全球泥炭地面积在全新纪期间的时空空间分布
Hui Liu1,2, Haibin Wu3,4, Wenchao Zhang1,5
1State Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China.
Scientific data
|January 9, 2025
概括
全球泥炭地在早期的全新世纪显著扩大,影响了碳循环. 这项研究重建了超过12,000年的泥炭地分布,有助于气候变化研究.
科学领域:
- 生态系统科学 生态系统科学
- 古气候学 古气候学
- 地理空间分析的研究.
背景情况:
- 泥炭地是影响全球碳循环和气候变化的关键陆地生态系统.
- 关于全球泥炭地的长期演变和空间分布存在不确定性.
研究的目的:
- 为了重建整个全新世纪的全球泥炭地的时空分布.
- 为分析陆地碳循环和气候变化提供一个强大的数据集.
主要方法:
- 编制了4700个基底泥炭地和669个花粉粉的数据.
- 使用的缓冲分析 (BA) 和反向距离加权 (IDW) 插值.
- 重建的泥炭地每1000年以0.5°×0.5°的分辨率发生变化.
主要成果:
- 在北美,欧洲和西西伯利亚的泥炭土面积在早期的全新纪期间大幅扩大.
- 全球泥炭地面积在12-6ka BP之间从2.18Mkm2增加到4.03Mkm2.
- 在6ka BP之后,泥炭土面积稳定在大约4.15Mkm2.
结论:
- 重建的全球泥炭地分布为Holocene碳循环和气候变化研究提供了有价值的数据.
- 该数据库对于模拟泥炭地甲排放特别有用.
- 了解过去的泥炭地动态对于预测未来气候变化影响至关重要.
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