福建省土地利用碳排放空间关联性与碳平衡分区

全球变暖与二氧化碳浓度升高密不可分，在工业化及城镇化发展过程中，人类对土地的利用和改造是造成全球大气中含碳量迅速增加的重要原因，且土地在利用过程中碳减排的潜力较大。因此，从不同土地利用方式视角研究福建省碳排放量，采用基尼系数来衡量福建省各设区市碳收支的空间差异，探索区域内土地利用碳收支规模和空间分异；运用社会网络分析方法对福建省土地利用碳排放空间网络结构的整体特征和设区市在网络结构中的角色进行考察，有助于从基础层面对人类活动所造成的环境影响进行评估，及时调整土地利用方式从而促进低碳经济发展。结果表明：2006-2018年福建省土地利用净碳排放量逐年递增，呈现东高西低的空间分布特征，建设用地是主要碳源，而林地起到主要碳汇的作用；区域内碳补偿率逐年递减且存在明显的空间差异，经济较发达的区域碳补偿率低于经济欠发达的区域，生态承载系数东西差距不断加强，东部地区碳排放的比例明显超过了碳吸收的比例；福建省土地利用碳排放在空间上具有明显的关联性和溢出效应，碳排放空间关联网络越来越复杂、稳定，各设区市在网络中所处地位和作用存在明显的不均衡性，厦门市在整个碳排放网络中占据领导地位，其他城市的碳影响力在网络中的地位及作用随着经济联系逐渐加强正在逐步提高；对网络空间聚类发现，第一模块和第三模块对模块内外均有溢出效应且密度值较大，属于"双向溢出模块"，其余第二、四模块均属于"净收益模块"。在研究的基础上将福建省各设区市分为3类区域：低碳优化区、碳总量控制区和碳汇功能区，并提出协同减排的差异性对策建议。     

Synergetic utilization of glucose and glycerol for efficient myo-inositol biosynthesis

myo-Inositol (MI) as a dietary supplement can provide various health benefits. One major challenge to its efficient biosynthesis is to achieve proper distribution of carbon flux between growth and production. Herein, this challenge was overcome by synergetic utilization of glucose and glycerol. Specifically, glycerol was catabolized to support cell growth while glucose was conserved as the building block for MI production. Growth and production were coupled via the phosphotransferase system, and both modules were optimized to achieve efficient production. First, the optimal enzyme combination was established for the production module. It was observed that enhancing the production module resulted in both increased MI production and better cell growth. In addition, glucose was shown to inhibit glycerol utilization via carbon catabolite repression and the inhibition was released by over-expressing glycerol kinase. Furthermore, the inducible promoter was replaced by strong constitutive promoters to avoid inducer use. With these efforts, the final strain produced MI with both high titer and yield. In fed-batch cultivation, 76 g/L of MI was produced, showing scale-up potential. This study provides a promising strategy to achieve rational distribution of carbon flux.     

Carbon emissions performance of commercial logging in East Kalimantan,Indonesia

Adoption of reduced‐impact logging (RIL) methods could reduce CO₂ emissions by 30–50% across at least 20% of remaining tropical forests. We developed two cost effective and robust indices for comparing the climate benefits (reduced CO₂ emissions) due to RIL. The indices correct for variability in the volume of commercial timber among concessions. We determined that a correction for variability in terrain slope was not needed. We found that concessions certified by the Forest Stewardship Council (FSC, N = 3), when compared with noncertified concessions (N = 6), did not have lower overall CO₂ emissions from logging activity (felling, skidding, and hauling). On the other hand, FSC certified concessions did have lower emissions from one type of logging impact (skidding), and we found evidence of a range of improved practices using other field metrics. One explanation of these results may be that FSC criteria and indicators, and associated RIL practices, were not designed to achieve overall emissions reductions. Also, commonly used field metrics are not reliable proxies for overall logging emissions performance. Furthermore, the simple distinction between certified and noncertified concessions does not fully represent the complex history of investments in improved logging practices. To clarify the relationship between RIL and emissions reductions, we propose the more explicit term ‘RIL‐C’ to refer to the subset of RIL practices that can be defined by quantified thresholds and that result in measurable emissions reductions. If tropical forest certification is to be linked with CO₂ emissions reductions, certification standards need to explicitly require RIL‐C practices.     

内蒙古大青山华北落叶松人工林乔木层碳密度年增量与气象因子的关系

以内蒙古大青山华北落叶松人工林为研究对象，通过树木年轮法和异速生长方程法，计算华北落叶松人工林生物量、碳密度及其年增量的年际变化，并分析碳密度年增量与气温、降水、湿度等气象因子的关系。研究发现：华北落叶松人工林碳密度随着林龄增加的变化曲线可用逻辑斯谛生长方程拟合，在1979—2016年，碳密度由1.05 t/hm~2增加到76.83 t/hm~2。华北落叶松人工林碳密度年增量存在显著的年际差异，总体上呈波动性的“慢-快-慢”趋势，碳密度年增量最高达到3.72 t hm^-2 a^-1,多年平均为2.05 t hm^-2 a^-1。华北落叶松人工林碳密度年增量与上年6月和当年6—8月的降水量显著正相关，与上年11月降水显著负相关；与上年11—12月、当年2月和12月的温度和大气相对湿度分别呈正、负相关；与上年7月、9月及当年8—9月的温度保持显著或极显著正相关。研究表明，温度、湿度和降水主要通过生长季的长短和土壤可利用水分及冬季的雪害冻害影响华北落叶松人工林的碳汇潜力，在未来该地区升温增湿的气候变化趋势下华北...     

长江经济带林地和其他生物质碳储量及碳汇量研究

以全国林业应对气候变化碳汇计量监测体系建设结果数据为基础，应用森林碳库专项调查建立的碳计量模型和参数，结合历次森林资源清查成果等数据，估算了2020年长江经济带林地和其他生物质碳储量和碳汇量。研究表明：（1）2020年长江经济带林地碳储量24543.58 Tg C （其中森林植被碳储量为4372.85Tg C），散生木和四旁树等其他生物质碳储量329.59 Tg C。2020年长江经济带林地碳汇量81.81 Tg C/a （300.26Tg CO₂/a）、散生木和四旁树等其他生物质碳汇量6.60 Tg C/a （24.21 Tg CO₂/a）。无论是林地和其他生物质碳储量、碳汇量、还是森林植被碳储量，乔木林地所占比例最大（69%-85%）；长江经济带11个省市中，云南省最大，上海市最小；林地碳储量中土壤有机质碳库贡献最大（81.46%），林地碳汇量中生物量碳库贡献最大（90.99%）；林地碳汇量中"一直为林地的土地"产生碳汇量贡献最大（71.74%），其中一直为乔木林的土地产生的碳汇量占69.89%；（2）阐述了长江防护林工程、天然林资源保护工程、珠江防护林工程和沿海防护林工程4大重点生态工程对长江经济带碳储量和碳汇量的贡献，长江防护林工程贡献率最大（81%-83%），其次是天然林资源保护工程（32%-38%），珠江防护林工程和沿海防护林工程影响较小。分析了人工造林、中幼林抚育、次生林和低效林改造、退化林修复等生态保护修复措施对长江经济带碳储量和碳汇量的贡献，并提出了碳中和愿景下森林固碳增汇的有效途径。     

接种丛枝菌根真菌对云南石漠化土壤呼吸的影响

为探明"丛枝菌根（Arbuscular mycorrhiza，AM）真菌-植物-土壤"耦合作用对石漠化土壤呼吸季节动态的影响，采用LI-6400-09土壤呼吸室和便携式光合作用测量系统，对圆柏（Sabina chinensis）接种摩西斗管囊霉（Funneliformis mosseae，FM）、根内根孢囊霉（Rhizophagus intraradices，RI）2种AM菌种处理下土壤呼吸季节动态进行野外连续定位观测，并探究AM真菌接种处理下石漠化土壤呼吸速率与植物生长、土壤理化性质之间的关系。结果表明：（1）相较于对照，接种AM真菌对石漠化生境土壤呼吸季节动态产生了显著影响（P<0.01）。AM真菌处理具有较高的土壤呼吸季节变化幅度，即根内根孢囊霉处理土壤呼吸速率（1.55-9.10 μmol m^-2 s^-1）显著高于摩西斗管囊霉（1.62-8.29 μmol m^-2 s^-1）和对照（1.23-4.46 μmol m^-2 s^-1）；（2） AM真菌接种处理下土壤温湿度变化对土壤呼吸的影响显著大于对照，即土壤温度与水分对土壤呼吸的平均解释量大小顺序为：RI （44.84%；52.35%）>FM （17.18%；41.65%）>CK （2.66%；16.55%）；（3）2种菌种处理下土壤呼吸速率均与土壤有机质、硝态氮、全氮、速效钾、树高、胸径及根系生物量呈显著或极显著正相关（P<0.01或0.05），而与pH呈极显著负相关（P<0.01），但对照处理土壤呼吸速率除与pH呈显著负相关（P<0.05）外，与其它土壤理化指标相关性不显著；（4）土壤温度和水分、硝态氮、铵态氮、有机质、易氧化有机碳、速效钾、全氮及全磷对土壤呼吸变化的贡献最大，而胸径、树高、有效磷、微生物生物量、根系生物量及pH的影响次之。因此，"AM真菌-寄主植物-土壤"相互作用对石漠化生境土壤呼吸季节动态的影响，主要取决于不同AM真菌接种处理对土壤微气候（如含水量）、碳素（有机质、易氧化有机碳）、无机氮库（铵态氮、硝态氮）、根系生物量及磷钾养分可利用性的调控。     

Warming increases soil carbon input in a Sibiraea angustata-dominated alpine shrub ecosystem

Plant-derived carbon (C) inputs via foliar litter, root litter and root exudates are key drivers of soil organic C stocks. However, the responses of these three input pathways to climate warming have rarely been studied in alpine shrublands. By employing a 3-year warming experiment (increased by 1.3 °C), we investigated the effects of warming on the relative C contributions from foliar litter, root litter and root exudates from Sibiraea angustata, a dominant shrub species in an alpine shrubland on the eastern Qinghai-Tibetan Plateau. The soil organic C inputs from foliar litter, root litter and root exudates were 77.45, 90.58 and 26.94 g C m⁻², respectively. Warming only slightly increased the soil organic C inputs from foliar litter and root litter by 8.04 and 11.13 g C m⁻², but significantly increased the root exudate C input by 15.40 g C m⁻². Warming significantly increased the relative C contributions of root exudates to total C inputs by 4.6% but slightly decreased those of foliar litter and root litter by 2.5% and 2.1%, respectively. Our results highlight that climate warming may stimulate plant-derived C inputs into soils mainly through root exudates rather than litter in alpine shrublands on the Qinghai-Tibetan Plateau.     

中国航空碳排放及其效率时空演化特征分析

航空碳排放不仅影响空气质量且可造成温室效应。中国正处于从民航大国向民航强国迈进的关键时期，提高航空碳排放效率是行之有效的航空碳减排手段。运用可拓展随机性环境影响评估模型(STIRPAT)对中国2004—2019年航空碳排放总量的时空演变特征进行分析，以探明不同尺度区域航空碳排放的空间差异与空间关联表现；运用基于非期望产出的超效率松弛变量模型(SBM)和标准差椭圆分析法(SDE)对中国航空碳排放效率的时空分布与格局演化过程进行判定，以分析各省域航空碳排放效率的差异，并给出有效的航空碳减排方略。研究发现：2004—2019年，中国航空碳排放总量持续增长，航空碳排放增长率和航空碳排放强度均呈波动下降趋势；四大经济区航空碳排放总量分布总体表现为“东部>西部>中部>东北”的格局，东部仍是中国航空碳排放的主要区域；高碳排放区较分散，还未形成省域之间连片的碳排放高值区。2004—2019年，中国航空碳排放效率总体呈现“M”型波动上升趋势，各省域航空碳排放效率均不同程度的提高，但主要以低效率区、中效率区为主；各省域之间的航空碳排放效率差异性经历了逐渐减小到逐步增大的过程，但总体航空碳...     

Forest floor photosynthesis and respiration in a drained peatland forest in southern Finland

Background: Although forest floor forms a large biomass pool in forested peatlands, little is known about its role in ecosystem carbon (C) dynamics.

Aim: We aimed to quantify forest floor photosynthesis (P _FF) and respiration (R _FF) as a part of overall C dynamics in a drained peatland forest in southern Finland.

Methods: We measured net forest floor CO₂ exchange with closed chambers and reconstructed seasonal CO₂ exchange in the prevailing plant communities.

Results: The vegetation was a mosaic of plant communities that differed in CO₂ exchange dynamics. The reconstructed growing season P _FF was highest in the Sphagnum community and lowest in the feather moss communities. On the contrary, R _FF was highest in the feather moss communities and lowest in the Sphagnum community. CO₂ assimilated by the forest floor was 20–30% of the total CO₂ assimilated by the forest. The forest floor was a net CO₂ source to the atmosphere, because respiration from ground vegetation, tree roots and decomposition of soil organic matter exceeded the photosynthesis of ground vegetation.

Conclusions: Tree stand dominates C fluxes in drained peatland forests. However, forest floor vegetation can have a noticeable role in the C cycle of peatlands drained for forestry. Similarly to natural mires, Sphagnum moss-dominated communities were the most efficient assimilators of C.