地质通报
地質通報
지질통보
GEOLOGICAL BULLETIN OF CHINA
2009年
7期
829-843
,共15页
邢立达%杰瑞德D.哈里斯%董枝明%林有利%陈伟%郭盛斌%季强
邢立達%傑瑞德D.哈裏斯%董枝明%林有利%陳偉%郭盛斌%季彊
형립체%걸서덕D.합리사%동지명%림유리%진위%곽성빈%계강
广东南雄盆地%晚白垩世主田组%南雄鸭嘴龙足迹%扬子足迹%禽龙足迹%嘉荫足迹%内乡足迹
廣東南雄盆地%晚白堊世主田組%南雄鴨嘴龍足跡%颺子足跡%禽龍足跡%嘉蔭足跡%內鄉足跡
엄동남웅분지%만백성세주전조%남웅압취룡족적%양자족적%금룡족적%가음족적%내향족적
记述了广东省南雄盆地上白垩统主田组3组恐龙行迹,由杨梅坑足迹点的足迹命名了南雄鸭嘴龙足迹(Hadrosauropodus nanxiongensis ichnosp.nov.)一新种;古市足迹点的足迹归入鸭嘴龙足迹一未定种(Hadrosauropodus isp.).这是中国鸭嘴龙足迹属的首次描述,将该足迹的分布从北美拓展至中国,并为南雄盆地存在大型的鸭嘴龙提供了新的化石证据.还整理了中国已描述的大型鸟脚类足迹:中国足迹(Sinoichnites)被定为非正式的塑模标本;扬子足印(Yanatzepus)被归入兽脚类足迹;禽龙足迹(1guanodonopus)被认为是裸名,归入禽龙足迹(Iguanodontipus);嘉荫足迹(Jiayinosauropus)增加了新材料并得以具体描述;内乡足迹(Neixiang footprint)得以重新描述.
記述瞭廣東省南雄盆地上白堊統主田組3組恐龍行跡,由楊梅坑足跡點的足跡命名瞭南雄鴨嘴龍足跡(Hadrosauropodus nanxiongensis ichnosp.nov.)一新種;古市足跡點的足跡歸入鴨嘴龍足跡一未定種(Hadrosauropodus isp.).這是中國鴨嘴龍足跡屬的首次描述,將該足跡的分佈從北美拓展至中國,併為南雄盆地存在大型的鴨嘴龍提供瞭新的化石證據.還整理瞭中國已描述的大型鳥腳類足跡:中國足跡(Sinoichnites)被定為非正式的塑模標本;颺子足印(Yanatzepus)被歸入獸腳類足跡;禽龍足跡(1guanodonopus)被認為是裸名,歸入禽龍足跡(Iguanodontipus);嘉蔭足跡(Jiayinosauropus)增加瞭新材料併得以具體描述;內鄉足跡(Neixiang footprint)得以重新描述.
기술료광동성남웅분지상백성통주전조3조공룡행적,유양매갱족적점적족적명명료남웅압취룡족적(Hadrosauropodus nanxiongensis ichnosp.nov.)일신충;고시족적점적족적귀입압취룡족적일미정충(Hadrosauropodus isp.).저시중국압취룡족적속적수차묘술,장해족적적분포종북미탁전지중국,병위남웅분지존재대형적압취룡제공료신적화석증거.환정리료중국이묘술적대형조각류족적:중국족적(Sinoichnites)피정위비정식적소모표본;양자족인(Yanatzepus)피귀입수각류족적;금룡족적(1guanodonopus)피인위시라명,귀입금룡족적(Iguanodontipus);가음족적(Jiayinosauropus)증가료신재료병득이구체묘술;내향족적(Neixiang footprint)득이중신묘술.
Herein we describe three trackways that pertain to Hadrosauropodus nanxiongensis ichnosp, nov. from the Yangmeikeng track site in the Nanxiong Basin, Guangdong Province, China. The tracks occur in the Upper Cretaceous Zhutian Formation. The nearby Gushi track site preserves trackways attributable to Hadrosauropodus isp. These represent the first occurrences of hadrosaur footprints in China. These discoveries expand the known distribution of hadrosaur tracks from North America to China, and provide evidence for the existence of large hadrosaurs in the Cretaceous of the Nanxiong Basin. Other previously-described, large, ostensible omithopod track occurrences in China are discussed: Sinoichnites is represented only by an informal "plastotype," Yangtzepus is at-tributable to a theropod, and Iguanodonopus is considered a nomen nudum and its specimens attributable to Iguanodontipus. New specimens of Jiayinosauropus allow some redescription of the ichnotaxon, and the unnamed Neixiang footprint is redescribed.