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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...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2019
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6551184/ https://www.ncbi.nlm.nih.gov/pubmed/31183398 http://dx.doi.org/10.1126/sciadv.aav3809 |