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The following diagrams illustrate the method; Les cartes, planches, tableaux, etc , peuvent etre film^s i des taux de reduction diff6rents. lorsque le document est trop grand pour etre reproduit en un seul cliche, il est film6 ^ partir de Tangle sup6rieur gauche, de gauche ci droite, et de haut en bas, en prenant le nombre d'images necessaire. Les diagrammes suivants illustrent la m^thode. 1 2 3 32X i 2 3 4 5 6 11 ..( QKll McGILL UNIVERSITY PAPERS FROM THE DEPARTMENT or Botany. iDon N mnn < \'-'i l.'^'nr.ff.- No. 5. — Myelopteris Topekensis, n.sp. >- > BY D.Pr^'PENHALLOVV. With Plates II. and III. [Reprinted from the Botanical Gazette, January, 1897, pp. 15-31] Montreal, 1897. MVKI.OITKKIS TOI'KKKNSIS, N. SI'. A M'W CAKIIOSII'ICKOUS I'r.ANT. I>. I'. I'K N II A I.I.OW, (wrni I'l.ATKS II AM) III) I)uKiN,'en. de vdg. foss. Diet. Univ. d' Hist. nal. * Goeppert : Die foss. Fil. der perm. Form. 5 Renault : Ktude du gen. de^.Myelopteris. Acad, dc Paris aa : — 1875. | no. 10. | * 1 am much indel)ted to Dr. H. J. Harrington for detenninations of tlie mineral constituents of these fossils. 1897] IS t I :CTg ?i S -S3 %i't'-^<'''^»HMtWJiswtfiW«i^,.u ' HW! ' ,' ' If Hot.lMi.U u.i/l III. I I^MAKV iImI <>| Iikiwii I u.iI. Tlir siirl.M r sliows ik ( iisiuii.il iir< ,i«i u| lliiii ( n,il\' ni;i»l«r iniK li hrnkiii u|» iiiti» Miiall angular Iragiiitiils, Itiit It IS iliiillv « li.iiailfri/»'il by » HnnH-whal fiiuly sliialti! a|i|ifaraiUf iliu' Ik ri'imtval hI iIk ...iliral lavi-r, with n»iis(t|ii( nt ixpnsiiif III iln- iiiKlfilyiiij^ >liafi'l-i u| M'lfrt'iichvriia. I'lu' tLiiisvi-rsi- scttinii III thi' iiiiir«' |»rrfcrllv |irfs(rv»il H|H'cmKii sliii\v> an iiiilir /niic i ,5""" tliii k. uliii li is (iiminiiniis (111 ,ill sidfs. Ci'nlial tn this ami thus Imiiiiii^' tin- axis of tin- original siriutiiii'. is .1 ili^tiii« tly ilaiktr ami smmwli.it im,ir l>c>ii»iis mass, r«»iilaiiiiii^. luii- aiiii tlinc. small irr(rj,Milarlv roiimlfd massis nl |iyrilf. l)'|i wnr luiiml tn lir din' tu wi'll lirfiiH'tl (lirffri'iicrs ol striu tiiri-. I 111' mil riisn)|iiial lUtails pifsctit iii.iiu li .ituics of iiiti rest ami, allliiuij;li the m-iifral i-ffi-cts of die av ami ( oinprissioii liavc iiiiii to complctfly (U-slioy tlu'^tiirral nlalioiis of |iiiits, ami in many I'ascs, also, to (U-stroy stnutiiral ditails, tlusr last imvc hccn preserved, in some instaiui's, in a n-markahly ptrfii t manm-r. Tin; ii;NrKAi axis. 1 In- intiif ci-iitral portion of the stiiii presents a romplete absence of strmtiiial ditail. 'llie whole central area is occupied i)y a mass of dark colored male-ial so disposeil as to indicate its prol)al)le derivation from thin walled tissue, but much altered by tiecay and tlii' sul)se(|uent effects of extreme compression. Here and there, dark colored masses appear, possibly the residue of the mucilajfe ori^Miiallv present. Thiouirhout this rej,non lari^^e rounded o|)eninjfs a|)pear. and while some of these undoubtedly represent the displacement of pyrite, many, and probably all, represent the former locations of vascular bundles, in the dark color and structural character of this area, we find amjile reason for its evident separation from the cortical /.one, as ascertained upon microsco])ical examination. Outwardly, this area is limited by a somewhat well defined but narrow and irregular darker line, which is obviously composed of much compressed thin walled cells, but which, nevertheless, seems to sug)j[est a somewhat definite boundarv line between a (lAM'MiV • »»'»7 I .Ul/./iU-// fi/.\ /(>/•/ A/. X,\/S n tii'ral tutor il an, IS of Irii^'itit'iils, ly sliialiil I MIlM l|lll lit |iri'sfrv<'i| ( lilltilllMMIS ixin (»f the Mliat iimrr irrt;>j[iilarly "roscopical he due t(i of iiiti rest Nsion have rts, ami in liavi' Iji'i'ii ii;iiiiii-r. I till' Slllll riif wliolf iiatr "ial so hill walli'il •nt rlfccts t(I masses y idcsciit. pear, ami iccmeiU of icitioiis of laracttr of ition from ;uiiinatioti. ll'fllK'tl l)llt composed I'crthclfss, between a central tiicilnlla in wliiih thin vvalli-il (iitiilatiKtilal tisrt'> \ more or Ichh liroki ii iIovvii slramlH of HcU'rciuliyina lelK, with surroiiiiilin)^' parcm liynia tissue, making; it i tear that a certain ,iiiioiiiit of struiture has tieeii ri iiio^ed ; ami thisairords witti wImI has .ilreadv lieiii noted in spii itiieiis of Myelopteris, that "tin- tissue layers outside the sclcreni hyma strands are very rait l\ prcservftl."' In tins ease the thin surface layers of coal .ilitMfiv ilest rilu'il are in .dl proliahilits to lie re^'anled as rt presenliiiL,' theitirtiial struiture, wlinh must li.ive lit in < hit fly or vvholK parent In iii.'itous in eharat-ter, ami of small radi.d vtilmne. I'm si 1. I o|< I |( \| I \\ I K. The outer, lontllMloUs /one. i.n""" thick as alreailv iltsi riheil, li.is iis maertist uph ilitlen nti,ition from the meilull.i explaim «l l»y the Iar|,(e ;inil.:iul)acli: r(i>>. H'.t. lOJ. i li HOiMXn.il I, iiiU'ri'i'lliil.ii sjMCCH onliiLirity mu*I \«illi in Hiich tiNNtit* tiru |ircNi'iil, Intt llit-u' It ID) t-viilciiti' III lilt- I'siHti-nt'f of l.u iiii.i- St i i him iuma. It l);iH Ih-cii hIiomii .ilitMilv that tln' siilf curtu.tl /t)iu' \% !.«;""" tlurk. Willuu Ihi-^ region tlu-n- arc iniiiii-roiiHuval or liiii^t'iiti.illy I'loii^atctl iHinilk'M i>f NtU'rciii'liyiiia, wliii'l) U»\\\ lon^: ttriiiitlH travi*r>tiii^; tlic stem luii^itiiilinallv lor ^'n-at ilKtaiui's <.//c>' /. •/. inul ./). I'Iuhi' straiuK, wlmli \ii\i' till* |ii-( (iliarly slriati-d a|i|ii-arai)('f to tlu' Mirlaci- ol tin- >t|ic( iiiuii wlti-rt'vrr cx|to>*rtl, .ir»' alwav* si'|»ar.itccl Iroiii oiU' aiiulhi i hv Hcvcral lai^f ,iiitl tiiiii \vallc«l |»iirciitliyma «i'lls {fi}^. i) uliirli iiri' Hccn to In- vory |tfrlicctly pnv^crvwil in ctrtain ari-as. ||ju Mi'lcrfniliviiiatoiis clciiu'iits arc always vfr\ tliick wallril in those strands uhiih lii' mxl the mrtix ( //^,^ >' ). t'»it luruini' nimh tliiiiiit'i w.illi'd toward tlu- (inter ol llu-siini wlure thes ollcn appear to III- in a forniative eoiidition. The strands an* Hcparatcd radially by rather wide areas ol (iindaniental tissue (//»|H'i iiiifii Itillirr l)V /I uliitli CJIH, I III li ill tlioNC illir lllticll lu'\ ullcn Ht'paiati'il (C- ■'I . 'it'l II relative (K-tiTinitu* m| tlu'Hi' liratc that fllU'il ruii- l>y I heir I limit III Is appears ■re(|iicntly uoveil l)y are then V riiundcd ,^hniit the nternal to |)reservtHl stnictiiral St ul the ), is I'oiiiul li 1)11 two • ■•»7 1 .U r A A r»/7/ A7.S / 1 »/'A A A \.S/M »'» Hlili'H l>y tttws )ii lliick walleii I'lhruiiH elritHMIts, The phlucrii, rtither Hiiiall tii vuliinie, in hen.* iiituh hrnki ii ilowii. hut it it •titiiiiteii riiiiiiilly outwanl, while in the other hiittille { Jijf. th where it in rather mure perleetly prcHervcil, it •« situated radially iiuv.iri!. The prntuxvli Ml in luri' sicn as n iiTnu\> of siiialU r elt iiienis iiiiuli altered l»y n»iiipre""i. //f. / / /i, •.\nn. lint. 7: />.'. / .111.1 //, /ii't. /. V. /y. /.'(»// \/l.l/ ( :.!//■ Ill: ( I A M \ K V ilUllMSi- ill IIIIHlhlT illUMld tin- 1 I'lltlT .111(1 1)C( lilllr llll>->t iiuiiu'r- oiis uilliin tlu' ci'iitiii' rii^JDii. Si cKi.TiiKv oK.iAN.-.. A ii()t,il)U- fi-at'irr ^li llu" prcsfiil fossil is tlir orciirronci- of mmuTous largi. iiiiicila^f passa^fs. As a nik' tln'SL- stniiluifs ait' imuli altiTiM hv ili-iay ami c-nmpiis- sioii, hilt ill two instances tlu'V wire foiiiul in a vi^y piTfi'Ct state ol preservation ( //;,'-. J\. So far as it is at pii'scii possible to deteriniiK', these organs occur tlirounliuut the siih-cortical region where thev are in nion- or less intimate association with the sclerencliyni.\ stran('s. i-Jsewhere it is not possible 1o determine the (listrihiition satisfactorily, l)nt, fiom our kii iwledi^c ol their occurrence in recent |re commonly somewhat elongated tangential Iv to the central canal, and by analogy with similar structures in recent plar.ts we may infer that they contained active proto])lasm. Thev thus forn: the secretory cells, or an epithelium which is not .-.pecially differentiated ^fig. _^). A comparison of the two canals {fig. 2) will serve to show, how- ever, that the secretory cells often show little or ikj dexiation from llie general character of tlie fundamental structure. ( I \ M \ H V st IIUIIUT- HMit fossil t"-. As ;i cumprcs- \- [HTli'Ct iussil)|i' to cal rr'^ioii I witli tlu' (Iftfiiniru' (• ol tlicir tlicv must idaiiu'iilal icrc in a wed tlitin D5X i3;/x; IcdiKc an it a|)|)(.-ais 1, in whicli The \rrv groups ol l.iCLM' and ;itudinallv stem for art^c el lip • ed of par- )f the sur- eloiigatcd itli similar contain. -d A\s, or an :^- /)■ A how, how- dexiation structure. iK>7| MVi.i.ori hRis hiI'I-.k i:\sis 31 Another important feat'ire of tliese laiials is t«. Ix- found in the fact that tliev are always devoid of contents. llii-. ap|)ears to justily tlie view tliat wliatever they may liave contained origi- nallv was of a soiul)ie nature and thus |)assed out ol the ixuly of tin- plant during the process of petrilactioii. In all tlieir principal structural aspects these canals hear a stronj,' reseml)lance to those of Ani^iof^fcris ivcctii (they are of the same tyi)e), and it mav al^o l)e |)ointed out that they are similar to tliose fourd in Riuliiophris / 1 '////le to refer them to the residue ol resin masses which the plant oriifinally contained, and they are, therefr)re, directlv c(jmparaljle with the similar resin bodiis fouiul in recent plants, particularly those of Ani^iopkns tVCiUi. It is tiui^- fairlv certain tiiat in the Topeka plant there were orii(inally at least two. and possibly niore, kinds of secretory origans, tiie one holding mucilage, the other resinous matter, and in these resjiects our plant is once more comparable with certain recent forms. The general view of tiie internal structure thus obtained permits us to gain some conception of the real composition of this stem or stipe, from which we may infer that a restoration would show a cortical layer of parenchyma at least several layers of cells thick, containing numerous mucilage passages. P'ollow- ing this is a sub-cortical zone distinguished by the presence of nuiiicrous rather widclv separatetl strands of sclcrenchyma, the elements of which are very thick walled toward the cortex, but ■'.\nn. Hot. 8: />/. .V///./(V.f. 'i' // t.'"- " .\nn. Uui. 7; //. I, figs. 1,1). -r*jSJ^^^^|J(^||flffff^^BnW^?J^''"' HO/AXJCl/. UA/./.J //: I.IANIARY Cdiuimially tliiiitu"' walled toward the mciliilla. Tlicsc strands iisuall)' liavf an accompunvin^ iiuicilajfc passaj^c on the oiiter lace, inul are inconstant {':) process of formation tow.ird tlie center. Within this zone, vascular bundles, distinf^uislied by tiieir broad scalariform vessels, appear, anil increase in number toward the central re^non. The central axis consists of a rather broad tract of parenchyma tissue, throuj^h which tlie vascular bu.ndles are distributed in larj, numbers. l*rom this point of view, and with ilue allowance for the effects of compression, it is possible to trace a strikinj^ similarity in several respects to a species of Myeloxvlon describeil by Solms-Laubach," and i lore |)articularly in certain respects to specimens of Myelopte is described bv Williamson.'^ The evi- dence is both clear and direct that this plant must be considered as belontrinn' to that peculiar trroup for which the name Myelo|)teris, pro])osed by Renault, has been most jrcnerally emploved. In 1S32, Cotta ilescribed certain fossils from the Carbonifer- ous of Kuro|)e under the name of Medullosa, which has more recently become mer^red in that of Myelopteris. Williamson, however, informs us that Cotta's figures of M. clegans are wholly misleading, the structure being represented in a much exagger- ated form, while his two .>^pecies, J/, stiilata and .]/. porosa, remain too obscure to be depended upon without further evi- dence than has come down to us.'^ The genus Medullosa, nevertheless, constitutes the basis of that group of i)lants which, ])assing under several names, ha;; finallv come to be known under that of Mvelopteris. In 1845, Corda assigned to his genus Falmacites two plants from the Coal Measures of Bohemia, under the names of P. ntrboiiigciiiis ami P. Icptoxylon.^^ An examination of Corda's figures shows that there is no very great resemblance, although "Fos.s. Hdt. l6i, fiji. 14A. ■'Fossi, plants of tlic Coal Measures. I'hil. Trans. 166: fin!. /,.?, 4. '■•Koss. plants of the Coal Measures. I'hil. Trans. 166'. 'SFIora tier Vcjrweit 4c, 41. //. /9, .?(). 1845, I.IAMARY c Strands the outer •ward the lislicd bv II iuinil)cr if a rather ■ vascular L' for the simihirity :ribecl l)y rspects to The evi- onsitlcred he name j^cne rally irbonifer- lias more illiamson, re wholly exagger- '/. poros(7, rther cvi- IcduUosa, )f plants be known \\o ])lants lies of P. ■ Corda's although lSi>7 M) / lor/ / h/S /<)/7A/:XS/S M there is a suggestion of similarity to our plant in the general eiiaracter of the fundamental tissue, and tiie presence of numer- ous mucilage passages. These latter, however, are small and a|)|iarentlv altogether separated from the vascular bundle.s. Subsecpient observers have not been unmimlful of certain structural aspects in these plants, which ha\e seemed to suggest their possii)le relationship to the palms, and more particularly to that tvpe of structure represented in the genus IJrac;ena, but much doubt has always been entertaineil as to the possibility of mono- cotyledons occurring so far back as the Carboniferous. These doubts w-ere first ijromiuently expressed by lirongniart as the result of comparing with the plants figuied by Cotta and Corda, new material obtained from Autun, France."' He says "il y ait des differences fort essentielles et (|ue rendent tres difficile d'etablir des rapports entre ces fossiles et les vegetaux vivants." He therefore preferred to regard Cotta's Midullo.ui i/t\!^'-a//s as the representative of a new genus, for which he proposed the name Mveloxylon. which thus seemed to indicate the leading structural features indicated by the former name, the signifi- cance of which was thereby jjcrpetuated. Fifteen years later, Goeppert, in reviewing Cotta's species, regartled Midiil/osa cligtiiis as possessing characters which were variously represented in the gymnosperms, in i)alms, and in the ferns. As a generalized type, he applied to it the name of .Stenzelia. In 1873, Williamson first drew attention to the belief that the relations of these fossils had not been correctly interjireted, and expressed the view that tiiey were really ferns allied to the Marattiace;e.'' In 1874. Renault reviewed the fossils obtained from the Carboniferous beds at Autun, as a result of which he supports the conclusions reached by Williamson, and while he regards the name proposed by Corda to be wholly untenable, and those of Cotta and Goeppert to be insufificiently indicative, he views that "'Tab. des gen. ile Veg. l-'oss. Oo. 1849. (Quoted from Williamxm.) "Hril. A.-is. .\ ^^ '^'^" i''*-' ^■'-"'■y thin walled elements of the funda- mental structure, all |)resent features almost identical with those observed in the Topeka specimens {Jigs. /, ^, .?). Williamson's specimens appear to differ from mv own chiefly with respect to the particular distribution of the sclerenchvma strands in the cortical region, a difference which, however, is ■' Reclierclies .sur les veKctaiix silicitics d'.Viitun. ( l-'rom Willjumxtn.) " Fos.sil plants of the Coal .Measures. I'liil. Trans. i66'. I i\\i;akv II as more ncl/" ifc late, (Idiiiu'" einc temps L' iKim triuture, preferring- ratiur to establish the aflinity i)y nicans of the more perfectly prestrved slriutmal elements. The distribution of the vascular l)imdles in concentric zones, as described by Williamson, may also be a feature of the Topeka specimen, but for reasons alreaily stated this cannot lie asserted with anv def^ree of confidence. More recently Solms-I.aubach* has reviewed the entire relations of this tfrouj) of i)lants, and while lie rejects Renault's name because he rei^ards the evidence as not altogether satis- factory, he prefers to retain HronLjni.irt's name (jf Myeloxylon ••rather than .Sten/elia, because it is better known." He \(\\c^ two il^nires, one of a i,a-neral transverse section, the other of a separate vascular bundle, and it is r)f considerable interest to note that this latter is almost the e.\act counterpart of a vascular bundle obtained from the Topeka fossil (y/!,^ /i. His ^a-neral vii-w of tlie structure is not so satisfactory, but it nevertheless exhibits a close similarity to my own material in all its principal features. Solnis-Laul)ach dissents from the conclusions of both Renault and Williamson, holdini( that there are stront^ reasons, on ana- tomical trrounds. for considerin^r the alliance to be with the CN-cadace;e, and cites Mcdnllosa Lciulun-ti as pnjbably affording important evidence in support of this view. The most recent contribution to our knowledL^e of these |)lants is that offered i)y Mr. A. C. Seward, who has not only reviewed tlie material originally described by Williamson, but has made a detaileil study of specimens contained in the Hinncy collection of the Woodwardian Museum. Cambrid;^^'. as well as of new naterial derived from the Millstone grit of Lancaster." The o.'r, ^.')ses show that his material is generically the same as tiiat represented by the Topeka specimens as described. In a ^'Koss. lii)t. 161. I^'OI. =" Ann. liot. 7:1. It a6 MO TAX/C.t I. GA/.E TTE [jANi-A«V scCDiid |);i|)cr, tlic same authority tuakcs a stiulv of certain spec- imens containetl in the Williamson collection and originally incliulcd by Williamson in the ^rcniis Myelopteris, hut which he fiiuls to be in reality ([uite distinct. lie therefore He|)arateH them under the name of Riuhhptcris WiUinnisoni." This species is quite tlistinct from our Topeka specimen with res|)ect to the character of '.he vascular bundles, which are concentric, and thus show a tlistinct approach to the type represented iit Aui:;iof>tins evccta. On the other hand, the mucilage passages, which are also of the type found in Angiopteris, are essentially the same as those of the Topeka specimen, differing only in distri- bution.'3 l'>om the review thus presented, it is tpiitc clear that our specimen must be regarded as a s|)ecies of myelopteris, accord- ing to the name adopted by Renault anil Williamson, and retained by me as expressing its probable relations, but that it differs s|)ecifically from any of the specimens heretofore described. It may be concluded further that the present mate- rial represents the stipe of a frond, rather than the stem proper. Heretofore the representatives of this genus have been derived wholly from the Carboniferous of Kuropc. The material now at hand from the Upper Carboniferous of Kansas thus afforils important evidence as to the wider geographical range of these plants, while the well ])reserved condition of portions t)f its structure permits a further discussion of its possible affin- ities. I have, therefore, carefully passed in review such species of living plants as are available in the botanic (iardens of McGill University, as affording a possible solution of this ques- tion. In jjrosecuting these studie;N I have had in view the sug- gestions of earlier investigators, as well as those which natu- rally arose in my own mind upon making a preliminary examination of these fossils. I have, therefore, carefully exam- ined Cordylinc tcrminalis. Phoenix dactylifcra , Kcntin Fosteruvia, =-■ Anil. Hot. 8 : 207. -■'.■\nn. Bot. 8://. /.^A^ *. f lAMAKV •rtain spoc- orijfinally t which he ; SL-paratcs his spt'cit's )ect to the c.and thus /hii^io/ifin's wliiclj are the same in tlistri- r that our is, accord- uson, and )iit tliat it heretofore scnt niate- tlie stem have been ic material msas thus ical ranjj^e if portions sible aflfin- ch species ardens of this ques- w the sug- hich natu- reliminary Lilly exani- Fosteriano, I8.J7I MM. I A tpTKKts ror/:Ki:\s/s >1 LiitiNiiii borbonha, Cyciis irroliitii, IHoon cdulc, /.lonio intn^ri/oliti, Cibotiiiin tr^iih, and .■hij;^io/'/iii.\ ivcitii. A close comparison of the Uracicna type, as represented by Cordvline, shows that any suj,fgeslion of resemblance which might at first appear, has no real basis in structural characters, while in manv essential respects there is a \ery wide difference. Noteworthy points of reseniblance being absent, it is wholly uiujecessarv to enter into a more iletailed consideration of the structural aspects of this type. \'ery nearly the same observa- tions arc applicable to the palms. In this grou|> of |)lants, how- ever, there is a somewhat closer point of contact to be found in the mucilage passages. Here these structures appear as tubular channels of great length, and in this respect, as well as in their distribution and great number, there is a general resemblance to the Topeka fossil. Their detailed structure is, on the other hand, (|uite different, anil it jxiints to a want of aflinity which is sup- ported bv the structure and distribution of the vascular bundles, as also the character of the funilamental structure, and no very searching comparison is required to establish the fact that the affinities of our fossil must be sought elsewhere. Hv several authorities the Cycadace;e ha\e been suggested as affording a satisfactorv basis of comparison, a view which, in more recent times, appears to have been particularly urged by Solms-Laubach,^* although he elsewhere agrees with other observers that certain exceptions which have been taken to the cycadaceous character of the Medullos;e are well fouiuled." Mr. Seward, vet more recentlv. has given expression to the same view, basing his opinion upon a very critical examination of a large amount of material.-''^ While admitting the many points of resemblance to ferns, he holds that in the position of the protoxvlem and in the structure of the fnucilage passages, as also in the distribution of the sub-cortical sclerenchyma, there arc strong reasons for considering the affinity to be with ^*l-'<)ss. Hot. Ibl. 'ilMii. 100. "'^Aiin. Hot. 7: iS. ! «l *. fi in I i .1 I! .'S /mr.iMc.if. i;.\/.i- 1 II: (lAMAHV tin- cyi.uls ratlur than with thi- firns. Without liopiii^- to settle this i|iicstine kind as represented by mucilage canals. These structures are distributicl throughout the funda- mental tissue and are represented by broad canals v/hich are chiefly limited by tangentially elongatetl parenchyma cells. These latter, therefore, differ somewhat conspicuously from the cells of the surrounding tissue, as already shown by Mr. .Sew- ard.'' .So far as apj)ears from the species above irulicated, how- e^'cr, these canals are alway.s lined with a layer of very thin- walled epithelium cells, which become ru|)tured with age and, shrinking back upon the main wall of the canal, give it a thick- ened and very ragged ajjpearance. In Angiopteris cvecta there are three distinct kinds of secre- tory organs: {a) tannin sacs, \,b) resin canals, and U) mucilage canals. =?Ann. l{unt'i\n u I, i/h lit \\SHV\*H llun* in no «<|»»cl;illv iliff«niiliattil t|iithiliiim, ;int! in tlii«« rtN|ntt w.' unit will) a Icitiiii' wliitli sirv«s tn sIi.m|iIv M|iai.ili- tlus«' .stiiiitmi's Iroin Uiuhi- hI tin- l.yiatlai «',r. < >ii llir^f uniiimh I mIiouIiI ti'il m» hositalioii iii ^l^•t•i(lill^; as tn wlnllitr a ^;iviii plant wi'rc cvi"iulai"iM)iiH m filimiil iti its alVinitits. l-'inm llii', |miiiiI ul vifW, tlu-n, It \\i>ultl sitin that tlir lt>|i«'ka s|iii iimii in inun- lu-arlv alli«'|iinii>n ii|Min tlir i'.\«illrnl li,niin-> u\ Mr. Si'waitl. Sin-i iiKin \i SI iiiKi'MiiVMA, — Tlu' ilistrilKilioii <>t tin- sclri- i'lu-hyma lan liaidly l>o taki-ii as an arj,Minu-nt uiu- way m tin- ..till r. siiui- lii luilli liTiis and cyfails tln-ir is siuli widf variation. I .should cons'clcr this a sprcilii latluT than a i-fniiu' i liar ictrr. In all of tiu' njycloxylons so lar studiid. tlu' m lirfiu hyiii.i is dislributi'd in st-paratc strands. In the i)iads studinl l>\ inc this tissue forms a continuous i)and in all lasi-s wht-rr slrnn^ly di'\clo|n"d. In .\n>jio|itiTis it forms a rontiniions /oiu' of ron- sidcrahli.' lliickiu'ss, with si'|>aralc stramls lyin^^ aloii^f tin.- iiiiur face. A rcsunu' i>f the results above- dctailoi.'lsr \H\ {ivcii |il.iiit MH |)niiit iif 11 i> mure il Myil.ix- I rinuifjt of I till- «.i;lfr- vv.iy or \]u' I- variation. rhaiatt«T. luliyiii.i is liid l)\ MM- rr sliniij^^ly ilJf ol 11)11- f tin.' iiiiur that in the • coiiru'ct it ■o|)t'an s|)c- to indiratc [iiittin,^: the respecting jvcrthelfss, nio to |)rc- iie Mvelo|)- sliip ; while my inotleni correctness hese plants a |>usition •>"•■; I l/l / /('/■// A/s .'0/7 A / \Sl% I Ml \S \ I InS Ml ri.A II n Wh III .M cf yn It (•'(»», ». I i,iii>^»l'>t "U Hull 'Imwilik.' Uli •»• lilt 111 In 111,1 li.iiiil', itit liii.il.i iiiriitiii liootif, iiimI Imm ttiM hIiii liiiitilliti. / l^i III, • I i,iii«vrt-«i' •»<•' Mull -iMm III.' Ill' «i iiit II' liv iii.i -li.iiiil-, Willi l»»" l;(ii.'f mm il4iK<' |'iii«MK»» • (X I I \ I I Ml III,, ( ri,iii»vt|i(r Ml linn "I .1 HI IciriM li\ MM -ll.ili'l 'tiumh"
  • ! >i I III iiiri'. ' iHcj. r" k t» i mnix/t'ff umrtA, < w// Htth M MVI.I.OITKklS Tol'KKKNSlS IViili;illu\v. J fWW >"* • :¥'^."^*'.-*^^_"-^'";'*VV"' i™*!*lU'5'l^£('r'*' /!(>/ l.\/l .1/ (..I// III-, Will. I I.I 1 1 III. MVKLOi'lKKlS I'ori'.KKNSIS I'enliallow. Ji fel I I I .) s I t* • !V i I5 ^IMlMi^-IF mk