Title Anaerobic ammonium oxidation coupled to arsenate reduction, a novel biogeochemical process observed in arsenic-contaminated paddy soil
Authors Zhang, Miaomiao
Kolton, Max
Haggblom, Max M.
Sun, Xiaoxu
Yu, Ke
He, Bin
Yuan, Zaijian
Dong, Yiran
Su, Xianfa
Chen, Zhenyu
Li, Hui
Xiao, Tangfu
Xiao, Enzong
Sun, Weimin
Affiliation Guangdong Acad Sci, Natl Reg Joint Engn Res Ctr Soil Pollut Control &, Guangdong Key Lab Integrated Agroenvironm Pollut, Inst Ecoenvironm & Soil Sci, Guangzhou 510650, Peoples R China
Guangzhou Univ, Sch Environm Sci & Engn, Key Lab Water Qual & Conservat Pearl River Delta, Minist Educ, Guangzhou 510006, Peoples R China
Ben Gurion Univ Negev, French Associates Inst Agr & Biotechnol Drylands, Jacob Blaustein Inst Desert Res, Sede Boqer Campus, IL-8499000 Beer Sheva, Israel
Rutgers State Univ, Dept Biochem & Microbiol, New Brunswick, NJ 08901 USA
Peking Univ, Sch Environm & Energy, Shenzhen Grad Sch, Shenzhen 518055, Peoples R China
China Univ Geosci Wuhan, Sch Environm Studies, Wuhan 430074, Peoples R China
Henan Normal Univ, Sch Environm, Key Lab Yellow River & Huai River Water Environm, Minist Educ, Xinxiang 453007, Henan, Peoples R China
Jinan Univ, Coll Life Sci & Technol, Dept Ecol, Guangzhou 510632, Peoples R China
Keywords NITROGEN LOSS
ANAMMOX BACTERIA
IRON REDUCTION
WATER
DENITRIFICATION
CHROMATE
HALOTOLERANT
BIODIVERSITY
MOBILIZATION
MANGANESE
Issue Date 15-Oct-2022
Publisher GEOCHIMICA ET COSMOCHIMICA ACTA
Abstract Anaerobic ammonium oxidation represents an important pathway of N loss, which can be coupled with reduction of nitrite and metal(loid)s (e.g., Fe(III) and Mn(IV)). Similar to Fe(III) and Mn(IV), As(V) is also an active metal(loid) and ammonium oxidation coupled with As(V) reduction is thermodynamically feasible. However, little is known about this poten-tial process. In this study, anaerobic ammonium oxidation coupled with As(V) reduction, designated as Asammox, was observed in cultures inoculated from As-contaminated paddy soil using N-15 isotope tracer analysis. Compared with the treat-ment amended with N-15-urea only, the production of N-15-labeled N-2 (i.e., N-30(2) and N-29(2)) was significantly greater in the treat-ment amended with As(V) and N-15-urea. Furthermore, the abundances of the genes encoding for arsenate reductase (arrA) and hydrazine synthase (hzsB) were significantly higher in the treatment amended with As(V) and N-15-urea than those in the treatment amended with N-15-urea only. In addition, putative Asammox bacteria affiliated with Halomonas, Pelagibacterium, and Chelativorans were identified by DNA-stable isotope probing. Members of Ca. Brocadia were the most dominant Anam-mox bacteria in the soil cultures and may interact with Asammox bacteria in ammonium oxidation, suggesting that the N loss may be attributed to the contribution of Asammox and Anammox in the As-contaminated soil. The observation of Asam-mox, a novel biogeochemical process, and identification of bacteria responsible for this biogeochemical process expands the fundamental understanding of both N and As biogeochemical cycling. In addition, this study provides a proof-of-concept for investigating anaerobic ammonium oxidation coupled with metal(loid)s reduction by combining stable isotope probing and isotope tracer microcosm incubations. (C) 2022 Elsevier Ltd. All rights reserved.
URI http://hdl.handle.net/20.500.11897/654733
ISSN 0016-7037
DOI 10.1016/j.gca.2022.08.020
Indexed SCI(E)
Appears in Collections: 环境与能源学院

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