Reduced diurnal temperature range does not change warming impacts on ecosystem carbon balance of Mediterranean grassland mesocosms

被引:27
|
作者
Phillips, Claire L. [1 ,2 ]
Gregg, Jillian W. [2 ]
Wilson, John K. [2 ]
机构
[1] Lawrence Livermore Natl Lab, Ctr Accelerator Mass Spectrometry, Livermore, CA 94551 USA
[2] Terr Ecosyst Res Associates, Corvallis, OR 97333 USA
关键词
asymmetric warming; carbon; diurnal temperature range; grassland; respiration; CLIMATE-CHANGE; TERRESTRIAL ECOSYSTEMS; NIGHT TEMPERATURE; CO2; FLUXES; RESPIRATION; GROWTH; RESPONSES; PHOTOSYNTHESIS; DIOXIDE; YIELDS;
D O I
10.1111/j.1365-2486.2011.02483.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Daily minimum temperature (T-min) has increased faster than daily maximum temperature (T-max) in many parts of the world, leading to decreases in diurnal temperature range (DTR). Projections suggest that these trends are likely to continue in many regions, particularly in northern latitudes and in arid regions. Despite wide speculation that asymmetric warming has different impacts on plant and ecosystem production than equal-night-and-day warming, there has been little direct comparison of these scenarios. Reduced DTR has also been widely misinterpreted as a result of night-only warming, when in fact T-min occurs near dawn, indicating higher morning as well as night temperatures. We report on the first experiment to examine ecosystem-scale impacts of faster increases in T-min than in T-max, using precise temperature controls to create realistic diurnal temperature profiles with gradual day-night temperature transitions and elevated early morning as well as night temperatures. Studying a constructed grassland ecosystem containing species native to Oregon, USA, we found that the ecosystem lost more carbon at elevated than ambient temperatures, but remained unaffected by the 3 degrees C difference in DTR between symmetric warming (constantly ambient + 3.5 degrees C) and asymmetric warming (dawn T-min = ambient + 5 degrees C, afternoon T-max = ambient + 2 degrees C). Reducing DTR had no apparent effect on photosynthesis, probably because temperatures were most different in the morning and late afternoon when light was low. Respiration was also similar in both warming treatments, because respiration temperature sensitivity was not sufficient to respond to the limited temperature differences between asymmetric and symmetric warming. We concluded that changes in daily mean temperatures, rather than changes in T-min/T-max, were sufficient for predicting ecosystem carbon fluxes in this reconstructed Mediterranean grassland system.
引用
收藏
页码:3263 / 3273
页数:11
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