旋回地层学: 地层学解读时间的第三里程碑

龚一鸣; 杜远生; 童金南; 张克信; 冯庆来; 谢树成; 胡斌; 齐永安; 张国成

旋回地层学: 地层学解读时间的第三里程碑

1.
中国地质大学生物地质与环境地质教育部重点实验室, 地质过程与矿产资源国家重点实验室, 湖北武汉 430074
2.
河南理工大学资源环境学院, 生物遗迹与沉积矿产河南省重点实验室, 河南焦作 454003

基金项目:

国家自然科学基金项目 40472020

国家自然科学基金项目 40072041

国家自然科学基金项目 40621002

高等学校学科创新引智计划项目 B08030

长江学者创新团队发展计划项目 IRT0546

SINOPEC项目 G0800-06-ZS-319

详细信息

作者简介:
龚一鸣(1958-), 男, 教授, 博士生导师, 主要从事泥盆纪地层、遗迹化石和沉积地质研究.E-mail: ymgong@cug.edu.cn

中图分类号: P534
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出版历程
- 收稿日期: 2007-10-29
- 刊出日期: 2008-07-25

Cyclostratigraphy: The Third Milestone of Stratigraphy in Understanding Time

1.
Key Laboratory of Biogeology & Environmental Geology of Ministry of Education, State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
2.
Institute of Resources and Environment, Henan Key Laboratory of Biogenic Traces and Sedimentary Minerals, Henan Polytechnic University, Jiaozuo 454003, China

摘要

摘要: 围绕对地质时间的认识, 地层学取得了从岩石地层学、生物地层学和旋回地层学3次里程碑性的重大进展.以生物地层学为基础并与放射性同位素定年技术相结合建立的、以百万年为计时单位的地质年代表既创造了地层学的辉煌, 也在一定程度上降低了地质学对精确数字定年的不懈追求和为人类社会服务的功能.本文以时间为线索, 简要回顾了地层学解读时间的漫长过程, 阐述了旋回地层学概念的起源、形成和发展, 以及旋回地层学与层序地层学在科学目标、研究内容和研究方法上的异同.以广西晚泥盆世弗拉期-法门期之交海相碳酸盐地层为例, 从理论与实践的结合上剖析了旋回地层学的研究方法以及在岩石地层学和生物地层学基础上构建高分辨率, 并能与人类社会时间接轨的地质时间坐标的广阔前景和科学意义.
- 旋回地层学 /
- 岩石地层学 /
- 生物地层学 /
- 时间 /
- 米兰柯维奇旋回 /
- 泥盆纪 /
- 华南
Abstract: Focusing on understanding geological time, stratigraphy has made three milestone achievements characterized by lithostratigraphy, biostratigraphy and cyclostratigraphy.A geological time scale based mainly on both biostratigraphy and radiometric dating created stratigraphic refulgence, but at the cost of lowered accuracy and preciseness and weakened function of serving the human society.The paper briefly reviews the long history of stratigraphy in understanding geological time, expatiating on the origin, formation and development of cyclostratigraphical concepts, and on similarities and differences between cyclostratigraphy and sequence stratigraphy in the scientific objective, research content and method.Taking the Late Devonian Frasnian-Famennian transitional marine carbonate successions from Guangxi, South China as an example, the paper discusses the research method of cyclostratigraphy, and the prospect and scientific significance of cyclostratigraphy in establishing the high-resolution geological time scale which bridges the gap between the existing geological time coordinate with time unit of million-year scale and anthropological time units such as millennium, century and year, etc.
- cyclostratigraphy /
- lithostratigraphy /
- biostratigraphy /
- time /
- Milankovitch cycle /
- Devonian /
- South China

HTML全文

图 1 地层学大事记

注: ①~⑦为转引文献编号, 分别转引吴瑞棠和王治平, 1994; 张守信, 1989; 王鸿祯, 1995; 龚一鸣等, 1996b; 朱筱敏, 2000; 金性春, 1984; Doyle and Bennett, 1998

Fig. 1. Stratigraphic memorabilia

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图 2 时间的传统表示(Prigogine, 1980; Holland, 1986)

Fig. 2. The traditional expression of time

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图 3 旋回地层的级序结构、描述术语及划分方法示意图

Fig. 3. Sketch showing the hierarchical structures, description terms and subdivision methods of cyclothems in cyclostratigraphy

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图 4 地-月-日系统和米兰柯维奇旋回示意图(据House, 1995a, 1995b改编)

Fig. 4. The sketch showing the earth-moon-sun system and Milankovitch cycle

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图 5 岁差和斜度周期随时间的变化(据Doyle and Bennett, 1998)

Fig. 5. Variations of precession and obliquity periods through time

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图 6 广西德保都安上泥盆统牙形石分带、旋回地层结构与数字定年(据龚一鸣等, 2004修改)

Fig. 6. The Late Devonian cyclostratigraphic hierarchy of the Du'an section, South China

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图 7 广西上泥盆统弗拉阶-法门阶之交旋回地层对比(据Gong et al., 2001修改)

Fig. 7. The Late Devonian cyclostratigraphic correlation in Guangxi, South China

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图 8 上泥盆统牙形石带数字定年(据龚一鸣等, 2004修改)

Fig. 8. Numerical dating of the Late Devonian conodont zones

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表 1 地史时期的岁差和斜度周期(据Berger and Loutre, 1994编制)

Table 1. Periods of precession and obliquity through time

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