Two centuries-long records of skeletal calcification in massive Porites colonies from Meiji Reef in the southern South China Sea and its responses to atmospheric CO_2 and seawater temperature

作     者：SHI Qi YU KeFu CHEN TianRan ZHANG HuiLing ZHAO MeiXia YAN HongQiang 

作者机构：Key Laboratory of Marginal Sea GeologySouth China Sea Institute of OceanologyChinese Academy of SciencesGuangzhou 510301China 

出 版 物：《Science China Earth Sciences》 (中国科学（地球科学英文版）)

年 卷 期：2012年第55卷第1期

页      面：1-12页

核心收录：

学科分类：07[理学] 0707[理学-海洋科学] 0708[理学-地球物理学] 09[农学] 0903[农学-农业资源与环境] 0704[理学-天文学] 

基　　金：supported by the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant No. XDA05080300) Important Direction Project of Knowledge Innovation Program of the Chinese Academy of Sciences (Grant No. KZCX2-YW-138) National Natural Science Foundation of China (Grant Nos. 40830852 and 41025007) Chinese Ministry of Science and Technology Projects (Grant Nos. 2007CB8015905 and 2006BAB19B03) 

主　　题：大气二氧化碳浓度 中国海 钙化 骨骼 海水温度 殖民地 微孔 反应 

摘      要：Rising atmospheric CO2 and warming of the global climate that have occurred since the industrial revolution are regarded as fatal threats to coral reefs. We analyzed the skeletal calcification rate of 14 massive Porites corals from the Meiji Reef in the southern South China Sea through X-ray photography of coral skeletons. A general pattern of change in coral skeletal calcification was determined. The change pattern of coral calcification on the Meiji Reef over the past two centuries can be divided into five periods: calcification increase in 1770–1830, 1870–1920, and 1980–2000 and calcification decline in 1830–1870 and 1920–1980. Over the past two centuries, the largest increase in calcification was 4.5%, occurring in 1770–1830, whereas the largest decline in calcification was 6.2%, occurring in 1920–1980. Coral calcification slightly increased in the recent 20 years (1980–2000). The response relationship of coral calcification to atmospheric CO2 and sea surface temperature (SST) shows that calcification was not correlated with atmospheric CO2 but responded nonlinearly to SST with maxima at ∼27.2°C in 1900–2000. On the Meiji Reef, increasing atmospheric CO2 had a negligible effect on coral growth in the past century. However, rising SST improved coral growth in the early and middle 20th century, and restricted coral growth in the recent 20 years.