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Impact of Elevated Atmospheric CO2 in Spartina maritima Rhizosphere Extracellular Enzymatic Activities

根际 盐生植物 生物地球化学循环 环境化学 微生物种群生物学 中观 沉积物 非生物成分 细胞外 酶分析 化学 生物 植物 生态学 盐度 生物化学 生态系统 细菌 古生物学 遗传学
作者
Bernardo Duarte,Alexandra Baeta,João Carlos Marques,Isabel Caçador
出处
期刊:Water [Multidisciplinary Digital Publishing Institute]
卷期号:15 (14): 2667-2667 被引量:1
标识
DOI:10.3390/w15142667
摘要

Atmospheric CO2 enrichment, which is caused to a large extent by anthropogenic activities, is known to interfere with sediment microbial communities via plant rhizospheres. The present work aimed to evaluate this interaction in Spartina maritima ((Curtis) Fernald.) rhizosediments, aiming to depict the impacts of atmospheric CO2 increase in the biogeochemical processes occurring in the rhizosphere of this pioneer and highly abundant Mediterranean halophyte. For this purpose, mesocosms trials were conducted, exposing salt marsh cores with S. maritima and its sediments to 410 and 700 ppm of CO2 while assessing rhizosediment extracellular enzymatic activities. An evident increase in dehydrogenase activity was observed and directly linked to microbial activity, indicating a priming effect in the rhizosphere community under increased CO2. Phosphatase showed a marked increase in rhizosediments exposed to elevated CO2, denoting a higher requirement of phosphate for maintaining higher biological activity rates. High sulphatase activity suggests a possible S-limitation (microbial or plant) due to elevated CO2, probably due to higher sulphur needs for protein synthesis, thus increasing the need to acquire more labile forms of sulphur. With this need to acquire and synthesize amino acids, a marked decrease in protease activity was detected. Most carbon-related enzymes suffered an increase under increased CO2. Overall, a shift in sediment extracellular enzymatic activity could be observed upon CO2 fertilization, mostly due to priming effects and not due to changes in the quality of carbon substrates, as shown by the sediment stable isotope signatures. The altered recycling activity of organic C, N, and P compounds may lead to an unbalance of these biogeochemical cycles, shifting the rhizosphere ecosystem function, with inevitable changes in the ecosystem services level.

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