Xue Jinzhuang, Deng Zhenzhen, Huang Pu, Huang Kangjun, Benton Michael J, Cui Ying, Wang Deming, Liu Jianbo, Shen Bing, Basinger James F, Hao Shougang
The Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, People's Republic of China; Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, People's Republic of China;
The Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, People's Republic of China;
Proc Natl Acad Sci U S A. 2016 Aug 23;113(34):9451-6. doi: 10.1073/pnas.1605051113. Epub 2016 Aug 8.
The colonization of terrestrial environments by rooted vascular plants had far-reaching impacts on the Earth system. However, the belowground structures of early vascular plants are rarely documented, and thus the plant-soil interactions in early terrestrial ecosystems are poorly understood. Here we report the earliest rooted paleosols (fossil soils) in Asia from Early Devonian deposits of Yunnan, China. Plant traces are extensive within the soil and occur as complex network-like structures, which are interpreted as representing long-lived, belowground rhizomes of the basal lycopsid Drepanophycus The rhizomes produced large clones and helped the plant survive frequent sediment burial in well-drained soils within a seasonal wet-dry climate zone. Rhizome networks contributed to the accumulation and pedogenesis of floodplain sediments and increased the soil stabilizing effects of early plants. Predating the appearance of trees with deep roots in the Middle Devonian, plant rhizomes have long functioned in the belowground soil ecosystem. This study presents strong, direct evidence for plant-soil interactions at an early stage of vascular plant radiation. Soil stabilization by complex rhizome systems was apparently widespread, and contributed to landscape modification at an earlier time than had been appreciated.
有根维管植物对陆地环境的定殖对地球系统产生了深远影响。然而,早期维管植物的地下结构鲜有记载,因此人们对早期陆地生态系统中植物与土壤的相互作用了解甚少。在此,我们报道了来自中国云南泥盆纪早期沉积物中亚洲最早的有根古土壤(化石土壤)。土壤中植物痕迹广泛,呈复杂的网络状结构,被解释为代表基部石松类植物镰蕨的长寿地下根茎。这些根茎形成了大型克隆体,帮助植物在季节性干湿气候带排水良好的土壤中频繁被沉积物掩埋的情况下存活下来。根茎网络促进了河漫滩沉积物的积累和成土作用,并增强了早期植物对土壤的稳定作用。在泥盆纪中期深根树木出现之前,植物根茎早已在地下土壤生态系统中发挥作用。本研究为维管植物辐射早期的植物 - 土壤相互作用提供了有力的直接证据。复杂根茎系统对土壤的稳定作用显然很普遍,且比人们之前认识到的更早地促成了景观改造。