CAJ | 학술논문

几十年前人们就已经开始研究中国东北侏罗纪-白垩纪界线附近地层中的小型兽脚类恐龙足迹,虽然这些遗迹化石比辽宁省义县组带羽毛的恐龙及其他实体化石逊色了许多.本文记述了河北省承德南双庙后城组(土城子组)最下部河流相沉积中发现的一组兽脚类恐龙足迹.南双庙足迹具有三趾,趾粗大,其形态与美国下侏罗统经典的"brontozoid"足迹(Gral-lator,Anchisauripus和Eubrontes)相符.虽然许多产自辽宁土城子组中基本同时的brontozoid足迹被鉴定为小型的跷脚龙足迹属(Grallator),但南双庙足迹更大一些(全长可达28.8 cm),可能应该归入安琪龙足迹属(Anchisauripus).南双庙足迹很可能是一群小型兽脚类行走而产生.在辽宁义县组的兽脚类恐龙中,最可能留下这类足迹的是小型的窃蛋龙类--尾羽龙(Caudipteryx).不过这个解释还很勉强,因为这些足迹缺乏鉴定性特征,而且河北的后城组与辽宁的义县组之间还有一定的时间及地理间隔.
궤십년전인문취이경개시연구중국동북주라기-백성기계선부근지층중적소형수각류공룡족적,수연저사유적화석비요녕성의현조대우모적공룡급기타실체화석손색료허다.본문기술료하북성승덕남쌍묘후성조(토성자조)최하부하류상침적중발현적일조수각류공룡족적.남쌍묘족적구유삼지,지조대,기형태여미국하주라통경전적"brontozoid"족적(Gral-lator,Anchisauripus화Eubrontes)상부.수연허다산자료녕토성자조중기본동시적brontozoid족적피감정위소형적교각룡족적속(Grallator),단남쌍묘족적경대일사(전장가체28.8 cm),가능응해귀입안기룡족적속(Anchisauripus).남쌍묘족적흔가능시일군소형수각류행주이산생.재료녕의현조적수각류공룡중,최가능류하저류족적적시소형적절단룡류--미우룡(Caudipteryx).불과저개해석환흔면강,인위저사족적결핍감정성특정,이차하북적후성조여료녕적의현조지간환유일정적시간급지리간격.
Small theropod footprints have been known from the Jurassic-Cretaceous boundary strata of northeastern China for several decades, although these ichnofossils have been overshadowed by the feathered dinosaurs and other body fossils from the Yixian Formation of Liaoning Province. This paper describes a sample of several theropod footprints from a coarse fluvial deposit at Nanshuangmiao, in the lowermost Houcheng (Tuchengzi) Formation of Hebei Province. The Nanshuangmiao tracks exhibit a tridactyl, pachydactylous morphology corresponding to classic "brontozoid" ichnites (Grallator, Anchisauripus and Eubrontes) from the Lower Jurassic of the United States of America. Although many brontozoid tracks from the roughly equivalent Tuchengzi of Liaoning have been previously assigned to the small ichnogenus Grallator, as G. ssatoi, the Nanshuangmiao trcks are larger (up to 28.8 cm total length) and are probably referable to Anchisauripus. The Nanshuangmiao tracks were most likely produced by small theropods travelling in a group. Of the abundant theropod taxa known from the Yixian Formation of Liaoning, the small oviraptorosaur Caudipteryx is the most plausible trackmaker, but this interpretation remains uncertain because of a lack of diagnostic features in the tracks and because of the temporal and geographic gap between the Houcheng of Hebei and the Yixian of Liaoning.