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风暴沉积的遗迹学研究

S.G.Pemberton 周志澄 J.Mac Eacher

S.G.Pemberton, 周志澄, J.Mac Eacher. 风暴沉积的遗迹学研究[J]. 沉积学报, 2000, 18(4): 489-494.
引用本文: S.G.Pemberton, 周志澄, J.Mac Eacher. 风暴沉积的遗迹学研究[J]. 沉积学报, 2000, 18(4): 489-494.
S.G.Pemberton, ZHOU Zhi cheng, J. MacEachern. Ichnological Studies on Tempestites[J]. Acta Sedimentologica Sinica, 2000, 18(4): 489-494.
Citation: S.G.Pemberton, ZHOU Zhi cheng, J. MacEachern. Ichnological Studies on Tempestites[J]. Acta Sedimentologica Sinica, 2000, 18(4): 489-494.

风暴沉积的遗迹学研究

基金项目: 国家自然科学基金,(批准号:49872046);古生物所创新基金成果
详细信息
  • 中图分类号: P512.2

Ichnological Studies on Tempestites

  • 摘要: 遗迹化石正在证明其在鉴别和解释事件地层中的作用。风暴沉积含有一套混合的、与能量水平变化相适应的遗迹化石组合,两种不同的遗迹群落反映变化着的行为方式对生物所移居的两种连续的,但是单个性质不同的生境所作出的反应:常住的或平常天气的遗迹群落可以作为一种稳定的底栖群落的代表,在这一群落里单个的居群达到或接近它们的承载能力;而周期性产生的风暴遗迹群落则代表着在一种不稳定的、生态环境恶化的、机械控制的环境下繁盛的机会主义生物的群落。典型的陆源碎屑的风暴沉积中的遗迹群落可以加拿大艾伯塔上白垩统卡迪组中的遗迹群落为例,而碳酸盐风暴沉积中的遗迹群落则可以中国华北地台东部上寒武统崮山组中的碳酸盐风暴沉积序列中的遗迹群落为例,本文详细介绍这两种类型的成因及结构、构造特点。
  • [1] Beynon B M, Pemberton S G, Bell D A et al. Environmerntal implications of ichnofossils fron the Lower Cretaceous Grand Rapids Formation, Cold Lake Oil Sands Deposit. In: James D J, Leckie D A, eds., Sequences, Stratigraphy, Sedimentology: Surface and Subsurface[C]. Canadian Society of Petroleum Geologists Memoir, 1988,15:275~90
    [2] Bromley R G, Asgaard U. Ichnofacies: A mixture of taphofacies and biofades[J]. Lethaia, 1991,24:153~63
    [3] Bromley R G,Ekdale A A. Chondrites: A trace fossil indicator of anoxia in sediments[J]. Science, 1984,224:872~74
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    [6] Dott H R Jr. 1982 SEPM Presidential address: Episodic sedimentation: How normal is average? How rare is rare? Does it matter? [J]. Journal of Sedimentary Petrology, 1983,53:5~23
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  • [1] 李忠.  “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, (6): 928-933.
    [2] 李 忠.  “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, 24(06): 928-933.
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出版历程
  • 收稿日期:  2000-05-29
  • 修回日期:  2000-06-20
  • 刊出日期:  2000-08-10

目录

    风暴沉积的遗迹学研究

      基金项目:  国家自然科学基金,(批准号:49872046);古生物所创新基金成果
    • 中图分类号: P512.2

    摘要: 遗迹化石正在证明其在鉴别和解释事件地层中的作用。风暴沉积含有一套混合的、与能量水平变化相适应的遗迹化石组合,两种不同的遗迹群落反映变化着的行为方式对生物所移居的两种连续的,但是单个性质不同的生境所作出的反应:常住的或平常天气的遗迹群落可以作为一种稳定的底栖群落的代表,在这一群落里单个的居群达到或接近它们的承载能力;而周期性产生的风暴遗迹群落则代表着在一种不稳定的、生态环境恶化的、机械控制的环境下繁盛的机会主义生物的群落。典型的陆源碎屑的风暴沉积中的遗迹群落可以加拿大艾伯塔上白垩统卡迪组中的遗迹群落为例,而碳酸盐风暴沉积中的遗迹群落则可以中国华北地台东部上寒武统崮山组中的碳酸盐风暴沉积序列中的遗迹群落为例,本文详细介绍这两种类型的成因及结构、构造特点。

    English Abstract

    S.G.Pemberton, 周志澄, J.Mac Eacher. 风暴沉积的遗迹学研究[J]. 沉积学报, 2000, 18(4): 489-494.
    引用本文: S.G.Pemberton, 周志澄, J.Mac Eacher. 风暴沉积的遗迹学研究[J]. 沉积学报, 2000, 18(4): 489-494.
    S.G.Pemberton, ZHOU Zhi cheng, J. MacEachern. Ichnological Studies on Tempestites[J]. Acta Sedimentologica Sinica, 2000, 18(4): 489-494.
    Citation: S.G.Pemberton, ZHOU Zhi cheng, J. MacEachern. Ichnological Studies on Tempestites[J]. Acta Sedimentologica Sinica, 2000, 18(4): 489-494.
    参考文献 (33)

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