Soil Organic Nitrogen Mineralization and N2O Production Driven by Changes in Coastal Wetlands

IF 5.4 2区 地球科学 Q1 ENVIRONMENTAL SCIENCES Global Biogeochemical Cycles Pub Date : 2024-05-30 DOI:10.1029/2024GB008154
Ping Yang, Hong Yang, Yan Hong, Xiao Lin, Linhai Zhang, Chuan Tong, Derrick Y. F. Lai, Lishan Tan, Yongxin Lin, Yalan Tian, Kam W. Tang
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Abstract

Plant invasion and land reclamation have drastically transformed the landscape of coastal wetlands globally, but their resulting effects on soil organic nitrogen (SON) mineralization and nitrous oxide (N2O) production remain unclear. In this study, we examined 21 coastal wetlands across southern China that have undergone habitat transformation from native mudflats (MFs) to Spartina alterniflora marshes (SAs), and subsequently to earthen aquaculture ponds (APs). We determined the SON net mineralization rate and the presence of pertinent enzyme-encoding genes, namely chiA, pepA, and pepN. The SON net mineralization rate increased by 46.7% following the conversion of MFs to SAs but decreased by 33.1% in response to the transformation of SAs to APs. Nevertheless, there was no significant difference in the estimated mineralization efficiency of soil microbes among the habitat types. The results of structural equation modeling showed that N-mineralization gene abundance played a major role in regulating SON mineralization. Although less than 20% of the SON was estimated to be labile/semi-labile, SON mineralization was important in sustaining soil N2O production, with 5.8% of the mineralized N being fed into N2O production. Overall, our findings showed that the presence of S. alterniflora increased both SON content and mineralization rate, which would in turn promote further proliferation of this exotic plant along the coast. The conversion of S. alterniflora marshes to APs partially mitigated the positive effects of exotic plant invasion on SON turnover.

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沿海湿地变化驱动的土壤有机氮矿化和一氧化二氮产生量
植物入侵和土地开垦极大地改变了全球沿海湿地的景观,但它们对土壤有机氮(SON)矿化和一氧化二氮(N2O)产生的影响仍不清楚。在这项研究中,我们考察了中国南方 21 个沿海湿地,这些湿地的生境经历了从原生滩涂(MFs)到Spartina alterniflora沼泽(SAs),再到土质水产养殖池塘(APs)的转变。我们测定了 SON 的净矿化率以及相关酶编码基因(即 chiA、pepA 和 pepN)的存在情况。在 MFs 转化为 SAs 后,SON 净矿化率提高了 46.7%,但在 SAs 转化为 APs 后,SON 净矿化率降低了 33.1%。尽管如此,不同生境类型的土壤微生物矿化效率估计值并无明显差异。结构方程模型的结果表明,N矿化基因丰度在调节SON矿化过程中发挥了重要作用。虽然据估计只有不到20%的SON是可亲和/半亲和性的,但SON矿化对维持土壤N2O的产生非常重要,5.8%的矿化氮被用于N2O的产生。总之,我们的研究结果表明,交替花属植物的存在增加了 SON 的含量和矿化率,这反过来又会促进这种外来植物在沿海地区的进一步扩散。将交替花沼泽转化为旱地沼泽在一定程度上缓解了外来植物入侵对 SON 转化率的积极影响。
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来源期刊
Global Biogeochemical Cycles
Global Biogeochemical Cycles 环境科学-地球科学综合
CiteScore
8.90
自引率
7.70%
发文量
141
审稿时长
8-16 weeks
期刊介绍: Global Biogeochemical Cycles (GBC) features research on regional to global biogeochemical interactions, as well as more local studies that demonstrate fundamental implications for biogeochemical processing at regional or global scales. Published papers draw on a wide array of methods and knowledge and extend in time from the deep geologic past to recent historical and potential future interactions. This broad scope includes studies that elucidate human activities as interactive components of biogeochemical cycles and physical Earth Systems including climate. Authors are required to make their work accessible to a broad interdisciplinary range of scientists.
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