刚果盆地中部泥炭地群的年龄,面积和碳储存
Greta C Dargie1,2, Simon L Lewis1,2, Ian T Lawson3
1School of Geography, University of Leeds, Leeds LS2 9JT, UK.
Nature
|January 13, 2017
概括
位于刚果盆地的Cuvette Centrale拥有世界上最大的热带泥炭地, 这些重要的泥炭地很容易受到气候变化和土地利用的影响.
科学领域:
- 生态学
- 地质科学
- 气候科学
背景情况:
- 泥炭地是重要的碳汇, 尽管只占地球表面的3%,
- 这些富含碳的生态系统主要在凉爽的气候条件下形成,但也存在于热带沼泽森林中.
研究的目的:
- 调查和量化刚果中部库维特中部地区的泥炭沉积量和碳储存量.
- 确定泥炭积累的年龄,并了解导致它们形成的环境条件.
主要方法:
- 进行了现场测量,以确定和描述泥炭沉积物 (有机物质≥65%,深度≥0.3米).
- 通过放射性碳测年法确定了泥炭积聚的时间表.
- 在现场和遥感数据被结合起来,估计了泥炭地的总面积和碳库存.
主要成果:
- 在中央库维特的沼泽森林下确认了大量的泥炭沉积物,大约在10,600年前开始积累.
- 据估计,Cuvette Centrale泥炭地占地145500平方公里,是最广泛的热带泥炭地.
- 这些泥炭地储存了大约30.6百克的碳,大大增加了全球热带泥炭地碳估计.
结论:
- 中央库维特是一个主要的,以前被低估的热带泥炭地系统.
- 发现的碳储量相当于整个刚果盆地热带森林的地表碳.
- 这些巨大的碳储量容易因土地使用变化和降雨模式的改变而退化.
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