Abstract
des-A-triterpenoids have been widely recognized as indicators of terrestrial vascular angiosperms and microbial activities. However, recent studies also suggested complex sources for des-A-triterpenoids in lakes and peatlands, thus complicating their applications in paleoenvironmental reconstructions. Here we present the occurrences of aliphatic and aromatic des-A-triterpenoids from a ∼160-year sedimentary core in Lake Wuliangsu in the upper reaches of the Yellow River, China. In these sediments, des-A-triterpane was not detected, whereas di-unsaturated des-A-triterpenes are more abundant than mono-unsaturated des-A-triterpenes. The δ13C values of di-unsaturated des-A-triterpenes range from –23.0‰ to –17.6‰, with an average value of –21.0‰. Accordingly, aliphatic des-A-triterpenoids from Lake Wuliangsu show a unique distribution pattern and more positive δ13C signatures compared with those sourced from terrestrial vascular angiosperms. By comparing the concentrations and δ13C values of des-A-triterpenoids with n-alkanes and triterpenoids, we suggest that des-A-triterpenoids from Lake Wuliangsu sediments might be degraded from oleanenone, which was produced by submerged macrophytes. In this sense, aliphatic des-A-triterpenes in Lake Wuliangsu could represent a novel proxy for submerged macrophytes, which would be more precise than those of mid-chain n-alkanes, considering that mid-chain n-alkanes are usually from multiple sources. Our results also demonstrate the importance of strong aerobic bacteria activities and photodegradation for the formation of di-unsaturated des-A-triterpenes. The aromatization process of aliphatic des-A-triterpenes show contrasting variation characteristic with the formation of aliphatic des-A-triterpenes over the past ∼160 years, probably due to different rates (production vs consumption of di-unsaturated des-A-triterpenes) and prerequisites (aerobic vs anaerobic conditions) for these two synthesis pathways.
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