(Table 1) Chemical composition of Mediterranean halite from DSDP Hole 13-134

Bromine content of a 15 cm halite core from Deep Sea Drilling Project Leg XIII Hole 134 was analyzed at 1.5 cm intervals. The Br varies from 140 to 254 ppm, and three maxima were found to coincide with three postulated horizons of desiccation. The Br profile confirms the interpretation from sedimentologic evidence that Mediterranean salts were deposited in a desiccating basin.对取自深海钻探计划（Deep Sea Drilling Project）第13航次134号钻孔的15厘米岩盐岩心，按1.5厘米的采样间隔开展溴含量分析。该岩心的溴含量介于140至254 ppm之间，共检测到三处含量峰值，且这三处峰值均与三处推测的干涸层位相吻合。该溴元素剖面验证了基于沉积学证据得出的解释结论：地中海盐类沉积形成于逐渐干涸的盆地之中。