首页> 外文期刊>Geochemistry: Interdisciplinary Journal for Chemical Problems of the Geosciences and Geoecology >Stable isotopic signatures of the modern land snail Eremina desertorum from a low-latitude (hot) dry desert-A study from the Petrified Forest, New Cairo, Egypt
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Stable isotopic signatures of the modern land snail Eremina desertorum from a low-latitude (hot) dry desert-A study from the Petrified Forest, New Cairo, Egypt

机译:来自低纬度(炎热)干燥沙漠的现代蜗牛埃雷米纳沙漠的稳定同位素特征-来自埃及新开罗的石化森林的研究

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This study was conducted on recent desert samples-including (1) soils, (2) plants, (3) the shell, and (4) organic matter from modern specimens of the land snail Eremina desertorum-which were collected at several altitudes (316-360m above sea level) from a site in the New Cairo Petrified Forest. The soils and shelle(E.desertorum) were analyzed for carbonate composition and isotopic composition (delta O-18, delta C-13). The plants and organic matter(E.desertorum)were analyzed for organic carbon content and delta C-13. The soil carbonate, consisting of calcite plus minor dolomite, has delta O-18 values from -3.19 to -1.78%. and delta C-13 values -1.79 to -0.27%.; covariance between the two values accords with arid climatic conditions. The local plants include C3 and C4 types, with the latter being dominant. Each type has distinctive bulk organic carbon delta C-13 values: -26.51 to -25.36%. for C3-type, and -13.74 to -12.43%. for C4-type plants. The carbonate of the shells(E.desertorum) is composed of aragonite plus minor calcite, with relatively homogenous isotopic compositions (delta O-18(mean) = -0.28 +/- 0.22 parts per thousand; delta C-13(mean) = -4.46 +/- 0.58 parts per thousand). Most of the 6180 values (based on a model for oxygen isotope fractionation in an aragonite-water system) are consistent with evaporated water signatures. The organic matter (E.desertorum) varies only slightly in bulk organic carbon delta C-13 values (-21.78 +/- 1.20%.) and these values suggest that the snail consumed more of 0-type than C4-type plants. The overall offset in delta C-13 values (-1732%.) observed between shelle(E.desertorum) carbonate and organic matters(E.desertorum) exceeds the value expected for vegetation input, and implies that 30% of carbon in the shell(E.desertorum) carbonate comes from the consumption of limestone material. (C) 2014 Elsevier GmbH. All rights reserved.
机译:这项研究是针对最近的沙漠样本进行的,包括(1)土壤,(2)植物,(3)壳和(4)现代蜗牛蜗牛标本的植物标本,这些标本是在多个海拔高度采集的(316) -从新开罗石化森林中的一块地高出-360m。分析土壤和贝壳(碳歧杆菌)的碳酸盐组成和同位素组成(δO-18,δC-13)。分析了植物和有机质(E.desertorum)的有机碳含量和δC-13。由方解石加少量白云石组成的碳酸盐土壤的O-18值介于-3.19至-1.78%之间。 C-13值在-1.79至-0.27%之间。两个值之间的协方差符合干旱的气候条件。本地植物包括C3和C4类型,后者占主导。每种类型都有独特的本体有机碳δC-13值:-26.51至-25.36%。对于C3型,则为-13.74至-12.43%。用于C4型植物。贝壳的碳酸盐由文石加少量方解石组成,同位素组成相对均匀(δO-18(平均值)= -0.28 +/- 0.22千分之一;δC-13(平均值)= -4.46 +/- 0.58千分之一)。 6180的大多数值(基于文石-水系统中氧同位素分馏的模型为基础)与蒸发水特征一致。有机物质(大肠埃希氏菌)的总体有机碳δC-13值(-21.78 +/- 1.20%)仅略有变化,这些值表明蜗牛消耗的0型比C4型植物更多。在贝壳碳酸盐和有机物碳中观测到的C-13增量的总偏移(-1732%。)超过了植被输入的预期值,这意味着贝壳中碳的含量为30% (E.desertorum)碳酸盐来自石灰石材料的消耗。 (C)2014 Elsevier GmbH。版权所有。

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