Acid Phosphatase Complex from the Freshwater Snail Viviparus viviparus L. under Standard Conditions and Intoxication by Cadmium Ions

Acid phosphatases differing in both subcellular localization and substrate specificity were isolated for the first time from the liver of the freshwater snail Viviparus viviparus L. by preparative isoelectrofocusing. One of five characterized phosphatases is highly specific to ADP and the others can hydrolyze (at variable rate) a series of natural substrates. A scheme is proposed for the involvement of the studied phosphatases in carbohydrate metabolism. We have also studied some peculiarities of the effect of Cd2+ in vitro and in vivo on the activities of individual components of the acid phosphatase complex and corresponding changes in metabolism of the freshwater snail as a new test-object allowing the estimation of toxicity in water.     

海马脑片抗癫痫药物研究的离体模型

目的：建立离体海马脑片癫痫样放电模型并用于抗癫痫药物研究。方法：在豚鼠海马脑片上灌流青霉素建立颠阗痫样放电的离体模型。并用此模型对抗癫痫药物苯巴比妥钠和苯妥英钠两种药物在不同浓度下对癫痫样放电的对抗作用进行了定量分析,结果：在海马脑片上灌流致痫药物可建立一个较好的离体组织癫痫样放电模型,苯的对抗作用进行了定量分析,结果：在海马脑片上灌流致痫药物可建立一个较好的离体组织癫痫样放电模型。苯巴比妥和苯妥英钠在一定浓度下均有显著对抗癫痫样放电的作用,且与整体实验的结果相一致。结论：本实验建立有离体脑片模型具有实验手段简单,方法灵活,易于建立药物量效关系等优点,可用于抗癫痫药物筛选和研究。     

电刺激大鼠脊神经皮支对远距离机械感受单位电活动的影响

实验采用分离神经细束的方法,观察逆行电刺激大鼠脊神经背侧皮支后,在相距较远的神经细束上记录到的Aδ和C类机械感受单位电活动的变化。刺激T9脊神经背侧皮支,在T12神经细束上记录到59.3%（16/27）的Aδ和71.2%(37/52）的C类单位在刺激后90～120s放电显著增加。刺激T8脊神经背侧皮支,在T12神经细束上记录到47.8%(11/23）的Aδ单位和36.6%(15/41）的C类单位在刺激后120～150s放电显著增加。大多数单位（18/23）的机械感受阈值在电刺激远距离脊神经背侧皮支后降低。结果表明,逆行电刺激外周感觉神经,可以使相距较远的Aδ和C类机械感受单位致敏,其传入放电增加。     

Freshwater bryozoans (Bryozoa) of Norway III: distribution and ecology of Plumatella fruticosa

Bryozoans were investigated during field studies of 601 lakes and other surface water bodies throughout Norway from 1960 to 1978. The frequency of occurrence of Plumatella fruticosawas evaluated in relation to 12 environmental variables. Statistically significant deviations from the frequencies expected on the basis of random distribution were described using the categories preference, avoidance, and absence. According to our material P. fruticosais one of the most common bryozoan species in Norwegian fresh water, represented in samples from 251 localities. This species occurred frequently all over the country, north to 71° 06 N (the northernmost record globally). Maximum elevation above sea level was 1179 m (maximum for Northern Europe).In most studies of freshwater bryozoans from the holarctic region, Plumatella fruticosahas been reported as widely distributed, but locally rare. In Norway, however, P. fruticosa is frequently found all over the country, even far to the north. The species apparently finds an optimal climate in the cold temperate and cold regions of Norway. Plumatella fruticosapreferred lakes, avoided slow-flowing rivers and ponds, and was absent in smaller water bodies. The species preferred somewhat higher elevation (400–900 m above sea level), but avoided lakes with the lowest summer temperatures (below 11 °C). P. fruticosa also preferred oligotrophic conditions with poor aquatic vegetation, stony shores, lakes poor in calcium and magnesium (sometimes almost comparable with distilled water), where the water was clear and colourless, and slightly acidic to neutral. The species also preferred lakes surrounded by Sphagnum bogs and was absent when pH was below 5.2. P. fruticosa avoided eutrophic conditions with rich aquatic vegetation, alkaline water (pH above 7.0), lakes with a higher content of calcium and magnesium and those with strongly coloured water (above 100 mg Pt l^–1). In spite of its preference for ion-poor conditions, it was also found in a brackish water lake. For most environmental variables, the species had a wider tolerance range than reported from elsewhere.     

8-OH-DPAT and MK-801 affect epileptic activity independently of vigilance

Vigilance and parallel occurrence of epileptic activity after administration of the 5-HT_1A agonist 8-OH-DPAT and the NMDA receptor antagonist MK-801 were studied in the genetic absence epilepsy model WAG/Rij rats. Spike-wave discharges (SWD) were present predominantly in passive awake and light slow wave sleep (SWS1) either in control animals or after treatments. Injection of 8-OH-DPAT (20.0 μg/rat i.c.v.) caused marked increase and MK-801 (10.0 μg/rat i.c.v.) decrease in SWD densities, thus the ratios of SWD in passive awake and in SWS1. SWD densities of MK-801 plus 8-OH-DPAT in combination were similar to those of CSF+CSF treated control rats. Both 8-OH-DPAT and MK-801 transiently increased the duration of active awake, increased latency and decreased duration of rapid eye movement (REM) sleep. 8-OH-DPAT increased the amount of SWD despite the decrease in the duration of SWS1. MK-801 decreased the amount of SWD despite the lack of significant change in duration of passive awake or SWS1. Pre-treatment with MK-801 reversed 8-OH-DPAT- induced increase in duration of SWD without any effect on 8-OH-DPAT-induced changes in sleep parameters. Our studies provide evidence that 8-OH-DPAT-induced epileptic activity is independent of its effect on sleep, and that interaction of serotonergic and glutamatergic systems plays a role in the generation of SWD, but not in the regulation of vigilance and sleep.     

非NMDA受体参与双相呼气和吸气神经元电活动的调节

在新生大鼠延髓脑片上同步记录舌下神经根和双相呼气神经元／吸气神经元单位的放电活动,并在灌流的改良Kredbs液中先后加以非NMDA受体的激动剂KA和拮抗剂DNQX,观察对神经元单位放电的影响,以进一步探讨非NMDA受体在对双相呼气神经元之间交互兴奋和吸气神经元兴奋性突触输入中的作用,结果表明,使用非NMDA受体激动剂KA以后,双相呼气神经元的放电频率和蜂频率都明显增大,吸气神经元中期放电的频率和非NMDA受体激动剂KA以后,双相呼气神经元的放电频率和峰频率都明显增大,吸气神经元中期放电的频率和峰频率也显著增大,而早期和晚期放电的频率无明显改变,用相应拮抗剂以后,上述效应明显被抑制,结果提示,非NMDA受体参与了双相呼气神经元之间的交互兴奋作用,并且也介导了吸气神经元的兴奋性突触输入／     

肌梭传入对呼吸的调节作用

实验用６３只麻醉、制动、切断双侧颈迷走神经、人工呼吸的家兔,以延髓呼吸相关神经元（ＲＲＮ）和膈神经放电（Ｐｈｒ．Ｄ）作为呼吸观测指标,观察了股动脉注射琥珀胆碱（Ｓｃｈ）诱发的肌梭传入活动对呼吸的影响。结果显示：（１）股动脉注射Ｓｃｈ可产生明显的呼吸易化作用,主要表现为吸气时程（Ｔｉ）延长、呼气时程（Ｔｅ）缩短不明显,Ｔｉ／Ｔｅ比值增加以及呼吸频率（ＲＦ）变化不在,称为吸气延长效应;或Ｔｅ缩短,Ｔｉ     

Habitat Preference, Reproduction and Diet of the Earthworm Eel, Chendol keelini (Teleostei: Chaudhuriidae)

The ecology of the earthworm eel, Chendol keelini, was studied in the field over a period of nine months. In addition this information was supplemented by aquarium observations. The species was most abundant in pools where it was associated with leaf litter and mats of fine tree roots along the banks. It fed on benthic invertebrates, especially chironomid and ephemeropteran larvae. C. keelini is sexually dimorphic; adult males develop a headhump and grow to a larger size than females. Reproduction was seasonal; the reproductive phase coincided with the wet season and lasted for several months. Fecundity was around 40 eggs per clutch. The eggs were spherical, between 1.2 and 1.5mm in diameter, and possessed a pair of long filaments for adhesion to the substrate. Females probably spawned more than once during the breeding season. The length frequency distributions and juvenile growth suggest that C. keelini is a short-lived species that matures during the first year with few individuals surviving to the second breeding season.     

Distribution and palaeoecology of freshwater algae and stromatolites: III, some new forms from the Carboniferous, Permian and Triassic of France and Spain

New collections allow us to describe some new algae forming: a) centimetric, unorganized, masses (Toutinella bifurcata from the Middle Triassic of Provence); b) large, decimetric masses (Zarramanella menorica from the ‘Buntsandstein’ of Minorca, Balearic Islands) and c) interesting, plurispecific biocenosis, laminated and silicified, from the French Massif Central: Lower Stephanian of Saint-Étienne basin (with Hankerpella minima, Baltzerella stephaniense, Ponsinella undulata) and Lower Autunian of Bourbon-l'Archambault basin (Hanskerpella pustulata, Baltzerella stephaniense, Ponsinella multifrons, Sarfatigirella intricata). Other forms are badly preserved, one is possibly a Broutinella sp. and another may be a coccoid form of cyanobacteria or chlorophyceae. Silicified biocenoses macroscopically occur in the form of regular laminations, exhibiting vertical, planar joints (1–2 cm wide) and horizontal, planar joints, 5 mm to 3 cm thick, with various sedimentary infillings. These facies represent early and late silicifications of biological felts (mats), probably previously partly calcified and affected by desiccation cracks partly infilled before the silicification. There is no evidence for an early silicification of living filaments and trichomes. The silicification also affects other types of sediments (petites, sandstones, conglomerates, breccias) associated with the algal formations. Macroscopically, these laminated formations do not show domes or hemispheres; on the other hand, these features clearly appear under the microscope, and these formations are true stromatolites. The basins of Saint-Étienne and Bourbon-l'Archambault contain volcanic rocks; the siliceous series, very localized in the basins, represent an impregnation of various primary materials by silica of hydrothermal origin. The present study is voluntarily limited to the palaeontological and palaeoecological appearances; algal laminations formed in ephemeral pools and small lakes, under very particular conditions, ‘hydrothermal’ sensu lato, are still to be stated more precisely.

Résumé

Des récoltes nouvelles permettent de décrire quelques algues nouvelles formant des amas centimétriques non organisés (Toutinella bifurcata du Trias moyen de Provence), de grosses masses décimétriques (Zarmmanella menorica du Buntsandstein de Minorque) et d'intéressantes biocrenoses plurispécifiques laminées et silicifiées du Massif central français: Stephanien inférieur de Saint-Étienne (à Hankerpella minima, Baltzerella stephaniense, Ponsinella undulata), Autunien inférieur du bassin de Bourbon-l'Archambault (Hanskerpella pustulata, Baltzerella stephaniense, Ponxinella multifrons, Sarfatigirella intricata). D'autres formes sont mal conservées, l'une serait attribuables à une ? Broutinella sp. et une autre à une coccoide (cyanobactéries ou chlorophycées). Les biocœnoses silicificées se présentent macroscopiquement sous forme de laminations régulières, accidentées de fentes planes verticales (1–2 cm de largeur) et de fentes planes horizontales (5 mm–3 cm de hauteur), à remplissages sédimentaires variés. Ces faciès correspondent à des silicifications précoces et tardives de feutres biologiques probablement en grande partie calcifiés précocement et affectés de fentes de dessiccation partiellement remplies avant la silicification. Aucun indice de silicification de filaments et de trichomes du vivant des organismes n'a pu être observé. La silicification affecte aussi d'autres sédiments (pélites, grès, conglomérats, brèches), associés aux anciennes formations algaires. Macrospiquement, ces formations laminées ne montrent pas de dômes ni d'hémisphères; en revanche ces structures apparaissent parfaitement au microscope, et ce sont de véritables stromatolites. Les bassins de Saint-Étienne el de Bourbon-l'Archambault contiennent des formations volcaniques; les formations siliceuses, qui sont très localisées dans les bassins, correspondent certainement à une imprégnation par de la silice d'origine hydrothermale de sédiments variés. La présente étude se limite volontairement à l'aspect paléontologique et paléoécologique; les laminations algaires se sont formées dans des bassins ou de petits lacs éphémères, dans des conditions très particulières, hydrothermales sensu lato, encore à préciser.