从同位素地球化学了解从冰盖到沿海海洋的循环
Katharine R Hendry1,2, Felipe Sales de Freitas3, Sandra Arndt3,4
1British Antarctic Survey, High Cross, Cambridge, UK.
概括
冰川气候变化释放出极地水中的轻溶,对藻至关重要. 这项研究使用同位素地质化学来追踪从冰川到海洋的二氧化,支持重要植物浮游生物的生长.
科学领域:
- * 生物地质化学
- * 海洋学 海洋学
- * 同位素地质化学
背景情况:
- *极地地区对于全球生物地球化学循环至关重要.
- *溶解的对于藻是必不可少的,藻是极地生态系统中关键的植物浮游生物群.
- * 冰川的气候变化被怀疑是溶解的主要来源沿海水域,特别是在藻面临限制的地方.
研究的目的:
- * 审查与循环有关的冰化边缘的生物地质化学复杂性.
- * 探索同位素地质化学如何提供洞察力,了解亚冰川的动员和陆地-海洋连续运输.
- * 了解来自冰川的二氧化在支持极地海洋生产力的作用.
主要方法:
- *对稳定性和放射性同位素测量的审查.
- *生物地质化学数值建模的应用.
- *分析同位素地质化学,以了解的动员和循环.
主要成果:
- * 亚冰川气候变化产生同位素轻型无形.
- *这种二氧化在海水中溶解,释放出溶解的.
- *同位素轻,冰川起源的破碎性二氧化到达海洋,可能支持显著的藻生产力,特别是在北极.
结论:
- *同位素地球化学提供了对动员和从冰川到海洋的循环的定量理解.
- * 来自冰川的二氧化在支持极地海洋生态系统中藻的生产力方面发挥着至关重要的作用.
- *未来的研究需要跨学科的方法来解决这些环境中循环的剩余问题.
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