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在波动的土壤氧化还原条件下具有类似开关调节的生物地球化学氮途径的组织

Organization of biogeochemical nitrogen pathways with switch-like adjustment in fluctuating soil redox conditions.

作者信息

Lamba Sanjay, Bera Soumen, Rashid Mubasher, Medvinsky Alexander B, Sun Gui-Quan, Acquisti Claudia, Chakraborty Amit, Li Bai-Lian

机构信息

School of Mathematics, Statistics and Computational Sciences , Central University of Rajasthan , Bandarsindri, Ajmer , India.

Institute of Theoretical and Experimental Biophysics , Pushchino 142290 , Russia.

出版信息

R Soc Open Sci. 2017 Jan 11;4(1):160768. doi: 10.1098/rsos.160768. eCollection 2017 Jan.

Abstract

Nitrogen is cycled throughout ecosystems by a suite of biogeochemical processes. The high complexity of the nitrogen cycle resides in an intricate interplay between reversible biochemical pathways alternatively and specifically activated in response to diverse environmental cues. Despite aggressive research, how the fundamental nitrogen biochemical processes are assembled and maintained in fluctuating soil redox conditions remains elusive. Here, we address this question using a kinetic modelling approach coupled with dynamical systems theory and microbial genomics. We show that alternative biochemical pathways play a key role in keeping nitrogen conversion and conservation properties invariant in fluctuating environments. Our results indicate that the biochemical network holds inherent adaptive capacity to stabilize ammonium and nitrate availability, and that the bistability in the formation of ammonium is linked to the transient upregulation of the mediated nitrification pathway. The bistability is maintained by a pair of complementary subsystems acting as either source or sink type systems in response to soil redox fluctuations. It is further shown how elevated anthropogenic pressure has the potential to break down the stability of the system, altering substantially ammonium and nitrate availability in the soil, with dramatic effects on biodiversity.

摘要

氮通过一系列生物地球化学过程在整个生态系统中循环。氮循环的高度复杂性在于可逆生化途径之间复杂的相互作用,这些途径会根据不同的环境线索交替且特异性地被激活。尽管进行了大量研究,但在波动的土壤氧化还原条件下,基本的氮生化过程是如何组装和维持的仍然难以捉摸。在这里,我们使用动力学建模方法结合动力系统理论和微生物基因组学来解决这个问题。我们表明,替代生化途径在波动环境中保持氮转化和守恒特性不变方面起着关键作用。我们的结果表明,生化网络具有稳定铵和硝酸盐可用性的固有适应能力,并且铵形成中的双稳态与介导的硝化途径的瞬时上调有关。这种双稳态由一对互补子系统维持,它们在响应土壤氧化还原波动时充当源型或汇型系统。进一步表明,人为压力的增加如何有可能破坏系统的稳定性,极大地改变土壤中铵和硝酸盐的可用性,并对生物多样性产生巨大影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ecb1/5319346/2bb20ba2cc2e/rsos160768-g1.jpg

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