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Exotic Spartina alterniflora invasion alters ecosystem-atmosphere exchange of CH4 and N2O and carbon sequestration in a coastal salt marsh in China

机译:外来互花米草入侵入侵改变了中国沿海盐沼的生态系统-大气交换CH4和N2O和固碳

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Coastal salt marshes are sensitive to global climate change and may play an important role in mitigating global warming. To evaluate the impacts of Spartina alterniflora invasion on global warming potential (GWP) in Chinese coastal areas, we measured CH4 and N2O fluxes and soil organic carbon sequestration rates along a transect of coastal wetlands in Jiangsu province, China, including open water; bare tidal flat; and invasive S. alterniflora, native Suaeda salsa, and Phragmites australis marshes. Annual CH4 emissions were estimated as 2.81, 4.16, 4.88, 10.79, and 16.98kg CH(4)ha(-1) for open water, bare tidal flat, and P. australis, S. salsa, and S. alterniflora marshes, respectively, indicating that S. alterniflora invasion increased CH4 emissions by 57-505%. In contrast, negative N2O fluxes were found to be significantly and negatively correlated (P<0.001) with net ecosystem CO2 exchange during the growing season in S. alterniflora and P. australis marshes. Annual N2O emissions were 0.24, 0.38, and 0.56kg N(2)Oha(-1) in open water, bare tidal flat and S. salsa marsh, respectively, compared with -0.51kg N(2)Oha(-1) for S. alterniflora marsh and -0.25kg N(2)Oha(-1) for P. australis marsh. The carbon sequestration rate of S. alterniflora marsh amounted to 3.16 Mg Cha(-1)yr(-1) in the top 100cm soil profile, a value that was 2.63- to 8.78-fold higher than in native plant marshes. The estimated GWP was 1.78, -0.60, -4.09, and -1.14Mg CO(2)eq ha(-1)yr(-1) in open water, bare tidal flat, P. australis marsh and S. salsa marsh, respectively, but dropped to -11.30Mg CO(2)eqha(-1)yr(-1) in S. alterniflora marsh. Our results indicate that although S. alterniflora invasion stimulates CH4 emissions, it can efficiently mitigate increases in atmospheric CO2 and N2O along the coast of China.
机译:沿海盐沼对全球气候变化敏感,可能在缓解全球变暖中发挥重要作用。为了评估互花米草入侵对中国沿海地区全球变暖潜能(GWP)的影响,我们测量了包括开放水域在内的江苏省沿海湿地样带的CH4和N2O通量以及土壤有机碳固存率。裸露的潮滩;以及入侵性互花米草,本土萨伊达州萨尔萨舞草和芦苇沼泽。对于开阔水域,裸露的潮滩和南方假单胞菌,莎莎沙门氏菌和互花米草沼泽地,CH4的年排放量分别估计为2.81、4.16、4.88、10.79和16.98kg CH(4)ha(-1)。 ,表明互花米草的入侵使CH4排放增加了57-505%。相比之下,在互花米草和澳大利亚对虾沼泽生长期中,N2O负通量与生态系统净二氧化碳交换量呈显着负相关(P <0.001)。在开阔水域,裸潮滩和S. salsa沼泽中,N2O的年度排放分别为0.24、0.38和0.56kg N(2)Oha(-1),而对于-0.51kg N(2)Oha(-1)互花米草沼泽和-0.25千克N(2)Oha(-1)用于南方沼泽。在最高的100cm土壤剖面中,互花米草沼泽的碳固存率达3.16 Mg Cha(-1)yr(-1),该值比天然植物沼泽高2.63-8.78倍。在开阔水域,裸潮滩,南极沼泽地和萨尔萨斯沼泽地中,估计的GWP分别为1.78,-0.60,-4.09和-1.14Mg CO(2)eq ha(-1)yr(-1) ,但在互花米草沼泽中降至-11.30Mg CO(2)eqha(-1)yr(-1)。我们的结果表明,尽管互花米草入侵会刺激CH4排放,但它可以有效缓解中国沿海大气CO2和N2O的增加。

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