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Temporal and Spatial Impact of Human Cadaver Decomposition on Soil Bacterial and Arthropod Community Structure and Function

机译:人尸分解对土壤细菌和节肢动物群落结构和功能的时空影响

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As vertebrate carrion decomposes, there is a release of nutrient-rich fluids into the underlying soil, which can impact associated biological community structure and function. How these changes alter soil biogeochemical cycles is relatively unknown and may prove useful in the identification of carrion decomposition islands that have long lasting, focal ecological effects. This study investigated the spatial (0, 1, and 5 m) and temporal (3–732 days) dynamics of human cadaver decomposition on soil bacterial and arthropod community structure and microbial function. We observed strong evidence of a predictable response to cadaver decomposition that varies over space for soil bacterial and arthropod community structure, carbon (C) mineralization and microbial substrate utilization patterns. In the presence of a cadaver (i.e., 0 m samples), the relative abundance of Bacteroidetes and Firmicutes was greater, while the relative abundance of Acidobacteria, Chloroflexi, Gemmatimonadetes, and Verrucomicrobia was lower when compared to samples at 1 and 5 m. Micro-arthropods were more abundant (15 to 17-fold) in soils collected at 0 m compared to either 1 or 5 m, but overall, micro-arthropod community composition was unrelated to either bacterial community composition or function. Bacterial community structure and microbial function also exhibited temporal relationships, whereas arthropod community structure did not. Cumulative precipitation was more effective in predicting temporal variations in bacterial abundance and microbial activity than accumulated degree days. In the presence of the cadaver (i.e., 0 m samples), the relative abundance of Actinobacteria increased significantly with cumulative precipitation. Furthermore, soil bacterial communities and C mineralization were sensitive to the introduction of human cadavers as they diverged from baseline levels and did not recover completely in approximately 2 years. These data are valuable for understanding ecosystem function surrounding carrion decomposition islands and can be applicable to environmental bio-monitoring and forensic sciences.
机译:随着脊椎动物腐肉的分解,富含营养的液体释放到下面的土壤中,这可能会影响相关的生物群落结构和功能。这些变化如何改变土壤生物地球化学循环是相对未知的,并且在证明具有长期,集中的生态效应的腐肉分解岛方面可能是有用的。这项研究调查了人类尸体分解对土壤细菌和节肢动物群落结构和微生物功能的空间(0、1、5 m)和时间(3–732天)动力学。我们观察到强有力的证据表明,对于土壤细菌和节肢动物群落结构,碳(C)矿化作用和微生物底物利用模式,尸体分解可预测的响应随空间而变化。在有尸体的情况下(即0m样品),与1m和5m的样品相比,拟杆菌和Firmicutes的相对丰度更高,而酸性细菌,绿弯曲菌,双歧杆菌和Verrucomicrobia的相对丰度较低。与1或5 m相比,在0 m处采集的土壤中的节肢动物更丰富(15至17倍),但总体而言,节肢动物的群落组成与细菌群落组成或功能均无关。细菌群落结构和微生物功能也表现出时间关系,而节肢动物群落结构则没有。累积沉淀比累积日数更有效地预测细菌丰度和微生物活性的时间变化。在尸体存在的情况下(即0 m样品),放线菌的相对丰度随着累积降水而显着增加。此外,土壤细菌群落和碳矿化对人类尸体的引入很敏感,因为它们偏离基准水平,并且在大约2年内没有完全恢复。这些数据对于理解腐肉分解岛周围的生态系统功能非常有价值,并且可以应用于环境生物监测和法医学。

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