CHELI, GIULIA Statistiche
CHELI, GIULIA
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Dryness at 4.7 ka is more intense than at 4.2 ka in Sardinia (Italy): what is the real structure of the so called “4.2 event”?
2025-01-01 Columbu, A.; Cheli, G.; Isola, I.; Dong, X.; Pérez-Mejías, C.; Cheng, H.; Dallai, L.; De Waele, J.; Zanchetta, G.
Why did the Neanderthals go extinct? The role of speleothems in answering this hot question
2025-01-01 Columbu, Andrea; Cheli, Giulia; Zanchetta, Giovanni; Isola, Ilaria; Spötl, Christoph; Cheng, Hai; Berna, Francesco; Barzilai, Omry; Benazzi, Stefano
Climate variability at around the 4.2 event based on novel δ18O- δ13C speleothem data from Sardinia (Italy, Western Mediterranean)
2024-01-01 Cheli, G.; Zanchetta, G.; Isola, I.; Dong, X.; Pérez-Mejías, C.; Cheng, H.; Dallai, L.; De Waele J., &; Columbu, A.
| Titolo | Data di pubblicazione | Autore(i) | File |
|---|---|---|---|
| Dryness at 4.7 ka is more intense than at 4.2 ka in Sardinia (Italy): what is the real structure of the so called “4.2 event”? | 1-gen-2025 | Columbu, A.; Cheli, G.; Isola, I.; Dong, X.; Pérez-Mejías, C.; Cheng, H.; Dallai, L.; De Waele, J.; Zanchetta, G. | |
| Why did the Neanderthals go extinct? The role of speleothems in answering this hot question | 1-gen-2025 | Columbu, Andrea; Cheli, Giulia; Zanchetta, Giovanni; Isola, Ilaria; Spötl, Christoph; Cheng, Hai; Berna, Francesco; Barzilai, Omry; Benazzi, Stefano | |
| Climate variability at around the 4.2 event based on novel δ18O- δ13C speleothem data from Sardinia (Italy, Western Mediterranean) | 1-gen-2024 | Cheli, G.; Zanchetta, G.; Isola, I.; Dong, X.; Pérez-Mejías, C.; Cheng, H.; Dallai, L.; De Waele J., &; Columbu, A. |