  Organic material found in meteorites and interplanetary dust particles is
enriched in D and 15N. This is consistent with the idea that the functional
groups carrying these isotopic anomalies, nitriles and amines, were formed by
ion-molecule chemistry in the protosolar nebula. Theoretical models of
interstellar fractionation at low temperatures predict large enrichments in
both D and 15N and can account for the largest isotopic enrichments measured in
carbonaceous meteorites. However, more recent measurements have shown that, in
some primitive samples, a large 15N enrichment does not correlate with one in
D, and that some D-enriched primitive material displays little, if any, 15N
enrichment. By considering the spin-state dependence in ion-molecule reactions
involving the ortho and para forms of H2, we show that ammonia and related
molecules can exhibit such a wide range of fractionation for both 15N and D in
dense cloud cores. We also show that while the nitriles, HCN and HNC, contain
the greatest 15N enrichment, this is not expected to correlate with extreme D
enrichment. These calculations therefore support the view that Solar System 15N
and D isotopic anomalies have an interstellar heritage. We also compare our
results to existing astronomical observations and briefly discuss future tests
of this model.
