Rl. Squires et Lr. Saul, REVIEW OF THE BIVALVE GENUS PLICATULA FROM CRETACEOUS AND LOWER CENOZOIC STRATA OF CALIFORNIA AND BAJA-CALIFORNIA, Journal of paleontology, 71(2), 1997, pp. 287-298
The Cretaceous and early Cenozoic species of the shallow-marine, warm-
water bivalve Plicatula from California (United States) and Baja Calif
ornia (Mexico) are reviewed, and three new species are named. All of t
hese species are representatives of Plicatula and not of the closely r
elated taxon Harpax, which is associated with high-latitude and cool-w
ater regions. The earliest-known Cretaceous species of Plicatula from
the study area is P. variata Gabb, 1864, from Lower Cretaceous (Hauter
ivian Stage) strata in northern California, and our studies show it to
be conspecific with Plicatula onoensis Anderson, 1958. Plicatula alli
soni new species is from Lower Cretaceous (Albian Stage) strata in Baj
a California, Mexico. Plicatula modjeskaensis new species is from Uppe
r Cretaceous (Turonian Stage) strata in the Santa Ana Mountains, south
ern California. A possible new species from the same strata is also me
ntioned. A poorly preserved specimen of Plicatula? sp. is known from U
pper Cretaceous (upper Campanian to lower Maastrichtian) strata in nor
thern California. The only Paleocene species of Plicatula from the stu
dy area is P. ostreiformis Stanton, 1896, from lower Paleocene strata
of Lake County, northern California, and our studies show it to be con
specific with Ostrea buwaldana Dickerson, 1914. The only previously de
scribed Eocene species of Plicatula from the study area is P. juncalen
sis Squires, 1987, from lower middle Eocene (''Capay Stage'') strata o
f Los Angeles County, southern California. Plicatula surensis new spec
ies is from middle lower Eocene (''Capay Stage'') strata in Baja Calif
ornia Sur, Mexico. In addition, there is a Plicatula? sp. from Eocene
strata of Baja California Sur, Mexico. Although Plicatula is of uncomm
on occurrence north of Baja California, its thermophilic trait makes i
t useful in recognizing periods of warm climate.