Hostname: page-component-586b7cd67f-gb8f7 Total loading time: 0 Render date: 2024-11-22T05:18:21.520Z Has data issue: false hasContentIssue false

New Eocene marine bivalves from Baja California Sur, Mexico

Published online by Cambridge University Press:  14 July 2015

Richard L. Squires
Affiliation:
Department of Geological Sciences, California State University, Northridge 91330
Robert Demetrion
Affiliation:
8839 Katherine Avenue, Panorama City, California 91402

Abstract

A new genus, a new subgenus, and five new species of pterioid bivalves are described from shallow-marine faunas in the middle lower to middle Eocene Bateque Formation in the vicinity of Laguna San Ignacio to about 105 km southward, Pacific coast of Baja California Sur, Mexico. Batequeus n. gen. is a medium-sized pectinid with equally convex valves, a short byssal notch, anterior auricles smaller than the posterior ones, the left valve with numerous very closely spaced radial riblets that show the imbricated growth lines very well, the right valve with about 30 low, flat-topped radial ribs that can be grooved, and intercalary ribs on both valves. It is only known from its type species, Batequeus mezquitalensis n. sp., which is from the middle Eocene part of the Bateque Formation. Spondylus batequensis n. sp., a very spinose species, is from the middle lower Eocene part of the Bateque Formation and is only the second reported Spondylus from the lower Eocene of the west coast of North America. Pycnodonte (Phygraea) pacifica n. sp., a species characterized by a radial sulcus that originates in the umbo area, occurs in both the middle lower and middle Eocene parts of the Bateque Formation. Phygraea has not been reported previously from the west coast of North America. Pycnodonte (Pegma) n. subgen. has a plicate left valve with a large attachment area (that can cover the entire valve) and a right valve that usually has an inflated smooth central area surrounded by plicate margins. It is only known from its type species, Pycnodonte (Pegma) bajaensis n. sp., which occurs in both the middle lower and middle Eocene parts of the Bateque Formation. Cubitostrea mezquitalensis n. sp., a strongly ornamented species, is from the middle Eocene part of the Bateque Formation and is the first occurrence of this genus from the west coast of North America.

Type
Research Article
Copyright
Copyright © The Paleontological Society 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Anderson, F. M. 1905. A stratigraphic study in the Mount Diablo Range of California. California Academy of Sciences, Proceedings, Ser. 3, 2:155248.Google Scholar
Arnold, R. 1906. The Tertiary and Quaternary pectens of California. U.S. Geological Survey Professional Paper U.S. Geological Survey Professional Paper, 264 p.CrossRefGoogle Scholar
Baldwin, E. M. 1964. Geology of the Dallas and Valsetz quadrangles, Oregon. State of Oregon, Department of Geology and Mineral Industries Bulletin 35, 56 p.Google Scholar
Berggren, W. A., Kent, D. V., Flynn, J. J., and van Couvering, J. A. 1985. Cenozoic geochronology. Geological Society of America Bulletin, 96:14071418.2.0.CO;2>CrossRefGoogle Scholar
Conrad, T. A. 1834. Descriptions of new Tertiary fossils from the southern states. Journal of the Academy of Natural Sciences of Philadelphia, 7:130157.Google Scholar
Conrad, T. A. 1840. Fossils of the Medial Tertiary of the United States, Vol. 2. Judah Dobson, Philadelphia, p. 3356.Google Scholar
Conrad, T. A. 1848. Observations on the Eocene formation, and descriptions of one hundred and five new fossils of that period, from the vicinity of Vicksburg, Mississippi, with an Appendix. Academy of Natural Sciences of Philadelphia, Journal, 2nd ser., 1(Pt. 2):111134.Google Scholar
Cossmann, A. E. M., and Pissarro, G. 1904-1906. Iconographie complète des coquilles fossiles de l'Éocène des environs de Paris. Vol. 1. H. Bouillant, Paris, 45 Pls.Google Scholar
Davies, A. M. 1971. Tertiary Faunas—A Text-book for Oilfield Paleontologists and Students of Geology. Vol. 1. The Composition of Tertiary Faunas. Revised and updated by F. E. Eames. George Allen and Unwin, London, 471 p.Google Scholar
Deshayes, G. P. 1824-1837. Description des coquilles fossiles des environs de Paris, Vol. 1(Conchifères):1392 (1824-1832); Atlas (Pt. 1):Pls. 1-65 (1837). Chez l'auteur and others, Paris.Google Scholar
Dockery, D. T. III. 1982. Lower Oligocene Bivalvia of the Vicksburg Group in Mississippi. Mississippi Department of Natural Resources Bureau of Geology Bulletin 123, 261 p.Google Scholar
Fischer de Waldheim, G. 1835. Lettre à M. le Baron de Férussac sur quelques genres de coquilles du Muséum Demidoff et en particulier sur quelques fossiles de la Crimée. Société Impériale des Naturalistes Moscow Bulletin, 8:101119.Google Scholar
Gabb, W. M. 1869. Cretaceous and Tertiary Fossils. Geological Survey of California, Vol. 1, Palaeontology. Caxton Press, Philadelphia, 299 p.Google Scholar
Gibson, T. G. 1987. Miocene and Pliocene Pectinidae (Bivalvia) from the Lee Creek Mine and adjacent areas, p. 31112. In Ray, C. E. (ed.), Geology and Paleontology of the Lee Creek Mine, North Carolina, Pt. 2. Smithsonian Contributions to Paleobiology, Number 61.Google Scholar
Givens, C. R. 1974. Eocene molluscan biostratigraphy of the Pine Mountain area, Ventura County, California. University of California Publications in Geological Sciences, 109:1107.Google Scholar
Glawe, L. N. 1967. Stop 16—Lone Star Cement Company quarry at St. Stephens Bluff on Tombigbee River 2.2 miles northeast of St. Stephens, Washington County, Alabama, p. 107113. In Jones, D. E. (ed.), Geology of the Coastal Plain of Alabama. Geological Society of America 80th Annual Meeting, New Orleans, Louisiana, Alabama Geological Society Guidebook, University, Alabama.Google Scholar
Gray, J. E. 1826. On a recent species of the genus Hinnita of De France, and some observations on the shells of the monomyaires of Lamarck. Annals of Philosophy, new ser., 12:103106.Google Scholar
Gümbel, C. W. 1861. Geognostische Beschreibung des bayerischen Alpengebirges und seines Vorlandes. Bavaria, K. Bayerisches Oberbergamt, Geognostische Abteilung Justus Perte. Gotha, 950 p.Google Scholar
Hanna, M. A. 1927. An Eocene invertebrate fauna from the La Jolla quadrangle, California. University of California Publications, Bulletin of the Department of Geological Sciences, 16:247398.Google Scholar
Harry, H. 1985. Synopsis of the supraspecific classification of living oysters (Bivalvia: Gryphaeidae and Ostreidae). The Veliger, 28:121158.Google Scholar
Harry, H., and Dockery, D. T. III. 1983. Notes on the lower Oligocene oysters of Mississippi. Mississippi Geology, 4:714.Google Scholar
Hertlein, L. G. 1933. A new gryphaeoid oyster from the Eocene of California. Transactions of the San Diego Society of Natural History, 7:277282.Google Scholar
Hertlein, L. G. 1969. Family Pectinidae Rafinesque, 1815, p. N348N373. In Moore, R. C. and Teichert, C. (eds.), Treatise on Invertebrate Paleontology, Pt. N, Vol. 1, Mollusca 6, Bivalvia. Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Linné, C. von. 1758. Systema naturae per regna tria naturae. Editio decima, reformata, Regnum animale, Vol. 1. Holmiae, 1327 p.Google Scholar
McLean, H., Hausbeck, B. P., and Knapp, J. H. 1985. Reconnaissance geologic map of part of the San Isidro quadrangle, Baja California Sur, Mexico. U.S. Geological Survey, Miscellaneous Field Studies Map MF-1799.Google Scholar
Moore, E. J. 1984. Tertiary marine pelecypods of California and Baja California: Propeamussiidae and Pectinidae. U.S. Geological Survey Professional Paper 1228-B, 112 p.CrossRefGoogle Scholar
Moore, E. J. 1987. Tertiary marine pelecypods of California and Baja California: Plicatulidae to Ostreidae. U.S. Geological Survey Professional Paper 1228-C, 53 p.CrossRefGoogle Scholar
Morton, S. G. 1834. Synopsis of the organic remains of the Cretaceous group of the United States. Appendix. Catalogue of the fossil shells of the Tertiary formation of the United States, by T. A. Conrad. Philadelphia, 88 p.Google Scholar
Müller, O. F. 1776. Zoologiae Danicae prodromus, seu animalium Daniae et Novegiae indigenarum, characteres, nomina, et synonyma imprintis popularium, Vol. 32. Havinae, Copenhagen, 282 p.Google Scholar
Newell, N. D. 1965. Classification of Bivalvia. American Museum Novitates, 2206:125.Google Scholar
Okada, H., and Bukry, D. 1980. Supplementary modification and introduction of code numbers to the low-latitude coccolith biostratigraphic zonation. Marine Micropaleontology, 5:321325.CrossRefGoogle Scholar
Packard, E. L. 1922. New species from the Cretaceous of the Santa Ana Mountains. University of California Publications, Bulletin of the Department of Geological Sciences, 13:413462.Google Scholar
Pomeroll, C., and Feugueur, L. 1974. Bassin de Paris. 2nd ed.Guides Géologiques Régionaux. Masson et cie, Paris, 216 p.Google Scholar
Rafinesque, C. S. 1815. Analyse de la nature, ou tableau de l'universe et des corps organisées. Palermo, 224 p.CrossRefGoogle Scholar
Röding, P. F. 1798. Museum Boltenianum sive catalogus cimeliorum e tribus regnis naturae quae olim collegerat. Bolten, J. F., M.D., ed. Pars Secunda. Johan Cristi Trappii, Hamburg, 199 p.Google Scholar
Sacco, F. 1897. Pelecypoda (Ostreidae, Anomiidae e Dimyidae): of L. Bellardi and F. Sacco, 1872-1904, I molluschi dei terreni Terziarii de Piemonte e della Liguria, 30 pts. separately paged, pt. 23. Carlo Clausen, Torino, 66 p.Google Scholar
Schmidt, F. C. 1818. Versuch über die beste Einrichtung zur Aufstellung, Behandlung und Aufbewahrung der verschiedenen Naturkörper und Gegenstande der Kunst. Gotha, 252 p.Google Scholar
Squires, R. L. 1984. Megapaleontology of the Eocene Llajas Formation, Simi Valley, California. Los Angeles County Natural History Museum Contributions in Science, 350, 76 p.Google Scholar
Squires, R. L. 1987. Eocene molluscan paleontology of the Whitaker Peak area, Los Angeles and Ventura Counties, California. Los Angeles County Natural History Museum Contributions in Science, 388, 93 p.Google Scholar
Squires, R. L. 1988. Rediscovery of the type locality of Turritella andersoni and its geologic age implications for West Coast Eocene strata, p. 203208. In Filewicz, M. V. and Squires, R. L. (eds.), Paleogene Stratigraphy, West Coast of North America. Pacific Section, Society of Economic Paleontologists and Mineralogists, Volume 58, Los Angeles.Google Scholar
Squires, R. L. 1989. Middle Eocene rocky nearshore molluscs, Tejon Formation, Tehachapi Mountains, California. The Western Society of Malacologists Annual report, 21:18.Google Scholar
Squires, R. L., and Demetrion, R. 1990. New early Eocene marine gastropods from Baja California Sur, Mexico. Journal of Paleontology, 64:99103.CrossRefGoogle Scholar
Stainforth, R. M., Lamb, J. L., Luterbacher, H., Beard, J. H., and Jeffords, R. M. 1975. Cenozoic planktonic foraminiferal zonation and characteristic index forms. University of Kansas Paleontological Contributions, Article University of Kansas Paleontological Contributions, Article, 425 p.Google Scholar
Stenzel, H. B. 1959. Cretaceous oysters of southwestern North America. Congreso Geologica Internacional 20th sesión, Ciudad de México, 1956. El sistema Cretacio, 1:1537.Google Scholar
Stenzel, H. B. 1971. Oysters, p. N953N1197. In Moore, R. C. and Teichert, C. (eds.), Treatise on Invertebrate Paleontology, Pt. N, Vol. 3, Mollusca 6, Bivalvia. Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Stenzel, H. B., Krause, E. K., and Twining, J. T. 1957. Pelecypoda from the type locality of the Stone City Beds (middle Eocene) of Texas. The University of Texas Publication 5704, 237 p.Google Scholar
Stephenson, L. W. 1936. New Upper Cretaceous Ostreidae from the Gulf region. U.S. Geological Survey Professional Paper 186-A, 8 p.CrossRefGoogle Scholar
Sundberg, F., and Riney, B. 1984. Preliminary report on the Upper Cretaceous macro-invertebrate faunas near Carlsbad, California, p. 103107. In Abbott, P. L. (ed.), Upper Cretaceous Depositional Systems Southern California-Northern Baja California. Pacific Section, Society of Economic Paleontologists and Mineralogists, Volume and Guidebook no. 36, Los Angeles.Google Scholar
Vaughan, T. W. 1945. American Paleocene and Eocene larger Foraminifera. Geological Society of America Memoir 9, Pt. 1, 175 p.Google Scholar
Vokes, H. E. 1939. Molluscan faunas of the Domengine and Arroyo Hondo Formations of the California Eocene. Annals of the New York Academy of Sciences, 38:1246.CrossRefGoogle Scholar
Vyalov, O. S. 1936. Sur la classification des huǐtres. Académie des Sciences URSS, Comptes-rendus (Doklady), new ser., 4:1720.Google Scholar
Ward, L. W. 1985. Stratigraphy and characteristic mollusks of the Pamunkey Group (lower Tertiary) and the Old Church Formation of the Chesapeake Group—Virginia Coastal Plain. U.S. Geological Survey Professional Paper U.S. Geological Survey Professional Paper, 78 p.CrossRefGoogle Scholar
Wiedey, L. W. 1928. Notes on the Vaqueros and Temblor Formations of the California Miocene with descriptions of new species. San Diego Society of Natural History Transactions, 5:95182.Google Scholar