2013
DOI: 10.1016/j.revpalbo.2012.11.007
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New insights and evolutionary significance of the megasporangiate strobilus of Minostrobus chaohuensis (Lycopsida) from the Upper Devonian of South China

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Cited by 21 publications
(22 citation statements)
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“…This stratum includes lower and upper clay layers intercalated with quartz sandstone, which represents the boundary between Devonian and Carboniferous sediments based on spore, plant and invertebrate assemblage [ 9 ]. Specimens in this study are the latest Devonian in age, some of them occur in the same layer with those described by Meng et al [ 7 ], while the others were collected from a higher horizon. No specific permission was required for the field study in the location, and the field study did not involve endangered or protected species.…”
Section: Methodssupporting
confidence: 58%
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“…This stratum includes lower and upper clay layers intercalated with quartz sandstone, which represents the boundary between Devonian and Carboniferous sediments based on spore, plant and invertebrate assemblage [ 9 ]. Specimens in this study are the latest Devonian in age, some of them occur in the same layer with those described by Meng et al [ 7 ], while the others were collected from a higher horizon. No specific permission was required for the field study in the location, and the field study did not involve endangered or protected species.…”
Section: Methodssupporting
confidence: 58%
“…New material was collected from the Fenghuangshan Section, about 3.0 km north of Chaohu City, Anhui Province, China. The specific location of this section (31°37′51″N and 117°50′54″E) was illustrated by Meng et al [ 7 ]. The fossil-bearing bed belongs to the middle part of the Leigutai Member (upper member of the Wutong Formation).…”
Section: Methodsmentioning
confidence: 99%
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“…However, only one species with leaves, assigned to the genus Lepidophylloides, is recorded in the Wuchiapingian, and no species with leaves are known from the Changhsingian. The fertile leaves (sporophylls) of Paleozoic lycopsids show spines, keels, alations, and heels developing in various combinations in different plants (Berry et al, 2003;Meng et al, 2013;Wang et al, 2014b). However, the features of sporophylls require a different character-coding system relative to the taxa considered here, and fall outside the focus of the present paper.…”
Section: Exclusion Of Lycopsidsmentioning
confidence: 93%
“…The cones of two other Devonian genera, which differ markedly from the Barraba cone, are those of Changxingia (Wang et al, 2014) and Minostrobus (Wang, 2001;Meng et al, 2013), both monosporangiate and of Famennian age. The pedicels of their sporophylls possess a keel and a conspicuous heel but, unlike those of the Barraba cone, they are short (less than 5 mm in length) and show distal alations.…”
Section: Comparison With Devonian and Carboniferous Lycopsid Conesmentioning
confidence: 99%