School of Environment, Nanjing Normal University, Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Jiangsu Key Laboratory of Environmental Change and Ecological Construction, Nanjing 210023, China.
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, China.
Sci Total Environ. 2022 Sep 15;839:156357. doi: 10.1016/j.scitotenv.2022.156357. Epub 2022 May 29.
Estuarine wetlands play important roles in the regional and global carbon cycle as well as greenhouse gas emissions; however, the driving factors and potential carbon emissions mechanisms are unclear. Here, the carbon emission fluxes were investigated in situ from different vegetated areas in the Chongming wetlands. The results showed that the highest methane (CH) and carbon dioxide (CO) emissions of 178.1 and 21,482.5 mg∙m∙min were in Scirpus mariqueter and Phragmites australis dominated areas, respectively. A series of microcosms was strategically designed to simulate the influence of tidal variation on carbon emissions and the litter decomposition on daily- and monthly-timescales in estuarine wetlands. All added litter promoted CH and CO emissions from the wetland soils. The CH and CO emission fluxes of the S. mariqueter treatment were higher (367.7 vs. 108.4; 1607.9 vs. 1324.3 mg∙m∙min) than those of the P. australis treatment without tidal variation on a monthly timescale, due to the higher total organic carbon (TOC) content of S. mariqueter. The decomposition of litter also released a large amount of nutrients, which enhanced the abundance of methane-producing archaea (MPA) and methane-oxidizing bacteria (MOB). However, the tidal water level was negatively correlated with CH and CO emission fluxes. The CH and CO emission fluxes in the S. mariqueter treatment at the lowest tide were 556.02 and 604.99 mg∙m∙min, respectively. However, the CH and CO emission fluxes did not change significantly on the daily timescale in the S. mariqueter treatment without tidal variations. Therefore, the prolonged timescales revealed increases in litter decomposition but a decrease in the contribution of tidal variations to carbon emissions in estuarine wetlands. These findings provide a theoretical basis for evaluating the carbon cycle in estuarine wetlands.
滨海湿地在区域和全球碳循环以及温室气体排放中发挥着重要作用;然而,其驱动因素和潜在的碳排放机制尚不清楚。本研究原位调查了崇明湿地不同植被区的碳排放通量。结果表明,互花米草和芦苇区的甲烷(CH)和二氧化碳(CO)排放通量最高,分别为 178.1 和 21,482.5 mg∙m∙min。一系列微宇宙实验被战略性设计以模拟潮汐变化对碳排放和湿地土壤中凋落物分解的影响,包括日时间尺度和月时间尺度。所有添加的凋落物都促进了湿地土壤中 CH 和 CO 的排放。在月时间尺度上,与无潮汐变化的芦苇区相比,互花米草区的 CH 和 CO 排放通量更高(367.7 比 108.4;1607.9 比 1324.3 mg∙m∙min),这是由于互花米草的总有机碳(TOC)含量更高。凋落物的分解也释放了大量养分,从而增加了产甲烷古菌(MPA)和甲烷氧化菌(MOB)的丰度。然而,潮水水位与 CH 和 CO 排放通量呈负相关。在最低潮位时,互花米草区的 CH 和 CO 排放通量分别为 556.02 和 604.99 mg∙m∙min。然而,在无潮汐变化的互花米草区,CH 和 CO 排放通量在日时间尺度上没有显著变化。因此,延长时间尺度会增加凋落物的分解,但会减少潮汐变化对滨海湿地碳排放的贡献。这些发现为评估滨海湿地的碳循环提供了理论依据。