2015
DOI: 10.1371/journal.pone.0124039
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Reanalysis of Wupus agilis (Early Cretaceous) of Chongqing, China as a Large Avian Trace: Differentiating between Large Bird and Small Non-Avian Theropod Tracks

Abstract: Trace fossils provide the only records of Early Cretaceous birds from many parts of the world. The identification of traces from large avian track-makers is made difficult given their overall similarity in size and tridactyly in comparison with traces of small non-avian theropods. Reanalysis of Wupus agilis from the Early Cretaceous (Aptian-Albian) Jiaguan Formation, one of a small but growing number of known avian-pterosaur track assemblages, of southeast China determines that these are the traces of a large … Show more

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Cited by 17 publications
(18 citation statements)
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(24 reference statements)
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“…Xing et al [ 6 ] gave the first detailed description of the Pteraichnus tracks and evaluation of their paleoecological significance. Xing et al [ 4 ] reviewed Wupus agilis from the Lotus tracksite. Wupus , originally identified as the trace of a small non-avian theropod track-maker [ 2 ], is now considered to be the track of a large avian and referred to the ichnofamily Limiavipedidae.…”
Section: History Of Researchmentioning
confidence: 99%
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“…Xing et al [ 6 ] gave the first detailed description of the Pteraichnus tracks and evaluation of their paleoecological significance. Xing et al [ 4 ] reviewed Wupus agilis from the Lotus tracksite. Wupus , originally identified as the trace of a small non-avian theropod track-maker [ 2 ], is now considered to be the track of a large avian and referred to the ichnofamily Limiavipedidae.…”
Section: History Of Researchmentioning
confidence: 99%
“…The lithological association of the Jiaguan Formation consists of massive sandstones intercalated with thinner mudstone intervals, exposed at the Lotus site in an impressive near-vertical cliff face. The track-and wrinkle structure-bearing levels first occur in dark purple redquartz sandstone in the lower part of the Jiaguan Formation about 30–40 m above the base of the unit [ 2 , 4 , 6 ]. The beds are near-horizontal with the result that notches have been eroded horizontally into the steep vertical cliff faces by removal of the soft siltstones and mudstones.…”
Section: Geological Settingmentioning
confidence: 99%
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