豌豆β-微管蛋白基因的分离

微管蛋白是在进化过程中最为保守的蛋白质中的一组。高等植物的微管蛋白基因与酵母的微管蛋白基因具有同源性。据此进行了如下实验：从豌豆（A561），大豆（黑农26）苗中提出的核DNA用EcoRI、BamHI和SalI限制性内切酶酶切，经Southern转移与32P标记的酵母β-微管蛋白cDNA进行杂交。从杂交图谱上可以看出豌豆、大豆均有两个拷贝的β-微管蛋白基因。豌豆核DNA经BamHI酶切后的5kb和10kb两个片段从电泳凝胶中回收，插入到puc9质粒中，宿主菌为JM83。然后以酵母β-微管蛋白基因为探针，用菌落原位杂交和Southern斑点杂交的方法筛选出含有豌豆β-微管蛋白基因编码序列的克隆。所克隆到的DNA序列的限制性酶切图谱及序列分析尚有待进一步研究。

美味猕猴桃和软枣猕猴桃种间杂交花粉管行为和早期胚胎发生的观察

美味猕猴桃(Actinidia deliciosa(A．Chev．)C．F．Liang and A．R．Ferguson)和软枣猕猴桃（Actinidia arguta）种间传粉后，花粉管在花柱内行为的荧光观察，以及早期胚胎发生的显微观察，结果如下： 1．花粉粒在柱头的乳头细胞表面萌发，在开放型的V形花柱道内生长。 2．花粉管生长速率比对照缓慢，到达胚珠珠孔的时间平均延迟50到60小时。 3．花粉管在花柱中下部出现形态变化：部分花粉管呈波纹状弯曲;花粉管顶端膨大，尖细或破裂;花粉管直径变化;花粉管解体。 4．花粉管胼胝质沉积的变化：胼胝质沿花粉管壁不规则沉积;有的膨大的花粉管顶端出现胼胝质;有的不出现胼胝质塞，而整个花粉管壁有胼胝质分布，荧光强烈。 5．基于显微结构和种子分析，种间杂交大约有30%的胚珠能够受精，并发育成为种子，种子的胚的大小和胚乳的量与对照有差别，有约70%或更多的表现不育或败育。胚发育为茄型，受精后台子保持休眠十几天后开始横分裂。传粉后七周形成子叶胚。胚发育较对照迟缓。胚乳细胞型。 6．种间杂交能够结实，正常种子占20% -30％，败育干瘪种子占10%左右，未受精胚珠占60%- 70％。种内传粉正常种子占95%，空瘪败育种子占0.7％，未受精胚珠占3.8％。 7．种间杂交果实大小、重量，种子大小及数目，胚的大小都比对照小。

玉米、谷子基因转化的研究

本工作用BT基因、PinⅡ基因和bar基因对青饲玉米、谷子进行了基因转化的研究，并且对转基因的受体、转基因的方法、转化后的筛选、检测及植株再生等问题进行了探讨。 玉米胚性细胞系，包括胚性愈伤组织和胚性细胞悬浮系，可作为基因转化的受体，它亦是原生质体培养的关键。玉米的基因型对胚性细胞系的获得有很大的影响。在相同的培养条件下，九个青饲玉米品系都得到了I型愈伤组织，但仅有两个品系(232和235)得到了胚性细胞系(L32和L35)。幼胚的长度及年龄也是影响诱导形成胚性愈伤组织的一个重要因素，最佳胚长是1-1.5mm，最佳胚龄是授粉后10-12天的幼胚。另外，适当提高蔗糖浓度对胚性细胞悬浮系的建立及保持均有好处。 从玉米原生质体培养获得了再生植株．在此基础上用电激法和PEG法将BT基因导入玉米原生体，发现在原生质体培养过程中，同对照相比，第一次细胞分裂及形成愈伤组织的时间往后推移． 诱导玉米I型愈伤组织没有基因型的限制，可以从大多数玉米品系中得到。并且玉米I型愈伤组织具有极强的分化能力．我们将玉米I型愈伤组织作为基因枪法转化的受体，获得了转基因工程植株。目前，尚未见这方面的报道． 基因枪法转化玉米胚性细胞系，得到抗性愈伤组织的效率约为1/40。用直径约3mm的玉米I型愈伤组织块作基因枪法转化受体，转化后经筛选平均每块可得到1-4个抗性愈伤组织系。用PEG和电激法转化玉米原生质体，转化后原生质体再生愈伤组织中，抗性愈伤组织的得率为9.3%和8.9%， 基因枪法适应完整的细胞和组织的转化，可较快得到抗性植株，在玉米基因转化研究中， 为了较快地得到转化植株，用基因枪法较电激法和PEG法更好，在玉米三种基因转化的受体中（原生质体、胚性细胞系和I型愈伤组织），以I型愈伤组织作受体最好，用它作受体可以避免原生质体培养的困难，克服获得胚性细胞系的基因型的限制。 胚性细胞系对抗菌素的耐受性随继代时间增长而增加．I型愈伤组织对抗菌素的耐受性 同愈伤组织块的大小呈正相关。 由于玉米愈伤组织对卡那霉素的本底抗性较高，所以需要用高浓度(800mg/L)的卡那霉 素进行筛选，过高的选择压力对芽的分化有抑制作用．用电激和PEG处理后的原生质体再生的愈伤组织，经卡那霉素筛选出的抗性愈伤组织未能得到再生植株。而对照则得到了再生植株。用PPT和Hyg筛选出的抗性愈伤组织得到了再生植株． 用PCR和Southern杂交对抗性愈伤组织和再生植株进行检测，证明外源基因已整合到 玉米基因组中。得到了携有BT基因、bar基因或PinⅡ基因的愈伤组织或工程植株。 用豫谷一号的幼穗诱导获得了胚性愈伤组织，基因枪转化后，经PPT筛选得到抗性愈伤组织。每个5cm的培养皿内装有谷子胚性愈伤组织约0.5g，经筛选后可得到5-10块抗性愈伤组织，此PPT抗性的愈伤组织用PCR和Southern杂交检测，证明bar基因已整合到了谷子的基因组中。从转化愈伤组织中已分化出了再生植株。

Predicting the distribution of Vibrio vulnificus in Chesapeake Bay

Vibrio vulnificus is a gram-negative pathogenic bacterium endemic to coastal waters worldwide, and a leading cause of seafood related mortality. Because of human health concerns, understanding the ecology of the species and potentially predicting its distribution is of great importance. We evaluated and applied a previously published qPCR assay to water samples (n = 235) collected from the main-stem of the Chesapeake Bay (2007 – 2008) by Maryland and Virginia State water quality monitoring programs. Results confirmed strong relationships between the likelihood of Vibrio vulnificus presence and both temperature and salinity that were used to develop a logistic regression model. The habitat model demonstrated a high degree of concordance (93%), and robustness as subsequent bootstrapping (n=1000) did not change model output (P > 0.05). We forced this empirical habitat model with temperature and salinity predictions generated by a regional hydrodynamic modeling system to demonstrate its utility in future pathogen forecasting efforts in the Chesapeake Bay.

Conserving oyster reef habitat by switching from dredging and tonging to diver-harvesting

A major cause of the steep declines of American oyster (Crassostrea virginica) fisheries is the loss of oyster habitat through the use of dredges that have mined the reef substrata during a century of intense harvest. Experiments comparing the efficiency and habitat impacts of three alternative gears for harvesting oysters revealed differences among gear types that might be used to help improve the sustainability of commercial oyster fisheries. Hand harvesting by divers produced 25−32% more oysters per unit of time of fishing than traditional dredging and tonging, although the dive operation required two fishermen, rather than one. Per capita returns for dive operations may nonetheless be competitive with returns for other gears even in the short term if one person culling on deck can serve two or three divers. Dredging reduced the height of reef habitat by 34%, significantly more than the 23% reduction caused by tonging, both of which were greater than the 6% reduction induced by diver hand-harvesting. Thus, conservation of the essential habitat and sustainability of the subtidal oyster fishery can be enhanced by switching to diver hand-harvesting. Management schemes must intervene to drive the change in harvest methods because fishermen will face relatively high costs in making the switch and will not necessarily realize the long-term ecological benefits.

The effect of intensive line fishing on the virgin biomass of a tropical deepwater snapper, the crimson jobfish (Pristipomoides filamentosus)

An intensive commercial hook-and-line fishing operation targeted the demersal fisheries resources at Saya de Malha Bank in the Southwest Indian Ocean. Fishing was conducted with 12 dories that were equipped with echo sounders and electric fishing reels and supported by a refrigerated mothership. Over a 13-day period in the 55–130 m depth range, a total of 74.3 metric tons (t) of fish were caught, of which the crimson jobfish (Pristipomoides filamentosus) represented 80%. Catch rates decreased with time and could not be attributed to changes in location, climatic conditions, fishing depth, fishing method, or bait type. The initial virgin biomass of P. filamentosus available to a line fishery at the North Western promontory of Saya de Malha Bank was estimated at 72.6 t through application of the Leslie model to daily catch and effort data. Biomass densities of 2364 kg/km2 and 1206 kg/km were obtained by applying the initial biomass estimates to the surface area and to the length of the dropoff that was fished. The potential sustainable yield prior to exploitation was estimated at 567 kg/km2 per year. The quantity of P. filamentosus caught by the mother-ship-dory fishing operation represented 82% of the initial biomass available to a hook-and-line fishery, equivalent to more that three times the estimated maximum sustainable yield. The results of the study are important to fisheries managers because they demonstrate that intensive line fishing operations have the potential to rapidly deplete demersal fisheries resources.

Stable isotopes in paleosols and origins of the Asian monsoon

The stable isotopic composition of buried soil carbonate and organic matter from northern Pakistan and Nepal can be used to reconstruct aspects of the paleoecology of riverine floodplain ecosystems over the past 17 Myr. Probable dry woodland dominated the floodplain biomass of large rivers ancestral to the modern Indus and Ganges up to 7.3 Myr. Between 7.3 and about 6 Myr, tropical grasses gradually displaced woodland and have dominated floodplain biomasses to the present. The paleovegetational transition beginning about 7.3 Myr likely signals the onset of the strongly seasonal precipitation pattern that typifies the monsoonal climate of the region today. One possible analog to the dry woodland soils of the Miocene are found under the Sal woodlands of the northern Indian subcontinent, while undisturbed modern analogs to the Plio-Pleistocene floodplain grasslands can still be found in the Chitwan area of southern Nepal.

东灵山森林生态系统若干水分问题的研究

东灵山地区年均降水量659.7mm，单次降水以雨量小、雨强低的降水为主。水汽压（年均17.7mb）、相对湿度（年均66％）的季节变化呈现生长季高、冬季低的趋势。年均蒸发量1019.5mm;气温、风速、日照时间和水压与月蒸发量和日蒸量相关显著;气温、日照时间和水压分别在11-6月、7－8月和9－10月为决定蒸发量的首要因子。枯枝落叶层、土壤层湿度主要受前十日降水量和坡向影响。 植物体含水量生长季节较高，冬季较低;含水量随径级的增大而降低。六个灌木树种的平均含水量大小顺序为：毛榛（48.62%）最高荆条（36.32%）最低;七个乔木树种水分含量为油松，56.14%;蒙椴，54.19%;华北落叶松，52.91%;五角枫，43.64%;辽东栎，41.87%;棘皮桦，41.13%;大叶白腊，37.79%。几种植被类型的储水量为：辽东栎林，82.08mm;华北落叶松林，47.35mm;混交林，34.60mm;油松林，31.33mm;灌丛，12.40mm。各树种叶片日最低水势的季节均值为：辽东栎，-16.1bar;五角枫，-15.8bar;大叶白腊，-15.1bar;糠椴，-13.4bar;棘皮桦，-12.3bar;蒙椴，-12.2bar。叶片水势的日间变化均呈一“V”形曲线;光照在叶片水势的日间变化中起着决定性作用。 96年各树种平均单株树干茎流量为辽东栎，30.3mm(4.19%);华北落叶松，16.1mm(2.22%);油松，8.9mm(1.23%);棘皮桦，2.9mm(0.40%)。两个生长季各林分冠层的水量平衡为：辽东栎林，树干流茎量101.87mm(9.18%)，穿透降水量823.08mm(74.15%)，截留量185.05mm(16.67%);华北落叶松林，树干径流量66.88mm(6.03%)，穿透降水量836.92mm(75.40%)，截留量206.20mm(18.58);混交林，树干径流量50.13(4.52%)，穿透降水量846.78mm(76.29%)，截留量212.20mm(19.12%);油松林，树干径流量33.90mm(3.05%)，穿透降水量934.88mm(84.22%)，截留量141.22mm(12.72%)。多元回归分析表明，树干流茎量S与降水量P和前24小时降水量P_1呈显著正相关关系;穿透降水量T与降水量P和最大雨强M正相关显著。附加截留量与降水时间成正比。 枯枝落叶层的生物量为：油松林，25.56t/hm~2;华北落叶松林20.01t/hm~2;辽东栎林，8.31t/hm~2;混交林，7.98t/hm~2。枯枝落叶层的平均实际持水量和有效持水量均以油松林最大，其次是华北落叶松林，而混交林和辽东栎林较低;枯枝落叶层的实际持水量和有效持水量的季节变化分别与前十日降水量P10成正相关和负相关关系。枯枝落叶层的截留量为油松林＞华北落叶松林＞辽东栎林＞混交林;油松林（145.632mm和90.800mm）混交林(61.816mm和54.504mm)。油松林、辽东栎林、混交林和华北落叶松林去除枯枝落叶层后，土壤入渗量比对照平均降低100mm以上;表层土壤含水量分别比对照土壤下降了6.26、18.26、15.06和15.07个百分点。地表径流量分别增加了，辽东栎林34.299mm(603%)和15.816mm(525%);油松林14.593mm(732%)和10.584mm(1321%);混交林12.004mm(181%)和7.275mm(364%);华北落叶松林3.555mm(118%)，3.275mm(229%)。96年生长季，各土壤流失量分别增加了：油松林172.751t/hm~2(124倍);辽东栎林836.500t/hm~2(119倍);混交林172.499t/hm~2(47倍);华北落叶松林11.557t/hm~2(11倍)。表层土壤容重分别增加了：油松林15.0%和20.6%，辽东栎林18.4%和28.2%，混交林11.5%和38.5%，华北落叶松林4.3%和17.1%。 0-60cm深度土壤容重平均值的大小顺序为：草地>灌丛>辽东栎林>油松林>混交林>华北落叶松林;而土壤孔隙度的大小顺序为华北落叶松林>混交林>油松林>辽东栎林>灌丛>草地。两个生长季为土壤实际储水量的均值：油松林，124.45mm，78.62mm;辽东栎林，131.23mm，87.72mm;混交林，180.41mm，113.90mm;华北落叶松林，165.53mm，127.95mm;灌丛，172.50mm，89.81mm;草地，152.92mm，89.59 mm分别比干旱年份97年高出45.83mm、43.51mm、51.63mm、37.58mm、82.69mm和63.33mm。两个生长季的地表径流量为草地，30.930mm(2.79%);灌丛，16.321mm(147%);油松林，2.911mm(0.26%);辽东栎林，8.703mm(0.78%);混交林，8.625mm(0.78%);华北落叶松林，4.447mm(0.40%)。油松林、混交林和华北落叶松林地表径流量与降水量P(mm)和最大雨强(mm/h)正相关显著;而辽东栎林、灌丛和草地的地表径流量则与降水量P(mm)、平均雨强Q(mm/hr)和最大雨强M(mm/hr)三者之间呈显著正相关关系。与草地相比(1220.093kg/hm~2，100％)，灌丛、辽东栎林、混交林、油松林和华北落叶松林96年生长季的土壤流失量分别降低了85.05%、94.26%、96.99%、98.86和99.14%。 降水量是影响小流域径流量时间变化的主要因素;南沟和马牙石沟96年的径流量分别是97年的8.19倍和7.87倍，而径流深(46.25mm，52.75mm)分别比97年(5.65mm,6.70mm)高出40.60mm和46.05mm。两个小流域由于面积的差异而使南沟两年的径流量分别比马牙石沟高出2773.136m~3(13.15%)和235.434m~3(8.79%)。96年和97年马牙石沟径流深比南沟高出6.5mm(14.05%)和1.05mm(18.58%)。在地处大陆性季风气候区的东灵山地区，用0.010m~3/min/km~2/hr能较好地分割小流域的洪峰和基流。在五次暴雨水文曲线中，马牙石沟的快速径流量分别比南沟高出25.00%到143.33%。五次洪水水文响应R的平均值南沟为0.218%，马牙石沟为0.404%;与海洋性气候地区相比，东灵山地区小流域的R值要低一到两个数量级。马牙石沟洪峰流量Qp的平均值为418.772L/min要比南沟(281.191L/min)大48.9%。东灵山地区小流域的洪水径流过程可分为三种类型。