales) from Middle Jurassic Haifanggou Formation, western Liaoning, China

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The Middle Jurassic Hangfanggou Formation is well exposed in Shangsanjiao and Xiasanjiao villages area,Baimashi town of Huludao,western Liaoning,China.Recently,abundant fossil plants were collected from the Hangfanggou Formation.One new species,Anomozamites sanjiaocunensis sp.nov.(Bennettitales),is described in this study.This is the first report of the genus Anomozamites from the Haifanggou Formation based upon the leaf morphology and epidermal structures.The discovery of the new species extends significantly the stratigraphic and geographic distribution of Anomozamites in the Middle Jurassic.It also shows that Anomozamites was a common member of Bennettitales once lived in the Middle Jurassic warm temperate region.The new species also improves the knowledge on understanding the leaf morphology,epidermal features and the diversity of Anomozamites during the Middle Jurassic.The epidermal characters of the new species and its associated plants reveal that the plants grew in a warm and moderately humid environment in the warm temperate zone.The presence of some deciduous plants,such as ginkgoaleans,czekanowskialeans and conifers,indicate the climate with seasonal fluctuations in temperature. The Middle Jurassic Hangfanggou Formation is well exposed in Shangsanjiao and Xiasanjiao villages area, Baimashi town of Huludao, western Liaoning, China.Recently, abundant fossil plants were collected from the Hangfanggou Formation. One new species, Anomozamites sanjiaocunensis sp.nov. (Bennettitales) , is described in this study. This is the first report of the genus Anomozamites from the Haifanggou Formation based upon the leaf morphology and epidermal structures. The discovery of the new species extends significantly the stratigraphic and geographic distribution of Anomozamites in the Middle Jurassic. It also shows that anomozamites was a common member of Bennettitales once lived in the Middle Jurassic warm temperate region. The new species also improves the knowledge on understanding the leaf morphology, epidermal features and the diversity of Anomozamites during the Middle Jurassic. epidermal characters of the new species and its associated plants reveal that the plants grew in a warm and m oderately humid environment in the warm temperate zone. the presence of some deciduous plants, such as ginkgoaleans, czekanowskialeans and conifers, indicate the climate with seasonal fluctuations in temperature.
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