File:Soil carbon cycle through the microbial loop-es.png

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Español: Ciclo del carbono (C) del suelo a través del bucle microbiano

El dióxido de carbono (CO2) de la atmósfera es fijado por las plantas (o microorganismos autótrofos) y añadido al suelo a través de procesos como (1) la exudación por las raíces de compuestos de carbono simples de bajo peso molecular, o la deposición de hojarasca y hojarasca radicular que conduce a la acumulación de polisacáridos vegetales complejos. (2) A través de estos procesos, el carbono se hace biodisponible para la "fábrica" metabólica microbiana y posteriormente es (3) respirado a la atmósfera o (4) entra en la reserva de carbono estable como necromasa microbiana. El equilibrio exacto entre el flujo de carbono y su persistencia depende de varios factores, como la composición de la comunidad vegetal sobre el suelo y los perfiles del exudado radicular, las variables ambientales y los fenotipos microbianos colectivos (es decir, el metafenoma). Figura inspirada en Bonkowski, 2004.

  • Bonkowski M.(2004) "Protozoa and plant growth: the microbial loop in soil revisited". New Phytol, 162(3): 617-31.
English: Soil carbon (C) cycle through the microbial loop

Carbon dioxide (CO2) in the atmosphere is fixed by plants (or autotrophic microorganisms) and added to soil through processes such as (1) root exudation of low-molecular weight simple carbon compounds, or deposition of leaf and root litter leading to accumulation of complex plant polysaccharides. (2) Through these processes, carbon is made bioavailable to the microbial metabolic “factory” and subsequently is either (3) respired to the atmosphere or (4) enters the stable carbon pool as microbial necromass. The exact balance of carbon efflux versus persistence is a function of several factors, including aboveground plant community composition and root exudate profiles, environmental variables, and collective microbial phenotypes (i.e., the metaphenome). Figure inspired by Bonkowski, 2004.

Bonkowski M.(2004) "Protozoa and plant growth: the microbial loop in soil revisited". New Phytol., 162(3): 617–31.
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Dan Naylor, Natalie Sadler, Arunima Bhattacharjee, Emily B. Graham, Christopher R. Anderton, Ryan McClure, Mary Lipton, Kirsten S. Hofmockel and Janet K. Jansson

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