{"title":"沉水植物增加了印度曼尼普尔邦Keibul Lamjao国家公园淡水湿地的碳排放(CO2和CH4)","authors":"Suraj S. Chingangbam, R.S. Khoiyangbam","doi":"10.1016/j.limno.2023.126125","DOIUrl":null,"url":null,"abstract":"<div><p><span><span>Worldwide, the exacerbation of global warming has accelerated the growth of </span>submerged macrophytes in wetlands, thereby substantiating the supply of labile substrates for carbon (CH</span><sub>4</sub> and CO<sub>2</sub><span>) emissions. Nevertheless, limited studies have been conducted on carbon emission from tropical wetlands with submerged macrophytes. In the current study an attempt has been made to reveal the role of submerged macrophytes in influencing carbon flux from a natural wetland in the Indo-Burma Biodiversity hotspots. The submerged macrophytes colonising the shallow freshwater wetland of Keibul Lamjao comprise of </span><span><em>Hydrilla verticillata</em></span>, <span><em>Ceratophyllum demersum</em><em>,</em></span> and <span><em>Potamogeton crispus</em><em>,</em></span> with primary productivity at community level ranging between 20.72 and 152.53 g m<sup>-2</sup> d<sup>-1</sup> (mean, 95.6 ± 54.66 g m<sup>-2</sup> d<sup>-1</sup>). This study gives a comparative analysis of the carbon gases (CH<sub>4</sub> and CO<sub>2</sub>) emission in two distinct zones of the wetland: areas with profuse submerged macrophytic growth and water free of macrophytes. The mean CO<sub>2</sub> and CH<sub>4</sub> emissions from the zone with submerged macrophytes were 8362.64 ± 2935.57 and 227.90 ± 73.50 mg m<sup>-2</sup> d<sup>-1</sup>, respectively, compared to 5558.07 ± 1222.05 and 149.72 ± 20.44 mg m<sup>-2</sup> d<sup>-1</sup> from those without macrophytes. The CO<sub>2</sub> and CH<sub>4</sub><span><span> emissions peak during the summer and wane in the following seasons, with minimum emissions occurring during the winter. It is apparent from the results that the generation of the gases in the wetland was temperature dependent, plus the macrophytic detritus availability. The carbon emissions were significantly correlated with the </span>physicochemical properties<span> of the water and the lake bottom sediment. A significantly positive correlation between carbon emission and dissolved organic carbon (DOC) and organic matter (OM) was established in the zone with macrophytes, thereby revealing that the growth of submerged macrophytes in the wetland enhances atmospheric carbon emissions.</span></span></p></div>","PeriodicalId":51110,"journal":{"name":"Limnologica","volume":"103 ","pages":"Article 126125"},"PeriodicalIF":2.0000,"publicationDate":"2023-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Submerged macrophytes enhance carbon emission (CO2 and CH4) from the freshwater wetland in Keibul Lamjao National Park, Manipur, India\",\"authors\":\"Suraj S. Chingangbam, R.S. 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The submerged macrophytes colonising the shallow freshwater wetland of Keibul Lamjao comprise of </span><span><em>Hydrilla verticillata</em></span>, <span><em>Ceratophyllum demersum</em><em>,</em></span> and <span><em>Potamogeton crispus</em><em>,</em></span> with primary productivity at community level ranging between 20.72 and 152.53 g m<sup>-2</sup> d<sup>-1</sup> (mean, 95.6 ± 54.66 g m<sup>-2</sup> d<sup>-1</sup>). This study gives a comparative analysis of the carbon gases (CH<sub>4</sub> and CO<sub>2</sub>) emission in two distinct zones of the wetland: areas with profuse submerged macrophytic growth and water free of macrophytes. The mean CO<sub>2</sub> and CH<sub>4</sub> emissions from the zone with submerged macrophytes were 8362.64 ± 2935.57 and 227.90 ± 73.50 mg m<sup>-2</sup> d<sup>-1</sup>, respectively, compared to 5558.07 ± 1222.05 and 149.72 ± 20.44 mg m<sup>-2</sup> d<sup>-1</sup> from those without macrophytes. The CO<sub>2</sub> and CH<sub>4</sub><span><span> emissions peak during the summer and wane in the following seasons, with minimum emissions occurring during the winter. It is apparent from the results that the generation of the gases in the wetland was temperature dependent, plus the macrophytic detritus availability. The carbon emissions were significantly correlated with the </span>physicochemical properties<span> of the water and the lake bottom sediment. 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引用次数: 0
摘要
在世界范围内,全球变暖的加剧加速了湿地淹没植物的生长,从而证实了碳(CH4和CO2)排放的稳定基质的供应。然而,对热带淹没植物湿地碳排放的研究有限。本研究试图揭示淹没植物对印缅生物多样性热点地区天然湿地碳通量的影响。京布兰老浅水湿地的淹没植物主要有水螅(Hydrilla verticillata)、角藻(Ceratophyllum demersum)和薯(Potamogeton crispus),群落初级生产力在20.72 ~ 152.53 g m-2 d-1之间(平均为95.6±54.66 g m-2 d-1)。本研究对比分析了该湿地两个不同区域的碳气体(CH4和CO2)排放,即沉水植物生长旺盛的区域和无水植物的区域。有淹没植物区CO2和CH4的平均排放量分别为8362.64±2935.57和227.90±73.50 mg m-2 d-1,而无淹没植物区CO2和CH4的平均排放量分别为5558.07±1222.05和149.72±20.44 mg m-2 d-1。CO2和CH4的排放在夏季达到峰值,随后的季节逐渐减弱,冬季排放量最小。从结果可以明显看出,湿地中气体的产生依赖于温度,加上大量植物碎屑的可用性。水体和湖底沉积物的理化性质与碳排放呈显著相关。在有大型植物的区域,碳排放与溶解有机碳(DOC)和有机质(OM)呈显著正相关,表明湿地淹没植物的生长促进了大气碳排放。
Submerged macrophytes enhance carbon emission (CO2 and CH4) from the freshwater wetland in Keibul Lamjao National Park, Manipur, India
Worldwide, the exacerbation of global warming has accelerated the growth of submerged macrophytes in wetlands, thereby substantiating the supply of labile substrates for carbon (CH4 and CO2) emissions. Nevertheless, limited studies have been conducted on carbon emission from tropical wetlands with submerged macrophytes. In the current study an attempt has been made to reveal the role of submerged macrophytes in influencing carbon flux from a natural wetland in the Indo-Burma Biodiversity hotspots. The submerged macrophytes colonising the shallow freshwater wetland of Keibul Lamjao comprise of Hydrilla verticillata, Ceratophyllum demersum, and Potamogeton crispus, with primary productivity at community level ranging between 20.72 and 152.53 g m-2 d-1 (mean, 95.6 ± 54.66 g m-2 d-1). This study gives a comparative analysis of the carbon gases (CH4 and CO2) emission in two distinct zones of the wetland: areas with profuse submerged macrophytic growth and water free of macrophytes. The mean CO2 and CH4 emissions from the zone with submerged macrophytes were 8362.64 ± 2935.57 and 227.90 ± 73.50 mg m-2 d-1, respectively, compared to 5558.07 ± 1222.05 and 149.72 ± 20.44 mg m-2 d-1 from those without macrophytes. The CO2 and CH4 emissions peak during the summer and wane in the following seasons, with minimum emissions occurring during the winter. It is apparent from the results that the generation of the gases in the wetland was temperature dependent, plus the macrophytic detritus availability. The carbon emissions were significantly correlated with the physicochemical properties of the water and the lake bottom sediment. A significantly positive correlation between carbon emission and dissolved organic carbon (DOC) and organic matter (OM) was established in the zone with macrophytes, thereby revealing that the growth of submerged macrophytes in the wetland enhances atmospheric carbon emissions.
期刊介绍:
Limnologica is a primary journal for limnologists, aquatic ecologists, freshwater biologists, restoration ecologists and ecotoxicologists working with freshwater habitats.