Wind as a main driver of the net ecosystem carbon balance of a semiarid Mediterranean steppe in the South East of Spain

Despite the advance in our understanding of the carbon exchange between terrestrial ecosystems and the atmosphere, semiarid ecosystems have been poorly investigated and little is known about their role in the global carbon balance. We used eddy covariance measurements to determine the exchange of CO₂ between a semiarid steppe and the atmosphere over 3 years. The vegetation is a perennial grassland of Stipa tenacissima L. located in the SE of Spain. We examined diurnal, seasonal and interannual variations in the net ecosystem carbon balance (NECB) in relation to biophysical variables. Cumulative NECB was a net source of 65.7, 143.6 and 92.1 g C m^?2 yr^?1 for the 3 years studied, respectively. We separated the year into two distinctive periods: dry period and growing season. The ecosystem was a net source of CO₂ to the atmosphere, particularly during the dry period when large CO₂ positive fluxes of up to 15 μmol m^?2 s^?1 were observed in concomitance with large wind speeds. Over the growing season, the ecosystem was a slight sink or neutral with maximum rates of ?2.3 μmol m^?2 s^?1. Rainfall events caused large fluxes of CO₂ to the atmosphere and determined the length of the growing season. In this season, photosynthetic photon flux density controlled day‐time NECB just below 1000 μmol m^?2 s^?1. The analyses of the diurnal and seasonal data and preliminary geological and gas‐geochemical evaluations, including C isotopic analyses, suggest that the CO₂ released was not only biogenic but most likely included a component of geothermal origin, presumably related to deep fluids occurring in the area. These results highlight the importance of considering geological carbon sources, as well as the need to carefully interpret the results of eddy covariance partitioning techniques when applied in geologically active areas potentially affected by CO₂‐rich geofluid circulation.     

Precipitation variability and fire influence the temporal dynamics of soil CO2 efflux in an arid grassland

Climate models suggest that extreme rainfall events will become more common with increased atmospheric warming. Consequently, changes in the size and frequency of rainfall will influence biophysical drivers that regulate the strength and timing of soil CO₂ efflux – a major source of terrestrial carbon flux. We used a rainfall manipulation experiment during the summer monsoon season (July–September) to vary both the size and frequency of precipitation in an arid grassland 2 years before and 2 years after a lightning‐caused wildfire. Soil CO₂ efflux rates were always higher under increased rainfall event size than under increased rainfall event frequency, or ambient precipitation. Although fire reduced soil CO₂ efflux rates by nearly 70%, the overall responses to rainfall variability were consistent before and after the fire. The overall sensitivity of soil CO₂ efflux to temperature (Q₁₀) converged to 1.4, but this value differed somewhat among treatments especially before the fire. Changes in rainfall patterns resulted in differences in the periodicity of soil CO₂ efflux with strong signals at 1, 8, and 30 days. Increased rainfall event size enhanced the synchrony between photosynthetically active radiation and soil CO₂ efflux over the growing season before and after fire, suggesting a change in the temporal availability of substrate pools that regulate the temporal dynamics and magnitude of soil CO₂ efflux. We conclude that arid grasslands are capable of rapidly increasing and maintaining high soil CO₂ efflux rates in response to increased rainfall event size more than increased rainfall event frequency both before and after a fire. Therefore, the amount and pattern of multiple rain pulses over the growing season are crucial for understanding CO₂ dynamics in burned and unburned water‐limited ecosystems.     

The role of mitochondrial electron transport in tumorigenesis and metastasis

Background

Tumor formation and spread via the circulatory and lymphatic drainage systems is associated with metabolic reprogramming that often includes increased glycolytic metabolism relative to mitochondrial energy production. However, cells within a tumor are not identical due to genetic change, clonal evolution and layers of epigenetic reprogramming. In addition, cell hierarchy impinges on metabolic status while tumor cell phenotype and metabolic status will be influenced by the local microenvironment including stromal cells, developing blood and lymphatic vessels and innate and adaptive immune cells. Mitochondrial mutations and changes in mitochondrial electron transport contribute to metabolic remodeling in cancer in ways that are poorly understood.

Scope of Review

This review concerns the role of mitochondria, mitochondrial mutations and mitochondrial electron transport function in tumorigenesis and metastasis.

Major Conclusions

It is concluded that mitochondrial electron transport is required for tumor initiation, growth and metastasis. Nevertheless, defects in mitochondrial electron transport that compromise mitochondrial energy metabolism can contribute to tumor formation and spread. These apparently contradictory phenomena can be reconciled by cells in individual tumors in a particular environment adapting dynamically to optimally balance mitochondrial genome changes and bioenergetic status.

General Significance

Tumors are complex evolving biological systems characterized by genetic and adaptive epigenetic changes. Understanding the complexity of these changes in terms of bioenergetics and metabolic changes will permit the development of better combination anticancer therapies. This article is part of a Special Issue entitled Frontiers of Mitochondrial Research.     

Effects of temperature on complexes I and II mediated respiration,ROS generation and oxidative stress status in isolated gill mitochondria of the mud crab Scylla serrata

Effects of fluctuations in habitat temperature (18–30°) on mitochondrial respiratory behavior and oxidative metabolic responses in the euryhaline ectotherm Scylla serrata are not fully understood. In the present study, effects of different temperatures ranging from 12 to 40 °C on glutamate and succinate mediated mitochondrial respiration, respiratory control ratio (RCR), ATP generation rate, ratio for the utilization of phosphate molecules per atomic oxygen consumption (P/O), levels of lipid peroxidation and H₂O₂ in isolated gill mitochondria of S. serrata are reported. The pattern of variation in the studied parameters was similar for the two substrates at different temperatures. The values recorded for RCR (≥3) and P/O ratio (1.4–2.7) at the temperature range of 15–25 °C were within the normal range reported for other animals (3–10 for RCR and 1.5–3 for P/O). Values for P/O ratio, ATP generation rate and RCR were highest at 18 °C when compared to the other assay temperatures. However, at low and high extreme temperatures, i.e. at 12 and 40 °C, states III and IV respiration rates were not clearly distinguishable from each other indicating that mitochondria were completely uncoupled. Positive correlations were noticed between temperature and the levels of both lipid peroxidation and H₂O₂. It is inferred that fluctuations on either side of ambient habitat temperature may adversely influence mitochondrial respiration and oxidative metabolism in S. serrata. The results provide baseline data to understand the impacts of acute changes in temperature on ectotherms inhabiting estuarine or marine environments.     

生境不完全重叠的两种鲤科鱼类耐低氧及运动能力比较

以乌江流域亲缘关系近,但分布并不完全重叠的马口鱼(Opsariichthys bidens)和宽鳍鱲(Zacco platypus)作为实验对象,分别考察这两种实验鱼的低氧耐受及游泳运动能力。将野外采回的实验鱼置于(25±1)℃条件下,分别测定两种鱼的临界氧分压(Pcrit)、水面呼吸(ASR)、失去平衡点(LOE)以及在不同溶氧水平(8.0、4.0和2.0 mg/L)下的临界游泳速度(Ucrit)和活跃耗氧率(MO2active)。研究发现:马口鱼的Pcrit(2.44±0.20)mg/L显著高于宽鳍鱲(1.86±0.10)mg/L(P=0.031)。但马口鱼的50%ASR(1.23±0.16)mg/L显著低于宽鳍鱲(1.97±0.11)mg/L(P=0.023);马口鱼的50%LOE(0.84±0.01)mg/L同样显著低于宽鳍鱲(0.97±0.02)mg/L(P=0.004)。宽鳍鱲在8.0和4.0 mg/L下的游泳能力显著高于马口鱼,然而马口鱼和宽鳍鱲的Ucrit均随测定溶氧水平的下降而显著降低(P0.01);宽鳍鱲和马口鱼的运动耗氧率均随水流速度的增加而呈现指数增加,但随测定溶氧水平的降低运动耗氧曲线变得相对平缓,尤其是在溶氧为4.0 mg/L时马口鱼的运动耗氧曲线与宽鳍鱲相比越发平缓;两种实验鱼的MO2active随溶氧水平下降的变化趋势与Ucrit相似(P0.001)。结果表明:两种野外生存的实验鱼不仅在低氧耐受能力方面存在显著差异,而且两者的游泳运动能力也有不同表现,这很有可能与其遗传特征、生存环境及生态习性相关。     

干湿交替下草地生态系统土壤呼吸变化的微生物响应机制研究进展

草地是陆地生态系统中最重要、分布最广的生态系统类型之一,对全球碳循环和气候调节有着重要的作用和效应.我国拥有极为丰富的草地资源,是巨大的陆地碳储存库,也是全球碳循环重要组成部分.干湿交替是土壤中普遍发生的自然现象,这种现象的发生可能会加速土壤的碳矿化过程、激增土壤呼吸以及影响微生物的活性和群落结构等.在全球变化日趋显著的背景下,降雨量、降雨强度以及降雨频率的变化将会加速土壤干湿交替进程,进而带来微生物活性、群落结构以及土壤呼吸的变化,并对全球碳循环过程产生重要影响.本文综述了近十年来国内外的相关文献,对干湿交替条件下,土壤释放CO₂消耗碳源、土壤呼吸随时间的动态变化趋势以及土壤呼吸与微生物量、微生物活性和微生物群落结构之间的关系进行了分析和总结,以期为更好地理解干湿交替过程中草地生态系统土壤呼吸的微生物学响应机制,更准确地预测和评估未来的全球陆地生态系统的碳收支与气候变化提供一定的理论基础.     

Responses of soil heterotrophic respiration to changes in soil temperature and moisture in a Stipa krylovii grassland in Nei Mongol

土壤异养呼吸在野外自然条件下除受温湿度影响外, 还受其他多种因子的综合影响, 很难利用野外观测数据确定土壤异养呼吸对温湿度变化的响应方程形式, 以及温湿度间是否存在交互作用。该研究在严格控制温湿度的条件下对内蒙古克氏针茅(Stipa krylovii)(西北针茅(Stipa sareptana var. krylovii))草原土样进行室内培养实验, 旨在解决上述问题。该研究的正交实验包括5个温度梯度(9、14、22、30、40 ℃)和5个湿度梯度(土壤持水力(water holding capacity, WHC)分别为20%、40%、60%、80%、100%)。室内培养实验持续71天, 土壤异养呼吸速率测定为2天(后期为1周)一次, 土壤可溶性有机碳和微生物生物量碳含量测定约为18天一次。研究结果显示: 土壤异养呼吸与温度呈显著正相关(p < 0.001)且温度间差异显著(p = 0.001), 呼吸温度敏感性(Q₁₀)与土壤水分含量呈正相关(p < 0.001); 呼吸与土壤水分二项式拟合效果较好, 在80% WHC时呼吸速率最大, 且最适湿度随温度上升而增加。土壤温度和水分的交互作用显著(p < 0.05), 土壤异养呼吸最适响应方程为lnRh = 0.914 + 0.098T + 0.046M + 0.001TM - 0.002T² - 0.001M² (Rh为异养呼吸, T为温度, M为湿度), 这说明加和形式的温湿度响应模型可能优于乘积形式。微生物生物量碳与土壤异养呼吸的相关性随培养时间发生变化, 土壤可溶性有机碳与土壤异养呼吸无显著相关(培养第20天除外), 原因可能是培养期间微生物死亡或群落结构改变导致微生物总体代谢活性的变化。     

A critical analysis of the causes of boron toxicity in plants

This study investigated the main factors contributing to boron toxicity in plants. Growth was rapidly inhibited by internal B concentrations in the range 1–5 m m across a range of plant types that included monocot, dicot and algal species. In contrast, mature cells were able to withstand up to 60 m m B for several days. In wheat, rapid inhibition of root growth occurred if high B was applied to the root tip, but not if high B was applied to mature sections of the root. In leaves, there were gradations in B concentrations that correlated with visible symptoms of toxicity. However, there was no evidence to support the hypothesis that toxicity in leaves is due to osmotic stress induced by the accumulation of B. Analysis of the sensitivity to B of a range of metabolic processes including photosynthesis, respiration and protein synthesis leads to the conclusion that growth is not restricted by effects of B on energy supply and not directly by inhibition of protein synthesis. At higher B concentrations, many cellular activities were found to be partially inhibited and the toxicity to mature tissues was therefore considered not to arise from the disruption of a single process, but from the accumulated retardation of many cellular processes, exacerbated in light by photo‐oxidative stress.