古地理学报
古地理學報
고지이학보
Journal of Palaeogeography
2015年
5期
593-610
,共18页
王能盛%旷红伟%柳永清%彭楠%许欢%章朋%汪明伟%王宝红%安伟
王能盛%曠紅偉%柳永清%彭楠%許歡%章朋%汪明偉%王寶紅%安偉
왕능성%광홍위%류영청%팽남%허환%장붕%왕명위%왕보홍%안위
恐龙骨骼化石%埋藏学%晚白垩世%国内外对比
恐龍骨骼化石%埋藏學%晚白堊世%國內外對比
공용골격화석%매장학%만백성세%국내외대비
dinosaur bone fossils%taphonomy%Late Cretaceous%comparison between domestic and a_broad
运用埋藏学与沉积地质学的研究方法与手段,对中国东部晚白垩世具有恐龙化石集群埋藏盆地中恐龙骨骼化石的埋藏地层层序与年代、埋藏骨骼化石特征、骨骼化石埋藏类型及其埋藏成因等进行了分析与总结,并将其产出时代、埋藏相、埋藏特征与国外进行了对比研究。研究认为:中国东部与国外相比,虽然化石产出的具体时期有所差异,但从恐龙种群、埋藏相及沉积地层学等方面均具有相似性,反映了晚白垩世全球古环境、古生态及古气候的相似性。(1)中国晚白垩世恐龙骨骼化石埋藏事件可分为早期与晚期2个阶段:早期的 Cenomanian 期与晚期的 Santonian_Maastrichtian 期。而国外晚白垩世恐龙骨骼化石埋藏事件只发生在晚期,在美洲及蒙古国发生在 Campanian 晚期,在欧洲则为 Campanian_Maastrichtian 期的过渡时期及 Maastrichtian 期。(2)中国埋藏骨骼化石种属以鸟脚类鸭嘴龙科与兽脚类恐龙为主,它们埋藏于紫红色地层中,埋藏环境主要为冲积扇与河流环境;美洲以鸭嘴龙科为主,欧洲与蒙古国的种群各地不相同,都埋藏于紫红色岩石地层中,埋藏环境主要为河流—泛滥平原。骨骼在不同沉积相组合地层中埋藏学特征各异,与古地理、古生态及古环境密切相关。(3)结合盆地中的化石埋藏学特征与盆地演化特征,总结了恐龙化石埋藏类型主要有原地埋藏与异地埋藏,盆地古地理格局变动、火山活动、古温度升高及古地震等事件的综合作用是可能的埋藏成因,并提出了恐龙化石的埋藏模式。此研究为揭示中国东部乃至全球晚白垩世的古地理、古气候及古生态环境及恐龙灭绝原因的探讨提供了新的材料与证据。
運用埋藏學與沉積地質學的研究方法與手段,對中國東部晚白堊世具有恐龍化石集群埋藏盆地中恐龍骨骼化石的埋藏地層層序與年代、埋藏骨骼化石特徵、骨骼化石埋藏類型及其埋藏成因等進行瞭分析與總結,併將其產齣時代、埋藏相、埋藏特徵與國外進行瞭對比研究。研究認為:中國東部與國外相比,雖然化石產齣的具體時期有所差異,但從恐龍種群、埋藏相及沉積地層學等方麵均具有相似性,反映瞭晚白堊世全毬古環境、古生態及古氣候的相似性。(1)中國晚白堊世恐龍骨骼化石埋藏事件可分為早期與晚期2箇階段:早期的 Cenomanian 期與晚期的 Santonian_Maastrichtian 期。而國外晚白堊世恐龍骨骼化石埋藏事件隻髮生在晚期,在美洲及矇古國髮生在 Campanian 晚期,在歐洲則為 Campanian_Maastrichtian 期的過渡時期及 Maastrichtian 期。(2)中國埋藏骨骼化石種屬以鳥腳類鴨嘴龍科與獸腳類恐龍為主,它們埋藏于紫紅色地層中,埋藏環境主要為遲積扇與河流環境;美洲以鴨嘴龍科為主,歐洲與矇古國的種群各地不相同,都埋藏于紫紅色巖石地層中,埋藏環境主要為河流—汎濫平原。骨骼在不同沉積相組閤地層中埋藏學特徵各異,與古地理、古生態及古環境密切相關。(3)結閤盆地中的化石埋藏學特徵與盆地縯化特徵,總結瞭恐龍化石埋藏類型主要有原地埋藏與異地埋藏,盆地古地理格跼變動、火山活動、古溫度升高及古地震等事件的綜閤作用是可能的埋藏成因,併提齣瞭恐龍化石的埋藏模式。此研究為揭示中國東部迺至全毬晚白堊世的古地理、古氣候及古生態環境及恐龍滅絕原因的探討提供瞭新的材料與證據。
운용매장학여침적지질학적연구방법여수단,대중국동부만백성세구유공룡화석집군매장분지중공용골격화석적매장지층층서여년대、매장골격화석특정、골격화석매장류형급기매장성인등진행료분석여총결,병장기산출시대、매장상、매장특정여국외진행료대비연구。연구인위:중국동부여국외상비,수연화석산출적구체시기유소차이,단종공룡충군、매장상급침적지층학등방면균구유상사성,반영료만백성세전구고배경、고생태급고기후적상사성。(1)중국만백성세공용골격화석매장사건가분위조기여만기2개계단:조기적 Cenomanian 기여만기적 Santonian_Maastrichtian 기。이국외만백성세공용골격화석매장사건지발생재만기,재미주급몽고국발생재 Campanian 만기,재구주칙위 Campanian_Maastrichtian 기적과도시기급 Maastrichtian 기。(2)중국매장골격화석충속이조각류압취룡과여수각류공룡위주,타문매장우자홍색지층중,매장배경주요위충적선여하류배경;미주이압취룡과위주,구주여몽고국적충군각지불상동,도매장우자홍색암석지층중,매장배경주요위하류—범람평원。골격재불동침적상조합지층중매장학특정각이,여고지리、고생태급고배경밀절상관。(3)결합분지중적화석매장학특정여분지연화특정,총결료공룡화석매장류형주요유원지매장여이지매장,분지고지리격국변동、화산활동、고온도승고급고지진등사건적종합작용시가능적매장성인,병제출료공룡화석적매장모식。차연구위게시중국동부내지전구만백성세적고지리、고기후급고생태배경급공룡멸절원인적탐토제공료신적재료여증거。
This paper analyzes the Late Cretaceous dinosaur bones according to stratigraphic succes_sions,dinosaur species,articulation and association,diversity,the quantity and quality of preservation and the arrangement of dinosaur fossils from the eastern China by method of taphonomy and sedimentology, and make a comparison between demestic and abroad from the points of occurrence age,and taphonomic facies and characteristics.The studies suggest that:Although the concrete preservation times are different, the species,taphonomic facies and characteristics are similar,which reflecting the similarity of palaeoen_vironment,palaeoecology,and palaeoclimate during the Late Cretaceous in a global scale.(1 ) The burial process of dinosaur bones in China during the Late Cretaceous can be divided into two stages:the early stage of Cenomanian and the late stage of Santonian to Maastrichtian.Foreign burial events appeared during the late Campanian in America and Mongolia,and the Campanian_Maastrichtian transitional period and Maastrichtian in Europe.(2) In China,bones were buried mainly in purple rocks of alluvial fan facies and fluvial facies,and the dinosaur species are mainly Ornithopod hadrosaurs and theropods.Compared with dinosaur mass extinction abroad,they were mainly preserved in lacustrine and flood plain.Hadrosaurs and ceratopsids were flourishing in America and Mongolia,while dinosaurs in Europe and Mongolia are dif_ferent.The characteristics are different in different successions,which are closely related with palaeogeog_raphy,palaeoenvironment and palaeoclimate.(3 ) By combination of taphonomic and basin evolution characteristics,it concluded that burial types are autochthonous and allochthonous,and the probable bur_ial comprehensive factors are:the change of palaeogeography,volcanism,high temperature etc.,then a taphonomic model were built.It is significant for further study of bone taphonomy and palaeogeography, palaeoenvironment and palaeoclimate,and proposes many new materials and evidence for the research of palaeogeography,palaeoenvironment and palaeoclimate.