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A synthetic standard for the analysis of carbon isotopes of carbon in silicates, and the observation of a significant water-associated matrix effect
BACKGROUND: Due to the biogeochemical fractionation of isotopes, organic material can be heterogeneous at the microscale. Because this heterogentiy preserves in the rock record, the microscale measurement of carbon isotopes is an important frontier of geobiology. Such analyses via secondary ion mass...
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Springer International Publishing
2015
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4569672/ https://www.ncbi.nlm.nih.gov/pubmed/26379472 http://dx.doi.org/10.1186/s12932-015-0029-x |