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Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years
The reasons for the early Holocene temperature discrepancy between northern hemispheric model simulations and paleoclimate reconstructions—known as the Holocene temperature conundrum—remain unclear. Using hydrogen isotopes of fluid inclusion water extracted from stalagmites from the Milandre Cave in...
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| Publicat a: | Sci Adv |
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| Autors principals: | , , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
American Association for the Advancement of Science
2019
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6551184/ https://ncbi.nlm.nih.gov/pubmed/31183398 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aav3809 |
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