Variation in stable carbon and oxygen isotopes of individual benthic foraminifera: tracers for quantifying the magnitude of isotopic disequilibrium
Stable carbon and oxygen isotopic compositions (δ<sup>13</sup>C and δ<sup>18</sup>O) of benthic foraminiferal carbonate shells have been used to reconstruct past bottom-water environments. However, the details of factors controlling the isotopic disequilibrium between the she...
Kaydedildi:
| Asıl Yazarlar: | , , , , , , , |
|---|---|
| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Copernicus Publications
2012-11-01
|
| Seri Bilgileri: | Biogeosciences |
| Online Erişim: | http://www.biogeosciences.net/9/4353/2012/bg-9-4353-2012.pdf |
| Etiketler: |
Etiket eklenmemiş, İlk siz ekleyin!
|