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互花米草入侵对中国长江口土壤呼吸的影响。

Effects of Spartina alterniflora invasion on soil respiration in the Yangtze River estuary, China.

作者信息

Bu Naishun, Qu Junfeng, Li Zhaolei, Li Gang, Zhao Hua, Zhao Bin, Li Bo, Chen Jiakuan, Fang Changming

机构信息

Coastal Ecosystems Research Station of the Yangtze River Estuary, Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, The Institute of Biodiversity Science, Fudan University, Shanghai, China; School of Environmental Science and Spatial Informatics, China University of Mining and Technology, Xuzhou, China.

Low-carbon Energy Research Institute, China University of Mining and Technology, Xuzhou, China.

出版信息

PLoS One. 2015 Mar 23;10(3):e0121571. doi: 10.1371/journal.pone.0121571. eCollection 2015.

Abstract

Many studies have found that plant invasion can enhance soil organic carbon (SOC) pools, by increasing net primary production (NPP) and/or decreased soil respiration. While most studies have focused on C input, little attention has been paid to plant invasion effects on soil respiration, especially in wetland ecosystems. Our study examined the effects of Spartina alterniflora invasion on soil respiration and C dynamics in the Yangtze River estuary. The estuary was originally occupied by two native plant species: Phragmites australis in the high tide zone and Scirpus mariqueter in the low tide zone. Mean soil respiration rates were 185.8 and 142.3 mg CO2 m(-2) h(-1) in S. alterniflora and P. australis stands in the high tide zone, and 159.7 and 112.0 mg CO2 m(-2) h(-1) in S. alterniflora and S. mariqueter stands in the low tide zone, respectively. Aboveground NPP (ANPP), SOC, and microbial biomass were also significantly higher in the S. alterniflora stands than in the two native plant stands. S. alterniflora invasion did not significantly change soil inorganic carbon or pH. Our results indicated that enhanced ANPP by S. alterniflora exceeded invasion-induced C loss through soil respiration. This suggests that S. alterniflora invasion into the Yangtze River estuary could strengthen the net C sink of wetlands in the context of global climate change.

摘要

许多研究发现,植物入侵可通过增加净初级生产力(NPP)和/或降低土壤呼吸来增强土壤有机碳(SOC)库。虽然大多数研究都集中在碳输入上,但很少有人关注植物入侵对土壤呼吸的影响,尤其是在湿地生态系统中。我们的研究考察了互花米草入侵对长江口土壤呼吸和碳动态的影响。该河口原本生长着两种本土植物:高潮带的芦苇和低潮带的海三棱藨草。在高潮带,互花米草和芦苇群落的土壤呼吸平均速率分别为185.8和142.3毫克二氧化碳·平方米-2·小时-1,在低潮带,互花米草和海三棱藨草群落的土壤呼吸平均速率分别为159.7和112.0毫克二氧化碳·平方米-2·小时-1。互花米草群落的地上净初级生产力(ANPP)、土壤有机碳和微生物生物量也显著高于两种本土植物群落。互花米草入侵并未显著改变土壤无机碳或pH值。我们的结果表明,互花米草增强的地上净初级生产力超过了入侵导致的通过土壤呼吸的碳损失。这表明在全球气候变化的背景下,互花米草入侵长江口可能会加强湿地的净碳汇。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6162/4370568/ba839de63536/pone.0121571.g001.jpg

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