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Sic and Underwent a Substantial Radiation in the Tron Microscopy and Microanalysis at the University Jurassic (Knight Et Al., 1960; Mclean, 1984)

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FOSSIL RECORD OF FISSURELLIDAE Hickman for use of a radular illustration of Clyp- eosectus delectus (Fig. 11 A). Other SEM micro- The Fissurellidae are traceable to the Middle Trias- graphs of radulae were made at the Center for Elec- sic and underwent a substantial radiation in the tron Microscopy and Microanalysis at the University Jurassic (Knight et al., 1960; McLean, 1984). of Southern California with the help of C. Clifton Earlier (McLean, 1984) I presented arguments in Coney, LACM. Support for this work was provided support of the scenario that fissurellids were derived by the LACMNH Foundation. Gerhard Haszpru- from Paleozoic bellerophontaceans, developing an nar, Richard S. Houbrick, George L. Kennedy, Da- idea proposed originally by Golikov and Starobo- vid R. Lindberg, and Anders Waren provided help- gatov (1975). No further evidence in support of this ful commentary. theory has been offered. Two primary objections This article is contribution number 81 of the remain: there is asymmetry in the ontogeny of all Galapagos Rift Biology Expedition supported by fissurellids, and the punctations or pores in the early the National Science Foundation. teleoconch of fissurellids have not been detected in bellerophontaceans. As noted most recently by Hickman (1988), the question of bellerophonta- LITERATURE CITED cean affinities remains as controversial as ever. Bandel, K. 1982. Morphologie und Bildung der frii- hontogenetischen Gehause bei conchiferen Mollus- TIME OF ENTRY TO THE ken. Fades, Universitat Erlangen 7:1-198, pis. 1- HYDROTHERMAL-VENT COMMUNITY 22. Batten, R.L. 1975. The Scissurellidae—Are they neo- Earlier (McLean, 1985, 1988a, 1988b, 1989), I hy- tenously derived fissurellidsf American Museum pothesized that the newly described families and Novitates, no. 2567:1-29. superfamilies of archaeogastropod limpets (Neom- Bourne, G. C. 1910. On the anatomy and systematic phalacea, Lepetodrilacea, Peltospiracea) from the position of Incisura [Scissurella] lytteltonensis. hydrothermal-vent community entered this com- Quarterly Journal of Microscopical Sciences 55:1- munity by the early Mesozoic, the time of diver- 47, pis. 1-5. gence and origin of other living archaeogastropod Boutan, L. 1885. Recherches sur l'anatomie et le de- superfamilies, and a time in which archaeogastro- velopment de la Fissurelle. Archives de Zoologie Ex- pods were the dominant gastropods in shallow seas. perimentale et Generate, ser. 2, tome 3, memoir 4, Fissurellaceans and scissurellaceans had an early pp. 1-173, pis. 31-44. Chase, R.L., J.J. Delaney, J.L. Karsten, H.P.Johnson, S.K. Mesozoic origin and there is no reason to disallow Juniper, J.E. Lupton, S.D. Scott, V. Tunnicliffe, S.R. a Mesozoic origin for temnocincline and sutilizo- Hammond, and R.E. McDuff. 1985. Hydrother- nine scissurellids and the clypeosectid fissurella- mal vents on an axis seamount of the Juan de Fuca ceans. The argument, however, is less compelling Ridge. Nature 331:212-214. than for the other newly described superfamilies Corliss, J.B., J. Dymond, L.I. Gordon, J.M. Edmond, R.P. because the rank of endemism (see Newman, 1985), von Herzen, R.D. Ballard, K. Green, D. Williams, i.e., the hierarchical level of new taxa, is below the A. Bainbridge, K. Crane, and T.H. van Andel. 1979. superfamily level for the slit-limpets. Submarine thermal springs on the Galapagos Rift. Science 203:1073-1083. Desbruyeres, D., P. Crassous, J. Grassle, A. Khripounoff, ACKNOWLEDGMENTS D. Reyss, M. Rio, and M. van Praet. 1982. Don- nees ecologiques sur un nouveau site d'hydrother- I am grateful to J. Frederick Grassle, Howard L. malisme actif de la ride du Pacifique oriental. Comptes Sanders, and Ruth D. Turner for entrusting material Rendus, Academie des Sciences, Paris, ser. 3, 295: collected by the Alvin at the Galapagos Rift and 489-494. 21°N to me for description. Most of this material Desbruyeres, D., and L. Laubier. 1983. Primary con- had been sorted and processed at Woods Hole sumers from hydrothermal vent animal communi- Oceanographic Institution by Isabelle Williams, who ties. In Hydrothermal processes at seafloor spread- also checked locality records in the manuscript. ing centers, eds. P.A. Rona, K. Bostrom, L. Laubier, Philippe Bouchet of the Museum National d'His- and K.L. Smith, Jr., pp. 711-734. New York: Ple- toire Naturelle, Paris, loaned specimens collected num. by the Cyana at 13°N. Verena Tunnicliffe, of the Fretter, V. 1988. New archaeogastropod limpets from hydrothermal vents, superfamily Lepetodrilacea. Part University of Victoria, British Columbia, forwarded 2: Anatomy. Philosophical Transactions of the Roy- material from the Juan de Fuca Ridge collected al Society of London, ser. B, 319:33-82. with Pisces IV. Material from the Mariana Back- . 1989. The anatomy of some new archaeogas- Arc vents collected with the Alvin was sent by tropod limpets (superfamily Peltospiracea) from hy- Robert R. Hessler of Scripps Institution of Ocean- drothermal vents .Journal of Zoology, London, 218: ography. Cindy Lee Van Dover forwarded material 123-169. collected at 12°N on the East Pacific Rise. Photog- Fretter, V., A. Graham, and J.H. McLean. 1981. The raphy of shells and limpet bodies is the work of anatomy of the Galapagos Rift limpet, Neomphalus Bertram C. Draper. I thank Ruth Turner for loaning fretterae. Malacologia 21:337-361. SEM negatives of juvenile shells and protoconchs Golikov, A., and Y.I. Starobogatov. 1975. Systematics of prosobranch gastropods. Malacologia 21:337- previously published in Turner et al. (1985), which 361. were made by Richard A. Lutz. I thank Carole S. Haszprunar, G. 1988a. On the origin and evolution of 10 • Contributions in Science, Number 407 McLean: New Slit-Limpets major gastropod groups, with special reference to Mollusca 1:169-310. Geological Society of America the Streptoneura. Journal of Molluscan Studies 54: and University of Kansas Press. 367-441. Lutz, R.A., D. Jablonski, and R.D. Turner. 1984. Larval . 1988b. A preliminary phylogenetic analysis of development and dispersal at deep-sea hydrothermal the streptoneurous gastropods. In Prosobranch phy- vents. Science 226:1451-1454. togeny, ed. W.F. Ponder. Proceedings of the 9th MacClintock, C. 1963. Reclassification of gastropod International Malacological Congress, Edinburgh, Proscutum Fischer based on muscle scars and shell 1986. Malacological Review, Supplement 4, pp. 7- structure. Journal of Paleontology 37:141-156. 16. McLean, J.H. 1981. The Galapagos Rift limpet Neom- . 1989. New slit-limpets (Scissurellacea and Fis- phalus: Relevance to understanding the evolution surellacea) from hydrothermal vents. Part 2. Anat- of a major Paleozoic-Mesozoic radiation. Malaco- omy and relationships. Contributions in Science, logia 21:291-226. Natural History Museum of Los Angeles County, . 1984. A case for derivation of the Fissurellidae no. 408, 17 pp. from the Bellerophontacea. Malacologia 25:3-20. Herbert, D.G. 1986. A revision of the southern African . 1985. Preliminary report on the limpets at hy- Scissurellidae (Mollusca: Gastropoda: Prosobran- drothermal vents. In The hydrothermal vents of the chia). Annals of the Natal Museum 27:601-632. Eastern Pacific: An overview, ed. M.L. Jones. Bio- . 1987. Taxonomic studies on the Emarginulinae logical Society of Washington, Bulletin 6:159-166. (Mollusca: Gastropoda: Fissurellidae) of southern . 1988a. New archaeogastropod limpets from Africa and Mozambique. Hemitoma, Clypidina, hydrothermal vents, superfamily Lepetodrilacea. Part Tugali, Scutus, Zeidora and two species of Emar- 1: Systematic descriptions. Philosophical Transac- ginula. South African Journal of Zoology 22:1-13. tions of the Royal Society of London, ser. B, 319: Herbert, D.G., and R.N. Kilburn. 1986. Taxonomic 1-32. studies on the Emarginulinae (Mollusca: Gastropo- . 1988b. New archaeogastropod limpet families da: Fissurellidae) of southern Africa and Mozam- in the hydrothermal vent community. In Proso- bique. Emarginula, Emarginella, Puncturella, Fis- branch phylogeny, ed. W.F. Ponder. Proceedings of surispeta and Rimula. South African Journal of the 9th International Malacological Congress, Edin- Zoology 21:1-27. burgh, 1986. Malacological Review, Supplement 4, Hessler, R.R., P. Lonsdale, and J. Hawkins. 1988. Pat- pp. 85-87. terns on the ocean floor. New Scientist, 24 March . 1989. New archaeogastropod limpets from hy- 1988:47-51. drothermal vents: New family Peltospiridae, new Hessler, R.R., and W.M. Smithey, Jr. 1983. The distri- superfamily Peltospiracea. Zoologica Scripta 18(1): bution and community structure of megafauna at 49-66. the Galapagos Rift hydrothermal vents. In Hydro- McLean, J.H., and G. Haszprunar. 1987. Pyropeltidae, thermal processes at seafloor spreading centers, eds. a new family of cocculiniform limpets from hydro- P.A. Rona, K. Bostrum, L. Laubier, and K.L. Smith, thermal vents. The Veliger 30:196-205. Jr., pp. 735-770. New York: Plenum. Newman, W.A. 1985. The abyssal hydrothermal vent Hessler, R.R., W.M. Smithey, Jr., and C.H. Keller. 1985. invertebrate fauna: A glimpse of antiquity? In The Spatial and temporal variation of giant clams, tube hydrothermal vents of the Eastern Pacific: An over- worms and mussels at deep-sea hydrothermal vents. view, ed. M.L. Jones. Biological Society of Wash- In The hydrothermal vents of the Eastern Pacific: ington, Bulletin 6:231-242. An overview, ed. M.L. Jones. Biological Society of Powell, A.W.B. 1979. New Zealand Mollusca; marine, Washington, Bulletin 6:411-428. land and freshwater shells. Auckland: Collins, 500 Hickman, C.S. 1981. Evolution and function of asym- pp. metry in the archaeogastropod radula. The Veliger Salvini-Plawen, L. 1980. A reconsideration of system- 23:189-194. atics in the Mollusca (phylogeny and higher classi- . 1983. Radular patterns, systematics, diversity, fication). Malacologia 19:249-278. and ecology of deep-sea limpets. The Veliger 26:73- Salvini-Plawen, L., and G. Haszprunar. 1987. The Ve- 92. tigastropoda and the systematics of streptoneurous . 1984a. Implications of radular tooth-row func- Gastropoda. Journal of Zoology, London, ser. A, tional integration for archaeogastropod systematics. 211:747-770. Malacologia 25:143-160. Spiess, F.N., K.C.
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    Gastropoda: Vetigastropoda: Scissurellidae)

    Zootaxa 4759 (4): 593–596 ISSN 1175-5326 (print edition) https://www.mapress.com/j/zt/ Correspondence ZOOTAXA Copyright © 2020 Magnolia Press ISSN 1175-5334 (online edition) https://doi.org/10.11646/zootaxa.4759.4.11 http://zoobank.org/urn:lsid:zoobank.org:pub:8D3B9B4C-5EA7-4746-9987-CBE75B771D0E Scissurella nesbittae, new species, from the Gries Ranch Formation, Lewis County, Washington State (Gastropoda: Vetigastropoda: Scissurellidae) DANIEL L. GEIGER1 & JAMES L. GOEDERT2 1Santa Barbara Museum of Natural History, 2559 Puesta del Sol, Santa Barbara, CA 93105, USA. E-mail: [email protected] 2Burke Museum of Natural History and Culture, University of Washington, Seattle, WA 98195, USA. E-mail: jamesgoedert@outlook. com Recent and fossil global scissurellids were monographed by Geiger (2012) and additional species were recently described from Brazil (Pimenta & Geiger 2015). Here, we describe an additional fossil species from shallow water strata of the late Eocene Gries Ranch Formation in Lewis County, Washington State, USA. Marine molluscan fossils were first described from exposures of the Gries Ranch Formation along the Cowlitz River more than 100 years ago (Dickerson 1917; Van Winkle 1918) and monographed 80 years ago by Effinger (1938). Since then, many studies have included molluscan taxa from the Gries Ranch fauna (e.g., Dell’Angelo et al. 2011; Goedert & Raines 2016, and references therein). Deposition of the Gries Ranch Formation likely occurred under subtropical condi- tions (Dickerson 1917; Van Winkle 1918) at depths of less than 100 m according to Effinger (1938), although Hickman (1984) has suggested that the Gries Ranch fauna may have been transported into deep water.
  • The Limpet Form in Gastropods: Evolution, Distribution, and Implications for the Comparative Study of History

    The Limpet Form in Gastropods: Evolution, Distribution, and Implications for the Comparative Study of History

    UC Davis UC Davis Previously Published Works Title The limpet form in gastropods: Evolution, distribution, and implications for the comparative study of history Permalink https://escholarship.org/uc/item/8p93f8z8 Journal Biological Journal of the Linnean Society, 120(1) ISSN 0024-4066 Author Vermeij, GJ Publication Date 2017 DOI 10.1111/bij.12883 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Biological Journal of the Linnean Society, 2016, , – . With 1 figure. Biological Journal of the Linnean Society, 2017, 120 , 22–37. With 1 figures 2 G. J. VERMEIJ A B The limpet form in gastropods: evolution, distribution, and implications for the comparative study of history GEERAT J. VERMEIJ* Department of Earth and Planetary Science, University of California, Davis, Davis, CA,USA C D Received 19 April 2015; revised 30 June 2016; accepted for publication 30 June 2016 The limpet form – a cap-shaped or slipper-shaped univalved shell – convergently evolved in many gastropod lineages, but questions remain about when, how often, and under which circumstances it originated. Except for some predation-resistant limpets in shallow-water marine environments, limpets are not well adapted to intense competition and predation, leading to the prediction that they originated in refugial habitats where exposure to predators and competitors is low. A survey of fossil and living limpets indicates that the limpet form evolved independently in at least 54 lineages, with particularly frequent origins in early-diverging gastropod clades, as well as in Neritimorpha and Heterobranchia. There are at least 14 origins in freshwater and 10 in the deep sea, E F with known times ranging from the Cambrian to the Neogene.