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H O X^osv^ ~ O 3 X 3 2 3 SMITHSONIAN INSTITUTION NOlinXUSNI NVINOSHXIINS S3UIVH9I1 LIB RAF “ 2 r- z *"~ ^ ^ m NVINOSHimS S3 I H VH 8 l “I L I B R AR I ES^SMITHSONIAN "INSTITUTION ^ NOIXOXI * 1 1 I i | | gRj| § 3 •/,* SMITHSONIAN INSTITUTION NOIXOiliSNI NVINOSHXHAIS0°S3 I 8VH 8 ll^LI B RAF x-x ■ to 1 Tha Glasgow Statural History Society (formerly The Andersonian Naturalists of Glasgow) The object of the Society is the encouragement of the study of natural history in all its branches, by meetings for reading and discussing papers and exhibiting specimens, and by excursions for field work. The Glasgow Natural History Society meet at least once a month except during July and August, in the University of Glasgow, the University of Strathclyde or the Glasgow Art Gallery and Museum. The present rates of subscription per annum are: for Ordinary Mem- bers, £4; for Junior Members, £1.25; for Family Members, £1; and foi School Members 50p. Further information regarding the Society’s activities and membership application forms are obtainable from the General Sec- retary: Mrs M. E. E. McLaughlin 15 Partickhill Road Glasgow Gil 5BL The Glasgow Naturalist Published by the Glasgow Natural History Society, November, 1980. ISSN 0373-241X. Price £4.00 Edited by E. W. Curtis with the assistance of A. C. Crundwell, R. M. Dobson, A. McG. Stirling and J. H. Dickson. Contributions are invited, especially when they bear on the natural history of Scotland. A note of information for contributors is available from the Editor. Smaller items are also welcome from members and others. These may cover, for example, new stations for a species, rediscoveries of old records, additions to records in the Atlas of the British Flora, unusual dates of flowering, unusual colour forms, ringed birds recovered, weather notes, occurrences known to be rare, interesting localities not usually visited by naturalists. (The nomenclature of vascular plants should be as in Dandy, List of British Vascular Plants, 1958 and its revision. 1969). All communications on editorial matters should be sent to: Mr E. W. CURTIS BOTANIC GARDENS GLASGOW, G12 OUE A limited number of advertisements can be accepted and enquiries should be sent to the Editor. Back numbers available are listed on page iii of cover Building Stones of Glasgow JUDITH LAWSON £ 47 Southbrae Drive, Glasgow Received May 1979 Building materials need to be strong, durable and easy to work. Before the building of the canals and railways made the transport of heavy, bulky loads easier, an important factor in the choice of material was its distance from the building site. A local stone (or timber or brick) even though of inferior quality was preferred unless a prestige building was involved. It was this local nature of materials, reflecting the enor- mously varied geology of the British Isles which contributed so much to the character of the towns and villages built before the late eighteenth century. Glasgow is predominantly a nineteenth century city and one of its interests from a geological point of view, is that it was built of stone at a time when better technology and transport resulted in many towns, particularly in England, being built of uniform mass-produced brick. Scotland is relatively poor in brick-clays and this was doubtless an important reason for using stone which was easily available. The building stone of Glasgow up until the 1914-18 war was sandstone — a medium-grained sedimentary rock formed of quartz grains, usually between 1 mm and 0.1 mm in diameter, cemented together by various minerals, such as quartz, calcium carbonate, iron oxides and clay minerals. As a building stone it is strong enough to form load- bearing walls and it is relatively easy to work. The durability of a sandstone, very important in the long term, depends on the amount and nature of the cementing agent. A poorly cemented sandstone is porous and therefore less frost resistant than a well cemented one. A sandstone in which the grains are bonded together by silica is more resistant to weathering than one with a calcareous cement which is likely to be dissolved by rainwater. Even at a first glance it will be seen that two distinct sandstones occur in Glasgow. One is a cream (weather- ing black) sandstone of Carboniferous age (about 300 million years old) Glasg. Nat. 20 part 1 (1980) 2 and the other is red, from the Permian New Red Sandstone (about 250 million years old). The oldest buildings in Glasgow which still exist, the Cathedral and Provand’s Lordship, are built of cream sandstone. At the time these were built in the thirteenth, fourteenth and fifteenth centuries, transport was difficult and a local stone was chosen. This, fortunately, was of good quality. Sandstones are common at many horizons in the Carboniferous System and are the deposits of rivers and deltas. Most are well bedded and show small-scale current bedding and rippling. The colour is cream with darker carbonaceous layers showing up the bedding planes. Sandstones were quarried from many different horizons in numerous small quarries, but particularly good beds occur in one part of the geological column known as the Upper Limestone Group (see Fig. 1). Here the sandstones had reasonably even grains, thick bedding and few or no joints so that they could be cut in any direction. ORCHARD LST moor rock! GIFFNOCK LIVER rock] SST LYONCROSS LST BARRHEAD GRIT HUNTERSHILL CST INDEX LST Fig. 1 Sections of the lower part of the Upper Limestone Group north and south of the River Clyde. Sections approximately 130 m in thickness. Sand- stones— stippled, shales — horizontal shading, limestone — boxes. LST — Limestone; SST — sandstone; CST — cementstone. NORTH SOUTH ORCHARD LST T~m LYONCROSS LST HUNTERSHILL CST BISHOPBRIGGS SST INDEX LST 3 Such sandstones are known as freestones or, as at Giffnock, as Liver Rock. The quartz sand1 grains are cemented with silica (quartz) some clay and some calcium carbonate (the latter is common in Giffnock sandstone). The early quarries are now obscured but the stone for the cathedral is thought to have come from the area on which Queen Street Station now stands. New construction works sometimes reveal the presence of old quarries; one occurred on the land between Ren- field and Renfrew streets on a site cleared for a new TV studio and another on the site of the multi-storey car-park on Cowcaddens Street (see Fig. 2). Later, in the nineteenth century, when the centre of Glasgow was built over, new quarries were opened in Bishopbriggs and Giffnock. This stone was used for tenements, houses and business premises. While these quarries were important it should be remembered that there were numerous smaller ones at many other levels also. Little can now be seen of these quarries as they were mostly underground. Miners were employed to cut horizontal adits from which quarrymen then cut blocks in galleries up to 20 m in height. ‘Pillars’ or ‘stoops’ of sandstone were left to support the roof. At the Huntershill Quarry in Bishopbriggs the sandstone was a very uniform cream colour except where it was weathered to yellow. In the important southern area around Giffnock, a sandstone of a very local extent was quarried, again underground. The best sandstone — the ‘Liver Rock’, about 10 m thick, occurred in the Braidbar area where it underlay about 10 m of more porous ‘Moor Rock’ which was usually left as the roof. The Liver rock thinned out both to the north and south of this area. Many of the sandstones are still in excellent condition and a new trend, much to be praised, is to clean up older tenements rather than to demolish them. Good examples of both red and cream sandstone tenements can be seen at Maryhill at, for example, Murano Street and Shakespeare Street. The other main building stone is a bright red sandstone. By compar- ison with the cream sandstone this has well rounded grains and is more porous i.e less well cemented. The red colour is due to the red iron oxide, haematite, which coats the sand grains. The actual amount of iron oxide is very small, possibly 1% or less. These red sandstones are very even grained and may show the very large scale current bedding, typically formed by drifting sand dunes. These are desert sandstones of the ‘New Red Sandstone’. They are found extensively in Ayrshire around Mauchline (e.g. Ballochmyle and Barskimming Quarries) and in Dumfriesshire (e.g. Locharbriggs, Corncockle and Gatelawbridge). 4 bishopbf(Tggs Ke n m u r e''fi| r o w h i I i Coltpark^P^ ^ U.M ^'■'^Huntershill V \ * N COWGLEN CATHEDRAL — s Post Upper Carboni- ferous Lst Group Other Upper Carboni- ferous Lst Group Giffnoc k Sst & Lyoncross Lst Bishopbriggs Sst & Index Lst Pre Upper Carboni- ferous Lst Group Burnfield-^ / V GIFFNOCK best quality li' rock from eastern part of outcrop ^ Fault -f- Quarry Braidbar New Braidbar Fig. 2 Sketch map of the Glasgow District showing the main sandstone horizons and quarries. 5 The vast majority of dwelling houses and tenements used one or other of these sandstones, often using a well shaped (ashlar) block on the front and a more irregular rubblestone at the sides and back of the building. Some buildings have red sandstone at the front and cream sandstone at the rear, implying that the red sandstone was more fash- ionable. Such a tenement can be seen on High Street near George Street. Very occasionally a striped building was built for effect as can be seen at 91 Buchanan Street, originally one of Miss Cranston’s Tearooms. In the centre of Glasgow, many buildings, particularly those of a com- mercial nature, have the lower part — up to ground floor level — built of granite. The granite was mainly of Scottish origin from Aberdeen- shire, Peterhead, Ross of Mull and Dumfriesshire, an exception being the Clyde Trust Building at the corner of Robertson Street and Broom- ielaw where polished slabs of Shap granite can be seen. Granite is an extremely strong, coarse grained acid igneous rock. Many granites have a pink or reddish colour which combines well with the red sandstone of the upper stories. The finish was usually highly polished or left matt. Granite is very little affected by weathering and extremely strong, but it has the disadvantage that it is difficult and expensive to work. Buildings with granite bases include the City Chambers (Correnie Quarry, Aberdeenshire) and Strathclyde University (Stirlingshill Quar- ry, Peterhead. Stone has had many other uses in Glasgow. Flagstones (thinly bedded fine, often micaceous sandstone) from Caithness, Arbroath (which was less slippery on steep hills) and also from more local sources, were used for pavements. Road setts which can still be seen in place in, for ex- ample, Dundas Street and which lie under the surface of many streets were of granite in main thoroughfares, and dolerite, largely from the Kilsyth area, for side streets. Kerbstones, mainly dolerite and granite, including a large number from Shap, can still be seen in place as they are virtually indestructible. A variety of granites were used for statue pedestals. George Square contains many different ones including a por- phyritic grey granite with individual crystals (phenocrysts) several centimetres long, probably from Cornwall. Granite was also used for bridges; for example the King George V bridge is of Dalbeattie granite. Another stone used in small amounts was limestone. This is common in England where it has been used extensively as a building stone. The startlingly white Portland Oolite Limestone of 86-90 St. Vincent Street, contrasts sharply with its mellow cream sandstone neighbour. After the 1914-18 war, little major building in stone occurred. The cost of labour increased so that it became more economic to build in concrete and confine stone to the cladding of such structures. Cladding panels can be thin and so far less stone is needed. Glasgow today can 6 show granites and other rocks from all over the world. The Clydesdale Bank at the comer of Buchanan Street and West George Street is clad with both polished and flamed (rough) surfaces of granite from Argen- tina and the Bradford and Bingley Building Society office in Gordon Street uses a brown orbicular granite from Finland. While these rocks from abroad are often very attractive, it is to be hoped that recent in- terest in reopening old Scottish quarries is successful and that ‘native’ stone can again be used in Glasgow. KHbirnie Loch, Ayrshire : an Ecological Appraisal P.S. MAITLAND, I.R. SMITH, A.E. BAILEY-WATTS, K. EAST. K.H. MORRIS, A.A. LYLE and A. KIRIKA Institute of Terrestrial Ecology, 78 Craighall Road, Edinburgh Received July 1980 Kilbimie Loch is a shallow loch in north-east Ayrshire, lying between Kilbimie, Glengamock and Beith. Brief descriptions of it have appeared in general accounts of the area (e.g. Adam, 1793; McClellan, 1793; Col- ville, 1845; Urquhart, 1845; etc.) but no comprehensive account of its ecology has been published. The bathymetry was surveyed in 1906 by Murray and Puller (1910). A short account of some aspects of the loch is given by Henton and Livingstone (1974). Originally called Garnoth Loch, then Loch Thankart, Kilbimie Loch has been used for a variety of purposes. Adam (1793) notes that the Earl of Crawford used it for pleasure boating; later a boat was used to transport coal from the west side to Beith. Colville (1845) records that in 1805 an Act of Parliament authorised the Ardrossan Canal to be con- structed from Ardrossan to Glasgow, with Kilbimie Loch as its summit level. This canal was never constructed (apart from a stretch from Glas- gow to Johnstone) and eventually a railway line (from Glasgow to Ayr) was built along the same route. The combination of this line, local coal, limestone, and some iron ore led to the development of an iron works near the south-west side of the loch around 1850. These works developed over the next 100 years and are in existence today. Over this period slag has been dumped continuously, encroaching into the south-west comer of the loch and filling in a substantial propor- tion of its area. Loch water has also been abstracted regularly by the iron works for cooling purposes. Recent proposals for redevelopment of the area have increased interest in the loch and the present survey was a direct result of this. The main object of the survey was to assess the present conservation interest of the loch and predict the likely impact Glasg. Nat. 20 part 1 (1980) 8 FIGURE 1. Kilbimie Loch: bathymetry, main inflows and outflow. (Bathy- metry after Murray & Pullar, 1910). Changes in the shoreline since 1858 are also shown. 9 of potential developments there. Though attempting to be comprehens- ive, its main deficiency results from the study being carried out within 8 weeks (October and November, 1978) thus little seasonal information is available. In addition to assessing its ecology and conservation status particular attention has been paid to the nature of its silts, the effect of infilling with slag and its potential for industry and recreation. Physical Background Kilbimie Loch lies 27 km south-west of Glasgow, at 31 m above sea level. It has a surface area of 0.85 km2, a maximum depth of 9.1 m and a mean depth of 3.4 m (Fig. 1). The loch has been reduced in size over the last 120 years by tipped waste from the steel works at its south end. Fig. 1 shows the changes in shore-line from 1858 to 1978. The surface area over that period has decreased from 1.13 km2 to 0.85 km2. The drainage area of the loch is 14.9 km2. CATCHMENT Geology The solid geology in the lower catchment is carboniferous limestone. The higher ground to the north and south is basalts with some calcifer- ous limestone, mugearite, trachyte and rhyolite. Drift geology shows a layer of peat on higher ground to the north, and a covering of boul- der clay and lake alluvium over the lower catchment. Land Use The catchment area of the loch includes rough grazing, permanent grass, industrial and urban types of land use. Rough grazing is confined to the upland north of the catchment and is approximately that land over 250 m. Farming land is mainly permanent grass for cattle with a small area for root crops. Glengarnock steel works and associated slag areas constitute the main industrial ground, but land on the south- east shore sites bonded warehouses. Beith (population: 5,859 in 1971), is the main urban area. HYDROLOGY Water Budget For the purpose of water balance calculations the drainage area is assumed to be water-tight. Maich Water is the major inflow but there are two small streams on the east shore and some direct run-off from slag heaps on the south-west shore. The values required to determine the net water balance are: rainfall, evaporation, water supply and industrial use (Linsley et al. , 1949), the outflow being estimated by difference. 10 Rainfall over the catchment and loch was calculated by the Th les- sen method using annual rainfall means for 1916-1950 from three local rain stations (Meterological Office, 1966). This produced a mean annual rainfall of 1789 mm. Evaporation was calculated in two parts - potential transpiration over the catchment, and evaporation from the loch surface. The potent- ial transpiration for the county of Ayr (1950-1964) is 470 mm per annum (Ministry of Agriculture, Fisheries and Food, 1967) and the evaporation rate 564 mm. The Lower Clyde Water Board own Maich Reservoir, which supp- lies the treatment works near East Auchenhean. The abstraction rate is quite low, approximately 36 m3 per day. (The Water Board are at present reviewing a scheme to divert some of the Maich Water to feed a reservoir in the River Calder). The steel works, running at half capacity, extracted 82 x 103 m3 per week from the loch in 1978. (This figure will be reduced to 26.5 x 103 m3 when a section of the works closes). Water is returned to the loch after use but evaporation losses during the process are assumed to be as high as 50%. These calculations give an estimated annual outflow of 18.472 x 106 m3. From the net annual water balance and the lake volume, a theoretical retention time of 57.3 days is calculated. Lake Dynamics In 1973, Henton and Livingstone (1974) concluded that the domin- ant factor in generating circulation currents was exposure to the pre- vailing south-west winds. Recent experiments by the authors support the view that, in the absence of wind-driven currents, a short circuiting between inflow and outflow exists, leaving the south end of the loch un- disturbed. This affects any calculations using retention time theory. Thermal currents induced by the returning water from the steel works are not thought to be significant. The possibility of stratification was examined by comparing the mean depth with a theoretical thermocline depth which was calculated to be 5.8 m. As this is greater than the mean depth of 3.4 m it is unlikely that stratification will occur, except in exceptionally calm and warm summer conditions. SUBSTRATES The softer deep water and firmer shallow water substrates of Kil- birnie Loch were examined separately during the survey, using differ- ent methods. These were linked to the sampling of the invertebrate benthos of deep and shallow water respectively. 11 Deep Water Sediments The substrate in water over 0.5 m deep consists mainly of soft silty sediments. Samples of these were taken at seven sites. At six sites two cores each of 16 cm depth were taken using a standard Jenkin mud corer (Jenkin & Mortimer, 1938): one of each pair of cores was used for sediment analyses, the other for determination of the zoobenthos. At the 7th site between the two deepest areas a different coring device was used (Maitland, 1969) and here a single core 64 cm in depth was obtained. This was subsequently divided horizontally into 4 vertical sub-samples (A-D), each 16 cm in depth. All cores used for sediment analysis were treated in the same way. After its depth had been measured and any overlying water siphoned off, each core was placed in a labelled jar and then thoroughly mixed. Approximately 100 gm was then removed, dried at 100°C, and passed for chemical analysis (see below). The remainder was then analysed for particle size composition (Holme & McIntyre, 1971). The surface sediments are all fine ones with a fairly high organic fraction (mean 11.6%). The sand fraction is rather low, and there is a high silt /clay fraction at all sites. The sand fraction at the north end of the loch is higher than elsewhere. Water movement (and subsequent dispersion of the finer particles) is greatest in this area due to prevailing winds and proximity to outflow and major inflow. A triangular plot of the percentages of sand, silt and clay indicates the similarity of the sediment samples taken. The depth of the sediment at most sites was substantial and at the 7th site was over 2 m. Analyses of segments of the deep core taken at this site indicates that there is little difference between shallow and deep fractions, the main point of interest being the increasing clay in the deeper sediments. Shallow Water Substrates The substrates round the edge of Kilbirnie Loch were mapped dur- ing a circuit of the perimeter. The assessment of substrate type was a subjective one, and the nature of each segment of shore examined was recorded as the percentage composition according to the particle size scale of Wentworth (1922). Field data were transformed in the laborat- ory to tabular and map representations. The predominant substrate was sand and gravel with numerous stones. Boulders were scattered sporadically along the east shore and on the west shore were mostly to the north of the slag. The slag heaps themselves were an obvious feature of the south-west shore and under water consisted of fine silt among numerous stone-sized pieces of slag. 12 Chemistry WATER Water was sampled at the substrate sites. Collections were made with a polythene pipe (I.D. 2.5 cm) weighted and lowered vertically into the water (Lund, 1949) to within ca 25 cm of the bottom. An additional dip sample of the Maich Water was taken just upstream from the loch. Chemical analyses were according to Allen et al (1974) except for total organic carbon which was assessed with a Model 400P Carlo-Erba (Swin- don, England) T.O.C. Analyser. At a central station vertical profiles of temperature, dissolved oxygen, conductivity and light attenuation were established with submersible probes and photocells. These analyses indicate a fairly well-mixed water body. Most physico-chemical parameters show virtually no spatial variation, whilst even those exhibiting at least a slight variation show no unidirectional trend. Vertical profiles indicate really very little difference with depth; the temperature was 10.68 °C at 0 m and 10.65 °C at 6 m, dissolved oxygen remained between 80 and 81% saturation, and conductivity (/xS) varied only by 1 in 142. Light attenuation is the only feature ex- hibiting a significant trend with depth. Integrative measures of water quality — conductivity, Hazen col- our, pH, total organic carbon — as well as the analysis for individual ions, indicate a base and nutrient rich water body with a potential for high organic production. The water is rich in both dissolved and par- ticulate inorganic and organic matter. These result in a murky water of low light transparency. At 1 m below the surface only 12% of the surface value of even the most penetrating wavelength (red) is present. A 20 cm diameter Secchi disc is lost from sight when lowered to depths greater than 1.5 m. The similarity between loch and inflow is of interest; alkalinity and calcium and magnesium ions, sodium, potassium and nitrogen are the few features showing a dissimilarity — higher values in the loch. Clyde River Purification Board results from May 1978 showed a sim- ilar relationship. The latter data also showed an increase in chloride content around the steel works inlet; no such variation is evident for the present survey. As far as water chemistry is concerned views on the influence of the loch-side industries would be conjectural; levels of alkaline earths are similar here to those of rich lochs lying in base- rich catchments elsewhere. The acidity of the loch water seems higher than might be expected for a catchment that is mainly base-rich. Pollution may provide part of the answer here for a possible source of acidity, not normally found in comparable catchments, is air-borne pollution from the steel works chimneys — the emission from which presumably has a high sulphur 13 content. Rain affected by aerial pollution of this type is highly acidic and has a marked effect on the pH and ecology of fresh waters on which it falls (Granat, 1972). SEDIMENTS Results of chemical analyses of the dried sediments for six par- ameters show that the surface sediments have a rather low pH (mean : 5.0), and a high organic fraction as expressed by loss on ignition (mean: 20%). Levels of calcium, iron, phosphorus and nitrogen ap- pear normal for a lake of this type. The analyses of the vertical samples of the deep core taken at a central site indicate little difference in chemical composition with depth. Though the highest concentrations of iron occurred in the shallowest sediment this is not necessarily related to the steel industry near by, for Gorham (1964) has shown that the surface sediments of Esthwaite Water and Windermere are richer in iron than the deeper ones. Botany PHYTOPLANKTON Subsamples for phytoplankton pigment (chlorophyll a) analyses and algal cell counts were taken from water collected for chemistry. Spectro- photometric measurements for chlorophyll were made on methanolic extracts of material filtered on to glass-fibre pads (Tailing, 1965). Stand- ard equations (Tailing & Driver, 1963) were used to relate concentrations of pigment to the absorbances measured. A Water Research Centre- modified Lund nanoplankton chamber was used for algal counts on material fixed with Lugol’s Iodine and concentrated by sedimentation (Youngman, 1971). Species names conform to descriptions in taxon- omic texts cited by George (1976). Only 16 algal species were recorded. The commonest was the small cryptomonad flagellate Rhodomonas minuta var nanoplanctica which existed with small green algae ( Ankistrodesmus falcatus. Scene desmus spp., Elakatothrix gelatinosd) and diatoms {Asterionella formosa and Melosira spp.). An over-riding feature was the comparative rarity of algal organisms within a very dense suspension of organic detritus and bacterial aggregates. Total numbers of algal cells varied among the 7 stations from 430 to 1,430 per millilitre and concentrations of chlorophyll from 3.1 to 4.4 pug. I”1. From 90 to 95% of the total algal biomass on this occasion is attributable to Rhodomonas. The number of cells in these samples is low for a nutrient-rich and potentially-— from physical and chemical viewpoints — highly productive loch. Evidently the primary production here is manifested more in the dense stands of macrophytes on the loch bed, than in algal plankton. 14 However, total amounts of organic matter in the water column are high. This is suggested both from the visual impression of material observed under the microscope, and by some of the chemical analyses. For example the measured total organic carbon concentrations approx- imates to 8 mg. I-1; by comparison the current algal crop (ca. 1,000 cells. ml-1) would contribute approximately only 0.1 mg C.l-1 i.e. 1.25% of the total carbon present. Much of the suspended matter may arise as a loading from the inflow; the total organic carbon value from the latter slightly exceeds those measured in the loch samples. This component could, along with certain dissolved compounds, limit phytoplankton production by ab- sorbing light. However, this idea should be tested further because of the presence of other photosynthetic organisms associated with the bed of the loch. MACROPHYTES A macrophyte survey of the loch from the water’s edge to about 50 cm depth was carried out in mid-October 1978. Plants were noted at 18 sampling stations. In addition, the emergent vegetation which formed a fringing zone was noted, as were plants at the five netting stations. The dominant plant at the water’s edge is Phalaris arundinacea. This occurs along the eastern half of the north shore, the outflow, the eastern shore and the southern end of the loch. It then becomes spor- adic and apparently disappears along the western shore. In fact, small plants may be found here and there along this shore also, and its great reduction is probably due to grazing pressure here. Another grass was common here, Agrostis stolonifera , and this merged into a pasture of other grasses and herbs above the water level. Other plants did occur in the Phalaris zone but not in large numbers: patches of Glyceria maxima and Iris pseudacorus. Some plants were only recorded at a single sampling station and not seen elsewhere e.g. Alisma plantago- aquatica. Plants which seemed abundant and/or widespread (and probably the most important) are the submerged Char a sp.. Ranunculus aqua- tilis , Myriophyllum spicatum, Elodea canadensis, Potamogeton perfoli- atus and Eleocharis acicularis and the emergent Phalaris arundinacea , Agrostis stolonifera and Eleocharis palustris. The nutrient status of waters and the types of substrates in which they grow have been dis- cussed by Haslam et al, (1975). All can be found in eutrophic waters and 6 of the 9 in oligotrophic waters also. However Myriophyllum spicatum, Potamogeton perfoliatus and Phalaris arundinacea are not found in oligotrophic waters, and Phalaris and Agrostis stolonifera are restricted to a mineral substrate. Thus the aquatic macrophytes of Kil- bimie Loch indicate a mesotrophic to eutrophic loch with a mineral substrate. 15 Zoology ZOOPLANKTON Microzooplankton were enumerated in the samples used for algal counts. The commoner rotifers were recorded from a phytoplankton net tow sample taken in open water. Types and numbers of Crustacea were estimated from integrated column samples collected by a tube sampler, capacity 7.85 litres per metre length (George & Owen 1978). The most common zooplankton was a protozoan closely resemb- ling Tintinnopsis — a ciliate; population estimates suggest an uneven distribution with densest aggregations of ca 2,000 ml-1 and sparsest of near 200 ml-1. Rotifers consisted mainly of Synchaeta, Polyarthra, Brachionus, Conochilus, Keratella and Notholca species. This is an assemblage typical of temperate eutrophic waters. Although present in far fewer numbers than Tintinnopsis , various Crustacea comprised the major proportion of zooplankton biomass. The means from seven sites (expressed per 10 1 of water) are : calanoids (mainly Diaptomus gracilis ), 35; cladocerans (mainly Daphnia hyalina var. lacustris ) 7 and cyclopoids (mainly Cyclops strenuus abyssorum) 4. At all sites Diaptomus was predominant (maximum 93.10 l-1), clado- cerans were the next most abundant, with cyclopoids comparatively rare. These zooplankton are common to many temperate eutrophic waters. Thus rather than the types present, their absolute abundances and their ratios are probably of greater value as indicators of the nature of the Kilbimie ecosystem. As with phytoplankton, zooplankton is sparse. In other small, shallow, eutrophic lakes populations of tens of Crustacea per litre might be expected. The predominance of Diaptom- us is particularly striking. In many lakes the zooplankton tends to be dominated by a cyclopoid and/or cladoceran with Diaptomus com- paratively rare. As Diaptomus and other Crustacea feed on small par- ticles including micro-algae it is possible that the low numbers result from a seasonal algal minimum; however, there is an abundance of other organic particles. The probable influence of fish predation on crustacean zooplankton cannot be ignored. ZOOBENTHOS The zoobenthos of the soft substrates in deep water (more than 0.5 m) and of the firmer sediments in shallower water (less than 0.5 m) were examined separately, using, because of the different nature of the substrates, quite different methods. Zoobenthos of Deep Water Cores were taken at six of the substrate sites using a Jenkin Corer, as described above. These were sieved fresh using a 20 cm diameter, 0.5 mm aperture sieve. Material retained in the sieve was preserved 16 in 70% alcohol and later sorted, all invertebrates being counted and identified. The zoobenthos is dominated by aquatic worms ( Tubificidae ), bi- valves (Pisidium), and midge larvae (Procladius) — common animals of soft sediments in lochs. Other invertebrates occurring in reasonable numbers are Asellus aquaticus and Valvata macrostoma. Some of the variety in the community is due to animals associated with Chara, growing over the mud in many places, and inevitably included with some of the cores. Zoobenthos of Shallow Water Samples of bottom-living invertebrates were taken at six approxi- mately equal intervals round the loch and included all the substrate types present. Samples were taken using a timed hand-net technique (Macan, 1957) where the substrate was disturbed by kicking and the debris swept into a 0.5 mm mesh hand-net. Kicking was over as wide an area as possible and into the loch to a depth of 0.5 m for a timed period. In addition, stones were selected randomly, and material attach- ed to their surfaces rubbed into the hand-net. This operation was also timed. The samples were preserved in 4% formalin and later sorted, and any zoobenthos identified and counted. The littoral invertebrate fauna was varied and included at least 44 taxa. Some were present in large numbers, especially those associated with organically rich waters e.g. flat worms, worms, leeches and water lice. There was a lack of those organisms which are susceptible to pol- lution i.e. stonefly and mayfly nymphs (Woodiwiss, 1964). The snail fauna was varied and individuals numerous. Most of the species found such as Lymnaea palustris and L. peregra are associated with both hard and soft waters and are widely distributed in Great Britain, but some are considered to be hard water species e.g. Bithynia tentaculata common in the south of England but rarer in Scotland (Macan, 1977). There was a notable lack of air-breathing organisms, the exception being the beetle Deronectes depressus. With the exception of the Orthocladiinae, Diptera also occurred in low numbers. The two stations with the small- est variety of organisms were both at the southern end of the loch. It is clear from the overall diversity of the littoral fauna that this is not a severely polluted site. The absence of certain organisms sus- ceptible to pollution, however, indicates its existence to some extent. There was visual evidence of oil, both on the surface of the water and in the sediments, particularly on the west and south shores. This oil could be a limiting factor in the success of air-breathing organisms. The presence in large numbers of invertebrates associated with nutrient enrichment could be the result of run-off from the farms on the west shore or the inflow streams on the east shore which drain from the dir- 17 ection of Beith. The low diversity of the southern sites near the slag heaps indicates some adverse effect of slag on the invertebrate popu- lations. FISH Only large fish in the loch were examined during this study. Five identical mixed-mesh gill nets, each 50 m in length, 2 m in depth with 10 mesh sizes ranging from 10-55 mm (ba) were set at three stations on the east and two on the north-west shore. Each net was set at right angles to the shore starting in about 2 m of water. The nets were set at 1300 hrs on 18 October and lifted at 1100 hrs on 19 October 1978. All fish caught were identified and measured for length. Scales were taken from the 10 largest specimens of each species and used for ageing. Small fish were seen and taken occasionally in hand-nets round the edge of the loch. The few species caught were Trout ( Salmo trutta ), Pike (Esox lucius ), Roach (Rutilus rutilus) and Perch ( Perea fluviatilis). In addition. Minnows ( Phoxinus phoxinus) were caught round the edge. Details of the lengths and numbers of the net-caught fish are given in Fig. 2. The total fish population in Kilbimie Loch appears to be large and all four common species there grow to a large size. The fish fauna of the loch has been known for a considerable time, for Adam (1793) remarked that it was “well stored with Pike, Perch, Trout and Eel”. The same comment is made by McClellan (1793), but neither author mentions Roach or any smaller species. Both Colville (1845) and Ur- quhart (1845) mention Trout, Pike, Roach, Perch and Eels, the latter pointing out that the Eels were particularly abundant, while very large Trout, Pike and Perch “have occasionally been killed”. It seems likely that Eels {Anguilla anguilla ) disappeared from the loch with the pollution of the Rivers Black Cart and Clyde, while Roach invaded the loch in the early 19th Century — either naturally or through introduction by Man. With the increasing improvement of water quality in the River Clyde and its tributaries (Clyde River Purification Board, 1977) it is possible that Eels could return to Kilbirnie Loch within the next 10 years. BIRDS Relatively little recent information is available concerning water- fowl at Kilbimie Loch and only a few Mallard, Tufted Duck and Goldeneye were seen during the actual survey. Atkinson- Willes (1963) mentions that the numbers of wildfowl there are small, “due partly to disturbance and partly to the tipping of slag from the iron works near- by”. For this reason it appears that this loch has never been included 5 0 5 0 30 25 20 15 10 5 0 10 5 0 ROACH Ju. ! 1 1 T 1 1 1 10 20 30 40 50 60 70 LENGTH IN CENTIMETRES Length-frequency histograms of Trout, Pike, Roach and Perch gill net in Kilbimie Loch. 19 in the national wildfowl counts. However, wildfowl on the neighbouring Barr and Castle Semple Lochs have been counted regularly for more than 20 years and data for the common species are available. Both these lochs provide a suitable environment for a rich variety of over- wintering wildfowl. There is no reason to suppose that Kilbirnie Loch, with less disturbance and oil pollution, could not harbour similar populations. It did in the past, for McClellan (1793) noted that it was “frequented by many aquatic birds such as ducks, geese, swans etc”. Discussion The descriptive information on Kilbirnie Loch, though limited from the seasonal point of view, allows a reasonable ecological appraisal of the loch, especially in relation to future developments there. Proposed changes which appear likely to affect the loch are the use of the soft sediments in reclaiming areas of slag, further infilling of parts of the loch in order to dispose of excess slag, and the increased use of the loch for industrial or recreational purposes. BASELINE SURVEY The overall results from the survey indicate that Kilbirnie Loch is a moderately rich, mesotrophic to eutrophic loch, with a varied flora and fauna. Originally part of a glacial trough between two sections of the Clyde Plateau lavas, Kilbirnie, Barr and Castle Semple Lochs were probably at one time a single elongate loch, now divided into three by the Maich Water delta (between Kilbirnie and Barr Lochs) and the Calder Burn delta (between Barr and Castle Semple Lochs). Though it has been a discrete water body for only a few hundred years, Kilbirnie Loch can be described as a mature lake in geomorphological terms — with a regular mature shoreline and deep, organically rich, sediments gradually filling its deeper basins. The catchment of Kilbirnie Loch is an unusual one with the loch lying very close to the Garnock (Ayrshire) and Cart (Renfrewshire) watersheds, but just within the latter. The main tributary (the Maich Water) lies close to the outflow. Thus, in some weathers at least, much of the Maich Water passes quickly out via the Dubbs Water with little mixing. These two circumstances have important biological implications as far as future management is concerned. At present, because of pollut- ion in the lower Cart and Clyde, no migratory fish enter Kilbirnie Loch. This situation is improving, however, and it is likely that Eels at least should be able to pass into Kilbirnie Loch in the not too distant future. Chemical results indicate that Kilbirnie Loch is mesotrophic to eutrophic in character and there is no evidence of serious pollution. However, the small tributary entering the south-east comer of the loch was polluted at the time of the survey and there was considerable oil 20 pollution of the water surface from the steel works in the south-west corner. Oil contamination of the sediments was also evident in a number of places. Oxygen levels of 80-81% saturation were recorded during the present survey. Hen ton & Livingstone (1974) noted that dissolved oxygen levels in Kilbirnie Loch (also 80% saturation) were lower than either Barr Loch (85%) or Castle Semple Loch (87%). They also observ- ed large vertical differences in the south-west corner of the loch beside the steel works outfall. Here the saturation at the surface was 115% but at a depth of 2 m was only 35%. They attributed this to a prolific growth of Potamogeton crispus encouraged by warm water from the outfall. The flora and fauna of Kilbirnie Loch is relatively rich both in variety of species and density of individuals. The impact of the steel works (and the former chemical works) appears not to be great, though there is evidence of a localised effect from the warm water effluent and of an impoverished insect fauna from oil pollution. The fish population is dense with a surprisingly good mix of four large species — Trout, Pike, Roach and Perch. Waterfowl, on the other hand, appear to have been significantly affected by disturbance and oil pollution and numbers are less than might be expected in natural circumstances. LOCH SEDIMENTS The particle size composition of the soft sediments is similar to that found in other lowland lochs te.g. Loch Leven, Kinross: Calvert, 1974), as is the organic content. Chemical features appear to be normal too, even iron, which might be expected to be high due to leaching from the enormous amounts of slag dumped beside and even into the loch over the last 100 years. The distribution of iron in lake muds has been discussed by Gor- ham (1964), who gives values for the upper sediments in Esth waite Water and Windermere of around 5.4 and 5.2% respectively. This compares to the mean of 3.9% in Kilbirnie Loch, which is thus sur- prisingly low. INDUSTRY AND RECREATION It has been noted that Man has used Kilbirnie Loch for a variety of purposes for several hundred years. Though some changes are ap- parent, there do not seem yet to have been any catastrophies in the ecology of the system. If the future of the loch is to be secured and its resources integrated in a sensible way with the redevelopment of the surrounding area, then the impact on the loch of any new proposals must be considered in forward planning. Though the scale is small, there is every reason to approach this planning (as far as Kilbirnie Loch is concerned) from the point of view of a multi-purpose river- basin project. 21 The main threat to the loch from industry (including housing) in its catchment is pollution — probably in the form of toxins, organic wastes or oil. Any such discharges will be subject to control by the Clyde River Purification Board and should therefore be reasonably acceptable. Since, however, because of their residual effect (especially if stratification occurred in summer) such discharges are more harmful to standing than to running waters, it would certainly be preferable if they were led to the River Garnock rather than to Kilbimie Loch. Im- provement of existing sources of pollution (e.g. sewage from Beith, oil from the steel works) would also be of considerable benefit. The main direct use of Kilbirnie Loch by industry is likely to be for water for cooling or other purposes. As indicated above, this has been happening there on a small scale for many years with apparently only a minor effect on the loch. Some abstraction also takes place in the upper catchment and there are proposals to increase this. The most serious damage likely to result from significant abstraction would be if large changes in the water level of the loch resulted. These would lead to an impoverishment of the shore flora and fauna with subse- quent changes in other parts of the ecosystem, including the fish pop- ulations. The barren shores of several water-supply and hydro-electric reservoirs elsewhere in Scotland are glaring examples of what to avoid. Noise, as such, from local industry is not likely to affect the loch other than through disturbance to the waterfowl. Numbers of these already appear to be substantially reduced through noise and disturb- ance from the steel works. The recreational potential of Kilbirnie Loch is high, and it is already used for water skiing, angling and amenity purposes. It offers a venue for other types of power boating, as well as canoeing and sailing. If power boating is developed further it will lead to a reduction in the ecological interest of the loch due to increased noise, direct dis- turbance of fish and birds, and pollution (from oil, etc.). In some other lowland lochs where user pressures are great some of the problems (e.g. boating v. wildfowl) have been overcome by zoning parts of the loch for different purposes. Linlithgow Loch in West Lothian is a good example of this. A small angling fishery already exists at Kilbimie Loch and sev- eral workers from the steel mill fish there. The potential for a mixed angling fishery is high for the loch holds good stocks of Brown Trout, Pike, Roach and Perch, many of which are large and of specimen size. A water of this quality would be of major angling importance in most parts of England or Wales and could be a tourist attraction. The potential amenity value of Kilbirnie Loch and its surround- ings is high and there is no doubt that it and the conservation value of the loch itself could be improved, thus making it a valuable asset 22 to the neighbourhood. Views of the loch from a number of vantage points are good, other than those looking towards the steel works and slag heaps, and to a lesser extent the bonded warehouses. Landscaping (particularly the slag areas) and the imaginative use of appropriate trees could improve these views considerably. If oil pollution and noise and organic pollution are reduced, there should be an increase in the variety of animals and plants in the loch. Conditions could be further improved by directing public use of the surroundings to the west shore, where a fenced path could prevent stock grazing down to the loch shore. This would encourage the growth of emergent plants there. Access to the east shore could be restricted and the habitat between the loch and the railway line diversified by the planting of native trees and shrubs. This would provide a reserve area for wildfowl breeding, etc., which could be encouraged even fur- ther by digging out a few shallow ponds. Acknowledgments This study was produced as a result of a contract between the Institute of Terrestrial Ecology and Robert Matthew, Johnson-Mar- shall and Partners (ITE Project No. 616). We are grateful to Mr C. Carter and Miss M. McGlynn of that firm for their advice and help during its preparation. The chemical analyses were carried out by the Chemical Section of ITE, and our thanks are due to Mr S. E, Allen and Mr J, Parkinson for the results concerned. Sediment particle size analyses were performed by Mr C. Main. Mr D. H. Jones and Miss L. May confirmed identities of Crustacea and Rotifera. Information of wildfowl numbers was kindly provided by the Scottish Ornithologists’ Club, while the Lower Clyde Water Board and the Clyde River Puri- fication Board were also good enough to provide background data. Detailed data obtained at each sampling station have been omitted from this account, but may be obtained from the Glasgow Natural History Society or the Institute of Terrestrial Ecology. They include the distribution and composition of the substrates, plankton, zooben- thos and macrophytes; the annual water budget and water chemistry are also tabulated. References Adam, J. 1793. Parish of Kilbimy. Stat. Acc. Scot., 7 : 149-152. Allen, S. E., Grimshaw, H. M., Parkinson, J. A. and Quarmby, C. 1974. Chemical analysis of ecological materials. Oxford, Blackwell. Atkinson-Willes, G. L. 1963. Wildfowl in Great Britain. London, H.M.S.O. Calvert, S. E. 1974. Distribution of bottom sediments in Loch Leven, Kin- ross. Proc . R. Soc . Edinb., B., 74: 68-80. Clyde River Purification Board. 1977. Annual Report. East Kilbride, C.R.P.B. 23 Colville, G. 1845. Parish of Beith. New Stat. Acc. Scot., 5: 570-604. George, D. G. and Owen, G. H. 1978. A new tube sampler for crustacean zooplankton. Limnol. Oceanogr., 23 : 563-566. George, E. A. 1976. A guide to algal keys (excluding seaweeds). Br. phycol. J. 11: 49-55. Gorham, E. V. 1964. Molybdenum, manganese and iron in lake muds. Verh. int. Verein. theor. angew . Limnol, 15: 330-332. Granat, L. 1972. On relation between pH and the chemical composition in atmospheric precipitation. Tellus, 24: 550-560. Haslam, S., Sinker, C. & Wolseley, P. 1975. British water plants. Field Studies 4: 243-351. Henton, M. P. & Livingstone, P. G. 1974. Kibimie, Barr and Castle Semple Lochs. Western Naturalist, 3: 1-7. Holme, N. A. & McIntyre, A. D. 1971. Methods for the study of marine ben- thos. Oxford, Blackwell. Jenkin, B. M. & Mortimer, C. H. 1938. Sampling lake deposits. Nature, Lond., 142: 834-835. Linsley, R. K., Kohler, M. A. & Paulhus, J. L. H. 1949. Applied hydrology, New York, McGraw-Hill. Lund, J. W. G. 1949. Studies on Asterionella. 1. The origin and nature of the cells producing seasonal maxima. J. Ecol., 37: 389-419. Macan, T. T. 1957. The Ephemeroptera of a stony stream. J. Anim. Ecol., 26: 317-342. Macan, T. T. 1977. A key to the British fresh and brackish water gastropods. Sci. Publ. Freshw. Biol. Ass., 13: 1-44. McClellan, D. 1793. Parish of Beith. Stat . Acc. Scot., 8: 314-328, Maitland, P. S., 1969. A simple corer for sampling sand and finer sediments in shallow water. Limnol. Oceanog., 14: 151-156. Meteorological Office. 1966. British rainfall. London, H.M.S.O. Ministry of Agriculture Fisheries & Food. 1967. Potential transpiration. London, H.M.S.O. Murray, J. & Pullar, L. 1910. Bathymetrical survey of the Scottish freshwater lochs. Edinburgh, Challenger. Talling, J. F. 1965. Comparative problems of phytoplankton production and photo synthetic productivity in a tropical and a temperate lake. Memorie 1st. ital. Idrobiol., SuppL, 18: 399-424. Talling, J. F. & Driver, D. 1963. Some problems in the estimation of chlor- ophyll a in phytoplankton. Proceedings, Conference on Primary Product Measurement. Hawaii, U.S. Atomic Energy Comm., TID — 7633: 142-146. Urquhart, R. 1845. Parish of Kilbimie. New Stat. Acc. Scot., 5: 689-727. Wentworth, C. K. 1922. A scale of grade and class terms for clastic sedi- ments. J. Geol, 30: 377-392. Woodiwiss, F. S. 1964. The biological system of stream classification used by the Trent River Board. Chem. Ind. : 1964, 443-447. Youngman, R. E. 1971. Algal monitoring of water supply reservoirs and rivers. Technical Memoranda Water Research Association, 63: 1-26. 24 Naturalists in Glasgow No. 1 : SIR WILLIAM JACKSON HOOKER (1785-1865) An anonymous engraving dated 1813. Appointed Regius Professor of Botany, University of Glasgow, in 1821. Left Glasgow to become Director when the Royal Botanic Gardens, Kew, became a public institution in 1841. While in Glasgow, Hooker made a reputation as an outstanding lecturer. His many publications included “Flora Scotica”, and he des- cribed many new plants then being introduced from overseas. His work did much to establish the Glasgow Botanic Gardens which had been founded in 1817. A Species of Water-flea new to Scotland (Alona weltneri) C. R. DOUGHTY Clyde River Purification Board, East Kilbride Received February 1980 The Cladocera (“water-fleas”) are among the most commonly encoun- tered invertebrates in static or slow-flowing freshwaters. The largest family, the Chydoridae, show great diversity of form and are predomin- antly littoral and benthic in habit, frequenting submerged vegetation and crawling across or through the substrate. Most are also capable of swimming with varying degrees of efficiency. The majority of species feed by scraping material from the substrate or from submerged plants by means of their trunk limbs (Fryer, 1968). As in other Cladocera, there are sexual and asexual phases in the life-cycle. When conditions are favourable, reproduction is by parthenogenesis, and only females are found in the population. At the onset of adverse conditions, males appear and sexual reproduction occurs, resulting in resting eggs which develop into parthenogenetic females when conditions improve. One of the least known members of the Chydoridae is Alona welt- neri Keilhack which was first described and figured by Keilhack (1905) from what is now northern Poland. A specimen had in fact already been found in England in 1895 by Thomas Scott, who collected it from a small pool at Scarborough. However, Scott’s specimen was not iden- tified as A. weltneri until the publication of Keilhack’s paper (Scour- field, 1907). It has remained the only known British record of the species. The relatively little known of A. weltneri has been summarised by Smirnov (1974) and Flossner (1972). Apart from England and Poland, the species has been reported from Germany, Switzerland and Southern Finland. It is apparently extremely rare. The ecology of A. weltneri is virtually unknown. According to Flossner, it occurs in the margins of lakes among submerged plants. A juvenile male from Northern Glasg. Nat. 20 part 1 (1980) 26 Germany has been described by Flossner (1962), but no adult male has yet been found. FIG. 1. Alona weltneri, mature female. The scale line is 0.1 mm. em= developing embryo, lk=labral keel, pa = postabdomen. On 12 September 1979 a specimen tentatively identified as A. weltneri was taken from the Forth and Clyde Canal near Kirkintilloch. The identification was subsequently verified by Dr Geoffrey Fryer of the Freshwater Biological Association, who has kindly deposited the specimen (unfortunately damaged during initial examination) at the British Museum (Natural History). The specimen found was a mature female, approximately 0.55 mm long, with two developing embryos in the brood chamber (Fig. 1). The most useful character for identification purposes is the shape of the postabdomen. In A. weltneri , the postabdomen tapers distally and its dorsal margin forms a right-angle with the bases of the claws. In other species known from Britain, the postabdomen either widens distally (e.g. A. rectangula), or it tapers distally and is indented terminally, the dorsal margin forming an acute angle with the bases of the claws (e.g. A. costata). For a detailed description of morphology, reference should be made to Keilhack (1905), Scourfield (1907), Smirnov (1947) and Floss- ner (1972). Certain characters, such as the shape of the labral keel, and the number, shape and configuration of the postanal denticles, appear to be somewhat variable. The specimen from the canal had a double 27 row of six relatively robust postanal denticles along the dorsal margin of the postabdomen. The labral keel was more strongly triangular than those figured in the literature. In view of the paucity of published information on the ecology of A. w el trier i, it may be worth-while to give some details of the chemistry and biology of the canal, particularly at the locality where the species was collected. The Forth and Clyde Canal between Kelvinhead and Bowling lies within the area of the Clyde River Purification Board. The Board has monitored chemical conditions in this stretch of canal regularly since 1972. The canal is nutrient-rich, generally well-oxygenated (although some stretches are prone to deoxygenation in summer), supports a thriving coarse fish population and has an interesting and varied aqua- tic flora. There are no major polluting inputs. Details of some chemical parameters at Hillhead Bridge, Kirkintilloch during 1979 are listed in Table 1. TABLE 1. Chemical analysis of Forth and Clyde Canal, Kirkintilloch 1979. pH Temperature (C) Dissolved oxygen (mg 1_1) Dissolved oxygen (% saturation) Ammonia (mg N l-1) Nitrite (mg N l-1) Nitrate (mg N l-1) Phosphate (mg P l"1) Alkalinity (as CaC03, mg 1_1) Total Hardness (as CaCO 3 , mg l-1) Chloride (mg 1_1) Conductivity (p, S) B.O.D (mg l-1) Suspended Solids (mg l”1) Maximum Minimum Mean 8.1 6.6 7.3 18 0 7.9 12.5 5.1 9.0 112 45.5 76.4 3.76 0.02 0.44 0.225 0.001 0.045 2.970 0.005 1.115 0.38 0.002 0.076 170 28 81.4 220 55 106.6 134 16 41.7 860 180 365 4.7 0.9 2.9 18 1 7 The site where A. weltneri was found is semi-rural. The substrate is relatively firm and the aquatic flora is dominated by Elodea cana- densis. The sample containing A. weltneri was taken by sweeping the submerged vegetation with a hand-held phytoplankton net. At the time of sampling, the microcrustacean fauna was dominated by Cladocera, 17 other species being present, the most numerous of which was Cerio- daphnia pulchella G.O. Fars. 28 As elsewhere, A. weltneri appears to be very rare in the canal. Its scarcity may be gauged by the fact that six major surveys undertaken between August 1978 and November 1979 have yielded only one speci- men. Acknowledgments I am grateful to Dr G. Fryer for his assistance with identification, and to Mr D. Hammerton, Director, Clyde River Purification Board for permission to publish this paper. The views expressed are those of the author and not necessarily those of the Board. References Flossner, D. 1962. Zur Cladocerenfauna des Stechlinsee-Gebietes I. Uber Morphologie und Variabilitat einiger Formen und uber Funde seltener Arten. Limnologica. 1 : 217-229. Flossner, D. 1972. Krebstiere,, Crustacea. Kiemen-und Bluttfusser, Branchio- poda, Fischlause, Branchiura. Tierwelt Dtl. 60: 1-501. Fryer, G. 1968. Evolution and adaptive radiation in the Chydoridae (Crusta- cea: Cladocera): a study in comparative functional morphology and ecol- ogy. Phil. Trans. R. Soc. B. 254: 221-385. Keilhack, L. 1905. Zur Cladocerenfauna des Madusees in Pommern. Arch. Naturgesch. 71: 138-162. Scourfield, D. J. 1907. An Alona and a Pleuroxus new to Britain (A. weltneri Keilhack, and P. denticulatus Birge). J. Quekett microsc. Club sen 2. 10: 71-76. Smirnov, N. N. 1974. Fauna of the U.S.S.R. Crustacea. Chydoridae, Jerusalem. Rare Beetles in the City of Glasgow R. A. CROWSON Zoology Department, University of Glasgow Received September 1980 Glaswegians are fortunate in having several good places for plant and animal study within the city boundary. Notable among them are the Pollok Estate, the Kelvin Walkway and Dawsholm Park, and Linn Park with its southern extension in Netherton Braes. There is also part of the Garscube Estate inside the boundary. The richest of these in unusual beetles seems to be Netherton Braes, visited by the Zoology Section on 1 June 1980. This has a con- siderable area of mainly young mixed woodland and some very herb- rich grassland on a flat in the bend of the River Cart. Leaf-litter in the woods has produced the Staphylinid Quedius nigriceps, for which I know of only one other record in the Clyde Valley, and the Clavicom Sphaerosoma piliferum, not previously recorded from the Clyde Valley. The herb-rich grassland has produced the rare Carabid Stomis pumicatus; the ant-associated Staphylinid Lamprinodes saginatus, not recorded elsewhere in the Clyde valley; the ladybird Hy per as pis pseudopustulata (ditto); the Weevils Apion aethiops with few other Clyde valley records, Sitona cambricus (ditto) and Gymnetron labile. The latter, on Plantago lanceolata, has very few previous records in the Clyde area. Decayed trees in the woods have produced a rather un- common fungus beetle, Cis alni. Dawsholm Park has produced the uncommon wood-boring weevil Pentarthrum huttoni. The adjacent area of the Garscube Estate has yielded, mainly in a suction trap catching flying insects, the Staphyli- nids Acrolocha sulcata (striata auct), Oxytelus sculpt us, Habrocerus capillaricornis and Cilea silphoides, all of very local occurrence in the Clyde valley; the Clambid Clambus pubescens, the first record from the Clyde valley; a male of the Stylopid (Strepsipteran) Elenchus tenuicornis, not hitherto recorded from the Clyde valley; and the Clavicorns Monotoma longicollis, Cryptophagus acutangulus, Strepto- Glasg. Nat. 20 part 1 (1980) 30 stethus angusticollis, Cartodere (Coninomus) constricta, Dienerella {Cartodere) elongata and D. filum, all with few other Clyde valley records. A number of these species may be associated with the stabling of horses in the Veterinary College at Garscube. The weevil, Rhinon- cus perpendicularis, recorded from Garscube on 25 May 1980, is ap- parently a new record for the Clyde area. Collecting in the Pollok Estate has produced the rather local Carabid Amara fulva; the Staphylinids Acidota crenata, Coryphium angusticolle and Habrocerus capillaricornis, all locally uncommon; the Cryptophagids Caenoscelis ferruginea and Atomaria munda; the Cery- lonid Cerylon histeroides; the Salpingid Salpingus reyi; the Melandryid Hallomenus binotatus; and the Scraptiid Anaspis burner alis — all of them with few records from the Clyde valley. Finally, I should mention the herb-rich railway cutting just south of Dawsholm Park, in which I have found two species in flowers of Linaria vulgaris, the Nitidulid Brachypterolus pulicarius and the weevil Gymnetron antirrhini, neither of them hitherto recorded from the Clyde area. NOTE: Names follow the second edition of the Kloet and Hincks Checklist of British Insects Part 3, revised by R. D. Pope (Royal Ento- mological Society Handbooks for the Identification of British Insects, Vol. 11 Part 3, 1977). The Freshwater and Terrestrial Fauna of the Clyde Area IV. Freshwater Fishes of the Upper Clyde Basin PETER S. MAITLAND Institute of Terrestrial Ecology, 78 Craighall Rd., Edinburgh Received July 1980 This paper is the fourth in a series of accounts of the fauna of the Clyde area, whose aims and objects have been discussed by Hosie and Mait- land (1973). It is also, incidentally, one of a number prepared by the author outlining the status of the freshwater fish fauna of different parts of Scotland. Previous accounts have dealt with south-west Scotland (Maitland, 1970c), Shetland (Maitland and East, 1976), the Forth area (Maitland, 1980a) and the Outer Hebrides (Maitland, 1981). Lying partly in the Highlands and partly in the Lowlands of Scot- land, the Clyde area includes a variety of freshwater habitats of the main types found in the British Isles. Its standing waters range from small pools (which are brackish near the coast), through numerous lochans and lochs to Loch Lomond, the largest area of fresh water in Great Britain. Most of these waters tend to be dystrophic or oligotro- phic and though some of those occurring in the lowland areas are eutro- phic, these are in the minority. Marl waters are uncommon. Running waters show a similar variety ranging from small burns in the north- west which drain directly into the sea, through numerous streams and small rivers which connect with larger systems, most notable among which is the River Clyde itself. Many of these running and standing waters are inter-connected. In past accounts of the fauna and flora of the Clyde area, the exact boundaries of the region dealt with have varied, some authors choos- ing county boundaries, others watersheds or a combination of the two. In this account, the area dealt with is that defined by Hosie and Mait- Glasg. Nat. 20 part 1 (1980) 32 land (1973) and includes the total catchment within a watershed starting at Skipness Point on the Mull of Kintyre (opposite the north end of Arran) and finishing north of Largs on the east side of the estuary. Geographically, the Clyde area includes parts of the three main divisions of Scotland — the Highlands, the Midland Valley and the Southern Uplands. In the Highland area, agricultural ground is limited to the valley floors and fringes of the lochs; the human population is sparse and tending to decrease. In the Midland Valley the presence of the Clyde estuary, the underlying carboniferous rocks (containing coal and iron) and the fertile agricultural soil have all combined to make this a very densely populated district. The Southern Uplands (consisting mainly of Silurian and Ordovician rocks) have weathered into rounded hills, covered in most places with grass. Much of this land is used for sheep farming, but on the lower slopes more intensive agri- culture is carried out. Thus the materials entering the waters in the area — including both nutrients and sewage — vary greatly in quality and quantity from place to place. The Waters In considering hydrological regions within the Clyde area in relation to the distribution of fish there, three main divisions can be recog- nised; (1) The Clyde estuary, including its sea lochs. (2) The Highland area, including the River Leven (Loch Lomond) catchment and all fresh waters west of this. (3) The Clyde system proper, including the Forth and Clyde Canal. ESTUARY The Clyde sea area has been considered in some detail by Mill (1901). The major part relevant to the present account is the estuary of the River Clyde itself, from the tidal weir at Glasgow Green down- stream to the firth. Several other areas are important, however, especi- ally the sea lochs (Gareloch, Loch Long, Loch Goil, Holy Loch, Loch Striven and Loch Fyne) and the small estuaries of streams entering them. The Clyde estuary runs west into a depression known as the Dunoon Basin, between Gourock and Kilcreggan. Most of the estuary is shallow and all areas between the tidal weir and a line joining Greenock and Rosneath Point are less than 10 m in depth. The surface area of the estuary is 70 km2 and the catchment draining into this occupies some 3870 km2. The average salinity in the estuary is about 18 mg/1, compared to some 33 mg/1 for the Clyde sea area as a whole. Much of the estuary from the tidal weir downstream is grossly polluted and devoid of oxygen during the summer months. Fish living in the less polluted areas are dependent on the high quality of fresh water from clean tributaries like the River Leven or on clean sea water flushed in by the tide. 33 HIGHLANDS The running waters in the Highland area consist mainly of small streams running directly into the sea lochs or into larger rivers (End- rick and Leven) and lochs (Eck and Lomond). These small streams rise in mountainous areas, often above 750 m, and have stony or rocky beds with steep gradients down to their mouths. Waterfalls are com- mon— an important feature where migratory species of fish are com cerned. Most waters in this area are unpolluted. The River Endrick (flowing eventually from Loch Lomond as the River Leven) is the only large river in the area and has a varied character. Near its source it is a typical Highland stream, but as it enters its main valley it broad- ens out to form a stony river. In its lower reaches its bed is mainly sand and the course of the river follows many slow meanders before eventually entering Loch Lomond in the south-east corner. Loch Lomond has a maximum length of 36 km and a total surface area of 70 km2. Its average depth is some 37 m with a maximum of 198 m. The northern part of the loch resembles many of the sea lochs in the Clyde area in being a long narrow trough; this reaches a maxi- mum depth of some 189 m below sea level. South of Ross Point the loch widens into a shallow basin with many islands. Like most of the large lochs in Scotland (e.g. Loch Ness and Loch Morar) Loch Lomond tends to be poor chemically. The northern basin runs through meta- morphosed Dalradian rocks and much of the land draining into it is exposed bare rock, its main covering in other places being blanket peat. The southern basin lies largely over Carboniferous and Devonian rocks; the land draining into it (mainly via the River Endrick) has an extensive covering of drift deposits, mainly boulder clay. Lock Eck has a maximum length of 9.7 km and a total surface area of 4.4 km2. Its average depth is some 17.1 m and its maximum depth about 42.3 m. Though narrower and less deep it is similar in many ways to the northern basin of Loch Lomond; thus it consists of an elongate glacial trough running from north to south parallel to most sea lochs in the area. Loch Eck has two main basins, both deeper than 16 m. Its shores are steep and there is little in the way of marginal vegetation. The water is poor chemically and most of the surrounding catchment is moorland, used either for rough grazing or forestry. It is of interest to note that Loch Eck and Loch Lomond, the only large lochs in the Clyde area, are both less than 10 m above sea level, and must undoubtedly have been sea lochs at one time. The catchment area draining into Loch Eck is some 104 km2; the River Cur is its main inflow. 34 CLYDE The River Clyde itself rises in the Leadhills area, in the extreme south-east of the region under consideration. Many similar burns have their sources in this area at a height of over 600 m; though not accepted conventionally as the source of the River Clyde, the Potrail Water is the most typical bum to consider as a source leading to the main river (Macphee 1969). Rising in peat-covered uplands, this burn has a swift gradient over a stony or bedrock substrate with numerous falls and cascades for the first few kilometres. Now the Clyde proper, the river flows in the Elvanfoot area as a medium-sized stream with a stony substrate and alternating stretches of pool and riffle. The river contin- ues on its course, twisting here and there, but running mainly in a north-westerly direction towards its estuary; as it does so it takes in its main tributaries — Duneaton, Medwin, Douglas, Mouse, Nethan, Avon, South Calder, North Calder and Rotten Calder. The tidal weir now interposes in the centre of the City of Glasgow. As the Clyde nears Glasgow it becomes a major river, but with this increase in size there is also an increase in pollution, especially with the inflow of the Calder Waters. Nevertheless, fish still occur as far downstream as Cambuslang and some invertebrates and recently even fish are found just above the tidal weir where, however, the river is very polluted. An intensive survey of the fauna of the River Clyde from its source to the tidal weir was carried out by Macphee (1969) and extensive surveys are now carried out by the Clyde River Purifica- tion Board. Below the tidal weir, two major tributaries enter the Clyde — the River Kelvin and the River Cart. Both are polluted in their lower reaches. The Forth and Clyde Canal runs from Grangemouth to Bowling, where it connects with the Clyde estuary; this main section has a length of some 56 km. In Glasgow a branch, formerly the Monkland Canal, ran to Airdrie. The canal was opened to traffic at the end of the 18th Century and was of major importance during a long period following this. It gradually became used less and less, however, and was eventu- ally closed to navigation in 1963. A few stretches have now been piped and filled over, but little else appears to be planned for this waterway, which is still of importance to several industries along its banks as a source of water for cooling and other purposes. Since their closure, many stretches have become weedy and overgrown. Fish There is a considerable volume of literature dealing with various aspects of the fish fauna of the Clyde area; some valuable old general accounts are available along with many short notes concerned only with one or a few species. Only Scott and Brown (1901) have pre- 35 viously dealt with the fish fauna of the whole area. The Loch Lomond district has been covered several times; by Brown (1891), Lumsden and Brown (1895), Lamond (1931), Hunter, Slack and Hunter (1959) and Maitland (1972b); these accounts deal mainly with the fish of the loch itself, while Maitland (1966a) studied its major inflow — the River En- drick. The fishes of the Clyde estuary, some of which are considered here as freshwater species, have been discussed by Elmhirst (1926) and more recently by Bagenal (1965). Perfect (1915) gave an account of the freshwater fish fauna of Renfrewshire. Macphee (1969) prepared a short account of the fishes of the River Clyde itself, while Maitland (1970, a, b) has briefly covered the fishes of the Forth and Clyde Canal and of streams in the Clyde area. Several individual species have been studied in the area in recent years (e.g. Copland, 1956; MacDonald, 1959a; Maitland, 1969b) and most of such references are listed below in the notes dealing with individual species. A number of studies deal with the parasites of fish in the area (e.g. Ritchie, 1914, 1915; Copland, 1957; Orr, 1967; Brattey, 1979). The nomenclature follows that given by Maitland (1972a). PETROMYZONIDAE Petromyzon marinus Linnaeus, 1758; Sea Lamprey. This species has been found occasionally in the estuary and sea lochs — e.g. Loch Fyne (Bagenal, 1965)— where it is probably commoner than supposed. In fresh water it appears to occur regularly only in the Loch Lomond system, where both larvae and adults have been recorded from the River Leven (MacDonald, 1959a), Loch Lomond (Lamond, 1931; Hun- ter, Slack and Hunter, 1959) and the River Endrick (Maitland, 1966a). There is only one other freshwater record from the Clyde area — of an adult seen in the River Eachaig, near Dunoon. The growth and tax- onomy of the Sea Lamprey in the area has been studied by MacDonald (1959a, b). There are several reports of numerous adults spawning in the River Leven in recent years. Lampetra fluviatilis (Linnaeus, 1758); River Lamprey. There ap- pear to be nq records of this species from the estuary, and much of the population may well be non-migratory. It is common in the Loch Lomond system— the River Leven (MacDonald, 1959a), Loch Lomond (L amond, 1931; Hunter, Slack and Hunter, 1959) and the River End- rick (Maitland, 1966a). Both larvae and adults have been recorded from these waters. The River Lamprey was recorded from the lower River Gryfe by Perfect (1915) but there appear to be no recent records from this water. In Loch Lomond, the adults are very common and prey extensively on the population of Powan there (Robertson, 1870; Maitland, 1968, 1980b). The growth and taxonomy of this species in the area have been studied by MacDonald (1959a, b). 36 Lam petra planeri (Bloch, 1784); Brook Lamprey. Apart from its absence from salt water, this is the most widespread lamprey in the Clyde area. Like the other two species, it is common in the Loch Lom- ond district — e.g. the River Leven (MacDonald 1959a), Loch Lomond (Hunter, Slack and Hunter, 1959) and the River Endrick (Maitland, 1966a) and other tributaries to the loch. The Brook Lamprey however, is also common in other waters not accessible to the migratory species because of pollution or waterfalls, e.g. the River Avon at Stonehouse and the River Allander at Milngavie. The growth and taxonomy of this species in the area have been studied by MacDonald, (1959a, b). ACIPENSERIDAE Acipenser sturio Linnaeus, 1758; Sturgeon. Only ever found in the estuary and sea loch areas of the Clyde, this species is recorded from time to time by commercial fishermen (Grieve, 1896). It has been recor- ded from Loch Fyne (Scott and Brown, 1901) and the more seaward parts of the Firth of Clyde (Scott and Brown, 1901); Rae and Wilson, 1952; Rae and Pirie, 1968). CLUPEIDAE Alosa alosa (Linnaeus, 1758); Allis Shad. This species occurs only in the estuary area but appears to be not uncommon there. It has been recorded from Loch Fyne (Scott and Brown, 1901; Rae and Wilson, 1952, 1953), Loch Striven (Rae and Wilson, 1953) and off Inchmar- nock, by Bute (Rae and Wilson, 1953; 1955). Two specimens were recently caught off Ailsa Craig (Burkel, 1971a). Most of the specimens noted have been taken accidentally by commercial fishermen. Alosa fallax (Lacepede, 1803); Twaite Shad. Also restricted to the estuary area, this species is less common than the Allis Shad and has been recorded only a few times from the Clyde area in recent years (Rae and Wilson, 1955; Bagenal, 1965). A single specimen was caught off Ailsa Craig early in 1969 (Burkel, 1971a). SALMONIDAE Sal mo salar Linnaeus, 1758; Salmon. Though virtually absent from the Clyde system proper, this species is common in parts of the estuary and the unpolluted waters running into it, e.g. River Leven, Loch Lomond (Wood, 1954), River Endrick (Maitland, 1966a), River Each- aig. Loch Eck, etc. Perfect (1915) notes that the salmon was formerly common in the River Cart and tributaries; though it disappeared there because of pollution it is of interest to note that several have rec- ently been recorded from the Rivers Gryfe and Kelvin. The growth and food of the young of this species in the Loch Lomond area have been studied by Maitland (1965). 37 Salmo trutta Linnaeus, 1758; Trout. Probably the most abundant and widespread species in the Clyde area. Trout occur in most unpol- luted waters where suitable spawning facilities are available but not too many predators. Thus they are found in small highland streams (the upper reaches of the River Clyde and the River Endrick (Mait- land, 1966a)), larger slow-flowing rivers (the River Clyde (Waddington, 1973), and the lower reaches of the River Endrick), in many small lochs (e.g. the Black Loch) and in large ones (e.g. Loch Lomond and Loch Eck). The Brown Trout, Salmo trutta fario L. occurs in most parts of the area, except the estuary, while the Sea Trout, Salmo trutta trutta L., is common in parts of the estuary (Lamond, 1931; Bag- enal, 1965) and Highland area but absent from the Clyde system and other polluted or inaccessible waters. The food and growth of the young of Salmo trutta in the River Endrick have been studied by Maitland (1965). Salmo gairdneri Richardson, 1836; Rainbow Trout. Though not a native to the Clyde area, this species (originally from North America) has been introduced to a variety of waters and is becoming increasingly popular with anglers and fish farmers. The first stocks were released in the Clyde area more than 50 years ago (Perfect, 19 i 5) but the species never seems to have become established here. All recent records are of introductions to angling waters (e.g. White Loch, Hillend Reservoir, etc.) or escapes from such waters (Maitland, 1966b). Salvelinus alpinus (Linnaeus, 1758); Charr. The existence of this species in the Clyde area was formerly doubtful, but as recently as 1955 specimens of a new subspecies were caught in Loch Eck (Friend, 1956; 1959) and the author has netted further specimens there since then. This is the only water in the area known to contain this species. The exist- ence of a population in Loch Lomond was suggested by Bidie (1896) but discounted by Brown (1896) and there is no proof that this exists at present. Salvelinus fontinalis (Mitchill, 1815); Brook Charr. Scott and Brown (1901) note that this species, originally native to North Amer- ica, was introduced to many lochs (including Loch Lomond) and rivers in the Clyde area. Though recorded at intervals from the River Calder (Perfect, 1915) there are no recent records, and the species does not seem to have established itself as it has done in several lochs elsewhere in Scotland. COREGONIDAE Coregonus lavaretus (Linnaeus, 1758); Powan (Whitefish). This species was originally described from material collected in Loch Lom- ond as Coregonus clupeoides (Lacepede, 1803) and though it is no longer regarded as a distinct species it can probably be considered the 38 most unique fish in the Clyde area (Maitland, 1979). Powan are found only in Loch Lomond and Loch Eck, though similar forms (treated as different sub-species) occur in three lakes in England and one llyn in Wales. Research on various aspects of the Powan has now been carried out, especially in Loch Lomond, and much of its biology is now known (e.g. Parnell, 1838; McNiven, 1863; Gervers, 1954; Slack, 1955; Slack, Gervers and Hamilton, 1957; Gasowska, 1965; Maitland 1967, 1968, 1969b). THYMALLIDAE Thymallus thymallus (Linnaeus, 1758); Grayling. Though indigen- ous to the British Isles this species did not occur naturally in the Clyde area but was introduced into the River Clyde by Man (Maitland, 1977). It is still restricted to the Clyde system proper but is very well established there, being found in the main river from Abington down- stream to about Hamilton and in many of the tributaries above Glas- gow (e.g. the Duneaton Water and River Avon). The Grayling is common also in the River Gryfe and may well invade waters north of the Clyde estuary from here at some future date. OSMERIDAE Osmerus eperlanus (Linnaeus, 1758); Smelt. This species is stated by Scott and Brown (1901) to be not uncommon in the Clyde (estuary) area and they note a specimen caught off Brodick. Very few specimens have been noted recently, however, and the Smelt may well be rare here now as is the case in the Firth of Forth. All published records have been from the estuary or sea lochs. ESOCIDAE Esox lucius Linnaeus, 1758; Pike. A widespread and common species in the Clyde area, the Pike occurs in all types of standing water and many slow-flowing streams and rivers. Though purely a freshwater species, and therefore absent from the estuary, it has been found in most other regions, e.g. Loch Lomond (Robertson, 1888), River End- rick (Maitland, 1966a), River Gryfe, the lower parts of the River Clyde and its tributaries. Forth and Clyde Canal (Maitland, 1969b) and many small lochs throughout the area — Ascog, Geal, Ardinning, Tannoch, Woodend, Libo, etc. Its food and parasites in Loch Lomond have been described by Copland (1956), and its biology has been studied there and in the neighbouring Dubh Lochan by Shaft and Maitland (1971b). Brattey (1979) has examined its parasites in the Forth and Clyde Canal. CYPRINIDAE Cyprinus carpio Linnaeus, 1758; Carp. Both Scott and Brown (1901) and Perfect (1915) record this species as having been success- 39 fully introduced to various ponds in the Clyde area. None of these is specified. No recent specimens appear to have been captured, however, apart from those taken from the thriving population described by Maitland (1964). The species has been introduced to the Forth and Clyde Canal (Burkei, 1971b). Carassius auratus (Linnaeus, 1758); Goldfish. Scott and Brown (1901) and Perfect (1915) recorded this species as having been intro- duced to waste ponds near Paisley, where it was said to breed freely. There is no recent record from these waters, however, though the spec- ies is certainly present in ponds in Glasgow, near Dunoon, and in the Forth and Clyde Canal. The latter population was associated with a heated water effluent in the Clydebank area and was unusual in having a very high proportion of coloured individuals (Maitland, 1971). Gobio gobio (Linnaeus, 1758); Gudgeon. Previously known in Scotland only from rivers on the east coast, this species has recently appeared in the River Irvine (Clyde River Purification Board, 1979) where specimens were found during a pollution fish kill. It was intro- duced to the Endrick system (Culcreuch Loch) several years ago by Dr D. L. Burkei (personal communication) and though it does not appear to have established itself it is likely to move into the Clyde area in due course. Tinea tinea (Linnaeus, 1758); Tench. Young (1870) and Brown (1891) both record this species from the mouth of the River Endrick and from a small pond near Balmaha. The latter has since been filled in, and though the author has netted the Endrick mouth area on several occasions, no Tench have been seen. The species may well be extinct here now. The only population known to exist at present in the Clyde area is a well-established one occurring in a small weedy lochan near Lesmahagow; specimens from this stock have recently been placed in several other waters in the Clyde area (Burkei, 1971b). Abramis brama (Linnaeus, 1758); Bream. In Scotland, this species was known previously only from the south-west (Maitland, 1970c). However, in recent years there have been several attempts to establish it elsewhere and introductions have taken place to Strathclyde Loch and to the Forth and Clyde Canal. It is not known yet whether these have been successful or not. Phoxinus phoxinus (Linnaeus, 1758); Minnow. This species is widely distributed and common in the Clyde area, apart from the estu- ary. It is found in most unpolluted running waters, from small burns (e.g. Craigton Burn) to large rivers such as the River Endrick, the River Clyde and its tributaries. It also thrives in many lochs which have spawning facilities in the form of streams or wave-washed stony shores and occurs in both Loch Lomond and Loch Eck. The food of the Minnow in the River Endrick has been studied by Maitland (1965) 40 while Scott (1963) carried out research on the reproductive biology of the species in lochs in the same area. Rutilus rutilus (Linnaeus, 1758); Roach. This is common in many standing and slow-flowing waters in the Clyde area including Loch Fad and Loch Ascog (Bute), Loch Lomond (Lumsden and Brown, 1895), Loch Libo, the lower reaches of the River Clyde and some of its tribu- taries (e.g. the River Avon), the Forth and Clyde Canal (Ritchie, 1917; Hammerton, 1972) and many small lochs in the area (e.g. Kilrnar- dinny, Woodend, Hogganfield, etc). It appears to be absent from Loch Eck and all other waters to the north-west of the Bute and Loch Lomond populations. Ure (1795) noted that, though the species is considered characteristic of slow-flowing water, the Loch Lomond population makes an annual migration in June upstream into the River Endrick to spawn in fast-flowing water there. Though the exis- tence of this spawning run is doubted by Brown (1891) it has been clearly verified by the author (Maitland, 1966a). The growth of Roach in some waters in the Clyde area has been studied by Mills (1969), and its parasites in the Forth and Clyde Canal by Brattey (1979). Leucisus idus (Linnaeus, 1758); Orfe. As with the Goldfish the golden form of the Orfe is often kept by aquarists in tanks and ponds and many have been introduced to different parts of the Clyde area. There are no authentic records, however, of the species establishing itself anywhere. COBITIDAE N oemacheilus barbatulus (Linnaeus, 1758); Stone Loach. This species, mostly found in running water, is fairly widespread in the Clyde area though it is never found in the estuary. It occurs in Loch Lomond (Hunter, Slack and Hunter, 1959) and associated waters, e.g. the River Endrick (Maitland, 1966a) in the River Kelvin, the River Gryfe and most parts of the River Clyde. It appears to be absent from the Forth and Clyde Canal and, though common in a few lochs in the area, it is absent from the majority. There are no records of this species from the west coast of Scotland north of Loch Lomond. The food of the Stone Loach in the River Endrick has been studied by Maitland (1965). ANGUILLIDAE Anguilla anguilla (Linnaeus, 1758); Eel. A very widely distributed and common species in the British Isles, the Eel is found in most parts of the Clyde area. It is common in all unpolluted parts of the estuary (Elmhirst, 1926; Bagenal, 1965); in most rivers and streams running into it, e.g. the River Leven, Loch Lomond (Hunter, Slack and Hunter, 1959), the River Endrick (Maitland, 1966a), the River Eachaig and 41 Loch Eck; and even the higher stretches of waters affected by pollution in their lower reaches such as the River Gryfe and parts of the Clyde system. It is rarely abundant in the latter type of water, however. Its biology in the Dubh Lochan has been studied by Shafi and Maitland (1973). GASTEROSTEIDAE Gasterosteus aculeatus Linnaeus, 1758; Three-spined Stickleback. This species is also very widely distributed in the Clyde area, occurring in the estuary and sea lochs (Elmhirst, 1926) and in most other reason- ably rich, still, or slow-flowing waters e.g. the River Eachaig, the River Leven, Loch Lomond (Hunter, Slack and Hunter, 1959), the River Endrick (Maitland, 1966a), the River Allander, the River Clyde and many of its tributaries. Loch Libo, the Forth and Clyde Canal, etc. Its food in the River Endrick has been studied by Maitland (1965). Pungitius pungitius (Linnaeus, 1758); Ten-spined Stickleback. Though widespread in the British Isles, this species is not common in the Clyde area. Scott and Brown (1901) record it from Loch Lomond and Possil Marsh, and Hunter, Slack and Hunter (1959) from Loch Lomond and Dougalston Loch. A scattered but never dense population undoubtedly exists in Loch Lomond and specimens have also been collected recently from the River Leven. Two further localities with breeding populations were found in May 1969 — both small streams, one near Dullatur the other near Kirkintilloch. No other recent records are available, though it is likely that the species does occur elsewhere in the Clyde area. SERRANIDAE Dicentrarchus labrax (Linnaeus, 1758); Sea Bass. The present status of this species in the Clyde area is uncertain. A marine species which commonly comes into estuaries and the lower reaches of large rivers, it has been recorded here only in the sea lochs and main firth, where Rae (1964) says that it may be common at times; two specimens were recorded from the firth in 1964 (Burkel, 1971a). Bagenal (1965) records a single specimen from Loch Striven. There have been recent reports from the lower reaches of the River Leven. PERCIDAE Perea fluviatilis Linnaeus, 1758; Perch. This species, though ab- sent from the estuary, is widespread and common in most parts of the Clyde area where suitable standing or slow-flowing waters occur. Thus it has been recorded from Loch Lomond (Hunter, Slack and Hunter, 1959), the lower parts of the River Endrick (Maitland, 1966a), the River Gryfe, the lower reaches of the River Clyde and its tributaries. 42 the Forth and Clyde Canal (Ritchie, 1917; Maitland, 1969b) and many small lochs in the area (Dumbrock, Tannoch, Libo etc.). It appears to be absent from many hill lochs and all waters (including Loch Eck) to the north and west of Loch Lomond. A detailed study of the biology of this species in Loch Lomond and the neighbouring Dubh Loch an has been carried out by Shaft and Maitland (1971a). Its parasites in the Forth and Clyde Canal have been studied by Rrattey (1979). GOBIIDAE Pomatoschistus microps (Kroyer, 1840); Common Goby. The only member of the Gobiidae found regularly in fresh and estuarine waters in the British Isles, the taxonomy of this species has only recently been clarified. It appears to be common in most parts of the estuary which are not affected by pollution (Hunter, Slack and Hunter, 1959; Bagenal, 1965) and in the sea lochs in the vicinity of river mouths. MUGILIDAE Crenimugil labrosus (Risso, 1826); Thick-lipped Mullet. Lumsden and Brown (1895) and Scott and Brown (1901) record this essentiall)) marine species from the Clyde estuary and the River Leven. A single specimen was recorded from Loch Fyne by Rae and Wilson (1961) and Bagenal (1965) notes that in the Clyde area this species is rare but probably commoner than it appears. Burkel and Dobson (1975) record it at Hunterston and large numbers are now netted each year in the mouth of the River Leven. Chelon ramada (Risso, 1826); Thin-lipped Mullet. Scott and Brown (1901) record a single specimen of this species from the Clyde area, but there appear to be no recent records and its present status here is uncertain. COTTIDAE Cottus gobio Linnaeus, 1758; Bullhead. Though often stated to be absent from Scotland (e.g. Regan, 1911) the Bullhead is well establish- ed in both the Clyde and Forth areas (Maitland, 1969a). Scott and Brown (1901) recorded it from the upper Kelvin and tributaries and from Dobb’s Bum near Paisley but there are no recent records from these waters. Patton (1951), however, recorded it from the River Earn and this population was subsequently confirmed by Gemmell (1962). The present author has found it to be abundant in several parts of the Earn system, and it has been recorded recently from the River White Cart at Stamperland (Livingstone and Wright, 1974). The age and growth of this species in parts of the River Earn has been studied by McAleer (personal communication). 43 PLEURONECTIDAE Platichthys flesus (Linnaeus, 1758); Flounder. This species is com- mon in the unpolluted parts of the Clyde estuary and those fresh waters easily accessible from it. Thus Bagenal (1965) notes that it is frequent in the Clyde Sea area, while Hunter, Slack and Hunter (1959) state that it occurs in parts of the estuary and Loch Lomond. Small fish are abundant in some streams running into the River Leven and the author has caught specimens in most parts of Loch Lomond — even in the northern part of the loch at depths greater than 30 m (Maitland, 1969a). Flounders also occur in the River Endrick (Maitland, 1966a), while Perfect (1915) recorded this species from the River Clyde as far up- stream as Crosslea. There appear to be no recent records from here however. Fish Communities The major hydrological regions related to fish distribution in the Clyde area have been described above. The estuary has many characteristic species and it is only in this part of the Clyde area that Sturgeon, Allis Shad, Twaite Shad, Smelt, Sea Bass, Common Goby, Thick-lipped Mullet and Thin-lipped Mullet occur. These are all typical marine or estuarine species found round various parts of the Scottish coast. Another typical element of the estuarine fish fauna is represented by migratory species (e.g. Sea Lam- prey, Salmon, Sea Trout, Eel and Flounder) which are found here on their migrations either to or from fresh water. A few ubiquitous species are also found (e.g. Three-spined Stickleback) while many purely marine species occur in various areas (e.g. Argentine; Argentina sphyraena Linnaeus, 1758; Plaice, Pleuronectes platessa Linnaeus, 1758). Waters in the Highland area associated directly with the estuary are characterised by the dominance or abundance of migratory species, notably Salmon, Sea Trout and Eels. Clearly, however, such species are absent from waters where severe pollution (uncommon in this area) or some physical obstacle (Stuart, 1962) prevents their migration up- stream. Many other freshwater species occur in this area, notably Minnow, Stone Loach, Three-spined Stickleback, Pike and Perch; the last two species occur mainly in lochs or slow-flowing rivers. Loch Eck is the most characteristic oligotrophic water in the area and its fish community is dominated by salmonid fishes, notably Salmon, Trout, Charr and Powan. As noted above, this is the only loch in the Clyde area known to contain Charr. Powan are found elsewhere only in Loch Lomond where, due to the dual character of the loch (Slack 1957) a wide variety of other fish species occur, notably Sea Lamprey River Lamprey, Brook Lamprey, Salmon, Trout, Pike, Eel, Minnow, 44 Roach, Stone Loach, Perch, Three-spined Stickleback, Ten-spined Stickleback and Flounder. This and the two largest lochs on Bute appear to be the only sites in the Highland area where Roach occur. Loch Lomond appears to have more fish species than any other loch in Scotland. The River Clyde itself is characterised by the presence of only two species not found elsewhere in the area, the Grayling which is quite widespread and the Bullhead which at the moment appears to be mainly confined to the Earn system. Apart from the presence of these species, however, the absence (or virtual absence) of migratory species is of major importance. A few of these (e.g. Salmon and Sea Trout) do occur occasionally in the tributaries below the tidal weir (e.g. the River Gryfe) and the Eel in some numbers even above Glasgow; such fish are never abun- dant and not part of the typical communities of this area at the mom- ent. Grayling, Minnow and Stone Loach occur in most streams and rivers in the system, while Pike, Roach and Perch are common in the slow-flowing parts of the river and many lochs. Brown Trout and Three-spined Sticklebacks occur in most waters in the Clyde system. The Forth and Clyde Canal has little in the way of characteristic fish species its population being dominated by Pike, Roach, Perch and Three-spined Stickleback. Its most unique feature was probably the dense population of coloured Goldfish noted above which was associ- ated with heated water effluent in the Clydebank area. With the closing of this effluent the population appears to have dispersed. Perhaps one of the most important features of the Forth and Clyde Canal is that it forms the major direct connection for aquatic animals to pass from the Clyde to the Forth catchment or vice versa. Thus it could be an im- portant route of dispersion for fish species at present confined to one side of Scotland. Commercial Fisheries Apart from marine fish, several freshwater species have been ex- ploited commercially in the Clyde area. Thus Salmon and Sea Trout were formerly netted in large numbers in Loch Lomond, the River Leven and parts of the Clyde estuary (Lamond, 1931). This fishing has virtually stopped, apart from fish netted each year in Loch Lomond. For some years Powan were netted in Loch Lomond and sold in the Glasgow market. This netting was intensified here and in Loch Eck (Mr W. Younger, personal communication) during and just after the 1st World War and many thousands of fish were caught and sold each year. This fishing finished about 1926 (Lamond, 1931). Eels too were fished commercially in Loch Lomond during this period and though this was abandoned along with the Powan fishing, attempts have been 45 made to revive this from time to time at Balmaha and in the River Leven. The only other important commercial fishery recorded from the Clyde area appears to have been that for Flounders at the mouth of the White Cart (Perfect, 1915). The main use being made at the present by Man of the freshwater fish fauna of the Clyde area is for sport fishing. The major species angled are Salmon, Trout, Grayling, Pike, Roach and Perch. Discussion As in most other parts of the British Isles, the present fish fauna of the Clyde area is made up of an assemblage of species, mostly indig- enous — of both marine and freshwater origin — but some of them introduced. Many species are by no means widely distributed and the waters in the area can be divided on the basis of their fish faunas into the three major systems outlined above: estuary. Highlands and Clyde proper. It is of interest to note that few of the barriers to fish in the area can be described as natural — the transition between salt water and fresh in the estuary being the major exception. Other major divisions are due to obstacles created by Man and it is probable that fish popu- lations in the area were much more homogeneous in the past with a domination by Salmon, Trout and Eel in accessible fast-flowing waters and oligotrophic lochs, and Pike, Roach and Perch in slow-flowing waters and richer lochs. The development of the canal system, the building of weirs, the intense pollution of some waters and the introduction of certain fish species have altered the communities to their present form. However, with the disuse of the canals and the extremely valuable pollution pre- vention work being carried out in the area by the Clyde River Purifi- cation Board, there has been a reversal of the situation and a steady change in the populations in some waters. Thus it is probable that migratory species like Salmon, Sea Trout and Flounder will become common in the River Gryfe, the River Kelvin and eventually the River Clyde itself. At this time too, when the barrier imposed by gross pollu- tion in the lower Clyde has been removed, a wider dispersal of species at present restricted to parts of the Clyde system, notably Grayling and Bullhead, can be expected. Many of the waters in the Loch Lomond area are highly suitable for both these species. The most unique features of the fish fauna of the Clyde Area are the populations of Powan in Loch Lomond and Loch Eck (Maitland, 1970d) and of Charr in Loch Eck. Both these species are of extreme ichthyological interest and as such their populations should be conser- ved as carefully as possible. Fortunately both the lochs concerned are very large (and therefore less liable to contamination) and of high amenity value (Maitland, 1976). Nevertheless, with the increasing pres- 46 sures from a variety of quarters — particularly to Loch Lomond (Mait- land, 1972b) — it is essential that the interests of both ecosystems, including their fish populations, be safeguarded as much as possible. Acknowledgments Much of the information described in this paper was obtained dur- ing my period of research at the University of Glasgow and I am grateful to Sir Maurice Yonge, Professor D. R. Newth, and Dr H. D. Slack for the facilities provided in the Department of Zoology there. Dr D. L. Burkel has helped me with information and specimens of rare species while Mr David N. Webster has given invaluable aid on numerous weekend fishing trips. My wife, Kathleen, was good enough to read and comment on the present manuscript. Many other people, too numerous to mention individually, have been kind enough to supply me with records of fish from the Clyde area and other places, and I am always interested to hear of or see specimens of freshwater fish from any part of the British Isles. References Bagenal, T. B. 1965. The fauna of the Clyde Sea area : 4, Fishes. Scottish Marine Biological Association. Bidie, G. 1896. Char in Loch Lomond. Ann. Scot. nat. Hist. 124: 258. Brattey, J. 1979. Intestinal helminths from fish of the Forth and Clyde Canal at Temple, Glasgow. Glasg. Nat. 19: 415-429. Brown, A. 1891. The fishes of Loch Lomond and its tributaries. Scott. Nat. 10: 114-124. Brown, A. 1896. Char in Loch Lomond. Ann. Scot. nat. Hist. 192. Burkel, D. L. 1971a. Fish records from the Clyde sea area. Glasg. Nat. 18: 574. Burkel, D. L. 1971b. Introduction of fish to new waters. Glasg. Nat. 18: 574-575. Burkel, D. L. and Dobson, R. M. 1975. Fish: Clyde sea area records. Glasg. Nat. 19: 200-201. Clyde River Purification Board 1979. Annual Report. CRPB. Glasgow. Copland, W. O. 1956 Notes on the food and parasites of Pike (Esox lucius ) in Loch Lomond. Glasg. Nat. 17: 230-235. Copland, W. O. 1957. The parasites of Loch Lomond fishes. Studies on Loch Lomond 1 : 128-133. Glasgow University. Elmhirst, R. 1926. Notes on fishes from the Firth of Clyde. Scott. Nat. 151- 158: 179-186. Friend, G. F. 1956. A new sub-species of Charr from Lock Eck. Glasg. Nat. 17: 219-220. Friend, G. F. 1959. Subspeciation in British charrs. Publ. Syst. Ass. 3: 121-129. Gasowska, M. 1965. A preliminary taxonomic revision of the British whitefish with especial reference to the Gwyniad of Llyn Tegid (Bala). Proc. zool. Soc. Lond. 145: 1-8. 47 Gemmel, H. 1962. Miller’s Thumb Bullhead in Renfrewshire. Glasg. Nat, 18: 213-214. Gervers, F. W. K. 1954. A supernumary fin in the Powan ( Coregonus clupe - aides Lacepede). Nature Land. 174: 935. Grieve, J. 1896. Sturgeon in the Clyde. Trans, nat. Hist. Soc. 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Studies on bottom fauna in streams in the West of Scot- land. Ph.D. Thesis, University of Glasgow. Maitland, P. S. 1964. A population of Common Carp ( Cyprinus carpio ) in the Loch Lomond district. Glasg. Nat. 18: 349-350. Maitland, P. S. 1965. The feeding relationships of Salmon, Trout, Minnows, Stone Loach and Three-Spined Sticklebacks in the River Endrick, Scotland. J. Anim. Ecol. 34: 109-133. Maitland, P. S. 1966a. The fauna of the River Endrick. Studies on Loch Lom- ond, 2: 1-194. Glasgow University. Maitland, P. S. 1966b. Rainbow Trout, Salmo irideus Gibbons, in the Loch Lomond district. Glasg. Nat. 18: 421-423. Maitland, P. S. 1967. The artificial fertilisation and rearing of the eggs of Coregonus clupeoides Lacepede. Proc. R. Soc. Edinb. 70: 82-106. Maitland, P. S. 1968. Echo sounding observations on the Lochmaben Vendace, Coregonus vandesius Richardson. Trans. J. Proc. Dumfries Galloway nat. Hist. Antiq. Soc. 44: 29-46. Maitland, P. S. 1969a. A preliminary account of the mapping of the distrib- ution of freshwater fish in the British Isles. J. Fish Biol. 1 : 45-58. Maitland, P. S. 1969b. The reproduction and fecundity of the Powan, Core- gonus clupeoides Lacepede, in Loch Lomond, Scotland. Proc. R. Soc. Edinb. 70: 233-264. Maitland, P. S. 1970a. The fauna of the Forth and Clyde Canal. Fid. Stud. Sch. 6: 179-187. Maitland, P. S. 1970b. The fauna of streams in the Clyde area. Fid. Stud. Sch. 6: 42-50. Maitland, P. S. 1970c. The freshwater fish fauna of south-west Scotland. Trans. J. Proc. Dumfries Galloway nat. Hist. Antiq. Soc. 47: 49-62. 48 Maitland, P. S. 1970d. The origin and present distribution of Coregonus in the British Isles. Proc. Ini. Symp. Biol. Coregonid Fish., Manitoba, 1 : 99-114. Maitland, P. S. 1971. A population of coloured goldfish, Carassius auratus, in the Forth and Clyde Canal. Glasg. Nat. 18: 565-568. Maitland, P. S. 1972a. A key to the freshwater fishes of the British Isles, with notes on their distribution and ecology. Scient. Publ. Freshwat. biol. Ass. 27: 1-139. Maitland, P. S. 1972b. Loch Lomond: man’s effects on the salmonid com- munity. J. Fish. Res. Bd. Can. 29- 849-860. Maitland, P. S. 1976. Fish in the large freshwater lochs of Scotland. Scottish Wildlife 12: 13-17. Maitland, P. S. 1977. Freshwater fish in Scotland in the 18th, 19th and 20th centuries. Biol. Conserv. 12: 265-278. Maitland, P. S. 1979. The status and conservation of rare freshwater fish in the British Isles. Proc. Brit. Freshw. Fish. Conf. 1 : 237-248. Maitland, P. S. 1980a. The freshwater fish fauna of the Forth area. Forth Nat. and Hist. 4: 33-47. Maitland, P. S. 1980b. Scarring of whitefish 0 Coregonus lavaretus ) by Euro- pean river lamprey (Lampetra fluviatilis) in Loch Lomond, Scotland. Can. J. Fish. Aqua. Sci., in press. Maitland, P. S. 1981. The freshwater fish fauna of the Outer Hebrides. Heb- rid. Nat. in press. Maitland, P. S. and East, K. 1976. The freshwater fish fauna of Shetland. Glasg. Nat 19: 321-324. Mill, H. R. 1901. Physical conditions in the Clyde Sea area. (pp. 385-398 in Elliot, G. F. S., Laurie, M. and Murdoch, J. B. Fauna, Flora and Geol- ogy of the Clyde Area. Glasgow). Mills, D. A. 1969. The growth and population densities of Roach in some Scottish waters. Proc. Brit. Coarse Fish Conf. 4: 50-57. Orr, T. S. C. 1967. Parasites of freshwater fish in the Glasgow area. Glasg. Nat. 18: 503-504. Parnell, R. 1838. Observations on the Coregoni of Loch Lomond. Ann. Mag. nat. Hist. 1 : 161-165. Patton, D. 1951. The Miller’s Thumb. Cottus gobio Linn. Glasg. Nat. 17: 48. Perfect, W. F. 1915. Renfrewshire freshwater fishes. Trans. Paisley Nat. Soc. 2: 61-65. Rae, B. B. 1964. Rare fishes. Scot. Fish Bull. 22: 17. Rae, B. B. and Pirie, S. F. 1968. Rare fish records. Scot. Fish Bull. 30: 31-32. Rae, B. B. and Wilson, E. 1952. Rare and exotic fishes recorded in Scotland during 1951. Scott. Nat. 64: 102-111. Rae, B. B. and Wilson, E. 1953. Rare and exotic fishes recorded in Scotland during 1952. Scott. Nat. 65: 141-153. Rae, B. B. and Wilson, E. 1955. Rare and exotic fishes recorded in Scotland during 1953. Scott. Nat. 66: 170-185. Rae, B. B. and Wilson, E. 1961. Rare and exotic fishes recorded in Scotland during 1956. Scott. Nat. 70: 22-33. Regan, C. T. 1911. The freshwater fishes of the British Isles. Methuen, London. 49 Ritchie, J. 1914. Argulus foliaceus. Glasg. Nat. 6: 98-99. Ritchie, J. 1915. A contribution to the parasitic fauna of the west of Scotland. Glasg. Nat. 7: 33-42. Ritchie, J. 1917. The epidemic among Roach ( Leuciscus rutilus L.) on the Forth and Clyde Canal during the summer, 1916. Glasg. Nat. 8: 160-163. Robertson, D. 1870. On Petromyzon fluviatilis, and its mode of preying on Coregonus clupeoides. Proc. Nat. Hist. Soc. Glasg. 2: 61-62. Robertson, D. 1888. The Pike, Esox Indus, Lin. Trans, nat. Hist. Soc. Glasg. 2: 212-214. Scott, D. B. C. 1963. Reproduction in female Phoxinus. Ph.D. Thesis, Univer- sity of Glasgow. Scott, T. and Brown, A. 1901. The marine and freshwater fishes, (pp.173-180 in Elliot, G. F. S., Laurie, M. and Murdoch, J. B. Fauna, Flora and Geol- ogy of the Clyde Area. Glasgow). Shafi, M. and Maitland, P. S. 1971a. The age and growth of perch ( Perea fluviatilis L.) in two Scottish Lochs. J. Fish. Biol. 3 : 39-57. Shafi, M. and Maitland, P. S. 1971b. Comparative aspects of the biology of pike, Esox lucius L., in two Scottish lochs. Proc. R. Soc. Edinb. 71 : 41-60. Shafi, M. and Maitland, P. S. 1973. Observations on the population of Eels — Anguilla anguilla (L) — in the Dubh Lochan, Rowardennan, Stirlingshire. Glasg. Nat. 19: 17-20. Slack, H. D. 1955. Factors affecting the productivity of Coregonus clupeoides Lacepede in Loch Lomond. Verh. int. Verein theor. angew. Limnol., 12: 183-186. Slack, H. D. 1957. The topography of the lake. Studies on Loch Lomond 1 : 4-13. Glasgow University. Slack, H. D., Gervers, F. W. K. and Hamilton, J. D. 1957. The biology of the Powan. Studies on Loch Lomond. 1: 113-117. Glasgow University. Stuart, T. A. 1962. The leaping behaviour of Salmon and Trout at falls and obstructions. Scient. Invest. Freshwat. Salm. Fish. Res. Scott. Home Dep . 28: 1-46. Ure, D. 1795. Parish of Killearn. Statist. Acc. Scot. 16: 100-129. W Addington, J. I. 1973. Record trout in Upper Clyde. Western Naturalist 2; 70. Wood, I. 1954. Loch Lomond and its Salmon. Glasgow. Young, J. 1870. Note on Tench in Loch Lomond. Proc. nat. Hist Soc. Glasg. 2: 67. 50 Glasgow Natural History Society On 13th November 1979 the name of the Society was changed from the Andersonian Naturalists of Glasgow to the Glasgow Natural History Society. This was done in order to make the aims of the Society more explicit and to show the links with similar organisations throughout the British Isles. It also relates back to the Natural History Society of Glasgow, the oldest constituent Society. It is interesting to quote from the last minutes of the Natural History Society of Glasgow of 50 years ago : 28th October 1930 “The report of the Amalgamation Committee which has been refer- red to the Council for consideration was fully gone into. It appeared that one of the greatest difficulties that lay in the way of an amalgamation was the disposal of the Society’s Library. This matter was taken up by a special Sub-Committee. As a result of their negotiations, the Mitchell Library agreed to house the collection under the same conditions as applied to the Society’s foreign Transactions already kept there. At the January meeting, the Amalgamation Committee was re-appointed to make the amalgamation effective. Meetings were held with represent- atives from the Andersonian Naturalists’ Society and the Microscopical Society of Glasgow and, as a result, a draft Constitution was drawn up which has been approved by all three Societies. A joint meeting of the Councils of the three Societies has also been held, at which it was decided that the first meeting of the new Society, the Glasgow and Andersonian Natural History and Microscopical Society, should be held in January 1931, in the Royal Technical College”. The Herbarium of the Glasgow Museum and Art Gallery *GWYNETH JONES Museum and Art Gallery, Kelvingrove, Glasgow Received January 1980 The collections of the City of Glasgow were initiated by the activities of a local coach-builder, Archibald McLellan (1796-1854), who was also an enthusiastic art collector. He left his collection, and the build- ing to house them, to the City, but unfortunately he was insolvent at the time of his death. In order to save the collection, the City had to “buy” both collection and building. In 1870, Glasgow Corporation purchased Kelvingrove Mansion House, built in 1783, in what is now Kelvingrove Park. It was known locally as the City and Industrial Museum, housing predominantly historic and scientific material. Natural history collections were by then rapidly accumulated, thanks to local interest, but little display space was available. In 1876, an extension was added for the technological items and 1888 saw the First International Exhibition, which raised funds to- wards a new building to house all the collections. By the 1890s construction was well underway and in 1901 the Sec- ond International Exhibition was held in Kelvingrove Park to coincide with the opening of the new museum. The journal “British Architect” commented in 1892 that it “combines both picturesqueness and dig- nity. The former quality is perhaps somewhat in excess”. The new building allowed the formation of various departments including natural history. ♦Present address: Council of Museums in Wales, 29 Chapel Street, Llandudno, Gwynedd. Glasg. Nat. 20 part 1 (1980) 52 The Herbarium Most of the botanical collections date from the decades around the turn of the century. Whilst the Universities of Glasgow and Strath- clyde (formerly the Glasgow and West of Scotland Technical College to 1912, then the Royal College of Science and Technology) tended to acquire herbaria of academic botanists, the Museum has those of local societies and dedicated enthusiasts. Most of the departmental curators of the time were more geologically inclined, which caused a backlog to accumulate. Recently a programme of conservation, cataloguing and almagam- ation has been underway, with additional help provided through the Special Temporary Employment Programme (S.T.E.P.) scheme. The herbarium has been rehoused in new purpose-built storage cabinets, and is now reasonably accessible, though much work still remains to be done. All extra-European material is treated as low priority for the present. The only collections to be retained as entities will be Dr James Stirton’s mosses and lichens, which include type specimens. The Collectors As most of the collectors were of local importance, with literature on them correspondingly local, I include some biographical details. Dr Walter G. Blackie (1816-1906) was pre-eminent in the busi- ness life of Glasgow, being the founder of W. G. Blackie & Co. (Printers) which was an adjunct to his father’s firm of Blackie & Son (Publishers). He was also deeply interested in education and in char- itable societies. Little is known of his botanical activities. Most of his specimens are Scottish. Charles Eadie flourished in 1873. He was employed in the Office of Public Works of the Corporation. Rev. John Fleming (1785-1857) was a Presbyterian minister, sometime professor of Natural Philosophy, Aberdeen, and of Natural Science, New College, Edinburgh. He published a flora of West Loth- ian in 1814 and was also a notable mineralogist and palaeontologist — his mineral collection is also in the museum. Most of his plant speci- mens are from his parishes in Shetland, Fife and Clackmannan as well as from Edinburgh. His vascular plants include our earliest specimens, plus some collected by George Don Sn. (the Scottish alpine botanist), and a number acquired through the exchange activities of the Botan- ical Society of Edinburgh, many of which had been obtained from eminent botanists of the period, for example J. H. Balfour, J. T. Boswell-Syme, J. S. Henslow, W. J. Hooker, W. A. Leighton, W. W. Newbould, T. B. Salter, N. B. Ward and H. C. Watson. (Some of the material in this collection was added after Fleming’s death). 53 Fleming also included seaweeds, fungi, lichens and mosses in his collection, and these may provide some early Scottish records. Mrs Esther Hopkins (1815-1897) lived in Bath and died in Chester. She seems mainly to have worked on vascular plants although her specimens here represented are bryophytes. Her herbarium is rec- orded as having been in the possession of D. M. Atkinson, Royal Infirmary, Glasgow. George Horn (1828-1912) was born in Camlachie, Glasgow. He donated his herbarium to the museum in 1902. Apart from an appar- ently unsuccessful foray to Australia during the Gold Rush, Horn spent most of his life running a grocery business in Glasgow. His collection of mosses and vascular plants is fairly comprehensive and includes many local specimens; others have been obtained through Scottish contemporaries in the case of mosses, and on a national scale for flowering plants through the Botanical Society of Edinburgh ex- change activities. A fair number of specimens are from Norway, probably indicative of the then growing interest in plant habitat, com- paring Scottish mountain flora with that of the European arctic ( vide the activities of the Scottish Alpine Botany Club in the 1880s). Rev. Robert Kerr (1857-1939) was a minister with the United Free Church, and later the Church of Scotland. For some 47 years he was with Kirkmuirhill Church in the parish of Lesmahagow, Lanark- shire, and it is from this area that many of his specimens were col- lected. Most are vascular plants including some 70 European alpines, but mosses are also represented. Prof. Thomas King (1834-1896) was well-known as a botanist in Glasgow, where he spent most of his life, except from 1864-1873 when he went to Chile. In 1889 he was made Professor of Botany at the Anderson Medical College, and a year later, of the Veterinary College. He was active in most of the local naturalist societies. His particular interest was seaweeds. David Lands borough (1779-1854) was well-known as a pioneer of marine biology, working mostly along the Ayrshire coast. The mus- eum holds three copies of bound seaweed fasciculi entitled “Treasures of the Deep”, probably sold, as D. E. Allan suggested, to holiday- makers “ ... in aid of his Kirk and its schools”. There are also letters to Prof. J. Fleming from Landsborough. William A. Mudd (1830-1879) came from Yorkshire, where he was originally a gardener; he later became curator of the Botanic Gar- dens at Cambridge. He is known to have produced exsiccatae fasciculi of lichens, but it is uncertain whether the Glasgow collection is from one of these as there is no trace of bound volumes. 54 George W. Ord (1871-1899) worked at the Museum and later at the People’s Palace (branch museum). His main interest was geology. His plants are Scottish alpines. David Robertson (1806-1896) was a former herd-boy, who stud- ied at night-classes, and became the owner of a successful pottery shop in Glasgow. Partly through the interest of his second wife and through friendship with Roger Kennedy, author of “Clydesdale Flora”, he developed an interest in marine flora and fauna, and later geology. It was because of the ill-health of his wife that the Robertsons moved to Great Cumbrae, in the Firth of Clyde, and it was there that, due to his interest in marine life, the Marine Biological Station was eventually established just before his death. As shown in the appendix, his botan- ical interests covered most groups, the algae being especially well represented. Richard Spruce (1817-1893) was a Yorkshireman, who spent some years in South America. He also maintained a close contact with the Botanical Society of Edinburgh. The collection of South American mosses in the Museum was obtained via the Natural History Society of Glasgow. Dr James Stirton (1833-1917) was a gynaecologist holding a pro^ fessorship at the old Anderson College in Glasgow from 1889. His lichens and mosses are the most important in the collection. Dr Stir- ton’s spare time was devoted to botany and he collected extensively in the Scottish Highlands. He also corresponded at home and abroad with many leading authorities, and received specimens from them (e.g. Alexander McKinlay, W. P. Schimper and Sir George Watt). Both collections contain type specimens named by him, although few of his names stand today. The original lichen collection was divided between Glasgow and the British Museum (Natural History) by Annie L. Smith in the early part of this century. Stirton was active in many local societies, including the Philo- sophical Society of Glasgow and the Glasgow Society of Field Natur- alists, as well as the Botanical Society of Edinburgh and the Linnean Society (Fellow). Most of his numerous papers appear in the Transac- tions of these societies, as well as in the Scottish Naturalist, Annals of Scottish Natural History and Grevillea. Robert Turner (1848-1894) was Assistant Registrar of Shipping in Glasgow, and was president of the Andersonian Naturalists’ Society (1890-1892). His collection of vascular plants are all local. The Philosophical Society of Glasgow came into being in 1802, receiving its Royal Charter a century later. The herbarium was started in 1843, when the Glasgow Botanical Society amalgamated 55 with them. However, by 1882, there were only three members left in the Botanical Section, probably due to the new interest in anatomy and morphology, and it was agreed to donate the herbarium, which is comprised wholly of vascular plants, to the museum. Most specimens are either Scottish or from Continental Europe, though some from India and North America are included. The Natural History Society of Glasgow (1851-1930) had close associations with the Museum. In 1881 the Society made an agreement with the Town Council by which the Society provided a collection of British plants and invertebrates and the Museum pro- vided storage and materials for mounting the specimens. Accordingly in 1883 a small collection of flowering plants and a larger collection of mosses was presented to the museum, to be followed by some hepat- ics in 1884. The moss collection was “the nucleus of a complete one, as far as British species are concerned. Its value . . . depends mainly on the number of representative species it includes . . . Many of the specimens have been gathered by . . . men such as Dr Greville, Dr W. Wilson, Prof. Dickie and Prof. Schimper . . . 268 specimens alone have been gathered by McKinlay”. The Andersonian Naturalists’ Society (1885-1931) was the second of three societies which amalgamated in 1931, later to become the Andersonian Naturalists of Glasgow and now the Glasgow Natural History Society. In 1903 the Society presented to the Museum a collec- tion of vascular plants, all obtained locally. There are two collections whose donors remain unknown: 138 vascular plants from Kirkcudbright and Dumfries, collected 1859-1860; and 177 vascular plants with poetry(!) from localities near Glasgow and Aberystwyth, no date. There are four collectors about whom I have no information: J. Booth, Holstein mosses in exsiccata bound volume (1819); Dr J. Foulds, S. American mosses (1896); Mrs M. Gunn, Firth of Clyde sea- weeds (1945); G. Scott, Scottish flowering plants (1860). Any informa- tion about these would be welcome. References It would be cumbersome to include biographical references, but some more general ones on herbaria and natural history societies in Glasgow are given, plus some on the history of botany in Scotland . Crundwell, A. C. 1952. Bryological Collectipns in Britain: the Glasgow Museum. Trans. Br. bryol. Soc. 2: 122 Fletcher, H. R. 1959. Exploration of the Scottish Flora. Trans. Proc. bot. Soc. Edinb. 38: 30-47. Lee, J. R. 1952. The History of the Society (Andersonian Naturalists of Glas- gow). Glasg. Nat. 17/1: 4-7. 56 Lloyd, B. 1964. The herbarium of the Royal College of Science and Tech- nology, Glasgow. Glasg. Nat. 18/7: 363-368. Mackechnie, R. 1958. Plant recording in Clydesdale. Glasg. Nat . 18/1: 3-14. McNair, P. 1907. On the history and development of the natural history col- lections in the Glasgow Museums. Proc. R. phil. Soc. Glasg. 38: 81-96, Patton, D. 1952. Glasgow’s Natural History Societies. Glasg. Nat. 17/1: 8-10. Patton, D. 1954. The British Herbarium of the Botanical Department of Glasgow University. Glasg. Nat. 17/3: 105-125. Power, W. 1951. A Kelvingrove Jubilee, 1901-1951. Glasgow Art Gallery and Museums. A note on the Nat. Hist. Soc. Glasg. agreement with the Museum to form a herbarium. Trans, nat. Hist. Soc. Glasg. 1880-83: 272-273. Various notes and reports on excursions of the Scottish Alpine Botany Club in Trans. Proc. bot. Soc. Edinb. 1870-1892. 57 APPENDIX: Approximate size of Collections. CLASSIFICATION COLLECTOR BRITISH EUROPEAN OTHER ALGAE I D. Robertson Mrs M. Gunn Rev. J. Fleming Prof. T. King D. Landsborough Unknown c. 900 30 c. 200 186 3 fasciculi 9 1 FUNGI Rev. J. Fleming 60 Museum Staff 40 ( freeze- dried) LICHENS Rev. J. Fleming 150 W. A. Mudd 260 Dr J. Stirton 1000 1 AAA Museum Staff 200 1000 BRYOPHYTES J. Booth 200 Dr J. Foulds 60 Mrs E. Hopkins 220 G. Horn 700 Rev. R. Kerr 360 D. Robertson 425 R. Spruce 291 Dr J. Stirton 5500 2000 Nat. Hist. Soc. Glasg. 800 VASCULAR Dr W. G. Blackie 445 PLANTS C. Eadie 212 Rev. J. Fleming 2000 G. Horn 2500 Rev. R. Kerr 1800 70 G. W. Ord 28 D. Robertson 280 G. Scott 215 R. Turner 69 Unknown 315 And. Nats. Soc. 260 Nat. Hist. Soc. Glasg. 85 Phil. Soc. Glasg. 4000 500 Museum Staff 100 58 Book Review The Butterflies of Scotland : a Natural History GEORGE THOMPSON Croom Helm 1980 256pp. 37 plates, 8 in colour. £19.95 The Scottish butterfly enthusiast will find in this volume the first ever complete study of the Scottish butterflies. There is a wealth of inform- ation brought together after considerable research and with great scholar- ship. Much of the information was previously not readily available or occurred in tantalisingly brief references, for example in the much con- sulted 1901 B.A. Handbook. Most if not all Scottish butterfly records are included, even the most tenuous, while the substantial records are supported with discussion of status, history, habits, forms in Scotland and distribution, with up-to- date maps, all comprising the longest chapter - the Butterfly Fauna. Background material from geology, climatology and vegetational studies, contributes to an understanding of past and present distribution of the butterflies. Distribution is a major theme, with detailed analysis and comparison between different periods, recent changes and an opti- mistic look forward, together with the author’s original thesis that in Scotland human interference has had minimal effect, during the period of recording, on the distributional ebb and flow of the butterfly popul- ations. Tribute is given to the early students of Scottish butterflies in the form of readable and often amusing biographies. The colour plates include photographs taken in the field by the author and plates of pinned specimens illustrating historical specimens and a range of variation in the species; of both categories more would have been welcome. The use of monochrome plates was undoubtedly an economic expedient. Conservation is a topic which is discussed in some detail, the author stating his views in a thoughtful and balanced manner coming out in favour of controlled collecting. The conservation viewpoint which says “no collecting” is dismissed as a matter of ethics, which to the reviewer seems a pity as much conservation thinking these days is clearly informed by the ethical outlook. One error noticed by this reviewer is the statement that the Purple Hairstreak overwinters in the pupal stage when in fact this species overwinters in the egg stage. In summary, an admirable compilation which is required reading for the student of Scottish and, yes, British butterflies. Gerald Rodway The Endemic Whitebeams of North Arran ERIC BIGNAL Nature Conservancy Council, S.W. Region (Scotland). Received April 1980 In 1897 Landsborough* described the occurrence and distribution of two kinds of cut-leaved whitebeam growing in the stream gorges of the northern half of Arran and pointed out that they were not found in any other part of Great Britain. A few of the small trees were des- cribed as standing back some distance from the edges of bums but these were generally moribund and the majority of healthy specimens grew on rocky sites close to the water. For many years Sorhus pseudofennica and S. arranensis were not separated and there has been a certain amount of taxonomic confu- sion. The fourth edition of Bryce’s “Geology of Arran” (1872) lists Pyrus pinnatifida as occurring in Gleann Easan Biorach, while Lands- borough (1897) mentioned a number of stations in north Arran for Pyrus aria and its varieties. In 1901 Hedlund described Sorbus arran- ensis, but it was not until Clapham, Tutin and Warburg’s “Flora of the British Isles” was published in 1952 that its endemic congener Sorbus pseudofennica E.F. Warburg ( Sorbus fennica auct. angl.) rec- eived authoritative recognition as a distinct species. The earliest herbarium specimen of Sorbus pseudofennica was that collected by T.B. Bell in 1838, lodged in the herbarium at the Bot- anical Society of Edinburgh and subsequently passed to the British Museum. The locality given is “Glens in Arran” and the designation is “ Pyrus pinnatifida ”. There are 14 sheets of specimens of S. pseudofennica in the British Museum, all but Bell’s giving the locality as Glen Catacol and most designating the plant as P. pinnatifida or P. fennica. Five Rev. David Landsborough Jn., son of Rev. David Landsborough 1779-1854. See Glasg. Nat. 19: 443-462. — Editor. Glasg. Nat. 20 part 1 (1980) 60 specimens were collected in the 1870s and five in the 1920s. One sheet carries the paratype which was collected by Warburg in 1937. The oldest herbarium specimens of S. arranensis are those of Smith and Sowerby but the two peaks of collecting were 1870-1890 and 1920- 1940. The localities given are either Glen Catacol or Gleann Easan Biorach. The various designations given are Pyrus scandica, P. pin- naiifida and P. fennica. The only reference to these Sorbus occurring outside the Glen Catacol — Gleann Easan Biorach — Glen Diomhan area is by Landsborough (1875) who remarked that “It is true the ravine is beautiful (Glen Diomhan) and in it grows abundantly the white beam tree ( Pyrus arid), called by the nurserymen the French Rowan Tree, which in its wild state is very rare and, with the exception of a few specimens growing on the northern slopes of North Glen Sannox, is found nowhere else in Arran.” The fullest and most up-to-date account of the British Sorbus is given in Richards (1975). “Of the 20 British species of Sorbus recognis- ed by Warburg (1962), three (S. aucuparia, S. aria and S. torminalis ) are sexual diploids . . . The other species have not all been investigated cy- tologically but those which have are polyploids and at least partially apomictic; it is possible that this is true of all of them. In that case hy- brids are likely to arise at the present time only between sexual species or between a sexual and an apomictic species where the latter is the male parent. The 17 presumed polyploid apomicts fall into four groups: those similar to S. aria (8 species); those intermediate between S. aria and S. aucuparia (5 species in S. intermedia agg.); those intermediate between S. aria and S. torminalis (3 species in S. latifolia agg.); and S. pseudofennica which is intermediate between S. aucuparia and S. arranensis (in S. intermedia agg.) It is thus likely that many of the aga- mospecies recognised today are of hybrid origin, involving the three sexual diploids and their derivatives or ancestors”. The genomic formula for many of the species is at present only speculative. McAllister has established (pers. com.) that S. arranensis is a polyploid species with 2n=51. It is therefore presumed to be an apomictic triploid hybrid between Sorbus aucuparia (2n=34) and S. rupicola (2n=68). The Welsh S. minima (2n=51) appears to have the same origin, differing only in that a different clone of S. rupicola is presumably involved. There are a number of apomicts that may have arisen from the hybridisation of Sorbus aucuparia and S. rupicola. These include the British triploids S. minima , S. ley ana and S. arranen- sis. In addition S. intermedia and S. anglica may have derived from backcrosses to S. aucuparia. Three of these are very localised endemics, S. minima and S. ley ana being restricted to V.C. 42 (Brecon) and S. arranensis to V.C. 100 (Clyde Isles). S. anglica is an endemic more 61 widespread in Wales and SW England, and S. intermedia is an intro- duced plant found over much of Britain. There is no indication that the primary hybrid has ever been discovered in Britain or abroad, but these, together with the Scandinavian S. lancifolia , S. subpinnata and S. neglecta, probably represent the direct apomictic progeny of primary hybrids between tetraploid S. aria sensu lato (of which S. rupicola is the commonest) and diploid S. aucuparia. S. pseudofennica has 2n— 68 and, from its closer morphological resemblance to S. aucuparia (more pinnate leaves which are not dist- ant, shortly and broadly triangular in outline and thinly grey-green tomentose beneath), is presumed to be the result of fertilisation of a normal unreduced ovule of S. arranensis with n— 51 by a normal re- duced pollen grain of S. aucuparia with n— 17. Sorbus pseudofennica has, therefore, presumably the same origin as the Scandinavian S. hybrida, with half of its chromosome complement from S. aucuparia and half from S. rupicola. It is assumed from the present distribution of the endemics that at some stage in the post-glacial forest history of Arran they occurred throughout the forest and scrub on suitable sites. This woodland cover must have clothed much of North Arran to an altitude of over 1200 feet. Pollen diagrams have been produced for sites on the south of the island, at Monamore Glen and Machrie (S. Durno, pers. comm.), as well as from sites at Aros Moss, Kintyre and Racks Moss, Solway (Nichols, 1967), and from Bloak and Kennock Mosses, Ayrshire (Tur- ner, 1975). On the basis of the results from these sites, it is likely that prior to the activity of man the forest was composed mainly of birch, pine and rowan, with groves of oak and hazel along the coast. Their limited distribution today can be attributed to a fragment- ation of their original range by deforestation. The present deforested landscape is interpreted as being due fundamentally to long-standing and recently much intensified human interference, directly by clearance for agriculture, indirectly through grazing animals preventing regener- ation (Dickson, 1977). Moor fires still continue to drive woody plants further and further back into the dampest and rockiest sites, and grazing (sheep, deer, hares) suppresses natural regeneration and sapling growth. In addition, gales and snow remove large specimens (a poten- tial seed source) from their precarious positions in steep ravines and gorges. While there has been no comprehensive survey of the distribution of the Arran whitebeams, several workers have surveyed various glens at the north of Arran and there are a number of unpublished reports relating to these1. There is no recent published work on the distribution i NCC files 144, 144R, 144MP. 62 of the species and the original paper by Rev. D. Landsborough (1897) is still the standard published work. It would be misleading to suggest that the following list of sites is comprehensive, but it seems unlikely that many more locations occur, bearing in mind the interest that has been shown in them. Sorbus arranensis : Sorbus pseudofennica : Not differentiated : Abhainn Bheag (Uisge solus) Glen Diomhan (and tributary) Glen Catacol Allt nan Caiman Allt Dubh Gleann Easan Biorach Glen Iorsa (Allt-nan-Champ) Abhainn Bheag (Uisge solus) Glen Diomhan Glen Catacol Allt nan Caiman Creag na h-Iolaire No S. pseudofennica are recorded from Gleann Easan Biorach or its tributaries or the headwaters of the Iorsa Water. The only definite extinction is in north Glen Sannox where no trees occur today (cf. Landsborough 1875 quoted above). The abundance of Sorbus arranensis and S. pseudofennica at each station is more difficult to establish than the overall distribution. Again, various workers have made both qualitative and quantitative estimates of abundance, but there is no standardisation between esti- mates. Consequently, some estimates include “seedlings” as small as J" in height, whilst others record only “trees”. From the information available, an optimistic estimate of the total wild populations (exclud- ing seedlings) may be put at approximately 236 Sorbus pseudofennica and 283 Sorbus arranensis. Bearing in mind their scattered occur- rence and the uneven age structure of the population, the Arran white- beams were considered by McVean (1954) to be closer to extinction than any other tree or shrub in Scotland with the exception of Salix lanata. As a result of this precarious position, their Arran stronghold, Glen Diomhan, was declared a National Nature Reserve in 1956. Within the reserve a central area was deer-fenced in 1962 and the entire reserve (only 25 acres) has been free from muirburn for over 25 years. Approximately 141 S. arranensis and 145 S. pseudofennica occur on the reserve. Within the enclosure, 57 and 124 occur re- spectively, mainly on the west bank of the Diomhan Burn. The fen- ced area therefore encloses 63% of the whitebeams in the reserve, that is 41% of Sorbus arranensis and 86% of S. pseudofennica. 63 Management of the reserve in the past has been based on a “care and maintenance” policy with no active management other than the er- ection of the deer-fence and some trial (unsuccessful) planting of the endemics in the 1960s. More recently it has become evident that al- though natural regeneration of Birch (Betula pubescens var. odorata ) and Rowan ( Sorbus aucuparia) is taking place, the process is exceed- ingly slow. The antiquity of the mature specimens in the gorge, coupled with consistently poor seed production and winter storm damage, have resulted in renewed concern for the endemics and proposals for more active intervention within the enclosed section of the reserve to ensure their survival. Collection of the seed of the endemics and of Sorbus aucuparia and Betula pubescens has taken place over the past four years. In 1978, 13 of the endemic Sorbus, grown from seed collected from the reserve 2 years earlier, were planted in a sheltered section of the enclosure. Shelter planting of birch and willow (Argyll provenance) was also carried out in the immediate area. It is proposed, over the next 5 years, to carry out further experimental establishment, together with the reafforestation of the glen with scrub woodland of native species of local (North Arran) provenance. This active management policy will run concurrently with a det- ailed field monitoring programme, a full enumeration survey of all the localities for both endemics as well as controlled environment and cytological investigations. This latter aspect will form part of a programme to investigate the cytological and taxonomic status of all the British Sorbus endemics. The Arran whitebeams are unique amongst the endemic British Sorbus in that they do not occur on base-rich or limestone soils, and occur with only one of the parents, Sorbus aucuparia. Sorbus rupicola occurs at Holy Island (off Lamlash Bay, South Arran) but nowhere at the northern end of the island. The apparent absence of base enrichment may be explained in part by the occurrence of shear zones in the granite parent rock within Glen Diom- han (and possibly at other stations). Associated with these shear zones is the release of epidote, a rather unstable mineral of calcium, alum- inium and iron silicate which weathers rapidly to release its component elements. Epidotised zones are also often rich in calcite, crystallised lime which could be related to lime richness in a derived soil. It is clear, then, that epidotized zones will be far more calcareous than the surrounding granites and will undoubtedly give rise to soils with chemical characteristics similar to those derived from limestones. There appears also to be a correlation between the Sorbus and the occurrence of igneous dykes of olivine, dolerite and theolite. While the weathering of these rocks would not of themselves give rise to calcium- rich soils, they will provide more base-rich soils than the granites since these rocks are themselves much more basic, consisting primarily of 64 iron, magnesium, aluminium, calcium etc. silicates. Green staining of the rocks in Glen Diomhan is assumed to indicate fluid transfer along shear zones in the granite and along existing joints. Thus the epidote is likely to occur as a thin skin on the joint surface, with little or none occurring on the main body of the granite (K. Duff and A. McKirdy, pers. comm.). So far as the absence of Sorbus rupicola is concerned, no explana- tion can be offered. Many possibilities have been suggested — perhaps it never occurred and the hybrids originated elsewhere (now extinct) and established themselves in North Arran perhaps by bird-sown seed. Maybe S. rupicola occurred somewhere in the presumed centre of origin of the endemics (Gleann Easan Biorach — Glen Diomhan — Glen Catacol) and later became extinct — perhaps because of the ephemeral soil enrichment associated with epidotization. Work is currently being proposed to investigate the vegetation history of this area by pollen analysis and perhaps future results will shed more light on the prob- lem. References Bryce, J. 1872. Geology of Arran and other Clyde Islands. (4th Edition) Glasgow. Clapham, A. R., Tutin, T, G. and Warburg. E. F. 1952. Flora of the British Isles. Cambridge. Dickson, J. H. 1977. Western Scotland II, INQUA Congress Excursion Book- let C13. Hedlund, T. 1901. Monographic der gattung Sorbus. Svensk vet Akad. Handl. 35/1: 60-61. Landsboroughs, The, Father & Son 1875. Arran, its topography, natural his- tory and antiquities. Ardrossan. Landsborough, D. 1897. Pyrus aria and its varieties in Arran. Trans. Proc. bot. Soc. Edinb. 21 : 56-62. McVean, D. 1954. Notes on the present position of the endemic Arran Sorbus. Glen Diomhan Management Plan I. NCC 144/MP. Nichols, H. 1967. Vegetation change, shoreline displacement and the human factor in the late Quaternary history of S.W. Scotland. Trans. R. Soc . Edinb . 67/6: 145-187. Richards, A. J. 1975. Sorbus. pp. 233-238 in Hybridization and the Flora of the British Isles, edited by C. A. Stace. Academic Press, London Turner, J. 1975. The evidence of land-use by pre-historic farming communi- ties: the use of three-dimensional pollen diagrams., pp. 86-95 in The effect of Man on the Landscape: Highland zone, edited by J. G. Evans and S. Limbrey. Council for British Archaeology. Warburg, E. F. 1962. Sorbus in Clapham, A. R., Tutin T. G, and Warburg. E. F. Flora of the British Isles. Cambridge. Carex elongata in Scotland J. MITCHELL Nature Conservancy Council, S.W. Region (Scotland) A. McG. STIRLING 17 Austen Road, Glasgow Received September 1980 In the Scottish Naturalist for 1885 Arthur Bennett reported the first finding of Carex elongata L. in Scotland, commenting “this is an inter- esting addition to the Scotch [sic] flora, its most northern station hitherto known being in Cumberland”. This very local sedge had been discovered in July of the same year at Kenmure Holms, beside Loch Ken, Kirkcudbrightshire, by James McAndrew of New Galloway who sent specimens to Bennett. Whether McAndrew knew the identity of his find before communicating with Bennett is not clear. Apart from a Dumfries record, to which we refer later, the Loch Ken station re- mained the only confirmed locality for almost a century and, due to lack of recent records, was actually considered to have become extinct in Scotland (Jermy & Tutin 1968). However, since 1967 not only has the Loch Ken site been refound, but an additional five Scottish sites for C. elongata have been discovered, so that it now seems appropriate to review the present status of the sedge in Scotland. Kirkcudbright, v.c. 73 As already stated, C. elongata was first found in the vice-county at Kenmure Holms in 1885, and we have traced several herbarium sheets by various collectors from this locality bearing dates between 1885 and 1907. No evidence has been found to indicate that the sedge was seen at this station subsequent to the latter date for almost seventy years. Milne-Redhead (1972) apparently had not seen the species in the vice-county as he lists the record among those requiring confirma- tion. This was forthcoming in 1976 when one of the authors (J.M.) Glasg. Nat. 20 part 1 (1980) 66 discovered a small colony, probably less than a dozen plants, in swam- py wooded ground close to Kenmure Castle, near the northern end of Loch Ken. This is almost certainly the site of Me Andrew’s original discovery. In June of the following year Dr D. A. Ratcliffe of the Nature Conservancy Council, while examining sites alongside the River Cree, north of Newton Stewart, on the western border of the county, found another colony of about thirty plants in willow-alder carr. Later in the same month A.McG.S., following up this report, found an additional single tussock of C. elongata in similar ground a little further north near the Dow Lochs. Dumfries, v.c. 72 In G. F. Scott Elliot’s Flora of Dumfriesshire (1896) a record of Carex elongata from Auchenhessnane, Penpont, is attributed to T. Brown. The date given is 1893. Recent repeated searches in the vicin- ity of Auchenhessnane in an attempt to refind the sedge have proved unsuccessful, but the possibility of its occurrence there cannot be discounted as there is moderately suitable ground in the general area. There is, however, some doubt as to whether C. elongata was actually found in the locality named, for at the time Auchenhessnane was the home of Brown, and may have been quoted in the Flora for this reason. Two herbarium specimens have been traced to date which seem to support the occurrence of C. elongata in Dumfriesshire, but unfortun- ately neither is precisely localised. The first, in the British Museum collection, is from Bennett’s herbarium and is labelled “Dumfriesshire, per T. Brown Esq.”. It is undated. The other specimen is in the col- lection at Dumfries Museum and is from the herbarium of J. Fingland of Thornhill. It bears no collector’s name, locality or date. The only other piece of documentary evidence concerning the Dumfries record is contained among the Scott Elliot papers in the Ewart Library, Dum- fries. This is an undated manuscript list of plants from v.c.’s 72, 73 and 74 sent by Scott Elliot to Bennett for naming, and C. elongata is included. Bennett adds a few words of congratulation on the finding of a new species for v.c. 72 and the comment that the only other Scottish locality was at Loch Ken. It is worth noting that Milne-Red- head (1972) chose not to include this species as a Dumfries plant although he must have been aware of the published record attributed to Brown, if not of the herbarium specimens. Dunbarton, v.c. 99 Carex elongata was first found on Loch Lomond-side by J. H. Penson in June 1967 and notice of this discovery has been given by Ribbons (1973). This site, below Boturich Castle on the south-east shore of the loch about two miles north of Balloch, is in wet alder 67 woodland, and the colony probably consists of between sixty and one hundred plants. In June 1975 a second population of the sedge was discovered by J. M. and Dr R. Mitchell beside the west shore of Loch Lomond within the policies of Rossdhu House, just south of Luss. This is a substantial colony of at least two hundred plants, growing in and around muddy lagoons under the shade of willows, alders and former coppiced oak. Stirling, v.c. 86 Continued search of suitable sites around Loch Lomond was re- warded in May 1977 by the discovery of a further population of C. elongata numbering about one hundred and fifty plants located beside the Mar Burn, near the mouth of the River Endrick on the east side of the loch. The site, which was also found by J. M., lies within the Loch Lomond National Nature Reserve and is particularly inter- esting as the Carex grows in swampy ground under the hybrid willow Salix X smithiana which in the past had been planted and cultivated for commercial purposes. This activity has long since ceased and the underlying vegetation, which was probably never unduly affected by the willow management, differs little in character from that of the other Scottish sites. In May 1979 a second colony of C. elongata was located by A. McG. S. in Gartfairn Wood about three-quarters of a mile north of the Mar Burn site. This is a much smaller colony of about thirty plants, growing in a wet depression among Salix cinerea and also sit- uated within the Loch Lomond National Nature Reserve. General Observations Tlie very local distribution of Carex elongata in the British Isles is almost certainly due to its quite stringent habitat requirements (David 1978). The favoured situations are those where the water table is perm- anently high, the sites usually being submerged for prolonged periods in winter and drying out only partially in summer. Two of the Loch Lomond colonies (sites 3 and 4) lie within fifty metres of the shore among Salix cinerea subsp. oleifolia and Alnus glutmosa. The sedge frequently forms its characteristic tussocks in a semi-epiphytic fashion on fallen trunks or emergent bases of these species. These lake-shore sites lie within the influence of the wide annual fluctuation of water level to which Loch Lomond is subject, and this condition is largely responsible for the reduced competition from other plant species which seems to be another requirement of the sedge. The Kenmure Holms and Mar Burn sites are best described as “hinterland” sites, subject to immersion almost annually due to high loch levels causing the river, feeder streams and ditches to “back up” and flood the surrounding land. 68 The Dow Lochs site is very similar to that at Kenmure Holms except that the adjacent fresh water system is a slow-flowing river, seasonally flooding out over low-lying ground with extensive development of sedge- swamp communities and in places assuming almost lake-like proportions- It is interesting to speculate on the reasons why this sedge should for so long have escaped notice in its Scottish localities. In the case of the Loch Lomond sites we believe the answer lies in their situation within the policies of large private estates. Until comparatively recently public access to these areas would have been difficult due to their exclusive nature. An additional contributory factor may be the relative remoteness of all the Loch Lomond sites from a public road. In the case of the two small populations in Kirkcudbrightshire their apparent confinement to extremely restricted areas is probably the reason for their having escaped notice. Carex elongata may well occur in other suitable localities in Scot- land and it should be looked for early in the season in the type of habi- tat described. It is a medium-sized sedge of tufted habit and older plants tend to form firm tussocks or “stools” rather like C. paniculata but on a much reduced scale. The foliage is a distinctive yellow-green colour which affords a useful identification character, particularly in early spring before the inflorescence develops. The latter appears towards the end of April, and by the end of June most of the spikes have shed their utricles. There is evidence that regeneration from seed is satis- factory in at least two of the Scottish populations, and there appear to be no obvious threats to the continued survival of any of the colonies described, a situation which contrasts very favourably with that in England where, due to losses of suitable habitat, the sedge is either ex- tinct or greatly reduced in numbers in many of its former stations (David 1978). The situation in the north of Ireland has recently been shown to be more satisfactory than had previously been supposed, and a number of sites are now known around Lough Neagh and Lough Erne, but the colonies are not large in terms of numbers of plants (Harron 1974; Faris 1974). It is evident from the foregoing that the status of Carex elongata in Scotland gives cause for considerable satisfaction. It can be confi- dently stated that the best of the Scottish colonies — those in the Loch Lomond area — rank among the finest in the British Isles. The only comparable populations, according to David (1978), are two in Staff- ordshire and one in Yorkshire. Vascular species most frequently associated with Carex elongata in the six known Scottish sites 1. Kenmure Holms, Loch Ken, v.c. 73 NX 635766 2. Dow Lochs, River Cree, Newton Stewart, v.c. 73 NX 374719 69 3. Boturich Castle policies. Loch Lomond, v.c. 99 NS 383845 4. Rossdhu House policies, Luss, Loch Lomond, v.c. 99 NS 359877 5. Mar Burn, River Endrick, Loch Lomond, v.c. 86 NS 437888 6. Gartfairn Wood, Balmaha, Loch Lomond, v.c. 86 NS 434898 1 2 3 4 5 6 Alnus glutinosa 4- 4- + Anemone nemorosa 4- 4- + Athyrium filix-femina + 4- 4- Caltha palustris 4- + + + Cardamine amara + + + + Carex remota + + + + Carex vesicaria + + + + Crepis paludosa + + + Deschampsia cespitosa 4- 4- + + + + Filipendula ulmaria + 4- + + + + Galium palustre + + + + + + Iris pseudacorus + + + 4- Lysimachia nummularia 4- + + Phalaris arundinacea + + + + + 4- Rumex aquaticus + + 4- Rumex sanguineus + + + Salix cinerea subsp. oleifolia + + + + 4- V aleriana officinal is + + + + 4- Acknowledgments We are indebted to the following for kind assistance in various ways during the preparation of this account: Dr E. M. Bignal, R. W. David, P. Harrold, Miss J. Martin, J. S. and Mrs M. Martin, R. D. Meikle and Dr D. A. Ratcliffe. References Bennett, A. 1885. New Scottish Flowering Plants. Scott. Nat. 2 (New Series), 181. Bennett, A. 1885. Carex elongata in Scotland. J. Bot . Land. 23, 253. Bennett, A. 1886 Carex elongata at Kenmure Holms. Trans. Proc. Bot. Soc. Edinb. 16, 316. David, R. W. 1978. The Distribution of Carex elongata in the British Isles. Watsonia 12, 158-160. Faris, R. C. 1974. Carex elongata in Counties Leitrim and Cavan. Ir. Nat. J. 18, 92-93. Harron, J. 1974. Carex elongata refound on Loch Neagh shores. Ir. Nat. J. 18, 91-92. 70 Jermy, A. C. & Tutin, T. G. 1968. British Sedges. London. Milne- Redhead, H. 1972. A Check List of the Flowering Plants, Ferns and Fern Allies of the Vice-Counties of Dumfries, Kirkcudbright and Wigtown. Penson, J. H. 1967. Unpublished personal field notes. Trans. J. Proc. Dumfries. Galloway nat. Hist. Antiq. Soc, 3rd Ser, 49, 1-19. Ribbons, B. W. 1973. Carex elongata on Loch Lomond-side. Glasg. Nat. 19, 68-69 Scott Elliot, G. F. 1896. The Flora of Dumfriesshire, including part of the Stewartry of Kirkcudbright. Dumfries. Veronica peregrina in the West of Scotland PETER MACPHERSON 15 Lubnaig Road, Glasgow Received March 1980 Veronica peregrina, American Speedwell, is well established in North- West Ireland, whereas most of the records from other parts of the British Isles are of casual occurrences. Perring and Walters (1962) re- corded it in only one 10 km square in the West of Scotland and that was almost on the Lanark (77)— Peebles (78) boundary. It related to a 1932 record from Biggar. Bangerter (1966) stated that it had been re- corded from 45 British vice-counties including a record each from Ayr (75) and Dunbarton (99) and two from Lanark (77). In addition, Dick- son (1974) reported that it had evidently persisted in Kiloran Garden, Colonsay (102), since recorded there in 1910. Seven plants of V. peregrina appeared in my Newlands (Glasgow) garden, Renfrew (76) in 1972 but did not persist; however Silverside (1976) has found it to be persistent in the Finlaystone Estate, in an- other part of the same vice-county. The Speedwell was recorded twice in 1978 during excursions of the Glasgow Natural History Society (at that time the Andersonian Naturalists of Glasgow). On 26 May plants were seen in the walled garden of Ross Priory, Dunbarton (99) and on 31 May it was noted in and around the walled garden of Rouken Glen Park, Renfrew (76). In 1979 it was seen in a nursery at Barcaldine, Argyll (98) (Con- acher, pers. comm.). Veronica is the name of a saint, but why given to this genus is un- known (Johns 1894). Peregrinus is Latin for stranger or immigrant, the plant being a native of North America, but naturalised in Europe and described by Linnaeus as “ Habitat in Europae hortis.” Veronica peregrina has tiny pale flowers and even the plant as a whole is rather inconspicuous. It is not illustrated in either Butcher (1961) or Ross -Craig (1966) so it is thought appropriate to include a detailed drawing to help with the identification as the species is obvi- ously becoming more widespread. Glasg . Nat. 20 part 1 (1980) 72 Acknowledgment I am grateful to Elspeth L. S. Macpherson for the illustration, drawn from a Newlands plant. 73 References Bangerter, E. B. 1966. Further notes on Veronica peregrina L. Proc. bot. Soc. Br . Isl. 6: 215-220. Butcher, R. W. 1961. A New Illustrated British Flora. Leonard Hill. London. Dickson, J. H. 1974. Colonsay. Glasg. Nat. 19: 140. Perring, F. H. and Walters, S. M. 1962. Atlas of the British Flora. Thomas Nelson & Sons, London and Edinburgh. Ross-Craig, S. 1966. Drawings of British Plants. XX 11 ( Scrophulariaceae ). G. Bell & Sons, London. Silverside, A. J. 1976. Veronica peregrina. Glasg. Nat. 19: 341-342. 74 Junior Excursion Meeting to the Clyde at Cambuslang ELSPETH L. S. MACPHERSON The first Junior Field Meeting of the Glasgow Natural History Society to be held for many years took place on the evening of 19 June 1980. Nine secondary school ipupils were transported to Cambuslang in a school mini-bus and together with the leaders set off down to the Clyde. Along the third of a mile stretch surveyed, habitats included road verge, hedgerow and wasteground as well as the river bank. All the pupils were studying biology at school, and some, photo- graphy. A list was compiled of all the plants found that evening and the pupils showed a keen interest in searching around for additions. They were eager to learn about those seen and we tried to teach them genus characteristics so that they could “family” any new find. We also endeavoured to explain the derivations of some of the English names of the plants being found to make them more mem- orable. For example those related to description of leaf — Milfoil (thousand leaf), Colt’s-foot; description of fruit — Crane’s-bill; descrip- tion of flower — Daisy (day’s eye) and Policeman’s Helmet; description of former use — Broom and Woundwort; other peculiarity — Jack-go-to bed-at-noon. To the surprise of the pupils, there were in this small area at least 121 different flowering plants. These included 12 species of grass, three of sedge and one of rush but no ferns. 22 of the plants were new rec- ords for the 10 km square (22/66), not having been included in the master card for that square held at the Biological Records Centre, Monks Wood. In addition to these records, we were all very interested to see a young plant of Teasel. This biennial is not recorded on any of the master cards for Lanarkshire. The evening was considerably enjoyed by all and, thus encour- aged, we intend to hold a further Junior Meeting next year. 75 Clyde Dock Aliens PETER MACPHERSON and ALLAN McG. STIRLING An alien hunt was held in the Meadowside dock area in September, 1979. Grain, mainly from North America, is unloaded from the ships at that site. First of all the north side of Castlebank Street was inspected and among the cobble stones were found American Pepperwort ( Lepidium densiflorum ), Grey Goosefoot ( Chenopodium opulifolium ), Rye Brome Grass ( Bromus secalinus) an alien Bent Grass ( Agrostis scabra ) and Green Bristlegrass {Set aria viridis). The party then went into the actual dock area and saw Turnip {Brassica rapa). Green Amaranth {Amaranthus hybridus ), Slender Fox- tail {Alopecurus myosuroides) and an alien Meadow Grass ( Boa sp.). A specimen of the latter was sent to the late Dr C. E. Hubbard and to Kew Gardens. The species has not yet been determined but it is thought that the plant has come from the southern hemisphere. When the Meadowside Dock security officer heard that we were looking for plants growing from imported seed he suggested that, in view of the prevailing wind, we should try the docks further up the Clyde. A visit to the more easterly, partly infilled. Queens Dock was made in August 1980. One might expect such plants as noted above to be purely casual in occurrence but at this site there was an abun- dance of the Bent Grass {Agrostis scabra) and of Flattened Meadow Grass {Poa compressa ) with a few plants of Tall Rocket {Sisymbrium altissimum) all of which had previously been seen on a visit to the docks in 1973. In addition there were many plants of the American Pepperwort, a further plant of Grey Goosefoot, one of Eastern Rocket {Sisymbrium orientate ) and a number of plants of Poa palustris. The usual habitat in Britain of the above plants and the continent of origin is given in the Table. We are grateful to Professor J. P. M. Brenan, Mr E. J. Clement, and the late Dr C. E. Hubbard for help with identification. 76 TABLE: The usual Habitat in British Isles, and Continent of Origin of the plants reported in the text. Agrostis scabra Alopecurus myosuroides Amaranthus hybridus Brass ica rap a Bromus secalinus Chenopodium opulifolium Lepidium densiflorum Boa compressa Boa pal ust ris Boa sp.? Setaria viridis Sisymbrium altissimum Sisymbrium orientale Habitat in British Isles Few previous reports Arable and waste ground Waste ground Arable and waste ground Arable ground (usually in winter wheat) Waste ground, especially S. England Docks Dry banks, walls and waste ground Marshy and waste ground Possibly new to Br. Isles Waste ground and docks Waste ground Waste ground, especially S. England Continent of Origin North America Native in British Isles (casual in Scotland) North America N. Africa, W. Asia, China Europe N. Africa, Asia, Europe Africa, Central Asia, S. Europe North America Native in British Isles (rare in Scotland) North America, Asia, Europe ? Southern Hemisphere Africa, Asia, Europe W. Asia, E. Europe N. Africa, W. Asia, S. and S.E. Europe The Flora of the Loch Lomond National Nature Reserve : A Supplement J. MITCHELL Nature Conservancy Council, S.W. Region (Scotland) A. McG. STIRLING 17 Austen Road, Glasgow Received April 1980 The following supplement to the published account of the Flora of the Loch Lomond National Nature Reserve (Idle 1978) brings up to date the Reserve’s list of flowering plants, ferns and allies to December 1979. In addition to previously unrecorded species, the supplement incorporates recently named segregates, together with a small number of hybrids which are included in the list for the first time. Localities are named for all records, but remarks on status and habitat already given in the main paper are not repeated for additional segregate species. Over half of the new records originate from a 404 acre (163.5 ha) extension added to the Mainland portion of the Reserve in June 1977. This extension, lying to the north of the River Endrick, falls within Stirlingshire (V.C. 86), unlike the southern part of the Mainland Re- serve which is situated in Dunbartonshire (V.C. 99). For botanical recording purposes, therefore, it is convenient to treat these two por- tions separately, and they are referred to in this paper as Mainland (N) and Mainland (S) respectively. The three major habitats represented on the Mainland Reserve extension are wet deciduous woodland, rough grazings interspersed with overgrown drainage ditches, and a period- ically inundated loch shore zone with both exposed and sheltered lagoons. The extension adds three national rarities to the Reserve’s flora — Leucojum aestivum, Juncus filiformis and Carex elongata — together with several other species of local distribution in Scotland. With a few exceptions the order and nomenclature followed is accord- ing to Dandy (1958 & 1969) and Stace (1975). Glasg. Nat. 20 part 1 (1980) 78 Equisetum palustre. One recorded station. Loch shore. Mainland (N). Equisetum sylvaticum. One recorded station. Wet wood. Mainland (N). Dryopteris X deweveri (D. dilatata X carthusiana ). One recorded sta- tion. Wet heath. Mainland (S). Poly podium vulgare agg. The following taxon has been named: Poly- podium interjectum. Creinch. Ranunculus trichophyllus. Locally frequent. Shallow water. Mainland (N) and (S). Ranunculus peltatus. Local. Shallow water. Mainland (N). Erophila verna. One recorded station. Erratic serpentine boulder. Mainland (N). Rubus fruticosus agg. [Rubus rosaceus] delete. The following additional taxa have been named: Rubus plicatus. Mainland (S). Rubus latifolius. Mainland (S). Rubus nemoralis. Mainland (N) and (S). Rubus leptothyrsos. Mainland (S). Rubus errabundus. Mainland (N) and (S). Rubus scoticus. Mainland (S). Rubus infest us. Mainland (S). Alchemilla vulgaris agg. The following taxon has been named: Alchemilla glabra. Main- land (N) and (S). Aphanes arvensis agg. The following taxon has been named: Aphanes microcarpa. Mainland (N). Rosa canina agg. The following taxa have been named: Rosa canina. Mainland (N) and (S). Rosa dumetorum. Mainland (N). Rosa afzeliana. Mainland (N). Rosa sherardii. Mainland (N). Rosa mollis. Mainland (N). Epilobium hirsutum. One colony. Riverbank, Mainland (S). Callitriche obtusangula. One recorded station. Side of former course of the Mar Burn, Mainland (N). Callitriche hamulata. Locally abundant. Lagoons, Mainland (N) and (S). Callitriche hermaphraditica . Local. Deep drainge ditches, Mainland (N). Anthriscus sylvestris. Uncommon. Track and hedge side. Mainland (N) and (S). 79 Polygonum aviculare agg. The following additional taxon has been named: Polygonum aviculare. Mainland (N). Polygonum minus. Twio colonies. Exposed mud in Crom Mhin Bay, Mainland (N). First recorded in this general locality in 1893 (Anon. 1897). Polygonum cuspidatum. One small colony. Streamside, Mainland (N). Rumex X platyphyllos ( R . aquaticus X obtusifolius). Local, River and drainage ditch sides. Mainland (N) and (S). First recorded in this general locality in 1939 (Lousley 1941). Rumex longifolius. No recent records, but previously reported on or near Mainland (N) in 1939 (Lousley 1941) and 1950 (Prasher 1950). Salix X smithiana (S. cinerea X viminalis). One large colony. Former commercial willow plantation. Mainland (N). Salix X multinervis ( S . aurita X cinerea ). One recorded station. Open willow carr. Mainland (N). [Limosella aquatica ]. Delete. Veronica arvensis. One recorded station. Erratic serpentine boulder. Mainland (N). Mentha arvensis. One recorded station. Wet grassland. Mainland (S). Mentha X verticillata (M. aquatica X arvensis). One recorded station. Overgrown drainage ditch. Mainland (N). Senecio X ostenfeldii ( S . aquaticus X jacobea). Uncommon. Wet grass- land, Mainland (N) and (S). Hieracium sparsifolium. One recorded station. Rocks by shoreline, Torrinch. Taraxacum officinale agg. The following taxa have been named : Taraxacum unguilobum. Torrinch. Creinch, Mainland (N). Taraxacum fulvicarpum. Mainland (N). Taraxacum landmarkii. Mainland (N). Taraxacum eximium. Mainland (S). Taraxacum maculosum (maculigerum). Creinch. Taraxacum praestans. Torrinch, Creinch. Taraxacum ostenfeldii. Creinch. Potamogeton X salicifolius (P. lucens X perfoliatus). Has been re- ported in Mainland (N) as P. decipiens (Stirling & Kidston 1891), but there are no recent records. The record should be treated with some caution as P. lucens is not known to occur in the vicinity. Potamogeton X nitens (P. gramineus X perfoliatus). Uncommon, poss- ibly washed in from elsewhere on the loch. Lagoons, Mainland (N) and (S). Potamogeton berchtoldii. Local. Lagoons, Mainland (N) and (S). 80 J uncus filiformis. Two small colonies. Shore grassland. Mainland (N). First recorded in this locality in 1947 (Lee 1953). Leucojum aestivum. One strong colony, with scattered individual plants nearby (Stirling & Mitchell 1978). Wet woodland. Mainland (N). Epipactis heleborine. Only one plant seen. Damp \Moodland, Mainland (N). First recorded in this general locality in 1890 (Stirling & Kid- son 1891). Dactylorhiza X transiens (D. fuchsii X maculata subsp. ericetorum). Occasional. Wet heath and grassland. Mainland (S). Dactylorhiza purpurella. Uncommon. Wet grassland. Mainland (N) and (S). Scirpus, lacustris. Two colonies. Sheltered lagoon. Mainland (N). Carex demissa X hostiana. One recorded station. Wet heath. Main- land (N). Carex X hibernica (C. aquatilis X nigra). One recorded station. For- mer arable field, now permanently flooded. Mainland (S). Carex elongata. Two colonies (Stirling & Mitchell 1980). Periodically flooded woodland. Mainland (N). Festuca pratensis. Local. Wet grassland. Mainland (S). Poa pratensis agg. The following taxon has been named: Poa subcaerulea. Mainland (N) and (S). Pda trivialis. Local. Wet rough grassland. Mainland (N). [Bromus erectus]. Delete. Bromus ramosus. Uncommon. Confined to serpentine exposures, Inch- cailloch. Acknowledgments In the preparation of this supplement to the Flora of the Loch Lomond National Nature Reserve we are indebted to J. M. Cameron (Reserve Warden), E. T. Idle, Dr A. J. Silverside and the late R. Mac- kechnie for a number of additional new records. Our thanks also to R. D. Meikle, Dr A. J. Richards, R. W. David and the Rev. G. G. Graham for their assistance with the identification of Salix, Taraxacum , Carex and Rosa spp. respectively. References Anon. 1897. Reports on excursions — Balmaha, 8th July 1893. Trans, nat. Hist. Soc. Glasg. 4 (NS): 116. Dandy, J. E. 1958. List of British Vascular Plants. London. Dandy, J. E. 1969. Nomenclature changes in the List of British Vascular Plants. Watsonia 7: 157-178. Idle, E. T. 1978. The Flora of the Loch Lomond National Nature Reserve. Glasg. Nat. 19: 403-421 81 Lee, J. R, 1953. Additions to the Flora of the Clyde Area. Glasg. Nat. 17: 65-82. Lousley, J. E. 1941. Notes on the British Rumices II. Rep. both Soc. Exch. Club Br. I si. (Report for 1940) 12: 547-585. Prasher, R. 1950. Botanical Section Report for 1950. Glasg. Nat. 16: 99. Stace, C. A. (Edit.) 1975. Hybridisation and the Flora of the British Isles. London. Stirling, A. McG. and Mitchell, J. 1978. Summer Snowflake. Glasg. Nat. 19: 429-430. Stirling, A. McG. and Mitchell, J. 1980. Care: c elongata L. in Scotland. Glasg. Nat. 20: 65-70. Stirling, J. S. and Kidston, R. 1891. Notes on the Flora of the North- western portion of Stirlingshire. Trans. Stirling nat. Hist, archaeol. Soc. 13: 88-102. 82 Acknowledgments The Glasgow Natural History Society is indebted to the City of Glasgow District Council and the University of Glasgow for generous grants towards the cost of publishing this part of the Glasgow Naturalist . 83 Short Notes COMPILED BY A. McG. STIRLING Invertebrates Orange-tip Butterfly E. A. CROWSON and R. H. DOBSON Lanark (77): Members of the Zoological Section attending the excur- sion to the Cart and Kittoch SSSI, which lies on the south-east boun- dary of the City of Glasgow, close to the Linn Park, were about to leave the area when a distinctively marked male of the Orange-tip Butterfly ( Anthocaris cardamines ) was observed on the wing. The damp clearing by the side of the Kittoch near its junction with the Cart has the food-plant of the Orange-tip, the common Lady’s Smock (Car da- mine pratensis ), as a member of the ground flora and appears to be a typical breeding ground for the butterfly. The male was observed on 1 June 1980 and it was not possible to discover any caterpillars on that occasion. A search of the area should be made to establish whether the species is breeding there. Pre-1901 records for the Orange-tip were published in the “Fauna, Flora and Geology of the Clyde Area” published by the Local Com- mittee for the Meeting of the British Association in Glasgow in 1901. Even at that time it was said that there were no recent records from the Clyde Area and there have been no subsequent published records. The Biological Records Centre of the Institute of Terrestrial Ecology has received a record from C. I. Rutherford of Cheshire of “males seen while driving on M73 on the eastern outskirts of Glasgow” on 24 May 1978. B. Forrester of Prestwick has also notified the Biologi- cal Records Centre of a record of the Orange-tip from Dalmellington in 1978. Outside the Clyde Area R. A. and E. A. Crowson have recorded the Orange-tip from Glentanner in Aberdeenshire and Gledswood in Berwickshire and have received reports of it occurring in a damp meadow by the River Jed in Roxburghshire. It seems that the species may be recolonising areas from which it has been absent for many years. A close watch should be kept to determine whether it has suc- cessfully established itself as a breeding member of the fauna. The female is relatively obscure and can easily be mistaken for another 84 species of white butterfly but the characteristic orange wing-tips of the male are unmistakable. Scottish Records of Glow-worm A. McG. STIRLING At approximately 11.30 p.m. on 12 June 1980, Mr J. P. Waltho, Hel- ensburgh, observed a single female Glow-worm ( Lampyris noctiluca ) on a stalk of dead bracken adjacent to the south-west shore of Inch- moan Island, Loch Lomond. The greenish glow from the abdominal segments could be seen from a distance of about twenty yards in almost total darkness. This observation prompted enquiry from personal con- tacts and in the literature regarding other Scottish records of Lampyris, from which it appears that this member of the Coleoptera is generally distributed in the southern half of Scotland — certainly as far north as mid-Perthshire. The following records have come to our notice in the course of fairly limited enquiries: Wigtown, v.c. 74 Portpatrick; Ayr, v.c. 75 Girvan, Barr; Renfrew, v.c. 76 Lochwinnoch, Kilmacolm; Selkirk, v.c. 79 Tushielaw; Stirling, v.c. 86 Balmaha; West Perth, v.c. 87 Aber- foyle. Pass of Leny; Mid Perth, v.c. 88 Crieff; Argyll, v.c. 98 Oban; Dunbarton, v.c. 99 Luss, Rosneath; Clyde Isles, v.c. 100 Millport. I am indebted to Dr R. A. Crowson, Mr J. Mitchell and Mr N. Tait for assistance in the compilation of this note. Reptiles Can Common Lizards Jump? WILLIAM K. STOVE I have known for many years that Wall Lizards are very active and can jump, but it never occurred to me that the British Common Lizard was capable of remarkable jumping feats. Let me recount to you an experience I had some years ago. I had just caught two Common Lizards, one male and one female, in the Callander area and had managed to tame them by means of a secret process of my own. I was sitting on the shore of a loch on a large stone with the male on my left thigh and the female on my right thigh, basking in the sun. All of a sudden the male leapt 9 to 12 inches on to my right thigh, landed on top of the female and proceeded to mate with her vigorously. To save the female from damage I was forced to separate them and put them in different containers. To render this story more credible let me tell you of two experi- ences I had with ordinary Wall Lizards. I was watching a Wall Lizard in one of my cases when all of a sudden it leapt vertically into the air, turned over in mid-flight and landed upside-down on a piece of perforated zinc which I used as a 85 ventilator. It was obviously not the first time it had done so, but I had not been present at the right times to observe it. The other story refers to an incident in a pet shop where I was examining a large male Wall Lizard before buying it. I had it in my left hand with my thumb on its back. The moment I released my thumb to study its coloration it leapt into the air and described a beautiful six foot parabola. Purely by reflex action I leaned forward and caught it six inches from the floor. The shop owner was amazed, and so was I, for it had been purely a reflex action on my part resulting from years of experience with lizards of all types. Birds Late departure of Swallows from Dairy, Ayrshire R. PR ASHER Ayr (75) : At the beginning of October 1979 a friend drew my attention to the fact that a brood of three young swallows, along with their par- ents, were still on the wing about our housing scheme in Dairy, Ayr- shire. I presumed that they had nested at the nearby farm. Usually about mid-day (or the warmest part of the day) they appeared above the houses, flying around, hawking for insects. Occasionally they alighted on an electric cable, and this gave me a chance to observe them more closely. The three young ones seemed quite strong and healthy although they were such a late brood. On 16 October the ground was white with frost and I saw no sign of the birds. I thought that they had departed. However, at noon my friend told me that they were still with us, but flying around the outbuildings of the farm. Evidently it was warmer there, and we did not see them again above the houses. On 17 and 18 October the wind changed to the east and they were still at the farm. Alas! on 19 October the swallows had disappeared and we did not see them again. Evidence of probable breeding of Storm Petrels on Ailsa Craig B. ZONFRILLO Ayr (75) : Storm Petrels {Hydrobates pelagicus) formerly bred on Ailsa Craig at least until the middle of the last century. Eggs of this species taken on the Craig were, until some years ago, displayed in the little museum in Girvan. Although birds were occasionally sighted during crossings, there has been no recent evidence to suggest that Storm Petrels still showed any interest in Ailsa Craig as a breeding site. In summer 1979 it was established, using mist nets and tape re- cordings of Storm Petrel calls, that birds frequented the island in good numbers. During a short stay in summer 1980 T. P. Daniels and I, assisted by A. Beck, M. Bradley and Assistant Lightkeeper M. Kelly, made some significant catches of Storm Petrels using the tape lures. 86 Birds were netted, ringed and released during the short hours of dark- ness. No Storm Petrels were seen on land or sea during daylight. The following individuals were handled on more than one night: Ring No. Date ringed Date retrapped 2218571 29 June 1980 30 June 1980 2 July 1980 2218577 29 June 1980 2 July 1980 2224687 27 July 1979* 29 June 1980 30 June 1980 * Ringed Sanda Island, Kintyre In addition to the above, two Storm Petrels were netted without recordings playing and other birds were observed over the boulder beach after dark, prior to the recordings being switched on. Former nest sites on Ailsa Craig were described as being under the large and immovable rocks around the base of the cliffs. Rats abound all over the Craig and would surely predate the eggs or young of such a small bird as the Storm Petrel. While catching birds I often observed Storm Petrels flying in to- wards the nets at height, or coming round the south cliffs again at height. It is my conjecture that, if Storm Petrels are breeding, the nest sites are high amongst the shattered granite. The area above the South Fog Horn seems suitable as it appears to be gull-free and perhaps also inaccess- ible to rats. This area is near to where all the Storm Petrels have been caught to date. Short of finding an egg or chick, which may prove virtually im- possible, these catches represent the best evidence so far recorded for the probable breeding of Storm Petrels on Ailsa Craig. Flowering Plants Elatine hydropiper at Loch Watston, West Perth R.J. KEYMER and J. MITCHELL West Perth: (87): In early July 1980, a substantial colony of Elatine hydropiper L. was found by R.J.K. at Loch Watston (NN 712004) near Doune, the first Scottish record for this small ephemeral plant outwith the Clyde area (see Bot. Soc. Edinb. News No. 22 pp. 7-9 for references to these sites). Loch Watston is a shallow, sandy bottomed, natural water body, the Elatine being particularly abundant on its wind-exposed eastern side where wave action has prevented the establishment of a Phrag - mites fringe. Both elongated and compact growth forms of E. hydro- piper were present, submerged under the water and exposed on the 87 drawn-down shore line respectively. Other weak-growing species such as C alii trie he stagnalis and C. hermaphroditica were close by in open association, but in contrast to most of the Clyde colonies a large pro- portion of the Elatine at Loch Watston was partially overshadowed by large aquatic plants including Potamogeton berchtoldii and P. pectin- atus ( det . Mr R. Stokoe), Nymphaea alba, Nuphar lutea and Equisetum fluviatile. From plant records in the Flora of Perthshire (1898) it is evident that the author, F. Buchanan White, and contributor R. Kidston were both personally acquainted with the botanical interest of Loch Wat- ston. As neither of these experienced field botanists recorded the presence of E. hydro piper, it is tempting to believe that its arrival and spread at the site are of comparatively recent origin. Erodium moschatum in Ayrshire RICHARD PRASHER Ayr (75): In July 1980, while gathering material at Kilwinning for the Kelvingrove Museum wild flower table, I collected along with Com- mon Storksbill, Erodium cicutarium agg. and Birdsfoot, Ornithopus perpusillus L., specimens of a plant which on a subsequent visit with the Natural History Staff of the Kelvingrove Museum was confirmed to be Erodium moschatum (L.) L’Herit. The Musk Storksbill is more robust and coarser than the Common Storksbill and smells of musk. Its leaves are not so finely divided and its fruits are larger and longer. It was growing vigorously on a landscaped area in the centre of the town. The Landscape Officer of Cunningham District, Mr Alistair Weir, informed us that the sandy soil in which the plants were growing had come from the Barassie area; however this site has now been built over. This same soil has also been used on a similar landscaped loca- tion at Kilwinning. From the literature it would appear that the Musk Storksbill has not been recorded for the West of Scotland. [Specimens in the herbarium of the Royal Botanic Garden, Edin- burgh indicate that Erodium moschatum probably occurs occasionally as a casual introduction in the Edinburgh area, and also as a wool alien in the Tweed Valley. Compiler ]. Rock Samphire in Ayrshire B. ZONFRILLO Ayr (75): While searching the cliffs at Bennane Head, south Ayrshire, for Fulmars on 31 August 1980, I discovered two large patches of Rock Samphire (Crithmum maritimum L.) growing on different parts of the cliffs above the main Girvan-Stranraer road. The clumps were 88 identified using 10 x 40 binoculars from a fairly close vantage point. Lee’s “Flora of the Clyde Area” (1933) gave the status of this plant as “very rare” and gave only one location, Dunure, within the Clyde area. There is one other reputed site in Ayrshire at Portencross. It is not known if Crithmum is still extant at these localities which, coincidentally, are also frequented by Fulmars. An Alien Sedge in the Glasgow area A. McG. STIRLING Renfrew (76): Members of the genus Carex of foreign origin are of decidedly rare occurrence in the British Isles and, when they do occur, are unlikely to be more than mere casuals. It is therefore of consider- able interest to record the existence of several clumps of the North American sedge Carex vulpinoidea Michx. on waste ground near Williamwood Station, Glasgow. These were noted by the writer on 10 July 1980 and appeared to have been growing on the site for some considerable time. The mode of introduction is not known. Carex vulpinoidea is one of only two alien species mentioned in Jermy’s “British Sedges” (1968). It formerly occurred as a persistent introduction in Surrey and Kent, and as a casual in Hampshire and Bristol, but the present population appears to represent the only ex- tant British record of this interesting sedge which cannot easily be mistaken for any native species. A fuller note is being prepared for publication elsewhere. Adventive Plants in Paisley A. McG. STIRLING Renfrew (76): During the summer of 1980 a number of uncommon adventive plants have appeared on waste ground and recently disturbed sites in central Paisley. A small plot of weed-infested ground close to the Central Public Library in High Street produced a number of speci- mens of Mullein ( Verbascum thapsus ), along with a few specimens of Viper’s Bugloss ( Echium vulgare). An area of disturbed ground created by road widening operations at Lonend yielded a surprising variety of unusual adventives including Tall Rocket ( Sisymbrium altissimum ), Wild Mignonette ( Reseda luted). Treacle Mustard ( Erysimum chieran- thoides), Norwegian Cinquefoil ( Potentilla norvegicd). Common Mel- ilot ( Melilotus officinalis) and Least Toadflax (Chaenorrhinum minus). These plants all occurred within an area measuring approxi- mately 20 yards long by 2 yards wide. Only one previous record of Potentilla norvegica for Renfrew, v.c. 76, has been traced. Plants of a refuse tip BARBARA C. M. MACPHERSON We looked at the ordnance survey maps of Lanarkshire to locate stretches of water where shore-line plants might be found. A large 89 reservoir south-east of East Kilbride seemed a likely situation, so we paid a visit in early September. Braving the fierce wind and driving rain we climbed up the steep 35 foot embankment and looked down at our goal — a corporation rubbish tip! However, our shock and disappointment turned to pleasure when we found (confirmed by Mr E. J. Clement) three garden crucifers — Garden Cress ( Lepidium sativum ), Candytuft ( Iberis umbellata ), Sweet Alison ( Lobularia maritima ), Cultivated Flax ( Linum usitatissimum ), and three canary seed grasses — Canary Grass ( Phalaris canariensis ), Foxtail Millet (Setaria italica) and Common Millet ( Panicum milliaceum). 90 Proceedings 1979 The chairman, place* and approximate number present, lecturer’s name and Institution, title of lecture and note of any exhibits are given for each meeting. *GMK: Glasgow Museum and Art Gallery, Kelvingrove. GUBD: Glasgow University Botany Department. GUZD: Glasgow University Zoology Department. USMB: University of Strathclyde. McCance Building. 9 JANUARY. Dr J. H. Dickson, GUZD, 50. Mr W. Anderson, Paisley Photographic Society: Nature Photographs from the 10th Paisley International Colour Slide Exhibition. 17 JANUARY : With Botanical Society of Edinburgh, Glasgow University Botanical Society and Strathclyde University Biology Club: Prof. W. W. Fletcher, USMB, 30. Dr Roy Watling, Royal Botanic Garden, Edinburgh : Salix Secrets Ex- posed. 13 FEBRUARY. Dr J. H. Dickson, GUZD, 45; 49th A.G.M. Reports on activities during 1978 were read, elections were held (see page 92) and appointments made by Council were announced. The report of Council stated that there were 240 ordinary members, 24 family members, 8 junior members and 5 honorary members. There were 18 excursions during the year (5 botanical, 2 geological, 2 ornithological, 3 zoological, 1 photographic, 1 botanical /geological, 1 botan- ical/ornithological, 3 botanical /photographic). 13 MARCH. Dr P. Macpherson, USMB, 54. Dr Judith Lawson, University of Glasgow: Building Stones of Glasgow. 10 APRIL. Dr P. Macpherson, GUBD, 61. Members’ Photographic Night. Guest of honour: Mr Richard Prasher MBE to whom a presentation was made. 8 MAY. Dr P. Macpherson, USMB, 29. Dr John Edmondson, Royal Botanic Garden, Edinburgh : Plant Hunting in the Mountains of Iran. 91 15 SEPTEMBER. Dr P. Macpherson, GMK, 50 Exhibition Meeting. The following lecture was given: Mr F. G. Rodway, Glasgow Botanic Gardens: British Orchids. The following exhibits were on display: Journals from the Andersonian Library (Mrs R. H. Dobson). Canary Island Plants (Dr J. H. Dickson). Flandrian Marine Incursion into Loch Lomond (Dr Duncan Stewart). A Selection of Rocks and Fossils (Mrs A. Cross). Geological Specimens (Mr A. A. Percy). Wild Flowers of Scotland (Mr R. Prasher). Some Fungi of the Glasgow Area (Dr Alan Silverside). Brambles: Differential features of some local members of the genus Rub us (A. McG. Stirling). Wild-life Gardening (Conservation Division, Glasgow Parks). Slides of Wild Flowers in and around Glasgow (C. E. Palmar). 9 OCTOBER. Dr P. Macpherson, GUZD, 38. Mr Gordon Ridley, Glasgow College of Building and Printing: Under- water Marine Photography. The President intimated that the following change to the Constitution had been unanimously recommended by the Council: Chapter 1. Name of Society, for “The Andersonian Naturalists of Glasgow” substitute “The Glasgow Natural History Society”. This would be put to the meeting on 13 November. 5 NOVEMBER. With Botanical Society of Edinburgh, Glasgow University Botanical Society and Strathclyde University Biology Club: The Student President, USMB, 35. Prof. J. L. Harper: The Shapes and Numbers of Plants. 13 NOVEMBER. Dr P. Macpherson, GUZD, 41. The proposed change to the Constitution, changing the name of the Society to The Glasgow Natural History Society was proposed by Prof. B. Lloyd-Binns and seconded by Mr D. Stewart. After discussion the motion was carried unan- imously by the 34 members present who were eligible to vote. The following lecture was given: Dr J. H. Dickson and Dr J. G. MacDonald: Visit to Tenerife, April 1979. Exhibit: Recent additions to the Library, Mrs R. H. Dobson. 11 DECEMBER. Dr P. Macpherson, GUZD, 18. Dr K. Ingham, Hunterian Museum, University of Glasgow: A Geologist in China. The death was announced of Mr H. A. Gemmell, a member of the Zool- ogy Sectional Committee and a member of the Society since 1957. 92 President : Vice-presidents : Councillors : General Secretary : Treasurer : Librarian : Editor : Conveners of Sections : Auditors : Trustees : Assistant Secretaries : Editorial Board : Officers and Council SESSION XLIX 1979 Peter Macpherson, F.R.C.R., D.T.C.D. F.L.S. Mrs Lilian M. Stallard, D.C.E. (1977) Bernard Zonfrillo (1977) Mrs Agnes Craib M.A, (1979) Charles E. Palmar A.R.P.S., M.B.O.U. F.M.A. (1979) Miss Gwyneth L. Jones, B.Sc., (1977) Alan Silverside, B.Sc., Ph.D. (1977) Duncan A. Stewart, B.Sc. Ph.D. (1977) Miss Anne McCourt B.Sc (1978) Mrs Margaret McLaughlin B.Sc., M.Sc. (1978) Arthur W. Babister M.A., Ph.D. (1978) James H. Dickson B.Sc. M.A. Ph.D. (1979) Mrs Margaret Anderson B.Sc., N.D.A. (1979) J. Campbell (1979) Miss Elizabeth R. T. Conacher F.L.S. Donald D. Clarke, B.Sc., Ph.D. Mrs Ruth H. Dobson M.Sc Eric W. Curtis, S.D.H. Allan McG. Stirling (Botany) Alfred A. Percy (Geology) Bernard Zonfrillo (Ornithology) Ronald M. Dobson (Zoology) F. Gerald Rodway (Photography) A. D. Chisholm R. D. McBeath Alex. R. Hill B.Sc., Ph.D. Stephen A. Hutchinson, T.D., B.Sc., Ph.D., F.R.S.E. Alfred A. Percy (Bulletin) Allan McG. Stirling (Excursions) Alan J. Silverside (Meetings) Arthur W. Babister (Minutes) Mrs Agnes Craib (Social) Duncan A. Stewart (Publicity) Miss Gwyneth L. Jones (Membership) R. Watson (Library) The Editor Alan C. Crundwell, B.A. Ronald M. Dobson James H. Dickson Allan McG. Stirling 93 Membership 1980 Honorary Members 1951 ANDERSON Sir David bsc phd Braehead East Montrose Street Helens- burgh 1951 BERRY John ma phd frse Tayfield Newport-on-Tay DD6 8HA 1973 CURRAN Sir Samuel phd ma dsc lld frs 1936 PR ASHER Richard mbe 52 Mair Avenue Dairy Ayrshire KA25 2D 1973 WILSON Sir Charles ma lld dlitt dcl Ordinary Junior (*) Family (f) and School ($) Members 1980 ALEXANDER Mrs Joyce E F 25 Seil Drive Glasgow G44 5DX 1962 ALLEN Mrs E S 138 Danes Drive Glasgow G14 9BH 1973 ANDERSON Mrs Margaret bsc nda 516 Shields Road Glasgow G41 2RE 1971 ANDERSON Mrs Rhoda 54 Maxwell Drive East Kilbride G74 4IJ 1976 BABISTER A W ma phd 286 Churchill Drive Glasgow Gil 7HB 1979 BAILEY Dr A B Endrickvale Fintry G63 OYH 1979 f BAILEY Mrs A B Endrickvale Fintry G63 OYH 1978 BARKER Mrs Hilary bsc msc Conservation Division Parks Department 20 Trongate Glasgow G1 5ES 1975 BARRIE Miss P 17 Lovat Avenue Bearsden G61 3LQ 1974 BEAVIS D Flat 4/4 190 Kestrel Road Glasgow G13 3PQ 1980 *BELL Stephen 11 Rowallan Gardens Glasgow Gil 7LH 1965 BERRIE Alex M M bsc phd Department of Botany University of Glasgow G12 8QQ 1978 BESSANT Edward D 22 Wallace Avenue Bishopton PA7 5BR 1978 BEVERIDGE Malcolm bsc Department of Aquatic Pathobiology Stirling University Stirling 1966 BIGGAR John 3 Westcliffe Street Shawlands Glasgow G41 1934 BINNS Prof B Lloyd phd mibiol fls 22 Edgemont Street Glasgow G41 3EN 1951 BLACK Miss F M 8 Millbrae Crescent Newlands Glasgow G42 1970 BLAIR Mrs A G bsc 17 Panton ville Road West Kilbride Ayrshire 1980 BLOUNT Mrs Jane White Lodge Tummel Bridge Pitlochry Perthshire PH16 5SB 1980 BLOUNT Paul White Lodge Tummel Bridge Pitlochry Perthshire PH16 5SB 1976 BONEY Prof A D phd dsc Department of Botany University of Glasgow G12 8QQ 1928 BRAID Prof K W obe ma bsc bsc(agric) Lochview Skene Aberdeen AB3 6XR (President 1949-1951) 1980 BRETT Dr C T ma phd 19 Huntley Gardens Glasgow G12 9 AT 1975 BROADLEY Brian J ba 92 Hyndland Road Glasgow G12 9PZ 94 1959 BYERS Miss M E ma 18 Stuart Avenue High Burnside Rutherglen G73 4JL 1964 CALVER Miss K M bsc phd 43 Dorchester Court Glasgow G12 OBS 1979 CAMERON Miss Heather M 4 Green Street Cambridge CB2 3JU 1972 CAMERON J M 15 Castle Street Balloch Alexandria G83 8HU 1976 CAMERON Jean M 197 Westland Drive Glasgow G14 9JQ 1974 CAMPBELL Miss E M 24 Woodlands Road Glasgow G3 6UR 1974 CAMPBELL Jack Flat 182 3 Pinkston Drive Glasgow G21 1PQ 1978 CARLIN Joseph mb chb 10 Glenturret Street Glasgow G32 7SG 1980 ^CARMICHAEL Grant Flat 8/c 5 Broomhill Lane Glasgow G12 9 AT 1957 CARTER Mrs M bsc 16 Berwick Drive Burnside Rutherglen G73 3JP 1971 CHAMBERS Helen H mb chb 14 Woodburn Road Glasgow G43 2TN 1978 CHAPMAN Miss Jan B 121 Randolph Road Jordanhill Glasgow Gil 7DS 1978 CHRISTIE I C Gartlea Caldarvan By Alexandria G83 9LX 1978 f CHRISTIE Mrs Jane Gartlea Caldarvan By Alexandria G83 9LX 1976 CLARKE Dr D D Department of Botany University of Glasgow G12 8QQ 1974 CLUGSTON David 14 Rosewood Avenue Paisley PA2 9NJ 1977 COLLINS Dr Linda J 10a Kirklee Quadrant Glasgow G12 1973 COLLIS G M bsc East Lodge Cambusnethan Estate Overtoun By Wishaw 1952 CONACHER Miss E R T fls An Fharaid Lawmarnock Bridge of Weir PA11 3AP 1952 f CONACHER Miss N C T An Fharaid Lawmarnock Bridge of Weir PA11 3AP 1975 COUBROUGH Ian M 43 Ormonde Avenue Glasgow G44 3QY 1975 COUBROUGH Mrs J C B 43 Ormonde Avenue Glasgow G44 3QY 1980 *COYLE John 38 Annette Street Glasgow G42 8EQ 1969 CRAIB Mrs A ma 23 Highburgh Road Glasgow G12 9YG 1976 CROMWELL Bryan 9 Lomond Drive Condorrat Cumbernauld G67 4JL 1969 CROSBY Mrs Anne 10 Winchester Road Petersfield Hants GU32 3RY 1957 CROSS Mrs A bsc 598 Tollcross Road Glasgow G32 8TE 1980 CROSS Mrs Gertha 7 Douglaston Crescent Milngavie G62 6HW 1955 tCROWSON Mrs E A 1012 Great Western Road Glasgow G12 0NR 1955 CROWSON R A dsc arcs dic Department of Zoology University of Glasgow G12 8QQ 1950 CRUNDWELL A C ba Department of Botany University of Glasgow G12 8QQ 1980 CULLEN Miss Elizabeth 38 Heathcot Avenue Glasgow G15 8NX 1970 GUMMING A bsc 289 Churchill Drive Glasgow Gil 7HE 1970 fCUMMING Mrs C M 289 Churchill Drive Glasgow Gil 7HE 1978 CURTIS Prof A S G ma phd Department of Cell Biology University of Glasgow G12 1961 CURTIS E W Curator’s House Botanic Gardens Glasgow G12 0UE 1971 CUTHILL Miss M G 23 Alcaig Road Glasgow G52 1NH 1978 DALE Robert 119 Kirkwood Avenue Clydebank G81 1972 DALY Ronald 1 Hamilton Drive Glasgow G12 1978 DAND Mrs E M 79 Marlborough Avenue Glasgow Gil 7BT 1972 DANIELS T P da 5 Dungoyne Street Maryhill Park Glasgow G20 0BA 95 1980 DIAMOND R I bsc msc University Library Hillhead Street Glasgow G12 8QE 1955 DICKSON J H bsc ma phd fls Department of Botany University of Glasgow G12 8QQ (President 1976-1978) 1976 tDICKSON Mrs C A 113 Clober Road Milngavie G62 1979 tDICKSON Miss K 113 Clober Road Milngavie G62 1969 DOBSON Mrs R H msc 664 Clarkston Road Glasgow G44 1963 DOBSON Ronald M ma phd Department of Zoology University of Glasgow G12 8QQ 1978 DOUGHTY C Ross 201 Croftside Avenue Glasgow G44 5NB 1963 DOYLE Charles ma 66 Brunton Street Glasgow G44 3NG 1957 DRYSDALE Miss Agnes R 7 Malcolm Court Dollar Clackmannanshire 1974 DUCHART B bsc phd Barloch Lodge Middleton Milngavie G62 1973 DUCHART Mrs P bsc Barloch Lodge Middleton Milngavie G62 1979 DUNCAN G K bsc 8 Dean’s Avenue Cambuslang Glasgow G72 1939 DUNLOP Miss Eva ma bsc 11 Grosvenor Crescent Glasgow G12 9AF 1978 ELLIOT Dr C G Department of Botany University of Glasgow G12 8QQ 1978 tELLIOT Mrs C G Department of Botany University of Glasgow G12 8QQ 1980 ELLIOT T bsc phd 15 Park Circus Place Glasgow G3 1978 ERSKINE Miss A B 1 Stevenson Street Kilmarnock KA1 2RF 1978 *FERGUSON Robert 69 Ravelston Road Bearsden G61 1960 FINDLAY Mrs A 158 Sunnyside Drive Glasgow G15 6RE 1951 FISHER Robert Ewing 366 Clarkston Road Glasgow G44 3JL 1963 FLETCHER Prof W W frse bsc phd mibiol fls Department of Biology University of Strathclyde Glasgow G1 1XW 1975 FORRESTER Miss H 41 Crofton Avenue Glasgow G44 5HY 1978 FREEMAN H E 478 Kilmarnock Road Newlands Glasgow G43 1978 FURNESS Dr R W Department of Zoology University of Glasgow G12 1979 GALL Ms Sandra 43 Partickhill Road Hyndland Glasgow G12 1978 GALLOWAY Sara L ab ma 11 The University Glasgow G12 1941 GARDNER J Allan Craiglinn Craig Street Airdrie 1961 GARDNER N bsc 28 Hamilton Park Avenue Glasgow G12 8DT 1980 GEDDES John M 12 Lochlea Road Newlands Glasgow G43 2XZ 1951 GIBSON J A mb chb mbou fzs Foremount House Kilbarchan Renfrew- shire 1978 GIFFARD Mrs Fiona 12 Banavie Road Glasgow Gil 5 AN 1979 t GLENNIE Susan 50/97 Kennishead Avenue Carnwadric Glasgow G46 1974 GORDON Ian 146 West Princes Street Glasgow G4 9DA 1973 GORDON Mrs J F 146 West Princes Street Glasgow G4 9DA 1979 GRAHAM E A c/o Strachan 22 Kingsborough Gardens Glasgow G12 9NJ 1976 GRANT Frederick 21 Snuff mill Road Cathcart Glasgow G44 5YA 1979 GRAY Bob 45 Bank Street Glasgow G12 1971 GRAYSTON Thomas B M bsc 3 Hillhead Road Stevenston Ayrshire KA20 4DX 1979 GREIG Mrs M G 44 Sidlaw Road Bearsden G61 4LD 1979 GRIFFIN Kenneth Garbank Lanark Road Garrion Bridge Larkhall ML9 1978 GRIFFITH R S c/o Macpherson 1445 Paisley Road West Glasgow 96 1980 GUNNION W S 80 Ledi Drive Bearsden G61 1976 HALLIGAN Miss S 10 Carron Crescent Bishopbriggs G64 1975 HARRIS J 213 Main Street Glasgow G40 1QH 1979 HAY Miss Isobel ma med 23 Underwood Road Burnside Rutherglen G73 1972 HENDERSON A A R ma 33a Dalkeith Avenue Glasgow G41 5LH 1980 HENDRY Mrs P W 28a Sutherland Avenue Glasgow G41 1964 HENRY Miss E 12 Stamperland Drive Clarkston Glasgow G76 8HE 1951 HILL Alex R bsc phd Department of Zoology University of Glasgow G12 8QQ 1972 HILLMAN Mrs T T 123 Ledi Drive Bearsden G61 4JR 1965 HINCHCLIFFE Mrs Doris H mrcvs Mill Cottage Drumbeg Loan Killearn G63 9LQ 1980 HOPKINS G W R 125 Ledi Drive Bearsden G61 41 R 1980 fHOPKINS Mrs M E 125 Ledi Drive Bearsden G61 4JR 1964 HOSIE Geoffrey bsc 12 Beech Avenue Bearsden G61 3EX 1977 HOUSTON David bsc dphil Department of Zoology University of Glasgow G12 1980 HUNT P 8 Athole Gardens Glasgow G12 9AZ 1980 fHUNT Mrs S 8 Athole Gardens Glasgow G12 9AZ 1979 HUNTER Ms I 3 Belhaven Terrace Glasgow G12 0TF 1978 HUNTER Ian 68 Campsie Drive Milngavie G62 1965 HUNTER Richard 30 Learmont Place Milngavie G62 7DT 1948 HUNTER Prof W D Russell bsc dsc mibiol fls 23 Hurd Street Cazenovia New York 13035 USA 1951 HUTCHINSON Dr Stephen A td bsc phd frse Applecross Frome Saint Quintin Dorchester Dorset (President 1964-1966) 1959 HUTCHISON Prof W M dsc fls fibiol frse 597 Kilmarnock Road Newlands Glasgow G43 2TH 1965 IDLE E T bsc Woodcroft Lauder Road Stow Galashiels 1968 t IRVINE W 47 Tintillo Drive Scotstounhill Glasgow G13 1968 IRVINE Mrs F 47 Tintillo Drive Scotstounhill Glasgow G13 1978 JARVIS M C bsc phd Department of Agricultural Chemistry University of Glasgow G12 1979 JOCELYN M J L c/o Scottish Universities Research and Reactor Centre East Kilbride G75 1969 JONES R W bsc 19 Herries Road Glasgow G41 4DE 1980 KEMP Mrs A F ma 1 Mansion House Drive Glasgow G32 1980 KENNEDY A F D 1 Eastern Crescent Kilbimie Ayrshire 1976 KENNEDY M W bsc Department of Zoology University of Glasgow G12 1966 KENNETH A G Stronachullin Ardrishaig Argyll 1980 KLEINBERG Stanley S ma bphil 109 Southbrae Drive Glasgow G13 ITU 1980 tKLEINBERG Mrs 109 Southbrae Drive Glasgow G13 ITU 1980 KNEPIL Mrs E 97 Shawood Crescent Glasgow G77 1980 KNOWLES D R 55 Bellshaugh Road Kirklee Glasgow G12 1980 fKNOWLES Mrs A 55 Bellshaugh Road Kirklee Glasgow G12 1979 LAIRD M G 102 Napiershall Street Woodside Glasgow G2 6HS 1957 LAIRD Miss Annie bsc 20 Windlaw Road Carmunnock Glasgow G76 9DN 97 1963 LAIRD Miss Marion K 28 North Middleton Drive Largs 1975 LENIHAN Mrs J M A 1 Kingsborough Gardens Glasgow G12 9QA 1980 fLINDSAY Bruce A 74 Kintore Road Newlands Glasgow G43 2EY 1978 LOGAN Mrs G 26 Berridale Avenue Cathcart Glasgow G44 1978 t LOG AN Dr N 26 Berridale Avenue Cathcart Glasgow G44 1965 LOGAN Mrs Helen M L bsc 21 Ashton Drive Glasgow G12 8SP 1978 LOGAN John W H 23 Cran worth Street Glasgow G12 1980 JLOWE E 100 Eastpark Avenue Newlands Glasgow C43 1958 LYTH John R S 26 Gardenside Street Uddingston Glasgow G71 7BY 1980 LYTH Miss Margaret M H 26 Gardenside Street Uddingston Glasgow G71 7BY 1941 McCALLUM Miss A H bsc 52 Dorchester Court 5 Dorchester Place Glasgow G12 0BS 1978 McCALLUM I C 1 Craigenbay Road Lenzie G66 5JN 1978 fMcCALLUM Mrs I C 1 Craigenbay Road Lenzie G66 5JN 1974 MCCARTHY Jim The Nature Conservancy 12 Hope Terrace Edinburgh 1979 McCOLL S N A 52 White Street Partick Glasgow Gil 5EA 1974 McCOURT Miss A H bsc 14 Hillside Avenue Bearsden G61 3QE 1979 McDADE H B mb chb mrcp 34 Garrowhill Road Carmunnock Glasgow G76 1971 McEWAN Duncan I bsc 73 Hazelwood Road Bridge of Weir PA11 3DX 1980 JMcFETRIDGE Alan 29 Garvock Drive Eastwood Glasgow G43 1980 McGINLAY Francis 24 Nairn Street Yorkhill Glasgow G3 8SF 1975 McHUGH James bsc 16 Carrick Road Bishopbriggs G64 1EN 1970 MacINDEOR D nda sda 21 Polnoon Street Eaglesham G76 0BH 1950 McINTYRE Charles T 75 Crosslee Street Craigton Glasgow G52 1SL 1978 McKAY Mrs M E 8 Hillside Avenue Bearsden G61 1978 McKECHNIE Miss C B 59 Polwarth Street Glasgow G12 9TH 1957 MACKECHNIE Mrs E L P 9 Skirving Street Glasgow G41 3AB 1965 McKELLAR Miss M E G ma 5 Dudley Drive Glasgow G12 9SE 1977 MACKELVIE Fiona 38 Wykeham Road Glasgow G13 3YK 1976 McKENDRICK John 14 Invergordon Avenue Glasgow G43 2HP 1976 MACKENZIE Miss Kathryn bsc 33 Dalkeith Avenue Dumbreck Glas- gow G41 1964 McKERRON John F bsc Glenruther 25 Crichton Road Rothesay Bute 1976 McLAUGHLIN Mrs M E bsc msc Institute of Genetics University of Glasgow G12 8QQ 1944 MACLAURIN Alan M 4 Sorley’s Brae Dollar Clackmannanshire FK14 7AS 1963 t MACLAURIN Mrs I 4 Sorley’s Brae Dollar Clackmannanshire FK14 7AS 1953 McLEAN Miss Ann 20 Tilt Street Glasgow G33 2BD 1980 $McLEAN Ewan 298 Kirkintilloch Road Bishopbriggs G64 2HF 1980 f McLEAN Mrs J 298 Kirkintilloch Road Bishopbriggs G64 2HF 1980 McLEAN Norman 298 Kirkintilloch Road Bishopbriggs G64 2HF 1978 McLEOD W J 119 Bathco Avenue Paisley PA1 3DZ 1979 McMURTRIE W M Ardyne 21 Eastwood Avenue Giffnock G46 6LS 1967 MACPHERSON Mrs A C mb chb mfcm dph 15 Lubnaig Road Glasgow G43 2RY 98 1967 *MACPHERSON Miss B C M 15 Lubnaig Road Glasgow G43 2RY 1967 MACPHERSON Miss E L S mb chb 15 Lubnaig Road Glasgow G43 2RY 1967 *MACPHERSON Miss L M D 15 Lubnaig Road Glasgow G43 2RY 1967 MACPHERSON P frcr dtcd fls 15 Lubnaig Road Glasgow G43 2RY (President) 1945 MACRAE Miss J G ma 38 North Lodge Avenue Motherwell Lanarkshire 1963 MAITLAND P S bsc phd Nether Sunnyside Haddington East Lothian EH41 1964 MATHISEN Miss Mary M 1048 Cathcart Road Glasgow G42 9XW 1970 MEIKLEJOHN Miss Norma 63 Lauderdale Gardens Glasgow G12 9QU 1979 MELLOR D bsc ama 19 Walker Street Paisley 1980 MICHNA Mrs 43 West Chapelton Crescent Bearsden G61 1979 MILLAR Ms Irene 8 St Stephens Avenue High Burnside Rutherglen G73 5LS .1972 MILLAR Mrs Jean M ma Syde Old Greenock Road Kilmacolm PA13 4TT 1934 MILLAR Miss Kathleen J bsc 23 Milner Road Glasgow G13 1QL 1959 MILLER Miss A R ma bsc 81 Viewpark Drive Rutherglen G73 3QQ 1961 MILLER Peter J bsc phd Department of Zoology The University Bristol BS8 1TH 1965 MITCHELL John 22 Muirpark Way Drymen G63 ODX 1979 ^MONTGOMERY Miss Rhona 28 Hopeman Avenue Thornliebank Glasgow 1975 MORGAN Miss G bsc 15 Belhaven Terrace Glasgow G12 OTG 1954 MORRISON C M ma Innis Righ Kingsmeadow Peebles EH45 9HR 1979 tMURRAY William 45 Kilmuir Road Arden Glasgow G46 1960 NAISH Bernard 7 Carron Crescent Bishopbriggs G64 1HE 1978 NAISMITH T D 56 Arisaig Drive Glasgow G52 1HP 1977 NATURAL HISTORY DEPARTMENT Art Gallery and Museum Kel- vingrove Glasgow G3 8 AG 1968 NEILSON J R Netherhall 9 Beech Avenue Lenzie G66 1968 t NEILSON Mrs D G NetherhaU 9 Beech Road Lenzie G66 1972 NEWTH Prof D R bsc phd Department of Zoology University of Glas- gow G12 8QQ 1953 NICOL Mrs C S 15 King’s Park Road Glasgow G44 4TT 1980 NOVE Mrs Irene 55 Hamilton Drive Glasgow G12 8DP 1965 OLDHAM S A J obe ndh 116 Beech Avenue Newton Mearns G77 1978 O’REILLY Myles 27 Newark Drive Glasgow G41 4QA 1948 PALMAR C E arps mbou fma 24 Hamilton Park Avenue Glasgow G12 8DT 1978 PATERSON D 4 Muir Street Stenhousemuir Stirlingshire 1980 PAULSEN Donald A bsc 9a Ailsa Drive Langside Glasgow G42 9UL 1980 fPAULSEN Mrs Jane bsc 9a Ailsa Drive Langside Glasgow G42 9UL 1972 PEARSON R 1 Simon’s Crescent Renfrew PA4 8TF 1959 PERCY A A 5 Buckingham Drive Carmyle Glasgow G32 8DJ 1979 RANDAL Ms Marion bsc 54 Golf Drive Old Drumchapel Glasgow G15 1964 REID David L bsc Bridge Cottage Balfron Station Stirlingshire G63 0HN 99 1950 RIBBONS B W bsc mibiol fls Department of Botany University of Glasgow G12 8QQ (President 1961-1963) 1978 t RIDDEL P J 12 Henrietta Street Glasgow G14 OBG 1976 ROBERTS Mrs B C 14 Valeview Terrace Glasgow G42 9LA 1940 ROBERTSON Ian bl 250 Churchill Drive Glasgow Gil 7HB 1956 ROBERTSON Prof J D scd phd frse Department of Zoology Univer- sity of Glasgow G12 8QQ 1978 ROBERTSON Mrs S bsc 59 North Grange Road Bearsden G61 1934 ROBERTSON Thomas 71 Mearns Road Clarkston Glasgow G76 7LF 1980 ROBSON Allen S S 202 Anniesland Road Glasgow G13 1XD 1953, 1972 ROOD AM Rupert 93 Keal Avenue Glasgow G15 6PA 1960 ROD WAY F G East Lodge Botanic Gardens Glasgow G12 0UE 1962 fRODWAY Mrs H East Lodge Botanic Gardens Glasgow G12 0UE 1975 JRODWAY Maxine East Lodge Botanic Gardens Glasgow G12 0UE 1965 ROLFE W D Ian bsc phd fgs Hunterian Museum University of Glasgow G12 8QQ 1978 ROY Miss A 274 Renfrew Street Glasgow G3 6TT 1972 RUTHERFORD Miss A Rosslyn Cottage Church Road Rhu Helens- burgh G84 8RW 1980 RUTHVEN Mrs C A bsc 46 Lubnaig Road Newlands Glasgow G43 2RX 1967 SCOTT John M 10 Hartfield Gardens Dumbarton G82 2DE 1931 SCOTT Miss Mabel G bsc ma 68 Evan Drive Giffnock Glasgow G46 6NQ 1952 SHANKLAND T E 72 Nelson Street Largs Ayrshire 1980 SHAPLEY D O 90 Liddel Road Seafar Cumbernauld G67 1JE 1963 SHARP E L ma 14 Blair Gardens Torrance G64 4HL 1964 fSHARP Mrs Jean 14 Blair Gardens Torrance G64 4HL 1972 SHARP Miss M I 468 Anniesland Road Glasgow G13 1YH 1976 SHEARER Mrs Sheila 19 Dalmeny Avenue Giffnock Glasgow G46 1979 SIBLY R M ma dphil Department of Zoology University of Glasgow G12 1974 SILVERSIDE A J bsc mibiol phd Department of Biology College of Technology High Street Paisley PA1 2BE 1979 SKINNER Mrs J A bsc 34 Dudley Drive Hyndland Glasgow G12 1948 SLACK A A P bsc Morvem View Kentallen Appin Argyll (President 1970- 1972) 1954 fSLACK Mrs M W Morvern View Kentallen Appin Argyll 1965 SMYTH Prof John C bsc phd Glenpark Johnstone Renfrewshire 1978 SNEDDON Mrs P 57 Moraine Avenue Glasgow G15 6HF 1978 SOUTAR Nicholas T bsc mibiol 4 Church Drive Lenzie G66 4HQ 1965 ST ALLARD G N Llwyn Derw Carno Nr Caersws Powys 1970 ST ALLARD Mrs L M Llwyn Derw Carno Nr Caersws Powys 1979 i STEWART Alan 6 Kilmuir Road Arden Glasgow G46 8BE 1974 STEWART Duncan A bsc phd 20 Ingleston Avenue Dunipace Denny Stirlingshire 1968 STEWART Miss L J 54 Underwood Road Burnside Rutherglen G73 3TF 1977 STEWART M 969 Gartloch Road Glasgow G33 5 AH 1979 STEWART R A 7 Jedburgh Gardens Glasgow G20 6BP 100 1951 1961 STIRLING A McG 17 Austen Road Jordanhill Glasgow G13 1SJ (President 1973-1975) 1980 STONE Mrs Irene 11 Park Gardens Kilbarchan Renfrewshire 1961 STOVE William K 37 Stamperland Avenue Clarkston Glasgow G76 8EX 1963 fSTOVE Mrs Margaret 37 Stamperland Avenue Clarkston Glasgow G76 8EX 1957 SUMMERS James L 11 Dalvait Road Balloch Alexandria G83 8LA 1980 f SUTCLIFFE Mrs A bsc Department of Botany University of Glasgow G12 1980 SUTCLIFFE Richard bsc Natural History Department Museum and Art Gallery Kelvingrove Glasgow G3 1976 SWIFT J Dean 65 Don Craigshill Livingston West Lothian 1973 TAIT T N Department of Botany University of Glasgow G12 1979 tTAIT Mrs P 11 Rosshall Place Renfrew PA4 0BA 1971 THURSTON June P bsc phd 47 Larkfield Road Lenzie G66 3AR 1961 TODD E C D bsc phd Microbiology Division Food and Drug Direct- orate Turney’s Pasture Ottawa Ontario Canada 1969 WALKER Mrs A bsc msc 20 St Vincent Crescent Glasgow G3 1964 WALKINSHAW D A bsc 10 Cluny Drive Bearsden G61 2JG 1970 tWALKINSHAW M A bsc 10 Cluny Drive Bearsden G61 2JG 1970 WALSH Mrs Veronica 81 Kenmure Street Pollokshields Glasgow G41 2NT 1969 WATERMAN P G bpharm mps 4 Conic Way Drymen G63 0DT 1970 f WATERMAN Mrs M B bpharm mps 4 Conic Way Drymen G63 0DT 1977 WATSON Robert G 59 Bank Street Glasgow G12 8NF 1975 WATT E T bsc 129 Fotheringay Road Glasgow G41 4LG 1979 | WAUGH Richard 71 Capelrig Street Camwadric Glasgow G46 1957 WEIR Mrs R M Drumganach Ross Loan Gartocharn Dunbartonshire G83 1959 WHITE John 64 Viewfield Road Coatbridge Lanarkshire 1979 J WHITE S 29 Glasserton Road Merrylee Glasgow G43 1971 WILSON Mrs J 68 Craigton Avenue Milngavie G62 1975 WOODWARD D C bsc 11 St Andrews Drive Bridge of Weir PA11 3HS 1980 WOODWARD Fred R bsc Natural History Department Art Gallery and Museum Kelvingrove Glasgow G3 8AG 1978 WOOLHEAD A S bsc University Field Station Rowardennan G63 1972 WYPER William bsc 197 Hillpark Drive Glasgow G43 1975 YORKE J P mbe frse 1855 London Road Glasgow G32 8XE 1969 ZONFRILLO B 28 Brodie Road Glasgow G21 3SB The Glasgow Naturalist This publication is included in the abstracted and indexing coverage of the Biosciences Information Service of the Biological Abstracts The following back numbers are available for purchase at the prices shown (plus postage). Volume II (1909-10) Parts 1, 2, 3, 4 Volume III (1910-11) Parts 1, 2, 3, 4 Volume IV (1911-12) Parts 1, 2, 3, 4 £1.50 each Volume V (1912-13) Parts 1, 2, 3, 4 Volume VI (1913-14) Parts 1, 2, (3 + 4) ) Volume VII (1915) Parts 1, 2, 3, 4 \ Volume VIII (1916-18) Parts 1, 2, 3, 4, 5, 6 j £1.25 each Volume XIII (1937-38) Parts 1, 2 Volume XIV (1940-44) Parts 1, 2, 3 Volume XV (1945-49) Parts 1*, 2, 3 Volume XVI (1951-52) Parts 1, 2, (3+4) L £1.00 each Volume XVII (1952-56) Parts 1, 2t, 3, 4, 5, 6 Volume XVIII (1958-71) Parts 1, 2, 3, 4, 5, 1 Parts 8, 9 £1.25 each Part 10 £2.00 Volume XIX (1973-79) Parts 1, 2, 3, 4 £2.00 each Part 5 £2.50 Part 6 £4.00 *Part 1 contains (18pp) The Flora of Easter Dunbartonshire by J. R. Lee. fPart 2 contains (18pp) Additions to the flora of the Clyde Area by J. R. Lee. {Part 6 (82pp) is a list of the less common Scottish Basidiomycctes by D. A. Reid and P. K. C. Austwick. Of the earlier journals, the only parts available are: Annals of the Andersonian Naturalists’ Society : Volume IV Part 3 £1.00 Proceedings and Transactions of the Natural History Society of Glasgow : Volume I Volume II Volume VI Volume VII Volume VIII (1885-86) Part 3 (1886-88) Parts 1, 2 (1899-1901) Parts 1, 2 (1904-05) Part 3 (1905-08) Parts 1, 2 £1.50 each Orders for any of the above and for copies of the current and future issues should be addressed to the Librarian — Mrs R. Dobson, 664 Clarkston Road, Glasgow, G44 3YS. Printed in Scotland by John Frood, Printers, Annan Contents Page 1 Building Stones of Glasgow. JUDITH LAWSON 7 Kilbirnie Loch, Ayrshire : an Ecological Appraisal. P. S. MAIT- LAND et al 24 Naturalists in Glasgow No. 1 : Sir William Hooker 25 A Species of Water-flea new to Scotland ( Alona weltneri). C. R. DOUGHTY 29 Rare Beetles in the City of Glasgow. R. A. CROWSON 31 The Freshwater and Terrestrial Fauna of the Clyde Area IV. Freshwater Fishes of the Upper Clyde Basin. PETER S. MAIT- LAND 50 Glasgow Natural History Society 5 1 The Herbarium of the Glasgow Museum and Art Gallery. GWYNETH JONES 58 Book Review: The Butterflies of Scotland 59 The Endemic Whitebeams of North Arran. ERIC BIGNAL 65 Carex elongata in Scotland. J. MITCHELL and A. McG. STIR- LING 71 Veronica peregrina in the West of Scotland. PETER MAC- PHERSON 74 Junior Excursion Meeting to the Clyde at Cambuslang. EL- SPETH L. S. MACPHERSON 75 Clyde Dock Aliens. PETER MACPHERSON and ALLAN McG STIRLING 77 The Flora of the Loch Lomond National Nature Reserve: a Sup- plement. J. MITCHELL and A. McG. STIRLING 82 Acknowledgments 83 Short Notes compiled by A. McG. STIRLING 90 Proceedings 92 Officers and Council 93 Membership 1980 Volume 20 Part 2 1981 / The Glasgow Natural History Society (formerly The Andersonian Naturalists of Glasgow) The object of the Society is the encouragement of the study of natural history in all its branches, by meetings for reading and discussing papers and exhibiting specimens, and by excursions for field work. The Glas- gow Natural History Society meet at least once a month except during July and August, in the University of Glasgow, the University of Strath- clyde or the Glasgow Art Gallery and Museum. The present rates of subscription per annum are: for Ordinary Members, £6; for Junior Members, £2.50; for Family Members, £2; and for School Members, £1. Further information regarding the Society’s activities and membership application forms are obtainable from the General Secretary : Mr RICHARD SUTCLIFFE, NATURAL HISTORY DEPARTMENT, MUSEUM & ART GALLERY, KELVINGROVE, GLASGOW, G3 8AG. The Glasgow Naturalist Published by the Glasgow Natural History Society, December, 1981. ISSN 0373-241 X. Price £4.00 Edited by E. W. Curtis with the assistance of A. C. Crundwell, R. M. Dobson, A. McG. Stirling and J. H. Dickson. Contributions are invited, especially when they bear on the natural history of Scotland. A note of information for contributors is available from the Editor. Smaller items are also welcome from members and others. These may cover, for example, new stations for a species, rediscoveries of old records, additions to records in the Atlas of the British Flora , unusual dates of flowering, unusual colour forms, ringed birds recovered, weather notes, occurrences known to be rare, interesting localities not usually visited by naturalists. (The nomenclature of vascular plants should be as in Dandy, List of British Vascular Plants , 1958 and its revision. 1969). All communications on editorial matters should be sent to: Mr E. W. CURTIS, BOTANIC GARDENS, GLASGOW, G1 2 OUE. A limited number of advertisements can be accepted and enquiries should be sent to the Editor . Back numbers available are listed on page iii of cover. ii 101 What is the Scottish Thistle? J. H. DICKSON Botany Department, University of Glasgow AGNES WALKER Department of Natural History, Glasgow Museums and Art Galleries Received August 1981 The thistle as an emblem of Scotland has early but spurious associations. Achaius, an unrecognisable, if not non-existent, king of the Piets did not found the Order of the Thistle, the early his- tory of which is unclear (Innes 1959; Malloch 1978) and needs further research. In the 11th century did an invading Dane step bare-footed on a thistle and howl to the alarm of the Scots? This is a good tale, often told from at least as early as 1829 (Denson 1832) without any stated original source. Can it be anything but pure myth? There are archaeological objects which might be taken to indicate early use of thistled decorations. These are the so-called thistle-headed pins and Norse thistle brooches of the 8th to 10th centuries in Scotland. However, the heads of the pins are not decorated in detail as thistles, while the brooches lodged in both the Hunterian and Kelvingrove Museums bear only the slightest superficial resemblance to thistle heads. Both these descriptive terms are misleading. The 1318 seal of Robert Bruce very probably does not show a thistle, contrary to the claim by Barker (1979) following Birch (1905); Stevenson and Wood (1940) make no mention of any thistle. The poem, written by William Dunbar, “The Thrissil and the Rose”, in honour of the marriage of Margaret Tudor and James IV in 1503 shows that the thistle was a Scottish emblem by the early 16th century at the latest. Queen Margaret (of Denmark, died 1486) possessed a bed or table covering embroidered with Glasg. Nat. 20 part 2 (1981) 102 thistles and her husband Janies III issued thistled coins. According to Innes (1959) the Earl of Orkney and Caithness is known to have been a Knight of the Order of the Thistle by 1470. All this takes the Scottish connection with thistles back with certainty at least to the mid to late 15th century. We cannot enlarge upon statements by Cameron (1900, p. 52) and Dwelly (1967, p. 215) that the Melancholy Thistle may have been the badge of James I (of Scotland). The badge of the Royal Stewarts as officially recorded by the Lyon Court is merely “Thistle” (Adam 1955). Botanical Identity What exactly is a thistle? The Oxford English Dictionary gives “The common name of the prickly herbaceous plants of the genus Carduus (N.O. Compositae, suborder Cynarocephalae) and several closely allied genera ( Cnicus , Cirsium, Onopordum, etc.) having the stems, leaves and involucres thickly armed with prickles, the flower-heads usually globular and the flowers most commonly purple ” This is perhaps too narrow a definition in its restriction to the Compositae and in its strong emphasis on prickliness. Howes (1975, p. 257) states “Name used for a range of herbaceous plants usually with prickly leaves and stems and flowers in heads”. This is better in its looseness; many plants not members of the Compositae are called thistles and one of the Compositae discussed here, Cirsium helenioides (Melancholy Thistle), has scarcely any prickliness. What exactly is the Scottish Thistle? There are many con- tenders, all Compositae. This article is the latest of many to attempt an accurate botanical recognition. The officially recommended English name of the large thistle Onopordum acanthium is now Cotton Thistle (Dony et al. 1974), which was the name used in the eighteenth and earlier centuries. However, there are many reputable botanical books published in recent decades which give the name Scottish or Scotch Thistle (Hutchinson 1948, Johns 1949, Keble Martin 1976, McCallum Webster 1978, Perring and Walters 1962). This is surprising in that few, if any, botanists have ever claimed that Onopordum acanthium is indisputably indigenous in Scotland and indeed the native status in the rest of Britain is very question- able. Flora Europaea (vol. 4, p. 245, Tutin et al. 1976) states 103 “Europe northwards to N. France and E. Russia but local in the extreme south; naturalised casual in the north The boun- daries between the native, naturalised and casual occurrence are hard to define”. There is a record of a fruit of Onopordum acanthium from Roman Silchester (Godwin 1975) but even that need not indicate that Onopordum acanthium is a natural member of the English flora. The Romans brought, deliberately or accidentally, many plants to Britain, including central Scotland (Dickson 1979). The Silchester Onopordum acanthium may only have been a garden escape, or casual weed as it still can be in both England and Scotland and it has been at least as early as the mid-eighteenth century, (Hope’s Hortus Siccus, anonymous 1907; Lightfoot 1777). Not a single one of the 18th century or earlier British botani- cal works we have consulted describes any species of thistle as the Scottish Thistle, not even works of Scottish origin. FIGURE 1. Thistles and roses from the frontispieces of Sibbald (1684). The plants are strongly conventionalized; qualities of both Grsium and Onopordum are shown by the thistle heads but the involucral bracts resemble those of Centaurea nigra (Knapweed). However, the stylisa- tion gives little botanical confidence. The leaves might be taken to resemble those of Onopordum but the poor quality of the rose leaves is such that the drawings cannot be taken as naturalistic. Though very stylised thistles appear on the frontispieces of the earliest of all Scottish botanical treatises (Fig. 1), Sibbald (1684) seems unaware of any particular Scottish Thistle but he did know of an English one! On page 17 of part two he lists (