新疆的短命植物（三）群落学意义和资源价值

在中亚西部荒漠亚区,短命植物种类丰富（乌兹别克斯坦即有２５０种之多）,且发育繁茂。由其所形成的草群,外貌状若草甸、草原或荒漠,曾被一些早期的地植物学家描述为不同的植物群落类型。我国的植物学工作者,对局部地段或小生境中群集生长的短命植物草被现象,常称之为“小群落”或“群聚现象”,在文献中也从不使用短命荒漠、短命草甸、萨旺纳或半萨旺纳等植物群落类型的名称。新疆的短命植物总是或多或少地出现在某些植物群落之中,所以我们更加强调它的群落学意义。在新疆北部的莫索湾沙区,短命植物种类占白梭梭群落全部种类组成的…     

论古尔班通古特沙漠植物多样性的一般特点

古尔斑通古特沙漠处于中亚荒漠与内亚（亚洲中部）荒漠之间的过渡,其气候虽以干旱少雨、蒸发强烈、多风、日照强、温度变化剧烈的大陆性荒漠气候为特点,但由于降水季节分配较均匀,冬春有一定雨雪,植被相对较为茂密,以固定和半固定沙漠为主,共采集记录到２０８种高等植物,１８个植物群落类型,ｌｌ类植物生活型。植物多样性还包括下列一般特点：区系地理成分多样,但中亚成分占优势;有少量古老种,特有现象微弱,黎科植物占明显优势;早生植物为主;长营养期１年生植物有一定比例;短命和类短命植物获得发育等。由于近几十年来的过牧（牲畜的“冬窝子”）和滥采滥挖燃料及有经济价值的植物,植物多样性受破坏严重。当前的紧迫任务是加强保护,对有些物种还须采取措施,进行抢救。     

新疆的短命植物（一）独特的生态生物学特点

短命植物又称短营养期植物、短期生植物。它包括当年完成其生活周期、整个植株干枯死亡,来年春季再由种子形成新个体的一年生短命植物;也包括植株当年生地上部分枯死,而地下器官则处于休眠状态,到第二年春天既可由种子繁殖新个体,也能从地下芽生长出新植物体的多年生短命植物。前者称为短命植物,后者叫做类短命植物。原苏联的中亚地区,是短命植物区系的现代分布中心。在我国,它集中分布于新疆北部的山前平原及低山丘陵地带,是新疆植物区系组成的一个独特类群,在学术上和生产实践中都受到人们的关注。不同的植物适应环境的方式各种…     

新疆准噶尔荒漠短命植物群落特征及其水热适应性

短命植物是一类利用短暂湿季快速生长的特殊植物类群, 包括一年生短命植物和类短命植物。作者在新疆北部准噶尔荒漠的莫索湾地区从2005-2008年进行了连续4年的群落调查研究, 通过25条样线201个样方的调查, 并结合同时段冬春季节的气温、降水资料, 探讨了短命植物对环境水热变化的适应性特征。结果表明: (1) 早春季节, 短命植物在准噶尔荒漠植物群落组成中占据优势地位, 物种数均占调查总物种数的52%左右; (2) 从群落优势种来看, 7种植物标准频度在40%以上, 其中6种是短命植物, 分别是旱麦草(Eremopyrum orientale)、卷果涩芥(Malcolmia scorpioides)、硬萼软紫草(Arnebia decumbens)、狭果鹤虱(Lappula semiglabra)、四齿芥(Tetracme quadricornis)和沙滨藜(Atriplex dimorphostegia); (3) 群落中短命植物萌发的个体数量与前一年冬季温度关系极为密切, 较低的冬季温度更易激发其萌发, 而当年群落外貌特征则更多地依赖于早春季节的降水, 若早春季节温度过低也会影响短命植物的萌发; (4) Shannon-Wiener多样性指数和Pielou均匀度指数年际间变化趋势与同期冬春降水总量变化趋势一致。总之, 温度和降水的不同配置是引起短命植物多样性发生年际变化的主要因素。     

新疆菊科短命植物异喙菊的解剖学研究

“短命”植物生活周期短,逃避干旱季节,是干旱区植被组成中一类特殊的草本植物。我国天山以北,古尔班通古特沙漠边缘生长有大量的短命植物。在这些地区年降水量虽少,但冬季有积雪,春季有一定的降雨:春夏期间,土壤湿润,为具浅根系的“短命”植物整个生长发育时期提供了十分有利的水份供应。尤其在冬季严寒已过,夏季酷热未到的春季,其气候可满足“短命”植物进行高效光合生产的需要,较大的日温差,     

梭梭萌生与初期存活的关键影响因素

在梭梭的主要分布区——古尔班通古特沙漠南缘,就种子萌发、幼苗存活展开研究,以确定在梭梭萌生初期,决定其成活的关键影响因素。实验于2008年36月进行,设置了9个水分处理(3倍降雪、正常降雪、无降雪条件与人工降雨、自然降雨、无降雨处理的交叉组合),同步监测梭梭萌发、存活数量动态及春季短命植物数量。结果表明,梭梭种子萌发数量与积雪量增加无显著相关关系,短命植物萌发数量与积雪量呈显著正相关。总体水分条件较好时,梭梭幼苗与短命植物萌发数量都增多,但由于短命植物竞争,幼苗成活率未必高;反之,在水分条件较差时,梭梭幼苗与短命植物萌发数量都降低,短命植物消耗的水分减少,梭梭幼苗存活率反而高。也就是说,在梭梭幼苗的生长初期,它在与短命植物的水分竞争中处于劣势,直接的降水增加并不能提高其存活率。     

古尔班通古特沙漠南缘3种生活型草本植物生物量分配及相关生长关系

为了解古尔班通古特沙漠不同生活型草本植物的生物量分配特征,通过取样调查当地34种草本植物的生物量研究表明：（1）采集到的每个物种样本的总生物量大多小于4 g,其中多数个体（大于80%）的地上与地下生物量分别在2和0.5 g以内,根冠比主要集中在0.25以内;（2）类短命植物向地下部分分配较多生物量,根冠比较大,集中分布在1.67左右;短命和一年生长营养期草本向地下部分配的生物量远小于类短命植物,两者的根冠比较小,主要集中在0.15左右;（3）短命植物地下与地上部生物量间为等速生长关系,而类短命植物和一年生长营养期草本植物地下与地上生物量间为异速生长关系,其中类短命植物随个体增大向地下部分配生物量的比例增多,而一年生长营养期草本则相反。综上所述,短命、类短命和一年生长营养期草本植物地下与地上生物量间具有不同的分配特征,与各自独特的生活史特征相一致。     

民勤沙区几种荒漠植物群落的现实生态位研究

民勤沙区属于典型的干旱荒漠气候,植被以灌木荒漠为主,盖度一般只有5%~15%.植物群落内生态位宽度悬殊,植物种之间的生态位相似比例很小.生态位宽度和生态位相似比例小是受制于干旱荒漠生境条件的结果,是干旱荒漠生态环境中稀疏荒漠植物的主要特征之一.植物的现实生态位宽度与年际降水量关系密切,在地貌、土壤颗粒、土壤水分、土壤养分等影响因子中,土壤水分是主导因子.当地地下水位深20 m左右,植物无法利用,植物种之间对资源的竞争主要表现为对水分资源的竞争,降水资源是植物种之间竞争的关键资源.同一种植物在不同群落中的生态位宽度变幅较大,不同群落内部植物种竞争关系的差异是由物种的生态位和由相对稳定的地貌、土壤条件以及随年际变动的降水条件共同作用的结果.群落中的优势种植物的生态位最宽,当优势种生态位减小时,一年生短命植物往往会进入群落中.荒漠植物的冠层单一,以冠幅占样方面积比作为植物的特征值计算其生态位特征值比较准确可靠.     

两种短命植物春萌秋萌个体生态生物学特征比较

短命植物是新疆北部荒漠生态系统中重要组成部分,对稳定该区沙漠生态系统、丰富物种多样性具有重要的意义。以往对短命植物的研究多集中在春季萌发的短命植物,秋季萌发的短命植物研究很少,对秋季萌发短命植物和春季萌发短命植物的生态生物学特征的异同以及它们对稳定荒漠生态系统的意义缺乏了解。选择小车前(Plantago minuta)和尖喙牻牛儿苗(Erodium oxyrrhynchum)为研究对象,采用野外定点标记观测和室内分析结合的方法,研究了两种短命植物春季萌发和秋季萌发两种表现型在冠幅、生物量、物候期、菌根侵染率等生态生物学特征方面的差异性。结果表明:秋季萌发的小车前和尖喙牻牛儿苗能够在覆雪下越冬,其单株的冠幅、叶片数量、干重等均远远大于同一时期生长的春季萌发的小车前和尖喙牻牛儿苗,尤其是单株结种数量更是比春季萌发小车前和尖喙牻牛儿苗的高13.0和4.4倍;秋季萌发的小车前和尖喙牻牛儿苗的花期分别比春季萌发小车前和尖喙牻牛儿苗早14和7 d,植株黄枯期和成熟期分别提早3和4 d;此外,秋季萌发小车前和尖喙牻牛儿苗各时期的菌根侵染率也显著高于同期春季萌发小车前和尖喙牻牛儿苗。本研究得到以下结论:秋季萌发的小车前和尖喙牻牛儿苗在稳定和扩大其后代种群繁衍能力、提高防风固沙能力、稳定荒漠生态系统等方面具有重要意义。     

南极菲尔德斯半岛南部植被类型,群落物种多样性及其保护

根据群落的种类组成、外貌和结构、生态因素将菲尔德斯半岛南部(包括阿德雷岛)的植被划分为冻原、草甸、沼泽、水生植被四大类型。对下属的群系和群丛进行了描述。这些群落的形成与分布主要依赖于水分状况和基质的稳定与否。论述了从海边到内陆的山顶群落的分布规律、植被特点,并对不同群系、生境进行了群落植物的丰富度(物种数)、均匀度和多样性对比。从对比结果提出对保护工作的建议。     

Fire season effects on the recruitment of non‐sprouting serotinous Proteaceae in the eastern (bimodal rainfall) fynbos biome,South Africa

Abstract Research in Mediterranean‐climate shrublands in both South Africa and Australia shows that recruitment of proteoid shrubs (non‐sprouting, serotinous Proteaceae) is best after warm‐season (summer and autumn) fires and worst after cool‐season (winter and spring) ones. This pattern has been attributed to post‐dispersal seed attrition as well as size of pre‐dispersal seed reserves. Here we investigate patterns of post‐fire recruitment for four proteoid species in the eastern part of South Africa's fynbos biome, which has a bimodal (spring and autumn) rainfall regime. Despite the lack of significant differences in recruitment between cool‐ and warm‐season burns, we find some evidence for favourable recruitment periods following fires in spring and autumn, immediately before, and coinciding with, the bimodal rainfall peaks. This suggests that enhanced recruitment is associated with conditions of high soil moisture immediately after the fire, and that rapid germination may minimize post‐dispersal seed attrition. In two of the species, we also find a shift from peak flowering in winter and spring in the Mediterranean‐climate part of the fynbos biome, to summer and autumn flowering in the eastern part. Because these two species are only weakly serotinous, warm‐season flowering would result in maximal seed banks in spring, which could explain the spring recruitment peak, but not the autumn one. We conclude that eastern recruitment patterns differ significantly from those observed in the western and central parts of the biome, and that fire management protocols for the east, which are currently based on data and experience from the winter‐rainfall fynbos biome, need to be adjusted accordingly. Fire managers in the eastern fynbos biome should be less constrained by requirements to burn within a narrow seasonal range, and should therefore be in a better position to apply the required management burns.     

The leaf anatomy of a broad-leaved evergreen allows an increase in leaf nitrogen content in winter

In temperate regions, evergreen species are exposed to large seasonal changes in air temperature and irradiance. They change photosynthetic characteristics of leaves responding to such environmental changes. Recent studies have suggested that photosynthetic acclimation is strongly constrained by leaf anatomy such as leaf thickness, mesophyll and chloroplast surface facing the intercellular space, and the chloroplast volume. We studied how these parameters of leaf anatomy are related with photosynthetic seasonal acclimation. We evaluated differential effects of winter and summer irradiance on leaf anatomy and photosynthesis. Using a broad-leaved evergreen Aucuba japonica , we performed a transfer experiment in which irradiance regimes were changed at the beginning of autumn and of spring. We found that a vacant space on mesophyll surface in summer enabled chloroplast volume to increase in winter. The leaf nitrogen and Rubisco content were higher in winter than in summer. They were correlated significantly with chloroplast volume and with chloroplast surface area facing the intercellular space. Thus, summer leaves were thicker than needed to accommodate mesophyll surface chloroplasts at this time of year but this allowed for increases in mesophyll surface chloroplasts in the winter. It appears that summer leaf anatomical characteristics help facilitate photosynthetic acclimation to winter conditions. Photosynthetic capacity and photosynthetic nitrogen use efficiency were lower in winter than in summer but it appears that these reductions were partially compensated by higher Rubisco contents and mesophyll surface chloroplast area in winter foliage.     

Fire season and intensity affect shrub recruitment in temperate sclerophyllous woodlands

The season in which a fire occurs may regulate plant seedling recruitment because of: (1) the interaction of season and intensity of fire and the temperature requirements for seed release, germination and growth; (2) post-fire rainfall and temperature patterns affecting germination; (3) the interaction of post-fire germination conditions and competition from surrounding vegetation; and (4) the interaction of post-fire germination conditions and seed predators and/or seedling herbivores. This study examined the effects of different fire intensities and fire seasons on the emergence and survival of shrubs representing a range of fire response syndromes from a summer rainfall cool climate region. Replicated experimental burns were conducted in two seasons (spring and autumn) in 2 consecutive years and fuel loads were increased to examine the effects of fire intensity (low intensity and moderate intensity). Post-fire watering treatments partitioned the effects of seasonal temperature from soil moisture. Higher intensity fires resulted in enhanced seedling emergence for hard-seeded species but rarely influenced survival. Spring fires enhanced seedling emergence across all functional groups. Reduced autumn recruitment was related to seasonal temperature inhibiting germination rather than a lack of soil moisture or competition. In Mediterranean-type climate regions, seedling emergence has been related to post-fire rainfall and exposure of seeds to seed predators. We think a similar model may operate in temperate summer rainfall regions where cold-induced dormancy over winter exposes seeds to predators for a longer time and subsequently results in recruitment failure. Our results support the theory that the effect of fire season is more predictable where there are strong seasonal patterns in climate. In this study seasonal temperature rather than rainfall appears to be more influential.     

毛乌素沙地沙丘土壤含水量特点——兼论老固定沙地上油蒿衰退原因

土壤表面干沙层在冬春少雨季节较厚,流动沙地的又明显地大于固和地的。流动沙地地表干沙层以下的土壤含水量一般在于同深化度固定沙地的,特别是在报系密集分布的土层。科季或早春土壤含水量比较低,雨季的明显较高,雨季结束后,土层中的水分在重力的作用下会向深层运动,导致根系层土壤含水量下降。在植物生长季,缺少降雨时,因少地的土土壤水量会因植物的蒸腾消耗而变得很低（１％～２％）,而流动沙地的不受或受此影响很小。地     

Soil moisture mediates association between the winter North Atlantic Oscillation and summer growth in the Park Grass Experiment

Several aspects of terrestrial ecosystems are known to be associated with the North Atlantic Oscillation (NAO) through effects of the NAO on winter climate, but recently the winter NAO has also been shown to be correlated with the following summer climate, including drought. Since drought is a major factor determining grassland primary productivity, the hypothesis was tested that the winter NAO is associated with summer herbage growth through soil moisture availability, using data from the Park Grass Experiment at Rothamsted, UK between 1960 and 1999. The herbage growth rate, mean daily rainfall, mean daily potential evapotranspiration (PE) and the mean and maximum potential soil moisture deficit (PSMD) were calculated between the two annual cuts in early summer and autumn for the unlimed, unfertilized plots. Mean and maximum PSMD were more highly correlated than rainfall or PE with herbage growth rate. Regression analysis showed that the natural logarithm of the herbage growth rate approximately halved for a 250 mm increase in maximum PSMD over the range 50-485 mm. The maximum PSMD was moderately correlated with the preceding winter NAO, with a positive winter NAO index associated with greater maximum PSMD. A positive winter NAO index was also associated with low herbage growth rate, accounting for 22% of the interannual variation in the growth rate. It was concluded that the association between the winter NAO and summer herbage growth rate is mediated by the PSMD in summer.     

增加降水对荒漠短命植物当年牧草生长及群落结构的影响

通过模拟降水增加试验研究了古尔班通古特荒漠常见短命植物盖度、密度及产量对水分输入量增加的响应.结果表明:尖喙牻牛儿苗、弯果胡卢巴、角果藜、琉苞菊、条叶庭芥及囊果苔草6种牧草生物量总和占总生物量的60%以上,是荒漠草原的优势牧草植物;供水量增加显著促进了角果藜、尖喙牻牛儿苗、弯果胡卢巴、条叶庭芥和琉苞菊5种牧草植物的个体生长;在自然降水的基础上,增加40mm和80mm供水使这5种植物生物产量比对照增加86%～230%.供水增加后,6种重要牧草对整个群落的生物贡献比例发生很大变化,只有角果藜和尖喙牻牛儿苗的贡献比例规律性增加,分别比对照增加了58%和11%,表明2种植物对供水增加的环境变化适应能力强;供水量增加促进了弯果胡芦巴、尖喙牻牛儿苗和角果藜3种植物N、P和K养分的吸收量;与此同时,供水量增加也显著提高了荒漠短命植物的密度和盖度.在降水增加的背景下,古尔班通古特沙漠南缘荒漠短命植物群落结构发生改变,植被盖度和群落净初级生产力提高,这对于防风固沙、稳定沙面,增加荒漠草原载畜能力有着积极的意义.     

Simulated climate change reduced the capacity of lichen-dominated biocrusts to act as carbon sinks in two semi-arid Mediterranean ecosystems

The importance of biological soil crusts (biocrusts) for the biogeochemistry of drylands is widely recognized. However, there are significant gaps in our knowledge about how climate change will affect these organisms and the processes depending on them. We conducted a manipulative full factorial experiment in two representative dryland ecosystems from central (Aranjuez) and southeastern (Sorbas) Spain to evaluate how precipitation, temperature and biocrust cover affected the assimilation and net C balance of biocrusts. Chlorophyll fluorescence, net photosynthesis and dark respiration were measured in situ bimonthly during a year. We also conducted daily cycle measurements of net photosynthesis in winter and at the end of spring. In Sorbas, warming reduced the fixation of atmospheric C in biocrust-dominated microsites throughout the year. In Aranjuez, there was an interaction between the three factors evaluated; during winter, net photosynthesis was significantly greater in high biocrust cover plots under natural conditions and in the rainfall exclusion treatment. During the daily surveys, rainfall exclusion and warming reduced C fixation in Sorbas and in Aranjuez respectively. The effects of the treatments evaluated varied with the rainfall and non-rainfall water inputs (NRWIs) registered before the measurements. Our results suggest that changes in NRWI regimes as consequence of warming could have a greater impact on the C balance of biocrusts than changes in rainfall amounts. They also indicate that climate change may reduce the photosynthetic ability of lichens, with a consequent reduction of their dominance in biocrust communities at the mid to long term. This could reduce the ability of dryland ecosystems to fix atmospheric C.     

Seasonality of canopy invertebrate communities in eucalypt forests of eastern and western Australia

Abstract Chemical knockdown procedures were used to sample canopy arthropods at 3 month intervals over 1 year at two sites, one in eastern Australia and the other in western Australia. Samples were taken from narrow-leaved ironbark, Eucalyptus crebra, and grey box, Eucalyptus moluccana, in the east and from jarrah, Eucalyptus marginata, and marri, Eucalyptus calophylla, in the west. Arthropods were more abundant on trees in eastern Australia and exhibited different seasonal patterns from those in the west. Members of different functional groups exhibited different seasonal patterns, with some herbivorous groups responding to times of leaf production, decomposers and fungus feeders responding to high moisture availability, and predators/parasites responding to the abundance of food items. Seasonal variability was slightly higher in the west, possibly reflecting the greater seasonal amplitude in rainfall. In the eastern forest, proportionately more taxa peaked in spring or summer and declined to minimum numbers in winter. In the western forest several taxa attained peak numbers in autumn, winter or spring, while others declined to minimum values in winter or summer. The phenological patterns of canopy arthropods appear to be linked to the condition of the host plant and/or to climatic factors. Comparison of the western Australian data to those from a second year of sampling at a time when rainfall was greater and fell later into the season indicated that variability in arthropod numbers between years can be as great as that between seasons. Implications of the variability in seasonal and annual patterns of canopy invertebrate communities are discussed in relation to the need for long-term sampling and in relation to evaluating the impact of disturbance on forest communities.     

Annual variation in soil respiration and its components in a coppice oak forest in Central Italy

In order to investigate the annual variation of soil respiration and its components in relation to seasonal changes in soil temperature and soil moisture in a Mediterranean mixed oak forest ecosystem, we set up a series of experimental treatments in May 1999 where litter (no litter), roots (no roots, by trenching) or both were excluded from plots of 4 m². Subsequently, we measured soil respiration, soil temperature and soil moisture in each plot over a year after the forest was coppiced. The treatments did not significantly affect soil temperature or soil moisture measured over 0–10 cm depth. Soil respiration varied markedly during the year with high rates in spring and autumn and low rates in summer, coinciding with summer drought, and in winter, with the lowest temperatures. Very high respiration rates, however, were observed during the summer immediately after rainfall events. The mean annual rate of soil respiration was 2.9 µ mol m^?2 s^?1, ranging from 1.35 to 7.03 µmol m^?2 s^?1. Soil respiration was highly correlated with temperature during winter and during spring and autumn whenever volumetric soil water content was above 20%. Below this threshold value, there was no correlation between soil respiration and soil temperature, but soil moisture was a good predictor of soil respiration. A simple empirical model that predicted soil respiration during the year, using both soil temperature and soil moisture accounted for more than 91% of the observed annual variation in soil respiration. All the components of soil respiration followed a similar seasonal trend and were affected by summer drought. The Q₁₀ value for soil respiration was 2.32, which is in agreement with other studies in forest ecosystems. However, we found a Q₁₀ value for root respiration of 2.20, which is lower than recent values reported for forest sites. The fact that the seasonal variation in root growth with temperature in Mediterranean ecosystems differs from that in temperate regions may explain this difference. In temperate regions, increases in size of root populations during the growing season, coinciding with high temperatures, may yield higher apparent Q₁₀ values than in Mediterranean regions where root growth is suppressed by summer drought. The decomposition of organic matter and belowground litter were the major components of soil respiration, accounting for almost 55% of the total soil respiration flux. This proportion is higher than has been reported for mature boreal and temperate forest and is probably the result of a short‐term C loss following recent logging at the site. The relationship proposed for soil respiration with soil temperature and soil moisture is useful for understanding and predicting potential changes in Mediterranean forest ecosystems in response to forest management and climate change.