DEVELOPING BIOGEOCHEMICAL TRACERS OF APATITE WEATHERING BY ECTOMYCORRHIZAL FUNGI
To test the utility of these tracers, we grew birch seedlings under controlled P-limited conditions, supplemented with mesh bags containing granite chips. Our experimental design included nonmycorrhizal (NM) and ectomycorrhizal cultures (Cortinarius or Leccinum). Resulting mycorrhizal roots and leachates of granite chips were analyzed for these tracers.
REE concentrations in roots were greatly elevated in treatments with granite relative to those without granite, demonstrating uptake of apatite dissolution products. Roots with different mycorrhizal fungi accumulated similar concentrations of REEs and were generally elevated compared to the NM cultures. Leaches of granite chips grown in contact with mycorrhizal hyphae show elevated REE concentrations and significantly radiogenic Pb isotope signatures relative to bulk rock, also indicating apatite dissolution. These results are consistent with analyses of sporocarps collected at the Bartlett Experimental Forest, in which Cortinarius Pb isotope ratios were more radiogenic than those of other ectomycorrhizal sporocarps. Taken together, the experimental and field results imply that the coupled approach of REE and Pb isotopic values afford a means to assess differences in the contribution of mycorrhizal weathering to ecosystem nutrient budgets.