豫西济源二叠纪末-三叠纪初陆相微生物成因构造及其古环境意义
- 1. 河南理工大学资源环境学院, 河南焦作 454003;
- 2. 河南省生物遗迹与成矿过程重点实验室, 河南焦作 454003
基金项目:
国家自然科学基金项目（41772110，41472083，41202071）
作者简介:
郑伟,男,1979年出生,副教授,地球生物学和沉积学,E-mail:zhengw99@hpu.edu.cn
- 收稿日期:
2016-08-23
- 修回日期:
2016-12-29
- 刊出日期:
2017-12-10
摘要: 在豫西济源地区发现的陆相微生物成因构造（Microbially Induced Sedimentary Structures，MISSs），主要发育在孙家沟组和刘家沟组，可分为2大类即微生物席生长构造和微生物席破坏构造，8小类即生长脊构造、瘤状突起、曲形脱水裂痕、纺锤状脱水裂痕、似正弦状构造、树枝状脱水裂痕、多边形脱水裂痕和直脊状脱水裂痕。镜下分析显示具有大"U"形脊、定向排列的石英颗粒、近平行的暗色黏土矿物条带及悬浮排列的云母颗粒等微生物成因特征。通过与鲁山、黎城中元古界以及宜阳、柳林早三叠系微生物成因构造对比研究，认为研究区的微生物成因构造具有较为特殊的埋藏学特征，受二叠纪末灾变事件、适宜的沉积条件和气候因素控制，代表着研究区以微生物群落为主、后生动物稀少、植被贫乏、气候炎热和水土流失严重等特征的一种陆相灾后生态系。
Characteristics and Paleoenvironmental Significance of Microbially Induced Sedimentary Structures(MISSs) in Terrestrial P-T Boundary in Jiyuan, Western Henan Province
- 1. Institute of Resource and Environment, Henan Polytechnic University, Jiaozuo, Henan 454003, China;
- 2. Key Laboratory of Biogenic Traces & Sedimentary Minerals of Henan Province, Jiaozuo, Henan 454003, China
Funds:
National Nature Science Foundation of China, No. 41772110,41472083,41202071
- Received Date:
2016-08-23
- Rev Recd Date:
2016-12-29
- Publish Date:
2017-12-10
Abstract: We have firstly reported the presence of eight kinds of microbially induced sedimentary structures (MISSs) or sedimentary surface textures, including growth ridges, growth postulas, curved desiccation cracks, spindle-shaped cracks, "Manchuriophycus" structures, dendritic desiccation cracks, polygonal desiccation cracks and desiccation cracks from the terrestrial upper Permian Sunjiagou Formation and lower Triassic Liujiagou Formation in Jiyuan western Henan. Large U ridges, oriented sand quartz, mica grains and thin clayey laminae arranged parallel to bedding plane are the main features visible under the microscope. A series of evidence indicate that the Jiyuan MISSs are of biogenic origin. Compared with MISSs of the Mesoproterozoic Yunmengshan Formation in Lushan, the Mesoproterozoic Changchougou Formation in Licheng, Lower Triassic Liujiagou Formation in Yiyang and Liulin, we concluded that microbially induced sedimentary structures has special taphonomic characteristics and was controlled by the end-Permian mass extinction, sedimentary environments and climate factor in Jiyuan. MISSs of Jiyuan stands for terrestrial ecosystems following the end-Permian mass extinction with rich microbial community, scarce metazoan, poor plant, hot weather and serious soil erosion.
郑伟, 齐永安, 邢智峰, 白万备, 陈百兵, 李小燕. 豫西济源二叠纪末-三叠纪初陆相微生物成因构造及其古环境意义[J]. 沉积学报, 2017, 35(6): 1121-1132. doi: 10.14027/j.cnki.cjxb.2017.06.004
ZHENG Wei, QI YongAn, XING ZhiFeng, BAI WanBei, CHEN BaiBing, LI XiaoYan. Characteristics and Paleoenvironmental Significance of Microbially Induced Sedimentary Structures(MISSs) in Terrestrial P-T Boundary in Jiyuan, Western Henan Province[J]. Acta Sedimentologica Sinica, 2017, 35(6): 1121-1132. doi: 10.14027/j.cnki.cjxb.2017.06.004
| Citation: |
ZHENG Wei, QI YongAn, XING ZhiFeng, BAI WanBei, CHEN BaiBing, LI XiaoYan. Characteristics and Paleoenvironmental Significance of Microbially Induced Sedimentary Structures(MISSs) in Terrestrial P-T Boundary in Jiyuan, Western Henan Province[J]. Acta Sedimentologica Sinica, 2017, 35(6): 1121-1132. doi: 10.14027/j.cnki.cjxb.2017.06.004
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