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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Millennial-scale changes in the molecular composition of Posidonia australis seagrass deposits: Implications for Blue Carbon sequestration
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Millennial-scale changes in the molecular composition of Posidonia australis seagrass deposits: Implications for Blue Carbon sequestration

机译:Posidonia Australis Seangrass沉积物分子组成的千禧一代变化:对蓝碳封存的影响

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Seagrass ecosystems are recognised for their role in climate change mitigation, due to their capacity to form organic-rich sediments. The chemical recalcitrance of seagrass organs is one characteristic driving carbon storage, but the molecular background of this feature is poorly understood. We assessed molecular composition changes of Posidonia australis sheaths (SH) and roots plus rhizomes (RR) along a sediment core, encompassing 3200 cal. yr BP, by means of nuclear magnetic resonance spectroscopy (C-13 NMR), conventional analytical pyrolysis (Py-GC-MS) and thermally assisted hydrolysis and methylation (THM-GC-MS). Significant trends with depth (age) in the composition of both SH and RR remains of P. australis were observed from all methods. In general terms, polysaccharides become depleted (degraded) and lignin enriched (selectively preserved) as age increases, and the minor constituents cutin, suberin and condensed tannin are also preferentially depleted during ageing in both fractions. Molecular changes with ageing were smaller in SH, especially regarding polysaccharides, indicative of a superior stability compared to RR. The molecular changes observed are most pronounced within the first 75 cm of the record, which reflects the recalcitrance of P. australis detritus once it is buried below that depth (corresponding to approximately 700 cal. yr BP). The capacity of P. australis to act as a long-term carbon sink seems to be mainly related to the resistance of buried lignocellulose materials to decomposition. The results on diagenetic effects on the molecular fingerprint of seagrass detritus contribute to our understanding of carbon sequestration in Blue Carbon ecosystems. Furthermore, data comparison of the methods applied using principal component analysis (PCA) allowed us to identify consistencies, discrepancies and complementarities. (C) 2019 Elsevier Ltd. All rights reserved.
机译:由于其形成有机肥胖的沉积物,海草生态系统被认可在气候变化中的作用。海草器官的化学批量是一种驾驶碳储存的一种特征,但该特征的分子背景知之甚少。我们评估了沿沉积物核心的Posidonia澳曲鞘(SH)和根部加根源(RR)的分子组成变化,包括3200克。 Yr BP,通过核磁共振光谱(C-13 NMR),常规分析热解(Py-GC-MS)和热辅助水解和甲基化(THM-GC-MS)。所有方法都观察到SH和RR遗骸的组成中的深度(年龄)的重要趋势。一般而言,多糖变得耗尽(降解),并且随着年龄的增长,富集的木质素(选择性地保存),并且在两种级分时也优先耗尽。 SH的分子变化较小,特别是关于多糖,与RR相比,表明优异的稳定性。观察到的分子变化在记录的第一个75厘米内最为明显,这反映了一旦埋在深度下方(对应约700克)的埋藏时,反映了P. Australis Detritus的重核。 P. Australis作为长期碳汇的能力似乎主要与埋藏的木质纤维素材料与分解的抗性有关。结果对海草碎屑分子指纹的成岩效应有助于我们对蓝碳生态系统中碳封存的理解。此外,使用主成分分析(PCA)施加的方法的数据比较允许我们识别一致性,差异和互补性。 (c)2019年elestvier有限公司保留所有权利。

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