全球变暖和海洋酸化背景下珊瑚礁生态响应的研究进展

李言达, 易亮. 全球变暖和海洋酸化背景下珊瑚礁生态响应的研究进展[J]. 海洋地质与第四纪地质, 2021, 41(1): 33-41. doi: 10.16562/j.cnki.0256-1492.2020080501
引用本文: 李言达, 易亮. 全球变暖和海洋酸化背景下珊瑚礁生态响应的研究进展[J]. 海洋地质与第四纪地质, 2021, 41(1): 33-41. doi: 10.16562/j.cnki.0256-1492.2020080501
LI Yanda, YI Liang. A review on ecological response of coral reefs to global warming and oceanic acidification[J]. Marine Geology & Quaternary Geology, 2021, 41(1): 33-41. doi: 10.16562/j.cnki.0256-1492.2020080501
Citation: LI Yanda, YI Liang. A review on ecological response of coral reefs to global warming and oceanic acidification[J]. Marine Geology & Quaternary Geology, 2021, 41(1): 33-41. doi: 10.16562/j.cnki.0256-1492.2020080501

全球变暖和海洋酸化背景下珊瑚礁生态响应的研究进展

  • 基金项目: 上海市自然科学基金“晚新近纪渤海盆地陆-海转换的环境过程”(19ZR1459800)
详细信息
    作者简介: 李言达(1997―),男,本科生,主要从事古生物学研究,E-mail:ydli@pku.edu.cn
    通讯作者: 易亮(1982―),男,副教授,主要从事海洋沉积与年代学研究,E-mail:yiliang@tongji.edu.cn
  • 中图分类号: P736

A review on ecological response of coral reefs to global warming and oceanic acidification

More Information
  • 生物礁是由珊瑚虫、藻类等造礁生物组成、具有抗浪结构的海相碳酸盐岩,是全球主要碳库之一,也是观察热带海洋影响中-高纬度环境过程的重要窗口。近二、三十年以来,伴随着海洋水体的显著酸化和增温,全球热带海洋生物礁的主体——珊瑚礁系统遭受了不同程度的影响。其中,对于高温强迫而言,海水温度上升诱发珊瑚白化、抑制珊瑚的自我修复;海洋酸化可以显著改变珊瑚钙化率、抑制珊瑚幼虫发育、引发珊瑚礁的溶解;两大因素均可改变珊瑚礁的群落结构。针对这些环境要素的改变,珊瑚自身可以通过共生藻的种类转换以及调控基因表达等手段在一定程度上抵抗高温胁迫;但若温室气体的排放不受控制,绝大多数珊瑚礁到21世纪末都将遭受灾难性打击。为应对未来不同场景下的珊瑚礁变化,还需要对高温、酸化等关键因子响应特征进行更深入的研究;珊瑚礁长序列研究有可能为珊瑚的长周期演化特征提供关键认识,也为现代观测提供有益补充。

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  • 图 1  2015—2016年白化事件中全球珊瑚礁的白化程度统计[9]

    Figure 1. 

    图 2  海表温度上升对珊瑚礁群落的影响[3]

    Figure 2. 

    图 3  海洋酸化对珊瑚礁的影响[3]

    Figure 3. 

    图 4  海底火山通风口处CO2排放量对生物礁群落的影响[82]

    Figure 4. 

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出版历程
收稿日期:  2020-08-05
修回日期:  2020-11-06
刊出日期:  2021-02-28

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