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OCCASIONAL PAPERS OF THE CALIFORNIA ACADEMY OF SCIENCES 
Number 159 
According to Powell (1998:70-71), LACMIP locality 423 (= LACM locality 3245) is in Pleistocene stra¬ 
ta, therefore a Pliocene record of G. tineatus from this locality is questionable. 
Genus Pogonias Lacepede 1801 
’fPogonias stringeri Takeuchi and Huddleston 2008b: 71-74, figs. 3,4 
Figure 83 
Type Specimen : fPogonias stringeri Takeuchi and Huddleston 2008b, holotype, LACM 151868, right saccu¬ 
lar otolith (figs. 3, 4A, B). 
Type Locality : LACM locality 6602, upper Olcese Sand, part of the Temblor Group, late Early Miocene, south¬ 
eastern San Joaquin Basin, Kern County. 
Paratvpe : LACM 151869, right saccular otolith (figs. 4C, D); LACM 151870, right saccular otolith (figs. 
4E,F). 
Figure 83. -fPogonias stringeri Takeuchi and Huddleston 2008b holotype, LACM 151868 [(from image provided by Gary Takeuchi 
(LACM)]; scale bar equals 5 mm. 
Genus Roncador Jordan and Gilbert 1880b 
Roncador stearnsii (Steindachner 1875) 
Selected References 
Roncador stearnsii (Steinachner 1875): Fitch and Reimer 1967: 1967:79, 84, 87, fig. 2, table 1. 
Type Specimen : Extant, Corvina stearnsii Steindachner, holotype, MCZ 10840 etal. (Eschmeyer 1998:1602). 
Type Locality : San Diego, California. 
Referred Specimens in Fitch and Reimer (1967) : From LACMIP locality 423 (= LACM locality 3245), Signal 
Hill (= Interstate 405 and Cherry Avenue, Long Beach), Fernando Formation, Plio-Pleistocene, Los 
Angeles County; 15 otoliths (see Remarks). 
Distribution of Neogene R. stearnsii outside of California : None known. 
Remarks : According to Powell (1998:70-71), LACMIP locality 423 (= LACM locality 3245) is in Pleistocene 
strata, therefore a Pliocene record of R. stearnsii from this locality is questionable. 
