玉米根系分布空间和空间密度分布的数学模型

应用重积分研究了土壤层中散根型和直根型玉米根系的分布空间,同时研究了玉米根系的空间密度分布．     

具有一般形式饱和接触率SEIS模型的周期解

利用重合度的延拓定理,导出了具有一般形式饱和接触率SEIS模型周期解的存在性准则.     

祁连山3种典型生态系统土壤微生物活性和生物量碳氮含量

 测定分析了祁连山高寒草甸、山地森林和干草原土壤中微生物活性、生物量碳氮含量。结果显示：就土壤微生物生物量碳含量,森林比干草原和高寒草甸中分别高60%和120%以上,干草原比高寒草甸中高40%以上(p<0.05)。就土壤微生物生物量氮含量,0～5 cm土层,森林比高寒草甸和干草原中分别高64%和111%以上,高寒草甸比干草原中高29%;5～15 cm土层,森林比干草原和高寒草甸中分别高7%和191%以上,干草原比高寒草甸中高171% 以上(p<0.05)。森林和干草原中土壤微生物生物量碳比例比高寒草甸中高32%以上,0～5和5～15 cm土层,森林和干草原中土壤微生物生物量氮比例比高寒草甸中高150%以上（p<0.05）。就土壤微生物活性,0～5和5～15 cm土层,森林和高寒草甸比干草原中高26%以上;15～35 cm土层,森林比干草原和高寒草甸中高28%以上 (p<0.05)。土壤微生物生物量碳氮含量与有机碳含量及微生物生物量氮含量和比例与微生物生物量碳含量和比例呈现正相关（r²>0.30,p<0.000 1）。土壤微生物生物量氮含量、微生物生物量碳氮含量比例、微生物活性与土壤pH值呈显著负相关,土壤微生物生物量碳氮含量及其比例、微生物活性与土壤湿度呈正相关。说明祁连山3种生态系统土壤中微生物生物量和活性受气候要素、植被、有机碳、pH值和湿度等因素 的共同影响。     

Differences in cellulose digestive systems among castes in two termite lineages

Abstract.  Termites (Isoptera) are eusocial insects and express polyphenism. Soldiers have specialized morphology for colony defense, but their feeding activity is dependent on other colony members. To determine differences in cellulose degradation between soldier and worker termites, enzymatic activity and cellulase gene expression, as well digestive tract histology, are examined in two phylogenetically distant species. In Hodotermopsis sjostesti (family Termopsidae) , endo-β-1,4-glucanase activity is identified in the salivary glands, whereas β-glucosidase activity is identified in salivary glands and hindgut. The relative expression levels of endo-β-1,4-glucanase genes in soldiers are significantly lower than in workers. Thin sections of salivary gland of workers and soldiers are different in H. sjostedti . In Nasutitermes takasagoensis (family Termitidae), the endo-β-1,4-glucanase activity is restricted to the midgut in four tested castes (i.e. three types of workers and soldier). Examination of activity per termite reveals the highest activity in minor workers and the lowest activity in major workers and soldiers. The β-glucosidase activity is also concentrated on the midgut in all four castes. The relative expression level of the endo-β-1,4-glucanase gene does not correspond with its activity in the midgut. In thin sections prepared from N. takasagoensis , the folds and pulvillus in the gizzards, and cuticle structure of soldiers are less developed compared with the other three worker castes. The differences in digestive system among termite castes in terms of caste development in each species are discussed.     

恒河猴群微卫星DNA多态性的分析

目的　确立一种对恒河猴群个体的遗传物质进行准确可靠、快速简便的遗传检测方法。方法　利用聚合酶链反应 (PCR)扩增技术对 2 0只恒河猴群个体间进行了DNA多态性的分析。结果　筛选出 9个微卫星DNA位点具有显著多态性 ,4个微卫星DNA位点没有多态性 ,还有 2个位点等位基因数目较少。结论　利用这些多态性微卫星位点建立一种对恒河猴群个体进行有效、准备可靠、快捷简便的遗传背景监测方法。     

绵羊GDF9和BMP15基因多态性检测

以绵羊GDF9基因FecG^H突变和BMP15基因FecX^B和FecX^G突变为候选基因,采用PCR—RFLP方法研究其在湖羊、夏洛来、陶赛特、萨福克、中国美利奴肉用多胎品系、中国美利奴羊和罗米丽羊7个品种中的多态性．结果发现,湖羊群体中存在GDF和BMP15基因的FecG^H和FecX^B突变,但发生率极低,分别为0．645％(2／310)和0．968％(3／310)：而其它品种中则没有发现GDF9和BMP15基因的相应突变．这一发现对于建立绵羊基因标记辅助选择方法具有重要意义．     

几种脊椎动物宽频带心电图波形与心电向量环特点的比较

对小鼠、家鸽、蟾蜍、鲫鱼4种脊椎动物宽频带心电图Ⅱ导联的波形特点及QRS额面心电向量环的位置、形态特点进行了比较研究。结果发现,(1)宽频带心电图Ⅱ导联QRS波群小鼠、蟾蜍、鲫鱼QRS波群的主波均向上,而家鸽的主波向下;(2)QRS波群时程(ms)小鼠88±09,家鸽365±14,蟾蜍790±110,鲫鱼283±57;(3)QRS心电向量环的位置家鸽的位于-90°～-180°象限内,这是家鸽心电图Ⅱ导联QRS波群主波向下的根本原因;小鼠、蟾蜍、鲫鱼的均位于0°～90°象限内,与它们的QRS波群主波向上相一致;(4)QRS心电向量环的形状;小鼠的QRS向量环较其它3种动物的要大,蟾蜍的最小。鲫鱼的不规则,有的呈三角形,有的呈“8”字形,还有的呈半圆形,这是导致鲫鱼的QRS波群出现较多切迹和扭挫的原因。     

抗淋巴细胞免疫球蛋白制品中热原处理

对热原不合格的抗淋巴细胞免疫球蛋白 (ALG)半制品再制条件进行了研究。将高热原的ALG半制品通过使用碱、酸以及A5 0处理后 ,细菌内毒素的含量明显降低 ,热原质经家兔和鲎试剂检测均合格 ,其生物学效价仍不低于 1 :4 0 0 0 ,而且它们的其它各项主要指标也都达到中国生物制品暂行规程的要求。这一试验结果表明碱、酸处理并辅以A5 0吸附是去除ALG制品中热原的一种有效方法     

南方鲇的营养学研究:饲料中大豆蛋白水平对消化率及摄食率的影响

以23.78±0.09g的南方鲇为实验对象,以Cr2O3作为测定饲料消化率的指示物,以大豆蛋白分别替代0%、13%、26%、39%、52%和65%的鱼粉蛋白,配制成6种等氮(粗蛋白48%)、等能(总能20KJ/g)的饲料,用于探讨饲料中大豆蛋白替代鱼粉蛋白的比例对南方鲇消化率及摄食率的影响。实验在27.5±0.02℃水温条件下进行6周,溶氧维持在5mg/L以上,光制为14L∶10D。结果表明,饲料中不同比例的鱼粉蛋白与大豆蛋白对南方鲇的消化率及摄食率均存在显著影响(P<0.05)。其中南方鲇对于物质、蛋白质、脂肪和能量的消化率随着大豆蛋白替代率的提高而逐步下降,当替代量为65%时,其消化率显著低于其余各组(P<0.05)。而南方鲇的摄食率均随着饲料中大豆粉添加量的升高而升高,当大豆蛋白替代鱼粉蛋白超过39%时,摄食率显著高于其余各组(P<0.05)。通过分析认为,消化率是限制南方鲇利用大豆粉的重要因素,而摄食率不是影响其利用率的主要原因。     

Re-examination of the lower stratigraphy in the classic section, limeworks site, Makapansgat, South Africa

At the end of Member 2 times, remnant mammillary-form stalactites in the roof and wall contacts show that an irregular wedge-shaped space existed from the Classic Section out to the Cone area. It was into this space that hyenas and other denning animals were able to gain access from an as yet unfilled Cone area. During the mining operations of the 1920’s, Eitzman (1958) recollects entering an impressive bone breccia resembling a charnel house. We suggest that it is most probable that the Grey Breccia corresponds to his main breccia as only the area on top of Member 2, between the dolomite walls, roof and stalagmite boss has the required volume. It also lies at the end of an incline first dug by the miners, (still in existence), and at the end of which he was able to note some of the deposits. The bone breccias at the same level at the back of the Cone suggest that other dens were created at about this time. As the roof continued to retreat upslope and more material was washed in or fell in from the surface so more sediment was winnowed into the back of the Cone. At some stage this allowed prey animals to enter the Cone area and gain access between the speleothem barrier to the area of the Classic Section. As most Australopithecine fragments came from this breccia, it seems likely that, as with Swartkrans, the hominid fragments are the result of predation. Then as sediments continued to wash into the Cone area, the Classic Section and the back of the Cone became inaccessible for denning purposes. Large speleothem remnants embedded in sediment starting part-way up the Cone shows that a roof continued to exist in this area for some time. In fact, even today, although bits of speleothems can be found in the eroded hardened surface sediments there are few, if any, dolomite blocks. We presume that they were removed along with the upper part of the infilled, cavern along with the country rock as the surface continued to erode. Although it may not be possible to reconstruct a complete strati-graphic sequence involving the whole of the site, we have presented summary of evidence here that shows it is possible to trace stratigraphic relationships from the base of the Ancient Entrance to the top of the Cone and which includes the Grey Breccia and the two other bone breccias. Present work is focussed on completion of a new chronology by comparing our site magnetostratigraphy with the global polarity timescale. The speleothem deposition today in any of the caves of the Makapansgat area, with its annual rainfall of about 700mm, is extremely low. It is commonly recognised by karst geomorphologists (eg, Ford and Williams, 1989) that massive deposits of speleothem are characteristic of humid tropical to semi-tropical karsts. Hence, at the time of their formation some 3 Ma or more ago, the massive speleothem deposits are evidence for a warmer, and certainly a much wetter, climate than that of today.