在北极阿拉斯加湖泊沉积物中增强的沉积与早期Holocene水气候转移相吻合
Melissa Griffore1, Mark Abbott1, Eitan Shelef1
1Department of Geology and Environmental Science, University of Pittsburgh, Pittsburgh, PA, USA.
The Science of the total environment
|January 15, 2025
概括
气候变化对北极流域的 (Hg) 有影响. 降雨量增加驱动Hg动员,而植被变化影响湖泊沉积物Hg度,最近的峰值表明人为影响.
科学领域:
- 古气候学 古气候学
- 环境科学 环境科学
- 地质化学 地质化学
背景情况:
- 永久土融化释放大量的 (Hg) 进入北极流域.
- 甲基化Hg生物放大,造成生态风险.
- 长期有限的北极Hg记录阻碍了对气候变化影响的理解.
研究的目的:
- 为了重建一个永久土流域的Hg动态,超过27,000年.
- 为了研究过去的温度,降水和植被变化对Hg调动的影响.
主要方法:
- 来自阿拉斯加埋葬湖的27,000年 (Hg) 沉积物记录的分析.
- 的度和流量与古气候代理 (温度,降水,植被) 的相关性.
主要成果:
- 在最后一个冰川最大时期,Hg水平保持稳定.
- 冰期后的变暖并没有立即增加Hg.
- 大约11,000年前降水量增加显著提高了Hg度和流量.
- 在1990年CE中Hg的峰值水平表明了相当大的人为影响.
结论:
- 夏季降雨是从北极水域调动 (Hg) 的主要驱动因素.
- 植被变化影响湖泊沉积物中的Hg度.
- 最近的Hg增加凸显了气候变化和人为排放的综合影响.
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