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21世纪人类造成的海洋酸化及其对化生物的影响.

James C Orr1, Victoria J Fabry, Olivier Aumont

  • 1Laboratoire des Sciences du Climat et de l'Environnement, UMR CEA-CNRS, CEA Saclay, F-91191 Gif-sur-Yvette, France. orr@cea.fr

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科学领域:

  • 海洋化学和海洋学
  • 气候变化对海洋生态系统的影响
  • 生物地质化学循环 生物地质化学循环

背景情况:

  • 目前,海洋表面已经和了碳酸.
  • 大气中二氧化碳的增加降低了海洋的pH值和碳酸盐离子度.
  • 这种趋势阻碍了包括珊瑚和浮游生物在内的海洋化生物保持其骨架.

研究的目的:

  • 为了预测未来的海洋碳酸和度水平.
  • 评估人为二氧化碳排放在商业常规场景下的影响.
  • 评估海洋生态系统中有害条件的时间表.

主要方法:

  • 利用了13个海洋碳循环模型.
  • 在IS92a排放场景下模拟碳酸和度.
  • 进行了船上的实验,将活类动物暴露在预测的低和水平下.

主要成果:

  • 预计到2050年,南大洋的地表水在阿拉贡石方面会变得不和.
  • 到2100年,低和可能会扩展到整个南大洋和亚北极太平洋.
  • 类动物的贝在暴露于预测的低和状态时显示出显著的溶解.

结论:

  • 几十年内,可能会出现对高度海洋生态系统有害的条件.
  • 以前的估计表明,这些变化将在几个世纪内发生.
  • 应对二氧化碳排放采取紧急行动,以减轻生态系统损害.