Your browser doesn't support javascript.
loading
Seasonal Controls on Microbial Depolymerization and Oxidation of Organic Matter in Floodplain Soils.
Anderson, Cam G; Tfaily, Malak M; Chu, Rosalie K; Tolic, Nikola; Fox, Patricia M; Nico, Peter S; Fendorf, Scott; Keiluweit, Marco.
Afiliación
  • Anderson CG; School of Earth and Sustainability, University of Massachusetts Amherst, Amherst, Massachusetts 01003, United States.
  • Tfaily MM; Department of Environmental Science, University of Arizona, Tucson, Arizona 85721, United States.
  • Chu RK; Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, Washington 99354, United States.
  • Tolic N; Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, Washington 99354, United States.
  • Fox PM; Earth and Environmental Sciences, Lawrence Berkeley National Laboratory, Berkeley, California 94720, United States.
  • Nico PS; Earth and Environmental Sciences, Lawrence Berkeley National Laboratory, Berkeley, California 94720, United States.
  • Fendorf S; Department of Earth System Science, Stanford University, Stanford, California 94305, United States.
  • Keiluweit M; Institute of Earth Surface Dynamics, University of Lausanne, 1015 Lausanne, Switzerland.
Environ Sci Technol ; 2024 Sep 15.
Article en En | MEDLINE | ID: mdl-39279153
ABSTRACT
Floodplain soils are vast reservoirs of organic carbon often attributed to anaerobic conditions that impose metabolic constraints on organic matter degradation. What remains elusive is how such metabolic constraints respond to dynamic flooding and drainage cycles characteristic of floodplain soils. Here we show that microbial depolymerization and respiration of organic compounds, two rate-limiting steps in decomposition, vary spatially and temporally with seasonal flooding of mountainous floodplain soils (Gothic, Colorado, USA). Combining metabolomics and -proteomics, we found a lower abundance of oxidative enzymes during flooding coincided with the accumulation of aromatic, high-molecular weight compounds, particularly in surface soils. In subsurface soils, we found that a lower oxidation state of carbon coincided with a greater abundance of chemically reduced, energetically less favorable low-molecular weight metabolites, irrespective of flooding condition. Our results suggest that seasonal flooding temporarily constrains oxidative depolymerization of larger, potentially plant-derived compounds in surface soils; in contrast, energetic constraints on microbial respiration persist in more reducing subsurface soils regardless of flooding. Our work underscores that the potential vulnerability of these distinct anaerobic carbon storage mechanisms to changing flooding dynamics should be considered, particularly as climate change shifts both the frequency and extent of flooding in floodplains globally.
Palabras clave

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Idioma: En Revista: Environ Sci Technol Año: 2024 Tipo del documento: Article País de afiliación: Estados Unidos Pais de publicación: Estados Unidos

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Idioma: En Revista: Environ Sci Technol Año: 2024 Tipo del documento: Article País de afiliación: Estados Unidos Pais de publicación: Estados Unidos