多面性颗粒驱动海洋中的碳捕获
Philip W Boyd1, Hervé Claustre2, Marina Levy3
1Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Tasmania, Australia. philip.boyd@utas.edu.au.
Nature
|April 19, 2019
概括
海洋通过颗粒沉积捕获大气中的碳,但其他"颗粒注入"也同样重要. 这些机制有助于平衡海洋
科学领域:
- 海洋学
- 气候科学
- 海洋生物学
背景情况:
- 海洋通过封存大气中的碳来调节全球气候起着至关重要的作用.
- 生物是由沉没的有机粒子驱动的, 是深海碳储存的关键机制.
- 目前的模型表明,仅重力沉积不足以解释深海的碳预算和营养循环.
研究的目的:
- 审查和突出额外的机制,称为"颗粒注入",有助于碳运输到深海.
- 建议这些颗粒注入在封存碳方面发挥重要作用, 可能与引力的贡献相匹配.
- 强调需要进一步研究这些对海洋碳排放的控制和重要性.
主要方法:
- 对深海粒子运输所涉及的生物和物理过程的文献综述.
- 综合现有的粒子流量和碳预算在半层区域的数据.
- "粒子注入"作为重力生物的补充机制的概念化.
主要成果:
- 确定了多种生物和物理机制,
- 建议这些颗粒注入对碳封存做出重大贡献,可能等同于引力沉积的流量.
- 通过包括这些额外的来更好地解释中性碳预算的差异.
结论:
- 粒子注入可能是海洋生物碳的主要,被低估的组成部分.
- 了解这些对于准确建模海洋碳捕获及其对气候变化的反应至关重要.
- 需要对粒子注入的环境驱动因素和定量影响进行进一步的调查.
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