2021
DOI: 10.1016/j.revpalbo.2020.104347
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T0 Early Permian coal-forest preserved in situ in volcanic ash bed in the Wuda Coalfield, Inner Mongolia, China

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Cited by 8 publications
(3 citation statements)
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“…In this paper, a similar physical model of the coal fire was established based on the geological conditions of the Wuda mining area in Inner Mongolia, China. 36 The length, width, and height of the model experimental platform were 2, 0.2, and 1 m, respectively. The length and width represent the strike and dip direction of the model, respectively.…”
Section: Building a Similar Physical Modelmentioning
confidence: 99%
“…In this paper, a similar physical model of the coal fire was established based on the geological conditions of the Wuda mining area in Inner Mongolia, China. 36 The length, width, and height of the model experimental platform were 2, 0.2, and 1 m, respectively. The length and width represent the strike and dip direction of the model, respectively.…”
Section: Building a Similar Physical Modelmentioning
confidence: 99%
“…Lastly, evidence from in situ forests suggests that late Pennsylvanian forests, while taxonomically and vertically heterogeneous, had rather open canopy strata with spatially separated arborescent taxa resulting in little crown overlap (reviewed in DiMichele and Falcon-Lang, 2011, but see Opluštil et al, 2009Opluštil et al, , 2014. In contrast, Cisularian forests show evidence of denser communities, suggestive of more continuous canopy strata (Gulbranson et al, 2012;Wang et al, 2012;Luthardt et al, 2016), although less dense forests also occurred (Gulbranson et al, 2012;Opluštil et al, 2021). It could thus be argued that selective pressure for an aerial locomotion in a continuous canopy was minimal prior to the Cisularian, but this assumption requires further paleoecological studies, especially with respect to canopy density and continuity.…”
Section: Paleoecology Of Weigeltisauridsmentioning
confidence: 99%
“…These have allowed lateral variation in the swamp vegetation at one stratigraphical level to be investigated; for instance, studies at the Štilec and Ovčín localities, about 20 km apart, yielded two contrasting assemblages, representing different stages of vegetation succession (Opluštil et al 2007(Opluštil et al , 2009a(Opluštil et al ,b, 2014Libertín et al 2009a). A similar situation is present in the earliest Permian Wuda ash bed that occurs over an area of more than 60 km 2 , enabling distinct assemblages to be recognised both vertically and laterally (Wang et al 2012;Opluštil et al 2020).…”
mentioning
confidence: 99%