Loh Zhi Hung, Hungerford Natasha L, Ouwerkerk Diane, Klieve Athol V, Fletcher Mary T
Queensland Alliance for Agriculture and Food Innovation (QAAFI), The University of Queensland, Health and Food Sciences Precinct, Coopers Plains, QLD 4108, Australia.
Agri-Science Queensland, Department of Primary Industries (DPI), Ecosciences Precinct, Dutton Park, QLD 4102, Australia.
Toxins (Basel). 2025 Mar 6;17(3):124. doi: 10.3390/toxins17030124.
poisoning of cattle is caused by the toxin simplexin present in native plant species. Surface weathering and burial of plant material under soil in -infested pastures previously showed simplexin degradation, suggesting soil microbial metabolism and/or abiotic degradation of simplexin in the field. This current study investigated whether soil from a -infested paddock was capable of simplexin degradation in the laboratory. The effects of temperature on isolated simplexin levels and simplexin levels in plant material treated with field-collected soil, acid-washed sand or bentonite were determined. plant material incubated in field-collected soil at 22 °C for seven days did not show any simplexin degradation. Isolated simplexin preadsorbed to field-collected soil, acid-washed sand or bentonite showed simplexin decrease after one hour of incubation at 100 °C with three breakdown products identified by UPLC-MS/MS, indicating that toxin breakdown can be a heat-induced process rather than a microbial-based metabolism. Decreased simplexin levels were observed in plant material mixed with acid-washed sand under similar incubation conditions. Overall, the study showed the field-collected soil did not contain soil microorganisms capable of simplexin metabolism within a short period of time. However, the co-exposure to high temperature resulted in significant abiotic simplexin breakdown, without microorganism involvement, with the product structures suggesting that the degradation was a heat promoted acid hydrolysis/elimination process. Overall, this study demonstrated that simplexin breakdown in the field could be a thermal abiotic process with no indication of microbial involvement.
牛中毒是由本地植物物种中存在的毒素单辛引起的。先前在受侵染牧场中,植物材料在土壤中的表面风化和掩埋显示单辛降解,这表明田间单辛的降解是土壤微生物代谢和/或非生物降解所致。本研究调查了来自受侵染围场的土壤在实验室中是否能够降解单辛。测定了温度对分离的单辛水平以及用田间采集的土壤、酸洗砂或膨润土处理的植物材料中单辛水平的影响。在22℃下于田间采集的土壤中孵育7天的植物材料未显示出任何单辛降解。预吸附到田间采集的土壤、酸洗砂或膨润土上的分离单辛,在100℃孵育1小时后显示单辛减少,通过超高效液相色谱-串联质谱法鉴定出三种分解产物,这表明毒素分解可能是一个热诱导过程而非基于微生物的代谢。在类似的孵育条件下,与酸洗砂混合的植物材料中单辛水平降低。总体而言,该研究表明田间采集的土壤在短时间内不含有能够代谢单辛的土壤微生物。然而,高温共同作用导致在无微生物参与的情况下单辛发生显著的非生物分解,产物结构表明降解是一个热促进的酸水解/消除过程。总体而言,本研究表明田间单辛分解可能是一个热非生物过程,没有微生物参与的迹象。