在未来的北极条件下,本土矿物重矿化,并评估温暖沉积物中碳封存变化的潜力
Arunima Sen1,2, Eric Jordà Molina3, Thaise Ricardo de Freitas4
1Department of Arctic Biology, The University Centre in Svalbard (UNIS), Longyearbyen, Norway. arunimas@unis.no.
Scientific reports
|October 7, 2024
概括
北极海洋变暖将导致海底再矿化增加,原因是温度升高和粮食供应. 实验表明,综合因素显著提高沉积物氧气需求,处理更多的碳和减少北极.
科学领域:
- 海洋科学 海洋科学
- 海洋学 海洋学 海洋学
- 生物地质化学生物地质化学
背景情况:
- 有机物质的地重矿化对海洋碳的命运和封存至关重要.
- 预计北极地区的变暖会增加海底水温,并给海底提供不稳定的碳供应.
- 预计这些变化将加速北极生态系统的盆地重矿化速度.
研究的目的:
- 实验研究沉积物氧需求 (SOD) 对北极温度升高和粮食供应的反应.
- 在模拟的未来海洋条件下提供关于北极盆地重矿化早期数据.
- 评估温度和碳供应对海底过程的综合影响.
主要方法:
- 收集了各种北极条件和制度的沉积物氧气需求 (SOD) 的实验数据.
- 操纵沉积物温度和可变碳供应以模拟未来的北极条件.
- 测量SOD速率作为横跨季节性和空间梯度 (架子到深盆地) 的盆地再矿化的一个代理.
主要成果:
- 温度的升高和食物供应的增加都单独导致SOD率显著上升.
- 温度升高和食物供应的结合导致SOD最大的增加 (50%到十倍).
- 这些综合效应在所有四个季节和研究的空间梯度中都是一致的.
结论:
- 北极土表现出一个显著的能力来处理增加的碳脉冲.
- 在变暖条件下,沉积碳的增加很可能被利用而不是积累.
- 这种处理对海洋碳储存产生影响,可能会降低北极作为全球碳汇的作用.
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