据邦德·兰姆伯蒂说，研究人员可能错误地理解了碳循环在北极土壤中起作用的方式。
According to Bond-Lamberty, researchers might have a flawed understanding of how carbon cycling works in Arctic soil.
氧同位素会随着大气水循环而变化，硫同位素则根据地球岩床的不同而变化，通过它们我们就能确定地理位置。
Oxygen isotopes vary with the water cycle, and sulfur with bedrock, so they're location proxies.
通过维护和强化景观培植过程中的自然循环，自然本身便可以帮助我们更好地理解生命和死亡。
To support and strengthen the natural cycle in landscape cultivating, nature in itself can help us to get a better understanding of life and death.
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