Limuloid trackways from Permian-Triassic continental successions of North China

被引:16
|
作者
Shu, Wenchao [1 ]
Tong, Jinnan [1 ]
Tian, Li [1 ,2 ]
Benton, Michael J. [2 ]
Chu, Daoliang [1 ]
Yu, Jianxin [1 ]
Guo, Wenwei [1 ]
机构
[1] China Univ Geosci, Sch Earth Sci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Hubei, Peoples R China
[2] Univ Bristol, Sch Earth Sci, Bristol BSB 1RJ, Avon, England
基金
中国博士后科学基金; 英国自然环境研究理事会; 中国国家自然科学基金;
关键词
Limuloid trace fossil; Ichnotaxobase; Size variation; Sexual dimorphism; Continental Permian-Triassic events; North China; TRACE FOSSIL SELENICHNITES; MASS EXTINCTION; HORSESHOE-CRAB; ICHNOLOGICAL EVIDENCE; ARTHROPOD TRACKWAYS; CLEVELAND BASIN; MIDDLE; DISCOVERIES; NETHERLANDS; WINTERSWIJK;
D O I
10.1016/j.palaeo.2018.07.022
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Forty-four well-preserved specimens of Kouphichnium, a typical limuloid (horseshoe crab) trackway, are reported and systematically studied for the first time from continental Upper Permian to Lower Triassic successions in North China. A new ichnotaxonomic system of Kouphichnium is proposed according to the ichnotaxobase of limuloid trackways, including simple foot imprints (T), pusher imprints (P), median impressions (M) and genal spine impressions (GS). In total, one ichnogenus and six ichnospecies are recognized, one of which is new: Kouphichnium liulinensis sp. nov. Ichnogenus Paramphibius is regarded as a synonym of Kouphichnium and the diagnoses of ichnogenus Kouphichnium and its two early ichnospecies, i.e. type ichnospecies Kouphichnium lithographicum Oppel, and Kouphichnium didactylum Willard, are revised. A morphological-palaeoethological pattern is proposed in reference to these ichnospecies from the continental Upper Permian to Lower Triassic successions in North China. These six ichnospecies are assigned to six types in the new ichnotaxonomic system and the locomotion rates of each type can be ranked by the possible speed index lambda. The size of trackmaker is estimated from the external width of the trackway, and it shows a drastic decrease from the Late Permian to Early Triassic, followed by a gradual increase in the Early Triassic. This size variation of trackmakers (limuloids) during the Permian-Triassic transition, especially the drastic drop, probably reflects the intensive environmental stress during the biotic crisis. In addition, the analysis of the sizes of pusher imprints (P) from certain well-preserved trackways suggests a potential sexual dimorphism of limuloids.
引用
收藏
页码:71 / 90
页数:20
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