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Squires—Northeast Pacific Oniscidia


gastropods that originated in the OldWorld Tethys Sea region. These particular gastropods diversified during warm times, especially during the Paleocene (PETM), early Eocene (EECO), and middle Eocene (Squires, 1987), as well as the early Miocene and early middle Miocene (MMCO) (Fig. 4). As discussed earlier, it is likely that Oniscidia was not a shallow-marine nearshore dweller. It preferred to live in subtidal offshore depths, which would have inherently been slightly cooler. Although Oniscidia seems to have virtually ‘disappeared’ from the fossil record, or was diminished greatly during warm times, it was present, most likely, in adjacent, deeper waters. During cool-ocean times, therefore, Oniscidia diversified somewhat. As depicted in Figure 4, Oniscidia was moderately


widespread in the early Miocene, with occurrences in northern Europe, southwest India, New Zealand, the Caribbean Sea region, and Florida. The closure of the western Tethys seaway (TTE) in the middle Miocene severely curtailed the distribution of Oniscidia. Starting in the late Miocene and continuing into the Pliocene, Oniscidia became restricted to the Caribbean Sea region and Florida. In the Pleistocene, Oniscidia dispersed into the western Pacific and, to a lesser degree, into the central Pacific. Formation of the Panama Land Bridge at the end of the Pliocene (Leigh et al., 2013) would have impeded dispersal of Oniscidia from the Caribbean region into the west coast of North America. Intermittent marine connections between the Pacific and Atlantic sides of the land bridge probably continued between these two areas, however, during high sea levels in middle interglacial times (Beu, 2001). Oniscidia has about 30 living species, found mostly in the western Pacific (especially in Taiwan and the Philippine Islands) and, to a lesser degree, in the Caribbean Sea, western Atlantic, and South Africa and Madagascar regions (Dance and Poppe, 1999). The long distances involved for the dispersals of Oniscidia


801


South American Neogene mollusks. J. DeMouthe (CAS) and A. Hendy (LACMIP) facilitated loans. T.J. DeVries and L.T. Groves critically reviewed the manuscript and gave valuable comments.


References


Adegoke, O.S., 1977, Stratigraphy and paleontology of the Ewekoro Formation (Paleocene) of southwestern Nigeria: Bulletins of American Paleontology, v. 71, p. 1–379.


Anderson, F.M., 1928, Notes on lower Tertiary deposits of Colombia and their molluscan and foraminiferal fauna: Proceedings of the California Academy of Sciences, ser. 4, v. 17, p. 1–29.


Anderson, F.M., and Hanna, G.D., 1935, Cretaceous geology of Lower California: Proceedings of the California Academy of Sciences, ser. 4, v. 23, p. 1–34.


Bayan, F., 1870, Études Faites dans la Collection de l’Ecole des Mines sur des Fossils Nouveaux ou mal connus. Pt. 1. Mollusques Tertiaries: Paris, Savyo, 80 p.


Beu, A.G., 1976, Revision of the southwest Pacific species of Morum (Oniscidia) (Gastropod: Cassidae): Journal of the Malacological Society of Australia, v. 3, p. 223–231.


Beu, A.G., 2001, Gradual Miocene to Pleistocene uplift of the Central American Isthmus: evidence from tropical American tonnoidean gastropods: Journal of Paleontology, v. 75, p. 706–720.


Beu, A.G., and Maxwell, P.A, 1990, Cenozoic Mollusca of New Zealand: New Zealand Geological Survey Paleontological Bulletin, v. 58, 518 p.


Boettger, O., 1875, Die Fossilen Mollusken der Eocänformation auf der Insel Borneo: Palaeontographica, Supplement 3, 59 p.


Bouchet, P., 2002, Protoconchs, dispersal, and tectonic plates biogeography: new Pacific species of Morum (Gastropoda: Harpidae): Journal of Conchology, v. 37, p. 533–549.


Bouchet, P., 2014, World register of marine species: <http://www.mar- inespecies.org> (accessed September, 2017).


Brocchi, G.B., 1814, Conchiologia Fossile Subappennina con Osservazioni Geologiche sugli Appennini e sul suolo Adiacente: Milano, Dalla Stamperia Reale, v. 2, p. 241–712.


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into the central Pacific argue for planktotrophic larvae. Although Emerson (1990) interpreted that the modern-day distribution of Oniscidia, which is largely restricted to continental margins and large islands, represents the relicts (remnants) of the ancient tropical Tethyan seaway, Bouchet (2002) rejected this model of vicariance events. He interpreted that the recent distribution of Oniscidia is the result of planktonic dispersal of larvae. The biogeographic history of tridacnine bivalves


(Harzhauser et al., 2008) is similar to that of Oniscidia. The lineages of both groups are rooted in the Paleogene of the Old World Tethys Sea, and starting in the late Oligocene and early Miocene, they both dispersed eastward and eventually became elements of the western Pacific region.


Acknowledgments


M. Perrilliat and the staff at IGM provided a replica of a speci- men from the Sepultura Formation. D. Morris and the staff at Oviatt Library-Interlibrary Loan of California State University, Northridge obtained some copyrighted journal papers. A.G. Beu (New Zealand Geological Survey, Lower Hutt) and L.T. Groves (Malacology Department, Natural History Museum of Los Angeles County) provided key references. T.J. DeVries (Burke Museum of Natural History and Culture, University of Washington, Seattle, Washington) shared his knowledge of


Chabaglian, J., 1959, Le Paléocene dans l’Ouest du Sénégal. Étude paléonto- logique: Annales de la Faculté des Sciences de l’Université de Dakar, v. 4, p. 133–187.


Clark, B.L., and Durham, J.W., 1946, Eocene faunas from Bolivar, Colombia: Geological Society of America Memoir, v. 16, 126 p.


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: Journal of the Academy of Natural Sciences of Philadelphia, ser. 2, v. 1 (pt. 2), p 111–134.


Cossmann, A.E.M., and Pissarro, G., 1927, The Mollusca of the Ranikot Series. Part 1. Cephalopoda and Gastropoda: Memoirs of the Geological Society of India, Palaeontologica Indica, n. ser., v. 3, Memoir 1, p 1–82.


Cox, L.R., 1960, General characteristics of Gastropoda, in Moore, R.C., ed., Treatise on Invertebrate Paleontolgy, Pt. I, Mollusca 1: Boulder, Colorado and Lawrence, Kansas, Geological Society of America and University of Kansas Press, p. I84–I169.


Cuvier, G. L. C., 1797, Tableau Élementaire de l’Histoire Nautrelle des Animaux [des Mollusques]: Paris, Baudonin, 710 p.


Dall, W.H., 1909, The Miocene of Astoria and Coos Bay, Oregon: U.S, Geological Survey Professional Paper 59, 216 p.


Dance, S.P., and Emerson, W.K., 1967, Notes on Morum dennisoni (Reeve) and related species (Gastropoda: Tonnacea): The Veliger, v. 10, p. 91–98.


Dance, S.P., and Poppe, G.T., 1999, The family Harpidae, in Poppe, G.T., ed., A Conchological Iconography: Hackenheim, Germany, ConchBooks, 69 p.


D’Archiac, A., and Haime, J., 1854, Description des Animaux Fossiles du Groupe Nummulitique de l’Indie: Paris, Gide et J. Baudry, 418 p.


Dey, A.K., 1961, TheMiocene Mollusca from Quilon, Kerala (India): Memoirs of the Geological Survey of India, Palaeontologica Indica, n. ser., v. 36, 120 p.


Dodge, H., 1956,Ahistorical review of the mollusks of Linnaeus: Bulletin of the American Museum of Natural History, v. 111, p. 157–311.


Emerson, W.K., 1967, A new species of Morum from Brazil, with remarks on related species (Gastropoda: Tonnacea): The Veliger, v. 9, p. 289–292.


Emerson, W.K., 1981, Two new Indo-Pacific species of Morum (Gastropoda: Tonnacea): The Nautilus, v. 95, p. 101–105.


Emerson, W.K., 1968, A new species of the gastropod Morum from the eastern Pacific: Journal de Conchyliologie, v. 107, p. 53–57.


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