在过去的八个冰川周期中,全球生物圈的初级生产率发生了变化
Ji-Woong Yang1, Margaux Brandon1,2, Amaëlle Landais1
1Laboratoire des Sciences du Climat et de l'Environnement/Institut Pierre-Simon Laplace, Université Paris Saclay/CEA/CNRS/UVSQ, Gif-sur-Yvette, France.
概括
全球生物圈的生产力,最大的二氧化碳 (CO2) 吸收,在过去的冰川时期较低. 增加的二氧化碳水平似乎推动了这种生产力,
科学领域:
- 古气候学
- 生物地质化学
- 地球系统科学
背景情况:
- 全球生物圈的生产力是大气中二氧化碳 (CO2) 循环的一个关键因素.
- 准确估计过去的全球生物圈生产力对于了解碳循环动态至关重要.
- 目前用于估计历史生物圈生产力的方法有局限性.
研究的目的:
- 为了重建全球生物圈生产力的80万年记录.
- 研究过去生物圈生产力与大气二氧化碳水平之间的关系.
- 了解生物圈在冰川间气候周期中的作用.
主要方法:
- 对被困在极地冰核中的大气氧的三倍同位素比率的分析.
- 在过去的80万年里重建了大气组成.
- 生物圈生产率指标与二氧化碳和气候数据的相关性.
主要成果:
- 这项研究提供了全球生物圈生产率的第一个80万年记录,
- 在过去的八个冰河时期, 全球生物圈的生产率低于工业化前的水平.
- 生物圈生产率的提高往往在几千年之前发生,并与二氧化碳的变化相吻合.
结论:
- 大气中的二氧化碳是全球生物圈生产力的首要驱动力.
- 在冰川气候条件下,生物圈的生产力表现出负反机制.
- 了解过去的生产率变化可以提高对未来碳循环应对气候变化的预测.
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