Fe(II)Cl2 amendment suppresses pond methane emissions by stimulating iron-dependent anaerobic oxidation of methane

Author:

Struik Quinten1ORCID,Paranaíba José R1,Glodowska Martyna2,Kosten Sarian1,Meulepas Berber M J W1,Rios-Miguel Ana B2,Jetten Mike S M2,Lürling Miquel3,Waajen Guido4,Nijman Thomas P A1,Veraart Annelies J1ORCID

Affiliation:

1. Department of Ecology, Radboud Institute for Biological and Environmental Sciences, Radboud University , 6525 AJ, Nijmegen , The Netherlands

2. Department of Microbiology, Radboud Institute for Biological and Environmental Sciences, Radboud University , 6525 AJ, Nijmegen , The Netherlands

3. Aquatic Ecology & Water Quality Management Group, Department of Environmental Sciences, Wageningen University , PO Box 47, 6700 AA, Wageningen , The Netherlands

4. Water Authority Brabantse Delta , 4836 AA, Breda , The Netherlands

Abstract

Abstract Aquatic ecosystems are large contributors to global methane (CH4) emissions. Eutrophication significantly enhances CH4-production as it stimulates methanogenesis. Mitigation measures aimed at reducing eutrophication, such as the addition of metal salts to immobilize phosphate (PO43−), are now common practice. However, the effects of such remedies on methanogenic and methanotrophic communities—and therefore on CH4-cycling—remain largely unexplored. Here, we demonstrate that Fe(II)Cl2 addition, used as PO43- binder, differentially affected microbial CH4 cycling-processes in field experiments and batch incubations. In the field experiments, carried out in enclosures in a eutrophic pond, Fe(II)Cl2 application lowered in-situ CH4 emissions by lowering net CH4-production, while sediment aerobic CH4-oxidation rates—as found in batch incubations of sediment from the enclosures—did not differ from control. In Fe(II)Cl2-treated sediments, a decrease in net CH4-production rates could be attributed to the stimulation of iron-dependent anaerobic CH4-oxidation (Fe-AOM). In batch incubations, anaerobic CH4-oxidation and Fe(II)-production started immediately after CH4 addition, indicating Fe-AOM, likely enabled by favorable indigenous iron cycling conditions and the present methanotroph community in the pond sediment. 16S rRNA sequencing data confirmed the presence of anaerobic CH4-oxidizing archaea and both iron-reducing and iron-oxidizing bacteria in the tested sediments. Thus, besides combatting eutrophication, Fe(II)Cl2 application can mitigate CH4 emissions by reducing microbial net CH4-production and stimulating Fe-AOM.

Funder

Netherlands Organisation for Scientific Research

Ministry of Education

Soehngen Institute of Anaerobic Microbiology

ERC

Publisher

Oxford University Press (OUP)

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