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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Detalles Bibliográficos
Autores principales: Affolter, Stéphane, Häuselmann, Anamaria, Fleitmann, Dominik, Edwards, R. Lawrence, Cheng, Hai, Leuenberger, Markus
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2019
Materias:
Research Articles
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

Internet

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

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