Printer Friendly

A fossil skull of the extant blue marlin (Makaira nigricans Lacepede, 1802) from the late Miocene of Orange County, California.

Abstract.--A nearly complete fossil skull, including the rostrum, of blue marlin, Makaira nigricans Lacepede, 1802 (Perciformes: Xiphioidei: Istiophoridae), was collected from the Oso Member (latest Miocene) of the Capistrano Formation, Mission Viejo, Orange County, California. The specimen is compared with extant and fossil istiophorids, and 19 of its 20 morphological variables are within the range of values observed for extant M. nigricans, whereas only 13 or less variables are within the observed range of other extant istiophorids. Because extant M. nigricans usually inhabits a water column with a height of about 200 m or more and is the most tropical of all xiphioid species, its presence supports the hypotheses that the Oso Member was deposited at upper bathyal depths or greater and that the coastal paleoclimate of southern California was warmer during the late Miocene than at present.

**********

The extant blue marlin, Makaira nigricans Lacepede 1802, (Perciformes: Xiphioidei: Istiophoridae) is an important commercial and recreational fish species that inhabits the tropical and temperate Atlantic, Indian, and Pacific oceans, various strata within a water column of about 200 m or more and average sea surface temperatures of approximately 24[degrees]C (Nakamura 1985). The blue marlin is rarely observed off the coast of southern California (Eschmeyer et al. 1983).

According to Fierstine (2006), the blue marlin or blue marlin-like xiphioids (M. cf. M. nigricans) are the most common fossils of the Family Istiophoridae. The earliest records are from the late Miocene where M. nigricans was identified in two rock units in southern California, the Monterey and San Mateo formations (Fierstine and Applegate 1968; Fierstine and Welton 1988; Fierstine 1998, 2001), and M. cf. M. nigricans was identified in three late Miocene rock units, the Eastover Formation, Virginia, U.S.A. (Fierstine 1998), Gatun Formation, Panama (Fierstine 1999), and Pietra leccese, Italy (Carnevale et al. 2002). In addition, blue marlin and blue marlin-like specimens also were described from the Trinidad Formation, Baja California Sur, Mexico, but because the age of the deposit ranges from late Miocene to late Pliocene (Fierstine et al. 2001), the specimens may or may not rank among the earliest known records of M. nigricans. The specimens from the two southern California localities were originally identified only to genus (Makaira sp.) (Fierstine and Applegate 1968; Fierstine and Welton 1988), but were re-identified by Fierstine (1998, 2001) after more comparative material became available.

In 1980, Hugh Wagner, during a paleomitigation project for the Mission Viejo Company, collected a nearly complete skull of M. nigricans, OCPC 31001 (Orange County Paleontology Collection), from the Oso Member (latest Miocene) of the Capistrano Formation near the current northern city limit of Mission Viejo, Orange County, California (Fig. 1). According to Barnes and Raschke (1991), the Oso Member is correlative with all but the latest Hemphillian North American Land Mammal Age [4.6 to 9.0 Ma (Woodburne and Swisher 1995)]. Although the specimen is the third record of a blue marlin in late Miocene deposits of southern California (Fierstine 2006), it is the only one with a skull and rostrum, and warrants description.

Materials and Methods

Approximately 160 whole and partial skeletons of extant (= Recent or Holocene) specimens, representing seven species of the family Istiophoridae, were examined and used for comparison with the fossil skull. The scientific and common names of Nelson et al. (2004) are used for Recent istiophorids with the exception that I follow Orrell et al. (2006) and place the istiophorids in the suborder Xiphioidei, and Collette et al. (2006) who recognize only one species of blue marlin (M. nigricans) instead of two species [M. nigricans and M. mazara (Jordan and Snyder 1901)]. A combination of the osteological terminology of Arratia (1997), Davie (1990), Gregory and Conrad (1937), Gudger (1940), Rojo (1991), and Schultz (1987) is used.

Anatomical abbreviations are:a-a, angular-articular; bo, basioccipital; de, dentary; fr, frontal; fv, facet on maxilla for articulation with vomer; ipr, internal (anterior) process of the maxilla; le, lateral ethmoid; mpr, maxillary (posterior) process of the maxilla; rex, maxilla(e); ha, nasal; nc, nutrient canal; pa, parasphenoid; pd, predentary; pmx, premaxilla(e); pn, prenasal; pop, preopercle; pt, pterygoid; qu, quadrate; sph, sphenotic; tr, triangular region of maxilla; vo, vomer.

Institutional abbreviations are: LACM, Natural History Museum of Los Angeles County, Los Angeles, California, U.S.A.; MAUL, Museo dell'Ambiente, Lecce University, Puglia, Italy; OCPC, Orange County Paleontology Collection, Santa Ana, California, U.S.A.; UCMP, University of California Museum of Paleontology, University of California, Berkeley, California, U.S.A.; USNM, United States National Museum of Natural History, Smithsonian Institution, Washington, D.C., U.S.A.

Characters and their definition for each bone or structure were taken liberally from Fierstine (1998, 2001) and are as follows:

Rostrum.--Rostra were measured according to the methods of Fierstine and Voigt (1996). Two regions were emphasized: 0.5 L, or one-half the distance between the distal tip and the orbital margin of the lateral ethmoid, and 0.25 L, or one-fourth the distance between the distal tip and the orbital margin of the lateral ethmoid. Cross-sections were obtained at 0.5 L and 0.25 L using computer tomography (CT) at scan values of 120 kv, 100 mA, and 2.0 sec. Characters studied in each region (.05 L and 0.25 L, respectively) were depth ([D.sub.1], [D.sub.2]) and width ([W.sub.1], [W.sub.2]) of the rostrum, height ([H.sub.1], [H.sub.2]) and width ([N.sub.1], [N.sub.2]) of the left nutrient canal (as seen in cross-section), and distance ([DD.sub.1], [DD.sub.2]) of the left nutrient canal from the dorsal surface of the rostrum (as viewed in cross-section). Characters studied without reference to region were distribution of denticles on the dorsal (DZ) and ventral (DVS) surfaces of the rostrum (both measured from the distal tip), length (P) from the distal tip of the rostrum to the distal extremity of the prenasal bone, presence or absence of denticles on the prenasal bone, and length from the tip along the ventral surface where the fused premaxillae divide (VSPM) into separate bones.

Predentary.--Three morphometric characters were studied: length along the ventral mid-line (PL); width across the widest expanse of the toothed surface (PW); and depth perpendicular to the long axis from the widest expanse of the toothed surface to the ventral surface of the bone (PD).

[FIGURE 1 OMITTED]

Quadrate.--Five characters were measured: greatest height from the condyle for articulation with angulo-articular to the tip of the dorsal process (QH); height from the condyle to the notch for the symplectic bone (QHS); greatest width (medial to lateral) in the region of the condyle (QAW); width of the condyle (QMW); and length of the condyle (QML).

Maxilla.--Six morphometric characters were studied, five in the triangular region (tr) that articulates with the nasal, premaxillae, prenasal, and vomer: length of the triangle (ML), height of the triangle (MH), width from the lateral surface of the triangle to the medial margin of the facet (fv) for articulation with the vomer (MW), and height (MVH) and width (MVW) of the facet. The sixth character is the length of the posterior limb from the anterior tip of the triangle to the posterior tip of the maxillary process (mpr) at the gape (MOL).

Neurocranium.--Because the neurocranium is badly crushed dorso-ventrally, only the presence or absence of its bony constituents is noted.

Systematic Paleontology

Class Actinopterygii Cope 1887

Division Teleostei Muller 1844

Order Perciformes Bleeker 1859

Suborder Xiphioidei Swainson 1839

Family Istiophoridae sensu Robins and de Sylva 1960

Genus Makaira Lacepede 1802

Makaira nigricans Lacepede 1802

Figures 2, 3; Tables 1, 2

Material.--OCPC 31001, partial skull, including the skull roof, rostrum, lower jaws and quadrate.

Locality.--OCPC locality 3101 (= MV19), a reddish brown, pebble conglomerate to coarse sand unit of the Oso Member (latest Miocene) of the Capistrano Formation, in a roadcut facing Los Alisos Boulevard approximately 3.5 km northeast of the junction of Los Alisos Boulevard and Trabuco Road, Mission Viejo, Orange County, California, NW 1/4, NE 1/4, Sec. 18, T. 6 S., R. & W., El Toro, California quadrangle, U.S.G.S., 1968 (photorevised 1982), 1:24,000 scale (Fig. 1).

Remarks.--The specimen mostly consists of the rostrum, lower jaws, and a dorso-ventrally crushed neurocranium (Figs. 2,3). The ventral and lateral skull region (basisphenoid, myodome, most of the otic bones and vomer), all the opercular bones (except for part of the preopercule), most of the lateral ethmoids, and suspensoria are missing. Measurements of the specimen are listed in Table 1.

In dorsal view (Figs. 2A, 3A), the distal one half of the rostrum is well preserved, but the proximal half is incomplete and dorso-ventrally compressed (Fig. 2C). Denticles are restricted to the distal 22 mm of the rostrum. The left prenasal (pn) is complete, except for a middle segment, and the right pn is poorly preserved, except for its most distal extension onto the rostrum. The left nasal (na) is more complete than the right na, and its sutures with the frontal (fr) and pn are well-defined. Both fr are preserved. Most of the bones (supraoccipital, epitotic, pterotic, opisthotic, parietal, etc.) that compose the posterior part of the neurocranium are crushed beyond recognition. The right maxilla (mx) is better preserved than its counterpart, with the former containing both the articulation for the vomer (fv) and the internal process (ipr). The right dentary (de) is well preserved, except for most of its denticles. The right angulo-articular (a-a) is incomplete posteriorly and is rotated clockwise with respect to the right de.

[FIGURE 2 OMITTED]

In ventral view (Figs. 2B, 3B), the distal segment of the rostrum is completely covered with denticles for approximately 261 mm (DZ) and then the denticles divide to form a narrow edentulous zone along the midline that terminates at the division (VSPM) of the right and left maxillae. Most of the right mx, including a large part of the maxillary (posterior) process, is visible. The rugose joint surface on the ventral margins of the left pn and na that articulates with the left mx (triangular region) is well preserved. The interior (ventral) surface of the left fr contains a fragment of the lateral ethmoid (le) and sphenotic (sph). The lateral surface of the left quadrate (qu) is complete; however, the entire element has undergone deformation that gives it a slightly melted appearance. The occipital condyle and ventral surface of the basioccipital (bo) are present. The lower jaw is complete from the distal tip of the predentary (pd) to the posterior part of the de. A small portion of the left a-a and most of the right a-a are visible, and both have been displaced and rotated from their normal anatomical position with respect to their dentaries. A large fragment of the left pterygoid (ecto- and entopterygoid) rests on the fight lower jaw. Two flat elements, presumably the ventral surface of the parasphenoid (pa) and a small portion of the vomer (vo), are visible.

In cross section at 0.5 L (Fig. 2C), the rostrum is crushed dorso-ventrally and the exact width and depth of the rostrum were only estimated. The left nutrient canal is abnormally larger than the right, thus the size of the canals ([H.sub.1], [N.sub.1]) and their position with respect to the dorsal surface ([DD.sub.1]) and to one another ([IC.sub.1]) were considered too uncertain for comparison with other istiophorids. In cross section at 0.25 L (Fig. 2D), the rostrum is preserved with no evidence of dorso-ventral compression. However, the left nutrient canal is abnormally larger than the right canal also, thus measurements of the size and position of the canals were not used for comparison with other istiophorids.

[FIGURE 3 OMITTED]

Discussion and Conclusions

Only 20 of the 26 variables (ratios) listed in Table 2 for OCPC 31001 are considered to have an adequate sample size (n [greater than or equal to] 7) in three or more species of recent istiophorids to warrant interspecies comparison. Nineteen of the 20 variables are within the range of values observed for M. nigricans, with other species having 13 or less variables within their observed range. One variable (ML/MOL) is within the observed range of three extant istiophorids, but not M. nigricans. However, the measurement of MOL is an estimate, and perhaps the variable would be within the observed range of M. nigricans if it could be more accurately determined. This evidence indicates OCPC 31001 is M. nigricans.

With exception of its rostrum, specimen OCPC 31001 has few bones in common with other fossils of the genus Makaira. For example, two specimens of M. cf. M. nigricans (MAUL 917/1; USNM 375733) are the only other Makaira with a preserved maxilla (Fierstine 1998; Carnevale et al., 2002) and four specimens of M. cf. M. nigricans (MAUL 917/1; NCSM 6944; USNM 476372, 481903) are the only other ones with preserved quadrates (Fierstine 2001; Carnevale et al. 2002). Of the 26 variables (ratios) listed in Table 2 for the Capistrano Formation blue marlin, only 22 have been measured in other fossil istiophorids, and, with the exception of specimens from the Yorktown Formation and Pietra leccese, measurements were recorded from a single bone or structure that represents a single individual. It is not surprising then that only 14 variables of the Capistrano marlin are close to ([+ or -] 25%) or within the observed range of other fossil istiophorids.

Paleoenvironment

The depth of deposition of the Oso Member has only been described in general terms. Based primarily on the stratigraphy of Vedder (1972), Barnes and Raschke (1991) interpreted the Oso Member as a nearshore (proximal) facies of the Capistrano Formation that has yielded remains of land mammals. Demere and Berta (2005), based on the biostratigraphy of White (1956) and Ingle (1979), interpreted the Oso Member as probably being deposited at continental shelf depths (i.e., somewhere between 0 and 200 m). Ehlig (1979) concluded that the Oso Member in the northeastern part of the Capistrano Embayment (Fig. 1) was deposited at upper bathyal depths (i.e., 200 m or greater). Because all three studies differ in their interpretation of the depth of the deposit, perhaps the billfish skull can provide more precise bathymetric evidence for the Oso Member in the northeastern portion of the embayment.

Recent blue marlins are oceanic fishes (i.e. favor inhabiting a water column with a height greater than 200 m) and are rarely encountered in shallow, nearshore waters. They are not seen near landmasses or islands unless they are in the vicinity of a deep drop-off from the continental shelf (Nakamura 1985). If it is assumed that fossil istiophorids had ecological preferences similar to extant istiophorids (Fierstine 1998, 2001, 2006), then the presence of blue marlin remains in the Oso Member suggests that the stratum was deposited in at least 200 m of water. Unlike the carcasses of large marine mammals that often float after death and sometimes end up in more inshore waters (Berta et al. 2006), the carcasses of xiphioid fishes usually sink, based on pop-up satellite archival tags released from dead fish (E. Prince, NOAA, Miami, FL, pers. comm., October 29, 2007). Because the fossil skull (OCPC 31001) is fairly complete and shows no wear or breakage (e.g., the rostrum is articulated with the neurocranium), it is unlikely it was transported by ocean currents or wave action. Therefore, the billfish probably died in the vicinity of the water column where its skull became entombed.

Blue marlins inhabit temperate and tropical waters of the Atlantic and Indo-Pacific Oceans and are considered the most tropical of all istiophorid species (Nakamura 1983). They are generally found in water with an average sea surface temperature of approximately 24[degrees]C. As noted above, extant blue marlins are occasionally found off southern California (Eschmeyer et al. 1983), but only during periods of anomalously high sea surface temperatures (The Southwest Fisheries Science Center's 1996 Billfish Newsletter [unpublished]). Thus, the presence of M. nigricans in the Capistrano Formation offers further support that the coastal paleoclimate of southern California was warmer during the late Miocene than at present (Fierstine 2006).

Acknowledgments

I want to thank H. Wagner (SDNHM) for his collecting expertise, and allowing me to prepare and study the fossil marlin. J. Cooper (OCPC) and L. Babilonia (Los Coyotes Paleontology Museum) encouraged study of the specimen. J. Cooper (OCPC) and G. Takeuchi (LACM) generously provided pertinent literature and critically read various drafts of the manuscript. T. Demere (San Diego Natural History Museum) furnished thoughtful criticisms of the submitted manuscript, and E. Prince (NOAA, Miami, FL) provided important literature and shared his extensive knowledge of tagging studies in billfishes.

Accepted for publication 12 October 2007.

Literature Cited

Arratia, G. 1997. Basal teleosts and teleostean phylogeny. Palaeo Ichthyologica, 7:5-158.

Barnes, L.G. and R.E. Raschke. 1991. Gomphotaria pugnax, a new genus and species of Late Miocene dusignathine otariid pinniped (Mammalia: Carnivora) from California. Contributions in Science, Natural History Museum of Los Angeles County, (426): 1-16.

Berta, A., J.L. Sumich, and K.M. Kovacs. 2006. Marine mammals: Evolutionary biology. 2nd ed. Elsevier/ Academic Press, San Diego, California, U.S.A. 547 pp.

Bleeker, P.E. 1859. Enumerato Specierum Piscium hucusque in Archipelago Indico obervataum. Verhandelingen der Natuurkundige Vereeniging in Nederlandsch Indie, 6:1-276.

Carnevale, G., C. Sorbini, W. Landini, and A. Varola. 2002. Makaira cf. M. nigricans Lacepede, 1802 (Teleostei: Perciformes: Istiophoridae) from the Pietra Leccese, Late Miocene, Apulia, Southern Italy. Palaeontographia Italica, 88:63-75.

Collette, B.B., J.R. McDowell, and J.E. Graves. 2006. Phylogeny of recent billfishes (Xiphioidei). Bull. Mar. Sci., 79(3): 455-468.

Cope, E.D. 1887. Geology and paleontology. Amer. Naturalist, 21:1014-1019.

Cuvier, G. 1832. Tetrapturus indicus, Pp. 554-626 in G. Cuvier and A. Valenciennes. Histoire Naturelle Poissons, volume 8 (9, Des Scomberoides). F.G. Levrault, Paris. 509 pp.

Davie, P. 1990. Pacific marlins: anatomy and physiology. Massey Univ. Press, Palmerston North, New Zealand. vii + 88 pp.

Demere, T.A. and A. Berta. 2005. New skeletal material of Thalassoleon (Otaridae: Pinnipedia) from the Late Miocene-Early Pliocene (Hemphillian) of California. Bull. Fla. Mus. Nat. Hist., 45(4): 379-411.

Ehlig, P. 1979. The late Cenozoic evolution of the Capistrano Embayment. Pp. A38-A46 in (D.L. Fife ed.), Geologic Guide of San Onofre Nuclear Generating Station and Adjacent Regions of Southern California. Pacific Sections of AAPG, SEPM, and SEG, Guidebook 46.

Eschmeyer, W.N., E.S. Herald, and H. Hammann. 1983. A field guide to Pacific Coast fishes of North America. The Peterson Field Guide Series. Houghton Mifflin Company, Boston, Massachusetts, U.S.A. 336 pp.

Fierstine, H.L. 1998. Makaira sp., el. M. nigricans Lacepede, 1802 (Teleostei: Perciformes: Istiophoridae) from the Eastover Formation, late Miocene, Virginia, and a reexamination Istiophorus calvertensis Berry, 1917. J. Vert. Paleo., 18:30-42.

--. 1999. Makaira sp., cf. M. nigricans Lacepede, 1802 (Teleostei: Perciformes: Istiophoridae) from the Late Miocene, Panama, and its probable use of the Panama Seaway. J. Vert. Paleo., 19(3): 430-437.

--. 2001. Analysis and new records of billfish (Teleostei: Perciformes: Istiophoridae) from the Yorktown Formation, Early Pliocene of eastern North Carolina at Lee Creek Mine. Pp. 21-69 in (C.E. Ray, and D.J. Bohaska, eds.), 2001. Geology and Paleontology of the Lee Creek Mine, North Carolina, III. Smithsonian Contributions to Paleobiology, no. 90.

--. 2006. Fossil history of billfishes (Xiphioidei). Bull. Mar. Sci., 79(3): 433-453.

--and S.P. Applegate. 1968. Billfish remains from southern California with remarks on the importance of the predentary bone. Bull. South. Calif. Acad. Sci., 67(1): 29-39.

--and N. Voigt. 1996. Use of rostral characters for identifying adult billfishes (Teleostei: Perciformes: Istiophoridae and Xiphiidae). Copeia, 1996(1): 148-161.

--and B.J. Welton. 1988. A late Miocene marlin, Makaira sp. (Perciformes, Osteichthyes) from San Diego County, California, U.S.A. Tertiary Research, 10(1): 13-19.

--, S.P. Applegate, G. Gonzalez-Barba, T. Schwennicke, and L. Espinosa-Arrubarrena. 2001. A fossil blue marlin (Makaira nigricans Lacepede) from the middle facies of the Trinidad Formation, (Upper Miocene to Upper Pliocene), San Jose del Cabo Basin, Baja California Sur, Mexico. Bull. South. Calif. Acad. Sci., 100(2): 59-73.

Gregory, W.K. and G.M. Conrad. 1937. The comparative osteology of the swordfish (Xiphias) and the sailfish (Istiophorus). Amer. Mus. Novitates, 952:1-25.

Gudger, E.W. 1940. The alleged pugnacity of the swordfish and the Spearfishes as shown by their attacks on vessels. Mem. Royal Asiat. Soc. Bengal, 12:215-315 + 9 pls.

Ingle, Jr., J.C. 1979. Biostratigraphy and paleoecology of early Miocene through early Pleistocene benthonic and planktonic Foraminifera, San Joaquin Hills-Newport Bay-Dana Point area, Orange County, California. Pp. 53-77 in (C.J. Stuart ed.), Miocene Lithofacies and Depositional Environments, Coastal southern California and Northwestern Baja California. Pacific Section SEPM.

Jordan, D.S. and J.O. Snyder. 1901. Description of nine new species of fishes contained in museums of Japan. J. Coll. Sci., Imp. Univ. Tokyo, 33:1-497.

Lacepede, B.G.E. 1802. Histoire naturelle des poissons. 4:689-697.

Morton, D.M. (compiler), K.R. Bovard, and R.M. Alvarez. 2004. Preliminary digital geologic map of the Santa Ana 30-minute X 60-minute quadrangle, Southern California, scale 1:100,000, U.S. Geological Survey Open-File Report, 99-172, version 2.0.

Muller, J. 1844. Uber den Bau und die Grenzen der Ganoiden, und uber das naturliche System der Fische. Physikalich-Mathematische Abhandlungen der koninglichen Akademie der Wissenschaften zu Berlin, 1845:1175-216.

Nakamura, I. 1983. Systematics of billfishes (Xiphiidae and Istiophoridae). Publ. Seto Mar. Biol Lab., 28: 255-396.

--. 1985. An annotated and illustrated catalogue of marlins, sailfishes, spearfishes, and swordfishes known to date. Food and Agricultural Organization of the United Nations (FAO) Fisheries Synopsis, 125(5): 1-65.

Nelson, J.S., E.J. Crossman, H. Espinosa-Perez, L.T. Findley, C.R. Gilbert, R.N. Lea, and J.D. Williams. 2004. Common and Scientific Names of Fishes from the United States, Canada, and Mexico. 6th ed., Amer. Fish. Soc. Spec. Publ. 29, 386 pp.

Orrell, T.M., B.B. Collette, and G.D. Johnson. 2006. Molecular data support separate Scombroid and xiphioid clades. Bull. Mar. Sci, 79(3): 505-519.

Philippi, R.A. 1887. Sobre los tiburones y algunos otros peces de Chile. Annales del Universidad de Chile, 71:535-574.

Poey, F. 1860. Memorias sobre la historia de la Isla de Cuba, acompandas de sumarios latinos y extractos in frances etc., volume 2, Pp. 97-336. La Habana.

Robins, C.R. and D.P. deSylva. 1960. Descriptions and relationships of the longbill spearfish, Tetrapturus belone, based on western north Atlantic specimens. Bull. Mar. Sci. of the Gulf and Caribbean, 10(4): 383-413.

--and--. 1963. A new Western Atlantic spearfish, Tetrapturus pfluegeri, with a redescription of the Mediterranean Spearfish, Tetrapturus belone. Bull. Mar. Sci. of the Gulf and Caribbean, 13(1): 84-122.

Rojo, A.L. 1991. Dictionary of evolutionary fish osteology. CRC Press, Boca Raton, Florida. 273 pp.

Schultz, O. 1987. Taxonomische Neugruppieriung der Uberfamilie Xiphioidea (Pisces, Osteichthyes). Annalen Naturhistorisches Museum Wien, Serie A, fur Mineralogie und Petrographie, Geologie und Palaontologie, Anthropologie, und Prahistories, 89:95-202.

Shaw, G. and F.P. Nodder. 1792. Xiphias platypterus: the broadfinned swordfish. The Naturalist's Miscellany, 28:pages unnumbered, plate 88 pp.

Swainson, W. 1839. The natural history and classification of fishes, amphibians, and reptiles, or monocardian animals 2. Longman, Orme, Green and Longmans & John Taylor, London. 448 pp.

Tanaka, S. 1915. Figures and descriptions of the fishes of Japan including Riuku Islands, Bonin Islands, Formosa, Kurile Islands, Korea and southern Sakhalin, 19:319-342, Daiichi Shoin, Tokyo.

Vedder, J.G. 1972. Review of stratigraphic names and megafaunal correlation of Pliocene rocks along the southeast margin of the Los Angeles basin, California. Pp. 158-172 in (E.H. Stinemeyer, ed.). Pacific Coast Miocene Biostratigraphic Symposium. SEPM.

White, W.R. 1956. Pliocene and Miocene Foraminifera from the Capistrano Formation, Orange County, California. J. Paleo. 30:237-260.

Woodburne, M.O. and C.C. Swisher, III. 1995. Land mammal high-resolution geochronology, intercontinental overland dispersals, sea level, climate, and vicariance. Pp. 335-364 in (W.A. Berggren, D.V, Kent, M.-P. Aubry, and J. Hardenbol, eds.), Geochronolgy, Time Scales and Global Stratigraphic Correlation. Soc. Sed. Geol., Spec. Publ. 54.

Harry L. Fierstine

Biological Sciences Department, California Polytechnic State University, San Luis Obispo, California 93407, hfiersti@calpoly.edu and Research Associate, Department of Vertebrate Paleontology, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007
Table 1. Selected measurements of the skull of Makaira nigricans
Lacepede 1802, OCPC 31001, Oso Member, Capistrano Formation, late
Miocene, Orange County, California. See text for definition of
abbreviations. Measurements that were distorted during fossilization
are given as estimates (est.), and those characters affected by
abnormal development of the nutrient canals are noted as questionable
(?). Values indicated by an asterisk (*) were taken from computer
tomography (CT) scans and not directly from the specimen.

Bone or region of skull Measurements (mm)

Overall length of specimen 780.0
 Rostrum
Length (L) 570.0
[D.sub.1] 23.5
[W.sub.1] est. 35.1
[H.sub.1] (?)5.7 (*)
[N.sub.1] (?)4.1 (*)
[DD.sub.1] (?)8.7 (*)
[IC.sub.1] (?)2.6 (*)
[D.sub.2] 17.3
[W.sub.2] 26.3
[H.sub.2] (?)4.3 (*)
[N.sub.2] (?)2.8 (*)
[DD.sub.2] 16.5 (*)
[IC.sub.2] --
DZ 22.0
DVS 261.0
P 231.0
VSPM 324.0
 Left maxilla
MH est. 24.8
ML 51.5
MOL est. 200.0
MVH 15.5
MVW 14.5
M W est. 26.5
 Left quadrate
QH est. 65.7
QFIS est. 52.2
QAW est. 17.0
QM W 12.0
QM L 14.4
Q W 74.4
 Predentary
PD 18.2
PL 61.0
PW 30.2

Table 2. Variables (ratios) of Makaira nigricans Lacepede 1802.
OCPC 31001, Oso Member, Capistrano Formation, late Miocene,
California, compared with the mean (z), observed range (or),
and number of bones examined (n) for the same variables of
eight extant species of the family Istiophoridae. Abbreviations
for variables are explained in the Materials and Methods section
of text. Only variables of normally developed characters (without
question marks [?] in Table 1) are listed.

 I. platypterus (Shaw M. indica (Cuvier
 OCPC and Nodder 1792) 1832
Ratios 31001 [bar.x] (or) n [bar.x] (or) n

Rostrum

D1/W1 .67 .68(.58-.78)31 .72(.66-.78)10
D2/W2 .66 .64(.55-.75)30 .68(.58-.77)10
D2/VSPM .05 .03(.03-.04)25 .06(0.5-.08)8
W2/VSPM .08 .05(.04-.06)24 .09(.07-.10)8
DVS/VSPM .81 .72(.48-.97)23 .72(.48-.94)8
P/VSPM .71 .58(.45-.83)17 .53(.48-.60)8
P/D2 13.4 18.8(13.0-23.2)18 9.0(7.3-10.5)10
P/W2 8.8 11.6(8.7-14.0)17 6.1(5.1-7.3)10
DZ/P .10 1.4(.76-2.5)18 .30(.10-.50)9
DZ/W2 .84 19.5(9.9-29.1)30 1.8(.71-3.0)9

Maxilla

ML/MOL .26 .31(.23-.35)9 --
MW/MOL .13 .12(.08-.14)9 --
MW/ML .51 .39(.25-.57)14 --
MH/ML .48 .33(.26-.47)14 --
MVW/MVH .94 1.4(.95-2.4)9 --
MVW/ML .31 .22(.17-.36)9 --
MVW/MW .55 .55(.48-.63)9 --
MVW/MH .53 .64(.59-.75)9 --

Predentary

PW/PL .50 .50(.23-.63)21 .54(.48-.62)5
PD/PL .30 .27(.20-.37)21 .38(.30-.41)5
PD/PW .61 .56(.48-1.0)21 .70(.63-.81)5

Quadrate

QAW/QH .26 .17(.15-.20)11 .29(.28-.31)2
QMW/QAW .71 .68(.58-.81)11 .85(.83-.88)2
QAW/QHS .33 .29(.24--.39)11 .44(.44-.45)2
QMW/QHS .23 .19(.17-.23)11 .38(.38-.38)2
QMW/QML .83 .73(.62-.80)11 1.1(1.1-1.1)2

 M. nigricans
 Lacepede 1802 T. albidus Poey 1860
Ratios [bar.x] (or) n [bar.x] (or) n

Rostrum

D1/W1 .70(.59-.80)41 .62(.56-.66)13
D2/W2 .64(.54-.83)41 .53(.47-.61)14
D2/VSPM .04(.04-.05)35 .04(.03-.05)12
W2/VSPM .07(.05-.08)35 .07(.06-.09)12
DVS/VSPM .86(.54-1.0)34 .80(.66-.95)9
P/VSPM .51(.38-.87)33 .53(.42-.66)11
P/D2 11.9(8.9-20.2)41 14.2(10.9-21.3)12
P/W2 7.6(5.9-12.3)41 7.6(5.7-10.3)12
DZ/P .04(0-.11)37 2.4(1.5-3.3)9
DZ/W2 .30(.00-.85)37 18.6(14.6-21.7)10

Maxilla

ML/MOL .20(.17-.23)14 .26(.23-.29)10
MW/MOL .13(.13-.13)5 .13(.12-.13)8
MW/ML .64(.60-.70)5 .47(.44-.51)8
MH/ML .43(.38-.49)14 .38(.34-.45)10
MVW/MVH 1.2(1.1-1.3)3 1.2(.80-1.8)3
MVW/ML .36(.35-.37)3 .20(.18-.24)3
MVW/MW .56(.53-.60)3 .44(.40-.48)3
MVW/MH .90(.81-.96)3 54(.50-.58)3

Predentary

PW/PL .65(.45-1.1)23 .41(.34-.57)15
PD/PL .36(.26-.58)23 .24(.20-.33)15
PD/PW .56(.48-.61)23 .59(.53-.65)15

Quadrate

QAW/QH .23(.19-.27)22 .21(.18-.24)17
QMW/QAW .77(.57-.92)22 .73(.48-.88)18
QAW/QHS .36(.30-.43)21 .35(.30-.40)18
QMW/QHS .27(.22-.35)21 .25(.19-.30)18
QMW/QML .86(.63-1.0)22 .83(.53-1.0)18

 T. angust-
 irostris Tanaka T. audas Philippi
 1915 1887
Ratios [bar.x] (or) n [bar.x] (or) n

Rostrum

D1/W1 .64(.57-.70)3 .68(.59-.80)13
D2/W2 .61(.58-.64)3 .61(.52-.67)13
D2/VSPM .15(.13-.19)3 .04(.03-.05)12
W2/VSPM .24(.20-.30)3 .06(.05-.08)12
DVS/VSPM .31(0-.52)3 .76(.64-.94)10
P/VSPM .39(.30-.45)3 .48(.38-.57)12
P/D2 2.7(2.3-3.3)3 12.9(10.8-16.1)12
P/W2 1.6(1.3-2.1)3 7.8(6.7-9.5)11
DZ/P 0(0)3 .93(.30-2.0)9
DZ/W2 0(0)3 5.8(2.5-9.5)11

Maxilla

ML/MOL -- .26(.25-.27)2
MW/MOL -- 0.12
MW/ML -- .47(.45-.49)2
MH/ML -- .37(.36-.37)2
MVW/MVH -- 1.2(.96-1.5)2
MVW/ML -- .28(.25-.31)2
MVW/MW -- .60(.51-.69)2
MVW/MH -- .77(.68-.85)2

Predentary

PW/PL .60(.54-.69)4 .42(.33-.51)13
PD/PL .59(.52-.69)4 .26(.22-.30)13
PD/PW .99(.97-1.0)4 .60(.53-.72)13

Quadrate

QAW/QH (.16)l .21(.20-.22)4
QMW/QAW (.65)l .71(.67-.77)4
QAW/QHS -- .38(.37-.39)2
QMW/QHS -- .28(.27-.28)2
QMW/QML (.56)l .79(.65-1.0)4

 T. pfluegeri Robins
 & de Sylva 1963
Ratios [bar.x] (or) n

Rostrum

D1/W1 .62(.59-.64)2
D2/W2 .65(.65)2
D2/VSPM .05(.05-.06)2
W2/VSPM .08(.07-.09)2
DVS/VSPM .02(0-.04)2
P/VSPM .55(.55-.56)2
P/D2 10.6(9.8-11.3)2
P/W2 6.9(6.4-7.4)2
DZ/P 0(0)2
DZ/W2 0(0)2

Maxilla

ML/MOL .33(.33-.33)2
MW/MOL .08(.08-.08)2
MW/ML .24(.23-.24)2
MH/ML .33(.31-.34)2
MVW/MVH --
MVW/ML --
MVW/MW --
MVW/MH --

Predentary

PW/PL (.65)1
PD/PL (.60)l
PD/PW (.92)l

Quadrate

QAW/QH (.17)1
QMW/QAW (.62)l
QAW/QHS (.30)1
QMW/QHS (.18)1
QMW/QML (.71)1
COPYRIGHT 2008 Southern California Academy of Sciences
No portion of this article can be reproduced without the express written permission from the copyright holder.
Copyright 2008 Gale, Cengage Learning. All rights reserved.

Article Details
Printer friendly Cite/link Email Feedback
Author:Fierstine, Harry L.
Publication:Bulletin (Southern California Academy of Sciences)
Article Type:Report
Geographic Code:1U9CA
Date:Aug 1, 2008
Words:5322
Previous Article:First occurrence of a Pacific crevalle jack, Caranx caninus, north of San Diego, California.
Next Article:An initial carnivore survey of Griffith Park, Los Angeles, California.
Topics:


Related Articles
A Fossil Blue Marlin (Makaira nigricans Lacepede) from the Middle Fades of the Trinidad Formation (Upper Miocene to Upper Pliocene), San Jose del...
Decapod crustaceans from the Puente formation (late middle to early late Miocene), California: a possible mass death.
Fossil pollen records of extant angiosperms in China.
Toward identification of larval sailfish (Istiophorus platypterus), white marlin (Tetrapturus albidus), and blue marlin (Makaira nigricans) in the...

Terms of use | Copyright © 2018 Farlex, Inc. | Feedback | For webmasters