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OCCASIONAL PAPERS OF THE CALIFORNIA ACADEMY OF SCIENCES 
Number 159 
Miocene, Santa Barbara County; CAS 55421 (SU 509, 197), complete left counterpart (pi. 25, incorrect¬ 
ly labeled pi. 24 in text) and five specimens with whereabouts unknown, SU 33, 220, 276, 296, and 510. 
Referred Specimens of fE. iordani in Jordan 0921ah None. 
Referred Specimens and Holotvpe of f E. hooveri (Jordan in Jordan and Gilbert 1920) reidentified bv David 
(4943) as fE. iordani : From Lompoc, Monterey Formation, Late Miocene, Santa Barbara County; CAS 
70080 (SU 512, 152), holotype, complete right counterpart (pi. 26). No referred specimens. See Remarks 
section. 
Referred Specimens of fE. hooveri in Jordan (4921a) : From Lompoc, Monterey Formation, Late Miocene, 
Santa Barbara County; two specimens with whereabouts unknown, SU 53, partial left counterpart (pi. 11) 
and SU 547. 
Referred Specimens of fE. iordani in David 11943k From Lompoc, Monterey Formation, Late Miocene, Santa 
Barbara County; CAS 70080 (SU 512, 152), holotype of fii. hooveri, right counterpart; CAS 55421 (SU 
509, 197, (text-fig. 36b), fairly complete left counterpart; CAS 70083 (SU 199), complete right counter¬ 
part; SU 198, left counterpart (see Remarks). Also, LACM (CIT) 10235, left counterpart (text-fig. 36a). 
Remarks : Gilbert (1909) published a preliminary note on f E.jordani, although figured, no name was assigned. 
Jordan in Jordan and Gilbert (1920) listed the specimen number of the holotype of fii. hooveri as SU 512 
in the text, but in the legend of plate 26 as SU 307. SU 198 is in the CAS collection, but no CAS number 
and not in its database. Chanet and Schultz (1994:102) mentioned that f Evesthes jordani was present in 
the Monterey Formation (Middle Miocene) of California and that fii. hooveri was too incomplete for 
comparison to the pleuronectiforms in their study. 
Genus Citharichthys Bleeker 1862 
Citharichthys sordidus (Girard 1854b) 
Selected References (fossils only) 
Citharichthys sordidus (Girard): Fitch: 1967:10. 
Citharichthys sordidus (Girard): Fitch and Reimer 1967:79, 82-84, table 1, fig. 17. 
Citharichthys sordidus (Girard): Fitch: 1968:11. 
Citharichthys sordidus (Girard): Downs 1968:53, text-fig. 25F. 
Citharichthys sordidus (Girard): Fitch and Lavenberg 1971:43. 
Citharichthys sordidus (Girard): Nolf: 1985:104. 
Type Specimen : Extant, Psettichthys sordidus Girard 1854, no types known (Eschmeyer 1998:1580). 
Type Locality : San Francisco, California. 
Referred Specimens in Fitch 11967:10k No specific specimens. Otoliths of C. sordidus are abundant in south¬ 
ern California Pliocene and Pleistocene deposits. 
Referred Specimens in Fitch and Reimer ( 1967k From LACMIP locality 423 (= LACM locality 3245), Signal 
Hill (= Interstate 405 and Cherry Avenue, Long Beach), Fernando Formation, Plio-Pleistocene, Los 
Angeles County; seven otoliths (one shown in fig. 17) (see Remarks). Bothidae. 
Referred Specimens in Fitch 11968:Ilk Same information as in Fitch (1967) above. 
Referred Specimens in Downs 11968k One otolith (text-fig. 25F). The figure legend gives the general age as 
Pliocene and Pleistocene for the specimen with no specific locality. 
Referred Specimens in Fitch and Lavenberg 11971:43k The authors state otoliths of C. sordidus have been 
identified from many Pliocene deposits throughout California (see Remarks). 
Referred Specimens in Nolf (4985:104k Cites Fitch (1967) that otoliths of C. sordidus have been reported 
from the Pliocene of California. 
Remarks : According to Powell (1998:70-71), LACMIP locality 423 (= LACM locality 3245) is in Pleistocene 
strata, therefore a Pliocene record of C. sordidus from this locality is questionable, especially since no 
other Neogene locality was given. 
