华北低丘山地人工林生态系统净碳交换与气象因子的关系

植树造林使我国森林碳储量显著增加,人工林潜在的碳汇功能不容忽视.基于涡度相关技术,对华北低丘山地30年生栓皮栎-刺槐-侧柏人工混交林生态系统进行了连续2a的碳通量观测,以探讨净碳交换(NEE)与气象因子的关系.结果表明:在主要生长季(4～9月份),夜间日平均NEE(生态系统呼吸)随气温升高呈指数增长(P<0.01).2006年和2007年生态系统呼吸的温度敏感系数(Q_(10))分别为1.92和1.86.气温在10℃以下时,NEE日总量较小.气温超过10℃后,人工林以净吸收大气CO_2为主,且日吸收量随温度升高迅速增加.白天净碳吸收量随光合有效辐射(PAR)增加而增大(P<0.01),可由直角双曲线方程描述;不过,当饱和差(VPD)小于1.0 kPa时,二者呈线性相关(P<0.01).2006年和2007年主要生长季(4～9月份)的平均表观初始光能利用率(α)分别为0.032和0.019,平均最大光合速率(P_(max))分别为0.96mg · m~(-2) · s~(-1)和1.10 mg · m~(-2) · s~(-1).α和P_(max)都存在季节变化.在月尺度,P_(max)与VPD和PAR呈明显的负相关关系(分别为P<0.01和P<0.05),但与气温相关性不显著;α与对应的PAR、气温和VPD均无明显相关关系.     

入侵植物马缨丹(Lantana camara)及其伴生种的光合特性

马缨丹(Lantana camara L.)是粤东地区的入侵植物之一.采用LI-6400光合作用仪对马缨丹及其常见主要伴生种鬼针草(Bidens pilosa L.)、肖梵天花(Urena lobata L.)、土牛膝(Achyranthes aspera L.)在不同有效光合辐射(PAR)和不同CO2浓度下的光合生理指标进行测定,结果表明:(1)马缨丹的光饱和点(LSP)与光补偿点(LCP)分别为1225、13.58 μmol·m-2·s-1,均低于伴生种,且和伴生种差异达到显著水平,光饱和点时的最大净光合速率(Pmax)为13.89μmol·m-2·s-1,表观量子效率(AQY)为0 0503 μmol·m-2·s-1,与土牛膝相当,而显著高于肖梵天花;(2) 马缨丹的CO2饱和点(CSP)与CO2补偿点(CCP)分别为1350、61.78 μmol·mol -1,CO2饱和点时马缨丹的最大净光合速率(Pmax)为20.08 μmol·mol-1,显著高于土牛膝,马缨丹的表观羧化效率(CE)与鬼针草相当,为0.0424 μmol·mol -1;(3)有效光合辐射与CO2浓度的增加,对马缨丹气孔导度(Gs)、蒸腾速率(Tr)影响不明显,但大大提高了其水分利用率(WUE),提示马缨丹对于环境中光强和CO2的变化具有良好的适应能力.这些信息对马缨丹生理生态学特性的认识是一个补充,并能为马缨丹入侵机制的研究提供一些有价值的参考.     

Net ecosystem production of a Douglas-fir stand for 3 years following clearcut harvesting

To investigate the variations in annual and seasonal net ecosystem production (F_NEP) during the development of a young forest, 3 years of continuous eddy covariance measurements of carbon dioxide (CO₂) fluxes were collected following clearcut harvesting and replanting of a coastal Douglas‐fir stand on the east coast of Vancouver Island, BC, Canada. The impact of changing weather and stand structure on F_NEP was examined by developing relationships between F_NEP and variables such as light, temperature, soil moisture, and leaf area index (LAI). In all 3 years, the stand was a large source of CO₂ (620, 520, and 600 g C m^?2 yr^?1 in the first, second, and third years, respectively). During this period, the growth of pioneer and understory species resulted in an increase in maximum growing season LAI from 0.2 in the year the seedlings were planted to 2.5 in the third year. The associated increase in annual gross ecosystem production (P=F_NEP?R_e, where R_e is ecosystem respiration) from 220 g C m^?2 yr^?1 in the first year to 640 g C m^?2 yr^?1 in the third year was exceeded by an increase in annual R_e from 840 to 1240 g C m^?2 yr^?1. Seasonal and interannual variations in daytime F_NEP and P were well described by variations in photosynthetically active radiation, temperature, and changes in LAI. Night‐time measurements of R_e exponentially increased with 2 cm soil temperature with an average Q₁₀ of 2 (relative increase in R_e for a 10°C increase in temperature) and R₁₀ (R_e at 10°C) that increased from 2.1 in the first year to 2.5 in the second year to 3.2 μmol m^?2 s^?1 in the third year. Although the re‐establishment of vegetation in this stand had a major impact on both P and R_e, interannual variations in weather also affected annual F_NEP. Drought, in the summer of the third year, resulted in early senescence and reduced both P and R_e. This resulted in more C being lost from the stand in the third year after harvesting than in the second year.     

Increased leaf area dominates carbon flux response to elevated CO2 in stands of Populus deltoides (Bartr.)

We examined the effects of atmospheric vapor pressure deficit (VPD) and soil moisture stress (SMS) on leaf‐ and stand‐level CO₂ exchange in model 3‐year‐old coppiced cottonwood (Populus deltoides Bartr.) plantations using the large‐scale, controlled environments of the Biosphere 2 Laboratory. A short‐term experiment was imposed on top of continuing, long‐term CO₂ treatments (43 and 120 Pa), at the end of the growing season. For the experiment, the plantations were exposed for 6–14 days to low and high VPD (0.6 and 2.5 kPa) at low and high volumetric soil moisture contents (25–39%). When system gross CO₂ assimilation was corrected for leaf area, system net CO₂ exchange (SNCE), integrated daily SNCE, and system respiration increased in response to elevated CO₂. The increases were mainly as a result of the larger leaf area developed during growth at high CO₂, before the short‐term experiment; the observed decline in responses to SMS and high VPD treatments was partly because of leaf area reduction. Elevated CO₂ ameliorated the gas exchange consequences of water stress at the stand level, in all treatments. The initial slope of light response curves of stand photosynthesis (efficiency of light use by the stand) increased in response to elevated CO₂ under all treatments. Leaf‐level net CO₂ assimilation rate and apparent quantum efficiency were consistently higher, and stomatal conductance and transpiration were significantly lower, under high CO₂ in all soil moisture and VPD combinations (except for conductance and transpiration in high soil moisture, low VPD). Comparisons of leaf‐ and stand‐level gross CO₂ exchange indicated that the limitation of assimilation because of canopy light environment (in well‐irrigated stands; ratio of leaf : stand=3.2–3.5) switched to a predominantly individual leaf limitation (because of stomatal closure) in response to water stress (leaf : stand=0.8–1.3). These observations enabled a good prediction of whole stand assimilation from leaf‐level data under water‐stressed conditions; the predictive ability was less under well‐watered conditions. The data also demonstrated the need for a better understanding of the relationship between leaf water potential, leaf abscission, and stand LAI.     

Using marine reserves to estimate fishing mortality

The proportion of a fish stock that is killed by fishing activity is often calculated as the catch divided by the estimated stock biomass. However, stock biomass is notoriously difficult to estimate reliably, and moreover, the catch may be uncertain or misreported and does not include losses due to discarding. In all too many fisheries, these difficulties have lead to underestimates of total fishing mortality and the commercial demise of the fishery. No‐take marine reserves eliminate fishing mortality from within their boundaries and, for species that exhibit seasonal migratory behaviour, comparison of reserves with fished areas can provide direct estimates of the proportion killed by fishing. For an important exploited species in New Zealand, seasonal changes in density of sub‐legal fish at three marine reserves were similar in both reserve and adjacent non‐reserve areas. However, this result did not hold for legal‐size fish, and the difference in seasonal change between reserved and non‐reserved areas was used to obtain direct estimates of the total localized fishing mortality in the non‐reserve area over 6‐month periods. Estimates of the percentage of legal‐size fish killed by fishing ranged from 70 to 96%. These results demonstrate an unanticipated practical benefit from marine reserves that goes beyond their ecological role.     

Regional Patterns in Carbon Cycling Across the Great Plains of North America

The large organic carbon (C) pools found in noncultivated grassland soils suggest that historically these ecosystems have had high rates of C sequestration. Changes in the soil C pool over time are a function of alterations in C input and output rates. Across the Great Plains and at individual sites through time, inputs of C (via aboveground production) are correlated with precipitation; however, regional trends in C outputs and the sensitivity of these C fluxes to annual variability in precipitation are less well known. To address the role of precipitation in controlling grassland C fluxes, and thereby soil C sequestration rates, we measured aboveground and belowground net primary production (ANPP-C and BNPP-C), soil respiration (SR-C), and litter decomposition rates for 2 years, a relatively dry year followed by a year of average precipitation, at five sites spanning a precipitation gradient in the Great Plains. ANPP-C, SR-C, and litter decomposition increased from shortgrass steppe (36, 454, and 24 g C m^–2 y^–1) to tallgrass prairie (180, 1221, and 208 g C m^–2 y^–1 for ANPP-C, SR-C, and litter decomposition, respectively). No significant regional trend in BNPP-C was found. Increasing precipitation between years increased rates of ANPP-C, BNPP-C, SR-C, and litter decomposition at most sites. However, regional patterns of the sensitivity of ANPP-C, BNPP-C, SR-C, and litter decomposition to between-year differences in precipitation varied. BNPP-C was more sensitive to between-year differences in precipitation than were the other C fluxes, and shortgrass steppe was more responsive than were mixed grass and tallgrass prairie.     

Pacta Tertiis and Regional Fisheries Management Mechanisms: The IUU Fishing Concept as an Illegitimate Short-Cut to a Legitimate Goal1

This article considers how international management of fisheries under the 1995 UN Fish Stocks Agreement and regional fisheries management organizations is affected by one of the basic principles of the law of treaties: the rule pacta tertiis nec nocent nec prosunt, by which international fisheries regulations as treaty-based obligations bind only the parties to the treaty concerned and not third states without their consent. It is shown that the relatively recent concept of IUU (illegal, unreported, and unregulated) fishing, often seen as a way to circumvent this problem, is flawed as a solution, largely because the leading global and European Union instruments in which it is embodied in effect equate unregulated fishing with illegal fishing in a way that pays insufficient heed to the constraints of the pacta tertiis rule.     

Variation of nitric oxide emission potential in plants: a possible link to leaf N content and net photosynthetic activity

Aims Ecological systems, especially soils, have been recently recognized as an important source of atmospheric nitric oxide (NO). However, the study on the contribution of plants to atmospheric NO budget is significantly lagged. The specific objectives of this study are to reveal the phylogenetic variation in NO emission potential existing in various plant species and find out the possible leaf traits affecting NO emission potential.Methods We measured NO emission potential, leaf N and C content, C:N ratio, specific leaf area, net photosynthetic rate (P n) and estimated photosynthetic N use efficiency (PNUE) of 88 plant species. Further investigation of the relationships between NO emission potential and leaf traits were performed by simple linear regression analysis and pair-wise correlation coefficients analysis.Important findings Major results are as follows: (1) NO emission from plant species exhibited large variations, ranging from 0 to 41.7 nmol m ?2 h^-1, and the species frequency distributions of NO emission potential could be fitted to a log-normal curve. (2) Among 88 species, NO emission potential was the highest in Podocarpus macrophyllus, but lowest in Zanthoxylum nitidum and Vernicia montana. (3) NO emission potential has strong correlation to leaf N content, P n and PNUE. The variations in NO emission potential among diverse plant species may be closely related to leaf N level and net photosynthetic ability.     

Can intensification reduce emission intensity of biofuel through optimized fertilizer use? Theory and the case of oil palm in Indonesia

Closing yield gaps through higher fertilizer use increases direct greenhouse gas emissions but shares the burden over a larger production volume. Net greenhouse gas (GHG) footprints per unit product under agricultural intensification vary depending on the context, scale and accounting method. Life cycle analysis of footprints includes attributable emissions due to (i) land conversion (‘fixed cost’); (ii) external inputs used (‘variable cost’); (iii) crop production (‘agronomic efficiency’); and (iv) postharvest transport and processing (‘proportional’ cost). The interplay between fixed and variable costs results in a nuanced opportunity for intermediate levels of intensification to minimize footprints. The fertilizer level that minimizes the footprint may differ from the economic optimum. The optimization problem can be solved algebraically for quadratic crop fertilizer response equations. We applied this theory to data of palm oil production and fertilizer use from 23 plantations across the Indonesian production range. The current EU threshold requiring at least 35% emission saving for biofuel use can never be achieved by palm oil if produced: (i) on peat soils, or (ii) on mineral soils where the C debt due to conversion is larger than 20 Mg C ha^?1, if the footprint is calculated using an emission ratio of N₂O–N/N fertilizer of 4%. At current fertilizer price levels in Indonesia, the economically optimized N fertilizer rate is 344–394 kg N ha^?1, while the reported mean N fertilizer rate is 141 kg N ha^?1 yr^?1 and rates of 74–277 kg N ha^?1 would minimize footprints, for a N₂O–N/N fertilizer ratio of 4–1%, respectively. At a C debt of 30 Mg C ha^?1, these values are 200–310 kg N ha^?1. Sustainable weighting of ecology and economics would require a higher fertilizer/yield price ratio, depending on C debt. Increasing production by higher fertilizer use from current 67% to 80% of attainable yields would not decrease footprints in current production conditions.     

The role of a cytosolic superoxide dismutase in barley–pathogen interactions

Reactive oxygen species (ROS), including superoxide ( / ) and hydrogen peroxide (H₂O₂), are differentially produced during resistance responses to biotrophic pathogens and during susceptible responses to necrotrophic and hemi‐biotrophic pathogens. Superoxide dismutase (SOD) is responsible for the catalysis of the dismutation of / to H₂O₂, regulating the redox status of plant cells. Increased SOD activity has been correlated previously with resistance in barley to the hemi‐biotrophic pathogen Pyrenophora teres f. teres (Ptt, the causal agent of the net form of net blotch disease), but the role of individual isoforms of SOD has not been studied. A cytosolic CuZnSOD, HvCSD1, was isolated from barley and characterized as being expressed in tissue from different developmental stages. HvCSD1 was up‐regulated during the interaction with Ptt and to a greater extent during the resistance response. Net blotch disease symptoms and fungal growth were not as pronounced in transgenic HvCSD1 knockdown lines in a susceptible background (cv. Golden Promise), when compared with wild‐type plants, suggesting that cytosolic / contributes to the signalling required to induce a defence response to Ptt. There was no effect of HvCSD1 knockdown on infection by the hemi‐biotrophic rice blast pathogen Magnaporthe oryzae or the biotrophic powdery mildew pathogen Blumeria graminis f. sp. hordei, but HvCSD1 also played a role in the regulation of lesion development by methyl viologen. Together, these results suggest that HvCSD1 could be important in the maintenance of the cytosolic redox status and in the differential regulation of responses to pathogens with different lifestyles.