环梅山岛海域春季浮游古菌群落空间分布特征研究

【目的】海洋浮游古菌是生物地球化学循环的关键驱动者,但其在近岸海域的水平空间分布特征还未被充分了解。本研究以与陆地紧密相连的环梅山岛海域为例研究浮游古菌在海陆过渡带的水平分布模式。【方法】利用16S rRNA基因扩增子测序,以期从优势类群分布、群落组成变化和物种共现模式3个层面揭示梅山湾潟湖区和临近海域春季浮游古菌的空间分布特征。【结果】该海域浮游古菌在原核生物群落中的相对丰度为0.6%–26.5%,向海侧古菌丰度显著高于潟湖区。浮游古菌群落由奇古菌门Marine Group(MG)I和广古菌门MGII主导,MGI的物种组成较为单一,而MGII的系统发育多样性较高。古菌群落的空间分布受同质扩散、环境选择和非主导过程(包括生态漂变)的共同塑造,其中环境选择主要由悬浮颗粒物、硝酸盐、溶解氧、水温和铵盐驱动。通过网络分析发现MGI与红杆菌科细菌呈广泛的负相关,MGII则普遍与SAR11、SAR116和SAR86等异养细菌类群呈正相关。【结论】本研究初步揭示了环梅山岛海域春季浮游古菌群落的空间分布特征及其调控因子,拓展了对古菌在海陆过渡带分布规律的认识。     

引物应用策略：基于2对古菌16S rRNA基因通用引物对环境样品古菌多样性分析

【目的】找到适宜的16S rRNA基因通用引物应用策略,应对复杂环境微生物多样性调查,尤其目前高速发展的高通量测序技术带来的巨大挑战。【方法】用Oligocheck软件分别将两对应试的古菌16S rRNA基因通用引物与RDP(Ribosomal database project)数据库中古菌16S rRNA基因序列进行匹配比对。用两对应试引物分别构建海洋沉积物样品的古菌16S rRNA基因文库。【结果】软件匹配结果显示引物f109/r958与目的基因的匹配程度高于引物f21/r958。该结果与古菌16S rRNA基因文库RFLP分析、古菌多样性指数分析结果相吻合。数据还表明,2对引物的综合文库能更好满足该沉积物样品的古菌多样性分析。【结论】选用与数据库中目的基因匹配性高的通用引物和多个引物的联合使用,可以有效提高环境样品微生物多样性调查的分辨率。     

从宏基因组推测扎龙湿地未培养甲烷古菌Rice Cluster II的代谢途径与可能的盐碱适应性

【背景】湿地是重要的甲烷排放源,因为其中栖息着各种产甲烷古菌。已知未培养甲烷古菌Rice Cluster Ⅱ (RCⅡ)类群广泛分布于低温酸性和北方泥炭藓湿地、淡水湿地及草本沼泽等环境,但它们在低温盐碱湿地中的分布及代谢途径尚未知。【目的】分析扎龙盐碱湿地未培养甲烷古菌RCⅡ类群的多样性、推测产甲烷代谢途径及其潜在的盐碱适应机制。【方法】16S rRNA基因扩增子测序分析扎龙湿地土壤中甲烷古菌群组成;构建16S rRNA基因克隆文库分析扎龙湿地土壤RCⅡ的多样性;宏基因组分析推测RCⅡ古菌编码的产甲烷途径及与耐盐碱相关物质的合成基因。【结果】16SrRNA基因高通量测序发现未培养甲烷古菌的RCⅡ类群占扎龙盐碱湿地总甲烷古菌的13.280%±0.019%;系统发育学分析表明该湿地的RCⅡ由3个分支组成;宏基因组分析组装了2个优势的未培养RCⅡ的基因组,均含完整的氢还原二氧化碳产甲烷途径的基因,并编码海藻糖的转运与合成基因。【结论】扎龙盐碱湿地土壤富含未培养RCⅡ甲烷古菌,推测它们通过氢还原二氧化碳产甲烷,利用细胞内高的海藻糖适应盐碱环境。     

SMRT测序技术及其在微生物研究中的应用

高通量测序技术的发展为研究者深入探索微生物世界提供可能。随着以Pacific Bio Sciences(PacBio)公司的单分子实时测序(Single molecule real time sequencing,SMRT)为代表的第三代测序(Third generation sequencing,TGS)技术逐渐发展成熟,微生物研究方法正面临又一次新的变革。SMRT测序技术凭借其特殊建库方式(SMRTbell)和超长的测序读长等特点,为微生物16S rRNA基因全长测序提供新的选择。同时,为组装完整可靠的宏基因组和微生物全基因组提供新方法。随着PacBio测序平台的成本大幅下降,SMRT测序技术的PacBio系列平台开始逐渐被应用于微生物16S rRNA基因测序、宏基因组测序和全基因组测序研究中。综述了SMRT测序技术的技术原理和特点及其在微生物16S rRNA基因全长测序、宏基因组测序等方面的应用,并分析了目前SMRT测序技术在微生物各方面研究中的优势和存在的问题,提出基于SMRT测序技术获得的长片段在后期分析中存在的问题。SMRT测序技术将越来越多地引入到微生物研究中,期望为将要选择使用SMRT测序技术研究微生物的研究人员提供一定参考。     

呼和浩特市周边地下水CPR和DPANN类群的检测及多样性分析

【背景】候选门级辐射类群(candidate phyla radiation, CPR)和DPANN是与绝大多数已知细菌和古菌具有显著差异的独特类群，因发现较晚，人们对其认识还非常有限。已知二者类群庞大、存在广泛，但在不同生境中的多样性研究还较少，生态功能尚属未知。【目的】分析不同地下水中CPR和DPANN的多样性，探讨不同方法对CPR和DPANN检出及富集的影响。【方法】采用0.1μm滤膜收集菌体和宏基因组测序的方法分析呼和浩特市周边4个不同地下水中CPR和DPANN的多样性。比较宏基因组测序与16S rRNA基因扩增子测序对CPR和DPANN检出的影响，以及不同过滤方式和不同滤膜组合对CPR和DPANN富集的作用。【结果】4个地下水样品CPR类群检出33-64个菌门，相对丰度在0.17%-1.67%之间；DPANN检出1-7个菌门，相对丰度在0.00093%-0.07100%之间。对于CPR和DPANN,16SrRNA基因V3-V4区扩增子测序仅检出了纳古菌门(Nanoarchaeota)。1.2μm与0.1μm滤膜组合具有最好的CPR和DPANN富集效果，在及时更换滤膜的过滤方式...     

西藏米拉山土壤古菌16S rRNA及amoA基因多样性?分析

摘要：【目的】硝化作用在全球土壤氮循环中具有重要的作用,虽然细菌一度被认为单独负责催化这个过程的限速步骤,但是最近一些研究结果表明泉古菌具有氨氧化的能力。本文通过构建古菌16S rRNA 基因克隆文库和氨氧化古菌amoA基因文库,分析西藏米拉山高寒草甸土壤中古菌及氨氧化古菌群落结构组成情况,为揭示青藏高原高寒草甸土壤古菌的多样性提供理论基础。【方法】采用未培养技术直接从土壤中提取微生物总DNA,分别利用通用引物构建古菌16S rRNA 基因和氨氧化古菌amoA基因克隆文库。【结果】通过构建系统发育树,表明古菌16S rRNA 基因克隆文库包括泉古菌门和未分类的古菌两大类,并且所有泉古菌均属于热变形菌纲。氨氧化古菌amoA基因克隆文库中序列均为泉古菌。通过DOTUR软件分析,古菌16S rRNA基因和古菌amoA基因克隆文库分别包括64个OTUs和 75个OTUs。【结论】西藏米拉山高寒草甸土壤中古菌多样性比较丰富,表明古菌在高寒草甸土壤的氮循环中可能具有重要的作用。所获得的一些序列与已知环境中土壤、淡水及海洋沉积物中获得的一些序列具有很高的相似性,其古菌及氨氧化古菌来自不同环境的可能性比较大,可能与青藏高原的地质历史变迁过程有关。米拉山古菌及氨氧化古菌与陆地设施土壤中相似性最高,说明与西藏米拉山高寒草甸土壤的退化有关。     

基于不同通用引物比较分析肠道微生物群落变化

肠道微生物对于人体健康的重要作用已经得到广泛证实,目前,对肠道微生物的研究大多采用基于扩增细菌16S rRNA基因V3-V4区的高通量测序分析,对古菌的关注较少。本研究选择了一对可以同时扩增细菌和古菌16S rRNA基因的引物,通过比较人为干扰肠道微生物前后的群落变化,说明这对引物适宜分析人类肠道细菌和古菌群落变化并具有一定优越性。采集志愿者粪便样品,同时用仅能扩增细菌引物 (B引物) 和细菌古菌通用引物 (AB引物) 进行扩增和高通量测序;使用几个常用的rRNA数据库判断引物对细菌的覆盖度和对古菌的扩增能力。结果表明,AB引物在可以展示B引物扩增出的细菌群落的基础上,可以得到肠道中常见的产甲烷古菌的序列,同时也展示出人为干扰肠道微生物前后的群落结构变化。AB引物可以仅通过一次扩增和测序同时分析肠道中的细菌和古菌群落,更加全面展示肠道微生物群落结构,适用于肠道微生物相关研究。     

几种农田土壤中古菌、泉古菌和细菌的数量分布特征

真核生物、细菌和古菌三者共同构成了生命的三域系统.古菌作为第3种生命形式,不仅能在高温、强酸和高盐等极端环境下生存,而且在海洋、湖泊和土壤等生境中也广泛分布,预示其在整个生态系统中有着不可估量的作用.本文以2个农田剖面土壤和2个长期施肥试验站祁阳(QY)和封丘(FQ)的土壤为对象,以实时定量PCR方法为主要研究手段,对土壤中古菌(包括泉古菌)和细菌的16S rRNA基因拷贝数丰度变化进行了研究.结果表明:土壤泉古菌16S rRNA基因拷贝数要低于古菌l～2个数量级,两者与细菌相比,16S rRNA基因拷贝数大小顺序为土壤泉古菌＜古茵＜细菌,而古菌和泉古菌16S rRNA基因拷贝数与细菌的比值均随土壤深度加深而增大.不同施肥处理对土壤古菌和泉古茵的数量有显著影响.QY试验站土壤古菌和细菌的数量与土壤pH值显著相关(分别为r=0.850,P＜0.01和r=0.676,P＜0.05).FQ古菌、泉古菌和细菌与土壤pH值相关性不显著,与土壤有机质含量相关性均达显著水平(分别为r=0.783,P＜0.05;r=0.827,P＜0.05;r=0.767,P＜0.05).了解古菌包括泉古菌在农田土壤中的分布,可为评价其在生态系统和物质循环中的作用提供重要的理论依据.     

高温菌16S rRNA与耐热性关系的初步研究

通过对80多种超高温菌的基因组G＋C含量,16S rRNA G＋C含量进行统计分析,结果显示高温菌耐热性与基因组G＋C含量之间没有直接关系,而与16S rRNA G＋C含量之间明显存在上正相关。16S rRNA 18 helix的二级结构分析显示高温菌生长温度越高,其16S rRNA热稳定性越高。     

珠江口外东澳岛海域MG I古菌和藻类的昼夜变化关系的研究

【目的】海洋古菌MG I (marine group I archaea)是海洋中主要微生物类群,拥有利用氨氮进行氨氧化自养的能力,是海洋环境中氨氧化过程的重要参与者。研究MG I古菌的昼夜变化规律,对揭示海洋中氨氧化过程以及碳氮循环有着重要的意义。【方法】此次研究的样品来自于珠江口东澳岛附近海域,使用无人机采样技术获取了以2 h为间隔的22 h连续时间序列海水样品。本研究重点关注以下科学问题：(1)昼夜尺度下珠江口MG I古菌与藻类的群落和丰度变化特征;(2)昼夜尺度下珠江口MG I古菌受温度和藻类的影响。本研究通过样品DNA,以qPCR、二代基因测序等手段,结合环境参数(温度、盐度、营养盐浓度等),以探究海水藻类与MG I古菌之间可能存在的关系。【结果】研究发现,MG I古菌丰度为(9.1±3.2)×107 copies/L,藻类的丰度为(3.7±0.7)×108 copies/L。通过古菌的高通量测序发现MG I古菌是该区域最主要的古菌类群(36.2%–50.0%)。在昼夜变化尺度下,MG I古菌与藻类的丰度表现出一定的负相关关系,且环境因子中,温度与MG I古菌之间表现出显著的...     

湿地微生物介导的甲烷排放机制

湿地生态系统是陆地上巨大的有机碳库,同时也是大气中甲烷(CH_4)的主要排放源。由于CH_4对全球的增温潜能是CO2的34倍,因此关于湿地CH_4排放在全球气候变化中有关碳汇、碳源的研究具有极其重要的意义。全球80%–90%的CH_4排放离不开微生物活动,湿地生态系统中产CH_4菌和CH_4氧化菌的种类组成、数量及功能与CH_4通量密切相关,但基于湿地生态系统中介导CH_4循环的功能微生物对甲烷排放通量的影响及作用机制研究相对比较分散。为更好地认识微生物介导的CH_4排放过程的微生物调控机制,本文综述了湿地生态系统中参与CH_4循环的功能微生物,对介导CH_4循环相关微生物活性的影响因子进行了回顾,重点总结了湿地生态系统微生物介导的CH_4排放机制,并对未来的相关研究方向进行了展望。由于湿地微生物介导的碳循环过程也可能决定了湿地生态系统对全球气候变暖的反馈,因此本文也能为全球气候变化研究提供微生物方面的参考。     

Global warming triggers the loss of a key Arctic refugium

We document the rapid transformation of one of the Earth''s last remaining Arctic refugia, a change that is being driven by global warming. In stark contrast to the amplified warming observed throughout much of the Arctic, the Hudson Bay Lowlands (HBL) of subarctic Canada has maintained cool temperatures, largely due to the counteracting effects of persistent sea ice. However, since the mid-1990s, climate of the HBL has passed a tipping point, the pace and magnitude of which is exceptional even by Arctic standards, exceeding the range of regional long-term variability. Using high-resolution, palaeolimnological records of algal remains in dated lake sediment cores, we report that, within this short period of intense warming, striking biological changes have occurred in the region''s freshwater ecosystems. The delayed and intense warming in this remote region provides a natural observatory for testing ecosystem resilience under a rapidly changing climate, in the absence of direct anthropogenic influences. The environmental repercussions of this climate change are of global significance, influencing the huge store of carbon in the region''s extensive peatlands, the world''s southern-most polar bear population that depends upon Hudson Bay sea ice and permafrost for survival, and native communities who rely on this landscape for sustenance.     

土壤微生物对气候变暖和大气N沉降的响应

气候变暖和大气N沉降是近一、二十年来人们非常关注的全球变化现象,它们所带来的一系列生态问题已成为全球变化研究的重要议题。它们不仅影响地上植被生长和群落组成,还直接或间接地影响土壤微生物过程,而土壤微生物对此做出的响应正是生态系统反馈过程中非常重要的环节。该文分别从气候变化对土壤微生物的影响(土壤微生物量、微生物活动和微生物群落结构)和土壤微生物对气候变化的响应(凋落物分解、养分利用与循环以及养分的固持与流失)两个角度,综述近期土壤微生物对气候变暖和大气N沉降响应与适应的研究进展。气候变暖和大气N沉降对土壤微生物的影响更多地反映在微生物群落的结构和功能上,而土壤微生物量、微生物活动和群落结构的变化又会通过改变凋落物分解、养分利用和C、N循环等重要的土壤生态系统功能和过程做出响应,形成正向或负向反馈,加强或削弱气候变化给整个陆地生态系统带来的影响。然而,到目前为止土壤微生物的响应对陆地生态系统产生的最终结果仍是未决的关键性问题。     

微生物驱动的滨海湿地N2O产生及其机制研究进展

滨海湿地位于海陆交界,具有初级生产力高、生物多样性丰富以及微生物驱动的营养元素循环活跃等特点,同时也是大气中一氧化二氮(N_2O)的重要排放源。N_2O是仅次于二氧化碳(CO2)和甲烷(CH4)的第三大温室气体,而全球90%以上的N_2O排放由微生物主导,并与滨海湿地氮循环的微生物群落多样性及功能密切相关。因此,滨海湿地系统中N_2O的产生与转化逐渐受到关注。本文综述了滨海湿地生态系统中微生物驱动下N_2O的产生过程,以及氮元素及其与碳、硫和金属元素耦合过程中产生N_2O的代谢途径,N_2O排放的时空变化与微生物调控,并对未来相关研究方向进行了展望,旨在揭示微生物驱动的N_2O产生及环境调控机制,为减缓全球变暖提供科学依据。     

Elevated nutrient inputs to marshes differentially impact carbon and nitrogen cycling in two northern Gulf of Mexico saltmarsh plants

Peatlands have accumulated vast quantities of organic carbon over thousands of years but it is unclear how these sensitive ecosystems will respond to future climate change. If emissions of methane from peatlands increase, then they may contribute increasingly towards climatic warming due to the higher greenhouse warming potential of this gas. We investigated the radiocarbon concentration of methane emissions from a temperate bog over 1.5 years, which we supported with measurements of the surface flux of methane and carbon dioxide. The radiocarbon content of methane emissions varied greatly, from modern (i.e. fixed from the atmosphere within recent decades) to ~ 1400 years BP. Flux rates of methane were spatially and temporally highly variable. A vegetation clipping experiment showed that plants had a great influence on the carbon isotope composition and flux of methane emitted from the peat surface, consistent with earlier studies showing the key role of plants in peatland methane emissions. When plants were absent, emission rates were 70–94% lower and the radiocarbon age of methane emissions was much younger and less variable. Our radiocarbon measurements show that at this peatland, plant-associated methane emissions contain carbon originally fixed from the atmosphere up to hundreds of years earlier, consistent with a contribution from plant mediated transport of methane sourced from sub-surface layers.

     

基于替代式自下而上法的区域旅游交通碳排放测度

区域旅游交通碳排放测度是分解旅游业减碳任务的一个难题。在剖析替代式自下而上法机理的基础上,以长三角为例,依托归纳法和变异系数法,尝试从人均GDP、人均消费水平和人均运输线路长度三方面测算出游距离,采取以实地调研数据为主、辅之以Mus TT模型法拟定各旅游交通方式的距离比例,立足区情确定碳排放系数,并以区域输入和输出的双向旅游流的人次比值法则对替代结果进行还原调整。研究表明:(1)2011年,长三角旅游交通碳排放总量为8.32 Mt,其中江苏省、浙江省和上海市分别为3.23、2.98 Mt和2.11 Mt;(2)飞机和自驾车共占排放量的71.64%,较明显低于世界平均比例,二者是降低旅游交通碳排放的关键;旅游公共交通的碳排放比例具有远高于发达国家甚至全球平均水平的"中国式"烙印;由高碳排放系数的旅游交通方式向低碳排放系数甚至零碳排放系数的转变,是旅游交通减排的基本方向。     

Coping with Commitment: Projected Thermal Stress on Coral Reefs under Different Future Scenarios

Background

Periods of anomalously warm ocean temperatures can lead to mass coral bleaching. Past studies have concluded that anthropogenic climate change may rapidly increase the frequency of these thermal stress events, leading to declines in coral cover, shifts in the composition of corals and other reef-dwelling organisms, and stress on the human populations who depend on coral reef ecosystems for food, income and shoreline protection. The ability of greenhouse gas mitigation to alter the near-term forecast for coral reefs is limited by the time lag between greenhouse gas emissions and the physical climate response.

Methodology/Principal Findings

This study uses observed sea surface temperatures and the results of global climate model forced with five different future emissions scenarios to evaluate the “committed warming” for coral reefs worldwide. The results show that the physical warming commitment from current accumulation of greenhouse gases in the atmosphere could cause over half of the world''s coral reefs to experience harmfully frequent (p≥0.2 year⁻¹) thermal stress by 2080. An additional “societal” warming commitment, caused by the time required to shift from a business-as-usual emissions trajectory to a 550 ppm CO₂ stabilization trajectory, may cause over 80% of the world''s coral reefs to experience harmfully frequent events by 2030. Thermal adaptation of 1.5°C would delay the thermal stress forecast by 50–80 years.

Conclusions/Significance

The results suggest that adaptation – via biological mechanisms, coral community shifts and/or management interventions – could provide time to change the trajectory of greenhouse gas emissions and possibly avoid the recurrence of harmfully frequent events at the majority (97%) of the world''s coral reefs this century. Without any thermal adaptation, atmospheric CO₂ concentrations may need to be stabilized below current levels to avoid the degradation of coral reef ecosystems from frequent thermal stress events.     

Sensitivity of mangrove soil organic matter decay to warming and sea level change

Mangroves are among the world's most carbon‐dense ecosystems, but they are threatened by rapid climate change and rising sea levels. The accumulation and decomposition of soil organic matter (SOM) are closely tied to mangroves' carbon sink functions and resistance to rising sea levels. However, few studies have investigated the response of mangrove SOM dynamics to likely future environmental conditions. We quantified how mangrove SOM decay is affected by predicted global warming (+4°C), sea level changes (simulated by altering of the inundation duration to 0, 2, and 6 hr/day), and their interaction. Whilst changes in inundation duration between 2 and 6 hr/day did not affect SOM decay, the treatment without inundation led to a 60% increase. A warming of 4°C caused SOM decay to increase by 21%, but longer inundation moderated this temperature‐driven increase. Our results indicate that (a) sea level rise is unlikely to decrease the SOM decay rate, suggesting that previous mangrove elevation gain, which has allowed mangroves to persist in areas of sea level rise, might result from changes in root production and/or mineral sedimentation; (b) sea level fall events, predicted to double in frequency and area, will cause periods of intensified SOM decay; (c) changing tidal regimes in mangroves due to sea level rise might attenuate increases in SOM decay caused by global warming. Our results have important implications for forecasting mangrove carbon dynamics and the persistence of mangroves and other coastal wetlands under future scenarios of climate change.     

Temperature and snowfall trigger alpine vegetation green‐up on the world's roof

Rapid temperature increase and its impacts on alpine ecosystems in the Qinghai–Tibetan Plateau, the world's highest and largest plateau, are a matter of global concern. Satellite observations have revealed distinctly different trend changes and contradicting temperature responses of vegetation green‐up dates, leading to broad debate about the Plateau's spring phenology and its climatic attribution. Large uncertainties in remote‐sensing estimates of phenology significantly limit efforts to predict the impacts of climate change on vegetation growth and carbon balance in the Qinghai–Tibetan Plateau, which are further exacerbated by a lack of detailed ground observation calibration. Here, we revealed the spatiotemporal variations and climate drivers of ground‐based herbaceous plant green‐up dates using 72 green‐up datasets for 22 herbaceous plant species at 23 phenological stations, and corresponding daily mean air temperature and daily precipitation data from 19 climate stations across eastern and southern parts of the Qinghai–Tibetan Plateau from 1981 to 2011. Results show that neither the continuously advancing trend from 1982 to 2011, nor a turning point in the mid to late 1990s as reported by remote‐sensing studies can be verified by most of the green‐up time series, and no robust evidence for a warmer winter‐induced later green‐up dates can be detected. Thus, chilling requirements may not be an important driver influencing green‐up responses to spring warming. Moreover, temperature‐only control of green‐up dates appears mainly at stations with relatively scarce preseason snowfall and lower elevation, while coupled temperature and precipitation controls of green‐up dates occur mostly at stations with relatively abundant preseason snowfall and higher elevation. The diversified interactions between snowfall and temperature during late winter to early spring likely determine the spatiotemporal variations of green‐up dates. Therefore, prediction of vegetation growth and carbon balance responses to global climate change on the world's roof should integrate both temperature and snowfall variations.     

中国陆地生态系统碳源/汇整合分析

国家尺度陆地生态系统碳收支及其循环过程的研究对于提升地球系统科学与全球变化科学的科技创新能力、提高我国参与应对全球气候变化国际行动和维护国家利益的话语权、保障国家生态安全和改进生态系统管理都具有重要意义。近年来,我国已经在气候变化与陆地生态系统碳循环领域开展了大量的研究工作,主要包括国家清查、生态系统模型模拟、大气反演等手段。然而,由于大尺度陆地生态系统碳源/汇的估算存在很大的不确定性,目前尚未形成国家尺度的陆地生态系统碳源/汇的整合分析。通过搜集已发表的关于中国陆地生态系统及其组分碳源/汇的59篇文献,整合国家清查、生态系统模型模拟、大气反演3种研究手段,分析中国陆地生态系统碳源/汇大小以及时间尺度上的动态变化。结果表明,在1960s-2010s期间中国陆地生态系统碳汇整体呈上升趋势,平均为（0.213±0.030）Pg C/a,其中森林、草地、农田和灌木生态系统碳汇分别为（0.101±0.023）Pg C/a、（0.032±0.007）Pg C/a、（0.043±0.010）Pg C/a和（0.028±0.010）Pg C/a。森林生态系统中的植被碳汇远大于土壤碳汇,然而这种格局在草地和农田生态系统却相反,而且1960s-2010s期间中国主要植被类型的生态系统碳汇总体上随时间呈增加趋势。融合多源数据（地面观测、激光雷达、卫星遥感等）、多尺度数据（样地尺度、站点尺度、区域尺度）以及多手段数据（联网观测、森林清查、模型模拟）,有助于全面准确地评估中国陆地生态系统碳源/汇及其对气候变化的响应。