期刊文献+

自贡大山铺恐龙动物群埋藏环境及集中埋藏原因分析 被引量:4

An analysis of the taphonomic environment of dinosaur faunae in Dashanpu of Zigong City and the cause of their concentrative burial
下载PDF
导出
摘要 四川自贡大山铺以其集中埋藏数量众多的恐龙化石而闻名于世,恐龙化石集中埋藏的原因一直是人们关注的焦点问题之一。笔者在对自贡恐龙博物馆内及其附近地层剖面调查的基础上,根据对该处埋藏恐龙化石地层的岩相、沉积构造、砂体形态特征以及沉积背景的分析,认为恐龙化石的埋藏环境为湖泊三角洲,恐龙由于某种原因死亡后,经过河流搬运埋藏于湖泊三角洲前缘的河口砂坝之中,而非由于中毒异常死亡原地埋藏。 Dashanpu of Zigong City in Sichuan Province is world-wide famous for its dinosaur fossils, particularly the concentrative burial of a large quantity of dinosaurs. The cause of their concentratrative burial remains a problem of much controversy. Based on an analysis of such characteristics of the strata in the Zigong Dinosaur Museum and its surrounding areas as the lithofacies, depositional environment, shape of sandstone, and deposition background, this paper deals with the taphonomic environment of dinosaur faunae in Dashanpu and the cause of their concentrative burial. The authors consider that dinosaur remains were buried in frontal river mouth sand bar of lacustrine delta after their depth due to an unknown cause and river transport of their bodies instead of being buried in situ after their death due to poisoning.
出处 《中国地质》 CAS CSCD 北大核心 2009年第1期131-137,共7页 Geology in China
基金 中国地质调查局"四川盆地中生代恐龙动物群研究"项目(200313000051)资助。
关键词 恐龙 埋藏环境 侏罗系 自贡大山铺 dinosaur taphonomic environment Jurassic Dashapu in Zigong, Sichuan Province
  • 相关文献

参考文献7

  • 1Christine E. Turner, Fred Peterson. Reconstruction of the Upper Jurassic Morrison Formation extinct ecosystem a synthesis [J]. Sedimentary Geology, 2004, 167:309-355.
  • 2Dodson P, Behrensmeyer A K, Bakker R T, et al. Taphonomy and paleoecology of the dinosaur beds of the Jurassic Morrison FormationlJ]. Paleobiology, 1980, 6(2):208-232.
  • 3梁斌,王全伟,阚泽忠,朱兵.四川珙县石碑恐龙化石埋藏地红层分子化石特征及其古环境意义[J].中国地质,2006,33(1):187-192. 被引量:2
  • 4阚泽忠,梁斌,王全伟,朱兵.广元恐龙化石埋藏地沙溪庙组地球化学特征及对物源区和古风化作用的指示[J].中国地质,2006,33(5):1023-1029. 被引量:19
  • 5Kolodny Y, Luz B, Sander M, et al. Dinosaur bones: fossils or pseudomorphs? The pitfall of physiology reconstruction from apatitic fossils []]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1996, 126,161-171.
  • 6Tauson L V, Barsbold R, Samoylov V S, et al. Trace Elements in Dinosaur Remains fi:om the Gobi Desert, Mongolian People's Republic[M]. Dokl AN SSStk, 1984, 278:974-978.
  • 7里丁.沉积环境和相[M].北京,科学出版社,1985.20-80.

二级参考文献33

  • 1王全伟,阚泽忠,朱兵,梁斌,杨恒书.四川广元恐龙化石埋藏地上沙溪庙组的双壳动物群[J].四川地质学报,2005,25(1):1-3. 被引量:2
  • 2Brassell S C, Eglinton G, Marlowe 1 T, et al. Molecular stratigraphy:a new tool for climatic assessment[J]. Nature, 1986, 320:129-133.
  • 3Meyers P A, Ryoshi Ishiwatari. Lacustrine organic geochemistry-an overview of indicators of organic matter sources and diagenesis in lake sediments[J]. Organic Geochemistry, 1993, 20(7):867-900.
  • 4Meyers P A. Application of organic geochemistry to paleolimnological reconstructions:a summary of examples from the Laurentian Great Lakes[J]. Organic Geochemistry, 2003, 34:261-289.
  • 5Cranwell P A, Eglinton G, Robinson N. Lipids of aquatic organisms as potential contributors to lacustrine sediments [J]. Organic Geochemistry, 1987, 11:513-527.
  • 6Huang Y, Street-Perrott F A, Perrott F A, et al. Glacial-interglacial environmental changes inferred from the molecular and compound-specific δ^13C analyses of sediments from Sacred Lake, Mt Kenya[J]. Geochimica et Cosmochinica Acta, 1999, 63: 1383-1404.
  • 7Ficken K J, Li B, Swain D L, et al. An n-alkane proxy for the sedimentary input of submerged/floating fi'eshwater aquatic macrophytes[J]. Orgamc Geochemistry, 2000, 31:745-749.
  • 8Aquino Neto F R, Resale A, Connan J, et al. Novel tricyclic terpanes (C19. C20) in sediments and petroleum [J]. Terabed on Letters,1982, 23: 2027-2030.
  • 9Dorsselaer Van A, Ersminger A, Spyckerelle C, et al. Degraded and extended hopane derivation (C27-C35) as ubiquitous geochemical markers[J]. Terabed on Letters, 1974, 1349-1352.
  • 10TissotBP WelteDH.石油的形成与分布[M].北京:石油工业出版社,1989.78-298.

共引文献23

同被引文献86

引证文献4

二级引证文献49

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部