Interactions between glyphosate and autochthonous soil fungi surviving in aqueous solution of glyphosate
Introduction
Increased consumption and high efficiency of herbicide Roundup stimulates studies not only on its activity and persistence in soil, but also on undesired interactions with soil microorganisms. Plants metabolize an active substance of Roundup–glyphosate only to low extent or do not metabolize it at all. Reactions catalyzed by microbial enzymes and adsorption on the surface of mineral components of soil play the mostly significant role in its persistence, bioavailability and mobility (Rueppel et al., 1997, Forlani et al., 1999, Busse et al., 2001, Araujo et al., 2003, Haney et al., 2003, Gimsing et al., 2004, Kools et al., 2005, Sorensen et al., 2006). Glyphosate is adsorbed by ferric and aluminum oxide (Gimsing et al., 2004) as well as by organic substances (Piccolo et al., 1996, Mamy and Barriuso, 2005).
The consequences of the application of glyphosate are changes in microbiological structure of soil, probably as the result of stimulation of growth of fungi. Araujo et al. (2003), pointed out on the increase of fungal counts in the presence of Roundup, which could be the effect of its direct or indirect interaction with other microorganisms.
Fungi can utilize glyphosate as nutriment and also as energetic substrate (Krzyśko-Łupicka and Orlik, 1997, Krzyśko-Łupicka et al., 1997). Significant for agricultural environment is the type of fungi arising after Roundup treatment, in particular the presence of phytopathogens in this group. Glyphosate inhibits growth of mycorrhizal fungi and consequently may stimulate the growth of Fusarium fungi (Levesque and Rahe, 1992). In spite of the persistence of C–P bond, glyphosate does not accumulate in soil, since microorganisms are capable to breakdown this bond, with the release of inorganic phosphorus.
Glyphosate degradation is performed co-metabolically and decomposition rate should depend on the general activity of soil microorganisms (Gimsing et al., 2004). Biodegradation products of glyphosate (N-phosphonomethylglycine) can be sarcosine – as the effect of direct activity of C–P lyase or aminomethylphosphonic acid (AMPA) formed as the result of the activity of glyphosate oxidoreductase (GOX) (Dick and Quinn, 1995, Dick and Quinn, 1995, Pipke and Amrhein, 1988, Obojska et al., 1999, Klimek-Ochab et al., 2004). Dick and Quinn, 1995, Dick and Quinn, 1995 suggest that sarcosine pathway is preferred by microorganisms. However, the presence of AMPA was also determined in some cases (Dick and Quinn, 1995, Dick and Quinn, 1995, Ternan et al., 1998, Araujo et al., 2003). The latter could be due to the presence of the enzyme oxidoreductase (GOX) in soil microorganisms. However, AMPA can further accumulate in soil and can be degraded with slower rate than glyphosate (Rueppel et al., 1997). Thus, Araujo et al. (2003) after 32 days of the experiments using various types of soil determined the presence of low quantities of glyphosate and significant level of the product of its degradation – AMPA.
Immediate products of decomposition of glyphosate are further degraded microbiologically to NH3, CO2, C2H5OH, H2O and phosphates (Dick and Quinn, 1995, Dick and Quinn, 1995, Obojska et al., 1999, Klimek-Ochab et al., 2004).
The time of decay of 90% of the initial dosage of the herbicide was 14–90 days, depending on the type of soil (Mensink and Janssen, 1994). In soils containing low levels of organic matter, nitrosoglyphosate was formed (Rueppel et al., 1997).
The aim of the present work was to isolate a group of autochthonous soil fungi that survive in 1 mM aqueous glyphosate solution as well as to investigate interactions between these fungal strains and glyphosate.
Section snippets
Glyphosate
N-Phosphonomethylglycine used in this study was obtained from commercial formulation by precipitation from its aqueous solution with concentrated hydrochloric acid.
Soil samples
The studied material consisted of samples of soil sampled in autumn period from the experimental field in which diversified content of organic carbon has been set up by fertilization with various dosage of sewage sludge (Table 1).
Ten grams soil samples were suspended in 90 ml of 1 mM glyphosate solution. After one and six months the
Results and discussion
Survival of autochthonous fungi in 1.0 mM glyphosate solution, depended on duration of its action and, in lower extent, on the content of total carbon in soil. Significant differences between total number of fungi in soil supplemented with different amounts of sludge were observed, as well as significant qualitative changes were encountered (Table 2).
As a result of 30 days of glyphosate action statistically significant change in fungal count was found in soils of high carbon content 1450 mg 100 g−1
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