Zhou Shangzhe, Xi Lei, Cui Mengchun, Cui Guipeng, Gao Pan, Zhu Jinlei, Kong Weiyuan, Jia Yufu, Lu Qi
Institute of Ecological Conservation and Restoration, Chinese Academy of Forestry, Beijing 100091, China.
Institute of Desertification Studies, Chinese Academy of Forestry, Beijing 100091, China.
Plants (Basel). 2024 Oct 17;13(20):2898. doi: 10.3390/plants13202898.
Fallen leaves and their decomposition directly deposit leaf wax -alkanes into sediments, which can be used to identify local flora. These -alkanes are important for studying past vegetation and climate, but their distribution in sediments must be known. Aeolian sand -alkanes are particularly important for understanding paleoclimates in arid regions, despite the challenges of extraction due to their extremely low abundance. To investigate the preservation of plant leaf wax -alkanes in deserts, we analyzed -alkanes in aeolian sands from the Northern Ulan Buh Desert (UBD), China, and compared them to the surrounding vegetation. We calculated the total -alkane concentration (ΣALK), average chain length (ACL), and carbon preference index (CPI). In the Northern UBD, aeolian sand -alkanes have lower ΣALK, indicating microbial degradation. The eastern aeolian sand has lower CPI and ACL than the adjacent vegetation, whereas the western sand values are consistent with the plants, likely due to the transport of plant-derived materials by wind and water from the nearby mountains. Our study shows that sedimentary -alkane signatures are not only determined by local vegetation but also influenced by environmental factors like temperature and precipitation. Additionally, local deposition processes play a significant role in determining the properties of these -alkanes.
落叶及其分解过程会直接将叶蜡烷烃沉积到沉积物中,这些沉积物可用于识别当地植物群。这些烷烃对于研究过去的植被和气候很重要,但必须了解它们在沉积物中的分布情况。尽管由于风沙烷烃丰度极低,提取存在挑战,但它们对于理解干旱地区的古气候尤为重要。为了研究沙漠中植物叶蜡烷烃的保存情况,我们分析了中国乌兰布和沙漠北部风沙中的烷烃,并将其与周围植被进行了比较。我们计算了总烷烃浓度(ΣALK)、平均链长(ACL)和碳偏好指数(CPI)。在乌兰布和沙漠北部,风沙烷烃的ΣALK较低,表明存在微生物降解。东部风沙的CPI和ACL低于相邻植被,而西部风沙的值与植物一致,这可能是由于植物源物质通过风和水从附近山脉输送过来。我们的研究表明,沉积烷烃特征不仅取决于当地植被,还受到温度和降水等环境因素的影响。此外,局部沉积过程在决定这些烷烃的性质方面起着重要作用。