年轻的有机物作为二氧化碳来源,来自亚马逊河流的排气
Emilio Mayorga1, Anthony K Aufdenkampe, Caroline A Masiello
1School of Oceanography, University of Washington, Seattle, Washington 98195, USA. emiliomayorga@alum.mit.edu
Nature
|July 29, 2005
概括
由于呼吸新鲜有机物质,亚马逊河流释放出大量的二氧化碳. 一个小的,快速循环的碳池驱动这些大流从陆地到大气.
科学领域:
- 环境科学 环境科学
- 生物地质化学生物地质化学
- 同位素地球化学 同位素地球化学
背景情况:
- 河流过度和二氧化碳,导致大量的气体逃逸.
- 亚马逊河流表现出大量的二氧化碳排放,影响了区域碳预算.
- 河流中呼吸碳的来源和周转时间仍在争论中.
研究的目的:
- 为了调查碳的来源和循环,推动亚马逊河流中的二氧化碳超和.
- 为了确定河流系统中呼吸的有机物质的年龄和起源.
- 为了将碳同位素组成与二氧化碳逃逸流联系起来.
主要方法:
- 对碳同位素组成 (13C和14C) 的广泛调查.
- 分析溶解的无机碳和三种有机碳的大小部分.
- 在整个亚马逊河流系统中采样.
主要成果:
- 当代有机物 (<5年) 的呼吸是二氧化碳过剩的主要来源.
- 河流运输的散装有机碳分数显著更古老 (几十到数千年).
- 一个小的,快速循环的有机碳池为高逃避流提供燃料.
结论:
- 当代的陆地和近河有机物为亚马逊河二氧化碳排放提供燃料.
- 一个小型有机碳池的快速循环是理解大热带河流碳流的关键.
- 这一发现对区域碳预算和气候模型有影响.
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