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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >A new sea surface temperature proxy based on bacterial 3-hydroxy fatty acids
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A new sea surface temperature proxy based on bacterial 3-hydroxy fatty acids

机译:基于细菌3-羟基脂肪酸的新型海表面温度代理

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3-Hydroxy fatty acids (3-OH-FAs), derived from Gram-negative bacterial outer membranes, have received recent attention for their potential as new terrestrial pH and temperature proxies for palaeoclimate studies. However, it is not known whether 3-OH-FA based proxies can be developed and applied to the marine environment. Here we analyze 3-OH-FAs from a latitudinal transect of marine surface sediments from the North Pacific Ocean (12 degrees N to 61 degrees N with a annual mean sea surface temperature (SST) range of 28.1-1.3 degrees C). The results show that distributions of 3-OH-FAs in marine sediments yield overall higher abundances of anteiso 3-OH-FA homologues compared to soils. Furthermore, 16S rRNA gene sequencing of the marine sediments and soils shows the Gram-negative bacterial community is dominated by Proteobacteria (ca. 94%) at the phylum level. In contrast, in regional soils the Gram-negative bacterial community is more diverse with significant contributions from Proteobacteria (ca. 50%), Acidobacteria (ca. 24%), Verrucomicrobia (6%), Bacteroidetes (6%) and other phyla. These distinct genomic and molecular differences suggest distinctly different aggregate compositions of bacteria that produce 3-OH-FAs in the marine realm vs soils. Moreover, we find that the ratio of anteiso to normal C-13 3-OH-FA (RAN(13)) measured in surface sediments is highly correlated with annual mean SST throughout the temperature transect. When applied to a short sediment core from the East China Sea, the SST changes reconstructed by the RAN(13) proxy are comparable to instrumental SST data. These findings demonstrate that RAN(13) and potentially other, so far undiscovered, proxies based on 3-OH-FAs have potential for environmental and palaeoclimate applications in marine environments. (C) 2020 Elsevier Ltd. All rights reserved.
机译:衍生自革兰氏阴性细菌外膜的3-羟基脂肪酸(3-OH-FAS)已接受其作为新的陆地pH值和古典气候研究的温度代理的潜力。然而,尚不清楚是否可以开发3-OH-FA基础的代理并应用于海洋环境。在这里,我们将3-OH-FA从北太平洋的海洋表面沉积物的纬度横向分析(12摄氏度至61摄氏度,年平均海表面温度(SST)范围为28.1-1.3摄氏度)。结果表明,与土壤相比,海洋沉积物中3-OH-FAS的分布会产生整体较高丰富的南甲基3-OH-FA同源物。此外,16S RRNA基因测序的海洋沉积物和土壤序列显示革兰氏阴性细菌群落在门诊,植物群(CA.94%)主导。相比之下,在区域土壤中,革兰氏阴性细菌群体更多样化,具有来自植物(CA.50%),抗酸杆菌(24%),VerrucoMicrobia(6%),菌兵(6%)和其他植物的显着贡献。这些明显的基因组和分子差异表明了在海洋境界与土壤中产生3 oh-Fas的细菌的明显不同的细菌组合物。此外,我们发现,在表面沉积物中测量的常规C-13 3-OH-FA(RAN(13))的比率与整个温度横断面的年平均SST高度相关。当从东海的短沉积物施加到来自东海的短沉积物核心时,RAN(13)代理重建的SST变化与仪器SST数据相当。这些研究结果表明,到目前为止,基于3-OH-FAS的代理有可能在海洋环境中具有环境和古典气候应用的潜力。 (c)2020 elestvier有限公司保留所有权利。

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