The benthic communities of the saline lakes Abijata and Shala (Ethiopia)

Lake Abijata lies in a shallow depression (maximum depth 8–9.5 m); the water is green with phytoplankton and it supports large fish and bird communities. Lake Shala lies in a deep caldera (maximum depth reputedly 260 m); phytoplankton is sparse and fish and bird communities scanty.Lakes Abijata and Shala, sampled in January, 1985, had conductivities of 14 000 and 21 000 microSiemens cm^-1 at 25 °C respectively, mainly due to high sodium, carbonate and chloride ions. Calcium concentrations are very low.The benthic fauna was studied with an Ekman grab to a depth of 8.5 m in Abijata and 15.5 m in Shala and was found to be dense in both lakes but varying greatly in composition at different depths. In Abijata the benthos consisted mainly of Ostracoda and Chironomidae, and in Shala mainly of Tubificidae, Ostracoda and Chironomidae. There were very few Nematoda. No true halophilic species were found but the community consisted of euryhaline forms found also in non-saline waters. Predatory invertebrates were absent and many of the dominant species, notably of the Chironomidae, were different from those of non-saline lakes nearby.     

Associations and distribution of benthic nematodes in the Ethiopian Rift Valley lakes

The nematode associations in six Ethiopian rift lakes, one man-made lake, and three crater lakes were studied and related to water conductivity, lake depth and sediment particle size. The lakes investigated lie at moderate altitudes (1200–2000 m), are alkaline and vary in their conductivities. The rift lakes Abijata and Shala and the crater lakes Aranguadi, Kilotes and Chitu are soda lakes (K₂₅ > 6000 μS cm⁻¹), while the remaining five lakes and the man-made Lake Koka are within the freshwater range of conductivity (K₂₅ < 6000 μS cm⁻¹). A total of 16 species were identified including six new species. The nematode associations varied between lakes and were restricted to very few species in each lake. Most nematodes were restricted to non-saline lakes. The most dilute L. Zwai had a higher number of nematode species (12) and abundance than other lakes. The saline lakes Shala and Kilotes had nematode assemblages made up of only a single species (Mesodorylaimus macrospiculum). No nematodes were found in the hypersaline crater L. Chitu. Tobrilus africanus appeared more euryhaline than other nematodes occurring at conductivities as high as 15 000 μ S cm⁻¹ (L. Abijata). Five of the most common species (Dorylaimus sp., Monhystera stagnalis, Aphanolaimus tudoranceai, Tobrilus africanus and Actinolaimus perplexus) were associated with medium grained sand. A monthly variation in density of nematodes in L. Zwai is also shown.     

Determination of bacterial cell number and cell volume by means of flow cytometry, transmission electron microscopy, and epifluorescence microscopy

Comparative measurements of bacterial total counts and volumes of flow cytometry (FCM), transmission electron (TEM), and epifluorescence microscopy (EFM), were undertaken during a four week mesocosm experiment. Total counts of bacteria measured by TEM, EFM, and FCM were in the range of 1 · 10⁶−6 cells ml⁻¹, 1 · 10⁶−3 · 10¹⁶ cells ml⁻¹, and 5 · 10⁵ cells ml⁻¹ respectively. The mean volume of the bacterial community, measured by means of EFM and TEM, increased from 0.12–0.15 μm³ at the start of the experiment to 0.39–0.53 μm³ at the end. Generally, there was good agreement between the two methods and regression analyses gave r = 0.87 (p < < 0.01) for cell volume and r = 0.97 (p < < 0.01) for cell number. DAPI stained bacteria with volumes less than 0.2 μm³ were not detected by flow cytometry and these were generally an order of magnitude lower than counts made by TEM and EFM. For samples where the mean bacterial cell volume was longer than 0.3 μm³, all three methods were in agreement both with respect to counts and volume estimates.     

Long-term changes in chemical features of waters of seven Ethiopian rift-valley lakes

Chemical and chlorophyll a concentrations of seven Ethiopian rift-valley lakes were studied during 1990–2000. Results were compared with studies made between 1960 and 1990 in an attempt to detect long-term changes. Three different trends are apparent in the salinities (and the correlates conductivity, alkalinity, sodium concentration) of these lakes over the last 40 years: three lakes (lakes Zwai, Shalla and Abaya) have maintained their salinity levels from the 1960s, two lakes (lakes Langano and Awassa) have become more dilute, and the salinity levels of Lake Chamo and the soda lake Abijata have increased. Concentrations of silicate decreased in almost all the lakes whereas soluble reactive phosphorus (SRP) increased in most lakes. Chlorophyll a concentrations were higher in the recent samples from all lakes except two, which in conjunction with results from SRP and silicate analyses suggest eutrophication in four out of the seven lakes studied. The study relates salinization in lakes with closed drainage to increased human activities in their catchments, intensified by changes in climate during the last three decades in sub-Saharan Africa.     

Magnetostratigraphy and sedimentologically derived geochronology of the Quaternary lacustrine deposits of a 3000 m thick sequence in the central Qaidam basin, western China

The Qaidam basin is a large basin in western China where the thickness of Quaternary deposits has a range of 2000–3000 m at its subsiding depocentre. This study investigated the chronology of the Quaternary deposits, including palaeomagnetics, biostratigraphic correlation, rates of sediment accumulation, seismic reflection surveys and electrical property correlations. The results give a full interpretation of ages for the sequence from bottom to top. The oldest sequence age was defined by the first appearance of Microlimnocythere sinensis Huang, and was placed in the Gauss Epoch, estimated at approximately 3 Ma by extrapolation of accumulation rates. The M/G boundary occurs at the base of the third fossil zone of Ostracoda (the first appearance of Qinghaicypris crassa Huang), or at the marker layer K₁₀ of the electrical log in the Sebei anticline area, considered here to be 2.48 Ma. The Olduvai event in the fifth fossil zone, spanning electrical layers K₄ and K₃ in the Sebei area, occurs at reflection layer T₀⁻¹ of seismic stratigraphy which could be stratigraphically correlated in the whole basin. The boundary of Early/Middle Pleistocene such as the Brunhes and Matsuyama (B/M) boundary, falls within the eighth fossil zone and coincides with electrical marker K₀¹. Two boundaries corresponding to Middle/Late Pleistocene and Pleistocene/Holocene occur at the bases of the 11th and 12th biozones respectively, neither of which can be correlated with seismic stratigraphy and electrical logs in the basin due to the lack of widely distributed lacustrine deposits since the Middle Pleistocene. The ages of the boundaries can be tested by deposition rates of different facies derived from the varves and synchronous deposits. As a result, geochronological sequences of subsurface stratigraphy could be established within a basin-wide area on the synchronology of seismic reflectors and correlations of electrical logs as well as biozones.     

Effect of products from heated amino acids on conductance in lipid bilayer membranes and non-aqueous solvents

The electrical conductance of lipid bilayer membranes of oxidized cholesterol is elevated 10²–10³ times by the addition of various products of the heating of amino acids. Solution of such products in chloroform yields a greater increase in conductance. The results are obtained with both water-soluble and water-insoluble fractions. They are discussed in the context of the origin of electroconductive tissue.     

Ontogeny of light response in the early life history of the red king crab Paralithodes camtschaticus (Anomura: Lithodidae)

Phototactic responses of light-adapted zoeae IV, glaucothoe, and first stage juveniles of the red king crab to three intensities of white light were quantitatively measured under laboratory conditions. All stages observed were photopositive to all light intensities tested, except for late glaucothoe (10 days since moulting) which did not respond to light stimuli. Phototactic response changed in the early life history of the red king crab. The extent of photopositive movement decreased after each metamorphosis. Peak phototactic response in zoea IV were observed at a light intensity of 1.9 × 10¹³ q cm^-2 s^-1, in early glaucothoe at 1.1 × 10¹⁰ q cm^-2 s^-1 and in juveniles at 1.3 × 10⁹ q cm^-2 s^-1. The data on behavioural responses to light may provide a better understanding of the early life history, survival and recruitment of the red king crab and assist the development of feasible methods and techniques for aquaculture of this species.     

Palaeoclimatic conditions in the upper Pleistocene and Holocene Bhimtal-Naukuchiatal lake basin in south-central Kumaun, North India

A 52 m thick upper Pleistocene and Holocene terrestrial succession in the Bhimtal-Naukuchiatal basin, south-central Kumaun Himalaya, India was studied using chronological, palaeontological, palynological and δ¹³C measurements. The section recorded evidence for climatic changes. At least two phases of arid climate and one phase of humid climate were recognised. Preliminary palaeomagnetic studies revealed a reversal of polarity, presumably correlatable with the Mono Lake excursion. Prior to this, no reversal event in the upper Pleistocene-Holocene terrestrial sediments of Indian subcontinent is known. A fossiliferous horizon, discovered in the lower part of the section, consisted of Sorex and Mus. This is the only report of a Late Pleistocene micromammalian assemblage in the Kumaun Himalaya.     

Energy transfer within the isolated light-harvesting B800–850 pigment-protein complex of Rhodobacter sphaeroides

We have used picosecond absorption spectroscopy with low intensity (5 · 10¹¹–5 · 10¹² photons · pulse⁻¹ · cm⁻²) continuously tunable infrared (800–900 nm) pulses to study the energy transfer dynamics in the isolated B800–850 pigment-protein complex of Rhodobacter sphaeroides. Our results suggest the following picture of the energy transfer dynamics: (i) a fast transfer, within approx. 1 ps, from BChl 800 to BChl 850; (ii) transfer among different BChl 800's with a rate which is at the most of the same order of magnitude as that of BChl 800 → BChl 850 transfer; (iii) very fast transfer (k > 1 · 10¹² s⁻¹) between BChl 850 molecules. Assuming Förster type of energy transfer maximum distances of about 22 and 15 Å are obtained for the BChl 800–BChl 850 and BChl 850–BChl 850 separations, respectively.     

QSAR study on inhibition of brain 3-hydroxy-anthranilic acid dioxygenase (3-HAO): A molecular connectivity approach

The ability of 4,5-, 4,6-disubstituted and 4,5,6-trisubstituted 3-hydroxyanthranilic acid derivatives to reduce the production of the excitotoxin quinolinic acid (QUIN) by inhibition of brain 3-hydroxyanthranilic acid dioxygenase (3-HAO) has been investigated using molecular connectivity indices (⁰χ^v, ¹χ^v, ²χ^v). The in-vivo inhibition of 3-HAO in rat cortex (pIC₅₀, nM) is used for this purpose. The regression models obtained suggest that the degree of branching of the compounds under study have a dominant role in the observed inhibition potency. The data were used to generate quantitative structure–activity relationship (QSAR) models for estimating the potency of 3-HAO. The information obtained from the correlation should be useful in designing more potent analogues.     

A late pleistocene and holocene vegetation and environmental record from Lake Wangoom, Western Plains of Victoria, Australia

Pollen, microfaunal and sedimentological evidence from the top 20 m of sediment in a closed volcanic crater lake is used to construct a detailed record of vegetation and environmental conditions through the Holocene and a substantial part of the Late Pleistocene. Radiocarbon dating suggests that the sequence covers tha last 51,000 yr or so. High lake-levels and the presence of forest or woodland vegetation indicate that the Holocene and the basal few thousand years of the record experienced wet and warm conditions. The earliest period was succeeded by a long phase of lower but variable moisture levels before more arid conditions resulted in the replacement of forest and woodland by herbaceous vegetation and frequent lake drying. Periods of slight amelioration occurred between about 27,000 and 19,000 and before 15,000 radiocarbon yr ago. Maximum aridity occurred between about 19,000 and 10,000 yr B.P., a period incorporating the height of the last glacial. During the Pleistocene, the lake became gradually more saline but has been fresh during the Holocene, even under low lake-levels.

An increase in charcoal values is recorded, probably around 20,000 years ago, and this could have resulted from increased burning as a result of the activities of Aboriginal people. This may have also caused a change in understorey vegetation from one composed largely of Asteraceae, to grassland.

The record is compared with others from southeastern Australia and there is good correspondence through the last 20,000 or 30,000 yr but, before this, problems of dating and the condensed nature of most sequences prevent detailed correlation.     

鄱阳湖流域植被总初级生产力时空变化特征及其气候驱动因子分析

植被总初级生产力(GPP)在陆地生态系统和全球气候变化研究中占有重要地位。基于MODIS GPP遥感数据产品、土地覆盖数据和气象观测数据,对2000–2013年鄱阳湖流域GPP的时空变化及其与气候因素的关系进行了分析。结果表明,鄱阳湖流域GPP的年总量变化介于88–2 493 g C·m~(–2)·a~(–1)之间,平均值为1 361 g C·m~(–2)·a~(–1);GPP年总量最小值出现在2002年,最大值出现在2004年。GPP年际变化呈现明显的上下波动现象,并呈缓慢增长趋势。近14年植被GPP年均值在空间分布上表现出由湖区中心向四周散射递增的特点,GPP显著增加的区域占全区总面积的40%,主要分布在研究区东北部。相关性分析显示,气温对GPP年际变化的影响程度强于降水。此外,火灾对GPP的年际变化也具有一定的影响。该研究可为了解研究区的植被生长状况和生态环境质量提供参考。     

Formation,evolution and demise of a tectonically controlled volcanic lake: A case study from the lower Pleistocene Sousaki succession

The complex interaction of local tectonics and volcanism usually produces palaeoenvironments that require to be studied in detail in order to define the role of each factor in the local palaeoenvironmental evolution. This is the case for the Sousaki Basin lying at the eastern part of the Gulf of Corinth. It presents a complex Pliocene and Pleistocene stratigraphy, affected by deformational processes due to the local tectonic regime. The Sousaki volcano is a low standing volcano that constitutes the western endpoint of the South Aegean Volcanic Arc and may also contribute to the palaeoenvironmental evolution of the basin. The studied section, in the Sousaki Basin, consists of marly and conglomeratic layers with intercalations of organic rich sediments. The base of the section consists of impermeable volcanic products. A micropalaeontological analysis based on 29 samples has been conducted in order to reconstruct the palaeoenvironment after the termination of the activity of the last volcanic period. A diversified fauna has been retrieved, consisting of Gelasian (early Pleistocene) ostracods, gastropods, diatoms, charophyte gyrogonites, thecamoebians, fish otoliths and teeth. Count-based statistical treatments performed on ostracod species revealed that a volcano-tectonic lake evolved after the emplacement of the volcanic products in the basin. Afterwards, a braided river environment dominated the landscape. Due to the lateral migration of the riverbed, several laterally evolving sub-environments were established, ranging from marginal lakes to marshes. Ultimately, the palaeoenvironmental reconstruction of the study area revealed the formation, evolution and demise of a tectonically controlled volcanic lake.     

Sources and accumulation rates of organic carbon in an equatorial peat bog (Burundi, East Africa) during the Holocene: carbon isotope constraints

The relationship between organic carbon accumulation rates and ¹³C/¹²C ratios of total organic carbon (TOC) was investigated in an highland peat bog core (Ru-3) from Equatorial Africa. This core yielded a sequence spanning the last 14 kyr and was analysed with a 100–300 yr resolution for TOC-δ¹³C values. The Holocene section shows contrasted TOC accumulation regimes and TOC δ¹³C varying between −28.5 and −19.5‰ with a few very short ‘isotopic excursions' (dated at ca. 9.3, 7.5, 4.2 ka B.P.). The organic carbon accumulation rates range from 2 to 20 mg C cm⁻² yr⁻¹. They increase when TOC becomes more depleted in ¹³C, notably between 12 and 9.8 ka B.P., 8.5 and 7.8 ka B.P. and after 1.6 ka B.P. Periods of restricted carbon storage correspond to heavier TOC accumulation at 9.3, and between 7.5 and 1.6 ka B.P. At the study site, the δ-variations can be related to variable C4-plant inputs, and possibly, to changes in the fractionation between CO₂ and the organic carbon in C3 vascular plants. The Ru-3 record indicates restricted carbon storage during the periods of increased contribution from C4 plants and/or of decreased fractionation between CO₂ and organic carbon in C3 plants. Changes in TOC-δ¹³C values in core Ru-3 seem to match fluctuations of East Equatorial African lakes. High lake stands correspond to low δ¹³C intervals and vice versa. This points to indirect climatic forcing of δ¹³C changes in intertropical peats.     

Late Quaternary Lake-level fluctuations and environments of the northern Rift valley and Afar region (Ethiopia and Djibouti)

The late Quaternary limnology of the Rift and Afar lakes is compared from two viewpoints: their record of lake-level fluctuations, and the evolution of their sedimentary facies and biocoenoses. The similarities and divergences are examined in the light of the volcano-tectonic and hydrological setting of the lake basins. All the lakes lie on an altitudinal gradient of precipitation and evaporation leading from the Ziway-Shala Basin, near the highest part of the Main Ethiopian Rift floor, to the desert basins of Afrera and Asal. The contribution of surface runoff relative to groundwater inflow decreases in the same. direction.Clear parallels exist between the main stages in the evolution of all the lakes. At least two distinct lacustral phases during the late Pleistocene were followed by a very arid period during which the lakes contracted to their present extent or less. An important early to mid-Holocene period of high lake levels, beginning ca. 10,000 B.P. in both regions, was followed by a clearly defined regression between 6,000 and 4,000 B.P.     

Haplotypes of nine single nucleotide polymorphisms on chromosome 19q13.2-3 associated with susceptibility of lung cancer in a Chinese population

To evaluate the joint effect of nine single nucleotide polymorphisms for three DNA repair genes in the region of chromosome 19q13.2-3 on susceptibility of lung cancer in a Chinese population, we conducted a hospital-based case–control study consisting of 247 lung cancer cases and 253 cancer-free controls matched on age, gender and ethnicity. Associations between the haplotypes and susceptibility of lung cancer were tested. The global test of haplotype association revealed a statistically significant difference in the haplotype distribution between cases and controls (global test: χ² = 60.45, d.f. = 15, P = 2.11E−07). The two haplotypes were underrepresented among cases (Hap5 defined by ERCC1118^A–ERCC2156^C–ERCC2312^G–ERCC2751^A–XRCC1194^T–XRCC1206^A–XRCC1280^G–XRCC1399^G–XRCC1632^G and Hap12 defined by ERCC1118^G–ERCC2156^C–ERCC2312^G–ERCC2751^A–XRCC1194^C–XRCC1206^A–XRCC1280^G–XRCC1399^A–XRCC1632^G). Three of the haplotypes were overrepresented among cases (Hap3 defined by ERCC1118^A–ERCC2156^C–ERCC2312^G–ERCC2751^A–XRCC1194^C–XRCC1206^A–XRCC1280^G–XRCC1399^G–XRCC1632^G, Hap4 defined by ERCC1118^A–ERCC2156^C–ERCC2312^G–ERCC2751^A–XRCC1194^C–XRCC1206^G–XRCC1280^G–XRCC1399^G–XRCC1632^A, and Hap10 defined by ERCC1118^G–ERCC2156^A–ERCC2312^G–ERCC2751^A–XRCC1194^T–XRCC1206^A–XRCC1280^G–XRCC1399^G–XRCC1632^G). Haplotypes 3 and 10 (cases = 5.7%, controls = 1.0%, OR = 6.56, 95%CI = 1.83–23.54, P = 0.001; cases = 13.3%, controls = 5.6%, OR = 2.73, 95%CI = 1.51–4.94, P = 0.0006) were the most strongly associated with increased lung cancer risk. There was considerable linkage disequilibrium exists between SNPs both within genes and between genes in the region. The two blocks for solid spine of LD and six htSNPs were found. The haplotype analysis suggested that the biologically effective polymorphisms co-segregate with some of the haplotypes. This result supports the hypothesis that the sub-region is important for lung cancer susceptibility. Haplotype studies using larger study groups will be required to obtain conclusive results.     

Topical delivery of retinyl ascorbate: 4. Comparative anti-oxidant activity towards DPPH

The free radical scavenging properties of retinyl ascorbate (RA-AsA) were determined by monitoring the decomposition of 2,2-diphenyl-1-picrylhydrazyl (DPPH) as a function of time and in comparison with ascorbic acid (AsA), ascorbic acid palmitate (AsA-Pal), retinoic acid (RA), retinol (ROL) and retinol palmitate (Rol-Pal). The rate constant of RA-AsA (mean₃±SD) was 4.9±0.3 M^-1 s^-1, and indicated greater potency as an antioxidant compared to the rest of the test compounds (AsA 3.4±0.4 M^-1 s^-1, AsA-Pal, 2.9±0.2 M^-1 s^-1, RA 1.4±0.3 M^-1 s^-1, ROL 1.3±0.1 M^-1 s^-1, Rol-Pal exhibited insignificant activity). The decomposition rate constant of DPPH, 5±0.6 × 10^-8 M^-1 s^-1, in ethanol and BHA, 154±3 M^-1 s^-1 were both used as control. The compound RA-2-carboxy-2-hydroxy-ethanoate was isolated by prep-TLC and was identified, by ¹³C and ¹HNMR spectroscopy, as the major by-product from the reaction of RA-AsA with DPPH, which was also found to be potent antioxidant, 2.1±0.2 M^-1 s^-1. This suggests that oxidation of AsA moiety did not lead to the production of erythrulose species, which could cause deleterious modifications of cellular proteins.     

Inhibition of cryogelation by the novel synthetic peptide (Gly-Arg-Lys-Lys-Thr): recognition site of extra domain A containing fibronectin for heparin in cryogelation

Cryogel is a physical gel formed by the heterophilic aggregation of extra domain A (EDA) containing fibronectin [EDA(+)FN], plasma fibronectin (pFN), fibrinogen (Fbg) and heparin (Hep) in the blood of rheumatoid arthritis (RA) patients. In cryogelation EDA(+)FN cross-links to form an interaggregate of cryogel with Hep. In the present study, we determined the recognition structure of Hep for EDA(+)FN by using oligo- and desulfonated-Hep. The affinity constant (KA) (1.2×10⁸ per M) of oligo-Hep for EDA(+)FN did not change with a decrease in number-average molecular weight (4.9×10⁴→6.0×10³). The KA-value of desulfonated-Hep for EDA(+)FN decreased from 3.2×10⁸ to 1.0×10⁷ per M with a decrease in the sulfonation ratio (7.0→4.3%). We also determined the recognition structure of EDA(+)FN for Hep by an inhibition experiment on the heparin binding domain II (HepII) in EDA(+)FN with the synthetic peptides, Arg–Arg–Ala–Arg (RRAR), Asp–Gln–Ala–Arg (DNAR), Ile–Lys–Tyr–Glu–Lys (IKYEK), and Gly–Arg–Lys–Lys–Try (GRKKT). The GRKKT sequence clearly inhibited bonding between EDA(+)FN and Heps containing oligo- and desulfonated-Hep. The amount of cryogel formed in the RA-patient model plasma corresponded to the EDA(+)FN concentration in cryogel (36.7%) normalized by the EDA(+)FN concentration in plasma. When GRKKT was added to plasma, the EDA(+)FN concentration fell to 10.5%. These results demonstrated that inhibition of cryogelation in plasma could progress to a novel treatment for RA.     

海河流域农田生态系统环境损益分析

根据生态系统服务的内涵,建立了海河流域农田生态系统服务功能评价指标体系,并利用市场价值法、影子工程法和机会成本法等,定量评价了海河流域农田生态系统服务的经济价值和农田环境成本.结果表明：2005年,海河流域农田生态系统环境效益总价值为1802.64亿元;其中,调节功能的价值（794.16亿元）占44.06%,支持功能的价值（1008.48亿元）占55.94%,提供产品和文化功能未进行核算.从不同的功能类型来看,其价值量大小依次为释氧>涵养水源>营养元素循环>土壤保持>废弃物净化>环境净化>固碳>秸秆还田.2005年,海河流域化肥流失和温室气体排放的环境成本较大,为422.93亿元.其中,化肥流失量为427.42×10⁴ t,成本为151.91亿元;产生的温室气体折算为CO₂的量为3599.65×10⁴ t,成本为271.02亿元.     

Peripheral and central actions of AF64A (ethylcholine mustard aziridinium ion) on acetylcholine release, in vitro: Comparison with hemicholinium

The acute effects of ethylcholine mustard aziridinium ion (AF64A) and hemicholinium-3 (HC-3) on the release of endogenous acetylcholine (ACh) from isolated tissues were examined. Whereas addition of HC-3 (10⁻⁶–10⁻⁵ M) significantly reduced the output of ACh from isolated guinea-pig ileum longitudinal muscle strip elicited by 10 Hz stimulation, AF64A had no effect and even enhanced the release of radiolabel elicited by 1 Hz stimulation when this tissue was pre-loaded with [³H]choline. Similarly, HC-3 (10⁻⁵ M) reduced ouabain-induced endogenous ACh release from isolated rat hippocampus. Addition of AF64A (10⁻⁵−5 × 10⁻⁵ M) caused a slight increase in ACh release. In isolated rat cortex, however, AF64A did not affect ACh release. Moreover, AF64A caused a decrease in ouabain-stimulated ACh release from striatum. The present study indicates that: (a) the in vitro actions of AF64A differ from those of HC-3 and (b) the acute effects of AF64A on endogenous ACh release vary, depending on the tissues studied and the stimulation parameters used.