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Root responses along a subambient to elevated CO gradient in a C-C grassland

机译:在C-C草地上,地下对CO梯度升高的根响应

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Atmospheric CO (Ca) concentration has increased significantly during the last 20 000 years, and is projected to double this century. Despite the importance of belowground processes in the global carbon cycle, community-level and single species root responses to rising Ca are not well understood. We measured net community root biomass over 3 years using ingrowth cores in a natural C-C grassland exposed to a gradient of Ca from preglacial to future levels (230-550 omol molp#). Root windows and minirhizotron tubes were installed below naturally occurring stands of the C perennial grass Bothriochloa ischaemum and its roots were measured for respiration, carbohydrate concentration, specific root length (SRL), production, and lifespan over 2 years. Community root biomass increased significantly (P<0.05) with Ca over initial conditions, with linear or curvilinear responses depending on sample date. In contrast, B. ischaemum produced significantly more roots at subambient than elevated Ca in minirhizotrons. The lifespan of roots with five or more neighboring roots in minirhizotron windows decreased significantly at high Ca, suggesting that after dense root growth depletes soil resource patches, plants with carbon surpluses readily shed these roots. Root respiration in B. ischaemum showed a curvilinear response to Ca under moist conditions in June 2000, with the lowest rates at Ca<300 omol molp# and peak activity at 450 omol molp# in a quadratic model. B. ischaemum roots at subambient Ca had higher SRLs and slightly higher carbohydrate concentrations than those at higher Ca, which may be related to drier soils at low Ca. Our data emphasize that belowground responses of plant communities to Ca can be quite different from those of the individual species, and suggest that complex interactions between and among roots and their immediate soil environment influence the responses of root physiology and lifespan to changing Ca.
机译:在过去的20000年中,大气中的CO(Ca)浓度显着增加,并且预计本世纪将翻番。尽管地下过程在全球碳循环中非常重要,但人们对钙水平升高对社区水平和单一物种根系的反应知之甚少。我们使用天然C-C草原的生长核测量了3年内的净群落根系生物量,该自然C-C草原暴露于从冰川前到未来水平(230-550 omol molp#)的Ca梯度。根窗和微型根管安装在多年生C多年生禾草的天然林下,并测量其根的呼吸作用,碳水化合物浓度,比根长(SRL),产量和2年以上的寿命。在初始条件下,Ca引起的群落根系生物量显着增加(P <0.05),线性或曲线响应取决于采样日期。相比之下,在小型根生植物中,B。ischaemum在周围环境产生的根比升高的Ca的根要多得多。在高钙下,小根茎窗中具有五个或更多邻近根的根的寿命显着降低,这表明密集的根生长耗尽了土壤资源斑块后,具有碳富余的植物很容易脱落这些根。 2000年6月,在湿润条件下,双歧杆菌的根呼吸显示出对Ca的曲线响应,在二次模型中,Ca <300 omol molp#时速率最低,峰值活性在450 omol molp#时最低。与较高Ca水平的那些相比,处于较高环境Ca水平的B. ischaemum根具有较高的SRL和较高的碳水化合物浓度,这可能与低Ca水平下较干燥的土壤有关。我们的数据强调,植物群落对Ca的地下响应可能与单个物种的响应完全不同,并且表明根与根之间以及根与土壤的直接土壤环境之间的复杂相互作用会影响根生理和寿命对改变Ca的响应。

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