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...
Furkejuvvon:
| Váldodahkkit: | , , , , , , , |
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| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
Copernicus Publications
2012-11-01
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| Ráidu: | Biogeosciences |
| Liŋkkat: | http://www.biogeosciences.net/9/4353/2012/bg-9-4353-2012.pdf |
| Fáddágilkorat: |
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