Carbon Transfer from the Host to Tuber melanosporum Mycorrhizas and Ascocarps Followed Using a 13C Pulse-Labeling Technique

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Abstract

Truffles ascocarps need carbon to grow, but it is not known whether this carbon comes directly from the tree (heterotrophy) or from soil organic matter (saprotrophy). The objective of this work was to investigate the heterotrophic side of the ascocarp nutrition by assessing the allocation of carbon by the host to Tuber melanosporum mycorrhizas and ascocarps. In 2010, a single hazel tree selected for its high truffle (Tuber melanosporum) production and situated in the west part of the Vosges, France, was labeled with 13CO2. The transfer of 13C from the leaves to the fine roots and T. melanosporum mycorrhizas was very slow compared with the results found in the literature for herbaceous plants or other tree species. The fine roots primarily acted as a carbon conduit; they accumulated little 13C and transferred it slowly to the mycorrhizas. The mycorrhizas first formed a carbon sink and accumulated 13C prior to ascocarp development. Then, the mycorrhizas transferred 13C to the ascocarps to provide constitutive carbon (1.7 mg of 13C per day). The ascocarps accumulated host carbon until reaching complete maturity, 200 days after the first labeling and 150 days after the second labeling event. This role of the Tuber ascocarps as a carbon sink occurred several months after the end of carbon assimilation by the host and at low temperature. This finding suggests that carbon allocated to the ascocarps during winter was provided by reserve compounds stored in the wood and hydrolyzed during a period of frost. Almost all of the constitutive carbon allocated to the truffles (1% of the total carbon assimilated by the tree during the growing season) came from the host. © 2013 Le Tacon et al.

Figures

  • Table 1. Description of the maturation stages of T. melanosporum ascocarps (modified from Giovanni Pacioni, personal communication).
  • Table 2. Kinetics of d13C (in %) in leaves of the hazel tree A11 after pulse labeling and d13C of buds and branches sampled during the winter following the pulses.
  • Table 3. Kinetics of d13C (in %) in the fine roots and T. melanosporum mycorrhizas beneath hazel tree A11 in 2010–2011 after the pulse labelings of the leaves with 13CO2.
  • Table 4. (A) Maturity, numbers and fresh weight of ascocarps harvested beneath the labeled tree A11; (B) d13C (in %) in T. melanosporum ascocarps (peridium and gleba) beneath the labeled tree A11, and beneath non-labeled trees (natural abundance) at each sampling date from October 2010 to January 2011.
  • Table 5. Characteristics of the T. melanosporum ascocarps harvested in 2010–2011 beneath the labeled hazel tree A11 and estimations of the amounts of ascocarpic 13C derived from the host tree.
  • Figure 1. Temporal variation of d13C (%) in the fine roots, mycorrhizas and peridium and gleba of ascocarps beneath hazel tree A11 in 2010–2011. Error bars represent the standard deviation of the means. doi:10.1371/journal.pone.0064626.g001
  • Table 6. d13C (%) in the soil compartments (bulk soil, mycorhizospheric soil, soil adhering to the ascocarps) following the pulse labelings of the A11 hazel tree.
  • Table 7. d13C (%) in soil water extracts following the pulse labeling of the A11 hazel tree.

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CITATION STYLE

APA

Le Tacon, F., Zeller, B., Plain, C., Hossann, C., Bréchet, C., & Robin, C. (2013). Carbon Transfer from the Host to Tuber melanosporum Mycorrhizas and Ascocarps Followed Using a 13C Pulse-Labeling Technique. PLoS ONE, 8(5). https://doi.org/10.1371/journal.pone.0064626

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