地质通报
地質通報
지질통보
GEOLOGICAL BULLETIN OF CHINA
2009年
1期
16-29
,共14页
邢立达%杰瑞德 D.哈里斯%关谷秀%藤田将人%董枝明
邢立達%傑瑞德 D.哈裏斯%關穀秀%籐田將人%董枝明
형립체%걸서덕 D.합리사%관곡수%등전장인%동지명
云南禄丰地区%下侏罗统禄丰组%张北足迹%卡岩塔足迹
雲南祿豐地區%下侏囉統祿豐組%張北足跡%卡巖塔足跡
운남록봉지구%하주라통록봉조%장북족적%잡암탑족적
Lufeng County,Yunnan Province%Lower Jurassic Lufeng Formation%Changpeipus%Kayentapus
记述了云南省禄丰县腰站乡下侏罗统禄丰组2个恐龙足迹,命名了棋盘张北足迹(Changpeipus pareschequicr ichnosp.nov.)一新种.这是在禄丰组中首次发现恐龙足迹化石,重新观察并修订了张北足迹一属的属征.滦平张北足迹(Changpeipus luanpingeris)应为石炭张北足迹(Changpeipus carbonicus)的亚成年个体,为同物异名.此前被认为是石发张北足迹(Changpeipus carbonicus)前足迹的IVPP V2472 2a,应为其未成年体的后足迹.张北足迹与卡岩塔足迹(Kayentapus)类似.综合种种特征.棋盘张北足迹(新种)的造迹恐龙很可能为禄丰组的腔骨龙类(Coelophysoidea).
記述瞭雲南省祿豐縣腰站鄉下侏囉統祿豐組2箇恐龍足跡,命名瞭棋盤張北足跡(Changpeipus pareschequicr ichnosp.nov.)一新種.這是在祿豐組中首次髮現恐龍足跡化石,重新觀察併脩訂瞭張北足跡一屬的屬徵.灤平張北足跡(Changpeipus luanpingeris)應為石炭張北足跡(Changpeipus carbonicus)的亞成年箇體,為同物異名.此前被認為是石髮張北足跡(Changpeipus carbonicus)前足跡的IVPP V2472 2a,應為其未成年體的後足跡.張北足跡與卡巖塔足跡(Kayentapus)類似.綜閤種種特徵.棋盤張北足跡(新種)的造跡恐龍很可能為祿豐組的腔骨龍類(Coelophysoidea).
기술료운남성록봉현요참향하주라통록봉조2개공룡족적,명명료기반장북족적(Changpeipus pareschequicr ichnosp.nov.)일신충.저시재록봉조중수차발현공룡족적화석,중신관찰병수정료장북족적일속적속정.란평장북족적(Changpeipus luanpingeris)응위석탄장북족적(Changpeipus carbonicus)적아성년개체,위동물이명.차전피인위시석발장북족적(Changpeipus carbonicus)전족적적IVPP V2472 2a,응위기미성년체적후족적.장북족적여잡암탑족적(Kayentapus)유사.종합충충특정.기반장북족적(신충)적조적공룡흔가능위록봉조적강골룡류(Coelophysoidea).
Herein described are two footprints that belong to the new ichnospecies Changpeipus pareschequier ichnosp, nov. from the Lower Jurassic Lufeng Formation near Yaozhan Village, Lufeng County, Yunnan Province, China. This is the first discovery of dinosaur footprints in the Lufeng Formation. The ichnogenus Changpeipus is revised after the re-study of its type specimens. Specimen IVPP V2472 2a, a supposed manus print that is part of the ichnogenoholotype of Changpeipus carbonicas, is re-studied herein and assessed as apes print of a juvenile individual of the Changpeipus carbonieus track maker. Changpeipus luanpingeri, is a junior synonym of Changpeip us carbonieus. Changpeipus pareschequier ichnosp, nov. resembles the ichnotaxon Kayenlapus. Based on its characteristics, the footprints are presumably made by a member of the Coelophysoidea from the Lufeng Formation.