Evidence of moisture control on the methylation of branched glycerol dialkyl glycerol tetraethers in semi-arid and arid soils

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• 作者：Xinyue Dang^a ; Huan Yang^a ; B. David A. Naafs^b ; Richard D. Pancost^b ; Shucheng Xie^a ; ^{xiecug@163.com" class="auth_mail" title="E-mail the corresponding author}
• 关键词：Soil water content ; MBT ; C6-methylated brGDGTs ; Precipitation ; Semi-arid and arid region
• 刊名：Geochimica et Cosmochimica Acta
• 出版年：2016
• 出版时间：15 September 2016
• 年：2016
• 卷：189
• 期：Complete
• 页码：24-36
• 全文大小：2975 K

文摘

The distribution of bacterial branched glycerol dialkyl glycerol tetraethers (brGDGTs) is influenced by growth temperature and pH. This results in the widespread application of the brGDGT-based MBT(′)/CBT proxy (MBT – methylation of branched tetraethers, CBT – cyclization of branched tetraethers) in terrestrial paleo-environmental reconstructions. Recently, it was shown that the amount of precipitation could also have an impact on CBT, as well as the abundance of brGDGTs relative to that of archaeal isoprenoidal (iso)GDGTs (R_i/b) and the absolute abundance of brGDGTs, potentially complicating the use of MBT/CBT as paleothermometer. However, the full influence of hydrology, and in particular soil water content (SWC), on GDGT distributions remains unclear. Here we investigated variations in the GDGT distribution across a SWC gradient (0–61%) around Qinghai Lake in the Tibetan Plateau, an arid to semiarid region in China. Our results demonstrate that SWC affects the brGDGT distribution. In particular, we show that SWC has a clear impact on the degree of methylation of C6-methylated brGDGTs, whereas C5-methylated brGDGTs are more impacted by temperature. This results in a combined SWC and temperature control on MBT′. In this context we propose a diagnostic parameter, the IR_6ME (relative abundance of C6-methylated GDGTs) index, to evaluate the applicability of brGDGT-based paleotemperature reconstructions. Using the global dataset, expanded with our own data, MBT′ has a significant correlation with mean annual air temperature when IR_6ME < 0.5, allowing for the use of MBT′/CBT as temperature proxy. However, MBT′ has a significant correlation with mean annual precipitation (i.e., a substantial reflection of SWC impact) when IR_6ME > 0.5, implying that MBT′ may respond to hydrological change in these regions and can be used as a proxy for MAP.