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Paleohydrology of the Upper Miocene Bicorb Lake (eastern Spain) as inferred from stable isotopic data from inorganic carbonates

机译:从无机碳酸盐的稳定同位素数据推断,上中新世比科尔布湖(西班牙东部)的古水文学

摘要

The hydrological evolution of the Upper Miocene Bicorb lake (eastern Spain) has been established based on sedimentology, carbonate mineralogy and stable isotopic data from inorganic carbonates from the upper lacustrine unit. Three main subunits have been recognized. In subunit A, the sedimentological features suggest a hydrologically closed lake although the isotopic data are not conclusive. The isotopic compositions of primary carbonates from subunit B display a distribution typical for a hydrologically closed lake, and allow the differentiation of four developmental stages. The first stage was defined by the deposition of gypsum, LMC, dolomite and aragonite, indicating large variations in the water Mg/Ca ratio. During the second and third stages only LMC was deposited suggesting only minor Mg/Ca fluctuations. The δ13C and δ18O pattern of the second stage shows a well-defined covariance (r = 0.8), while in the third stage the isotopic data display a negative covariant relationship (r = -0.8). Changes in dissolved inorganic carbon composition are considered the main factor to explain the variations from positive to negative covariance. In the fourth stage the lake waters underwent large Mg/Ca fluctuations, as indicated by the deposition of LMC, HMC and aragonite. The isotopic trend is also covariant. Finally, subunit C is characterized by LMC and minor amounts of HMC, suggesting minor changes in Mg/Ca ratio. The isotopic features of this subunit are more congruent with a hydrologically open lake. The lowest δ13C and δ18O values are very similar in the three subunits, reflecting the most dilute conditions of the lake water, and a uniform isotopic composition of the local meteoric water during these periods. The changes in water balance and solute inputs recorded in the mineralogy and isotopic signatures of carbonates were controlled by the diapiric evolution and changes in the E/P balance.
机译:根据沉积学,碳酸盐矿物学和来自上湖相单元的无机碳酸盐的稳定同位素数据,建立了中新世比科布湖(西班牙东部)的水文演化。已经认识到三个主要的亚单位。在亚单元A中,尽管同位素数据尚无定论,但其沉积学特征表明该湖处于水文封闭状态。来自亚基B的初级碳酸盐的同位素组成显示出水文封闭湖泊的典型分布,并可以区分四个发育阶段。第一阶段的定义是石膏,LMC,白云石和文石的沉积,表明水Mg / Ca比值存在较大差异。在第二和第三阶段中,只有LMC沉积,表明只有微小的Mg / Ca波动。第二阶段的δ13C和δ18O模式显示出明确的协方差(r = 0.8),而第三阶段的同位素数据显示出负的协变量关系(r = -0.8)。溶解的无机碳成分的变化被认为是解释从正协方差到负协方差变化的主要因素。在第四阶段,湖水经历了Mg / Ca的大幅度波动,这表明LMC,HMC和文石的沉积。同位素趋势也是协变的。最后,亚基C的特征是LMC和少量的HMC,表明Mg / Ca比值的变化很小。该亚基的同位素特征与水文开放的湖泊更为一致。在这三个亚基中,最低的δ13C和δ18O值非常相似,反映了湖水的最稀薄条件,以及在这些时期内局部陨石水的同位素组成均匀。碳酸盐的矿物学和同位素特征所记录的水平衡和溶质输入量的变化是由双底演化和E / P平衡的变化控制的。

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