泥炭藓: 一类具有重要生态、经济和科学价值的碳封存植物

全球气候变暖是人类面临最严峻的环境挑战。有效控制碳排放, 充分发挥生态系统的固碳能力是实现碳中和目标的重要手段。作为碳封存能力最强的一种湿地类型, 泥炭地是加快实现碳中和目标的关键陆地生态系统。作为泥炭地“有效的生态系统工程师”, 泥炭藓(Sphagnum)在泥炭地的碳汇功能、过滤淡水及保护土地免受洪水侵袭等方面具有极其重要的作用。100多年来, 泥炭藓广泛应用于医药保健、污染监测和废水处理等领域, 尤其是作为一类最值得信赖的土壤介质和保湿材料一直被广泛用于园艺产业。在全球气候变暖和“双碳”目标的大背景下, 泥炭藓已经成为生命科学和生态学研究的热点。该文主要从泥炭藓的形态、物种多样性和起源、生境与分布、繁殖和保护、培养与种植、环境指示和监测、用途和应用, 以及碳封存、储水和酸化能力等方面进行综述, 旨在为泥炭藓研究、泥炭地的保护和恢复以及泥炭藓开发利用和产业发展提供借鉴与参考。     

A New Initiative to Use Carbon Trading for Tropical Forest Conservation

I describe a new initiative, led by a coalition of developing nations, to devise a viable mechanism for using carbon trading to protect old-growth tropical forests. I highlight some of the practical and political hurdles involved in forest-carbon trading, and explain why this initiative is rapidly gaining broad-based political support.     

Photosynthetic and Respiratory Acclimation to Experimental Warming for Four Species in a Tallgrass Prairie Ecosystem

Global temperature has been Increased by 0.6 ℃ over the past century and is predicted to Increase by 1.4-5.8 ℃ by the end of this century. It is unclear what impacts global warming will have on tallgrass species. In the present study, we examined leaf net photosynthetic rate （P.） and leaf respiration rate in darkness （Rd） of Aster erlcoldes （L.） Nesom, Ambrosia psllostachya DC., Helianthus mollis Lam., and Sorghastrum nutans （L.） Nash In response to experimental warming in a tallgrass prairie ecosystem of the Great Plains, USA, in the autumn （fall） of 2000 and through 2001. Warming has been Implemented with infrared heaters since 21 November 1999. The P. increased significantly In spring, decreased in early fall, and did not change in summer and late fall in the four species under warming compared with control. The Rd of the four species increased significantly until mid-summer and then did not change under warming. Measured temperature-response curves of P. showed that warming Increased the optimum temperature of P. （Topt） by 2.32 and 4.59 ℃ for H. mollis and S. nutans, respectively, in August, whereas there were no changes in May and September, and A. ericoldes and A. psllostachya also showed no changes in any of the 3 months. However, P. at optimum temperature （Popt） showed downregulation in September and no regulation in May and August for all four species. The temperature-response curves of Rd Illustrate that the temperature sensitivity of Rd, Q10, was lower in the warmed plots compared with the control plots, except for A. ericoides in August, whereas there were no changes In May and September for all four species. The results of the present study indicate that photosynthetic and respiratory acclimation varies with species and among seasons, occurring In the mid-growing season and not in the early and late growing seasons.     

增温、光照时间和氮添加对蒙古栎主要物候期的影响

利用大型人工气候室模拟研究增温(对照、增温1.5 ℃、增温2.0 ℃)、光照时间(10、14、18 h)和氮添加(0、5、10、20 g N·m^-2·a^-1)对东北地区蒙古栎主要物候期的影响。结果表明: 增温1.5和2.0 ℃使芽膨大期显著提前,完全变色期显著推迟,生长期延长,且延长天数随增温幅度的增大而增加。光照时间显著影响秋季物候(叶黄始期、叶黄普期、完全变色期),与光照14 h相比,短光照(10 h)使叶黄始期显著推迟7.0 d,生长盛期相对延长。氮添加使芽膨大期、芽开放期、展叶始期、展叶盛期均显著提前,完全变色期仅在高氮水平(20 g N·m^-2·a^-1)下显著推迟9.5 d,表明高氮添加使蒙古栎生长期延长。增温和高氮添加(20 g N·m^-2·a^-1)协同作用显著推迟完全变色期,导致叶黄期延长。增温和短光照协同作用、氮添加和短光照协同作用以及增温、氮添加和短光照协同作用均使叶黄始期显著推迟,生长盛期相对延长。     

模拟降雨条件下砾石含量对塿土工程堆积体坡面产流产沙的影响

为探究砾石含量对塿土堆积体坡面产流产沙的影响,采用室内人工模拟降雨试验,以土质坡面为对照,研究5种砾石含量(10%、20%、30%、40%、50%)堆积体坡面在不同降雨强度(1.0、1.5、2.0、2.5 mm·min^-1)下的产流产沙特征。结果表明:不同试验条件下的平均径流率在2.18～13.07 L·min^-1,不同雨强条件下平均径流率均在砾石含量10%(或20%)和50%时分别达到最大值与最小值;平均流速在0.06～0.22 m·s^-1,流速变化复杂,砾石含量越小,流速变幅越大,变异系数也越大,砾石含量10%时平均流速最大。砾石的存在可有效抑制产沙,最大减沙效益可达84.2%,雨强相较于砾石含量对平均产沙率的影响更大。偏相关分析表明,平均径流率、流速、产沙率均与砾石含量呈极显著负相关;平均产沙率与平均径流率、平均流速以及二者交互项均呈极显著线性函数关系,其中,与平均径流率的相关性最强。本研究可为塿土区工程堆积体水土流失治理和侵蚀模型的建立提供参考。     

增温及隔离降水对杉木幼树细根生物量、形态及养分特征的影响

为揭示全球变暖和降水格局改变对我国中亚热带地区森林生态系统地下生态过程的影响,在福建三明森林生态系统国家野外科学观测研究站内开展杉木(Cunninghamia lanceolata)幼树土壤增温和隔离降水双因子试验,研究增温和隔离降水在夏季对杉木幼树细根生物量、形态及养分特征的影响。结果表明,增温(+5℃,W)、隔离降水(–50%,P)和增温+隔离降水(WP)处理的细根总生物量分别比对照(CT)显著降低35.7%、51.7%和59.1%,P和WP处理的细根总生物量分别比W处理显著降低24.9%和36.4%;W、P和WP处理的0~1 mm细根比根长(specific root length,SRL)比对照均显著增加,而0~1和1~2 mm细根比表面积(specific root area,SRA)均无显著变化;与对照相比,W处理的细根N含量、C/N和δ¹⁵N均无显著变化,P处理的细根N含量和C/N分别显著增加和下降,WP处理的细根N含量和δ¹⁵N显著增加,而C/N显著降低。因此,未来在全球变暖和降水减少的双重环境胁迫下,调整表层细根形态特征可能不是杉木幼树的主要应对策略;而相较于温度升高,降水减少可能是影响杉木幼树细根生物量及表层化学元素分配的主要环境因子。     

Temperature × light interaction and tolerance of high water temperature in the planktonic freshwater flagellates Cryptomonas (Cryptophyceae) and Dinobryon (Chrysophyceae)

Using microcosm experiments, we investigated the interactive effects of temperature and light on specific growth rates of three species each of the phytoplanktonic genera Cryptomonas and Dinobryon. Several species of these genera play important roles in the food web of lakes and seem to be sensitive to high water temperature. We measured growth rates at three to four photon flux densities ranging from 10 to 240 μmol photon · m^?2 · s^?1 and at 4–5 temperatures ranging from 10°C to 28°C. The temperature × light interaction was generally strong, species specific, and also genus specific. Five of the six species studied tolerated 25°C when light availability was high; however, low light reduced tolerance of high temperatures. Growth rates of all six species were unaffected by temperature in the 10°C–15°C range at light levels ≤50 μmol photon · m^?2 · s^?1. At high light, growth rates of Cryptomonas spp. increased with temperature until the temperature optimum was reached and then declined. The Dinobryon species were less sensitive than Cryptomonas spp. to photon flux densities of 40 μmol photon · m^?2 · s^?1 and 200 μmol photon · m^?2 · s^?1 over the entire temperature range but did not grow under a combination of very low light (10 μmol photon · m^?2 · s^?1) and high temperature (≥20°C). Among the three Cryptomonas species, cell volume declined with temperature and the maximum temperature tolerated was negatively related to cell size. Since Cryptomonas is important food for microzooplankton, these trends may affect the pelagic carbon flow if lake warming continues.     

Rapid shifts in the thermal sensitivity of growth but not development rate causes temperature–size response variability during ontogeny in arthropods

Size at maturity in ectotherms commonly declines with warming. This near‐universal phenomenon, formalised as the temperature–size rule, has been observed in over 80% of tested species, from bacteria to fish. The proximate cause has been attributed to the greater temperature dependence of development rate than growth rate, causing individuals to develop earlier but mature smaller in the warm. However, few studies have examined the ontogenetic progression of the temperature–size response at high resolution. Using marine planktonic copepods, we experimentally determined the progression of the temperature–size response over ontogeny. Temperature–size responses were not generated gradually from egg to adult, contrary to the predictions of a naïve model in which development rate was assumed to be more temperature‐dependent than growth rate, and the difference in the temperature dependence of these two rates remained constant over ontogeny. Instead, the ontogenetic progression of the temperature–size response in experimental animals was highly episodic, indicating rapid changes in the extent to which growth and development rates are thermally decoupled. The strongest temperature–size responses occurred temporally mid‐way through ontogeny, corresponding with the point at which individuals reached between ~5 and 25% of their adult mass. Using the copepod Oithona nana, we show that the temperature‐dependence of growth rate varied substantially throughout ontogeny, whereas the temperature dependence of development rate remained constant. The temperature‐dependence of growth rate even exceeded that of development rate in some life stages, leading to a weakening of the temperature–size response. Our analyses of arthropod temperature–size responses from the literature, including crustaceans and insects, support these conclusions more broadly. Overall, our findings provide a better understanding of how the temperature–size rule is produced over ontogeny. Whereas we find support for the generality of developmental rate isomorphy in arthropods (shared temperature dependence of development rate across life stages), this concept appears not to apply to growth rates.     

Temperature‐dependence of minimum resource requirements alters competitive hierarchies in phytoplankton

Resource competition theory is a conceptual framework that provides mechanistic insights into competition and community assembly of species with different resource requirements. However, there has been little exploration of how resource requirements depend on other environmental factors, including temperature. Changes in resource requirements as influenced by environmental temperature would imply that climate warming can alter the outcomes of competition and community assembly. We experimentally demonstrate that environmental temperature alters the minimum light and nitrogen requirements – as well as other growth parameters – of six widespread phytoplankton species from distinct taxonomic groups. We found that species require the most nitrogen at the highest temperatures while light requirements tend to be lowest at intermediate temperatures, although there are substantial interspecific differences in the exact shape of this relationship. We also experimentally parameterize two competition models, which we use to illustrate how temperature, through its effects on species’ traits, alters competitive hierarchies in multispecies assemblages, determining community dynamics. Developing a mechanistic understanding of how temperature influences the ability to compete for limiting resources is a critical step towards improving forecasts of community dynamics under climate warming.     

Isoprene is more affected by climate drivers than monoterpenes: A meta‐analytic review on plant isoprenoid emissions

Isoprene and monoterpenes (MTs) are among the most abundant and reactive volatile organic compounds produced by plants (biogenic volatile organic compounds). We conducted a meta‐analysis to quantify the mean effect of environmental factors associated to climate change (warming, drought, elevated CO₂, and O₃) on the emission of isoprene and MTs. Results indicated that all single factors except warming inhibited isoprene emission. When subsets of data collected in experiments run under similar change of a given environmental factor were compared, isoprene and photosynthesis responded negatively to elevated O₃ (?8% and ?10%, respectively) and drought (?15% and ?42%), and in opposite ways to elevated CO₂ (?23% and +55%) and warming (+53% and ?23%, respectively). Effects on MTs emission were usually not significant, with the exceptions of a significant stimulation caused by warming (+39%) and by elevated O₃ (limited to O₃‐insensitive plants, and evergreen species with storage organs). Our results clearly highlight individual effects of environmental factors on isoprene and MT emissions, and an overall uncoupling between these secondary metabolites produced by the same methylerythritol 4‐phosphate pathway. Future results from manipulative experiments and long‐term observations may help untangling the interactive effects of these factors and filling gaps featured in the current meta‐analysis.