印度尼西亚加利曼坦地区的泥土的诞生和发展
Gusti Z Anshari1,2, Monika Ruwaimana3, Rasis Putra Ritonga4
1Soil Science Department, Universitas Tanjungpura, Jalan Hadari Nawawi, Pontianak, West Kalimantan, 78124, Indonesia. gzanshari@live.untan.ac.id.
Scientific reports
|January 20, 2026
概括
卡利曼坦的泥炭地始于中 Holocene (沿海) 和晚 Pleistocene (内陆). 稳定的水文是碳捕获的关键,排水造成了大量的容量损失.
科学领域:
- 地球科学 地球科学 地球科学
- 环境科学 环境科学
- 古气候学 古气候学
背景情况:
- 加利曼丹的泥炭地具有多样化的地形特征.
- 由于时间数据有限,人们对泥炭地开始的时间和驱动因素的了解很少.
研究的目的:
- 重建加利曼丹泥炭地的发展和碳积累历史.
- 为了确定泥炭地启动和碳封存的驱动因素.
主要方法:
- 利用55个放射性碳年龄和贝叶斯年龄深度建模.
- 分析了来自西部和东喀里曼丹内陆和沿海地区的15个泥炭核心.
主要成果:
- 沿海泥炭的开始发生在中 Holocene,与海平面上升有关.
- 内陆泥炭的形成始于普莱斯托纪晚期.
- 碳积累在稳定的水文条件下在中 Holocene 达到峰值,但在 Holocene 晚期下降.
- 目前热带泥炭地的排水造成了碳捕集能力的显著损失.
结论:
- 可持续的水平衡对于长期的泥炭生长和碳捕获至关重要.
- 水文干扰大大减少了泥炭地中的碳储存.
- 由于排水,碳捕获能力的下降与自然速度相比是相当大的.
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