Cargando…
Penultimate deglacial warming across the Mediterranean Sea revealed by clumped isotopes in foraminifera
The variability of seawater temperature through time is a critical measure of climate change, yet its reconstruction remains problematic in many regions. Mg/Ca and oxygen isotope (δ(18)O(C)) measurements in foraminiferal carbonate shells can be combined to reconstruct seawater temperature and δ(18)O...
| Autores principales: | , , , , , , , |
|---|---|
| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2017
|
| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5707372/ https://www.ncbi.nlm.nih.gov/pubmed/29185446 http://dx.doi.org/10.1038/s41598-017-16528-6 |