热带地理 ›› 2016, Vol. 36 ›› Issue (1): 41-47.doi: 10.13284/j.cnki.rddl.002803

• 论文 • 上一篇    下一篇

珊瑚礁海水pH变化及其对海洋酸化的意义

陈雪霏,韦刚健,邓文峰,邹洁琼   

  1. (中国科学院广州地球化学研究所,同位素地球化学国家重点实验,广州 510640)
  • 出版日期:2016-01-05 发布日期:2016-01-05
  • 通讯作者: 韦刚健(1968―),男,广西南宁人,研究员,博士,主要从事珊瑚礁气候变化研究(E-mail)gjwei@gig.ac.cn。
  • 作者简介:陈雪霏(1989―),女,陕西西安市人,博士研究生,主要从事珊瑚礁海水酸化研究,(E-mail)chenxf@gig.ac.cn
  • 基金资助:
    国家重大科学研究计划项目(2013CB956102);国家自然科学基金项目(41325012、41076025)

Reef Water pH Variation and Its Implications for Ocean Acidification

CHEN Xuefei,WEI Gangjian,DENG Wenfeng,ZOU Jieqiong   

  1. (State Key Laboratory of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China)
  • Online:2016-01-05 Published:2016-01-05

摘要: 珊瑚钙质骨骼δ11B重建的海水pH时间变化序列显示:珊瑚礁海水pH的长期变化具有显著的年际―年代际波动周期,并且这些波动是区域海洋气候过程和珊瑚礁海水生物活动共同作用的结果。珊瑚礁生态系统中的生物活动(光合呼吸作用和钙化作用)控制着海水碳酸盐系统的组成,调节着海水pH的变化。这一过程在全球气候环境变化和区域海气过程的影响下,一起作用于珊瑚礁海水pH的变化,因而使得不同海域的珊瑚礁海水对海洋酸化的响应有所差别。研究珊瑚礁生物活动在长时间尺度上对海水pH的作用对认识珊瑚礁海水酸化机理十分重要,同时也是了解珊瑚礁生态系统如何响应海洋酸化的重要手段。

关键词: 珊瑚礁, 碳酸盐体系, 海洋酸化, 硼同位素

Abstract: In the recent century, it is calculated that reef water pH has fallen by 0.2-0.3 pH units worldwide due to the increase of atmospheric CO2 concentration, threatening the life of coral reefs. However, the long-term variation of reef water pH revealed by δ11B in the calcareous skeletons of coral demonstrates eminent interannual and decadal periodicities, and the variation was a result of the combined influences of regional marine climate processes and biological activities in the reef ecosystem. Metabolism in reef waters controls the dynamics of carbonate system parameters and regulates the variations of water pH. Influenced by global climate and environmental changes and regional marine climate processes, biological activities in reef water exert effects on variations of seawater pH, resulting in differential responses to ocean acidification from coral reef water of different sea areas. Therefore, learning the effects of the biological activities of coral reefs on marine water pH at long-term time scales is very important for understanding the acidification mechanisms of coral reef waters, and it is also an important means to learn how the coral reef ecosystem responds to ocean acidification.

Key words: coral reefs, carbonate system, ocean acidification, Boron isotope composition