New insights into the heterosporous lycopsid <Emphasis Type="Italic">Changxingia</Emphasis> from the Upper Devonian Wutong Formation of Zhejiang Province,China |
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Authors: | Email author" target="_blank">De-Ming?WangEmail author Min?Qin Mei-Cen?Meng Le?Liu David?K?Ferguson |
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Institution: | 1.Key Laboratory of Orogenic Belts and Crustal Evolution, Department of Geology,Peking University,Beijing,China;2.Science Press, China Science Publishing and Media Ltd.,Beijing,China;3.School of Geoscience and Surveying Engineering,China University of Mining and Technology (Beijing),Beijing,China;4.Department of Palaeontology,University of Vienna,Vienna,Austria |
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Abstract: | A heterosporous lycopsid plant is described from the Upper Devonian (Famennian) Wutong Formation, Changxing County, northern Zhejiang Province, China. The plant is known for its terminal and many detached megasporangiate strobili, most of which do not have sporophylls preserved. Some megasporangiate strobili are closely associated with a vegetative axis bearing leaf cushions and with a mass of microspores. Because of the monosporangiate strobili, the present lycopsid belongs to the Dichostrobiles of the Isoёtales sensu lato. This lycopsid conforms to Changxingia in the vegetative leaves, leaf cushions (including leaf scar and ligule pit), some parts of the megasporophyll (pedicel, heel and lamina), the megasporangium and the megaspores, although the branching pattern of axes, the arrangement and other parts of megasporophyll are still unknown. The fossils are described as Changxingia sp., and this genus is expanded with character of microspore. Hence, the previous and present data indicate that the earliest lycopsids with monosporangiate strobili from the Upper Devonian of China are consistent in Lagenicula megaspores with gula and Lycospora microspores with equatorial cingulum. In contrast, the Carboniferous lycopsids with monosporangiate strobili in Euramerica and Cathaysia show great diversification of both megaspores and microspores. |
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