科利托对碳酸盐化学和海洋酸化的敏感性
L Beaufort1, I Probert, T de Garidel-Thoron
1CEREGE, CNRS/Université Aix-Marseille, Avenue L. Philibert BP80, 13545 Aix-en-Provence, Cedex 4, France. beaufort@cerege.fr
Nature
|August 5, 2011
概括
海洋酸化威胁着海洋生物. 这项研究表明,增加二氧化碳 (CO2) 水平会降低可可利多,关键植物浮游生物的化,影响海洋碳循环.
科学领域:
- 海洋生物学 海洋生物学
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
背景情况:
- 海洋吸收大约三分之一的人为二氧化碳 (CO2).
- 这种吸收导致海洋酸化,对海洋生态系统,特别是化生物构成重大威胁.
- 丰富的植物浮游生物科科科利托福,是海洋碳酸盐生产的关键贡献者.
研究的目的:
- 量化过去4万年来占主导地位的科利托福的石质量.
- 为了研究化,二氧化碳水平和碳酸盐化学之间的关系.
- 了解可可利多对环境变化的集合级反应.
主要方法:
- 在占主导地位的科利多中量化石质量.
- 与海洋碳酸盐化学相关的科利托分布的分析.
- 检查了4万年历史的化石记录.
主要成果:
- 观察到一个明显的减少化的模式,随着二氧化碳部分压力的增加和碳酸离子度的下降.
- 具有不同化水平的物种和形态类型根据海洋碳酸盐化学分布.
- 在现代低pH水中发现了一种严重化的Emiliania huxleyi形态.
结论:
- 海洋酸化显著影响了可可利托的化和分布.
- 化模式的变化表明对海洋碳循环有重大影响.
- 集合级响应的复杂性凸显了对海洋生态系统适应的进一步研究的需要.
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