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Global analysis reveals climatic controls on the oxygen isotope composition of cave drip water
The oxygen isotope composition of speleothems is a widely used proxy for past climate change. Robust use of this proxy depends on understanding the relationship between precipitation and cave drip water δ(18)O. Here, we present the first global analysis, based on data from 163 drip sites, from 39 ca...
| Autores principales: | , , , , , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2019
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6611902/ https://www.ncbi.nlm.nih.gov/pubmed/31278295 http://dx.doi.org/10.1038/s41467-019-11027-w |