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bn:01014205n
Noun Named Entity
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No term available
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In geochemistry, paleoclimatology, and paleoceanography δ13C is an isotopic signature, a measure of the ratio of the two stable isotopes of carbon—13C and 12C—reported in parts per thousand. Wikipedia
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σταθερά ισότοπα
άνθρακα-13
άνθρακας-12

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