The carbon isotopic signature of the upper mantle is heterogeneous
Abstract Knowledge of the carbon isotopic (δ13C) signature of the mantle source region of mid–ocean ridge basalts, is key to understanding carbon cycling on a planetary scale. This value has long been held at –4‰ from the study of popping rocks or –5‰ from the study of peridotitic diamonds, with lit...
I tiakina i:
| Ngā kaituhi matua: | , , , , , |
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| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Nature Portfolio
2025-01-01
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| Rangatū: | Communications Earth & Environment |
| Urunga tuihono: | https://doi.org/10.1038/s43247-024-01973-9 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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