Anthesis and seed production in Zostera marina L. (eelgrass) from the chesepeak by

Anthesis and seed production in Zostera marina L. were studied in three areas of the Chesapeake Bay from January to June 1980. Inflorescence primordia with distinguishable anthers and pistils were first observed in February when water temperature was 3°C. Development of the reproductive shoots in the field continued after February as water temperature rose, with the first evidence of pollen release in mid-April (water temperature 14.3°C). Stigmata loss was first observed in samples taken in late April at all locations by as water temperatures averaged above 16°C. Pollination was complete at all locations by 19 May and anthers were no longer present. Few reproduction shoots were found on 3–5 June and seed release was assumed to be complete by this time (water temperature 25°C). The density of flowering shoots ranged from 11 to 19% of the total number of shoots, producing an estimated 8127 seeds m^?2.Comparison of flowering events with other areas along a latitudinal gradient from North Carolina to Canada indicated that reproductive events occurred earlier in the most southern locations and at successively later dates with increasing latitude.     

Life cycle and growth ofPotamogeton crispus L. in a shallow pond,ojaga-ike

The life cycle and growth ofPotamogeton crispus L. were studied in a shallow pond, Ojaga-ike. With respect to the shoot elongation and seed and turion formations, the life cycle of this plant in the pond could be divided into following five stages: germination, inactive growth, active growth, reproductive and dormant stages. It was suggested that the plant showed these successive stages depending mainly upon water temperature. The turions germinated on the bottom in autumn when the water temperature fell below ca. 20 C. The plant showed hardly any growth during winter (December—early March) when the temperature was below 10 C. In the spring when the bottom water temperature rose to above 10 C (mid-March), the plant started to grow again and the shoot elongated rapidly at the rate of 4.2 cm day⁻¹ until the shoot apex reached the pond surface in late April. Both the increment of node number and the internodal elongation were associated with this rapid shoot growth. On 10 May (last sampling date), the mean values of shoot length, internodal length and the number of nodes estimated for 10 predominant plants were 238.2±5.6 cm, 7.1±0.8 cm and 34.9±4.0 cm, respectively. The turion formation and flowering occurred during the period from mid-April to mid-May when the surface water temperature ranged 19 and 22 C. The dry weight of a plant reached the maximum mean value of 1180 mg on 10 May. At its peak biomass, an individual plant produced 1–10 turions (5.5 on average) of which the mean individual turion dry weight was 53.2 mg. The turion dry weight accounted for ca. 42% of the total plant biomass m⁻² at that time.     

黄土高原不同降水区休闲期土壤贮水效率及其对冬小麦水分利用的影响

土壤贮水是影响黄土高原冬小麦生产力的最重要因素,分析休闲期贮水效率对有效利用水资源具有重要意义。利用黄土高原旱作区4个农业气象观测站土壤水分长期观测资料和冬小麦产量资料,探讨了不同气候区休闲期土壤贮水和耗水特征及对冬小麦水分利用的影响。结果表明:(1)黄土高原旱作区休闲期1 m土层多年平均贮水量半湿润区为9 1mm,贮水效率为30.7%,半干旱区为32 mm,贮水效率为16.5%,且不同降水年型、不同气候区休闲期贮水量和贮水效率差别较大;(2)黄土高原旱作区1 m土层贮水量从土壤解冻至封冻期间基本呈波谷型分布,休闲期为主要贮水阶段,冬小麦返青—开花期为休闲期贮水的主要消耗阶段。半湿润区休闲期土壤贮水量主要消耗在起身至开花期,半干旱区主要消耗在越冬至拔节期;(3)黄土高原旱作区播种—越冬前消耗0—40 cm土层贮水,越冬-起身期各土层贮水量都有消耗,起身—开花期半湿润区主要消耗0—40 cm土层贮水量、半干旱区主要消耗0—60 cm土层贮水量,开花—成熟期半湿润区主要消耗40 mm以下土层贮水量、半干旱区主要消耗60 cm以下土层贮水量;(4)黄土高原休闲期贮水效率与冬小麦产量显著相关,半湿润区水分利用效率远高于半干旱区。黄土高原不同区域降水时空分布不均和土壤贮水能力的差异是造成不同气候区休闲期水分贮存差异的主要原因,通过调整耕作方式、水肥管理、种植结构进一步实现冬小麦增产和水分高效利用。     

Spatial and Temporal Variability of Zooplankton in a Great Plains Reservoir

Seasonal and daily patterns of zooplankton populations are often predictable in natural lakes. Distinct zonation and geomorphic differences in reservoirs, however, make ecological extrapolations from lakes to reservoirs uncertain. We describe the spatial and temporal distribution of zooplankton, algae, and water clarity across reservoir zones and along a depth gradient in Glen Elder Reservoir, Kansas. Daphnia species were most abundant in the lacustrine zone, with D. pulicaria numerically dominant in early spring and D. mendotae dominant later in 1999 and 2000. Rotifers (Keratella quadrata, Asplanchnaspp.) were dominant in the riverine zone in 1999, 2000, and 2001. Algal biomass was not significantly different between zones through most of the sampling periods, except late April in 1999 and mid-April in 2000. Chlorophyll a exceeded 81 μg l^?1 in the lacustrine zone in mid- to late-April in 1999 and 2000, and exceeded 90μg l^?1in the riverine zone in mid-April. Water clarity was significantly lower in the riverine zone in 1999 and 2000. Most zooplankton taxa had similar depth distributions at night and day, indicating a lack of diel vertical migration behavior on a large scale. However, in small scale (30 cm vertical enclosures) laboratory experiments, both D. pulicaria and D. mendotae occupied significantly deeper depths (>25 cm) under lighted conditions in the presence of fish chemical cues compared to shallow water (7–17 cm) under dark conditions and in the absence of fish cues. These contrasting results suggest that, as in other studies, Daphnia sense cues from predators and alter their depth in the water column on small scales without natural constraints on movement and choices. However, other factors in the reservoir such as wind-generated water movements and cues from other predators may prevent depth choices similar to those seen under controlled conditions. These results illustrate biotic and abiotic differences between riverine and lacustrine zones in a large reservoir, and contrast with Daphnia depth segregation and migration patterns in natural lakes.     

灰化苔草对不同水位环境的生理适应性

水位是影响湿地植物生长发育和繁殖的重要因素,为明确不同水位环境对灰化苔草(Carex cinerascens)生理特性的影响,采用室内盆栽法,设置上升、下降与稳定3种水环境类型,各设置8 cm(0.2cm/d)、16cm(0.4 cm/d)、24 cm (0.6 cm/d)、32 cm (0.8 cm/d)、40 cm (1.0 cm/d)、48 cm (1.2 cm/d)、56 cm (1.4 cm/d)7个试验处理,以0 cm水位为对照,试验时间持续40 d。分析了不同水位条件下灰化苔草抗氧化酶活性、渗透调节物质含量、丙二醛含量和超氧阴离子产生速率等指标。研究结果表明:1)稳定水位中,8、16 cm淹水深度下,超氧阴离子产生速率、渗透调节物质含量和抗氧化酶活性与对照组之间差异显著。48、56 cm的淹水条件下,抗氧化酶活性与渗透调节物质先增后减、丙二醛与超氧阴离子产生速率持续增加;2)水位上升条件下,在0.2、0.4 cm/d变化强度下,20—30 d后丙二醛含量与超氧阴离子产生速率无显著变化。1.0 cm/d为灰化苔草生理调节耐受极限,当变化强度大于1.0 cm/d时、各生理指标与变化强度小于1.0 cm/d变化明显异常;3)水位下降条件下,受初始水位高度的影响。丙二醛含量在1.2、1.4 cm/d变化强度下呈现高-低-高的变化趋势,其余试验指标表现为先升后降的变化趋势,并且随着变化强度的增加、各生理指标变化的差异越来越大、由升高转向降低的时间节点不断延后。可见,淹水环境会破坏灰化苔草细胞内环境的稳态,相比稳定水位,灰化苔草的抗氧化与渗透调节系统能够更快的适应水位变化环境,并且短时间、低强度的水位变化一定程度能促进灰化苔草的生理代谢。     

The period of occurrence,density, and distribution of larvae of three commercial crab species in Peter the Great Bay,Sea of Japan

Based on materials from plankton surveys carried out in 2004–2009, the period of occurrence, density, and distribution of larvae of three commercial species of crabs in the Peter the Great bay and adjacent areas of Sea of Japan were studied. The larvae of the horsehair crab Erimacrus isenbeckii (Brandt, 1848) occurred in the plankton from mid-March to early June, within the range of water temperature from −1 to 10.8°C. The larvae of the helmet crab Telmessus cheiragonus (Tilesius, 1812) appeared in the plankton in mid-April and occurred to the end of June within the temperature range from 2.8 to 13.0°C. The larvae of the snow crab Chionoecetes opilio (O. Fabricius, 1788) appeared in the plankton in mid-April as well, but some individuals sporadically occurred until early August. All the species of crabs produced one generation of larvae for their reproduction season. The terms of larval stay in plankton depended on water temperature and the duration of the pelagic period increased in colder years. In that area, the larvae of C. opilio were the most abundant (up to 41 ind./m³) and the zoea density of horsehair and helmet crabs was significantly lower (no more than 2 ind./m³). The larvae of C. opilio occurred over the entire area of the Peter the Great bay; the greatest aggregations of their early stages were observed in its southwestern open part. The maximum density of E. isenbeckii zoea was recorded in the south of the Amursky bay and in the Posyet bay. Individual larvae of T. cheiragonus occurred in the Posyet bay and in the southern part of the Amursky and Ussuriisky bays. The late-stage larvae of all crab species were concentrated in areas of the coastal circulation.     

Behavior of Aldicarb in Soil Relative to Control of Heterodera schachtii

The adsorption characteristics of two soils for aldicarb sulfoxide were similar to that described by the Freundlich equation, The adsorption constant for the Holtville clay was 3.3, and that of the Buren silt loam, 0.34. Planting beds in a field of Holtville clay and another of Buren silt loam were side-dressed at 25 kg and 50 kg/ha 10% aldicarb (Temik® 10G). Comparison of field measurements of aldicarb concentrations with previous laboratory determinations of aldicarb effects on Heterodera schachtii allowed predictions of soil zones in which hatching, infectivity, and orientation of males to females would be affected. Aldicarb in the soil water of Holtville clay sufficient to interfere with male orientation extended through most of the bed profile to a depth of 46 cm 1 week after the first irrigation. Orientation could be affected in only the top 20 cm of the bed 37 days after treatment and application of 712 mm of irrigation water. In Buren silt loam, disorientation of males was estimated to occur throughout the bed 42 days after treatment and 600 mm irrigation water. Aldicarb persisted in extensive areas of the bed at concentrations sufficient to prevent infection. In small areas of the profile, aldicarb sufficient to inhibit hatching persisted. Amounts of aldicarb in soil water samples obtained directly from beds agreed well with those from the analysis of the air dried soil samples.     

Seasonal succession of a microphagotroph community in a small pond during litter decomposition

Temporal dynamics of a lentic microphagotroph community were studied during leaf litter decomposition from December to May. Small plastic vessels containing leaf litter were placed on a pond bottom. They were sampled periodically to collect microphagotrophs. Three abiotic factors and abundance of two food items were also measured to analyze the autogenic and allogenic phenomena during a microphagotroph succession. Three behavior types were recognized in dominant taxa: a free-swimming type, a vagile (creeps on substratum, sometimes swims) type, and a voluntarily fixed type. Dominant taxa changed from the free-swimming to the vagile type up to mid-March, and the reverse change occurred from mid-April. Principal component analysis (PCA) indicated four factors affecting the dynamics of the community: water temperature as a seasonal factor, detritus volume on the litter surface as a habitat factor, and densities of bacteria and small flagellates as food factors. Taxa replacement appeared to occur through two mechanisms. (1) Dominance of small holotrichs, a free-swimming type, was brought about by a high bacterial density caused by seasonal events, i.e., leaf fall in December and detritus formation by litter feeders in mid-April. This is an allogenic aspect of community dynamics. (2) The free-swimming type was replaced by the vagile one during the period with high taxa diversity. This replacement occurred through intertaxa competition for scarce food and/or selective predation by larger microphagotrophs. It is an autogenic process within the community.     

Life cycle, horizontal microdistribution and current resistance of Allogamus auricollis Trichoptera: Limnephilidae in an Austrian mountain brook

SUMMARY. 1. The life history, horizontal distribution at the sediment surface and the effect of water flow on the microdistribution of Allogamus auricollis (Pictet, 1834), a case-bearing caddisfly, was investigated in a mountain brook near Lunz, Lower Austria.
2. The average head-width increment per moult was proportionately constant at c . 48%; therefore Dyar's rule was applicable.
3. Allogamus auricollis has a 1-year life cycle with first and second instars most abundant in October. It overwinters primarily as third and fourth instars; pupae were observed in August.
4. Horizontal distribution patterns were investigated by means of bimonthly samples taken along the stream profile. All instars were most abundant near the banks: 86.5% of the total catch 1987–88 were collected 0–1.5 m from the banks.
5. Current speeds were measured at the sites of 2191 larvae (including all instars) and eighty-six pupae. Larvae were most abundant at current speeds of 0–5 cm s⁻¹ (i.e. 86.6% of the total catch 1987–88).
6. Laboratory data on different stages of resistance to drift in A. auricollis (Waringer, 1989) were tested for their application to field conditions. 90% of the total catch 1987–88 preferred areas at the substrate surface where they could remain fully retracted within their cases, unattached, even when the large lateral case surface area was directed towards the water flow. This was also true at times of high discharge where the size of these areas was considerably reduced.     

The diversity,abundance and fate of ice algae and phytoplankton in the Bering Sea

Despite being an essential part of the marine food web during periods of ice cover, sea ice algae have not been studied in any detail in the Bering Sea. In this study, we investigated the diversity, abundance and ultimate fate of ice algae in the Bering Sea using sea ice, water and sub-ice sediment trap samples collected during two spring periods in 2008 and 2009: ice growth (March–mid-April) and ice melt (mid-April–May). The total ice algal species inventory included 68 species, dominated by typical Arctic ice algal diatom taxa. Only three species were determined from the water samples; we interpret the strong overlap in species as seeding of algal cells from the sea ice. Algal abundances in the ice exceeded 10⁷ cells l^?1 in the bottom 2-cm layer and were on average three orders of magnitude higher than in the water column. The vertical flux of algal cells beneath the ice during the period of ice melt (>10⁸ cells m^?2 day^?1) exceeded export during the ice growth period by one order of magnitude; the vertical flux during both periods can only be sustained by the release of algae from the ice. Differences in the relative species proportions of algae among sample types indicated that the fate of the released ice algae was species specific, with some taxa contributing to seeding in the water column, while other taxa were preferentially exported.     

基于稳定同位素技术的塔里木河下游不同林龄胡杨的水分利用来源

水分是制约很多陆地生态系统植物生长和繁殖的重要因素, 在干旱地区尤为明显。利用稳定同位素技术探究塔里木河下游不同林龄胡杨(Populus euphratica)的水分来源情况, 了解生态输水背景下荒漠河岸林的水分利用循环与利用策略, 可为生态输水提供科学依据, 同时也可对同类地区的生态恢复提供借鉴。本研究通过测定塔里木河下游胡杨茎干水和各潜在水源(土壤水、地下水)的稳定氢氧同位素值(δD、δ¹⁸O), 应用多源线性混合模型(IsoSource)分析了各潜在水源对不同林龄胡杨的贡献比例, 并结合3种林龄胡杨不同土壤深度含水量的变化, 分析了胡杨的主要吸水层位。结果表明: (1)不同林龄胡杨样地的不同深度区间上的土壤水δ¹⁸O值存在显著差异(P < 0.05): 胡杨幼龄木、成熟木、过熟木木质部δ¹⁸O分别为-7.83 ± 0.07‰、-8.53 ± 0.11‰、-9.36 ± 0.21‰; 而δD值不存在显著差异(P > 0.05)。可据此来推断胡杨的主要吸水层位。(2)总体上, 三种林龄胡杨土壤水δ¹⁸O值随土壤深度增加而减小, 并趋于接近地下水的δ¹⁸O值。其中, 0-60 cm土壤水受蒸发影响比较大, 其同位素组成经历了强烈的蒸发分馏过程, 土壤含水量极少, 土壤水δ¹⁸O值偏正。(3)不同林龄胡杨所利用的水分来源不同: 胡杨幼龄木对于地表80 cm以下的土壤水以及地下水均有一定程度的利用, 对80-140 cm、140-220 cm和220-340 cm的土壤水平均利用比率依次为16.2%、21.4%和24.6%, 对地下水平均利用比率为24.5%; 成熟木主要利用220-340 cm的土壤水及地下水, 平均利用比率分别为36.9%和42.3%; 过熟木主要利用140-340 cm的土壤水及地下水, 平均利用比率分别为32.8%和49.3%。     

Community structure of branchiopods (Anostraca,Notostraca and Conchostraca) in the Banat province in Yugoslavia

A survey of large branchiopods in the Banat provincein Yugoslavia revealed a particularly diverse fauna in the vicinity of the village Melenci, 100 km north of Belgrade. The temporary ponds here include 10 species of branchiopods, 5 anostracans, 2 notostracans and 3conchostracans (all belonging to the Spinicaudata group). This diversity represents 53% of the species known in Yugoslavia. Community structure, spatial distribution and seasonal dynamics of the species were analyzed over the period 1991–1995. More than one species was found in about 67% of ponds. The maximum number of coexisting species was 7.Anostracans were the most common as a group, while the notostracan Triops cancriformis and the conchostracan Leptestheria saetosa were the most frequent species. A high frequency of coexistence was established. Regarding community structure, two significantly different periods during the season were distinguished: the first, from the end of February to mid-April, and the second, from mid-April to the end of July. This extensive pool longevity may underlie the high diversity in this region. This revised version was published online in August 2006 with corrections to the Cover Date.     

宁夏盐池不同坡位旱地紫苜蓿水分来源

紫苜蓿(Medicago sativa)是一种经济和生态价值较高的优良牧草, 但其耗水量大, 在西北半干旱地区仅靠天然降水难以满足紫苜蓿的正常生长发育。宁夏盐池北部地处毛乌素沙地南缘, 地下水埋深较浅, 地下水有可能成为紫苜蓿的潜在水源, 弥补天然降水的不足。本试验在地势平坦的缓坡丘陵梁地和丘间低地, 选择8年生旱地紫苜蓿试验地作为研究对象, 采用稳定同位素技术, 研究了不同海拔的4个坡位(海拔自低到高分别为: 坡1、坡2、坡3和坡4)紫苜蓿的水分来源及其生长生理表现。结果表明: 坡位对0-300 cm土壤剖面含水量有显著影响, 海拔最低的坡1土壤含水量最高。土壤水和植物茎秆水δ ¹⁸O-δD坐标点大部分位于中国西北地区地方大气降水线(LMWL)的右侧, 说明植物利用的水源氢氧同位素组成受到蒸发的影响而发生了富集作用。0-450 cm土壤剖面水δ ¹⁸O值随着海拔高度的增加而增大。同一坡位土壤水δ ¹⁸O值随着土壤深度的增加逐渐下降。深层土壤水δ ¹⁸O值与地下水δ ¹⁸O相近, 说明地下水通过土壤毛细管上升而补充其上层土壤水分。0-40 cm土壤水δ ¹⁸O值随季节波动较大, 270 cm以下土壤水δ ¹⁸O值较为稳定。4、7、8月份坡1紫苜蓿茎秆水δ ¹⁸O值显著低于其他3个坡位(p < 0.001)。在4、6、7三个月, 坡位1紫苜蓿对深层土壤水(270 cm以下)的利用率最高。而在8月份, 坡1、坡3、坡4紫苜蓿主要利用150-270 cm、270-450 cm土层土壤水以及地下水, 坡2对表层(0-20 cm)土壤水利用率最高。坡1紫苜蓿的产量、整株Δ ¹³C值及气孔导度显著高于其他3个坡位。本研究表明: 在平均年降水量只有280 mm的西北半干旱地区种植旱地紫苜蓿要尽量选择地势较低的滩地, 使其能够利用到埋深较浅地下水, 以满足植物生长发育的需要并取得较好的生态和经济效益。     

沿海蝗区东亚飞蝗(Locusta migratoria manilensis)产卵场所选择的Logistic回归模型

以沿海蝗区南大港水库为研究区域,通过2002和2003两年野外450,50m规则栅格取样获取东亚飞蝗卵块、植物种类及其密度、土壤特性如含盐量、5cm含水量、pH、有机质及地形（阴坡和阳坡）等数据,采用多元Logistic回归模型,运用SAS软件筛选出与飞蝗产卵场所选择密切相关的变量,建立用于预测飞蝗产卵场所选择的Logistic回归模型。结果表明用植株密度（veg—d）和土壤含水量（water）所组建的模型能较好地预测飞蝗产卵选择,log（P（Y=1）/1-P（Y=1））=21．63-76.23/water-5．43log（water）-0．86（veg_d）。利用拟合优度（Goodness of fit）、预测准确性（Predictive accuracy）及模型x^2统计（Model chi—square statistic）等指标对模型进行评价的结果表明,所组建的用于预测飞蝗产卵场所选择的Logistic回归模型是可靠的,且能较好地预测事件是否发生。研究结果为区域蝗灾早期预警提供了科学依据和方法,对今后预测飞蝗产卵地点选择及防治决策有较高的实用性和应用价值。     

Grazing catfish,fishing birds,and attached algae in a Panamanian stream

Synopsis In streams where algivorous fishes abound, striking variation of attached algae often develops along depth gradients, with bands of high standing crops in shallow water (<20 cm) and sparse standing crops on deeper substrates. Experimental results from a stream in central Panama support the hypothesis that vertical variation in algal standing crops arises when grazing fishes avoid predators in shallow water by forgoing food resources that accumulate there. When 38 rocks bearing algae in a stream in central Panama were transferred from shallow (<20 cm) to deeper (>20 cm) water, algae were rapidly consumed by grazing catfish. Catfish were removed from three stream pools and left in place in three control pools. Ten days after catfish removal, algal standing crops in deep and shallow areas of removal pools were similar, while algal standing crops were higher in shallow than in deep areas of control pools. Catfish were exposed to fishing birds in open-topped enclosures. In one of three series of these pens, most catfish in shallow pens (10 and 20 cm) disappeared after 14 days, while catfish in deeper pens (30 and 50 cm) did not. Other groups of catfish which were caged 8 days showed differences in behavior depending on whether they had been fed or starved. After their release into their home pool, starved catfish spent more time feeding than did fed catfish. Despite their apparently increased hunger levels, starved catfish did not venture into shallow water to obtain algae. These results support the view that predator induced avoidance by grazers of certain areas can produce spatial pattern in the flora of flowing water communities.     

基于沿海蝗区飞蝗卵块分布格局的土壤空间异质性

以沿海蝗区南大港水库为研究区域,通过连续2a野外450m,50m规则栅格取样,利用地统计学方法,在GIS平台下,分析东亚飞蝗卵块分布格局与土壤空间异质性的研究,结果表明：（1）飞蝗卵块呈斑块、聚集分布,并具有明显的空间异质性,其空间自相关范围为390m,且主要分布在南大港水库的中部和东部,少数分布在南部,而在西部和北部地块几乎没有卵的分布。（2）研究区域内土壤含盐量和5cm含水量由空间自相关引起的空间异质性分别占总空间异质性的76.15%、78.04%,即表现出较强的空间相关性,空间自相关范围分别为594m,621m,土壤有机质和pH值具有中等强度的空间相关性,由空间自相关引起的空间变异分别为61.85%和57.19%,空间变异尺度分别为1014m,1368m。（3）研究区域内卵块主要集中在土壤含盐量较低（〈1.9%）、含水量适中（10.1%~29.9%）的中部和东部地块,而在土壤含水量较高（〉30%）的西部和盐分过重（〉3%）的北部几乎没有卵块的分布。即在一定程度上,蝗区土壤理化特性的空间异质决定了飞蝗卵块的空间分布特点。（4）卵块和土壤理化特性的空间格局图不仅为野外抽样调查、蝗灾预测预报及其防治提供科学依据,而且对蝗区环境改造具有重要指导作用。     

FTIR detection of water reactions during the flash-induced S-state cycle of the photosynthetic water-oxidizing complex

Photosynthetic water oxidation is performed via the light-driven S-state cycle in the water-oxidizing complex (WOC) of photosystem II (PS II). To understand its molecular mechanism, monitoring the reaction of substrate water in each S-state transition is essential. We have for the first time detected the reactions of water molecules in WOC throughout the S-state cycle by observing the OH vibrations of water using flash-induced Fourier transform infrared (FTIR) difference spectroscopy. Moderately hydrated (or deuterated) PS II core films from Synechococcus elongatus were used to obtain the FTIR difference spectra upon the first, second, third, and fourth flash illumination, representing the structural changes in the S(1) --> S(2), S(2) --> S(3), S(3) --> S(0), and S(0) --> S(1) transitions, respectively. In the weakly H-bonded OH region, bands appeared at 3617/3588 cm(-1) as a differential signal in the first-flash spectrum and at 3634, 3621, and 3612 cm(-1) with negative intensities in the second-, third-, and fourth-flash spectra, respectively. These bands shifted down by approximately 940 cm(-1) upon deuteration and by approximately 10 cm(-1) upon H(18)O substitution, indicating that they arise from the OH stretches of water including the substrate and its intermediates. Strongly D-bonded OD bands of water were also identified as broad features in the range of 2600-2200 cm(-1) by taking the double difference between the spectra of D(2)(16)O- and D(2)(18)O-deuterated films. In addition, broad continuum features that probably arise from the large proton polarizability of H-bonds were observed around 3000, 2700, 2550, and 2600 cm(-1) in the first-, second-, third-, and fourth-flash spectra, respectively, of the hydrated PS II film, revealing changes in the H-bond network of the protein. The negative OH intensities upon the second to fourth flashes might be related to proton release from substrate water. The results presented here showed that FTIR detection of water OH(D) bands can be a powerful method for investigating the mechanism of photosynthetic water oxidation.     

Stable isotopic observation of water use sources of Pinus sylvestris var. mongolica in Horqin Sandy Land, China

Since the late 1950s, Mongolian pine (Pinus sylvestris var. mongolica) has been widely planted for vegetation restoration in arid and semi-arid areas in North China. We used stable isotope signals from precipitation, soil water, and xylem water of Mongolian pine trees, which were planted in early 1980s on sand dunes in the east-southern margin of Horqin Sandy Land, to identify water uptake sources of this tree. (1) Stable ¹⁸O isotope composition of the xylem water exhibited little seasonality, suggesting that the trees use a relatively stable water source; (2) the water source of the pine trees primarily came from a soil depth of 20–60 cm (sampling depth up to 60 cm in this study) and the trees might use groundwater when soil moisture became extremely low; and (3) there was not much difference in water sources used by the pine trees grown at the top of the fixed dune and in the inter dune lowland, although these two sites had 3–8 m elevation difference. This study suggests that it is critical for Mongolian pine trees to access relatively reliable and stable water sources to grow in sandy land habitats, and timely recharging of rainwater to the trees’ rooting depth is requisite for avoiding and/or reducing their degradation caused by water shortage.     

Comparisons of habitat availability and habitat use by an allopatric cohort of juvenile Atlantic salmon Salmo salar under conditions of low competition in a Norwegian stream

Allopatric Atlantic salmon parr occupied a wider and lower range of mean water velocities than have been previously reported for parr in sympatry. With regard to depth, substrate and cover no substantial differences were found. Different fish sizes did not affect habitat use by parr significantly, neither did habitat use change during the season. Habitat availability strongly influenced observed habitat use thus, invalidating use of habitat suitability curves based on observations of habitat occupancy by fish only. The allopatric parr consistently selected habitats different from the available habitat, i.e. had preferences also in the absence of intraspecific interactions between age classes. Habitat conditions not used by the fish were more readily identifiable than habitats used. The parr rarely used shallow (≤ 10 cm) and deep (> 60 cm) stream areas, low mean water velocities (< 10 cm s^-1), fine substrate (sand and finer) and stream areas without cover. However, the calculated habitat preferences were also affected by habitat availability. Multivariate analysis did not identify any of the habitat variables as substantially more important than the others, but suggested that the importance of variables may vary with type of habitat studied.     

Artificial expression of aquaporin-3 improves the survival of mouse oocytes after cryopreservation

Successful cryopreservation of mammalian cells requires rapid transport of water and cryoprotective solutes across the plasma membrane. Aquaporin-3 is known as a water/solute channel that can transport water and neutral solutes such as glycerol. In this study we examined whether artificial expression of aquaporin-3 in mouse oocytes can improve water and glycerol permeability and oocyte survival after cryopreservation. Immature mouse oocytes were injected with aquaporin-3 cRNA and were cultured for 12 h. Then the hydraulic conductivity (L(P)) and glycerol permeability (P(GLY)) of matured oocytes were determined from the relative volume changes in 10% glycerol in PB1 medium at 25 degrees C. Mean +/- SD values of L(P) and P(GLY) of cRNA-injected oocytes (3.09 +/- 1.22 micro m min(-1) atm(-1) and 3.69 +/- 1.47 x 10(-3) cm/min, respectively; numbers of oocytes = 25) were significantly higher than those of noninjected oocytes (0.83 +/- 0.02 micro m min(-1) atm(-1) and 0.07 +/- 0.02 x 10(-3) cm/min, respectively; n = 13) and water-injected oocytes (0.87 +/- 0.10 micro m min(-1) atm(-1) and 0.08 +/- 0.02 x 10(-3) cm/min, respectively; n = 20). After cryopreservation in a glycerol-based solution, 74% of cRNA-injected oocytes (n = 27) survived as assessed by their morphological appearance, whereas none of the water-injected oocytes survived (n = 10). When cRNA-injected oocytes that survived cryopreservation were inseminated in vitro, the penetration rate was 40% (n = 48) and the cleavage rate was 31% (n = 70), showing that oocytes retain their ability to be fertilized. This is the first report to show that artificial expression of a water/solute channel in a cell improves its survival after cryopreservation. This approach may enable cryopreservation of cells that have been difficult to cryopreserve.