高寒草地甘肃臭草根系分形结构的坡向差异性

根系分形结构是植物根系构型应对环境异质性的表型可塑性结果, 可反映植物对生长环境的适应策略。利用ArcGIS建立研究区域的数字高程模型, 并提取坡向数据, 采用全根挖掘和Win-RHIZO根系分析仪相结合的方法, 研究了祁连山北坡高寒退化草地不同坡向甘肃臭草(Melica przewalskyi)的根系分形结构。结果表明: 随着坡向由北坡向东坡、西坡、南坡转变, 草地群落的密度、高度和土壤含水量逐渐减小, 甘肃臭草种群的密度、高度以及根系分形丰度呈逐渐增大的趋势、分形维数逐渐减小; 不同坡向甘肃臭草根系分形维数和分形丰度间的相关性存在差异(p < 0.05), 南坡和北坡甘肃臭草根系分形维数分形丰度之间存在极显著负相关关系(p < 0.01), 东坡和西坡之间存在显著负相关关系(p < 0.05), 甘肃臭草根系分形维数和分形丰度存在着“此消彼长”的权衡关系; 随着坡向由北坡向东坡、西坡、南坡转变, 甘肃臭草根系分形维数和分形丰度回归方程的标准化主轴(SMA)斜率逐渐增大(p < 0.05), 说明在干旱的南坡, 根系所开发利用的相同体积的土壤内, 根系分支更少、更稀疏。不同坡向甘肃臭草合理权衡根系分形维数和分形丰度的资源配置模式, 体现了植物根系构型构建的资源投资权衡机制。     

Exploring the community assembly of subalpine meadow communities based on functional traits and community phylogeny

Aims The community assembly has been a prominent issue in community ecology. This work was intended to explore the mechanisms of the species coexistence and biodiversity in communities. Our objective was to explore the mechanisms of community assembly in subalpine meadow plant communities along slope gradients in Gannan Tibetan Autonomous Prefecture, Gansu Province, Northwest China.Methods We selected five slope-oriented plots to construct a super-tree representing the species pool. We surveyed the leaf functional traits and soil environmental factors in different slopes. Then we tested the phylogenetic signal of leaf dry matter content (LDMC), specific leaf area (SLA), leaf nitrogen content (LNC) and leaf phosphorus content (LPC).Important findings The changes of slope aspect had significant influence on soil water content (SWC) and soil nutrient content. Most of the plants leaf functional traits had significant difference along different slope aspects. The LDMC was higher in south and southwest slope than north slope, while SLA, LNC and LPC were relatively high in north and northwest slope. The LPC showed feeble phylogenetic signal, while LDMC, SLA, LNC did not have a significant phylogenetic signal. With changes in the slope aspect from south to north, community phylogenetic structure shifted from over-dispersion to clustered dispersion. In south and southwest slope, habitat filtering was the driving force for community assembly. Interspecific competition was the main driving factor for community assembly in north and northwest slope aspects. But in west slope, two indices showed contrary consequence. This means the process of community assembly in west slope was more complicated and its phylogenetic index may be the result of several mechanisms working together.     

采用最大溯源径流路径法估算RUSLE模型中地形因子探讨

采用基于AML的提取坡长值的新方法--最大溯源径流路径法,对贵州省毕节地区5个不同范围区域的DEM数据进行坡长值、地形因子的提取,并与基于AML的迭代累计坡长法和基于C⁺⁺的迭代累计坡长法对提取坡长值的时间消耗、地形因子值进行了比较.结果表明：基于AML的最大溯源径流路径法能够实现修正的通用土壤流失模型(RUSLE)中坡长值、地形因子的提取,可达到与迭代累计坡长法相同的效果;与基于AML的迭代累计坡长法相比,该方法计算效率较高,大大减少了提取坡长值的时间消耗,可实现基于AML的坡长值、地形因子提取在大范围区域上的扩展;与基于C⁺⁺的迭代累计坡长法相比,该方法计算时效和结果相当,程序编写简单,容易修改和调试,能更普遍应用于GIS用户.     

Functional properties of the newly observed γ-chain fetal hemoglobin variant Hb F-Monserrato-Sassari (HBG2:c.280T > C) or [γ93 (F9) Cys → Arg]

Background

HbF-Monserrato-Sassari is a newly discovered abnormal fetal hemoglobin observed in an apparently normal newborn baby during a hemoglobinopathies survey at birth in North Sardinian population.

Methods

Electrophoretic analysis of the cord blood lysate evidenced for an abnormal tetramer due to a mutated fetal globin chain. Electrospray ionisation-mass spectrometry and gene sequencing were used to identify the mutation. Oxygen binding ability of the variant Hb was determined.

Results

Sequencing of the γ globin genes revealed the TGT → CGT transition at codon 93 in one of the two ^Gγ genes, which leads to the Arg for Cys amino acid replacement at position 9 of the F α-helix. The amino acid substitution was confirmed by mass spectrometric analysis of the globin chains. Since modifications or substitutions at position β93 are known to affect the arrangement of a salt bridge at the α1β2 sliding contacts that are crucial for subunit cooperativity, the functional properties of the variant were studied to evaluate the effect of the replacement at the same position in the γ globin chain. With respect to normal HbF, the variant showed a significant increase in oxygen affinity and a slight decrease of both Bohr effect and cooperativity.

General significance

Result indicates a key role of the Cys γ93 residue for subunit cooperativity in the T → R transition of the HbF tetramer. Substitutions at the F9 position of the ^Gγ globin may result in stabilization of the high affinity R-state of the Hb tetramer. Because of the loss of Cys γ93 residue, this variant is considered to be potentially compromised in nitric oxide transport.     

Migration patterns and navigation cues of Atlantic salmon post-smolts migrating from 12 rivers through the coastal zones around the Irish Sea

The freshwater phase of the first seaward migration of juvenile Atlantic salmon (Salmo salar) is relatively well understood when compared with our understanding of the marine phase of their migration. In 2021, 1008 wild and 60 ranched Atlantic salmon smolts were tagged with acoustic transmitters in 12 rivers in England, Scotland, Northern Ireland and Ireland. Large marine receiver arrays were deployed in the Irish Sea at two locations: at the transition of the Irish Sea into the North Atlantic between Ireland and Scotland, and between southern Scotland and Northern Ireland, to examine the early phase of the marine migration of Atlantic salmon smolts. After leaving their natal rivers' post-smolt migration through the Irish Sea was rapid with minimum speeds ranging from 14.03 to 38.56 km.day⁻¹ for Atlantic salmon smolts that entered the Irish Sea directly from their natal river, to 9.69–39.94 km.day⁻¹ for Atlantic salmon smolts that entered the Irish Sea directly from their natal estuary. Population minimum migration success through the study area was strongly correlated with the distance of travel, populations further away from the point of entry to the open North Atlantic exhibited lower migration success. Post-smolts from different populations experienced different water temperatures on entering the North Atlantic. This was largely driven by the timing of their migration and may have significant consequences for feeding and ultimately survivorship. The influence of water currents on post-smolt movement was investigated using data from previously constructed numerical hydrodynamic models. Modeled water current data in the northern Irish Sea showed that post-smolts had a strong preference for migrating when the current direction was at around 283° (west-north-west) but did not migrate when exposed to strong currents in other directions. This is the most favorable direction for onward passage from the Irish Sea to the continental shelf edge current, a known accumulation point for migrating post-smolts. These results strongly indicate that post-smolts migrating through the coastal marine environment are: (1) not simply migrating by current following (2) engage in active directional swimming (3) have an intrinsic sense of their migration direction and (4) can use cues other than water current direction to orientate during this part of their migration.     

Geomorphic principles of terrain organization and vegetation gradients

Abstract. Moisture and nutrient gradients consistently explain much of the variation in plant species composition and abundance, but these gradients are not spatially explicit and only reveal species responses to resource levels. This study links these abstract gradients to quantitative, spatial models of hill‐slope assembly. A gradient analysis in the mixed‐wood boreal forest demonstrates that patterns of upland vegetation distribution are correlated to soil moisture and nutrient gradients. Variation in species abundance with time since the last fire is removed from the gradient analysis in order to avoid confounding the physical environment gradients. The physical‐environment gradients are related to qualitative positions on the hill slope i.e. crest, mid‐slope, bottom‐slope. However, hill‐slope shape can be quantitatively described and compared by fitting allometric equations to the slope profiles. Using these equations, we show that hill‐slope profiles on similar surficial materials have similar parameters, despite coming from widely separated locations. We then quantitatively link the moisture and nutrient gradients to the equations. Moisture and nutrients significantly increase as distance down‐slope from the ridgeline increases. Corresponding vegetation composition changes too. These relationships characterize the general pattern of vegetation change down most hill slopes in the area. Since hill slopes are a universal feature of all landscapes, these principles may characterize landscape scale spatial patterns of vegetation in many environments.     

道路边坡绿化防护工程中的生态学原理

随着我国公路和铁路建设的快速发展,公路护坡及山体边坡的绿化工程也日益受到人们的重视并付诸实施。然而,出于急功近利的目的,一些工程并没有按照科学的规律开展工作,结果导致了最终的失败。本文从生态学的观点出发,提出在路坡边坡绿化工程中应遵循的一些生态学原理,如适应性原理、生物多样性原理、生态位原理、生物共生原理、限制因子原理和力能学原理,试图为有关从业人员提供有益的帮助。     

朝鲜南部的Pseudogl yptagnostus(三叶虫)并论朝鲜寒武纪斜坡相的意义

朝鲜南部Ｍａｃｈａｒｉ组Ｏｌｅｎｏｉｄｅｓ带的Ａｇｎｏｓｔｕｓ（Ｐｔｙｃｈａｇｎｏｓｔｕｓ？）ｏｒｉｅｎｔａｌｉｓ Ｋｏｂａｙａｓｂｈｉ一种应归于Ａｇｎｏｓ－ｔｏｔｅｓ（Ｐｓｅｕｄｏｇｌｙｐｔａｇｎｏｓｔｕｓ）Ｌｕ,１９６４一属,时代是晚寒武世长山期,不是早期中寒琥世,小林贞一的Ｏｌｅｎｏｉｄｅｓ带是中及晚寒武三叶虫混杂在一起的一个化石带。他建立的该组５个化石带也有问题。Ｃｏｒｅｏｌｅｎｕｓ,Ｃｈ     

基于城市微气候模拟软件的城市道路绿化带对PM2.5消减作用的研究

随着经济的快速发展及机动车保有量的持续增长,车辆造成的道路污染问题日益严重。广州作为中国重要的经济发展城市,交通源排放问题高度集中,机动车排放是城市PM2.5的主要来源之一,开展减缓城市道路污染危害的研究具有重要意义。本研究为调查绿化带对广州城市道路PM2.5的影响,运用实测与城市微气候模拟软件（ENVI-met）模拟结合的研究方法,实测并分析城市道路空间PM2.5的浓度分布及其影响因素,使用实测数据对模拟软件进行验证分析,模拟研究理想道路模型下不同高宽比、风向等因素及绿化带植配类型对PM2.5的消减作用。研究表明：（1）城市道路空间PM2.5浓度分布受污染源、街道高宽比、风速风向、绿化带等综合影响,自然消减情况下,其主要受风速风向和高宽比双因素影响;（2）通常街道高宽比越大,越有利于道路空间PM2.5的扩散;（3）城市道路空间PM2.5自然沉降最小距离为12 m,0-12 m范围内应保持无障碍物的开敞环境,PM2.5消减的关键范围是12-24 m,此范围内可以利用生态手段沉降颗粒物;（4） PM2.5消减率受绿化带和风向的双控制,应根据主导风向选择绿化带植配方式。在主导风平行面和垂直迎风面绿化带对PM2.5有正消减效应,建议植配类型为"乔-乔+灌+草";在主导风垂直背风面绿化带对PM2.5呈负消减效应,植配类型为"乔-灌"绿化带消减率接近于自然消减率,而植配类型为"乔-灌+草"和"乔-乔+灌+草"的绿化带加重了颗粒物在该区域的积聚。     

升温突变对川西不同坡向和海拔岷江冷杉径向生长的影响

坡向和海拔作为重要的地形因子决定着林木立地条件的水热分配,为揭示川西地区升温突变前后制约岷江冷杉(Abies fargesii var.faxoniana)径向生长的气候因子变化及其在坡向和海拔上的响应格局,通过树木年轮学方法构建了4个坡向(NE、N、NW和W)的3个海拔梯度(≥3650 m)共12个岷江冷杉的标准年表,采用皮尔逊相关分析和回归分析的方法分析了升温突变前后(1980年)限制岷江冷杉径向生长主要气候因子的变化及径向生长的变化趋势。结果表明：升温前,生长季(7月)低温和降水、前一年冬季(10—11月)最高温和平均温制约岷江冷杉的生长,而当年春季(3月)温度的升高和生长季前(5月)较多的降水不利于其生长。升温后,4个坡向的林线、东北坡中海拔,西坡中、低海拔岷江冷杉的径向生长与大部分月温度表现为正相关关系,且上述样点树木径向生长明显加速。1980年升温前,制约不同样点岷江冷杉径向生长的气候因子具有一致性——坡向和海拔对其径向生长与温度相关关系的干扰和影响较小。增温促进了各坡向林线岷江冷杉的径向生长,且偏阳坡在更大的海拔范围内对增温表现出正反馈。研究对未来气候变化背景下川西不同坡...