A. Muench, T. Elsey-Quirk, J. R. White, R. D. DeLaune
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The purpose of this study was to examine seasonal C fluxes, specifically, gross ecosystem productivity (GEP), ecosystem respiration (ER), and net ecosystem exchange (NEE) of CO<sub>2</sub> in unvegetated and vegetated (<i>Spartina alterniflora</i>) areas of a 2-year old created marsh, and <i>S. alterniflora</i> and <i>Spartina patens</i> communities in a “natural” reference brackish marsh. <i>S. alterniflora</i>-dominated areas were sinks for CO<sub>2</sub> in both the newly created and reference marsh with an average CO<sub>2</sub> uptake rate of 7.0 ± 1.0 μmol m<sup>−2</sup> s<sup>−1</sup>. The unvegetated areas in the newly created marsh and <i>S. patens</i> areas in the reference marsh had approximately net neutral CO<sub>2</sub> fluxes. <i>S. alterniflora</i> areas of the created marsh had similar carbon fluxes to that in the reference marsh, despite a much lower soil organic matter content. Because vegetation develops much faster than soil properties, restored marshes can be a C sink equivalent to natural marshes as soon as the marsh is vegetated. Ecosystem productivity and C assimilation in <i>S. alterniflora</i> areas of the reference marsh were enhanced by lower elevations (up to 6 cm) and higher soil bulk density (up to 0.28 g cm<sup>−3</sup>). At similar elevations, <i>S. alterniflora</i> in both the created and reference marshes was a greater C sink than <i>S. patens</i> areas of the reference marsh. 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Wetland loss due to anthropogenic and natural causes reduces the carbon (C) storage capacity and potentially releases previously fixed C in biomass and soil to the water column and atmosphere through decomposition. Coastal wetland restoration has the potential to mitigate some of the C losses depending on the balance of C fluxes. However, the role of vegetation and environmental conditions in governing rates of C accumulation in restoration sites is not well resolved. The purpose of this study was to examine seasonal C fluxes, specifically, gross ecosystem productivity (GEP), ecosystem respiration (ER), and net ecosystem exchange (NEE) of CO<sub>2</sub> in unvegetated and vegetated (<i>Spartina alterniflora</i>) areas of a 2-year old created marsh, and <i>S. alterniflora</i> and <i>Spartina patens</i> communities in a “natural” reference brackish marsh. <i>S. alterniflora</i>-dominated areas were sinks for CO<sub>2</sub> in both the newly created and reference marsh with an average CO<sub>2</sub> uptake rate of 7.0 ± 1.0 μmol m<sup>−2</sup> s<sup>−1</sup>. The unvegetated areas in the newly created marsh and <i>S. patens</i> areas in the reference marsh had approximately net neutral CO<sub>2</sub> fluxes. <i>S. alterniflora</i> areas of the created marsh had similar carbon fluxes to that in the reference marsh, despite a much lower soil organic matter content. 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引用次数: 0
摘要
沿海湿地是地球上最具生产力的生态系统之一,具有吸收大量二氧化碳的能力。由于人为和自然原因造成的湿地损失降低了碳(C)的储存能力,并可能通过分解将生物质和土壤中先前固定的碳释放到水柱和大气中。沿海湿地恢复有可能减轻部分碳的损失,这取决于碳通量的平衡。然而,植被和环境条件对恢复地点碳积累速率的影响尚未得到很好的解决。本研究的目的是在一个“自然”参考半咸水湿地中,研究无植被和有植被(互花米草)区域以及互花米草和白米草群落的季节碳通量,特别是总生态系统生产力(GEP)、生态系统呼吸(ER)和净生态系统二氧化碳交换(NEE)。在新建湿地和参考湿地中,以互花草为主的区域均是CO2的汇,平均CO2吸收量为7.0±1.0 μmol m−2 s−1。新造沼泽的无植被区和参考沼泽的S. patens区CO2通量近似为净中性。尽管土壤有机质含量比对照沼泽低得多,但该湿地的互花草区碳通量与对照沼泽相似。由于植被的发展速度比土壤特性快得多,一旦沼泽被植被覆盖,恢复的沼泽就可以成为相当于天然沼泽的碳汇。参考沼泽互花草区域的生态系统生产力和碳同化在低海拔(不超过6 cm)和高土壤容重(不超过0.28 g cm−3)的条件下得到增强。在相同的海拔高度下,互花草在创建湿地和参考湿地的碳汇均大于参考湿地的互花草。我们的研究结果表明,植被的建立对促进湿地碳汇功能至关重要,尤其是物种。
Carbon dioxide fluxes and the dominant role of vegetation in recently created and reference Gulf Coast marshes
Coastal wetlands are one of the most productive ecosystems on Earth with the capacity to sequester large amounts of carbon dioxide (CO2). Wetland loss due to anthropogenic and natural causes reduces the carbon (C) storage capacity and potentially releases previously fixed C in biomass and soil to the water column and atmosphere through decomposition. Coastal wetland restoration has the potential to mitigate some of the C losses depending on the balance of C fluxes. However, the role of vegetation and environmental conditions in governing rates of C accumulation in restoration sites is not well resolved. The purpose of this study was to examine seasonal C fluxes, specifically, gross ecosystem productivity (GEP), ecosystem respiration (ER), and net ecosystem exchange (NEE) of CO2 in unvegetated and vegetated (Spartina alterniflora) areas of a 2-year old created marsh, and S. alterniflora and Spartina patens communities in a “natural” reference brackish marsh. S. alterniflora-dominated areas were sinks for CO2 in both the newly created and reference marsh with an average CO2 uptake rate of 7.0 ± 1.0 μmol m−2 s−1. The unvegetated areas in the newly created marsh and S. patens areas in the reference marsh had approximately net neutral CO2 fluxes. S. alterniflora areas of the created marsh had similar carbon fluxes to that in the reference marsh, despite a much lower soil organic matter content. Because vegetation develops much faster than soil properties, restored marshes can be a C sink equivalent to natural marshes as soon as the marsh is vegetated. Ecosystem productivity and C assimilation in S. alterniflora areas of the reference marsh were enhanced by lower elevations (up to 6 cm) and higher soil bulk density (up to 0.28 g cm−3). At similar elevations, S. alterniflora in both the created and reference marshes was a greater C sink than S. patens areas of the reference marsh. Our findings illustrate that establishment of vegetation is critical to promoting C sink functions in created marshes and, notably, species do matter.
期刊介绍:
The scope of Ecosphere is as broad as the science of ecology itself. The journal welcomes submissions from all sub-disciplines of ecological science, as well as interdisciplinary studies relating to ecology. The journal''s goal is to provide a rapid-publication, online-only, open-access alternative to ESA''s other journals, while maintaining the rigorous standards of peer review for which ESA publications are renowned.