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LELAND STANFORD JUNIOR UNIVERSITY PUBLICATIONS UNIVERSITY SERIES Fossil Fishes of Diatom Beds of Lompoc, California BY DAVID STARR JORDAN Chancellor-Emeritus of Stanford University AND JAMES ZACCHEUS GILBERT Teacher of Zoology, Los Angeles High School STANFORD UNIVERSITY, CALIFORNIA PUBLISHED BY THE UNIVERSITY FEBRUARY, 1920 THE FOSSIL FISHES OF THE DIATOM BEDS OF LOMPOC, CALIFORNIA In a previous paper (Fossil Fishes of Southern California: Leland Stanford Junior University Publications, issued September 16, 1919) the present writers have noted a number of new species of fishes, of Miocene Age, from the deposits at Lompoc. Since that time, through the courtesy of Mr. Arthur H. Krieger, director of the Celite Products Company, and his assistants, Messrs. Ed- ward J. Porteous and Edward B. Starr, Dr. Gilbert and Dr. Jordan have successively visited these deposits, making extensive collections. Still later, Mr. Willard J. Classen, a student in Geology at Stanford University, through the kindly interest of Mr. Timothy Hopkins, has spent some time there securing fossil fishes for Stanford University. A large collection of fish has been obtained, this forming the basis of the present paper. The Lompoc deposit itself is wholly unique. It lies in Santa Barbara County, California, within an angle on the north side of the Sierra Santa Ynez, a range composed mainly of Miocene sandstones and shales. This angle or ancient bay covers about four square miles. In this space a continuous and almost uniform mass of diatoms has been deposited, to the maximum depth of 1,400 feet. The erosion of a stream on the west side has cut this deposit through to its bottom of yellowish sandstone. Over most of this space, the diatom deposits come to the surface, but in places the mass is overlaid by a coarse, hard breccia or conglomerate, containing many bones of whales, and occasionally teeth of sharks. On the extreme west, it is overlaid by limestone in which a species of Pecten is very abundant. In places, there are thin layers of flinty rock, apparently of animal origin, interstratified with diatoms. At one horizon, about six feet above the Xyne layer noted below, there is a thin stratum of volcanic glass. Scarcely anywhere in the whole mass does any sand or clay appear. This shows that the deposit was made in quiet water undisturbed by fresh water or rains. It may be noted that in deposits of the Monterey period of the Miocene age, from Monterey to San Diego, diatoms abound, some- times mixed or interstratified with sand or clay as about Los Angeles, at other places forming immense deposits. It has been thought that such deposits when buried under later rocks, as in Kern County and parts of Santa Barbara, are the source of the oil found in these districts. When the deposits are not covered, as at Lompoc, it is presumed that the oil has all evaporated. 6 FOSSIL FISHES OF LOMPOC The probable conditions of the deposits at Lompoc are thus indicated by Dr. Albert Mann of the Carnegie Institution at Washington, to whom we have sent specimens of material from various parts of the beds. "The samples of diatom material received seem to indicate the follow- ing facts, unfortunately of small value for your fish-deposit problem: "1. Marine, with no infiltration of fresh or brackish water forms. "2. Not plankton material. Diatoms all large and massive. Heavy sponge-spicules abundant; heavy Radiolaria present, though few. "3. Not transported a great distance nor by swift or violent currents to their present position, as the diatoms, though somewhat broken by pressure, show no wear ; also as there is an absence of any appreciable quantity of sand, shells, clay, etc. "4. Not a complex of materials from different localities, as the dia- toms, though abundant, are remarkably few in species, being chiefly two species of COSCINODISCUS. "5. Slowly and evenly deposited in their present position, with regular fluctuations in quantity (seasonal ?), resulting in the mass being formed of thin laminated plates, easily separable, but uniform in composition. "It looks to me as if my samples were laid down in situ, in some quiet, shallow marine bay, into which no considerable quantity of fresh water drained. . . . "As to the oil relationship, I do not know a thing. As you know, all sorts of theories, have been advanced regarding the contribution of diatoms to the so-called mineral oils. But I had the good luck last summer at Woods Hole to secure a perfectly pure gathering of plankton diatoms of a single species, unmixed with a single Copepod, Nematode, or any other organism. I secured a solid liter of it, and it is now in the hands of a chemist for the ether extraction of the oil, which will be sufficient in quantity for the first accurate analysis of diatom oil. . . "The large amount of oil laid up as a reserve food material by dia- toms is certainly significant. I have found it making fully 50 per cent of the bulk, and I have never found it to be less than 5 per cent." The economic use of these deposits, made up of the silicious shells of microscopic plants, known as diatoms, is at present two-fold. The material is cut into bricks, which, being non-conductors of heat, are used as packing about steam-pipes and the like, and sold as Sil-O-Cel. The second use is for filtering liquids. The silicious shells are insoluble, and poured into any fluid, they carry at once to the bottom all solids in suspen r sion. The whole can then be filtered and the liquid is left perfectly clear. This is "Filter-eel," made of the crushed rock. "Celite" is a meaningless trade name, adopted for the output of this particular deposit. LIST OF SPECIES 7 Since the period of deposition, the rocks of the Santa Ynez range have undergone some folding, leaving the strata of diatoms nowhere hori- zontal. The Xyne layer stands where examined by us at an angle of about thirty degrees, the north side highest. From the natural history view, this stratum is the most remarkable fea- ture of the deposit. At about 950 feet from the bottom, at a certain hori- zon everywhere the same, is a layer of an extinct herring, described by us in a previous paper as XYNE GREX. Individuals lie on the bottom wherever this layer has been exposed. They are all of about the same size, about six inches long, all adult and nowhere mixed with any other fish. Apparently the species swarmed in the bay for spawning purposes, and the entire mass was heated, suffocated, or otherwise killed in an instant and with no evidence of agony or distortion. In the rocks above, occasional examples are found, always as im- prints, while those of the main mass have been mostly carbonized and left black or nearly so. The other fishes found in these deposits mainly occur in the upper strata. Only large fishes, a foot or more herrings ex- cepted are found here, these being mainly mackerel, flounders, bass, rock-fish and the like, which were apparently in pursuit of the herring. All of these are described and figured in the pages which follow. This Lompoc fauna contrasts strongly with that described from the impure diatomaceous shales at El Modena and Bairdstown of the same age, but evidently under different conditions. All the fishes of these deposits are immature, evidently residents of shallow bays within the archipelago which now forms the counties of Los Angeles and Orange. The species thus far found at Lompoc are the following (new names in italics) : Family LAMNIDyE 1. CARCHARODON ARNOLDI Jordan. Family CLUPEID^E 2. XYNE GREX Jordan and Gilbert (J. Z.). 3. XYNE fitgeri Jordan and Gilbert. 4. LYGTSMA TFNAX Jordan and Gilbert. Family SCOMBRID^ 5. Turio wilburi Jordan and Gilbert. 6. Thyrsion velo.v Jordan. 7. Thyrsocles KRIEGERI Jordan and Gilbert. 7A. Thyrsocles escharion Jordan. 8. Ocystias sagitta Jordan. g FOSSIL FISHES OF LOMPOC Family ZAPRORID^E. 9. Araosteus rothi Jordan and Gilbert. Family ZAPHLEGID/E 10. Zaphleges longurio Jordan. Family SERRANIM) 11. EMMACH.ERE RHACHITES Jordan and Gilbert. Family SPARID^E. 12. Rhythmias starrii Jordan and Gilbert. 13. Plectrites classeni Jordan. Family SCLENIDjE. 14. LOMPOQUIA RETROPES Jordan and Gilbert. 15. Lompochites hopkinsi Jordan Family SCORP^NIM). 16. Rixator porteousi Jordan and Gilbert. 17. Rixator inezice Jordan and Gilbert. Family HEXAGRAMMID^. 18. HEXAGRAM MOS ACHRESTOS Jordan and Gilbert. Family OPHIODONTID^E. 19. OZYMANDIAS GILBERTI Jordan. Family PLEURONECTID^ 20. EVESTHES JORDANL J. Z. Gilbert. 21. EVESTHES hooveri Jordan. 22. DIATOMCECA ZATIMA Jordan and Gilbert. 23. Zororhombus veliger Jordan. Family BROTULIDyE. 24. ECLIPES VETERNUS Jordan and Gilbert. Family . 25. Atkinsonella strigilis Jordan. Family DUSSUMIERIID^. QU^SITA alhambra Jordan and Gilbert. QU.ESITA fragilis Jordan and Gilbert. CARCHARODON Family 1. Carcharodon arnoldi Jordan. No teeth of sharks have been found in the diatom deposits. In the breccia which overlies part of these beds, shark's teeth occur occasionally among the broken bones of whales. We obtained two such teeth corresponding to the form called CAR- CHARODON RIVERSI Jordan, which we take to be a back tooth of the common CARCHARODON ARNOLDI. Family CLUPEID-ffi. 2. Xyne grex Jordan and Gilbert. (Plates I, II, III) In the original description of this species (Jordan and Gilbert, Fossil Fishes S. Cal., p. 25) it is stated that numbers XXIV and XXVIII, Stanford Collections, came from Bairdstown. This is an error: all came from the same stratum as the type slab (CVIII) from Lompoc. Outside the mass of this species, which covers four square miles of deposit all at the same geological level, this fish is scantily distributed through the rocks higher up. The most remarkable feature of the diatom beds is the evidence of a tremendous catastrophe which overwhelmed millions of individuals of this herring, at a single moment, apparently in the spawning season. It is evident that these fishes were gathered together in the sheltered bay in which these deposits occur. At a horizon 950 feet from the base of the deposit is the layer of this species. The individuals are of about the same size (6 to 8 inches) lying flat, not distorted nor much piled. All are in the same horizon and this wherever opened is covered with these fishes. No other species is mixed with them, and there are but few remains of the species in the rocks higher up. Nearly all these specimens are dark brown or black, showing them to have been carbonized. In the rocks above, this and other species are mainly prints merely, the marks of their bones being replaced by diatoms. Of this species numerous slabs were obtained, through the energetic help of Messrs. Krieger, Porteous, and Starr, and Mr. John Sells, fore- man. These were taken from a tunnel near the north side of the deposit. The largest slab is about eight feet by four, containing hundreds of individuals. The genus XYNE is characterized by a symmetrical herring-like form, the belly, however, compressed and armed with sharp lanceolate scutes, the dorsal nearly median and opposite the ventrals, the bones of 10 FOSSIL FISHES OF LOMPOC the head finely striated and enameled. The vertebrae are about 45, a char- acter which separates the genus from the modern forms with sharp ventral scutes. We find no trace of dorsal scutes nor of finlets ; the slen- der ribs are about as long as head and nearly four in length to base of caudal. Intermuscular bones are very evident : the ribs are forked below, and the ventral spinules are well marked. We give the record of the most perfect examples found above the horizon in which the multitudes occur. No. 110 is about six inches long, the back abruptly broken and the head crushed ; ribs 4^2 in length of body. Vertebras 43 ; 24 behind in- sertion of ventrals. These are nearly under middle of dorsal, as usual in this group. No. 116. Eight inches long; is well preserved: mouth large, the lower jaw projecting; ventrals just behind front of dorsal; vertebrae 43; 23 caudal vertebras ; depth of body 5 in length. 24. Broken in three parts, the head much crushed. 27. Fair. 36. Two specimens with ECLIPES VETERNUS. Tail and posterior dorsal rays. 39. Backbone. 51. Fairly good imprint. 123. Fair. 126. Two in bad order. 153. Bad condition. 157B. In fair shape; no head nor fins. 203. Fragments of four fishes. 243. Fair condition. 288. Two damaged skeletons. 3. Xyne fitgeri Jordan and Gilbert, new species. (Plates IV, V) Besides XYNE GREX, a second species of herring occurs in these deposits. This we may provisionally refer to the same genus. It is deeper in body, with the head much heavier, the form much less symmetrical. The vertebras are 45 in number, rather heavier than in XYNE GREX, and the anterior vertebrae seem loosely connected, becoming readily crushed out of place, or as in the type example bowed into an arch. The ribs are longer than in XYNE GREX, nearly as long as head, about 3^4 in length of body. The form of the head and the tendency to curvature of the back- bone, with the less symmetrical form of the body, may indicate generic distinction for this species, but it is certainly a near relative of XYNE. XYNE 11 The two species (possibly identical with each other) already described by us from El Modena and Carpinteria (LLIMMA ELMODEN.E * and EL- LIMMA BARBARA) are certainly nearer XYNE than ELLIMMA; and may be temporarily assigned to XYNE, with which they agree in general traits and especially in the number of vertebrae (.44). The ribs are longer than in X. GREX or X. FITGERI, being about 3% to 3^ in length of body. It is very doubtful whether these species belong to the group of double-armed herring, the presence of dorsal scutes being uncertain. In this group the Eocene genera, DIPLOMYSTUS, KNIGHTIA, ELLIMMA, and ELLIMICH- THYS, find their place. The type of XYNE FITGERI is a specimen (No. 167) seven inches long, lacking the upper and low T er fins. Body heavy forward with large head. Head 2% in length to base of caudal ; depth about 2%- Head very large, with steep, straightish pro- file; eye moderate; lower jaw long, low, protruding; maxillary 1% in head. Vertebrae 43, the first 24 forming a notable arch, its arc 21/2 times its height, a character apparently due to distortion, as only partially shown in other specimens. Vertebrae rather longer than deep, ribs many, very slender, U/4 in head, nearly 3*4 in body ; some intra-muscular bones ; neu- rals and hsemals moderate, interspinal bones weak and mostly obliterated ; pectoral fins narrow, inserted low ; dorsal, anal, ventrals, and scales wholly obliterated except for the lanceolate sharp ventral scutes which are about 15 in number; caudal strong, well forked, the lobes 1% in head, the rays slender, about twenty-five to be counted. This specimen is preserved in duplicate, the other half (167B) being exactly like it. The species is named for Mr. August Fitger, the excel- lent proprietor of the Lompoc quarries. A second specimen (26) is in fair condition, 6 inches long, the ver- tebral column elevated anteriorly, but not perfectly arched ; dorsal and ventral present, the ventral just behind front of dorsal. Head 3 in length ; depth 3 ; vertebrae 43. Another specimen (No. 241), 4i/ 2 inches long, has the head large and with steep profile. The head is, however, crushed back on the body, so that the dorsal fin is close behind it, and the anterior vertebrae are dis- located and scattered about the nuchal region. There are 25 to 28 ver- tebras behind the line of insertion of dorsal. The vertebral column in this species seems exceptionally fragile, for when not arched, it is usually broken or distorted. A specimen 3% inches long (the total fish about five) (No. 205), with the head and tail broken, much resembles the type of ELLIMMA EL- * We may here note that in the original description of ELLIMMA ELMODEN^E "head 2y 2 in length" is a misprint for "head 3%." 12 FOSSIL FISHES OF LOMPOC as figured by Jordan and Gilbert. It is, however, unquestion- ably a member of this species. The dorsal, pectoral, and ventral fins are fairly preserved, as are also the vertebrae and the ribs. There are eight vertebras before the ventrals. Ribs about 22. Vertebrae rather deeper than long, those anteriorly a little elevated. Other specimens are the following: 29. Probably the same, body only, anterior vertebrae out of place. 44. Vertebral column little arched; pectoral complete, short, 2y 2 in head; about 15 scutes before ventrals. 124. Fair; head large, broken; ventrals a little nearer gill opening than base of caudal. Caudal well forke'd, anterior vertebrae moderately arched, vertebrae 45, dorsal and anal wanting. 140. Young the vertebral column little arched. Vertebrae about 40 poor condition. 507. In fair condition, much like No. 26. The backbone not arched, but undulated. 146. Column a little arched; paired fins wanting. 149. Bad order ; column little arched. 150. Broken head. 196. An example with a big head, deep body, and .median dorsal. Vertebrae about 40. the column somewhat arched anteriorly: belly with strong scutes. 244. Broken torso, showing 15 ventral scutes. 235. Shows a short dorsal nearer head than base of caudal; spinal column little arched, broken, apparently very fragile. The whole struc- ture very weak. 274. Broken torso, vertebral column somewhat arched. 278. Part of a large example. No new features. 291. Part of side no arch in vertebral column. 314. Broken skeleton and head. The vertebral column a little arched anteriorly. 324. Head and torso much broken. 411. Fair condition; shows ventral scutes and paired fins. Head large, 3y 2 in length, depth 3 ; 13 scutes before ventrals. In addition to those noted above there are numerous fragments more or less definitely referable to this species. 4. Lygisma tenax Jordan and Gilbert. No. 79. Seven inches long. Head and vertebral column, the head badly crushed, the vertebral column intact and much twisted as in the original types: neural and LYGISMA 13 haemal spines strong, interhaemals, interneurals and fins lost; head large, with large orbit, median in position; lower jaw prominent; pectoral in- serted low. Vertebras about 40, reduced posteriorly, longer than deep and constricted. No scales or scutes preserved. We identify this specimen doubtfully by the tough antf twisted spinal column, which seems to be a distinctive trait. No. 121 shows the head with some of the vertebrae, of the same species. Family SCOMBRID^ Next to the evidence of the extraordinary catastrophe which over- whelmed the herring known as XYNE GREX, the most remarkable feature of the Lompoc beds is the presence of five different species of mackerel predatory fishes, doubtless lured into the bay to feed on the herring. All of these forms are related to the living species known as Spanish mackerels, SCOMBEROMORUS Lacepede (CYBIUM Cuvier). But differences in the vertebral column, the dentition and the interspinal bones, necessitate the recognition among them of four distinct genera. To these, we assign the names of TURIO (WILBURI), THYRSION (VELOX), THYRSOCLES (KRIEGERI), and OCYSTIAS (SAGITTA). The six genera of SCOMBRID^; found in the Miocene deposits of Southern California may be thus compared with each other and with the living genera of this type. (a) Anterior vertebrae simple, not "trellis-like" ; teeth not serrate, nor greatly enlarged ; posterior vertebrae not held immovable by backward ex- tensions from apophyses ; no canine teeth ; body without corselet of modi- fied scales, as far as known. (fe) Vertebrae few, about 28 in number; dorsal spines about 10 in number, slender, close-set. (Allies of SCOMBER.) (c) Interspace between dorsals short, not more than the length of two vertebrae ; body rather deep, tapering backward ; the depth about 3^ in length ; teeth unknown ; opercular region short. TUNITA. (cc) Interspace between dorsals long; as long as four or more verte- brae ; body elongate, tapering slowly backward ; depth about 4% in length ; interhaemals slender and short, weak. (d) Opercular region moderate, teeth unknown (supposedly conic and pointed, close set). AUXIDES. (bb) Vertebrae about 28; dorsal spines about 20. Opercular region very long, longer than distance from front of eye to edge of preopercle ; teeth compressed, wide set, about 20/20 on each side; body moderately elongate, the depth about 5 in length ; dorsal spines slender, close-set, the anterior elevated. (Ally of EUTHYNNUS.) TURIO. 14 FOSSIL FISHES OF LOMPOC (bbb) Vertebra numerous, 40 to 55, subquadrate, strongly grooved; post-ocular region not expanded, shorter than rest of head ; dorsal spines low, slender. (Allies of SCOMBEROMORUS). ( S^% . :-:--rJ^ S%' PLATE XX. LOMPOCHITES HOPKIXSI Jordan & Gilbert: type No. 301 (reduced two-thirds natural size). PLATE XXI. KIXAFOR wmnousi Jordan & Gilbert; type No. 300 (one-third size); second anal spine broken. m : *c^ ^ - - 7.W^r**'.<**s*sr . ',-- ^ ' X!^ - * \. | - ~^'"' "t-A?^ \ "> -- V r "~W- ^^ssntV'X v k ';, /- PLATE XXI\ . OZYMANDIAS GILBERTI Jordan; No. 13 (reduced about half) ; identification uncertain. PLATE XXV. EVESTHES 'JORDAN'! Gilbert; No. 509 (three-fifths natural size). 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