AH | | UU AS Ha {i | i HAAN | | | | | é htehtoo TOEO O ~ OVUM UA IOHM/18lN oS <. 4 | | t r : f 4 i THE ANATOMY OF WOODY PLANTS THE UNIVERSITY OF CHICAGO PRESS CHICAGO, ILLINOIS THE BAKER & TAYLOR COMPANY 2 NEW YORK THE J. K. GILL COMPANY PORTLAND THE CUNNINGHAM, CURTISS & WELCH COMPANY LOS ANGELES THE CAMBRIDGE UNIVERSITY PRESS LONDON AND EDINBURGH THE MARUZEN-KABUSHIKI-KAISHA TOKYO, OSAKA, KYOTO, FUKUOKA, SENDAI THE MISSION BOOK COMPANY SHANGHAI Diagrammatic figure of the French artichoke, Cynara Scolymus, showing distri- bution of oil canals in the various organs and regions. For explanation see chapter xxxi. THE ANATOMY OF WOODY PLANTS By EDWARD CHARLES JEFFREY THE UNIVERSITY OF CHICAGO PRESS CHICAGO, ILLINOIS CopyRIGHT 1917 By EpDWARD CHARLES JEFFREY All Rights Reserved Published October 1917 12 546 Composed and Printed By The University of Chicago Press Chicago, Illinois, U.S.A. PREFACE It is now forty years since De Bary’s classic Comparative Anatomy of the Vegetative Organs of the Phanerogams and Ferns made its appearance. In the interval much has been added to our knowledge, particularly in the paleobotanical and experimental . fields. The doctrine of descent, too, has now reached a degree of prominence and importance which it did not possess in De Bary’s time. As a consequence, it is desirable that the general subject of the anatomy of the woody or so-called vascular plants should be reviewed, with special reference to its historical and experi- mental aspects. This is perhaps all the more desirable as an effective counterpoise to the extreme mechanistic tendencies of the time. It will accordingly serve a useful purpose to indicate how large a part of the organization of existing plants is an inherit- ance from their ancestors of earlier geological times. In De Bary’s textbook both paleobotany and development are deliberately eschewed. The first of these is now essential for any adequate comprehension of comparative anatomy in its all-important evolutionary aspects. It is abundantly clear that the most fruitful results from the standpoint of the doctrine of descent are to be derived from the comparative study of extinct and existing plants belonging to the same orders, families, or genera. It is, moreover, obvious that the living forms cannot be interpreted without a knowledge of their past, and that to an even greater degree the organization of fossil plants is a closed book to those who are unfamiliar with the anatomy of allied and still living types. The wide range of facts which must of necessity be covered calls for a somewhat brief and even elementary treat- ment. Fortunately, since De Bary’s time, it has become more and more evident that the study of the development of organs and tissues throws little trustworthy light on the processes of evolution, and consequently that aspect of our subject need receive no more attention than was vouchsafed to it by the great German anatomist nearly half a century ago. Vv vi PREFACE In the seventeenth chapter are summarized the important general principles derived from the investigation of related living and extinct organisms. The beginning of the studies leading to the formulation of these anatomical canons stands largely to the credit of French and English paleobotanists. Since they have worked mainly with Paleozoic types, their activities have been preponderantly in the direction of comparisons between the organization of the earlier cryptogams and gymnosperms and their still living survivors. It has been in some measure the good fortune of American anatomists to continue the lines of investigation thus begun and to extend them to the study of Mesozoic and still living gymnosperms. The extremely harmoni- ous conclusions resulting from the anatomical comparison of both Paleozoic and Mesozoic forms with their surviving descendants have justified the extension of the same principles to the evolu- tionary investigation of other woody plants (particularly to the angiosperms), concerning the geological past of which we are still ignorant. The canons formulated in chapter xvii have as a conse- quence been regarded of such importance that any conclusions not in harmony with them have ordinarily not been considered in the following pages unless they have held the ground for many years or are at the present time advocated by anatomists of great emi- nence. On account of the large field covered in the present neces- sarily elementary work, this procedure has been regarded as essential, and it is hoped that, with the explanation offered, it will not appear to the reader too dogmatic. The author has been fortunate in utilizing the services of his students in the preparation and illustration of this volume. He is particularly indebted to Mr. R. E. Torrey for his skilful and artistic execution of a large number of the figures. Help in this respect has also been supplied by Mr. R. C. Staebner and Mr. Charles Drechsler. Miss Ruth Cole has rendered invaluable aid in the onerous task of preparing the text and reading the proof. Miss Edith S. Whitaker has also assisted in the prepa- ration of the index. To Professor M. A. Chrysler, of the University of Maine, the author owes illustrations of secondary growth in monocotyledons, PREFACE vii and to Miss Eloise Gerry, of the United States Forest Service, an admirable photograph elucidating the ‘‘bars of Sanio” in coniferous wood. Last but not least, the author records the valuable services of Mr. James Austin, assistant in the labora- tories, in connection with the preparation of the numerous photo- graphic illustrations. Dr. D. H. Scott and his publishers, Messrs. A. and C. Black, have very kindly permitted the reproduction of a number of figures from the admirable Studies in Fossil Botany, which are among the comparatively few illustrations in the present work which are not original. To Dr. R. T. Jackson the author is indebted for the opportunity of photographing for illustration a number of the sections of carboniferous plants under his care in the Botanical Museum. Professor John M. Coulter has been good enough to read the proofs as the present volume passed through the press. To my friend Mr. R. W. Sayles, Director of the Geological Museum, I am indebted for valuable criticisms in the field of paleoclimatology and also for other essential aid. The author is alone responsible for the views expressed and for any errors. BoTANICAL LABORATORIES, HARVARD UNIVERSITY June, 1917 CONTENTS CHAPTER Shar (CErp . THE TISSUE SYSTEMS . . THE FIBROVASCULAR TISSUES: WooD—GENERAL . THE FIBROVASCULAR TISSUES: SECONDARY Woop—TRA- CHEIDS AND FIBERS . . THE FIBROVASCULAR TISSUES: SECONDARY Woop—PAREN- CHYMA . THE FIBROVASCULAR TISSUES: SECONDARY Woop—Rays . . THE FIBROVASCULAR TISSUES: SECONDARY WOOD—VESSELS . THE FIBROVASCULAR TISSUES: PHLOEM . THE EPIDERMIS . THE FUNDAMENTAL TISSUES . . DEFINITIONS OF THE ORGANS . THE Root . THE STEM . THE LEAF . THE MICROSPORANGIUM . THE MEGASPORANGIUM AND SEED . THE CANONS OF COMPARATIVE ANATOMY . THe LycopsipA AND PTEROPSIDA . THE LYCOPODIALES . THE EQumsETALES (INCLUDING SPHENOPHYLLALES) . THE FILICALES . . THE ARCHIGYMNOSPERMAE: CYCADOFILICALES AND CyCa- DALES . Toe ARCHIGYMNOSPERMAE: CORDAITALES AND GINKGOALES . THe METAGYMNOSPERMAE: CONIFERALES . Tue METAGYMNOSPERMAE: GNETALES . . THE ANGIOSPERMS . PAGE 2.4 CONTENTS CHAPTER XXVII. THE Woopy DIcoTyLEDONS XXVIII. THE HerBAceous DICOTYLEDONS XXIX. THE MoNOCOTYLEDONS XXX. ANATOMICAL STRUCTURE AND CLIMATIC EVOLUTION XXXTI. EvoLurIONARY PRINCIPLES EXHIBITED BY THE COMPOSITAE XXXII. ANATOMICAL TECHNIQUE INDEX PAGE 379 387 409 417 433 444 473 CHAPTER I THE CELL It has been recognized since the seventeenth century that living beings, particularly plants, are composed of cells. The English investigators Hooke and Grew in the latter half of that century noted the fact that the body of vegetable organisms was often con- stituted of minute chambers, and to these Hooke first gave the name of cells. Grew was apparently the originator of the term ‘tissue,’ and he compared the organization of plants with the woven texture of lace. A clear conception of the cellular structure of living beings was not, however, reached until nearly two centu- ries later. Plants differ from animals in the fact that their gross internal organization is of relatively slight scientific importance compared with the more obvious bony and muscular structures of the animal body. The anatomy of plants is thus essentially a matter for microscopic investigation. Some knowledge of the general features of the structure of the cell in plants is accordingly necessary as a preliminary to the more detailed pursuit of anatomy. The cell in vascular plants has certain features which bring it into sharp contrast with the corresponding unit of structure in the higher animals. The essential substance of all living cells is proto- plasm, simply distinguished from inanimate matter by the posses- sion of a capacity for change and reproduction, which does not characterize matter devoid of life. In the higher plants the proto- plasm does not show the large degree of solidity which is a feature of the animal cell, but is ordinarily reduced to a thin vesicle sur- rounding a larger or smaller central cavity known as the vacuole. The bladder-like protoplasmic vesicle is rendered possible in plants by a containing, supporting, and likewise more resistant envelope called the cell wall. This wall is not nitrogenous in its chemical composition, as is true of the living protoplasmic body, but is, primi- tively at least, a ternary compound, containing carbon, oxygen, and hydrogen, the first-named element being the most abundant. I 2 THE ANATOMY OF WOODY PLANTS Fig. 1 will make clear the organization of cells in an immature seed pod or pericarp of an iris. Each element obviously consists of a large central cavity as noted above, variously known as hydro- plastid, hydroleucite, tonoplast, and vacuole. The last designa- tion seems best for descriptive purposes. Surrounding the median space, which in life contains water with various substances in solution, is the proto- plasmic utricle. The nature of the latter varies in different cells. In the ele- ments to the left side of the illustration the protoplasm appears as a somewhat minutely granular substance, while in the cells to the right the structural organi- zation of the proto- plasm is marked by the presence of oval bodies, the chloro- plastids, which in life color are green. A Fic. 1.—Transverse section of young pericarp of Tris species, showing organization of cells of epidermal and fundamental tissues. dark body of larger size is to be seen somewhere against the cell wall and imbedded in the protoplasm. This is the nucleus, one of the most important organs of the cell, which appears to preside over all its changes and activities. Another body, generally larger and lighter than the nucleus, is frequently present in the cells under discussion—the oilplastid or eleoplast. This is conspicuously spongy in its structure. We may now turn with advantage to the organization of the cell wall. On the left side of the illustration the common outer wall is limited by a distinct membrane, the cuticle, which is chemically different from the rest of the wall substance and is viable to THE CELL 3 gases but not to fluids. Below the cuticle lies the cell wall proper, in this case composed of cellulose. The cuticle and its underlying wall are continuous except in the region of certain apertures, the stomata, one of which is represented in the figure. From the stoma there passes inward an air space, which quickly divides into fine canals lying in the angles between the internal cells. These are intercellular spaces and are a practically unfailing accompaniment of the living elements in vascular plants. The next illustration (Fig. 2) visualizes the conditions in a harder tissue, namely, one of the wood rays of a dicotyledon. Here the mass of cells present individually somewhat rounded contours, and in the result- ing angular interstices appear the intercellular spaces. The protoplasm in the cells under consideration is much denser than in the elements of the wall of the ovary figured above, Bree aential seeriantat and accordingly the nucleus lies near cells of a ray in a dicotyledon the geometrical center of the cell, as (Primys species), showing pitting é : : in relation to cells and intercellu- is commonly the case in highly proto- ,,. . ee plasmic elements, in contrast to its ‘peripheral position in those in which the protoplasm is only a bounding utricle. The cell wall in the present instance is, rela- tively to the size of the cells, much thicker than in the first figure. As a consequence of this increased thickness of the wall, special devices are necessary for the purpose of permitting interchanges between the cellular elements and their environment. The wall is thin in certain definite regions for the attainment of this end, and these locally thin spots are known as pits. It is clear that the pit of one cell always coincides with a corresponding pit in a neighbor- ing element. Further, it is obvious that, although the cells are in close relation to one another by means of their pits, these are prevented from becoming actual holes by the persistence of the middle lamella or cement substance as the membrane of the pits. Not all the pits, however, meet a corresponding depression. It 4 THE ANATOMY OF WOODY PLANTS will be observed that there are well-developed pits toward the inter- cellular aérating spaces. These are known as air pits and have no counterpart on the side of the air space. They are commonly found wherever the thickening of the cell wall makes difficult the interchanges between the living protoplasm and the outside air. In the figure under consideration the cells are united by the cement substance of the middle lamella, which appears dark and contains the air spaces within its sub- stance. Most of the cells have had both the top and the bottom walls removed Sent ! by the plane of section, but = oie cs De in one or two the cell wall Z meets the eye. Here the pits are seen in face view, and it becomes clear that they vary somewhat in size and are characteristically outlined by a single contour. On account of this condi- Fic. 3.—Section of inner pericarp tion, which results from the (“stone”) of a peach, showing cells with ex- fact that the bounding walls tremely thick and layered walls as well as do not overhang, pits of this numerous elongated pits. 5 5 type are called simple pits. Communicating pores of this kind are found in cells which in their functional condition contain living protoplasm. Let us now turn to the examination of cells in which the wall is so greatly thickened that the space containing the protoplasmic body becomes much reduced in size. Fig. 3 reproduces some of the elements of a peach stone which has been softened by a pro- longed sojourn in hydrofluoric acid. The protoplasmic structures have been largely consumed in the thickening of the cell wall. The latter shows well-marked indications of layering, a feature often present when much thickening has taken place. The layer- ing doubtless has some numerical relation to the age of the wall in days. The pits are of special interest in this instance. Their correspondence in adjacent cells is as marked as in the former THE CELL E illustration. In many cases two or more near-lying pits of the same cellular element become confluent as they pass inward, and open into the cavity of the cell by a common aperture. The cement — Fic. 4.—Wood of the spruce (Picea canadensis), showing ray cells with simple pits and longitudinal water-conducting elements with bordered pits. substance is strongly developed here and the thickened walls of the cells are lignified. The pits, in spite of the complications noted above, are to be regarded as simple pits. 6 THE ANATOMY OF WOODY PLANTS The examples of cells hitherto considered have been those which in their functional condition contain living protoplasm. It is now necessary to refer to those very important histological elements of vascular plants, which in the mature condition normally con- tain no protoplasm and serve to conduct water. Elements of this nature are typically much elongated and are provided with a different sort of intercommunicating pitting than that found in the case of those which in the active state shelter a protoplasmic body. In the accompanying figure (Fig. 4) are seen a number of cells of this sort cemented together by the middle lamella (repre- sented as a black framework around the cell walls). The pits which bring about intercommunication are figured as occurring on two of G) ©) the four nearly parallel sides of the tracheids or water-conducting cells. Their openings have overhanging margins, and the membrane, the Fic. 5.—Diagram of simple and Presence of which precludes the bordered pits in face and profile views. possibility of actual openings, is In the center a bordered pit from much thickened in the middle to heartwood is shown. : constitute the so-called torus. The presence of overhanging margins clearly distinguishes this type of pore from that found in the walls of living cells. The cement substance uniting the cells with one another is in general lignified (that is, has undergone that somewhat complex and obscure modification chemically known as lignification) like the cell walls which it holds together, but is likewise partially in the pectic or mucilaginous condition, a state which causes it to absorb hema- toxylin strongly. In the region of the pit membranes the middle lamella becomes pectic cellulose, and here water passes through the walls much more readily than it does elsewhere. On either side of the figure is seen a ray of the wood, the cells of which are in relation with the tracheids by means of pits. It is clear that the pits which bring about intercommunication are bordered on the side of the elongated element of the wood (the tracheid) and are THE CELL 7 simple on the side of the medullary-ray cells. Pits of this nature are called half-bordered. In Fig. 5 simple and bordered pits are represented diagram- matically side by side and from both profile and face view. Ob- viously the simple pits in face view are single in contour, while those which are bordered have a triple concentric outline, the outer- most circle corresponding to the boundary of the broad membrane of the pit, the innermost to the narrow mouth, and the intermediate representing the outline of the torus. The distinction between simple and bordered pits is an extremely important one, particularly in the lower groups of vascular plants. In higher forms the dis- tinction is of less value, but the presence of bordered pores in vas- cular elements in general still indicates that an important function of the element so provided is the transport of water. It should be further noted that elements with bordered pits are usually without intercellular spaces, while those in which the pits are of the simple type normally possess such aérating cavities. Exceptions to this statement are found ordinarily only in plants which have become highly specialized in connection with resistance to drought. CHAPTER II THE TISSUE SYSTEMS The cells in higher plants are generally grouped into well-marked systems of elements which are known as the tissues. ‘Tissues are sometimes defined as aggregations of cells performing a similar function. This definition is, however, open to some objections, as is also that which describes a tissue as a mass of cells of similar origin. Characterization of tissues, either by their functions or by their mode of origin, seems less desirable than a definition which makes clear that the aggregations of cells have a common organiza- tion. From the standpoint of evolution it is the structural features of the tissues which are of the greatest significance. In works dealing with so-called physiological plant anatomy the functions of the tissues rather than their peculiarities of structure are naturally most emphasized. From the point of view of the doc- trine of descent functional features are of less significance, since it is precisely these which are the most readily modified and as a consequence furnish the least valuable indications of the course of evolutionary development in any given large group. Because the present work deals with anatomy from the outlook of evolution, structural organization in the case of the tissues stands in the fore- ground, although, of course, the question of the functioning of the various tissue systems cannot be left out of view. It is an interesting general fact that the boundaries between the tissue systems are much more marked in the plants which are geologically older and lower in the scale of evolution than they are in the higher seed plants, the conifers, and the angiosperms. Further, the more conservative organs of the higher forms—namely, the root and leaf—exemplify a sharper delimitation of the tissue systems than does that most progressive of all plant parts, the stem. For the purpose of the present work the tissues of plants may be divided into three distinct systems, which can be most easily identified by reference to the accompanying figure (Fig. 6) of a 8 THE TISSUE SYSTEMS 9 transverse section of the creeping stem of Pteris aquilina. 'Through- out the area of the figure are scattered oval masses, the fibrovas- cular bundles. These are very sharply marked off from the rest of the tissues by a boundary appearing as a dark circumscribing line. On the outside of the stem is the integumentary system, or Fic. 6.—Transverse section of the rootstock of Pteris aquilina, showing three categories of tissue—namely, epidermal (external), vascular, and fundamental. epidermal tissue, consisting of a single layer of cells. The epidermis is characteristically uniseriate in the lower forms, and only in some of the higher vascular plants does it become a multiple layer. The remaining structures of the stem of the bracken fern belong to the fundamental system. The next illustration (Fig. 7) shows a part of the stem of Pteris more highly magnified, so that the details of fe) THE ANATOMY OF WOODY PLANTS structure may be more easily discerned. External is the single layer of the epidermis, made up of cells with thick, heavily pitted walls. With the greater magnification employed, the cellular organization becomes very obvious. Underneath the epidermal layer is situated the fundamental system, in turn clearly outlined against the fibrovascular tissues by a striking boundary composed of a single series of cells with dark tanniniferous contents. This is the most internal layer of the fundamental system and is known either as the endodermis or as the phloeoterma (the latter term in its ety- mology indicating the inner layer of the cortex or fundamental tissue). The fundamental tissues are characterized locally by Fic. 7.—A portion of a transverse section of the rootstock of Pieris aquilina more highly magnified, showing the three tissue systems. certain bands of dark-brown skeletal tissue, which are very char- acteristic of the lower vascular plants and subserve to a large extent the mechanical function which in the higher plants is attended to by the fibrovascular system. Those regions of the fundamental system which are not mechanical in their nature take over the function of storage and are crowded with granules of starch forming a cordon around the periphery of the cells. Centrally the elements of storage show the presence of a dark-brown substance in the region of the vacuole. This is tannin-like in its nature and is commonly present in the fundamental system of ferns. The fibrovascular structures stand out sharply from the rest of the tissues and are obviously much more complicated in their organiza- tion than are those previously considered. The fibrovascular aggre- gations of cells are of the greatest anatomical importance, both because their very complexity of structure supplies many valuable THE TISSUE SYSTEMS II features for comparison which may be utilized in the study of evolution, and because their conservatism makes them on the whole the least variable of the elements entering into the composition of the higher plants. Likewise, by reason of their resistance to decay, they are more likely to be preserved as fossils. Beyond emphasiz- ing the complexity of the fibrovascular system, it need not be further considered at the present time. a Fic. 8.—Transverse section of the leaf of the white pine (Pinus Strobus), showing the three tissue systems in a leaf. We may next consider the tissue arrangements in another of the plant organs, namely, the leaf. In the figure (Fig. 8) is repre- sented the transverse section of the needle of Pinus strobus. Ex- ternally the epidermis forms a boundary of a single row of cells, continuous except where interrupted by the occurrence of stomatic openings. Beneath the epidermis lies a layer which is ordinarily known as the hypoderma and is more strongly developed in fossil 12 THE ANATOMY OF WOODY PLANTS than in living pines. The fibrovascular strand is sharply bounded in the median region by the endodermis, a layer circular in con- figuration and well developed in Pinus, though often absent in the higher conifers. The organization of the fibrovascular strand need not particularly occupy our attention at this stage, as it will be considered in detail more appropriately in the sequel. It is enough to note that its upper or woody part is composed of empty cells often showing bordered pits—in other words, of tracheids. These are continuous on the flanks of the strand with short-pitted elements, the transfusion cells, which are of great interest from the evolutionary standpoint. The cellular complex lying outside the endodermis and within the epidermis is the mesophyll, the repre- sentative of the funda- mental tissues in the leaf. The cells of the mesophyll are infolded in a manner Fic. 9.—Transverse section of the root of characteristic of most the sarsaparilla (Smilax), showing the three livin g pines In the meso- systems of tissues in root organs. phyll if also, athe lower side of the leaf, conspicuous secretory spaces, the resin canals. In the root of the pine, as in the leaf, the same sharp distinction between the fibrovascular structures and the fundamental tissues is present. In the stem of the conifers generally, however, the limit between the tissues belonging to the central conducting cylinder (the fibrovascular system) has become obsolete and can be judged to have been formerly present only on theoretical grounds. In the case of the root of vascular plants in general, from the lowest to the highest, the limit between conducting or fibrovascular tissues and the fundamental system is usually very distinct and is one of the features which so clearly and universally mark the root as the most conservative of the organs of plants. Fig. g illustrates THE TISSUE SYSTEMS 13 the situation in this respect for the monocotyledons, which may on strong grounds be considered as the highest of the seed plants. Externally is the piliferous layer, from which the root hairs are derived, and which may be considered in a general way as the equiva- lent of the epidermis of the stem and the leaf. The central region is occupied by the fibrovascular system, sharply limited by the endodermis, composed of cells ordinarily thick-walled. Between the endodermal limiting membrane and the piliferous layer lies the cortex of the root, and this corresponds to the fundamental category of tissues in the case of the stem and leaf. It will be clear from the account given above that there are three tissue systems in plants which are very distinct in lower forms and in the less changeable and more conservative parts. Of these the epidermal tissues are always clearly limited both toward the out- side and also in relation to the tissue system which lies inside. The boundaries dividing the fibrovascular from the fundamental tissues are often less plainly indicated, and in the case of the higher groups of plants, particularly those in which the secondary growth is strongly developed, may disappear altogether; in such cases the limits of the tissues can only be inferred from comparative and developmental anatomy. CHAPTER III THE FIBROVASCULAR TISSUES: WOOD—GENERAL Since the fibrovascular tissues are on the whole the most impor- tant in the organization of the higher plants both from the evolu- tionary and from the physiological standpoint, it will be well to begin with their anatomy. The most conspicuous and _best- developed portion of the fibrovascular system in land plants is the wood. The aggregation of elements assembled under this heading affords also the best exemplification of the process of evolution in the higher plants as the result of the progressive development of the principle of division of labor and the gradual adaptations of plants to the more complicated conditions of life obtaining in later geological times. The resistance of the wood to the organisms of decay is greater than that of any other common plant tissue except those possessing cutinized or suberized cell walls. We have, consequently, in the woody structures past and present an almost perfect biological document, carrying back the history of plants in relation to their changing conditions of environment into remote epochs of our earth’s history. In beginning the discussion of the organization of wood it will be well to direct our attention in the first instance to the contrasts in structure presented by woods of ancient and modern types. The first illustration (Fig. 10) shows us the situation in the oak. The wood is conspicuously marked into areas by boundaries running at right angles. Crossing the figure from top to bottom are rows of large openings which represent the vessels or water-conducting tubes of our modern forest trees. It is clear that these are large only along the lines which mark the beginning of each year’s growth. Farther out the vessels become suddenly of much smaller caliber. Not only is the ligneous structure of the oak transversely banded by reason of the strikingly larger size of the vessels which signalize the spring development, but also by an equally significant change in the diameter and the distribution of other more or less highly 14 FIBROVASCULAR TISSUES: WOOD 15 differentiated elements, to be described in a later chapter. At right angles to the annual zones of growth and crossing these are the large wood rays. These are extremely conspicuous structures, and as a result of a variation in the rate of growth due to their presence they bring about very evident depressions on the faces of the annual rings. The intervals between the large wood rays are occupied by more numerous linear stor- age bands, which are but a single row of cells in thickness and are known as uniseri- ate rays. A marked con- trast to the wood of the oak is presented ! by the ligneous organization of the Paleozoic gymno- sperm Cordaites, illus- iiabed Ane hie. Ta. Here the annual rings, so clearly pres- Tic. 1o.—Transverse section of the wood of the red ent in the oak as qa ak (Quercus rubra), showing annual rings and highly differentiated structure which characterizes the organiza- tion of the woody cylinder in modern trees. result of a differentia- tion in the size and character of the elements corresponding to regularly recurring annual changes, are conspicuous by their absence. ‘This situation is directly correlated with the more equable annual cycle of remote geological times. We find illustrated in the case of Cordaites abso- lutely no indication of seasonal changes in temperature or varia- tions in other important conditions of a periodic or seasonal nature. Not only is the wood monotonously the same as one passes from the inner regions to the exterior layers, but it likewise shows slight differentiation in the direction from left to right. Large rays of the oak type are quite absent, and the radial storage strands are entirely linear in their nature. 16 THE ANATOMY OF WOODY PLANTS Having noted the varieties involved in wood structure in correla- tion to the more variable conditions of environment present in modern times, we may now with advantage direct our attention to other features of organization which characterize the evolution of the woody cylinder in the higher plants. Fig. 12 illustrates the transverse section of the wood of a lepidodendrid, an ancient tree of the Paleozoic age. It as clearcin this case that the wood has a circular outline correspond- ing to that of the stem as a _ whole. Although there is no indication of the ex- istence of annual inienements, OF growth, the wood is obviously divided into a central mass, in which the cells are irregularly dis- posed, surrounded by a zone regularly Fic. 11.—Wood of a Paleozoic gymnosperm from Prince Edward Island, Canada, showing absence of ? annual rings and extremely simple organization. seriate and marked by the presence of wood rays. The portion of the wood which shows no linear disposi- tion of its elements is known as the primary wood. This region of the wood is sometimes designated the ‘‘cryptogamic”’ or “‘old”’ wood, because it is particularly characteristic of the organization of vascular cryptogams and of the older groups of plants generally. As will be made clear later, the structure and mode of development of wood of this category is of considerable importance from the evolutionary point of view. The zone of secondary wood, outside the primary or cryptogamic ligneous core, is conspicuous by reason of its regular radial seriation and the presence of storage bands FIBROVASCULAR TISSUES: WOOD 17 called wood rays. The secondary wood need not further occupy us in the present chapter. Turning our attention now to the longitudinal organization of the primary wood, we find it characterized by the presence of certain elements appearing in a somewhat regular sequence. The general situation is represented in Fig. 13. On the left of the diagrammatic illustration lies an elon- gated thin-walled cell marked by the presence of spiral strengthening bands. In its present state this element is de- void of protoplasmic sub- stance, but in an earlier phase, as indicated in the next figure (Fig. 14), liv- ing matter was present and specially aggregated in the regions of the thickened spiral bands. To the right lies a second element in which the strengthening horizontal ridges, which reinforce {b-= Fic. 12.—Transverse séction of a stem of a from the inside the gen- _lepidodendrid trunk from the Paleozoic (after erally thin walls of the Scott), showing the strong distinction between secondary (radially seriate) and primary (unsert ate) xylem characteristic of ancient forms. water-conducting cell, are nearer to one another and in some instances are more or less united. By accentuation of the condition of approximation, fusion between the bands results and we have as a consequence the presence of the scalariform or reticu- late tracheid. In general, among the Pteridophyta this is the extreme stage of evolution of the tracheary cells of the primary wood, but occasionally among the more complicated and extinct vascular cryptogams, and characteristically in all seed plants, the final state of the primary wood is characterized by the presence of 18 THE ANATOMY OF WOODY PLANTS the pitted element, marking a distinct advance on the scalariform and reticulate tracheids of the primary ligneous organization of the ferns and their allies. In the case of the primary wood those elements which have in their walls thickenings of the nature of rings and spirals are ordinarily designated the protoxylem. This Fic. 13.—Diagrammatic longitudinal section of the fibrovascular tissues of a dicotyledon (after Sachs), showing organization of primary wood. characterization of the first-formed portion of the primary wood is not always justified by the structures present, because in slowly growing organs and in subterranean parts even of rapid development typical ringed and spiral elements Fic. 14.—Dia- may be nearly or quite absent. Usually, how- 8’ 23s#Be views p i I oa heal of a young ele- ever, the protoxylem as defined is the ligneous em a) foe See structure present when the organ is undergoing ~=mary wood. In A rapid elongation and by its constitution permits the normal condi- - : ; : tion is shown, of accommodation by stretching to correspond a é : ph ae while in B the pro- with the increase in length. Its elements as a toplasm has been consequence are frequently drawn out and almost _ caused to contract obliterated. The cells of the primary wood laa ofrples: . : : : a molysis. which are thickened in the reticulate, scalari- form, or pitted manner are formed after elongation has ceased, since by their organization they are incapable of increasing their FIBROVASCULAR TISSUES: WOOD 19 length. Elements in the aggregation belonging to this category are known as the metaxylem or, more specifically, as the primary metaxylem. In the preceding paragraph, for the sake of convenience it has been assumed that the order of development of the primary wood is always in the same direction. As a matter of fact the time and the order of appear- ance of the elements in this, from the evolutionary stand- point, highly signifi- cant tissue vary within certain im- portant limits. We may first consider the most ancient order of seriation of the constituents of the primary wood— that found in the stems of the most antique plants and in the roots of all Fic. 15.—Transverse section of the upright stem of vascular organisms Lycopodium clavatum, showing centripetal or centrad development of the primary wood; the smaller elements represent the protoxylem. from the lowest to the highest. Fig. 15 illustrates the organization of the wood in a stem of the common club moss, Lycopodium. The tissues of the xylem constitute a sort of star, the points of which are occupied by the small-sized elements of the protoxylem. As the rays of the star broaden inwardly, there is a transition from protoxylem tometaxylem. The situation becomes more clear by reference to transverse sections of the root in a fern shown in Fig. 16a. Spiral sculpture marks the small elements on the outside, while toward the center of the organ the typical sculp- ture of the metaxylem becomes more and more conspicuous. In the club mosses and their allies, as well as in all roots, the seriation in the development of the elements of the primary wood is very 20 THE ANATOMY OF WOODY PLANTS generally from the exterior toward the center, and the metaxylem, as a consequence, is more axial or central in position than the protoxylem. This mode of development of the primary wood is characteristic of the most ancient plants, the lycopods and their allies, and is likewise universally present in the most conservative organ of all plants, the root. When the primary woody tissues develop from the outer region inward, as indicated above, they are said to be exarch. The situation just described will become more apparent by reference to Fig. 16, which shows 16a in an immature Fic. 16.—a, transverse section of the bundle of an old root of Osmunda cinna- momea, showing primary wood complete; 6, younger condition of the same with central region (metaxylem) of bundle still immature and containing protoplasm. condition. The outer regions of the oval mass of xylem are alone developed, the center being still occupied with thin cells filled with protoplasm. In the stem organs of the ferns and lower gymnosperms a some- what different mode of development of the primary wood is char- acteristically present. This may be illustrated by reference to one of the fibrovascular strands of the bracken fern, Pteris aquilina. The smallest elements of the wood are situated in the woody tissue constituting the center of the bundle. As in the case of Lycopodium and its allies, the smaller first-formed cells belong to the protoxylem. The situation which presents itself in the later development of the woody strand of ferns, however, is usually quite different from that found in the lycopod series. In the ferns the tissues of the primary metaxylem, instead of lying entirely toward the center of the organ FIBROVASCULAR TISSUES: WOOD 21 in the exarch condition featured in the lowest vascular plants, characteristically surround the first-formed ringed and spiral ele- ments (the protoxylem). This situation so frequently presented by the ferns and lower gymnosperms is designated as mesarch. The longitudinal topography of the bundle in this type is shown in Fig. 17. Fig. 13, described at the outset, pictures the relative position of the constituents of the primary wood in the stem of the higher seed plants, the Gnetales, the Con- iferales, and the angiosperms. In this case, since the seria- tion of the successive elements is always outward from an internal starting-point, the primary wood is known as endarch. This condition is the typical one for all the higher plants, and no form Fic. 17.—Longitudinal section of a characterized by it can, with- bundle from the rootstock of Pteris aquilina, : showing the elements of the protoxylem in Out che-clearest, evidence, (be 4... cantar-of tha mood: regarded as low in the scale of plants. Although the endarch condition is a feature of the development of the stem and generally of the leaf in the highest plants, it is important to emphasize at this stage that the root, even in the most advanced organisms, betrays its extreme con- servatism by, adhering in its primary structures to the mode of development and seriation of the elements characteristic of the most ancient known plants, the lycopods and their allies. Fig. 18 reveals the organization of a young root of the American larch. We may disregard in the present connection all but the central tissues of the root. Right and left can be distinguished two spaces, the resin canals. Inside of each of these two secretory cavities lies a cluster of protoxylem, distinguishable by the small size of its elements. Toward the center from each aggrega- tion of protoxylem extends the metaxylem, which in the young condition represented in the figure has not yet become joined in the center. 22 THE ANATOMY OF WOODY PLANTS It may be summarily stated in regard to the present chapter that wood in the older types is much simpler in structure and less differentiated than in modern forms. Further, in most cases it is necessary to distinguish between primary and secondary wood. WG Y ps a AL OK a ) AM (8% a Fic. 18.—Transverse section of the young root of the American larch. The primary wood has not yet been developed in the central region of the root. The endodermis separates the central or fibrovascular region of the root from the external fundamental tissue or cortex. The former is first to appear and is characterized by the lack of distinct seriation in its elements. The secondary wood, by con- trast, is formed later and the cells which constitute its structure are arranged in rows corresponding to radii; files of storage cells, FIBROVASCULAR TISSUES: WOOD 23 known as wood rays, are a marked feature of its organization. The primary wood consists typically of two regions: one composed of elements with ringed and spiral thickenings and capable of elonga- tion in accordance with the growth of the organs; the other con- stituted of tracheary cells thickened in a reticulate, scalariform, or pitted fashion and, as a consequence, incapable of extension to meet the needs of lengthening parts. The former region of the primary wood is designated the protoxylem and the latter the metaxylem. The order of development of the protoxylem and metaxylem differs significantly in different groups of plants. In the very oldest forms the progress of differentiation is entirely toward the center (lycopods and their allies). In the ferns and the lower gymnosperms the sequence is first central or centripetal and later peripheral or centrifugal, with the result that the protoxy- lem occupies a median position. In the higher gymnosperms and in the angiosperms the inward order of development has nearly or quite disappeared, and, as a consequence, the protoxylem lies on the inside of the metaxylem, which is formed characteristically outward or centrifugally. Technically these three types of organi- zation of the primary wood are designated exarch, mesarch, and endarch. Finally, it may be recalled that the primary wood of the root of all vascular plants has the exarch organization of the older types of stems and exemplifies the fact that the root in this respect as in so many others (to be shown in the sequel) is the most conservative of plant organs. CHAPTER IV THE FIBROVASCULAR TISSUES: SECONDARY WOOD— TRACHEIDS AND FIBERS Very important constituents of all woody organizations are the tracheids and fibers. These present a wide range of structure from the lower forms to the higher and illustrate some interesting general evolutionary principles.. Fig. 19 is a highly magnified transverse view of the wood of the white pine (Pinus strobus) in the region of transition from one annual ring to the next. Woods of this type are very simple and consist h st lAy ry ae mostly of elongated tapering elements a Lf | 2 Mi JU IL on 2 Ora =. with bordered pits in their walls and known as tracheids. The only fea- pl : Y ey YU} tures of organization not tracheary in =Ssaaq =e their nature are the rays and the =I Soeaae eX resin cavity. The tracheids are dis- A SATs 1 my tinctly of two kinds. Some are large eof I/ \ 4 and thinner-walled and begin the A FoI N /] (= annual ring as the so-called spring A SN) elements. Others, thicker as to their walls and with a smaller lumen or cen- Fic. 19.—Part of a transverse 4 : section of the wood of the white) | Lalucawity. | CONSUILULe fe msunimenr pine (Pinus Strobus), showing tracheids. The two kinds of tra- radial and tangential pitting of Cheids are in further contrast with the tracheids. Lite one another because of the position of the bordered pits on their walls. In the spring elements the pits are confined to the radial walls—that is, those sides of the fibers which are either in actual contact with, or are parallel to, rays. In the case of the summer tracheary cells pits are pre- dominant on the tangential walls which are at right angles to the rays. In addition to being in communication with one another by means of bordered pits, the tracheids both of the spring and of the summer wood are likewise related to the rays by 24 FIBROVASCULAR TISSUES: TRACHEIDS AND FIBERS) 25 pits which are bordered on the side of the tracheids and are simple on the side of the elements of the rays. In order to form an adequate conception of the nature of the fibrous or tracheary elements of coniferous woods it is necessary to view them in isolation from the tissues of which they form so essential a part. It will be advanta- geous to consider a simpler condition first and then to proceed to the more complex situation presented by the elongated elements of the wood of the pine. In Fig. 20 are shown tra- cheids of the Big Tree (Sequoia gigantea) belonging to the spring and summer growth respectively. On the left, one of the spring tracheids is seen from its radial face. The cell is obviously bluntly tapering at the ends and has a length many times that of its diameter. The pits which orna- ment the radial aspect are of two sizes. The larger bordered pits are those which connect tracheid with tracheid. The smaller pores bring about relations between the rays and the tracheids. The latter are bor- dered only on the tracheary side, although this feature is naturally not obvious in the illustration. The tra- Z cheid is represented as still surrounded Fic. 20.—Tracheids of by its cement substance, which is indi- Big Tree Sequota gigantea): 5 : planation in the text. cated by ja) heavier) line, On the lateral or tangential walls of the cell may be seen the profile aspect of other bordered pits. These are tangential pits and are very rarely present in the spring wood of conifers. Fig. 20b reproduces the appearance of the same tracheid from the tangential side. The general configuration of the fibrous element is now much more pointed and only a few pits can be seen in face. On the side 26 THE ANATOMY OF WOODY PLANTS walls in this position numerous pores may be distinguished, in profile, forming the principal means of communication between tracheid and tracheid and the sole one between tracheid and ray. To the right of the figure are to be seen the radial c and tangential d views of a summer tracheid. The narrower lumen and thicker walls are conspicuous. In the case of the pitting the most marked fea- ture of contrast with the spring fibers is the greater number of bordered pits occurring on the tangential walls. The situation in Pinus may now be advantageously considered. Figs. 21a and 6 reproduce the spring tracheary elements of this genus from the same aspects as represented in the case of Sequoia. Beginning with the spring element on the left, it is clear that the pits in relation to the rays show a considerable degree of differentiation, since they consist of two categories—namely, small, dis- tinctly bordered pores which form the intermediary between marginal ray cells and tracheids, and large, angular, scarcely bordered apertures uniting the central ray cells with the tracheids. The more pointed tan- gential contour of the tracheid in } surrounds an area entirely free from pits, a situation nearly universal for the spring elements of coniferous woods. In the lateral walls of b numerous radial pits are seen in profile. On the right of the figure are shown the corresponding views of the summer tracheids in Pinus. The narrower diameter and thicker walls, as well as the numerous tangential pores, clearly differentiate elements terminating the annual growth from those formed at the beginning of the year. Fic. 21.—Tracheids of the pine. Explanation in the text. FIBROVASCULAR TISSUES: TRACHEIDS AND FIBERS = 27 Tangential pits are so obviously and constantly a criterion of structure at the end of the annual rings in conifers that they may be used for the purpose of distinguishing the yearly increments in tropical species, in which, by reason of the slightly marked seasonal conditions, the zonal woody bands are indistinctly indicated or even apparently absent. This is notably the case, for example, in the tropical or subtropical species of the genus Araucaria. The phenomenon of annual rings is very closely correlated with the appearance of tangential pits, and the general phenomena in this respect are worthy of much greater attention than has hitherto been devoted to them. The incipient yearly zones in trunks of trees of earlier ages are the clearest indication of the progressive climatic refrigeration of the earth, and these become ever more marked in later geological times. Secondly, it will be made clear in the sequel that the modification of the annual ring in response to inclement seasonal conditions has been on the whole the most important factor in the evolutionary development of plants from the earlier epochs to the present. A consideration of the organiza- tion of the wood in a gymnosperm without annual rings—that is, a seed plant of Paleozoic time—is of extreme interest in the present connection. The tracheids of the secondary wood of the gymno- sperms of this age, without exception so far as is at present known, had the pitting confined to the radial walls; as a consequence water could move, easily at any rate, only in a spiral and tangentially through the tracheary elements. The truth of this situation may readily be grasped by reference to Fig. 11, in chapter iii, representing wood of the Paleozoic gymnosperm Cordaites. Details of the structure of the wood in this genus can be gathered from the inspection of Fig. 22 in the present chapter. It is clear that the tracheids communicate with one another and with the cells of the uniseriate rays by radial pits. Pits are conspicuously absent on the tangential walls of all the fibrous elements of the wood. It will be obvious from the facts put forward in this paragraph that the distinction between spring and summer tracheids did not exist in the case of Paleozoic woods; in other words, the modifica- tions in structure and pitting which have become a fixed feature of the organization of the summer tracheids of trees of the Mesozoic 28 THE ANATOMY OF WOODY PLANTS and Tertiary had not yet made their appearance in the Paleozoic age. It has been suggested that the function of the tangential pits in the summer wood is the rapid supply of water to the Zeer FS) ee SIAN aT Ace Sa \@, “BG FSA ESI NGI = soe Sag Saaz Bey SIZE 22742 > ig PE D -CA> oo <> eS A_ & ll YN WAH NSM WG NEEL as i Se =fzG: ce PNAS HES C= VED Eo \Y) (SEF (B27 \2AV C2 ZH _ Kee Bs EC Mm AC/ MS; MEL, _ 5 Z, a = x Je = x RUS, 5 a HAY) S Se —— — UfZaw. 7 AAS “2 ———} 1 21 223 BSE Gee ee ee, eS > —w EQS! : = zs = NYG Fic. 39.—Terminal parenchyma in Populus. Explanation in the text uncommon in the case of woods with reduced vasicentric paren- chyma. As in so many other instances, the situation is made clear by reference to more conservative parts, such as the root and the first annual ring of the stem, or to injured material showing a reversion to the primitive condition. By such control of evidence it becomes clear that in the Salicaceae, as well as in Magnolia and Liriodendron among the Magnoliaceae, the characteristic mode of distribution of the storage cells is vasicentric, for they occur in this manner both in conservative organs and parts and likewise as the result of experimental injury. It cannot, of course, be too strongly emphasized in the case of comparative anatomical investigations that a wide view of any particular situation is essential to an ade- FIBROVASCULAR TISSUES: PARENCHYMA 53 quate comprehension of a given problem. The truth of this statement will become more and more obvious as a result of repeated illustrations in the sequel. Much more rarely does the diffuse condition of parenchymatous disposition in the dicotyledons give rise by reduction to a state in which storage elements are to be found only at the end of the annual zones of growth. This situa- tion is exemplified by certain species of the antarctic beech (Notho- fagus), in which, in contrast to all the boreal species of the Fagaceae, : the parenchyma is confined to the face of the summer wood and is not distributed throughout the annual ring, as is the rule for the family as a whole. Similar reasoning to that employed in the case of the Salicaceae and certain Magnoliaceae results in the correct conclusion as to the typical and primitive mode of occur- rence of parenchymatous elements. It is necessary to emphasize the different interpretations of terminal parenchyma which must be adopted in the case of the conifers and the dicotyledons. In the coniferous series the presence of wood parenchyma on the face of the summer wood is clearly a primitive phenomenon, both because of the comparative and historical data and because of the equally cogent evidence derived from the consideration of the origin of parenchyma cells in this position in the conifers. Clearly, terminal parenchyma in the gymnospermous series is in the act of origination in view of its almost imperceptible transition to septate tracheids. In the dicot¥ledons, on the other hand, comparative and experimental data alone, in the absence at the present time of any adequate information in regard to the historical evolution of woods of this type, lead to the conclusion that the occurrence of storage elements in the terminal region of the annual rings is rather the result of reduction from a more elaborate and advanced condition (diffuse or vasicentric) than one of primitive simplicity. It is obvious that in general among the dicotyledons we need not expect to have as clear evidence in regard to the problem of the derivation of the longitudinal storage elements of the wood as in the case of the gymnosperms, and in particular the conifers, which present themselves to our gaze in so long and continuous a series in geologic time. Evidence for the origin of parenchymatous 54 THE ANATOMY OF WOODY PLANTS elements from the tracheary and other fibrous constituents of the secondary wood in the dicotyledonous angiosperms is sufficiently Fic. 40.—Longi- tudinal view of tracheids and paren- chyma from the root of the alder. authentically supplied by the grouping of such elements in longitudinal terminally pointed groups possessing the exact configuration of tracheids or fibers. Fig. 40 illustrates this situation for the wood of the alder. To the right and left are seen fiber-tracheids which constitute the mechanical elements of the wood in this genus. Between these two cells lies a file of parenchymatous elements of the wood. It is clear that the latter, represented with heavy black boundaries, form a series which both in length and in contour corresponds with the adjacent fibrous elements. Normally there are no transitions from tracheids to parenchy- matous cells in the case of the dicotyledons, and even experimental means do not in general suffice to bring about the clear production of parenchyma as the result of the progressive septation of the original tracheary elements of the wood. Some information on this subject, however, is furnished by the phenomena of injury in Liqguidambar and Prunus. Here, as a response to experimental or accidental injuries, tangential rows of gum or mucilage canals are formed in the wood. About these canals may sometimes be detected short elements which grade from abbreviated tracheids, resulting from the septation of tracheids of normal length, to typical parenchymatous elements, characterized by persistent protoplasmic contents and simple pits in their walls. Certain general characteristics of wood which depend as much as anything on the condition of the wood parenchyma may be conveniently introduced here. Fig. 41 is a photograph of the FIBROVASCULAR TISSUES: PARENCHYMA 5 On polished end of the trunk of an oak. The wood is clearly separated into two regions, a darker central and a pale peripheral. The deeply colored central region of the trunk constitutes the heartwood or duramen. ‘The uncolored zone which surrounds this is the sapwood or alburnum. ‘The dark-hued heartwood is extremely resistant to decay and constitutes the only material properly utilizable for exposed Seruetures. | | int the case of dicotyledonous trees in general, one frequently notes even with the naked eye a difference in color between the heartwood and the sapwood. Sometimes this impor- tant distinction is not revealed to the eye, but becomes obvious only under microscopic investigation. Fre- quently the sap indi- cates its boundaries in the felled trunk by the discoloration brought about in its tissues either by oxidases or by fungi, or by both agencies united. In conifers, likewise, a distinction between a darker central heartwood and a surrounding pale-hued sapwood can be often recognized by the naked eye. The redwood or red cedar presents the contrast in color in a very marked manner. The larch and the spruce, which in the microscopic organization of their woods are practically identical, can be readily distinguished from one another by the gross aspect of their trunks. The larch has a dark-brown heartwood, while in the species of spruce the central region of the woody cylinder is in no way contrasted in color with the peripheral sapwood. It will be convenient in connection with the discussion of the parenchymatous or storage elements of the wood to elucidate certain features of the microscopic organization of the heartwood Fic. 41.—Transverse view of an oak log showing heart- and sapwood. 56 THE ANATOMY OF WOODY PLANTS as contrasted with the sapwood. In this connection it will be well to begin with a conifer. Fig. 42 represents side by side the micro- scopic aspects of heart and sap tissues in the case of the white pine (Pinus strobus). Beginning with the sapwood, which appears on the right of the illustration, it is clear that both its rays and the cells surrounding a resin space or canal are possessed of nuclei and likewise contain a somewhat granular living substance or proto- plasm. Imbedded in the protoplasm are usually found oval bodies, aS = \ Se t——— fae $ Sa = Rial s | a Fic. 42.—Sap- and heartwood of the pine. Explanation in the text the grains of starch, which are lacking, indeed, only in the cells immediately surrounding the resin canal or space. By examination of the bordered pits of the tracheids it becomes evident that in the wood of the sap the membranes of the pits are central in position. Turning to the left side of the figure, we find represented the corre- sponding organization of the wood in the case of the heart. The elements distinguished by simple pits in the delineation on the right—in other words, the living cells—here have lost their living contents and are quite empty. Moreover, in the water-conducting cells, or tracheids, distinguished by the presence of bordered pits, we discover that the membranes of the pores with their thickened central region, or torus, are no longer median in position, but in general have become adherent to one side or the other. Further, the resin space has been stopped by an ingrowth known as tylosis. FIBROVASCULAR TISSUES: PARENCHYMA 57 In other coniferous woods, particularly those higher in the scale than Pinus, the parenchymatous elements, whether radial or longitudinal in position, secrete antiseptic substances such as essential oils, tannin, etc., which preserve the heart. structures from the decay resulting from the attacks of wood-destroying fungi. Fig. 43 throws light on the similar conditions as regards the organization of heart and sap in the oak, as an example of the dicotyledons. To the right, radial and longitudinal parenchymatous i Geen) TaN a epee ry, Se wae Lk TN = aN ES > Bas) Bis) Sy. of \Y) else S25 @) an 4 mAoUn fa\ SX \ EIN N A \EGrs Frc. 43.—Heart- and sapwood in the oak. Explanation in the text la deo Jerr S Sy = exam) elements appear loaded with starch and provided with proto- plasm and nucleus. The radial storage cells are represented with light walls, while the true wood parenchyma is delineated with thick, black, bounding membranes. Larger and smaller vessels are to be seen corresponding to the spring and summer region of the wood. The rest of the area is occupied by tracheids (larger and thinner-walled) and fiber-tracheids (narrower and with thicker walls). Turning now to the left, where the organization of the heartwood is indicated, we discover the same absence of contents in the radially and longitudinally directed elements with simple pits (in other words, the parenchymatous elements) as in the case of the similar structures of the pine. In this instance the larger vessel presents a certain analogy to the resin canal of the conifer by reason of the fact that it is occluded by an ingrowth in the form of 58 THE ANATOMY OF WOODY PLANTS a tylosis. An adhesion of the pit membranes to one overhanging margin or the other of the pit cannot be made out. Occasionally a torus is present in the relatively narrow membranes of the small bordered pits of the water-conducting elements of the dicotyledons, but it does not present the phenomenon of fusion with the margins of the pit characteristic of heartwood in conifers. The paren- chymatous constituents of dicotyledonous woods in many cases give rise to highly efficient antiseptics in the case of the heartwood. In many instances, such as the oak, the blue gum, the quebracho, etc., large amounts of tannin are formed which serve as an effectual preservative. In other cases ulmic and even humic acids make their appearance and exercise greater or less inhibitive action on the organisms which ordinarily bring about the decay of woody structures. In teak we have the rare example of a structurally valuable dicotyledonous wood which in the transformation from heartwood to sapwood elaborates, not acid substances which exer- . cise a corrosive action on metals, particularly on iron and steel, but an essential oil. The enduring heartwood of the teak (Tectona grandis) is consequently valuable above all others for naval con- struction by reason of its compatibility with iron and steel, since it neither corrodes this fundamental structural material of present naval architecture nor, in turn, is rotted by iron rust. It will be apparent from the foregoing paragraphs that those longitudinal elements which subserve the function of storage in the woods of Mesozoic, Tertiary, and actual plants are of great evolutionary significance. Their importance in this respect can be gauged only after the rays or radial storage devices have been considered in the next chapter, and they will receive their final and fullest appreciation in connection with the highest groups of plants. It is obvious that the incentive to the development of longitudinal parenchymatous elements was the appearance of an annual winter period of rest which in later geological times, begin- ning with the earlier Mesozoic, with progressively greater emphasis marked the originally unvarying cycle of the year. The first parenchymatous elements came into being, so far as our knowledge at present goes, in the earlier Jurassic. Their primitive occurrence was at the end of the annual ring. In the conifers in this position FIBROVASCULAR TISSUES: PARENCHYMA 59 they often clearly reveal their derivation from tracheids by almost imperceptible transitions into elements belonging to this category. The terminal situation of the primitive parenchymatous cells is probably of advantage to the cambium awakening from its winter sleep and standing much in need of instantly available food. In general, the tangential terminal parenchyma of the more primitive conifers has the same nutritive relation to the cambial elements as the similarly located tangential pitting of the tracheids has to the water supply of the cambial zone. Later the longitudinal elements devoted to the function of storage, like the tangential pitting of the tracheids, became dis- tributed throughout the annual ring. So long as there was no further differentiation of the elongated elements of the wood there was no incentive to further evolution on the part of the elements of the wood parenchyma. With the appearance of the vessel as the final expression of efficiency in the transport of water on the part. of the wood and the correlated gradual loss of the aquiferous function on the part of the tracheids (which progressively gave rise to fiber-tracheids and libriform fibers, respectively more and more specialized in the mechanical direction), a new tendency found expression in the organization of the longitudinally oriented storage devices of the wood. In the case of the higher gymnosperms (Gnetales) and lower dicotyledons the fibrous elements of the wood are still largely capable, by reason of the presence of numerous bordered pits in their walls, of the transport of water. The higher dicotyledons, however, are in general characterized by the strict allocation of the function of movement of water to the vessels, and the tracheary structures of lower types become transformed into purely mechanical or partially mechanical and partially food-storing elements designated progressively as fiber-tracheids, libriform fibers, septate fibers, and substitute fibers. With the appearance of this situation the parenchymatous elements of the wood become more and more relegated to the vicinity of the vessels for their necessary supplies of all-important water. This situation receives its final morphological and evolutionary expression in the appearance of strictly localized vasicentric parenchyma in the case of high dicotyledonous groups, such as the Compositae, Sapindales, 60 THE ANATOMY OF WOODY PLANTS Verbenaceae, Oleaceae, etc. It must not be assumed, however, that the localization of the parenchyma about the vessels is strictly referable to the transformation of the tracheids into purely mechani- calelements. It has been shown by Miss Holden in her interesting investigations on the Sapindales that it makes no difference whether the fibrous elements of the wood here are of the nature of tracheids (and hence are capable of conducting water) or are libriform and mechanical as regards the distribution of the elements of the wood parenchyma, which in the group throughout are vasicentric. It is thus clear that the distribution of the parenchymatous cells in dicoty- ledonous woods is of morphological importance and is not physiolo- gically conditioned by the nature of the fibrous portions of the wood, whether tracheary and with bordered pits or libriform and thus definitely relegated to purely mechanical functions. It is finally important to note that not even the obvious facts of distribution can without proper discrimination be subjected to evolutionary inference. For example, in many dicotyledonous woods terminal parenchyma occurs which might be regarded as prima facie evidence of a primitive systematic position in view of the situation presented by the conifers, exhibiting parenchyma on the face of the summer wood. A comparative and experimental investigation of this situation makes it clear in the case of the dicotyledons that the terminal position of parenchyma is the result of degeneracy either from the vasicentric or from diffuse modes of parenchymatous distribution. CHAPTER VI THE FIBROVASCULAR TISSUES: SECONDARY WOOD—RAYS In the preceding chapter the subject of the origin of longitudinal storage cells has been discussed and to elements of this type the general appellation of wood parenchyma has been given. In the case of the ligneous tissues of vascular plants a much older type of storage device exists in the form of radially directed bands of masses of cells which often, with a high degree of im- propriety, are desig- nated medullary rays. This denomination is erroneous from the historical and evolu- tionary standpoint, since it is clear that in the first instance and in the earlier and primitive forms rays had no relation what- éver, to the pith or =! one SuSE medulla and _ conse- Fic. 44.—Transverse section of the stem of a quently cannot with lepidodendrid, showing well-developed primary and secondary wood, the latter being radially seriate and provided with storage rays (after Scott). any degree of pro- priety be designated as medullary. Fig. 44 illustrates the conditions obtaining in the case of the so-called medullary rays of the ancient genus Lepido- dendron. The region of the pith () is represented largely by an empty space, which is in turn surrounded by the primary wood. This is distinguished by the non-seriate and irregular arrangement 61 62 THE ANATOMY OF WOODY PLANTS of its cells in contrast to the regularly and radially disposed structures of the secondary xylem which lies just outside the primary region. It is clear from the figure here introduced that the so-called medullary rays which extend from the primary wood outward cannot be properly so designated, since they never come in contact with the pith. The same situation occurs in the stem ,( ( sNatit— ol =e ce i; Ml Lk UU, { i im \\\ \\\y) I” Ss Sy A Gee ees Mh Minin = ANliny HI eet al ee: NS ea lf aa Mn ! —— Fic. 45.—Longitudinal view of the primary wood of a lepidodendrid. Explana- tion in the text. of many other extinct fernlike or gymnospermous plants with secondary growth. It is worth while to note, too, in this connec- tion, that in the root of living plants in which the wood undergoes secondary increase its radially disposed bands of storage cells have nothing to do with a pith or medulla. It is accordingly evident from an examination of older and consequently more primitive forms, and likewise from the study of the organization of the con- servative root structure of living groups, that the term medullary FIBROVASCULAR TISSUES: RAYS 63 ray is a misnomer. The most appropriate name for the radial stripes of storage elements in the secondary wood is the merely descriptive one of wood ray. The status of the ray having been preliminarily defined from the evolutionary standpoint there now remains the question of the origin of the hori- zontally directed bands of storage tis- 1 sue which it is cus- tomary to consider ( under this head. I [Fa has been made clear | ‘a that the lepidoden- | ig ean drids are the only & Ge oN = 28 plants which supply decisive evidence as ' to the origin of the ‘ parenchymatous ele- » & & @ ments found uni- 6 Q ® / versally in the primary wood of vascular plants. It be P Fic. 46.—Transition from primary to secondary wood will be well to recall jn a lepidodendrid. Description in the text. the situation here by reference to Fig. 45, which shows a longitudinal view of the tracheary and allied structures of the first-formed wood of a speci- men of the genus Lepidodendron from the Carboniferous of Lanca- shire, England. It is obvious that, in addition to the longer cells with reticulately thickened walls—the tracheids proper—there are numerous short elements with a similar kind of sculpture. In series with these are other cells again which are quite without the usual tracheary thickenings and which belong, in fact, not to the water-conducting system, but to the storage category. These are wood parenchyma. It is evident in the present instance that the storage cells of the primary wood have been derived from what were originally tracheids by septation or division and subsequent differentiation. It has been demonstrated in the previous chapter 64 THE ANATOMY OF WOODY PLANTS that the parenchymatous structures of the secondary wood are in the first place derived from modified tracheids. In Fig. 46 is shown the region of transition from primary to secondary wood in a lepidodendrid, somewhat highly magnified. The secondary tissue is most characteristically distinguished by its rays running in alternation with bands of large tra- cherds:. dhiesie radially directed stripes of storage elements at once attract attention by reason of the unu- sual organization of their component cells. The constit- uent units of the rays in this instance are reticulately thickened after the manner of tracheids and, in fact, differ from these only by their abbreviated length and the somewhat more delicate nature of their sculpture. There is, indeed, not the slightest doubt that in the case of the lepidodendrids the rays are largely, and in some instances wholly, composed of cells belonging to the category of tracheids. This situation is clear in radial sections taken length- wise through the wood. Fig. 47 represents such a section from the root of the lepidodendroid type know as stigmaria. The heavy sculpture of the tracheids composing the mass of the wood can be easily made out. Running at right angles to the direction of the tracheary elements of the wood are the cells of a ray. These again show a considerable degree of scalariform thickening, only a few being completely devoid of this form of sculpture. It is obvious from the conditions described in the case of the lepidodendrids, a group of arboreal club mosses flourishing Fic. 47.—Radial view of the secondary wood of a lepidodendrid, showing tracheary origin of the rays. FIBROVASCULAR TISSUES: RAYS 65 in the Paleozoic, that rays in this type were more or less largely composed of tracheids. It seems clear for this reason that the radial bands of storage parenchyma which constitute the rays in secondary wood, like the longitudinal parenchyma included under the caption of wood parenchyma, are derived from the modification of tracheary tissue. It thus becomes apparent that originally all the parenchymatous constituents of wood, whether primary or secondary or radial or longitudinal, in the first instance made their appearance by the modification of tracheary tissues. Tracheids, in fact, constitute the sole original feature of organiza- tion in woods, and the course of evolution expressing itself in con- tinued differentiation has led to the derivation of all the other features of ligneous structure from this primary constituent. In other words, wood primitively was a purely water-conducting tissue, and the superadded mechanical and storage functions subserved by its organization in later geologic times resulted in appropriate modifications of the original tracheary elements. The derivation of the rays from tracheary tissues can be distinguished clearly only in the lepidodendrids and their allies. In others of the arboreal cryptogams which were so characteristic of the forests of the Paleozoic age no evidence of the origin of ray cells from tracheids has been observed. The same statement holds for the lower and ancient gymnosperms, the Cycadofilicales (Pteridospermae of Oliver and Scott) and the Cordaitales and their allies. These antique gymnospermous groups, as well as the arboreal cryptogams sig- nalized above, had no storage tissues in their wood other than radial parenchyma; for the longitudinal parenchymatous elements known as wood parenchyma proper made their appearance only in connection with the seasonal refrigeration which became ever more pronounced during Mesozoic and later geologic time. The rays of the older plants with secondary growth were of two main types. In some instances (e.g., Cycadofilicales) they were composed of bands of cells several elements in width and greatly varying in height. In the Cordaitales and allied forms the rays were ordi- narily uniseriate—that is, a single cell in width, in contrast to their often multiseriate and considerable height. In a general way it seems clear that woods of the first type are perpetuated in the still living, although much reduced, Cycadales, while the Cordaitales, 66 THE ANATOMY OF WOODY PLANTS according to common consent, find their successors in the conifers of the present age. Since it is highly probable that the Cordaitales gave origin to the Coniferales, and since, as a consequence, they present us with iN VY VO NVQ SN ) SZ ra, WY) N ay WN 0 on 1\\) WON SG me, AVY 8 LOK VO. a Ni Gee WW mM igs SON wok aN ~2-8 ) S| TS eee NS \ ORS oe AS SAME Sz EEENSCE ECA So CE 2 — = — _ —= a = Gx = S AE BE @, H AIS Ge— AIS]. eee —§ Zz. = = =a BG Ae e2sa6 oN a Fic. 48.—View of cordaitean wood in three dimensions. Explanation in the text. the starting-point of the radial parenchyma of the latter, it will be well to consider the organization of this group in respect to the structure of the rays. Fig. 48 shows the structure of a cordaitean wood. The tracheids in this genus are usually extremely long; FIBROVASCULAR TISSUES: RAYS 67 consequently only a portion of their length is represented in the figure. The pitting is somewhat characteristic and is ordinarily marked by the large number of pores and their consequent crowded and alternating arrangement. The rays cross the direction of the longitudinal elements and are characterized by their thin walls, which are, however, clearly pitted laterally in relation to the radial walls of the tracheids. It is to be noted in passing that there are no tangential pits on the walls of the longitudinal elements of the wood—a feature, as has been indicated in a previous chapter, very generally characteristic of the woods of the gymnosperms of the Paleozoic regardless of their affinities. In the transverse section of the wood the rays stand out distinctly as uniseriate files of cells, having their axes radially elongated. The rays are in lateral communication with the tracheids by half-bordered pits. Other- wise their thin walls are not characterized by the presence of pores. The tracheary elements of the wood are tangentially in com- munication by numerous radial pits, but their tangential walls are quite free from pores, so that in these ancient gymnosperms water could make progress in the trunk only in a tangential direction. The tangential view of the wood shows the radial pits of the tra- cheids as well as the lateral ones of the cells of the medullary rays in profile view. After the discussion of the organization of rays in the Cordaitales we are in a favorable position to understand the condition in the conifers. In this connection it will be well to start with the most complicated condition in living representatives of the group, since the coniferous gymnosperms, as will be shown clearly in a subse- quent chapter, constitute a reduction series with the more complex forms at the bottom and those with simpler organization at the top. Fig. 49 represents radial and tangential views of the wood of the white pine (Pinus strobus). Taking first the radial view shown in a, a number of important contrasts in organization to cordaitean woods are to be seen. First of all as regards the tracheids, or rather such part of them as is included in the field of view, it is clear that they are distinguished from similar structures in the Cordaitales by the smaller number of pits and the considerably larger size of these. Further, the pits in face view, instead of presenting the 68 THE ANATOMY OF WOODY PLANTS merely double contour of the more ancient group, are marked by triple concentric outlines. The outer circle corresponds to the boundary of the pit membrane, while the inner one outlines the mouth or aperture of the pit. The intermediate circular outline delimits the thickened central region of the torus, a structure, which so far as is known, was not present in Paleozoic gymnosperms. Its presence in the conifers is in all probability correlated in some SS Ce) P i [ c LS @ —<— Fic. 49.—Radial and tangential sections of the wood of the white pine (Pinus Strobus). Explanation in the text. way with the large size of the bordered pits; it has, in fact, as pointed out in an earlier chapter, been interpreted as a safety device useful in preventing the rupture of the broad pit membranes under extreme pressure. Not only are the pits of large size and more complex organization in the pine than in cordaitean forms, but the walls of the tracheary elements in their vicinity, partic- ularly toward the ends of the tracheids, are distinguished by trans- verse bands of cellulosic or pectocellulosic material, and these are conveniently designated “bars of Sanio.”’ They should not be confused with the trabeculae, radially directed lignified bars running transversely through the lumina of the cells of many gymnosperms living and extinct. (They are even found in some cases among the FIBROVASCULAR TISSUES: RAYS 69 angiosperms.) There is good reason to believe that the “‘bars of Sanio”’ are an original and characteristic feature of the organization of the wood of the Coniferales and allied groups. The tracheids shown in the figure differ from those of the cordaitean forms by their periodic variation in size, those laid down in the beginning of the annual increment being of larger caliber than those coming into existence toward its close. The late tracheids are distinguished, as indicated in earlier pages, by their tangential pits seen in profile in the radial section. Turning our attention now to the ray itself, we see at once from the figure that a considerably greater degree of complication is present than that exemplified by the similar structure in the case of the Cordaitales. Manifestly the radial elements are of two kinds. First there are the cells which constitute the central region of the ray and which in life are char- acterized by protoplasmic and other contents. This situation is indicated by the copious simple pits which ornament the vertical and horizontal walls of the cells. The strong pitting is also a clear feature of difference from the Cordaitales where the walls of the ray cells are in general thin and unpitted. Laterally the central elements of the rays are related to the tracheids by means of very large, somewhat angular pits. The second type of element char- acteristic of the ray in Pinus is likewise distinguished by the nature of its pitting. All the pits seen on the walls, whether horizontal, vertical, or lateral (related to the tracheids), belong to the bordered type. The cells of the ray possessing this peculiar organization are typically marginal in position and, naturally, are quite without protoplasmic contents, except in the early stages of development. Such tracheary elements in coniferous rays are commonly desig- nated marginal tracheids or simply marginal cells. They obviously permit the easy movement of water in the radial direction in those woods characterized by their presence. In the tangential view presented in 0, Fig. 40, it is clear that there are two types of rays—namely, narrow uniseriate ones and broader ones tapering at either end to the uniseriate condition. The former are known as linear rays and the latter as fusiform rays. It is evident from the figure that the ray of greater width is char- acterized by the presence of a partly occluded cavity, a resin canal. 70 THE ANATOMY OF WOODY PLANTS The stopping up of the resin canal is explained by the fact that the section is taken from the heartwood, which, as has been pointed Fic. 50.—Tangential view of the wood of the Pseudotsuga. Explanation in the text. out in a former chapter, is distinguished by the phenomenon of tylosis or occlusion of the secre- tory spaces by means of ingrowths of the resi- niferous parenchyma. In the case of the nar- row or linear ray it is possible to distinguish in the tangential view, by means of their char- acteristic pitting, both the parenchymatous central cells and the tra- cheary marginal ele- ments. "The cemtrat elements with their simple pits are in rela- tion to air spaces in the angles. The presence of both linear and fusiform rays is a constant fea- ture of organization in the pine and its nearer allies. The linear rays are doubtless an older feature than the larger ones which contain the horizontal resin canals, since they resemble most nearly the radial paren- chymatous structures of the Cordaitales. The fusiform rays serve to bring about a connec- tion between the vertical resin canals in different annual rings, not FIBROVASCULAR TISSUES: RAYS qe only with one another, but often with the similar but larger secre- tory cavities which are present in the bark. Fig. 50 illustrates the relation between the vertical and hori- zontal resin canals as seen in a vertical section of the wood of the Douglas fir (Pseudotsuga). To the left of the center lies a fusiform ray with its included resin space, which opens broadly on the right into a vertical secretory canal. The plane of sec- tion happens to lie near the end of the annual ring so that the cellular struc- tures lying in view are almost entirely parenchy- matous. The lining of the resiniferous spaces is evidently largely com- posed of elements with thick walls and bordered pits, a condition very com- monly present in the representatives of the Pineae other than Pinus itself. After the discussion of the pine and its nearer allies we may proceed with advantage to the description of the ray structures in coniferous woods of simpler organization. Fig. 51 illustrates the structure of the ray in the wood of the balsam fir (Abies balsamea). It is clear that in this case the cells of the rays are all of one kind and that the marginal tracheids are conspicuous by their absence. The parenchymatous elements which compose the rays in the genus under considera- tion are in relation to one another on both vertical and hori- zontal walls by numerous simple pits. The lateral walls show bordered pores such as ordinarily, except in certain species of Pinus, characterize the relation between rays and _tracheids. The organization of the linear rays in conifers other than the Abietineae is in general of a simple nature; and in the higher Fic. 51.—Ray of the balsam fir. Explana- tion in the text. V2 THE ANATOMY OF WOODY PLANTS subtribes, such as the Cupressineae, Taxodineae, and Taxineae, even the intercommunicating simple pits of the horizontal and vertical walls of the ray cells are clearly and often conspicuously absent. In such cases, as is to be expected, the wall of the ray elements is in general thinner and often curved. An interesting condition of organization of the radial paren- Faq als “ole “oll Meals ([to Ik “all oll ell Ie Foil cello Slee Wellollll& Al “alle aCe ®ollNllells Alle ilo ll(eo lst ell SIs chase che Iolo Kell Q|"Ol_ © Ric 2 s Hole Fic. 52.—Ray of the Nootka cypress. {s9| De- chyma is presented by Chamaecyparis nootkaten- sis. Here, as is shown in Fig. 52, the rays are fre- quently marked by the presence of tracheary ele- ments on one or both margins. The illustration represents the radial aspect of the transition from summer to spring wood, and the features of structure are in general such as one would expect to find under the circum- stances, except as regards The ray organization. normal presence of margi- nal tracheids in the species figured gains a special evolutionary sig- nificance from the fact that similar conditions are found in other representatives of the Taxodineae, Cupressineae, and the genus Abies among the Abietineae as a consequence of injury. For reasons which will be fully discussed in a subsequent chapter it seems quite clear that the structures which are found to appear as a result of injury in vascular plants with secondary growth are often of the nature of reversions to an ancestral condition. Fig. 53 illus- trates in radial view the wood formed after injury in a root of the Big Tree (Sequoia gigantea). Parts of two annual rings are included, and the ray clearly shows features of structure which are abnormal for the Taxodineae. To the left below and in the spring wood can be seen several cells included in the substance of the ray which are scription in the text. FIBROVASCULAR TISSUES: RAYS 70 clearly tracheary in their character, since they contrast with the adjoining elements both in the absence of protoplasmic contents and in the occurrence of bordered pits in all their walls. It is evident that in the case under discussion short tracheids may make their appearance among the elements of the radial parenchyma as a sequel to injury. The interesting investigations of Miss Holden Fic. 53.—Ray from the injured root of Sequoia gigantea. Explanation in the text (after Holden). on the Cupressineae and Taxodineae as a whole make it clear that abnormalities of this kind in these subtribes of coniferous gym- nosperms are a common feature in the wood formed after injury. It follows from the statements and illustrations in connection with the last paragraph that normally in Chamaecyparis noot- katensis and traumatically in practically all representatives of the Cupressineae and Taxodineae, ray-tracheids are found such as are a feature of the normal structure of the wood in the lower members of the Abietineae. The most natural interpretation of this phenomenon is in connection with the biological doctrine of 74 THE ANATOMY OF WOODY PLANTS reversion. This general doctrine will receive particular considera- tion at a later stage and consequently need not be elucidated here. If the radial tracheids occurring under the conditions described in the foregoing paragraph are interpreted as a reversion to an ances- tral condition, it follows that the simple type of ray found in Abies and in the Cupressineae or Taxodineae is by no means primitive, but is the result of simplification from the more complex state of organiza- tion of the ray, characteristic of the lower living Abietineae. Obvi- ously an experi- mental as well as a purely anatomical investigation of ray structures is necessary for their complete morpho- logical and evolu- tionary under- standing. Not only does — ee- me. -@8069 Boee TITEL al 220e0en e20786G00 «+ OF 88: S8IBDevrecccsesres S80ee oe .. eteaneregs => 2888 we apt. soe mcmmasanee @ -=-@°*S O0e8050d GhebeteBDeg. nm @0*@sanceoosag ™ eee +s seas o © by Bam © @ e600 see (i jeaietie Aas ir, es stee- ~<« ences meantime OS® een, se = @Os8eeeep" a0 ) . e ® e s e s e = es . s e 8 s ec; ® 9 \OPRD® O2OS0Or00 CO@Be ‘se Oe G0G02D SEESeeon — = I'tc. 54.—Tangential section of the normal wood of Cedrus Libant. one find in the case of certain coniferous woods of simpler organization evidence of derivation from ancestral types present- ing the complication of marginal ray-tracheids, but likewise in the genus Cedrus among the Abieteae, which has normally only linear or uniseriate rays, fusiform radial structures containing horizontal resin canals are found. This situation is made clear by Figs. 54 and 55, which present tangential views of the normal and injured wood of Cedrus Libani (the cedar of Lebanon). In the traumatic or injured wood of cedar, which, so far as the geological record supplies us with definite evidence, is the oldest representative of the Abieteae or firlike conifers, we have clearly indicated a condition ensuing from injury which definitely unites the cedar FIBROVASCULAR TISSUES: RAYS 75 with the genus Pinus, much older geologically and more complicated in the normal organization of the wood. It will be clear from the statement in this connection that fusiform rays have also an impor- tance from the experimental standpoint, quite comparable with marginal tracheids, but less copiously expressed in traumatic phenomena. The rays of the Cycadales and their allies present no features of spe- cial evolutionary interest, so far at _ any rate as is known at the pres- ent time; they may therefore be dis- missed with the simple statement that they are typi- cally multiseriate bands and not the linear structures constituting the primitive condition of organization of the radial parenchyma for the Cordaitales, Coniferales, and Ginkgoales. The ray structures in the highest gymnosperms, the Gnetales, are best discussed in connection with the similar features of dicotyledonous woods, which they resemble in so many respects. This procedure is the more desirable because the living Gnetales are represented by a very small number of genera of widely separated geographical ranges. At this point the dicotyledonous angiosperms may appropriately be considered in regard to the organization of their rays. Fig. 56 reproduces a transverse section of the wood of the oak. The struc- ture in this case is highly complicated and corresponds to a marked development of the principle of division of labor. The movement of water, the functions of strength and of storage, are all distinctly a 2 ts, a os rs ° J ° . 8 . e = e J Bay sed eee LEE aan een. eee eet Sevenuess’** es o ‘eoecseeeege--* -— .@ Sea‘ PRR N O00 O Margy Fic. 55.—Tangential section of the wood of Cedrits Libani formed after injury. 76 THE ANATOMY OF WOODY PLANTS allocated to particular and highly differentiated categories of cells. In the present connection we are concerned only with the struc- tures included under the heading of radial parenchyma. Clearly the rays in the oak are of two types, even as seen in transverse section. A small number are very broad and constitute a large bulk of storage tissue. In contrast to these in respect both to size and to number are linear rays, abundantly present in the figure. It is best in this instance to focus our attention on the composition of the uniseriate or linear rays and their relation to the various ele- ments represented in the complex organization of the wood in the same genus, Quercus. Fig. 57 repre- sents the uniseriate rays in radial and ; : tangential aspect. Fic. 56.—Transverse section of the wood of the : Meet ae In a is seen the tangential view. The ray is obviously composed of cells which are all alike and related to one another and to the air spaces by simple pits. Half- bordered pits connect ray cells with tracheids. In b and ¢ are shown radial aspects of the ray in relation to the various structural elements of the wood. On the left and right in 6 files of vertical parenchyma cross its course and are related to the radial elements by groups of clustered pits. To the left of the middle of b is shown a vessel (this type of element will be considered in the following chapter) which communicates with the radial storage elements by large, generally oval, pits. The rest of the width of 6 is occupied by tracheids, which in turn communicate with the cells of the FIBROVASCULAR TISSUES: RAYS 77 rays by small bordered pits. Inc is seen a region where the linear ray passes through a purely fibrous portion of the wood; and here there are no pits at all, since the mechanical elements which, as has been indicated in a:former chapter, have been differen-’ tiated from the tracheids no longer supply water to the other structures of the wood. It will be clear from the foregoing account that the uniseriate or linear rays of the oak are of uni- form and simple organization as regards their constituent ele- ments, but that these are characterized by a variety of pitting corresponding to the high degree of differentiation of the wood ACTUAL UB Receareber ||| k DAIL Fic. 57.—Longitudinal and transverse views of linear rays in the oak. Explana- tion in the text. through which they pass. The large rays of the oak can better be considered at a later stage after a type showing a more general- ized condition of radial organization has been examined. It will be convenient and profitable to consider in the present connection the genus Casuarina, which occurs in the East Indian and Australasian regions, since here we find in various species all the main types of organization of the wood rays exemplified by the dicotyledons. First is presented the tangential, longitudinal view of the wood in Casuarina Fraseri. Here the structural conditions are manifestly very similar to those found in the oaks of northern latitudes, for there are two distinctly contrasted categories of rays— namely, the numerous linear or uniseriate and the sparse broad rays. In comparison with the wood of C. Fraseri, presenting a strong resemblance to that of a white or black oak (Fig. 58), is that of C. torulosa, shown in Fig. 59. Here the linear rays are as 78 THE ANATOMY OF WOODY PLANTS in C. Fraseri, but the large band of radial parenchyma is obviously not homogeneously parenchymatous, but is separated into pointed groups by the presence of interspersed fibers. In other words, instead of a continuous mass of storage tissue there is present an aggregation of rays of a certain size, separated from one another by strands of fibers. This condition of the large ray may be conveniently designated as aggregate. In Fig. 60 is represented the tangential aspect of the wood in C. equisetifolia. In this type we no longer see a sharp contrast between large multiseriate or aggregate rays and small entirely uniseriate ones, but, as it were, a more democratic organi- zation of the radial parenchyma, in which no extremely large radial paren- chymatous masses < ———— oo ’ ase: =a “ :@ a Fic. 58.—Tangential section of the wood of Casuarina Fraseri. Explanation in the text. are found, as all grade almost imper- ceptibly into one another in size. The last-described condition of the rays, for reasons to be indicated later, is here designated as diffuse. We have thus in the single genus Casuarina three distinct types of radial parenchyma: first, the northern oak type in which huge rays stand in the sharpest contrast to narrow uni- seriate bands; secondly, a condition in which the contrast still obtains as regards the dimensions of the rays, with the dis- tinction that the large masses are not homogeneous but pene- trated by bands of fibers; and, finally, there is to be noted a state or organization in which all rays are of moderate width and are scattered somewhat evenly throughout the tangential or transverse FIBROVASCULAR TISSUES: RAYS 79 section of the wood. In the first condition the large rays are known as compound; in the second they are designated as aggre- gate, and in the third state, where there is generally no marked superiority in size and the rays intergrade almost imperceptibly, they are known as diffuse. Of the three conditions of organization of radial parenchyma in the dicotyledons described above, the compound is extremely rare in trees but is commonly found in climbing and _her- baceous types. The diffuse condition of the radial paren- chyma is very com- mon in forest trees, but is much less characteristic of plants of herba- ceous texture. The genus Casuarina has purposely been chosen for the exemplification of the problems con- A Fic. 59.—Tangential section of the wood of Casu- nected with the arina torulosa. Explanationin the text. evolution of radial parenchyma in the dicotyledons, not because it is necessarily a primitive form, but because it shows the situation synoptically and, moreover, furnishes very clear evidence as to the relation of the various types to one another from the evolutionary standpoint. An exposition of the interesting and important situation of the ray structures in the dicotyledons can best be approached by a diagrammatic comparison with the conditions presented by the conifers. Fig. 61 reproduces the essential features of organization of a coniferous stem with whorled leaves—for example, a Juniperus or a Cupressus. The leaves, three in number, are indicated in 80 black on the periphery of the stem. THE ANATOMY OF WOODY PLANTS Centrally placed is the pith, surrounded by the woody cylinder, which in turn is circled by the phloem and the cortex. The woody tissues are encroached upon by three deep bays extending from the medulla and subtended by the three leaves. These extensions from the pith mark the presence of the leaf gaps, interrup- tions in the con- tinuity of the woody cylinder re- lated to the passing out of the fobhar traces. Later the intervals in the wood are covered Fic. 60.—Tangential section of the wood of Casua- rina equisetifolia. Explanation in the text. that the cylinder becomes continuous in the second or third year of growth. Clearly there is no structural feature of importance in the woody cylinder related to the leaf trace other than the foliar gap. This is the general situa- tion in the case of coniferous stems as well as in that of their Paleozoic ances- tors, the Cordaitales. Having diagrammatically compassed the organization of the stem in the coni- fers, we are in a position to consider the case of such a dicotyledon as Casuarina. by the activity of the cambium, so gully PY ly \ é [Re wy Dy, WD o» LZR) lr ANN! UAL ey < oo] > | | \ es mh (awe Fic. 61—Diagrammatic transverse section of a coniferous twig. Explanation in the text. In Fig. 62 are reproduced the essential features of topography of a small branch in this genus. Leaves, as in the case of the conifer- FIBROVASCULAR TISSUES: RAYS 8L ous diagram given previously, are represented in black on the periphery of the stem. The central pith is likewise encircled in turn by wood, phloem, and cortex. Here, too, there are excur- sions of the pith at six points, extending into the second annual increment of the wood; these subtend radially six corresponding leaves. In the diagram under discussion there are, however, two marked features of contrast to those presented in the foregoing scheme of a coniferous axis. First of all, the wood is character- | ized by the presence of vessels, and secondly by a broad radial stripe "y, which extends from each leaf gap « Bey Has ; ' a7 \ outward. This radial stripe con- TE eS Z trasts with the rest of the woody cylinder by the absence of vessels and the clustering of rays. The radial parenchymatous stripes which lie in the region of the six radial bands corresponding to six leaves are not only more prominent than the A Bia Fic. 62.—Diagrammatic trans- : : verse section of the stem in Casua- linear and somewhat Sparse rayS IN yjna, Explanation in the text. the rest of the wood but are of greater width. The aggregations of rays related to the leaves shown in the diagram are, in fact, clustered rays of the type exem- plified by C. torulosa (Fig. 59) and are, as a consequence, aggregate rays. Since they are in this instance clearly related to leaves, they may at the same time be appropriately designated foliar aggregate rays. With the exposition of the essential features of organization present in coniferous and dicotyledonous stems, respectively, we are in a position to proceed further with the highly important discussion of the evolution of the radial parenchymatous structures _ of dicotyledonous woods. Simplicity will be served and ambiguity avoided if in further elaboration we hold to the conception of the rays as they present themselves in a small twig of a few years’ growth. Fig. 63 illustrates synoptically the main types of rays in the dicotyledons as seen in small branches. The only essential departure from the conditions in nature is the delineation of the 82 THE ANATOMY OF WOODY PLANTS three important categories of rays as occurring side by side in the same stem. In the center of the circle representing diagram- matically a dicotyledonous stem is figured a leaf gap and iN Ha \ as ax l'IG. 63.—Synoptical diagram representing the transverse and longitudinal topography of the rays related to the leaves in species of Casuarina. Explanation in the text. peripherally its subtending leaf. Between the two lies a corre- sponding ray of the aggregate type. It is to be noted here that there is a modification of the rate of growth of the annual rings FIBROVASCULAR TISSUES: RAYS 83 in the region of the aggregate ray which results in their being locally depressed. To the right is to be seen another leaf with its corresponding gap and ray. Im this case the ray structure where it is still near the leaf trace (solid black) is the same as in that just described, namely, aggregate. Farther out, however, the components of the aggregate ray, instead of maintaining their original relations to one another, begin to diverge in the tangential plane. At the same time | vessels which are conspicuous by their absence while the ray is in the aggregate condition begin to appear in the widening strands of wood which separate the diverging rays. This process continues and becomes more and more marked in successive outer annual rings. ‘The final result is that what was once a congery or aggre- gation of rays separated from one another by purely fibrous strands becomes a more and more diffuse cluster of rays separated by ever- widening vascularized intervals of wood. In this condition the original aggregation of rays not only becomes diffuse in a fanlike fashion in the outer region of the woody cylinder, but the individual rays subdivide, thus accentuating the condition of diffusion. The phenomenon of the subdivision of the rays for the sake of simplicity is omitted in the diagrammatic representation. It is clear that the appearance of the conditions depicted in the ray to the right of the diagram (at 6) in the case of all the foliar rays of a stem would result in a diffusion of rays of a medium breadth throughout the older wood—in other words, to the condition shown in Fig. 60 for the adult wood of Casuarina equisetifolia or an allied species. Turning now to the left of the diagram (at c), we observe a foliar or leaf ray of still another type. Here, as in the diffuse con- dition of the foliar ray represented in 0, the original state is that of aggregation with the exclusion of vessels, a situation which is per- manent in the type diagrammed at a. In the later annual rings in this type the aggregation becomes a homogeneous mass of paren- chyma by the disappearance of the fibrous strands which separate the components of the aggregation or congery from one another. Where the clusters become fused into large homogeneous bands of storage tissue by the parenchymatous transformation of the original separating fibers of the aggregation, the result is the compound ray 84 THE ANATOMY OF WOODY PLANTS represented at c in our diagram. This condition is present in the adult structure of the wood of Casuarina Fraseri, as is shown in Fig. 58. The primitive aggregate condition persists, on the other hand, in C. torulosa, as is shown in Fig. 59. 1 Naame i Fic. 64.—Diagrammatic representation of a twig of Picea canadensis. Explana- tion in the text. In the longitudinal aspect of the diagram presented to the reader are shown the vertical views of the three types of rays illustrated horizontally in a, 6, c. Fig. 63a’ shows the tangential topog- raphy of an aggregate ray. The clustering of the masses of radial FIBROVASCULAR TISSUES: RAYS 85 parenchyma and the exclusion of vessels can be readily seen. At b’ is indicated the tangential projection of the diffuse condition of rays. Here the original cluster has become scattered and vessels are now present among the rays. In c’ is shown the longi- tudinal tangential aspect of the compound ray—that is, the con- dition in which the original aggregation has become fused into a large solid mass of radial parenchyma. The conditions in a diagram of a coniferous stem in three dimensions may now be dis- cussed. Fig. 64 illustrates the topography of .a two-year-old twig of Picea canaden- sis. In the trans-: verse aspect the pith surrounded by xylem, phloem, and cortex can be distinguished. Projecting from the surface are the leaves or their bases. The outline of the pith is indented by a num- ber of bays, which are the deeper the nearer they are in the vertical plane to the departing trace of a leaf. In relation to one of these on the side of the pith nearer the observer is an actual trace running horizontally in the wood. The transverse aspect of the wood shows the presence of numerous narrow rays. The face of the stem facing the observer is cut away to show the topographical relations of the leaf traces in the wood. It is clear that, contrary to the conditions observed in the stem of Casuarina diagrammati- cally represented in Fig. 62, there are no modifications in the grouping of the rays or in other features with reference to the foliar traces (appearing as oval dots). Fic. 65.—Transverse section of a twig of Casuarina Fraseri 86 THE ANATOMY OF WOODY PLANTS It will be advantageous as a sequel to the representation of the prominent types of rays in the dicotyledons in diagram to view them in actual photographs in the case of the genus Casuarina. We may profitably begin here, as in the case of the diagrams, with transverse sections. Fig. 65 reproduces the cross-section of a small twig of Casuarina Frasert. The leaves are in the main still present in depressions on the surface of the stem and clearly sub- tend the foliar rays. Rather nar- row leaf gaps pene- travertine ins § annual ring and are twice as numer- ous as the append- ages at a given node (that is, there are twelve gaps, although only six appendages). This duplication of the gaps is due to the fact that the whorls of leaves alternate at differ- Fic. 66.—Part of transverse section of a twig of Casuarina Fraseri more highly magnified. ent nodes, and the gaps correspond- ing to these are persistent, with the natural result of gaps twice as numerous as the appendages. Fig. 66 shows part of the foregoing much more highly magnified. At the top is a persistent leaf and in the middle line below lies the pith, which is sending off an extension, the leaf gap; and this, on reaching the second annual ring, undergoes considerable enlargement. Between the wide termination of the leaf gap in the beginning of the second annual ring and in line with and subtending the leaf on the outside of the stem lies the foliar ray. The magnification is not sufficient in the figure to show the organization of the leaf ray; hence a more enlarged representation is introduced in Fig. 67. Here it is clear FIBROVASCULAR TISSUES: RAYS 87 that the structure of the ray in the twig in C. Fraseri is different from the adult condition, shown in Figs. 58 and 63, for in the younger axis the ray is obviously penetrated by fibers, and these are absent in the adult. The truth of this statement will become still more apparent by reference to Fig. 68, which reproduces the tangential aspect of the wood in a somewhat older branch of the same species. The prominent mass of radial storage tissue in the center is the foliar ray. It is dis- tinctly fibrous and is consequently still in the condition of aggregation. As the stem thickens the fibers are grad- ually transformed into parenchyma- tous elements more and more like the cells: of “the ray. Thus it is that the compound ray of C. Fraserit comes into being. It is 3 A Fic. 67.—Portion of Fig. 66 still more highly magni- evident that its fied to show organization of the foliar ray. Explanation early condition is __ in the text. one of aggregation, and that this is followed by a gradual transformation into the compound state by the fusion of the originally separate members of the aggregation. The photographic representations lead likewise to conclusions in harmony with the diagrammatic figures in the case of the diffuse condition of the foliar ray. It will not be necessary to introduce a total general and a partial more detailed view of the twig in this instance, since the topographical relations are practically the same as those shown in the case of C. Fraseri. Fig. 69 illustrates the situation in the diffusion of the foliar ray as exemplified by 88 THE ANATOMY OF WOODY PLANTS C. stricta. It is evident from the photograph that a mass of ray tissues on the left (representing the end nearer the pith), charac- terized by moderate breadth and the absence of vessels, passes toward the right (outer side topographically) into a continually widening fanlike cluster of rays among which vessels become more and more prominent. Fig. 70 shows a tangential, longitudinal section of the wood in a small branch of C. equisetifolia. Here is present an aggrega- tion of rays, foliar in its character, which as yet has scarcely begun to diverge into the diffuse condition and consequently includes no vessels a ° ees te oe as +. &@ fi ol an t 4 ers om —" ee Orr” @eecoere in its substance. C.SinicteranduG: equisetifolia are both species with the diffuse type of ray in the adult wood. C. stricta has been chosen to younger stem of Casuarina Fraseri, showing aggregate illustrate the trans- condition. verse aspect of the Fic. 68.—Tangential section of a large ray in the diverging rays in the diffuse type only because the larger size of the radial bands in this species make the topographical relations more obvious. The difference in gross appearance between stems with aggre- gate or compound rays on the one hand and diffuse rays on the other hand, is very striking. This is well illustrated by Fig. 7oa. On the left is seen a polished segment of the trunk of C. Fraseri (compound and aggregate rays). On the right appears a polished trunk of C. séricta (diffuse rays). Here the rays are at first distinct and later die out. The conspicu- ous stage is aggregate, while that representing the disappearance FIBROVASCULAR TISSUES: RAYS 89 of noteworthy bands of radial parenchyma marks the diffuse condition. It has been demonstrated in the case of Casuarina that there are three main types of radial parenchyma in the secondary wood —namely, the aggregate, the diffuse, and the compound. Of these three types the aggregate is manifestly the oldest, and the other two have originated from it by divergence in the diffuse Fic. 69.—Transverse section of aggregate rays diverging into the diffuse condi- tion in Casuarina stricta. condition and by fusion in that state designated compound. What is diagrammatically clear in Casuarina for the radial paren- chymatous structures is much less obvious in most other dicotyle- dons, and in no case are the relations so well shown as in the genus named. Among arboreal forms the oak is of interest in exhibiting both the aggregate and the compound condition of the rays. In this genus the species occurring in warm regions are ordinarily characterized by the possession of clustered or aggregate large rays in contrast to the uniseriate or linear rays present in the mass of the wood. In species of northern climates the rays are solid or compound in their nature, but even here the condition of aggregation go THE ANATOMY OF WOODY PLANTS is found in the young plant as a passing phase and as frequently persisting for many years in that most conservative of plant organs, Fic. 70.—Tangential section of young twig of Casuarina equisetifolia, showing an aggregate foliar ray in center flanked on either side by uniseriate rays. the root. In the Betu- laceae, by contrast, the diffuse type of wood ray prevails, and it is likewise clearly derived from a primitive state of aggre- gation. In the birch, for example, diffuse rays more usually distinguish the stem, while the aggre- gate type is often found present in the case of the root. The general ana- tomical conditions as well as experimental data in the Fagaceae and Betu- laceae justify the conclu- Fic. 7oa.—Photographs of transverse views of polished stems of Casuarina stricta (right) and Casuarina Fraseri, showing the general topography of diffuse and compound rays. The diffusing rays of C. stricta appear to die out, while the rays of the other species become not only accentuated but also clearly more numerous. FIBROVASCULAR TISSUES: RAYS gI sion that wherever the compound or diffuse types of rays are present in members of these groups they have been derived from an earlier condition of aggregation. The type of ray structure is not strictly related to any particular organization of the flower, since amentaceous, archichlamydeous, and metachlamydeous fami- lies present to an almost equal extent the various categories of rays. Ina general way it may, however, be stated that the diffuse condition of the rays is characteristic of arboreal forms, while the compound condition occurs mainly in vines and herbs. CHAPTER VII THE FIBROVASCULAR TISSUES: SECONDARY WOOD—VESSELS The vessel is an element of structure which in the higher forms and in the secondary wood is of extremely great evolutionary importance. Before we take up this type of ligneous element in the seed plants it will be well to consider its occurrence in lower forms and in the primary wood. It was pointed out by De Bary many years ago that many of the scalariform tracheids of the bundles in the bracken fern are of the nature of vessels, using that term to apply to elements which are not merely pitted but actually perforated at the ends, thus permitting a much more ready passage of water. The statements of the distinguished anatomist of Strassburg have been confirmed and denied by more recent inves- tigators, but there seems to be no doubt whatever on the basis of our improved technique that he was in every respect correct. Fig. 71a illustrates the organization of a vessel in Pteris aquilina isolated from the surrounding tracheids by maceration. It is clear that the scalariform bars are separated from one another by wider intervals at the ends of the element and that the bars them- selves are considerably more slender in this region and are not distinguished by as pronounced overhanging margins as is the case in the similar structures on the lateral walls. In 6 is represented a profile view of the terminal inclined wall of the tracheid, indicat- ing plainly the absence of the membrane which characterized the lateral scalariform pits. Further, the margin or border in the case of the terminal open pits is slightly developed in comparison with that of the lateral pores with membranes intact. Conditions similar to those found in the bracken appear in many other repre- sentatives of the Filicales and are by no means confined to the Polypodiaceae, which at the present time not only are the largest, but also are considered in many respects the most specialized family of the group. Elements resembling vessels in the presence of terminal perforations have likewise been described for the genus Q2 FIBROVASCULAR TISSUES: VESSELS 93 Selaginella among the lycopodineous forms. It is thus clear that, so far as the primary structures of the wood are concerned, vessels are present even in the case of representatives of the lower vas- cular plants. Although in certain ferns and lycopods structures occur which, physiologically at any rate, represent vessels, these cannot be regarded as quite on the same morphological and evolutionary footing as the ves- sels of the highest gymnosperms and the angiosperms. ‘The step from a tracheid to a vessel, where all the tracheids are scalariform, as is the case with the tracheids of ferns and lycopods, is a much shorter one than when the fibrous elements are pitted and not scalariform. We find as a consequence that, although ves- sels or elements which have been regarded as such occur low in the scale of the Vasculares in the primary structures, they make their appearance in the secondary wood only in the higher representatives of the seed plants. The secondary wood of the extinct Paleozoic arboreal cryp- togams, although often perfectly preserved, in no authentic instance has yet revealed ele- Fic. 71.—Face and profile views of the type of vessel found in the primary wood of the bracken. \ ments which may with any degree of propriety be designated as vessels. The same situation obtains in the case of the lower 94 THE ANATOMY OF WOODY PLANTS gymnosperms and even in the higher representatives of the group as far up as the conifers. Fic. 72.—Smaller and larger vessels of Ephedra. the angiosperms, as will It is in the Gnetales, the most advanced forms among the naked-seeded Spermo- phyta, that vessels first make their appear- ance in the cylinder of the secondary xylem. Fig. 72a represents a smaller ele- ment of this type from the wood of the genus Ephedra. The walls terminating the structure under discussion are dis- tinctly at angles to the lateral ones and are remarkable for the extremely large pits which cover their surfaces. The pits of the terminal walls are not only very much larger than the lateral pits, but, with two or three exceptions, they have lost their membranes. In the pores where the membranes still persist a well-marked © torus reveals its presence in face view. The pits of the lateral walls of the tra- cheids in the case of Ephedra are not very much narrower than those of the terminal surfaces, but invariably are closed by membranes thickened centrally by a well- marked torus. Fig. 725 shows a some- what larger vascular element from the wood of Ephedra, which has its enlarged terminal pit entirely perforate as a result of the complete disappearance of the mem- branes. In Fig. 73 is shown a vessel in which, as an exceptional condition for the genus under discussion, there is a tendency to fusion on the part of the enlarged termi- nal pit. Although in the Gnetales the phenomena of fusion of the end pits of the vessels is rare, it becomes the rule in be shown at a later stage. At a appears a vessel which is transitional from an element of this type to a FIBROVASCULAR TISSUES: VESSELS 95 tracheid. It is distinguished by the fact that its end walls do not make a definite angle with the lateral ones but taper grad- ually. It is further peculiar in the circumstance that its terminal pits are imperforate with one exception and have their mem- branes marked by the presence of a very distinct torus. In ¢ is figured a tangential view of a vessel in Ephedra, showing the enlarged terminal pores in profile and making it clear that in this case, as in Pteris aquilina, the vessels become patent by the dis- appearance of the membranes of the pits. The organization of the © a A Oo} _© Cc Fic. 73.—Vessels of Ephedra (after Thompson). Explanation in the text tracheae or vessels in the two remaining genera of the Gnetales— namely, Welwitchia and Gneéum—is not essentially different from that described for Ephedra, and consequently need not be considered here. The Gnetales as a whole are distinguished, not only by the presence of vessels in their wood, but by the possession of rays of the angiospermous type, as has been indicated in the preceding chapter. The angiosperms are characterized throughout by the presence of vessels, generally of a high type, but in some cases showing clear indications of derivation from tracheids. It is only in certain xerophytic genera among the Magnoliaceae and in certain Cactaceae and Crassulaceae that these characteristically angiospermous 96 THE ANATOMY OF WOODY PLANTS elements are absent in the dicotyledons. No case is at present known of their default in monocotyledons. There are two main modifications of vascular elements or ¢racheae in the angiosperms— namely, vessels with scalariform perforations and those with Fic. 74.—Vessel from Alnus, showing the scalariform type of perforation. porous perforations. The term perforation is applied to the actual apertures which make their appearance in the terminal or other walls of typical vessels. The first-named condition of perforation is characteristic of lower groups and lower genera among the dicotyledons, while the second is usually found in the case of the higher orders (the Compositae, for example) of the dicotyledons and seems to be universal for the monocotyledons. In Fig. 74 is represented a vessel of the lower type—that is, one in which the perfora- tions in the terminal wall are scalariform. This is an element from the root of the alder. The lateral confines of the vessel are covered with small bordered pits which in this particular case are arranged in a somewhat regularly banded fashion as a result of the contact of the con- ducting element under discussion with the cells of a ray of the wood. If the relation had been with tracheids or other vessels, the arrangement of the pores would not be so regular. Pits are clearly seen in profile on the sides of the vessels, indicating the fact that water-conducting ele- ments belonging to this category do not neces- sarily have their lateral pitting confined to the radial walls. The ends of the vessel are strongly inclined and are manifestly at definite angles to the lateral walls. The illustration presents the vascular element from the radial view; hence it is obvious in this case that the perforated end walls are radial. This is a situation seldom departed from in the woods of dicotyledonous trees. In other words, a radial section of a dicotyledonous wood FIBROVASCULAR TISSUES: VESSELS 97 ordinarily reveals the face view of the characteristically perforated terminal walls of the vessel. We find that it is distinguished by the presence of open slits which are in general without borders and by smaller or larger clearly bordered pits. The latter structures retain their membranes and, where they become extremely elon- gated, are clearly the result of the fusion of two or more horizontally approximated bordered pits. Fig. 75, which represents part of the termi- nal wall somewhat diagram- matically and on a larger scale, shows the mode of fusion of pits and also shows that the final result of this process, when a number of horizontally seriate pits are concerned, is the formation of an elongated slit which reveals its primitive nature only by the retention of bor- ders at the ends. The slit as a whole not only has lost its Fic. 75.—Diagram showing the origin ; z of scalariform perforations by the fusion of borders, but likewise the mem- pits in the end wall of the vessel. brane of the row of fused pits has disappeared. It is thus evident that the slits which occur between the horizontal bars of the lattice work in the terminal walls of a vessel of this type are the result of the fusion of rows of pits, accompanied by a simultaneous loss of pit membranes. Before we leave the subject of the mode of origin of the per- forations which characterize the terminal walls of vessels of the lower type in the angiosperms it will be well to discuss the situa- tion in another group which shares with the true Amentiferae in the minds of students of evolution the claim to be primitive repre- sentatives of the dicotyledons. In Fig. 76a is shown a vessel from the root of Liriodendron Tulipifera. In this instance there is no sharp differentiation between terminal and lateral walls, although in general in the genus such a distinction is clearly present. In 98 THE ANATOMY OF WOODY PLANTS passing from the upper part of the figure downward there is a transition from bordered pits arranged in horizontal rows to per- forations of somewhat larger dimensions which are obviously derived from bordered pits by the disappearance of borders and membrane. The truth of this statement can be inferred from the fact that some of the perforations still retain more or less of the original bordered condition, particularly along their lateral margins. Fig. 76) shows another vessel from the root of the same Fic. 76.—Vessels from root of Liriodendron Tulipifera (a and b); c, vessel-like elements formed after injury in the non-vascular magnoliaceous genus Drimys. genus in which the situation is somewhat different. Here the pits are scalariform, as in the tracheary elements of the Pteridophyta, but with an important distinction which is not always kept in mind in evolutionary speculations. In the ferns and allied forms scalariform elements are a primitive feature of organization of the wood, while in the secondary wood of the angiosperms the scalari- form sculpture of the lateral walls is an exclusive feature of the vessels and is the result of the lateral fusion of horizontal rows of pits and consequently cannot in any way be regarded as a primitive condition of structure as in the lower forms. Proceeding from top to bottom, as in a, we find in this case the same loss of borders and membranes leading to the appearance of perforations of the scalariform type. The structure in question, in fact, exactly FIBROVASCULAR TISSUES: VESSELS 99 simulates the vessel of Pteris aquilina figured in connection with an earlier paragraph. Although the result is the same, the manner ° of reaching it is different in the two cases, and a distinction should of course be made in drawing any evolutionary conclusions. It will be clear to the reader from the evidence presented in the present and in a former paragraph that the vascular structures of the lower dicotyledons do not originate as in the Gnetales simply by enlargements of pits and the disappearance of the pit membranes in the terminal regions of the vessels. On the contrary, they typically take their origin as a consequence of the lateral fusion of horizontal rows of pits with a correlated disappearance of the membranes. ‘The vessel in the lower angiosperms is, however, as clearly a derivative of the tracheid as it is in the case of the highest of the gymnosperms. Further, in the angiosperms the vessel or trachea, as a result of its much more complex mode of evolution, is more distinct from the fibrous or tracheary element than it is in any of the lower groups. The type of vessel characteristic of the higher dicotyledons and the mass of monocotyledons may now profitably occupy our attention. Fig. 77 illustrates three vessels belonging to the category of elements with porous end walls (that is, vessels with so-called porous perforations). In @ is shown such an element from the oak in approximately radial aspect. The terminations of the vessel taper and are distinguished by the large aperture or pore. The lateral surfaces are covered with pits, which are of two kinds. The smaller ones, provided with a distinct border, put the vessel in relation with other similar structures and with tracheids. The simple and slightly irregular pits represented in about the middle horizontal region indicate the presence of a small ray in contact with the vascular element. In 0 is represented a vessel from the wood of the poplar in radial view. The same slanting ends and large terminal pores as are present in the oak similarly characterize the vessel of Populus. The uniform crowded lateral pitting indicates that the face of the vessel presented to the observer was in contact with another vessel. Inc is presented the somewhat tangential view of a vessel in the maple. The ends of the vascular element do not differ essentially from those of the oak and poplar. 100 THE ANATOMY OF WOODY PLANTS In this case the wall to the left has been in contact with a ray, as evidenced by the grouping of the pits. The region of the lateral wall to the right has been in contact with another vessel and is ay ww 9 Le) 989 9 QO 9 §, Lolo) O Loo oO 0 0 Oo o® Wy Y\O 0 XS 0 00 po © \O\g\9 Q\VN o6\s WOW \Y WS) O® / 0 Fic. 77.—Various types of vessels in the dicotyledons. Explanation in the text conspicuous, not only by reason of the characteristic arrangement — of the pits, but also by the presence of a somewhat spiral internal sculpture, the so-called tertiary thickening, which always marks (when present) the contact or “party wall’ between vessel and vessel. Those surfaces of the vascular element which are in contact FIBROVASCULAR TISSUES: VESSELS LOL with the libriform fibers are devoid of both pits and spiral internal sculpture. It will be profitable to consider next the type of vessel charac- teristic of the older wood of the stem of Lirioden- dron. ‘This category of vessel is covered with pits in horizontal rows, indicating contact with another vascular element. Below and above the sharply sloped end walls are seen; these are neither porous, as in the case of the vessels of the last figure, nor marked by the simultaneous presence of narrow scalariform perforations and bordered pits, as in the rootwood of Magnolia and in the general secondary wood of many of the Betu- laceae, etc. The terminal apertures of the vessel, in fact, are crossed by a few remote bars. The type of vascular element characteristically present in the old wood of Liriodendron serves, indeed, as an intermediate stage between the vessel with true scalariform perforations and that with porous terminal apertures. The truth of this assertion becomes manifest from a consideration of Fig. 79, which represents vascular structures from the wood of the high blue- berry, Vaccinium corymbosum. In a, 6, and ¢ are shown successive transitions from end walls with many pits and few narrow scalariform perforations to fewer pits and more scalariform apertures, and to a third condition where the pits have dis- appeared and only somewhat wide scalariform Openings remain. In d and e. appear further stages in which the bars separating the terminal large slits become fewer and more degenerate until finally a simple porous condition is reached. It is Fic. 78.—Ves- thus clear that the vessel with porous perforations sel from the stem - , A A of Lirtodendron. is a further elaboration of that with scalariform perforations, just as this in turn has taken its origin from a vascular element with pitted perforations of the nature found in the Gnetales. 102 THE ANATOMY OF WOODY PLANTS The hypothesis that the scalariform vessel is the forerunner of the porous one is also confirmed by a consideration of the first-formed region of the woody cylinder. In the oak, for example, as well as in many other instances, although vessels with porous terminal apertures are characteristic of the mature wood, elements of vascular nature with scalariform perforations are commonly present in the first annual ring, particularly in the vicin- ity of the protoxylem. It is thus evi- dent that the vascular structures in dicotyledonous woods supply a valu- able argument for the general validity of the hypothesis of organic evolution. The lateral walls of the vessels may next receive further considera- tion. It has been indicated in a former paragraph that the side walls of a vessel have their sculptural features largely determined by the nature of the adjacent cells of the wood. Where vessels are in contact with rays, the communicating pits are characterized by a grouping and seriation corresponding to the outlines and direction, whether transverse or SE longitudinal, of the ray cells. Where Fic. 79.—Vessel of Vaccinium the relation is with other vessels or corymbosum, illustrating the with true tracheids, the pits are origin of the porous type of a y di perforation from the scalariform. numerous and likewise arranged In a Explanation in the text. somewhat definite manner. If merely mechanical elements abut on the vascular walls, pitting is quite absent. Further, if so-called tertiary spirals are present on the inner side of the walls of the vascular elements, these are confined to those vertical regions in contact with other vessels or with tracheids. FIBROVASCULAR TISSUES: VESSELS 103 Where vessel comes in contact with vessel, we find frequently a mode of pitting characteristic of a genus or even a family. Details in this connection are beyond the range of a work so elementary as the present one, but a few prominent features may be indicated. As has been shown in the figure of the vessel of Liriodendron above (Fig. 76), lateral pits may be in horizontal rows. In other instances, as in the oak shown in Fig. 80a, the lateral pits are arranged in an alternating fashion. Again, in 8, representing the lateral pitting of the vessel in the poplar, alternation is accompanied by crowding to such an extent that the pits become angular by mutual contact. OZEOLS6] |18eesexe, | SS Ox© QOLEX OGOSO| losseses ee) 252 SOes] | SS OO XO} SSL OC] IELSZOLS S55 Fic. 80.—Lateral pitting of vessels of dicotyledons. Explanation in the text In ¢ is shown the characteristic pitting of the vessels of the vine family (Vitaceae). Here the sculpture of the lateral walls consists of elongated slits closed by equally elongated membranes. A reference to the structure of the secondary wood in the region of the pith in this instance makes it clear that the slitlike pits of the Vitaceae are not persistent scalariform pores of the first-formed region of the xylem, but are the result of the lateral fusion of horizontal rows of pits in the side walls of the vessels. In d is represented a condition of structure of the vascular wall which is common in the higher types of dicotyledonous woods. Here the alternating pitting is overlaid internally by spiral structures which it is customary to call tertiary thickenings. In concluding the statements in regard to vessels it is necessary to refer to the phenomenon of tylosis or occlusion of the lumina or cavities of the vessels by parenchymatous ingrowths. These 104 THE ANATOMY OF WOODY PLANTS structures originate under various conditions, but are more usually found in connection with those changes which precede the trans- formation of sapwood, or alburnum, into heartwood, or duramen. As the living cells in proximity to the vessels (whether they belong to the radial or vertical systems of storage tissues appears not to a =) ra) ian) “| — Fic. 81.—Tyloses in oak and locust. Explanation in the text be of importance) are about to die, they push processes into the adjacent vessels by the bulging and growth of the cellulose mem- branes of the pits connecting them with the vascular structures. These ingrowths are occupied by protoplasm and, sometimes at any rate, by nuclei as well. When abundantly developed, they completely close the lumen of the vessel and render impossible the passage of water. Fig. 43, on page 157, has made clear the contrast resulting from this phenomenon in the sapwood and the heartwood FIBROVASCULAR TISSUES: VESSELS 105 of the oak. In Figs. 81a and 6 is shown the phenomenon of tylosis in the vessels of the white oak. In this species all the larger vessels are more or less completely occluded | by tyloses extending from and only excluding the latest complete annual ring. Inc and d a similar condition is represented in the case of Quercus Engelmannt. In this instance the tyloses have developed a very thick and strongly pitted wall, a condition more rarely found. In e and f tylosis as found in the case of the black locust, Robinia Pseudacacia, is represented. Here the ingrowths derived from adjoin- ing parenchyma cells are very numer- ous and form a mass completely occluding the cavity of the vessel. In Fig. 82 are seen, both in transverse view, earlier stages of the invasion of a vessel in the oak through the agency of tyloses. The representation in this a Fic. 82.—Diagrammatic representation of the process of tylosis. illustration is somewhat diagram- matic to show more clearly the entry of the ingrowths through the medium of the pits in the walls of the vessels. The phenomenon of tylosis is in all probability an extremely ancient one for the higher plants, as it is found far back into the Fic. 83.—Tylosis in tracheids of Liquidambar. 106 THE ANATOMY OF WOODY PLANTS Mesozoic. It is not confined by any means to vessels and even occurs rarely in the tracheids of dicotyledons. Fig. 83 shows the presence of tylosis in the fiber-tracheids of the sweet gum (Liquid- ambar styraciflua). The heavily outlined bodies in the cavities of certain of the fibrous elements are of the nature of tyloses. Similar conditions have been found in the case of other dicotyledonous woods. It has been made clear in an earlier chapter that ingrowths resembling tyloses occur in the resin canals of the pine in the region of the heartwood. Occlusion by means of parenchymatous inva- sions is, however, not confined to the resiniferous spaces in the genus mentioned. In the roots and likewise in the cone the tra- cheids of the wood often show themselves occluded by ingrowing parenchyma cells. Such conditions are not normally found in the vegetative stem of living pines, although they are known to occur in the branches of cretaceous Pityoxyla from the Eastern United States. CHAPTER. VIII THE FIBROVASCULAR TISSUES—PHLOEM The ligneous or woody tissues which have been discussed under various headings in previous chapters are of great importance on account of their conservatism. They manifest a high degree of differentiation and are also important by reason of the fact that their relative imperishability has resulted in their being abundantly preserved as fossils from the most ancient times to the present. Woods consequently furnish on the whole the most important historical document in favor of the hypothesis of evolution, and those who are interested in the doctrine of descent as applied to the case of plants cannot afford to neglect the investigation of the ligneous tissues of the vascular plants. The situation for the plants provided with tracheary tissues is, in fact, very different indeed from that presented by the lower vegetable organisms, where evolutionary data are necessarily largely speculative and experi- mental. Invariably associated with the woody tissues are those of the phloem. The primal function of the woody tissues was appar- ently to conduct water into the superior or outlying parts of the plant. To this function have been superadded in the long course of geologic time, as pointed out in preceding chapters, the functions of strength and storage, with corresponding and appropriate modifications of structure. Just as the wood in the first instance served the purpose of the movement of water from the soil, so the primal condition of the tissues of the phloem was that of conducting the elaborated foodstuffs manufactured in the leaves to other parts of the plant where they are either utilized in the processes’ of growth and respiration or stored up as reserves. The primitive type of phloem, as that of xylem, appears to have existed in the case of the lepidodendrids. Its structure has not been satisfactorily preserved in these primitive vascular plants, and there is some difference of opinion as to interpretation. Some investigators have expressed the opinion that no true phloem is 107 108 THE ANATOMY OF WOODY PLANTS present in these ancient organisms, while others have contended for a very simple type of organization in the arboreal club mosses of the Paleozoic age. In view of the differences of opinion and the uncertainty of the data in the case of the phloem of Paleozoic Pteridophyta, it will be well to confine our attention in this instance to the living representatives of the fern alliance. Fig. 84 shows the detailed organization of one of the fibro- vascular strands of the bracken Pteris aquilina. The bundle as a Fic. 84.—Bundle of Pteris aquilina. Explanation in the text whole is clearly limited by a dark uniseriate layer, the endodermis, which is ordinarily interpreted as the innermost layer of the funda- mental tissues in juxtaposition to the fibrovascular system. Within the endodermis is situated a layer one or sometimes two cells in breadth, the pericycle, which constitutes the external boundary of the fibrovascular tissues, just as the endodermis marks the internal limit of the fundamental system. Next to the pericycle are certain extremely minute, apparently empty, cells, the first- formed elements of the phloem, or, as they are technically desig- nated, the protophloem. Next inward lie storage cells, nucleate FIBROVASCULAR TISSUES: PHLOEM 109 and more or less loaded with starch. These are the parenchyma of the phloem. We are not acquainted with the origin of paren- chymatous cells in the phloem for reasons indicated at the outset of the present chapter. Farther inward lie the larger conductive elements of the phloem, known as the metaphloem. These are cells which have no contents but a delicate lining of protoplasm, and this does not appear in the illustration. The elements under discussion as well as those of the protophloem are known, on ° account of certain structural features to be described later, as sieve tubes. It is important to note in the present connection that sieve tissues do not present the variety of modes of development which characterizes the xylem. Almost invariably in this cate- gory of tissues the first-formed elements are external and those of later appearance are laid down in centripetal order. As a con- sequence the terms exarch, mesarch, and endarch, which are so sig- nificant in connection with the development of the primary wood, have little bearing in the case of the sieve tissues. Internal to the larger sieve elements of the metaphloem lies a more or less continu- ous band of parenchyma, separating the phloem from the xylem. The tracheary elements of the wood are individually more or less completely surrounded with parenchyma. ‘The phloem does not form a continuous band about the xylem, but is interrupted at the two ends of the elongated mass of wood. In certain ferns the tissues of the phloem occur only on one side of the bundle, in which case the strand of fibrovascular tissue is known as collateral. Where the phloem forms a complete jacket about the xylem the condition is known as concentric; and where, as in the bundle appearing in the figure under discussion, the sieve tissues are confined to two opposite sides the condition may be designated as bicollateral. In Fig. 85 is represented a longitudinal view of part of the same bundle. The sieve tubes now appear as elongated cells with tapering ends and sculptured walls. The relief of the walls consists of somewhat angular crowded areas, although on the whole they are tolerably evenly distributed. These areas are per- forated with very small simple pits and are the sieve plates. It is these structures which give to the sieve tube its name. After the characteristic elements of the phloem have reached a certain age 110 THE ANATOMY OF WOODY PLANTS their pores become more or less completely occluded by slimy plugs known as callus. The details of origin and the significance of this substance are not fully understood and from the standpoint of the present statement are of relatively little importance. In Fig. 86 is re- produced a photo- graph of the wood and inner bark of the pine. The xylem is clearly very regular in its structure and consists of a series of annual rings, the organization of which has been dealt with in a preceding chap- ter. In contrast to the persisting regu- larity of the wood the phloem presents itself as a mass of tissue radially seriate only for a short distance outward from the cambium, or zone of growth. Externally Fic. 85.—Longitudinal view of part of a bundle its elements are of Pteris aquilina. On the left is shown a vessel, thrown into more or while toward the right and represented in black are 2 i less meandering lines sieve tubes. as a result of the col- lapse of certain of its constituent cells, which will be considered more in detail in the sequel. The section reproduced in the photograph under discussion was made from material secured in the winter period of rest. The uncollapsed part of the phloem corresponds to a single year’s growth, and all that region of the inner bark or phloem characterized by the meandering course of the rays is non- functional so far as the most characteristic elements, the sieve LAN FIBROVASCULAR TISSUES: PHLOEM III tubes, are concerned. Fig. 87 shows a highly magnified view of the region immediately outside and inside the zone of growth, or cam- bium. Internal to the active layer the wood is recognizable by its bordered pits. The initial region, known as the cambium, is dis- tinguishable by the richly protoplasmic character of its cells and their thin tangential walls, which are in contrast with the thick- ness of the radial boundaries. Ex- ternal to the cam- biwm ives the phloem, composed most characteristi- cally of somewhat rectangular cells, the sieve tubes. In these, unlike the cambial elements, there is no nucleus, and the scanty parietal proto- plasm presents likewise a striking difference from the Fic. 86.—Inner bark with cambium and adjacent richly protoplas- wood of the pine. mic cambial region. Scattered thinly through the phloem are a few rounded cells which contain protoplasm and grains of starch (represented black as if stained with iodine). The rays cross the longitudinal elements of the phloem, the sieve tubes, and the parenchyma cells at right angles and appear in the figure as single files running nearly straight for a short distance and then pursuing a meandering course outward. The cells of the two rays shown in the figure present a different appearance. In the file of radial parenchyma on the right the elements are filled with protoplasm and show the presence of a nucleus. In addition, a considerable amount of starch is present in the form of grains tinctured black by iodine. It is clear that the cellular elements of the ray to the right continue elements r] ip Hi ne ir] ¢ SS Lo THE ANATOMY OF WOODY PLANTS 112 —S (ki. 3) — j ra Fic. 87.—Transverse section of xylem, phloem, and cambium of the pine, more highly magnified. Explanation in the text. FIBROVASCULAR TISSUES: PHLOEM 113 of a similar nature in the portion of the ray contained in the wood. If we now turn our attention to the ray on the left, a somewhat different situation is presented to the eye. Here the cells are entirely without starch, although they still show protoplasm and a nucleus. Internally they are in line with the marginal tracheids of the ray in the wood, which have been described in an earlier chapter. Obviously there are two categories of cells in the rays of the phloem in Pinus, just as has been shown to be the case for the radial parenchyma of the xylem. It will now be con- venient to consider the relations of the various elements of the phloem to one another. In this connection we may first discuss the sieve tubes. It will be noticed that there are certain dark lines stained with iodine occurring in groups on the radial walls of the sieve elements. These are the transverse sections of sieve pores. Parenchymatous cells of the phloem have no intimate relation to the tubes, as no pits facilitate interchanges between the two types of elements. The same statement holds in regard to the cells of the ray shown on the right side of the figure. On the left, however, the elements of the ray are clearly related to the sieve tubes by means of sieve plates, distinctly differentiated on the side of the sieve tubes, but not well developed on the side of the ray. It is evident that there is a specially intimate connection between certain ele- ments of the ray, which are contrasted with the remaining constitu- ents by the absence of starch, and the conductive elements of the phloem or sieve tubes. If the organization or, more correctly, the disorganization of the phloem is followed more externally, it will be observed in the illustra- tion that the ray on the right continues to retain its protoplasmic contents and its grains of starch, while that on the left has entirely lost its living contents. A further feature of the phloem as repre- sented in the external region of the figure is the distortion and final collapse of the sieve tubes, preceded by the loss of the delicate pro- toplasmic lining surrounding the inner walls of these elements. The parenchymatous cells retain their integrity in the collapsed region of the phloem, precisely as is the case with the ray indicated on the right of the figure. Another feature of the disorganization of the phloem is the appearance of large masses or plugs of material, 114 THE ANATOMY OF WOODY PLANTS appearing black in the figure, which are present exclusively on the radial walls of the elements, although in some instances the col- lapsed state of the tubes gives rise to the appearance of a tangential position for the bodies under discussion. The plugs mentioned above constitute the callus, a substance which in the conifers and the great majority of seed plants higher in the scale makes its appearance on the sieve plate at the time the tube is in the initial stages of collapse. The callus completely blocks the pores of the sieve plate and, after persisting for a short time, disappears, leaving the pores of the sieve area quite open. It is also apparent that in the case of the ray cells on the left of the figure the callus present is unilateral and occurs only on the side of the sieve tube. Obviously the type of ray element appearing on the left in the illustration is definitely related in its duration to the life of the sieve tube, and both structures cease to be functional at the same time. In the next figure (Fig. 88) the radial aspect of the phloem is shown. Here the ray naturally appears in longitudinal section. Above and below in the region of the phloem it shows vertically placed cells which contrast in the position of their axis of greatest length to the central elements of the radial parenchyma. These so- called “erect cells”? correspond to the elements shown in the ray to the left of Fig. 87 and are similarly characterized by the absence of the starch, which is a feature of the contents of the central or prone cells of the ray. In passing toward the right from the cam- bium the protoplasmic filling of these elements becomes less abundant, until finally, where the callus presents itself in face view, it disappears altogether, in this respect presenting a con- trast to the central cells which retain their protoplasm and starch indefinitely. The sieve tubes.now appear in longitudinal view, and nearer the cambium they have a delicate protoplasmic lining often containing some small grains of so-called transitory starch. The sieve areas, or sieve plates, are presented to the observer in face view, and toward the extreme right callus plugs occlude their pores and at the same time the tube has lost its living contents. It is clear in the radial view, as in the transverse, that sieve tube and marginal erect cell cease to exist and develop callus plugs FIBROVASCULAR TISSUES: PHLOEM ELS simultaneously. A single row of parenchymatous elements is represented as crossing the axis of the ray. To the left of the cambium lies the wood with its tracheids and the continuation of the ray. The radial structures in the xylem show also a differentia- tion into central and marginal cells, but here ray-tracheids take the place of the erect cells of the ray in the phloem. Fic. 88.—Radial section through xylem, cambium, and phloem of the pine. Explanation in the text. In Fig. 89 appears the tangential section of the tissues of the phloem in Pinus. The plane of incidence of the section is tan- gentially slightly oblique; hence elements of different ages appear on the opposite sides. Toward the right are represented sieve tubes in which the protoplasmic lining has disappeared and the sieve areas (seen here in profile) are blocked by masses of callus. In the case of the rays which are naturally shown in transverse section the marginal or erect elements are calloused on the side of the tubes. The central cells of the rays still show the presence of 116 THE ANATOMY OF WOODY PLANTS protoplasm and starch. - In the middle region of the figure a file of parenchyma cells is present. To the left of the middle line the sieve elements show the delicate protoplasmic lining which char- acterizes them in the functional condition. The radial parenchyma is also entirely in a living condition, although the marginal cells are differentiated by the absence of the starch contents found in the Fic. 89.—Tangential section through the phloem. Explanation in the text central region of the ray structure. The callus in both sieve tubes and marginal cells is here conspicuous by its absence. A somewhat complicated condition of the phloem has purposely been chosen in the case of the coniferous gymnosperms, because there is good reason to believe that in this group, which is a decadent one, the more elaborately organized condition is antecedent to that marked by a greater degree of simplicity. On the whole, the pine and its allies represent the most highly differentiated structure of the phloem in the group. In the Cupressineae, Taxodineae, Araucari- neae, Podocarpineae, and Taxineae the radial structures of the phloem show a marked degree of simplification as compared with FIBROVASCULAR TISSUES: PHLOEM vs the pine family proper. It is not necessary in an elementary work like the present one to enlarge further on the organization of the phloem of the gymnosperms in general or the conifers in particular. The structure of the phloem in the angiosperms, and especially of arboreal dicotyledons, will next occupy our attention. Here the = \( ‘ % z i) Z ary Gr EC p° A a SSE S ees s NK | BEAT) ~ Mis! Gian = = (2g ey LS ZE \ TBA Fic. 90.—Transverse section of the xylem, cambium, and phloem in the American linden. Explanation in the text. general organization is quite different from that characteristic of gymnospermous groups and accordingly merits detailed considera- tion. Fig. 90 shows a transverse section of the region immediately internal and external to the cambium in the trunk of Tilia americana, the American linden or basswood. ‘Toward the lower side of the 118 THE ANATOMY OF WOODY PLANTS illustration appears the xylem, consisting of vessels, libriform fibers, parenchyma, and wood rays. Above the tissue so organized lies the cambium, or zone of growth, which alternately adds ele- ments to the structure of the xylem and that of the phloem. The latter tissue appears above the cambium. in the figure and outside it in the trunk of the tree. The preparation which served as the basis of the illustration was made from material secured during the period of winter rest. Next to the cambium lie fibrous and similar elements, to the abundant development of which in its inner bark the basswood (literally bastwood or tree useful for binding) owes its name. The fibers of the phloem are often called hard bast. Examination of the figure will show that the fibrous elements are separated from the cambium by a row of cells either quite empty or containing large crystals of calcium oxalate. These are the so- called crystallogenous cells and are very commonly present inter- nal to the zones of fibers or hard bast in the phloem of the form under discussion. External to the hard bast lies a zone distin- guished by the presence of cells either richly protoplasmic as to their contents or, in case the protoplasm is more scanty, characterized by relatively thin and unlignified walls. This region is the so-called soft bast and shows considerable complexity of organization. First taking the cells with abundant protoplasm, we see clearly that these can be divided into two categories—namely, those which contain grains of starch (represented in black as if treated with strong iodine solution) and those in which amylaceous substances are absent. The latter are further distinguished by their generally small size and somewhat triangular shape, due to the fact that they are usually accommodated in the angles of large thin-walled ele- ments with a delicate protoplasmic lining. The triangular cells are known as ‘“‘companion cells’? and are a constant feature of structure of phloem of the angiosperms as contrasted with the gymnosperms. The larger elements of the phloem with thin walls and scanty parietal protoplasm are the sieve tubes. In some in- stances the sieve plate can be seen in the transverse section repro- duced in the figure, and it is clear that its position is characteristically radial. Farther outward the densely filled parenchymatous cells of the soft bast give place again to the dead crystallogenous elements, FIBROVASCULAR TISSUES: PHLOEM 119 which are in turn followed by bast fibers. The rays of the phloem in the basswood and other dicotyledons show no special feature of interest, since they do not in any case manifest the intimate rela- tion to the sieve tubes described above in the pine. Soe We. eo oe % oh 4 a6 oe ¢ ete @- es ose Seeeery® Fic. 91.—Radial section of the xylem, cambium, and phloem of the linden, or basswood. Explanation in the text. In the next illustration (Fig. 91) the radial aspect of the phloem in Tilia is shown. Here the rays appear naturally in longitudinal section and are composed of heavily pitted cells containing dense protoplasm and much starch. Above the ray are represented the various elements of the hard and soft bast. On the extreme left 120 THE ANATOMY OF WOODY PLANTS are to be seen the summer elements of the wood in contact with the cambium. They are followed by parenchyma and by crystal- logenous cells, empty and heavily pitted on their horizontal walls. Next, the fibers of hard bast meet the view, and these pass in suc- cession into bast parenchyma, characterized by heavy pitting, abundant starch, and protoplasmic contents, and by sieve tubes of large lumen and scanty parietal protoplasm. Within, in the walls of the sieve elements, lie the companion cells, distinguished by their slender form and the absence of starch in their protoplasm. The sieve tubes in the radial aspect present to the eye strongly inclined end walls which may be compared with the similarly slanting partitions in the vessels of the wood. The sieve element is, in fact, the exact analogue of the vessel, and, just as the vascular elements in angiospermous woods play the main part in the trans- port of water, so the sieve tubes perform the principal réle in the movement of the elaborated organic stuffs from the leaves. Another feature of analogy between the sieve tube and the vessel is not only the more or less inclined terminal walls at angles to the lateral ones, but also the function of transport specially provided for in connection with the ends of the element. In the vessel this condition finds its expression in the develop- ment of scalariform or porous perforations and in the case of the sieve tubes by the appearance of particularly extensive and large- pored sieve plates on the terminal inclined walls; and these in highly specialized forms, such as herbaceous dicotyledons and monocotyledons, may be the only functional regions. Following the sieve tubes is a zone of bast parenchyma, succeeded in turn by another zone of crystallogenous cells and hard-bast fibers. In Fig. 92 is shown the tangential longitudinal aspect of the phloem in the basswood. Here the rays naturally appear in trans- verse section and are clearly of diverse sizes, but are all composed of strongly pitted cells containing abundance of protoplasm and starch. In this aspect the plane of section is purposely slightly oblique so as to exhibit all categories of constituents of the phloem at the same time. To the left lie crystallogenous cells near a large ray. ‘The ray is in contact on the opposite side with parenchyma of the soft bast. Then follow sieve tubes and their related com- FIBROVASCULAR TISSUES: PHLOEM 121 panion cells. In the tangential aspect the terminal sieve plate, since it is radial in position, is shown in profile. The protoplasm, present more densely in the region of the terminal plates, is pur- posely omitted in order that the sculpture of the lateral walls may 2 0°5%4000 Oe o¢ 39,0 o 2\ \o o 0\ \os as a 3 990, 0F 8 Gn ee 2% 0) 3 eo 5 Foor a 2 59, oS cy oo} | (2 e * So ag Bx) 0% Be 05? Ta e0) ° eZ “ 2 A °° =) rx 09) Le & ou a os Q PART. 6a 0 0°20 0 kao, Do Tip 250007028) PY | 1293 BO2™ 0% o2h0 BO0'00% 00 88% 0F E ge 205 Pp Dooe RS. poog oS a 0. : o - 2 a 09090% 9 00 °, A J ° 00; 0009 3 ° 3 p eof | fb 0.°d a 30% c 8, 8% 29,90 500 68-5 0°0 90 | 2° 90000 20008098 5 0 9909 30009) cos — S50, 0 2 00%o ‘On? of fPa20°, i200) \2 5 a 595.300] & TT Qu TT cS TTT] << i 6%] | [rarer QTM T_T TTS Q Zain ML FERS ay 6 Pr: 2 3 Fic. 141.—Diagram of stem of Labiatae. Explanation in the text as regards the presence of large foliar rays, elucidate the origin of the herbaceous type. The situation illustrated in Fig. 140 is not, however, by any means a universal expression of the topography in herbaceous stems. It will be well to show further possibilities in this direction by reference to a family of dicotyledons much higher in the scale than are the Rosaceae. In Fig. 141a is shown the perennial stem of the common garden sage, Salvia officinalis. The outside is covered with an armor of periderm within which lies the narrow cortex, Igo THE ANATOMY OF WOODY PLANTS in turn abutting directly on the fibrovascular cylinder. The latter is circular in outline and shows no variation of structure in different segments. In 6 an annual branch of the sage is diagram- matically represented so as to indicate the essential features of organization. The stem is now square in outline, as is the usual condition in herbaceous representatives of the Labiatae. It is to the flat surfaces of the quadrilateral stem that the paired leaves are attached. An examination of the fibrovascular cylinder shows that the uniformity of structure characteristic of the round peren- nial region is no longer present. Opposite the flat surfaces the cylinder is much thinned out, and vessels are conspicuous by their absence, except in small clusters marking the position of the leaf trace, which will pass outward at a higher node. Although the fibrous modification of the structure of the wood in relation to the foliar fibrovascular strands is found here as in the case of Potentilla and Alnus, it seems clear that we have to do with a less primitive phase of the origin of the herbaceous type. In ¢ is presented a diagram of the extremely herbaceous stem of Lamium album. The situation as regards flattening of the stem in connection with the quadrangular structure characteristic of the axes in the labiates is virtually the same as in the annual shoots of the sage, with the difference that rays are no longer seen in the purely fibrous and very narrow portions of the cylinder facing the flat surfaces and flanking the leaf traces on either side. In still softer and more herbaceous stems the fibers in turn may be largely or entirely replaced by parenchyma, so that the cylinder becomes definitely broken up into separate strands. Similar conditions in a general way present themselves in all cases in which the axial organs of dicotyledons become annual and assume the herbaceous texture—for example, the Solanaceae, as illustrated by the woody stem of the bittersweet (Solanum Dulcamara) and the angular soft one of the potato (S. tuberosum) and of the tomato (S. esculentum). In the two last- named species the furrows of the stem as well as the fibrous or parenchymatous regions of the fibrovascular cylinder correspond in position to the leaves which are a factor in the evolutionary processes under consideration. The Labiatae and Solanaceae have been chosen to illustrate the development of the herbaceous THE STEM IQI type in higher dicotyledonous orders because the simple foliar trace, which is a feature of the two groups under discussion, makes the topographical conditions more easily understood. The Legu- minosae in the case of the garden bean or, better, of the garden pea, illustrate the situation appropriately for forms with plural traces. At the same time the two types just mentioned, as well as the tomato and the sage, exemplify the principle of recapitulation, since, in all, the young stem is round and woody and only later assumes the angular or furrowed configuration of maturity. The hypocotyledonary region of the stem in the bean, for example, and the lower region of the epicotyl in the pea both present a circular and complete woody cylinder. The developmental evidence, as also that derived from comparative anatomy, thus clearly points to the derivation of herbaceous forms from woody ones and not of arboreal perennials from annuals, logically following from the account of the origin of the structures of the stem in dicotyledons originated by Sanio and disseminated by Sachs and De Bary. Another feature of organization of herbaceous stems which often, although not invariably, appears is the degeneracy of the rays other than those broad masses of storage parenchyma which, as has been set forth in the foregoing paragraphs, flank the foliar traces in their vertical course in the stem. This situation is well illustrated among the ranunculaceous representatives of the Ranales, for example, the buttercup, the meadow rue, and the clematis. It has already been discussed in sufficient detail in connection with the vine type of stem in a former paragraph and therefore need not be referred to here. The discussion of the herbaceous dicotyledons brings us to the consideration of the stem in the monocotyledons. ‘This important group of plants, which in physiological efficiency excels all the other large divisions of vascular plants, is practically entirely herbaceous in its structure; and even in those of arboreal habit the internal organization is that of herbs. The monocotyledons on account of the relative simplicity of their fibrovascular strands have been referred by many to affinities with the ferns or, on the basis of their habit, to relationship with the older gymnosperms. These attri- butions of relationship are, however, little supported by either 192 THE ANATOMY OF WOODY PLANTS anatomical evidence or reliable data derived from the study of the remains of plants in the geological strata. The stem in this large and important group is distinguished both by the structure of the fibrovascular strands and by their mode of arrangement in a transverse section of the stem (Fig.142). The con- tinuous woody cylinder of the older dicotyledons in the herbaceous types more adapted to modern climatic conditions in temperate regions has already given place to a con- dition of disconti- mu tty ene tae monocotyledons the process of disinte- gration of continuity has gone much far- ther than even in the herblike dicotyle- dons. For here the separate strands abandon, under the further influence of the necessities con- nected with the leaves, the original circular arrangement for a scattered disposition through the transverse section of the stem. The high efficiency of the monocotyledons in the elaboration of foodstuffs naturally has correlated with it an ample provision of numerous fibrovascular strands for conducting the assimilates into the stem or axis. This situation brings it about that many traces enter the stem at a node instead of the three or, at most, several traces which pass into the nodal region of the axis in the mass of dicotyledons. This multiplication of the conducting strands brings with it complications of arrangement in the stem, for the number is too large to be accommodated on the periphery as is the rule even among herbaceous dicotyledons. As a con- sequence of the necessities which have thus arisen, the leaf traces are displaced from the margin of the central cylinder into the pith or medulla. It is thus clear that, just as the woody stem has given Fic. 142.—Stem of Smilax THE STEM 193 place to the herbaceous one under the influence of necessities con- nected with the greater elaborative efficiency of the leaves, so a still further accentuation of foliar efficiency, correlated with a corresponding multiplication of foliar traces, has led to the further modification of the cylinder of the stem, resulting from the necessity of accommodating a very much larger number of foliar traces in the transverse area of the cylinder. This is usually effected by moving the foliar traces from a peripheral position to the medullary region and more rarely by the running of the foliar traces for one or more internodes in the cortex. The multiplication of the conductive strands from the leaves has a further effect in the organization of the bundles which will be discussed in a later paragraph. Not only in the arrangement of the fibrovascular bundles do the monocotyledons differ from the dicotyledons. The bundles themselves differ in the mass of monocotyledonous forms from the great majority of the dicotyledonous angiosperms in the fact that cambial activity is absent. Fig. 143 shows the general topography of the bundle in Smilax herbacea, the carrion flower. The fibro- vascular strand is surrounded by a well-marked sclerenchymatous sheath in all probability corresponding to the pericycle in lower forms. It is only rarely that in the group under discussion endo- dermal structures are well developed about the strands in the stem. Generally a continuous external endodermal sheath sur- rounds the bundles in common and no internal structures of this nature can be made out. That the parenchymatous tissue lying between the bundles in the stem belongs to the fundamental system can often clearly be inferred from its histological character where its elements strongly resemble those of the cortex. The internal organization of the bundle is distinguished by the presence of phloem and xylem collaterally disposed in relation to one another. The xylem consists for the most part of vessels and parenchyma, and the vessels are of the porous type. The elements of the wood farthest away from the phloem are typical spiral and ringed proto- xylem. No cambium or zone of growth ordinarily is interposed between the wood and the phloem, and this condition has gained for the fibrovascular strands of the monocotyledons the appellation of closed bundles. It has often been supposed that the closed 194 THE ANATOMY OF WOODY PLANTS character of the bundles in the group is an indication of affinity with the pteridophytes, but this view seems to have little value when it is realized that the earlier vascular cryptogams usually an anew Tair rh SY \ ae eae Fic. 143.—Bundle of Smilax herbacea possessed well-marked secondary growth. ‘Toward the periphery of the stem in each fibrovascular strand lies the phloem, composed mostly of sieve tubes and their companion cells. The small elements of the phloem lying on the very outside and close to the bundle sheath represent the protophloem and are often in a some- THE STEM Gk Co): what swollen condition. The sieve tubes in the monocotyledons are of a high type and are characterized by terminal walls which are generally horizontal. The lateral abortive sieve plates, known as lattices, present on the side walls of the sieve tubes in woody dicotyledons and many herbaceous ones as well, are usually absent in the group. Both phloem and xylem consequently represent a high condition of organization and indicate an advanced phylo- genetic position for the monocotyle- ; dons. In certain monocotyledonous families cambial activity has been detected in some instances. This phenomenon is quite generally pres- ent in the grasses, as has been pointed out by Chrysler. In the Liliaceae and aroids as well as in the Cyperaceae the presence of a cambium has also been recorded. Fig. 144 shows the pres- Fic. 144.—Bundle of Erianthus ence of secondary growth in the region oe ee of the node in Erianthus Ravennae. Frequently the bundles of the stem in monocotyledons are of the closed collateral character, but in some cases, particularly in rootstocks with closely approximated nodes, they present a different type, a concentric condition which differs from that found in the Pteridophyta by the fact that the xylem surrounds the phloem instead of the phloem forming a continuous girdle about the xylem. This modification of the bundle is known as amphivasal to distinguish it from the amphicribral condition charac- teristic of fern allies. A strand of this nature is shown in Fig. 145. The phloem occupies the center of the figure and is surrounded completely by the tissues of the xylem. Bundles of this type are apparently the result of the crowding and fusion of the foliar strands at the nodes, for it is in the nodal region that they are best developed. Where the nodes are remote from one another, the amphivasal condition may entirely disappear in the internode to reappear at the next node. With the approximation of nodes, characteristic of many creeping monocotyledonous rootstocks with 196 THE ANATOMY OF WOODY PLANTS tufted leaves, the amphivasal condition becomes continuous. Fibrovascular strands of this type are, in fact, a common feature of organization of the subterranean regions of many monocoty- ledons, even when they are absent in the stem. This situation is well exemplified by the orchids and Iridaceae. In Gramineae and Cyperaceae, on the other hand, amphivasal strands are present in the somewhat remote nodes of the annual flowering stems, but disappear in the internodes, ee a= and a similar situation is pres- yer ) 4 AS, ent in the perennial subterra- nean stem in case the nodes are not crowded. In the latter condition the amphivasal state becomes continuous. In the true palms (Principes) and in many Scitamineae the amphi- vasal bundle seems to have entirely disappeared, although this is a matter for further investigation. There seems to be little doubt that the forma- tion of amphivasal bundles in the region of the nodes is an original feature of organization of the monocotyledons, and that it persists very strongly in the perennial subterranean stem or rootstock, but may entirely disappear in the annual stem. The amphivasal condition of the bundles seems to be definitely cor- related with the numerous leaf traces passing into the stem at the node in the monocotyledonous angiosperms. This hypothesis of its origin is supported by the fact that in herbaceous dicotyledons with numerous leaf traces the occurrence of amphivasal bundles at the node can frequently be observed. The Umbelliferae may be cited as an excellent example of this condition. The consideration of the stem has now been completed, and it will be advantageous in conclusion to indicate the main tendencies manifested in its course of evolution from lower to higher forms. It has been noted that the first important phase in the evolution is connected with the primary structures of the fibrovascular region. Be ai ag> SB Fic. 145.—Amphivasal concentric bundle of rootstock of Smilax. THE STEM 107 In the stems of lower types these present themselves under two general conditions: namely, the protostelic and the siphonostelic. In the former the xylem constitutes a solid mass without any central pith, while in the latter the fibrovascular complex is thrown into a hollow cylinder in which gaps are frequently present. These are ~ generally related to certain of the appendages, but may not have any topographical connection with the lateral parts. In the siphonostelic condition internal phloem is often seen, particularly in the lower forms, and the stele or central cylinder is clearly separated from the central pith or medulla by the presence of an internal endodermis. In higher types the internal surface of the tubular stele tends to degenerate, with the resulting disappearance of internal phloem and endodermis. The original state of the wall of the hollow cylindrical stele can often be inferred from the character of the foliar strands which, in accordance with a general principle to be enlarged upon in a later chapter, often perpetuate a situation which has disappeared in the stem. Where the foliar traces are concentric and separated from the fundamental tissues by a well-marked endodermis, it may be assumed that a similar condition was formerly present in the organization of the central cylinder of the axis. A further interesting phase in the evolutionary development of the vascular cylinder is to be noted in connection with the progressive degeneracy of the primary wood. In the lower forms this region of the xylem is. well developed, and both by its massive character and by the lack of seriation of its elements it is clearly distinguishable from the secondary cylinder which surrounds it. The stem of higher groups presents the primary structures in an obsolete condition, which results in the bringing of the rays of the secondary wood into apparent contact with the pith or medulla. This advanced state of modification of the central cylinder is responsible for the extremely inappropriate name medullary rays, which is applied to the radial parenchyma of the secondary wood. These structures are best called wood rays or simply rays, since primitively in the stem and always in the root they are quite divorced from any connection with the pith. 198 THE ANATOMY OF WOODY PLANTS The next important modification in the case of the fibrovascular structures of the stem is the appearance of aggregations of rays by reason of the increased efficiency of the secondary fibrovascular cylinder in regard both to its conducting and to its storage elements. The clusters or congeries of rays originally diffused throughout the woody structure tend in higher groups to become somewhat definitely related to the appendages. By further progress in the evolution of radial parenchyma we have the compound and diffuse types of rays making their appearance, the former particularly characteristic of herbaceous types, and the latter of the mass of dicotyledonous forest trees. The appearance of large rays, inter- rupting the continuity of the central cylinder and bringing about the differentiation of separate fibrovascular strands, is a particular feature of the herbaceous type representative of later geologic time and of cooler climatic conditions. The woody cylinder broken up into fibrovascular bundles as the result of the evolution of storage devices in connection with the appendages in the herbaceous dicotyledons, in the monocotyledons undergoes further modification in relation to decrease in size and increase in number of the bundles in correlation with the greater efficiency and consequently more numerous conducting strands of the leaves. The decrease in size of the bundles is definitely related to the loss of the cambial activity which characterized the fibrovascular structures of the monocotyledonous angiosperms as a whole. The increase in number of the cauline bundles, resulting from the entry of very numerous leaf traces into the stem at the nodes, brings with it the distribution of the fibrovascular strands throughout the transverse section of the stem. The monocotyle- dons may, in a sense not altogether figurative, be said to represent the second childhood of the vascular plants, just as the Pteridophyta constitute its true infantile phase of development. It is necessary, however, to distinguish very clearly between the primary structures of the monocotyledonous angiosperms which are the result of the loss of secondary growth, and the primary structures of the Paleo- zoic forms which, so far as we know, are a primitive feature of organization. CHAP THe hy THE LEAF A general definition of the leaf or foliar organ has been supplied on an earlier page. The leaf is important, not only on account of its features of structure as an organ of vegetation, but also because of the primitive and intimate relation between it and the organs of reproduction. The latter parts will be discussed in two chapters following the present one, while the main features of organi- zation of the leaf itself will occupy attention in the DEECSEME “CONnMEC- tion. The anat- omy of the fohar organs of the cryp- togamic forms, living or extinct, need not be con- sidered at this stage, as any refer- emcees to, them which are neces- Fic. 146.—Leaf bundle of Cycas revoluta. Explana- tion in the text. sary will appear in later chapters dealing with particular groups. We may conveniently begin the discussion of the leaf with the most primitive type of living gymnosperms, the Cycadales. This group, much reduced in numbers under modern conditions, has a type of organization in the leaf which is of great interest from the evolutionary standpoint. Fig. 146 presents the transverse view of one of the bundles of the main axis or rachis of the leaf in Cycas 199 200 THE ANATOMY OF WOODY PLANTS revoluta. ‘Toward the lower side of the figure is seen the phloem, composed of elements which in the main are arranged in regular radial rows indicating an origin from cambial activity. The upper region of the bundle is composed of xylem, consisting of very large elements which become progressively smaller and fewer in number in the downward direction. The lower point of this aggregation of cells is the protoxylem. This region is surrounded inferiorly by a few rows of parenchyma which give place in turn to more xO AL | ‘ YS & oe eee eee) Sec: iste OS eh GH (\) ) Sieg) Py $1) 3@) ae) STS Ay Cen Swe: Paes oe 0 Siig Rees (ay < OP 25808 ae Orwcee ea oe eae: SOY ne ey Fic. 147.—Transverse section of leaf of Cycas revoluta. Explanation in the text thick-walled elements of the xylem, in contact with the regular radial files of the cambium. The lower region of the xylem is the so-called centrifugal xylem; the upper portion broadening from the narrow protoxylem is the centripetal or cryptogamic xylem. The first-mentioned group of elements of the xylem are pitted in their character, as will be made clear in a subsequent longitudinal illus- tration. The latter, the so-called cryptogamic wood, is of impor- tance from the evolutionary standpoint because it indicates at once a clear relationship on the part of the Cycadales to the vascular cryptogams and to the lower and extinct gymnosperms. In the next figure (Fig. 147) is represented a transverse section of one of the THE LEAF 201 divisions of the leaf. The cryptogamic wood is here relatively bet- ter differentiated than in the axis of the leaf, and it is obvious that the seriation of its elements is toward the upper surface of the foliar organ. The centrifugal wood is very slightly developed. In the next figure (Fig. 148) appears a foliar bundle of Cycas revoluta in its course in the cortex of the stem. There is a mass of irregularly arranged primary wood in the center, surrounded by the radially disposed second- ary wood, which in turn is followed by the tissues of the phloem. The phloem entirely surrounds the bundle, and this is consequently of the concentric type often found in the living ferns and their allies. The contrast in organization of the bundles of the leaf in different parts is very strik- aes The lower Ror Fic. 148.—Concentric foliar bundle from the cortex centric region, IN of Cycas revoluta. accordance with generally accepted principles of comparative anatomy to be eluci- dated later in a special chapter, may be regarded as supplying evidence of the former concentric character of the woody cylin- der of the stem in the Cycadales, a hypothesis entirely justified by the existence of a remarkable group of fernlike seed plants in the Paleozoic, known as the Medulloseae, from which on both anatomical and reproductive evidence the living group seems to have been derived. In these forms the bundles of the stem were, as will be subsequently shown, often concentric in their organiza- tion. In the higher region of the leaf trace in the cycads the concentric character is lost, but the centripetal development of 202 THE ANATOMY OF WOODY PLANTS part of the wood still sufficiently vouches for the cryptogamic affinities of the lowest living gymnosperms. In Fig. 149 is shown the longitudinal view of the leaf trace in the rachis of the leaf. To the right appears the phloem made up of elongated ele- ments, the sieve tubes. To the left of this region lie certain pitted tracheids belonging to the centrifugal or modern wood. Then inter- vene a few parenchymatous cells, followed by the spiral elements of the centripetal or cryptogamic wood. ‘These pass farther to the left —e OOO OO Ga & — > By S S SS Mm = => 2) = KAAAZS4SS iZ N AW \ VA )VAVAVAVAYNINAVAVAAVAVYAS ODOOOO @ CODAAG®A DO@O®O OOGO cS \ WAVY y QOZZ2 Fic. 149.—Longitudinal section of a foliar bundle in Cycas revoluta into ringed, scalariform, and, finally, pitted tracheids. The struc- ture of the leaf in the Cycadales is clear evidence of their rela- tionship with the ancient fernlike gymnosperms, which in turn were doubtless in filiation with actual ferns in the remote geologic past. The Cycadales have their nearest affinities in the past with a group of gymnosperms, the Cycadofilicales or the Pteridospermeae, which were so strikingly fernlike in their habit that until the very end of the last century they were regarded as ferns. In contrast to the Cycadales the mass of surviving gymnosperms have taken their origin from forms which are known as Cordaitales. These had nothing in their habit which recalls the ferns, but often THE LEAF 203 present a strong superficial resemblance, particularly in the con- formation and venation of their leaves, to the monocotyledons. The Cordaitales had leaves varying in width, but always char- acterized by few or numerous parallel veins. The structure of the fibrovascular bundles constituting these veins, however, was entirely different from the features of organization found in the nerves of the leaves of living monocotyledons. Fig. 150 illus- trates the general organization of the leaf in Cordaites princi- palis. The veins are numerous and separated from one another by intervals of the soft mesophyll of the leaf. The epidermis is EET BS = Wag: AGT Oo Ms res Fic. 150.—Transverse section of the leaf of Cordailes principalis strengthened, particularly in the region of the fibrovascular bundles, by hypodermal bands of. thick-walled cells. In Fig. 151 is shown an enlarged transverse section of one of the foliar bundles of the species under consideration. The wood was entirely cen- tripetal in its development and ended on either flank in a band of thick-walled elements with narrow central cavities. The zone of thick-walled elements was in contact externally with a second zone made up of cells with thinner walls and much larger lumina. Both the zones just described inclose the phloem, which lies below the mass of centripetal wood. The longitudinal view (Fig. 152) throws addi- tional light on the organization of the bundle. The double sheath connected with the flanks of the xylem and forming a complete circle about the phloem is composed of elongated elements with bordered pits on their walls. These are known as transfusion cells and are 204 THE ANATOMY OF WOODY PLANTS an important and phylogenetically interesting component of the foliar fibrovascular strands in many gymnosperms. They are not a salient, and certainly not a primitive, feature of organization of iS Ze % ~ SS Fic. 151.—Transverse section of the leaf bundle in Cordaites principalis Medulloseae. the leaf bundles of the living Cycadales and their allies, the Paleozoic The transfusion sheath of the foliar bundles in the Cordaitales did not always manifest the complexity that it shows in the case of C. principalis figured above. In most instances only the broader and shorter thin-walled elements were present, the THE LEAF 205 elongated and thicker-walled inner sheath being absent. The intimate connection between the centripetal or cryptogamic wood and the transfusion tissue is observed in all cases. It is clear accordingly in the Cordaitales that the transfusion tissue which, as will be subsequently shown, plays an interesting réle in the evolu- tionary history of higher gymnospermous groups is primarily related to the centripetal or cryptogamic wood. — [ I LAs VA Y\2 >> SS AE SSS8 | Y,| = | =z | 2ORSq: ys |= LST : \ 2 | = Ises %| 2) = Sed : AR i IISSsSy i | SS | ISS: | = | = | soa: ES aESSSE pS | | SS g =| >= | aBess a= A= A= = nM Fic. 152.—Longitudinal section of a leaf bundle in Cordaites principalis The organization of the leaf in the conifers will next occupy our attention, since the present chapter deals with the leaf only in the features which are of general evolutionary importance. Fig. 153 shows an enlarged view of the whole leaf of Pinus strobus, the white pine. The epidermis, reinforced by a hypoderma, surrounds the median green part of the leaf, the mesophyll, in which lie resin canals and a single fibrovascular bundle. The latter, exceptionally for the conifers, is marked off from the surrounding fundamental tissues by a well-defined circular endodermis. The fibrovascular strand consists of xylem entirely centrifugal and mostly secondary in its origin, and this meets with the phloem on its lower border. Sur- rounding the conducting strand of the leaf is a mixture of ordinary 206 THE ANATOMY OF WOODY PLANTS parenchymatous elements containing protoplasmic structures and short empty cells with bordered pits. These are the transfusion elements, and it is easy to observe that they are most abundant on the flanks of the xylem and, in fact, take their origin from this general region. As in the case of the Cordaitales, the cells of the transfusion tissue surround the phloem as well as the xylem. An important difference, however, is the absence of intermingled {AS SAS ; LEV Poy Fic. 153.—Transverse section of leaf of Pinus Strobus parenchymatous elements in the girdle of transfusion tissue of the older group. Transfusion tissue is better developed in the leaf of the pine than in any other of the subtribes of conifers. In most of the other subgroups of the Coniferales the transfusion tissue is mainly confined to the flanks ef the fibrovascular bundle, and the conducting strand as a whole is not sharply separated from the remaining tissues of the leaf on account of the absence of an endo- dermis. THE LEAF 207 A link between the conditions found in the case of Pinus and the anatomical organization of the Cordaitales is presented by a mesozoic fossil form allied to Pinus to which the name Prepinus has been given. Fig. 154 illustrates the organization of the leaf in this species. It is bounded by flat surfaces as a result of contact with surrounding leaves of the many-leaved fascicle. The hypodermal structures are strongly developed as in the Cordaitales and con- stitute the same strengthening ribs as are found in the leaves of Fic. 154.—Transverse section of leaf of Prepinus statenensis that genus. On account of the changes resulting from fossiliza- tion the endodermis is not so distinct as in living pines, and the mesophyll or soft substance of the leaf is very poorly developed. The bundle is surrounded by a very dense transfusion sheath in which all the cells are empty and provided with bordered pits. Not only is the transfusion sheath massive in Prepinus and entirely composed of transfusion tracheids to the exclusion of paren- chymatous elements, but it is further complicated by the presence of an internal thick-walled zone comparable with the similar structure in C. principalis figured above. In the comparatively 208 THE ANATOMY OF WOODY PLANTS low magnification shown in the photomicrograph the inner zone of the transfusion sheath appears merely as a dark boundary sur- rounding the fibrovascular bundle proper. The conducting strand of the leaf is represented by the xylem alone, the phloem having disappeared during fossilization. In Fig. 155 the central region of the foregoing is represented under a higher degree of magnification. Fic. 155.—Portion of leaf of Prepinus statenensis, more highly magnified The tracheary character of the transfusion sheath can now clearly be discerned, as well as the fact that it contains no cells of the nature of parenchyma. The narrowness of the cells constituting the inner transfusion sheath is also now quite apparent. In Fig. 156 are shown the various structures of the fibrovascular bundles lon- gitudinally and on a still higher scale of magnification. The outer transfusion sheath is composed of elements with distinct and rather large bordered pits which abut inwardly on the narrow thick-walled cells of the inner transfusion sheath, in turn connected THE LEAF 209 with the xylem of the fibrovascular bundle. Before we consider the nature of this relation it will be well to examine more carefully the bundle itself. The conductive strand is represented by its xylem only; this consists, interestingly enough, of two regions— a lower one in contact with the empty space once occupied by the phloem, and an upper, consisting of distinct rows separated by thinner-walled elements. The latter is the true centripetal or Fic. 156.—Longitudinal section of the leaf of Prepinus statenensis. Explanation in the text. cryptogamic wood which in Prepinus alone among the conifers is present in a typical form. The lower region of the xylem is cen- trifugal and corresponds to the whole of the xylem in the leaf of the modern Pinus. In the modern or centrifugal region of the wood, rays are distinctly present, and these pass from its substance into the cavity once filled by the phloem. The centrifugal region of the wood provided with rays is related to the inner transfusion sheath on its flanks alone. This relationship corresponds in fact to that observed in the case of living pines, as is shown above in 210 THE ANATOMY OF WOODY PLANTS Fig. 153. The most significant relation of the xylem in the leaf trace is by means of the series of centripetal or cryptogamic elements. These are numerous and serve to bring about a very intimate and copious connection between the bundle proper and the transfusion tissues. There is good reason on the basis of the anatomy of Prepinus and the Cordaitales to regard the transfusion tissue which characterizes the foliar organization of all but the very lowest of the gymnosperms as a product. of the differentiation of the centripetal or cryp- togamic wood. In the true pines of the Cretaceous,the centripetal wood was absent, as it is in modern species of the genus, but the internal transfusion sheath was often well developed, thus showing a clear filia- tion with Prepinus. Where the centrip- etal xylem has dis- appeared, the relation between the bundle and the transfusion tissues occurs on the flanks of the centrifugal wood. It will be obvious to the reader that the tissues surrounding the fibrovascular bundle in the conifers and their allies are of considerable interest from the evolutionary standpoint. The transfusion tissue at the present time has a significance in the vegetative leaves of all but the lowest gymnosperms in connection with the storage of water and the con- ducting of it to the green cells of the mesophyll. In the repro- ductive leaves it has taken on another but equally interesting function, as will be indicated in the next chapter. Transfusion elements are found in the leaves of all seed plants from (and excluding) the cycads upward. In the conifers they are Fic. 157.—Leafy twig of Casuarina equisetifolia (after Solerderer). THE LEAF 21% well developed, but are distinctly degenerate in the higher subtribes of the group and are less well developed in any living conifers than they are in Prepinus and Cretaceous species of Pinus. The Gnetales often show the transfusion tissues in a high degree of development. The small leaves of Ephedra naturally show them less distinctly than the large persistent foliar organs of Welwitschia, where they constitute a very conspicuous feature of the organiza- tion of the leaf. In Gnetum, again, in accordance with its higher AN : C \ di Wot Wehie. Fic. 158.—Base of leaf of Casuarina equisetifolia, showing transfusion tissue systematic position, the transfusion sheath is Jess conspicuous. Among the angiosperms transfusion tissues are present in the dicotyledons, but present themselves in the condition typical for the higher gymnosperms only in the genus Casuarina. Here, as is shown in Fig. 157 illustrating the organization of a leafy twig of Casuarina equisetifolia, there are clusters of thick-walled empty cells flanking the leaf traces. This relation to the foliar strands strikingly resembles that found in the higher gymnosperms and appears to be good evidence of the primitive position of this interest- ing genus. In Fig. 158 is shown one of the foliar bundles of the THE ANATOMY OF WOODY PLANTS 22 genus under discussion much more highly magnified. The flanking relation of the transfusion elements to the strand of xylem is now very distinct and recalls that found in the leaves of the Cupres- Less typical manifestations of the develop- ment of transfusion tissues in the dicotyledons are provided by those forms in which bundles related to stomata exuding fluid water, and consequently known as water-stomata, terminate below sineae, Taxineae, etc. Dan Se 2 ©. > > LQo Y 1 , "eas A ZS ES ag , = q 9 S ¢)) ©Se oo O@ = RSTONOD Ala 2 C2000 900 oR — —=A = X29 682_9000G0 ® COCO. A ——— G (eteceo) a 20009 ONG ors Ce \Voogoe SEES GEES —@ © @@ OG ( b J —- = OS < 2 he OOO O00 72505908 SOO HCO D2 6 oe SO00GG COaVGGo > 56 GER) 2 O°S OS) A d Fic. 159.—Transverse section of leaf of Alnus incana the stomatic pores in a mass of wide, short, tracheary elements. This condition, although doubtless derived from ancestral gymno- spermous structure, has departed so far from the original transfusion tissue that it can scarcely be included in the same morphological category. Transfusion tissue, as will be apparent from the last paragraph, has become a feature of very subordinate importance in the organi- zation of the leaf in the mass of the dicotyledons. The general structure of the foliar organs in the group may profitably occupy attention at this stage. Fig. 159 reproduces somewhat diagram- THE LEAF 213 matically the anatomical features of the leaf of Alnus incana. Above is a layer of cells containing only protoplasm and a nucleus. A similar situation is presented by the lower surface of the leaf, with the exception that the continuity of the epidermis is locally perforated by stomatic openings. The elements related to these, the guard cells, are distinguished from the rest of the epidermal layer by the presence of chloroplastids. The upper epidermis is contrasted with the lower, not only by the absence of stomata, but also by the presence of a rough impervious covering, the cuticle. Another feature of interest in the superior epidermal cells is the mucilaginous modification of their inner walls, and this is expressed in the illustration by a thick layering. The central portion of the leaf is occupied by the mesophyll, composed of the palisade (upper) region and the spongy (lower) region. The development of palisade parenchyma in foliar organs is definitely related to the amount of insolation or exposure to light, while the spongy layer is less well developed when the leaf is strongly illuminated, and becomes much more accentuated in foliar organs exposed to shade and a damp atmosphere. The leaf of the monocotyledons supplies little in a general way which is of interest from the standpoint of evolutionary anatomy, except the occasional persistence of cambial activity. CHAPTER XV THE MICROSPORANGIUM The microsporangium of the vascular plants is considered first; because there can be no question that it is the primitive type of sporangial structure for the long series of forms which are character- ized by the possession of water-conducting tracheary tissues. In the lower representatives of the Vasculares the microsporangium is the only type present, and in the heterosporous cryptogams and the seed plants it keeps its place, with little change of its original condition of organization, side by side with the highly modified megasporangium and seed. The relative constancy of microspo- rangial structures makes them in many respects of the greatest value from the evolutionary standpoint. If the liverworts are correctly regarded as the forms nearest to the Pteridophyta in the series of the bryophytes, there can be little doubt that the sporangium in its primitive form of sporogo- nium is the forerunner of the sporophyte of the vascular series. Professor Bower has brought forward an impressive aggregation of evidence in favor of the hypothesis that the sporophyte is the result of progressive sterilization of sporogenous tissue. Although the definite mode by which the simple sporogonium of the thallose liverworts gave rise to the sporophyte of the Pteridophyta, so complicated in its internal structure and external organization, is highly speculative, it will serve a useful purpose to indicate the main probabilities in this connection based for the most part on the investigations of Leitgeb. In certain liverworts, such as, for example, Corsinia and Boschia, the spore sac gives rise to sterile cells as well as spores. There is clear evidence in these and in similar cases that the sterile cells are modified or, as Professor Bower expresses it, sterilized potential sporogenous cells. In many liverworts the sterile cells are useful in distributing the spores. In this instance they are much elongated and have their walls spirally thickened. The spirals recoil when the spores are ripe, 214 THE MICROSPORANGIUM 215 giving them an impetus which scatters them over the surface of the ground. These spore-distributing mechanical cells are known as elaters. In certain liverworts, such as Pellia and Aneura, the elaters, in addition to occurring loosely among the spores which they serve to scatter, are aggregated in a compact elon- gated mass at one end or the other of the spore sac or theca. This longitudinal cluster of elaters may be regarded with some degree of probability as the prototype of the fibrovascular bundle of the Pteridophyta and higher groups of vascular plants. In Anthoceros and allied forms the cluster of elaters, known as the columella, becomes a much more important structure and traverses the sporangium from end to end. Laterally at intervals it gives off transverse ramifications which divide the mass of spores into separate clusters, and these may perhaps be regarded as the proto- types of the sporangia found in the vascular series. The situation in the horned liverwort Anthoceros, in which there is an extensive columella with lateral ramifications, gives some support for the hypothesis of the derivation of the sporophyte from the sporogonium by the sterilization of potential sporogenous tissues. The mode in which the organs, leaf, stem, and root arose from such a primitive condition of organization is much disputed, since none of the hypo- thetical transitional forms between the moss capsule and the sporo- phyte of the higher plants have yet been discovered. There can be little doubt, however, in a general way that the sporogonium is the forerunner of the sporophyte and that the elater is the prototype of the tracheid in vascular plants. It will be clear from the foregoing statement that the sporangium is so intimately involved in the primitive organization of the most ancient spore-producing members that it is entirely proper to consider it a definite organ of higher plants on a footing of equality with the root, stem, and leaf. If this view of the matter is sound, obviously no very useful purpose can be served by the examination of the development of particular cells of the foliar organs which are in some way or other related to the origin of sporangia. It is likely, moreover, that the sporangia of the Pteridophyta give us on the whole a less accurate picture of the original type of sporangium than those of the lowest seed plants. It is therefore appropriate 216 THE ANATOMY OF WOODY PLANTS in the present connection to begin the discussion of the sporangium with the consideration of the situation presented by the lowest living gymnosperms, the Cycadales. Fig. 160 shows the organiza- tion of a microsporangium in Zamia muricata. The structure in question is covered on the outside by an envelope of thick-walled cells which in the condition of maturity determine its dehiscence. The mechanical structure is known as the annulus and is of great importance in bringing about the Ase WO) re Ny Uy) Up distribution of the spores, particu- Syesia ~AN fy // Yj} larly in the lower Vasculares, in 8 which it takes the place of the elaters found in many of the liver- worts. The annulus is plainly an epidermal structure, both because it is actually the external layer of the sporangium and because its con- tinuity is interrupted by the pres- ence of stomata. ‘These can be seen in the figure in profile view. The situation in regard to the annulus in the Pteridophyta may be briefly summarized. In lower forms the thick-walled epidermal cells which serve as the mechanism for the opening of the sporangium are massive in their development, while in the higher forms of the vascular cryptogams the amount of mechanical tissue tends to become more and more restricted. Fig. 161a shows the structure of the sporangium and its annulus in Selaginella. The mechanical layer in this case is extensive and is almost coextensive with the surface of the spore sac. In contrast to the conditions shown in Selaginella are those presented by many of the ferns. In Fig. 161) is reproduced the organization of the sporangium of Polypodium vulgare as an illustration of the higher type of annulus in the Pteridophyta. The opening mechanism here constitutes an incom- plete vertical ring and in consequence literally merits the name of annulus. The further consideration of the types of annulus Fic. 160.—Sporangium of Zamia muricata. THE MICROSPORANGIUM 207 presented by those forms included under the general heading of Pteridophyta need not occupy our attention in the present con- nection, important as these structures are from the standpoint of taxonomy and the evolution of particular groups. Returning to the seed plants, we find that the Cycadales are the only living forms in which the organization of the mechanical tissues of the sporangium corresponds with that generally existing Fic. 161.—Sporangium of Selaginella spc. and of Polypodium vulgare in the Pteridophyta; and in accordance with this general situation it will be made clear that the epidermis has not an important rela- tion to the distribution of the microspores of plants producing seeds. The interesting genus Ginkgo will serve to illustrate advan- tageously the situation for the lower living seed plants. Fig. 162 shows the organization of one of the two sporangia of the micro- sporophyll of this genus as viewed in longitudinal vertical section. Clearly the cells of the epidermis are thin-walled and can perform no important office in the openings of the spore cavities. Beneath the epidermis is found a broad zone of cells provided with barred 218 THE ANATOMY OF WOODY PLANTS thickenings in their walls, resembling, in fact, short tracheids with reticulate thickenings. By following the mass of reticulate mechan- ical cells to the proximal end of the sporangium we find that they are continuous with, and pass by imperceptible transitions into, transfusion elements related to the fibrovascular bundles of the sporophyll. In Ginkgo it is evident that the opening mechanism of the sporangium is a derivative of the fibrovascular system, and does not take its origin from the cells of the epidermis, as is the case with the annulus of the Cycadales, and forms lower in the scale of vascular plants. The situation is so important in this respect that it is worthy of being given a special nomen- clature. In those types in which the dehiscence depends on epidermal mechanisms, in- cluding the Pteridophyta and the very lowest seed plants, the term ectokinetic may be ap- plied to the sporangium. On the other hand, in the long series of forms beginning with Ginkgo and ending with the monocotyledons, in which the opening mechanism is of internal origin and related to the fibrovascular system, the designa- tion endokinetic definitely indicates the origin of the apparatus involved. It is necessary to examine more in detail the conditions found in the walls of the sporangia of the forms above Ginkgo. In Fig. 163 is represented a longitudinal vertical section of the microsporan- gium in Pseudolarix Kaempferi, a representative of the Abietineae or pinelike conifers. Here the situation resembles in a general way that found in the case of Ginkgo, for the opening of the sporan- gial sac is due to the presence of reticulately thickened cells which are likewise related to the fibrovascular system of the trace of the aE ArH reeset Y same Fic. 162.—Sporangium of Ginkgo biloba THE MICROSPORANGIUM 219 microsporophyll. As in Ginkgo, the transition from the mechan- ical tissue to the tracheids of the fibrovascular bundle is effected by transfusion elements. An interesting difference between the situation found in Ginkgo and that illustrated in the Abietineae and other conifers is the fact that the mechanical elements invade the epidermis in Pseudolarix, but fail to do so in the more primitive genus. In other members of the Abietineae, particularly where the wall of the sporangium is very thin, the mechanical tissue becomes correspond- ingly reduced in [\ amount and no IN \ longer shows any Kh clear relation to the 8 fibrovascular sys- tem. In the sub- tribes of Coniferales above the Abie- tineae this condition, in fact, becomes the rule, and so abortive does the mechanical layer become that it is represented by the reticulately thickened cells of the epidermis alone. It thus results that the opening of the sporangial cavity is once more effected by superficial cells, but the situation here represented should be carefully distinguished from that in the Pteridophyta and Cycadales, since it is the result of the invasion of the epidermis by mechanical tissues of fibrovascular origin. Subsequently, when the dehiscing mechanism was reduced, the epidermis once more became secondarily the seat of the opening device. It is not without significance in this connection that the araucarian conifers, which are often regarded as the lowest, present the sporangial arrangements of the mass of conifers in which the dehiscing mechanism is reduced to its lowest terms, and not that luxuriant and apparently primitive condition exemplified by Ginkgo and the Abietineae. In the Gnetales the small sporangia are not characterized by the presence of a very well-developed opening device. The situation Fic. 163.—Sporangium of Pseudolarix Kaempferi 220 THE ANATOMY OF WOODY PLANTS in the case of the angiosperms, however, is different. In Fig. 164, showing transverse sections of the anthers of a tulip and a honey- suckle, the mechanical tissues are clearly differentiated and occupy an entirely internal position precisely as in Ginkgo. There is a very important difference between the situation presented by the angiosperms, whether dicotyledons or monocotyledons, and Ginkgo and the Abietineae. In the higher group the mechan- ical tissues, constituting the so-called fiber layer of the anther Wx Ps WANS NS Ah NS \ WW NU TN unis CW UN NYS CTA er yy) ae ® Py fl ‘. nk 2 ey Fic. 164.—Sporangia of tulip and honeysuckle wall, have no longer any relation to the fibrovascular bundles of the filament. In the case of the angiosperms the relation once existing between the fibrovascular system and the opening mechan- ism has apparently been lost. The dehiscing apparatus is, however, still in a good state of development and in this respect contrasts to the situation presented by the Gnetales and the higher Coniferales. The structure of the walls of the microsporangia of the vascular plants from Ginkgo upward is highly interesting from the stand- point of the doctrine of descent. In the lower members of this series the opening device of the sporangium is clearly in relation to the transfusion tissue connected with the fibrovascular bundles of the reproductive leaves. In the Cycadales, the lowest living seed THE MICROSPORANGIUM 221 plants, we find a complete absence of typical transfusion tissue in the leaves, although its presence has been erroneously described for the group. The cycadean gymnosperms in the absence of foliar transfusion tissue resemble the true ferns, which are also characterized by the exclusion of tracheary tissues belonging to this category from their foliar organs, whether vegetative or reproductive. It is highly significant that an epidermal sporangial mechanism and the absence of transfusion tissue are features which alike mark the Pteridophyta and the seed plants most nearly allied to these. Beginning with the Ginkgoales and proceeding upward, we find transfusion tissue progressively taking the place of the centripetal or cryptogamic wood in the vegetative leaves; and in the reproductive leaves the transfusion tissues or structures definitely associated with them assume the function of opening the sporangium at the time of the ripening of the spores. The cor- rectness of this interpretation of the situation is best seen in Ginkgo, in which in the lower region of the sporophyll the trans- fusion tissues are developed very much after the manner in which they present themselves in the case of the vegetative leaves. In the upper region of the sporophylls, bearing the microsporangia, the transfusion elements grade imperceptibly into the reticulately thickened mechanical tissues of the sporangial walls. In the sub- tribe of the conifers which is beginning to assume importance as a candidate for the most primitive phylogenetic position in the group (namely, the Abietineae), we find the transfusion zone not only well developed in the vegetative leaves of both living and fossil repre- sentatives, but likewise occurring under highly significant condi- tions in relation to the sporangial mechanisms. In the remaining gymnosperms the mechanical tissue shows a strong tendency to become reduced in amount and loses all direct relationship to the fibrovascular tissues proper. In the angiosperms, as has been pointed out above, the fiber layer characteristically present in the anther wall is well developed, but no longer has any relation what- soever to the fibrovascular system. In conclusion, it may be stated that the opening mechanism of the sporangia of the Pteridophyta and of the lowest gymnosperms is epidermal in its origin, while that of the seed plants from Ginkgo 222 THE ANATOMY OF WOODY PLANTS upward is clearly derived from transfusion tissue. This category of tissue is the final stage of persistence of the protean centripetal or cryptogamic wood of the lowest vascular plants. In the angio- sperms the mechanical tissues in the walls of the anthers exemplify the highest level of survival of the old centripetal wood of the Pteridophyta and the lowest gymnosperms. In fact, the so- called fiber layer of the anther in the case of the angiosperms supplies the clearest instance of the persistence of this ancestral structure outside of that most conservative of all organs, the root, in which, as has been made clear in an earlier chapter, it still maintains its pristine development in the primary organization. The two mechanisms correlated with sporangial dehiscence pre- viously described may appropriately be designated as ectokinetic and endokinetic. CHAPTER XVI THE MEGASPORANGIUM AND SEED In the Pteridophyta the phenomenon of heterospory has de- veloped in many different groups. The result of the realization of this condition has been the appearance of smaller sporangia producing numerous small spores known as microspores and of larger ones giving rise to a few large spores designated as mega- spores or macrospores. In the case of the sporangia which give rise to megaspores, or the megasporangia, the conditions connected ' with opening are the same as those exhibited by the mass of Pteri- dophyta; in other words, the spore sacs are ectokinetic and owe their dehiscence to the activity of a mechanical layer derived from the epidermis. As this situation has been sufficiently discussed in the previous chapter, it will not be profitable to return to the matter here. Megasporangia in the proper sense of the word, wherever they occur, are ectokinetic. It has been recognized since the times of the great German morphologist Hofmeister that seeds represent modified mega- sporangia. This view of the origin of seeds is justified, not only by their anatomical structure and by the cytological conditions observed in the development of the endosperm, but also by the actual persistence of the megaspore membrane in the seeds of many of the lower gymnosperms. If any remaining doubt existed as to the origin of seeds from megasporangia, it would be removed by the discovery of certain interesting structures in the case of Paleozoic lycopods which present at the same time many of the distinctive characteristics of megasporangia and seeds. So strik- ingly does one of these (described by Scott) resemble a seed in its external appearance that it was for a time actually regarded as one, until its internal organization revealed its anomalous character. Fig. 165 illustrates the vertical section of Lepidocarpon Lomaxt, the seedlike fructification of a lepidodendrid. Internally is shown a mass of cells, the gametophyte, surrounded by a heavy dark line, 223 224 THE ANATOMY OF WOODY PLANTS the section of the megaspore membrane. In addition to the germinated megaspore shown in the figure, three other abortive megaspores make their appearance at an earlier stage, and these have thicker walls than the functional spore. These are not shown in the late stage of development appearing in the figure. Not only does the megaspore retain its thick membrane in the fructification of Lepidocarpon, but, contrary to the conditions found in typical seeds, the mechanical layer of the megasporangium likewise is well developed and was prob- ably capable of dehiscence. The integument with which true seeds are provided is rep- resented in this foreshadowing of seminal structure by the upfolded edges of the sporo- phyll. The absence of an apparatus for receiving the microspores or pollen likewise differentiates the fructification under consideration from the seeds of even the lowest of the seed plants. Fis. 165.—Seedlike sporangium of In Fig. 166 is shown the Lepidocar pon (after Scott). A ‘ longitudinal view of another seedlike structure from the Carboniferous of England known as Miadesmia. Here the resemblance to the real seed is much more marked than in Lepidocarpon. The sporophyll so completely involves the megasporangium that only a small aperture is left which corresponds physiologically, although not morphologically, to the micropyle of the seed in the true seed plants. Within the “integument” is inclosed, not only the megasporangium, but also the ligule. The megasporangium is much less typical than that of Lepidocarpon, for its mechanical layer fails to develop and it pro- duces only one spore in contrast to the four that come into existence in the case of the Lepidocarpon. ‘There is no good reason, however, to regard the structure here described as representing a THE MEGASPORANGIUM AND SEED 225 true seed any more than that delineated in connection with the last paragraph. An interesting condition has been described by Miss Lyon in the American species of Selaginella, S. apus, and S. rupestris. Here the spores germinate and are fertilized within the mega- sporangia, a condition favored by the fact that the micro- sporangia are situated in the upper region of the cones. The microspores undergo development unshed, and on a wet day the antherozoids to which they S give rise are able to make their way to the lower region of the strobilus, where the germinated megaspores present their archegonia for fertilization. The development of the embryo takes place after Fic. 166.—Seedlike sporangium of Miadesmia the union of the sexual ele- {0 Seward, after Scott). ments, and the sporelings later grow out among the leaves of the cone. The situation represented by the two species mentioned appears to be somewhat general for the genus and throws an interesting light on the conditions which were probably present in Lepidocarpon and Miadesmia. The most ancient types of seeds known to us have an organiza- tion differing in important particulars from the seedlike structures described in the two preceding paragraphs. In the first place, the most antique seeds are provided with a true integument and are not merely wrapped in the sporophyll as a whole. Secondly, they present a very important feature in the presence of a so-called ‘pollen chamber”’ which receives the microspores and provides a fluid in which they may undergo germination and later effect fertilization. A primitive type of seed is diagrammatically represented in Fig. 167. The megasporangium appears within the integument which covers it almost completely, so that communication with the outer world is only by a narrow canal at the apex known as the micropyle. The megasporangium is without any mechanical layer 226 THE ANATOMY OF WOODY PLANTS such as appears in the seedlike structures described above for the lycopods. Such a layer was doubtless originally present, but has ceased to be necessary as a protection on account of the shelter afforded by the integument; moreover, it could no longer be func- tionally useful in opening the spo- rangium since the megaspores in the case of true seeds are permanently inclosed. The elimination of the ectokinetic me- chanical layer of the older seeds must lie far in the geological past, be- cause no evidence of its presence has been observed in the oldest seeds with the structure of which we are acquainted. The pointed apex of the megasporangium is occupied by a cavity, the pollen chamber, in which the pollen grains or microspores come to rest before germination. This cavity has its capacity much reduced by the presence of a central column known as the columella. Below the pollen cham- ber lies the germinated megaspore with its somewhat thickened megaspore membrane. ‘The membrane incloses the gametophyte, bearing the archegonia in its upper region. Surrounding the part Fic. 167.—Diagram of seed of a cycad of the seed corresponding to the megasporangium and fused with it, except in the upper region, is the integument, and this consists THE MEGASPORANGIUM AND SEED 227 of a hard inner layer known as the sclerotesta and a softer outer one which contains mucilage canals and to which the name of sarcotesta is applied. Both sclerotesta and sarcotesta are pro- vided with a system of fibrovascular strands, but tracheary ele- ments of any kind are absent in the region of the nucel- lus or megaspo- rangium. Dre: type ol seed delineated in connection with the foregoing para- graph is not the only one charac- teristic of more ancient plants. In Fig. 168 is shown another category of seed which, although present- ing the general features of the Paleozoic type, is characterized by certain interesting and important peculiarities. The Fic. 168.—Diagram of an ancient type of seed with integument in the _ ttacheary mantle surrounding the gametophyte (modified ; : after Oliver). diagram is repre- sented as consisting of an outer softer sarcotesta and an inner resistant sclerotesta. It incloses, as in the other type, the mega- sporangium or nucellus, and this is likewise provided with a pollen chamber. The only important difference between the seed under discussion and that described in the preceding paragraph is the distribution of the fibrovascular bundles. In the seeds of the first type the tracheary strands are present in both 228 THE ANATOMY OF WOODY PLANTS sarcotesta and sclerotesta, but are lacking in the nucellus or megasporangium. In the seed now under consideration a fibro- vascular envelope surrounds the megaspore and ends upwardly in the pollen chamber. It is clear in the present instance that the tracheary tissues invade the megasporangium precisely as they do the microsporangium of Ginkgo and seed plants higher in the evolutionary scale. The function of the tracheary tissue which ends under the pollen chamber doubtless was that of supplying water to facilitate the germination of the microspores, and the fertilizing movements of the antherozoids originated from these. It seems clear that we have in the type of seed figured in connection with the present paragraph a counterpart to microsporangia with the endokinetic mode of dehiscence. A number of ancient seeds of the anatomical organization indicated here have been investigated, but unfortunately they have not been connected with absolute certainty with any definite vegetative types. The seed of the living Ginkgo throws no light upon the question of the affinities of the second type of Paleozoic seeds, for, although tracheary tissues are abundant in the base of the seed, they do not penetrate into the megasporangium proper. It is likely that degeneracy of the fibrovascular structures has here obscured the real situation, since from the organization of the microsporangium in the genus we should expect to discover tracheary elements in the walls of the nucellus or megasporangium. In the seeds of the Cycadales we have realized the general features of organization depicted in Fig. 167, which is, in fact, modeled from the young seed of Cycas revoluta. The organization of the microsporangium in the cycads does not support the hypoth- esis that nucellar tracheids were once present in the seed of the group and have disappeared in its modern representatives. The conservative tendencies of microsporangial structures as contrasted to those of the megasporangium or seed which is considerably more rapidly influenced by the course of evolution constitute a valuable situation from the standpoint of comparative morphology. The general anatomical features of the seed in the higher gymno- sperms may next be considered. In Fig. 169 is illustrated the more THE MEGASPORANGIUM AND SEED 229 important structures of the seed in one of the Abietineae or pine family. It is provided with an integument in which a small pore known as the micropyle is present at the apex of the seed. Within the integument is accommodated the nucellus or megasporangial portion of the seed. This is not characterized, as is that of the older and fernlike gymnosperms, by the presence of a pollen cham- ber. The pollen grains or micro- spores are received, in fact, on the smooth apex of the nucellus and very soon send out pollen tubes which bore their way through the tissues of the nucellus in order to reach the archegonia, situated on the apex of the gametophyte. The absence of the pollen cham- ber and the presence of functional pollen tubes are features which most clearly distinguish the seeds of the modern gymnosperms from those of the lower largely extinct types included under the heading of the Archigymnospermae. The nucellus is not provided with a tracheary mantle, such as is found in the ovular structures of certain extinct gymnosperms. The soft sarcotesta often presented by yy, 169.—Diagram of seed of a conifer more ancient types of seeds is likewise conspicuous by its absence in the case of the more typical representatives of the higher gymnosperms. In the angiosperms the situation in regard to the seed is still further modified by the fact that the pollen is no longer received on the apex of the ovule or young seed, but comes to rest on a special region of the closed sporophyll known as the stigma (Fig. 170). The microspores or pollen in germinating send out pollen tubes, of greater or less length, which penetrate first the tissues of the % % Ld © So 7% OK 0:0. 0:0, PEE RLEK , 230 THE ANATOMY OF WOODY PLANTS closed reproductive leaf or megasporophyll, and later enter the ovule, either through the micropyle (in porogamous forms) or through the chalaza or breech of the seed (a condition found in the so-called chalazogamous dicotyledons). Not only do inclosure of the ovules Fic. 170.—Diagram of a poroga- Fic. 171.—Diagram of a chalazog- mous dicotyledon. amous dicotyledon. in an ovary and the consequent exclusion of the pollen from direct access distinguish the angiospermous seed from that found in lower forms, but likewise the very considerable reduction in the amount of gametophytic tissue. In this large group of seed plants the prothallial portion of the young seed contains typically eight THE MEGASPORANGIUM AND SEED 231 nuclei, which by the fusion of two become seven. Of these, one nucleus surrounds itself with a protoplasmic body to become the egg, while two others are related to the so-called synergidae. Of the remaining four nuclear structures, three belong to the antipo- dals, a group of cells present in the base of the embryo sac or prothallus, while the fourth, the product of the fusion of two nuclei as mentioned above, becomes the : so-called endosperm nucleus, which later develops the endosperm or food substance of the ripened seed. In certain of the chalazogamous angiosperms (Fig. 171), notably Casuarina and the hazel (Corylus), tracheids are found present in the nucellus. The most natural inter- pretation of this condition is in connection with the tracheary apparatus in certain extinct seeds described in a foregoing paragraph. If the presence of tracheary tissues in the substance of the megaspo- rangium or nucellus in certain angiosperms is to be interpreted as the persistence of an ancestral char- ‘acter, it would indicate a relatively primitive position for the chalazog- amous forms in which it occurs. The structure of the mature seed in the angiosperms naturally claims a greater interest in a work devoted to anatomy. We may first take the cases of dicotyledons and monocotyledons. Fig. 172 illustrates the organization of the seminal organ of the Indian corn (Zea). To one side lies the embryo, which is provided with a single seminal leaf or cotyledon. This is very large in size and has its inner surface applied broadly to the food substance of the seed or endosperm. The embryo proper lies to the outside of the cotyledon and is characterized by the presence of the primary shoot, or plumule, and the primary root, or radicle. These are inclosed Fic. 172.—Seed of Zea mais 232 THE ANATOMY OF WOODY PLANTS in protective sheaths respectively known as coleoptyle and cole- orhiza. The endosperm and embryo are inclosed by a covering composed of the fused wall of the ovary and the integuments of the ovule. On the flatter side of the seed toward which the embryo Fic. 173.—Seed of Celastrus scandens Fic. 174.—Seed of Pinus palustris. is placed a more or less prominent elevation is seen which is the base of the style. Fig. 173 is a photomicrograph of a dicotyledonous seed. Here the embryo occupies a median position and is provided with two cotyledons instead of a single one. The endosperm or food substance, as a result of the position of the embryo, entirely sur- rounds the rudiment of the young plant. In the seed illustrated the coat consists of the hardened integument, and the wall of the ovary is not involved in the formation of the seminal covering. ' THE MEGASPORANGIUM AND SEED 233 The typical condition, of course, for both monocotyledons and dicotyledons so far as the coat or coats of the seed are concerned is that shown in Fig. 173, since only rarely does the wall of the ovary participate in the formation of the protective envelope. Certain other varieties are presented by the organization of the seeds of angiosperms. For.example, the endosperm or food sub- stance may be absent altogether, a condition illustrated by ‘the legumes and the Compositae among the dicotyledons and by the Orchidaceae among the monocotyledons. Again, the nucellar or megasporangial substance, usually absorbed as the development of the endosperm and embryo proceeds, sometimes persists and is then known as perisperm. Another variation which may present itself is the development of a supernumerary integument, often brightly colored, after the seed has been fertilized. This subsidiary coat is. known as the arillus and is frequently found in families not nearly related systematically. The organization of the seed in the pine is presented in Fig. 174 for comparison with the angiospermous conditions illustrated in Fig. 173. The integument is clearly distinguished as a hard in- vestment surrounding the abundant endosperm. The food sub- stance in the seeds of the gymnosperms is derived directly from the transformation of the gametophyte and is not a new structure, as is the case with the endosperm of angiospermous seeds. Within the substance of the endosperm lies the embryo, with its narrower end toward the micropylar region of the integument. The more slender portion of the embryo or young sporophyte is the primary root, which is capped with more or less lax tissues. These are the remains of the suspensors which in the developing seminal organ forced the young embryo down into the midst of the endosperm, The larger end of the embryonic sporophyte owes its breadth to the presence of numerous cotyledons or seed leaves, and these dis- tinguish the embryo of the pine from those of the angiosperms. CHAPTER XVII THE CANONS OF COMPARATIVE ANATOMY With the completion of the consideration of the various tissues and organs we are in a position to take up the relation of anatom- ical structure to evolutionary sequence in the various groups of vascular plants. Before we proceed to this phase of the subject, however, it will be necessary to consider the general principles or canons of comparative anatomy. It may be pointed out in this connection that anatomy, in common with other branches of the sciences, 1s based on inductive reasoning. The general principles are consequently arrived at as the result of the consideration of large numbers of facts with particular regard to the conclusions which may be drawn from them! The anatomy of plants has made great progress in recent years and in direct proportion to our increasing knowledge of fossil forms. The most interesting and valuable results from the evolutionary standpoint have been reached in connection with the anatomical investigation of extinct organisms of earlier geological ages. Naturally those of the great coal-producing period, the Paleozoic, first received attention on account of the importance of the study of plants of that age in connection with the search for productive coal seams. In more recent years the Mesozoic, which is of the greatest interest in relation to the appearance of our modern types, has begun to be studied. The results bearing on the advancement of our knowledge of the general principles of the evolution of plants exemplified in their anatomical structure cannot be too highly estimated. It will be the aim of the present chapter to set forth comprehensively the main conclusions of anatomical paleobotany in their relation to the interpretation of the affinities of the main groups of vascular plants now in existence on the earth. THE DOCTRINE OF RECAPITULATION An important general doctrine developed in connection with the evolutionary study of living beings is the hypothesis of recapitu- 234 THE CANONS OF COMPARATIVE ANATOMY 235 lation. It is assumed in connection with this doctrine that the young of any species may in the course of its individual development pass through the phases present in ancestral forms. As examples of this principle we may take extreme types of vegetation, such as the almost leafless cacti, forms with phylloclads, or those character- ized by the presence of short-shoots. In the mass of Cactaceae the leaves are abortive and are represented at most by spines. Inthe seedlings, in contrast to the adult, _z, the foliar organs are distinctly pres- . ent and are clearly recognizable as such. In coniferous species belong- ing to the genus Phyllocladus the branches in the mature state form flattened expansions known as phylloclads. If a seedling of any species of Phyllocladus be exam- ined, it becomes clear that a nor- mal round and leafy axis is present such as ordinarily characterizes the conifer (Fig. 175). Likewise in the pine the seedling shows the primary leaves arranged on the stem in the usual fashion for coniferous gymnosperms and not clustered on short-shoots or brachyblasts as in the adult branches of the genus. Further, in a conifer like the larch, which is differentiated in habit from the mass of the group by its deciduous foliage, we find in the seedling that the leaves persist for several years, thus revealing the probable ancestral condition for the genus. An additional example among the dicotyledons is supplied by the oak. The adult in north- ern oaks is characterized by deciduous leaves. Oak seedlings and saplings, however, even in the case of typically northern species, retain their leaves during the winter, thus recalling a situation characteristic of the live oaks of warmer latitudes which have evergreen foliage and represent anatomically the primitive type of organization. Fic. 175.—Seedlings and mature branch of Phyllocladus species. 236 THE ANATOMY OF WOODY PLANTS The phenomenon of recapitulation is not confined, however, to external features of organization, for it is often equally well exempli- fied by internal anatomical structure. A good illustration of the principle of recapitulation is presented by the seedling of the araucarian conifers. The adult stem of the kauri, or of any other araucarian conifer, is characterized by two unique features. One of these is the persistence of the traces belonging to the leaves long after the foliar organs have fallen. The foliar fibrovascular strands are continued for many years, amounting in some cases to centuries, through the activity of the cambium, even when the surface of the trunk has long ceased to show even the scars of the leaves of which they were once the fibrovascular supply. Further, in araucarian woods there is present a peculiar variety of tracheary structure which clearly differentiates their ligneous organization from that of all other living subtribes of conifers. The tracheids in the Arau- carlineae have their bordered pits arranged in an alternating manner and not disposed in an opposite fashion, as is the characteristic condition in the rest of the living conifers. In araucarian woods of the Mesozoic belonging to the genus Brachyoxylon the leaf traces persist only for a short time and are no longer formed through the instrumentality of the cambium after the leaves to which they belong have fallen from the stem. Again, the pits do not manifest the alternating and crowded condition presented by the wood of the living genera. In the seedling of both Agathis and Araucaria the leaf trace persists only so long as it is related to a functional leaf, and does not continue to develop for many years after the fall of the foliar organs, as is the case in the older trunk. Also in the araucarian seedling the pitting is like that found in the Cretaceous araucarian genus Brachyoxylon. In this instance we have a striking exemplification of the principle of recapitulation. The law or principle under consideration has many illustrations in the vascular plants, but on the whole it cannot be said to have so great a validity as among the higher animals. It is further necessary to note in the present connection that the absence of a given structure in young individuals is by no means evidence of its absence in the ancestral forms from which they have been derived. For example, there is good evidence that the cycadean THE CANONS OF COMPARATIVE ANATOMY 237 gymnosperms have come from ancestors possessing concentric bundles and centripetal wood, yet the seedlings of cycads in general do not support this conclusion by their anatomical organization. The doctrine of recapitulation is of value, accordingly, when it presents positive evidence from the seedling for the ancestral occurrence of a given feature of organization; but negative testi- mony from this standpoint must be estimated as having little or no value. A failure to realize this situation is responsible for much fallacious biological reasoning. A very important exemplification of recapitulation is frequently supplied by the first annual ring of the older stem of arboreal forms. Often in groups which have suffered considerable reduction, such as, for example, the gymnosperms in general, the phenomenon of recapitulation, although absent in the seedling, may be clearly illustrated by the first annual increment of woody growth in the older regions of the stem. An illustration of this principle is supplied by the living araucarian conifers. Taking as an example the genus Agathis, the kauri of Australasia and the East Indian region, we find in the first annual ring an organization distinctly different from that in the subsequent annual increments of the wood. More or less abundant wood parenchyma is present, although longitudinal storage elements are conspicuous by their absence in the adult wood of the stem. ‘This situation is of great interest in view of the fact that the fossil wood of the kauri from American Cretaceous deposits is characterized by the presence of parenchymatous cells, not only in the first annual ring, but in all subsequent zones of ligneous growth. The persistence of the structure of Mesozoic forms in the first annual ring of living species of the genus Agathis is a feature most appropriately falling under the principle of recapitulation. The situation here indicated is of great value and wide validity, not only for the gymnosperms, but also for the dicotyledons. It might readily be much more abun- dantly exemplified in the present connection, but the instance supplied above will serve to make the situation clear. Many other cases will present themselves in later chapters in connection with the discussion of the evolution of the different groups as inferred from their anatomical organization. 238 THE ANATOMY OF WOODY PLANTS THE DOCTRINE OF CONSERVATIVE ORGANS This doctrine has received a great impetus from the study of Mesozoic conifers, but was first put forward, naturally enough, in connection with comparisons between the older existing gymno- sperms and their Paleozoic ancestors. The leaf first came into prominence in relation to the hypothesis of conservative organs. It has been known for many years, particularly since the investiga- tions of Mettenius, that the foliar organs of the Cycadales present remarkable features of anatomical structure. Here the fibro- vascular bundles of the leaves are distinguished by the presence of centripetal or cryptogamic wood, a detail of organization conspicu- ously absent in the stem of the genera of the living Cycadales. In the Cycadofilicales of the Paleozoic the bundles of the stem were always characterized by the presence of centripetal xylem and sometimes by concentric organization as well. The Cycado- filicales are by common and competent consent regarded as the ancestral types from which the living cycads have been derived. The clear and universal presence of centripetal wood in the foliar fibrovascular bundles of living genera of the Cycadales is good evidence at once of the relationship of these gymnosperms to the Cycadofilicales and of the validity of the doctrine of conservative organs so far as it applies to the anatomy of leaves. Many other illustrations of the prevalence of this principle might be supplied in foliar organs, but the one described above will serve appropri- ately to elucidate the situation and is particularly apposite in the present connection because it is probably the first case to be cited in evolutionary anatomy. The foliar organs are not, however, the only parts of the adult plant which present illustrations of the principle of conservative organs. The stem in that region devoted to the function of repro- duction has also figured strikingly in this connection. To Scott belongs the credit of having drawn attention to the fact that the peduncle or base of the cone in certain Cycadales furnishes a clear example of the persistence of an ancestral structure in the reproductive axis which has quite disappeared in the ordinary vegetative stem. In Stangeria, Zamia, and other genera of the Cycadales he noted that the fibrovascular strands of the axes THE CANONS OF COMPARATIVE ANATOMY 239 of the cones frequently manifested the presence of vestiges of centripetal wood, although xylem belonging to this category has wholly disappeared in the vegetative axis. The value of this generalization can scarcely be overestimated. During the interval of nearly twenty years dating from Scott’s brilliant discovery, much additional evidence has been supplied in support of the conservatism of the anatomical structure of the reproductive axes. For example, it has been shown by comparison of the vegetative organization of Mesozoic conifers with the anatomical structures found in the ovuliferous cones of living forms that the latter fre- quently perpetuate features which have vanished in the vegetative parts. This is manifestly the case in the abietineous and arauca- rian conifers which compete with each other for the claim of being the most ancient representative of the coniferous stock. The cone in both Pinus and Agathis presents numerous Mesozoic features which have disappeared elsewhere in the stem organs of existing species belonging to these genera. The value of the anatomy of reproductive axes cannot be estimated so highly in the case of the angiosperms, since the relatively slight development of fibrovascular structures in flowers and inflorescences leaves less scope for the appearance of phylo- genetically significant structures. This situation needs to be particularly emphasized in view of some recent highly fallacious attempts to utilize the anatomy of reproductive axes in working out evolutionary sequences in the woody dicotyledons. Clearly in this instance only structures are significant which find adequate development in the somewhat slender annual woody cylinder of the flowering parts of perennial dicotyledons. In the monocotyledons the restrictions on interpretation are still greater on account of the usual absence of secondary growth in this great division of the angiosperms. In the application of the doctrine of conservative parts to the reproductive axes of the angiosperms it must be recognized that a little knowledge is a dangerous thing. It has been made clear in the preceding paragraphs that the doctrine of conservative parts is well exemplified by the leaf and is manifested in the stem by the more archaic axes connected with reproduction. The situation in the organs cited has for a long time 240 THE ANATOMY OF WOODY PLANTS been apparent. Of more recent origin is the realization that, in modern plants at any rate, the root is the most valuable of all organs from the standpoint of evolutionary anatomy. In the case of comparisons between Paleozoic and Mesozoic groups the root, in fact, has proved to be in general too conservative to furnish significant examples of the retention of ancestral characters. The search for centripetal or cryptogamic wood has been in the fore- ground in investigations bearing on the relationship between Paleozoic and Mesozoic groups. Since in all forms of every geo- logical age the root has centripetal primary wood, in regard to this crucial feature of more ancient types it obviously does not supply distinctive evidence in connection with the doctrine of descent. In other respects, however, and particularly with reference to the organization of the tissues of the secondary wood, the root has proved itself to be of greater significance than any other organ of the higher plants. Of course the most striking evidence of con- servatism in the root has resulted from the comparison of Mesozoic and modern forms. It has, for example, been shown that the root in modern conifers clearly and persistently perpetuates the features of organization which characterized the structure of the stem in the Cretaceous and earlier periods of the Mesozoic age. In Pinus and Agathis the root presents in many of its earlier annual rings the distinctive organization found in the stem of these types in the Mesozoic. Nor is the inherent conservatism of the root of value in the study of the gymnosperms alone. Although our knowledge of the anatomical structures of the angiosperms in Mesozoic times is as yet extremely inadequate, we are able in many instances by the application of the doctrine of the con- servatism of the anatomical organization of the root to infer the ancestral type of stem in the highest vascular plants. It will be evident from the foregoing paragraphs that conserva- tism is particularly inherent in the leaf and root of vascular plants and that the highly progressive stem presents only features which are of interest from the standpoint of the doctrine of descent, either in its first annual ring or in axes specially allocated to the function of reproduction. The sporangium is a fourth structure recognized as a primitive organ of vascular plants in an earlier chapter of the THE CANONS OF COMPARATIVE ANATOMY 241 present work. Here the lack of complexity of organization rather militates against the presence of phylogenetically important structures. It must nevertheless be noted that the sporangium is an extremely conservative organ and, as far as the relative simplicity of its organization supplies points of comparison, is of very great significance for the doctrine of evolution. It has been demonstrated in an earlier chapter that the sporangium perpetuates the protean centripetal xylem in the form of its opening mechanism to a higher point than any other organ but the root. The value of the spore sac in phylogeny, although limited by the relative simplicity of the organ,-must consequently be estimated as great. The doctrine of conservative organs is of the greatest signifi- cance in cqnnection with the study of the evolutionary history of plants, because of the abundance and reliability of the evidence which the various parts furnish in this connection. Obviously, if leaf, reproductive axis, root, and sporangium all supply consonant and harmonious testimony in the same direction, a sound con- clusion must inevitably be reached. There can be little question that the doctrine of conservative organs is the most important one which modern inductive anatomy has supplied as a tool of evolu- tionary investigation. In fact, the general principles included under this head are of such great significance that the present volume may be considered as written only for those whose anatom- ical training has progressed to such a point that they are able to appreciate the universal value and validity of the doctrine here discussed. THE DOCTRINE OF REVERSION This doctrine is well shown in the case of plants with a consider- able amount of secondary growth—namely, the gymnosperms and the dicotyledonous angiosperms. It is of little value in herba- ceous forms, whether cryptogamic or phanerogamic, since in these the effects of injury are usually in the direction of degeneracy only. In plants with secondary growth and consequently more massive organs the effect of injuries frequently is to recall ances- tral features of organization. This phenomenon is called reversion. Only in certain conifers can we observe the effect of injury in recalling in living forms features which are known to have been 242 THE ANATOMY OF WOODY PLANTS present in their Mesozoic forebears. For example, in the arau- carian conifers, cited earlier in another connection, the Mesozoic organization of the wood is recalled in the stem of the existing species as a consequence of injury. The wood formed subsequent to the infliction of the injury shows a type of structure charac- teristic of the group in an earlier geological epoch. Although only in rare instances can structures which are actually known to have been present in the past be recalled by injuries, in many other cases we find the infliction of wounds followed by the for- mation of features which are normally present in the conserva- tive organs. Consequently the doctrine of reversion finds support, not only in the facts of paleobotanical anatomy, but also in the much more richly exemplified doctrine of conservative parts. It is further clear that we cannot interpret all structural peculiarities which result from injury as reversions to a former condition of organization, but only those which are definitely paralleled by known conditions in fossil forms or are illustrated in the anatomy of the conservative organs—the leaf, reproductive axis, and stem, or at least some of these. Carefully as the doctrines of recapitulation and of conservative parts must be applied to elucidate the course of evolution, the principle of reversion must be invoked in phylogenetic studies with even greater precautions. A wide knowledge of fossil forms as well as an extensive acquaintance with the facts of comparative anatomy are necessary for a successful application of this doctrine to the data derived from the investigation of injuries. In this connection it is further necessary to distinguish clearly between the phenomena of hypertrophy and those of actual reversion. For example, when the stem of a dicotyledon or of a conifer is injured, a local damming of food substances results as a consequence of the elimination of the conducting tissues of the phloem in the immediate vicinity of the wound. Overdevelopment consequent on over- nutrition accordingly is locally most conspicuous. Very often true reversionary changes resulting from the impulse supplied by the injury present themselves only at some distance from the wound. This situation is found in the conifers in connection with reversionary conditions following injuries in the case of the rays THE CANONS OF COMPARATIVE ANATOMY 243 which ordinarily manifest themselves, not in the actual wound cap or hypertrophied mass of wood formed after injury, but on the opposite side of the stem. Among the dicotyledons the birch exemplifies the same condition in regard to the formation of aggre- gate rays. The diffuse structure of radial parenchyma which characterizes the normal organization of the wood of the genus Betula gives way to a condition of aggregation following injury, not on the edges of the wound (that is, in the actual wound cap), but in the region of the axis diametrically opposite to the injury. In accordance with the general reversionary principles here stated, the wound cap as often as not presents structures in an advanced or accelerated, and not in a reversionary, condition. Some recent publications on the anatomy of the dicotyledons reveal a failure to realize this fundamental principle, and therefore it is well that it should be emphasized in the present connection. The foregoing paragraphs elucidate the most important canons or principles of evolutionary anatomy. It cannot be too strongly urged that all the evidence available under the various principles here described and exemplified should be brought into considera- tion, as a failure to check up one kind of evidence against another often results in a fallacious and ephemeral deduction. The most cogent testimony to the validity of any evolutionary conclusion is naturally supplied by the conditions actually realized in ancestral fossil forms. Since, however, by reason of the incompleteness of the geological record and our consequent ignorance of the organiza- tion of older forms we are frequently not in the position to avail ourselves of the actual past history of given plant types, we must of necessity have recourse to the valuable aid furnished by the important general principles described in the earlier paragraphs of the present chapter. Where the canons of evolutionary anatomy are judiciously employed, the result is usually so clear and convin- cing as to commend itself to the unprejudiced mind. CHAPTER XVIII THE LYCOPSIDA AND PTEROPSIDA The discussion of tissues and organs and the elucidation of the general principles applicable to these in the earlier chapters of the present work bring us to the point where the higher plants may profitably be discussed in regard to their general anatomy and evolutionary affinities. Obviously, if it is possible to compass a general grouping which will at the outset indicate the main lines of evolution, the consideration of the particular groups will be much facilitated. Some years ago the writer put forward a general classification of vascular plants, based on the cardinal features of the reproductive structures and the salient anatomical characters. This attempt to group the higher plants in accordance with their more important reproductive and anatomical features has met with approval among competent judges and as a consequence may be conveniently utilized in the present connection. A general survey of vascular plants, existing and extinct, reveals the fact that there are certain features correlated in a significant way. For example, a large number are characterized by the possession of ventral or adaxial sporangia together with usually small leaves. Another large assemblage presents relatively large leaves and more numerous sporangia which are dorsal or abaxial in position. The former group is characteristically repre- sented by the lycopods or club mosses and their allies, while the latter includes the ferns and the forms more nearly related to them, the gymnosperms, and the angiosperms. The first aggregation of types, known as the Lycopsida, is now practically extinct, but played a large réle in the Paleozoic and furnished a considerable proportion of the raw material of that extremely important com- bustible called coal, together with its derivative products, petroleum and natural gas. The second alliance, to which the appellation Pteropsida is appropriately given, although abundantly present in the remote past, still prevails and has given rise to the seed plants 244 THE LYCOPSIDA AND PTEROPSIDA 245 and to the forests of Mesozoic and Cenozoic times, as well as to the herbaceous types which under modern conditions more and more predominate in the plant population of our earth. A more detailed characterization of the Lycopsida is now desir- able. Fig. 176 represents diagrammatically the organization of an axis of the lycopsid type together with its appendages. The latter consist of leaf, branch, and root. Root and branch are intimately associated, the former usually proceeding from the base of the latter. The upper end of the main axis is represented in transverse section to show the anatomical relations of the organs. The fibrovascular cylinder in the particular case illustrated is siphonostelic, although it might equally well be protostelic, espe- cially in the lower representatives of the group. The tubular stele or central cylinder constituted by the fibrovascular sys- tem is interrupted only at one point—where the fibrovascular supply of a branch takes its origin from the main cylinder. The gap thus appearing is known as the branch gap or ramular lacuna. On the margin of the stem appear certain projections, the leaf bases, within which are included the fibrovascular strands destined for the leaves or foliar traces. These subtend projections on the surface of the central cylinder occupied by groups of proto- xylem. The projections in question are the starting-points ‘of the foliar traces, and it is clear that in no instance is there an inter- ruption in the continuity of the central cylinder corresponding to the departing leaf traces. The central cylinder of the Lycopsida is said on this account to be without foliar gaps. The absence of leaf gaps or foliar lacunae is characteristic of all the Lycopsida and is a diagnostic feature of importance for the great group or phylum which they represent. Even in those Lycopsida in which the leaves are, superficially at least, relatively large (for example, the Sigillariae, in which the foliar organs were sometimes over a meter in length) there were still no foliar gaps. The absence of foliar gaps is an anciently inherited or palingenetic feature of the Lycopsida, and they may therefore be technically characterized as palin- genetically microphyllous (small-leaved). Not only has this large group universally small leaves, but it also possesses another important, salient, and constant general XXX? OXXXXXXXX? XK KOS SONS KORY EK ‘ XXX (\ AX) oN x) XXX? “ OX’ % THE ANATOMY OF WOODY PLANTS Fic. 176.—Diagrammatic representation of the Lycopsi THE LYCOPSIDA AND PTEROPSIDA 247 feature of organization—in this instance related to reproduction. In the phylum under discussion the sporangia or spore sacs are invariably on the upper or adaxial (ventral) surface of the sporo- phyll or reproductive leaf. The sporangia are single or at most relatively few in number and are invariably ectokinetic in their mode of dehiscence. ‘True seeds seem never to have made their appearance in the Lycopsida, although, as has been pointed out in an earlier chapter, structures somewhat simulating seeds have been found in certain of the Paleozoic representatives of the group. The organs in question, however, lacked a true integu- ment and, so far as is known, were without arrangements for receiving the microspores or pollen grains, a universal equipment in the case of pteridospermous and gymnospermous seeds. Possibly the failure to achieve true seminal structures was the cause of the decline of the Lycopsida, which at the present time constitute an insignificant proportion of the vegetation of the world. The group is very ancient and goes back to the beginning of the geological record. The primitive forms representing the Lycopsida were often arboreal in their habit, and the alliance reached its culmina- tion in the carboniferous forests of the Paleozoic. It became largely reduced in the Mesozoic, and the Cenozoic saw its virtual extinction. In the Pteropsida we have to do with forms in which the leaves are relatively large in comparison to the stem and often extremely complicated in structure. As is shown in the diagram (Fig. 177), the transverse section of the stem reveals a central cylinder which, when siphonostelic, as in the illustration, is characterized by gaps corresponding to the traces departing to the leaves. This feature of its anatomy is in marked contrast to that found univer- sally in the Lycopsida, in which the leaves are not related to foliar gaps. The traces of the branches in the Pteropsida likewise sub- tend gaps in the central cylinder (which may be designated as ramular gaps). The fibrovascular supply of the root makes its exit from the stele or fibrovascular cylinder without causing any gap or interruption. The roots are often, but not invariably, related to the bases of the leaves. The foliar organs, usually much larger in size than in the Lycopsida and often of great dimensions and lobed in a complicated manner, are to be regarded as palin- se 25 COOYY RRR YOOea Se SEB) RRR) LAS Qo < Ter 5 ae a ‘ ea \ \\* . NS \\ < Fic. 177.—Diagrammatic representation of the Pteropsida THE LYCOPSIDA AND PTEROPSIDA 249 genetically megaphyllous, since their anatomical relations are always characterized by the presence of foliar gaps. The repro- ductive organs or sporangia in the case of the Pteropsida are on the lower or abaxial (dorsal) surface of the leaf, and are often numerous and complicated in structure. In the lower forms the dehiscence of the spore sacs is ectokinetic, but in the higher representatives of the phylum the opening mechanism is derived from modified transfusion tissue (in turn derived from the centripetal wood of the ectokinetic and lower forms). Those Pteropsida characterized by an internal reproductive mechanism derived from transfusion tissue are appropriately designated as endokinetic. The higher members of the series have developed true seeds provided with an integument and equipped with an apparatus either related to the seed itself or to the seed leaf (or megasporophyll) for the reception of microspores. or pollen. Although developed in very early geological times in forms resembling ferns, the Pteropsida are still in full vigor; and in their highest manifestation, the angiosperms, they constitute an overwhelmingly large proportion of the present vegetable population of the earth. They have reached their zenith of efficiency in the herbaceous angiosperms, which in all probability will supplant arboreal angiospermous types in the not very remote future. The gymnosperms, and in particular the conifers, were the prevailing Pteropsida of the Mesozoic, while in the Paleozoic age pteridosperms (Cycadofilicales) and other lower gymnosperms and fern allies represented the group. The Pteropsida and Lycopsida are distinct as far back as the geological record can be perused, and there seems to be little doubt that they constitute two primitive stocks of vascular plants. They are so clearly diverse even in their earliest manifestations that it is difficult to picture how they may have been formerly connected. It is obvious, however, that the lycopsid type has not been able to cope with the changing conditions of environment and, comparatively early in the periods recorded in the rocks, was relegated to a position of relative inferiority. Whether this situa- tion was the result of the failure to achieve true seeds or is to be explained as the basis of some fundamental defect of internal organization incapacitating the Lycopsida to succeed in competition 250 THE ANATOMY OF WOODY PLANTS with the large-leaved Pteropsida must, for the present at any rate, be left an open question. Although the Lycopsida were the pre- dominant constituent of the Paleozoic forests, the Pteropsida in many cases have entered largely into the composition of the more ancient coals and can often be clearly recognized, particularly in the carboniferous coals of the Middle Western states (Illinois, Ohio, etc.), as charred remains of the axes and even as pinnae or smaller segments of the leaves in the form of so-called ‘“‘ Mother of Coal.” After having described the general characteristics of the Lycop- sida and Pteropsida, we find it in order to indicate the main groups which come under these two great divisions of the vascular plants. The Lycopsida include two principal subdivisions—the Lycopo- diales and Equisetales. The Lycopodiales are characterized by the alternating nature of their foliage, while the Equisetales have their leaves disposed in whorls on a stem presenting marked ridges and furrows. The Lycopodiales are again subdivided into isos- porous and heterosporous families. Of the former there are two— the Lycopodiaceae and the Psilotaceae. The Lycopodiaceae are characterized by the possession of well-developed roots and un- divided sporangia, while in the Psilotaceae the sporangial struc- tures are septate, and organs of the nature of roots are entirely absent. ‘The heterosporous Lycopodiales have in common a foliar appendage, known as a ligule, which is present on both vegetative and reproductive leaves, and in the case of the latter occurs just above the insertion of the sporangium. Of the three families presenting the phenomenon of heterospory the first, the Selaginel- laceae, are terrestrial forms included under a single genus, Selaginella, in which the megasporangia never produce more than four spores. In the second and usually aquatic family, the Isoetaceae, there is likewise a single genus, but the sporangia are provided with trans- verse processes known as trabeculae, and the megaspores are numerous in each sack. Lastly, the Lepidodendraceae, including the Sigillariae and their allies, are terrestrial extinct forms often of arboreal habit and of somewhat diverse megasporangial structures. The Equisetales, as has been indicated at the beginning of the foregoing paragraph, are distinguished by the whorled arrangement of their leaves. Another feature which they possess in common is THE LYCOPSIDA 'AND PTEROPSIDA 251 the usual exhibition of a high degree of multiplication of the sporangia which are often disposed on common stalks known as sporangiophores. The branches instead of being truly axillary are borne alternately with the leaves at the nodes. The Equisetales may conveniently be divided into three families—the Sphenophyl- laceae, the Calamitaceae, and the Equisetaceae—which are in all probability related to one another in the order indicated by their enumeration. The Sphenophyllaceae were forms in which the central cylinder of the stem was protostelic. The cones consisted of sporophylls presenting various degrees of complication. In the simplest forms the sporangia were inserted singly on the stalks or sporangiophores and were numerous for each sporophyll. In more advanced types the sporangia became two or more for each spo- rangiophore. The Calamitaceae, like the Sphenophyllaceae, are organisms entirely extinct. They usually possessed the arboreal habit and were invariably characterized by a siphonostelic central cylinder. The sporangiophores bore four sporangia and were variously related to the sporophylls. In the Equisetaceae are included a number of genera, living and extinct, of herbaceous habit and possessing so far as is known a simplified type of cone in which sporophylls are represented by the sporangiophores alone. In the Pteropsida, marked by the general features enumerated in earlier paragraphs of the present chapter, there are three large subdivisions—the Filicales, the Gymnospermae, and the Angio- spermae. ‘The first of these, as the name indicates, include the fernlike forms—that is, those in which the reproduction takes place through unicellular bodies known as spores. In the Gymnospermae true seeds are present which in every case are equipped to receive the microspores; and these after germination effect fertilization either by means of antherozoids (Archigymnospermae) or through the agency of pollen tubes (Metagymnospermae). In the last and (in the present epoch) most important subdivision of the Pterop- sida, the Angiospermae, the pollen is received on the apex of the closed megasporophyll and no longer falls upon the seed. Fertiliza- tion is invariably by means of a pollen tube. The habit of the angiosperms is either arboreal or herbaceous, and the fibrovascular tissues show a high degree of specialization. CHAPTER XIX THE LYCOPODIALES This group, as has been indicated in the last chapter, has spiral phyllotaxy. It includes both isosporous and _heterosporous families. The latter are distinguished by the presence of a ligule, while in the former this structure is lacking. In the genus Lyco- podium the central cylinder of the stem is radial and protostelic. Asa consequence of the radial organization of the stele, the masses of phloem lie in the intervals between the generally radially directed bands of xylem. The sieve tubes are separated from the tracheids by several rows of parenchyma on either side. In the vertically directed reproductive axes of Lycopodium the organization of the fibrovascular tissues is typically radial, while in the creeping stems or rootstocks the arrangement of the xylem and phloem is somewhat dorsiventral. The upright axes of Lycopodium, aside from the fact that they bear leaves, are scarcely distinguishable in structure from the roots. This resemblance in organization between root and shoot is an indication of the antiquity of the lycopodineous stock, since in the higher groups the differentiation between the axial and radical organs becomes more and more marked. The monotypic genus P/ylloglossum possesses a siphonostelic stem. In this form the lower region of the axis is tuberous and contains the most massive development of the fibrovascular system. In the tuber also, as is shown in Fig. 178, there is both internal phloem and internal endodermis. As the stele of the inferior region passes upward, it gives off a branch into the peduncle of the tuber which is to perpetuate the plant in a subsequent season. The trace of this appendage in departing from the central cylinder leaves a well-marked branch gap. The foliar organs indicated as swellings on the outline of the section cause no interruptions in the continuity of the central cylinder by their departure from its surface. In this respect Phylloglossum shows itself to be a veritable repre- sentative of the Lycopsida. In the higher and aérial region of the 252 THE LYCOPODIALES 253 axis the fibrovascular tissues become so much reduced that internal phloem is no longer developed, and the continuity of the cylinder is interrupted by gaps which are not related to organs, but merely indicate the incom- plete development Otitine xylem: Where a trace is given off, as is shown in Fig. 179, it takes its origin opposite a strand and does not sub- tend an interval be- tween the bundles, clearly showing the lycopsid condition, even in the state of stelar reduction pre- sented in the evan- escent aérial axis. The Psilotaceae are anatomically distin- guished from the Lyco- podiaceae by the absence of true roots. Here the aérial stem, unless it be of very small size, is siphono- stelic in its organiza- tion. A thick-walled medulla is often pres- ent, but no internal phloem has been ob- Fic. 179.—Diagram of exit of leaf traces in the served. The organiza- aérial stem of Phylloglossum (after Bertrand). Fic. 178.—Diagram of the lower region of the stem in Phylloglossum (after Bertrand). dx@2s By G'e%e: f, () 5c Ia gto ee 5) tion of the conducting tissues is radial and exarch; the leaf traces, as in Lycopodium, take their origin from the angles of the stele. In smaller aérial shoots and in the subterranean ones the central cylinder is usually protostelic. Sometimes gaps are present in the walls of the tubular cylinder of 254 THE ANATOMY OF WOODY PLANTS the larger stems, but these in no case are related to outgoing foliar traces. The general topography of a stem of the type found in the Psilotaceae is presented in Fig. 180. In the Lycopodiaceae in general the leaf traces are ordinarily mesarch in their organization, a condition more or less characteristic of the Lycopsida as a whole. An endodermis can usually be distinguished about the foliar strands, although this limiting layer is ordinarily con- spicuous by its absence Fic. 180.—Transverse section of the stem of in the stem in most spe- Psilotum. cies of Lycopodium. In other representatives of the two families under discus- sion an external endoder- mis is usually found in the stem, and, as has been shown above, an internal endodermal zone is seen in the tuberous subterranean stem of Phylloglossum. In the genus Selaginella the fibrovascular tissues of the axis are distinguished by considerable variety in topography. In some spe- Fic. 181.—Transverse section of stem of cies the stele is a single Selaginella laevigata, showing a siphonostelic mass, separated from the central cyan: cortical tissues by an air-containing region representing the endo- dermis. In other species the fibrovascular system becomes divided, and the protostelic condition as a result passes into that known as THE LYCOPODIALES 255 polystelic. In still another modification, presented by S. /aevigata from Madagascar (Fig. 181), a true siphonostele is exemplified which is complicated by the presence of medullary strands joining up with the walls of the tube in the regions where branches are given off. In the species under discussion the traces of the leaves illustrate the condition typical for the Lycopsida and pass off from the cylinder without causing any gaps in its continuity. 7 @ TOL SAS jak : ; Ne BAGG O7.- Pm. Tsoetes has a protostelic stem We ay oy > S — oe, y NS eee ee/ which is remarkable among ex- &. ~. isting Lycopsida in manifesting .,-“\dc Ser, well-marked secondary growth fi Wei v7 PS), (Fig. 182). The external prod- SE uct of cambial activity is a eee radially disposed storage paren- as oS REE chyma, while internally the di- oN (Sa viding layer originates additions EWS to the fibrovascular tissues Cat ae. < which are most commonly inter- SRN — preted as consisting of alternate ay wa 9 mee a zones of xylem and phloem. Fs OG Be The situation here, however, is Y 5S GS) disputed, and uncertainty per- LOSS SSL) = sists as a result of the indifferent ” “8G Vo fe) ax development of the tissues re- sulting from the characteristic- ally aquatic habit of the plant. The roots in /soetes are distin- guished, in common with the smaller radical organs of a number of the lower Lycopsida, by the fact that they develop a single mass of xylem in proximity to a single strand of phloem. The leaf is not worthy of special note. In the Lepidodendraceae the stem manifests great diversity of structure, as would naturally be expected in a group which in Paleozoic times displayed numerous types with generally marked secondary growth. The primary structures of the stem were either protostelic or siphonostelic. In the former condition a considerable amount of parenchymatous tissue was developed Fic. 182.—Cambial activity in Isoetes 256 THE ANATOMY OF WOODY PLANTS among the tracheids, particularly toward the central region of the stele. This peculiar organization of the median area of the stele in protostelic lepidodendrids is responsible for a hypothesis as to the origin of the medulla or pith. Quite generally it is con- sidered that by continuing the process of transformation of tracheids, first into short tracheary elements and then into paren- chymatous cells, there is formed in the center of the stele a pith of stelar origin. In accordance with this view the central re- gion of the stele in many protostelic lepidodendrids is called a ‘‘ partial pith.”” There is no conclusive evidence, however, that the so- called “ partial pith” in reality gives rise to the true medulla in those lepidoden- droid types which possess it. More- over, the evidence in thevea sie ots thie Pteropsida, which are very much better displayed in the period of time which we are able to investigate, is distinctly against the validity of the stelar origin of the pith, since the medulla in the large-leaved vascular cryptogams shows very marked indications of derivation from the fundamental system. It seems on the whole more likely that the medulla in the lepidodendrids, where such a structure is found, is an inclusion of fundamental tissues on the part of the stele. This conclusion is particularly favored by conditions found in lepidodendroid stems in which there is no indication of secondary growth, as, for example, in Lepidodendron Spenceri, shown in Figs. 183 and 184. Here the medulla is largely occupied by dark-brown sclerenchymatous tissues similar Fic. 183.—Transverse section of the stem of Lepido- dendron S penceri. THE LYCOPODIALES 257 to those appearing in the cortical region. It may accordingly be stated that even the imperfect evidence supplied by the stem of the lepidodendrids in a condition of obvious degeneracy of the primary stelar tissues when they are first presented on the pages of the geological record does not definitely justify the conclusion that the pith is of stelar origin. In a later chapter it will be made clear that the evidence supplied by the lower Pteropsida, which is at once more abundant and more decisive, dis- tinctly vouches for the extra-stelar derivation of the medulla. The degeneracy of the tracheary elements which has already been noted in the case of the protostelic type of cylinder in the lepidodendrids makes itself par- is ticularly obvious Fic. 184.—Part of the same, more highly magnified im” the higher siphonostelic representatives of the group and especially in the stems included under the Sigillariaceae. The reduction in amount of the primary tissues results in the appearance of gaps in the wall of the stelar tube which are not related to appendages. The central cylinder consequently becomes discontinuous, as has been shown in Fig. 122, page 170. Since the later-developed secondary tissues naturally first appear opposite the framework outlined in the primary wood, the secondary xylem is likewise at the beginning of its formation discontinuous, and continuity appears only after cambial activity has resulted in the formation of a woody cylinder of some thickness. Where the primary struc- ture of the xylem has undergone the extreme degree of reduction 258 THE ANATOMY OF WOODY PLANTS found in the stem of many of the Equisetales as well as of all but the very lowest seed plants, the initial discontinuity of the secondary wood often becomes very marked. The situation presented by these extreme types unco-ordinated with the eluci- dative anatomical features presented by more primitive forms has been the cause of serious misunderstanding as regards the origin of the so-called medullary rays. The case of the siphonostelic lepidodendrids and Sigillariae, as diagrammatically represented in Fig. 122, page 170, seems to indicate definitely that parenchymatous interruptions in the secondary cylinder resulting from the dis- continuity of the primary wood cannot be interpreted as true rays any more than are the gaps related to the departing traces of appendages to be brought into the category of rays. Much confusion of definition has resulted from the failure to interpret the conditions found in higher forms in terms of the structures presented in earlier and more primitive types. It has been made clear in an earlier chapter that the lepido- dendrids proper, which beyond question represent the more primitive state of organization for the Lepidodendraceae as a whole, supply evidence for the derivation of radial parenchyma as the result of the transformation partial or complete of radial tra- cheary strands into storage parenchyma. The older representa- tives of the Lepidodendraceae show themselves in this respect the most archaic of all the vascular plants with secondary growth. Not only is the origin of radial storage cells in the secondary xylem elucidated by the lepidodendrids, but, as has been pointed out in an earlier chapter, the parenchymatous elements of the primary wood have their origin illustrated in the conditions found in the primary region of the stem in this ancient group of vascular plants. It has been indicated in Figs. 29 and 30 that the living cells occurring in the wood of the primary region of the axis in protostelic lepido- dendrids have been derived by septation from elements belonging to the category of tracheids. Some of the resultant elements persist as short tracheids with thickly reticulated walls, while others maintain a thinner wall and in all probability in life were occupied by living protoplasm. In the siphonostelic Lepidoden- draceae and in the sigillarian forms as a whole there is no evi- THE LYCOPODIALES 259 dence as to the origin of parenchymatous elements in the primary xylem. In the later (Permian) representatives of the Sigillariae the primary cylinder became so much reduced that it was no longer continuous. This topographical condition of the primary wood was responsible, as indicated above, for a resultant discontinuity of the secondary xylem. The processes of the pith extending between the primary bundles and a short distance into the second- ary cylinder are in a certain sense medullary rays, since they take their origin from the medulla; but they have nothing in common with the radial masses of storage tissue resulting from cambial activity which characterize the organization of the secondary cylinder. Further, they should not in any way be confused with foliar gaps, since in the Lycopsida interruptions of this nature in the fibrovascular cylinder do not occur. In the particular case under consideration the leaf traces originate opposite the strands of primary xylem and do not subtend the intervals between them. It is clear that the Lepidodendraceae, although entirely extinct, furnish extremely valuable data for the elucidation of the origin of the parenchyma in the primary wood and for that of the radial storage devices of the secondary xylem. Further, they throw a very clear light on the general morphology of the secondary woody cylinder in vascular plants, since the comparative study of their stems from lower to higher geological levels makes it obvious that the radial parenchymatous bands of the secondary wood cannot appropriately be called medullary rays. They should be called wood rays, as the inward relation to the medulla is neither a primitive nor an essential condition. Not only in regard to the parenchymatous structures of their primary and secondary wood, as well as by their great geological age and early culmination, do the lepidodendrids in the large sense show themselves to be primitive representatives of vascular plants, but also by the organization of the fibrous elements of the secondary wood. It has been pointed out in an earlier chapter that a typical element of the primary wood in all plants is the scalariform tracheid. In the secondary xylem of plants in general the scalariform element has given place to the pitted tracheid, which is universal for the various groups of gymnosperms and for the angiosperms with 260 THE ANATOMY OF WOODY PLANTS secondary growth. In the Lepidodendraceae in the narrower sense the secondary wood is distinguished from the primary struc- tures only by the presence, exclusively, of radial parenchyma and by the radial seriation of its tracheary elements (Fig. 185). The organization of the tracheids of the secondary wood is, in fact, identical with that found in the primary region. In the higher lepidodendroid forms assembled under the appellation Sigillariae very frequently, 2a ee particularly in the Pee regvon, of “ihe secondary wood more remote from the pith, the tra- cheids cease to be scalariform and assume the pitted type characteristic of the gymno- sperms and other higher representa- tives of the Vascu- lares. The vascular Fic. 185.—Longitudinal section through primary and strands of leaves in secondary wood of Lepidodendron species. the lepidodendrids are characterized, as are those of the Lycopodiales in general, by mesarch organiza- tion. This condition is clearly shown in Fig..186. It is appar- ent that the foliar trace is surrounded by secondary wood. It has been stated by Scott that true transfusion tissue is present in the leaf of the lepidodendrids, but this statement, in view of the situation present in the Lycopodiales in general and in the Lepido- dendraceae in particular, seems open to some question, and certainly the subject seems to require further investigation. The foliar organs of the lepidodendroid stock were characterized by the presence of two aérating strands on either side of the foliar trace; these were in communication below with the external air through the agency THE LYCOPODIALES 261 of stomata, ordinarily accommodated in furrows on the lower surface of the leaf. The aériferous structures of the blades of the leaves were continuous with air-containing radial structures in the outer and inner bark known as parichni. ‘These are a noteworthy feature of structure in the lepidodendrids and have attracted a large amount of attention from students of the group. It should be pointed out, however, tt that they are by no means a unique structure, since special aérating devices are likewise found present in relation to the leaves of the Coniferales. The roots of the lepido- dendrids have been the subject of much discus- sion. Their ultimate divisions, the so-called stigmarian rootlets (Fig. 187), are character- ized by a very simple organization, since only a single group of protoxy- lem is present. The root- mrp oma lets of this order divided Fic. 186.—Leaf trace of a lepidodendrid dichotomously, as is often Sch G the case with those of the living Jsoetes and Lycopodium. The main roots of the lepidodendroid forms are in all probability only partially known to us and present a curious type of structure. To begin with, there is a large pithlike mass around which is developed an extremely small amount of primary wood, at times so rudimen- tary as to be scarcely recognizable. The small degree of develop- ment of the primary structures and the quincuncial arrangement of the lateral rootlets of Stigmaria have led to a great deal of doubt as to their morphological nature. They have often been regarded as creeping stems or rootstocks, and this view of their nature is found even in recent literature on the subject. The mass of anatomical 262 THE ANATOMY OF WOODY PLANTS opinion now, however, is united in favor of the view that they represent the larger or main roots of lepidodendroid forms. They are, in fact, to some extent comparable to the anomalous roots found in the genus Selaginella known as rhizophores. It seems highly improbable that the type of organization presented by Stigmaria could have belonged to lepidodendrids with protostelic central cylinders. In general, the subterranean organs of plants are less frequently preserved with structural organization, since they are from the nature of things less likely to find their resting-place in open bodies of water, and this condition must usually be realized in order to insure petrifac- tion. It is accordingly probable that the genus Stigmaria, as at present defined, represents only to a limited extent the main radical organs of lepidodendroid forms. The Lycopodiales as a whole are a group which reached its culmination in the Paleozoic age and from the richness of its display in earlier geological times must be regarded as extremely ancient. Although the group is almost extinct, its interest from the evolutionary standpoint is great by reason of its antiquity, which supplies valuable data for the elucidation of some of the most important problems of primitive organiza- tion in vascular plants. Clearly the group as a whole displays a reduction series in which the few types which survive under modern conditions represent, not primitive states, but the final results of a process of simplification extending through almost countless ages. Consequently it is highly inadvisable, in attempt- ing to arrive at a conception of the evolutionary significance of the group, to turn exclusive attention to modern simple forms, Fic. 187.—Rootlet of Stigmaria (after Scott) THE LYCOPODIALES 263 such as Lycopodium or Selaginella. On the contrary, the most valuable results from the standpoint of the doctrine of descent can be derived from the study of the complicated arboreal extinct types known as lepidodendrids and sigillarians. It has been made clear in the preceding paragraphs that study of the last-mentioned types throws extremely important light on the origin of storage devices in the primary and secondary wood and makes clear the status of the so-called medullary rays. The Lycopodiales, although largely extinct, cannot accordingly be neglected by students of the data of evolution, and they supply valuable evidence, if any were needed, for the necessity of a knowledge of extinct forms as an indispensable basis for the understanding of organisms now living. CHAPTER XX _ THE EQUISETALES (INCLUDING SPHENOPHYLLALES) The forms to be discussed in the present chapter are contrasted with the Lycopodiales by the general fact that the appendages of the stem are arranged in a whorled or verticillate manner instead of in the spiral fashion characteristic of the group considered in the preceding chapter. Not only, however, are they characterized by the verticillate arrangement of the appendages, but also by the longitudinal ridges and furrows which mark the surface of their stems. Contrary to the conditions found in the furrowed or angular stems of certain woody dicotyledons, the traces or fibrovascular strands of the leaves correspond in position to the salient regions of the stem and not to its depressions. The branches, moreover, are not truly axillary as is characteristic of the higher forms, but occur at the node in alternation with the foliar organs. This ' situation is very striking and characteristic. The older forms in the Equisetales usually possessed dichotomously divided leaves or at least foliar organs in which the veins repeatedly forked. Another important characteristic of the older representatives of the Equisetales was the continuity of the ridges and furrows at the nodes. In more modern types this condition gives place to distinct and finally universal alternation of the ridges and furrows in the nodal region. The Equisetales may be conveniently divided into three groups —the Sphenophyllaceae, the Calamitaceae, and the Equisetaceae. Of these the first-named may now be discussed. The Sphenophyl- laceae are Paleozoic forms with slender stems marked by the pres- ence of a relatively small amount of secondary growth. Their slender conformation has led to the suggestion that they were either vines or aquatics. There is, however, no convincing evidence of the correctness of either of these views in regard to their habit. Fig. 188 illustrates the organization of the stem in Sphenophyllum insigne. ‘The center of the cylinder is occupied by the primary 264 THE EQUISETALES (INCLUDING SPHENOPHYLLALES) 265 wood, which is triangular in configuration, with the small elements of the protoxylem at the angles. The primary wood presents no features of special interest as viewed in transverse section beyond the fact that it is protostelic in its organization and consequently lacks a parenchymatous medulla or pith. The secondary wood which surrounds the primary structure is characterized by the radial seriation of its elements and by the presence of medullary rays. There are no other parenchyma- tous structures in the secondary wood ex- cept the rays. The radial parenchyma of the Sphenophyllaceae is peculiar in the fact that its cells, instead of being strictly elon- gated in the radial direction and at right angles to the longer axis of the tracheids, ‘frequently have their : greatest dimensions OE Sas es 5 : Fic. 188.—Transverse section of the stem of in the vertical 2g lane. Sphenophyllum insigne. This situation leads to the extension of the cells of the rays along the edges upward and downward among the tracheids in a manner simulating true wood parenchyma. This is, however, merely an appearance, for longitu- dinal storage cells of the type ordinarily known as wood parenchyma have not yet been found in any Paleozoic wood of secondary origin. Wood parenchyma, indeed, as has been indicated in an earlier chap- ter, was primitively intimately associated with the phenomenon of annual rings which appeared for the first time in the Mesozoic age. It is clear from the description of the wood of the Sphenophyllaceae supplied in the present connection that it shows, as indeed might be expected, a general resemblance to that of the more ancient representatives of the Lycopodiales. The tracheids were somewhat NS . \Y) \ ‘ 4 Cri~ 8 266 THE ANATOMY OF WOODY PLANTS scalariform in their sculpture, but tend, like those of the arboreal Lycopodiales, to develop the pitted condition. The pits, whether scalariform or rounded, were found equally on radial and tangential surfaces of the elements of the secondary wood, a condition par- alleled in the ancient treelike representatives of the Lycopodiales. The outer region of the figure shows the soft tissues in a condition of relative disorganization, which does not make their discussion profitable. The most interesting general features presented by the anatomy of the stem in Sphenophyllum are its essentially pro- tostelic character, thie: spect an organization of the rays, and the tan- gential as well as radial pitting of the tracheids. The leaves and roots are not well known as to their ana- tomical organization and in the actual state of our ignorance mani- fest no features of unusual interest. The Calamitaceae are distinguished from the Sphenophyllaceae anatomically by the siphonostelic organization of their central cylinder. In the more ancient types of Calamites the ridges and furrows of the stem were continuous at the nodes, precisely as is the case in Sphenophyllum. Moreover, in the Archaeocalamitaceae the leaves divided dichotomously. In more modern calamitean types the alternation of the ridges and furrows in the nodal region began to become a marked feature of organization except in the cones or reproductive axes, which adhered to the more ancient topography with non-alternation at the nodes. Fig. 189 illustrates the organization of a younger stem in a calamite. The outer region of the axis has generally disappeared as a result of fossilization, but the woody and medullary regions are Fic. 189.—Transverse section of a small stem of Calamites. THE EQUISETALES (INCLUDING SPHENOPHYLLALES) 267 clearly shown. The wood is apparently entirely secondary in its origin, but it is distinguished by certain lacunae or cavities which occupy the apices of the wedgelike masses constituting the rather slender cylinder under discussion. These cavities indicate the posi- tion of the poorly differentiated and evanescent primary wood. So far as is known, the primary xylem of the calamites of the later Paleozoic was entirely centrifugal or peripheral in its development. The great reduction in the primary structures of the calamites has led to a discontinuity of the cylinder comparable to that found in the higher and more modern members of the Sigillariae described in the preceding chapter. The lack of continuous development in the cylinder of primary wood brings with it a corresponding organiza- tion of the secondary xylem. The general result of the situation portrayed is the organization of the secondary cylinder in the first instance as separate wedges which finally become united by their increasing breadth. In the group under consideration we have one of numerous examples of an interrupted secondary cylinder resulting from the meager and sporadic development of the primary wood when the latter presents an extreme degree of reduction. The pointed, outward excursions of the pith in calamitean forms are in marked contrast to the true medullary rays, which in this case are narrow structures. The rays in Calamites are characterized by the often vertical elongation of their elements, a situation which parallels that described above in Sphenophyllum. The slight development and the entirely centrifugal origin of the primary xylem in the true calamitean forms is in marked contrast to the conditions presented by the genus Sphenophyllum, where the primary structure is not only massive, but also entirely centrad or centripetal in its development. There is, of course, a very wide gap between the organization of the axis in Spheno- phyllum and that found in Calamites. This gap is for the most part still unbridged by the discovery of intermediate forms, but an interesting condition is found in a stem from the lower Car- boniferous which is described by Scott. In Fig. 190 is repro- duced a somewhat oblique section of the primary region of one of the woody wedges of a calamitean stem. The lacuna or cavity representing the position of the ephemeral primary wood has 268 THE ANATOMY OF WOODY PLANTS tracheary elements, not only on the side which lies toward the secondary wood, but also on that in juxtaposition to the medulla or pith. In other words, this calami- tean stem, to which its discoverer has applied the name Protocalamites, somewhat clearly presents xylem of the centrad or cen- tripetal type. The secondary wood of calamitean forms was in its early organization Fic. 190.—Transverse section through the primary larg ely composed wood of Protocalamites (after Scott). of scalariform ele- @ ‘ m Y Py 8 A it; mY te ments which in the later development gave place more or less completely to the pitted tracheids. Fig. 191 illustrates the structure of the stem of a calamite in proximity to the primary region. It is clear that the tra- cheids are still very largely scalariform. The pitting of the tracheary elements inCalamites,whether scalariform or rounded, was confined to the radial walls of the ele- ments as in the lower gymnosperms, and was not present on the ae vee > 3 =e FS ss aie nee Fic. 191.—Longitudinal section of the wood of Calamites THE EQUISETALES (INCLUDING SPHENOPHYLLALES) 269 tangential aspects. True wood parenchyma did not occur in the secondary wood of Calamites. Although the primary xylem of calamitean forms has departed far from the primitive condition, the secondary ligneous organization of the group is characterized by features which are only less primitive than those presented by the lepidodendrids. The organization of the leaf in Calamites is not well known as regards those features which are of inter- est from the comparative anatomical standpoint, but this situation is fortunately relieved by certain data observed in the case of the foliar organs of the living genus Equisetum, which will be described in a sub- sequent paragraph. The root of calamitean forms was not recognized at first as belonging to the forms included under this appellation and was called Asiromyelon. Its organization can best be discussed in connection with that of the root of the living genus Equisetum. In Fig. 192 is portrayed the structure of a transverse section of the stem of the genus Equisetum. It is evident that the center of the figure is occupied by a large air space shared by the calamitean forms and indicative both for the Equisetaceae and their fossil forebears, the Calamitaceae, of a primitively amphibious habitat. This central cavity is often called the medullary fistula and in the case of the ancient representatives of the Equisetales was often molded in stone as pith casts resulting from mud entering the central spaces of the fallen trunks rotting in the shallow waters of Paleozoic lakes. Surrounding the large medullary space are the fibrovascular bundles, which are of small size and somewhat remote from one another. The strands are marked by cavities in their Fic. 192.—Transverse section of stem of Equisetum variegatum var. Jesupi. 270 THE ANATOMY OF WOODY PLANTS inner region which from their topographical relation to the ridges of the stem are known as carinal air spaces. In alternation with these are larger spaces in the cortex situated beneath the furrows of the stem and designated consequently as vallecular lacunae. Fic. 193.—Transverse section of bundle of rootstock of Equisetum arvense. true scalariform or reticulate elements which are laid down after the elonga- tion of the internodes has come to an end. The two masses of metaxylem inclose between them the tissues of the phloem, consisting of larger sieve tubes and smaller parenchymatous cells. In Fig. 194 is shown a longi- tudinal view of the fibrovascular bundles taken a little to one side of the central region. To the left may be seen the carinal cavity containing The cortex is largely com- posed in life of green cells and performs the assimila- tive and transpiratory functions inadequately sub- served by the minute leaves. The fibrovascular bundle must now receive further consideration (Fig 193). The tracheary elements are scantily present on the mar- gins of the so-called carinal lacunae. This region is the protoxylem. Outwardly on either flank is seen a row of tracheids which constitute the metaxylem. These are Fic. 194.—Longitudinal sec- tion of bundle of rootstock of Equisetum silvaticum. remains of ringed and spiral protoxylem. ‘To the right appear the reticulate elements of the metaxylem which in the transverse view flank the phloem. The organization of the pith and the distribution of the endo- dermal structures in the genus Eguisetum are of considerable THE EQUISETALES (INCLUDING SPHENOPHYLLALES) 271 evolutionary interest. In Eguisetum arvense (Fig. 1950), in all probability one of the most highly specialized members of the group, an external endodermis alone is for the most part present, an internal boundary of this nature being found only in certain instances in the region of the nodes. In E. silvaticum, which may be considered a somewhat less specialized type, only an external endodermis ap- pears in the aérial stem, which accordingly presents a condition very similar to that found in E. arvense. In the subterranean stems, however, and in primitive Fic. 195 a, b, and c.—Diagrams illustrating the distribution of the endodermis in the genus Eguisetum. regions of the aérial axis an internal endodermis is likewise seen. In other species such as E. hiemale (Fig. 195a), etc., both internal and external limiting layers are developed throughout, while in E. limosum (Fig. 195c) each bundle is surrounded by an individual 272 THE ANATOMY OF WOODY PLANTS endodermis except in the region of the nodes where continuous internal and external endodermal layers are seen. The pith of the genus Equisetum, particularly in the region of the nodes, is frequently characterized by the.presence of nests of dark-brown sclerotic cells, resembling similar structures found in the cortical tissues of both stem and leaf. On the grounds of comparative anatomy we shall accordingly be compelled to regard the pith of Equisetum as of cortical origin. The arrangement of the fibrovascular strands at the nodes in living and fossil representatives of the Equisetales (Equisetaceae and Calamitaceae) must now be considered. The situation present is best revealed by means of diagrams (Fig. 196). In A is depicted the arrangement of the fibrovascular structures at the node in the vegetative stem of the living Equisetum. Across the center of the diagram passes a heavy transverse band, the so-called nodal wood. In this the strands of the upper and lower internodes end in such a manner that they alternate with one another. ‘The traces of the leaves originate from the strands of the lower internode and thus subtend the intervals between the strands which are joined with the nodal wood from above. A superficial view of the topograph- ical conditions represented here would result in the conclusion that the Equisetaceae are provided with foliar gaps precisely as is the case in the Pteropsida. A consideration of B makes this view of the matter difficult to sustain. In the figure the foliar strand is represented in radial aspect as it comes off from the fibrovascular tissues of the axis. It is clear that the trace of the leaf takes its origin below the so-called nodal wood and passes out without showing any foliar gap above it. It is true that, as is indicated in both A and B, a gap is present subtending the foliar trace above the continuous zone of the wood at the node; but a consideration of the historical and comparative anatomical data makes it difficult indeed to regard the gap in question as a foliar one. In C is shown the arrangement of the strands of the primary wood in an ancient calamitean form (Archaeocalamites). It is evident in this case that the strands of the upper and lower internodes, instead of meeting the nodal wood in alternation as they typically do in Equisetum, exactly coincide with one another and are not subject THE EQUISETALES (INCLUDING SPHENOPHYLLALES) 273 to alternation. As a result of this condition the leaf traces, which here, as in the modern type, originate from the lower internodal strand, subtend, not a gap above the nodal wood, but the strand of the upper internode. It is thus clear that the older condition mein LAL a a it Fic. 196 a, b, c, and d.—Diagrams illustrating the relations of the bundles in Equisetum and Archeocalamites. Explanation in the text. for the Equisetales is one in which there cannot possibly be a gap corresponding to a leaf, even above the so-called nodal wood. A radial view of the situation in Archaeocalamites makes the topog- raphy still more clear, and this is furnished in D. Obviously on historical grounds the Equisetales are without foliar gaps and 274 THE ANATOMY OF WOODY PLANTS hence are to be regarded as Lycopsida. The comparative anatom- ical evidence on this point is equally unequivocal. In the repro- ductive axes or cones of both Calamitaceae and Equisetaceae the strands typically fail to alternate at the nodes, and the traces of the sporophylls are consequently quite without corresponding gaps. There apparently can be no question on anatomical grounds that the Equisetales are justly included in the Lycopsida. Ifthe evidence jas to the relationship of the Equisetales to the phylum Lycopsida is clear on anatomical grounds, it is equally definite from a consideration of the features of organization of the Fic. 197.—Longitudinal section of bundle in vegetative and reproductive leaves of Equisetum (after Eames). cones. In the Sphenophyllaceae and Calamitaceae the sporangia or sporangiophores are known to be ventral appendages of the sporophylls and thus present the condition characteristic of the Lycopsida. On the basis of both reproductive and anatomical features the group under discussion clearly belongs under the large heading of Lycopsida. The leaf in the genus Equisetum is of considerable interest in view of the fact that it. displays the presence of centripetal or cryptogamic xylem which has entirely disappeared in the stem. Fig. 197a illustrates the organization of the trace of the vegetative leaf of E. maximum. It is obvious that the xylem includes a central THE EQUISETALES (INCLUDING SPHENOPHYLLALES) 275 spiral protoxylem region flanked inwardly and outwardly by reticulate metaxylem. The condition present is, in fact, mesarch and strikingly resembles the common anatomical situation in the leaf of the Lycopodiales as described in an earlier chapter. In the sporophyll of the living representatives of the Equisetales the mesarch structure of the trace is even more conspicuous than in the vegetative leaf. The situation in this respect is shown for E. palustre (b). But the reproductive leaf not only manifests cen- tripetal wood in its trace, but it also presents an equally significant condition in the rela- tion of the phloem to the xylem. In c is shown a transverse sec- tion of the trace of the sporo- phyll in E. hiemale. Sieve tubes can plainly be seen sur- rounding the xylem elements, while the latter have in their midst a more or less obvious lacuna representing the evanes- cent protoxylem. On the grounds of comparative anat- Saeed it is clear that the Fic. 198.—Transverse section of the Equisetaceae once possessed oot of Equisetum hiemale. centripetal wood in the stem. That this was the former situation for the stock as a whole is clearly indicated by the anatomy of Protocalamites shown in Fig. 190. It is further rendered highly probable by the concentric as well as the mesarch organization of the trace of the sporophyll in the living genus that the bundles of the axis were formerly concentric in their organization. This condition must, however, have been realized in the extremely remote past, as no indication of concentric structure has been found in the stems of even the most ancient anatomically investigated remains of calamitean forms. The root in the genus Equisetum (Fig. 198) shows the presence of four protoxylem groups alternating with as many clusters of elements of the phloem. The metaxylem consists ordinarily of a PatBSe . ° “* ) J ty +e r) @o° 22. Set veo ns es o> a A 276 THE ANATOMY OF WOODY PLANTS single large central tracheid in which the four masses of protoxylem unite. In the smaller roots of Calamites the same general organi- zation is found as presents itself in Equisetum. The radical organs of this extinct group of the Equisetales are known as Astromyelon, a name given before their connection with calamitean stems was known. In the Equisetales as a whole, represented by the Sphenophy!l- laceae, Calamitaceae, and Equisetaceae, very marked features of organization are present. In fact, the group shows characteristics which may well be denominated unique. It is clear that the group is of very ancient origin, since when it first comes into view it is distinctly set off from the other large alliance of the Lycopsida, the Lycopodiales, by the whorled character of its appendages, the ridges and furrows of the stem, and the sporangiophoric manner of reproduction. Scott has regarded these features as sufficiently distinctive to warrant the establishment of a third great phylum of vascular plants, the Sphenopsida. This group he considers as on the whole more nearly allied to the Pteropsida than to the Lycop- sida. In view of the absence of foliar gaps in the series under discussion in the present chapter, particularly clear when both fossil and living forms are brought into consideration, there does not seem to be any adequate anatomical evidence to support the sepa- ration of the Equisetales under the heading of Sphenopsida. The reproductive characters of the equisetal series are likewise most easily reconciled with an affinity to the Lycopsida in general and to the Lycopodiales in particular. Scott regards the Psilotaceae as more nearly related to the Sphenophyllaceae than to the lycopo- dineous forms. The evidence in favor of this view does not seem, however, to be of a compelling character. CHAPTER XXI THE FILICALES This group of vascular plants presents the features of the Pteropsida in their most primitive and least modified condition. Large leaves are consequently the rule, and these normally, when functioning as sporophylls, bear numerous sporangia on the lower or abaxial (dorsal) surface. When the central cylinder of the stem is siphonostelic, as is most frequently the case, the traces of the leaves take their departure from the wall of the stelar tube with the formation of foliar gaps subtending the departing strands. In the Filicales reproduction is always by means of spores, which are in general isosporous, but which in a few instances represent the heterosporous condition. The Filicales constitute a remarkably clearly defined group, at least so far as their modern representatives are concerned; and the only family which has had its affinities with the Pteropsida brought into question is the Ophioglossaceae, regarded in some quarters as derived from lyéopsid ancestry. This attribution of affinity, however, is not now considered justi- fied. The Filicales constitute the largest element composed of vascular cryptogams in the existing flora of our earth and are on that account of great importance from the evolutionary stand- point. Anatomical problems which, in the Lycopsida, are difficult of elucidation by reason of the large degree to which the group has suffered extinction in the existing flora are much more advanta- geously approached, in the group under consideration, as a conse- quence of the large number of forms which are offered for study by the existing plant population of the earth. The value of the filicinean Pteropsida is particularly great in respect to the fibrovascular structures, and an attempt will be made in the present connection to utilize these to the full. Naturally, in a group surviving in relatively large numbers only the more salient and significant facts can be brought into prominence in an elementary treatise like this. 277 278 THE ANATOMY OF WOODY PLANTS The stem as the most plastic of the organs in vascular plants presents the greatest variety of structure in the Filicales. The leaf, and particularly the root, offer little diversity of organization and may consequently be dismissed with relatively slight con- sideration. Anatomically the stem presents itself in the case of the Filicales under two main conditions: the protostelic, in which there is no medulla present in the fibrovascular system, and the siphonostelic, characterized by the existence of a central mass of parenchyma known as the medulla or pith. The first con- dition is represented in Fig. 199, portray- ing the transverse section of the stem of a species of Glei- chenia. The siphon- ostelic modification is delineated in Fig. 200, reproducingthe 3y transverse aspect of Fic. 199.—Transverse section of the stem of the stem of the Gleichenia species. maidenhair fern, Adiantum pedatum. In the second figure we find the fibrovascular tissues organized in the form of a tube, limited both internally and externally by an endodermal boundary which becomes continuous around the margins of the gaps caused by the exit of the traces of the lateral branches and leaves. Not only is the tubular central cylin- der bounded continuously by an endodermal layer, but it is likewise characterized in the particular case under discussion by an inner and outer lining of phloem. In the walls of the stelar tube so organized there are gaps formed in connection with the exit of the fibrovascular strands leading to both leaves and lateral branches. In addition to these there may be interruptions in the continuity of the fibrovascular hollow cylinder which are not related to THE FILICALES 279 departing strands of any organs. The root is not responsible for the appearance of a gap in the wall of the stelar tube unless it happens, as is sometimes the case, to be closely related to a foliar organ. Under these conditions the apparent gap is naturally foliar and not radical. Before passing to the discussion of modifications of the siphon- ostelic central cylinder as presented by the stem in the Filicales it will be well to consider the general topography of the fibrovascular system in the various organs. The account of the stelar system Fic. 200.—Transverse section of the stem of Adiantum pedatum of the stem outlined in the preceding paragraph will suffice for the cauline organ, so that it is possible to turn at once to the discussion of the leaf and the root. As has been indicated above, the foliar trace departs from the tubular central cylinder of the axis in topographical relation to a lacuna in the stelar wall which is known as the foliar gap. The outgoing foliar trace in the lower region where it runs in the stipe or rachis or even sometimes in the subdivisions in the main veins of the flattened region or lamina, is concentric or bicollateral in its organization. This characterization means that the xylem is either completely surrounded by phloem or at least has phloem on its two opposite sides. As the fibrovascular strands which innervate the blade of the leaf become more finely divided they lose 280 THE ANATOMY OF WOODY PLANTS their original concentric or bicollateral structure and develop a collateral organization. This condition of the finer fibrovascular structure of the foliar organ is clearly correlated with the dorsi- ventral structure of the leaf as a whole, and favors its function- ing in relation to photosynthesis and transpiration. The upper region of the foliar strands is consequently largely under the sway of physiological conditions, while in their lower course, and espe- cially before they have suffered much in magnitude as a result of subdivision, the ancestral conditions may as a rule be more readily observed. . Further, the more aberrant the anatomical structures are in any given case the less will be the degree of development of the ancestral conditions in the foliar traces. In argument regarding the interpretation of the fibrovascular structures in stems the organization of the foliar trace after it has left the stele of the leaf is of great importance. In the root of such relatively low types as the Filicales little evidence is supplied which is of value in the interpretation of the primitive organiza- tion of the tubular stele of the stem. This statement holds, not only for the true ferns, but also for those lower and ancient gymnosperms which have the most marked filicinean affinities. It will be apparent, however, when the discussion of the anatomical organization of the axis in higher gymnosperms and angiosperms is reached, that the root assumes an evolutionary significance which is not observed in the lower groups of the Vasculares. With these preliminary remarks it is possible to pass with advantage to the consideration of the organization and evolution of the tubular central cylinder of the axis. » First will be discussed modifications of the tubular stele which are in the direction of greater complexity. In many ferns the central cylinder or stele in the adult stem is represented by a complex grouping of strands. In the bracken fern (Pleris aquilina), as is shown in Fig. 201, the older stem presents in transverse section two series of bundles—two large central ones and a ring of usually much smaller ones forming a circle outside these. The significance of the conditions present in the stem of this most commonly studied fern have been very generally misunderstood. It has been maintained by the distinguished French anatomist THE FILICALES 281 Van Tieghem that the vascular system of the bracken arises by the continued forking of an originally simple (protostelic) strand. According to his view the two large central bundles are the first to appear as the result of the process of forking, and the smaller circle of strands lying outside these is formed later. On account of the supposed origin of the strands in the stem of Pleris aquilina by repeated division, the name polystelic was given by Van Tieghem to this and similar conditions of ana- tomical organization in the ferns and their allies. As a matter of fact the situation is very different indeed from that indicated by the term polystelic. In Fig. 202a is shown the transverse sec- tion of a very young stem of the bracken when it is still in the upright condition and has not given rise to the subterranean horizontal branches which come into existence at a comparatively early stage. The stem at this age is obviously siphonostelic and is marked by a gap correlated to an outgoing leaf trace. In 0 a later stage of development, characteristic of the young horizontal stem, is shown. Here the tubular central cylinder is giving off internally and toward the center a medullary strand. Later the single medullary strand becomes double and the condition attained in the adult is reached. It is clear from an examination of the actual course of development in the stem of the bracken fern that the medullary strands are not formed first, as is assumed by Van Tieghem, nor does the stelar system of the adult result from repeated bifurcation of an originally single strand. On the contrary, the course of development presents first a protostelic Fic. 201.—Complicated bundle system of Pteris aquilina 282 THE ANATOMY OF WOODY PLANTS condition in which no medullary tissues are present, a phase followed by the siphonostelic one, which in turn develops medullary strands from the inner surface of its walls. The outer series of bundles is consequently antecedent to the medullary bundles, a situation which may be readily inferred without the study of the young plant from the fact that the roots are attached to the external strands. Not only does the bracken manifest the general Fic. 202.—Diagram to illustrate the development of the stem in Péeris aquilina. Explanation in the text. conditions described above, but all ferns with complicated arrange- ments of conducting strands in the stem can readily be included under the same general statement. This, for example, is true of the complex stem of the Cyathaceae or tree-ferns and also of that of the large tropical ferns known as the Marattiaceae. It is apparent from the account supplied in the present connection that the tubular condition is both typical and primitive for the ferns in general, with the sole exception of those forms in which the organization of the stele maintains the original protostelic condition. This type of structure is, however, comparatively rare in existing ferns, although it has been found, as would THE FILICALES 283 naturally be expected, much more generally in Paleozoic types belonging to the Filicales. Before proceeding further with the question of the organization of the tubular or siphonostelic type of central cylinder, it will be well to discuss the important problem of the origin of the pith or medulla in the Filicales. The situation in this group is much more favorable than it is in the Lycopsida, living and extinct, because the facts at our disposal are much fuller and as a conse- quence put the whole subject on a more satisfactory footing. There are two views in regard to the origin of the medulla in stems of the type here designated siphonostelic. One hypothesis considers it as originating from the central region of the xylem of the stele by the transformation of tracheary elements into parenchyma. It has been shown in earlier chapters that there can be no question that parenchymatous elements may be derived _from tracheids in the primary wood, and the evidence in this direction clearly points to a possible origin of the medullary tissues from transformed tracheids. Indeed, in the case of the lepidoden- drids the facts which favor the tracheary origin of the medulla are not without importance. Therefore, if we are to regard the medulla as derived from tracheary tissue on the basis of the exist- ence of transitional stages between tracheids and parenchyma, it will be only fair on the other side to assume that where elements clearly of a cortical nature occur in the region of the pith they afford evidence for the other hypothesis of the origin of medullary parenchyma, namely, its derivation from the included cortex. It is, of course, illogical to admit evidence for a derivation of medullary structures from tracheids and at the same time to reject equally cogent data as to the origin of the pith from cortical tissues. Even in the lepidodendrids the evidence for the trache- ary derivation of the medullary structures is not complete, for transitions from tracheids to parenchymatous cells are pre- sented only by protostelic stems and are entirely absent in tubular cylinders. Indeed, in cases where secondary growth is not characteristic of the siphonostele in this group, the medullary region of the stele is frequently occupied by sclerenchymatous elements similar to those which occur in the cortex. The hypothesis 284 THE ANATOMY OF WOODY PLANTS of the tracheary origin of the pith is also open to question in other representatives of the Lycopsida. In Phylloglossum the medulla in the region of the tuberous portion of the stem is actually sur- rounded by an endodermal layer, a structure peculiar to the cortex. In Selaginella laevigata, also, the tubular stele is bounded internally as well as externally by a well-defined endodermal layer, and the tissues of the pith, further, clearly resemble those of the cortex. In both Psilotum and Tmesipteris the medullary tissues are fre- quently composed to a large extent of brown sclerenchymatous elements resembling similar structures found in the external fundamental tissues. In the genus Egquisetum dark-brown scle- renchyma is present in the medulla and the cortex. It is clear on the basis of data derived from resemblances between the tissues of the pith and the cortex, on the one hand, and the tracheary tissue, on the other, that the preponderance of evidence weighs heavily on the side of the fundamental or cortical origin of the medulla. And heavily as the scale seems to incline on the side of the fundamental derivation of the pith in the Lycopsida, it seems entirely overwhelming in the case of the Filicales. There are two general arguments which have been invoked against the origin of the pith from the fundamental tissues in the Filicales. One is the denial that it is possible for the stele to include the tissues of the cortex. This reasoning cannot be given very serious weight in view of the fact that in certain fili- cinean steles—for example, that of the polypodiaceous genus Onoclea and the schizeaceous genus Anemia—the possibility of the inclusion of fundamental tissues within the tubular stele must apparently be granted, because the epidermis and chaffy ramentum as well as the outside air are actually included within the medullary region of the central cylinder. Moreover, the phloem, a tissue primitively occurring on the outer surface of the central cylinder, is frequently included in its interior. If any further evidence were needed as to the possibility of the xylem including tissues of another morphological category, it is furnished by the case of certain filicinean foliar traces within which it is universally admitted, even by the most convinced adherents of the hypothesis of the tracheary origin of the pith, fundamental tissues may not THE FILICALES 285 only be included, but in some instances may be entirely shut off from the similar tissues outside. Good illustrations of this con- dition are provided by species of the Gleicheniaceae, Polypodiaceae (notably the common bracken fern), and Marattiaceae. The possibility, then, of the inclusion of the pith within the stele must apparently be granted. The second argument against the cortical origin of the medulla is directed against the evidence based on the similar histological nature of pith and cortex in many cases, a resemblance which is the more marked the more the medullary tissues are in histo- logical continuity with those lying outside the tubular stele. It is assumed by the advocates of the tracheary origin of the pith that the striking histological similarity which often exists between the medulla and the cortex is merely ‘‘physiological.”’ This argument would be worth more if its exponents did not admit all histological evidence in favor of the tracheary origin of the medullary tissues while denying that indicating their derivation from the fundamental system. Such argument is clearly fallacious, and the logical procedure is to admit to equal consideration evi- dence for the tracheary hypothesis of the appearance of the medulla on the one hand and that for its derivation by the inclusion of cortical or fundamental tissues on the other. The advocates of the cortical origin of the central parenchyma of the tubular stele are apparently advantageously situated in this respect, for they can equally well emphasize the extremely abundant data for the origin of the pith from the fundamental system and at the same time explain away the meager evidence for the tracheary derivation of the medullary tissues. So far as the plentiful evi- dence in the case of the Filicales is concerned, it seems beyond reasonable doubt that the median parenchyma of the tubular or siphonostelic central cylinder has come from the outside and is not the result of internal differentiation within the stele. The question of the origin of the pith is a very important one from the phylogenetic standpoint, since correct views in regard to this matter are necessary for the interpretation of the evolution of the tubular cylinder from lower to higher forms. It would be going beyond the range of the present somewhat elementary 286 THE ANATOMY OF WOODY PLANTS treatise upon the anatomy of the vascular plants to elaborate at any length the question of the phylogeny of the tubular central cylinder, important as this is for the proper understanding of the higher plants in the light of the doctrine of descent. The whole situation may conveniently be illustrated by reference to the Osmundaceae. In discussing the evolutionary principles involved in the development of the siphonostele in this group, we Fic. 203.—Transverse section of the stem of Osmundites skidegatensis shall appropriately start with types from earlier geological periods. In Fig. 203 is shown a photograph of the central cylinder of a fossil osmundaceous stem from the Lower Cretaceous of Western Canada. In the stem under discussion the magnitude of the stelar system is much greater than that found in any living species belonging to the tribe and, in fact, more clearly resembles the conditions presented in a large stem of a fern of the ordinary type. The pith as well as the cortex is occupied by numerous dark masses of brown sclerenchyma—a condition closely resembling the state found in siphonostelic stems of ordinary ferns. An inspection of the periphery of the stele shows the presence of numerous THE FILICALES 287 foliar gaps, through some of which the cortex and the pith are actually continuous, as is made clear by Fig. 204, representing a small segment of the fibrovascular cylinder. In Fig. 205 is shown a still more magnified view of the marginal region of the stele, and it is here apparent that phloem is present both on the inside and on the outside of the stelar tube. The situation re- vealed by the three figures of the stem of Osmundites skidegatensis shown above makes it evident that in this ancient representative of the group a condi- tion of organiza- tion more nearly resembling that found in our ordi- nary polypodiace- ous ferns was present. The only important differ- ence is furnished by the extremely numerous foliar gaps correspond- : Fic. 204.—Part of the last, more highly magnified to ing to the more _ show the leaf gaps. crowded condition of the leaves. This, of course, is not a morphologically important distinction. After the description of an osmundaceous fern from the Meso- zoic, the stele of living species of the Osmundaceae may con- veniently be considered. Fig. 206 illustrates the organization of the central cylinder of Osmunda cinnamomea, the cinnamon fern. The fibrovascular tissues in this case are characterized by the same numerous foliar gaps as are found in O. skidegatensis, but the cortex and the pith do not communicate through them as in the Mesozoic type. Further, the phloem in the specimen under discussion, unlike that present in the cretaceous species, 288 THE ANATOMY OF WOODY PLANTS is confined to the outside of the xylem. Endodermal layers, both internal and external, are present, and the pith often contains patches of brown sclerotic cells similar to those found in the cortex. In spite of the fact that the bundles of the central cylinder of the stem are collateral, those of the leaves are concentric in organiza- tion. Applying the principles of comparative anatomy to the situation, we find that in O. cinnamomea the pith and cortex are of common origin and that the bundles of the stele, on the evi- dence furnished by the foliar strands, were formerly con- centric instructure. The conclusion which is reached from the considera- aes 208% eo Beem ie Oege ae ee tion of the stem of 08> . the species under discussion, in the light of universally valid principles of Fic. 205.—Part of the stem of O. skidegatensis, still comparative anat- more highly magnified to show the presence of both internal and external phloem. omy, is that its tubular stele was formerly concentric and that the foliar gaps were once large enough to permit of the joining of cortical and medullary tis- sues with one another. The inferences drawn from the data indicated above are, moreover, entirely justified by the considera- tion of the anatomy of the Lower Cretaceous species described in the preceding paragraph. In particularly vigorous specimens of the stem in O. cinnamomea the ancestral condition, moreover, frequently returns, for both open foliar gaps and internal phloem are often seen in such axes. In O. regalis among living repre- sentatives of the Osmundaceae medullary brown sclerenchyma is occasionally found in the pith, although an internal endo- THE FILICALES 289 dermis has never been observed. In O. claytoniana the pith never resembles the cortical tissues, and neither internal phloem nor endodermis is known to exist even in the most vigorous speci- mens. In the three living species cited in the present chapter we find a reduction series in which O. cinnamomea represents the most primitive condition and O. claytoniana the most aberrant. A quite different interpretation is put on the anatomical facts cited in the two preceding paragraphs by those who adhere to Fic. 206.—Photographs of the fibrovascular region of the stem in Osmunda cinnamomea, showing internal endodermis and medullary sclerenchyma. the hypothesis of the tracheary origin of the pith. To those who adopt the view that the medulla is derived from the substance of the stele, the type of Osmunda without either internal phloem or endodermis is the more primitive, while that in which both these structures occur is more modern. Those who regard the anatomi- cal facts from this standpoint are in a position that offers many difficulties. First of all, they have to assume that an old type like Osmunda skidegatensis has gained a high degree of development and that the modern forms without open foliar gaps, sclerotic pith, internal endodermis, and internal phloem represent in reality a more primitive condition of organization than does the Mesozoic type cited above. This view is not only not in harmony with 290 THE ANATOMY OF WOODY PLANTS the paleontological facts, but is likewise at variance with the fundamental principles of comparative anatomy. It presents the further serious difficulty of supposing that the simpler type of stele characteristic of the more modern representatives of the Osmundaceae, although primitive, has nevertheless come from a more complicated condition in the past. Finally, the hypothesis of the greater primitiveness of tubular steles without internal phloem supplies no valid explanation of the frequent occurrence of internal phloem, internal endodermis, and cortical sclerenchyma in the medullary region of various existing species of the Osmun- daceae. The view that such structures where they occur are “physiological” has little to commend it and is, moreover, a hypothesis which cuts both ways; for if we are to interpret cortical structures occurring in the medulla as merely physiological, we must likewise consider the possibility of a similar explanation of the rare and quite exceptional occurrence of a so-called ‘‘ mixed pith,” consisting partially of tracheary tissue and partially of parenchyma. The Osmundaceae on the whole present the evidence in regard to the evolution of the tubular stele in later geological times more clearly than does any other group of ferns. It should, however, be emphasized that in practically all cases where the siphonostelic central cylinder without internal phloem or endodermis is present there are found elements in the region of the medulla which present the characteristics of cortical tissues. It seems illogical to interpret these structures as possessing in every case merely a physiological significance, particularly since, in view of their imperfect and sporadic development, it is difficult to attribute to them any functional importance whatever. The structures in question possess, in fact, all the criteria of vestigial features persisting from an earlier more complicated condition of organiza- tion. Our knowledge of groups which have their climax of devel- opment in the past justifies the view that evolution in decadent series proceeds by simplification. A final general objection to the tracheary hypothesis of the origin of the pith is the outstanding fact that the more modern groups of plants, and especially the seed plants, are the ones which particularly and universally represent THE FILICALES 291 the condition which the supporters of this hypothesis regard as primitive—that of the tubular stele without internal phloem and endodermis. On the other hand, the Filicales, in:which the sipho- nostele commonly incloses a pith strikingly resembling the tissues of the cortex and quite generally lined inwardly with endodermis and phloem, must be regarded as more modern. The improbability of this general hypothesis seems very great. It may be assumed on the basis of the considerations advanced in earlier paragraphs that the siphonostelic condition in the Filicales is susceptible of complication through the development of medullary strands on the one hand, and, on the other, of simplification through the loss of internal phloem and endodermis and the progressive narrowing of the leaf gaps resulting in sequestration of the pith. The view that the latter simpler condition is more primitive not only runs counter to the conditions shown in the general sequence of types in geological time, but is also at variance with the general principles of comparative anatomy detailed in a former chapter of this work. The hypothesis that the simpler condition of the tubular stele is more primitive than the more complex marks, moreover, an evolutionary attitude which is becoming generally obsolete as our knowledge of the actual organ- ization of extinct forms, particularly of those types which mani- fested their greatest luxuriance in the past, becomes fuller and more complete. It is now clear from evidence of this kind that the lower gymnosperms have come from the Filicales as a result of the simplification and reduction of the primary structures of the stele of the stem on the one hand, accompanied by the marked development of secondary fibrovascular tissues on the other. In the gymnospermous Pteropsida this anatomical progress has been associated with the attainment of the seed habit. In the Lycopsida, by contrast, a similar anatomical progress culmi- nated in much earlier geological times and was not accompanied by the evolution of true seeds. CHAPTER XXII THE ARCHIGYMNOSPERMAE: CYCADOFILICALES AND CYCADALES The earlier seed plants of Paleozoic and Mesozoic time were characterized by the possession of naked seeds upon which the microspores or pollen grains were directly deposited. The free exposure of the seminal structures to the air has gained for the types marked by this feature the appellation of gymnosperms. In the large group thus characterized there are two main modifi- cations. In the earlier and more primitive gymnosperms the pollen grains or microspores were accommodated in a chamber in the apex of the megasporangium known as the pollen chamber. This cavity, filled with fluid derived either from the surrounding parenchymatous cells or in some cases from a special fibrovascular system present in the walls of the megasporangium, provided for the germination of the microspores and the subsequent fertil- - ization, effected in every instance by swimming sperms. These forms in general present a marked resemblance to the Filicales, often in external habit and always in internal anatomical structure. In contrast to them are the higher gymnosperms, in which there is no true pollen chamber. Here the act of fertilization is effected, not by swimming sperms, but by means of a pollen tube developed as an outgrowth of the microspore and directed toward the egg. The external habit of these gymnosperms is never fernlike, and their anatomical organization shows only the slightest cryptogamic features in living forms. The types possessing pollen chamber, swimming sperms, frequent filicinean habit, and cryptogamic organization of the fibrovascular structures are conveniently designated as the Archigymnospermae or more primitive gymno- sperms. ‘Those forms which are contrasted to these by the absence of pollen chamber and the presence of pollen tube in connection with fertilization, as well as by the disappearance of filicinean habit and anatomical characteristics, may be, on the other hand, designated as the Metagymnospermae or higher gymnosperms. 292 CYCADOFILICALES AND CYCADALES 293 The present and the following chapter will deal with the repre- sentatives of the Archigymnospermae. Our knowledge of the Archigymnospermae, from the fact that many of the group are extinct, is necessarily incomplete. It will accordingly be convenient in the present chapter to focus attention on the best-known fossil group and the nearly related family which possesses living representatives. The extinct aggrega- tion of forms which here present the strongest claim to attention are the Cycadofilicales, characterized by a _ habit so closely re- { “ae sembling that of the ‘ true ferns that it is 8 er tt only since the very | é end of the last cen- tury that they have been recognized as seedplants. The type of seed con- : nected with the veg- to tt. x etative structures of Fic. 207.—Transverse section of the stem of Heter- fee Gre ealieaics angium (after Scott). has been diagrammatically indicated in an earlier chapter, to which the reader is here referred. In the present connection only ana- tomical features of the group need be discussed. The antiquity of the Cycadofilicales is vouched for, not only by their Paleozoic occurrence, but also by the occasional presence of protostelic stems, axes of this type not being known for any other group of seed plants living or extinct. Fig. 207 illustrates the organiza- tion of the protostelic axis of the genus Heterangiwm from the English Carboniferous. The transverse section shows the presence of an external ribbing of sclerenchymatous strands, a feature com- mon to many older representatives of the Gymnospermae. The fibrovascular apparatus consists of protostelic primary wood sur- rounded by a thin layer of secondary xylem. t} i} WEE, r if MY,.U02 Uh, WML CLI GME GE Rael Laea fi 204 THE ANATOMY OF WOODY PLANTS We may now turn our attention to more complicated stems belonging to the general group of the Cycadofilicales. The genus Medullosa is of particular importance, since it possesses a type of stelar organization presented by several or many concentric strands which are best considered as belonging to a siphonostelic cylinder. The general organization of the axis in the genus under discussion is well shown in Fig. 208, which portrays in a somewhat diagram- matic fashion the structures involved. There are three large concentric fibrovascular strands present which consist of a central core of primary wood indicated by cross-hatching, surrounded Fic. 208.—Transverse section of the stem of Medullosa anglica (after Scott) with a cordon of secondary xylem, represented by radiating lines. The outline of the stem is irregular, the salients being due to the presence of the bases of large leaves. The surface is covered with the reticulated sclerenchymatous strands already described in the case of Heterangium. The fundamental tissues are occupied by secretory canals, which probably contained mucilage, as do those of the living Cycadales. In the cortical region are accommodated larger and smaller strands ordinarily lacking secondary growth. The bundles of greater dimensions are mostly the larger foliar bundles and possess concentric organization. The small strands which are found characteristically in the actual leaf bases are collateral in their organization and exarch in the structure of their xylem. Fig. 209 illustrates two of the smaller strands together with fundamental tissues and contained mucilage- canals. The general situation in the genus Medullosa is complicated frequently CYCADOFILICALES AND CYCADALES 2905 by the presence of more numerous large concentric fibrovascular strands than those shown in Fig. 208. In such instances the con- centric strands often show a more or less complete degeneracy of the secondary xylem on their inner surfaces. This situation has been regarded with reason as of significance in foreshadowing the type of organization found in the axes of the Cycadales, living and extinct. It will be seen from the account of Medullosa here supplied that the genus presents some marked features of ana- tomical resemblance to ferns, the main contrasts in organization being due to the appearance of secondary growth in con- nection with the strands belonging to the stem proper. In accordance with the canons of anat- omy formulated in an earlier chapter of the pres- ent work, the secondary activity has not yet pene- trated into the traces which pass out into the more con- servative foliar structures. The Medulloseae are undoubtedly of great interest from the standpoint of the evolution of cycadean forms, and there can be little question that these types so common as charred remains in the Carboniferous coals of Europe and America came very near to being the actual ancestors of our living Cycadales. As a third illustration of the Cycadofilicales we may take the genus Lyginodendron, the organization of which has been so admir- ably described by English anatomists. Fig. 210 illustrates the structure of the stem in this genus. The same sclerified ribbing is observed as in the other two genera discussed above. The central cylinder, however, presents a marked contrast to that of either Heterangium or Medullosa, for it consists of collateral strands arranged in a closed circle. The pith is occupied by sclerotic Fic. 209.—Foliar bundles of Medullosa anglica 2096 THE ANATOMY OF WOODY PLANTS nests of cells which are duplicated by similar structures in the cortex. The inner surface of the cylinder of xylem shows clusters of primary wood which sharply contrast with the secondary region by the irregularity of the arrangement of the elements and the absence of rays. Fig. 211 illustrates a portion of the cylinder more highly magnified, and with the greater enlargement the distinct and mesarch character of the primary region becomes apparent. The secondary wood is characterized both by its regularly radial arrangement and by the presence of rays which Fic. 210.—Transverse section of the stem of Lyginodendron oldhamtum (after Scott). are often two or three cells in width. The tracheids of secondary origin are marked by crowded pits which alternate in position and are often angular from mutual contact. These pores are confined strictly to the radial walls of the elements, no tangential pitting occurring in the secondary tracheids of any Paleozoic gymnosperms with which we are at the present time acquainted. The foliar traces in Lyginodendron are at first single, but bifurcate shortly after leaving the primary region of the stem, and lose their secondary xylem, becoming concentric instead of collateral in their organization. It is evident on the basis of the general canons earlier elucidated that the bundles of the stem in the case of Lyginodendron must formerly have been concentric in their structure, since this condition persists in the traces of the leaves. Further, the presence of secondary wood in the stem CYCADOFILICALES AND CYCADALES 207 and its absence in the foliar traces show that secondary growth is a comparatively recently acquired feature in the genus under discussion. The sclerotic nests in the pith appear to vouch for the extra-stelar origin of the medullary region. The situation as a whole is like that found in the case of the Osmundaceae, except for the complication introduced by the presence of the secondary growth. In the genus Botrychium among the Ophio- glossaceae secondary tissues, however, are often well developed, and it has long been realized that the occurrence of secondary activity in the fibrovascular tissues is not an extremely impor- tant criterion from the evolutionary standpoint. It was at one time thought that the genus Lyginoden- dron was the proto- Eye 7 ot, thie Cycadales, but this opinion has been oe Woe ee ey Ae P oe a) EB aw, pt s¥ Bex e +) nen Se =< as PRE eee less See — Fa Cao EEE eet Ba eS oS IGS) . EO FA Te q FIG. 219.—Stereoscopic view of a cordaitean wood from Lancashire, England and constitute the so-called double transfusion sheath. In 8, the longitudinal view, the various elements of the bundle are shown in the median section. The protoxylem is continuous with tra- cheids which by the usual transitions gradually pass into the CORDAITALES AND GINKGOALES 309 pitted elements of the last-formed metaxylem. Below the pro- toxylem lies the phloem, and still farther down the more elon- gated and narrower elements of the inner transfusion sheath, which in turn abut on the short, broad tracheary elements of the outer transfusion sheath. At the very top lie other short transfusion cells, and the inner elongated sheath in this region is absent as a result of conditions which can readily be inferred from the in- spection of the transverse view in a. There is some variety in the development of the foliar bundles of the Cordaitales, but all are characterized by the presence of well-marked centripetal wood and a cordon of short tracheary elements, known as trans- p pe 8p 8c bt Fic. 220.—Longitudinal view of cordaitean wood near the pith (after Scott) fusion cells, which are closely related to the centripetal or crypto- gamic wood. The root in cordaitean forms, for reasons applying equally to all Paleozoic gymnosperms, presents no features of special interest beyond illustrating the general cordaitean organization modified to the needs of root organs. It will be obvious from the statements made in the foregoing paragraphs that there is clear evidence in the organization of the foliar structures in the Cordaitales for their close affinity with the Filicales, although naturally the degree of relationship is much less intimate than that which characterizes the Cycadofili- cales and even the Cycadales. Concerning the organization of the microsporangia and seeds of the Cordaitales our knowledge is unfortunately somewhat meager. The evidence in regard to the microsporangium is not sufficiently definite to warrant an opinion as to whether it was ectokinetic or endokinetic in its 310 THE ANATOMY OF WOODY PLANTS mode of dehiscence; but, in view of the strong development of transfusion tissue in the foliar organs of the group under discus- sion, a clear feature of distinction from the Cycadales and Cyca- dofilicales (in both of which the microsporangia are ectokinetic), it is somewhat probable that the pollen sacs owed their dehiscence to a layer of tracheary origin. The seeds of Cordaites have been Toe 957050900 200 WOOrI00 a raron lavoro Zander a en ECCRN SOUR ERR CRUE Fic. 221.—Transverse and longitudinal sections of a leaf bundle in Cordaites principalis. anatomically investigated by Renault and they possessed a well- marked pollen chamber. A more complete knowledge of the reproductive structures of cordaitean forms and of the types which connected them in the more remote Paleozoic with filicinean ancestors is much to be desired. The Ginkgoales are represented by a single living genus, but were extremely abundant in the Mesozoic and are thought to have been continued into the Paleozoic by the somewhat problem- atical genus Whittleseya. Unfortunately our anatomical knowledge of the group beyond that supplied by the investigation of the CORDAITALES AND GINKGOALES ail living genus is extremely meager and in fact is confined to the structure of woods which have been referred to the group. The stem in Ginkgo is characterized by the presence of clear annual rings which terminate with tracheids provided with tan- gential pits and in this respect reveal a marked contrast to the tracheary elements constituting the remainder of the annual increment. It is obvious that as regards the organization of the annual ring the group under discussion is distinct from those rare cordaitean stems in which yearly zones of growth can be dis- tinguished, by the presence of tangential terminal pitting. In other respects, however, the structure of the wood is clearly archaic, for there are no parenchymatous elements present other than those related to the rays. The pith and cortex in the group possess secretory canals which are comparable to those found in certain Abietineae. The longitudinal aspect of the secondary xylem in Ginkgo is very different from that of the Cordaitales. In the more ancient group the radial pits are often extremely numerous and they are then angular by mutual contact. In Ginkgo the pores of the tracheids are not so abundant as to be described as crowded and, moreover, instead of being alternating and angular as in the older tribe are round and opposite. Another equally striking feature offers itself in the presence of transverse bars of pectic cellulose in the walls of the tracheids between the pairs of opposite pits. These may conveniently be designated bars of Sanio, to distinguish them from the trabeculae of Sanio, structures which are found not uncommonly in all woods of secondary origin from (and including) those of the Cycadales to those of the dicotyledons. The latter structures consist of ligneous processes crossing the cavity of the tracheid, possibly due to the activity of parasitic fungi, while the true bars of Sanio are concealed in the wall itself and consist of pectic cellulose. Bars of Sanio are found only in the walls of tracheids of secondary origin, and statements as to their occurrence in any elements of the primary wood are erroneous. An interesting condition appears in the organization of the secondary wood of the peduncle of the seed. In Fig. 222 is shown the transition region in the xylem. It will be observed gi THE ANATOMY OF WOODY PLANTS that the pitted tracheids nearest to the primary wood are entirely without bars of Sanio, which make their appearance only at an interval from the protoxylem. The pitting to a large extent is alternate. It is very generally admitted by competent judges at the present time that the Ginkgoales are derived from cordaitean ancestry, | MIAN CN YY UA XX NN \ WA\ 7 AN) V (X Wi N \ fl = QIi-\4¢ —S Os) Co} o) SHH GIBZZizsies © SiS Z| Zeko (oX2) Ware) || A= Ze Slale Skies |e Clio | 4S Bee 6O 2 —- SSO. gl |=|S—\Co == ell = tele) f= 60) |S ee, and it is accordingly highly interesting to find in the ©) (0) Ooo) ecco aaa Co) ote QO (oo) ©) ® ®& ) All V4 } 8 Q : @l/ | le NSS) AE IRS Se = ell =| © ell| ello Jel = 2 ll] oll off Rant lel iin nn Fic. 222.—Longitudinal view of the tracheids in the peduncle of a seed in Ginkgo. To the right is shown the arrangement of the tracheids in the mature wood. organization of vegetative and reproductive axes evidence based on the pitting and distribution of the bars of Sanio favorable to such an opinion. Farther away from the primary wood the secondary tracheids quickly develop the opposite pitting and bars of Sanio characteristic of the mature wood. It is clear from the figure, moreover, that the tracheids of the primary wood are quite devoid of structures of the nature of the bars of Sanio. It is well to emphasize the conditions found in the organization of the root and reproductive axis of Ginkgo, because there prevails CORDAITALES AND GINKGOALES 313 at the present time an almost inexcusable ignorance in regard to the nature and distribution of the structures here designated bars of Sanio. They are clearly correlated with opposite pitting and are a feature of the secondary wood, not appearing in the organization of the tracheids of the primary xylem. Evidently the structures in question are of considerable value in the identi- fication of gymnospermous woods and consequently must rank high as a diagnostic criterion among competent anatomists. The mature vegetative leaf in Ginkgo supplies very little evidence Fic. 223.—Foliar bundle of Ginkgo, showing transfusion tissue (after Sprecher) of the presence of centripetal elements in the strict sense of the term. In the terminal region of the blade of the leaf a well- marked zone of transfusion tissue manifests itself, as is shown in Fig. 223; but typical centripetal tracheids are usually conspicuous by their absence. In the cotyledon, however, the centripetal or cryptogamic wood is present in a much clearer manner in accord- ance with the principle of recapitulation discussed in an earlier chapter. The reproductive leaves, both ovuliferous and staminate, also show the centripetal elements in a good condition of develop- ment, although even here they more nearly resemble transfusion tissue. In the stalk which supports the pair of ovules centrip- etal elements and ordinary transfusion cells are seen in the upper region in great abundance and are likewise found in the collar sur- rounding the base of the seeds. The situation presented by the 314 THE ANATOMY OF WOODY PLANTS microsporophyll is, however, of greater interest in the present connection. In the petiole of the bisporangiate microsporophyll tracheary elements of a centripetal character occur on the upper side of the protoxylem (Fig. 224). These elements can scarcely be said to constitute typical centripetal tracheids, since they are often of wide lumen and are correspondingly abbrevi- ated in length. As the foliar traces ascend into proximity to the sporangia, they separate from one another and the xylem of each rotates so as to occupy a position near the middle line of the Fic. 224.—(a) longitudinal, (b) transverse, section of wood of bundle in micro- sporophyll of Ginkgo. sporophyll, while the strands of phloem turn outward, to end in the bases of the sporangia. Meanwhile the transfusion elements occur- ring on the upper side of the tracheary strands in their upward course pass imperceptibly into the fibrously thickened mechanical elements which are responsible for the dehiscence of the sporangium. Further, the apex of the tracheary strands passes gradually by means of short transfusion tracheids into the mechanical elements which lie along the median sides of the sporangia. In this fashion there is established an intimate relation between the tracheary tissues of the bundles of the reticulate cells which constitute the CORDAITALES AND GINKGOALES 315 opening mechanism of the microsporangia. The microsporophyll of Ginkgo accordingly has a double interest from the evolutionary standpoint, for it not only shows the centripetal or cryptogamic wood more clearly than it is exhibited by the vegetative leaves, but at the same time manifests its transition by imperceptible gradations into the mechanical tissues of the sporangium wall. As has been indicated in an earlier chapter, Ginkgo is the lowest type in which the dehiscence of the microsporangium no longer depends on an annulus derived from the epidermis but is effected by an internal mechanism derived from the old centripetal or cryptogamic wood of the fibrovascular bundle. In the stalk of the ovule centripetal elements and transfusion tissue are also well developed, but they apparently do not at any time penetrate into the substance of the megasporangium. It is not unlikely that tracheary tissues of a transfusionary nature were formerly present in the megasporangial structures of the Gink- goales, but that in the course of time they have suffered abortion. The organization of a number of seeds of Paleozoic age of unascer- tained affinities is good evidence in favor of the probability of this view. Moreover, in one of these, Stephanospermum, characterized by a tracheary mantle in the wall of the nucellus ending in the pollen chamber, pollen grains are present, winged all around and strongly resembling those of Ginkgo. It is accordingly not im- possible that Stephanospermum was the seed of some Paleozoic representative of the Ginkgoales. The importance of the sole surviving and monotypic genus Ginkgo from the standpoint of the evolutionary transition from the ancient to the modern gymnosperms cannot be overestimated. It constitutes virtually a link between the Archigymnospermae and the Metagymnospermae, since it presents to so large a degree the characteristics of both. Its affinities on the lower side are clearly with the Cordaitales, as has been recognized by all com- petent investigators in recent years. Its relationship with the Abietineae among the Coniferales is equally well indicated by comparative anatomical and paleobotanical data, as will be shown in the following chapter. The indications of relationship with the Cordaitales are pre- sented in connection with the organization of the wood in primitive 316 THE ANATOMY OF WOODY PLANTS organs and regions. It has been pointed out in the foregoing paragraphs that, although centripetal wood of the cryptogamic type is represented almost exclusively by transfusion tissues in the mature vegetative leaf of Ginkgo, it is present in a clearly recognizable form in the cotyledon, in the microsporophylls, and in the peduncle of the ovuliferous apparatus. In the case of the microsporophyll the xylem, and more particularly the vestigial centripetal xylem and transfusion tissue, are in clear relation to the reticulately thickened opening mechanism of the microspo- rangia. ‘This feature is of value, not only as indicating the filiation of the Ginkgoales with lower groups, but also as indicating the morphological nature of the arrangements for dehiscence of the spore sac in the seed plants above the Cycadales. The absence -of longitudinal parenchyma in the secondary wood is another criterion of the relationship of the Ginkgoales with lower groups, while the presence of tangential pitting in the terminal region of the summer wood clearly relates the group with modern gymno- spermous types. The radial pitting of the tracheids and associated structures is also of importance as indicating the phylogenetic position of the genus. As has been shown above, the radial pits of Ginkgo are opposite in the mature wood, and often in the inter- vals between them, particularly toward the ends of the tracheids, have transverse bars of pectic cellulose imbedded in the tracheary wall, and these are conveniently designated bars of Sanio. The opposite pitting and the occurrence of bars of Sanio are features which clearly co-ordinate the wood of the Ginkgoales with that of the higher gymnosperms. However, in the primitive regions and organs of the living Ginkgo we find both the pitting of the Cordaitales and the absence of bars of Sanio which are universally characteristic of the older gymnosperms from the Cycadales downward. It seems quite obvious that Ginkgo is a genus of the utmost importance from the standpoint of evolution- ary anatomy, since it summarizes in such a remarkable manner the anatomical characteristics of both Archigymnospermae and Metagymnospermae. Its significance in the direction indicated will be fully realized only after the next tribe, the Coniferales, have been anatomically considered in the following chapter. CHAPTER XXIV THE METAGYMNOSPERMAE: CONIFERALES As has been indicated at an earlier stage, the gymnosperms are somewhat clearly divisible into two large groups: the Archi- gymnospermae, which are often fernlike in habit and always cryptogamic in the anatomical organization of their primary wood and in their mode of fertilization by antherozoids, and the Metagymnospermae, which present no external resemblance to the members of the fern series, and in which the centripetal or cryptogamic primary xylem has given place, in living forms at any rate, to transfusion tissue, and in which, also, fertilization by means of a pollen tube is a universal feature. The Coniferales are the largest and the most important group under the Meta- gymnospermae. Their significance from the evolutionary stand- point can scarcely be overestimated, not only because they are more abundantly represented in the living plant population of the earth than are any other gymnosperms, but also because they are copiously preserved as fossils as far back as the Paleozoic age. They thus supply the most important document for the inductive study of general principles of evolution presented by any group of living organisms, vegetable or animal, living or extinct. The paleobotanical and anatomical investigation of the Coniferales has greatly changed our views in regard to their phylogenetic sequence in recent years. The older students of the group restricted to a knowledge of living forms naturally assumed that the conifers, which are the simplest in organization of their vegetative and reproductive parts, are most primitive. By those entertaining this view the Taxineae are considered the most ancient conifers, and with them have been connected, not only the Cordaitales, but also the living genus Ginkgo. In the most recent systematic treatment of the coniferous tribe as a whole we find this attitude maintained, for Ginkgo and Taxus are regarded as closely related. It is needless to state that there 317 318 THE ANATOMY OF WOODY PLANTS is nothing in common between the anatomical structures of vege- tative and reproductive parts in Ginkgo and the Taxineae. A later, but apparently equally erroneous, tendency is to interpret the evolutionary sequence of the Coniferales entirely in the light of the data derived from the study of Paleozoic gymnosperms. This attitude is of course found strongly in evidence in those countries which have contributed notably to the elucidation of the organization of the seed plants of the Paleozoic. By those who are affected by the Paleozoic bias the araucarian subtribe of the Coniferales is considered the oldest representative of the group. There are those again who attempt to reconcile the taxinean and araucarian hypotheses of derivation by the assump- tion that the Araucariineae have come from the Cordaitales, while the remaining coniferous subtribes have been derived from the Taxineae. The hypothesis of a lycopodineous origin of the group has been put forward at various times, but need only be mentioned here, as it has few advocates and does not appear to derive any support from paleobotanical or anatomical facts. The views in regard to the phylogeny and evolution of the Co- niferales adopted in the present work represent an attempt to interpret this large and important group of gymnosperms in the light supplied by the anatomy of Mesozoic forms as compared with representatives of the group still living. The method of treatment adopted will be, so far as the limits of space in an ele- mentary textbook permit, purely inductive. As has been em- phasized in an earlier paragraph, the conifers, on account of their abundant presence in the floras past and present, supply a most valuable document for the interpretation of the fundamental principles of evolution. Since the araucarian conifers are quite generally regarded at the present time as the primitive representatives of the group, it will serve a useful purpose to consider these first. A transverse section of the wood of the stem in this subtribe (Fig. 225) generally reveals the presence of annual rings, unless the particular species under investigation happens to be of lowland tropical origin. The autumnal tracheids are marked by tangential pitting, a general feature of organization of the more modern gymnosperms. The CONIFERALES 319 wood normally shows the presence of only radial parenchyma, lon- gitudinal storage elements being absent. The longitudinal radial section of the wood (Fig. 226) shows a condition of pit- 2eees8eeen ting resembling that . 6 86 6 6 0@ 6 eee > found in the Cordai- tales, namely, one which is alternating and _ characterized by the absence of the bars of Sanio. The absence of wood parenchyma and the alternating char- acter of the pitting are features which at first sight would seem to justify the Fic. 225.—Transverse section of the wood of A gathis assumption of gq wstralis. Troe SORE Re A a & al ae wan Fic. 226.—Longitudinal section of the wood of A ga- this australis. close degree of rela- tionship between the araucarian coni- fers and the Cordai- tales, and this view of their affinities has been the one almost universally adopted. Before we inquire as to its validity it is necessary to exam- ine the organization of Mesozoic repre- sentatives of the group. In Fig. 227 is shown in trans- verse section the 320 THE ANATOMY OF WOODY PLANTS structure of a Cretaceous araucarian wood of the type designated Araucarioxylon. The annual rings are much less clearly developed Fic. 227.—Transverse section of Araucarioxylon from the Cretaceous of the eastern United States. rived as an exuda- tion from the rays. This is a condition often present in both living and extinct woods of araucarian affinities. We may now turn our atten- tion to another araucarian type commonly present in the Mesozoic— the genus Brachy- oxylon. In this type the wood in trans- verse section shows annual rings and the than in the wood of Agathis. The rays are uniseriate, as in the living type, but a marked contrast is presented by the presence of wood parenchyma in the fossil. The longitu- dinal section por- trayed in Fig. 228 shows both alter- nating pitting and the presence of parenchyma. Cer- tain of the tracheids are also filled with dark contents de- 228.—Longitudinal section of the same Araucarioxylon. CONIFERALES 321 absence of longitudinal parenchyma. In longitudinal radial aspect it manifests a kind of pitting which is only partially araucarian, for more often than not the pores are separated by con- siderable intervals and fail to alternate (Big..-220:)! (It) is only occasionally that the typical ar- aucarian crowding and alternation are present. More- over, in woods of the Brachyoxylon type wounding brings about the formation of trau- matic resin canals (Fig. 230) such as appear after injury in certain of the Abietineae and in the ! genus Sequoia. After the consideration of the conditions in the mature wood of living and extinct representatives of the araucarian conifers, we may now turn our atten- tion to the organization of the xylem in the conserv- ative organs of the exist- ing araucarian conifers. Fig. 231 illustrates the structure of the wood in the root of A gathis australis Fic. 230.—Transverse section of the wood ina region not very remote of Brachyoxylon formed after wounding. from the primary wood. Fic. 229.—Longitudinal section of the wood of Brachyoxylon. 322 THE ANATOMY OF WOODY PLANTS It is evident that, in the secondary xylem of the root, parenchyma, conspicuous by its absence in the mature wood of the stem, is abundantly present. Not only is this the case with the root, but the same situation is found in the first annual ring of the vegetative stem and also very strikingly in the woody axis of the ovuliferous cone. The facts here mentioned are of particular significance when correlated with the organization of the Cretace- ous Araucarioxylon shown in Fig. 227. Obviously the parenchyma pres- ent in the older type of araucarian wood is perpet- uated in those re- gions of the living form which we have learned in an earlier chapter to regard as conserv- ative: lt may accordingly be logically assumed Fic. 231.—Longitudinal section of the wood of the that woods of the root in Agathis australis. eH eee % eek Oaane o ce, te ‘ae, type of the living araucarian conifers formerly possessed longitudinal parenchyma and in this respect are at variance in organization with the ligne- ous structure of the Paleozoic Cordaitales. This conclusion is reinforced by an examination of the effects of injury in the living genera, for the infliction of wounds results frequently in the recall of the lost parenchyma even in the adult axis. We may now pass to the consideration of other features which are supposed to indicate a close degree of relationship between the Araucariineae and the Cordaitales. The most important of these are the crowded pitting and the absence of bars of Sanio. In Fig. 232 is shown the organization of the wood in the stem of the seedling of A gathis australis as viewed in longitudinal CONIFERALES 323 radial section. The pits are neither crowded nor alternating as in the wood of the adult. An examination of the organization of the seedling in the living representatives of the araucarian conifers therefore justifies the view that the ancestral forms did not possess crowded pitting. Precisely similar conditions are found in the cone, for here the pits in the tracheids nearer the primary wood lack the crowded and alternating disposition of the mature vegeta- . a tive wood of the genus. But a still more important feature is pre- sented by the organization of the wood of the ovu- liferous cones of the living A gathis and Araucaria. Fig. 233 shows: a longitudinal radial view of the second- ary wood of Arau- caria Bidwillit in the vicinity of the protoxylem. The pits show a very strong tendency to opposition in arrangement, and are certainly not angular by mutual contact, as is often the case in cordaitean woods. The most interesting feature shown by the figure, however, is the presence of bars of Sanio such as are entirely lacking in the adult vegetative wood of existing species of the araucarian conifers. As a consequence of the situation revealed in the conservative reproductive axis of the araucarian conifers, we are justified in assuming that the absence of bars of Sanio and the presence of alternating pitting are not primitive features of the organization of the wood of the subtribe, and consequently cannot be brought into court to prove its cor- daitean affinities. The evidence, in fact, must be read in exactly Fic. 232.—Longitudinal section of the wood of the seedling in A gathis australis. 324 THE ANATOMY OF WOODY PLANTS the opposite sense from that in the Ginkgoales; for, as has been shown in the preceding chapter, the anatomical facts there justify the assumption of the original presence of cordaitean structure, characterized by alternation of pitting and absence of bars of Sanio. In the case of the Araucariineae, on the contrary, we must assume on the basis of the structure of primitive regions that bars of Sanio and opposite pitting were an older feature of 10) (oo) { =| OY So) |= ee 1c 6 OS S| © S||O A]ite lito Cle ak S) Ss © © ON Fic. 233.—Longitudinal section of the wood of the cone axis in Araucaria Bid- willit in the region of the pith. organization of the wood and that they are as a consequence not nearly related to the Cordaitales. It becomes clear, when we consider the arguments derived from comparative anatomical data and those furnished by the study of extinct forms, that the organization of the mature wood in the living Araucariineae cannot be accepted as sufficient evidence of their relationship with the Cordaitales. The persistent foliar traces of the two living araucarian genera have been regarded in some quarters as an important indication of their primitive character. Here again the comparative anatomical situation CONIFERALES 325 as well as the conditions found in allied fossil conifers do not justify the conclusion reached. The seedlings of both Araucaria and Agathis show the earlier leaf traces as evanescent structures which cease to be formed by the cambium after the leaves to which they belonged have disappeared. It is only in the older trunk that the formation of foliar strands is perpetuated for many years, amounting even to centuries, after their corresponding leaves have disappeared. The persistent leaf traces which con- stitute so remarkable a feature of the organization of the mature trunk of the existing Araucariineae cannot therefore be regarded as anything but a bizarre and freakish feature which has no evo- lutionary importance. If any remaining doubt can be considered to exist on the subject, it is set aside by the organization of the Mesozoic araucarian woods, which (with the exception of the type known as Araucarioxylon), are distinguished by the absence of persistent foliar traces. Comparative anatomy lends very little support to the inference of cordaitean affinities for the araucarian conifers, and the evidence against this widely cherished view becomes quite overwhelming when the anatomical situation in the other subtribes of the Coniferales is considered. The further estimation of the claims of the Araucariineae to the pre-eminence of being the oldest’ conifers may appropriately be delayed until the anatomical features of other important subtribes have been examined. The Abietineae have in recent years made progress as claimants to the primitive position among Coniferales and to that of nearest proximity to the Cordaitales. At first sight the extremely com- plicated organization of both vegetative and reproductive struc- tures in the abietineous conifers appears to stand in the way of any such conclusion; but the results of the comparative investiga- tion of the living and fossil representatives of groups which have passed the zenith of their development has taught us not to consider complexity of organization as necessarily a criterion of modernity. It will be shown in subsequent paragraphs that the Abietineae are in a very strong position as regards primitiveness, both because they are apparently related, on good anatomical evidence, to such ancient groups as the Cordaitales and Ginkgoales and because 326 THE ANATOMY OF WOODY PLANTS they are clearly antecedent to the mass of other living coniferous subtribes. The mature wood of Pinus, illustrated in Fig. 234, is char- acterized in transverse section by the presence of resin canals and by rays of complex organization. The longitudinal structure of the wood, as is shown in Fig. 235, is characterized by the presence of bars of Sanio. The rays are of complicated structure, even when uni- seriate, and are composed of central storage cells and marginal elements resembling tracheids. If a primitive region such as that provided by the wood of the cone axis or root be investigated, it becomes clear that the bars of Sanio are not an ancestral feature of organization of the wood, since they are absent in the inner region of the wood of the cone and are also often lacking in the tracheary elements of the root, especially in proximity to the primary wood. This situation is portrayed for the cone of the Italian nut pine (Pinus pinea) in Fig. 236. It is obvious that the tracheids retain for some time the spiral markings of the primitive region. The walls of the tracheary elements show not the slightest indication of the presence of bars of Sanio until a region remote from the pith has been reached. The rays also are without the marginal tracheids which manifest themselves at an early stage in the organization of the wood of the vegetative branches. Clearly, so far as the structure of the wood in the reproductive axis is concerned, the Abietineae as represented by Pinus are derived from ancestors possessing the structure of the wood of the Cordaitales. Another interesting PNK 5a) Fic. 234.—Longitudinal view of the wood in Pinus resinosa. CONIFERALES 327 feature of resemblance to cordaitean forms is the absence of:a torus in the membranes of the bordered pits of the tracheids lying nearer to the primary wood. The situation in this respect is the exact opposite of that found in the case of the araucarian conifers, sl Fic. 235.—Highly magnified view of the tracheids of a species of pine, showing the bars of Sanio (after Gerry). in which the torus is sometimes present in the region near the primary xylem of the wood of the cone axis and is entirely absent elsewhere. The organization of the wood alone in primitive organs and regions justifies the conclusion of a filiation between the Abietineae and the Cordaitales rather than between the Araucariineae and the Cordaitales. 328 THE ANATOMY OF WOODY PLANTS We may now turn to the brief consideration of evidence derived from the organization of the wood of fossil forms and bearing on the respective antiquity of the Abietineae and the Araucariineae. The investigations of recent years have brought to light in the Jurassic and Cretaceous numerous coniferous woods which to a large degree possess characteristics intermediate between those VKANY YA TZ VAN AA \\ axe =i (Y YX N L\ WY AY [AN WWI Ti ra" c\\ WW ¥YYVN LAY ¥Y - a; = WO OANYY CRAWAG OHOAY, M TVW Oy \\ Fic. 236.—Transitional region from the xylem of the cone of Pinus pinea of the Abietineae and Araucariineae. The conclusion naturally follows that the two subtribes were less remote from one another in Mesozoic time than they are in the present epoch. The question of interpretation is strongly debated in the case of these woods. The mass of paleobotanists, obsessed by the araucarian hypothesis of the derivation of the Coniferales from their cordaitean ancestors and little concerned with the fundamental principles of comparative CONIFERALES 320 anatomy, have assumed that the transitional woods in question are those of Abietineae which are losing their primitive araucarian characters. A fatal objection to this point of view, however, is the fact that none of these transitional woods shows the presence of bars of Sanio. In other words, they must clearly be diagnosed as belonging to the araucarian side on the basis of the most reliable of diagnostics of coniferous woods—bars of Sanio. Attempts in the direction of proving the woods in question abietineous rather than araucarian have chiefly taken the form of discus- sions as to the value of ray structure in the diagnosis of coniferous woods. It is beyond the range of the present volume to discuss details of the organization of the radial structures in the Coniferales; but it may be stated in a general way and on the basis of com- parative anatomy that no feature is more subject to variability within the limits of a single subtribe and hence is less available for comprehensive conclusions in regard to evolutionary sequence. A final argument against the araucarian descent of the Coniferales from the Cordaitales is supplied by the extremely abundant Mesozoic araucarian type of wood known as Brachyoxylon. In wounded specimens of wood of this genus traumatic resin canals are formed (Fig. 237), resembling those of the normal wood of the pinelike conifers. The occurrence of resin canals as a consequence of injury in Brachyoxylon, in view of the fact that this genus is admitted by competent paleobotanists to be of unquestionable araucarian affinities, is of great significance. This being the case, we are justified in interpreting the canals formed after wounding as a reversionary phenomenon, indicating relationship to the pinelike ti a ' canta ditt Fic. 237.—Wood of Brachyoxylon formed after wounding. 330 THE ANATOMY OF WOODY PLANTS Abietineae. This interpretation of the situation is vindicated by the recent discovery of normal resin canals in the wood of the axis of the ovuliferous cone of a Javanese species of Agathis, A. Bidwillii (Fig. 238). Having discussed, so far as the limits of the present volume permit, the organization of the wood in conservative axes and in fossil forms, we must now turn to the discussion of that extremely important organ, the leaf. It has been made clear in an earlier chapter that the foliar organ of Pinus is char- acterized by the remark- able structure of its fibrovascular tissues. In the genus under discussion and to a less extent in allied genera the foliar conducting strand is sur- rounded by a cordon of transfusion tissue. The situation in this respect may be clearly ascertained by reference to Fig. 239. eevee immer es are distinguished by the absence of protoplasmic contents and by the occurrence of bordered pits in their walls. It is obvious that the tissues of this nature become joined with the xylem of the foliar bundles on its flanks. The transfusion tissue in modern representatives of the genus Pinus is not a continuous mass of tracheary cells, but has interspersed throughout its substance a considerable number of living cells provided with protoplasm and a nucleus. The investi- gation of the Cretaceous deposits at Kreischerville, Staten Island, has provided us with,extremely valuable data for the determina- tion of the organization of the leaf in Pinus and allied forms in the later Mesozoic. In some of the numerous species of Pinus which flourished in the American Cretaceous, transfusion tissue was present in large amount and contained little or no admixture CONIFERALES 331 of parenchymatous elements. In still other species the short tracheary elements ordinarily called transfusion cells were much less well developed. It is the remarkable genus Prepinus, however, which provides the most important evidence for estimating the bearing of the anatomical organization of the leaf on the problem of evolution of the genus Pinus in particular and that of the Abietineae in general. In Fig. 240 is shown the transverse section KX Fy Ss. Fic. 239.—Leaf bundle of Pinus Strobus of the leaf in P. statenensis. The outline is angular because of mutual contact with other and surrounding leaves of the fascicle. In Prepinus the growing point of the short-shoots persisted as it does in the living Ginkgo, and the fascicular leaves, instead of being few and definite in their number, were indefinitely numerous. It is interesting to note in this connection, however, that, although in the true Pinus of the Cretaceous the number of leaves in the fascicle was few and fixed as in modern forms, nevertheless the growing point of the short-shoot persisted indefinitely and did not disappear at an early stage, as in the living representative of 222 THE ANATOMY OF WOODY PLANTS the genus. Within the angular outline of the leaf in Prepinus is seen, beneath the epidermis, the ribbed hypodermal tissues, recalling those of the older gymnosperms. The cortical region of the leaf terminates in a not very clearly marked endodermis which doubtless owes its loss of definiteness to the changes resulting from fossilization. Within the endodermal boundary lies the entirely tracheary and strongly pitted transfusion tissue of the Fic. 240.—Leaf of Prepinus statenensis leaf. The elements of this category are differentiated into two zones—an outer one composed of short, broad, pitted elements, and an inner one consisting of thick-walled cells of narrow lumen. The former are known as the outer transfusion sheath and the latter as the inner transfusion sheath. Both structures have their counterpart in the leaf of certain of the Cordaitales. The double transfusion sheath was also frequently present in the foliar organs of true pines of the American Cretaceous. Another most interesting feature of the organization of Prepinus was the struc- ture of the xylem. As may be seen from Fig. 241, the wood presents two regions, an upper and a lower. In the former the CONIFERALES 333 elements are arranged in radial rows and usually increase in size toward the upper surface of the leaf. In the xylem directed down- ward are seen indications of wood rays, and the inspection of the longitudinal aspect reveals the fact that it is made up largely of tracheids with bordered pits. This is the centrifugal xylem and corresponds to the mass of wood in the foliar trace of the fascicular C) p : e 2° ia O) C@ © oO Po WA spe - “a D2 @ 17-7 = wend a oe) ie ae = (XA LS Zed, wake EEE Se, PAS SIT RACER Ee eee OT Sexee se of © Fic. 241.—Portion of leaf of Prepinus statenensis leaves of living pines. The upwardly developing wood is the cryptogamic xylem and confirms the conclusion as to the affinity of Prepinus, already suggested by the organization of its trans- fusion sheath, namely, that the genus is allied to the Cordaitales. It is thus apparent that the details of organization of the leaf in Prepinus, which in turn is clearly the ancestor of Pinus, justify an attribution of cordaitean ancestry to the Abietineae. This conclusion as to relationship is supported by the primitively cor- daitean character of the pitting which so strikingly indicates a 334 THE ANATOMY OF WOODY PLANTS relationship of the Abietineae rather than the Araucariineae with the Paleozoic gymnosperms known as Cordaitales. Not only do the Abietineae as a result of their anatomical organization and paleobotanical history present a strong claim to direct relationship with the older gymnosperms, but they supply equally compelling evidence that they are ancestral to other prominent coniferous subtribes. It will be well in this connection to begin with the in- ternal situation in the abietineous subtrrbe. it 1s readily subdivided into two series on the basis of ana- tomical structure— the Pineae and the Abieteae. - Ihe former are char- acterized by the possession of well- developed resin Fic. 242.—Transverse section of the root of Abies canals in the wood balsamea, showing the presence of a resin canal in the jn both vertical primary wood. and horizontal planes. In contrast to these, in the second series the ligneous resin canals of the secondary wood are notably absent. It is only in regions recognized as conservative that they make their appear- ance—in the primary structures of the xylem of the root (Fig. 242), in the secondary wood of the axis of the ovuliferous cone, and some- times in the first annual ring of the vegetative branches. Further, resin canals are found in the wood of the Abieteae as a result of in- jury. Both comparative anatomical and experimental evidence, as a consequence, vouch for the derivation of the Abieteae from ancestral forms possessing well-developed ligneous resin canals. It is of significance to note in this connection that the genus Cedrus, for the great antiquity of which the geological record supplies clear CONIFERALES 335 testimony, not only from American, but also from European de- posits, is strikingly distinguished by the fact that it produces both horizontal and vertical resin canals resulting from injury (Fig. 243). This condition is in contrast to that manifested by the other genera of the Abieteae, in which only vertical resin canals make their appearance in the secondary wood after wounding. It is now generally admitted by competent anatomists that there is strong evidence for the derivation of the Abieteae from the Pineae as a re- sult of reductionary modification. This con- Ue fen ¢ ne Go 4g ° ¢ ts Orie & ° ° ‘ ov iN clusion is reached, not | ies (| Gh aan inter att a) auars 9 ea 181B, =@@ 88 only on the testimony supplied by the resin canals as described above, but also from the com- parative anatomical consideration of the organization of the rays and the parenchyma of the secondary wood. It Fic. 243.—Transverse section of the wood of is apparent in regard to Cedrus deodara formed after injury, showing : reversionary appearance of resin canals in both these particular struc- vertical and horizontal planes. tures that the Pineae are more primitive than are the Abieteae. The ray of the Abieteae is often characterized by the loss of the marginal tracheids so dis- tinctively developed in the radial parenchymatous strands of Pinus and its living allies. The internal conditions in the Pineae may now claim our attention. Here we find a striking separation between Pinus on the one hand and Picea, Larix, and Pseudotsuga on the other, resulting from a consideration of the lining of the resin canals in the wood. In the first-named genus the secretory canals are lined by thin-walled parenchyma which, in the transformation of heartwood into sapwood, develops processes known as tyloses, which more or less completely occlude the resin canals. In the 336 THE ANATOMY OF WOODY PLANTS three remaining genera of the Pineae the lining of the secretory space is composed mostly of thick-walled more or less lignified cells. The resin canals in these forms do not accordingly contain well-developed tyloses in the heartwood. Another important distinction between Pinus and allied genera is the complete absence of wood parenchyma in the former. It has been shown in an earlier chapter that longitudinal storage parenchyma is formed in the secondary wood as the result of the modification of elements Ls eae. REY ae U mt js SO tS (\ ci | A Jit KO) O ; @E ; SS : ‘ RE Gy PO BVA: HVS YON wae JOOS. NOR Fic. 244.—Wood of Picea canadensis, showing terminal parenchyma destined to be tracheids. In Picea, Larix, and Pseudotsuga storage parenchyma is present, but at the end of the annual ring only (Fig. 244). In this position, particularly in the case of the root, it manifests convincing evidence as to its derivation by the occurrence of transitional stages between merely septate tracheids and rows of parenchymatous elements, resembling in their general configuration tracheary elements. In Pinus, therefore, there is no true paren- chyma of the wood, since such storage cells are found only in the three other genera of the Pineae. Where wood parenchyma is present, moreover, it is confined to the end of the annual ring and is clearly in a condition of derivation from tracheids, a state found normally in no other living representative of the Coniferales. It CONIFERALES S37 has been demonstrated in earlier pages that Paleozoic gymno- sperms are characterized by the complete absence of parenchyma- tous elements in the wood and at the same time by the general absence of annual rings in the stem. Pinus, as regards the organ- ization of the storage devices of the wood, is therefore clearly allied with Paleozoic types such as the Cordaitales. There are other conditions, however, which indicate for Pinus a primitive position among the Abietineae. First of all there is the possession of short-shoots. Pinus in this feature of organiza- tion presents a marked resemblance to the Ginkgoales, which Fic. 245.—Microspores of Ginkgo and Abies also bear their foliar organs on special spurs or short-shoots. Nor is the common possession of short-shoots unparalleled by other significant characteristics. Ginkgo and the Abietineae strongly resemble one another in the possession of bisporangiate sporo- phylls. In the two groups there are two microsporangia and two megasporangia or seeds on the reproductive foliar organs. The view sometimes advanced that the ovuliferous scales in the Abietineae consist of a fused pair of foliar structures has apparently no evidence in its favor. It is as clearly a single leaf as is the microsporophyll. ‘The microspores in the Abietineae and in the Ginkgoales also present striking points of resemblance which have only. recently been completely realized. In the monotypic Ginkgo the pollen is winged as in the more primitive Abietineae and resembles in its internal organization the structures found in the microspores of that subtribe of conifers. Fig. 245 illustrates the numerous features of internal and external resemblance between 338 THE ANATOMY OF WOODY PLANTS the pollen of the Abietineae and that of the Ginkgoales. Nor is the similarity confined to the structure of the microspores. It has been pointed out in an earlier chapter that the organ- ization of the wall of the sporangium in relation to the opening mechanism and to its derivation from the fibrovascular structures is practically identical in the Ginkgoales and Abietineae. Finally, the organization of the tracheids of the wood is similar in the case of the two groups under consideration. Pinus seems beyond question, by the possession of short-shoots, the number and organization of its microsporangia and megasporangia, as well as by the structure of its microspores, the general organization of the wood, and, finally, by the absence of true wood parenchyma, clearly allied to the sole surviving genus, Ginkgo. Pinus, lastly, presents a very strong claim to primitiveness among the Coniferales by reason of the general presence of short- shoots, such as are usually regarded as the prototypes of the ovuliferous scales of the female cone of the Coniferales as a whole. It follows, on the general principles of anatomy laid down in an earlier chapter, that the genus which still shows vegetatively the structures known as short-shoots is in an excellent position to claim a primitive position among the Coniferales. The absence of short-shoots in the seedling of Pinus is obviously no ground for an argument of any significance against the primitive presence of short-shoots in the genus. Negative evidence furnished by seed- lings is of no value, since only positive testimony in connection with the hypothesis of recapitulation can be accepted as valid in evolutionary argument. We may therefore assume that the presence of short-shoots in Pinus and Ginkgo, as well as many other features of resemblance between the two genera, is an unmis- takable indication of affinity. Further, since short-shoots are very generally assumed to have been the prototype of the ovulif- erous scale in the female cones of the Coniferales throughout, we may infer that the coniferous genus which has manifested these structures as a normal vegetative feature from remote geological times must be a very ancient representative of the Coniferales. But we are not by any means limited to a consideration of the general organization of the female cone in inferences regarding CONIFERALES 339 the relationship of Pinus to the other Coniferales. An excellent illustration of the value of anatomical evidence in the case of this problem is furnished by the interesting taxodineous genus Sequoia. The Taxodineae as well as the nearly allied Cupres- sineae are characterized anatomically by the organization of the female cone and the structure of the wood. The scales of the cone are superficially single, but in section they show the presence of a double series of oppositely orientated fibrovascular bundles, thus indicating the origin of the seed scales from the externally Fic. 246.—Transverse section of the cone scale of Sequoia gigantea, showing a double system of bundles with opposite orientation. double structures of the ovuliferous cone of the Abietineae (Fig. 246). In the organization of their wood the Taxodineae differ from the Abietineae in the absence of resin canals. There is, how- ever, a resiniferous secretion produced by scattered parenchymatous elements of the wood. In the structure of the radial parenchyma a condition of simplicity contrasting with that found in the Abie- tineae is manifested, for the marginal tracheids of the rays of the Abietineae are conspicuously absent in the normal wood of the Taxodineae in general and of Sequoia in particular. If we con- sider the genus Sequoia in the light of the canons of anatomy formulated above, very interesting results are reached. First, if a transverse section of the axis of the cone or of the ovuliferous scale of Sequoia gigantea be examined, resin canals reveal them- selves in the wood in proximity to the primary xylem (Fig. 247). J 340 THE ANATOMY OF WOODY PLANTS Further, an investigation of the first annual ring of the stem in trees which have attained such vigor of development as to pro- Fic. 247.—Transverse section of reproductive axis of Sequoia gigantea, showing resin canals in the wood. gions indicated above is good evi- dence of the origi- nal presence of such structures in the woody tissues of Sequoia. Addi- tional information on this subject is furnished by the wound reactions of the eenus. En either of the two species, S. gigantea or S. sempervirens, the infliction of wounds may. be fed erry eee me, 4 * Ld * ‘ * t e he OR wy duce seed often shows the pres- ence of resin canals such as are not normally found in the subsequent an- nual increments of growth (Fig. 248). Finally, the fibro- vascular strand of the leaf frequently contains in the region of the xylem a single resin canal. The occurrence of ligneousresin canals in the vari- ous primitive re- Fic. 248.—Twig of Sequoia gigantea, showing pres- ence of resin canals in the first annual ring. CONIFERALES 341 followed by the appearance of traumatic or wound resin canals as areversionary feature. In S. sempervirens, the redwood, this is the only mode of occurrence of these structures. It may be added in this connection that the normal seedling of Sequoia (either species) shows no resin canals in the wood. On the fallacious logic that structures absent in the seedling are not ancestral it could be argued that resin canals in the secondary wood are not an ances- tral feature of the genus Sequoia. This genus is the only one in any coniferous subtribe, other than the Abietineae, characterized in living species by the formation of traumatic resin canals. In Sequoia a sound inference based on the principle of conservative organs is that its ancestral forms were provided with resin canals throughout their structure. Although only the genus considered in the foregoing paragraph presents the abietineous feature of resin canals in the secondary wood as a result of injury, many genera of both taxodineous and cupressineous affinities revert to the abietineous type of ray as a response to wounding. This is notably the situation in Sequoia and is illustrated in Fig. 53. In another figure (Fig. 52) the occur- rence of marginal tracheids is indicated for the cupressineous species Chamaecyparis nootkatensis. The investigations of Miss Holden have made it clear that the presence of traumatically recalled ray-tracheids is a common feature of the Cupressineae and the Taxodineae. In neither of these tribes are such structures known to occur normally in conservative organs; hence their former presence is revealed only by reversionary phenomena. It is worth while to note that the recurrence of marginal tracheids as the result of injury is usually exemplified, not in the immediate region of the wound where hypertrophy alone prevails, but in a region of the stem more or less remote from the actual injury. This situation is of interest because it is paralleled by conditions found in connection with certain other wound reactions, notably those presented in the case of the rays in certain angiosperms. It is obvious from what has been stated above that ray-tracheids, although of much wider occurrence among the Cupressineae and Taxodineae, probably appear only as the consequence of experi- mental conditions and are no longer a normal feature of structure. 342 THE ANATOMY OF WOODY PLANTS Normal and traumatic resin canals and traumatic ray-tracheids are abietineous structures occurring in certain Taxodineae and Cupressineae, facts which, in accordance with the general prin- ciples of comparative anatomy already elucidated, may be regarded as indicating the abietineous origin of the two coniferous subtribes in which they occur. This conclusion is now somewhat generally accepted by those whose anatomical knowledge of the conifers makes their opinion of weight. Before we take leave of the two subtribes considered in the foregoing paragraphs it will be well to direct attention to the distribution and origin of wood parenchyma in woods of this type. The secondary xylem is characterized by the presence of usually abundant wood parenchyma, not confined to the end of the annual rings, but scattered throughout. The parenchyma- tous elements secrete a generally highly antiseptic essential oil. As a result of the presence of essential oils, and sometimes also by the infiltration of the tracheary walls with tannin, woods of taxodineous and cupressineous origin are frequently resistant to decay. The oil-secreting cells in the subtribes under discussion do not under normal conditions betray their derivation from tracheids except by the fact that they are grouped in series which have the fusiform shape of tracheary elements. In injured woods it is often possible to observe transitions between septate tracheids and rows of parenchymatous elements. It may accordingly be assumed, independently of the evidence of abietineous affinities supplied in the previous paragraphs, that the storage elements in the woods of the Cupressineae and Taxodineae are of tracheary origin. Another feature must be considered in this connection. In the minds of those who regard the Coniferales as an ascending series and not one of reduction, the resin canals which characterize the wood structure of the older Abietineae owe their origin to the clustering of the resin cells of the cupressineous or taxodineous type. This view of the origin of secretory canals in the coniferous series has been particularly emphasized by Penhallow. It meets with numerous difficulties, the chief of which is that the cells which surround the resin canals are not resin cells. The latter possess dark-brown contents and produce their secretion in an CONIFERALES 343 intracellular manner. The epithelial cells of the resin canals in the abietineous conifers, on the contrary, do not manifest the dark-brown (so-called) ‘‘resin,’’ but pour their secretion at once into the secretory space. The secretory canals found in the case of Sequoia gigantea are surrounded by cells which correspond only to a very limited extent to the resin cells of cupressineous woods. Most of the secretory elements are devoid of the so-called ‘‘resin”’ or dark-brown contents, and those containing this substance | are present in about the same proportion near the canal as they are in the structure of the adjacent wood. This situation is clearly revealed in Figs. 249 and 250. In addition to the Taxineae, Araucariineae, Abietineae, Cu- pressineae, and Taxodineae— subtribes of the Coniferales which have been discussed to a greater or less extent in the earlier paragraphs of the pres- ent chapter—there remain the Podocarpineae, a group which in the present period is con- fined almost entirely to the FAG 240: peavetre secre One : traumatic or wound resin canal of Southern Hemisphere. The — sSeguoia sempervirens. podocarpineous forms are generally regarded, and with a strong degree of probability, as somewhat closely allied to the Taxineae or yews, which have their main distribution in the Northern Hemisphere. They are char- acterized, however, by a less degree of simplification in their ovuliferous cones and frequently by the possession of winged pollen of the abietineous type, produced always in bisporangiate microsporophylls. The organization of the female cone in the Podocarpineae as a whole, and particularly in the genus Podocar pus, recalls by the presence of a bract and a subtending ovuliferous 344 THE ANATOMY OF WOODY PLANTS scale the conditions found in the double scales of the ovuliferous strobilus of the Abietineae. The reproductive features conse- quently supply some evidence for the association of the podocarps GAGS L_ SW i oe Ss SIDA SS, CESS. WOES KCOYa2D} Fic. 250.—Longitudinal section of a traumatic resin canal in the same species. with the abietineous conifers. The organization of the wood in the group under consideration is very similar to that found in the Cupressineae and Taxodineae. The tracheids possess opposite pitting and bars of Sanio. The parenchyma is abundant and scattered throughout the annual ring. A clear difference from the Cupressineae and Taxodineae is supplied, however, by experi- mental evidence, since neither traumatic resin canals nor margi- nal ray-tracheids have been found as yet in any of the genera of the Podocarpineae. We shall prob- ably not make further advance in the final determination of the phylogenetic or evolutionary position of this subtribe of the Coniferales until our present ex- tremely meager knowledge of the - fossil conifers of the Southern Hemisphere has been notably in- creased. It seems highly prob- able, on the basis of the organiza- tion of the scales of the female cone and of the sporophylls and spores of the male cone, that the Podocarpineae have abietineous affinities. Their final position will ultimately be determined by a better knowledge of the anatomy of extinct forms. Of the coniferous subtribes enumerated in the preceding pages the Taxineae have not as yet been considered anatomically. CONIFERALES ‘345 The reproductive structures in this group are extremely simple, and the ovuliferous apparatus produces in maturity a single ovule. In the genus Cephalotaxus of the Eastern Hemisphere an ovuliferous strobilus is present in the early stage of development; this is composed of scales each producing a pair of ovules—a condition comparable with that found in the Abietineae. As the develop- ment of the seed progresses all but a single seminal structure abort, so that in the end no vestige of the presence of a true fe- male cone can ordi- narily be observed. In accordance with the principle of re- capitulation, we must regard the young cone of Cephalotaxus as in- dicating the more primitive condition for the ovuliferous apparatus in the Cenmws 2 exws pre- sents a marked con- trast to that genus by the fact that at no PES ESSA Sar. aa) rs eg meal Loe Nel eee CNC TSCA FEES Sahm etl glixb- SACAIVAN SS WSN SSSIbSa ie) Bi alizs Soles Seileslesieclss aes: eSiZ>SI Sit she, egal esos ZI E ) ERIE IS = = See 7 ma R Re 1S f) aa ©) a | : i aX SS RA A tes cS = = ES SAIPSS SIKH Re 2S ASS) aes ) eS2 Se SZ beSa SSSI SIS Beales So beSa, eS II>< 9 SASSSz pion POR eSIRSS WPS! eo mae elo £6 (S- | Be ANY ee ll SSSI 8 ISI ocd ray Set A O it SSS TISS IRS bss eSeleseceet Fic. 251.—Semidiagrammatic view of the longitudi- nal organization of the wood in the Taxineae. time is the presence of a female or ovuliferous cone indicated. From the first there is but a single ovule, and this is not related at any time to a visible ovuliferous scale. The organization of the male cones in the Taxineae is naturally less reduced than that of the female, in accordance with the general principle of the conservatism of the microsporangial apparatus in heterosporous groups. In the case of - the Taxineae the reproductive structures furnish convincing evidence for the origin of the subtribe as the result of a process of reduction. The structure of the wood in the Taxineae is quite characteristic. The tracheids are marked by internal spiral bands which are of late origin and are frequently for that reason designated as tertiary thickenings(Fig. 251). Opposite pitting is present when the pores are 346 THE ANATOMY OF WOODY PLANTS numerous, and bars of Sanio are clearly developed. The state- ment is often made that the ligneous structure of the Taxineae is free from parenchymatous elements (Fig. 252). This is certainly true of the mature wood of the stem in both Taxus and Torreya. If, however, the roots in the two genera be examined, a varying amount of storage parenchyma is discovered which is ordinarily better developed in proximity to the region of the primary wood (Fig. 253). In species common to Europe and America, namely, Taxus baccata and its vari- eties, very little paren- chyma is found even in the root; but in oriental species of the genus storage ele- ments are somewhat abun- dant in this organ. The young stem, and particu- larly the root, of the genus Torreya show clearly developed longitudinal parenchyma in the wood. In Cephalotaxus, which by reason of the presence of a well-developed female cone at an early stage must be regarded as a primitive genus of the subtribe, parenchyma is markedly abundant in the organization of the wood. Injuries, also, frequently result in the recall of parenchyma in those taxineous woods which are normally without it. The generally uniseriate rays of the subtribe do not show the presence of traumatic ray- tracheids as a result of injury, and in this respect they present a marked resemblance to the woods of the Podocarpineae. Resin canals are conspicuously absent in the ligneous structures of the Taxineae, and not the slightest evidence of their former occurrence can be produced by experimental data. The genus Taxus is entirely without resin canals, even in its leaves, thus providing the only example of a conifer completely lacking these structures. An interesting parallel is presented by the hemlock (Tsuga) among Fic. 252.—Transverse section of the wood of the stem in Taxus cus pidata. CONIFERALES 347 the Abietineae. Here resin canals are normally absent, not only in the structure of the wood, but also in the other tissues of the stem. In the root of the genus they occur in the primary wood; and in the cone and leaves, in the tissues of the cortex. This distribution of resin canals is of course entirely in accord with the general principles of evolutionary anatomy. TJsuga, however, differs markedly from Taxus in the degree of obliteration of resin canals, since these structures here persist in conservative regions, while in the latter genus they have entirely disap- peared. In Cephalotaxus resin canals are well devel- oped except in the wood, but are apparently not susceptible of reversionary recall in ligneous struc- tures. It will be obvious from the description of the re- productive and vegetative organization supplied in the two preceding para- graphs that so simple a type as the genus Taxus cannot, according to the well-established principles of anatomy, be regarded as a primitive form. Its acceptance in this capacity by the earlier and philosophical taxonomy is shown on inductive evi- dence to be entirely unjustified. It appears on the basis of the facts at present available that the Taxineae are a reduction series in which the oriental Cephalotaxus among existing genera occupies the lowest position, while Taxus represents the summit. It is further obvious that the absence of wood parenchyma is not a primitive feature of organization of the group. If it be admitted that longitudinal parenchymatous elements primitively character- ized the organization of the wood, a derivation from the same stock as the Podocarpineae is plainly indicated. This conclusion is justified by the consideration of the young ovuliferous cone in as Ge x Fic. 253.—Transverse section of the wood of the root in Taxus cus pidata (after Bliss). 348 THE ANATOMY OF WOODY PLANTS the genus Cephalotaxus. The anatomical evidence points very clearly to the Taxineae as a reduction series, taking its origin from the same general group or plexus as the Podocarpineae. The somewhat meager fossil data at our disposal do not warrant us in assuming a very ancient occurrence for the subtribe Taxineae, since woods of this type are not found earlier than the Tertiary or Cenozoic. It is true that cones and leafy twigs from various levels of the Mesozoic have from time to time been referred to taxineous affinities, but there is no anatomical evidence that they belonged here. So far as any data derived from anatomical | structure are concerned, we are not justified in attributing to the Taxineae a great geological age. The external habit as a diagnostic criterion in the Coniferales has been shown in recent years to be almost as misleading as it has proved to be in the Cycadofilicales and other Paleozoic groups. Having considered the anatomical organization of the various subtribes of the Coniferales in such detail as comports with an elementary work like the present, before summing up the situation ° from the evolutionary standpoint we may well make some refer- ence to the anatomical characteristics of coniferous woods which are utilized by paleobotanical investigators. The genera of fossil woods logically increase in number as our knowledge of the ligneous organization of extinct plants becomes fuller and more complete. For the present purpose only a few of the more important genera of fossil woods need be considered. By reason of its relative resistance to decay, wood naturally often becomes isolated from its accompanying tissues and frequently is the sole surviving evi- dence of the former existence of gymnospermous groups. The situation thus presented is a difficult one, and the earlier charac- terizations of fossil wood were naturally largely empirical and made without reference to the facts or principles of comparative anatomy. In deference to the prevailing view that the araucarian conifers are the most ancient and form the connecting link between the Coniferales and the Cordaitales, we may consider them first. It has been indicated in a previous paragraph that the mature secondary wood of the two living genera of the Araucariineae is CONIFERALES 349 characterized by alternating crowded pitting and the absence of bars of Sanio as well as of parenchymatous storage elements. To this type of wood occurring as a fossil the name Araucarioxylon is given. A second genus of fossil woods is diagnosed by the presence of spirals on the inner walls of the tracheids and by the absence of wood parenchyma, under the generic designation Taxoxylon. Those woods characterized by the possession’ of ligneous resin canals in the horizontal and vertical planes are included under the generic appellation Pityoxylon. In coniferous wood without either resin canals or conspicuous storage paren- chyma, the name Cedroxylon is adopted. Woods which, on the contrary, are provided with abundant storage parenchyma are designated Cupressinoxylon. In all genera of fossil woods except the first the pitting is characteristically opposite. In the Araucarioxylon type the pitting is frequently crowded and alternation and bars of Sanio, universally present in other existing coniferous woods, are conspicuous by their absence. Clearly the use of even the small number of genera of fossil woods indicated in the preceding paragraph in connection with evolutionary inferences must, in the light of the conditions de- scribed for the various living conifers in the earlier part of the present chapter, be a matter of great difficulty. This arises from the fact that the organization of the mature wood in a given conifer is by no means necessarily an indication of its true system- atic position. The interpretation of the significance of wood structure in fossil and existing conifers can be successfully attacked only with a knowledge of the general principles of comparative anatomy. A failure to realize this situation has led to very many erroneous interpretations, both anatomical and _ paleobotanical. For example, it is quite clear from the data supplied at an earlier stage that the primitive condition of both the Avraucarioxylon and Taxoxylon type was a Cupressinoxylon, since abundant wood parenchyma diffused throughout the annual ring was formerly a feature of organization of these ligneous types, as is shown by a consideration of conservative organs, experimental results, and fossil evidence. Further, in some instances the Cupressinoxylon type has been clearly derived from the complicated structure 350 THE ANATOMY OF WOODY PLANTS found in Pityoxylon. This is, for example, true in the case of the genus Sequoia, which, on the basis of general anatomical principles, obviously formerly possessed both the ligneous resin canals and the marginal ray-tracheids of the older Abietineae. Examples might be indefinitely multiplied to show that the use of the mature structure of the wood in the Coniferales, without recourse to comparative anatomical and experimental data, is almost certain to lead in a given case to fallacious conclusions. It is now possible to sum up the situation from the standpoint of evolutionary anatomy for the phylogenetic sequence. It will be convenient to indicate preliminarily that the most generally accepted hypothesis of the morphological nature of the ovuliferous cone in the Coniferales furnishes a prima facie argument in favor of the primitive position of the Abietineae. In this subtribe the female cone consists of pairs of scales, the upper of which is ovulif- erous and the lower sterile. The ovuliferous scale is with a strong degree of probability to be regarded as a persistent single sporophyll bearing two seeds or megasporangia on its morphologically lower but physically upper surface. The megasporophyll is in relation to the abortive axis of the reproductive short-shoot. Aside from the morphological interpretation of the structures concerned, however, the fact remains that the units of structure in the ovulif- erous cone of the Abietineae are double and separate in their nature. In the female cones of the remaining coniferous sub- tribes there is clear evidence from comparative anatomy of the presence of fused pairs of scales in the ovuliferous structures. In accordance with general principles of morphology and without necessarily accepting the hypothesis of the short-shoot nature of the vertically paired scales of the abietineous cones, it is probable that the Abietineae are an older group than are the remaining coniferous subtribes. An additional argument for the antiquity of the Abietineae is furnished by their obviously close relationship to the Ginkgoales, which are admitted on every hand to be a primitive group of gymnosperms. The affinity with the Ginkgoales shows itself in the common possession of vegetative short-shoots by both the sole surviving Ginkgo and by the ancient but still prolific genus CONIFERALES 351 Pinus. Further, both megasporophylls and microsporophylls in the two cases produce paired sporangia. The microsporangia of Ginkgo present a common difference with those of the Abie- tineae from lower forms in owing their dehiscence to a mechanical layer derived, not from the epidermal, but from the fibrovascular, tissues. An additional feature of affinity is supplied by. the winged character and the internal organization of the microspores in the two groups, for they are practically identical. The structure of the tracheids of the wood in the Abietineae and Ginkgoales is significantly similar in the presence of opposite pitting and bars of Sanio, a common feature which distinguishes them from the Cordaitales and other older gymnospermous groups. Further, although the pitting and other details of organization of the tracheids in the two groups is of the modern gymnospermous type, the structure of the xylem in primitive regions clearly shows a filiation with the conditions characteristically presented by the Paleozoic gymnosperms. If a strong argument for the primitive position of the Abie- tineae is supplied by a comparison with the structural features of the Ginkgoales, an even more cogent one is furnished by their resemblance in important anatomical characteristics to the Cor- daitales. It is the leaf of the extinct genus Prepinus which mani- fests, as has been indicated in earlier pages, the most categorical and distinct similarity to the foliar organization of certain Cor- daitales. Not only is Prepinus the only known representative of the Coniferales to show distinct and unmistakable centripetal wood as distinguished from transfusion tissue, but it manifests its affinity to cordaitean forms by the presence of a double trans- fusion sheath in relation to the centripetal wood of the foliar bundle. It is further impossible to deny for Prepinus a close degree of relationship with Cretaceous species of Pinus which, like Prepinus, possess a well-marked double transfusion sheath and differ from the more primitive genus only in the absence of true centripetal wood. The agreement in foliar organization between Prepinus and cretaceous species of Pinus on the one hand and the Cordaitales on the other cannot be overlooked in any discussion of the evo- lution and affinities of coniferous subtribes. Although the wood 352 THE ANATOMY OF WOODY PLANTS of Pinus and Prepinus resembles that of Ginkgo in possessing opposite pitting and bars of Sanio, this organization contrasting with the tracheary structure of older types like the Cordaitales and the Cycadales in reality presents no difficulty. For in prim- itive regions and organs the alternating pitting without bars of Sanio characteristic of the Cordaitales is present in the Abietineae (particularly in Pinus and Prepinus), and passes by gradual transitions into the opposite pitting with bars of Sanio exemplified in the structure of the mature wood both in Ginkgo and in the Abietineae. The reproductive structures of the Cordaitales are too little known to us to supply appropriate points of comparison. It may be stated in summary that the Abietineae present as good anatomical evidence for derivation from the Cordaitales as do the Ginkgoales; and, moreover, they have an additional claim to such affinity by their clear relationship with the Ginkgoales. But it is not only by reason of resemblances to the Ginkgoales and the Cordaitales, neither few nor unimportant, that the Abie- tineae show themselves to be a primitive subtribe of the Coniferales. When the anatomical organization of the remaining coniferous subtribes is investigated in the light of the general principles so often emphasized in the present volume, it supplies in many cases distinct evidence that the Abietineae are the primitive stock from which all have taken their origin. This situation may be illus- trated first in the case of the Araucariineae, which are somewhat generally regarded as the primitive conifers and those most nearly connected with the Cordaitales. The strongest evidence for this claim is supplied by the organization of the tracheids, presenting the same alternating pitting and the absence of bars of Sanio as are manifested in the cordaitean and cycadalian gymnosperms. If alternating pitting alone were a sufficient criterion of relation- ship, many angiosperms by the possession of this feature could establish a claim to relationship with that ancient group of gymno- sperms. The evidence here as in other cases should be read in the light of the general principles of comparative anatomy. The longitudinal radial section of the cone axis, and to a lesser extent of the leaf trace, of either Araucaria or Agathis at once reveals the true situation. In these cases one always finds bars of Sanio CONIFERALES 353 in the region of the secondary wood near the primary xylem, and, where the pitting is abundant, frequent opposition of the pores. In other words, a situation presents itself which is the exact con- verse of that found, for example, in the Ginkgoales, in which the primitive region of the secondary wood shows alternating pitting and no bars of Sanio. In the later-formed wood the pits begin to appear in opposition and are separated by bars of Sanio. If we are justified in regarding the type of tracheid found in Ginkgo as originating from that typical of Cordaitales and other ancient gymnosperms, we are similarly warranted on the same evidenceé in viewing the alternation of pitting and the absence of bars of Sanio in the adult wood of the existing araucarian conifers as derived from a state in which both opposition of pitting and bars of Sanio were present. The evidence supplied by fossil forms, moreover, justifies the derivation of the Araucariineae from abie- tineous forbears, since many distinctly araucarian woods have been discovered in recent years in the Mesozoic which clearly present either normal or traumatic features uniting them with the Abietineae. In some instances, for example, thick-walled, heavily pitted ray cells, similar to those commonly characteristic of radial parenchyma in living and fossil Abietineae, are found in Mesozoic araucarian woods. This feature is significantly paral- leled in the rays of the cones of living araucarians. Traumatic resin canals are also found commonly in woods which are transi- tional from the abietineous to the araucarian type. This is notably the case in Brachyoxylon, a very common Mesozoic type of wood, and also in the much rarer Araucariopitys. Normal resin canals are, moreover, found in the wood of the ovuliferous cone of the living Agathis Bidwillii, from Java. It has been stated in earlier pages that there is distinct evidence from the organization of actual fossils and from the structure of conservative. regions in the existing Araucariineae that abundant wood parenchyma was an original feature of organization of the araucarian as contrasted with the abietineous Coniferales and the Ginkgoales, in which tangential storage elements are conspicuously absent. Not only, however, have abietineous forms obviously given rise to the araucarian stock on the basis of the general principles of 354 THE ANATOMY OF WOODY PLANTS comparative anatomy and the organization of fossil forms, but the same derivation is likewise indicated by two other series—the Taxodineae-Cupressineae on the one hand and the Podocarpineae- Taxineae on the other. The first series, on the basis of com- parative anatomical evidence, formerly possessed the ligneous resin canals and the marginal ray-tracheids of the later Mesozoic Abietineae. The supposed species of Seguota of the Mesozoic are not representative of the living genus, but have the organiza- tion of araucarian conifers, as has been shown by recent anatomical investigation of the forms from the American Cretaceous. They accordingly have no bearing on the question of the origin of the Taxodineae-Cupressineae. In the case of the series which has been described above as the Podocarpineae-Taxineae, the evidence from fossil forms is practically non-existent in the present state of our ignorance in regard to the organization of the Mesozoic conifers of the Southern Hemisphere. The situation must there- fore be judged on the basis of the living forms. The reproductive structures of the Podocarpineae, particularly those of the genus Podocarpus, are strikingly abietineous and sufficiently clearly indicate the affinities of the subtribe. The primitive Taxineae, obviously in accordance with the established principles of com- parative anatomy, formerly possessed the abundant wood paren- chyma of the Podocarpineae, and their systematic position is therefore elucidated. If the statements in the present paragraph are well founded, evidently both the Taxodineae-Cupressineae and the Podocarpineae-Taxineae are of abietineous origin. The time has now come to summarize the phylogenetic affini- ties of the Coniferales, both as regards the general relationship of the tribe and as regards the affinities of its particular subtribes with one another. It seems clear that the Abietineae have on all counts the strongest claim to be considered as primitive repre- sentatives of the Coniferales. These may be summarized as follows: filiation with the Cordaitales and co-ordination with the Ginkgoales; precedence to the Araucariineae, to the Taxodineae- Cupressineae, and to the Podocarpineae-Taxineae. The evidence for the ancestral character of the abietineous conifers may in the future be fuller, but scarcely any stronger, than it is at the CONIFERALES 355 present time. The accompanying genealogical tree (Fig. 254) will make clear the views as to sequence and affinities developed in the previous paragraphs of the present chapter. The Cordaitales of the Paleozoic serve as the starting-point, and from them were derived two cognate stocks—the Coniferales and the Ginkgoales. The latter have suffered much extinction and end in the present epoch in the sole surviving genus, Ginkgo. The Abietineae in earlier Mesozoic time Raves hice lOrmt ae Araucariineae, which flourished greatly in \ | 3| the later epochs of } J _noainece that period, to become ji! fF Proucerineg. we" almost extinct in the NY iS ; ly” glaciation which VS <| WA ushered in the Ter- \ | Vigo o tiary. The arauca- \ ‘i pales “a rian conifers dis- 7®eecepizeze\\ : NA “ tinctly took their Sil origin from the " abietineous stock calli } after it had developed Eee NW) eee TCLs. ligneous resin canals, but before marginal ray-tracheids had made their appearance. The Podocarpineae-Taxineae may have originated at a still earlier epoch and before the abietineous stock had developed the resin canals or the marginal ray-tracheids which distinguish it from the Cretaceous onward. Unlike the Arau- cariineae the Podocarps and their allies, the yews, did not lose the opposite pitting and bars of Sanio common to the parent stock of both Abietineae and Ginkgoales. The Taxodineae are a still later offshoot of the strong abietineous line and come into existence sub- sequent to the appearance of marginal ray-tracheids and ligneous resin canals. Certain conifers of the earlier and later Mesozoic, such as Voltzia, Brachyphyllum, Geinitzia (sometimes erroneously desig- nated Sequoia), etc., which have been referred to taxodineous Fic. 254.—Genealogical tree of the Coniferales, showing their proximity to the Ginkgoales. 356 THE ANATOMY OF WOODY PLANTS affinities, in reality have nothing to do with that group, but are araucarian or pre-araucarian in their relationships. There is at the present time no trustworthy evidence that the Taxodineae were in existence before Tertiary times, although it is quite possible in view of the general situation that they made their appearance in the later Cretaceous. The Cupressineae must be regarded as a con- tinuation of the taxodineous line and as having a similar relation to the abietineous ancestral forms. In conclusion, it may be remarked that, whatever may be the differences of opinion in regard to the reading of the evolution- ary document supplied by the Coniferales as they now present themselves to our gaze or are preserved for us as fossils from earlier geological epochs, there can be no doubt that they con- stitute the most important of all documents for the develop- ment of general evolutionary principles as the result of inductive reasoning. The treatment of the group in the present and preceding chapters is intended to clear the way for their further study by the development of general situations in relation to particular anatomical and paleobotanical facts. A continued investigation of the group, for which our American Mesozoic deposits have already yielded so much material of crucial impor- tance, is likely to result in the firm establishment of extremely valuable general principles for that type of biological research which bases its conclusions on inductive reasoning rather than on any purely philosophical attitude, either mechanistic or vital- istic. CHAPTER XXV THE METAGYMNOSPERMAE: GNETALES The aggregation of forms included in the present chapter is very small, but is of great importance from the phylogenetic standpoint. The Gnetales are represented in the existing flora of our earth by three genera. Of these the genus Ephedra occurs throughout the Northern Hemisphere, being somewhat abundant in the American and Asiatic continents and rare in Europe. Gnetum is a characteristically vinelike form occurring in the eastern and western tropics. The third genus, Welwitschia, is monotypic and is confined to the southwestern region of the African continent. Of the three generic types enumerated, Ephedra must be consid- ered on account'of both its reproductive and its vegetative features as on the whole the most primitive, although naturally its desert habitat has exerted more or less influence on its internal organiza- tion. Gnetum in general represents the highest stage of develop- ment attained in the group, and this statement is particularly true of the features presented by the organization of its gameto- phytes. Anatomically, however, Gnetum seems to occupy a somewhat less specialized position than does the extremely xero- phytic Welwitschia. The South African genus just named in its gametophytic organization is in a general way intermediate between Ephedra and Gnetum. The consideration of the repro- ductive structures proper, using that designation to cover both the floral organization and the gametophytes, need not be cov- ered more than incidentally in the present volume, since the morphology of the parts related to sex has recently been fully discussed in Coulter and Chamberlain’s Morphology of Gymno- Sperms. A transverse section of a stem of Ephedra (Fig. 255) reveals an anatomical situation not found in any of the Coniferales. Here the woody cylinder is characterized by rays which become very broad in the outer region of the wood but are quite narrow in the vicinity 357 358 THE ANATOMY OF WOODY PLANTS of the pith. Not only is the structure of the wood in the genus under discussion contrasted in the nature of its radial parenchyma with that of the Coniferales, but it also presents a striking resem- blance to the dicotyledons in the possession of true vessels, albeit of a primitive type. The correlation of large rays and true vessels in the organization of the wood in both Gnetales and dicotyledons is a feature which is clearly not without evolutionary significance, as will be shown in subsequent pages. The pith is of moderate size and the phloem and cortex constitute a rather thin layer on the surface of the strongly convoluted woody cylinder. The depressions on the face of the wood plainly correspond to the position of the large rays, as is the case with identical conditions in certain dicotyledons. In Fig. 256 as shown a_ transverse view of the structure of the wood some- what highly magnified. The features presented by the vessels and rays stand out very clearly. It is obvious that annual rings are present, although not conspicuously developed. The paren- chyma is of diffuse distribution as in the higher conifers. The large rays, however, illustrate interesting and phylogenetically important features. Even in the transverse view they are clearly composite structures and do not consist homogeneously of paren- chyma, as in the corresponding radial bands in our northern oaks and in the genus Gnetum. Vessels are seen intimately incorporated in the organization of the ray. The vascular are not the only elements of the longitudinal structure of the wood Fic. 255.—Transverse section of the stem of Ephedra gerardiana. GNETALES 350 incorporated in the large ray, for fibers are also present, although they cannot be so well recognized in the transverse section. The constitution and origin of the large rays in Ephedra are of great signifi- cance, not only for the Gnetales them- selves, but also in connection with the problem of the evo- lution of the higher forms known as dicotyledonous an- giosperms. It will accordingly be con- sidered somewhat in detail. Fig. 257 illus- Fic. 256.—Transverse section of the wood of Ephedra trates the organiza- species. tion of the large ray in an early stage of development when it is still rather nar- row and close to the medullary region of thevstem*, “Aniin-= spection of the illus- tration makes it clear that the ray is © bay) oO) ime amis. a homogeneous struc- tue) composed entirely of storage parenchyma. Fi- brous elements Fic. 257.—Longitudinal section of a large ray of i Ephedra in proximity to the pith. necessarily enter 360 THE ANATOMY OF WOODY PLANTS largely into its composition, and these are often in the condition of septation. The ray, in fact, is a composite structure, organized only partially from true radial parenchyma and also consisting largely of transformed longitudinal fibrous elements of the wood. These first become septate, and, particularly in the more external regions of the wood, their divisions become progressively more and more like the ordinary storage elements of the ray. Fig. 258 por- trays the longitu- dinal organization of the wood in the outer region of a rather thick stem of Ephedra californica. The large rays are here conspicuous and numerous, but not of equal size. In general, those of greater dimensions have originated in the region of the medulla, while those less conspicu- Fic. 258.—Tangential view of a large ray of Ephedra one by their Sac in its external region. have come into ex- istence more re- cently. The small degree of magnification employed in the figure does not make it possible to discern clearly the composite character of the radial parenchyma. The next illustration, Fig. 129, which reproduces one of the smaller radial masses under a higher magnifica- tion, makes the organization of these structures apparent. Obvi- ously not only ordinary radial parenchyma is concerned in the constitution of the rays, but also numerous fibers and even vessels. It may here be stated, although that situation is not clearly shown in the illustration, that fibers are seen in such rays in all conditions of transformation into elements resembling the ordinary radial parenchyma. In the genus Ephedra we have the wedding, as GNETALES 361 it were, of radial and longitudinal storage devices to constitute a new and, from the evolutionary standpoint, an extremely important type of radial organization. A fact not without significance in the present connection is the correlation of vessels with the more abundant storage devices present in the wood of the Gnetales. The large ray in the Gnetales is evidently a composite derived. from the fusion in certain radii of the wood of the original radial storage paren- chyma with paren- chymatous ele- ments derived from the copious trans- formation of the longitudinal tra- cheary elements of the wood by septa- tion. As has been indicated in earlier pages, wood paren- chyma made its appearance in the earlier and lower Coniferales first in relation to the end Fic. 259.—Another view of the same of the annual ring and in Mesozoic times, when well-marked annual periods of vege- tative inactivity had become established. Subsequently the wood parenchyma, in its inception clearly derived from the septation of tracheids, became diffused throughout the annual ring. When it had become abundant and well established in this condition, a situation favorable to the appearance of large rays was attained. The final impetus to the appearance of these structures was supplied by the origin of vessels which, by providing a greater supply of food substances and water from the soil, rendered possible larger and more efficient leaves. These in turn pro- duced larger quantities of assimilates which by the appearance of the large rays (co-ordinate in their origin with vessels and Mee M #84 3 se peek ¢; ak F 362 THE ANATOMY OF WOODY PLANTS diffuse wood parenchyma) found storage in the woody tissues of the axis. It will be obvious from the facts brought forward in the pre- ceding paragraph that diffuse and abundant wood parenchyma, vessels, and large rays are features which are intimately corre- lated in the organization of the woods of the Gnetales and the dicotyledons. That the situation portrayed is correct from the evolutionary stand- point is rendered clear by a condi- tion presented not infrequently in the wood of our living species of Pinus. Fig. 260 illustrates an interesting ab- normal feature which is often found in the wood of the white pine. Dhe annual rings are strongly depressed . locally, and in these Fic. 260.—Aggregate ray from Pinus Strobus regions the rays of the wood are unusually abundant, or, in other words, are clustered or aggregated. Since in the genus Pinus wood parenchyma is absent—a feature, as has been indicated in earlier pages, definitely correlated with its primitive phylogenetic position—the clustering of the rays, particularly in the absence of vessels, is of no evolutionary signifi- cance. This, of course, is primarily the result of the absence of the later acquired capacity of producing the longitudinal paren- chyma so necessary for the fusion of the aggregation of rays into large and homogeneous storage units. It may further be remarked in a general way that there is no evidence to show that the large masses of storage parenchyma which are so striking a feature of the organization of the woody cylinder of both the Gnetales GNETALES 363 and the dicotyledons were in the first instance related to the appendages, whether branch, leaf, or root. While, however, the prominent masses of radial storage parenchyma which dis- tinguish the groups under consideration are not primarily related to the appendages, they become somewhat definitely limited to this position in many forms, and even in the Gnetales themselves are more strongly developed in connection with lateral organs. We may next turn to the anatomical organization of the genus Gnetum. Fig. 261 illustrates the general structure of the stem in this genus as exem- plified by a young stem of Gnetum scandens. The appearance is very similar to that of a dicotyledonous vine like Clematis or Vitis. Extremely prominent large rays separate the woody cylinder into Fic. 261.—Transverse section of young stem of Gnetum scandens. distinct fibrovascular strands. The large rays of Gnetum are distinguished from the corre- sponding features of organization in Ephedra by two important details. In the first place, like those of the dicotyledonous climbers cited above, they extend broadly to the pith and do not appear first as narrow rudiments which are widened as they pass toward the out- side of the woody cylinder. Secondly, the broad rays of Gnetum are in the stem usually entirely homogeneous; that is, they contain no distinct vestiges of fibrous and vascular structures such as appear in the broad radial storage bands of Ephedra, although in types like G. scandens the broad rays of the stem are not obviously derived from compounding of aggregations of rays and longitudinal elements of the wood. Investigations on the part of Professor W. P. Thompson as yet unpublished seem to make it clear, how- 364 THE ANATOMY OF WOODY PLANTS ever, on the basis of the organization of primitive organs and regions that the condition of aggregation presented by the genus Ephedra was once present in Gnetum. We may therefore regard the large rays of the genus as comparable with the similar struc- tures in the mature wood of the stem of our northern oaks and derived in a similar manner as the result of aggregation and fusion. The minute organization of the secondary xylem in Guetum reveals she Bes. ly in addition to the aaa prominent rays, which have been dis- cussed in the pre- ceding paragraph, other radial struc- tures which are of the uniseriate type and correspond with the similar rays in the Coniferales and with the linear rays of the wood of the oak and allied dicotyledonous types. Parenchyma Fic. 262.—Transverse section of an older stem of js likewise abundantly the same. present in the diffuse condition. Last and by no means least, vessels which in most species of the genus present the large caliber characteristic of climbers are present. These will be considered later in a special paragraph. In Fig. 262 is shown an older stem of G. scandens. Here the woody cylinder instead of consisting of a single circle of bundles has become polydesmic. This condition cannot be regarded as having any large evolutionary significance, as it is commonly found in the stems of climbers of remote systematic affinities. Its chief significance is in connection with the origin of the type of cylinder presented by the genus Welwitschia and that found in certain cycadean types, living and extinct. Gnetum shows, not only the polydesmic stem often found in woody climbers, GNETALES 365 but also the extreme condition found in strap-shaped lianae. Fig. 263 portrays this condition in the stem of G. latifolium. The woody strands of the polycyclic cylinder fail to develop on two opposite sides of the axis, and this organization is correlated with the flattened transverse section in the stem. It is obvious that the genus under discussion has advanced to a condition of organization such as is paralleled by perennial climbers among the dicotyledons, and it must therefore be considered as having reached a high evolutionary position. The broad short axis of the remarkable genus Welwitschia may now claim our attention. Here the stem never attains a height Fic. 263.—Transverse section of the flattened stem of Gnetum latifolium of more than a half-meter and bears two large perennial leaves which, according to the investigations of Bower, are not the persistent cotyledons, but a subsequent pair of foliar organs. The perennial leaves of Welwitschia are inclosed at their bases in hollow spaces resulting from the outgrowth of the stem. Within these cavities, which function as moist chambers, are situated the basal growing regions of the leaves; they are thus preserved from fatal desiccation under the extremely arid conditions connected with the desert habitat of the genus. Professor W. P. Thompson has been able, through the co-operation of the Sheldon Foundation of Harvard University, to secure an abundant supply of material illustrating the anatomical organization of Welwitschia. When the results of his investigations have been published, our knowledge of this interesting and aberrant South African genus will be largely increased beyond that supplied in Hooker’s well-known memoir. The general organization of the axis in the genus is well illustrated 366 THE ANATOMY OF WOODY PLANTS by the accompanying figure (Fig. 264) of the stem of a seedling collected by Professor Thompson in Southwest Africa. It is clear that the same polydesmic organization of the axis is present as is found in the older stem of species of Gnetum. In the South African genus, however, the polydesmic condition extends to the roots and is accordingly to be regarded as a more innate feature of organization than in Guetum. The structure of Welwitschia suggests a climbing ancestry. Although we do not know the explanation of the polydesmic condition in climbers, it is clearly co-ordinated with the vine habit. We may suppose that the forbears of the genus were originally forest climbers and that the surviving strongly truncated desert species has per- sisted in its present Fic. 264.—Transverse section of young stem of mee Welwitschia mirabilis. habitat with the re- tention of the ances- tral polydesmy. A similar suggestion has been made in an earlier chapter as a possible explanation of the phenomenon of polydesmy in the cycadean forms, living and extinct. Having considered the general topography of the stem in the Gnetales with particular reference to the presence of large rays of the dicotyledonous type and the phenomenon of polydesmy, we may now profitably turn our attention to the more minute organ- ization of the wood. The ligneous tissues consist of rays and longitudinal elements. The former have already been sufficiently discussed in previous paragraphs. The longitudinal structures of the xylem consist of tracheids, vessels, and storage parenchyma. The tracheids do not need any extended reference, as they have GNETALES 367 been described in an earlier page of the present work. They possess clearly marked bordered pits larger than those of the dicotyledons and provided with a distinct torus. The vessels of the tribe are of considerable interest from the standpoint of the doctrine of descent, as they clearly indicate the derivation of vascular structures from tracheids. This takes place by the modification of the terminal regions of the incipient vessel from gradually tapering to distinctly inclined walls at angles with the sides of the element. These differentiated terminal aspects of the vessels are provided with very much larger pits than are found in the lateral walls. These pits, however, generally in Ephedra, and apparently universally in the two higher genera, lose their membranes at an early stage, and free intercommunication is thus established. In the higher genera there is a marked tendency for the terminal walls of the vessel to develop a single huge bordered pit in which the membrane is lacking. In Ephedra, on the other hand, the terminal pits are numerous, and in a few cases are found to fuse with one another horizontally with the resultant ap- pearance of slits comparable to those in the vessels of the lower dicotyledons. The type of vessel found in Ephedra has been re- cently stated to persist in the reproductive axes of the genus Gnetum. The parenchymatous structures of the Gnetales need no extended reference, for on the whole they resemble those of the higher Coni- ferales, both in their distribution in the annual ring (and this is diffuse) and in their configuration. Sometimes structures occur in the woods of the Gnetales more or less resembling substitute fibers, since with pointed elongated configuration they unite a persistence of protoplasmic contents. It is clear from the brief summary of the organization of the wood here supplied that the Gnetales are of great importance from the evolutionary standpoint, particularly in connection with the important problems presented by the evolution of large rays and vessels. They furnish a valuable criterion for the estimation of primitive anatomical characteristics in the organization of the wood in that huge heterogeneous aggre- gation of forms assembled under the caption of dicotyledons. Their value in this respect will appear, at a later stage. Although the Gnetales clearly indicate conditions of anatomical organization 368 THE ANATOMY OF WOODY PLANTS which are of a primitive nature, we are unfortunately even less well informed as to their fossil representatives than in the case of the angiosperms. There are, in fact, no well-authenticated gnetalian remains, even from the later period of the Mesozoic, in which the dicotyledons had become well established as an important component of the plant population of the earth. The wide geographical distribution of the three living’ genera may perhaps be regarded, in conjunction with their anatomical organ- ization, as a definite indication of their earlier more abundant occurrence. The root in the Gnetales needs no special consideration in the present connection. In the genus Guetum it furnishes some evidence as to the original organization of the large rays, but in Welwitschia it is polydesmic like the stem and is of little value from the standpoint of evolutionary anatomy. The structure of the root in Ephedra closely resembles that in the stem, except as regards those general features which distinguish root from axis. The foliar organs of the group which forms the subject of the present chapter are distinctly gymnospermous in their anatomy and frequently exhibit the copious development of transfusion tissues of the type characteristic of the leaves of the Ginkgoales and Coniferales. Centripetal wood is conspicuously absent in the leaves of the Gnetales, unless it be assumed that the transfusion elements are actually representatives and not merely derivatives of the old centripetal or cryptogamic wood. On account of the small size of the leaves in Ephedra the transfusion tissues are relatively poorly developed. In Gnetum a higher systematic position is strongly vouched for by the organization of the leaf, in which transfusion elements are not particularly well developed. The foliar organ of Welwitschia supplies us with transfusionary features most strongly manifested. The truth of this statement may be verified by reference to Fig. 265, which illustrates a part of a transverse section of the leaf of the South African genus. Transfusion elements originating on the flanks of the xylem extend, as in certain Coniferales, above and below outside the sclerenchyma- tous sheath which surrounds the fibrovascular bundles of the leaves. GNETALES 369 The anatomy of the Gnetales is of particular importance at the present time when they have come to the front once more, either as a cognate stock with the dicotyledons or as their actual ancestors. The study of the internal organization of the group in comparison with the dicotyledonous angiosperms reveals many features of marked resemblance. Both are provided with large rays which are clearly fusion products; and in both the wood shows conducting elements belonging to the category of vessels. The rays apparently supply a very cogent argu- ment for the close affinity of the Gnetales and the angiosperms. In the case of the vascular struc- tures, however, it is not so clear that a morphological identity of the ele- ments present in the two groups can be successfully maintained. = oe "ia oe J, ‘f - oad eo wall? Tips Y ye IY g ae * Satan gr a AA ETS 12 IPS @5 Oe) S3¢ cS) Sse fears = See - See Seis , gb os .23 4 at 4 4 ( bis TL 7] 4, VG G44 UT SEES SS NY Ss SS rs 2 WHYS SSF SS = PRINS ‘ if WG, Fic. 265.—Transverse section of a leaf bundle in Welwitschia mirabilis. In the dicotyledons the pits present on the terminal walls of the vascular elements are not larger than those which appear laterally, and the perforation of the vessel takes place as the result of fusions of opposite pits, as has been shown in an earlier chapter. A very different situation manifests itself, as indicated above, in the genera of the Gnetales. Here the vascular elements have exceedingly large pits on their terminal walls, and in Ephedra these are usually without membranes, 370 THE ANATOMY OF WOODY PLANTS while in the other two genera they are invariably so characterized. The phenomenon of fusion of the pits to form the scalariform perforations present in the lowest type of vessel of the dicoty- ledons is rare in the woods of the Gnetales. The general anatomical organization of the fibrovascular tissues in the Gnetales, however, may be said distinctly to favor the hypothesis of dicoty- ledonous affinities, or, at any rate, to be more in harmony with such relationship than with that of any other group of seed plants. The affinities of the Gnetales on the gymnospermous side are much more difficult to discover. This situation is due no doubt in large part to the fact that as yet no properly authenticated fossil representatives of the group have been found. In recent years there has been a tendency to associate this group with the Cycadales, but it is extremely difficult to discover any valid reasons from the anatomical side to justify such a relationship. There seem, in fact, to be no anatomical features of wide validity which can be invoked in favor of an affinity between the highest living gymnosperms and the lowest. It seems on the whole more probable that the Gnetales are cognate with, or derived from, the Coniferales, since there are a number of features which make such a connection likely. The transfusion tissue of the highest gymnosperms is clearly of the coniferous type, and this feature must count strongly against any close relationship with the Cycadales, in which, owing to the strong persistence of the centripetal wood, true transfusion tissues have not yet made their appearance. The uniseriate rays of Ephedra and Gnetum also point to coniferous affinities and not toward a connection with the Cycadales, in which the rays are universally multiseriate. The presence of bars of Sanio in the vessels of Ephedra supplies likewise an argument for the coniferous rather than the cycadalian relationship. : The main support for the cycadean origin of the gymnospermous group which forms the subject of the present chapter has been derived from the reproductive structures of the living and extinct representatives of the cycadean stock. The investigations of Wieland have brought to our knowledge the complete organization of the reproductive parts in the Bennettitales. These consist GNETALES 371 of cones involved in the young condition in rather large sheltering, bracts. Immediately above the series of bracts microsporophylls (usually of large size and pinnate structure) are attached to the axis of the strobilus. The main part of the cone is, however, made up of the seminal organs, consisting of pedicels to which single seeds are attached in an orthotropous manner. The seeds are somewhat sheltered by the swollen ends of sterile appendages inserted among the seminal organs on the axis. The protected condition of the seeds has given rise to the suggestion of angio- spermous organization. This apparently cannot be regarded as more than the merest analogy, since the seeds are not shel- tered within a closed megasporophyll and the pollen is deposited directly upon them after the typical gymnospermous manner. Further, the cycadean fertilization is not even siphonogamous, as would be expected of a group presenting valid claims to be regarded as ancestral to the highest seed plants. Nor is the analogy with the flower of the angiosperms to be given greater weight, for the arrangement alone and not the intimate organiza- tion of the reproductive parts shows any real resemblance to the conditions found in the floral structures of the angiosperms. An androgynous cone such as is frequently present in the Coniferales supplies an equally good basis for comparison; for here the bracts below correspond to the floral envelopes of the flower, while the lower whorls of microsporophylls simulate the anthers, and a plausible resemblance to the carpellary whorls is presented by the ovuliferous scales of the upper region of the modified cone. The most striking objection and the same as occurs in the case of the Bennettitales is the fact that the ovuliferous scales are not angio- spermous. The siphonogamic fertilization of the Araucarian coni- fers, on the other hand, reveals a nearer degree of resemblance to the conditions found in the flower of the angiosperms than does the zoidogamy of the archigymnospermous Bennettitales. In the present state of our ignorance of the fossil ancestors of the Angio- spermae it seems impossible to fix on any group of gymnosperms, living or extinct, except the Gnetales, which can be regarded with any degree of probability as having been either ancestral to the highest of the seed plants or even cognate with them. Bo THE ANATOMY OF WOODY PLANTS In accordance with the hypothesis of the derivation of the angiosperms from the Bennettitales, a relationship between this cycadean group and the Gnetales has been suggested. There seem to be very slight grounds for this assumption of affinities. The so-called “pollen chamber” of Ephedra is not morphologically equivalent to the pollen chamber of the lower gymnosperms which is derived by the breaking down of cells in the lysigenous manner, and in this respect is in marked contrast to the depression on the apex of the nucellus of Ephedra, which is continuously covered with the epidermis. Moreover, Ephedra and the other Gnetales are siphonogamous in contrast to the zoidogamous condition of fertilization in the Cycadales. The details of organ- ization of such a flower-like structure as is found in Welwitschia apparently supplies no adequate basis for comparison with the bisporangiate strobilus of the Bennettitales. The original error of Saporta in designating the impressions of the fructifications of bennettitean types as belonging to hypothetical proangiosperms or primitive angiosperms has manifested a considerable degree of vitality in the rather long interval since it was first advanced; but there seems little reason to accept it at the present time, in view of our increased knowledge of the organization of both vege- tative and reproductive parts in the various groups of seed plants, living or extinct. The Gnetales are clearly gymnosperms which in certain features of anatomical structure and reproductive organization have made a marked advance in the direction of the characteristics of the angiosperms, and it is not improbable that they are at least a cognate group. They present, however, no valid resemblances in either their reproductive or their vegetative parts which justify an assumption of relationship, even remote, with the extinct bennettitean Cycadales. It therefore appears highly unlikely that either the angiosperms or the Gnetales have any close degree of relationship with any archigymnospermous group, although it seems not at all improbable that they are somewhat closely related to one another. CHARTER XcxvVi THE ANGIOSPERMS The angiosperms as a whole possess features which separate them sharply both reproductively and vegetatively from gymno- spermous groups. The first of these in importance is the phenom- enon of angiospermy itself. In the group the microspores or pollen grains no longer reach the micropylar canal at the apex of the ovule, but are accommodated on the tip of the megasporophyll, which becomes modified as the receptive prominence or stigma. The reception of the microspores on the terminal region of the carpel or sporophyll is not, however, an exclusive characteristic of the angiosperms, since the same feature is presented by the surviving araucarian conifers. The megasporophylls in this largest and most important group of the seed plants are either folded upwardly upon themselves in such a manner as to inclose the young seeds or ovules, or undergo protective fusions with other similar structures in the same flower. The angiosperms are characterized anatomically throughout by the possession of vessels, these structures being absent only in certain aberrant representatives of the Cactaceae, Crassulaceae, and Trochoden- draceae. In all the exceptional cases mentioned there is clear evidence on comparative anatomical and experimental grounds that vessels were formerly present. The possession of histological structures in the wood known as vessels may accordingly be set down as a primitive feature of organization of the angiosperms. Associated with the vascular structures just indicated, there is a general improvement in the storage devices of the wood which, in an extreme form, leads to the appearance of the herbaceous type. The gametophytes, particularly the male gametophytes, of the angiosperms present a very marked degree of uniformity in the two great divisions of the group. The microspore or pollen grain undergoes part of its germination in the microsporangium and develops normally a tube nucleus and a generative cell. The 373 374 THE ANATOMY OF WOODY PLANTS latter, unlike the similar structure in the microspores of the higher Coniferales, does not give rise to stalk and body cells, but originates directly by division the two generative nuclei which function in fertilization. The microspores are sheltered in sporangia, which are typically four in number, on each sporophyll. The sporangia owe their dehiscence to a mechanical layer within the wall, resem- bling in structure that found in Ginkgo and certain Coniferales, but no longer related, as in these, to the fibrovascular system of the sporophyll. The megasporangium is much modified and, as in other known seed plants, is without any opening mechanism. In certain of the lower and amentiferous dicotyledons, however, tracheary structures have been discovered in the inferior region of the megasporangium (Casuarina, Corylus, Castanea). The germinated megaspore normally gives rise to a gametophyte containing originally eight naked nuclei which result from three successive divisions. Of these, six become organized as cells by the development of inclosing protoplasmic bodies, while the two remaining nuclei, one from each pole of the elongated sac, unite to constitute the endosperm nucleus, a structure characteristic for the angiosperms and not occurring in any lower forms. ‘Three cells in the micropylar region of the gametophyte become organized as the single egg and the two synergidae. Three others constitute the antipodals in the base of the gametophyte. After the egg has been fertilized by one of the sperm nuclei of the pollen tube and the endosperm nucleus has contracted a union with the remaining male element, the egg develops as the embryo and the endosperm nucleus gives rise to a mass of tissue which usually quite supplants the original gametophyte or embryo sac as nourishing substance for the developing embryo. The seed of the angiosperms conse- quently typically contains, in addition to the gametophyte and sporophyte of lower seed plants, a third generation. This is known as the trophophyte or endosperm, and it is distinguished from gametophyte and sporophyte, not only by its peculiar mode of origin, but also by the fact that in its nuclear divisions three times as many chromosomes are present as in the gametophyte and one-half more than in the sporophyte. This cytological condition is doubtless due to the three nuclei which are fused to THE ANGIOSPERMS S15) constitute the original endosperm nucleus from which the cells of the endosperm or trophophyte take their origin. The high degree of constancy in the essential features of organization of both sporophyte and gametophyte in the angiosperms mark them as a monophyletic group in which the two great divisions, dicoty- ledons and monocotyledons, have had a common origin. There seems to be no reasonable doubt that both divisions of the angiosperms—the dicotyledons and monocotyledons—have originated from gymnospermous ancestors and not directly from any existing or extinct group of vascular cryptogams, since they entirely lack cryptogamic features of organization in all their organs with the sole exception of the root. The radical organ, however, is without significance as indicating cryptogamic deriva- tion, for cryptogamic or centripetal primary wood is present in all roots without exception. It further seems obvious that the angiosperms in neither of their two divisions can have originated from the Archigymnospermae, since they present the siphonoga- mous mode of fertilization in contrast to the zoidogamy or fertiliza- tion by antherozoids present in the lower gymnospermous tribes which are more nearly related to the Filicales. The general features of the angiosperms indicated above characterize the two great divisions, dicotyledons and monocotyle- dons, in common; and it is now necessary to specify the distinguish- ing structures which separate these from one another. Since the dicotyledons are with the greater probability the older and more primitive of the two main groups, they will first be considered. In the dicotyledonous angiosperms the seed is distinguished by an embryo possessing paired cotyledons or seed leaves. This feature is perhaps the most constant characteristic of the group. In the fibrovascular structures the wood is distinguished by well- marked secondary growth which becomes feeble only in forms in which the herbaceous habit has become distinctly developed. The tissues belonging to the conductive category are, moreover, typi- cally arranged in the form of a cylinder which is continuous in woody forms but becomes broken up into separate strands in stems with herbaceous texture. When the fibrovascular organiza- tion consists of isolated bundles, these are ordinarily arranged in 376 THE ANATOMY OF WOODY PLANTS a circular fashion, but occasionally in stems with large leaves provided with numerous foliar traces the periphery of the cylinder is no longer capable of accommodating the bundles, so they have to be disposed of in a position either medullary or cortical. The leaves of the dicotyledons are usually distinguished by skeletal structures or veins ending freely toward the margins. The main veins may be arranged either in a radiating or in a palmate fashion, or may take their origin in an alternating manner from opposite sides of a main vein or midrib, in which case the venation is said to be pinnate. The free venation of dicotyledonous angiosperms gives them a considerable advantage over the monocotyledons in the possibility of submerged existence or a shaded habitat, when their leaves often become finely dissected. The root of dicotyledons presents no special features worthy of note in a general statement. The floral parts are ordinarily present in multiples of five, and the floral envelopes show themselves on the whole less likely to vary from the pentamerous condition than do the essential or strictly reproductive whorls, the stamens and pistils. Pollination is sometimes effected through the agency of currents in the air, but more commonly in the higher families by insects. Fertiliza- tion results from the penetration of the pollen tube from the stigma to the micropyle of the ovule. The course of the pollen tube after it leaves the region of the style may either be direct through the cavity of the ovary to the micropyle or, avoiding the leap across the ovarial air space, it may make its way round through the basal or chalazal region of the ovule. The last method of fertilization is characteristic of the genus Casuarina, the Betu- laceae, the Juglandaceae, certain Urticaceae, etc., and is known as breech fertilization or chalazogamy. It has been suggested by Treub and Nawaschin that this is a primitive method of pene- tration for the angiosperms and marks a transition from the siphonogamous and higher gymnosperms in which the pollen, being deposited directly upon the ovule, has not become accustomed to leaping an air space. In the lower representatives of the dicotyledons the pollen, although no longer deposited on the micropyle, still maintains its primitive inability to cross an air space. There is much to be said for the hypothesis of the primitive THE ANGIOSPERMS ite | significance of chalazogamy from the standpoint of fibrovascular anatomy. It seems, however, a feature too likely to be modified somewhat rapidly by conditions to rank as a criterion of the first order for the distinguishing of the most primitive dicotyledons. The monocotyledons are distinguished, as their name indicates, by a seed containing an embryo with a single cotyledon or seed leaf. This feature is very constant, but there are indications of the presence of a second cotyledon in certain of the grasses, such as Zizania, Avena, etc. The fibrovascular strands of this group are ordinarily closed; that is, they do not possess the capacity to increase in thickness through the activity of a cambial layer. The arrangement of the strands in the monocotyledonous angio- sperms is also distinctive, since the bundles, instead of being disposed in a circular fashion as in the mass of herbaceous dicotyle- dons, are scattered throughout the transverse section of the cylinder and sometimes even occur in the cortex. This peculiar disposition is, beyond any reasonable doubt, the result of the entrance of numerous leaf traces into the axis at each node, a consequence of the high assimilative efficiency of the foliar organs. The veins of monocotyledonous leaves are distinguished primitively by a closed arrangement; that is, starting out at the base of the leaf as a closed system, they reunite at the apex of the leaf. This disposition of the skeletal tissues of the leaf makes it immune from tearing action. The lateral veins, in consequence of this situation, are largely abortive. In many palms, aroids, and Scitamineae the venation of the leaf becomes open as a result of changes in the apex. In such cases the venation of the early- formed leaves of seedlings is closed, showing that this condition is the primitive one for the group. The root in monocotyledons is distinguished, as is the stem, by the absence of secondary growth. The bundles are usually distributed in a circular and radial fashion, but in certain palms and orchids they may be scattered throughout the transverse section of the organ as they are in the stem. The floral parts occur in multiples of three, and the floral envelopes, as in the dicotyledons, show less numerical variability than do the essential whorls consisting of stamens and carpels. Pollination is effected usually through the agency of insects, but may be 378 THE ANATOMY OF WOODY PLANTS brought about by currents of air in some of the probably more primitive groups. Fertilization is always porogamous (through the micropyle), and chalazogamy is at the present time quite unknown in the monocotyledons. The members of this group are extremely important as food plants on account of their high efficiency in the elaboration of assimilates. The proportion of seed produced by some of the cereals in a vegetation period of three or four months is often over 30 per cent of the total weight— a relative productiveness seldom realized in other plants. CHAPTER XXVII THE WOODY DICOTYLEDONS As a matter of convenience the anatomical organization of the woody dicotyledons will be considered in the present chapter. It must not be supposed, however, that such a mode of treatment implies that the woody texture of the stem has any value from the phylogenetic or taxonomic standpoint. Perennial dicotyledons are distinguished by the possession of a thick woody cylinder resulting from the activity of a cambial layer situated between phloem and xylem; this adds largely to the wood and less copiously to the inner bark during the periods of growth. The woods of the dicotyledons offer a great range of structural organization, and their identification on the basis of anatomical features is corre- spondingly difficult. In all except a few instances dicotyledonous woods are pro- vided with vessels. These belong to two main types, namely, those with scalariform and those with porous perforations. It has been made clear in an earlier chapter dealing with the structure and organization of the vessel that the type with scalariform per- foration of the inclined terminal walls results from the fusion of rows of opposite pits which gives rise to elongated horizontal pores from which the membranes quickly disappear. This process repeated in successive rows of pits results in the appearance of lattice-like or scalariform perforations in the ends of the vessels, and these permit a ready passage of water. On general evolution- ary principles the vessel with scalariform perforations is to be regarded as more primitive than the porous type presently to be discussed. It is not surprising for that reason that it is a characteristic feature of groups which are considered on good grounds to be low in the dicotyledonous scale. The vessel with the porous type of perforation is clearly derived, as has been dem- onstrated in an earlier chapter, from the scalariform condition, in the first instance at any rate, by the loss of the bars of 379 380 THE ANATOMY OF WOODY PLANTS lattice-work through mucilaginous degeneration. The vessel of the second type is found in the woods of the higher groups and indi- cates a more advanced condition of evolution, other things being equal, than does the vascular type with scalariform terminal perforations. Frequently woods with the porously perforated type of vessel in their mature structure show the scalariform con- dition in the region of the primary wood, thus providing confirma- tion of the conclusion that the latticed terminal wall of the vessel is phylogenetically older than that in which large pores are present. In many instances vessels in dicotyledonous woods become more or less degenerate and are then easily recognized by their inclined end walls and in any case by a lateral pitting and internal sculpture which clearly distinguishes them from tracheids or fibers. Such vessels are often present in woods in which the fibrous ele- ments are of the nature of libriform, substitute, or septate fibers, and are frequently inappropriately designated as tracheids. True tracheids have always tapering or fusiform ends and are not provided with the lateral pitting and sculpture of vessels. It is important to diagnose degenerate vessels as such, because a failure to make this distinction may result in quite erroneous views as to the relationship of woody dicotyledonous forms. In some cases typical vessels may disappear altogether from the mature structure, either generally or locally. Cases of the general dis- appearance of vascular elements are supplied by certain Cactaceae and Crassulaceae. In the genus Drimys among the Magnoliaceae and in certain genera of the allied Trochodendraceae vessels have also entirely disappeared from the normal wood. In Drimys, interestingly enough, wounds, especially wounds of the root, recall elements which have the lateral sculpture of normal vessels of the Magnoliaceae, without manifesting, however, their charac- teristic scalariform perforations. This defect is easily explained as a result of the comparatively small size of the reversionary elements simulating vessels. Local absence of vessels is frequently found in connection with the development of the large rays in dicotyledonous woods. This is particularly well illustrated in the wood of Alnus and in the root-wood of certain of our northern oaks. In the region of the aggregate ray, as has been indicated THE WOODY DICOTYLEDONS 381 in earlier pages, the organization includes only tracheary elements. It is thus apparent that vessels, a characteristic feature of structure in dicotyledonous woods, may in certain instances be absent. There is no reason based on the general principles of comparative anatomy for regarding their absence as a primitive feature. In woods of temperate climates the vessels in the spring wood are often much larger than in the later growth, and the organization in such cases is described as ring-porous. The ring-porous condi- tion is not, however, universal in trees of higher latitudes and is not ordinarily found in tropical woods which in general have their annual zones indistinctly marked. : The tracheary elements in dicotyledonous wood, as has been indicated previously, undergo very numerous modifications. In the lower forms they resemble the similar structures in the gym- nosperms, but quite generally they lose to a large extent their water-conducting function and become mechanical or storage elements. The least advanced condition in the mechanical direc- tion is designated the fiber-tracheid, distinguished by the re- duction in size and decrease in number of the bordered pits as well as by increase in length and by thickening of the walls. The libriform fiber, a further modification, has lost or nearly lost the bordered pits, these being replaced by simple pores. In the sub- stitute fiber, which retains its protoplasmic contents, and in the septate fiber, which is divided by delicate partitions of pectic cel- lulose into a number of separate units, are seen storage modifica- tions of the tracheids present in the higher types of dicotyledonous woods. . The parenchymatous elements of dicotyledons are primitively scattered throughout the annual ring. Although rarely and only under experimental conditions revealing by actual transitions derivation from tracheids, the storage parenchyma is generally grouped in longitudinal fusiform or pointed series with robust and lignified partitions which clearly indicate its origin. In the systematically higher dicotyledons the parenchyma is character- istically grouped in clusters around the vessels. This condition is known as vasicentric and is a common feature of woods in which the tracheary elements have become partially or entirely mechanical. 382 THE ANATOMY OF WOODY PLANTS It must not be supposed, however, that the relation between me- chanical fibrous elements and vasicentric parenchyma is abso- lute, for in groups characterized by this mode of parenchymatous distribution it is present even in genera with tracheary mechanical cells. In other words, the grouping of parenchyma about the vessels has a deeper significance than that of mere convenience to water supply. In not a few instances the storage cells may be confined to the end of the annual ring. This is, for example, the situation found in the Salicales, and it also frequently characterizes genera of the Magnoliaceae occurring in temperate climates. In these instances an examination of the primitive regions, together with experimental investigation, reveals as the original condition either the vasicentric or the diffuse distribution of parenchyma. It may be stated summarily that diffuse storage elements constitute the primitive conditions in the woods of the dicotyledons, and that a later modification is the vasicentric. By reduction either of the two types mentioned may give rise to the terminal condi- tion. Terminal parenchyma is accordingly a phenomenon of reduction in the dicotyledonous series, while in the Coniferales, as has been elucidated at an earlier stage, it represents the primitive state in which all transitions between tracheary and storage ele- ments are frequently and normally found. It is in the organization of their wood rays or radial storage tissues that the dicotyledons manifest the most distinct differences from the mass of the gymnosperms. It has been made clear in previous pages that the primitive type of ray organization for the group was the linear or uniseriate ray. In the earliest conditions presented to our investigation, however, that is ac- companied by the aggregate ray, consisting of more or less fused congeries or clusters of rays separated by fibrous elements. This type we must regard as an original one for rays other than unise- riate in the dicotyledons, because it is clearly found in Ephedra, by common consent the most primitive representative of the Gnetales, and because it is extremely persistent in primitive organs and regions in the dicotyledons themselves. The facility with which fibrous elements are transformed into storage cells in the group under consideration has led to the metamorphosis THE WOODY DICOTYLEDONS 383 of the aggregate ray, described above, into large homogeneous masses of radial parenchyma as a consequence of the parenchyma- tous modification of the separating fibers. This condition, known as the compound ray, is found in relatively few dicotyledonous woods, and these are ordinarily regarded as low in the systematic scale. In woody types, moreover, it very readily passes into the antecedent aggregate condition. A third and the commonest condition of organization of the radial parenchyma in dicoty- ledonous woods is presented by the diffuse condition. Here the original aggregation, instead of retaining its identity or passing into the compound state last described, spreads out in the manner of a fan. This procedure results in the diffusion of the original aggregations of rays evenly throughout the structure of the wood. As a consequence of this phenomenon the organization of the wood in the mass of dicotyledons is characterized by the presence of abundance of rays which are of mediocre width. Sometimes the rays of this type are nearly equal in size, but very generally they range from extremely small to moderately large. Now and then, however, as, for example, in the wood of beeches of the North- ern Hemisphere and in the genus Platanus, extremely large rays are found, readily distinguishable from those of the oak type by the fact that they grade almost imperceptibly into radial parenchymatous bands of mediocre dimensions. In the typical compound ray such as occurs in certain species of Quercus, Cas- uarina, and the Ericaceae the large ray is in sharpest contrast to the primitive uniseriate condition. In the foregoing paragraphs a general account has been sup- plied of the various anatomical features of dicotyledonous woods, and an attempt has been made to indicate the primitive condition in connection with each category of structures. It must not, however, be supposed that a primitive condition of organization in regard to any one of the categories described in the preceding pages necessarily indicates for a given group a low position in the evolutionary scale. Taken altogether, nevertheless, they supply extremely valuable testimony from the standpoint of the doctrine of descent and on the whole the best available in the present state of our ignorance regarding fossil ancestors of the angiosperms. 384 THE ANATOMY OF WOODY PLANTS It will accordingly be of interest in the present connection to summarize the evidence in regard to the primitive type of dicotyle- don supplied by anatomical data. A tendency of long standing is to consider the amentiferous forms as representing a low condition among the dicotyledonous angiosperms. In discussions in this connection it is well to dis- tinguish the true Amentiferae from types which simulate them. The Salicales, for exdmple, on the grounds both of their anatomical organization and of important details of floral structure, cannot be regarded as allied in any but the remotest way with types like the alder and the oak. Further, on anatomical ground types with more or less well-organized floral structure must be admitted to affinity with the Betulaceae, Fagaceae, etc. This is true of the Casuarinaceae and Ericaceae. On the basis of the co-ordinate occurrence of vessels with scalariform perforation, tracheary fibrous elements, diffuse wood parenchyma, and aggregate rays we must accord to the genus Casuarina a primitive position among the dicotyledons. This designation of affinity on the basis of the organization of the wood is supported by the fact that it alone among the dicotyledons possesses transfusion tissue of the flanking gymnospermous type. A further indication of its primitive position is furnished by the presence within the ovules of excep- tionally large amounts of sporogenous tissue and also of tracheary elements. Finally, we have the phenomenon of chalazogamy, the significance of which is still much disputed. On anatomical grounds there could scarcely be stronger reasons for regarding Casuarina as the most primitive representative of the dicotyledons. The only objection that has been seriously urged against this position is the fusion of parts in the ovuliferous floral structures. This objection, however, must weigh lightly in the balance in view of our knowledge of the extreme conservatism of anatomical structures in the case of living and extinct gymnosperms. It has, for example, been pointed out that the living cycads are practically identical in anatomical organization with the extinct bennettitean forms, although their reproductive structures differ very widely. Fusion of floral parts does not furnish a sufficient argument for a high systematic position, as on that ground the genus Welwitschia THE WOODY DICOTYLEDONS 385 would be put in a higher taxonomic position than Ranunculus, because its reproductive structures present a condition of cohesion not found in the flower of the buttercup. The suggestion that Casuarina owes its anatomical organization to its xerophytic habit must be definitely rejected because of the extremely general- ized type presented by the organization of its woody structures. In the single genus under consideration all the types of rays found in dicotyledons, as has been shown in an earlier chapter, are presented in the different species. Since all the species are equally xerophytic, it is quite impossible to connect any type of radial parenchymatous organization with the xerophilous habit. Physio- logical or ecological explanations of anatomical facts are always to be welcomed when they have any logical probability, but when they fail in this respect they only obscure the evolutionary situa- tion. The general anatomical evidence in the case of the interest- ing genus Casuarina seems, in the present state of our knowledge at any rate, entirely to justify the primitive position assigned to it in the great systematic work of Engler and Prantl, in which it is placed at the very base of the dicotyledons. If on anatomical and other grounds Casuarina must be regarded as a primitive representative of the dicotyledonous angiosperms, it is equally clear on the same evidence that with it must be joined the Betulaceae and Fagaceae and in all probability the Ericaceae. The usual fusion of parts in the flowers of the groups enumerated cannot apparently, in view of the overwhelming anatomical evidence for their primitive position, be regarded as a very im- portant systematic criterion. Wind pollination and the general absence of herbaceous forms further supply striking features of conformity to the conditions found in the higher gymnosperms from which it is very likely the dicotyledons have taken their origin. Another assemblage of forms which has been pushed into the foreground, particularly in recent years, as the primitive repre- sentatives of the dicotyledonous angiosperms are the Ranales. Without discussing whether the families included under this. general heading all properly belong here, we may point out that on anatomical grounds the claims of that group to affinity with 386 THE ANATOMY OF WOODY PLANTS the Gnetales and other gymnospermous types must be regarded as somewhat doubtful. The general anatomical organization of the Ranales presents some range of variety; but they do not strikingly exhibit either vessels, fibers, parenchymatous distribu- tion, or organization of the rays such as would be expected from the study of the higher gymnospermous types and the investigation of primitive regions and organs in the dicotyledons themselves in primitive representatives of the angiosperms. The only strong argument which can be advanced for the low systematic position of the Ranales is based on their floral organization. The fact that this has been deliberately disregarded in the WNatiirliche Pflanzenfamilien of Engler and Prantl shows that from the sys- tematic standpoint it is a criterion which cannot be considered as of overwhelming importance. With the ranalian origin of the angiosperms is tied up the whole hypothesis of their derivation from the Bennettitales. It has been pointed out that, from the point of view of anatomy, there seems to be little reason to enter- tain the hypothesis that the proangiosperms were of cycadean origin, even if the earlier discovered impressions of the reproductive remains of Mesozoic cycadean forms were originally referred to angiospermous affinities by so distinguished a paleobotanist as Saporta. Anatomically speaking, there seems accordingly to be equally slight grounds for the derivation of the angiosperms from zoidogamous gymnosperms as from ranalian dicotyledons. The whole question, however, must await final and satisfactory solu- tion until we are actually acquainted with the earlier angiospermous types which will doubtless be sooner or later brought to light from the Jurassic or from even earlier epochs of the Mesozoic. In the meantime such knowledge of the general anatomical principles as has been gained from the comparison of extinct and living gymnosperms appears to point toward types like Casuarina and its allies as representing, at any rate anatomically, the most primitive conditions. CHAPTER XXVIII THE HERBACEOUS DICOTYLEDONS The herbaceous type in the dicotyledons, although not of any definite systematic value, has a considerable significance from the anatomical and evolutionary standpoints. It has been pointed out in earlier pages that discontinuity of the woody cylinder in siphonostelic forms simulating that found in herbaceous dicoty- ledons is frequently present in older groups. In such cases, how- ever, the situation has a very different anatomical explanation and a diverse evolutionary interpretation from that presented by the dicotyledonous angiosperms. In many of the lower groups of plants belonging to both Lycopsida and Pteropsida we find the surviving representatives distinguished from those characteristic of the period of greatest luxuriance by a herbaceous, as opposed to an arboreal, habit. Such herbaceous types owe their origin to degenerative changes and present a distinct contrast to the situation exemplified in the herbaceous dicotyledons, where the modification is the result of differentiation and specialization and not the consequence of mere degeneracy. It is necessary to illustrate clearly the mode of appearance of the herbaceous type in the older groups before passing on to the consideration of the situation manifest in the herbaceous angio- sperms. Fig. 266a illustrates the organization of a siphonostelic stem in a lepidodendrid. Here the primary wood is well developed and constitutes a continuous cylinder. The secondary xylem, which is the result of cambial activity on the inside of the primary phloem, forms a continuous layer interrupted only in the region of exit of a strand destined to a branch, which causes a gap in the primary cylinder that is naturally perpetuated in the earlier organization of the secondary cylinder. In 0 is shown the condi- tion presented by a sigillarian of Permian age. In this instance the siphonostelic primary cylinder has become degenerate and consequently is only well developed in the regions facing departing 387 388 THE ANATOMY OF WOODY PLANTS foliar traces. Asa direct result of this discontinuity of the primary cylinder, the secondary cylinder becomes united only by the gradual broadening of the originally separate secondary segments. In c is portrayed the condition found in the stem of a third rep- resentative of the Lycopsida—namely, a calamite. Here the primary wood is extremely degenerate, and the secondary segments as a consequence are very narrow and quite widely separated. In the herbaceous living Equisetum, the stem of which is depicted on an earlier page, secondary growth has disappeared, being present only as a vestige in conservative organs and regions. The series indicated above illustrates the origin of the herbaceous type by degeneracy. The Lycop- sida have been chosen because they reveal the situation in the clearest Fic. 266.—Diagram showing the effect of Manner and with the degeneracy of the primary wood on the develop- fewest complications. In cara the secondary cylinder. Explanationin po Pteropsida the topog- “ raphy is rendered less easy of comprehension by the presence of the often numerous foliar gaps which characterize the anatomical organization of the siphonostelic central cylinder of that phylum of vascular plants. The principles involved are, however, the same. It may accord- ingly be stated that discontinuity in the primary siphonostelic central cylinder is due either to gaps related to the exits of traces supplying the appendages or to the local degeneracy of the cylinder itself. These interruptions are perpetuated in the early organiza- tion of the secondary cylinder. If the secondary tissues are also degenerate, as in the existing survivors of cryptogamic groups, a pronounced herbaceous condition is the result. This is, however, THE HERBACEOUS DICOTYLEDONS 389 pre-eminently the consequence of degeneracy and has no dynamic evolutionary significance in contrast to herbaceous modifications presented by the stems of dicotyledonous angiosperms. With the foregoing preliminary statement in regard to the appearance of the herbaceous type in primary and secondary cylinders (or in the secondary cylinder alone) in lower forms we are in a position to attack the origin of the stems of herbaceous texture in the highest seed plants. It has been noted in the preceding paragraphs that the degenerate herb is derived from ancestral forms characterized by woody stems. The same general condition is found in dynamic herbaceous types among dicoty- ledons; and it is extremely important to keep this situation clearly in view, as a failure to do so results in an anatomical fallacy.. It cannot accordingly be too strongly emphasized that a proper understanding of herbaceous axes in the angiosperms can be reached only by the comparison of nearly related stems of woody and herbaceous texture. Any other procedure leads to erroneous results. In former chapters the various types of rays in the Gnetales and the dicotyledons have been discussed. In the present con- nection only one of these need seriously be considered—the com- pound ray. The large or compound type of ray is characteristic of only a few arboreal types of probably primitive antecedents, but occurs in a more or less modified form in many herbaceous and climbing stems. It will be convenient to discuss first the condi- tions present in vines, as these are usually more woody in their character and consequently serve as an appropriate transition to axes of soft or herbaceous texture. As a preliminary to the con- sideration of the anatomy of the vine, it will be well to devote some attention to the organization of an exotic member of the Vitaceae from the tropics. Fig. 267 reproduces the woody cylinder of the shrubby genus Leea from the eastern tropics. To the right are to be seen:a number of large rays which clearly belong to the category designated in an earlier chapter as compound. Above and below, and particularly to the left of the illustration, the com- pound rays become much smaller in size. Those which are of greater dimensions are in relation to leaf traces passing out in the 390 THE ANATOMY OF WOODY PLANTS region of the node. Fig. 268a@ shows one of these on a higher scale of magnification. In the large ray and toward the bottom of the figure lies the leaf trace, which is both subtended and flanked by storage parenchyma. The wood on either side of the large ray shows the presence of the primitive rays, which, as has been pointed out on an earlier page, may be considered in a general way as equivalent to the narrow rays of the conifers and similar forms. In Fig. 2680 is seen a vertical tangen- tial section through one of the large leaf rays of the same genus. It is evident that the foliar trace runs in a much enlarged ray and is sur- rounded on all sides in its horizontal course by ray parenchyma. It is very clear from the con- sideration of the genus Leea that there are pres- ent large rays in storage relation to the leaf traces, precisely as in the oak, Casuarina, and similar forms. We may now pass to the situation in Vitis, where the conditions are not so manifest, but are quite intelligible by comparison with the shrubby member of the Vitaceae just described. Fig. 269 shows the general topog- raphy of the stem of the Concord grape in the region of the node. Seven leaf traces are to be seen as darker masses. Of these only one is passing into the cortex and the rest are still contained within the woody cylinder. Fig. 270a illustrates one of the foliar seg- ments of the stem with a higher degree of magnification. The segment in question is separated on either hand from the rest of the woody cylinder by broad radial bands of parenchyma. In the leaf trace itself may be found radial dark stripes, the primitive rays. These are absent in the segments of the cylinder which Fic. 267.—Transverse section of woody cylin- der of Leea. Explanation in the text. THE HERBACEOUS DICOTYLEDONS 391 lie on either side of the trace. The leaf trace thus illustrates in the genus Vitis the conservative character which has been asserted for it on earlier pages. The most interesting feature presented by Fig. 270a is, however, the fact that the leaf trace is subtended externally by a broad mass of parenchyma which on its flanks passes inwardly into the broad rays, separating the foliar segment from its neighbors on either hand. The situation in a general Fic. 268.—a, transverse section of leaf ray in Leea; b, vertical section of leaf ray in Leea. way, in fact, duplicates that found in the case of Leea, except that primitive rays are confined to the traces proper in Vitis and the broad ray subtending the trace is very much shortened in its radial dimension. Fig. 270b shows the same trace in a lower section or, in other words, considerably below the node. Here the broad ray facing or confronting the leaf trace has disappeared, having been gradually replaced by typical woody tissues, con- sisting of septate fibers and vessels. As a consequence of this situation the flanking rays are now separately continuous to the outside of the cylinder and are not united by a broad tangential 392 THE ANATOMY OF WOODY PLANTS mass of storage parenchyma, as is the case in the region shown in Fig. 270a. Vertical tangential sections make the situation more apparent. Fig. 271a@ shows a plane of section near the surface of the cylinder. The leaf trace (seen as a dark mass) is completely surrounded by storage parenchyma, which, however, is less well developed below than on the upper side of the strand. It is particularly obvious in this plane that the trace runs in a mass of storage parenchyma precisely as in Leea, described above. The tangential sections taken nearer the cen- ter of the*cylinder present a very differ- ent appearance. In this region the trace will still be pursuing “its vertical course in the stem and as a consequence will be flanked by storage Fic. 269.—Transverse section of the node of the parenchyma laterally. Concord grape. Explanation in the text. Above the trace lies the parenchyma of the foliar gap. This statement may be verified by reference to Fig. 271. The trace distinctly contains numerous primitive rays, conspicuously absent in the segments on either side, the segment on the right showing the presence of some vasicentric paren- chyma, such as is characteristic of the Vitaceae in general. It will now be convenient to consider the topography of the foliar trace in its relation to the woody cylinder of the stem in a slender upper node of the vine. Fig. 272 reproduces the general relations exhibited by such a thin axis. Obviously, as the cyl- inder of the wood becomes more attenuated, the trace of the leaf will increase in size relatively to surrounding parts. This situa- tion is clearly shown in the illustration, which represents a plane of section immediately below the node and corresponding in THE HERBACEOUS DICOTYLEDONS 393 level to that in Fig. 270a. It is thus evident that, if the woody cylinder is thin enough, the leaf trace will correspond to it in thickness, and that as a result the subtending or confronting parenchyma, so prominent a feature of the topography of the leaf trace in the cylinder of Leea, Casuarina, the oak, and other woody stems with compound rays, is plainly absent. The comparison of very slender and thicker annual stems of the vine with those Fic. 270.—a, transverse section of foliar ray in Vzizs in the region of the node b, transverse section of foliar ray below the node. of the shrubby Leea makes it clear that an extreme thinning of the axis brings with it a condition of organization in which the storage parenchyma no longer surrounds the foliar trace, but merely flanks it on either hand. In climbing or herbaceous axes, in which this slenderness has become a fixed feature, some com- pensation for the loss of subtending or confronting storage tissues is provided by the great lengthening of the flanking rays, which often extend, as was pointed out by Strasburger over a quarter of a century ago, through one or more internodes. It will be obvious from the facts introduced in the present paragraph that 304 THE ANATOMY OF WOODY PLANTS woody axes with the compound type of foliar ray, if they become sufficiently slender, as in stems of herbaceous texture, give rise to a condition in which the storage parenchyma is entirely lateral to the leaf traces. The subject of the organization of rays in typical vines will be made clearer by diagrammatic representation. Fig. 273 illustrates the appearance of decorticated stems of Leea and Vitis in three Fic. 271.—a, tangential section showing leaf trace surrounded by storage paren- chyma; ), section of leaf trace and ray near the pith. Explanation in the text. dimensions. In a is seen a total view of the nodal region of Leea. The traces originate from the axis along a crescentic line and are shown in face view on the surface of the cylinder and in section on its cut end. Obviously the leaf strands are imbedded in foliar rays when viewed from either the superficial or the transverse aspect. In addition to the foliar rays, which in this case are both broad and shallow, there are other narrower rays, which are usually of greater depth. There are also uniseriate rays, diffused throughout the structure of the wood and presenting a rather marked contrast to the two sorts of broad rays. In 0 is shown a THE HERBACEOUS DICOTYLEDONS 395 magnified image of a part of the transverse aspect of the stem, making clearer the relations of the leaf trace to the large foliar ray. It is apparent that the ray is similar to that found in oaks in cooler climates and that it has a like relation to the leaf trace. In c is shown a diagram of Vitis, illustrating the relations of large rays and foliar traces. The cylinder in this instance shows only a single annual ring, and the rays subtending the leaf trace in transverse section are consequently less deep in the radial direction than those of Leea. Further, in the facial aspect of the cylinder the leaf rays are seen to be much elongated below and separated by a median process of wood into pairs of rays. This situation is strikingly unlike that in the shallow foliar rays of Leea. Still another con- Fic. 272.—Transverse section of part of a thin axis trast to the exotic of Vitis. Explanation in the text. genus is offered by the absence of uniseriate rays except in the actual leaf trace, an interesting exemplification of the persistence of primitive characters in foliar organs. A more highly magnified view (d) of a segment of the transverse aspect of the cylinder makes clear the presence of uniseriate rays in the leaf trace and their absence in the adjoining parts. We may now pass conveniently to the diagrammatic comparison of the topographical relations presented by thicker and thinner annual stems of Vitis. In Fig. 274a is shown a view of a thicker axis from the surface of attachment of a leaf at the median node. The upper part of the figure shows a transverse view of the stem 306 THE ANATOMY OF WOODY PLANTS just below the next superior node. In the latter the foliar traces, seven in number, are clearly subtended by a greater or less depth of storage parenchyma, precisely as is the case in the oak. In b the foliar trace is shown in its radial and tangential aspects. In the radial view the trace is confronted in its upper region by storage parenchyma (black), while below it is subtended by ordi- nary wood. Above the trace lies the storage tissue of the leaf gap. In the tangential figure the trace appears as a light spot in a mass ee (iM Ss ety I Si! | C d Fic. 273.—Diagram of decorticated stems of Leea and Vitis in three dimensions. Explanation in the text. Poo 0 ON O06 5 OF of darkly rendered storage parenchyma. ‘The latter, farther down, is divided into two by a median mass of unmodified wood. In ¢ is shown a view of a slender stem. In this instance, for variety, the opposite or tendril side of the stem is exposed to observation. On account of the shallow diameter of the woody cylinder the trace is of a radial dimension so great that it equals that of the cylinder from which it is derived. As a consequence there is no parenchyma facing the leaf trace, and storage tissue is entirely flanking in its distribution. This is a natural and necessary geometrical result of the thinning of the cylinder of wood in the more slender axes of the vine type. In d are shown the radial and tangential relations of the foliar traces and the adjacent storage THE HERBACEOUS DICOTYLEDONS 397 tissues. It is clear in the radial view that there is in thin axes no parenchyma subtending the leaf traces immediately below the node. This situation necessitates the tangential aspect shown below, where the leaf trace appears flanked by storage tissues on either side. Plainly, therefore, by reason of the slenderness of the woody cylinder and the great lengthening of the rays related to the leaf traces, which may be regarded as in some measure a a b C d Fic. 274.—Diagram of thicker and thinner axes of Vitis. Explanation in the LEXIE: compensation for their small radial dimension, axes of the vine type approximate very closely those found in herbs. The discussion of typical herbs may now be advantageously taken up; and it may here be remarked that, although necessary brevity makes it impossible to consider more than a few instances of the origin of the herbaceous stem, a wide investigation of the situation in many groups of herbaceous dicotyledons has made it clear that the same general conditions are present in every instance. Fig. 275 reproduces part of a transverse section through the upper slender region of the stem of the common stinging 308 THE ANATOMY OF WOODY PLANTS nettle, chosen on account of its chalazogamous affinities for com- parison with Casuarina, Betula, Quercus, etc. In the illustration a leaf trace with its flanking broad rays is shown, as well as the adjacent segments of the cylinder. No primitive rays are to be seen in the trace, which is composed of vessels and wood fibers. In order properly to interpret the slender axis of the nettle, the stouter and more woody regions of the stem should be examined. Fig. 276a repro- duces the appear- ance of a part of a section through the thick stem of the species under con- sideration, taken immediately below the: Snvodess duke trace appears as a highly vascularized nF radially directed ee . Piste: :@: mass on the mar- poe oy, gin of the pith. ; On either side of it are radial bands of parenchyma, which ¥ = Fic. 275.—Transverse section through part of a slen- der stem of the nettle. Explanation in the text. correspond to those shown lateral to the leaf traces in Fig. 275. In addition to flanking storage tissue the woody region of the stem of Urtica shows a very mas- sive band of radial storage tissue confronting the leaf trace, com- parable to the similar structures found in the case of the oak and Leea. The banded appearance of the broad foliar ray in this instance is due to the presence of alternating stripes of true parenchyma and substitute fibers. A region of the axis farther below the node may now be considered. Fig. 2765 shows a part of a transverse section of the stem some distance below the node. The mass of confronting storage tissue in the region of the node at the lower level has become transformed centrally THE HERBACEOUS DICOTYLEDONS 309 into typical wood, precisely as has been shown above to occur in the vine. A careless study of the facts and, above all, a neglect to examine the conditions present in the region of the node, might lead to the conclusion that the leaf trace in the more primitive and lower woody portion of the stem in Urtica is flanked but not confronted by storage parenchyma. Although the Urticaceae have been chosen to illustrate the herbaceous condition in a comparatively low order of dicotyledons, Fic. 276.—a, part of the thick stem of the nettle immediately below the node; b, section of the same some distance below the node. Explanation in the text. the Ranunculaceae, as represented by the woody and herbaceous species of Clematis or the more slender and thicker region of the same woody species, yield like results. A group in an approxi- mately intermediate position systematically is the Rosaceae. Herbaceous representatives when compared with woody forms of allied organization yield similar conclusions. For example, in Rubus we find well-marked compound rays, which both flank and subtend the foliar traces. In many herbaceous types of the genus Potentilla broad rays like those of the oak are found in the 400 THE ANATOMY OF WOODY PLANTS lower regions of the aérial axis, while in the upper parts the con- fronting parenchyma is eliminated from the cylinder as a result of its progressive reduction in thickness, precisely as in Vitis and Urtica. The Compositae, so generally conceded a very high systematic position among the dicotyledons, exemplify exactly the same principles as have been noted above. Fig. 277 represents a low region of a somewhat woody axis of Helianthus hirsutus. The leaves, opposite as in Urtica, have three traces each. The foliar strands corre- spond to depressed seg- ments of the stem a situation which, as has been noted in an earlier chapter, 1s commonly found in the vicinity of large storage rays and which results from the Fic. 277.—Thick stem of Helianthus hirsutus greater amount of vege- table substance present in such segments and a consequent retarded rate of growth as com- pared with the more woody regions of the cylinder. In H. tuberosus the fluting of the lower part of the stem in the region of the storage rays related to the leaves becomes extremely marked. As there are six leaf traces at a given node, it follows that there are six cor- responding furrows in the internode below. Further, since the traces of successive internodes alternate, the furrows of necessity show a similar alternation. The narrow bundles of greater diam- eter in the figure represent the foliar traces of the next higher node, and the masses of sclerenchyma subtending the median region of the phloem of the broadest bundles correspond to the now fused traces of a still higher node of the axis. Fig. 278 reproduces a high and herbaceous region of the aérial axis of H. hirsutus. The figure is equivalent in nodal relations to the fore- THE HERBACEOUS DICOTYLEDONS 401 going, but the topography is strikingly different. Here the foliar traces, instead of merely standing flush with the surface of the cylinder, as in the upper region of the more woody herbace- ous types, are actu- ally outstanding, or salient. As a conse- quence of this situa- tion the leaf traces no longer correspond to depressions of the stem, but actually underlie ridges on its surface. This condi- tion is, in fact, highly characteristic of ex- treme herbs, in which Fic. 278.—Slender upper region of the stem of the leaf trace has become the dominant factor in the organization Fic. 279.—Section showing the leaf trace in the herbaceous region of Helianthus. of the cylinder of the axis. This ana- tomical situation corresponds to a very high degree of assimilative effi- ciency on the part of foliar organs, result- ine ion ae lado amount of food storage or seed pro- duction, as the case may be. In: Fig. 27oas shown the trace of the herbaceous re- gion more highly magnified. The 402 THE ANATOMY OF WOODY PLANTS foliar strand projects beyond the surface of the cylinder and is merely flanked and not subtended by storage parenchyma, as in similar regions in other herbaceous stems of the most varied affinities. In contrast, in Fig. 280, which is from a lower and more woody node, a large amount of confronting storage tissue is seen, as well as that present on the flanks of the trace. The topographi- cal conditions in the stem of Helianthus, as representing a high and typical herbaceous condi- tion, may now advantageously be depicted in stereo- diagram. Fig. 2814 reproduces the lower portion of the stem of Helian- thus. The scar of the leaf of one node Of TS BGL ¢. << Pe. - af faces the observer, Fic. 280.—Section of trace in thick woody region of while the region Helianthus. 1 é wus just below the next higher node is shown in transverse section. The six traces of the two opposite leaves are clearly seen, and it can be readily observed that they are both flanked and faced by storage tissue (black). The very narrow deep bundles in the cross-section represent leaf traces of the next higher node, while the light masses on the periphery of the broad remaining strands indicate the position of the fused foliar traces of a still higher node. In 6 is shown (above) a radial and (below) a tangential view of the topographical relations of the leaf traces in these planes. In the upper figure of 6 there is obviously much storage tissue con- fronting the trace. In the lower item the trace in tangential section is seen entirely surrounded by storage tissue. Fig. 281¢ is a picture of the solid relations of a higher part of the stem in THE HERBACEOUS DICOTYLEDONS 403 the sunflower. In this region the foliar traces, instead of being depressed below the level of the woody cylinder, are outstanding, a condition very commonly found in extreme herbs, which have largely lost their woody texture. In the case of the vine the radial diameter of the trace in the slender region of the stem merely equals that of the cylinder, while in strongly herbaceous types the leaf trace is outstanding or salient. In the high part of the sunflower stem the trace is only flanked by storage tissue in contrast Fic. 281.—a, diagram of lower region of stem of Helianthus hirsutus; 6, radial and tangential view of the topographical relations of leaf traces in a; c, diagram of the upper region of the stem in the sunflower; d, topography of the trace in radial and tangential aspects. Full explanation in the text. to the both flanking and facing topography of the storage paren- chyma in the lower and more woody part of the axis. It will be noted that in the high portion of the axis the foliar traces cor- respond to elevations or ridges on the surface of the stem, while in the regions lower down they subtend longitudinal furrows. In Fig. 281d the topography of the foliar trace is represented in radial and tangential aspect. In the upper figure the absence of subtending parenchyma can be clearly discerned, while in the lower one the flanking disposition of the storage tissues is apparent. 404 THE ANATOMY OF WOODY PLANTS It will be advantageous at this stage to compare the woody region of the herbaceous stem of Helianthus with the axis of Ca- suarina. Fig. 282a represents diagrammatically a Casuarina with compound foliar rays. The best developed of the rays are di- rectly related to leaf traces, while the intervening less pronounced ones belong to the foliar strands of another node. In order that the vertical relations of the foliar bundles to storage rays may a Fic. 282.—Stems of Casuarina and Helianihus. Explanation in the text be seen, the bark of the stem is removed on the side facing the reader. The distant aspect still retains its bark as well as its leaf bases, which are represented as pyramidal elevations on the surface. In Fig. 282b is seen a corresponding diagram of the lower region of a stem in Helianthus. The topographical condi- tions are virtually the same, but for the fact that there are three leaf traces to each leaf in the sunflower, instead of a single one, as in Casuarina. In the oak the longitudinal depressions of the woody cylinder do not correspond to rays belonging to a single leaf trace, but THE HERBACEOUS DICOTYLEDONS 405 to pairs of these related to the foliar strands of diverse leaves at different nodes. This phenomenon is rather rare in the herbaceous type, but is occasionally found in the genera Aster and Solidago, among the Compositae. Fig. 283 represents an axis of this type in Aster multiflorus. There are five depressed segments correspond- ing to five pairs of foliar traces, to be seen in the woody cylinder. Fig. 284a is a diagram of the topography of the axis in the oak. The bark is represented as removed on the side toward the reader and as still present on the opposite side. To the right on the distant aspect of the stem is shown a leaf base. Into this run three traces. Since the median one passes out at a different level from the other two and exercises no impor- tant influence on the topography of the stem, it is represented bya dotted outline. It is to . be noted that the lateral Fic. 283.—Transverse section of the stem of a ree Aster multiflorus. traces take their origin from the foliar rays which are most remote from the median trace. On the left of the posterior aspect of the axis is shown by a dotted outline a leaf base of a succeeding node. ‘The traces of this leaf are plotted in by broken outlines, so as to indicate their relation to the foliar rays of the stem. It is clear from the illustration that the depressed segment lying uppermost in the diagram is flanked by two foliar rays which belong to the lateral traces of two successive leaves. The depressed segment of the woody cylinder in this instance owes its position to the retarding effect on growth of the two closely approximated foliar rays which bound it on either side. In the case of stems in which the large rays are equidistant there are no depressions, showing clearly that the depressed segment is the result of growth mechanics. This is 406 THE ANATOMY OF WOODY PLANTS clearly exemplified in certain species of Clematis. In the numerous species in which the large rays are approximated in pairs there are depressed segments in the stem; but in Clematis paniculata, in which the large compound rays are equidistant, the segments of the woody cylinder are all on a level and there are no depressed regions. It is not possible to follow this subject further in the present connection, but it is enough to point out that the facts ne 2 ite A 0 \" SINS FO nt, RE Ae ES a b Fic. 284.—Diagram of the topography of the cylinder in Quercus and Aster. Explanation in the text. entirely invalidate the interpretation of depressed segments ad- vanced by Sanio, Sachs, and De Bary and now classic in botanical textbooks. The view of these authors is that the depressed seg- ments, where they occur, owe their topography to a later forma- tion than the rest of the cylinder. This is distinctly not the case. The classic view just mentioned further involves the equally erroneous hypothesis that the continuous cylinder of woody forms has been derived from the discontinuous one of herbaceous types, a conclusion which, on the evidence furnished in the present and previous chapters, is exactly opposite to the true situation. In THE HERBACEOUS DICOTYLEDONS 407 Fig. 284) is shown a diagrammatic view of the stem in the genus Aster. Obviously exactly the same general conditions are found as in the axis of the oak. The result of all the evidence considered in the previous para- graphs of the present chapter is to show that the herbaceous type of stem is distinctly derived from the woody one in the dicotyledons. Its earlier expression is in the rather thick stem of herbaceous texture, in which the storage parenchyma especially related to the foliar traces both subtends and flanks the fibrovascular bundles of the leaf in that part of their course which lies within the cylinder of the stem. With subsequent thinning of the cylinder, clearly connected with greater efficiency in the production of seed and coupled with a more strictly annual duration, the subtending parenchyma is wiped out, and only the flanking storage tissues continue to exist. Obviously a very high potency in the produc- tion of seed, correlated with high assimilative power, ultimately makes for a type of annual stem in which storage is effected mainly in the seeds and no longer in the axis itself. Under these circum- stances we have the herbaceous type reaching its extreme sim- plification. The situation just pictured involves a final marked reduction in the organization of the fibrovascular strands which is expressed in its completest form in the bundle system of the axes of the monocotyledons. This group, however, will be con- sidered in the following chapter. The result of the appearance of the herbaceous type in the angiosperms has been momentous for the development of higher organisms. It is a fact of very obvious significance that the highest vertebrates and the highest seed plants have had a nearly contemporaneous existence. The warm-blooded mammal is in reality rendered possible by the appearance of the herbaceous type in the angiosperms, which directly or indirectly supply the most important part of the food of all the higher animals. It should further be emphasized in the present connection that the dicotyledonous herbs are very different indeed in their mode of origin from those exemplified by lower types and in particular by the vascular cryptogams. Here the herbaceous condition is the result of mere degeneracy in the tissues of the xylem. In 408 THE ANATOMY OF WOODY PLANTS the herbaceous dicotyledons, on the contrary, we find the origin of herbaceous texture closely associated with special modifications in the organization of the secondary cylinder, and this involves a high degree of specialization on the part of the plants in which it is manifested. The local transformation of the tissues of the woody cylinder, in relation to improved storage in proximity to the leaf trace, had its early expression in the phenomenon of aggregation of rays in proximity to this in its course through the woody cylinder. The phenomenon of aggregation is succeeded in turn by that of compounding, the direct consequence of the facility with which the longitudinal elements of the xylem become transformed into storage elements in the case of the dicotyledons. The final result achieved in the compound ray is the wedding of longitudinal and radial parenchyma in the complex, which becomes of such marked significance in the herbaceous dicotyledons. CHAPTER XXTX THE MONOCOTYLEDONS This group of plants, although only about one-fifth as numer- ous as the dicotyledons, is nevertheless of great importance on account of its significance in supplying extremely valuable food plants and also by reason of its remarkable anatomical organiza- tion, which has been the cause of much speculation and dispute. In this large group of the angiosperms we have exemplified a practically complete absence of secondary growth coupled with a complicated arrangement of the numerous though slender fibrovascular strands. The absence of secondary growth has led to the association of the monocotyledonous angiosperms with the ferns and their allies. This view of their affinities has been reinforced at various times by the discovery of leaves and even inflorescences in Paleozoic strata which have been referred to monocotyledonous affinities. The foliar and reproductive parts from Paleozoic deposits have, however, in more recent times been clearly recognized as the parts either of cryptogamous or of gymnospermous types not related even remotely to the angio- sperms. There is accordingly no reason based either on the possession of cryptogamic characters or on very ancient occurrence as fossils which justifies the view that the monocotyledons are the more primitive group of the angiosperms. The evidence, in fact, when considered in the light of the general principles of comparative anatomy, points in quite the opposite direction and seems to indicate that the group under consideration is derived from herbaceous representatives of the dicotyledons. A characteristic feature of organization of the axis in the monocotyledons is the scattered distribution of the fibrovascular bundles. These, instead of being arranged in the circular fashion which usually distinguishes the structure of the herbaceous stem in the dicotyledons, are disposed through the transverse section of the organ. An examination of the seedlings and reproductive 409 410 THE ANATOMY OF WOODY PLANTS axes in the group supplies convincing evidence that the peculiar arrangement of the fibrovascular bundles in the monocotyledons is not a primitive one. The original manner of distribution of the conducting strands of the stem was in all probability that found in the dicotyledons, characterized by a prevailing circular arrangement of the bundles. The root in monocotyledons has the usual radial organization, and is distinguished from that of the mass of dicotyledons by the absence of secondary growth. Another feature which is often present in monocotyledonous roots is the origin of lateral roots, not opposite the groups of protoxylem, as is the general situation in the roots of the remaining vascular plants, but in the interval between two protoxylem clusters. This peculiarity has gained for such roots the not very appropriate designation of ‘‘double roots.” Another feature which has been described in the roots of the group under consideration is found in the abnormal order of development of the elements of the xylem. In vascular plants in general the protoxylem occupying the outside of the xylem star of the root is differentiated first and the successively more central elements in later order. In a number of monocotyledonous roots a remarkable exception to this well-nigh universal seriation of development has been observed, for the more central elements belonging to the metaxylem are differentiated first and the tra- cheids of the protoxylem are the last to manifest the sculptural features of maturity. The leaf in the monocotyledons is cracasterOed in general by the closed disposition of the nerves or fibrovascular strands. These usually come together at the tip of the foliar organ and sometimes in this region are in relation to rifts or pores in the epidermis, which allow fluid water to escape in the form of drops of dew. ‘In certain tropical plants with large leaves—such, for example, as the Agave—the loss of water during the night through the rifts in the tips of the leaves where the foliar bundles converge is so great that a constant dripping is heard, often so pronounced as to disturb slumber. As a consequence of the closed disposition of the fibrovascular bundles in monocotyledonous leaves, only the longitudinal veins are, as a rule, well developed, and the THE MONOCOTYLEDONS 411 lateral ones are weak and degenerate. The fibrovascular bundles of the leaf in monocotyledons are ordinarily very numerous and _ consequently enter the stem in large numbers at the nodes. The large number of foliar bundles passing from the base of the mono- cotyledonous leaf into the stem is correlated with a high degree of assimilative efficiency which finds expression in a proportion of seed production which has scarcely ever been reached in her- baceous dicotyledons. In many of the cereals, for example, the relative weight of the seed to that of the whole plant very frequently reaches over 30 per cent. The high efficiency of the group, both from the standpoint of production of assimilates and from that of the formation of seeds, naturally puts it in a unique position in supplying important food plants. In many cases, particularly in the grasses and sedges, cam- bial activity, absent in the stem Fic. 285.—Transverse section of a 5 : bundle of Avena barbata, showing cambial and root, is often retained in actinty iter Chaalen! the basal or sheath region of the leaf or sometimes in relation to the node in the stem. ‘The capacity which grasses manifest for erecting their stems after “lodging” is to some extent the result of the presence of a persistent cambium in the nodal region, either in the base of the leaf or in relation ‘to the stem itself. Fig. 285 illustrates such cambial activity in the case of Avena barbata. It is permissible to view this cambial activity as a persistence of an ancestral character, particularly as it is often found to be present in monocotyledonous seedlings in the lower region of the epicotyl or primitive stem. The organization of the closed fibrovascular bundles of the monocotyledons is in many cases collateral and, as the descriptive term implies, exhibits no indication of cambial activity. The collateral type of fibrovascular strand is characteristic of the leaf, since that organ, here as elsewhere, is conservative in its structure. 412 THE ANATOMY OF WOODY PLANTS In the stem, however, particularly in the subterranean axis, the collateral type gives place to a concentric condition in which phloem is completely surrounded by xylem. This modification is known as amphivasal, to distinguish it from the amphicribral concentric strands of the Filicales and certain lower gymnosperms. The concentric strands of the monocotyledons present themselves in a very interesting fashion in the grasses and sedges. Here, in the reproductive axes, amphivasal bundles are very numerous in the nodal regions, where the entering of many foliar traces produces a marked degree of crowding and disturbance. The amphivasal bundle, in fact, seems to have originated as a con- sequence of the multiplication of foliar traces in the nodal regions of monocotyledonous stems. This hypothesis of the ori- gin of the amphivasal strand is justified by a consideration of parallel conditions exemplified in the organization of the axis in certain dicotyledons. In many instances where the foliar traces are numerous in the nodal region of herbaceous dicotyledons, these become amphivasal in their structure. This organization, for example, is frequently seen in the Araliaceae and Umbelliferae. In the annual stems of the mass of monocotyledons, whether leafy or scapose, amphivasal bundles are ordinarily absent. When the anatomical structure of the perennial subterranean axis which is often found in the monocotyledons is examined, it very generally presents amphivasal bundles in great abundance and not by any means confined to the nodal regions, even when—as less rarely happens—the nodes are not closely approximated. The common occurrence of amphivasal strands in the rhizomes of monocoty- ledonous stems is no doubt primarily related to the crowded and tufted character of the leaves which results in the strong approxi- mation of the nodes with the consequent multiplication of amphi- vasal strands. It is highly probable that the glumaceous representatives of the monocotyledons represent somewhat primitive conditions in the stock, for here both reproductive and anatomical data seem to harmonize in indicating a low systematic position for both grasses and sedges. It is, moreover, probable that the Juncaceae, which in anatomical organization agree very closely with the THE MONOCOTYLEDONS 413 glumaceous monocotyledons, are nearly related to these forms. A striking contrast is presented in the anatomy of the true palms and the Scitamineae. In these groups amphivasal strands seem to be entirely lacking. In the Principes, or true palms, we find a marked difference in anatomical structure from the western tropical Cyclanthaceae, which have on floral grounds often been considered to form a systematic link between the palmlike mono- cotyledons and the aroids. The anatomical structure of Carlu- dovica and allied Cyclanthaceae is rather that of the aroids than of the true palms, since amphivasal strands are conspicuously present. Our knowledge of the development and comparative anatomy of the groups which appear to lack amphivasal bundles is still too meager to warrant any hypothetical conclusions as to the phylogenetic significance of the apparent lack of amphivasal fibrovascular strands in the conspicuously large-leaved forms, which are united systematically under the headings of Principes and Scitamineae. It may well be that the two large groups above indicated, by the anatomical peculiarities revealed as a result of an examination which is as yet only preliminary, occupy a position high among the monocotyledonous orders. It will be convenient to elucidate in a general way by means of diagrams the main anatomical conditions presented by the monocotyledons. Fig. 286a illustrates the distribution of amphi- vasal regions in the stem of a sedge. In the reproductive axis the amphivasal segments are remote and are clearly in the nodal regions. In proximity to the substratum the nodes become more approximated, and in the subterranean axis they are frequently so closely disposed that amphivasal organization is often contin- uous. This condition is well illustrated by the sedges and rushes and less distinctly by the grasses, since the last have well-spaced nodes. The next diagram (b) shows the situation commonest among the monocotyledons. In this type of anatomical organ- izations the amphivasal structures are found exclusively in the perennial subterranean axis and do not appear in the annual stem. In the last type (c), which portrays the conditions apparently characteristic of the true palms and the Scitamineae: (bananas, cannas, ginger, etc.), amphivasal regions are absent both in the THE ANATOMY OF WOODY PLANTS 414 subterranean and in the aérial stem. Only continued investiga- 1 situation 1ca ficance of the anatomi igni ll show the real s exemplified in these cohorts or orders. ion wi t 286.—Diagrams to illustrate the distribution of amphivasal bundles in the Fic. monocotyledons. The general anatomical configuration of the monocotyledons the pre sent condition of our knowledge warrants the conclusion is impor mM tant class or division of the angiosperms formerly that th possessed bundles arranged in a circular fashion and characterized by secondary growth. This condition is indicated by the study of conservative organs and regions and seems to justify the inference THE MONOCOTYLEDONS 415 that the monocotyledonous angiosperms have been derived from a dicotyledonous ancestry. The justice of this hypothesis, how- ever, will be finally established only when we shall have at our disposal for anatomical investigation remains of monocotyledons from Mesozoic deposits. Whether or not it is ultimately estab- lished that the large group at present under discussion has actually been derived from the dicotyledons, it will doubtless in any case be clear that they cannot in any way be regarded as primitive representatives of the angiosperms. The monocotyledons in fact represent the herbaceous type in its extremest form. In the group the fibrovascular tissues are released from the rigid confinement of the tubular stele in the ancestral forms with sec- ondary growth by the development of large parenchymatous storage devices in relation to the foliar traces. Correlated with this release is the possibility of accommodation of the numerous foliar strands which characterize the basal regions of monocotyledo- nous leaves throughout the transverse section of the stem. There is doubtless some correlation also between the extreme multipli- cation and consequent displacement of the strands in the stem of monocotyledons and the disappearance of secondary growth. Possibly an aquatic or amphibious habitat long maintained may likewise have acted as a contributory cause in bringing about the obliteration of cambial activity, since in the dicotyledonous Nymphaceae, in which there is diffuse distribution of the bundles and also the absence of cambial activity, we find these features correlated with an aquatic habitat. It has, indeed, often been suggested that the Nymphaceae or Ranunculaceae are the dicoty- ledonous ancestors of the monocotyledons. The interesting inves- tigations of Sargent on the fusion of the cotyledonary structures in Ranunculus ficaria, etc., are of importance in indicating how monocotyledony may have arisen as a result of the union of two originally separate seed leaves. Another possibility, of course, is the origin of the monocotyledonous embryo as a consequence of the abortion of one of the two original cotyledons, and this view is perhaps supported by the conditions found in certain grasses, such as Zizania, Avena, etc., in which the vestige of a second cotyledon is considered to be present. The problem of the origin 416 THE ANATOMY OF WOODY PLANTS of the monocotyledons cannot yet be regarded as by any means settled, and a much fuller knowledge of the anatomy of extinct and living representatives of this extremely important group is necessary before any final results can be reached. If we attempt to picture to ourselves the probable future course of evolution in the angiosperms, it is difficult to concede to the monocotyledons a prominent position. This group seems to have reached such an extreme degree of specialization that it will probably in the long run entirely disappear and be replaced by new derivatives of the still plastic dicotyledons. CHAPTER XXX ANATOMICAL STRUCTURE AND CLIMATIC EVOLUTION — General views in regard to the ancient climatic conditions must first occupy attention in the present connection. It is commonly conceded, on the basis both of the nature of ancient organisms and of the evidence supplied by geologic strata, that the earth was formerly much warmer than it is in the present epoch. It is further clear that, other things being equal, the greatest degree of warmth existed in the most remote past. This general situation, however, does not exclude the recurrence at long intervals of periods of refrigeration or glaciation. An age of ice is known to have occurred, not only at the end of the Cenozoic as originally established by Agassiz, but glacial periods also termi- nated both the Mesozoic and the Paleozoic as ordinarily defined. Evidence of still earlier glacial epochs which exercised a devastating influence on the most ancient animal and plant populations of our earth is not lacking. Evidence in regard to glaciation in former epochs is both direct and indirect. Direct testimony concerning former ages of ice is supplied by the comparative study of deposits formed in con- nection with the existing glaciers of high latitudes or of high altitudes. Intimately connected with glacial phenomena are the formations of clays, till, and coarse morainal matter resulting from the movement and melting of ice. Indications of the kinds just enumerated in earlier geological strata supply direct testimony as to former glacial action. Indirect information in the same direction is often furnished by the wholesale extinction of impor- tant groups of plants and animals. For example, in the Permian glaciation which marked the close of the Paleozoic the treelike cryptogams, which have contributed so largely to the formation of the older deposits of combustible minerals, disappeared entirely as an important constituent of the plant population of our earth. Glacial epochs are, however, not of direct importance in relation 417 418 THE ANATOMY OF WOODY PLANTS to the evolution of plants in response to climatic influences, since their action is mainly negative. It is true, however, that by bringing about the obliteration of important groups of plants or animals greater opportunity is supplied for the surviving and more adaptable forms to develop in the following warmer epochs. It is the more gradual and not the spasmodic refrigeration which has produced perhaps the greatest effect on the organization of the successive plant populations of the earth. As a preliminary to the discussion of the anatomical modifications which are more or less definitely correlated with climatic changes in the successive geological ages, the evidence furnished by plants in regard to progressive climatic cooling must be considered. This evidence is of two kinds. Perhaps the most important and trustworthy is derived from the organization of the secondary woods in trees of the various geological periods. This testimony can hardly be estimated too highly in arriving at any conclusions in regard to plants as reliable indicators of climatic change. Another kind of evidence is afforded by the character of the plants them- selves. At the present time there are large groups of plants which are of more or less definite tropical occurrence and others which prevail characteristically in cooler regions. The advance of tropical types toward the poles or the progress of polar plants in the direction of the equator in earlier geological eras must, other things being equal, indicate variations in climatic conditions in the direction either of greater or of less warmth, as the case may be. Unfortunately, in earlier geologic times the differen- tiation between polar and equatorial types was not nearly so marked as it is at present, and this general situation militates more or less strongly against reliable conclusions in regard to climate in all but the latest geological eras. Since the present work deals with anatomy, the subject of plant geography in rela- tion to the climatic changes which have marked the successive ages of the earth is obviously of less importance, aside from the limitations indicated above. As has been already shown, the organization of the secondary wood in extinct plants furnishes the most reliable evidence as to the climatic conditions which prevailed in earlier geological ise present in kewi hi 1S t 1 but The information derived from this source is not only ANATOMICAL STRUCTURE AND CLIMATIC EVOLUTION 419 on the whole the most trustworthy, epochs. eoue eeree oe we * rei 227d ROK enerey & Ly m e AN) LEAS) Bade O80see Cope ee ee au Aveciaccens ‘ere SVC aveene’ Veale ceedamnaes: a Sees Jéeee bus name ve SESS ay igo Or ay a ti aia. (sla sof SS Preah Similan SSG oy, ea eS) o) q a oan (0 seed a fs ee o n N =>} cS 3 tol 8) iS) m oN q ie) Ceieree AOn re ree Lo o oO bp O Lal Ss oo aH = dt (oF 11) | n fae) Cc oO 5 wn aw ale eG eas SRR Bee seas 2 DH EG) fas} = OQ, or) of which indicate any perio- dicity in annual con- Pet erty eer ee ee. rei enere f the wood of Cor- Sant seeette woeteos modifications StELUIC TUNE tS) ditions of growth. The truth of this statement is well illustrated by the ac- 10n oO G. 287.—Transverse sect FT ites from Prince Edward Island. the no da organization of the eran! i toma Southern re d by the ica of a oO o formity eolo unl trunks which are supplie wood shows great tions Cra mned ala there o 5 Mes ar colina ace a = my OS to S i ee ie 72 AS Cm = ao) aosks aera’ eee Sr one ; Lael fs) ee 8 SE) So Se Oa O ele ma Ea ™ si I o S OS SG © ea O 6 SS Bie, ea eae ee er = Ce aen a Go Ge eg cons g Or ors ao ae) Gu © aS OS Fic. 288.—Transverse section of the wood of Cor- daites from the north of England. 420 THE ANATOMY OF WOODY PLANTS of periodic growth is, however, frequently found in regions of higher latitude than that portrayed in Fig. 288. The next illustration shows the organization of a Carboniferous cordaitean wood (Mesoxy- Jon) from the northern part of England and consequently of consider- = = IL. 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