Section IV, 1880. [ 1^3 ] Teans. Roy. Soc. Canada. X.—Somc Remarl-s on the Cla^'sification of the Trilobites, as influenced Inj Strati- (jraphkid Relation.s : toith Outline of a New Grouping of these Forms. By E. J. Chapman, Ph.D., LL.D., Professor in the University of Toronto. (Kead May 8, 1889.) (1.) It may be takon as an undoubted fact that pal:voutologioal classification has been very greatly iuiiuenced of late years by stratigraphical considerations. This is seen not only in the current subdivisions of the Trilobites, but in those also of the Ammonites and other extensive groups. These stratigraphical classifications have the advantage of being readily effected. They save trouble, by requiring little or no thought for their construction, and they are of course useful to the geologist as paloeontological lists : but there their value ceases. Structural afliuities become by this plan more or less unrecognized ; and forms with but few characters in common, if occurring at the same geological horizon, are thus often forced into false relationship, rendering even moderately rigid definitions of families ai:d other groups practically impossible. (2.) It might be thought, in opposition to this view, that contemporary forms of a given order or family must be more nearly related to each other than to forms of the same order or family occurring at earlier or later periods. But this conception is cer- tainly in the main erroneous. Forms of the same geological horizon should naturally otfer fewer points of generic agreement than forms of dilferent horizons. The latter may be connected by more or less direct evolution : whereas forms of the same horizon '-an only be related generically, if at, all, through some remote ancestral type, from which, also, other distinct orders and classes may have sprung. In one case, there may be direct relationship : in the other, the conueition can be little more than indirect. (3.) An impression prevailed widely at one time, and perhaps still prevails, that the so-called " Primordial Trilobites " are distinguished from the Trilobites of higher horizons by a combination of iharacters peculiar to themselves, by which a marked " primordial aspect" is imparted to them. These characters, as commonly formulated, comprise : — A large, typically horned or spiny head-shield, wilh numerous body segments and a A'ery small pygidium. This definition fails, of course, completely in the case of the eminently Cambrian family, the Agnostida;. But setting aside these still somewhat problematical forms, and looking only to the typical Trilobites, it is foxmd to be equally inapplicable ui many other cases. Whilst, for example, it holds good in Paradoxides, Olenus, Eurycare, and some few other Caml^rian genera, we find the same combination of characters — the large and horned head-shield, the long thorax, the small pygidium — present also in Harpes, an essentially Upper Silurian and Devonian genus, unknown in Cambrian strata. The imaginary primordial aspect is suiiiciently well marked in the Cambrian Olenus ; but in the Silurian and Devonian Arethusina or Aulacopleura we see a combination of characters very similar to those of Olenus, among whi<'h may be specially cited the comparatively short glabella, spiny head-shield, open facial suture, small eyes connected Sec. IV, 1889. 15. 114 K. J. CHAPMAN by a ridge or baud with the glabelhi, narrow body-axis with numerous or comparatively numerous segments, and small, short pygidium. Again in the Cambrian Dikeloeephalus, and in Cteuopyge (Linuarsson), the pygidium is very large — thus presenting a marked departure from the so-called primordial type. Other examples might be cited to prove, (1) that these imaginary primordial characteristics are present in various post-primordial genera, and (2) that they are not always present in primordial or Cambrian tyi^es. (4.) Nothing. p<^rhaps, shows more forcibly the arbitrary, unnatural character of stratigraiihical groupings, than the collocation in recent classiiications of Neseuretus, Hicks, side by side with Paradoxides in the family of th<' Olenidte. In all its leading characters, Neseiiret as is simply a Cambrian Calymenc, probably the ancestral source of the latter type ; l)ut in the classifications referred to, these genera are placed in ditlerent families and widely apart. To show these points in all their distinctness, viz., the close agreement of Neseuretus with Calymeue, and its remote relations to Paradoxides, a com- parative view of their more characteristic structures is given in the following table ; — NESEVKBm-S. Calymbse. PARilW-XIDEi. Glabella Contracted anteriorly, 3 later- al furrows- Contracted anteriorly, 3 later- al furrows. Expanded anteriorly. Trans- verse and lateral furrows. Tliorax 13 segments 13 segments 10 to 20 segments. Pygidium Comparatively wide, witli fur- rowed sides, an t(j 11 rings in its axis. Very small and narrow, with rarely more than 2 or 3 rings in its axis, the sides forming merely a smooth border. In these recent clajsiiicatious, also, we find Dikelocephalus arranged under the Olenida*, whilst Arethusina and Harpides, which agree very strikingly with Olenus in their more salient characters, are placed far apart from the latter under the Proetidte, evidently upon purely stratigraphical grounds. The structural relations oi these genera are brieflv indicated in the annexed tabular view : — DiKEi.ocEPiuLue. O1.ENCS. AKErriiusiNA. Glahdla Facial stttwes ■ Comparatively large, Comparatively small. Quite small. Forming a point above the Open anteriorly. Open anteriorly, glabella Eyes Large. Unconnected with tho glabella. Comparatively small. Con- nected by a hand with the ' glabella. Comparatively small. Con- nected by a (Kind with the glabella. Body-axis. •••• Comparatively broad Narrow. Narrow. Pygidixem Very large, with comparative- ly short axis. 1 Small, but with extended Small, but with extended axis. axis- i ON TEILOBTTES. 115 (•").) As the Trilobiles have no known Post-Pakuozoic representatives, and are prac- lioally confined to strata representing the earlier and middle periods of the Pakeozoic Age, broad dislimtions, surh as those which separate the Pakeozoic Criuoids and Eehinida from Mesozoic and higher forms oi' these orders, cannot obviously be looked for in any classification. Added to this disadvantage, there are other drawbacks which beset at present, and render dilFieult, the systematic grouping of the Trilohites. lirielly stated, these comprise, first of all, the very lax manner in which fragmentary examples have been referred to known types, or placed, as new genera, in families with which they have but few points of resemblance. Definitions, applicable enough in the first instancfe, become thus, after a time, of almost impossible application — the original definition being so extended as to iiicludt> forms of very dissimilar structure. Mathematically rigid defini- tions in the grouping of organic forms cannot, of course, be strictly enforced without, at least, greatly multiplying our classification groups ; but better an undue multiplication of orders and families, than this license of indefiniteness that now so habitually prevails. Another source of difficulty lies in the remarkable dissimilarity of aspect which exists in tho .•■)se of many species commonly referred to one and the same genus, as seen in Asaphus, Proetus, Cheirurus and other forms. This has led to the creation of numerous sub-genera, by which, how^ever, the diihculty is in no way lessened — family definitions still remaining vague and diffuse. (G.) In the classification shown, as regards its leading features, in the annexed synopsis, the Trilobites, considered as an order of Crustacea, are arranged under four sub- orders, or primary groups, founded on general structure and configuration, with subordi- nate sections based, as far as possible, on some striking or typical character. This latter, however, is to be taken in connection with the general characters of the sub-order to which the section may refer. The names attached to these sections refer necessarily to single characters, and they are thus to be regarded as names only, not as defmit.'ons. It is thought, however, that they may serve to bring rapidly before the mind's eye the more salient or special features of the types to which they refer. In the collocation of the families, an attempt is made to place them in as connected a sequence as possible, so that each family shall present relations to the family which tbllov>'s it, whether placed in the same section or under contiguous sections ; but in a linear system of arrang(>ment, and especially where the objects to be classified are not very numerous, it is not possible to avoid occasional breaks in the continuity of the series. In offering this new classification, I am not sanguine enough to expect that it will meet with general acceptance. In its subdivision of genera, and the recognition of these subdivisions in one or two cases as the types of new families, and in its disregard of stratlgraphical considerations, it will necessarily rullle existing prejudices. Hut it may tend to bring under more immediate notice the indefinite and hence unsatisfactory character of our commonly received subdivisions, and so lead eventually to a more successful groxiping of these ancient forms. 116 E. J. CHAPMAN Order TKII.OBITA. Sub-Ordcr I.— PUSILLIFORMES.— Small, aberrant trilobites, with typically two thoiaoic segments, and head-sliield and pygidinm of nea, '3' ecjjiial size. Fam. 1. Agnostidw. — Typical <^enus, Agnostus, Cambrian, Lower Silurian. SnlvOrder IT.— LATIFOEiLFS :— More or loss broad, often Iar, is hero separated on account of ' Ko doubt a series of intermediate varieties might bo found in which tlio distinction becomes gradually lessened or obscured ; but connecting series of tliis kind may be traced more or les.s everywhere, and if rigidly followed out woukl render generic distinctions practically impossible. 118 E. J. CHAPMAN its very distinct aspect, fn some of its forms it looks almost like u transition type between the Calymenidii' and the Asaphidie. Triarthrus, which nuich leseniblcs Calymeno in its facial suture, pleura) and pygidiiini, forms the connecting link between this seelion and the Conoecphulida>. § 2. CuRTicoNi. — Glabella typically short, smooth or lightly fui-rowed. JJody-rings 12 to 17 in number, typically over I'.i. Pygidium ^mall or comjiarativcly small, with typically 2 or 3 (more rarely 6 to 8) rings in its axis. Fam. 13. Conocephalichc. — Kycs present. Typ. gen. : Elllpsoce})halus (?), Cam. ; Ciji>has}iis, Sil., Pev.; Amjetina, Cam. ; Cunocephalites, Cam., Lr. Sil. ; Ayratdus (= Arwndluti), Cam. ; Liostracus, Cam. ; Piijcluiparia, Cam. ; Solenopkura, Cam. ; Sao, Cam. Kam. 14. Conocoryphida;. — Eyeless forms of Comcephaltdw. Typ. gen. ; Conocoryplie, Cam. ; Cttno- cephalus, Cam. Note. — The genus Ellipsocophalus, as regards the character of its glabella, is a somewhat aberrant type; but in its genei-al stiucture and aspect it is closely related to the Conocephalidie and cannot very well be placed in any other family. The separation of the eyele-is forms, typilicd by Conocoryphe, is a convenient, if not strictly necessary, subdivision. Cyphaspis connects the Cono- cephalidie with Arethusina. s; 3. ViTTATi. — Eyes connected ii}' a narrow band with the glabella. The latter sliort and small. Bt)dy-segments numerous, with nai-row axis. Pygidium, typically, very t-mall. Fam. 15. Olen'dtr. — Bod}--segments 12 to 15 or Ki in number. IL .ad-shield straight nv flattened along its anterior margin, and prolonged posteriorly into spines or horns. 'I"yp. gen. : Olenus, Cam. : Eurycare, Cam. Fam. Hi. Arethminida;. — Body-segments 22 in adult forms. Head-Shield semicircular, terminating in points or spines. T^'p. gen. : Arethii>ina (= Aitldcopleura), Sil., I>ev. ; Ilarpidts, Cam., Lr. Sil. Fam. n. — Harpesidii'. — Head-shield very large and horned, with bro.id, finely punctured border. Typ. gen. : ILirpes, Up. Sil., Dev. ; Ifirpina, Lr. Sil. Note. — The section in which these families are placed is named after one of their more striking cbaracterf, the band or fillet which connects the ej-cs with the sides of the glabella; but they have also other points of agreement, as seen more especially in tlieir numerous bodi'-segments, their narrow axis and small pygidium. Thrf)Ugh Harpides, the Harpesida' ]iropor are connected botii with Arethusina and with Olenus. Sub-Order IV. — FEONTONES. — Trilobites with large or stiongl^- pronounced glal>ella, widening as a rule anteriorly. Pygidium very small or of moderate si/.e, the many-i'inged body-axis extending quite or nearly to its extremity. S 1. AsNULATi. — Many-ringed, comparatively elongated forms, with pygidium obscurely separated from the thorax. Body-segments typically 1 1 in number. Facial sutures terminating at the sides of the head-shield. Fam. 18. Plwcopsida: — Pleurai furrowed. Eyes coarsely fticetted. Pygidium rounded or spinose. Typ. gen. : Phacops, Up. Sil., I)ov. ; Dalmanites, Sil. ; Odontocephalus, Dev. Fam. lit. Encrinuridii'. — PIcuito with raised band. Pygidium long, narrow, with mauy-ringed axis. Typ. gen. : £ncrmurus, Sil.; Cybele, Jjv.Bil.; Cromus, Up. Sil. ; Amphion,l.v.BW. ON TBILOBITES. 119 Fam. 2(». ( 'hciruridn: — Pleura' with raised band. EycH finely facetted. Pygidinin hi^rncd, spino.so III diii;ituled. Typ. ^ijcn. : '"'Af/ri/ri/s, Up. Cam., Dev. ; Pi ioplwn, V\t. S'i\.; Sjt/ia;rexochus,iii\.; St(iur..cqiluiliis, Sil. ; Flacojuiria, Lr. Sil. NoTK. — The taniilies of lliis section arc moi'c m- loss closely connectee character generally — connects the Chciruridse with the Acidasj)idn3 of tho next section. 45 2. Ak-mati. — Hssentially broad-headed, spinoso forms, with pointed or spiny pleuijc, and small to very small (commonly spine-bearing or digitated) pygidium. Body-scgmeids 1) to 20. Fam. 21. Acidaspidw. — Head, pleursc and pygidium, all spine-bearing. Body-segments 9 to 10. Pleura; witli " bourrelet." Typ. gen. : Acidasjies, Sil., Dev. Fam 22. Faradoxidd'. — Head-shield ver}- largo and bruad, with horned angles and largo, anteriorly expanded glabella. Body-segments 12 to 20 ; pleurte, furrowed, terminating in spines; Jiygi- dium very small. Typ. gen. : Paradoxides, Cam. ; Hydrocephalus, Cam. : Telephus (?) Lr. Sil. § 3. tlLOBOSi. — Glabella large and prominent, oval or globular, and unfurrowed. Thorax short, with 5 to G segments. Fam. 23. Trinudeida: — Head-shield very largo, terminating in horns, and surrounded by a broad, perforated border. Eyes commonly absent. Typ. gen. : Trinucleus, Lr. Sil. ; Dionide, Lr. Sil. ; Microdiscus {?), Cam. Fam. 24. AmpyxidZe«r('c/er TRII.OBITA. Sul)-Or(ler I.— I'USl IJJl-ORMKS. Fain. 1, Agnostidffi. Sub-Ordor II.— LATIFORMES. § 1. Lkvati. Fain. 2, Ill.ionidit!. F\tm. 3, Asaphidte. § 2. SUUATI. Fam. 4, Basilicidio. Fum. 5, Dikeloiephalidti;. § ?,. 1'ai,m.\ii. Fum. 6, Licliasidic. Fum. 7, Bronteidic. § 4 Col.l'MNATI. Fam. 8, Phaetouidic. Fam. 9, Proetidtc. Sub-Order III.— CONIFKONTES. § 1. LOXdlCX/NI. Fam. 10, HomalonotidiO. Fum. 11, Calymenidpc. Fam. 12, Triartbrida?. § 2. Cl'kticoni. Fam. 13, Conooepbalidtc. Fam. 14, Conocoryphidfc. § 3. VlTTATI. Fam. 15 Olonidio. Fum. 16, Aretluisinidio. Fam. 17, Harpesidio. Sub-Order IV.— FKONTONES. § 1. Annilati. Fam. 18, Pbacopsid;e tarn. 19, Eiicriuuridtc. Fam. 20, Cbeiruridaj. § 2. AliMATI. Fam. 21, Acidaspidrc. Fam. 22, Paradoxidse. § 3. Globosi. Fam. 23, Trinucleidse. Fam. 24, Ampyxidic. Ihm. 25, ^glinidie. § 4. OCULOSI. Fam. 26, Boliemillida?. Fam. 27, Remopleurida?.