陆地生态系统类型转变与碳循环

 土地利用变化引起的陆地生态系统类型转变对于全球碳循环有着极其重要的作用。　通过总结国内外有关森林砍伐以及森林、草地转变成农田对于碳循环的影响,阐述了可能引起全球“未知汇”现象的重要原因,强调未来中国陆地生态系统碳循环研究应充分重视陆地生态系统类型转变对于全球碳循环的影响研究,包括研究陆地生态系统的不同发展阶段(自然与退化生态系统)、利用方式的改变(森林转化为人工林或农田,草地转化为农田、退耕还林草等)所引起的碳库类型转换的增汇机理及其对全球变化响应,并指出了建立统一观测方法与规范的陆地生态系统碳通量观测网     

陆地生态系统碳循环模型研究概述

陆地碳循环研究是全球变化研究中的一个重要组成部分,而碳循环模型已成为目前研究陆地碳循环的必要手段.本文针对有关碳循环研究方面的进展,介绍了陆地碳循环模型的基本结构、碳循环过程中涉及的两个基本模型以及目前陆地生态系统碳循环模型的两大类型,并通过对现有主要陆地生态系统碳收支模式的分析,指出了未来陆地碳循环模型的研究方向可能是发展基于动态植被的生物物理模型.这种耦合模型也可能是地球系统模式的重要组成部分.     

增强UV-B辐射和干旱对春小麦光合作用及其生长的影响

在室外盆栽条件下研究了UV-B辐射和土壤干旱对春小麦 '和尚头'生长和光合作用的影响.结果显示:(1)干旱、UV-B辐射、干旱+UV-B(复合)处理均可使叶片类黄酮含量增加,且干旱+UV-B处理增加显著高于其他处理(P<0.05).UV-B辐射和干旱单独处理均能显著降低叶片光合色素含量,但UV-B辐射的副作用大于干旱,复合处理对光合色素的影响介于UV-B和干旱之间.(2)各处理间的光合速率日均值大小次序为:对照>UV-B+干旱>UV-B>干旱;增强UV-B对净光合速率的抑制作用大于干旱,而UV-B+干旱处理的抑制作用较二者单独处理有所减轻.(3)UV-B辐射和干旱单独处理后总生物量比对照减少15%,且抑制作用为:干旱>UV-B>复合处理; UV-B辐射和干旱胁迫不但影响春小麦的生物量,而且影响小穗特征和产量.研究表明,UV-B辐射和干旱之间存在交互作用,说明一种胁迫可以减缓(轻)另外一种胁迫对春小麦的抑制作用.     

土壤溶解性有机碳在陆地生态系统碳循环中的作用

土壤溶解性有机碳(DOC)是有机碳库的活跃组分,在陆地生态系统碳循环中发挥重要作用.本文从碳循环重要性着手,综述了土壤DOC在土壤碳固持与温室气体排放中的作用;结合我国的现实情况(如土壤酸化、气候变暖等),探讨了土壤DOC的相关影响因素如土壤性质、环境因素、人为活动对土壤DOC的影响及作用机制,对进一步理解土壤DOC在陆地生态系统碳循环与温室气体减排中的作用具有重要意义.     

地表UV-B辐射增强对土壤-大豆系统N2O排放的影响

通过大田试验和室外盆栽试验,采用人工增加紫外辐射的方法模拟UV-B辐射增强,用静态箱-气相色谱法测定N_2O排放通量,研究地表UV-B辐射增强对土壤-大豆系统N_2O排放的影响.结果表明:在相同的气象条件和田间管理措施下,UV-B辐射增强没有改变土壤-大豆系统N_2O排放通量的季节性变化规律.但从植株结荚到成熟,UV-B辐射增强降低了土壤-大豆系统N_2O排放通量,进而降低了N_2O的累积排放量.收割实验发现,在分枝开花期,UV-B辐射增强对土壤N_2O排放影响明显,降低了土壤N_2O排放通量;从结荚至鼓粒期,UV-B辐射增强主要通过降低植株地上部分N_2O排放通量来降低土壤-大豆系统的N_2O排放.UV-B辐射增强显著降低了植株的生物量,并影响到植株的氮代谢和土壤NH_4~+-N与微生物氮.UV-B辐射增强可能会导致农田生态系统N_2O排放量降低.     

增强的UV-B辐射对麦田生态系统中种群数量动态的影响

研究了大田栽培和自然光条件下,模拟UV-B辐射(UV-B,280～315nm)增强对麦田生态系统杂草、大型土壤动物和麦蚜种群数量动态的影响。在UV-B辐射下,杂草和大型土壤动物的种类和数量降低,物种多样性改变,杂草总生物量也降低。UV-B辐射降低麦蚜复合种群数量,并与麦叶粗纤维、可溶性蛋白、可溶性糖、Mg和Zn含量有显著的相关性。UV-B辐射还导致麦蚜与麦叶Mg、Fe和Zn含量均显著增加。     

植物对UV-B辐射的响应与调控机制

UV-B(ultraviolet-B)辐射会在多个方面对植物产生影响,随着研究的不断深入,人们发现UV-B除了作为一个胁迫因子外,还会作为信号调节因子来调节植物的生长发育.本文把UV-B辐射对植物形态建成和生理代谢的影响、植物响应UV-B辐射的信号通路以及UV-B与其他因子复合作用对植物的影响等进行了论述,并对植物响应UV-B辐射的研究做了展望.     

磷影响陆地生态系统碳循环过程及模型表达方法

全球气候变暖已大大改变了陆地植物碳吸收能力, 提高了全球植被净初级生产力。随着气候变暖的加剧, 磷对植物生长的限制作用逐渐显现且不断增强, 磷影响陆地生态系统碳循环的机理和模型研究已成为研究热点。该文系统分析了磷影响陆地生态系统碳循环的相关机理以及模型对相关过程的定量化表达方法。综合对比分析了国际上的Carnegie- Ames-Stanford Approach-CNP (CASA-CNP)、Community Land Model-CNP (CLM-CNP)和Jena Scheme for Biosphere-Atmosphere Coupling in Hamburg-CNP (JSBACH-CNP)等碳、氮、磷耦合模型中磷影响植物光合作用与同化物分配过程、植物对磷的吸收过程、土壤中磷的转化过程以及生态系统磷输入与输出等过程的相关数学表达方法, 指出了模型算法的局限与不确定性以及未来模型发展与改进的方向。同时综合对比分析了CASA-CNP、CLM-CNP、JSBACH-CNP模型的基本特征, 总结了磷循环模型的建模方法, 为未来开展磷影响陆地生态系统碳循环的模型模拟研究提供了借鉴方法与参考思路。     

蓝藻对UV-B增强的响应与适应

平流层臭氧破坏导致地球表面紫外辐射(主要是UV-B)增强逐渐受到人们重视。由于蓝藻在生态系统中的重要性和在生物进化过程中的特殊性,用于研究UV-B对生物体的影响具有诸多优势。目前国内关于UV-B与蓝藻的研究报道较少,所以本文介绍了近年来国外该领域的相关研究,主要包括UV-B对蓝藻生物量、光合机构以及固氮等方面的影响,同时着重介绍了蓝藻对UV-B的适应策略。     

磷影响陆地生态系统碳循环过程及模型表达方法

全球气候变暖已大大改变了陆地植物碳吸收能力,提高了全球植被净初级生产力。随着气候变暖的加剧,磷对植物生长的限制作用逐渐显现且不断增强,磷影响陆地生态系统碳循环的机理和模型研究已成为研究热点。该文系统分析了磷影响陆地生态系统碳循环的相关机理以及模型对相关过程的定量化表达方法。综合对比分析了国际上的CarnegieAmes-Stanford Approach-CNP (CASA-CNP)、Community Land Model-CNP (CLM-CNP)和Jena Scheme for Biosphere-Atmosphere Coupling in Hamburg-CNP (JSBACH-CNP)等碳、氮、磷耦合模型中磷影响植物光合作用与同化物分配过程、植物对磷的吸收过程、土壤中磷的转化过程以及生态系统磷输入与输出等过程的相关数学表达方法,指出了模型算法的局限与不确定性以及未来模型发展与改进的方向。同时综合对比分析了CASA-CNP、CLM-CNP、JSBACH-CNP模型的基本特征,总结了磷循环模型的建模方法,为未来开展磷影响陆地生态系统碳循环的模型模拟研究提供了借鉴方法与参考思路。     

Enhanced UV-B radiation has little effect on growth, δ13C values and pigments of pot-grown rice (Oryza sativa) in the field

Predicted increase in ultraviolet-B (UV-B: 280–320 mn) radiation may have adverse impacts on growth and yield of rice ( Oryza sativa L.), as has been found in studies hitherto. However, most of the studies were conducted in growth chambers or greenhouses where the plants are generally more sensitive to UV-B than in the field, presumably because of the distorted balance between UV-B and ultraviolet-A as well as PAR. This study was conducted to address the effects of enhanced UV-B on growth and yield of rice under a realistic spectral balance in the field. Three cultivars, "Koshihikari",'IR 45'and'IR 74'were pot-grown and irradiated with enhanced UV-B for most of the growing season in the field at Tsukuba, Japan (36°01'N, 140°07'E). The UV-B enhancement simulated ca 38% depletion of stratospheric ozone at Tsukuba. The results showed no UV-B effects on plant height, numbers of tillers and panicles, dry weight of the plant parts or the grain yield for any of the 3 cultivars. Natural abundance of ¹³C in the flag leaves was not altered by the UV-B enhancement either. While UV-absorbing compounds showed no response to the UV-B enhancement, chlorophyll contents decreased with enhanced UV-B. However, the decrease of chlorophyll was limited to an early growth stage with no effect later. We thus found no extraordinary impact of the nearly doubled UV-B radiation on rice in the field, and it would appear that a reliable prediction of the effects of UV-B will require experiments carried out over a number of years under various climatic and solar UV-B regimes.     

UV-B辐射对马尾松凋落叶分解和养分释放的影响

由大气臭氧层减薄导致的UV-B辐射变化将直接影响到凋落物的分解。目前,有关UV-B辐射影响木本植物凋落物分解的研究还很少,在国内还没有开展。采用分解袋法开展了马尾松凋落叶在自然环境和UV-B辐射滤减两种辐射环境下的分解试验。结果表明：在UV-B辐射滤减环境下的马尾松凋落叶年分解速率比对照环境减慢了47.74%。UV-B辐射极显著(p<0.01)地加快了马尾松凋落叶的分解速率,促进了凋落叶中碳、磷、钾的释放和木质素的降解,对氮的释放无明显影响。研究结果意味着UV-B辐射将加快马尾松林的营养循环速度,降低马尾松林凋落物层的碳储量。     

UV-B辐射增强对陆地植物次生代谢的影响

平流层臭氧的减薄已导致地表中波紫外辐射(UV-B,280～320nm)增强,由于UV-B能被许多生物大分子如蛋白质和核酸吸收并引起分子构象的变化,因此可对植物的各方面产生影响。本文将近年来特别是近5年的UV-B辐射增强对植物次生代谢物影响的研究工作进行了综述。主要包括：UV-B辐射增强对植物紫外吸收物的影响和可能的机制;环境因子的复合作用对植物紫外吸收物的影响和可能的机制;UV-B辐射增强对次生代谢物影响的生态学意义。并对该领域未来的研究作了展望。     

紫外线B辐射对几种植物种间竞争的影响

对大田条件下增强的紫外线B(UV-B 280～315nm,约相当于15％臭氧层衰减)对小麦和野燕麦等4个种对的竞争性平衡的影响进行了研究．结果表明,对照和UV-B处理时小麦和野燕麦的密度制约死亡规律没有显著差异,相对较大的竞争压力加强了UV-B对这两个物种生物量降低的效应．UV-B辐射处理后,按单株生物量和地上部生物量。UV-B增强了小麦对野燕麦的竞争优势,但是以单株籽粒数及籽粒重为依据的k1-2值在紫外辐射处理后却下降．竞争性平衡的改变伴随着两者总生物量的显著下降,特别是在较高的密度条件下．紫外辐射对其它3个种对的竞争性平衡有着不同程度与方向上的影响．一般情况下UV-B使竞争性平衡向有利于单子叶植物的方向发展．这一结果暗示,竞争胁迫,特别是种间竞争对正确评估UV-B辐射增强对农田生态系统的影响是至关重要的．     

Effects of climate extremes on the terrestrial carbon cycle: concepts,processes and potential future impacts

Extreme droughts, heat waves, frosts, precipitation, wind storms and other climate extremes may impact the structure, composition and functioning of terrestrial ecosystems, and thus carbon cycling and its feedbacks to the climate system. Yet, the interconnected avenues through which climate extremes drive ecological and physiological processes and alter the carbon balance are poorly understood. Here, we review the literature on carbon cycle relevant responses of ecosystems to extreme climatic events. Given that impacts of climate extremes are considered disturbances, we assume the respective general disturbance‐induced mechanisms and processes to also operate in an extreme context. The paucity of well‐defined studies currently renders a quantitative meta‐analysis impossible, but permits us to develop a deductive framework for identifying the main mechanisms (and coupling thereof) through which climate extremes may act on the carbon cycle. We find that ecosystem responses can exceed the duration of the climate impacts via lagged effects on the carbon cycle. The expected regional impacts of future climate extremes will depend on changes in the probability and severity of their occurrence, on the compound effects and timing of different climate extremes, and on the vulnerability of each land‐cover type modulated by management. Although processes and sensitivities differ among biomes, based on expert opinion, we expect forests to exhibit the largest net effect of extremes due to their large carbon pools and fluxes, potentially large indirect and lagged impacts, and long recovery time to regain previous stocks. At the global scale, we presume that droughts have the strongest and most widespread effects on terrestrial carbon cycling. Comparing impacts of climate extremes identified via remote sensing vs. ground‐based observational case studies reveals that many regions in the (sub‐)tropics are understudied. Hence, regional investigations are needed to allow a global upscaling of the impacts of climate extremes on global carbon–climate feedbacks.     

Evaluation of global warming impacts on the carbon budget of terrestrial ecosystems in monsoon Asia: a multi-model analysis

This study assesses the potential impacts of future global warming on the carbon budget of terrestrial ecosystems across monsoon Asia using the Inter-Sectoral Impact Model Intercomparison Project (ISI-MIP) dataset. We used simulation results of two emission pathways (RCP2.6 and RCP8.5), climate projections of five climate models, and seven terrestrial biome models to analyze the changes in net primary production and carbon stocks in the South, Southeast, and East Asian subregions during the period 1981–2099. The simulations indicated that by the end of the 21st century, net primary production would increase by 9–45 % and ecosystem carbon storage would increase by 42–86 Pg C. The clearest climatic impacts were found when using the adaptation-oriented emission scenario (RCP8.5), which assumes a greater CO₂ increase and a larger change in climatic conditions. Substantial disparities in temporal trajectories and spatial patterns were found in the estimated changes, owing to the uncertainties in the emission scenarios, climate projections, and ecosystem models. We attempted to derive consistent patterns throughout the simulations to specify potential hotspots of climatic impacts (e.g., soil carbon change in the southern Tibetan Plateau). Finally, we discuss changes to the climatic characteristics in the study region (e.g., a change in the rainy season), the implications for ecosystem services, and the need for collaborative field monitoring studies.     

陆地生态系统碳汇评估方法研究进展

“碳中和”是我国作出的一项重大的国家战略决策,陆地生态系统碳汇作为碳增汇的重要组成部分,在碳中和目标实现的过程中发挥着重要的作用。但当前基于不同观测数据和方法的陆地碳汇计算仍有很大的不确定性,为了全面了解陆地生态系统碳汇分布特征,提高陆地生态系统碳汇评估的准确性,梳理了近年来关于陆地生态系统碳汇评估的国内外研究进展,从“自下而上”和“自上而下”两类途径阐述了陆地生态系统碳汇评估的主要方法(样地清查法、涡度相关法、模型模拟法和碳同化反演法)的主要原理和特征,优势和缺陷,及在不同尺度碳汇研究中的应用,并从土地利用/覆盖变化、气候因素(大气CO₂浓度、氮沉降)、环境因素(太阳辐射、温度、降水)等因素阐述了陆地系统碳汇主要驱动因子;分析了我国陆地生态系统碳汇的主要特征及时空变化趋势,并从人类活动(生态工程)和环境因素阐述了中国陆地生态系统碳汇的驱动因素;最后,展望了新的监测手段和评估方法在提升陆地生态系统碳汇评估精度中的作用,从而更好的服务于我国“碳中和”的长远目标。     

Boreal peatland ecosystems under enhanced UV-B radiation and elevated tropospheric ozone concentration

Boreal peat-forming wetlands, mires, are globally important sources of methane and sinks for CO₂. As peatland vegetation plays a significant role regulating the exchange of these greenhouse gases, we have assessed the responses of the dominant plants and ecosystem functions to increasing tropospheric ozone concentration and enhanced ultraviolet-B (UV-B) radiation in long-term experiments, the results of which are summarized in this review. The dominant sedge, Eriophorum vaginatum, and especially the Sphagnum mosses common on peatlands, appear fairly tolerant to the future predicted ozone levels. Similarly, UV-B radiation only caused few alterations in the carbohydrates and pigments of the dominant sedge, Eriophorum russeolum, and had no effects on the dominant moss species of the experimental site, Warnstorfia exannulata. Surprisingly, there were alterations in organic acid concentrations in the peat pore water and peat microbial community composition in both experiments. Elevated ozone caused a transient decrease in ecosystem-level gross photosynthesis and methane (CH₄) emission, which shifted to a slight increase later on. Enhanced UV-B decreased dark ecosystem respiration and increased CH₄ emission in the course of the six measurement years. The emission of isoprene was increased by both ozone and UV-B during warm weather periods, suggesting interactive effects with temperature. All in all, we suggest that ozone and UV-B have limited effects on the carbon cycle in boreal peatlands, because other environmental factors, such as temperature, water level and photosynthetically active radiation more strongly regulate CO₂ and CH₄ exchange rates.