Negative effects of climate change on upland grassland productivity and carbon fluxes are not attenuated by nitrogen status

被引:16
作者
Eze, Samuel [1 ]
Palmer, Sheila M. [1 ]
Chapman, Pippa J. [1 ]
机构
[1] Univ Leeds, Fac Environm, Sch Geog, Leeds LS2 9JT, W Yorkshire, England
关键词
Climate change; Warming; Drought; Carbon flux; Grassland management; Biomass productivity; NET ECOSYSTEM EXCHANGE; SOIL ORGANIC-CARBON; SUMMER DROUGHT; ELEVATED CO2; PRECIPITATION CHANGE; MICROBIAL BIOMASS; ALPINE MEADOW; PLANT-GROWTH; RESPONSES; RESPIRATION;
D O I
10.1016/j.scitotenv.2018.05.032
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Effects of climate change on managed grassland carbon (C) fluxes and biomass production are not well understood. In this study, we investigated the individual and interactive effects of experimental warming (+3 degrees C above ambient summer daily range of 9-12 degrees C), supplemental precipitation (333 mm + 15%) and drought (333 mm -23%) on plant biomass, microbial biomass C (MBC), net ecosystem exchange (NEE) and dissolved organic C (DOC) flux in soil cores from two upland grasslands of different soil nitrogen (N) status (0.54% and 0.37%) in the UK. After one month of acclimation to ambient summer temperature and precipitation, five replicate cores of each treatment were subjected to three months of experimental warming, drought and supplemental precipitation, based on the projected regional summer climate by the end of the 21st Century, in a fully factorial design. NEE and DOC flux were measured throughout the experimental duration, alongside other environmental variables including soil temperature and moisture. Plant biomass and MBC were determined at the end of the experiment. Results showed that warming plus drought resulted in a significant decline in below ground plant biomass (-29 to -37%), above ground plant biomass (-35 to -77%) and NEE (-13 to -29%), regardless of the N status of the soil. Supplemental precipitation could not reverse the negative effects of warming on the net ecosystem C uptake and plant biomass production. This was attributed to physiological stress imposed by warming which suggests that future summer climate will reduce the C sink capacity of the grasslands. Due to the low moisture retention observed in this study, and to verify our findings, it is recommended that future experiments aimed at measuring soil C dynamics under climate change should be carried out under field conditions. Longer term experiments are recommended to account for seasonal and annual variability, and adaptive changes in biota. (C) 2018 Elsevier B.V. All rights reserved.
引用
收藏
页码:398 / 407
页数:10
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