2011
DOI: 10.1017/s001675681100077x
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Lochkovian plants from the Xitun Formation of Yunnan, China, and their palaeophytogeographical significance

Abstract: A megafossil plant assemblage containing three zosterophyll plants (Gen. nov. A, aff. Huia sp. and a unnamed spike) is described from the Lower Devonian Xitun Formation (Lochkovian) of Qujing, Yunnan Province, China, providing new data on the diversity of plant types during the Lochkovian, a time poorly represented by fossil vascular plants. Gen. nov. A has a character combination of naked axes, a diagnostic branching pattern (i.e. K-type branching as well as small lateral branches scattered along the axes) an… Show more

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Cited by 21 publications
(16 citation statements)
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“…The specimens come from a locality south of the Shangxishan Reservoir, near Qujing city, Yunnan, China (25°30.43′79″N 103°42.12′71″E; see Fig. 1 of Xue ), from the lower part of the Xishancun Formation, a thin bed of greenish grey mudstone in which axes of the marine dasycladalean alga Uncatoella verticillata have also been found. The specimens are in a fine sandy matrix with abundant plant remains; eurypterid fragments were also collected along with the specimens described here.…”
Section: Methodsmentioning
confidence: 99%
“…The specimens come from a locality south of the Shangxishan Reservoir, near Qujing city, Yunnan, China (25°30.43′79″N 103°42.12′71″E; see Fig. 1 of Xue ), from the lower part of the Xishancun Formation, a thin bed of greenish grey mudstone in which axes of the marine dasycladalean alga Uncatoella verticillata have also been found. The specimens are in a fine sandy matrix with abundant plant remains; eurypterid fragments were also collected along with the specimens described here.…”
Section: Methodsmentioning
confidence: 99%
“…The Xishancun, Xitun, Guijiatun and Xujiachong formations (in ascending chronological order) represent the Early Devonian non-marine strata in Qujing District ( Liu & Wang, 1973 ; P’an et al, 1978 ; Zhu, Wang & Fan, 1994 ; Liu, Gai & Zhu, 2018 ). The Xitun Formation consists mainly of grayish-green muddy limestone and mudstone ( Fang et al, 1985 ; Xue, 2012 ), yielding a rich biota (Cuifengshan Assemblage) characterized by the diversification of sarcopterygians ( Chang & Yu, 1981 ; Chang & Yu, 1984 ; Zhu, Yu & Janvier, 1999 ; Zhu, Yu & Ahlberg, 2001 ; Zhu & Yu, 2002 ) and primitive antiarchs including Yunnanolepis, Parayunnanolepis , Zhanjilepis , Chuchinolepis and Phymolepis . Other fishes in the Xitun Formation include the endemic agnathans ( Liu et al, 2015 ), arthrodires ( Dupret, Zhu & Wang, 2017 ), actinopterygians ( Zhu et al, 2006 ; Lu et al, 2016 ), acanthodians and chondrichthyans, the latter two of which are mostly known from microvertebtrate remains ( Wang, 1984 ).…”
Section: Methodsmentioning
confidence: 99%
“…Other fishes in the Xitun Formation include the endemic agnathans ( Liu et al, 2015 ), arthrodires ( Dupret, Zhu & Wang, 2017 ), actinopterygians ( Zhu et al, 2006 ; Lu et al, 2016 ), acanthodians and chondrichthyans, the latter two of which are mostly known from microvertebtrate remains ( Wang, 1984 ). The Xitun Formation has been dated as late Lochkovian (c. 410–415 million years ago) with evidence from fossil assemblages ( Gao, 1981 ; Fang et al, 1994 ; Zhao et al, 2011 ; Xue, 2012 ).…”
Section: Methodsmentioning
confidence: 99%
“…The Xishancun, Xitun, Guijiatun and Xujiachong formations (in ascending chronological order) represent the Early Devonian non-marine strata in Qujing District (Liu & Wang, 1973;P'an et al, 1978;Zhu, Wang & Fan, 1994;Liu, Gai & Zhu, 2018). The Xitun Formation consists mainly of grayish-green muddy limestone and mudstone (Fang et al, 1985;Xue, 2012), yielding a rich biota (Cuifengshan Assemblage) characterized by the diversification of sarcopterygians (Chang & Yu, 1981;Chang & PeerJ reviewing PDF | (2018:02:24591:2:0:NEW 25 Apr 2018)…”
Section: Methodsmentioning
confidence: 99%