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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Glycerol dialkyl glycerol tetraethers in surface sediments from three Pacific trenches: Distribution, source and environmental implications
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Glycerol dialkyl glycerol tetraethers in surface sediments from three Pacific trenches: Distribution, source and environmental implications

机译:甘油二烷基甘油四乙醇中的三个太平洋沟槽的表面沉积物:分布,来源和环境影响

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Glycerol dialkyl glycerol tetraethers (GDGTs) have been widely used to elucidate sources of sediment total organic carbon (TOC), past temperature and presence of methanogenesis in diverse environments. However, their applicability to hadal trenches with their unique deposition dynamics remains unknown. Here, we analyzed GDGTs and their stable isotope values and content of TOC in surface sediments from the Kermadec Trench region (KT; 6080-10010 m), New Britain Trench region (NBT; 1553-8931 m), and Atacama Trench region (AT; 2560-8085 m). These regions are at very different distances from terrestrial sources and have varying net primary productivity (NPP) in the waters above them. The GDGT concentration was highly variable (54.5-2416 mu g g(-1) TOC) within and between trench regions and was not directly related to local NPP or apparent terrestrial inputs. This finding is presumably due to complex deposition dynamics within the trench interior. Isoprenoidal GDGTs (isoGDGTs; 75.4-99.1%) were dominant over branched GDGTs (brGDGTs, 0.91-24.6%) in all samples, leading to low levels of Branched versus Isoprenoidal Tetraether (BIT) index (0.01-0.27). Thus, sediment TOC is mainly derived from marine sources. However, compared to adjacent non-hadal sites, trench axis sites have a higher BIT index, lower acyclic hexa-/pentamethylated brGDGT and lower delta C-13, supporting relative enrichment of terrestrial organic carbon at the trench axis. The application of TetraEther indeX of tetraethers consisting of 86 carbon atoms (TEX86) resulted in sea surface temperature (SST) estimates of 18.9-23.7 degrees C in the KT, 28.6-30.2 degrees C in the NBT, and 17.9-20.4 degrees C in the AT. The close agreement between TEX86-SST with observed in situ SST suggests that isoGDGTs are not selectively degraded during the transport towards the hadal realm, and that TEX86 from hadal settings robustly records an integrated regional SST signal. (C) 2020 Elsevier Ltd. All rights reserved.
机译:甘油二烷基甘油四乙酯(GDGT)已被广泛用于阐明沉积物总有机碳(TOC)的来源,过去的温度和甲烷发生在不同的环境中。然而,它们对具有独特沉积动态的牵引沟的适用性仍然未知。在这里,我们分析了基于Kermadec沟槽区(KT; 6080-10010米),新英国沟槽区(NBT; 1553-8931 M)和Atacama沟槽区域(AT ; 2560-8085 m)。这些区域与地面源极距离非常不同,并且在它们上方的水中具有不同的净初级生产率(NPP)。 GDGT浓度在沟槽区域内和之间的高度变化(54.5-2416μg(-1)TOC),并且与局部NPP或表观陆地输入没有直接相关。这一发现可能是由于沟槽内部内的复杂沉积动态。异常GDGTS(ISOGDGTS; 75.4-99.1%)在所有样品中占分枝GDGT(BRGDGTS,0.91-24.6%),导致低水平的支化与等异细胞体四醚(钻头)指数(0.01-0.27)。因此,沉积物TOC主要来自海洋来源。然而,与相邻的非辐射位点相比,沟槽轴位点具有更高的比特指数,低循环六甲基/五甲基化BRGDGT和下δC-13,支持沟槽轴上的陆地有机碳的相对富集。在86个碳原子(Tex86)中组成的四醚指数的应用导致KT中的海面温度(SST)估计为18.9-23.7摄氏度,在NBT中为28.6-30.2摄氏度,17.9-20.4摄氏度at。 Tex86-SST与原位SST之间的密切一致认为,ISOGDGTS在运输到牵引领域期间没有选择性地降级,并且来自HADAL设置的TEX86强大地记录了集成的区域SST信号。 (c)2020 elestvier有限公司保留所有权利。

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