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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Effect of water depth on the TEX86 proxy in volcanic lakes of northeastern China
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Effect of water depth on the TEX86 proxy in volcanic lakes of northeastern China

机译:水深对中国东北火山湖泊Tex86代理的影响

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The TEX(86 )index, based on the distribution of isoprenoid glycerol dialkyl glycerol tetraethers (iGDGTs), has been widely applied for reconstructing past sea surface temperature (SST). However, its successful application in lacustrine environments has been limited to certain large lakes in which aquatic Thaumarchaeota are thought be the dominant iGDGT producers. In small lakes, multiple factors, such as iGDGTs from soil and non-thaumarchaeotal sources, could complicate the use of TEX86 as a temperature proxy (Powers et al., 2010). Here we investigate iGDGTs from surface sediments and suspended particulate matter (SPM) in a series of small volcanic lakes (areas: similar to 0.1-8.2 km(2)) from three main volcanic fields of northeastern China. The iGDGT distribution patterns from surface sediments of these lakes differ significantly from those of surrounding soils, global marine sediments, as well as cultured Group I.1 a and Group I.1b Thaumarchaeota, suggesting a substantial contribution of autochthonous non-thaumarchaeotal sources. Interestingly, however, the correlation between TEX86 values in the SPM samples and in situ water temperatures remain strong and display temperature sensitivity similar to previously published linear calibrations from global marine and lake sediments. Our results suggest that the in situ TEX86-temperature relationship is little affected by the non-thaumarchaeotal iGDGT sources in these lakes. However, the TEX86-inferred temperatures from surface sediments show increasingly colder offsets relative to air temperatures with increasing lake depth, which can be explained by the observed increase in iGDGTs production and decrease in water temperatures in water column as depth increases. Our results thus suggest that TEX86 values in the sediments of these volcanic lakes are affected by both temperature and lake depth, and when temperature can be constrained independently or remains constant over a given period of time, have potential application
机译:基于异戊二烯甘油二烷基甘油四乙酯(IgDGT)的分布的Tex(86)指标已被广泛应用于重建过去海表面温度(SST)。然而,它在湖泊环境中的成功应用仅限于某些大型湖泊,其中水生素谱系被认为是主要的IGDGT生产商。在小湖泊中,多种因素,如土壤和非伤寒源的IgDGT,可以使TEX86的使用使TEX86作为温度代理(Powers等,2010)。在这里,我们将来自地表沉积物和悬浮颗粒物质(SPM)的IGDGT在一系列小火山湖(区域:类似于中国东北部三大火山场的0.1-8.2 km(2))中。这些湖泊的表面沉积物的IGGT分布模式显着不同于周围土壤,全球海洋沉积物,以及培养的I.1a和I.1b族·孕段培养的群体,这表明了对自身的非ThaumarchoTaeoTals来源的大量贡献。然而,有趣的是,SPM样品中TEX86值与原位水温之间的相关性仍然坚强,显示温度敏感性,类似于全球海洋和湖泊沉积物的先前公布的线性校准。我们的研究结果表明,原位Tex86温度关系受到这些湖泊中非Thaumarchootal IGGT来源的影响。然而,来自表面沉积物的Tex86推断的温度示出了相对于增加湖泊深度的空气温度越来越冷的偏移,这可以通过观察到的IGGTS生产的增加和水柱中的水温降低随着深度增加而解释。因此,我们的结果表明,这些火山湖泊沉积物中的Tex86值受温度和湖泊深度的影响,并且当温度可以在给定的时间内独立约束或保持恒定,具有潜在的应用

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