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地球科学进展  2017, Vol. 32 Issue (3): 221-233    DOI: 10.11867/j.issn.1001-8166.2017.03.0221
综述与评述     
珊瑚礁的成岩作用
王瑞1, 2, 3, 余克服1, 2, 3, *, 王英辉1, 2, 3, 边立曾3, 4
1.广西大学海洋学院,广西 南宁 530004;
2.广西南海珊瑚礁研究重点实验室,广西 南宁 530004;
3.广西大学珊瑚礁研究中心,广西 南宁 530004;
4.南京大学地球科学与工程学院, 江苏 南京 210093
The Diagenesis of Coral Reefs
Wang Rui1, 2, 3, Yu Kefu1, 2, 3, *, Wang Yinghui1, 2, 3, Bian Lizeng3, 4
1.School of Marine Sciences, Guangxi University, Nanning 530004,China;
2.Guangxi Laboratory on the Study of Coral Reefs in the South China Sea, Nanning 530004, China;
3.Coral Reef Research Center of China Guangxi University, Nanning 530004, China;
4.School of Earth Science and Engineering, Nanjing University, Nanjing 210093, China
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摘要: 珊瑚礁作为古环境记录的良好载体,时常受到成岩作用的制约,正确认识和评价成岩作用,是开展珊瑚礁古环境重建的关键。珊瑚礁成岩作用主要包括胶结作用、溶解作用、新生变形作用和白云岩化作用等类型。一方面,成岩作用本身可记录珊瑚礁经历的海平面升降、气候变化、海水性质改变、热液改造、微生物活动等地质过程,利用成岩演化过程可恢复古环境变化过程;另一方面,成岩作用又对珊瑚礁记录的原始环境信息产生了破坏,恢复古环境时需识别成岩作用对其影响的程度。在未来研究中,应加强成岩作用与现代气候环境、海平面变化、大气淡水改造、微生物活动的关系研究,以期提供更准确、更长时间序列的珊瑚礁古环境记录。
关键词: 珊瑚礁古环境古气候成岩作用发育模式    
Abstract: Coral reefs are often constrained by diagenesis as a sound environmental archive. The correct understanding and evaluation of diagenesis is the key to the paleoenvironmental reconstruction of coral reefs. The diagenesis of coral reefs mainly includes cementation, dissolution, neomorphism and dolomitization etc. On the one hand, the diagenesis itself can record the paleoenvironment that coral reefs underwent, such as sea-level fluctuation, climate change, change of sea water, hydrothermal alteration, microbial activity and so on. The diagenetic evolution thus can be used for the reconstruction of paleoenvironment change. On the other hand, diagenesis also destroys the original environmental information which recorded of coral reefs recard, and it is necessary to know the degree of the impact of diagenesis. In the future, we should pay more attention to the study on the relationships among diagenesis, modern climate, sea-level change, atmospheric water transformation and microbial activity. It can provide more accurate and longer time series of paleoenvironmental information that coral reefs recorded.
Key words: Coral reefs    Palaeoenvironment    Paleoclimate.    Development Model    Diagenesis
收稿日期: 2016-11-26 出版日期: 2017-03-20
ZTFLH:  P737.2  
基金资助: 国家自然科学基金重大研究计划重点支持项目“珊瑚礁千米深钻记录的西沙碳酸盐台地形成演化和环境变迁史”(编号:91428203); 广西珊瑚礁资源与环境八桂学者项目(编号:2014BGXZGX03)资助
通讯作者: 余克服(1969-),男,湖北公安人,教授,主要从事珊瑚礁地质与生态环境研究.E-mail:kefuyu@scsio.ac.cn   
作者简介: 王瑞(1983-),男,安徽淮南人,讲师,主要从事珊瑚礁沉积岩石学研究.E-mail:wrzfl@gxu.edu.cn
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王瑞, 余克服, 王英辉, 边立曾. 珊瑚礁的成岩作用[J]. 地球科学进展, 2017, 32(3): 221-233.

Wang Rui, Yu Kefu, Wang Yinghui, Bian Lizeng. The Diagenesis of Coral Reefs. Advances in Earth Science, 2017, 32(3): 221-233.

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http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2017.03.0221        http://www.adearth.ac.cn/CN/Y2017/V32/I3/221

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