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When Stevenson followed the carbon-14 trail back in time, he found carbon-14 levels change with the intensity of solar burning.
当史蒂文森依据碳-14的痕迹追溯过去时,他发现碳-14的含量随着太阳燃烧的强度而变化。
The particles interfere with the formation of carbon-14 on earth.
这些粒子干扰了地球上碳-14的形成。
Doctors Stevenson is analyzing one element—carbon-14 in ring from both living and dead trees.
史蒂文森博士正在分析一种元素——活树和死树年轮中的碳-14。
And carbon 14, 6 again and it has 8, and it is found in vanishingly small amounts, 10 10 to the minus 12 or part per trillion.
碳14,6个质子,8个中子,它的存在是非常微小的,几乎趋于零,万亿分之。
4 And then there are the last four, carbon 14, which is a radioactive form.
然后,还有碳,以放射性形式存在。
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