新疆塔里木河下游荒漠河岸(林)植被合理生态水位

 该文依据塔里木河下游地下水位多年监测资料, 将地下水位按不同埋深划分为0~2、2~4、4~6、6~8、8~10和>10 m 6个梯度, 并设置植 被调查样方进行连续监测, 以分析地下水位变化对植物物种多样性与种群生态位的影响。研究结果表明: 在地下水位2~4 m时, 物种多样性最高 , 其次为4~6 m, 再次为0~2 m; 当地下水位在6 m以下时, 物种多样性锐减, Hill多样性指数曲线变化趋势趋于平直化。荒漠河岸(林)植被主要 植物种群生态位随着地下水位的逐步下降而扩展, 并在地下水位4~6 m处达到最宽; 尔后, 生态位又显著变窄; 地下水位4~6 m时, 种群间生态 位重叠最不显著, 物种数较为丰富。因此, 该文分析得出结论: 塔里木河下游植被恢复的地下水位应确保达到6 m以上, 大部分地区地下水位应 维持在4~6 m, 而部分河道附近地区地下水位争取达到2~4 m。     

Responses of saltcedar (<Emphasis Type="Italic">Tamarix chinensis</Emphasis>) to water table depth and soil salinity in the Yellow River Delta,China

Significant studies about Tamarix chinensis as an introduced invasive plant species have been implemented in North America. However, the response of native T. chinensis to its environment is not well known in China. T. chinensis is a useful species in preventing sea water intrusion in coastal areas of northern China. It is necessary to fully understand the relationships between environmental conditions and ecological characteristics of this species to better preserve its habitats. The Yellow River Delta Natural Reserve, one of the major distribution regions of T. chinensis, was then selected as a case study area to investigate the response of this species to water table depth and soil salinity (Na⁺, Cl⁻, Mg²⁺). It was found that sites with shallow water table depths (less than 1.5 m) and low soil salinity (less than 30 psu), provided the best habitat conditions for T. chinensis. The results also showed that plant height, stem diameter, and crown width were all positively correlated to plant age, while they had negative correlations with water table depth. Negative correlations between plant height and soil salinity, plant stem diameter and soil salinity were also concluded. However, no obvious relationship between the crown breadth of T. chinensis and soil salinity was observed. Four types of T. chinensis habitats were obtained based on the ecological characteristics of T. chinensis individuals associated with soil salinity and water table depth, i.e., (1) Low water table with high soil salinity; (2) Deep water table with high soil salinity; (3) Deep water table with low soil salinity; (4) Inundation with low salinity. These results provide a sound basis for wetland management in the Yellow River Delta.     

民勤绿洲边缘地下水位变化对植物种群生态位的影响

在民勤绿洲边缘,利用空间区域不同地下水位(湖区8～12m,泉山区15～17m,坝区20～23m)和时间序列(1984～1992年)民勤沙井子地区地下水位下降(7.45～11.65m)梯度,研究地下水位下降对荒漠植物种群生态位的影响。结果表明:空间区域地下水位下降,植物种群生态位宽度均减小,种群退化;时间序列地下水位下降,白刺种群在扩展,其它植物种群在退化。白刺种群生态位宽度在民勤绿洲边缘荒漠植物群落中最大,是该区的建群种。由于白刺种群在地下水位7.45～11.65m范围内扩展,民勤绿洲生态环境治理中地下水位达到该范围是一个主要目标。     

物种多样性及生物量与地下水位的关系——以海流兔河流域为例

以3条样带上117块植被群落调查样方为基础资料,研究了海流兔河流域植被物种多样性及生物量与地下水位之间的关系。结果表明:1)地下水位高低及地貌类型均会影响草本层植物群落组成及优势种构成。滩地样地中,随地下水位降低,优势草本的更替方向为寸草,芨芨草,马蔺,狗尾草,碱茅;沙坡样地中,优势草本的更替方向为大针茅,沙鞭,沙蓬,沙打旺。2)地下水位为1.5 m时是草本植物群落生长发育最适宜区域,物种多样性及丰富度达到最大,而灌木层物种多样性及丰富度随地下水位下降呈现波动变化的特征;当地下水位埋深小于5.0 m时,草本层物种多样性及丰富度明显高于灌木层,在地下水位埋深大于5.0 m时,草本层物种多样性指数开始出现低于灌木层的现象。3)草本植物多样性及丰富度和生物量之间关联性不强,滩地样地中,草本层地上生物量及地下生物量在地下水位为1.8 m时具有最大值,但植物群落结构较为单一;沙坡样地中,地上生物量最大值出现在地下水位为5.0 m的区域内,而地下生物量最大值出现在地下水位为3.5 m时。综上,物种多样性、地上及地下生物量与地下水位都不是简单的线性关系,而是有一个最适水位;高于或低于这个最适水位,多样性和生物量都会下降。     

Changes in fossil chironomid remains along a depth gradient: evidence for common faunal thresholds within lakes

Many environmental variables that are important for the development of chironomid larvae (such as water temperature, oxygen availability, and food quantity) are related to water depth, and a statistically strong relationship between chironomid distribution and water depth is therefore expected. This study focuses on the distribution of fossil chironomids in seven shallow lakes and one deep lake from the Plymouth Aquifer (Massachusetts, USA) and aims to assess the influence of water depth on chironomid assemblages within a lake. Multiple samples were taken per lake in order to study the distribution of fossil chironomid head capsules within a lake. Within each lake, the chironomid assemblages are diverse and the changes that are seen in the assemblages are strongly related to changes in water depth. Several thresholds (i.e., where species turnover abruptly changes) are identified in the assemblages, and most lakes show abrupt changes at about 1–2 and 5–7 m water depth. In the deep lake, changes also occur at 9.6 and 15 m depth. The distribution of many individual taxa is significantly correlated to water depth, and we show that the identification of different taxa within the genus Tanytarsus is important because different morphotypes show different responses to water depth. We conclude that the chironomid fauna is sensitive to changes in lake level, indicating that fossil chironomid assemblages can be used as a tool for quantitative reconstruction of lake level changes.     

Life on the edge – to which degree does phreatic water sustain vegetation in the periphery of the Taklamakan Desert?

Questions: Do the vegetation‐specific patterns in the forelands of river oases of the Taklamakan Desert provide clues to the degree to which a vegetation type depends on unsaturated soil moisture, brought about by extensive floodings, or phreatic water? Location: Foreland of the Qira oasis on the southern rim of the Taklamakan Desert, Xinjiang Uygur Autonomous Region, China. Methods: A vegetation map was prepared using a SPOT satellite image and ground truthing. Measurements of soil water contents were obtained from a flooding experiment and transformed into water potentials. Sum excedance values were calculated as the percentage of days on which different thresholds of soil water potentials were transgressed. Groundwater depth was mapped by drilling 30 groundwater holes and extrapolating the distances to the whole study area. Results: The vegetation was characterized by only six dominant or codominant species: Alhagi sparsifolia, Karelinia caspia, Populus euphratica, Tamarix ramosissima, Calligonum caput‐medusae and Phragmites australis. The vegetation patterns encountered lacked any linear features typical of phreatophytes, thus not allowing direct conclusions on the type of the sustaining water sources. Soil water potentials never transgressed a threshold of pF 5 (?10 MPa) in horizons above the capillary fringe during periods without inundation, thus representing water not accessible for plants. Depth to the groundwater ranged between 2.3 and 17.5 m among plots and varied between 1.7 and 8.0 m within a plot owing to dune relief. The seven main vegetation types showed distinct niches of groundwater depths, corresponding to the observed concentric arrangement of vegetation types around the oasis. Conclusions: Inundation by flooding and unsaturated soil moisture are irrelevant for the foreland vegetation water supply. Although distances to the groundwater table can reach about 20 m, which is exceptionally large for phreatophytes, groundwater is the only water source for all vegetation types in the oasis foreland. In consequence, successful maintenance of oasis foreland vegetation will crucially depend on providing non‐declining ground water tables.     

Root growth of soybean (Glycine max L. Merr.) and cowpea (Vigna unguiculata Walp.) on a hydromorphic toposequence in Western Nigeria

Summary The effects of variations in edaphic and hydrologic factors over a short distance on the root growth of soybean cv. Hernon 237 and cowpea cv. IT 82 E-60 were studied in a hydromorphic toposequence. During the growing season the water table (WT) fluctuated from 0.43 to 0.94 m (high), 0.60 to 1.12 m (medium) and 0.72 to 1.51 m (low), respectively in 1983 and from 0.47 to 0.84 m (high), 0.63 to 1.13 m (medium) and 0.83 to 1 20m (low). respectively, in 1984. Poor soil aeration did not limit growth, even for high WT.Root penetration into the deeper soil was prevented at the low and medium water table sites by the presence of a naturally occurring compacted gravel layer at the 0.30–0.40 m depth. The absence of this layer at the high water table site resulted in root growth and proliferation of soybean roots even within the capillary fringe zone immediately above the water table. Cowpea roots, however, were not observed in this saturated soil zone. Cowpea roots penetrated deeper in high than in medium and low WT. Evapotranspiration (Et) and E_t/E_o values of both crops were significantly greater at the high than at medium or low water table.     

Ellenberg’s water table experiment put to the test: species optima along a hydrological gradient

An important aspect of niche theory is the position of species’ optima along ecological gradients. It is widely believed that a species’ ecological optimum takes its shape only under competitive pressure. The ecological optimum, therefore, is thought to differ from the physiological optimum in the absence of interspecific competition. Ellenberg’s Hohenheim water table experiment has been very influential in this context. However, the water table gradient in Ellenberg’s experiment was produced by varying the soil thickness above the water table, which confounded the potentially disparate impacts of water table depth (WTD) and soil depth on species growth. Accordingly, here we have re-evaluated Ellenberg’s work. Specifically, we tested the hypothesis that physiological and ecological optima are identical and unaffected by interspecific interaction. We used the same six grasses as in Ellenberg’s experiments, but in our mesocosms, WTD was varied but soil depth kept constant. The design included both an additive component (with/without plant interaction) and a substitutive component (monocultures vs. species mixtures). The results show that the physiological optima along the hydrological gradient varied greatly between species, even in the absence of interspecific interaction. Within species, however, physiological and ecological optima appeared identical in most cases, irrespective of the competition treatment. We conclude that the ‘physiological capacity’ of species largely determines where they are able to persist and that any impact of interspecific interaction is only marginal. These findings are at variance with Ellenberg’s rule, where competition is considered to shift the distribution of a species away from its physiological optimum.     

Small-scale spatial heterogeneity of arbuscular mycorrhizal fungal abundance and community composition in a wetland plant community

Although it has become increasingly clear that arbuscular mycorrhizal fungi (AMF) play important roles in population, community, and ecosystem ecology, there is limited information on the spatial structure of the community composition of AMF in the field. We assessed small-scale spatial variation in the abundance and molecular diversity of AMF in a calcareous fen, where strong underlying environmental gradients such as depth to water table may influence AMF. Throughout an intensively sampled 2 × 2 m plot, we assessed AMF inoculum potential at a depth of 0–6 and 6–12 cm and molecular diversity of the AMF community using terminal restriction fragment length polymorphism of 18S rDNA. Inoculum potential was only significantly spatially autocorrelated at a depth of 6–12 cm and was significantly positively correlated with depth to water table at both depths. Molecular diversity of the AMF community was highly variable within the plot, ranging from 2–14 terminal restriction fragments (T-RFs) per core, but the number of T-RFs did not relate to water table or plant species richness. Plant community composition was spatially autocorrelated at small scales, but AMF community composition showed no significant spatial autocorrelation. Saturated soils of calcareous fens contain many infective AMF propagules and the abundance and diversity of AMF inoculum is patchy over small spatial scales. An erratum to this article can be found at     

水、盐梯度下黄河三角洲湿地植物种的生态位

利用排序等方法将黄河三角洲湿地19个植物种在水深和土壤盐分梯度下依次排列,并分别划分为低、中、高水深（或土壤盐分）3个生态种组,分析了水、盐梯度下植物种的生态位宽度和生态位重叠.结果表明:水深梯度下,芦苇、盐地碱蓬等中水深生态种组植物种生态位宽度较大,香蒲、穗状狐尾藻等高水深生态种组植物种生态位宽度最小;土壤盐分梯度下,盐地碱蓬、柽柳等高土壤盐分生态种组植物种生态位宽度较大,而中、低土壤盐分生态种组的植物种生态位宽度均较小.水深和土壤盐分梯度下的生态位重叠分别沿着植物种在两种梯度上的排序而规律变化,通常同一生态种组内部植物种的生态位重叠较大,不同生态种组植物种的生态位重叠较小.黄河三角洲湿地植物种在水深、土壤盐分梯度下的生态位分化现象,可能有助于阐释湿地植物共存及带状分布的形成机制.     

The influence of local elevation on the effects of secondary salinity in remnant eucalypt woodlands: Changes in understorey communities

Increasing land salinization in Australia is predicted to lead to severe declines in species diversity in affected areas, and perhaps significant numbers of species extinctions. Much of the diversity that will be lost consists of understorey and mid-storey species, yet the overwhelming majority of research has focussed on salinity tolerance in tree species. We investigated how the presence of a shallow, saline water table affected the understorey species composition, species richness and species diversity in two remnant Eucalyptus wandoo Blakely woodlands in the Western Australian wheatbelt. Species richness and species diversity were significantly lower in areas with a shallow water table at elevations < 0.5 m above the lowest local elevation, compared with both higher elevations and with areas of low elevation without a shallow water table. Species composition (Bray-Curtis similarities) was also significantly different in low elevation, saline areas. At one site, saline areas were colonized by native and alien species that were not present in the surrounding vegetation, yet the community that has developed does not contain either the species or structural diversity of the surrounding system. At the other site, no colonisation of saline areas by new species occurred. Even though small differences in elevation (< 0.5 m) at our study sites were important in moderating the impacts of salinity in areas with a shallow water table, the loss of species diversity, species richness and structural complexity in low-lying elevations indicated that the ecological risk from secondary salinity to species associated only with drainage lines, seasonally wet flats and other low-lying areas is severe. The priority is to identify those vegetation communities that are restricted to only low relative elevations within the landscape and that only occur in remnants predicted to be at a high risk of developing a shallow and saline water table.     

The Effects of Infrared Loading and Water Table on Soil Energy Fluxes in Northern Peatlands

Increased radiative forcing is an inevitable part of global climate change, yet little is known of its potential effects on the energy fluxes in natural ecosystems. To simulate the conditions of global warming, we exposed peat monoliths (depth, 0.6 m; surface area, 2.1 m²) from a bog and fen in northern Minnesota, USA, to three infrared (IR) loading (ambient, +45, and +90 W m^–2) and three water table (–16, –20, and –29 cm in bog and –1, –10 and –18 cm in fen) treatments, each replicated in three mesocosm plots. Net radiation (Rn) and soil energy fluxes at the top, bottom, and sides of the mesocosms were measured in 1999, 5 years after the treatments had begun. Soil heat flux (G) increased proportionately with IR loading, comprising about 3%–8% of Rn. In the fen, the effect of IR loading on G was modulated by water table depth, whereas in the bog it was not. Energy dissipation from the mesocosms occurred mainly via vertical exchange with air, as well as with deeper soil layers through the bottom of the mesocosms, whereas lateral fluxes were 10–20-fold smaller and independent of IR loading and water table depth. The exchange with deeper soil layers was sensitive to water table depth, in contrast to G, which responded primarily to IR loading. The qualitative responses in the bog and fen were similar, but the fen displayed wider seasonal variation and greater extremes in soil energy fluxes. The differences of G in the bog and fen are attributed to differences in the reflectance in the long waveband as a function of vegetation type, whereas the differences in soil heat storage may also depend on different soil properties and different water table depth at comparable treatments. These data suggest that the ecosystem-dependent controls over soil energy fluxes may provide an important constraint on biotic response to climate change.     

河套灌区干渠衬砌对地下水及生态环境的影响

采用统计学方法、普通克里格法和ArcGIS 9.0等工具,分析了2001和2009年9月内蒙古河套灌区地下水位埋深和矿化度的时空分布,并实地调查了杨家河干渠衬砌对植被分布的影响.结果表明：节水灌溉工程实施多年后,河套灌区年均引水量降为44.5×10⁸ m³（2009年）;浅层地下水埋深在2.5～3.0 m的区域面积由2001年9月的1.2×10⁴ hm²增至2009年9月的9.11×10⁴ hm²,浅层地下水埋深在2.0～2.5 m的区域面积（2009年9月）占灌区总面积的80%;灌区西北部的咸水带（2001年9月,矿化度>5000 mg·L^-1）变为半咸水带（2009年9月,矿化度在3000～5000 mg·L^-1）;乌拉特灌域的咸水带面积扩大,半咸水带呈扇形向灌区北部扩张;渠道衬砌后,两岸植物物种和多样性指数均降低,一些根系较浅的草本植物出现退化的迹象.灌区引水量的减少,并没有对保持乌梁素海现状水面面积产生负面影响.     

Community and species responses to water level fluctuations with reference to soil layers in different habitats of mid-boreal mire complexes

The present paper discusses water level fluctuations in different parts of boreal mire complexes (eleven localities), mainly aapa mire complexes, on the basis of measurements performed by means of shallow observation wells and a few deeper observation tubes (piezometers) in the coastal half of the southern aapa mire zone in Finland. The sites represented intact vegetation from 12 different habitat types (communities), which were divided a priori into habitats with a stable surface moisture status (stable habitats) and into habitats with an unstable surface moisture status (unstable habitats). In stable habitats water level fluctuations took place according to the acrotelm–catotelm model, but the unstable habitats clearly deviated from the general pattern: water level fluctuations in them were not at all concentrated to the surficial, porous peat layer. Direct gradient analysis was used for arranging the communities along the water level fluctuation gradient. Variability of the water table, using 80% amplitude of water table residence, was used for the arrangement. The gradient was split into three groups: (1) habitats with a slightly fluctuating water table, (2) habitats with a considerably fluctuating water table and (3) habitats with an extremely fluctuating water table. The last group nearly corresponded to aro wetlands, and represented a very special habitat type. Indirect gradient analysis (NMDS ordination) also revealed the water level fluctuation gradient along with the gradient of traditional water level categories. According to the results of direct and indirect gradient analysis, the water level fluctuation seems to be an independent and important vegetation gradient. In peatlands, it occurs alongside with the traditional gradient of water level categories reflecting the mean water table. The responses of species to the range of water level fluctuations seem to reflect their tolerance to disturbances and evidently to seasonal drought. Most Sphagnum species are absent or in poor condition in habitats with extremely fluctuating water table. Vascular plant species that experienced most extreme water level fluctuations (Carex nigra, Juncus filiformis) have earlier been regarded as disturbance indicators. In addition, the difference between the piezometric water level and simultaneously measured water table depth reached the highest values within the habitats of those species (i.e., within Polytrichum commune aro wetlands) showing the downward direction of water movement in sandy mineral soil.     

Phenology of five tree species of a tropical dry forest in Yucatan, Mexico: effects of environmental and physiological factors

In order to relate phenological responses of trees to environmental variables we recorded the phenological patterns and select morphological and physiological traits (wood density and water potentials) of five tree species (Acacia gaumeri, Apoplanesia paniculata, Bursera simaruba, Gymnopodium floribundum, and Diospyros cuneata) in the tropical dry deciduous forest of the National Park of Dzibilchaltún, Yucatan, Mexico, over a period of 2 years (2004 and 2005). We chose two sites: one close to a permanent water source, locally known as ‘cenote’ (the CC site, ground water table was found at 2 m) and the other far from the cenote (FC site ground water table was at a depth of 10 m). Sites mainly differed in soil depth (FC site having greater soil depth) and soil nutrient characteristics (FC site more potassium, CC site more phosphorous). Our results indicated significant differences in phenology within species between sites and years, with leaf, flower and fruit production tending to be higher at the CC site and in the year 2004. Wood density and xylem water potentials were negatively related to each other, and midday water potentials were higher at the CC site. Differences in phenology found among years suggest that the timing of rainfall as well as the duration of periods without rain may play a more important role in phenology than total annual precipitation. Also differences inter-sites suggest a strong effect of site on tree phenology. Proximity to superficial bodies of water, such as cenotes, coupled with a greater concentration of available phosphorus in the soil may modify the effect of drought in this tropical dry deciduous forest.     

鄱阳湖四种水鸟的栖息地利用与水深和食物的关系

为了了解水深和食物资源对水鸟栖息地利用的影响,2012 ~ 2013年越冬期,采用样方法,对鄱阳湖沙湖的白鹤 (Grus leucogeranus)、小天鹅 (Cygnus columbianus)、东方白鹳 (Ciconia boyciana) 和白琵鹭 (Platalea leucorodia) 4种水鸟的数量、觅食地和休息地的水深以及主要食物——沉水植物冬芽的密度和生物量进行了调查。每个样方为150 m? 150 m的栅格,全湖共设置152个样方。结果显示,10月份沉水植物冬芽的平均水深为 (124.2 ± 12.0) cm。4种水鸟觅食地的水深均显著高于其休息地的水深 (白鹤：Z = 11.96, 小天鹅：Z = 4.69, 东方白鹳：Z = 14.44, 白琵鹭：Z = 29.33, 所有P < 0.01);对于2种食冬芽的水鸟,白鹤觅食地的水深、冬芽生物量、取食深度以及休息地水深均显著低于小天鹅 (觅食地水深: Z = 8.56, 冬芽生物量: Z = 2.93, 取食深度: Z = 14.69, 休息地水深: Z = 4.34, 所有P < 0.05),但两者觅食地的冬芽密度差异不显著 (Z = 0.6, P = 0.55);对于2种食鱼性水鸟,东方白鹳觅食地水深、取食深度和休息地水深均显著大于白琵鹭 (觅食地水深: Z = 10.60; 取食深度: Z = 9.35; 休息地水深: Z = 8.47, 所有P < 0.01)。回归分析表明,白鹤、东方白鹳、白琵鹭的觅食个体数量均与水深呈二次项关系,个体数量最大的觅食地水深分别为23.9 cm,33.0 cm和22.6 cm;白鹤、小天鹅的觅食个体数量均与冬芽生物量呈线性关系。3种涉禽均只能分布在一定的水深范围内,且同种食性的水鸟利用不同的水深从而减少在空间生态位的重叠。     

Water relations and growth responses of Uniola paniculata (sea oats) to soil moisture and water-table depth

Summary This study examined the water relations and growth responses of Uniola paniculata (sea oats) to (1) three watering regimes and (2) four controlled water-table depths. Uniola paniculata is frequently the dominant foredune grass along much of the southeastern Atlantic and Gulf coasts of the United States, but its distribution is limited in Louisiana. Throughout most of its range, U. paniculata tends to dominate and be well adapted to the most exposed areas of the dune where soil moisture is low. Dune elevations in Louisiana, however, rarely exceed 2 m, and as a result the depth to the water table is generally shallow. We hypothesized that if U. paniculata grows very near the water-table, as it may in Louisiana, it will display signs of water-logging stress. This study demonstrated that excessive soil moisture resulting from inundation or shallow water-table depth has a greater negative effect on plant growth than do low soil moisture conditions. Uniola paniculata's initial response to either drought or inundation was a reduction of leaf (stomatal) conductance and a concomitant decrease in leaf elongation. However, plants could recover from drought-induced leaf xylem pressures of less than-3.3 MPa, but prolonged inundation killed the plants. Waterlogging stress (manifested in significantly reduced leaf stomatal conductances and reduced biomass production) was observed in plants grown at 0.3 m above the water table. This stress was relieved, however, at an elevation of 0.9 m above the water table. As the elevation was increased from 0.9 to 2.7 m, there were no signs of drought stress nor a stimulation in growth due to lower soil moisture. We concluded that although U. paniculata's moisture-conserving traits adapt it well to the dune environment, this species can grow very well at an elevation of only 0.9 m above the water table. Field measurements of water-table depth in three Louisiana populations averaged about 1.3 m. Therefore, the observed limited distribution of U. paniculata along the Louisiana coast apparently cannot be explained by water-logging stress induced by the low dune elevations and the corresponding shallow water-table depth.     

Phenotypic plasticity of the coarse root system of Prosopis flexuosa, a phreatophyte tree, in the Monte Desert (Argentina)

Prosopis flexuosa trees in the Monte Desert grow in dune and inter-dune valleys, where the water table is located at 6–14 m depth. We asked whether trees in the dunes, which are less likely to access the water table, present a coarse surface root architecture that might favor the exploration / exploitation of dune resources, compensating for water table inaccessibility. We characterized the architecture of surface roots of valley and dune trees, together with the soil environment. The dune held 50 % less and deeper gravimetric soil water (along a 4 m profile), 3-times less organic matter, 2-times less available phosphorous, and a sharper contrast of ammonium and nitrate concentration between plant canopies and uncovered soil than the valley. Coarse surface roots of dune trees were highly branched and grew tortuously at 0.56?±?0.16 m depth before sinking downward near the tree crown, suggesting an intensive exploitation of the ephemeral, deep, and canopy-linked resources. In contrast, trees from the valley spread their profuse and less branched surface roots mainly horizontally at 0.26?±?0.08 m depth, several meters outside the crown probably exploring this resource-rich site. A model for the environmental control of root architecture together with potential ecological effects is discussed.     

Water source partitioning among trees growing on shallow karst soils in a seasonally dry tropical climate

The sources of water used by woody vegetation growing on karst soils in seasonally dry tropical regions are little known. In northern Yucatan (Mexico), trees withstand 4–6 months of annual drought in spite of the small water storage capacity of the shallow karst soil. We hypothesized that adult evergreen trees in Yucatan tap the aquifer for a reliable supply of water during the prolonged dry season. The naturally occurring concentration gradients in oxygen and hydrogen stable isotopes in soil, bedrock, groundwater and plant stem water were used to determine the sources of water used by native evergreen and drought-deciduous tree species. While the trees studied grew over a permanent water table (9–20 m depth), pit excavation showed that roots were largely restricted to the upper 2 m of the soil/bedrock profile. At the peak of the dry season, the δ¹⁸O signatures of potential water sources for the vegetation ranged from 4.1 ± 1.1‰ in topsoil to −4.3 ± 0.1‰ in groundwater. The δ¹⁸O values of tree stem water ranged from −2.8 ± 0.3‰ in Talisia olivaeformis to 0.8 ± 1‰ in Ficus cotinifolia, demonstrating vertical partitioning of soil/bedrock water among tree species. Stem water δ¹⁸O values were significantly different from that of groundwater for all the tree species investigated. Stem water samples plotted to the right of the meteoric water line, indicating utilization of water sources subject to evaporative isotopic enrichment. Foliar δ¹³C in adult trees varied widely among species, ranging from −25.3 ± 0.3‰ in Enterolobium cyclocarpum to −28.7 ± 0.4‰ in T. olivaeformis. Contrary to initial expectations, data indicate that native trees growing on shallow karst soils in northern Yucatan use little or no groundwater and depend mostly on water stored within the upper 2–3 m of the soil/bedrock profile. Water storage in subsurface soil-filled cavities and in the porous limestone bedrock is apparently sufficient to sustain adult evergreen trees throughout the pronounced dry season.