Research progresses and development directions of carbonate rocks
碳酸盐岩研究进展与发展方向
Ya-Sheng Wu (吴亚生)1
1 University of Chinese Academy of Sciences, Beijing 100049, China
Abstracts
With the exceptions of inorganic origin, carbonate rocks are mainly
biogenic and are the main type of bioliths. Biocarbonate rocks are divided into
microbial carbonate rocks (microbiolith) and macrobiocarbonate rocks
(macrobiolith). Macrobiocarbonate rocks are divided into reef rocks and
non-reef carbonate rocks. Microbioliths are divided into microbialites, microallolites
and micro- reef rock (microlithite). The progresses in the study of carbonate
rocks are mainly manifested in the study of microbial carbonate rocks and
reefs, including the progresses of theories and methods, and some new important
understandings. The main objective of the speech is to review the key advances
in carbonate research, find existing problems, and propose key research
directions in the future.
除少数无机成因的以外，碳酸盐岩主要是生物成因的，是生物岩的主要类型。生物碳酸盐岩分为微生物碳酸盐岩、宏生物碳酸盐岩。宏生物碳酸盐岩分为生物礁岩和非礁碳酸盐岩。微生物碳酸盐岩分为微生物岩、微屑岩、微礁岩。碳酸盐岩研究的进展主要表现在微生物碳酸盐岩和生物礁研究方面，包括理论和方法的进步，以及一些重要认识的改变。报告的主要目标是梳理碳酸盐岩研究的关键进展，发现存在问题，提出今后的重点研究方向。
引用格式: 吴亚生，2025. 碳酸盐岩研究进展与发展方向. Biopetrology, 5(1): 8-68. https://biopetrology.com/tsyyyj