2013
DOI: 10.1016/j.ecoleng.2013.09.056
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Consequences of short-term C4 plant Spartina alterniflora invasions for soil organic carbon dynamics in a coastal wetland of Eastern China

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Cited by 113 publications
(76 citation statements)
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“…This area is characterized as warm temperate with an average annual temperature of 13.8 °C, average annual precipitation of 1000 mm, and average annual sea water salinity of 3.09%16. JYWNNRRB was designated as an internationally important wetland site (Ramsar) in 2002.…”
Section: Methodsmentioning
confidence: 99%
“…This area is characterized as warm temperate with an average annual temperature of 13.8 °C, average annual precipitation of 1000 mm, and average annual sea water salinity of 3.09%16. JYWNNRRB was designated as an internationally important wetland site (Ramsar) in 2002.…”
Section: Methodsmentioning
confidence: 99%
“…was founded in 1983, and is one of the best-preserved natural salt marshes in China (Yang et al 2013;Zhou et al 2009). It was recognized as a part of the UNESCO World Network of Biosphere Reserves in 1992 and is critical to China's biodiversity conservation (Yang et al 2015).…”
Section: Study Areamentioning
confidence: 98%
“…)。 滨海湿地生态系统的有机碳主要有外源输入 和内源输入两种途径。外源输入通过水源载体, 例 如潮汐等横向通量带来的悬浮颗粒和溶解的有机碳 (Hemminga et al, 1996)。内源输入包括土壤有机质 与凋落物分解、 浮游生物代谢等 (Harvey & Mannino, 2001)。滨海湿地受到河水径流和海洋潮汐的影响, 因此水流和泥沙中携带的大量悬浮有机物可以通过 横向通量进入土壤碳库 (Wolaver & Spurrier, 1988)。 互花米草具有密集粗壮的茎秆和发达的地下根系 (Liao et al, 2007), 其缓流消浪的能力更促进了泥沙 的沉降和淤积, 因而在互花米草入侵对生态系统碳 收支影响的研究中, 潮汐活动导致的横向通量是其 中的重要组成部分 (Cheng et al, 2006(Cheng et al, , 2008Zhang et al, 2010) 碳含量 , 其周转较慢, 因此互花 米草能够明显增加土壤有机碳和总氮 (Cheng et al, 2006(Cheng et al, , 2008Liao et al, 2007), 并在时间尺度上表现 出累积效应 Yang et al, 2013) Mixing diagram for a mixing model utilizing one isotope value and two sources for the soil organic carbon pool, the triangles represent the soils of SA-4 sampling points, the POC and SA represent sediment and Spartina alterniflora plant sources, respectively.…”
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