Sedimentary processes dominate nitrous oxide production and emission in the hypoxic zone off the Changjiang River estuary
Coastal oceans, known as the major nitrous oxide (N2O) source to the atmosphere, are increasingly subject to eutrophication and concurrent near-bottom hypoxia. The natural nitrogen cycle is likely to be altered markedly in hypoxic coastal oceans. However, the processes responsible for N2O production...
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| Published in | The Science of the total environment Vol. 827; p. 154042 |
|---|---|
| Main Authors | , , , , , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Netherlands
Elsevier B.V
25.06.2022
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| Subjects | |
| Online Access | Get full text |
| ISSN | 0048-9697 1879-1026 1879-1026 |
| DOI | 10.1016/j.scitotenv.2022.154042 |
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| Abstract | Coastal oceans, known as the major nitrous oxide (N2O) source to the atmosphere, are increasingly subject to eutrophication and concurrent near-bottom hypoxia. The natural nitrogen cycle is likely to be altered markedly in hypoxic coastal oceans. However, the processes responsible for N2O production and emission remain elusive because of lacking field rate measurements simultaneously conducted in the water column and sediment. Here, we quantified N2O production rates using a 15N-labeled technique in the water-column and surface sediments off the Changjiang (Yangtze) River estuary, the largest hypoxic zone in the Pacific margins. Our results showed that the estuarine surface sediments were the major source for N2O production, accounting for approximately 90% of the total water-column accumulation and consequent efflux of N2O in the hypoxic zone, whereas the water-column nitrification and denitrification combined only contributed <10%. More importantly, the coupling of nitrification and denitrification at the presence of abundant supply and remineralization of labile organic matter was the main driver of the N2O release from the sediment-water interface in this region. This study highlights the dominant role of benthic processes occurring at the sediment-water interface controlling the coastal N2O budget, as the anthropogenic eutrophication and hypoxia are expanding in coastal oceans.
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•Low dissolved oxygen levels enhanced the N2O production in the hypoxic zone.•Surface sediments were the major source for N2O production in the hypoxic zone.•Sedimentary N2O release was predominated by coupled nitrification-denitrification.•Remineralization of labile organic matter may stimulate sedimentary N2O production. |
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| AbstractList | Coastal oceans, known as the major nitrous oxide (N₂O) source to the atmosphere, are increasingly subject to eutrophication and concurrent near-bottom hypoxia. The natural nitrogen cycle is likely to be altered markedly in hypoxic coastal oceans. However, the processes responsible for N₂O production and emission remain elusive because of lacking field rate measurements simultaneously conducted in the water column and sediment. Here, we quantified N₂O production rates using a ¹⁵N-labeled technique in the water-column and surface sediments off the Changjiang (Yangtze) River estuary, the largest hypoxic zone in the Pacific margins. Our results showed that the estuarine surface sediments were the major source for N₂O production, accounting for approximately 90% of the total water-column accumulation and consequent efflux of N₂O in the hypoxic zone, whereas the water-column nitrification and denitrification combined only contributed <10%. More importantly, the coupling of nitrification and denitrification at the presence of abundant supply and remineralization of labile organic matter was the main driver of the N₂O release from the sediment-water interface in this region. This study highlights the dominant role of benthic processes occurring at the sediment-water interface controlling the coastal N₂O budget, as the anthropogenic eutrophication and hypoxia are expanding in coastal oceans. Coastal oceans, known as the major nitrous oxide (N2O) source to the atmosphere, are increasingly subject to eutrophication and concurrent near-bottom hypoxia. The natural nitrogen cycle is likely to be altered markedly in hypoxic coastal oceans. However, the processes responsible for N2O production and emission remain elusive because of lacking field rate measurements simultaneously conducted in the water column and sediment. Here, we quantified N2O production rates using a 15N-labeled technique in the water-column and surface sediments off the Changjiang (Yangtze) River estuary, the largest hypoxic zone in the Pacific margins. Our results showed that the estuarine surface sediments were the major source for N2O production, accounting for approximately 90% of the total water-column accumulation and consequent efflux of N2O in the hypoxic zone, whereas the water-column nitrification and denitrification combined only contributed <10%. More importantly, the coupling of nitrification and denitrification at the presence of abundant supply and remineralization of labile organic matter was the main driver of the N2O release from the sediment-water interface in this region. This study highlights the dominant role of benthic processes occurring at the sediment-water interface controlling the coastal N2O budget, as the anthropogenic eutrophication and hypoxia are expanding in coastal oceans. [Display omitted] •Low dissolved oxygen levels enhanced the N2O production in the hypoxic zone.•Surface sediments were the major source for N2O production in the hypoxic zone.•Sedimentary N2O release was predominated by coupled nitrification-denitrification.•Remineralization of labile organic matter may stimulate sedimentary N2O production. Coastal oceans, known as the major nitrous oxide (N O) source to the atmosphere, are increasingly subject to eutrophication and concurrent near-bottom hypoxia. The natural nitrogen cycle is likely to be altered markedly in hypoxic coastal oceans. However, the processes responsible for N O production and emission remain elusive because of lacking field rate measurements simultaneously conducted in the water column and sediment. Here, we quantified N O production rates using a N-labeled technique in the water-column and surface sediments off the Changjiang (Yangtze) River estuary, the largest hypoxic zone in the Pacific margins. Our results showed that the estuarine surface sediments were the major source for N O production, accounting for approximately 90% of the total water-column accumulation and consequent efflux of N O in the hypoxic zone, whereas the water-column nitrification and denitrification combined only contributed <10%. More importantly, the coupling of nitrification and denitrification at the presence of abundant supply and remineralization of labile organic matter was the main driver of the N O release from the sediment-water interface in this region. This study highlights the dominant role of benthic processes occurring at the sediment-water interface controlling the coastal N O budget, as the anthropogenic eutrophication and hypoxia are expanding in coastal oceans. Coastal oceans, known as the major nitrous oxide (N2O) source to the atmosphere, are increasingly subject to eutrophication and concurrent near-bottom hypoxia. The natural nitrogen cycle is likely to be altered markedly in hypoxic coastal oceans. However, the processes responsible for N2O production and emission remain elusive because of lacking field rate measurements simultaneously conducted in the water column and sediment. Here, we quantified N2O production rates using a 15N-labeled technique in the water-column and surface sediments off the Changjiang (Yangtze) River estuary, the largest hypoxic zone in the Pacific margins. Our results showed that the estuarine surface sediments were the major source for N2O production, accounting for approximately 90% of the total water-column accumulation and consequent efflux of N2O in the hypoxic zone, whereas the water-column nitrification and denitrification combined only contributed <10%. More importantly, the coupling of nitrification and denitrification at the presence of abundant supply and remineralization of labile organic matter was the main driver of the N2O release from the sediment-water interface in this region. This study highlights the dominant role of benthic processes occurring at the sediment-water interface controlling the coastal N2O budget, as the anthropogenic eutrophication and hypoxia are expanding in coastal oceans.Coastal oceans, known as the major nitrous oxide (N2O) source to the atmosphere, are increasingly subject to eutrophication and concurrent near-bottom hypoxia. The natural nitrogen cycle is likely to be altered markedly in hypoxic coastal oceans. However, the processes responsible for N2O production and emission remain elusive because of lacking field rate measurements simultaneously conducted in the water column and sediment. Here, we quantified N2O production rates using a 15N-labeled technique in the water-column and surface sediments off the Changjiang (Yangtze) River estuary, the largest hypoxic zone in the Pacific margins. Our results showed that the estuarine surface sediments were the major source for N2O production, accounting for approximately 90% of the total water-column accumulation and consequent efflux of N2O in the hypoxic zone, whereas the water-column nitrification and denitrification combined only contributed <10%. More importantly, the coupling of nitrification and denitrification at the presence of abundant supply and remineralization of labile organic matter was the main driver of the N2O release from the sediment-water interface in this region. This study highlights the dominant role of benthic processes occurring at the sediment-water interface controlling the coastal N2O budget, as the anthropogenic eutrophication and hypoxia are expanding in coastal oceans. |
| ArticleNumber | 154042 |
| Author | Yang, Jin-Yu Terence Kang, Sijing Hsiao, Silver Sung-Yun Tan, Ehui Lee, Kitack Zou, Wenbin Dai, Minhan Hsu, Ting-Chang Kao, Shuh-Ji Yan, Xiuli Tian, Li Krom, Michael D. |
| Author_xml | – sequence: 1 givenname: Jin-Yu Terence surname: Yang fullname: Yang, Jin-Yu Terence organization: State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China – sequence: 2 givenname: Ting-Chang surname: Hsu fullname: Hsu, Ting-Chang organization: School of Urban and Environmental Sciences, Huaiyin Normal University, Huaiyin 223300, China – sequence: 3 givenname: Ehui surname: Tan fullname: Tan, Ehui organization: State Key Laboratory of Marine Resource Utilization in South China Sea, Hainan University, Haikou 570228, China – sequence: 4 givenname: Kitack surname: Lee fullname: Lee, Kitack organization: Division of Environment and Engineering, Pohang University of Science and Technology, Pohang, Republic of Korea – sequence: 5 givenname: Michael D. surname: Krom fullname: Krom, Michael D. organization: School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK – sequence: 6 givenname: Sijing surname: Kang fullname: Kang, Sijing organization: State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China – sequence: 7 givenname: Minhan surname: Dai fullname: Dai, Minhan organization: State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China – sequence: 8 givenname: Silver Sung-Yun surname: Hsiao fullname: Hsiao, Silver Sung-Yun organization: Institute of Astronomy and Astrophysics, Academia Sinica, Taipei, Taiwan – sequence: 9 givenname: Xiuli surname: Yan fullname: Yan, Xiuli organization: Institute of Marine Science and Guangdong Provincial Key Laboratory of Marine Biotechnology, College of Science, Shantou University, Shantou 515063, China – sequence: 10 givenname: Wenbin surname: Zou fullname: Zou, Wenbin organization: State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China – sequence: 11 givenname: Li surname: Tian fullname: Tian, Li organization: State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China – sequence: 12 givenname: Shuh-Ji surname: Kao fullname: Kao, Shuh-Ji email: sjkao@xmu.edu.cn organization: State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/35217039$$D View this record in MEDLINE/PubMed |
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| CitedBy_id | crossref_primary_10_1016_j_marenvres_2023_106119 crossref_primary_10_1016_j_watres_2022_119121 crossref_primary_10_1016_j_marpolbul_2024_116528 crossref_primary_10_1021_acs_est_3c00950 crossref_primary_10_1016_j_scitotenv_2023_168795 crossref_primary_10_1080_20442041_2025_2478953 crossref_primary_10_1021_acs_est_3c05526 crossref_primary_10_1016_j_envpol_2024_124436 crossref_primary_10_1016_j_gsd_2024_101194 crossref_primary_10_1016_j_marpolbul_2023_115815 crossref_primary_10_1016_j_scitotenv_2022_157381 crossref_primary_10_1029_2023JC020677 crossref_primary_10_1038_s43017_023_00453_6 crossref_primary_10_1007_s10533_023_01021_2 crossref_primary_10_1029_2024JG008617 crossref_primary_10_3390_atmos14081291 crossref_primary_10_1016_j_scitotenv_2023_166930 crossref_primary_10_1029_2022JC019355 crossref_primary_10_1016_j_scitotenv_2025_178568 crossref_primary_10_1016_j_marpolbul_2024_116046 crossref_primary_10_1016_j_marpolbul_2024_117190 |
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| Keywords | Denitrification Sediment-water interface 15N-labeled techniques N2O production rate Coupled nitrification-denitrification Nitrification N-labeled techniques NO production rate |
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| Snippet | Coastal oceans, known as the major nitrous oxide (N2O) source to the atmosphere, are increasingly subject to eutrophication and concurrent near-bottom hypoxia.... Coastal oceans, known as the major nitrous oxide (N O) source to the atmosphere, are increasingly subject to eutrophication and concurrent near-bottom hypoxia.... Coastal oceans, known as the major nitrous oxide (N₂O) source to the atmosphere, are increasingly subject to eutrophication and concurrent near-bottom hypoxia.... |
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| SubjectTerms | 15N-labeled techniques Coupled nitrification-denitrification Denitrification environment estuaries eutrophication hypoxia N2O production rate Nitrification nitrogen cycle nitrous oxide nitrous oxide production organic matter rivers Sediment-water interface sediments Yangtze River |
| Title | Sedimentary processes dominate nitrous oxide production and emission in the hypoxic zone off the Changjiang River estuary |
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