Royal Ontario Museum Ufs Sciences Miscellaneous Publications M\v>* 0& Digitized by the Internet Archive in 2012 with funding from Royal Ontario Museum http://archive.org/details/earthwormslumbriOOreyn LIFE SCIENCES MISCELLANEOUS PUBLICATIONS ROYAL ONTARIO MUSEUM john w Reynolds The Earthworms Illustrated hv /T i • • i daniel l dindal (Lumbncidae and Sparganophilidae) of Ontario Publication date: 15 June 1977 isbn 0-88854-191-0 issn 0082-5093 Suggested citation: Life Sci. Misc. Pub.. R. Ont. Mus. ROYAL ONTARIO MUSEUM PUBLICATIONS IN LIFE SCIENCES The Royal Ontario Museum publishes three series in the Life Sciences: life sciences contributions, a numbered series of original scientific publications, in- cluding monographic works. LIFE sciences occasional papers, a numbered series of original scientific publications, primarily short and usually of taxonomic significance. LIFE sciences miscellaneous publications, an unnumbered series of publications of varied subject matter and format. All manuscripts considered for publication are subject to the scrutiny and editorial poli- cies of the Life Sciences Editorial Board, and to review by persons outside the Museum staff who are authorities in the particular field involved. LIFE SCIENCES EDITORIAL BOARD Chairman: a. r. emery Senior Editor: IAN R. BALL Editor: allan j baker Editor: Gordon edmund john w Reynolds is an Assistant Professor in the Department of Forest Resources, University of New Brunswick, Fredericton, New Brunswick. daniel L dindal is a Professor in the Department of Forest Zoology, College of Environmental Science and Forestry, Syracuse, New York. ^ KOYAL ONTARIO MlLSEUWf I* PRICE: $8.00 © The Royal Ontario Museum, 1977 100 Queen's Park, Toronto, Canada M5S 2C6 PRINTED AND BOUND IN CANADA BY THE HUNTER ROSE COMPANY This book is dedicated to Dr. Gordon E. Gates on the occasion of his 80th birthday and 51st year of publication on the Oligochaeta. Contents Foreword vii Acknowledgments i\ Introduction 1 General Biology 3 Introductory Remarks 3 General Activity 3 Parasites and Predators 4 Environmental Requirements and the Effects of Pesticides 4 Rearing and Culturing Earthworms 6 Methods of Study 8 Sampling Techniques 8 Preservation Techniques 10 Ontario Collection Coding 10 Figure Coding 1 1 General Morphology 13 External Structure 13 Internal Structure 14 Glossary 18 Identification of the Earthworms of Ontario 3 1 Key to Sexually Mature Earthworms Found in Ontario 32 Systematic Section 34 Family LUMBRICIDAE 34 Genus A llolobophora 35 A. chlorotica 36 Genus Aporrectodea 40 Ap. icterica 40 A p. longa 43 Ap. trapezoides 46 Ap. luberculata 50 Ap. turgida 56 Genus Bimastos 61 B. parvus 61 Genus Dendrobaena 64 D. octaedra 65 Genus Dendrodhlus 69 Dd. rubidus 69 Genus Eisenia 74 E. foetida 74 E. rosea 78 Genus Eiseniella 83 £/. tetraedra 84 Genus Lumbricus 88 L. castaneus 89 L.festivus 92 L. rubellus 94 L. terrestris 99 Genus Octolasiun 104 0. cyaneum 105 0. tyrtaeum 108 Family SPARGANOPHILIDAE 112 Genus Sparganophilus 1 12 5. mew 1 13 Distribution and Ecology 1 16 Appendix: Provincial Description 123 Literature Cited 127 v/ Foreword "I would not enter on tin list of friends, (Tho' grae'd with polish'd manners and tine sense Yet wanting sensihilit\ ) the man Who needlessly sets foot upon a worm". Wilham Cowper, The Task (1784) Nobody could needlessly set foot upon one of the giant earthworms of Australia or Brazil, large specimens of which may attain lengths of 1 1 feet and weigh up to 1 pound. But to many people earthworms are lowly insignificant creatures whose main utility is to act as bait for catching larger and more edible animals. The Canadian earthworms are indeed represented only by the smaller, more modest, forms and even though to the uninitiated they all seem to be the same there are in fact several species which are not too difficult to distinguish. In this book Dr. Reynolds has assembled, for the first time, all pertinent data, both sys- tematic and biological, on the Canadian earthworm fauna, and with the aid of a key, and the fine illustrations of Dr. Dan Dindal, any naturalist or fisherman should be able to name accurately the specimens that he has at hand. Earthworms are a significant component of the soil fauna and their beneficial effects on the agricultural properties of soils have been documented since the time of Darwin. Some idea of the extent of their activity can be obtained by reflecting on the fact that something apparently so permanent as the monument of Stonehenge is being buried at the rate of about seven inches per century as a result of the burrowing activities of earthworms. Because of their effects on the soil there can be little doubt that a proper understanding of these creatures is greatly to man's benefit but, as Dr. Reynolds points out, very little is known of their biology in North America. This book should form a valuable basis for fur- ther study of these important aspects. Dr. Faustus, in part I of Goethe's Faust, speaks disparagingly of him who "finds his happiness unearthing worms". And an old Chinese aphorism warns "watch the earthworm; miss the eclipse". But anybody who has spent time in- vestigating and observing the smaller and lesser known animals of this planet knows that there is much intellectual satisfaction to be gained from such efforts. The great Victorian naturalist, Thomas Henry Huxley, likened the uninformed naturalist to a person walking through an art gallery in which nine-tenths of the pictures have their faces to the walls. With the aid of this book a few more pic- tures are now on view. The Royal Ontario Museum is fortunate to have persuaded Drs. Reynolds and Dindal to collaborate in producing this book, and zoologists, farmers, fishermen, naturalists, and teachers throughout northern North America should have cause to appreciate their labours. Ian R. Ball Assistant Curator of Invertebrate Zoology Royal Ontario Museum vii Acknowledgments [his project was sponsored in pan under a Gerald L. Beadel Research Grant from the Tall Timbers Research Station, Tallahassee, Florida. The author wishes to thank Mr. E.V. Komarek, Si. o\ Tail limbers for his support. The au- thor also expresses his gratitude to Mr. Dennis Clarke of Canadian Motor In- dustries (Toyota Ltd.) for providing a 4-wheel drive Land Cruiser to conduct this study. The author is grateful to Mr. and Mrs. C.W. Reynolds o\' Islington, Mr. D.W. Reynolds o( Mitchell, and Mr. K. Burns of the Biology Department of Lakefield College for providing laboratory space during the field work. The contribution of Mr. C.E. Meadows. Oligochaetology Laboratory. Knoxville to the various laboratory and statistical analyses in this project is appreciated. The author thanks Mrs. W.M. Reynolds of Tall Timbers for constant encourage- ment and support during the course of the study, for reviewing the manuscript, and for her comments, criticisms, and suggestions. The author would also like to thank Ms. Jennifer Smith of the Royal Ontario Museum for typing the final drafts of the manuscript and he is especially grateful to Dr. Ian R. Ball of the Royal Ontario Museum for the considerable time and effort he devoted to ed- iting the manuscript, which, in the author's opinion, has improved the text. The author is indebted to the following for providing specimens for examination from collections in their care: Dr. LR. Ball (ROM). Dr. E.L. Bousfield (CNM), Mr. S. Fuller (ANSP), Dr. S.B. Peck (Carleton University), Dr. M.B. Pettibone (USNM), and Mr. D.P. Schwert (University of Waterloo). IX The Earthworms (Lumbricidae and Sparganophilidae) of Ontario Introduction Earthworms (Annelida. Clitellata, Oligochaeta) are familiar to almost everyone. In North America, they are one of the most popular forms of live bait for fishing (Harman. 1955): gardeners hold them in high esteem as nature's ploughmen (Darwin, 1881); folklore and scientific accounts tell of their medicinal uses (Ste- phenson. 1930; Reynolds and Reynolds, 1972), and soil inhabiting vertebrates (moles, voles, etc.) store them as a source of food (Plisko, 1961; Skoczeii, 1970). The role of some species in organic matter decomposition and mineral cycling may be important (Bouche, 1972; Edwards and Lofty, 1972), and a great deal has been written concerning earthworm farming (Myers, 1969; Morgan, 1970; Shields, 1971). Biology students the world over study their anatomy (mainly Lumbricus terrestris) in great detail (Whitehouse and Grove, 1943). The great amount of literature that has been devoted to a group of organisms that are nei- ther pests nor sources of human nutrition is truly amazing, yet their biology and distribution are still relatively unknown. Many of the world's hundreds of me- gadrile ( = terrestrial oligochaetes) species are known only from a limited series of one or a few specimens. This text has been designed to introduce the non-specialist to the taxonomy, nomenclature, morphology, distribution, and general biology of earthworms in Ontario and neighbouring areas. The identity, distribution, and habitats of these animals have been surveyed for a variety of habitats in each of the southern counties and districts of the province. An illustrated glossary is included to- gether with a new key to the identification of the earthworms of Ontario that also is applicable to the rest of eastern Canada and to the northern tier of states of the United States. French and English common names are included for each species. The first records of earthworms from Ontario were provided by Eisen (1874). Recently Reynolds (1972a) reviewed the complete published and verified un- published records of terrestrial earthworms from this province, and a second re- port examined those data quantitatively for habitat factors governing megadrile activity in the Haliburton Highlands (Reynolds and Jordan, 1975). This study is a continuation of those reports and presents subsequent collections from 50 counties and districts of southern Ontario in detail (Fig. 1). In addition, unpubl- ished records derived from collections in North American museums and univer- sities, including records from northern Ontario, are presented for the first time. Fig. 1 The Counties and Districts of Ontario. Thirty-eight of the counties and districts have never had any earthworms re- ported previously. At present, there are insufficient megadrile data available to utilize fully some of the habitat information. For example, it would be unwise to try to correlate in detail megadrile distribution with the distribution of soil types until addi- tional surveys from other parts of the continent are completed (cf. Jordan et al., 1976). A preliminary examination of megadrile-vegetation relationships has been presented recently (Reynolds, 1976b). A provincial description is included in an appendix to assemble regional habitat information for future use as well as to familiarize native and foreign readers with Ontario. The technical terms and conventions necessary for earthworm discussion will be found in the Glossary (p. 18). For additional information on earthworm ter- minology Stephenson (1930), Causey (1952), Gerard (1946), Ljungstrom (1970), or Gates (1972c) may be consulted. General Biology Introductory Remarks There can he little doubt thai earthworms are the best known of all soil animals. It is common knowledge that the) have a beneficial efTect on the structure and properties of the soil and that the) influence the decomposition processes in or- ganic materials. However, it cannot be denied that much work purporting to demonstrate these aspects has been far from rigorous. In fact, far less is known than is generalh believed, and most work is applicable only to Europe. The problem is compounded b\ the fact that many of the hundreds of described species are known onl\ from a morphological study of a few individuals. Fortu- natelv, nearlv all of the species present in Ontario and the neighbouring areas are the widelv distributed European species that have received the greatest at- tention. Major limitations to the interpretation of the literature have been old nomenciatural and taxonomic designations (Reynolds, 1973b). Sources of information on various biological attributes for species found in Ontario and the surrounding region are Evans and Guild (1948), Bouche (1972), Edwards and Lofty (1972), Gates (1972c), Reynolds (1973d). and Reynolds et al. (1974). Recent reviews of earthworm activity will be found in Kevan (1962) and Wallwork( 1970). General Activity The main activities of earthworms that affect the soil involve the ingestion of soil and the mixing of the main soil ingredients of clay, lime, and humus; the production of castings of a fine crumb structure which are ejected on the soil surface by some species; the construction of burrows that enhance aeration, drainage, and root penetration; and the production of a tilth that makes suita- ble habitats for the smaller soil fauna and micro-organisms. It should be re- membered, however, that not all Lumbricidae work in the same manner. Some, for example, burrow deeply whereas others do not. The influence of earthworms on the translocation of soil material may be quite considerable. There have been abundance estimates as high as three mil- lion worms per acre and their role in soil fertility is very important. Studying forms that eject casts to the surface, Darwin (1881) estimated that between IVz and 18 tons of soil per acre per year (about 3 cm per 10 years) can be moved, and the burial of many Roman ruins in Europe has been attributed to the activ- ity of earthworms (Atkinson, 1957). Earthworms are omnivorous and can utilize many materials in the soil as food, including plant remains, and occasionally animal remains. Lumbricids can withstand considerable starvation and, in L. terrestris at least, a water loss of up to 70% of the body weight. Some species can withstand total immersion in water for many weeks, though normally they avoid waterlogged soils. The reproductive cycle of many Lumbricidae is quite straightforward. Al- though hermaphrodite, they possess a mechanism to prevent self-fertilization. During copulation the two worms lie side by side with their anterior ends over- lapping. A mucous sheath envelops the worms and holds them tightly together. Sperm are released from the testes and flow down the seminal groove in the side of each worm to the spermathecae of its partner. Both worms do this at the same time. Some time after copulation has taken place, and after the worms have separated, the egg cocoons are formed. A mucous tube or belt is secreted around the clitellum. The worm then wriggles out of this belt and as the belt passes the female apertures the eggs are deposited in it. Spermatozoa to fertilize the eggs are deposited as it passes the spermathecal openings. On release the ends of the belt close over to form a cocoon in which the young worms develop. Cross-fertilization does not occur in all earthworms, however, despite asser- tions to the contrary in many textbooks. In some species there is parthenogenes- is, with concomitant reduction of the male apparatus. Pseudogamy, in which sperm play no part in the development of the egg other than as a stimulant, also may occur. Thus, even if copulation has been observed, the exchange of sperm alone is not evidence for amphimixis. The whole question of reproduction in earthworms has been reviewed by Reynolds (1974c). Parasites and Predators Some earthworms {Allolobophora chlorotica and Eisenia rosea) are parasitized by Pollenia rudis (Fabr.), a calliphorid fly known as the cluster fly, which may lay its eggs directly in the earthworm or merely on the surface of the soil (Thom- son and Davies, 1973a, 1973b). Cluster flies are the most common and annoying of the flies that overwinter in buildings. Other insects such as ants and beetles are predaceous on earthworms (McLeod, 1954). Furthermore, some earthworms may act as intermediate hosts of parasitic worms that affect domestic animals (Kevan, 1962). Reports of mites (Acari) parasitizing earthworm cocoons and adults {Allolobophora chlorotica and Eiseniella tetraedra) were made by Stone and Ogles (1953) and Oliver (1962). Earthworms are also an important component of the diet of many birds and mammals. In Europe moles may store them as a source of food (Skoczeh, 1970; Gates, 1972c), usually after biting off four or five of the anterior segments to prevent the worms from escaping (Evans, 1948b). In North America they are eaten by many organisms, including some of economic or recreational impor- tance. According to Liscinsky (1965), for example, the diet of the woodcock (Philohela minor Gmelin), a favourite game bird in eastern North America, is primarily earthworms. From my current surveys, and from gut analyses of woodcock, it appears that in the area bounded by Ontario to Nova Scotia and Minnesota to Maryland, 90% of the earthworms in the diet of these birds are Aporrectodea tuberculata, Dendrobaena octaedra, Dendrodrilus rubidus, and Lumbricus rubellus. Snakes, too, may prey extensively on earthworms. This is true especially of two of our most common species, the red-bellied snake (Storeria occipitomaculata occipitomaculata Say) and the eastern garter snake (Thamnophis sirtalis sirtalis Linnaeus), and perhaps of four or five other species as well (Logier, 1958). As this book is in proof, the author has examined the gut contents from Thamnophis butleri Cope collected in Essex and Lambton Coun- ties, Ontario. The earthworms identified in these snakes' stomachs were Allolobophora chlorotica, Aporrectodea tuberculata, and Lumbricus terrestris. Ac- cording to the author and Dr. S.W. Gorham (pers. comm.), this is the first valid report of earthworm species identified from snake stomachs in North America. A recent account was presented by Dindal (1970) of a terrestrial turbellarian, 4 Bipalium adventitium Hyman, attacking Demlrodhlus mbidus and Lumbricus terrestris. This flatworm is currently a major problem in outdoor earthworm beds in central New York state (Dindal. pers. comm.). Environmental Requirements and the Effects of Pesticides Daylight and ultraviolet light are injurious to earthworms unless the intensity is very low. Temperature relations have been reviewed by Reynolds (1973a), and Gates (1970) quotes interesting accounts of lumbricids studied from the Arctic circle; Eisenia foetida, for example, has been found in snow, even though gener- ally associated with warm habitats such as manure piles, and it remains vigor- ous below 5° C. In Maine L. lerrestris has been seen copulating while bathed with melt water, and other individuals crawled from under the ice and remained active (Gates. 1970). The pH tolerance (see Glossary) of earthworms varies from species to species (Reynolds. 1973d). Usually they occur in soil with a pH range of about 4.5 to 8.7 and the earthworm density diminishes as the soil acidity increases. Gener- ally speaking, the greatest earthworm densities are found in neutral soils. The type of soil also may influence the distribution and abundance of the var- ious species. Gates (1961), for example, divides the earthworms of Maine into three groups depending upon whether or not they are geophagous, in that they pass much soil through the intestine; limiphagous (mud-eating) or limicolous (mud-inhabiting); or. finally, litter-feeding, and hence found primarily in or- ganic matter. From his studies in Sweden. Julin (1949) divided the Lumbricidae into four ecological groups. These were hemerophiles, species favoured by hu- man culture; hemerophobes, species averse to culture; hemerodiaphores, spec- ies indifferent to the influence of culture; and hemerobionts, species entirely de- pendent on culture. Julin's classification has never been applied to the North American Lumbricidae with the exception of a preliminary attempt for the earthworms of Tennessee by Reynolds et al. (1974). Regrettably, there are as yet insufficient data to permit an attempt for the Ontario earthworms; this is a topic worthy of further study. The application of pesticides to control soil pests, or the earthworm parasites mentioned above, may also kill the earthworms. This devastating effect on earthworm populations has frequently occurred after the application of orchard sprays. Fruit growers have long held earthworms in high esteem for their help in controlling the disease apple scab which is produced by the fungus Ventuha inequalis (Cke.) Wint. This disease overwinters on the fallen leaves in the or- chard. One method of cultural control is to burn the fallen leaves and twigs in the fall of the year. An equally effective and less costly method is to introduce earthworms (preferably Lumbricus terrestris), which will pull the fallen leaves into the soil for food and eventual decomposition. According to the findings of Reynolds and Jordan (1975). for example, earthworms have a distinct prefer- ence for apple leaves over those of maple. Once the leaves are beneath the soil surface the conidiospores of the fungus are ineffectual inoculating agents of the disease. The preventive measure most commonly used for control of apple scab is frequent spraving of copper sulphate solutions which are toxic to earthworms (Raw and Lofty, 1959). Many studies have been conducted to determine the effects of pesticides on earthworms. There is little effect on earthworms with normal doses of Aldrin (Edwards and Dennis, 1960; Edwards et al., 1967; Hopkins and Kirk, 1957; Legg, 1968), or benzene hexachloride (BHC) (Dobson and Lofty, 1956; Lipa, 1958; Morrison, 1950); chlordane is extremely toxic to them (Doane, 1962; Ed- wards, 1965; Hopkins and Kirk, 1957; Schread, 1952). DDT, of course, has been studied by many workers. In general, the application of this pesticide at normal rates does not harm earthworms (Baker, 1946; Doane, 1962; Edwards, 1965; Edwards and Dennis, 1960; Edwards et al., 1967; Hopkins and Kirk, 1957; Thompson, 1971). Although earthworms are not susceptible to many pesticides at normal dosag- es, they do concentrate these toxic chemicals in their tissues. Since many of these chemicals have long-lasting residual periods in the soil, there is ample op- portunity for earthworms to absorb them from the soil. The importance of this phenomenon is that these pesticides can become concentrated in the food chain. Earthworms are eaten by many species of birds and certain species of amphibi- ans, reptiles, and mammals, which can continue to concentrate these pesticides in their bodies (Hunt and Sacho, 1969). Additional reports of pesticides and their effects on earthworms can be found in Edwards and Lofty (1972). Herbicides, another group of chemicals, also can affect earthworm popula- tions (Edwards, 1970; Fox, 1964). These chemicals may kill earthworms direct- ly, or indirectly by killing the vegetation on which they feed. One last group of potential poisons that could become concentrated in the food chain are metal residues. Recently, Gish and Christensen (1973) found that concentrations of certain metals (cadmium, nickel, lead, and zinc) in earth- worms were many times that of the surrounding soils. This study was the first report of metal residues in earthworms. Because of the earthworms' position in the food chain and the current studies in other fields on metal toxicity, this is an area requiring further investigation. Rearing and Culturing Earthworms It may be of interest to some readers to discuss briefly the rearing or culturing of earthworms. This is not difficult for the species found in Ontario. There are many books available describing techniques (e.g.. Ball and Curry, 1956; Myers, 1969; Morgan, 1970; Shields, 1971), although their citation here must not be taken as an endorsement. The location for earthworm containers depends upon the climate of the region. Outdoor containers or pit-runs (benches) in northern areas will require insulation during the winter period when the soil is normally frozen. Smaller wooden pit-runs, or one of the various types of metal tubs, can be housed in a basement or shed to avoid winter freezing problems. Since the indoor facilities permit year-round activity, these can be a source of replenish- ment for outside gardens, compost piles, flower beds or earthworm beds, etc. The size of the container can vary. A convenient size is a box 50 cm long X 35 cm wide and 15-20 cm deep. Larger containers, when filled with medium and earthworms, will be extremely hard to move. These boxes should have holes 0.5 cm in diameter drilled in the bottom. Plastic window screening should be placed on the inside bottom of the box with a burlap lining on top of the screen and sides of the box before the soil is added. This permits the excess water to drain and presents (he soil medium from sticking to the box, and also prevents the earthworms from escaping through the holes. Various combinations of soil and organic matter can serve as a medium in which to raise earthworms. A frequently used mixture is 16 soil and % organic- matter. Sources of suitable organic matter are: decayed sawdust, hay, leaves, manure, peat moss. sod. or straw. Additional materials which can be added to the medium to serve as food sources are: chicken starter, cornmeal, and kitchen scraps and fats. Earthworms are omnivorous and can utilize many materials as food sources. Some important facts to remember are: 1) the medium should contain sufficient organic matter so that it will not pack into a dense, soggy mass. 2) the containers must not be overwatered, and 3) the presence of low- watt bright white or blue light will prevent the earthworms from crawling on the surface of the medium and eventually out of the box. The species most frequently used as fish bait, and therefore the ones most likely to be cultured, are: Aporrectodea trapezoides, Ap. tuberculata, Ap. turgida, and Eisenia foetida. Two other species, Lumbricus rubellus and Octolasion tyrtaeum, have also been sold or reared as fish bait, though not so commonly as the others mentioned. The night-crawler Lumbricus terrestris is widely used by fishermen but cannot be commercially cultured economically because of its long life cycle, low reproductive rate, and large spatial requirements. Methods of Study Sampling Techniques There are numerous methods for sampling earthworm populations. These fall mainly under the general categories of hand sorting, chemical extraction, elec- trical extraction, and vibration methods. The effectiveness of these methods de- pends upon the species and habitat; no one method is equally suitable for all species and all habitats. Digging and hand sorting is the most reliable sampling method, and the one used primarily to obtain the specimens for this study (Low, 1955; Reynoldson, 1955; Satchell, 1955, 1967, 1969; Svendsen, 1955; Nelson and Satchell, 1962; Zicsi, 1962). Though laborious, digging and hand sorting have been widely used for sampling earthworms and for assessing the effectiveness of other methods. Digging to locate earthworms should be done with two factors in mind, mois- ture and organic matter (cf. Reynolds and Jordan, 1975), and collecting success will be high if one concentrates on sites where both are present. The digging can be done with a variety of tools — shovel, trowel, garden fork, soil cores, etc. The soil can then be pressed and passed through the fingers, or sieves may be em- ployed. The advantages of this method are two-fold: within a sample area active individuals, aestivating individuals, and cocoons may be collected, and, in addi- tion, a well-defined sampling area may be chosen so that quantitative data may be obtained. There are some disadvantages, however. The method is laborious and time-consuming, specimens less than 2 cm in length may escape collection, and, if digging is restricted to the top layers of soil, very large individuals may escape into the deeper layers. Furthermore, specimens may be damaged and there is considerable habitat destruction. Chemical extraction is a method widely used to collect earthworms and was a second method employed in the present study. Initial studies on chemical ex- traction were done by Evans and Guild (1947) using potassium permanganate solution to expel earthworms from the soil. Further experiments with chemical extraction, notably using formalin, were conducted by Raw (1959) and Waters (1955). The standardized sampling format that I have employed over the years of quantitative extraction is based on a 0.25m2 quadrat of soil surface. A solu- tion of 25 ml of formalin (37% Formaldehyde Solution, U.S. P.) in four and a half litres of water is sprinkled over each quadrat so that all of it infiltrates the soil without runoff. The earthworms that surface in the ten minutes following the application of the expellant are collected. If the collection is to be obtained for other than scientific purposes (e.g., for bait), the time, strength, and number of applications can be varied, but it should be noted that solutions stronger than 15 ml formalin per litre of water may kill the grass in lawns, and if specimens are to be kept alive for more than a few minutes they must be washed in fresh water immediately upon surfacing because formalin can act as a vermicide. Other materials such as Mowrah meal have been used to expel earthworms from the soil (Jefferson, 1955). With a chemical extraction method the sampling time and labour are reduced, a well-defined sampling area may be chosen, and there is minimum disturbance of the habitat. The disadvantages of the method are that only active individuals are collected, and not cocoons and aestivating or hi- fi bernating individuals, onl\ shallow dwelling species or species with burrow sys- tems are collected, there may be poor penetration of the vermicide when certain soil conditions prevail, and there is a variability of response to the vermicides by different species. The technique is generally good for Lumbricidae but poor for the other families. Electrical extraction, a method described by several authors (Walton, 1933; Johnstone- Wallace, 1937; Doeksen, 1950; Satchell, 1961). has long been used bv fishermen to obtain bait. The method requires a generator and one to three electrodes. The current conducted through the soil acts as an expellant. The ad- vantage of this method is minimal disturbance to the habitat. The disadvantages are the excessive time required per sample, the difficulty of defining the exact limits of the volume of soil treated, and the variability of the physical and chem- ical properties of the soil (for example, when soil is moist, deep dwelling species will surface, but if the surface soil is dry the earthworms may go deeper into the soil). The use of too much current kills the earthworms near the electrodes, and the response to electricity varies in different species. Vibration methods, or mechanical extraction, are currently limited to the south- eastern United States. Various modifications of this technique ("grunting" in Florida and Georgia, and "fiddling" in Arkansas) are employed by fish bait col- lectors and yield earthworms in amazing quantities (Vail, 1972; Reynolds, 1972d. 1973d). Mechanical stimulation by vibrations seems to have very little effect on the Lumbricidae but it is extremely successful for some Acanthodrili- dae and some Megascolecidae. These two latter families are not found either in Canada or in Europe, which may account for omission of this technique in Eu- ropean discussions of earthworm sampling, except for one small note (Edwards, R., 1967). The advantages of mechanical extraction are the minimal habitat de- struction and the reduced sampling time required for each sample. The disad- vantages are the difficulty of defining the exact volume of soil treated, the effects of the variability of the physical and chemical properties of the soil, and the var- iable response of the different species. There are several other sampling methods that may be used. Wet sieving in- volves washing soil with a jet of water through a series of sieves after the soil samples have been removed from the field (Morris. 1922; Bouche and Beugnot, 1972a). There are no available data on the efficiency of this method. The disad- vantages, according to Ladell (1936), are the excessive time required per sample, the inordinate amount of labour in residue separation, and the damage to the specimens during separation. The flotation method employed by Raw (1960) for extracting the microfauna from soils unsuitable for hand sorting was patterned after a technique designed by Salt and Hollick (1944). Its advantage is that it can be adapted to extract earthworm cocoons; thus, all stages of the population can be sampled. The heat extraction method operates on the principle of the Baermann funnel (Baermann. 1917) and has been used for extracting small surface dwelling spec- ies that are difficult to hand sort. Similar designs employing Tullgren funnels and incandescent lights have been used by this author. Considerable time per sample is required for this method as the soil samples have to be brought in from the field and placed on the wire sieves in the funnels for several hours. The method has limited use for earthworm sampling. Trapping techniques are unlikely to yield accurate population estimates but do form a useful method of studying the activity patterns where population den- sities are low (Svendsen, 1957). A mechanized soil washing method, involving rotating containers and standing sieves, was described by Edwards et al. (1970). This method is faster than previous washing techniques and is apparently suita- ble for most soils. Several authors have compared and discussed the relative efficiency of ex- tracting earthworms from soil by two or more of the previous methods (Svend- sen, 1955; Raw, 1960; Bouche, 1969a; Satchell, 1967, 1969). From my own observations, the choice of chemical, electrical, or mechanical methods for ex- traction of earthworms from the soil is greatly dependent on the genus and species of earthworm to be collected. Preservation Techniques The proper preservation of specimens for identification, shipping, and storage has long been a problem. Few good accounts of preserving techniques are read- ily available to those who wish to send material to a specialist for examination. One of the best media for earthworm preservation is 10-15% formalin because it hardens the specimens to facilitate handling. Weak alcohol solutions leave the specimens soft and limp while strong alcohol solutions produce an undesirable brittleness. In both cases, alcohol also causes a condition known as "alcohol browning". This condition makes the reporting of colour of preserved alcohol specimens valueless. Generally, formalin does not distort the colour greatly. A simple and effective technique is to kill the worms by immersing them in 70% ethyl alcohol. When movement stops they are placed on absorbent paper in a straight position, and allowed to dry for a few minutes. For preservation they should then be transferred to a container of 10-15% formalin where they will harden in the position thus placed. They must be straight because curled or twisted specimens are more difficult to handle when internal examination and dissection are required. The specimens should be left in this container overnight and may then be stored in bottles or vials filled with fresh formalin preservative without much danger of curling. For best results, the preservative should be changed again in a week, especially for such species as Aporrectodea trapezoides, Lumbricus rubellus, and L. terrestris. Diffusion of body fluids from these species to allow replacement with the preservative seems to take a longer period. As a general rule, the preservative should be changed at weekly intervals until it re- mains clear. Ontario Collection Coding Under the Ontario Distribution for each species (Systematic Section), the col- lection data have been coded in a consistent manner: location, habitat (when available), date of collection, collector(s), number of specimens (by age classifi- cation, explained in the Glossary), and museum number (if any). When an au- thor and date are given, the collection information can be found in that source. If the data are given for a literature source, it is because the author has exam- ined that collection. An asterisk (*) before a location means that the author has a 35 mm colour slide of the habitat in his photographic collection. The abbrevi- ations used in the Ontario Distribution records are: 10 ANSP Academj of Natural Sciences, m metre(s) Philadelphia mm millimetre^) AT Alexis Troicki MKG Matthew K. Graham BP h\ pass n north CNM National Museums of Canada n.e. north edge CO couim RC R. Cain CWR Charles W. Reynolds Rd road DIST district RGR Ruth G. Reynolds DPS Donald P. Schwert RLH R. Landis Hare DRB David R. Barton RNS R.N. Smythe DWR David W. Reynolds ROM Royal Ontario Museum e east RVW R.V. Whelan e.e. east edge s south GE Gustav Eisen s.e. south edge GM G. Mueller ST Steve Tilton GMN G. Morley Neale St street GWA George W. Abbott TTRS Tall Timbers Research H\v\ highway Station IMS Ian M. Smith TW Thomas Weir Jet Junction TY Toshio Yamamoto JEM John E. Moore III w west JO Jack Oughton w.e. west edge JPM J. Percy Moore WMR Wilma M. Reynolds JRD John Richard Dymond USNM United States National JWR John W. Reynolds Museum (Smithsonian) km kilometre(s) UW University of Waterloo LWR L. Whitney Reynolds Figure Coding The figures for each species were drawn with a camera lucida from preserved specimens in the author's collection. The source of the specimens for each draw- ing is given in parentheses after each figure caption. The abbreviations used in all figures are: a anus es oesophagus be buccal cavity fp female pore cag calciferous gland g gizzard cg cerebral ganglion gl gut lumen chl chloragogen cells GM genital markings cl clitellum GS genital setae elm coelom GT genital tumescence cm circular muscle h heart epe circumpharyngeal connectives if intersegmental furrow cr crop int intestine cut cuticle lm longitudinal muscle dp dorsal pore lnv lateral neural vessel dv dorsal vessel m mouth epi epidermis mf male funnel // mp male pore mL mid-lateral line n nephridium nb nephridial bladder np nephropore ns nephrostome nt nephridial tube o ovary od oviduct OS ovisac ph pharynx phm pharyngeal muscle PP periproct Pr prostomium ps peristomium ptm peritoneum s sep seta septum s§ seminal groove sm setal muscle snv subneural vessel sp spermathecae spp spermathecal pore sv seminal vesicle t testes TP tubercula pubertatis typ typhlosole vd vas deferens ve vas efferens vnc ventral nerve cord vv ventral vessel 12 General Morphology The Oligochaeta are defined as annelids with internal and external metameric segmentation throughout the bod\. without parapodia but possessing setae on all segments except the peristomium and periproct, with a true coelom and closed vascular system, generally hermaphroditic with gonads few in number in specific locations, with special ducts for discharge of genital products, with a cli- tellum that secretes cocoons in which ova and spermatozoa are deposited, and which are fertilized and develop without a free larval stage. The following brief discussion refers primarily to the Lumbricidae. which make up nearly all of the Canadian megadnle fauna. The terms used in this sec- tion that are not explained in detail in the text will be found in the illustrated Glossary. For additional information and details of megadrile morphology con- sult Stephenson (1930) or Edwards and Lofty (1972) for English accounts, and Avel (1959) or Bouche (1972) for French. External Structure Terrestrial oligochaetes vary greatly in size. Bimastos spp. are less than 20 mm long, the largest tropical species are over 1200 mm (Glossoscolex, Megascolides), and some Australian forms may reach 3000 mm in length. The largest species in Canada is Lumbricus terresths (p. 99). which varies from 90 to 300 mm when mature. The bodv shape is generally cylindrical though usually flattened dorso- ventrally in the posterior region in the case of burrowing species. The entire body is divided along the longitudinal axis into segments separated by intersegmental furrows and septa. This is primary segmentation. There are also secondary annuli. or furrows, which appear to subdivide some of the indi- vidual segments, usually in the anterior region. These demarcations are only ex- ternal. Ljungstrom and Reinecke ( 1969) have suggested using a and B for these subdivisions and I use y for a third subdivision; the primary segments are num- bered by roman numerals. There is a loss of uniformity in segmentation at the anterior end of the earthworm; this condition is referred to as cephalization (cf. Gates. 1972c). The first body segment, containing the mouth, is known as the peristomium and may have a tongue-like lobe projecting anteriorly. The pros- tomium is located above the mouth, and is not a true segment. Its appearance is often important in species identification. The last, or caudal, body segment is referred to as the periproct. Sometimes a swelling may be seen around the body, the clitellum. The lay- man frequently mistakes this for the scar of a regenerated animal. In fact it is an epidermal modification of sexually mature specimens where gland cells secrete material to form the cocoon. Characteristic of all earthworms are the short bristles or setae, retractile struc- tures that add to the worm's grip during tunneling and locomotion. The setae are produced bv cells in the body wall. In the Lumbricidae and Spargnnophil- idae there are four pairs of setae per segment, except for the peristonv .m and periproct. which are asetal. The type and position of these setae have been used as taxonomic characters (see Glossary — setae, setal formula, setal pairings). The colour of the megadriles is primarily a result of pigment in the body wall. 13 But it may be a secondary result of lack of pigment and the red colour of some forms is due to haemoglobin in the blood. Some colour is due to the presence of yellow coelomic corpuscles near the surface, but the presence of chloragogen cells near the surface is rarely, if ever, an influence on colour. Preliminary re- sults of current North American studies indicate that the physical and chemical properties of the soil are a possible influence on earthworm colour. The body wall, upon which the excretory, genital, and reproductive apertures all open, comprises six layers. From the outside these are: cuticle, epidermis, nerve plexus, circular muscle, longitudinal muscle, and peritoneal layer. The well-developed muscle layers are important in locomotion. The body wall is the foundation for many glandular swellings such as the clitellum, tubercula puber- tals, and genital tumescences, all of which have long been employed as taxon- omic characters. Internal Structure The annelids have often been characterized as possessing a "tube-within-a- tube" body style (Figs. 2 and 3). The outer tube is formed by the body wall and the inner tube by the alimentary canal. Between these two tubes is the second- ary body cavity, or coelom, which is divided at each segment by a septum at the intersegmental furrow. Non-segmental alignment may occur anteriorly in some species as a result of cephalization. The coelomic cavity is filled with a fluid that varies in composition interspecifically, and also intraspecifically for those spec- ies that are euryecious in that they tolerate a wide range of habitat conditions. Pores in the septa permit the coelomic fluid to pass freely between segments. The alimentary canal or digestive tract is essentially a tube extending from mouth to anus. The anteriormost part of the tract consists of a muscular buccal cavity, followed by a pharynx which has a sucking action during feeding, the oe- sophagus, the crop, a crushing organ known as the gizzard, and finally the intes- tine. The intestine may possess a dorsomedian fold, the typhlosole, that serves to increase the absorptive surface. Many associated structures are connected to the alimentary system, viz., blood glands, chloragogen cells, calciferous glands, and salivary glands. An extensive account of the alimentary canal is found in Gansen(1963). The circulatory system is closed but there is an extensive sinus between the intestinal epithelium and the choragogen cells. Extending almost the total length of the body are three main vessels (Fig. 3): the dorsal vessel, closely asso- ciated with the alimentary canal for most of its length, and two ventral vessels (ventral and sub-neural vessels). The ventral vessel is located between the nerve cord and the alimentary canal, while the sub-neural vessel is located between the nerve cord and the body wall. These main vessels are connected in each seg- ment by paired connectives. In several anterior segments these connectives, termed "hearts", are enlarged and contractile, and possess valves. There are other trunks and branches which anastomose throughout the body. The circula- tory or vascular system has not yet achieved its proper position in oligochaete systematics. Its importance has been discussed by Gates (1972c) and Reynolds (1973e). There is no formalized respiratory system in earthworms; exchange of oxygen and carbon dioxide takes place through the moist cuticle. Respiration normally 14 XXXV XXX Fig. 2 Diagrammatic longitudinal section of a lumbncid earthworm showing internal organs. 15 Fig. 3 Diagrammatic cross section of a lumbncid earthworm. occurs in air but earthworms can exist in water for long periods of time (e.g., six months) if the water is highly oxygenated (Brown, 1944, Roots, 1956). The excretory system is composed of a series of coiled tubes called nephridia (sing, nephridium). These are the main organs for nitrogenous excretion in earthworms. In the Lumbricidae, they are paired organs in each segment except the first three and the last. A nephridium occupies part of two successive seg- ments where the nephrostome, or funnel, is in the anterior segment and the coiled tube and nephridial bladder are in the posterior segment. The nephridial bladder passes through the body wall opening to the outside forming the neph- ropore. The position of the nephropore, as well as the structure and type of ne- phridium, are used as taxonomic characters. The most complete discussion of nephridia and their classification was presented by Bahl ( 1947). The nervous system is concentrated, with a bilobed mass of nervous tissue (cerebral ganglia) on the dorsal surface of the pharynx which is connected to subpharyngeal ganglia by a pair of circumpharyngeal connectives. The nerve cord, a fusion of the circumpharyngeal connectives, extends caudad from the subpharyngeal ganglia ventrally between the alimentary canal and the body wall (Fig. 2). In each segment, posterior to iv, a ganglion is formed and three pairs of nerves (peripheral nervous system), one pair anterior to the ganglion and two pairs posterior to the ganglion, extend to the motor and sensory areas. The nervous system is another portion of somatic anatomy that has not yet achieved its proper position in oligochaete systematics. The reproductive system has long been used as the main source of taxonomic characters. In amphimictic species the male gonads are paired testes found in segments x and xi close to the anterior septa, a condition termed holandric. An- terior to each testis, in segments ix and x, and also posteriorly in segments xi 16 and \ii. lobed seminal vesicles occur in which the sperm develop. Sperm are transferred via the sperm tunnel and sperm ducts to a vas deferens that may traverse several segments before opening to a male gonopore. The female go- nads are represented b) a pair o\ gonads found in segment xiii. Ripe oocytes pass through the coelomic fluid into ovisacs which lead via an oviduct to the fe- male genital pore. In each of segments ix and x there is a pair of sac-like organs, opening ventrallv. that receive the sperm during copulation. These are the sper- mathecae. In recent years the inadequacies and inconsistencies of reproductive charac- ters in taxonomy have been discussed (Reynolds et al., 1974; Reynolds, 1974c; Gates, 1974a). Unfortunately, statements such as "Oligochaetes are hermaphro- dite, and have more complicated genital systems than unisexual animals" (Ed- wards and Lofty. 1972) are true onlv in the broadest sense (cf. Reynolds, 1974c). In this study, eight of the 18 lumbricids are parthenogenetic (or unisexual). In megadriles. only the clitellum. ovaries, oviducts, and possibly ovisacs are essen- tial to reproduction (cf. Gates, 1974a; Reynolds, 1974c). Therefore, when repro- duction is parthenogenetic all of the following are no longer required: testes, seminal vesicles, seminal receptacles, vas deferens, copulatory chambers, copu- latory penes, prostates and ducts, genital markings, spermathecae, tubercula pu- bertates. genital and penial setae. The external position and morphology of the genital apertures, setae and tumescences, clitella. and tubercula pubertates have been widely used in lumbri- cid identification. If these characters are constant for a given species, they are excellent simple characters that non-specialists can use with reliability. 17 Glossary A, B, C, D These single capital letters refer to the meridians oflongitude pass- ing anteroposteriorly along the aper- tures of the respective setal follicles. Thus, A represents a line along the a, the most ventrally located setal folli- cles. ss 1 . | . 1 • / -!• c lj A AA, BB, CC, DD See setal formula. acinus (Fr. acine m.) A sac-like termination of a branched gland. aclitellate adults (Fr. adultes sans clitellum, anteclitellienne f.) These are prere- productive individuals without a clitellum but in which genital markings are obvious. The second number in the age classification formula (q.v.) refers to such individuals. adiverticulate (Fr. sans diverticule) Without diverticula, and usually referring to spermathecae. aestivation (Fr. estivation f., anhydrobiose) A period of inactivity, or dormancy, resulting from unfavourable moisture conditions. age classification formula A series of numbers following a binomen (usually three or four numbers) separated by dashes indicating the number of: juveniles — aclitellate adults — clitellate adults — postclitellate adults in a col- lection. If there are no postclitellate adults in the collection the final zero is omitted from the formula. See juveniles, aclitellate adults, clitellate adults, postclitellate adults. amphigony See amphimixis. amphimixis (Fr. amphimixie f.) Reproduction involving fertilization of an ovum by a sperm. In megadriles the same as biparental reproduction. Cf. par- thenogenesis. anal segment See periproct. anastomosis (Fr. anastomose f.) Cross connections of ducts, branches of or- gans, or, more usually, of blood vessels. anthropochore (Fr. anthropochore) Transported by man, usually unintentional- ly. Cf. peregrine. aortic arch See hearts. 18 asetal (Fr. sans soies) Without setae. Ct\ peristomium, periproct. atrial gland (Fr. glande atriole f.) Glandular tissue associated with a cleft or coelomic invagination containing the male pore. blood glands (Fr. glandes sanguines f.) Follicles clustered in the pharyngeal re- gion, supposed to function in the production of haemoglobin and blood cor- puscles. brain (Fr. cerveau m.) See cerebral ganglion. buccal cavity (Fr. cavite buccal f.) (be) The first region of the alimentary canal, between mouth and pharynx (Fig. 2). C. Abbreviation for circumference (in German publications replaced by U). See setal formula. caecum (Fr. caecum m.) A blind diverticulum or pouch from the alimentary canal. calciferous gland (Fr. glande de Morren, glande calcifere f.) (cag) Whitish gland that secretes calcium carbonate and opens into the gut via the oesophageal pouches. In Lumbricidae. it is generally found in segments x-xiv. castings (Fr. dejections de surface f., turricules m.) Faeces, the voided earth and other waste matter that are commonly deposited on the surface of the ground. Not all species, however, form their casts above the ground. cephalization (Fr. cephalisation f.) The loss of metameric uniformity at the an- terior end of the body. cerebral ganglion (Fr. ganglion cerebral m.) (eg) Concentrated nerve cells above the alimentary canal that function as a simple brain (Fig. 2). cf. (confer) Compare. ehaeta See seta. chloragogen cells (Fr. cellules chloragogues f.) (chl) Cells surrounding the ali- mentary canal; their function is uncertain but is attributed to excretion and regeneration in the literature (Fig. 3). unguium See clitellum. circumpharyngeal connective (Fr. connectif circumpharyngien m.) (epe) Nerve collar, between cerebral ganglion and ventral nerve ganglion (Fig. 2). clitellate adult (Fr. adulte avec clitellum, clitellienne f.) Those individuals with 19 developed clitellum and genital markings. The third number in the age clas- sification formula (q.v.) refers to these individuals. clitellum (Fr. clitellum m.) (cl) A regional epidermal swelling where gland cells secrete material to form the cocoon. There are two types recognizable. An an- nular clitellum or cingulum (Fr. anneau m.) encircles the body whereas a cli- tellum that encompasses only the dorsal and lateral parts of the body is refer- red to as a saddle (Fr. selle f.). The convention xxvi, xxvii-xxxii, xxxiii means that the clitellum is generally found on segments xxvii-xxxii, but may in some individuals overlap onto segments xxvi and/or xxxiii. SADDLE ANNULAR In the case of Eisenia rosea the clitellum has been termed flared. This ventral flared condition is easily recognizable. FLARED NON-FLARED coelom (Fr. cavite coelomique, coelome f.) (elm) The body cavity between the body wall and the alimentary canal (Fig. 3). congeneric (Fr. congenere) Belonging to the same genus. copulation (Fr. accouplement m., copulation f.) Sexual union, mating. crop (Ft. jabot m.) (cr) A widened portion of the digestive system that lacks the muscularity of the gizzard, in Lumbricidae anterior to the gizzard and poste- rior to the oesophagus (Fig. 2). cuticle (Fr. cuticule f.) (cut) A thin, non-cellular, colourless, transparent outer layer of the body wall. See iridescence 2. diapause (Fr. diapause f.) An obligatory resting stage in development. digitiform (Fr. digit if orme) Finger-shaped. dorsal pore (Fr. pore dorsal m.) (dp) Small single in- tersegmental apertures in the mid-dorsal line (mD) leading to the coelomic cavity (Fig. 3). The con- vention first dorsal pore 5/6 means that the dorsal pore is found in the intersegmental furrow between segments v and vi. 20 dorsal vessel (Fr. vaisseau dorsal m.) (dv) A major blood vessel located above the dorsal surface of the alimentarx canal (Figs. 2, 3). ectal Outer, external, toward the body wall. egg sac See ovisac. endemic (Fr. endemique) Restricted to a certain region or part of a region, na- tive. Cf. exotic, indigenous. ental Inner, internal, away from the body wall. epidermis (Fr. epiderme m.) (epi) The outer cellular layer of the body wall, which secretes a protective cuticle (Fig. 3). epilubic (Fr. epilobique) See prostomium. eq. Equatorial, see mL. euryoecious (Fr. eurvoeciques) Having a wide range of habitat tolerance. exoic (Fr. exoique) Opening to the exterior through the epidermis, referring to the excretory system. exotic (Fr. exotique) Introduced, foreign. Cf. endemic, indigenous. facultative (Fr.facultatiJ) Conditional, having the power to live under different conditions. Cf. obligatory. female ducts Gonoducts. See oviducts. female pores ( Fr. pores femelles m.) (fp) The external openings for the oviducts on segment xiv (Lumbricidae) and ventrad of the mid-lateral line. They are usually more difficult to see than the male pores. fide On the authority of, or with reference to publication, to a cited published statement. flared clitellum ( Fr. clitellum evasse m.) See clitellum. genital markings (Fr. mamelons antiarrheniques, mamelons periarrheniques m.) (GM) Glandular swellings, pits or grooves of the epidermis. See genital tumescences. genital setae (Fr. soies genitales f.) (GS) See setae. 21 genital tumescences (Fr. papille puberculienne f.) (GT) In Lumbricidae, areas of modified epidermis (glandular swellings) without distinct boundaries and through which follicles of genital setae open. -GT cl- girdle See clitellum. gizzard (Fr. gesier m.) (g) The muscularized portion of the digestive system, in Lumbricidae, anterior to the intestine and posterior to the crop (Fig. 2). gonopore (Fr. gonopore m.) See male pores, female pores. hearts (Fr. coeurs m.) (h) The enlarged, segmental, pulsating connectives of the blood system between the ventral and one or two other longitudinal trunks (e.g., dorsal and/or supra-oesophageal) (Fig. 2). hemerobiont A species dependent on human culture. hemerodiaphore A species indifferent to the influence of human culture. hemerophile A species favoured by human culture. hemerophobe A species averse to the influence of human culture. hibernation (Fr. hibernation f.) A period of inactivity or dormancy resulting from unfavourable temperature conditions. holandric (Fr. holandrique) The condition where the testes are restricted to segments x and xi, or a homoeotic equivalent. holoic (Fr. holonephridique) The condition of having a pair of stomate, exoic nephridia in each segment of the body except the first and last. homoeotic (Fr. homoeotique) The condition of having glands or organs in a segment(s) where they do not normally occur. Refers principally to intraspe- cific variation. indigenous (Fr. indigene) Belonging to a locality, not imported, native. Cf. en- demic, exotic. 22 in lift. (//; liiteris) In correspondence. intersegmental furrow (Fr. sillon intersegmen- taire m.) (if) The boundary between two con- secutive segments; the area where the epider- mis is thinnest and where, in pigmented spec- ies, colour is lacking. > -&. — > 3 r? ^ > 4 -J iridescence (Fr. irisation, iridescence f.) In the context of earthworm biology this refers to 1) the appearance of sperm aggregated on the male funnels (q.v.), or 2) the appearance of cuticular colour as a result of refracted light. juveniles (Fr. lanes f.) Those individuals with no recognizable genital mark- ings such as the clitellum. tubercula pubertatis. tumescences, etc.. i.e., in the life stage between hatching and the appearance of genital markings. The first number in the age classification formula (q.v.) refers to these individuals. lamella (Fr. lamelle f.) Any thin plate- or scale-like structure. mD (Fr. medio-dorsale) Mid-dorsal line. mL (Fr. medio-laterale) Mid-lateral line. raV (Fr. medio-venirale) Mid-ventral line. male funnel (Fr. entonnir male m.) (mf) The enlargement of the ental end of a sperm duct with a central aperture through which sperm pass into the lumen of the duct on their way to the exterior. Sperm may temporarily aggregate on the funnels, prior to entering the ducts, their presence being indicated by ir- idescence (q.v.). male pores (Fr. pores males m.) (mp) The external openings for the male ducts through which sperm are liberated during copulation. In Lumbricidae they are usually conspicuous near the mL on segment xv; any variation is noted in the diagnosis. 23 male sterility (Fr. sterilite male f.) Often cited as evidence for parthenogenesis (q.v.) and may be indicated by the following: 1) adult retention of juvenile testes, 2) adults with juvenile seminal vesicles and no evidence of sperm, 3) the absence at maturity of iridescence on the male funnels, indicating that there are no mature sperm aggregations, 4) the absence of similar iridescences in the male ducts and/or spermathecae, and 5) the absence of externally ad- hesive spermatophores. These criteria will only suggest male sterility in any given individual and many cases of repeated evidence are required before a species can be considered male sterile or parthenogenetic. megadrile (Fr. megadrile m.) Sensu Gates (1972c: 29) and Reynolds and Cook (1977), this term is synonymous with terrestrial oligochaetes. There is some morphological basis for the megadrile/microdrile division of the Oligochaeta (cf. Gates, 1972c). Brinkhurst (in Brinkhurst and Jamieson, 1971: 104) em- ploys microdrile as a major heading when discussing the aquatic oligochaetes. In general, these old terms are used to describe terrestrial and aquatic oligo- chaetes without any systematic judgments. mesial (Fr. medial) In the middle vertical or longitudinal plane. metamere (Fr. metamere m.) A segment. moniliform (Fr. moniliforme) Arranged like a string of beads. monotypy (Fr. monotypie f.) The situation arising when a genus-group taxon is established with only one originally included species; or when a family-group taxon is established with only one originally included genus. morph (Fr. forme f., morph f.) A group of individuals that share a common anatomy resulting from degradations, deletions, or other changes from struc- ture of the ancestral amphimictic population caused by reproductive isola- tion. Such isolation usually comes about as a result of parthogenesis. Morren's gland See calciferous gland. mouth (Fr. bouche f.) (m) The anterior opening to the alimentary canal located in the peristomium. mouth cavity See buccal cavity. muscular tube See nephridial bladder. nearctie (Fr. nearctique) A zoogeographical region including Canada, the United States, Greenland, and northern Mexico. neotype (Fr. neotype m.) A single specimen designated as the type specimen of a nominal species-group taxon of which the holotype (or lectotype). and all 24 paratypes or all s\ni\pes are lost or destroyed. Neotypification is the act of selecting a neotype. (For nominal taxon, see taxon.) nephridial bladder (Fr. vesicule de la nephridie f.) (nb) The extended portion of the nephridial tube connected to the nephropore (Fig. 3). nephridial pore See nephropore. nephridial reservoir See nephridial bladder. nephridiopore See nephropore. nephridium (pi. nephridia) (Fr. nephridie f.) (n) The organ for nitrogenous ex- cretion (Figs. 2. 3). nephropore (Fr. nephridiopore m.) (np) The external opening of a nephridium (Fig. 3). nephrostome (Fr. nephrostome m.) (ns) The ciliated funnel at the ental end of the nephridium (Fig. 3). obligator) (Fr. obligatoire) Limited to one mode of life or action. Cf. faculta- tive. oesophagus (Fr. oesophage m.) (es) The portion of the gut between the pharynx (anterior) and crop (posterior), ending in an oesophageal valve (Fig. 2). omnivorous (Fr. omnivore) Eating both animal and plant tissue. op. cit. (opere citato) In the work or article previously cited for this writer (no page cited). ovary (Fr. ovaire m.) (o) The organ for ova (egg) production (Fig. 2). oviducal pores See female pores. oviduct (Fr. oviducte m.) (od) The duct carrying the ova from the coelomic fun- nel to the exterior (Fig. 2). ovisac (Fr. ovisac m.) (os) An egg-capsule or receptacle (Fig. 2). ovum (pi. ova) (Fr. ovule, oeufm.) The female germ cell, matured egg-cell. palaearctic (Fr. paleoarctique) A zoogeographical region including all of Eu- rope and the U.S.S.R. to the Pacific Ocean, Africa north of the Sahara Desert, and Asia north of the Himalaya Mountains. 25 papilla (FT.papille f.) A protruding dermal structure. parietes ( Fr. parietes m.) Walls or sides of structures. parthenogenesis (Fr. parthenogenese f.) Uniparental reproduction in which the ova develop without fertilization by spermatozoa. Cf. amphimictic. penial setae (Fr. soies de la verge m.) See seta. peregrine (Ft. peregrin) Widely distributed, not necessarily involving man. periproct (Fr. pygidium m.) (pp) The terminal (last, caudal) "segment" of the body, without coelomic cavity, asetal. peristomium (Fr. peristomium m.) (ps) The first body segment, asetal, and con- taining the mouth (Fig. 2). pH (Fr./?// m.) An indication of acidity or alkalinity measured as the negative logarithm of the hydrogen-ion concentration, and expressed in terms of the pH scale (0-14) where pH 7 is neutral, less than 7 is acidic, and more than 7 is alkaline. Previously, North American studies employed an aqueous solution to make soil pH readings, and these are the figures given in the text, but varia- tions can occur when the amount of water present in the soil changes as well as when the amount of dissolved gases in this water, e.g., C02, changes. To overcome these variations in the pH readings, one of several salt solutions of differing strengths may be employed instead of water, e.g., KC1 or CaCl:. (For details, see Peech, 1965.) pharynx (Ft. pharynx m.) (ph) The portion of the gut between the buccal cavity (anterior) and the oesophagus (posterior) (Fig. 2). pinnate (Fr.penne) Divided in a feathery manner. polymorphism (Fr. polymorphisme m.) Occurrence of different forms of individ- uals within the same species. postclitellate adult (Fr. adulte apres clitellum, postclitellienne f.) Postreproduc- tive individuals without a clitellum but with areas of discolouration in the re- gions of the clitellum, and with genital markings. If these discolourations 26 disappear (which is not abnormal), differentiation between aclitellate adults and postclitellate adults may be impossible even after dissection. These indi- viduals have reverted to an aclitellate state and in the future may become eli- te 1 1 u t e again and be reproductive. The fourth number in the age classification formula refers to these individuals, but if such individuals are not present in the sample then this fourth figure is omitted instead of using a zero. prostates (Fr. prostates f.) In Lumbricidae. the same as atrial glands, and of unknown function. prostatic pores (Fr. pores prostatique m.) See male pores. prostoniium (Fr. prostomium m.) (pr) The anterior lobe projecting in front of the peristomium and above the mouth. There are four types as seen in dorsal view: EPILOBIC » ■ PROLOBIC * ' TANYLOBIC ' "ZYGOLOBIC1 1) Epilobic: tongue of the prostomium partly divides the peristomium. 2) Prolo- bic: prostomium demarcated from the peristomium without a tongue. 3) Tany- lobic: with a tongue that completely divides the peristomium. 4) Zygolobic: prostomium not demarcated in any way. pseudogamy (Fr. pseudogamy) The activitation of ova by a sperm without nu- clear fusion and thus without true fertilization. pygidium See periproct. pygomere See periproct. pyriform ( Fr. pyriforme) Pear-shaped. quiescence (Fr. quiescence f.) A period of inactivity, or dormancy, resulting from an unfavourable environment; cf. aestivation and hibernation. q.v. (quod vide) Which see. ridge of puberty (Fr. cretes depuberte f.) See tubercula pubertatis. sacculate (Fr. saccule m.) Provided with sacculi, small sacs or pouches, saddle See clitellum. 27 secondary annulation (Fr. sillons transversaux m.) (sa) The furrows which occur between the intersegmental furrows (q.v.). These demarcations are only exter- nal and are labelled a, /?, or y. mD segment (Fr. segment m.) A portion of the body, along the anteroposterior axis, be- tween two consecutive intersegmental fur- rows and the associated septa. Segments are numbered with lower case roman nu- merals, i, ii, iii, etc., beginning anteriorly with the peristomium as i. The older sys- tem and some microdrile workers used up- per case numerals, I, II, III, etc. seminal receptacles See spermathecae. seminal reservoirs See seminal vesicles. Trr seminal vesicles (Fr. vesieules seminales f.) (sv) The storage sacs for an earthworm's own sperm until copulation. septum (pi. septa) (Fr. cloison f.) (sep) The internal partition at intersegmental furrows. Also acts as a supporting membrane for internal organs (Fig. 2). seta (Fr. soie f.) (s) A solid rod or bristle se- creted by cells at the ental end of a tubular epidermal ingrowth, the setal follicle. Setae are of several types: 1) general: sigmoid shape with pointed outer tip; 2) genital: asso- ciated with genital tumescences and/or go- nopores, and not sigmoid; 3) penial: associ- ated with the male pores and not sigmoid. Individual setae are referred to as a, b, c, dy as shown in the first diagram of this Glossary, a being the most ventral and d the most lateral of the setae on a particular segment. GENERAL PENIAL 28 setal formula (Fr. des soies f.) The distance between ^DD-^/ the setae, usually measured on segments x and/or \^NA0 xxx, and being an estimate of the space between the / \ \_ A. B, C. and D meridians (q.v.). The data can be ex- I ^_ pressed as a ratio (e.g., AA:AB:BC:CD:DD = 9:3:6: Jj» /* JL 2:30), as groupings (e.g., AA >BC BC, DD = ','2 C anteriorly, and DD < Vi C posteriorly. Setae c and d on x often on white genital tumescences. Male pores in xv with large elevated glandular papillae extending over xiv and xvi. Seminal vesicles, four pairs in 9-12. Sper- mathecae, three pairs opening on level cd in 8/9, 9/10 and 10/1 1. Colour varia- ble, frequently green but sometimes yellow, pink, or grey. Body cylindrical. Biology This species has been found in a wide variety of soil types, with a pH of 4.5-8.0, including gardens, fields, pastures, forests, clay and peat soils, lake shores and stream banks, estuarine flats, and among all sorts of organic debris. It has been found in caves in Europe and North America and also in botanical gardens and greenhouses in these same continents. Most of the sites where A. chlorotica was obtained in the present survey were moist, low areas, such as under various forms of debris and logs in ditches, relatively close to the Great Lakes. Eaton (1942) reported the habitat preference of this species as "wet and usually highly organic or polluted soil." In eastern Tennessee almost 85% of the specimens col- lected were from wet, highly organic habitats (Reynolds et al., 1974). In appropriate conditions activity, including breeding, possibly occurs all year. In the northern part of the range there may be a single period of activity in the summer. There are records of active specimens occurring 300 mm below the soil surface although the species generally is characterized as shallow burrow- id 1st dp xxx XXV XXXV Fig. 4 External longitudinal views of Allolobophora chlorotica showing taxonomic characters, a. Dorsolateral view. B Ventrolateral view. (ONT: Haldimand Co., cat. no. 734 1) 37 ing. Defecation occurs below the soil surface as does copulation. A. chlorotica is obligatorily amphimictic (Reynolds, 1974c). This species has been reported as the secondarily preferred host of the cluster fly, Pollenia rudis (Fabr.) (Yahnke and George, 1972; Thomson and Davies, 1973b); otherwise it is of minimal economic importance. It seems not to be pre- ferred by fish, and anglers have found little use for it as bait. Range A native of Palaearctis, A. chlorotica is known from Europe, Iran, North Ameri- ca, South America, North Africa, and New Zealand (Gates, 1972c). North American Distribution British Columbia (Smith, 1917). New Brunswick (Reynolds, 1976d), Nova Scotia (Reynolds, 1975a, 1976a), Ontario (Reynolds, 1972a), Quebec (Reynolds, 1975b, d, e, 1976c), Arizona (Gates, 1967), California (Smith, 1917), Connecticut (Reynolds, 1973c). Delaware (Reynolds, 1973a), District of Columbia (Smith, 1917), Idaho (Gates, 1967), Illinois (Smith. 1928), Indiana (Smith. 1917), Maine (Gates, 1961), Maryland (Reynolds, 1974b). Massachusetts (Reynolds. 1977). Michigan (Murchie, 1956), Missouri (Olson, 1936), Montana (Reynolds, 1972c), Nevada (Gates, 1967), New York (Ol- son, 1940), North Carolina (Smith, 1917), Ohio (Olson, 1928), Oregon (MacNab and McKey-Fend- er, 1947), Pennsylvania (Eaton, 1942), Tennessee (Reynolds, 1972b), Utah (Gates, 1967), Vermont (Gates, 1972c), Virginia (Gates, 1949), Washington (MacNab and McKey-Fender, 1947). West Vir- ginia (Williams, 1942), Wisconsin (Gates, 1972c), Greenland (Levinsen. 1884). New records: Mani- toba, Alaska, Minnesota. Ontario Distribution (Fig. 5) CARLETON CO. Reynolds (1972a); *Ottawa-Carleton Rd 34, Cumberland, under paper, 1 1 May 72, JWR, 0-0-1. DUNDAS CO. *Hwy 2, 5 km w of Iroquois, under logs, 11 May 72. JWR. 0-1-0. *Hwy 43, 1.29 km e of Chesterville, under rocks in ditch, 1 1 May 72, JWR. 0-0-4. 'Hwy 31. 2.1 km s of Winchester Springs, under logs, 11 May 72, JWR, 0-0-3. DURHAM CO. 'Hwy 401. .16 km w of Liberty Rd, Bowmanville, digging under log by railroad tracks, 15 May 72, JWR, 1-0-1. ELGIN CO. *Hwy 73, 3.06 km s of Harnettsville, under rotten log, 4 May 72, JWR. 0-1-1. *Hwy 73. 6.77 km n of Aylmer, under logs, 4 May 72, JWR, 3-2-4. *Hwy 3, 6.77 km e of Wallacetown, under pine logs, 4 May 72. JWR, 0-1-0. Hwy 3, 7.9 km w of Frome, under logs. 4 May 72, JWR, 0-0-7. ESSEX CO. •Hwy 3, 1.45kmeofCottam, under logs, 4 May 72, JWR, 1-1-8. FRONTENAC CO. *Hwy 2. 1.13 km e of Westbrook, under logs and paper, 16 May 72, JWR, 0-0-10. *Hwy 15, 4.03 km n of Hwy 401, under paper in wet ditch, 16 May 72, JWR, 0-0-1. GRENVILLE CO. *Hwy 2. Johnstown, w.e., under logs, 1 1 May 72. JWR, 0-1-4. HALDIMAND CO. *Hwy 54, 2.26 km n of Caledonia, digging, 3 May 72. JWR. 2-2-0. H ALTON CO. *Hwy 7, 4.84 km e of Georgetown, under burnt logs in soil. 4 May 73, JWR, 0-0-2. HASTINGS CO. *Hwy Jet 2 and 49. wet ditch, 15 May 72. JWR, 0-2-37. HU- RON CO. *Hwy 4, 1.29 km s of Wingham, under logs in wet area, 5 May 72, JWR, 0-5-7. KENT CO. 'River Rd, 6.45 km w of Chatham, under logs, 23 Apr 72, JWR & TW, 0-1-0. Hwy 3, 1.77 km w of Palmyra, under logs, 4 May 72, JWR, 1-2-15. LAMBTON CO. Hwy 21. 2.1 km n of Wyoming, under logs in wet ditch, 4 May 72, JWR, 0-0-10. LANARK CO. *Hwy 43, 3.71 km e of Smiths Falls, under telephone pole in ditch, 1 1 May 72, JWR, 0-0-18. LEEDS CO. *Hwy 15, 2.26 km n of Seeley's Bay, under logs and concrete blocks in ditch. 16 May 72. JWR, 10-2-15. LENNOX AND AD- DINGTON CO. *Hwy 2, 9.68 km w of Napanee. under paper in wet ditch. 15 May 72. JWR, 8-2- 17. MIDDLESEX CO. Judd ( 1970). *Hwy 7, 2.26 km s of Parkhill, under posts. 4 May 72. JWR. I- 1-1. NIAGARA CO. 'Niagara Co Rd 12, 3.06 km s of Grimsby, under paper in wet ditch, I May 72, JWR. 0-1-9. NIPISSING DIST. 'Hwy 17. 1.29 km e of Verner, under paper in wet ditch. 13 May 72. JWR & JEM, 1-1-2. NORTHUMBERLAND CO. 'Northumberland-Durham Rd 1. .65 km w of Hwy 33, under logs, 15 May 72, JWR, 3-0-3. ONTARIO CO. 'Hwy 7. 1.61 km e of Green 38 Fig. 5 The known Ontario distribution of A llolobophora chlorotica. River, under logs. 26 Apr 72. JWR. 2-0-9. PEEL CO. *Hwy 5. .81 km e of Dixie Rd. 29 Apr 72, JYVR. 0-0-2. »Hwy 7. Brampton, e.e.. under debris. 4 May 73, JWR, 0-0-2. Hwy 401, 1.3 km w of Dixie Rd. wet ditch. 4 Mav 73. JWR, 0-0-1. PERTH CO. 'Mitchell, next to Collegiate, under logs, 4 Slav 73. JWR & DWR, 2-3-2. PRESCOTT CO. *Hwy 34, 2.58 km n of Vankleek Hill, under logs and rocks. 11 May 72. JWR. 1-2-6. PRINCE EDWARD CO. *Hwy 33, 1.61 km s of Carrying Place, under log in wet ditch, 15 May 72, JWR. 3-0-8. *Hwy 33. Consecon, n.e.. dump, 15 May 72, JWR, 0-0-1. 'Hwy 33, 2.58 km e of Hillier. digging. 15 May 72. JWR. 0-3-0. Indian Point, in grab sample, approximately 1 metre depth in Lake Ontario. 24 Jul 74, DRB, 1-0-2, UW-0001. STORMONT CO. *Hwy 43. 5.48 km w of Finch, in and under wet straw in wet ditch, 11 May 72, JWR. 0-0-42. WATERLOO CO. Waterloo. Amos Ave.. 1 Sep 75. DPS, 1-3-0. UW-0003. WENTWORTH CO. Reynolds (1972a). *Hwy 5, Waterdown, e.e, edge of corn (Zea maize L.) field, 29 Apr 72, JWR, 0- 0-4. YORK CO. 'Edenbrook Park, Islington, under logs and rocks near stream bank, 30 Apr 72, JWR & DWR. 1-1-2. Scarborough, 21 Kingston Rd.. small wooded valley, 30 Nov 41, JO. 0-0-1. ROM. 39 Genus Aporrectodea Or ley, 1885 1885 Aporrectodea Orley, Ertek. Term. Magyar Akad. 15(18): 22. 1900 AUolobophora (part.)-Michaelsen, Das Tierreich, Oligochaeta 10: 480. 1930 AUolobophora (part.)-Stephenson, Oligochaeta, p. 905, 906, 907, 908. 1 94 1 A Uolobophora (part.)-Pop, Zool. Jb. Syst. 74: 20. 1956 AUolobophora (part.)-Omodeo, Arch. Zool. It. 41 : 180. 1972 AUolobophora (part.)-Gates, Trans. Amer. Philos. Soc. 62(7): 68, 69. 1972 Allolobophora-Gates, Bull. Tall Timbers Res. Stn. 12:2. 1972 Nicodrilus Bouche, Inst. Natn. Rech. Agron., p. 315. 1975 Aporrectodea-Ga\es, Megadrilogica 2(1): 4. Type Species Lumbricus trapezoides Duges, 1828. Diagnosis Calciferous gland, opening into gut through a pair of vertical sacs equatorially in x. Calciferous lamellae continued onto posterior walls of sacs. Gizzard, mostly in xvii. Extraoesophageal vessels, passing to dorsal trunk in xii. Hearts, in vi-xi. Nephridial bladders, ^/-shaped, ducts passing into parieties near B. Nephropores, inconspicuous, irregularly alternating between levels slightly above B and above D. Setae, paired. Prostomium, epilobic. Longitudinal mus- culature, pinnate. Pigment, if present, not red (after Gates, 1975a: 4). Discussion This forgotten genus originally included Enterion chloroticum Savigny, 1 826 and Lumbricus trapezoides Duges, 1828. Since Omodeo (1956) designated the former as the type species of AUolobophora, the latter automatically becomes the type for Aporrectodea. Bouche (1972) erected a new genus Nicodrilus with Enterion caliginosum Savigny, 1826 as the type and included Lumbricus trapezoides Dug- es, 1828 in this new genus. Since Aporrectodea is a valid and available genus, Nicodrilus must be considered the junior synonym of Aporrectodea. Aporrectodea icterica (Savigny, 1826) Mottled worm Ver marbre (Fig. 6) 1826 Enterion ictericum Savigny, Mem. Acad. Sci. Inst. Fr. 5: 183. 1837 Lumbricus /'c7m'cu.y-Duges, Ann. Sci. Nat., ser. 2, 8: 17. 1886 AUolobophora icterica-Rosa, Atti 1st. Veneto, ser. 6, 4: 685. 1900 Helodrilus /c/en'cw^-Michaelsen, Das Tierreich, Oligochaeta 10: 500. 1926 Bimastus / xv te . ;J GT cl XX, XXV -■ 1 — -li XXX XXXVI xl< I . — -5J1 xlv TP. xx XXV XXX -GT Fig. 6 External longitudinal views of Aporrectodea icierica showing taxonomic characters, a. Lat- eral view, b Ventral view. (ONT: Wellington Co., cat. no. ROM 148) 41 Diagnosis Length 55-135 mm, diameter 3-5 mm, segment number 140-190, prostomium epilobic, first dorsal pore 4/5. Clitellum xxxiii, xxxiv-xlii, xliii. Tubercula puber- tals in the form of a band xxxiv, xxxv-xli, xlii, xliii. Setae closely paired, poste- riorly AA.AB.BCCD = 45:5:25:4; c and d in form of genital tumescences in ix and a and b in xi-xvii, xxix-xxxiv, and xlii-xlv. Male pores on xv, minute, about at mid BC, with tumescences small and restricted to xv. Seminal vesicles, four pairs in 9-12, the anterior two pairs smaller. Spermathecae, three pairs with ducts opening on level c in 8/9-10/11, sometimes an anterior pair opening in 7/8. Colour, lacking. Body cylindrical. Biology In Europe Cernosvitov and Evans (1947), Gerard (1964), and Tetry (1938) re- ported the species from garden soil, meadows, and orchards. With the exception of Bouche's (1972) study in France, Ap. icterica has been reported infrequently and in low numbers in Europe. The species is obligatorily amphimictic (Gates, 1968). Ap. icterica is not known to have any economic importance. Range A native of Palaearctis, Ap. icterica is now known from western Europe and North America (Reynolds, 1976e; Schwert, 1977). Fig. 7 The known Ontario distribution of A porreclodea icterica. 42 North American Distribution Ontario (Schwert. 1977), New York (Reynolds. 1976e). Ontario Distribution (Fig. 7) WELLINGTON CO. Schwert~(1977). University of Guelph Arboretum, May-Jul 1976, DPS. Aporrectodea longa (Ude, 1885) Black head worm Ver a tete noire (Fig. 8) 1826 Enterion terrestre (non 1820) Savigny, Mem. Acad. Sci. Inst. Fr. 5: 180. 1837 Lumbricus terrestris-Duges, Ann. Sci. Nat., ser. 2, 8: 17, 18. 1845 Lumbricus agricola (non 1842) (part.) Hoffmeister, Regenwiirmer, p. 5. 1885 A llolobophora longa Ude, Z. Wiss. Zool. 43 : 1 36. 1889 Lumbricus terrestris + L. longus-L. Vaillant, Hist. Nat. Annel. 3(1): 113, 121. 1893 A llolobophora terrestris-Rosa, Mem. Ace. Torino, ser. 2, 43: 424, 444. 1900 Helodrilus (A llolobophora) / 130, prostomium epilobic, first dorsal pore 12/13, usually. Clitellum xxvii, xxviii-xxxiii, xxxiv. Tubercula pubertatis xxxi-xxxiii. Setae closely paired, pos- teriorly AA > AB, DD < V2C. Genital tumescences including a and b setae only, in ix-xi, xxxii-xxxiv, often in xxviii and occasionally in the region of xxvi-xxix. Male pores on xv. Seminal vesicles, four pairs in 9-12. Spermathecae, two pairs opening in 9/10 and 10/1 1. Colour variable and often lighter behind the clitellum until near the hind end, then deeper, slate, brown, brownish, red- dish brown, and occasionally almost reddish, but not purple. Body dorsoven- trally flattened posteriorly so that a cross section is nearly transversely rectangu- lar with setal couples at the corners. Biology This species is found in a wide variety of habitats, according to the material examined by Gates (1972a). Similar statements have been made by Smith (1917), Olson (1928), Eaton (1942), Gates (1967), Reynolds (1973 a-c), and Rey- nolds et al. (1974). According to Gates (1972a, c) Ap. trapezoides is found in the earth around the roots of potted plants, in gardens, cultivated fields, forest soils of various types, on the banks of streams, and sometimes in sandy soil. It has been recorded from caves in North America and Afghanistan, and in California and Arizona may occur at elevations of 1525 m or more. Activity may be year round under suitable conditions but it is not possible yet 46 to make a similar statement concerning breeding. Ap. trapezoids is partheno- genetic, sometimes with pseudogamy, and male sterility is also common (Gates, 1972c; Reynolds, 1974c). I his species is often found in earthworm culture beds and is one of the five species commonl) sold and used for bait in North America (Gates, 1972c). It should be noted that many literature records of this species must be treated with caution because oi' taxonomic confusion. For a long time Ap. trapezoides was considered to be a variety of subspecies of A caliginosa but it is unlikely that all references to A. caliginosa subspecies, variety, or forma, trapezoides do in fact refer to Ap. trapezoides (cf. Gates, 1972a: 4). mp xv xxxv XXXVIII Fig. 10 External longitudinal views of Aporrectodea trapezoides showing taxonomic characters, a. Lateral view, b Ventral view. (ONT. Waterloo Co., cat. no. 8002) 47 Range A native of Palaearctis, Ap. trapezoides is now known from Europe, North America, South America, Africa, Asia, and Australasia (Gates, 1972c), and also from Iceland (Backlund, 1949). North American Distribution Alberta (Gates. 1972a). British Columbia (Gates. 1972a). Manitoba (Gates, 1972a). New Brunswick (Resnolds, 1976d). Nova Scotia (Reynolds, 1975a. 1976a). Ontario (Reynolds. 1972a). Prince Ed- ward Island (Reynolds, 1975c), Quebec (Reynolds. 1975b. e. 1976c). Alabama (Gales. 1972a), Alaska (Gates, 1972a) Arizona (Gates, 1972a). Arkansas (Gates. 1972a). California (Gates. 1967). Colorado (Gates. 1967). Connecticut (Resnolds. 1973c). Delaware (Reynolds. 1973a). District of Columbia (Gates. 1966). Florida (Gates, 1972a). Georgia (Gates. 1972a). Idaho (Gates. 1967). Illi- nois (Gates, 1972a), Indiana (Gates, 1972a). Iowa (Gates. 1967). Kentucky (Gates, 1959). Louisiana (Harman. 1952). Maine (Gates, 1966). Maryland (Reynolds. 1974b). Massachusetts (Reynolds, 1977). Michigan (Gates, 1972a), Minnesota (Gates. 1972a). Mississippi (Gates, 1972a), Missouri (Gates. 1967), Montana (Reynolds. 1972c), Nebraska (Michaelsen, 1910). Nevada (Gates. 1967), New Hampshire (Gates, 1972a), New Jersey (Gates, 1972a), New Mexico (Reynolds et al.. 1974), New York (Gates, 1972a), North Carolina (Cernosvitov. 1942), Ohio (Gates. 1972a). Oklahoma (Gates. 1967). Oregon (Gates. 1972a). Pennsylvania (Gates, 1972a), Rhode Island (Reynolds, 1973b), South Carolina (Gates, 1972a), Tennessee (Reynolds, 1974a), Texas (Reddell. 1965). Utah (Gates. 1967), Virginia (Gates, 1972a), Washington (Gates, 1972c), West Virginia (Gates, 1972a), Wisconsin (Gates. 1972c). Wyoming (Gates. 1967). Ontario Distribution (Fig. 1 1) Aporrectodea trapezoides was first reported from Ontario by Reynolds (1972a). BRANT CO. *Hwy. 53, 2.74 km e of Mt. Vernon, under logs, 1 May 72. JWR, 0-0-3. »Hwy 54, 5.16 km e of Middleport, in ditch, 3May 72. JWR. 1-0-1. BRUCE CO. *Hwy 4, 6.77 km s of Teeswater. under logs, 5 May 72, JWR, 0-0-0-1. *Hwy 4, .48 km s of Hwy 9, under logs. 5 May 72, JWR, 2-4-4. Hwy 9, .81 km w of Bervie, under logs in pasture. 5 May 72. JWR. 0-0-1. *Hwy 21. 6.94 km n of Kincardine, under logs, 5 May 72, JWR, 0-3-0-1. Hwy 21. 2.76 km n of Port Elgin, under logs, 5 May 72. JWR. 6-0-2-1. CARLETON CO. *Ottawa-Carleton Rd 34. Cumberland, under paper. 1 1 May 72. JWR, 1-1-3. "Ottawa-Carleton Rd 34. .97 mi n of Leonard, under paper in wet ditch. II May 72, JWR, 2-0-4. DUFFERIN CO. *Hwy 9, 2.1 km w of Hwy 104, digging in road bank, 2 May 72, JWR. 0-0-1. *Hwy 9. 3.71 km w of Orangeville. under logs in ditch, 2 May 72. JWR, 0-0-1. DUNDAS CO. *Hwy 2. 5.48 km e of Iroquois, under logs, 1 1 May 72. JWR. 0-1-0. *Hwy 31. 2.1 km s of Winchester Springs, under logs, II May 72, JWR, 1-0-2. *Hwy 43, 1.29 km e of Chesterville. un- der rocks in ditch, 1 1 May 72, JWR, 3-0-2. *Hwy 43, 1.77 km e of Hallville, under logs. 1 1 May 72. JWR, 1-5-2. DURHAM CO. *Hwy 401, .16 km w of Liberty Rd. Bowmanville, digging under log by railroad tracks. 15 May 72, JWR, 6-0-4. ELGIN CO. *Hwy" 73. 3.06 km s of Harrietsville. under rot- ten log, 4 May 72, JWR, 1-3-1. ESSEX CO. Hwy 3. 3.87 km w of Leamington, under lumber in dump. 4 May 72, JWR, 1-1-1. *Hwv 3, Ruthven. n.e.. in wet ditch by railroad tracks. 4 May 72, JWR. 0-1-0. *Hwy 3, 1.45 km e of Cottam. under logs. 4 May 72. JWR. 1-0-11. FRONTENAC CO. •Hwy 15. 4.68 km s of Seeley's Bay. under logs, 16 May 72, JWR. 0-0-1. GLENGARRY CO. *Hwy 401, 7.42 km w of Summerstown Rd, under log, 1 1 May 72. JWR. 0-2-1. *Hwy 34, 2.58 km n of Lan- caster, under dung in pasture, 1 1 May 72. JWR, 0-0-1. *Hwy 34. 1 1.13 km n of Lancaster, under log, 1 1 May 72, JWR. 4-1-4. GRENVILLE CO. Hwy 43. Merrickville. under logs. 1 1 May 72. JWR, 1- 1-1. HALIBURTON CO. Reynolds ( 1972a). -Hwy 121, 3.22 km e of Tory Hill, dump. 16 May 72, JWR. 3-2-7. HALTON CO. *Hwy 7. 4.84 km e of Georgetown, under burnt logs in soil. 4 May 73, JWR. 0-0-1. Halton Co. Rd, 8.87 km n of llalton Co. Rd 8. wet ditch under logs by digging. 4 May 73. JWR, 0-2-0. HASTINGS CO. "Hwy Jet 62 and 620. under logs. 27 Apr 72. JWR. 0-0-1. HU- RON CO. *Hwy 4, 3.71 km s of Brucefield, under logs and rocks. 5 May 72. JWR, 0-1-0. Hwy 4, 5.16 km s of Clinton, under logs, 5 May 72, JWR. 0-0-2. *Hwy 4. 2.74 km n of Clinton, under logs. 5 May 72. JWR, 0-0-1. KENT CO. 'Hwy 3. 3.55 km e of Wheatley. digging, 4 May 72. JWR, 5-0-0. LAMBTON CO. 'Hwy 21. Edy's Mills, s.e.. under railroad ties. 4 May 72. JWR. 0-0-1. LANARK CO. *Hwy 43. 5.32 km w of Smiths falls, under logs, 1 1 May 72. JWR, 5-1-27. *Hwy 7. 5.32 km e of 48 Fig. 1 1 The known Ontario distribution of Aporreclodea irapezoides. Maberly, under dung in pasture. 1 1 May 72. JWR. 1-0-7. LEEDS CO. *Hwy 15. 3.22 km s of Mor- ton, under log. 16 May 72. JWR. 0-0-2. *Hwy 15. 4.84 km n of Elgin, digging. 16 May 72. JWR, 0- 0-7. LENNOX AND ADDINGTON CO. *Hwy 500. .81 km n of Denbigh, under logs, 16 May 72, JWR. 0-0-1 MANITOULIN DIST. »Hwy 68, 5.97 km n of Birch Island, under rocks, 13 May 72, JWR & JEM. 0-0-1. *Hwy 68. 3.06 km n of Birch Island, under logs and paper in ditch, 13 May 72, JWR & JEM. 1-2-1. ♦Hwy 68. Birch Island, s.e., under logs. 13 May 72, JWR & JEM, 1-2-4. *Hwy 68, 2.42 km s of Birch Island, under logs, 13 May 72. JWR & JEM, 0-0-3. MUSKOKA DIST. *Hwy 11. Melissa, s.e.. under paper in ditch. 9 May 72. JWR, 0-0-1. NIAGARA CO. 'Niagara Co. Rd 12, 3.06 km s of Grimsby, under paper in wet ditch, 1 May 72, JWR. 0-3-5. NIPISSING DIST. *Hwy 17, 8.39 km e of Warren, house site— digging, 13 May 72, JWR & JEM, 3-3-4. "Hwy 17, 5.48 km e of Warren, under logs and dung :n pasture, 13 May 72. JWR & JEM, 0-0-1. ONTARIO CO. *Hwy 7, 1.61 km e of Green Rjver. under logs, 26 Apr 72, JWR, 1-0-1. 'Hwy 47, 10.48 km w of Uxbridge, digging, 9 May 72, JWR, 0-1-0. Duffenn Creek area, day after use of lampncide. 1 1 May 71, TY, 0- 0-6. ROM-I40. OXFORD CO. *Hwy 59, 1.77 km e of Burgessville, under logs and wood chips, 1 Ma) 72. JWR. 0-1-1. PARRY SOL ND DIST. »Hwy 124, 3.06 km e of McKellar, under logs, 9 May 72. JWR. 0-1-3-1. PEEL CO. Hwy 401. 1.3 km w of Dixie Rd. wet ditch, 4 May 73, JWR, 1-1-6. PERTH CO. Hwy Jet 7, 8 and 59. Shakespeare, under logs, 3 May 72, JWR, 0-0-1. 'Mitchell, next to Collegiate, under logs. 4 May 72, JWR & DWR. 0-0-1. PRESCOTT CO. *Hwy 34, 5.48 km s of Vankleek Hill, under logs. 1 1 May 72, JWR, 1-0-2. Hwy 17, 3.22 km w of Alfred, wet ditch, 1 1 May 72, JWR, 2-2-1. PRINCE EDWARD CO. "Hwy 33, Consecon, n.e., dump, 15 May 72, JWR, 0-1-4. •Hwy 49. 14.84 km n of Picton. under paper in ditch, 15 May 72. JWR, 0-1-4. RUSSELL CO. *Hwy 17. 4^35 km w of Rockland, under logs, 1 1 May 72, JWR, 1-1-0. SIMCOE CO. 'Hwy 89, 1.94 km e of Rosemont. under logs in wet ditch, 2 May 72, JWR, 0-0-2. *Hwy 27, 5.97 km s of Cookstown. un- der logs. 2 May 72. JWR. 9-2-1. Hwy 27, 3.22 km s of Newton Robinson, wet ditch, 2 May 72. JWR, 0-1-1. Barne, 14 Greenfield, under logs and digging in garden. 7 May 72, JWR & MK.G, 4-1-0. 'Barrie. park opposite 14 Greenfield, under rocks and grass clippings, 7 May 72. JWR & GWA, 0- 49 0-1. *Hwy 11, 15.16 km s of Severn Bridge, under logs, 9 May 72, JWR. 0-0-1. STORMONT CO. •Hwy 43, 5.48 km w of Finch, in and under straw in wet ditch, 1 1 May 72, JWR, 1-0-3. SUDBURY DIST. *Hwy Jet 64 and 69, under rocks, 13 May 72, JWR & JEM, 1-1-4. *Hwy 69. 1.94 km s of Hwy 607, under rocks, 13 May 72, JWR & JEM, 3-0-3. VICTORIA CO. 'Hwy 35, 8.71 km s of Hwy 7, under log, 26 Apr 72, JWR, 0-0-2. *Hwy 7. 7.26 km e of Hwy 35, under log, 26 Apr 72, JWR, 0-1-1. "Hwy 7, 1.94 km w of Hwy 46, under logs and dung, 9 May 72, JWR, 0-1-2. WATERLOO CO. *Hwy 7 and 8, 2.58 km w of New Hamburg, under paper in wet ditch, 3 May 72, JWR, 4-1-8. Hwy 7 and 8, 1.77 km w of Petersburg, under log, 3 May 72, JWR, 1-0-4. Hwy 85, 1.45 km n of St. Jacobs, digging, 3 May 72, JWR, 0-0-3. Hwy 86, West Montrose, e.e., under logs, 3 May 72, JWR, 0- 0-1. Waterloo, Beechwood South, on sidewalk after rain (evening), 15 Jun 75, DPS, 5-1-0-3, UW- 0004. Waterloo, Amos Ave., 1 Sep 75, DPS, 0-0-0-1, UW-0003. WELLINGTON CO. *Hwy 24, 5.16 km e of Eramosa, under logs in cedar (Thuja occidentalis) woodlot, 29 Apr 72, JWR, 0-0-1. Hwy 6, University of Guelph, on wet driveway behind Soil Science Building, 2 May 72, JWR. 0-0-4. *Hwy 6, 10.64 km s of Arthur, under logs, 2 May 72, JWR, 2-1-0. WENTWORTH CO. *Hwy 5, Water- down, e.e., edge of corn (Zea maize) field, 29 Apr 72, JWR, 0-0-1. YORK CO. 'Hwy 27. 1.45 km n of Hwy 7, under logs, 29 Apr 72, JWR, 0-0-1. Edenbrook Park, Islington, quantitative study #2 (formalin), 18 May 72, JWR, 2-1-1. Toronto, 1875, GE, 0-0-4, USNM-4559. Toronto, 1875, GE, 0- 0-2, USNM-19704. Scarborough Bluffs, Brimley Rd, garden, 28 Oct 41, JO, 0-0-1, ROM. Aporrectodea tuberculata (Eisen, 1874) Canadian worm Ver canadien (Fig. 12) 1874 Allolobophora turgida f. tuberculata Eisen, Ofv. Vet-Akad. Forh. Stock- holm 31(2): 43. 1910 Allolobophora similis Friend, Gardener's Chron. 48: 99. 1911 Aporrectodea similis-Friend, Zoologist, ser. 4, 15: 144. 1927 Helodrilus caliginosus trapezoides-B\ake, 111. Biol. Monogr. 10(4): 63. 1930 Allolobophora turgida (part.) + Allolobophora trapezoides (part.)-Borne- busch, Forstl. Forstfgs. Danm. 1 1 : 94. 1942 Allolobophora caliginosa (part.)-Eaton, J. Wash. Acad. Sci. 32(8): 246. 1952 Allolobophora arnoldi Gates, Breviora, no. 9: 1. 1962 Allolobophora arnoldi + A. nocturna-Omodeo, Mem. Mus. Civ. Sto. Nat. Verona 10: 92. 1963 Lumbricus terrestris-Camtron and Fogal, Can. J. Zool. 41 : 753. 1969 Allolobophora caliginosa-va.n Rhee, Pedobiologia 9: 130. 1969 Allolobophora caliginosa (part.)-St0p-Bowitz, Nytt. Mag. Zool. 17(2): 191. 1972 Nicodrilus (Nicodrilus) caliginosus alternisetosus Bouche, Inst. Natn. Rech. Agron., p. 333. 1972 Allolobophora tubereulata-Gates, Bull. Tall Timbers Res. Stn. 12: 44, 45. 1973 Allolobophora caliginosa f. typica (part.)-Plisko, Fauna Polski, no. 1. p. 107. 1975 Aporrectodea tuberculata-Reyno\ds, Megadrilogica 2(3): 3. 50 Diagnosis Length 90 150 mm. diameter 4-8 mm. segment number 146-194, prostomium epilobic. first dorsal pore 11 12 or 12 13. Clitellum xxvii-xxxiv. Tubercula pu- bertals \\\. Kxxi-xxxiii, xxxiv. Setae closely paired, AB =* CD, AA > BC, DD ~ ':C. Genital tumescences absent in xxxi and xxxiii, present in xxx, xxxii, and wxiv and frequentl) in xxvi. Male pores in xv between b and c. Seminal vesi- cles, four pairs in 9 12. Spermathecae, two pairs opening on level c in 9/10 and 10 11. Colour, unpigmented, almost white or greyish or sometimes with light pigmentation on the dorsum. Body cylindrical. IstdpH XXV xxx Fig. 12 External longitudinal views of Aporrectodea tuberculoid showing taxonomic characters. A. Lateral view, b Ventral view. (ONT: Sudbury Dist. cat. no. 8544) 51 Discussion Aporrectodea tuberculoid was described by Eisen in 1874 with specimens ob- tained from Niagara County (then Welland County), Ontario. Scandinavian specimens of Ap. tuberculata seem to have first been identified by Eisen as Allolobophora cyanea (tide Hoffmeister) (Gates. 1972a). Eisen recorded no Type Locality for Ap. tuberculata: but subsequently this has been designated as Niag- ara County. Ontario. Biology Gerard (1964) reported this species' habitat as pastureland. In the western United States Gates ( 1967) found it in wet areas near streams and springs where there was a large concentration of organic matter. In east Tennessee (Reynolds et al., 1974) Ap. tuberculata was recorded 75% of the time from ditches, or under logs or debris such as lumber. Gates (1972c) records it from soils of pH 4.8-7.5 including turf, compost, peat, bogs, and rarely manure. In Ontario this species was found primarily under logs and rocks in all but four eastern counties (cf. Fig. 11). Under favourable conditions activity, including breeding, can be year round. However, Gates (1972c) states that probably throughout New England, New York, and Canada aestivation and hibernation are climatically imposed with breeding restricted to spring and late autumn. Reproduction in this species is obligatorily amphimictic with copulation beneath the soil surface (Reynolds, 1974c). Ap. tuberculata has been obtained from culture beds on earthworm farms and being so common in gardens and fields is the species most likely to be dug for bait in much of Canada. Range A native of Palaearctis, Ap. tuberculata is now known from Europe, North America, South America, Asia, and Australia (Gates, 1972c), and also from Ice- land (Backlund. 1949). North American Distribution Alberta (Gates. 1972a). British Columbia (Wickett. 1967). Manitoba (Gates, 1972a). New Brunswick (Reynolds. 1976d). Newfoundland (Gates, 1972a), Nova Scotia (Reynolds. 1975a, 1976a). Ontario (Eisen, 1874). Prince Edward Island (Reynolds, 1975c). Quebec (Reynolds. 1975b. d. e. 1976c). Sas- katchewan (Gates, 1972a), Alaska (Gates, 1972a), Arizona (Reynolds et al.. 1974). California (Gates. 1967), Colorado (Gates, 1967), Connecticut (Reynolds, 1973c), Delaware (Reynolds. 1973a). Florida (Gates. 1972c), Idaho (dates. 1967). Indiana ((rak-s. 1972a), Iowa (Gates, 1967). Maine (Gates. 1966). Maryland (Reynolds, 1974b). Massachusetts (Reynolds. 1977). Michigan (Gates, 1972a). Minnesota (Gates, 1972a). Montana (Reynolds. 1972c). Nevada (Gates. 1967). New Hamp- shire (Gates, 1972a). New Jersey (Gates. 1972a). New Mexico (Gates, 1967). New York (Gates, 1972a). North Carolina (Ciates. 1972a). Ohio (Gates. 1972a). Oregon (Gates. 1972a). IVnnsslvania (Gates, I972ai. Rhode Island (Reynolds, 1973a), 1 enncssee (Reynolds. 1974a). Utah (Gates. 1967). Vermont (Reynolds, 1976c). Virginia (Gates, 1972a). West Virginia (Gates. 1972a), Wisconsin (Gates. 1972a), Wyoming (Gates. 1967). New records: Arkansas. Illinois. 52 Fig. 13 The known Ontario distribution of Aporreclodea tuberculata. Ontario Distribution (Fig. 13) \I GOMA DIST. *Hw) 17. 7.58 km e of Spanish, under logs, 13 May 72, JWR & JEM. 4-0-2. •Hw) 17. .48 km e of Spanish, under logs and paper in ditch, 13 May 72, JWR & JEM, 22-16-13-1. Gargantua Ba>. 1 1 Jun 75. DRB. 0-1-0-1. UW-0001. BRANT CO. *Hwy 53, 5.48 km w of Cathcart, under railroad ties. 1 May 72, JWR, 0-1-1. *Hwy 53, 4.35 km e of Cathcart, under logs, 1 May 72, JWR. 10-8-25. "Hwy 53. 2.74 km e of Mt. Vernon, under logs, 1 May 72, JWR, 1-0-7. *Hwy 54, 5.16 km e of Middleport, ditch. 3 May 72, JWR, 0-1-0. *Hwy 2. 5.45 km e of Paris, under lumber and pa- per. 3 \la\ 72. J\\ R. 4-0-2. BRUCE CO. *Hwy 4, .48 km s of Hwy 9, under logs, 5 May 72, JWR, 0- 0-2. 'Hwy 21, 6.94 km n of Kincardine, under logs, 5 May 72, JWR, 0-2-6. Hwy 21, 2.76 km n of Port Elgin, under logs. 5 Ma) 72. JWR. 0-0-4. *Hwy 21, 1.61 km e of Elsinore, under logs (pair in copula), 5 Mas 72. JWR. 4-4-2-1. COCHRANE DIST. Reynolds (1972a). DUFFERIN CO. Hwy 9, 1.61 km eofHw) 10. under logs. 29 Apr 72. JWR, 17-1-0. *Hwy 9, 2.1 km w of Hwy 104, digging in road bank, 2 May 72. JWR. 4-1-13. *Hwy 9. 10.16 km w of Orangeville, under junk, 2 May 72, JWR. 0-0-1. •Hwy 9. 3.71 km w of Orangeville, under logs in ditch, 2 May 72, JWR, 6-4-10. *Hwy 10-24. 7.74 km n of Camilla, under logs. 2 May 72. JWR, 6-1-3. *Hwy 89, 10 km e of Primrose, wet ditch, 2 May 72. JWR. 0-0-10. DUNDAS CO. *Hwy 31. .81 km n of Hwy 43, under logs. 1 1 May 72. JWR. 0-0-3. DURHAM CO. *Hwy 7A. 1 1.77 km e of Hwy 7-12, digging in ditch. 26 Apr 72, JWR. 0-0-1. *Hw) 7,\. 2.1 km e of Nestleton Station, under logs, 26 Apr 72, JWR, 2-7-3. *Hwy401, .16 km w of Libert) Rd. Bowmanville. digging under log next to railroad tracks. 15 May 72. JWR, 0- 0-3. 'Hwy 401. .32 km e of Mill St. Newcastle, under logs, 15 May 72, JWR, 0-0-5. "Hwy 401, 1.61 km e of Newtonville. under logs. 15 May 72. JWR. 2-1-8. Hwy 401, 1.61 km w of Hwy 28, under pa- per, 15 Maj 72, JW R. 2-0-3 El GIN CO. *Hw) 73. 3.06 km s of Harriettsville, under rotten log, 4 Mas 72. JWR. 0-3-9. Hwy 3. 9.19 km e of St. Thomas, under logs. 4 May 72, JWR. 9-3-0. "Hwy 3, 6.77 km e of Wallacetown, under pine logs, 4 May 72. JWR. 13-2-1. 'Hwy 3, 2.1 km e of Wallace- 53 town, under logs. 4 May 72, JWR. 1-0-4. Hwy 3. 3.87 km w of New Glasgow, under logs in aban- doned school yard, 4 May 72, JWR, 9-4-3-1. ESSEX CO. *Hwy 3. 4.03 km e of Leamington, under logs, 4 May 72, JWR, 2-2-3. Hwy 3. 3.87 km w of Leamington, under lumber in dump. 4 May 72, JWR. 5-4-3. *Hwy 3, Ruthven, n.e., wet ditch by railroad tracks. 4 May 72, JWR, 4-1-0. FRONTE- NAC CO. Reynolds (1972a). "Hwy 7, 3.71 km e of Hwy 38. under log, 11 May 72, JWR. 4-0-6. •Hwy 2. .97 km w of Westbrook, under logs, 16 May 72. JWR. 0-0-2. *Hwy 2. 1.13 km e of West- brook, under logs and paper. 16 May 72. JWR. 0-1-3. *Hwy 15, 4.68 km s of Seeley's Bay. under logs, 16 May 72, JWR, 5-1-1. *Hwy 7. 15.81 km e of Kaladar, under logs. 16 May 72, JWR. 2-0-3. GRENVILLE CO. *Hwy 2, 5.16 km w of Prescott, under rocks. 10 May 72. JWR. 3-2-1. Hwy 2, Cardinal, w.e., under log and paper, 1 1 May 72. JWR. 7-5-0. *Hwy 43, 3.87 km e of Kemptville, un- der logs, 11 May 72, JWR. 0-0-11. GREY CO. *Hwy 21, 7.26 km w of Spnngmount. under rock, 5 May 72, JWR, 0-0-1. *Hwy 6BP, Rockford, w.e.. under logs, 5 May 72. JWR, 1 1-1-2. *Hwy 6. 3.06 km s of Chatsworth, under logs, 5 May 72, JWR, 9-2-10. *Hwy 6, 6.94 km s of Dornoch, under logs, 5 May 72, JWR, 1-1-2. *Hwy 10, 8.06 km s of Flesherton, under logs, 5 May 72. JWR. 5-1-1. HAL- DIMAND CO. 'Hwy 3. 6.29 km w of Dunnville, under logs, 1 May 72, JWR. 5-1-2. *Hwy 3. 6.13 km w of Cayuga, under logs, 1 May 72, JWR, 0-1-5. *Hwy 54. 2.26 km n of Caledonia, digging, 3 May 72, JWR, 0-1-2. HALIBURTON CO. *Reynolds (1972a). HALTON CO. *Hwy 5. 9.19 km w of Hwy 10, under log next to barn, 29 Apr 72. JWR. 0-0-1. 'Halton Co. Rd 3, Esquesing Communi- ty, under rocks and logs next to Town Hall, 4 May 73, JWR, 7-3-0. *Hwy 7. 4.84 km e of George- town, under burnt logs in soil, 4 May 73, JWR, 0-0-3. Halton Co. Rd 3, 8.87 1cm n of Halton Co. Rd 8, wet ditch under logs and digging, 4 May 73, JWR, 7-1-15. Halton Co. Rd 3. .48 km n of Halton Co. Rd 8, under logs in field, 4 May 73, JWR. 5-5-6-1. Rattlesnake Point, 1 Nov 41. JO, 0-0-2, ROM. HASTINGS CO. "Hwy 620, 5.16 km e of Coe Hill, under logs. 27 Apr 72, JWR, 1-0-1. *Hwy Jet 62 and 620, under logs, 27 Apr 72, JWR, 5-1-1. Hwy 62, 7.42 km n of Bannockburn, under logs, 27 Apr 72, JWR, 6-0-3. 'Hwy 62, 1.61 km n of Hwy 7, under log in wet ditch, 27 Apr 72, JWR, 0-0-1. HU- RON CO. *Hwy 4, 3.71 km s of Brucefield, under log, 5 May 72. JWR, 0-0-1. 'Hwy 4. 1.29 km s of Wingham. under logs in wet area. 5 May 72, JWR, 3-0-1. KENORA DIST. Rushing River Provin- cial Park, stream trickle in campground, 13-14 Jun 71, ROM Field Party, 0-1-0, ROM-I37. KENT CO. *River Rd, 6.45 km w of Chatham, under logs, 23 Apr 72. JWR & TW, 0-1-1. "Hwy 3. 9.03 km e of Port Alma, under log, 4 May 72, JWR, 9-0-4. LAMBTON CO. *Hwy 21, 6.45 km n of Dresden, under logs, 4 May 72, JWR, 3-6-7. *Hwy 21, Edy's Mills, s.e., under railroad ties, 4 May 72. JWR, 0- 0-6. Hwy 21,2.1 km n of Wyoming, under log in wet ditch. 5 May 72, JWR, 0-0-1. *Hwy 7. 1.61 km n of Arkona, under log, 4 May 72, JWR, 6-4-1. LANARK CO. *Hwy 43, 3.71 km e of Smiths Falls, under telephone pole in ditch, 1 1 May 72, JWR, 4-3-4. *Hwy 43, 5.32 km w of Smiths Falls, under logs, 1 1 May 72, JWR, 0-0-13. *Hwy 7, 4.35 km w of Perth, digging under gate post. 1 1 May 72, JWR, 3-0-12. LEEDS CO. *Hwy 15. 3.22 km s of Morton, under log. 16 May 72, JWR. 2-0-3. *Hwy 15, 5.64 km n of Morton, wet ditch. 16 May 72, JWR. 0-0-11. *Hwy 15, 4.84 km n of Elgin, digging. 16 May 72, JWR, 0-0-13. *Hwy 15, 4.19 km s of Lombardy, under logs and crawling on the surface during rain. 16 May 72, JWR. 1 1-14-28. *Hwy 15. 7.1 km n of Lombardy, under paper in ditch. 16 May 72, JWR, 0-0-1. LENNOX AND ADDINGTON CO. *Hwy 2, Napanee, w.e.. under rocks be- hind EEEE Motel, 15 May 72, JWR, 2-1-2. *Hwy 2, 6.61 km w of Hwy 133. under logs, 16 May 72, JWR, 1-1-4. *Hwy 500, .81 km n of Denbigh, under logs, 16 May 72, JWR, 6-1-4. Hwy 7. Kaladar. e.e., under lumber in school yard. 16 May 72, JWR. 0-0-2. MANITOULIN DIST. *Hwy 68, 3.22 km n of Little Current, under logs and lumber. 13 May 72. JWR & JEM, 0-0-8. MIDDLESEX CO. Judd (1964). *Hwy 73, .97 km n of Mossley, under logs, 4 May 72, JWR, 20-2-8. "Hwy 7. 2.26 km s of Parkhill, under fence posts, 4 May 72, JWR, 0-0-3. MUSKOKA DIST. 'Hwy 1 1. 1.13 km n of Se- vern Bridge, under logs, 9 May 72, JWR, 2-0-2. *Hwy 11, 11.45 km n of Severn Bridge, under pine logs, 9 May 72, JWR, 1-1-4. "Hwy 11. 12.9 km s of Bracebridge, under rocks, 9 May 72, JWR, 3-1-2. •Hwy 1 1, 9.19 km s of Hwy 516, under logs and rocks in wet ditch, 9 May 72, JWR, 3-1-5. *Hwy 1 1, Melissa, s.e., under paper in ditch, 9 May 72, JWR. 3-1-1. NIAGARA CO. Niagara, 1873, GE. 0- 2-0, USNM-1156. Niagara, 1873, GE, 0-1-3, USNM-1157. •Queen Elizabeth Hwy. 1.13 km w of Ontario St, Grimsby, under log. 1 May 72, JWR, 0-0-1. NIPISSING DIST. *Hwy 17. 5.48 km e of Warren, under logs and dung in pasture, 13 May 72, JWR & JEM, 6-1-7. *Hwy 17. 1.29 km e of Verner, under paper in wet ditch, 13 May 72, JWR & JEM. 3-1-2. Hwy 17, 7.90 km w of North Bay, digging under rocks, 13 May 72. JWR & JEM, 12-4-17. Temagami, Bearls (Hudson Bay Co. Post), 30 Jun 37, JO & GMN, 0-0-1. ROM-I27. NORFOLK CO. Hwy 6. 4.84 km s of Jarvis, under log, 1 May 72, JWR, 0-0-1. *Hwy 24, 3.06 km n of Hwy 6, under logs, 1 May 72, JWR, 5-4-0. *Hwy 3, 54 1 I 29 km e of Delhi, under logs. 1 Ma) 72, JWR 8-9-0. *Hw) .let 3 and 59. under junk under pine trees. | Ma) 72, JWR, 7-1-2. NORTHl MBERLANDCO. *ll\\\ 45, 10.69 km s of Norwood, under logs around Kirn. 28 \pr "1 JWR. 14-2-0 Hwj 45. 4 35 km n of Roseneath, under logs. 28 Apr 72. JWR, 4-0-6. »Hw) 45,9.03 km n of Baltimore, under logs, 28 Apr 72. JWR. 0-1-1. Mlwy 45, 4.84 km n of Baltimore, under logs. 2S Apr "2. JWR, 0-0-2. *Hw) 401, 8.06 km w of Grafton, under log, 15 Ma) 72, JWR. 1-1-2. »Hw) 401, 5.64 km e of Grafton, under logs. 15 Ma) 72, JWR, 4-0-18. •Northumberland-Durham Rd I. .65 km w of Hwj 33. under log, 15 May 72. JWR. 1-0-0. Lakeport, on pebhK beach ot 1 .ike Ontario. 25 Jul 74, DRB, 0-0-1. UW-0001. ONTARIO CO. *Hwy 7. 1.61 km e of Green Riser, under logs. 2d Apr 72. JWR. 0-0-4. *Hwy 7-12. .81 km n of Myrtle, under logs. 26 Vpr "2. JWR. 4-3-0. *Hw) 4". 8.22 km e of Uxbndge, under login wet area, 9 May 72, JWR, 3- 1-0. »Hwy 47, 10.48 km w of I xhridge. digging. 9 May 72, JWR, 10-4-1-1. *Hwy 7-12, 3.22 km n of Blackwater. under log-.. ^ Ma) "2. JWR. 2-3-1. DufTerin Creek area, day after use of Lampricide. 1 1 Ma) 71. TY. 0-0-1. ROM-I41. OXFORD CO. »Hw) 59. 6.54 km n ofHwy 3. under logs. 1 May 72, JWR, 6-0-2 *Hw) <9. 1.13 km s of Curries, under junk. 1 May 72. JWR, 0-0-4. *Hwy 59, 1.77 km e of Burgesville, under logs and wood ehips. 1 Ma) ^2. JWR. 2-2-4. *Hwy 97, Washington, w.e., un- der log, 3 Ma) 72, JWR. 0-0-1. *Hwy 59. .32 km n of Hickson. under logs, 3 May 72, JWR, 0-4-2. PARRY SOL ND DIST. *Hw) 1 1. 4~03 km s of Scotia Rd, under logs, 9 May 72, JWR. 0-3-1. Hwy II. 3.87 km s of Katrine, under log, 9 Ma) 72, JWR, 0-0-0-1. *Hwy 1 1, 4.52 km s of Burks Falls, un- der logs. 9 Ma) 72, JWR. 7- 1 1-0. Hw) 520. 5 km w of Burks Falls, under log, 9 May 72, JWR, 0-1-0. *Hw) 520. Magnetawan, e.e.. under rocks. 9 May 72. JWR, 3-0-3. *Hwy 124, 3.55 km w of Hwy 69, under logs. ^ Ma) "2. JWR. 0-0-5. PEEL CO. *Hwy 5. .81 km e of Dixie Rd, under logs. 29 Apr 72, JW R. 5-0-1. *Hw) 5. 4.35 km w of Hwy 10. under mattress, 29 Apr 72. JWR, 0-0-6. *Hwy 24, 8.87 km n of Erin, under log and dung. 29 Apr 72, JWR, 0-4-0. 'Hwy 9, 4.35 km e of Mono Mills, under logs. 29 Apr 72. JW R^O-lO. Hwy 401. 1.3 km w of Dixie Rd". wet ditch, 4 May 73, JWR, 0-0-3. PERTH CO. .81 km n of Fullarton, under rock, 29 Apr 72. DWR & LWR, 0-0-1. *Mitchell. next to Collegiate, under logs. 4 Ma) 72, JWR & DWR. 8-0-6. PETERBOROUGH CO. *Hwy 28, Lakefi- eld College, waterfront under logs. 27 Apr 72, JWR & CWR. 4-0-1. "Hwy 504, 1.61 km e of Apsley, under logs. 27 Apr 72. JWR. 1-1-1. "Hwy 504. .81 km w of Lasswade, old house site under logs, 27 Apr 72, JWR, 10-0-7. PRINCE EDWARD CO. *Hwy 33, 1.61 km s of Carrying Place, under log in wet ditch. 15 May 72. JWR, 1 1-3-1 1. 'Hwy 33, Consecon. n.e., dump, 15 May 72, JWR, 4-0-1. Hwy 33. Bloomfield. e.e.. under paper. 15 May 72, JWR. 1-0-1. *Hwy 49. Picton, n.e., under leaf pile, 15 Ma) 72. JWR. 4-0-1. RENFREW CO. 'Hwy 500. 12.26 km n of Denbigh, under logs, 16 May 72, JWR. 3-1-6. RUSSELL CO. *2.42 km s of Limonges, under lumber at old house site, 1 1 May 72, JWR. 0-0-2 SIMCOE CO. 'Hwy 89. 5.48 km e of Alhston, under logs, 2 May 72. JWR, 12-0-5. *Hwy 89. 1.94 km e of Rosemont. under logs in wet ditch. 2 May 72, JWR, 0-0-2. Barrie, 14 Greenfi- eld, under logs and digging in garden. 7 May 72. JWR & MK.G, 35-3-4. *Barrie, park opposite 14 Greenfield, under rocks and in grass clippings, 7 May 72, JWR & GWA, 0-1-9. *Hwy 400, .81 km s of Hwy 103. under logs. 9 May 72, JWR, 2-1-1. SUDBURY DIST. »Hwy 17, 3.06 km e of Nairne Centre, under logs in ditch. 13'May 72, JWR & JEM. 0-0-5. VICTORIA CO. *Hwy 7, 7.26 km e of Hwy 35. under logs. 26 Apr 72. JWR. 5-3-3. *Hwy 7, 1.94 km w of Hwy 46. under logs and dung, 9 Ma) 72, JWrR. 8-6-13. 'Hwj 46. 3.71 km n of Hwy 7. under logs, 9 May 72, JWR, 1-3-1. *Hwy 46, .81 km n of Argyle. under logs, 9 May 72, JWR, 15-1-2. *Hwy 46, 8.22 km n of Argyle, under logs, 9 Ma) "2. JWR. '3-6-9. WATERLOO CO. *Hwy 24A. 1 1.45 km n of Paris, under log, 3 May 72, JWR, 2-1-5 "Hwy 9". Gait. .81 km w of Hwy 24A, under grass clippings, 3 May 72, JWR. 1-0-3. *Hwy97, 3.71 km w of Hwy 401, under logs, 3 May 72, JWR, 4-1-3. Hwy 85, 1.45 km n of St. Jacobs, digging. 3 Mas 72, JW R. 6-1-4. Waterloo, Laurel Creek Conservation Area, 3 Aug 74, DPS, 2-1-6, UW-0007. Waterloo. Amos Ave.. 1 Sep 75. DPS. 0-0-0-2, UW-0003. WELLINGTON CO. *Hwy 6, 2.26 km n of Aberfoyle. under logs, 29 Apr 72, JWR, 3-1-4. *Hwy 24, 4.03 km n of Erin, under logs, 29 Apr 72, JW R. 4-2-1. *Hwy 24. 5.16 km e of Eramosa, under logs in cedar (Thuja occidentals) woodlot, 29 Apr 72. JWR, 1 1-5-2. Hw) 6, University of Guelph, on wet driveway behind the Soil Science Build- ing. 2 May 72. JWR, 3-0-1 1. *Hw) 6. 1.13 km s of Ennotville, under paper in wet ditch. 2 May 72, JWR. 6-0-1 W EM WORTH CO. »Hwy 6. 5.32 km n of Hwy 5. under log, 29 Apr 72, JWR, 0-0-1. YORK CO. Hw) 27. 8.55 km s of Hwy 9, under logs, 29 Apr 72, JWR, 8-0-1. 'Edenbrook Park, Is- lington, under rocks and logs near stream bank. 30 Apr 72, JWR & DWR, 9-5-1. Hwy 27, Bell's Lake, under lumber, 2 May 72. JWR, 5-0-4. Edenbrook Park, Islington, quantitative study 1, forma- lin. 18 May 72. JWR. 10-0-3. Edenbrook Park. Islington, quantitative study 2, formalin, 18 May 72. JWR, 2-1-6. Toronto. GE, 0-0-4. USNM-4563. Toronto, GE, 0-4-0, USNM-4564. 55 Aporrectodea turgida (Eisen, 1873) Pasture worm Ver du paturage (Fig. 14) 1873 Allolobophora turgida Eisen, Ofv. Vet.-Akad. Forh. Stockholm 30(8): 46. 1874 Allolobophora turgida (part.)-Eisen, Ofv. Vet.-Akad. Forh. Stockholm 31(2): 43. 1946 Allolobophora caliginosa-Evans, Ann. Mag. Nat. Hist., ser. 11, 13: 100, 101. 1947 Allolobophora caliginosa-Cemosvitov and Evans, Linn. Soc. Lond., Syn. British Fauna, no. 6: 13. 1952 Allolobophora caliginosa + A. molita Gates, Breviora, no. 9: 1,3. 1959 Allolobophora caliginosa-Zicsu Acta Zool. Hung. 5(1-2): 172. 1964 Allolobophora caliginosa (in toto)-Gerard, Linn. Soc. Lond., Syn. British Fauna, no. 6: 27. 1969 Allolobophora caliginosa (part.)-St0p-Bowitz, Nytt. Mag. Zool. 17(2): 191. 1970 Allolobophora caliginosa-Za]onc, Biol. Prace 16(8): 23. 1972 Allolobophora caliginosa f. typica (part.) + A.c.f. trapezoides (part.)-Ed- wards and Lofty, Biol, earthworms, p. 217. 1972 Nicodrilus caliginosus caliginosus-Boxiche, Inst. Natn. Rech. Agron.. p. 326. 1972 Allolobophora turgida-Gates, Bull. Tall Timbers Res. Stn. 12: 89. 1973 Allolobophora caliginosa f. typica (part.)-Plisko, Fauna Polski, no. 1, p. 107. 1975 Aporrectodea turgida-Keyno\ds, Megadrilogia 2(3): 3. Diagnosis Length 60-85 mm, diameter 3.5-5.0 mm, segment number 130-168, prostomium epilobic, first dorsal pore 12/13 or 13/14. Clitellum xxvii, xxviii, xxix-xxxiv, xxxv. Tubercula pubertatis xxxi-xxxiii. Setae closely paired, AA:AB:BC:CD:DD = 3: 1:2:%: 10. Genital tumescences contain a and b only in xxx, xxxii-xxxiv, and frequently in xxvii. Male pores on xv between b and c. Seminal vesicles, four pairs in 9-12. Spermathecae, two pairs, with short ducts opening at level cd in 9/10 and 10/1 1. Colour, unpigmented with the region an- terior to the crop flesh pink and the remaining segments pale grey, or occasion- ally with light pigmentation on the dorsal surface. Body cylindrical. Discussion Aporrectodea turgida, along with the previous two species, has given oligochae- tologists great difficulty until a recent publication by Gates (1972a). This species was first recorded from Ontario (Niagara County) by Eisen in 1874. Four speci- mens labelled Ap. turgida from Niagara were sent by Eisen to the United States National Museum (cat. no. 1 157). One specimen may be an aberrant individual of Ap. turgida, but the other three appear to be Ap. tuberculata (Gates. 1972a). I have subsequently examined these specimens and confirm this report. 56 1st dp- t V ■■ (• To • ; j X 1 9" 1 XV "^r -' ' < 3? -LO :IT XXV XXX XXXV Fig. 14 External longitudinal views of Aporrectodea turgida showing taxonomic characters, a. Lat- eral view. (ONT: Grey Co., cat. no. 7988) B. Ventral view. (ONT: Parry Sound Dist., cat. no.. 7891) Biology Gates (1972c) records this species from a variety of habitats, including gardens, fields, turf, forest humus, compost, banks of springs and streams, wasteland and city dumps, and from a cave in West Virginia. The widespread distribution and variety of utilized habitats for Ap. turgida were recorded also by Eaton (1942), Cernosvitov and Evans (1947), Murchie (1956), and Gerard (1964). The amaz- ing water tolerance of this species was reported by Guild (1951) and Reynolds et al. (1974). in Scotland and the United States respectively. The variety of habi- tats utilized by Ap. turgida in Ontario can be seen from the collection data. 1~2 Dendrobaena (part.) Bouche, Inst. Natn. Rech. Agron., p. 388. 1973 Dendrodrilus ; Plisko. Fauna Polski. no. 1, p. 78. 1975 Dendrodrilus-G&tts, Megadrilogica 2(1): 4. Type Species Enterion rubidum Savigny. 1 826. Diagnosis C'alciferous glands, opening into gut ventrally through a pair of sacs posteriorly just in front of insertion of 10/11. Calcierous lamellae continued along lateral walls of sacs. Gizzard, mainly in xvii. Extraoesophageal trunks, passing to dor- sal trunk in xii. Hearts, in vii-xi. Nephridial bladders, (/-shaped loop. Nephro- pores. inconspicuous, alternating irregularly and with asymmetry on each side between a level above B and one above D. Setae, not closely paired. Prosto- mium epilobic. Longitudinal musculature, pinnate. Pigment, red. (after Gates, 1972c: 88 and 1975a: 4). Discussion Species of Dendrodrilus formerly congeneric with species in Dendrobaena be- cause of similarities in genital anatomy are now separated on the basis of differ- ences in their more conservative somatic anatomy. Dendrodrilus rubidus (Savigny, 1826) European bark worm Ver europeen de Tecorce (Fig. 20) 1826 Enterion rubidum Savigny, Mem. Acad. Sci. Inst. Fr. 5: 182. 1836 Lumbricus xanthurus R. Templeton, Ann. Mag. Nat. Hist. 9: 235. 1837 Lumbricus rubidus-Duges, Ann. Sci. Nat., ser. 2, 8: 17, 23. 1849 ? Lumbricus valdiviensis E. Blanchard, Hist. Chile 3: 43. 1867 ? Hypogeon havaicus Kinberg, Ofv. Vet.-Akad. Forh. Stockholm 23: 101. 1873 Allolobophora norvegica + A. arborea + A. subrubicunda Eisen, Ofv. Vet.-Akad. Forh. Stockholm 30(8): 48, 49. 51. 1874 Allolobophora tenuis Eisen, Ofv. Vet.-Akad. Forh. Stockholm 31(2): 44. 188 1 Allolobophora fraissei Orley, Zool. Anz. 4: 285. 1881 ? Dendrobaena puter (part.)-Orley, Math. Term. Kozlem. Magyar Akad. 16: 586. 1884 Allolobophora constricta Rosa, Lumbric. Piemonte, p. 38. 69 1st dp Fig. 20 External longitudinal views of Dendrodrilus rubidus showing taxonomic characters, a Dor- solateral view, b Ventrolateral view. (ONT: Manitoulin Dist., cat. no. 7502) 70 1884 Lumbricus subrubicunda (part.)-Levinsen. Vidensk. Meddel. Naturhist. Forh. Copenhagen, ser. 4. 5: 242. 1885 Octolasion constrictum + (). subrubicundum -Or\ey, Ertek. Term. Magyar Mead. 15(18): 20.21. 1888 Allolobophora putra (part.)-Vejdovsky, Entwickgesch. Unters., p. 41. 1889 Lumbricus (Allolobophora) constrictus L. Vaillant, Hist. Nat. Annel. 3(1): 113. 1 Ss> 1 Allolobophora nordenskioldii (laps.) Michaelsen. Abh. Ver. Hamburg 11(2): 3. 1891 Allolobophora rubicunda (laps.)-Beddard. Proc. R. Phy. Soc. Edinburgh 10: 273. 1893 Allolobophora putris arborea (part. ?)-Rosa, Mem. Ace. Torino, ser. 2, 43: 433. 1893 Dendrobaena const ricta (part.)-Friend, Naturalist, p. 19. 1896 Allolobophora helvetica + A. darwini Ribaucourt, Rev. Suisse Zool. 4: 18, 82. 1900 Allolobophora (Bimastus) constricta-Michaeteen, Abh. Nat. Ver. Hamburg 16(1): 10. 1900 Helodrilus (Dendrobaena) rubidus-Michaeken, Das Tierreich. Oligo- chaeta 10: 490. 1908 Helodrilus (Bimastus) cw?.?/ncrw5-Michaelsen, Denskschr. Med.-Naturew. Ges. Jena 13: 41. 1917 Helodrilus (Bimastus) tenuis-Smith, Proc. U.S. Natn. Mus. 52: 157. 182. 1958 Dendrobaena rivu/icola Chandebois. Bull. Soc. Zool. France 83: 159. 1969 Dendrobaena rubida + D. subrubicunda + D. tenuis-Sl0p-Bowilz, Nytt. Mag. Zool. 17(2): 220. 224. 227. 1970 Dendrobaena rubida var. typica-Zajonc. Biol. Prace 16(8): 22. 1972 Dendrobaena (Dendrodrilus) rubida rubida + D. (D.) rubida tenuis + D. (D.) subrubicunda-Bouche. Inst. Natn. Rech. Agron., p. 410, 411, 414. 1972 Dendrobaena subrubicunda + Bimastos tenuis + Dendrobaena rubida-Edwards and Lofty. Biol, earthworms, p. 215. 216. 1973 Dendrobaena (Dendrodrilus) rubida + D. (D.) r. f. typica + D. (D.) r. f. subrubicunda + D. (D.) r. f. tenuis-Plisko, Fauna Polski, no. l.p. 79, 84, 85.87. 1975 Dendrodrilus rubidus-Reynolds, Megadrilogica 2(3): 3. Diagnosis Length 20-90 mm. diameter 2-5 mm, segment number 50-120. prostomium epi- lobic. first dorsal pore 5/6. Clitellum xxvi, xxvii-xxxi, xxxii. Tubercula puberta- ls, if present, xxviii, xxix-xxx. Setae widely paired, AB<^CD, and BC = 2 CD. Male pores on xv between b and c. Seminal vesicles in 9, 11, and 12. Spermathe- cae, two pairs with short ducts on level with setae c opening in 9/10 and 10/11. Body cylindrical. Colour, red and darker dorsally. Biolog) Dendrodrilus rubidus has been found in a wide range of habitats including gar- dens, cultivated fields, stream banks, in moss in running water and wells and springs, peat, compost, and sometimes in manure. It seems acid tolerant. The 71 species is known from caves in Europe and North America, and in greenhouses, botanical gardens, and the culture beds of earthworm farms (Gates, 1972c). Dd. rubidus lives in the upper soil layers though on wet nights the worms have been seen wandering on the soil surface or climbing trees. Under experimental condi- tions it can withstand prolonged immersion in water (Roots, 1956). Cernosvitov and Evans (1947) and Gerard (1964) reported it from under the bark of old trees, and under moss, leaf mould, or rotten wood in moist areas. In Ontario Dd. rubidus was most frequently found under logs. Although activity can be year round it is probable that in much of North America, including Ontario, a winter rest is imposed by the climate. Copulation has not been properly studied but one published observation records an unusual position of ventral apposition, head to head and tail to tail (see Gates, 1972c). Dd. rubidus is facultatively parthenogenetic with male sterility and absence of spermathecae common (Gates, 1972c; Reynolds. 1974c). Range A native of Palaearctis, Dd. rubidus is now know from Europe, North America, South America, Asia, Africa, and Australasia (Gates, 1972c). Also known from Iceland (Backlund, 1949). North American Distribution Alberta (Gates, 1972c), British Columbia (Gates. 1972c). Manitoba (Gates, 1972c), New Brunswick (Reynolds, 1976d). Newfoundland (Eaton. 1942). Nova Scotia (Reynolds, 1975a. 1976a). Ontario (Eisen, 1874). Prince Edward Island (Reynolds, 1975c). Quebec (Reynolds, 1975d. 1976c). Saskat- chewan (Gates, 1972c), Alabama (Smith, 1917), Alaska (Michaelsen. 1903a), Arizona (Reynolds et al.. 1974), Arkansas (Causey, 1953), California (Smith, 1917). Connecticut (Reynolds, 1973c), Dela- ware (Reynolds, 1973a), Hawaii (Ude, 1905), Idaho (Gates, 1967), Illinois (Smith 1917). Indiana (Heimburger, 1915), Kentucky (Giavannoh, 1933), Louisiana (Harman, 1952), Maine (Gates. 1949), Maryland (Reynolds, 1974b), Massachusetts (Reynolds. 1977), Michigan (Smith, 1917). Missouri (Olson, 1936), Montana (Reynolds, 1972c), Nevada (Gates. 1967). New Hampshire (Southern, 1910), New Jersey (Eaton, 1942), New York (Olson. 1940), Ohio (Olson. 1928). Oregon (Gates, 1972c), Pennsylvania (Gates, 1959), Rhode Island (Reynolds, 1973a), Tennessee (Reynolds. 1974a). Utah (Gates, 1967), Vermont (Reynolds, 1976c), Virginia (Reynolds, 1974b). Washington (Smith. 1917), West Virginia (Gates, 1972c), Wyoming (Gates, 1967), Greenland (Omodeo, 1955a). New records: Florida. Georgia. Iowa. Minnesota. New Mexico. North Carolina. Ontario Distribution (Fig. 21) Dendrodrilus rubidus was the third species reported for Ontario by Eisen (1874). Later reports of this species in Ontario were made by Stafford (1902), Gates (1943), Judd (1964), and Reynolds (1972a). ALGOM A DIST. *Hwy 17. 7.58 km e of Spanish, under logs. 13 May 72, JWR & JEM, 0-0-1. Al- ona Bay Mine. 4 Jun 71. GM. 0-1-0. Wawa Mine. Wawa, 5 Jun 71. GM. 0-1-0. BRANT CO. *Hwy 54, .64 km w of Onondaga, under logs in wet area, 3 May 72, JWR. 0-1-3. BRUCE CO. *Hwy 4, 6.77 km s of Teeswater, under logs, 5 May 72, JWR, 0-0- 1. Hwy 21, 2.57 km n of Tiverton, under lumber, 5 May 72. JWR. 0-1-1. 'Hwy 21. 1.61 km e of Elsinore. under logs, 5 May 72. JWR. 0-1-1. COCHRANE DIST. Smoky Falls, under lumber, 16 Apr 38. RVW. 0-0-2. ROM-I26. DUFFERIN CO. *Hwy 10-24. 8.06 km n of Orangeville. under logs, 2 May 72. JWR, 0-1-6. DURHAM CO. •Hwy 401. .32 km e ol Mill St, Newcastle, under logs. 15 May 72. JWR. 0-0-1. ESSEX CO. *Hwy 3, Ruthven. n.e.. wet ditch next to railroad tracks. 4 May 72. JWR. 0-1-0. *Hwy 2, 8.55 km e of St. Joa- chim, ditch. 4 May 72. JWR. 0-1-0. FRONTENAC CO. *Hwy 2. .97 km w of Westbrook. under logs, 16 May 72. JWR. 0-0-1. 'Hwy 7, 15.81 km e of Kaladar. under logs, 16 May 72. JWR, 0-0-1. GRENVILLE CO. Hwy 43, Merrickville. in grass clippings, 11 May 72, JWR, 0-0-2. GREY CO. 72 Fig. 2 1 The known Ontario distribution of Dendrodrilus rubidus. •Hwy 6BP. Rockford. w.e., under logs, 5 May 72, JWR 1-0-1. *Hwy 4, 8.22 km e of Durham, under logs. 5 May 72, JWR, 0-0-2. HALDIMAND CO. *Hwy 3, 6.29 km w of Dunnville, under logs, 1 Ma) 72. JWR. 0-0-1. HALIBURTON CO. Reynolds (1972a). HASTINGS CO. 'Hwy 62, .64 km w of Maple Leaf, under log, 16 May 72. JWR, 1-1-3. KENT CO. *River Rd, 6.45 km w of Chatham, under log. 23 Apr 72, JWR & TW, 0-0-1. *Hwy 3. 9.03 km e of Port Alma, under log. 4 May 72, JWR. 0-T-0. MANITOULIN DIST. Gates (1943). *Hwy 68, 3.22 km n of little Current, under logs and lumber, 13 May 72. JWR & JEM, 0-0-2. MIDDLESEX CO. Judd (1964). MUSKOKA DIST. *Hwv 1 1. 1.13 km n of Severn Bridge, under log. 9 May 72. JWR, 0-0-1. *Hwy 103, 2.26 km n of Hwj 660. under logs in ditch. 9 May 72. JWR, 0-0-3. NIAGARA CO. Niagara. 1873, GE, 0-0-1, USNM- 18937. N I PISSING DIST. Hwy 17, 15.81 km e of Sturgeon Falls, dump, 13 May 72. JWR & JEM. 0-0-2. Lake Temagami. under rotten logs. 2 Jul 37. GMN, 1-0-2, ROM-I24. NORFOLK CO. St. Williams Forestry Experimental Station, 5 Oct 75, DPS, 0-0-1, UW-0001. ONTARIO CO. Du- ffenn Creek area, day after use of lampricide. 11 May 71, TY, 0-0-1, ROM-I39. OXFORD CO. •Hwy 59. 1.94 km s of Norwich, under log, 1 May 72. JWR. 0-0-1. PARRY SOUND DIST. *Hwy 124, 3.06 km eof McKellar. under logs, 9 May 72^ JWR, 1-1-1. PRESCOTTCO. »Hwy 34, 5.81 km n of Vankleek Hill, under logs, 1 1 May 72, JWR, 0-2-6. Hwy 17. .64 km e of Plantagenet, under log, II \la\ 72. JWR. 0-0-1. RENFREW CO. Reynolds ( 1972a)' *2.26 km n of Schutt, ditch. 16 May 72, JWR. 0-0-1. '4.19 km s of Palmer Rapids, under paper in wet ditch, 16 May 72, JWR, 0-0-3. *2.42 km s of Palmer Rapids, under paper in ditch. 16 May 72. JWR, 0-0-3. RUSSELL CO. *2.96 km e of Embrun. under logs. 1 1 May 72, JWR, 0-0-1. SUDBURY DIST. Webbwood Mine, Webbwood, 1 Jun 71. GM. 1-1-0. THUNDER BAY DIST. Jackfish Mine. Terrace Bay, 6 Jun 71. GM, 0-1-1. Schneber Mine. 6 June 71. GM. 0-1-2. VICTORIA CO. *Hwy 7. 7.26 km eof Hwy 35, under log, 26 Apr 72, JWR, 0-0-1. WATERLOO CO. 'Hwy 97, Gait, .8l'km w of Hwy 24A, under grass clip- pings. 3 May 72. JWR. 9-0-9. Waterloo, Laurel Creek Conservation Area, 3 Aug 74, DPS, 0-3-5, UW-0007. WELLINGTON CO. 'Hwy 6, 1.4 km n of Aberfoyle. under logs, 29 Apr 71, JWR. 0-0-3. •Hwy 6. 10.64 km s of Arthur, under logs, 2 May 72. JWR. 0-0-2. YORK CO. *Hwy 48, .32 km n of Steeles Avenue, under logs. 26 Apr 72. JWR. 1-6-8. Hwy 27, 8.55 km s of Hwy 9. under log, 29 Apr 72. JWR. 0-0-1. Edenbrook Park. Islington, quantitative study 2, formalin, 18 May 72, JWR, 0-1-3. 73 Genus Eisenia Malm, 1877 1877 Eisenia Malm, Ofv. Salsk. Hortik. Forh. Goteborg 1: 45. 1900 Eisenia (part.)-Michaelsen. Das Tierreich, Oligochaeta 10: 474. 1969 £«e/i/a-Gates. J. Nat. Hist. Lond. 9: 305. Type Species Enterion foetidum Savigny, 1826 by Gates (1969). Diagnosis Calciferous gland, without sacs, opening into gut behind insertion of 10/11 through a circumferential circle of small pores. Calciferous sacs, lacking. Giz- zard, mostly in xvii. Hearts, in vii-xi. Nephridial bladders, sausage-shaped or digitiform, transversely placed. Nephropores, inconspicuous, in two ranks on each side, alternating irregularly and with asymmetry between a level just above B and one above D. Setae, closely paired. Prostomium epolobic. Longitudinal musculature, pinnate. Pigment, red. (after Gates, 1972c: 96; 1975a: 3). Discussion Eisenia was erected for three species, Enterion foetidum Savigny, 1826, and Allolobophora norvegica and A. subrubicunda Eisen, 1873 by Malm (1877) with- out the designation of a type species. The two Allolobophora species are now sy- nonyms of Dendrodrilus rubidus. Gates (1969) redefined Eisenia with Eisenia foetida as type species, but another of Savigny's species, Enterion roseum, has been congeneric with Eisenia foetida since Michaelsen (1900b) solely because of spermathecal pore location. If future revisions are based on the more conserva- tive somatic anatomy these two species will not remain congeneric. Most Euro- pean workers have followed Pop (1941) and Omodeo (1956) and have transfer- red E. rosea to Allolobophora. However, on the basis of somatic anatomy it is not reasonable to place E. rosea in any genus of which Enterion chloroticum Savigny is the type species. Until this problem is solved I will continue to use Eisenia rosea to reduce confusion. Recently Gates (1976) transferred E. rosea to the genus Aporrectodea. Eisenia foetida (Savigny, 1826) Manure worm Ver du fumier (Fig. 22) 1826 Enterion fetidum {con. foetidum) Savigny, Mem. Acad. Sci. Inst. Fr. 5: 182. 1835 Lumbricus semifasciatus Burmeister, Zool. Hand. Atl. 33: 3. 1836 Lumbricus annularis R. Templeton, Ann. Mag. Nat. Hist. 9: 234. 1837 Lumbricus foetidus-Duges, Ann. Sci. Nat., ser. 2, 8: 17, 21. 1842 Lumbricus olidus Hoffmeister, Verm. Lumbric, p. 25. 1 849 ? Lumbricus luteus Blanchard, Hist. Chile 3 : 42. 74 1st dp J Fig. 22 External long.tud.nal views of Eiscnia foetida showing taxonomic characters, a Lateral view b Ventral view. (ONT: Nipissing Dist.. cat. no. 7604) 1873 ? Lumbricus rubro-fasciatus Baird. Proc. Linn. Soc. Lond. 1 1 : 96. 1873 Allolobophorafoetida-E\sen, Ofv. Vet.-Akad. Forh. Stockholm 30(8): 50. 1877 Lumbricus annulatus Hutton, Trans. N.Z. Inst. 9: 352. 1877 Eisenia foetida-Ma\m. Ofv. Salsk. Hortik. Forh. Goteborg 1 : 45. 1887 Endnlus annulatus W.W. Smith, Trans. N.Z. Inst. 19: 136. 1889 Lumbricus lAllobophora) annulatus + L. (A.) foetidus-L. Vaillant, Hist. Nat. Annel. 3(1): 147. 149. 1913 Helodrilus (Eisenia) foetidus-Michaeken, Zool. Jb. Syst. 34: 55 1 . 1963 Eisenia foetida var. unicolor Andre, Bull. Biol. Fr. Belg. 81:1. 1972 Eisenia fetida fetida + E. f. andrei Bouche, Inst. Natn. Rech. Agron.. p. 380,381. 75 Diagnosis Length 35-130 mm (generally < 70 mm), diameter 3-5 mm, segment number 80-110, prostoinium epilobic, first dorsal pore 4/5 (sometimes 5/6). Clitellum xxiv, xxv, xxvi-xxxii. Tubercula pubertatis on xxviii-xxx. Setae closely paired, AB = CD, BC < AA, anteriorly DD = ViC but posteriorly DDBC 72, JWR, 0-6-2. *Hwy21, 1.61 km e of Elsinore, under logs, 5 May 72, JWR, 3-0-0-1. CARLE- TON CO. Reynolds (1972a). *Ottawa-Carleton Rd 35. 2.42 km s of Leonard, under logs, 1 1 May 72, JWR, 3-1-3. DUFFERIN CO. Hwy 9. 1.61 km e of Hwy 10. under logs, 29 Apr 72, JWR, 0-0-6. •Hwy 9. 2.1 km w of Hwy 104. digging in road bank, 2 May 72. JWR, 0-0-1. *Hwy 9, 3.71 km w of Orangeville, under logs in ditch, 2 May 72. JWR. 0-2-1. *Hwy 10-24, 8.06 km n of Orangeville. un- der logs, 2 Ma> 72, JWR. 3-0-3. DUNDAS CO. *Hwy 2, 5 km w of Iroquois, under log, 1 1 May 72, JWR. 5-3-5. *Hwj 2. 5.48 km e of Iroquois, under logs, 11 May 72, JWR, 0-0-15. *Hwy 31, 3.55 km n of Mornsburg. under lumber. 1 1 May 72, JWR. 0-0-2. DURHAM CO. Hwy 7A, 2.1 km e of Nes- tletown Station, under logs. 26 Apr 72. JWR. 0-2-1. *Hwy 401. .61 km w of Liberty Rd, Bowman- ville. digging under log next to railroad tracks. 15 May 72. JWR, 2-0-3. *Hwy 402, .32 km e of Mill St. Newcastle, under logs, 15 May 72, JWR, 0-0-2. *Hwy 402, 1.61 km e of Newtonville, under log, 15 May 72, JWR, 0-0-1. ELGIN CO. *Hwy 73, 3.06 km s of Harrietsville, under rotten log, 4 May 72, JWR, 3-1-6. *Hw> 73. 6.77 km n of Aylmer, under logs, 4 May 72, JWR, 0-0-6. Hwy 3, 9.19 km s of St. Thomas, under logs. 4 May 72, JWR. 0-2-8. Hwy 3, 5.16 km w of Talbotville, under log. 4 May 72. JWR. 5-0-6. 'Hwv 6.77 km e of Wallacetown, under pine logs, 4 May 72. JWR, 2-2-0. Hwy 3. 7.9 km w of Frome. under logs, 4 May 72, JWR. 1-2-3. ESSEX CO. *Hwy 3, 1.45 km e of Cottam, un- 81 der logs, 4 May 72, JWR, 0-0-4. *Belle River, s.e., under logs in dump. 4 May 72, JWR, 1-0-1. FRONTENAC CO. *Hwy 15, 4.68 km s of Seeley's Bay. under logs, 16 May 72, JWR, 0-0-3. GLENGARRY CO. *Hwy 34. 1 1.13 km n of Lancaster, under log, 11 May 72, JWR. 2-1-4. 'Hwy 34, 5.64 km n of Alexandria, under logs, 11 May 72, JWR, 3-0-13. GRENVILLE CO. *Hwy 2, Johnstown, w.e., under logs, 11 May 72, JWR, 5-0-6. Hwy 43. Merrickville, under log. 11 May 72, JWR, 0-0-1. GREY CO. *Hwy 6BP. Rockford, w.e.. under log, 5 May 72, JWR, 0-0-1. *Hwy 6, 3.06 km s of Chatsworth, under logs, 5 May 72, JWR. 1-0-3. *Hwy 10, 8.06 km s of Flesherton. under logs, 5 May 72, JWR, 1-0-1. HALDIMAND CO. *Hwy 3. 6.13 km w of Cayuga, under log. I May 72, JWR, 0-0-1. *Hwy 54, 2.26 km w of Caledonia, digging, 3 May 72, JWR, 0-0-2. HALIBURTON CO. 'Reynolds (1972a). HALTON CO. *Hwy 5, 9.19 km w of Hwy 10. under logs next to barn. 29 Apr 72, 1-1-0. 'Halton Co. Rd 3, Esquesing Community, under rock, next to Town Hall, 4 May 73, JWR. 0-1-0. *Hwy 7, 4.84 km e of Georgetown, under burnt log in soil, 4 May 73. JWR. 0-0-1. HASTINGS CO. *Hwy62, 1.61 km n of Hwy 7. under log in wet ditch, 27 Apr 72. JWR. 0-0-1. HU- RON CO. *Hwy 83, 6.77 km w of Russeldale, under logs, 5 May 72. JWR, 0-2-5-1. *Hwy 4. 3.71 km s of Brucefield, under logs and rocks, 5 May 73, JWR. 3-3-7. Hwy 4, 1.29 km n of Hensall. under corn (Zea maize) cobs in pasture, 5 May 72, JWR, 0-0-1. Hwy 4, 5.16 km s of Clinton, under logs, 5 May 72, JWR, 4-1-3. *Hwy 4, 2.74 km n of Clinton, under log, 5 May 72, JWR, 0-0-1. KENT CO. Hwy 3, 1.77 km w of Palmyra, under logs, 4 May 72, JWR, 1-1-2. *Hwy 3, 9.03 km e of Port Alma, under log, 4 May 72, JWR, 0-1-0. *Hwy 3. 3.55 km e of Wheatley. digging, 4 May 72. JWR, 4-1-1. LAMBTONCO. *Hwy 21, 6.45 km n of Dresden, under log, 4 May 72, JWR, 0-0-1. Hwy 21. 11.29 km n of Dresden, under dung in pasture, 4 May 72, JWR, 0-0-1. Hwy 21, .64 km s of Petrolia, ditch, 4 May 72, JWR, 3-0-1. *Hwy 21, Edy's Mills, s.e., under railroad ties, 4 May 72, JWR, 0-0-1. "Hwy 7, 1.61 km n of Arkona, under log, 4 May 72, JWR, 0-4-2. LANARK CO. *Hwy 43. 12.1 km e of Smiths Falls, under logs, 1 1 May 72, JWR, 4-0-6. *Hwy 43, 3.71 km e of Smiths Falls, under tele- phone pole in ditch, 11 May 72. JWR, 0-0-1. *Hwy 43, 5.32 km w of Smiths Falls, under logs, 11 May 72, JWR, 4-0-17. LEEDS CO. *Hwy 15, 2.26 km n of Seeley's Bay, under logs and concrete blocks in ditch, 16 May 72, JWR, 4-1-9. *Hwy 15, .97 km s of Portland, under logs, 16 May 72, JWR, 0-0-5. LENNOX AND ADD1NGTON CO. *Hwy 2, Napanee, w.e., under rock behind EEEE Motel, 15 May 72, JWR, 0-0-1. *Hwy 2, 6.61 km w of Hwy 133, under log, 16 May 72. JWR, 0-0-1. MANITOULIN DIST. *Hwy 68, 5.97 km n of Birch Island, under rock, 13 May 72. JWR & JEM, 0-0-1. *Hwy 68, Birch Island, s.e., under logs, 13 May 72, JWR & JEM, 4-2-8. MIDDLESEX CO. Judd (1964). Reynolds (1972a). *Hwy 73, .97 km n of Mossley, under logs, 4 May 72, JWR, 0- 0-2. *Hwy 7, 2.26 km s of Parkhill, under fence posts, 4 May 72, JWR, 0-1-6. NIAGARA CO. *Hwy 20, 1.61 km e of Smithville, old house site, 1 May 72, JWR, 0-1-4-1. NIPISSING DIST. 'Hwy 17, 1.29 km e of Verner, under paper in wet ditch, 13 May 72. JWR & JEM, 0-0-3. NORTHUMBER- LAND CO. *Hwy 45, 10.65 km s of Norwood, under logs next to barn, 28 Apr 72, JWR, 3-3-3-1. *Hwy 45, 4.84 km n of Baltimore, under log, 28 Apr 72, JWR. 0-0-1. ONTARIO CO. *Hwy 7, 1.61 km e of Green River, under logs, 26 Apr 72, JWR, 3-0-1. *Hwy 7-12, .81 km n of Myrtle, under logs, 26 Apr 72, JWR, 9-0-2. 'Hwy 7. 5.32 km ne of Sunderland, under logs, 9 May 72, JWR. 0-0-4. OX- FORD CO. *Hwy 59, 1.77 km e of Burgessville, under logs and wood chips, 1 May 72, JWR, 3-0-7. *Hwy 59, 1.13 km s of Curries, under junk, 1 May 72, JWR, 5-0-1. *Hwy 59, .32 km n of Hickson, under logs, 3 May 72, JWR, 0-0-2. PEEL CO. *Hwy 5, .81 km e of Dixie Rd, under logs. 29 Apr 72. JWR, 0-0-2. *Hwy 5. 4.35 km w of Hwy 10, under mattress, 29 Apr 72, JWR, 0-0-1. *Hwy 24. 8.87 km n of Erin, under log and dung, 29 Apr 72, JWR, 1-1-0. *Hwy 7, Brampton, e.e., under debris, 4 May 73, JWR, 0-1-4. PERTH CO. .81 km n of Fullarton. under rocks, 29 Apr 72, DWR & LWR, 2- 1-3. 'Mitchell, next to Collegiate, under logs, 4 May 72, JWR & DWR, 0-0-2. PETERBOROUGH CO. *Hwy 28, Lakefield College, under logs near waterfront, 27 Apr 72, JWR & CWR, 14-5-10. •Hwy 28, 5.48 km n of Burleigh Falls, under logs, 27 Apr 72, JWR, 1-0-6. PRESCOTT CO. *Hwy 34,5.81 km n of Vankleek Hill, under logs, 11 May 72, JWR, 1-1-3. PRINCE EDWARD CO. *Hwy 33, 2.58 km e of Hillier, digging, 15 May 72, JWR, 1-0-0. *Hwy 49, Picton, ne., under leaf pile. 15 May 72, JWR, 5-1-4. RUSSELL CO. *Hwy 17. 4.35 km w of Rockland, under log, 11 May 72. JWR, 2-0-1. SIMCOE CO. *Hwy 89, 5.48 km e of Alliston. under log. 2 May 72, JWR, 0-1-0. *Hwy 27, 5.97 km s of Cookstown, under logs, 2 May 72, JWR, 1-0-1. *Barrie. park opposite 14 Greenfield, under rocks and grass clippings, 7 May 72, JWR & GWA. 5-1-3. STORMONT CO. 'Hwy 43. 1.29 km w of Finch, under logs, 1 1 May 72, JWR, 4-2-8. Hwy 43, 1.61 km e of Finch, under log. 1 1 May 72, JWR, 3-1-1. Hwy 43, 3.71 km w of Monkland, under logs, 1 1 May 72. JWR, 2-1-2. THUNDER BAY DIST. Hwy 17, 15.17 km e of Thunder Bay, small stream, 17 Jun 71, ROM Field Party, 9-0-0, 82 ROM -1 34. VICTORIA CO. 'Il«\ 46. 3.71 km nofHwj 7. under log, 9 May 72. J WR. 0-0-1. *Hwy 46. SI km n of Argyle, under logs, 9 Ma> 72, JW R. 1-0-2. WATERLOO CO. *Hw) 97. 3.71 km n of Hwj 401, under log, 3 \l.i\ 72, JWR.0-0-I. Hwy 7-8. 1.77 km w of Petersburg, under log, 3 May 72. JWR, 1-2-& Hw) 86, Wesl Montrose, under log, 3 Ma) 72. JWR, 0-0-1. Waterloo. Laurel Creek Conservation \rea, 3 Any 74, DPS. 0-0-1, UW-0007. Wl I 1 1NGTON CO. *Hwy 24, 5.16 km e of Eramosa. under logs in cedar (77iu/a occidentalis) woodlot, 29 Apr 72, JWR, 3-0-1. *Hwy 24. 4.03 km n of Inn. under logs. 29 Apr 72. JWR. 3-0-1. WENTWORTH CO. Reynolds ( 1972a). YORK CO. *Hu\ Jet 4S and 401, Progress and Bellamy Rdv n« corner under lumber. 26 Apr 72. JWR. 1-1-7. •Hwj 48, .32 km n ol Steeles \venue, under logs. 26 Apr 72. JWR. 3-5-7. *Hwy 27, 1.45 km n of Hw) 7. under logs. 29 Apr 72, JWR, 1-4-9. *Edenbrook Park. Islington, under logs and rocks near Stream bank. 30 Apr 72. JWR & DWR. 25-2-13. Edenbrook Park, Islington, quantitative study 1, formalin. IS Ma) '1 JWR. 16-3-13. Edenbrook Park. Islington, quantitative study 2. formalin, 18 Ma\ 72, JWR. 36-5-12-2 Genus Eiseniella Michaelsen, 1900 1900 Eiseniella Michaelsen. Das Tierreich, Oligochaeta 10: 471. Type Species Enlerion tetraedrum Savigny, 1826. Diagnosis Calciferous sacs, in x, digitiform. opening posteriorly into the gut ventrally in re- gion of insertion of 10/11. Oesophagous of nearly uniform width through xi-xiv, calciferous channels narrow, lamellae low and continued along the lat- eral walls of the sacs. Intestinal origin, in xv. Gizzard, in xvii, weak, 17/18 not fenestrated. Typhlosole, simply lamelliform. Extraoesophageal trunks, joining dorsal vessel in xii. Hearts, in vii-xi. Nephridial bladder, short, sausage-shaped. Nephropores, inconspicuous, behind xv alternating irregularly and with asym- metry between a level just above B and one above D. Setae, not closely paired behind the clitellum. Prostomium epilobic. Longitudinal musculature, pinnate, (after Gates. 1972c: 108). Discussion Michaelsen (1900b) proposed the new name Eiseniella for a genus erected by Ei- sen in 1873. Although designated only as a new name for Allurus Eisen, 1873, Michaelsen included a second genus of Eisen's (Tetragonurus Eisen, 1874) in his Eiseniella. Both of Eisen's generic names were preoccupied (i.e.. already in use as generic names in other groups); Allurus Foerster, 1862 had been used as a genus of hymenopterous insects, while Tetragonurus Risso, 1810 had been em- ployed as a genus of fish. The type species for both of Eisen's genera are syno- nyms of Enlerion tetraedrum Savigny, 1826. Insufficient data are available con- cerning the somatic anatomy of species included at various times in the classical Eiseniella to determine if they can be congeneric with Eiseniella tetraedra. 83 Eiseniella tetraedra (Savigny, 1826) Square-tail worm Ver a queue carree (Fig. 26) 1826 Enlerion tetraedrum Savigny, Mem. Acad. Sei. Inst. Fr. 5: 184. 1826 ? Lumbricus quadrangularis Risso, Hist. Nat. Eur. Merid. 4: 426. 1828 ? Lumbricus amphisbaena Duges, Ann. Sci. Nat. 15: 289. 1837 Lumbricus tetraedrus-Duges, Ann. Sci. Nat., ser. 2, 8: 17, 23. 1843 Lumbricus agilis Hoffmeister, Arch. Naturg. 9(1): 191. 1871 Lumbricus tetraedrus-Eisen + L. t. luteus + L. t. obscurus Eisen, Ofv. Vet.-Akad. Forh. Stockholm 27(10): 966, 967, 968. 1873 Allurus tetraedrus-Eisen, Ofv. Vet.-Akad. Forh. Stockholm 30(8): 54. 1874 Tetragonurus pupa Eisen, Ofv. Vet.-Akad. Forh. Stockholm 31(2): 47. 1885 Allurus neapolitanus Orley, Ertek. Term. Magyar Akad. 15(18): 12. 1886 Allurus ninnii Rosa, Atti 1st. Veneto, ser. 6, 4: 680. 1889 Lumbricus (Allolobophora) neapolitanus + L. (Allurus) tetraedrus + L. (Eisenia)pupa-L. Vaillant, Hist. Nat. Annel. 3(1): 1 13, 151, 154. 1889 Allurus hercynius-M'ichadsen + A. dubius Michaelsen + A. n/wi/7-Michaelsen, Mitt. Mus. Hamburg 7(3): 7, 10. 1890 Eisenia pupa-Benham, Quart. J. Micros. Soc, n.s., 31(2): 266. 1892 Allolobophora tetragonurus-Friend, Sci. Gossip 28: 194. 1892 Allurus tetraedrus + A. amphisbaena + A. flavus + A. tetragonurus- Friend, Proc. R. Irish Acad., ser. 3, 2: 402. 1896 Allurus tetraedrus-K\bd.\xco\xr\ + A. bernensis + A. novis + A. infinitesi- malis Ribaucourt, Rev. Suisse Zool. 4: 69, 73, 74. 1900 Eiseniella te?raeCD, DD ^ V2C anteriorly and Z)D60 mm), diameter 4-6 mm, segment number 70-120, prostomium tanylobic, first dorsal pore 5/6-8/9. Clitellum xxvi, xxvii-xxxi, xxxii. Tubercula pubertatis on xxviii-xxxi. Setae closely paired, AA > BC, AB > CD, DD = V2C posteriorly. Genital tumescences in viii-xii (less frequently on x), xx-xxiii, xxvi-xxxvi. Male pores, inconspicuous, without glan- dular papillae on xv. Seminal vesicles, three pairs in 9, 11, and 12+ 13. Sper- mathecae, two pairs with short ducts opening in 9/10 and 10/11. Colour, ruddy brown or red-violet and iridescent dorsally, pale yellow ventrally. Body cylindri- cal and sometimes dorsoventrally flattened posteriorly. Biology Lumbricus rubellus has been recorded from natural soils of pH 3.8-8.0 and shows a wide tolerance of habitat factors. Olson (1928, 1936) reported it from under debris. Eaton (1942) found it in stream banks, under logs, and in woody peat and stated that it seemed to require a great deal of moisture and organic matter. Cernosvitov and Evans (1947) recorded the habitats of this species as places rich in humus, abundant in parks, gardens, pastures, on river banks, un- der stones, moss, or old leaves. Gerard (1964) also found this species frequently aggregated beneath dung in pastures as well as the sites mentioned above. In Ontario, L. rubellus was obtained from a wide variety of habitats. This species also is known from caves in Europe. Under suitable conditions activity, including breeding, is year round. L. rubellus is obligatorily amphimictic (Reynolds, 1974c) and copulation, like defe- cation, occurs below the soil surface, or in the litter layer, at any time of day. It seems that copulation does not involve a mucous tube (Gates, 1972c). This species has been cultured by the fish bait industry (Gates, 1972c). It is also important in the decomposition of litter. Range Lumbricus rubellus is now known from Europe, Iceland, North America, Mexi- co, Asia, South Africa, and New Zealand (Gates, 1972c). North American Distribution British Columbia (Berkeley. 1%8), New Brunswick (Reynolds. 1976d). Newfoundland (Smith. 1917), Nova Scotia (Reynolds, 1975a, 1976a), Ontario (Reynolds, 1972a), Prince Edward Island (Reynolds, 1975c), Quebec (Reynolds, 1975b. e. 1976c). Alaska (Gates, 1954), Arkansas (Causey, 95 1st dp- -pr -GT -GT Q o ■GT GT £) I — TP Fig. 32 External longitudinal views of Lumbricus rube/lux showing taxonomic characters, a Lateral view, b Ventral view. (ONT: Parry Sound Dist., cat. no. 7505) 96 1952). California (Smilh 1917). Colorado (dates. 1967). Connecticut (Reynolds. 1973c). Delaware (Reynolds, 1973a), District of Columbia (Eaton, 1942). Florida (Gates, 1 972c). Idaho (Gates, 1967), Illinois (Smith. 1928), Indiana (Jo\ner, I960). Mars land (Reynolds, 1974b), Massachusetts (Rey- nold-. 1977), Michigan (Smith. 1917), Missouri (Olson. 193m. New Hampshire (Reynolds. 1976c), New Jersej (Davies, 1954), Now York (Olson, 1940), Ohio (Olson, 1928). Oregon (Smith. 1917), Pennsylvania (Eaton, 1942). Rhode Island (Reynolds, 1973b). Tennessee (Reynolds, 1972b), Utah (dates. 1967). Vermont (Reynolds, 1976c). Virginia (Reynolds, 1974b), Washington, (Smith, 1917), West Virginia (Reynolds, 1974b), Greenland (Omodeo, 1955a). New records: Manitoba. Oeorgia, Minnesota. North Carolina. Ontario Distribution (Fig. 33) Lumbricas rubelhis was first reported from Ontario by Stafford (1902) and only once since then (Reynolds, 1972a). The species is widely distributed across the province and additional collecting under favourable conditions should fill the gaps in its distribution. ALGOMA DIST. "Hwy 17. 7.58 km e of Spanish, under logs, 13 May 72, JWR & JEM, 16-10-8. *Hwy 17, .48 km e of Spanish, under logs and paper in ditch. 13 May 72. JWR & JEM, 4-1-5. Gar- gantua Bay. 1 1 Jun 75. DRB. 1-0-0. UW-0001. BRANT CO. »Hwy 53, 5.48 km w of Cathcart. under railroad ties. 1 May 72. JWR. 0-1-0. *Hwy 54. .64 km w of Onondaga, under log in wet area, 3 May 72. JWR. 0-1-0. BRUCE CO. Hwy 21, 2.57 km n of Tiverton, under lumber. 5 May 72, JWR, 1-0-0. CARLETON CO. Reynolds (1972a). COCHRANE DIST. Reynolds (1972a). DUFFERIN CO. •Hwy 9. 10-16 km w of Orangeville. under junk, 2 May 72, JWR, 0-1-0. *Hwy 9, 3.71 km w of Or- angeville. under log in ditch. 2 May 72, JWR. 0-1-0. DUNDAS CO. *Hwy 34, 1.29 km e of Chester- Fig. 33 The known Ontario distribution of Lumbricus rubellus. 97 ville, under rock in ditch, 11 May 72, JWR, 0-1-0. *Hwy 31..81 km n of Hwy 43. under logs. 11 May 72, JWR, 1-1-4. DURHAM CO. *Hwy 401, .16 km w of Liberty Rd. Bowmanville. digging under log next to railroad tracks, 15 May 72. JWR, 1-0-0. *Hwy 401, .32 km e of Mill St. Newcastle, under log, 15 May 72, JWR, 1-0-0. ELGIN CO. *Hwy 73, 3.06 km s of Harnetsville, under rotten log, 4 May 72, JWR. 2-0-0. *Hwy 73, 6.77 km n of Aylmer, under logs, 4 May 72, JWR. 4-2-3. Hwy 3, 9.19 km e of St. Thomas, under logs, 4 May 72, JWR. 0-2-0. *Hwy 3. 6.77 km e of Wallacetown. under pine logs, 4 May 72, JWR, 2-0-0. Hwy 3, 3.87 km w of New Glasgow, under lumber in abandoned school yard, 4 May 72, JWR, 3-0-0. ESSEX CO. Hwy 3, 3.87 km w of Leamington, under lumber in dump, 4 May 72, JWR, 10-0-0. FRONTENAC CO. *Hwy 2, 1.13 km e of Westbrook, under logs and paper, 16 May 72, JWR, 5-1-9. *Hwy 15, 4.03 km n of Hwy 401, under paper in wet ditch, 16 May 72, JWR, 0-1-0. *Hwy 41, 1.29 km n of Clovne, under logs in ditch, 16 May 72. JWR. 0-0-8. GRENVILLE CO. Hwy 2, Cardinal, w.e., under log and paper, 1 1 May 72, JWR, 2-0-0. GREY CO. *Hwy 6BP, Rockford, w.e., under logs, 5 May 72, JWR, 7-1-0. *Hwy 6, 3.06 km s of Chatsworth, under logs, 5 May 72, JWR, 2-0-0. HALD1MAND CO. *Hwy 3. 9.03 km e of Dunnville, wet ditch, I May 72, JWR. 3-0-1. HALIBURTON CO. 'Reynolds (1972a). *Hwy 121. 3.22 km e of Tory Hill, dump, 16 May 72. JWR, 6-1-21. HURON CO. *Hwy 83, 6.77 km w of Russeldale, under logs. 5 May 72, JWR, 3-1-0. »Hwy 4, 1.61 km n of Exeter, wet ditch, 5 May 72, JWR, 5-1-0. Hwy 4, 1.29 km n of Hensall, under corn (Zea maize) cobs in pasture, 5 May 72, JWR, 1-0-0. *Hwy 4, 3.71 km s of Brucefield, under log and rock, 5 May 72, JWR. 2-0-0. *Hwy 4, 2.74 km n of Clinton, under logs, 5 May 72, 2-1-2. *Hwy 4, 1.29 km s of Wingham, under log in wet area, 5 May 72, JWR, 1-0-0. KEN- ORA D1ST. Rushing River Provincial Park, stream trickle in campground, 13-14 Jun 71. ROM Field Party, 1-0-0, ROM-I36. LENNOX AND ADDINGTON CO. 'Hwy 500, .81 km n of Den- bigh, under log, 16 May 72, JWR, 1-0-0. Hwy 7, Kaladar, e.e., under lumber in school yard. 16 May 72, JWR, 2-0-2. MAN1TOUL1N DIST. *Hwy 68, 5.97 km n of Birch Island, under rock. 13 May 72, JWR & JEM, 0-0-1. *Hwy 68, 2.42 km s of Birch Island, under logs, 13 May 72, JWR & JEM.3-1- 22. MIDDLESEX CO. *Hwy 73, .97 km n of Mossley, under logs, 4 May 72, JWR, 6-1-6. MUS- KOKA DIST. *Hwy 11, 12.9 km s of Bracebridge, under rock, 9 May 72, JWR, 1-0-0. *Hwy 11, 9.19 km s of Hwy 516, under logs and rocks in wet ditch, 9 May 72, JWR, 3-1-0. NIAGARA CO. *Queen Elizabeth Hwy, 1.13 km w of Ontario St, Grimsby, under logs and lumber, 1 May 72, JWR, 4-1-0. 'Niagara Co. Rd 12, 3.06 km s of Grimsby, under paper in wet ditch, 1 May 72. JWR, 5-1-6. *Hwy20. 1.61 km e of Smithville, old house site under lumber, 1 May 72, JWR, 4-1-1. NIPISSING DIST. *Hwy 17, 5.48 km e of Warren, under log and dung in pasture, 13 May 72. JWR & JEM, 5- 5-10. Hwy 17, 15.81 km e of Sturgeon Falls, dump. 13 May 72, JWR & JEM, 6-4-5. NORFOLK CO. *Hwy 6, 4.84 km s of Jarvis, under logs, 1 May 72. JWR, 1-1-1. OXFORD CO. "Hwy 97, Washington, w.e., under log, 3 May 72, JWR, 1-0-0. PARRY SOUND DIST. "Hwy 520, 10.32 km e of Magnetawan, under lumber, 9 May 72, JWR, 5-2-3. *Hwy 520, Magnetawan. e.e., under rocks, 9 May 72, JWR, 2-0-1. *Hwy 124, 2.26 km w of Hwy 520. under logs, 9 May 72, JWR, 4-3-2. *Hwy 124, 3.06 km e of McKellar, under logs, 9 May 72, JWR, 0-0-3. "Hwy 124, 3.55 km n of Hwy 69, un- der logs, 9 May 72, JWR, 1-0-3. PETERBOROUGH CO. 'Hwy 28, Lakefield College, under logs near waterfront, 27 Apr 72, JWR & CWR, 2-0-0. *Hwy 504, 1.61 km e of Apsley, under log. 27 Apr 72, JWR, 1-0-0. RENFREW CO. M.19 km s of Palmer Rapids, under paper in ditch. 16 May 72, JWR, 2-2-3. RUSSELL CO. *Hwy 17, 7.74 km e of Rockland, under paper in wet ditch, 1 1 May 72, JWR, 9-1-0. 'Hwy 17, 4.35 km w of Rockland, under logs, 1 1 May 72, JWR, 9-2-4. *2.42 km s of Li- monges, under lumber at old house site, 1 1 May 72, JWR, 0-1-0. *2.9 km e of Embrun. under logs, I I May 72, JWR, 3-0-3. SIMCOE CO. Hwy 27, 3.22 km s of Newton Robinson, wet ditch. 2 May 72, JWR, 2-0-0. 'Barrie. park opposite 14 Greenfield, under rock and grass clippings. 7 May 72, JWR, 6-1-0. STORMONT CO. *Hwy 43, 5.48 km w of Finch, in and under straw in wet ditch, 1 1 May 72, JWR. 3-1-0. SUDBURY DIST. *Hwy 69, 3.39 km n of Estaire, under rocks and grass near house, 13 May 72, JWR & JEM, 3-0-6. *Hwy 17, 2.74 km e of Whitefish, under paper in ditch, 13 May 72, JWR & JEM, 3-2-8. VICTORIA CO. *Hwy 7, 1.94 km w of Hwy 46, under logs and dung in pasture, 9 May 72, JWR, 5-0-0. Hwy 48, Bolsover. e.e., under paper in wet ditch. 9 May 72. JWR. 0-1-0. WATERLOO CO. Hwy 86, West Montrose, under log, 3 May 72, JWR. 1-0-0. Waterloo, Beechwood South, on sidewalk after rain (evening), 15 Jun 75, DPS, 2-0-1, UW-0004. WELLING- TON CO. *Hwy 24, 5.16 km e of Eramosa, under log in cedar (Thuja ocadentalis) woodlot. 29 Apr 72. JWR, 1-0-0. WENTWORTH CO. Reynolds (1972a). "Hwy 6, 5.32 km n of Hwy 5. under logs, 29 Apr 72, JWR, 2-0-1. YORK CO. Edenbrook Park. Islington, quantitative study I, formalin. 18 May 72, JWR, 34-0-0. Edenbrook Park, Islington, quantitative study 2, formalin, 18 May 72. JWR. 47-0-1. 98 Lumbricus terrestris Linnaeus, 1758 Nightcrawler, Dew-worm Ver nocture rampant (Fig. 34) 1758 Lumbricus terrestris (part.) Linnaeus. Syst. Nat. (ed. 10), p. 647. 1774 Lumbricus terrestris (part.)-Miiller, Verm. Terr. Fluv. 1(2): 24. 1780 Lumbricus terrestris (part.) + L. norvegicus (part.)-Fabricius, Fauna Gr0nlandica, p. 277. 1825 Lumbricus terrester (part.)-Blumenbach. Hand. Naturg. (ed. 1 1), p. 365. 1826 Enterion herculeum Savigny, Mem. Acad. Sci. Inst. Fr. 5: 180. 1837 Lumbricus herculeus- Duges, Ann. Sci. Nat., ser. 2, 8: 17, 21. 1842 Lumbricus agricola Hoffmeister. Verm. Lumbric, p. 24. 1867 Lumbricus infelix Kinberg, Ofv. Vet.-Akad. Forh. Stockholm 23: 98. 1872 ? Lumbricus americanus E. Perrier, Nouv. Arch. Mus. Paris 8: 44. 1884 Lumbricus herculeus-Rosa., Lumbric. Piemonte, p. 22. 1896 Lumbricus studeh Ribaucourt, Rev. Suisse Zool. 4: 5. 1900 Lumbricus /w?5/m-Michaelsen, Das Tierreich, Oligochaeta 10: 511. 1937 Lumbricus herculeus-Tetry, Bull. Mus. Hist. Nat. 9: 151. 1953 Lumbricus terrestris-Gx&R, Zool. Anz. 161(1 1/12): 324. 1958 Lumbricus terrestris-Gales, Breviora, Mus. Comp. Zool. 91: 8. 1969 Lumbricus herculeus-Bouche, Pedobiologia 9: 89. 1970 Lumbricus herculeus-Bouche, Rev. Ecol. Biol. Sol 7(4): 541. 1972 Lumbricus herculeus-Bouche and Beugnot, Rev. Ecol. Biol. Sol 9(4): 697. 1972 Lumbricus herculeus-Bouche, Inst. Natn. Rech. Agron., p. 352. 1973 Lumbricus terrestris-Sims. Bull. Zool. Nomencl. 30(1): 27. NOTE: These are the major synonyms and references for Lumbricus terrestris Linnaeus. Unfortunately, Lumbricus terrestris has become almost synonymous with "earthworm" in many parts of the world. This has led to many published studies and reports about the species which in fact were undertaken on differ- ent, and frequently distantly related, species (Orley, 1881; Vaillant, 1889; Ste- phenson, 1930: xi; Causey, 1952; Stebbings, 1962: 905; Cameron and Fogal, 1963; Gates, 1972a: 1 14-1 15; and Gates, 1972c: 120-123). Diagnosis Length 90-300 mm, diameter 6-10 mm, segment number 120-160, prostomium tanylobic. first dorsal pore 7/8. Citellum xxxi, xxxii-xxxvii. Tubercula puberta- ls xxxiii-xxxvi. Setae enlarged and widely paired in the caudal and cephalic re- gions (i.e.. AB and CD are greater) but closely paired and smaller in the central region. AA>BC, AB>CD. and DD = V2C anteriorly, DD Rd. garden. 28 Oct 41. JO. 1-0-8. ROM. 103 Genus Oetolasion Orley, 1885 1885 Oetolasion (part.) Orley, Ertek. Term. Magyar Akad. 15( 18): 13. 1889 Lumbricus (Oetolasion) (part.) + L. ( A llobophora) (part.) + Dendrobaena (part.) + L. (L.j (part.) + Titanus ? (part.)-L. Vaillant, Hist. Nat. Annel. 3(1): 113. 130. 116. 121.93. 1896 Oetolasion + Allolobophora (OctolasionhRibaucourt, Rev. Suisse Zool. 4:95. 1900 Octolasium (part.)-Michaelsen, Das Tierreich, Oligochaeta 10: 504. 1930 Octolasium (part.) Stephenson, Oligochaeta (Oxford), p. 914. 1972 Octolasium-Bouche, Inst. Natn. Rech. Agron., p. 253. 1975 Octolasion-Gates, Megadrilogica 2( 1): 4. Type Species Oetolasion lacteum Orley, 1885 (= Enterion tyrtaeum Savigny, 1826). Diagnosis Calciferous sacs, in x, large, lateral, communicating vertically and widely with gut lumen though reaching beyond oesophagus both dorsally and ventrally. Calciferous lamellae continued onto posterior walls of sacs. Intestinal origin, in xv. Gizzard, mostly in xvii. Extraoesophageals. passing up to dorsal trunk poste- riorly in xii. Hearts, vi-xi. Nephridial bladders, ocarina-shaped. Nephropores, obvious, behind xv in one regular rank on each side, just above B. Setae, behind the clitellum not closely paired. Prostomium epilobic. Longitudinal muscula- ture, pinnate, (after Gates, 1972c: 123, 1975a: 4). Discussion There has been considerable confusion concerning the spelling of this genus name since the early 1900s. Michaelsen (1900b) changed many of the Greek generic endings to Latin endings, i.e., Oetolasion to Octolasium and Bimastos to Bimastus. According to the International Code of Zoological Nomenclature (Article 32), the original spelling is the correct spelling. Therefore, Oetolasion Orley, 1885 and Bimastos Moore, 1893 are the correct spellings and most cur- rent oligochaetologists are now employing them. The genus Oetolasion Orley, 1885 contains only two species, O. cyaneum and O. tyrtaeum. Species in Europe and elsewhere often placed in Oetolasion are now considered to belong in the genus Octodrilus Omodeo, 1956 with Lumbricus complanatus Duges, 1828 as the type (cf. Bouche, 1972, Gates, 1975a). 104 Octolasion cyaneum (Savigny, 1826) Woodland blue worm Yer bleu des bois (Fig. 36) 1774 Lumbricus terrestris (part.) Miiller, Verm. Terr. Fluv. 1(2): 24. 1826 Enterion cyaneum Savigny, Mem. Acad. Sci. Inst. Fr. 5: 181. 1837 Lumbricus cyaneus Duges, Ann. Sci. Nat., ser. 2, 8: 17,21. 1845 Lumbricus stagnalis (part.) HofFmeister, Regenwiirmer, p. 35. 1867 Lumbricus alyattes Kinberg. Ofv. Vet.-Akad. Forh. Stockholm 23: 99. 1889 Lumbricus alyattes + Lumbricus ( Dendrobaena) stagnalis + Lumbricus cyaneus-L. Vaillant. Hist. Nat. Annel. 3(1): 96, 1 18. 124. 1890 Allolobophora studiosa Michaelsen. Arch. Ver. Mechlenb. 44: 50. 1893 Allolobophora (Octolasion) cvanea (part.)-Rosa, Mem. Ace. Torino, ser. 2, 43:424.455,456. 1896 Allolobophora (Octolasion) cvanea studiosa-Ribaucourl, Rev. Suisse Zool. 4: 95. 1900 Octolasium cvancum- Michaelsen, Das Tierreich, Oligochaeta 10: 506. 1972 Octolasium cyaneum— Boxxche + O. c. var. armoricum Bouche, Inst. Natn. Rech. Agron.. p. 258, 260. 1972 Octolasium ow?euw-Edwards and Lofty, Biol, earthworms, p. 214. 1972 Octolasion cyaneum-Gates, Bull. Tall Timbers Res. Stn. 14: 31. Diagnosis Length 65-180 mm. diameter 7-8 mm, segment number 140-158, prostomium epilobic, first dorsal pore 11/12 or 12/13. Clitellum xxix-xxxiv. Tubercula pu- bertals xxx-xxxiii. Setae closely paired anteriorly, CD<^AB<^BC<^AA<^DD, and widely paired posteriorly, AB^>BC^>CD. Setae of x, xviii, xix, xx, xxi fre- quently on white genital tumescences. Male pores on xv with well-defined nar- row papillae. Seminal vesicles, four pairs in 9-12, with the pairs in 11 and 12 larger than the pairs in 9 and 10. Spermathecae, two pairs opening between c and d in 9 10 and 10/11. Body cylindircal but octagonal posteriorly. Colour, blue-grey or whitish. Biology This species is known from soils of pH 5.2-8.0 and may well be ubiquitous with respect to this factor. Gates (1972c) records it from under stones in water, in moss, stream banks, and other limnic habitats. It is known also from ploughed fields, wet sand, forest soils, and from caves in Europe. Cernosvitov and Evans ( 1947) reported it mostly from under stones and occasionally under moss. Gates ( 1973a) found the species under logs and under rocks near stream beds. Under logs and rocks was the most common site for O. cyaneum in Ontario. Activity may be year round but in central Maine summer drought and winter freezing impose two periods of inactivity (Gates, 1972c), and this is probably the case in Ontario. In experimental studies casting was below ground but occa- sional surface casting has been reported (Gates, 1972c). O. cyaneum is obligato- 105 1st dp—; XXV XXX XXXV mp Fig. 36 External longitudinal views of Octolasion cvaneum showing taxonomic characters, a Lat- eral view. b. Ventrolateral view. (ONT: Durham Co., cat. no. 3384) 106 nl\ parthenogenetic (Reynolds. 1974c): copulation has not been recorded and ma\ never have boon observed (Gates, 1972c). This species is relatively rare in North America and is of little or no economic importance. Range A native of Palaearctis, O. cyaneum is now known from Europe, Iceland. North America. South America. India. Azores, and Australasia (Gates, 1972c). North American Distribution British Columbia (Wickett, 1967), Ontario (Reynolds, 1972a), Nova Scotia (Reynolds. 1976a), Cali- fornia (Gates. 1966). Colorado (Gates. 1967). Georgia (Gates. 1973a), Indiana (Reynolds et al., 1974). Iowa (Evans. 1948a). Maine (Gates. 1966). Massachusetts (Reynolds. 1977), New York (Schwert. 1976). North Carolina (Gates. 1973a). Pennsylvania (Reynolds. 1974b), Tennessee (Rey- nolds. 1974ai. Virginia (Gates. 1973a), Washington (Gates. 1973a). New records: Quebec. Mississip- pi- Ontario Distribution (Fig. 37) Octolasion cyaneum was first reported from Ontario by Reynolds (1972a) and the report presented here is only the second account of this species in Ontario. O. cyaneum has been obtained only from Haliburton and Perth counties. H ALIBL'RTON CO. 'Reynolds (1972a). PERTH CO. .81 km n of Fullarton. under rocks. 29 Apr 72. DWR& l.WR. 1-1-0. Fig. 37 The known Ontario distribution of Octolasion cyaneum 107 Octolasion tyrtaeum (Savigny, 1826) Woodland white worm Ver blanc des bois (Fig. 38) 1826 Enterion tyrtaeum Savigny, Mem. Acad. Sci. Inst. Fr. 5: 180. 1837 Lumbricus tyrtaeus-Duges, Ann. Sci. Nat., ser. 2, 8: 17, 22. 1845 Lumbricus communis cyaneus + L. stagnalis (part.) Hoffmeister, Regen- wiirmer, p. 24, 35. 1881 Lumbricus terrestris var. lacteus + L. t. var. rubidus Orley, Math. Term. Kozlem. Magyar Akad. 16: 584. 1884 Allolobophora profuga Rosa, Lumbric. Piemonte, p. 47. 1885 Octolasion rubidum-Or\ey + O. profugum-Ox\ty + O. gracile Orley + O. lacteum-6r\ey, Ertek. Term. Magyar Akad. 15(18): 16, 17, 18, 21. 1889 Lumbricus (Allobophora) profugus + L. (O.) gracilis L. Vaillant, Hist. Nat. Annel. 3(1): 113. 1896 Allolobophora (Octolasion) rubida-R\ba.ucourt + A. (O.) gracilis- Ribaucourt + A. sylvestris Ribaucourt, Rev. Suisse Zool. 4: 63, 65, 67, 95. 1900 Octolasium lacteum-Michaeteen, Das Tierreich, Oligochaeta 10: 506. 1900 Allolobophora (Octolasion) profuga-MichaeXsen, Abh. Nat. Verh. Ham- burg 16(1): 16. 1900 Allolobophora profuga-Smhh, Bull. Illinois St. Lab. Nat. Hist. 5: 441. 1917 Octolasium lacteum-Smith, Proc. U.S. Natn. Mus. 52(2174): 178. 1952 Octolosium ladeum (laps.)-Goff, Amer. Midi. Nat. 47: 484. 1971 Octolasium lacteum-Crossley, Reichle and Edwards, Pedobiologia 11: 71. 1972 Octolasium lacteum-Edwards and Lofty, Biol, earthworms, p. 216. 1972 Octolasium lacteum lacteum + O. I. gracile-Bouche, Inst. Natn. Rech. Agron., p. 253, 257. 1972 Octolasion tyrtaeum-Gales, Bull. Tall Timbers Res. Stn. 14: 35. Diagnosis Length 25-130 mm, diameter 3-6 mm, segment number 75-150, prostomium epilobic, first dorsal pore 9/10-13/14, usually 11/12. Clitellum xxx-xxxv. Tu- bercula pubertatis xxxi-xxxiv. Setal pairings as in Octolasion cyaneum. Fre- quently setae a and/or b on xxii and occasionally on ix-xii, xiv, xvii, xix-xxiii, xxvii, xxxvii, or xxxviii are on genital tumescences and modified into genital se- tae. Male pores on xv and on large glandular papillae extending over xiv and xvi, occasionally limited to xv. Seminal vesicles, four pairs in 9-12, with pairs in 11 and 12 larger than pairs in 9 and 10. Spermathecae, two pairs opening on level C or between c and d in 9/10 and 10/1 1. Body cylindrical but slightly oc- tagonal posteriorly. Colour variable, milky white, grey, blue, or pink. Biology Reported from soils of pH 5.5-8.08, O. tyrtaeum has been found under stones and logs, in peat, leaf mould, compost, forest litter, gardens, cultivated fields and pastures, bogs, stream banks, in springs, and around the roots of submerged vegetation (Gates, 1972c). The species is also known from caves in Europe and 108 1st dp } — mp Fig. 38 External longitudinal views of Octolasion tyrtaeum showing taxonomic characters, a. Dor- solateral view, b Ventrolateral view. (ONT. Bruce Co., cat. no. 7557) 109 North America. Smith (1917) reported this species as commonly found under logs, leaf mould, and debris of various kinds, in compost heaps, and to some ex- tent in the soil. Some workers believed this species preferred rich, moist organic material (Causey, 1952), while others presented data to the contrary (Eaton, 1942). Octolasion tyrtaeum was the most abundant species in Tennessee (Rey- nolds et al., 1974) and was obtained under logs, debris, and rocks, and by dig- ging. In Ontario it was most frequently found under logs. Activity may be year round although summer drought and winter cold may impose two rest periods. Octolasion tyrtaeum is an obligatorily parthenogenetic species (Gates, 1973a; Reynolds, 1974c) and copulation occurs below the sur- face of the soil. The species is of little economic importance although one dealer in Michigan is reported to have sold it for fish bait (Gates, 1972c). Range A native of Palaearctis, O. tyrtaeum is known from Europe, North America, South America, Asia, Africa, and Australia (Gates, 1972c). North American Distribution British Columbia (Wickett, 1967), Manitoba (Gates, 1972c), Nova Scotia (Reynolds, 1975a, 1976a), Ontario (Reynolds, 1972a), Quebec (Reynolds, 1975d, e, 1976c). Alabama (Gates, 1972c), Arkansas (Causey, 1952), California (Smith, 1917), Connecticut (Reynolds, 1973c). Florida (Gates. 1972c), Georgia (Gates, 1972c), Idaho (Gates. 1967), Illinois (Smith, 1917). Indiana (Reynolds, 1972e). Iowa (Gates, 1967), Kentucky (Allee et al., 1930) Maine (Gates. 1961), Maryland (Reynolds, 1974b), Massachusetts (Reynolds. 1977). Michigan (Murchie, 1956). Minnesota (Gates. 1973a), Missouri (Olson, 1936), Nebraska (Gates, 1967), New Jersey (Davies, 1954), New York (Olson. 1940), North Carolina (Gates, 1973a), Ohio (Smith, 1917), Oregon (MacNab and McKey-Fender, 1947). Pennsyl- vania (Davies, 1954), South Carolina (Gates, 1973a), Tennessee (Reynolds, 1974a), Utah (Gates. 1967), Virginia (Gates, 1973a) West Virginia (Gates, 1959). New records: Alaska. Mississippi, Wis- consin. Ontario Distribution (Fig. 39) Octolasion tyrtaeum was first reported from Ontario by Reynolds (1972a) and the present study is only the second report of the species from Ontario. It is more widely distributed than O. cyaneum and there are two main centres of dis- tribution, the first around the Kawartha Lakes region in central southern Ontar- io, and the second in western southern Ontario running along the Niagara Es- carpment and to the west. BRANT CO. *Hwy 54, .64 km w of Onondaga, under log in wet area, 3 May 72, JWR, 0-0-1. BRUCE CO. *Hwy 4, 6.77 km s of Teeswater, under log, 5 May 72. JWR. 0-0-1. *Hwy 4. .48 km s of Hwy 9, under logs, 5 May 72, JWR, 2-2-4. Hwy 21, 2.57 km n of Tiverton, under lumber. 5 May 72, JWR, 9-0-2. DURHAM CO. *Hwy 7A, 2.1 km e of Nestleton Station, under log, 26 Apr 72, JWR, 0-0-1. ELGIN CO. Hwy 3, 9.19 km e of St. Thomas, under logs, 4 May 72. JWR. 2-2-8. GREY CO. *Hwy 6, 6.94 km s of Dornoch, under logs, 5 May 72, JWR. 2-1-2. *Hwy 4, 8.22 km e of Durham, under logs, 5 May 72, JWR, 1-0-1. HALIBURTON CO. •Reynolds (1972a). HALTON CO. Hwy 5, 5.81 km e of Hwy 25. under paper and leaves in ditch. 29 Apr 72. JWR, 1-0-1. *Halton Co. Rd 3, Esquesing Community, under rocks and logs next to the Town Hall. 4 May 73. JWR. 0- 4-3-1. Campbellville, rapids in cold stream, 15 May 66. IMS, ST, & RNS. 0-1-0, ROM-I6. HURON CO. *Hwy 83, 6.77 km w of Russeldale, under logs, 5 May 72. JWR, 3-0-1. NORTH UMBER- 110 Fig. 39 The known Ontario distribution of Octolasion tyrtaeum. LAND CO. *Hwy 45. 4.84 km n of Baltimore, under logs, 28 Apr 72, JWR, 1-4-1. OXFORD CO. •Hwy 97, Washington, w.e., under logs, 3 May 72, JWR, 0-1-3. PEEL CO. *Hwy 5, .81 km e of Dixie Rd. under logs. 29 Apr 72, JWR. 0-1-1. PETERBOROUGH CO. *Hwy 28, Lakefield College, under logs near waterfront, 27 Apr 72, JWR & CWR, 4-5-8. VICTORIA CO. *Hwy 7, 7.26 km e of Hwj 35. under log, 26 Apr 72, JWR, 0-3-1. WATERLOO CO. *Hwy 24A, 1 1.45 km n of Pans, un- der log, 3 May 72, JWR. 4-0-2. *Hwy 97, 3.71 km w of Hwy 401, under log, 3 May 72, JWR, 0-1-0. Hwy 7-8. 1.77 km w of Petersburg, under log, 3 May 72, JWR, 1-2-1. Waterloo, Beechwood South, on sidewalk after rain (evening), 15 Jun 75, 0-0-1, DPS, UW-0004. WELLINGTON CO. *Hwy 6, 2.26 km n of Aberfoyle, under log, 29 Apr 72, JWR, 0-0-1. *Hwy 24, 5.16 km e of Eramosa, under logs in cedar ( Thuja occidentalis) woodlot, 29 Apr 72, JWR, 0-1-1. *Hwy 6, 10.65 km s of Arthur, un- der log, 2 May 72, JWR. 0-0-1. WENTWORTH CO. Reynolds (1972a). *Hwy 6, 5.32 km n of Hwy 5, under logs, 29 Apr 72, JWR, 1-0-2. Ill Family SPARGANOPHILIDAE Michaelsen, 1921 Diagnosis Digestive system: without gizzard, calciferous glands, lamellae, caeca, typhlo- sole, or supra-intestinal glands, with an intestinal origin in front of the testis seg- ments. Vascular system: with complete dorsal and ventral trunks, two pairs of anterior lateroparietal trunks, one of which passes to the dorsal vessel and the other to the ventral vessel in xiv, but without subneural and supra-oesophageal trunks. Hearts: lateral, moniliform, in vii-xi. Blood glands: protuberances from capillaries in septal glands. Nephridia: holoic. aborted at maturity in first 12 or more segments, avesiculate, peritoneal cells investing postseptal portions en- larged, ducts without muscular thickening passing into parieties in AB. Nephro- pores: inconspicuous, in AB. Setae: eight per segment. Dorsal pores and pig- ment, lacking. Prostomium, zygolobous. Anus, dorsal. Reproductive apertures: all minute and superficial, female pores in xiv, spermathecal pores in front of testis segments. Clitellum multilayered, including male pore segment. Seminal vesicles, trabeculate. Ovaries, in xiii, each terminating in a single eggstring. Ova, not yolky. Ovisacs, in xiv, small and lobed. Spermathecae, adiverticulate (after Gates, 1972c: 314). Type Genus Sparganophilus Benham, 1892 by monotypy (Michaelsen, 1921). Discussion This family is still monotypic and contains but a few nearctic species, only one of which occurs in Canada. Originally, Benham placed the genus in the Rhino- drilidae, a taxon no longer employed by oligochaetologists. Following Michael- sen (1900b), most authors have placed Sparganophilus in various subdivisions of the Glossoscolecidae. In a recent review Brinkhurst and Jamieson (1971) still considered the genus as belonging to the Glossoscolecidae. Genus Sparganophilus (Benham, 1892) 1892 Sparganophilus Benham, Quart. J. Micros. Soc. (n.s.), 34: 155. 1895 Sparganophilus-Smilh, Bull. 111. St. Lab. Nat. Hist. 4(5): 142. 1900 Sparganophilus-Michaeken, Das Tierreich, Oligochaeta 10: 463. 1921 Sparganophilus-Michaehen, Arch. Naturg. 86(A): 141. 1930 Sparganophilus-Slephenson, Oligochaeta (Oxford), p. 899. 1971 Sparganophi lus-Brmkhursl and Jamieson, Aquatic Oligochaeta World, p. 810. 1972 Sparganophilus-Gates, Trans. Amer. Philos. Soc. 62(7): 314. 112 Type Species Sparganophilus tamesis Benham, 1892. Diagnosis Calciferous gland and gizzard, absent. Hearts, in vii-xi. Nephridia, absent in ce- phalic region (segments i-xii). Nephropores, inconspicuous, in AB. Setae, paired. Prostomium zygolobic. Lateral lines, absent. Colour, unpigmented. Sparganophilus eiseni Smith, 1895 American mud worm Ver americain de la vase (Fig. 40) 1895 Sparganophilus eiseni Smith, Bull. 111. St. Lab. Nat. Hist. 4(5): 142. 1906 Sparganophilus eiseni-Moove. Bull. Bur. Fish. 25: 153. 1911 Helodrilus elongatus Friend, Zoologist, ser. 4, 15: 192. 1921 Sparganophilus elongatus-Friend. Ann. Mag. Nat. Hist., ser. 9, 7: 137. 1934 Pelodrilus cuenoti Tetry, C.R. Acad. Sci. Paris 199: 322. 1934 Eiseniella tetrahedra (laps.)-Moon, J. Anim. Ecol. 3: 17. Diagnosis Length 150-200 mm, diameter uniformly about 2.5 mm, segment number 165-225, prostomium zygolobic, dorsal pores absent. Clitellum xv-xxv. Tuber- cula pubertatis xvii-xxii. Setae closely paired, with setae c and d above mL line. Male pores on xix, female pores on xiv. Seminal vesicles, two pairs, in 1 1 and 12 with a pair of testes in 10 and 1 1. Spermathecae, three pairs, in 7, 8, and 9 with ducts opening just ventral to level C in 6/7-8/9. Gizzard, calciferous glands, and tvphlosole absent. Prostate-like glands, four pairs, in 13, 14, 15, and 16. Body cylindrical. Colour, unpigmented but sometimes appearing pink with blue and green iridescence. Biology This species is limicolous and confined to the muddy banks of streams, rivers, ponds, and lakes. Smith (1915) found it to be abundant in the mud of the bot- tom and margins of many waters east of the Mississippi River. Olson (1928) re- ported it along the shores of Lake Erie, and similar habitats are recorded for New York (Lake Ontario) (Olson, 1940), New Jersey (Davies, 1954), Louisiana (Harman. 1965) and Tennessee (Reynolds, MS). S. eiseni is relatively rare in North America except for an area bounded by the Great Lakes, Mississippi River, Atlantic Ocean, and the Gulf States. It is as- sumed to be amphimictic (Reynolds, 1974c). 113 XXVIII Fig. 40 External longitudinal views of Sparganophilus eiseni showing taxonomic characters, a. Dorsolateral view, b Ventrolateral view. (GA: Thomas Co., cat. no. 3285) 114 Range A native of North America. S. eiseni is known also from Central America and has been introduced into England and France (Brinkhurst and Jamieson, 1971; Gates, 1972c). North American Distribution Ontario (Moore. 1906), Alabama (Gales. 1967). Connecticut (Reynolds, 1973c), Florida (Smith. 18%). Illinois (Smith. IS95). Indiana (Heimburger, 1915). Iowa (Hague. 1923), Louisiana (Harman. 1965), Maryland (Reynolds, \^-Xb). Massachusetts (Reynolds, 1977). Michigan (Moore, 1906), New Jersej (Davies, 1954). New, York (Olson. 1940). Ohio (Olson. 1928). Oregon (MacNab and McKey- Fender. 1947). New records: Arkansas, Georgia, Kentucky, Mississippi, North Carolina, Pennsylva- nia, Tennessee. Virginia. Wisconsin. Ontario Distribution (Fig. 41) Sparganophilus eiseni has been previously recorded from only two sites in On- tario (Moore. 1906). BRCCE CO. Howdenvale, 2 metres depth. Lake Huron, airlift sampler, 1 1 Jul 75. DRB, 0-1-0. UW- 0001. HALDIMAND CO. Selkirk Provincial Park, 2 metres depth. Lake Erie, airlift sampler. 5 Aug 75. DRB. 0-1-3. L'W-0001. HALTON CO. Sixteen Mile Creek, intersection of creek and Lower Baseline Road. 1 Jun 71. AT. 0-0-6. ROM. KENT CO. Rondeau Harbour, 30 Aug 99. JPM. 1-1-0. \\SP-41Sa i\loore. 1906). MANITOULIN DIST. 2 metres depth. Georgian Bay, airlift sampler while scuba diving. 17 Aug 74. DRB. 0-0-1. UW-0001. NORFOLK CO. Long Point, 23 Aug 99, JPM, 4-0-0. ANSP-382 (Moore. 1906). PARRY SOUND DIST. Parry Sound, 3 metres depth, in sheltered shallow bay, Ekmann dredge. 18 Aug 75. RLH. 0-0-1, UW-box 1. ^r> Fig. 41 The known Ontario distribution of Sparganophilus eiseni. 115 Distribution and Ecology Even among oligochaetologists the question of megadrile distribution, particu- larly in North America, has long been controversial. Except for the southern tip of Queen Charlotte Island (British Columbia), almost the entire megadrile fauna in Canada is composed of species of the family Lumbricidae that are pri- marily European forms. Of the 19 Ontario species, for example, 18 are lumbri- cids. Two species, Bimastos parvus (Lumbricidae) and Sparganophilus eiseni (Sparganophilidae), are natives of North America. There are 16 currently accepted genera in the family Lumbricidae: Allolobophora, Aporrectodea, Bimastos, Dendrobaena, Dendrodrilus, Eisenia, Ei- seniella, Eiseniona, Eisenoides, Eophila, Helodrilus, Kritodrilus, Lumbricus, Octo- lasion, Octodrilus, and Satchellius. Of these, the genera Eiseniona, Eophila, Helo- drilus, Kritodrilus, Octodrilus, and Satchellius are restricted to Europe and a few adjacent areas, such as North Africa (in the case of Eophila), except that four specimens of Satchellius were recorded in New Jersey. Two genera, Bimastos and Eisenoides, are nearctic but are restricted to the southeastern region of the United States except for two species, Bimastos beddardi and B. panus, which have been carried around the world. B. parvus has been reported from Canada (Reynolds, 1972a), but subsequent investigation (E.L. Bousfield, pers. comm., 1973) nullified this as the only Canadian natural record because the one collec- tion of four clitellate adults came from the Arboretum at the Central Experi- mental Farm, Department of Agriculture, Ottawa. There are five other nearctic megadrile genera: Argilophilus and Diplocardia (Acanthodrilidae), Komarekiona (Komarekionidae), Lutodrilus (Lutodrilidae), and Sparganophilus (Sparganophilidae) (Reynolds, 1976b; Gates, 1977, 1974d, McMahan, 1976). The first four have not been reported from Canada or from any areas north of the southern limit of Quaternary glaciation in the United States. Sparganophilus eiseni has been reported from Canada once (Moore, 1906) but has never been recorded again in Canada until now. This species has also been introduced, probably by man, into Britain and France. There is little disagreement among specialists that the centre of origin of the Lumbricidae is in Europe. Here the family is a very diverse group and the num- ber and variety of species in the genera are greater than anywhere else in the world. There is less agreement, however, as to how those lumbricids became es- tablished in North America, a problem that has been discussed in detail most recently by Gates (1967, 1970) and Omodeo (1963) and reviewed by Reynolds et al. (1974) and Reynolds (1975f, 19760- Assuming that lumbricids have indeed travelled from Europe to North Amer- ica, either they must have migrated actively by their own power, or they must have been transported passively by some agent. Since the Atlantic Ocean now forms an effective barrier to their active migration some workers have hypothes- ized that long ago they arrived in North America by migration via a land- bridge, or were perhaps aided by continental drift (e.g., Omodeo, 1963). Such explanations, however, clearly are inadequate to explain the occurrence of some of the same species in South Africa, Australasia, and South America. Moreover, if such hypotheses are accepted then it is necessary to explain why it should be that of all the North American earthworms only the European lumbricids sur- 116 vived the Quaternary glaciations that otherwise depauperated the North Ameri- can megadrile fauna. In fact Gates (1961. 1^70) and Reynolds (1975f, 19760 have assembled a great deal of data indicating that during the Quaternary all the earthworms of glaciated North America were exterminated and such extermination extended, perhaps, almost as far as the area north of the Appalachian Mountains. Early settlers, for example, found that glaciated portions of the United States and Canada had no earthworms excepting where they were introduced (see Gates, 1967). Consequently, and contrary to the usual belief, surviving species did not follow the retreating glaciers. The earthworm species currently found in regions formerh covered b\ the ice sheets are all introductions, probably by man, either from other continents or from refugia south of the Appalachians. In recording the occurrence of some European lumbricids in South Africa, Australasia, and South America, the efficacy of transportation by man has rarely been ques- tioned and there is no reason why this method of introduction need be denied for the large European element in the North American earthworm fauna. Gates ( 1966) therefore suggested that the colonization of North America by European lumbricids has occurred since 1500 A.D. and was made primarily by European settlers who brought potted plants and other agricultural material with them to the New World. Certainly this hypothesis explains both the diversity of the Eu- ropean element in glaciated North America and the near absence of nearctic en- demics in the same region. The relative merits of the opposing views of Omodeo and Gates have recently been assessed from a theoretical viewpoint by Ball (1975). who concluded that the rival hypotheses were not mutually exclusive, and that on logical grounds it was not possible to prefer one over the other. Our detailed knowledge of megadrile distribution within North America is rather limited and a summary of the North American biogeographical surveys to date is presented in Table 1 . Little work has been done on the ecology and distribution of Canadian earthworms and it is an open field of study. From a study of 14 species from Maine. 13 of which occur also in Ontario, Gates (1961) concluded that dietary preferences might be an important factor influencing distribution. He divided these species into three groups. The first group comprised those species that pass much soil through the intes- tine and hence are termed geophagous, viz., A. chlorotica, Ap. longa, Ap. tubercu- lata, Ap. turgida, E. rosea, L. terrestris, and O. cyaneum. These species are known from soils of pH as low as 4.5-5.5 and the kinds of soil seem to be of little sig- nificance. Within this group only L. terrestris normally and regularly copulates at the surface. Because these species are tolerant of different soil types and oc- cur in a wide range of habitats they are likely to be widely distributed, aided es- pecially by the activities of man. The second group, containing only El. tetraedra, is limiphagous (mud-eating) or hmicolous (mud-inhabiting). Outside of Maine other species such as Sparganophdus eiseni and possibly A. chlorotica belong in this group, the mem- bers of which thrive in mud well under water or in saturated soils. The fact that on a few occasions El. tetraedra has been found to be geophagous suggests an adaptability that would prove advantageous if the animal were introduced to a new area. The third group consisted of the litter feeders: E.foetida, D. octaedra, Dd. ru- in Table 1. Regional earthworm surveys in North America. Region Number of Number of Total References species counties number of obtained sampled counties in state or province Arkansas 21 22 75 Causey (1952, 1953) Cape Breton 14 4 4 Reynolds (1975a) Connecticut 21 8 8 Reynolds (1973c) Delaware 15 3 3 Reynolds (1973a) Gaspe 15 8 8 Reynolds (1975e) Iles-de-la-Madeleine 9 8 10' Reynolds (1975b) Indiana 25 + 92 92 Reynolds (MS) Louisiana 8> 64 64 Tandy (1969) Maryland 26 23 23 Reynolds (1974b) Massachusetts 21 13 14 Reynolds (1976e) Michigan 18 51 83 Murchie(1956) Missouri 21 31 115 Olson (1936) New Brunswick 13 15 15 Reynolds (1976d) New York 18 29 62 Olson (1940). Eaton (1942) Nova Scotia 15 18 18 Reynolds (1976a) Ohio 22 55 88 Olson (1928. 1932) Ontario 18 52 54 Reynolds' Oregon 25 10 36 MacNab and McKev-Fender (1947) Prince Edward Island 12 3 3 Reynolds (1975c) Quebec (sud cote) 15 37 37 Reynolds (1975d. 1976c) Tennessee 44 + « 95 95 Reynolds (1974a, MSS) Washington 16. 9 39 Altman(1936) 'Municipality and iles. 2Tandy was concerned only with the genus Pheretima. Other reports by Gates (1965 and 1967) bring the state list to 25 species. 'Data included in this book. "•Includes species currently in manuscript. bidus, L. castaneus, and L. rubellus. Litter includes all types of accumulation of organic matter such as leaves, manure, compost, etc. The activities of farmers and horticulturists greatly affect the distribution of these forms, and also, of course, of geophagous species that may stray into organic matter. In contrast, prior to hibernation, litter feeders become geophagous when they burrow down to the levels where they hibernate. The extent to which Julin's (1949) ecological classification of the Lumbricidae (p. 5) can be applied to the Ontario earthworms is unknown. Only Reynolds et al. (1974) have attempted to apply the system to a North American fauna. Con- sidering here only those species common to both Tennessee and Ontario, they placed Allolobophora chlorotica, Dendrobaena octaedra, Dendrodrilus rubidus, Eisenia foetida, E. rosea, Eisenielta tetraedra, Lumbricus rubellus, and Octolasion cyaneum among the hemerophiles. The hemerodiaphores included Ap. trape- zoides, Ap. turgida, and O. (yrtaeum, and information was lacking for Ap. longa, Bimastos parvus, and Lumbricus terrestris. There were none that appeared to be true hemerophobes. 118 There is evidence to suggest, how ever, that this classification is not strictly ap- plicable to Ontario. Thus, in Tennessee Ap. tuberculata, E. rosea, and /.. terrestris are sparseh distributed and probabK will become widespread and established only with the aid of human culture, whereas in Ontario these species alread) are widespread in great numbers (Reynolds et al., 1974). For these spec- ies there is a change from the hemerophilic to the hemerodiaphoric category from Tennessee to Ontario. The reverse is the case for Ap. trapezoides and Octolasion tyrtaeum, for these are of restricted distribution in Ontario and wide- spread in Tennessee (Reynolds et al., op. cit.). There is no cause to consider any of the local lumbricids as hemerobionts ex- cept in areas where the natural habitats have been completely destroyed, as in the Sudbury-Copper Cliff region of the Sudbury District of Ontario. Ontario lumbricids. like those of Maine (Gates. 1961). must have become ha- bituated to rather low temperatures. Nothing is known about the state in which winter is spent but. in Maine at least. E. rosea has been found active under leaves surrounded by snow and frost and active specimens of Ap. tuberculata, L. castaneus. D. octaedra and Dd. rubidus, some in breeding condition, have been found in a ridge surrounded with 75-cm deep snow. L. terrestris has been found at night on frozen ground and it seems that melt water from snow and ice is not too cold for many of these lumbricids. Presumably the same holds for the On- tario species, though it is evident that a study of environmental and climatic fac- tors affecting the distribution and activity of the Ontario fauna is greatly need- ed. In determining the presence and distribution of the earthworms in Ontario, 330 new county and district records were established. Ten of these new distribu- tion records were found in the ROM unidentified collections by the author, two came from Carleton University collections, and the remainder were collected by the author. For a detailed breakdown of these records see Table 2 and the On- tario Distribution records for each species. When careful and thorough collection procedures are followed, earthworm species will be found in associations. The size and number of associations ob- tained in this study are reported in Table 3. The maximum number of species found at any one site was eight, while single species, or associations of two or three, were most frequently encountered. Associations vary considerably in size depending on habitat and geography. Reviews of some previously reported habitat associations were presented by Bouche (1969b) and by Reynolds (1972b, 1973d). Since then, another study from one of Bouche's (1969b) stations has been reported (Reynolds, 1972d). This latter report records lumbricid species associations of two, five, and eight for woodlots in north central France. In the previous Ontario study (Reynolds, 1972a), species associations ranged from four with most sites in the single spec- ies and two species association categories. The most common association was Aporrectodea tuberculata — Lumbricus rubellus. Recent lumbricid studies in Ten- nessee (Reynolds et al., 1974) involving almost 1,700 sites and 18,000 specimens, recorded associations most frequently of between three and four species per site with a range of one to eight species. When the remaining families of earthworms have been analyzed these values should increase. The most frequent associations found in this study were: 1) Aporrectodea tuberculata — Aporrectodea turgida — Eisenia rosea, 2) Aporrectodea 119 Table 2. Summary of numbers of new county Distribution Records for Ontario earthworms recorded herein. Species Number of new county records First provincial record A llolobophora chloroiica Aporrectodea icierica Aporrectodea longa Aporrectodea trapezoides Aporrectodea tuberculata Aporrectodea turgida B i mas l os parvus Dendrobaena octaedra Dendrodrilus rubidus Eisenia foetida Eisenia rosea Eiseniella letraedra Lumbricus castaneus Lumbricus festivus Lumbricus rubellus Lumbricus terrestris Oclolasion cyaneum Oclolasion tyrtaeum Sparganophilus eiseni Total 25 0 0 34 41 41 0 9 25 7 39 11 1 7 33 37 1 14 5 330 Stafford (1 902)' Schwert(1977) Smith (1917) Reynolds (1972a) Eisen(1874) Eisen(1874) Reynolds (1972a) Reynolds (1972a) Eisen(1874) Stafford (1902)' Stafford (1902)' Eisen(1874) Eisen(1874) Stafford (1902)' Stafford (1902)' Stafford (1 902) ' Reynolds (1972a) Reynolds (1972a) Moore (1906) 'First reported by Stafford (1902) but he gave no collection details and no locations other than On- tario, Quebec, New Brunswick, and Nova Scotia. tuberculata — Aporrectodea turgida — Lumbricus rubellus, 3) Aporrectodea tuberculata — Lumbricus terrestris, 4) Aporrectodea tuberculata — Aporrectodea turgida, and 5) Aporrectodea tuberculata or Aporrectodea turgida — Dendrodrilus rubidus. Because of the limited diversity of earthworms in Ontario, one should not be surprised at the repetitive nature of the species associations. Even though 19 species have been recorded from Ontario, this does not represent a particu- larly diverse fauna when compared with other political regions of North Amer- ica (Table 1) because the fauna comprises principally exotic European forms; the nearctic endemic species characteristic of more southern regions are absent. Tennessee, for example, has over 44 species known to exist in various habitats within its boundaries (Reynolds et al., 1974). Three of Ontario's 19 species (Apporectodea icterica, Lumbricus castaneus, and L. festivus) are not found in Tennessee, the remainder are. The many species in Tennessee not found in On- tario belong mainly to the nearctic genera Bimastos, Diplocardia, Eisenoides, and Komarekiona. Recent observations by this author (Reynolds, 1973a, 1973b, 1973c, and 1974b) indicate that the habitats utilized by the nearctic species in the southern portions of the United States are those which in Ontario are in- vaded and utilized by exotic European lumbricids. The success of these species in these habitats no doubt is a result of the lack of competition from endemic forms. 120 Table 3. Earthworm associations in Ontario b> counties and districts. Counties and Numb er of Frequency of obtaining he following nurr iber districts collec in cou or disi ions nls of species per collection ricl 1 2 3 4 5 6 7 8 Mgoma 3 0 .33 .33 .33 0 0 0 0 Brant 6 0 .50 .33 0 .17 0 0 0 Bruce 8 .12 .12 .12 .38 .12 0 .12 0 Carieton 5 0 .20 .60 .20 0 0 0 0 Cochrane 3 0 .67 0 0 .33 0 0 0 Dufferin 7 0 .42 .29 0 0 0 0 0 Dundas 7 .14 .57 .29 .29 0 0 0 0 Durham 6 .33 0 .33 0 .17 .17 0 0 1 Igin 8 .12 .25 .12 .25 .12 .12 0 0 \ svC\ 7 .29 .29 .14 .29 0 0 0 0 Frontenac 8 .25 ,25 .38 .12 0 0 0 0 Glengarr\ 4 0 .25 .75 0 0 0 0 0 Grenville 5 0 .40 .40 .20 0 0 0 0 Circs 6 0 0 .83 .17 0 0 0 0 Haldimand 6 .33 0 .17 .33 .17 0 0 0 Haliburton 72 .52 .33 .12 .03 0 0 0 0 Halton 9 .33 .44 0 .11 0 .11 0 0 Hastings 7 .43 .43 .14 0 0 0 0 0 Huron 7 0 0 .57 .29 .14 0 0 0 Kent 6 .33 0 .33 .17 0 .17 0 0 Kenora 1 0 1.00 0 0 0 0 0 0 Lambton 6 .17 .50 .33 0 0 0 0 0 Lanark 5 .20 .20 .40 .20 0 0 0 0 Leeds 7 0 .72 .14 0 .14 0 0 0 Lennox & Addington 5 0 .60 .40 0 0 0 0 0 Manitoulin 6 .17 .17 .17 .50 0 0 0 0 Middlesex 5 .20 .20 .20 .20 0 0 .20 0 \luskoka 9 .56 .44 0 0 0 0 0 0 Niagara 4 0 0 .25 .50 .25 0 0 0 Nipissing 6 .33 0 .50 0 .17 0 0 0 Norfolk 7 .57 .29 0 0 .14 0 0 0 Northumberland 9 .44 .11 .33 .11 0 0 0 0 Ontario 7 .43 .14 0 .29 0 .14 0 0 Oxford 7 .29 .14 .14 .29 .14 0 0 0 Parr\ Sound 11 .45 .45 .10 0 0 0 0 0 Peel' 6 .17 0 .33 .33 .17 0 0 0 Perth 4 0 .50 0 0 .25 0 .25 0 Peterborough 4 .25 25 .25 .25 0 0 0 0 Prescott 5 .20 .60 .20 0 0 0 0 0 Prince Edward 7 .14 .29 .57 0 0 0 0 0 Rentreu 11 .73 .18 .09 0 0 0 0 0 Russell 4 0 .25 .25 .50 0 0 0 0 Simcoe 8 0 .12 .63 .12 .12 0 0 0 Stormont 5 .40 .40 0 20 0 0 0 0 Sudbury 7 72 .14 .14 0 0 0 0 0 Thunder Bay 1 1.00 0 0 0 0 0 0 0 Victoria 7 .14 .14 .43 .29 0 0 0 0 vs.iierloo 10 .10 0 .60 .30 0 0 0 0 Wellington 6 0 .17 .33 .17 .33 0 0 0 Went worth 5 .20 0 .20 .20 0 0 .40 0 York 10 .30 10 .20 ,10 .10 0 .10 .10 Total collections 384 Vwerage frequents .22 .26 .26 .15 .06 .01 .02 .00 of obtaining the number of species per collection Appendix: Provincial Description It is the author's hope that this text will facilitate and stimulate further studies of North American earthworms. Certainly we need to know more concerning their detailed distribution if we are to assess fully their biological importance. For Ontario readers, therefore, a provincial description now follows. This is in- tended to form a basis upon which regional surveys can be made. It is to be hoped that ultimately we will be able to correlate distribution with edaphic and vegetational factors. The provincial description also will serve as a reference point for foreign readers unfamiliar with the Canadian environment. Southern Ontario lies between 42° and 46° N latitude and 75° and 83° W longi- tude (Fig. 1. p. 2) in the St. Lawrence Drainage Basin and primarily in the Plains of the lower Great Lakes and St. Lawrence Lowlands, a physiographic region underlain bv relatively undisturbed Paleozoic sedimentary beds of limestone, shale, and sandstone. The northern portion of southern Ontario (Algoma, Co- chrane. Manitoulin, Nipissing, and Sudbury districts) is underlain by Precam- brian formations in a physiographic region known as the Canadian Shield. All of Ontario has been glaciated. Since 1915, soil surveyors have been at work in Canada, and most of the set- tled area has been mapped on a preliminary scale at least, except for the great unoccupied areas of northern Canada. One should consult Ehrlich (1968) and United States Department of Agriculture (1964, 1967 and 1968) for a detailed explanation of the soil classification schemes used in the following paragraphs and in other megadrile surveys. Southern Ontario contains large expanses of three soil orders — Alfisols, Spo- dosols, and Inceptisols. The Alfisols (Aquic and Ochreptic Hapludalfs), mineral soils, also known as Grey Brown Podzolic soils, are located in two areas: 1) a line through Simcoe. Victoria, Peterborough, Northumberland, and Prince Ed- ward counties and all counties to the west, and 2) a line through Carleton and Leeds counties and all counties to the east. The parent materials either are gla- cial in origin or were deposited in the great bodies of water which occupied the lowlands at the close of the glacial epoch. Under deciduous forests the leaching is not intense. The surface soil (A horizon) is greyish (10YR 4/2-5/2) (Munsell, 1954; USDA, 1951) and slightly acid, and has a moderate amount of organic matter. The B horizon is brown (10YR 5/3, 4/3, 3/2, 2/2) and nut-like in struc- ture because of the accumulation of clay (argillic B horizon). Normally, all lime is leached from the soil profile which may be slightly acid throughout. Generally the soils of this suborder (Udalfs) are reasonably fertile and well suited to culti- vation. The Spodosols appear to be more weathered than the Alfisols. Spodosols are mineral soils with a spodic epipedon and a subsurface horizon with an accumu- lation of organic matter and aluminium oxides + iron oxides. These soils (Spo- dosols: Boralfic Cryorthods, Typic Cryorthods, and Humic Haplorthods) are also known as Bisequa and Orthic Podzolic soils and occupy the major region not included above for the Alfisols. These soils form mostly on coarse-textured, acid parent material subject to ready leaching occurring in humid climates com- 123 monly where it is cold and temperate. Forests are natural cover vegetation. Conifers, low in metallic ion content, seem to encourage the development of Spodosols. As the litter from these low-base species decomposes, a strong acid- ity develops and percolating water leaches acids down into the profile. Since the upper horizons are so intensly leached, Spodosols are not naturally fertile. If properly fertilized, these soils can become quite productive. The inceptisols are young mineral soils whose profiles contain horizons which 1) have formed quickly, 2) result mostly from alteration of parent materials, 3) are free of extreme weathering, and 4) lack accumulation of clay, and iron and aluminium oxides. These Degraded Brown Forest soils (Mollic Alfic Eutro- chrepts) are located mainly on a line from Bruce to Glengarry counties. These soils are generally in forests as agricultural productivity may be limited without considerable expense. These three soil groups make up nearly all of the soils of southern Ontario. But there are other minor areas of note, such as the sands or Orthic Regosols (Entisols: Udipsamments and Udorthents) in portions of Durham, Haliburton, Norfolk, and Victoria counties. Also there are many areas comprised of Histo- sols (Fibrists, Hemists, and Saprists), known previously as Bog and/or Half-bog soils. These organic or bog soils are found covering sizeable areas of Essex, Kent, Lambton, and Simcoe counties. In both cases, these groups (Entisols and Histosols) have in recent decades been converted into areas of productive spe- cialized cropping. Of the 14 major regions of vegetation in Canada, southern Ontario contains part of the Great Lakes-St. Lawrence Forest and all of the Niagara Forest (Rowe, 1972). The Great Lakes-St. Lawrence Forest extends from Lake-of-the- Woods to Baie de Chaleur and is essentially a transition between the boreal coniferous forest and the deciduous forest of eastern North America. The dominant coni- fers are: white pine (Pinus strobus L.), red pine (P. resinosa Ait.), hemlock (Tsuga canadensis (L.) Carr.), and white cedar (Thuja occidentalis L.); others, ap- parently invaders from the north, are: jack pine (Pinus banksiana Lamb.), ta- marack (Larix laricina (Du Roi) K. Koch), balsam fir (Abies balsamea (L.) Mill.) and white spruce (Picea glauca (Moench) Voss). The dominant hardwoods are: sugar maple (Acer saccharum Marsh.), beech (Fagus grandifolia Ehrh.), yellow birch (Betula alleghaniensis Britt.), red oak (Quercus rubra L.), bur oak (Quercus macrocarpa Michx.) and white oak (Quercus alba L.) on upland soils; with red maple (Acer rubrum L.), silver maple (Acer saccharinum L.), elm (Vlmus) and ash (Fraxinus) in the low ground. This forest region has probably more species and a greater number of associates than any other in Canada. The vegetation also includes many smaller plants, shrubs, and herbaceous forms on the forest floor and cleared lands. Some of the more prominent are: ground ivy (Glecoma hederacea L.), juniper (Juniperus virginiana L.), witch-hazel (Hamamelis virginiana L.), sumach (Rhus typhina L.), poison ivy (Rhus radicans L.), service- berry (Amelanchier oblongifolia T. & G.), wild grape (Vitis labrusca L.), hawt- horn (Crataegus foetida Ashe), raspberry and blackberry (Rubus spp.), thimble- berry (Rubus odoratus L.), and honeysuckle (Lonicera (atarica L.). Hawthorns have taken over many thousands of hectares of pasture land, and large areas are occupied by tangles of raspberries and brambles. There are many herbaceous 124 plants on the floor of the deciduous forest, such as may apple (Podophyllum peltatum 1..). herb Robert {Geranium Robertianum L.), Jack-in-the-pulpit (Arisaema triphyllum (L.) Schott), lily-of-the-valley (Maianthemum canadense Desf.). trillium (Trillium grandiflorum (Michx.) Salisb.). and sarsaparilla (Alalia nudicaulis L.). Manv species of aster (Aster spp.) and goldenrod (Solidago spp.), almost unnoticed in the Forest, dominate large areas of unimproved, low pasture land. Dry sites are covered bv mullein (Verbascum thapsus L.) and blueweed (Echium vulgare L). The roadside flora is just as characteristic as that of the for- est. The Niagara Forest is a strip along the northern shore of Lake Erie (Essex, Kent. Lambton. Elgin, Middlesex, Norfolk. Brant. Niagara, Oxford, and Went- worth counties). Much of what was said concerning the composition and ap- pearance of the vegetation of the larger Great Lakes-St. Lawrence Forest also applies to the Niagara Forest. However, there are differences. Except for the pines on the sand plains there are few conifers while, on the other hand, there are additional species of deciduous trees such as: blue ash (Fraxinus quadrangulata Michx.). tulip poplar (Liriodendron tulipifera L.), sassafras (Sassafras albidum (Nutt.) Nees), magnolia (Magnolia acuminata L.), Kentucky coffee tree (Gvmnocladus dioica (L.) K. Koch), sycamore (Plantanus occidentalis L.). black walnut (Juglans nigra L.), pawpaw (Asimina triloba (L.) Dunal), and others. This area is also the habitat of many small plants not found farther north. There are large areas of cultivated land in southern Ontario. Prior to Euro- pean settlement there were no forages and few natural meadows. The natural meadows were assigned to settlers on a livestock number basis. The lack of feed made it necessary to seed and cultivate meadows for wintering cattle. Most of the forages are of European origin. Recent values for areas of cultivated land in Ontario are: seeded pasturages 1.35 million hectares, rough pasture >1.30 mil- lion hectares, and small grains slightly >2 million hectares. One of the most popular grasses in pasture mixtures is timothy (Phleum pratense L.), which is used on 75-80% of Ontario farms. Other prominent pas- ture species are: orchard grass (Dactylis glomerata L.), brome grass (Bromus in- ermis Leyss.), tall fescue (Festuca elatior L.), reed canary grass (Phalaris arundinacea L.). Kentucky bluegrass (Poa pratense L.), Canada bluegrass (Poa compressa L.), red fescue (Festuca rubra L.), perennial ryegrass {Lolium perenne L.), alfalfa (Medicago sativa L.), red clover (Trifolium pratense L.), white clover (Trifolium repens L.). and birdsfoot trefoil (Lotus corniculatus L.). Various com- binations of these species are found in Ontario depending on the soil type, an- nual precipitation, physiographic position, and topography of the pasture, etc. For example. Canada bluegrass is well adapted to drier areas while Kentucky bluegrass can only be sown in moist areas. The major small grains sown in Ontario are: oats (Avena sativa L.), barley (Hordcum vulgare L.), wheat (Triticum spp.), rye (Secale cereale L.), sorghum (Sorghum vulgare Pers.). and very limited areas of rice (Oryza sativa L.). The climate of Ontario, according to the Koppen system (Pettersen, 1968), is in the cool snow-forest climatic type (D/b) with warm summers and the absence of a dry season. The Holdridge system (Sawyer and Lindsay, 1964) places the province in the cool temperate moist forest bioclimatic formation. Utilizing the 125 Thornthwaite (1948) classification of climate for Ontario, the province is char- acterized in the following manner: 1. Moisture Regions — Climatic Type (moisture deficiency surplus index): B, Humid (20-40) — south and west of a line through Huron and Wentworth counties, southern Kenora and Rainy River districts. B: Humid (40-60) — the rest of southern Ontario. 2. Seasonal Variation of Effective Moisture: r (little or no water deficiency in any season) — all of southern Ontario. 3. Average Annual Thermal Efficiency — Thermal Efficiency Type (TE index, in inches): B1, or Mesothermal (22.44-28.05) — south and west of a line through Huron and Wentworth counties. C2 or Microthermal (16.83-22.44) — the rest of southern Ontario. 4. Summer Concentration of Thermal Efficiency — Thermal Efficiency Type (%): b': (56.3-61.6) — south and west of a line through Huron and Went- worth counties, b', (61.6-68.0) — the rest of southern Ontario. The mean annual precipitation for southern Ontario ranges from 711 mm (Essex and Niagara counties and Manitoulin District) increasing eastward to 916 mm (Prescott County). The mean January air temperature is -1 to -7° C (maximum) and -12 and -18 °C (minimum) while the mean-July air tempera- ture is 24 to 27 °C (maximum) and 10 to 16 °C (minimum). For further details, see Brown et al. 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