Natural History Museum Library 000141895 /$r v I i .♦ * » * No. 49 the Journal of the LONDON NATURAL HISTORY SOCIETY EUROPEAN CONSERVATION YEAR 1970 Published : August 1970 Price : One pound • Post free • acae- THE LONDON MML HISTORY SOCIETY WHATEVER your interest in natural history — even if you are still a beginner — the Society will welcome you as a member. You are offered a wonderful oppor¬ tunity of extending your knowledge and increasing your enjoyment. The Society’s Area lies within a 20-mile radius of St. Paul’s and here most of its activities take place. Although so much of the area is covered with bricks and mortar it is a most exciting region with an astonishing variety of fauna and flora. The Society consists of Sections whose meetings are open to all members without formality. If you are interested in: archaeology, botany, ecology, ento¬ mology, GEOLOGY, MAMMAL STUDY, ORNITHOLOGY, RAMBLING, Or if yOU are a Young Naturalist there is a section ready to help you. We offer you . . . INDOOR MEETINGS Nearly every week throughout the vear with Films, Lectures and Discussions on all aspects of natural history. FIELD MEETINGS Led by experts, at week-ends and on summer evenings to visit “ good ” natural history places, often outside our Area. These excursions are very popular with beginners wishing to improve their knowledge. PUBLICATIONS The London Naturalist , published annually, a permanent record of the Society’s activities, including records of plants and animal life in the London Area. The London Bird Report, published annually, containing papers, facts and figures of special interest to bird watchers in London. Compiled bv the Ornithological Section which also issues a bi-monthly Bulletin (6s. Od. a year 10s. Od. non-members post free). LIBRARY A large selection of books and periodicals, many with special reference to London, now housed at Ealing Central Library and available for the use of members. READING CIRCLES Many important natural history journals enabling members who subscribe to these circles to read any of the journals at a fraction of the cost of an individual subscription. UNIVERSITY LECTURES With the co-operation of the University of London, Department of Extra-Mural Studies, courses of evening lectures during the autumn and spring. They are designed to meet the needs of members for more knowledge of any particular aspect of natural history. MEMBERSHIP AND SUBSCRIPTIONS MEMBERS ..... SENIOR MEMBERS .... JUNIOR MEMBERS .... FAMILY MEMBERS .... ENTRANCE FEE .... All members except family members receive and The London Bird Report. FIFTY SHILLINGS TWENTYFIVE SHILLINGS FIFTEEN SHILLINGS HALF THE APPROPRIATE RATE FIVE SHILLINGS one free copy of The London Naturalist All details may be obtained from : — THE MEMBERSHIP SECRETARY, MR. A. J. BARRETT, 40 FRINTON ROAD, KIRBY CROSS, FRINTON-ON-SEA, ESSEX THE LONDON \ \ *1. \ •V \J % '/> /o , NATURALIST the Journal of the LONDON NATURAL HISTORY SOCIETY No. 49 World List Abbreviation: Lond. Nat. Published August 1970 by the London Natural History Society and printed by F. J. Milner & Sons Ltd. Brentford, Middlesex LEONARD PARMENTER (1903 - 1969) LONDON NATURAL HISTORY SOCIETY Founded 1858 President: R. E. BUTLER, B.Sc., F.G.S. Honorary Vice-Presidents: C. P. CASTELL, B.Sc., J. B. FOSTER, B.A., R. C. HOMES, M.B.O.U., ERIC HOSKING, F.R.P.S., M.B.O.U., Rt. Hon. LORD HURCOMB, G.C.B., K.B.E., Miss C.E. LONGFIELD, F.R.G.S., F.R.E.S., M.B.O.U., E. M. NICHOLSON, C.B., M.B.O.U., R. M. PAYNE, F.R.E.S., J. H. G. PETERKEN, F.L.S., Mrs. L. M. P. SMALL, H. SPOONER. Honorary Librarian: R. A. SCOALES, M.A., A.L.A. Officers for 1970 Vice-Presiden ts : E. B. BANGERTER, B. L. J. BYERLEY, F.R.E.S., C. P. CASTELL, B.Sc., S. CRAMP, B.A., F.Z.S., M.B.O.U., R. W. HALE, V. F. HANCOCK, M.B.O.U., J. E. LOUSLEY. Secretary: P. C. HOLLAND Treasurer: A. J. BARRETT Joint Membership Secretaries: A. J. and Mrs. B. F. BARRETT, 40 Frinton Road, Kirby Cross, Frinton-on-Sea, Essex. Editor, London Naturalist: PAUL A. MOXEY, B.Sc., Dip. Cons., F.L.S. Editor , London Bird Report: P. J. GRANT Librarian: Miss H. BRITTON Programme Secretary: D. G. HALL Administration: Film Hire: P. J. Sellar, B.Sc., M.B.O.U.; Mapping Schemes: H. A. Sandford, B. Sc., A.D.E., M.Phil.; Minuting ( General Meetings): Miss M. E. Kennedy; Bookings: Miss M. E. Kennedy. Members of Council: Miss E. P. Brown, Miss D. C. Hersey, Dip.Geog., F.R.G.S., M.B.O.U., A. M. Hutson, Miss M. E. Kennedy, R. Kettle, B.A., D. Griffin, M.A., M.B.O.U., R. F. Moorman, F.G.S. , C. F. Sayers, P. J. Sellar, B.Sc., M.B.O.U., Mrs. A. G. Side, F.L.S., Mrs. H. M. Smith, Miss J. M. Stoddart, R. C. Vernon, M.B.E., Mrs. A. Warren. Information about the Society may be obtained from the Joint Membership Secretaries. CONTENTS PAGE Leonard Parmenter (1903-1969) Frontispiece Officers for 1969-70 3 Editorial... ... ... ... ... ... ... ... ... 5 Looking into the Past — R. E. Butler . Report of the Society for 1969 . 13 The Hindson Bequest — The President . 16 Botanical Records for 1969 — J. Edward Lousley . 17 London’s Lichens — J. R. Laundon . 20 The Behaviour of Common Carp and Crucian Carp as indicated by Angling Records — David Marlborough . 69 Observations on the return of fishes to a polluted tributary of the River Thames, 1964-69 — B. S. Meadows . 76 A Review of the Macrolepidoptera of the London Area for 1968 and 1969 — C. G. M. de Worms . 82 Ladybird Survey — Second Report — D. G. Hall . 90 Survey of Bookham Common: Twenty-Eighth Year — Progress Report for 1969 93 Short Notes : Mammal Recording . 104 Badger Corpses . 104 The Society’s Collections . 104 Flowers and Figures — E. M. Hillman . 105 Some Recent Temporary Exposures of London Clay in the London Area— Adrian J. Rundle and John Cooper . 113 Further Additions to the London Clay Biota of Oxshott, Surrey — Adrian J. Rundle and John Cooper . 125 Conservation Report, 1969 — Daphne C. Hersey . 127 Obituary: Leonard Parmenter, 1903-1969 . 130 A tribute to L. Parmenter— Cynthia Longfield . 131 Books ... ... ... ... ... ... ... ... ... 1 32 The Library . 135 Statement of Affairs at 31st October 1969 . 136 General Account and Publications Account . 138 EDITORIAL 5 Editorial ALTHOUGH this issue of the London Naturalist records the activities of our Society in 1969, it appears in European Conservation Year, 1970. It is for this reason that the E.C.Y. symbol appears on the cover, and that some passing comment is appropriate here. By the time this journal is published, the Strasbourg Conference will have receded into the past, European Conservation Year itself will have run more than half its course, and the problems of environment will have have been explained and debated in broadcasts, books, newspapers and magazines, and at a multitude of meetings throughout Britain and abroad. For London, indeed, the process began on December 16, 1969 at the Dinner given by the Corporation of London to launch European Con¬ servation Year in this country; since then, in the words of His Royal Highness the Duke of Edinburgh, speaking in the Guildhall that evening: “we are in changing times, as we are tirelessly reminded, and one of the charges is that today the words conservation and environment are bandied about like tennis balls at Wimbledon”. Some, indeed, have expressed the fear that we shall tire of the words before we understand their meaning. There are many aspects of conservation, and their sum is the concern for the overall environment; it w7ould be invidious to select any one as being more important than the others. Nonetheless, one particular aspect, nature conservation, is, and has long been, the particular concern of our Society. In the Greater London area wildlife exists by virtue of two facts: its ability to adapt to a changing environment on the one hand, and the extent to which remnants of semi-natural habitats survive in our parks, commons and open spaces on the other. The London Natural History Society is composed of people, living or working in London, who are interested in Natural History; since its formation in 1858 it has seen the metropolis expand from under three million persons to over seven million in 1969. With this growth in numbers has come the expansion of the built-up area and the consequent disappearance of the rural environs which harboured an abundance of plant and animal life and were well known to the earlier members of the Society. Today housing estates, in some cases already facing demolition, stand on the site of fields which, in the early years of this century, provided hay for London’s horses, and it requires a vivid imagination indeed to envisage the scene described by a poet of 1902: “Hendon and further out afield. Low water-meadows are his ken; And lonely pools by Harrow Weald, And solitudes unloved of men”. In these circumstances, it is hardly surprising that the Society showed an early interest in conservation. The history of this particular aspect of 6 THE LONDON NATURALIST, NO. 49, I97O our activities has been admirably documented by C. P. Castell in his papers, Nature Conservation in the London Area (Castell, 1947) and Post-War Progress in Nature Conservation in the London Area (Castell, 1954); the significance of his own personal role in this, as in so many other facets of the Society’s work, can never be sufficiently stressed. In more recent years, the reports of the London Nature Conservation Com¬ mittee reflect the Society’s continuing concern and vigilance, whilst the extensive programme of special lectures and meetings for 1970 itself records this Committee’s enthusiasm and effort. A full report on these activities will, of course, have to wait until 1971. The formation of the various County Trusts for Nature Conservation bordering on our Society’s area has in many ways eased the burden. Whilst the London Natural History Society includes the promotion of nature conservation amongst its aims, for the Trusts it is their prime function and one of their most important contributions has been the establishment and management of nature reserves in our Society’s area. Like the L.N.H.S., however, they are concerned also with records, since without a foundation of knowledge there can be no secure building of management practice. Thus, although the Trusts and our own Society overlap in interest and function, they are essentially complementary, and anything which weakens one weakens the other. As today conservation becomes increasingly complex, drawing on a wide range of skills and experience, voluntary bodies and local authorities are being drawn together in the planning process, so that organisations such as our own are more and more being asked for advice and comment. Wildlife is an integral part of our en¬ vironment, and the participation we are now offered in its planning is a responsibility the early members of the Society would have envied. Again, this year, pressure of papers have exceeded space available, with the result that, regretably, Part VII of Eric Groves’ Hemiptera- Heteroptera of the London Area will appear in the London Naturalist No. 50. This year, however, we publish three papers held over from the past : Flowers and Figures , by Miss E. M. Hillman, London's Lichens , by J. Laundon, and Some Recent Temporary Exposures of London Clay in the London Area, by Adrian J. Rundle and John Cooper. REFERENCES CASTELL, C. P., 1947. Nature Conservation in the London Area. Lond. Nat., 26, 17-41. — — - — , 1954. Post-War Progress in Nature Conservation in the London Area. Lond. Nat., 33, 6-20. LOOKING INTO THE PAST 7 Looking into the Past By R. E. Butler {Presidential address delivered on October 9th 1969 ) THE past has a potent appeal to most minds. Because of this, I am inviting you as naturalists, to take a look at a few aspects of it. We may consider the past in two parts, the longer part covers that enormous period of time which takes one back to the beginning, and brings one to within a million years or so of the Present Day. One may regard this as the field of the geologist, but even he is unable to trace earth history right back to the very beginning. The second and shorter part may be considered as dating from the arrival of man, himself a product of the story of evolution, but seemingly bent upon changing so much, and des¬ troying so much of his natural environment. In this part the geologist is still deeply concerned, but the archaeologist also takes a hand and plays a dominant role. How long life has existed on this planet of ours no one really knows. If we consider the earth to be 5,000 million years old then perhaps life has existed for half this time in some form or another. There are some people who think that life may be as old as the earth itself — possibly was there in the original primeval matter. The recent discovery of formaldehyde in the galaxy could point to this. One thing is certain, and that is that man has not been around for very long — possibly for only If million years. It was once suggested that if we represent the age of the earth by means of a clock, then man would have arrived at one minute before midnight. In looking into the past, recollections, images and interests are special to every individual. We, all of us, tend to wear blinkers and restrict the width of our interests, and so miss much which is concerned with the very field we are studying. To the farmers and gardeners, the success or failure of the current results of their labours in controlling Nature, depends on the past of a few months ago. To the leaders of field meetings in demon¬ strating Living Nature, “yesterday” could be as much the past as is last Spring or last year. To the archaeologist and the geologist the past is much more static, and has to be organised on to an historical type of basis. We certainly have better ideas today, compared with when Bishop Ussher made his notorious statement that the Earth was created in the year 4004 B.C. It was even suggested that fossils had been deliberately put into the rocks at the time of the Creation in order to confuse man. Fossil collecting goes back more than 3,000 years. Famous Greeks such as Hippocrates and Aristotle were interested in them. In round barrows on Dunstable Down there have been found remains of people dating back to the Beaker cultures of the Bronze Age. They had been buried with specimens of fossil sea urchins. For many years fossils were usually associated with the Great Flood of biblical times. Theories post¬ ulated that fossils had important scientific significance were found difficult to accept. Among the many pursuits that the remarkable man Leonardo da Vinci followed, was canal building. He came upon fossils when engaged upon 8 THE LONDON NATURALIST, NO. 49, I97O the construction of a canal across Northern Italy. He was convinced of marine submergence as the explanation for the beds containing fossils. It was, however, left to another canal builder in England, William Smith, living three hundred years after Leonardo da Vinci, to really pioneer the work of examining the natural history of the past. Smith made a great study of fossils and used them to interpret geology. Smith is often referred to as the “Father of English Geology”. His collections are preserved in the Natural History Museum at South Kensington. The year 1969 is of some significance as it is the bicentenary of his birth. However, it is not my intention to give details of the work and records of fossil collectors and naturalists of the past. Written accounts put down as events were taking place can only take us back a certain distance in time. I wonder how many naturalists looking into the past would turn to the translations of the Anglo-Saxon Chronicles. These contain entries relat¬ ing to natural events. One entry dated 1087 could perhaps be one of the first records of nature conservation is this country. It reads : — “He planted a great preserve for deer, and he laid down laws therewith, that whosever should slay hart or hind should be blinded. He forbade the harts and also the boars to be killed. As greatly did he love the tall deer as if he were their father. He also ordained concerning the hares, that they should go free. His great men bewailed it, and the poor men murmured thereat; but he was so obdurate, that he recked not of the hatred of them all; but they must wholly follow the king’s will, if they should live, or have land, or property, or even his peace.” The reference is of course to King William II and to the New Forest. The word “deer” may be “deor” meaning beasts in general (this is an observation made by the translators). I must not fail to mention the Roman writer and historian, the younger Pliny, who has left us an eye witness account of the eruption of Vesuvius on August 24th 79 A.D. This eruption was the one which buried Pompeii and Herculaneum. Pliny’s account is so detailed, that any volcanic erup¬ tion today that approximates in character to it, i.e. a stupendous blast of uprushing gas which rises to several miles and then spreads out into an expanding globular cloud, is called a Plinian type of eruption. Pliny only takes us back to Roman times. Of such times we have ample evidence, and can build up from it a more or less complete picture of what life was like during those times. All over our country are magnifi¬ cent remains of Roman cities, villas and farms; some provide us with evi¬ dence of the natural history as well. The Roman palace at Fishbourne, near Chichester, had a fine garden, and evidence of the plants which grew in that garden is to be seen from decorative drawings on wall plaster that have been recovered from the site. Evidence has also been uncovered there, which provides a clear picture as to how the nearby coastline has altered. Even ballast used by the Roman ships has been discovered, this consisted partly of granite brought from the Channel Islands. The arch¬ aeologist and geomorphologist must be relied upon a lot to take us back into prehistoric times before the Romans. Frequently Archaeology has been rejected as a subject having much to do with natural history. Earlier there may have been some truth in this up to a point, but modern arch¬ aeological techniques certainly have very close links with natural history. The biggest archaeological monument in Europe, Silbury Hill, has rec¬ ently been re-excavated. A full report is awaited. I wonder how many LOOKING INTO THE PAST 9 people have said “Well what did they expect to find"’ — I have heard this said on more than one occasion. Professor Atkinson, who directed the excavations, stated during one of the last programmes presented by BBC Television on the dig, that the archaeologist may by past experience have a “hunch” as to what is likely to be there, but he does not expect to find any particular thing. He deals with whatsoever he finds. Silbury produced no skeleton but a wealth of remains of insects, molluscs and plants. Radio carbon dating enables us to know how many thousands of years ago these creatures lived. At Silbury it has been possible to examine the former land surface covered up by man four thousand years ago. Pollen analysis in¬ dicates mainly grassland weeds; the presence of the remains of beetles and winged ants suggests the months of July and August when the old land surface was first covered, but the presence of winged queen ants narrows this down to the month of August. From evidence obtained from numerous sites we have considerable in¬ formation on the plants used by Palaeolithic man. One of our earliest pieces of evidence of vegetable foods is to be found in the carbonised hazel nuts discovered in the Farnham Pit dwellings. The Glastonbury lake dwellers were known to have made great use of wild plants — sloe and black¬ berry for food — moss for plugging cracks in their timber buildings — ferns and bracken for bedding — hair moss and osiers for basketry — certain fungi were used for tinder, whilst caraway and poppy seeds were used as delic¬ acies. We also know that certain succulent grubs and snails were appreci¬ ated. We find much evidence of the natural history of the past in peat deposits. After the withdrawal of the ice sheets at the end of the Ice Age, much of the soil had been removed from the higher areas, whilst on the lower lying areas glacial debris had been left as moraine and boulder clay, awaiting recolonisation by plants. Numerous lakes left by the glaciers filled up and became swamps. Southern England was probably at a slight¬ ly higher level then, than today, and became covered with swampy forest and peat bogs. Much of the floor of the North Sea is submerged forest. The peat and submerged forest contain much evidence of the past, part¬ icularly in the pollen grains which became fossilised. The pollen grains can be identified, whilst radio carbon present enables us to date them. The ice probably retreated for the last time about 8,300 B.C., and we passed from a glacial into a pre-boreal climate (cold and dry but becoming warmer) with birch as the dominant tree. By 6,000 B.C. having passed through a warm dry period, the country was enjoying an Atlantic type of climate (warm and wet) with alder, oak, hazel and elm trees growing successfully. By 3,000 B.C. the Mesolithic period had passed into the Neolithic, and the climate became sub-boreal (cooler and drier) with alder, oak, lime and ash. Climatic conditions continued to change through the Bronze Age and the Iron Age. By 500 A.D. — well into what are usually regarded as historical times the Atlantic type of climate had returned. The present day levels of the peat are used as arguments in proving that the British Isles are tilting — unfortunately this is not in favour of London. Nine sites in Britain, and two in Holland have been investigated, and it is shown that there has been a subsidence of East Anglia and Kent by 6 metres during the last 6,500 years. The temple of Mithras, discovered in 1953-54 on the Walbrook site, was well below present high water mark. Roman pottery discovered in Southwark was at levels 1*5 and 2 metres below present high water. The fact that the Thames is tidal today as far as 10 THE LONDON NATURALIST, NO. 49, I97O Teddington, whereas in Roman times it was less affected by tides, adds weight to the subsidence ideas. Going back into Glacial times, we are really getting back to the early days of man— a million years into the past saw the first ice sheets arrive. Much of Britain was icebound and south of the ice margins the vegetation was certainly of tundra type. However, the ice made several advances and retreats, and there were periods of better times — Interglacial periods. The story of one such interglacial period is preserved in the famous Hoxne lake deposits near Diss. At this locality there was a lake, and in its deposits are preserved the remains of animals and plants — of special interest are the fossil pollen grains. Going from the botton layers to the top of these deposits one can, with the aid of the pollen, trace a gradual warming up of the climate from the very cold arctic type to conditions which were certainly much warmer than our present day conditions. Then the reverse occurred and the climate cooled off again so in the uppermost layers the plants are back to those typical of an arctic type such as arctic birch. Much evidence concerning interglacial conditions was unearthed in London during 1957. During excavations for the foundations of the Uganda Government build¬ ings in Trafalgar Square, a wealth of material was found. Dr. A. J. Sutcliffe and others of the Natural History Museum investigated this mat¬ erial. Remains of animals included hippopotamus, the now extinct straight tusked elephant; rhinoceras, wild ox, red deer, fallow deer and lion. Over 1,300 specimens of land and river molluscs representing some 60 species were recovered. Among them was the pearl bearing mussel and a tiny snail neither of which live today in Britain but inhabit areas of South¬ ern Europe. These molluscs not only provide information on the climate of the past, but tell us quite a lot about the River Thames in those days. Numerous insect remains were discovered, along with many plants. Some of the plants such as the South European maple are certainly not native to this country today. I have made several references to radio carbon used for dating purposes. This, and other similar radioactive substances have become very import¬ ant. Nitrogen is an element whose atom normally has a mass of 14. Natural radiations convert some of the nitrogen atoms in the air into carbon atoms of the same mass. Carbon atoms normally have a mass of 12. The ratio of Carbon 14 to Carbon 12 appears to be fairly constant, and both types of carbon atoms are absorbed by plants during photosyn¬ thesis, so in the living plants this constant ratio between the carbon atoms is unchanged. With the death of the plant, absorption of carbon ceases, and the carbon 14 is not replaced to preserve the ratio. Cl 4 slowly decays. Now, we know that radioactive changes go on at speeds which are com¬ pletely unaffected by external conditions and that half of the original carbon 14 will have decayed in 5,568 years (the half life value). Three quarters will have gone after 11,140 years. Hence it is quite easy to date a piece of carbonised wood from its carbon 14 content. This radio carbon method is surprisingly accurate— the classic test for this was on a piece of wood from Qumran (A Dead Sea scroll locality) — this wood was known to date from about 68 A.D.— the radio carbon dating gave an age of 1,940 years. Carbon dating suggests that Stonehenge was constructed in 1860- 1560 B.C., the first phase of Avebury about 1700 B.C., and the extant barrow of Wayland Smithy was made in 2820 B.C. The geologist however, cannot go back very far with radio carbon, but he has other similar methods. Many minerals in the rocks contain the LOOKING INTO THE PAST 11 metal Potassium, the atom of which normally has a mass of 39 but there are some atoms of mass 40. These slowly decay into the inert gaseous element Argon which becomes trapped within the mineral crystals. The half life of Potassium 40 is 1,300 million years and so by examining the amount of Argon present one can deduce how much of the potassium has decayed. The element Uranium likewise decays very slowly and in a mil¬ lion years 1 gm of uranium will produce 1 /7000 gm of lead — hence uranium/ lead ratios in minerals may also be used for dating purposes. Such tests have been carried out on the ancient rocks of Scotland, and ages ranging from 740 million to 885 million years have been determined. No doubt the rocks from the Moon brought back by the Apollo missions have also been put to these tests. I will now return to fossils, which are one of our greatest assets for help¬ ing us to build up a picture of the past. A very large number of people become interested in geology simply because of fossils. Many youngsters collect fossils, and if they continue to do so into adult life, there is a good chance of their becoming fully fledged geologists. However there is much more to fossils than building up a massive collection. The scientific im¬ portance of fossils may be summarised as follows : — (i) They are the remains of prehistoric life, and often it is possible to build up a reconstruction of what the creature or plant actually looked like when living. (ii) They provide important information on evolution. (iii) They provide information about the rocks in which they are found, i.e. whether the sediment which formed the rock was laid down in shallow water or in deep water, in rivers, swamps or even in deserts. (iv) They provide information on the geography and ecology of the past. We know from fossil evidence that Alaska and Siberia were once joined — also Australia and Malaya — the separation of the latter may have been earlier than the former. (v) The distribution of shallow water molluscs help us to trace ancient shorelines. (vi) Fossils provide information about past climates. Both the Silurian and Jurassic periods in British geology are rich in corals, and so in those times warm shallow seas must have covered parts of the British Isles — corals generally need warm water. Fossil plants found in Greenland and Antarctica prove that these areas once enjoyed very warm climates. (vii) Certain fossils of limited time distribution are useful in correlating strata from one district to another. (viii) Some fossils are of economic value. Coal is mainly fossil material. Above all the geologist uses fossils to fix geological time (the fourth dimension of the earth’s past). The first rocks which contain abundant fossils are those of the Cambrian period reckoned to begin about 600 mil¬ lion years ago. This period starts off the great Palaeozoie era which lasted 375 million years. Major biological changes are taken by the geologist for fixing the beginnings and endings to the great geological eras. Large scale extinctions of many groups of animals and the arrivals of many new types provide the deciding factors. The trilobites and many groups of the bra- chiopods vanished to mark the end of the Palaeozoic, whilst the arrival of the true ammonites and newer types of brachiopods marked the start of the second great era, the Mesozoic. This era saw the ascendency of the rep¬ tiles culminating in the well known group called the dinosaurs. The Mesozoic lasted for 155 million years, and then again occurred massive 12 THE LONDON NATURALIST, NO. 49, I97O extinctions. The ammonites which had undergone rapid and often pecu¬ liar evolutionary changes just vanished. The dinosaurs which had roamed the Earch also vanished. The extinctions of great animal groups provides us with difficult biological problems which have never really been solved. As regards the dinosaurs, it has been suggested that large scale vegetation changes at the end of the Mesozoic may have killed off the herbiferous dinosaurs, and this in turn killed off the carnivorous ones that lived on them. This suggestion does not find much favour because in the Upper Cretac¬ eous it would appear that some dinosaurs were flourishing quite well on the newer types of vegetation. There is also the question of the heat control of their bodies — they had no protective covering to retain heat like birds and mammals. At the end of the Mesozoic, the climate became cooler and the dinosaurs could not cope. However, these creatures died out even in the warmer parts of the world. Some people have suggested that their great size indicated possibly an overactive pituitary gland but I must men¬ tion that not all dinosaurs were enormous and the small ones also became extinct. With the general decline in the reptiles, mammals and birds became important, and into the next great era the Caenozoic or Tertiary, the animals and plants are assuming the characters of present day forms. Man’s arrival some If million years ago is the last great biological time fixing event. Animal extinctions however continue, as for example with the Irish elk. The geologist does not rely entirely on fossils. One must appreciate that some rocks are without fossils and so other features must be looked for. Ripple marking can be fossilised; this occurs in shallow water, and can occur in deserts, but if one looks closer at the rock, if it is a sandstone, one can tell from the sand grains themselves whether they were deposited in a desert or under water. Desert sands show heavy attrition effects — they are often called millet seed sands. Rain prints and suncracks can be fossilised into the rocks — these would indicate possible mudflat con¬ ditions at the time of deposition. Elementary chemistry can be brought into the methods of delving into the past. During the Triassic peroid which opened the Mesozoic era, Britain was suffering rigorous conditions of a hot desert. Typical desert sands from that period were laid down as the Bunter sandstones of the Midlands — ironically these sandstones provide us with the best water bearing strata that we have in this country today. At times these deserts had areas of water. As these lakes dried up the waters dep¬ osited numerous minerals, among them calcium sulphate. Now calcium sulphate will crystallise as the hydrated salt forming gypsum under normal conditions, but if the water is fairly warm then the anhydrous salt will crys¬ tallise as anhydrite. In some places where these lakes existed we do in fact find deposits of anhydrite indicating a very warm temperature for the water. From Neolithic times and possibly earlier, ancient man must have un¬ wittingly helped in the spread of plants. The principal roads and tracks were chosen so that they followed the higher well drained ground i.e. the limestone and chalk outcrops such as the Jurassic scarp which runs from Yorkshire to the Cotswolds; the Harroway along the Chalk from Kent to Stonehenge and beyond; and the Icknield Way/Ridgeway route from the Wash to the Berkshire Downs, Marlborough Downs and beyond. In the clay vales away from these ridges, were dense oakwoods inhabited by such animals as the wolf, the bear and the lynx. These routes were lines of trade and must have greatly assisted in the spread of wild plants. Many of our common wild plants, it is agreed, have had a southern European LOOKING INTO THE PAST 13 origin and were probably introduced accidentally by the Celts and the Romans. Rightly or wrongly the Romans are credited with the accidental introduction of the pimpernell and the poppy, together with others such as fool’s parsley and the small stinging nettle. It is certain that they deliber¬ ately introduced the gardener’s curse, — the ground elder, which was prized as a medicinal herb. They also introduced hemlock and henbane, the lat¬ ter valued for its narcotic properties. Sir Edward Salisbury has pointed out that Roman roads with sloping sides to their embankments would have been eminently suitable for colon¬ isation by plants, as have our own railway embankments. To study the present in any field of natural history may seem a full enough task, but it remains incomplete without some knowledge of evolu¬ tion. Here, museum collections of fossil plants, birds, mollusca and other animals are invaluable: it is in Geology that we find the beginning and interdependance of all aspects of natural history, and the results of changes of climate or conditions are convincingly demonstrated. We examine moon rock; and map the geology of the ocean floors. From an aeroplane we are at times able to see much more of the geological structure, and certainly a lot of archaeological evidence. As seen from the ground alone, the study of man through the ages, shows what a destructive animal he is of the natural history surrounding him. Report of the Society for 1969 COMPARED with the figures quoted in the Report for 1968, the present membership in all classes, 1,202, seems to show an alarming drop of 527. Some loss of membership was expected arising from the necessity to review the subscription structure. This year has, in addition, seen the completion of a critical and prolonged examination of the membership records by the Membership Secretary. Such a review is essential from time to time but is an exacting task not lightly to be under¬ taken. As a result, however, it may be fairly claimed that the figure quoted, 1,202 made up as to:— Ordinary members 974 Affiliated members 23 Family members 82 Junior members 85 Honorary members 18 Life members 20 1,202 represents the membership of the Society as at October 31, 1969. The death is announced with regret of the following members during the year: Mrs. P. Bates, W. J. Kaye (the Society’s longest serving member), Miss K. Marks, Miss L. Mathieson (the Society’s second-longest serving member), H. Greenfield, H. G. Denvil and L. Parmenter, a former President. 14 THE LONDON NATURALIST, NO. 49, I97O So far as the Society’s administration is concerned, the year has been an exacting one, illness causing a serious gap for some months, but further expert assistance has now been embodied into the Secretariat and some of the accumulated work has been disposed of. Undoubtedly the most important task was the disposition of so much of the Hindson Bequest as has as yet been paid to the Society, a sum at October 31 amounting to £14,000. From the outset this bequest has been regarded as a capital asset and none of the monies available has been diverted to revenue accounts. The settlement of the bequest has not yet been completed, but in the meantime arrangements have been made with the Westminster Bank Trustee Department for the investment of £10,000. At Bookham Common, the soil analysis survey which suffered a serious set-back when illness overtook Mr. C. P. Castell has now been resumed under the Directorship of Mr. H. A. Sandford. A successful application has been made to the Carnegie Trustees for a grant towards the cost of this scheme. The Director is in urgent need of further assist¬ ance and will welcome workers able to help him and his team in this investigation. As reported last year, 1970 is to be European Conservation Year and your Council arranged to sponsor a special programme of activities in this connection. Mrs. L. M. P. Small has organised this with co-operation from the sectional officers and a very full and varied programme awaits us. During the year, the officers of the Archaeology Section ran into difficulties, finding themselves unable to fill gaps following resignations among their number, but a happy solution was found in the amalgamation of the section with the Geologists. The new joint section was formally inaugurated on November 19, 1969 and we can look forward to a healthy programme embodying activities of interest to adherents of both dis¬ ciplines. The Archaeology Section listing some interesting meetings, report with regret that none of them was well-attended. Work has continued during the year on the pottery found at Borough High Street. The work on post-medieval pottery having been completed expert assistance is being obtained for the Roman material. Thursday evenings, the Chairman leads work on the masses of pottery found this summer in Montague Close, Southwark and any members interested in pottery are invited to join. In view of poor attendances and the difficulty of finding officers, this Section asked the Geology Section to consider an amalgamation, and the respective Committees having formally proposed such action, the Council on September 18, 1969 approved the amalgamation of the two Sections. The Botanists are pleased with an increase to 37 in their average attendance at the three sectional meetings : an improvement on the figures for last year. A useful fact emerges from their report that informal meetings, always well attended, seem attractive to new members. Of the wide range of field meetings, the Whitsun Weekend held at Lyndhurst in the New Forest attended by 24 members was “happy and profitable”. The Section record their thanks to Mrs. Yule for her expert guidance and making freely available her knowledge of the Hampshire flora. The Ecologists have averaged an attendance of 34 at their three indoor REPORT OF THE SOCIETY FOR 1 969 15 meetings. Joint outdoor meetings have been held with the Herts. /Middle¬ sex Naturalists’ Trust and with the Entomological Section. They already have in mind their contribution to European Conservation Year 1970 as a Nature Trail at Bookham Common. Their report stresses that all records are important, and they ask all members of the Society to assist by sending records (mammals, fish, molluscs, reptiles and amphibians) to the appropriate addresses. The Entomologists held nine indoor meetings, but with the exception of a joint meeting with the British Arachnological Society which attracted an audience of over 60, of whom about half were Society members, in the main attendances were poor. It is hoped to arrange further joint meetings. A joint visit to Farthing Down with the Ramblers was well received but the same success did not attend a joint meeting with the Ecologists. Whilst the response to the Ladybird survey has not been as great as had been hoped, accent has now been placed on two of the commonest species (the 2- and the 7-spot ladybirds) and Society members are asked to assist in this survey. The Epping Forest Field Section strike a new note in their annual report by complaining of the lack of mud which is likely to cost them their reputation for rough and heavy walking. Neither of the fungus meetings was very successful because the specimens were undersized and dried up, but experience reveals that the August meeting is the more popular and successful of the two. Showing an increase over previous years, the average attendance at field meetings was 13. The Geology Section reports a varied and interesting year. The talks included one on agates with a distribution of samples. Successful field trips were led by members of the section: the highlight of the year probably being the Easter field meeting on the Isle of Wight during which there were one or two notable finds including the vertebra of an iguanodon. Two members of the section made the remarkable find of a fossil turtle skull at Abbey Wood, possibly the oldest complete turtle skull in Europe. The Ornithology Section held 9 formal indoor meetings with an average attendance of 90 to 100 members including, at one of the best attended meetings, a stimulating progress report on the Atlas Project. A joint meeting with the B.T.O. was arranged, followed by a buffet supper, the address being given by the President of the Cambridge Bird Club. The most successful meeting of the year attended by 300 people, was that held jointly with the R.S.P.B. at Caxton Hall on November 4, at which Bobby Tulloch gave an excellent talk, superbly illustrated about the Birds of the Shetland Islands. Eight informal meetings were held monthly through the winter, covering a variety of subjects and which were consistently well attended by an average of 40 members. The Section’s Annual Dinner was held in March, Mr. S. Cramp being the guest of honour who gave a most excellent talk on his expedition to Libya. A very successful programme of field meetings was arranged and these consisted of six weekend outings, 13 day coach trips and 41 whole or half day meetings. In addition, two weekends were specially arranged for junior members. Three of the weekends were based on Cley in Norfolk, one on Southwold, one on Weston-super-Mare and one on Dumfries. 16 THE LONDON NATURALIST, NO. 49, I97O All were successful from an ornithological point of view, particularly the weekend on the Solway. So far as whole or half day meetings were concerned, these were well attended and in many instances numbers of over 40 were present. Coach outings, which last year proved very popular and were usually over-subscribed, seem not to have been so popular this year. Coach outings to new venues are being arranged this year but rising costs necessi¬ tate watching the position of this activity. Three enquiries have been organised, covering the Black Redstart, gull flight-lines and the Atlas Project, which has again been the main research project for the year. The possible hazards of bird-strikes to jet aircraft are causing increas¬ ing concern as the air space around the major airports becomes more congested. The subject has assumed added importance recently in view of the enquiries into the siting of a new airport. One of the ways in which it was felt that the Section could provide some useful information towards the study of this problem was by recording the movement of gulls across the approach routes to London airport to and from their roosts on the reservoirs. A remark applicable to all sections is made in the report of the Research Committee, “The success of our research projects depends very much on the help given by members”. Behind a very modest report, the Ramblers hide what has obviously been an interesting year. Not surprisingly, since the subjects range from Thailand to the Bass Straits, the average of attendance at the indoor meetings remained constant with last year at 30. A wide variety of out¬ door meetings attracted a smaller average and varied from a cruise through the London Docks, to a visit to the Victoria and Albert Museum to see tapestries. The South West Middlesex Section have averaged 19 members at indoor meetings. Like the Ramblers, this Section has wandered far outside the Society’s area with lectures dealing with the birds and flowers of Austria and the botany of the Pyrenees. At outdoor meetings the numbers attending ranged between 3 and 30. Despite an increased subscription, the Section retains its membership of the Hounslow Council for the Arts. The Hindson Bequest Members will be aware of the substantial bequest made to the Society by the late Mr. M. T. Hindson. The final total of the bequest is still uncertain as further instalments are anticipated. It is Council’s intention that this money should be used for the lasting benefit of the Society, and considers that this will be best achieved by giving first priority to the acquisition of premises to serve as a permanent centre for the Society and its library. It may take some time to find premises suitable to our needs. In the meantime members will be kept informed of the progress made. R. E. Butler, President. BOTANICAL RECORDS FOR 1 969 17 Botanical Records for 1969 Compiled by J. Edward Lousley FOLLOWING several years with unfavourable summers, 1969 gave the botanists little cause for complaint. After a wet May, and cold spell in early June, the summer and autumn were dry and warm. The rainfall for the year at St. James’s was only 21-01 inches, 90% of the average, but there was no serious drought and few ponds fell to very low levels. This was due to the absence of excessive heat and the soaking early in the year. The number of records contributed was about the same and of con¬ siderable interest, but there was no outstanding new discovery. The most valuable features were the records from several members of the persistence of salt-marsh species in north Kent where the habitats by the Thames are changing rapidly, and the additions to our records for Hertfordshire and N. Essex. In this report “Tetrad” references, as used in the Mapping Scheme, are cited where available, and failing this 10-kilometer squares of the National Grid. In both cases these appear in brackets following the place names. The nomenclature is based on the List of British Vascular Plants (1958) prepared by J. E. Dandy, and for species in that List authors’ names are omitted to save space. V.-c. 16, West Kent From a small bit of chalk down above Longfield Station (66/T08), P. C. Hall reports Filipendula vulgaris , Dropwort. This is less than a mile from Pinden Farm, and may be the same locality as reported by Cooper in 1837. We have only one previous record for this species as found by our members in the part of our Area in Kent. On the same down there were trees of Sorbus torminalis. R. M. Burton sent a useful list from the eastern part of the Arsenal ground at Woolwich, now being developed as Thamesmead, and from Crossness (51/48). Near the latter he found Rumex palustris and F. J. Holroyde drew his attention to hundreds of plants of Thorn Apple, Datura stramonium at Thamesmead. Mr. Burton found one clump of Carex strigosa near the ornamental pond in Abbey Wood (51/48), and an uncommon alien grass Urochloa panieoides Beauv. on a refuse tip at Horn’s Cross (57/T74) whence J. R. Palmer also reports Rumex palustris. It is pleasing that Mr. Palmer was also able to find a single clump of Juncus maritimus persisting on Swanscombe Marshes (67/T06) and he also supplied an interesting list of cultivated shrubs regenerating from seed in the Downe area. Mrs. L. M. P. Small’s records include Musk, Mimulus moschatus , at New Eltham (47/T42). We are grateful to H. M. Pratt for his usual useful list of his observations in the Dartford district. V.-c. 17, Surrey A surprising discovery was the finding by Miss Ruth Hartas Jackson of a colony of a Marsh Orchis, Dactylorhiza praetermissa on Wimbledon Common. This was seen regularly until about thirty years ago in the Farm Bog but the new locality is in a different part of the Common (27/T20). She also found Hordeum jubatum L. on disturbed ground by 18 THE LONDON NATURALIST, NO. 49, 1970 the Kingston Road near Tibbett’s Corner (27/T22). This beautiful grass has been found by new roads in several counties in recent years and is probably introduced with grass seed mixtures. On a wall by a church in the Upper Richmond Road, Putney (27/T24) she found Geranium lucidum, a species which tends to favour churchyards but not previously found so far into London. Two ferns, Asplenium adiantum-nigrum and Phyllitis scolopendrium, from Mortlake parish-churchyard (27/T04) were localised by J. L. Gilbert with admirable precision as on the tomb of Henry Taylor who died in 1786! A grass on a bank near the Thames by Twickenham Bridge (17/T64) was determined for J. R. Palmer by Dr. A. Melderis as Bromus x pseudo - thominii P. Smith ( = B . thominii auct.). In April C. W. Ward showed me a magnificent patch of Common Club Moss, Lycopodium clavatum on Banstead Heath (25/T24). In October, R. Clarke sent a specimen of Cyperus eragrostis Lam. from a clay-chalk bank below a garden at Warlingham (51/T35) — a handsome sedge which has become established in the Channel Islands. V.-c. 18, South Essex It is over forty years since our last record of Long-leaved Sundew, Drosera intermedia in Epping Forest, and then only one plant was seen. This year it was refound and B. T. Ward reports 20 plants. The grid reference is suppressed as this species is not known elsewhere within the Society’s Area. The Purple Helleborine, Epipactis purpurata, was found by Mrs. L. M. P. Small in Epping Forest (49/T16) and her identification confirmed by Dr. D. P. Young. This is the first time this orchid has been reported to us from the Forest or the vice-county. From the Grays chalkpit (51/67), R. M. Burton noticed Pyramidal Orchid, Anacamptis pyramidalis and Dactylorhiza fuchsii, while Miss D. E. Woods found Orchis mascula in North Stifford Chalkpit (57/T88). From north of Grays (51/67) R. M. Burton reported the grass, Apera spica-venti. At the Exhibition Meeting of the Botanical Society of the British Isles a grass from our Area new to Britain was exhibited by Dr. A. Melderis. This was the American Bromus pumpellianus Scribn. which J. Whicker collected from the bank of a reservoir at Walthamstow in 1967. It is very closely allied to the Hungarian Brome, Bromus inermis from which it is dis¬ tinguished by the lemmas being pubescent near the margins. From Banbury Reservoir, Walthamstow (39/T50) Mrs. Small sent me a specimen of Rumex cristatus. V.-c. 19, North Essex This has long been a rather neglected part of our Area and Miss M. E. Kennedy and D. H. Kent, have again added a number of interesting species. These include Thalictrum flavum from the Stort Canal at Huns- don Mead (41 /TOO) and east of Burnt Mill Station (41/T40); Ranunculus trichophyllus also E. of Burnt Mill Station (41/T40); Apium inundatum abundant on the edge of a pond on Harlow Common (40/T88); and Anthemis arvensis in arable land near Langridge (30/T84). In fields and roadsides near the site of Roydon Hall (41/TOO) they found Chenopodium bonus-henricus and this was presumably the station reported by the Rev. P. H. Cooke in 1936. Miss Kennedy found Adder’s Tongue, Ophioglossum vulgatum in abundance in a water meadow at Hunsdon BOTANICAL RECORDS FOR 1 969 19 Mead (41 /TOO) and Genista tinctoria on the verge of a wood near Harlow Crematorium (40/T46) and Mr. Kent reports Pentaglottis sempervirens from the Town Park at Harlow (41/T40). V.-c. 20, Herts. Several members have made useful additions to our records for Hertfordshire. E. B. Bangerter added Avena fatua from near Colesdale Farm (20/T80), Epilobium roseum from north of Cooper’s Lane Road (20/T80), Agrostis gigantea from Jack’s Hatch (29/T64) and, with Miss Kennedy, Campanula trachelium and Mentha spicata from a gravel pit east of Hoddesdon Park Wood (30/T48). Miss Kennedy reports Mentha x niliaca from Cuffiey (30/T02), Melissa officinalis from Northaw (20/T82), Kickxia spuria from near Cassiobury Park (09/T86), and, with P.C. Holland, Arum italicum from Roxford Copse (31/T00). From Bushey Mrs. Small sent Oxalis europaea. V.-c. 21, Middlesex The joint field meeting of BSBI/LNHS members arranged by E. J. Clement and T. B. Ryves on October 4 visited refuse tips at Shepperton, West Drayton, Harefield and New Year’s Green and an account of the interesting adventives seen will no doubt appear in Watsonia. At the end of the day Portulaca oleracea was shown as a weed in flower beds near the Tower of London (38/T20). On waste ground at the junction of Harrow Road and Edgware Road (28/T60), Digitaria ciliaris (Retz.) Koel. ( = adscendens (H. B. K.) Henrard) was found by Don Turner and in Newgate Street, in the City (38/T20) R. M. Burton found Spergula arvensis. In Bishop’s Park, Fulham (27/T46) Mrs. W. Roberts noted Orobanche minor , and Mrs. J. McLean collected Epilobium lanceolatum (confirmed by D. H. Kent) from a road¬ side at Ealing (18/T80), the first record from the west part of Middlesex. Miss M. E. Young had Kickxia elatine in her window-box in Elm Park Lane, Chelsea (27/T68) and Humulus lupulus grew nearby. Mrs. Small reports Bunias orientalis from a canal path at Greenford (18/T22). On a visit of the Quekett Club to Stanmore, A. Le Gros found the leaves of a bladderwort, which is probably Utricularia neglecta, in ponds near Wood Lane (19/T62). We are grateful to the following for their contributions to our records during the year: — E. B. Bangerter, R. M. Burton, R. Clarke, E. J. Clement, Mrs. P. O. Dunkley, Mrs. M. C. Foster, J. L. Gilbert, Mr. and Mrs. P. R. Green¬ wood, P. C. Hall, P. C. Holland, F. J. Holroyde, Miss R. Hartas Jackson, Miss M. E. Kennedy, D. H. Kent, A. Le Gros, J. E. Lousley, W. Mackin¬ tosh, D. McClintock, Mrs. J. McLean, Dr. A. Melderis, J. R. Palmer, H. M. Pratt, B. R. RatclifFe, Mrs. W. Roberts, T. B. Ryves, Mrs. L. M. P. Small, D. E. Turner, B. T. Ward, C. W. Ward, J. Whicker, P. Widgery, Miss D. E. Woods, Miss M. E. Young, and Dr. D. P. Young. 20 THE LONDON NATURALIST, NO. 49, I97O London’s Lichens By J. R. Laundon Department of Botany, British Museum ( Natural History ) This “Glorious and Antient City . . . should wrap her stately head in Clowds of Smoake and Sulphur, so full of Stink and Darknesse” — J. Evelyn, Fumifugium (1661). CONTENTS Synopsis 20 Introduction 21 Topography 23 Air Pollution and Lichen Distribution 24 Habitats 30 Conservation 37 Lichen Flora 39 Acknowledgements 67 References 67 SYNOPSIS The past and present lichen flora within a radius of 16 kilometres from Charing Cross, the official centre of the monocentric conurbation of London, is described and analysed. The land-use of this Area comprises Central London, the Inner Urban Ring, the Suburban Ring, and three small “wedges” of the Green Belt Ring. Air pollution by sulphur dioxide is the chief factor affecting the lichen flora. Early lichen records prove that this pollution was restricted to the small built-up part of London before the early nineteenth century, and that it spread over the whole Area around the middle of the nineteenth century to cause serious damage to the lichen vegetation. Since the curtailment of London’s expansion in 1938 the continuous decline in the lichen flora appears to have been halted. At present the ground-level concentration of sulphur dioxide has remained fairly constant, and as a result there has been little recent change in the lichen flora. At present the largest numbers of species are found in north-west London in and near the Totteridge Green Belt and across south London, excluding Croydon, whilst the smallest numbers of species are found in the City and East End. Individual species, several of which have been mapped on the one kilometre grid, are either ubiquitous, circumurban, disjunct in an arc from north-west to south-east (via west and south), or south¬ western heathland, in distribution. 165 species have been recorded, of which 71 have been seen since 1950. The numbers of lichen species increase at advancing distances from the centre of London. 68 per cent of the present lichen flora occurs on calcareous substrata, which are favourable because of their high pH, as a result of which the sulphur is converted to a less toxic form. The good lichen flora of the remaining areas of heathland proves that terricolous lichens are able to survive in moderately polluted districts, probably because LONDON’S LICHENS 21 of the narrow layer of purer air which occurs over urban turf. 65 per cent of the flora occurs on memorials in churchyards and cemeteries, chiefly on limestone in the former, where bird excreta promotes nitrophilous communities, and where some species survive as relics, unable to colonise new surfaces. Only 11 per cent of the flora survives in woodland, this lichen habitat being the most adversely affected by air pollution. Lichen conservation requires a reduction in sulphur dioxide con¬ centration, and the preservation of surviving semi-natural vegetation, important old limestone churchyard memorials, and old walls. The detailed records on which these conclusions are based are given under the heading “Lichen Flora”. INTRODUCTION The rapid increase in the population of the world results in an in¬ creasing amount of rural land being utilised for urban development. When urbanisation occurs, and rural habitats are destroyed, restricted or altered, many plants and animals are lost, whilst others are able to adapt themselves to the new environment and therefore manage to survive. Species associated with man-made habitats become established, replacing those which have disappeared. For planning and conservation it is important to know the changes in wild life which are to be expected when urbanisation takes place. Comparative studies of the flora and fauna of rural areas with those of existing towns may provide many of the answers. The monocentric conurbation of London is especially suitable for studies of wild life in a completely urban environment, because of its large size and because of the diversity of habitats within the built-up area. This study of the lichen flora has been carried out strictly within a radius of 16 kilometres (9-9 miles) from the official centre of London, namely the statue of King Charles I at Charing Cross, on the south side of Trafalgar Square, Westminster. The perimeter of the circle passes through Enfield, Woodford, Barking, Woolwich, Bromley, Croydon, Kingston, Isleworth, Harrow on the Hill, and New Barnet (Fig. 1). This includes 804 sq. km. (310 sq. miles), almost wholly built-over and all within the administration of Greater London. It is subsequently referred to as the Area. This account of the lichen flora includes a digest of my paper in The Lichenologist (Laundon, 1967), excluding sociology, history of lichen study, introduced and excluded species ; the editor of The Lichenologist is thanked for his permission to make extensive use of the earlier article. This present work gives more detailed consideration to the distribution of lichens in London in relation to air pollution, incorporates recent records, and includes more locality data than was possible in the earlier study. Since The Lichenologist article was published, 45 old churchyards not previously examined were visited in order to obtain better distri¬ butional coverage. Nine species, Buellia canescens, Catillaria lenticular is, Lecanora contorta , L. polytropa, Lecidea fnscoatra , Parmelia sulcata , Polyblastia dermatodes, Stereocaulon nanodes and Toninia aromatica have been added to the present lichen flora of the Area, and the percentages previously published have been adjusted accordingly. These additions are chiefly of species long present but not previously found, although it is possible that Buellia canescens , Parmelia sulcata and Stereocaulon nanodes 22 THE LONDON NATURALIST, NO. 49, I97O vm GREEN BELT SUBURBAN RING INNER URBAN RING CENTRAL LONDON Fig. 1. Map of the Area showing the land-use of the London boroughs. The thick lines mark the boundaries of the boroughs and the River Thames. The corresponding names to the official numbers of the boroughs are given on p. 40, whilst the City of London has no number. The borough boundaries are drawn from a map published by the Evening Standard. The Figure is reproduced with permission from The Licheno/ogist. LONDON’S LICHENS 23 may be recent arrivals. The last two are the most interesting of the new records. The single Parmelia sulcata plant was found by E. T. Rose on concrete coping in Haringey, which is one of the more polluted boroughs in the Area; this species is predominantly corticolous in south-east England, but is unlikely to occur today on bark in the Area. Stereocaulon nanodes has only recently been found in Britain in rural Somerset and Teesdale, and therefore its occurrence in an urban area is of special interest. Only two old records additional to The Lichenologist account have been discovered. TOPOGRAPHY In medieval times the only built-up part of London was the City, whilst Westminster formed an isolated precinct further up the River Thames. “Farther afield the open country stretched away on all sides, dotted with villages, hamlets and manor houses, much as in parts of England where no great city lay” (Pevsner, 1952, p. 13). Expansion along the River took place during the 16th and early 17th century so that Westminster and the City became linked by continuous buildings, which also extended eastwards to Stepney. By the middle of the 18th century most of Westminster and parts of Kensington, St. Marylebone, Holborn, Finsbury, Shoreditch, Bethnal Green, Stepney and Bermondsey had been built over. In the early 19th century huge new docks were built in the East End and vast slum housing formed around them. Later the con¬ struction of railways, tramways and piped water supply enabled London to make much more rapid growth so that most of the old county of London, excluding parts of the south-east, had become built over by the early twentieth century, and the Inner Urban Ring (Fig. 1) completed. Between the World Wars, aided by the development of electric railways, new suburbs were built to more spacious standards all around London, thus creating the Suburban Ring (Fig. 1). In 1938, The Green Belt (London and Home Counties) Act was passed which halted further extensions of London, and ensured that a rural zone encircled the urban area. The Act “was passed to preserve from industrial or building development areas of land in and around the administrative county of London in the interest of the health and amenity of persons living in this county” (Burrows, 1950, p. 229). The Town and Country Planning Act of 1947 ended almost all uncontrolled development in Britain by making new building subject to planning permission. This Act has been effectively used to ensure the survival of the Green Belt, and to contain London to the boundaries reached in 1938 except for some infilling. This growth of London over a long period has resulted in distinct types of development (Abercrombie, 1945, p. 22) forming irregular rings (Fig. 1): 1. Inner Urban Ring. This comprises that part of London which was built over before the First World War in 1914, and extends from about 10 kilometres on the west side of the centre of London (Charing Cross), to about 16 on the east. It is characterised by high density Victorian terraced housing with a maximum of 75 to 200 persons to the acre (0-00405 sq. km). The housing is particularly characterised by the use of sash windows and the presence of projecting rooms at the rear. The chief industrial areas are Lea Valley — Lower Thames Side, Wandle 24 THE LONDON NATURALIST, NO. 49, I97O Valley and parts of north-west London. In this study Central London, defined by Abercrombie {op. cit .) as the “Commercial, Administrative and Cultural Centre of Greater London”, and bounded by Euston, Aldgate, Waterloo and Green Park (Fig. 1), is separated from the Inner Urban Ring. The whole of Central London and almost the whole of the Inner Urban Ring occurs within the Area. 2. Suburban Ring. This includes that part of London which was built over between 1918 and 1938, and extends from the Inner Urban Ring to a radius of about 19 kilometres from the centre of London. It is characterised by low density mainly semi-detached housing, with sizable gardens at front and rear and wide, tree-lined roads with asphalt or grass verges. The housing is particularly characterised by the use of casement windows and the absence of back projections. The maximum density is 30 to 50 persons to the acre (0-00405 sq. km). The inner part of this Ring occurs within the Area. 3. Green Belt Ring. This includes that part surrounding London from which building has been prohibited since 1938. It occupies a zone extending from the Surburban Ring to a radius of about 32 kilometres from the centre of London. It is characterised by its predominantly rural character, which varies from unspolit open countryside to the horrors of subtopia. The Green Belt is represented in the Area only in north London, by the “wedges” of countryside of Oakwood, Totteridge and Walthamstow (Epping Forest) (Fig. 1). The vast size of the built-up area of London affects the climate. Reduced winter sunshine, higher temperatures in almost all times and lowered humidities are amongst the characteristics of London in com¬ parison with the surrounding countryside. Chandler in Coppock & Prince (1964, p. 47) reports that “throughout the year the differences in minimum temperatures in central districts and in the country areas around London average 1-9°C (3-4°F) by night and 0-6°C (1T°F) by day, but on individual nights the difference may be as much as 9°C (16°F).” Air pollution, which might also be considered as part of the climate, is discussed below. The low rainfall of between approximately 53 and 74 centimetres (21 to 29 inches) makes London unfavourable for oceanic lichens. Much of the soil overlies London Clay, but some low hills of sand and gravel occur on which heath communities are developed. Outcrops of hard acid rock are absent, and the chalk within the Area forms only a short narrow strip in the extreme south which has been built over. The whole of the land is below 150 m. in altitude. AIR POLLUTION AND LICHEN DISTRIBUTION In 1273 the burning of coal in London was prohibited as being “pre¬ judicial to health” (National Society for Clean Air, 1968, p. 46), but this law was later relaxed. In 1955 coal burning was again prohibited by declaring the City of London a smokeless zone, the first to be established in the Area. Until the 19th century air pollution was largely confined to the built-up parts of London, where its undesirable characteristics had been frequently commented upon over the preceding centuries. The impact of the Industrial Revolution resulted in the spread of pollution London’s lichens 25 far beyond London and other cities so that the whole of the air over western Europe is now contaminated (see Junge, 1963, pp. 364-365). The Clean Air Act of 1956 enabled local authorities to establish Smoke Control Areas, which may be entirely smokeless (i.e. smokeless zones) or may make certain exemptions or impose special conditions. Sulphur dioxide is not controlled by the Act, except for a provision to promote its discharge through higher chimneys. At present 63% of Greater London is covered by Smoke Control Areas, and the whole programme should be completed by 1978. The establishment of Smoke Control Areas in districts of older houses has been shown to lead to reductions in smoke concentrations of up to 45%, and reductions in sulphur dioxide concentrations of up to 20% (Anon., 1968, p. 55). Over London as a whole, significant changes are taking place in both the emissions and the concentrations of air pollutants. The rapid and widespread introduction of Smoke Control Areas, together with the dramatic decline in domestic coal consumption, has led to both the emissions and ground-level concentrations of smoke in London being reduced by about two-thirds between 1956 and 1965 (Anon., 1968, p. 50). The emission of sulphur dioxide has increased by about 30% between 1952 and 1965, partly due to increased fuel consumption by the electric power industry. However the ground-level concentration of sulphur dioxide in London has remained fairly constant, partly because large quantities are dispersed from tall chimneys into the upper atmosphere. Smoke pollution at any point depends on the density of the population, and on the coal consumption per head of population, in a relatively small area surrounding that point (Williams, 1960), whilst sulphur dioxide pollution shows no strong correlation with population density, because of the large emissions from industrial and electricity works. The approxi¬ mate average concentration of sulphur dioxide pollution for the year ending March 31, 1958 for the Area is shown in Fig. 2. All pollution shows a similar proportional annual variation, so that the depicted pattern applies in all recent years. The heaviest pollution of sulphur dioxide occurs in central London, with high concentrations to the east and west and lower levels to the north and south. Entirely accurate distribution maps of average pollution levels over large areas are generally considered to be impossible to draw. The predominance of westerly winds appears to have little overall effect on the distribution of sulphur dioxide pollution in London (see Department of Scientific and Industrial Research, 1945, for a discussion of this same phenomenon relating to Leicester). Air pollution is the chief factor affecting the distribution of lichens in London. Lichens accumulate a wide range of substances from water (usually rainwater) passing over their thallus, and it appears that when an area becomes polluted, thalli also absorb contaminating substances and so build up lethal concentrations (see D. C. Smith, 1962, p. 562). Rao & LeBlanc (1966), however, consider that pollution directly harms the algal symbiont, thus impairing the metabolic processes in the lichen. Whatever the truth, the polluted air of towns prevents many species of lichen from becoming established. Smoke, carbon monoxide, sulphur dioxide and grit and dust are the chief air pollutants, and it is the sulphur dioxide which appears to be the one which is harmful to lichens. A correlation between the numbers of lichen species present and the con¬ centration of sulphur dioxide in the air is demonstrated by Skye (1958, p. 159, Fig. 6; 1964, p. 330), and by Gilbert in Goodman et al. (1965, p. 42), 26 THE LONDON NATURALIST, NO. 49? 197° Fig. 2 London's lichens 27 who also shows a lack of correlation between the lichen flora and the level of smoke pollution. One kilometre grid maps of the London distribution of lichens show a direct relationship with sulphur dioxide levels (Fig. 2). Gilbert {op. cit., p. 43) shows that the sulphur content of the thallus of Parmelia saxatilis increases considerably as the quantity of sulphur dioxide in the air becomes greater. Grit and dust, which frequently cover thalli in towns between rain, may not be harmful in themselves, because roadside dust frequently covers lichens in rural areas and nitrophilous species appear to thrive on it (see Barkman, 1958, p. 103; Gilbert, op. cit., p. 40). The absence of many lichens from towns cannot be solely attributed to the lower relative humidity (see Chandler, 1967), as Rydzak (1959) has claimed (see Laundon, 1967, p. 283). The lichen records for the Area dating back to the late 17th century indicate the effects of air pollution on the lichen flora at different times. Forster's late 18th century records of such toxiphobous lichens as Anaptychia ciliaris, Arthonia radio ta, Arthopyrenia spp., Candelaria concolor, Gr aphis scrip ta, Lecanora pallida, Lecidea limitata, Opegrapha atra, Phaeographis dendritica, Thelotrema lepadinum and Usnea spp. from tree boles in and around Walthamstow, 1 1 kilometres from the centre of London, prove the lichen flora to have been unaffected by air pollution during this period. Therefore air pollution affected the lichen flora only in the small built-up area of London before the early 19th century. In 1865-68 and 1881-82 Crombie visited the Walthamstow district and other parts of Epping Forest and found that the lichen flora has declined markedly due to the spread of pollution, whilst “about Hoe Street, Walthamstow . . . where numerous species were collected by Forster . . . we would at present vainly search for any in a fully-developed condition” (Crombie, 1885, p. 74). Indeed, Crombie {op. cit., pp. 56-70) recorded no lichens at all from Walthamstow, although a few species were doubtless present in St. Mary’s churchyard, since they still survive there today. By 1881 Crombie {op. cit., p. 71) noted that lichens which “were both general and plentiful” in Epping Forest in 1865 were “now to be seen only here and there in very small quantity”. Thus the main decline in London’s lichen flora appears to have taken place under the major impact of the Industrial Revolution around the middle of the 19th century, when polluted air first spread far beyond the built-up area. During and after the late 19th century the lichen flora continued to decline as London expanded, but at a much slower rate. As late as 1929-33 specimens of Parmelia were collected in Richmond Park. The Fig. 2. Distribution of lichens in order of “increasing sensitivity” to air pol¬ lution by sulphur dioxide. A — Candelariella medians , B — Caloplaca heppiana , C — Physcia orbicularis , D — Xanthoria parietina (agg.), E — Physcia adscendens, F — Physconia grisea. The closed circles represent post- 1950 records from 1 km grid squares, whilst the open circles represent pre-1950 records; some old records are excluded because of lack of precise localities. The lines show the average concentration of sulphur dioxide in microgrammes per cubic metre, the inner being equivalent to 10 parts per 100 million, and the outer to 5 parts per 100 million, from April 1957 to March 1958. Where these lines are broken there is uncertainty as to their precise location. The wavy line across the centre denotes the River Thames. The sulphur dioxide levels are taken from Chandler (1965, Fig. 30) with permission, and the London Natural History Society's Recording Map is used as a base. 28 THE LONDON NATURALIST, NO. 49, I97O curtailment of London’s expansion in 1938 through the passing of The Green Belt (London and Home Counties) Act has brought relative stability to the lichen vegetation of the Area, and later changes have been minimal. This is because all new urban development results in a local increase in air pollution, and the containment of London has prevented any major extension to the area of pollution. In recent years sulphur dioxide concentrations have remained fairly constant and there has been little change in the lichen flora. A few minor improvements indicate that the long period of decline since the early 19th century may have been finally halted. At Holland Park (Kensington and Chelsea) Lecanora conizaeoides was scarce on tree boles in both 1953 and 1967 in the northern section of planted woodland, but whereas it was seen on only two boles in the public walks in 1953, small thalli occurred on 14 in 1967. No change in the status of the lichens in the Central Parks has been observed, but green algae are increasing on tree boles. Out of a total of 165 species recorded for the Area, 71 have been observed since 1950. Nearly all of those which have not been refound are now extinct. It appears likely that the total number of lichens in the Area in the early 19th century exceeded 200, for the early botanists frequently ignored saxicolous lichens because of collecting difficulties. The decline to the present 71 is primarily due to the increase in air pol¬ lution, but the destruction of suitable habitats accounts for some of the losses. It appears that any small changes in the lichen flora in the immediate future will be because of changes in land-usage, and not because of changes in pollution levels. The present distribution of lichens in London is an indicator of the concentration of sulphur dioxide in different localities. In places where few species occur sulphur dioxide levels are high, but where a number of lichens are present the sulphur dioxide pollution is less severe. The present numbers of lichen species recorded in the London boroughs are shown in Fig. 3; terricolous records are excluded because these are con¬ centrated in the south-west of London in relict heathland, and their distribution bears little relationship to air pollution. The following conclusions can be drawn from the map : 1 . There is no one part of the Area which has a very rich lichen flora in comparison with the remainder. 2. The largest numbers of species are found in north-west London in and near the region of the Totteridge Green Belt (Fig. 1), and across south London, excluding Croydon. Croydon has much high density Inner Urban Ring housing and the Waddon industrial area, and would therefore be expected to have a poorer flora than the neighbouring pre¬ dominantly Surburban Ring boroughs. 3. The largest numbers of species occur in the least sulphur dioxide polluted parts of London. 4. Low numbers of species occur throughout the inner districts, corresponding largely to the Inner Urban Ring (Fig. 1). 5. The smallest numbers of species are found in the City and East End, where there is high air pollution. Studies of the present distribution of individual species, maps of some of which are shown in Fig. 2, indicate that the following types of lichen distribution occur in London : 1 . Ubiquitous species. This group comprises lichens which are found London’s lichens 29 16 -25 36 -45 26-35 Fig. 3. Map showing the present numbers of lichen species, excluding terri- colous records, found within the Area in the London boroughs. 30 THE LONDON NATURALIST, NO. 49, I97O throughout the whole of London and which can therefore withstand very high levels of air pollution. Leccmorci dispersa is the only representative of this group. 2. Circumurban species. This group consists of lichens which have an orbicular distribution around central and east London from where they are absent because of the high air pollution. Some species ( e.g . Caloplacci citrina, C. teicholyta , Candelariella medians (Fig. 2a), Lecanora conizaeoides ) are completely circumurban, whilst others which are more sensitive to pollution {e.g. Caloplaca heppiana (Fig. 2b), Physcia caesia, P. orbicularis (Fig. 2c) and Rinodina subexigud) are circumurban apart from their absence from the low-lying eastern districts of Newham, Barking and Woolwich, which are polluted from industrial Lower Thames Side. 3. Disjunct species. This group comprises pollution-sensitive lichens restricted to an arc from north-west to south-east London, via west and south. The species {e.g. Lecidea lucida, Physcia adscendens (Fig. 2e), Physconia grisea (Fig. 2f) and Xanthoria parietina (agg.) (Fig. 2d), chiefly represented in the Area by X. aureola) are scarce in scattered localities within the arc. 4. South-western heathland species. This group consists of terricolous lichens now confined to the acid heaths of south-west London. The species {e.g. Cladonia cocci f 'era, C. floerkeana, Cornicularia aculeata (for distribution map see Laundon, 1967, Fig. 2a)) are not restricted by air pollution like the circumurban and disjunct species, but by the occurrence of suitable habitats. HABITATS The survey of the Area shows that the popular view that London is devoid of lichens is incorrect. However the present total of 71 species is not large when compared with the 73 species recorded recently from the small area of Bookham Commons (Laundon, 1958), situated only 29 kilometres from the centre of London. The Bookham Commons survey covered only 1-54 sq. km in comparison with the present area of 804 sq. km. All post- 1950 records are considered as belonging to the present, and are analysed in relation to the London Rings, distance from the centre, substrata and habitats. The distribution in relation to air pollution has been discussed above. A. London Rings The London Rings have already been described, and the left-hand columns of Table 1 show their present lichen flora. One one species (1 %) of the total London lichen flora, namely Lecanora dispersa , occurs in Central London. L. dispersa is also the only lichen occurring in Central New York (Brodo, 1966, p. 435), and it is evident that New York and Lon¬ don have the poorest lichen flora for their central areas of any towns on record. Their large size and high sulphur dioxide levels over a wide area probably account for this poverty. 45 species (63% of the flora) occur within the Inner Urban Ring of London, or on open spaces on its fringe, which is a high percentage for land built over before 1914. Predictably 64 species (90 %) of the lichens in the Area occur in the Suburban Ring, where lower levels of pollution predominate. Records from the Green Belt Ring are not considered here, as such a small portion is included within the Area. Bacidia sabuletorum, Chaenotheca ferruginea and Parmelia physodes have been recorded from the Area only within the Green Belt Ring. 31 London’s lichens Table 1. The present lichens in the London Rings (excluding the Green Belt Ring) (left-hand columns) and their presence ( + ) in concentric circles drawn from the centre of London at Charing Cross (right-hand columns). C = Central London; I = Inner Urban Ring; S = Surburban Ring 0-2 2-4 4-6 6-8 8-10 10-12 12-14 14- S Acarospora f us cat a + S Bacidia chloroeocca + S B. herb arum B. sabuletorum 4" S B. umbrina -b + S Buellia canescens + S B. punctata + I S Caloplaca aurantia -r 4- T I s C. citrina 4- -f -t- + 4- + I s C. decipiens + 4- 4- + I s C. heppiana -f -r + 4_ + I s C. holocarpa + + + s C. murorum 4- + I s C. teicholyta -r + + 4- + I s Candelariella aurella -r 4~ + + 4- + I s C. medians 4- 4“ -f + 4- + I s C. vitellina -f ~r + 4- + I s Catillaria lenticularis + + + Chaeonotheca ferruginea + I s Cladonia bacillaris + 4~ + I s C. chlorophaea + + -f + 4- + I s C. coccifera -r + + I s C. coniocraea + + -r T 4- + I C. crispata -r I s C. fimbriata T 4* + + 4- + I s C. floerkeana -r + 4- -r I s C. furcata -f -f + I s C. impexa C. macilenta + + I s C. pyxidata + 4- s Collema crispum + I s Cornicularia aculeata -f + 4- I s Lecania erysibe -r + -f + + -f + s Lecanora atra I s L. calcarea -r + 4- + s L. campestris 4- I s L. conizaeoides + 4~ T -f + 4- + I s L. contorta + + I s L. dispersa 4~ ~r + + + 4- + I s L. muralis + -f + + + 4- + I s L. polytropa 4 + I s Lecidea coarctata “T 4 4- + s L. fuscoatra + I s L. granulosa -f 4 + I s L. lucida 4 4- + I s L. stigmatea + 4 4- + s L. sulphurea T I s L. uliginosa -f 4 4- + I s Lepraria incana 4~ + + 4 4~ + s Ochrolechia androgyna Parmelia physodes ~T~ + s P. sulcata + I s Physcia adscendens + + I s P. caesia -r -j- 4 4- + s P. nigricans 4- I s P. orbicalaris + 4 4~ + s Physconia grisea + s Polyblastia albida + I P. dermatodes 4 s Protoblastenia rupestris 4 + I s Rinodina subexigua + -r 4 4- + I s Sarcogyne regularis -r 4- + I Stereocaulon nanodes ■f* I s S. pile a turn -f. + 4 4- -j- s Thelidium decipiens + s T. incavatum + s Toninia aroma tica 4- + I s Verrucaria muralis -f 4- + I s V. nigrescens + _L 4 4- + s V. viridula 4- + I s Xanthoria parietina (agg.) + 4 4- + 45 64 Total 3 9 10 19 39 38 42 59 63 90 % 4 13 14 27 55 54 59 83 32 THE LONDON NATURALIST, NO. 49, I97O B. Distance from the Centre Concentric circles at two kilometre distances from the centre of London (Charing Cross) were drawn on Ordnance Survey Maps and the dis¬ tribution of lichens within each circle was plotted on the right-hand columns of Table 1. The majority of corticolous and saxicolous species occur at several localities within a particular circle, whilst terricolous lichens are concentrated in south-west London where relict heathland survives. The results from the Table show that there is an increase in the numbers of species at advancing distances from the centre of London. This is correlated with the progressive average decline in pollution levels, housing densities and age of urbanisation at increasing distance from the centre of London. C. Substrata The present lichen flora on the five types of substrata which are present in the Area is shown in the left-hand columns of Table 2. Calcareous soil is absent as a lichen substrate. Calcareous stone includes limestone, concrete, mortar and asbestos-cement sheeting, whilst acid stone includes brick and sandstone. Calcareous stone is by far the richest substratum for lichens with 48 species (68 %), because of its high pH value. Gilbert (1968, p. 15) suggests that a high pH influences the degree of ionisation and rate of oxidation of sulphite ions, so as to render them less harmful to lichen vegetation. All other types of substrata support considerably fewer lichens. 21 species (30%) occur on acid stone whilst acid soil supports 15 (21%). Although air pollution is harmful to the lichen flora on acid stone, the list of records suggests that most acid terricolous lichens are unharmed. At Putney Heath, where there are extensive areas of heather ( Calluna vulgaris), the lichen flora is essentially similar to that found on unpolluted heaths, with Cladonia coccifera , C. crispata , C. floerkeana, C. impexa and Cornicularia aculeata. Gilbert (1968, p. 24) shows that a layer a few centimetres deep of air containing much reduced sulphur dioxide, but with little reduction in smoke, occurs over urban turf, and it is probably this reduction which enables terricolous lichens to occur in urban areas. However, this phenomenon does not enable terricolous lichens to escape from the effects of particularly high sulphur dioxide levels, for they were absent from the bombed sites in Central London (see below). 36 terri¬ colous species were recorded for the Area before 1950, and the decline to the present number appears to be mainly due to the destruction of habitats. The absence of Pel tiger a spp. from the Area at the present time is note¬ worthy, for apparently suitable habitats abound, and P. rufescens is abundant on the air polluted heaths around Scunthorpe, Lincolnshire (Seaward, 1966). Nine species (13%) are found on bark and eight species (11 %) occur on wood. These small numbers fully support the well-known fact that air pollution has a much greater adverse effect on corticolous and ligni- colous species than on those on other types of substrata. Prior to 1950 50 species were recorded from bark in the Area, and 36 from wood, so their decline has been catastrophic. D. Habitats The present lichen flora in different habitats is shown in the right-hand Table 2. The present lichen flora on types of substrata (left-hand columns) and m different habitats (right-hand columns). Chaenotheca ferruginea and Parmelia physodes occur m habitats other than those listed. sjgoj jusurao-sojssqsy qouq pio + + sojss paqtnos SilOAJOSS^J suuibj sSb/ass suspisg 91JBAU0 + sdUdiainao pua spjaAqojmo suoiuuioo ptre ***** + spooM + -£ . rjio + + + + + + M® r + + + +++ + + oi w + + + + + + + + ++ + + + + + + +^52 !l | till ! j| I a§ . «ISf § -gl .1.. ...Ill 1 g-s'PlfitSgliPl I 41111 1 §11 SI ^ II 1 1 14f?sul ptilj fl| 111 +85 oo — 1 C3 I ill !| 11-1113 ill ill 11? 8 rsllAt nil § p 1 8 II nuuftf |l 11 1 fis-ii l-tji P°°A\ JflBg « Itos ppv 911 OJS pK>V < << £ ££ aa £ ££ cecace w ww < < < « < «« < < < aao?s snoararc) OU U OOOOOOOUOOO QUO UU O OOOOOO O OO O OOOOOOOOUUU UUUUUUU^ H LONDON’S LICHENS 33 columns of Table 2. 46 species (65 %) of the total flora are found in churchyards and cemeteries, chiefly in the former because the memorials are older. A comparison of the percentages shows that this habitat is more important for lichens than all others. Only a few Central London churchyards which retain good collections of headstones (e.g. St. Bartholo¬ mew The Great, Little Britain, City) are devoid of lichens. Churchyards near the perimeter of London have a lichen flora on their limestone memorials which is often almost as rich as that on memorials in rural areas. St. Andrew, Totteridge, situated in the Green Beit, appears to have the largest number of species, 23 having been recorded. Many of the churchyard lichens occur in the nitrophilous community called Cciloplacetum heppianae (see Laundon, 1967, pp. 296-300), which is characterised by an abundance of orange and yellow lobate Calop/aca and Candelariella species. The community is well-developed on limestone memorials (Plates 1 and 2) in old churchyards in the Suburban Ring and beyond, occurring on the top surfaces of headstones and near the outer edge of chest-tombs where there is maximum illumination and high nitrogen concentrations. The memorials are used as bird perches, and the lichens evidently obtain their nitrogen supply chiefly from the bird excreta which occurs in quantity amongst the lichen vegetation. The mite Ameronothrus maculatus (Mich.) occurs in many London churchyards, where it feeds on lichen thalli; it is possible that it may exterminate some species from certain churchyards, but this needs further investigation. The community Caloplacetum heppianae survives in London church¬ yards as a relict from earlier times of rural surroundings and lower levels of air pollution, being absent from nearby cemeteries of more recent date. Thus at St. John, Hampstead, it is frequent on the oldest memorials in the 18th century churchyard, but is absent from the nearby Highgate Cemetery, which was not opened until 1838; evidently Camden was already becoming too polluted after 1838 for the community to spread to new areas. High levels of air pollution in the 19th century also prevented the Caloplacetum heppianae from establishing itself in the other early cemeteries of Abney Park (Hackney), opened in 1840, Brompton (Ken¬ sington and Chelsea) opened in 1831-40, and Kensal Green (Westminster) opened in 1833. Even in existing old churchyards the community is confined to the 18th and 19th century memorials and unable to colonise those erected in the present century. Thus at St. Peter and St. Paul, Mitcham, Caloplaca heppiana (here the principal component of the Caloplacetum heppianae ) occurs on over 80 % of the non-shaded limestone memorials erected in the 18th century (Plate 2), compared with none on those dating from the 20th century (Fig. 4 ); Lecanora disperse i, on the other hand, shows no decline in colonising ability. Posing levels of air pol¬ lution during the 19th century have made it increasingly difficult for Caloplaca heppiana to colonise new surfaces in Mitcham, with the result that all further colonisation ceased before 1900. Patterns of distribution which appear to indicate species in order of sensitivity to air pollution can therefore be misleading; Fig. 2 indicates that Caloplaca heppiana is less sensitive than Physcia orbicularis , but the reverse is the case today as regards present colonisation. Old brick walls are the second richest habitat, on which 32 species (45 %) are recorded. The early 18th century wall at Church Lane, Bedding- ton, has 23 species (of which one, Lecidea lucida, appears to have become recently extinct), including the only known plants of Buellia canescens, 34 THE LONDON NATURALIST, NO. 49, I97O o vO u"> (N O £7 un T- . LO 00 00 t- v- | O \D LO