The endophyte is surrounded by a membrane of apparent host plant origin. 内生植物是明显地被起源于寄生植物的膜包围的。
The apparent isotopic fractionation factor between brine and lake sediments is 1.009 ± 0.002. The δ 6Li value of source water ranges from+ 6.1 ‰ to-28.60 ‰, depending on their origin. 湖水与沉积物间的同位素分馏因素α=1.009±0.002,来源水的δ ̄6Li值变化范围为+6.1‰--28.6‰,由它们的来源所决定。