珊瑚礁将在本世纪末之前转变为净溶解
Bradley D Eyre1, Tyler Cyronak2, Patrick Drupp3
1Centre for Coastal Biogeochemistry, School of Environment, Science and Engineering, Southern Cross University, Lismore, NSW 2480, Australia. bradley.eyre@scu.edu.au.
概括
海洋酸化加速了碳酸 (CaCO3) 礁石沉积物的溶解,这一过程比珊瑚化敏感10倍. 这种净溶解的转变将在2050年全球威胁珊瑚礁.
科学领域:
- 海洋化学
- 地质化学
- 珊瑚礁生态
背景情况:
- 由于大气中的二氧化碳吸收而导致的海洋酸化降低了海洋pH值.
- 珊瑚礁由于酸性增加而面临较低的化.
- 碳酸 (CaCO3) 沉积物溶解对珊瑚礁来说是一个不明确的威胁.
研究的目的:
- 量化CaCO3沉积物溶解对海洋酸化的敏感性.
- 评估海洋酸化对珊瑚礁沉积物稳定的全球影响.
主要方法:
- 在五个全球地点的珊瑚礁沉积物中分析CaCO3溶解率.
- 溶解速度与覆盖海水的和度 (Ωar) 的相关性.
- 沉积物溶解对海洋酸化和珊瑚化的敏感度的比较.
主要成果:
- 沉积物的CaCO3溶解与海水的和状态 (Ωar) 有负相关性.
- 珊瑚礁沉积物溶解对海洋酸化的敏感性比珊瑚化高10倍.
- 全球珊瑚礁沉积物预计将在2.92±0.16的 Ωar中从净降水过渡到净溶解,预计在2050年左右.
结论:
- 海洋酸化对珊瑚礁沉积物的完整性构成重大威胁.
- 珊瑚礁沉积物比之前估计的更容易溶解.
- 一些珊瑚礁已经经历了沉积物净溶解,表明迫切需要减缓策略.
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