在湖泊沉积物中以温度控制的有机碳矿化
Cristian Gudasz1, David Bastviken, Kristin Steger
1Limnology, Department of Ecology and Evolution, Uppsala University, Norbyvägen 18D, SE-752 36 Uppsala, Sweden. cristian.gudasz@ebc.uu.se
Nature
|July 24, 2010
概括
温暖的温度增加了湖泊沉积物中的有机碳矿化,减少了碳埋葬. 气候变化可能会大大降低北极湖泊储存碳的能力.
科学领域:
- 环境科学 环境科学
- 临界技术 临界技术
- 生物地质化学生物地质化学
背景情况:
- 像湖泊这样的内陆水是全球碳循环的关键组成部分,但与其他碳汇相比,研究关注度有限.
- 在湖泊沉积物中沉积的有机碳经历矿化或长期埋葬,影响全球碳预算.
- 了解控制沉积物有机碳动态的因素对于预测气候变化影响至关重要.
研究的目的:
- 研究沉积物有机碳矿化与北极湖泊温度之间的关系.
- 评估预计气候变暖如何影响湖泊生态系统中的有机碳埋葬.
主要方法:
- 进行了瑞典北极湖泊的跨系统调查.
- 汇编和分析了全球各种湖泊的公布数据,气候,生产力和碳来源各不相同.
- 研究了沉积物有机碳矿化率与水温之间的相关性.
主要成果:
- 在湖泊沉积物中的有机碳矿化和温度之间发现了显著的正相关性.
- 更高的温度导致矿物化增加,因此减少有机碳埋葬.
- 据估计,在IPCC气候变化情景下,北极湖泊每年有机碳埋葬量可能减少4-27% .
结论:
- 湖泊沉积物有机碳矿化对温度非常敏感.
- 全球气温上升可能会降低北极湖泊作为长期碳沉积物的作用.
- 未来的碳埋藏在湖泊中可能会受到气候变暖的影响,需要更新全球碳循环模型.
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