Stepwise combustion analyses of distinct nitrogen isotopic compositions on Paleoproterozoic organic matter

抄録

Nitrogen isotopic analyses were conducted on two kerogenous samples from the Gunflint Formation (ca. 1.9 Ga) using the stepwise combustion technique to evaluate a potential analytical problem for the carbonaceous samples and to assess if this method is appropriate for the analysis of ancient rocks. Two discriminated δ¹⁵N plateaux are identified for each sample with mean values of +5.0‰ and +7.3‰ for sample 0708, and +6.1‰ and +5.2‰ for sample 0704, respectively. The direction of the δ¹⁵N shift is opposite in each sample. This characteristic excludes the possibility of analytical artifact as the source of isotope fractionation and metamorphism isotope fractionation. The two δ¹⁵N plateaux observed for each of the samples are characterized by different activation energies for the co-released carbon. These results suggest that similarly aged sedimentary rocks may contain at least two types of organic matter that record different source information for δ¹⁵N.