Reciprocal transfer of carbon and nitrogen by decomposer fungi at the soil-litter interface

We have investigated whether decomposer fungi translocate litter-derived C into the underlying soil while simultaneously translocating soil-derived inorganic N up into the litter layer. We also located and quantified where the translocated C is deposited within the soil aggregate structure. When ¹³C-labeled wheat straw was decomposed on the surface of soil amended with ¹⁵N-labeled inorganic N, we found that C and N were reciprocally transferred by fungi, with a significant quantity (121-151 μg C g⁻¹ whole soil) of litter-derived C being deposited into newly formed macroaggregates (>250 μm sized aggregates). Fungal inhibition reduced fungal biomass and the bidirectional C and N flux by approximately 50%. The amount of litter-derived C found in macroaggregates was positively correlated with litter-associated fungal biomass. This fungal-mediated litter-to-soil C transfer, which to our knowledge has not been demonstrated before for saprophytic fungi, may represent an important mechanism by which litter C enters the soil and becomes stabilized as soil organic matter within the macroaggregate structure.     

Differential production of oxalate by mycorrhizal fungi in arid ecosystems

Oxalate crystals and elements binding to the surfaces of mycorrhizal fungal hyphae were examined using scanning electron microscopy coupled with X-ray analysis of elemental composition. Mycorrhizae from the arid zone vegetation types in southern California were examined including chaparral, riparian oak woodlands, coastal sage, grasslands, and deserts. Only mat-forming ectomycorrhizal hyphae, such as Hysterangium separabile, were found to produce oxalate crystals. None of the arbuscular mycorrhizal fungal hyphae (Glomus spp. and Acaulospora elegans) examined had crystal structures associated with them. The hyphae of Hysterangium separabile without crystals did not show the Ca peaks that were present when the crystals existed nor did the arbuscular mycorrhizal fungal hyphae have the Ca peaks. The elimination of arbuscular mycorrhizae using benomyl did not affect soil P or oxalate. These data indicate that there are some fundamental differences in chemical exudation between mycorrhizal fungi that could affect P uptake and cycling in arid ecosystems. Received: 7 December 1994     

Evidence for gluconic acid production by Enterobacter intermedium as an efficient strategy to avoid protozoan grazing

The effect of pure gluconic acid and of gluconic-acid-producing bacteria on the activity of three protozoan species, Colpoda steinii (a ciliate), Vahlkampfia sp. (an amoeba) and Neobodo designis (a flagellate), was determined in vitro and in soil microcosms. Pure gluconic acid was shown to mediate disappearance of active cells, due to encystment and/or death of protozoa, at 0.15 mM in saline medium. Similarly, the presence of gluconic acid inhibited excystment of the three protozoa tested. Enterobacter intermedium 60-2G (Wt), a gluconic acid-producing rhizobacterium, elicited the same effects on protozoa when co-cultured in the presence of 5 g L⁻¹ glucose. However, the effect was not observed when glucose was omitted from the medium. Similarly, a pqqA isogenic mutant strain, unable to produce gluconic acid from glucose, exhibited a reduced effect on protozoan activity. Rhizosphere-microcosm studies performed with wheat (Triticum aestivum L.) confirmed the reduced ability of the pqqA mutant to limit protozoa reproduction compared to the Wt strain. Since the sodium salt of gluconic acid did not cause any significant stress to protozoa and considering that addition of 50 mM Tris-Cl (pH 7.2) abolished the deleterious effect of gluconic acid, acidification of the medium appeared as the key factor that induced encystment/death of protozoa. We propose that production and excretion of gluconic acid should be considered an efficient mechanism evolved by bacteria to escape, tolerate or defend themselves against protozoan grazing in rhizosphere environments.