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The Ontogeny of an Ostracodologist

Published online by Cambridge University Press:  21 July 2017

Richard H. Benson*
Affiliation:
Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20013-7012 USA
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Abstract

The context and reasons for the study of ostracodes have changed greatly over the past half-century, as well as how fossil ostracodes are viewed. Their use for the reconstruction of major changes in paleogeography and paleoceanography has been amply demonstrated. Some of the increased importance of ostracodes is due to new exploration via drilling and the discovery of new forms in the floors of sea and ocean basins. Some of it has been made possible by the development of the scanning electron microscope and attention to details in carapace morphology, particularly in mapping patterns of reticulation. The discovery that the shape of the carapace subscribes to architectural restraints of a membrane static-frame used in dome construction has introduced the possibility to describe it in functional and adaptive terms, and those principles are set forth here. [see Chapter 6 for details on the latter]

Type
Research Article
Copyright
Copyright © 2003 by The Paleontological Society 

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References

Adams, C. G., Benson, R. H., Kidd, R. B., Ryan, W. B. F., and Wright, R. C. 1977. The Messinian salinity crisis and evidence of Late Miocene eustatic changes in the world ocean. Nature, 269:383386.Google Scholar
Benson, R. H. 1955. Ostracodes from the type section of the Fern Glen Formation. Journal of Paleontology, 29:10301039.Google Scholar
Benson, R. H. 1965. Photography of microfossils, pp. 433446. In Kummel, B. and Raup, D. (eds.), Handbook of Paleontological Techniques. W.H. Freeman and Co., San Francisco.Google Scholar
Benson, R. H. 1970. Architectural solutions to structural stress in rigid micro-organisms, through SEM examination, Proceedings of the Third Annual Stereoscan Colloquium, 1970. Kent Cambridge Scientific, Incorporated: Private Publ., p. 7177 Google Scholar
Benson, R. H. 1973. Psychrospheric and continental ostracoda from ancient sediments in the floor of the Mediterranean, p. 10021008. In Ryan, W. B. F., Hsü, K. J., et al. (eds.), Initial Reports of the Deep Sea Drilling Project, 13. Washington, D.C.: U.S. Government Printing Office.Google Scholar
Benson, R. H. 1972. The Bradleya problem with descriptions of two new psychrospheric ostracode genera, Agrenocythere and Poseidonamicus (Ostracoda: Crust.). Smithsonian Contributions to Paleobiology, 12: 1138.Google Scholar
Benson, R. H. 1975. The origin of the psychrosphere as recorded in changes of deep-sea ostracode assemblages. Lethaia, 8:6983.Google Scholar
Benson, R. H. 1976a. The evolution of the ostracode Costa analyzed by “Theta-Rho Difference.” p. 127139. In Hartmann, G. (ed.), Evolution of Post-Paleozoic Ostracoda, Abhandlungen und Verhandlungen des Naturwissenshafliches Vereins (Hamburg), 18/19.Google Scholar
Benson, R. H. 1976b. Testing the Messinian salinity crisis biodynamically: an introduction. Palaeogeography, Palaeoclimatology, Palaeoecology, 20: 311.Google Scholar
Benson, R. H. 1976c. Miocene deep-sea ostracodes of the Iberian Portal and the Balearic Basin. Marine Micropaleontology, 1:249262.Google Scholar
Benson, R. H. 1976d. Changes in the ostracodes of the Mediterranean with the Messinian salinity crisis. Palaeogeography, Palaeoclimatology, Palaeoecology, 20:147170.Google Scholar
Benson, R. H. 1977. Cenozoic ostracode faunas of the Sao Paulo Plateau and the Rio Grande Rise (DSDP Leg 39, Sites 356 and 357). p. 869883. In Supko, P. R., Perch-Nielsen, K., et al. (eds.), Initial Reports of the Deep Sea Drilling Project, 39, Washington, D.C.: U.S. Government Printing Office.Google Scholar
Benson, R. H. 1978. On the use of ostracodes for tracing changes in oceanic circulation, p. 1521. In Loffler, H. and Danielopol, D. (eds.), Aspects of Ecology and Zoogeography of Recent and Fossil Ostracoda, W. Junk: The Hague.Google Scholar
Benson, R. H. 1979. In search of lost oceans; a paradox in discovery, p. 379389. In Gray, J. and Boucot, A. J. (eds.), Historical Biogeography, Plate Tectonics and the Changing Environment, Oregon State University Press.Google Scholar
Benson, R. H. 1984. The Phanerozoic Crisis as viewed from the Miocene, p. 437446 In Berggren, W. A. and Van Couvering, J. (eds.), Catastrophes and Earth History: The New Uniformitarianism, Princeton Univ. Press.Google Scholar
Benson, R. H. 1990. Ostracoda and the discovery of global Cainozoic palaeoceanographical events, p. 4158. In Whatley, R. and Maybury, C. (eds.), Ostracoda and Global Events. Chapman and Hall, London.Google Scholar
Benson, R. H. 1991. Messinian Salinity Crisis. Encyclopedia of Earth Sciences, 3:161167.Google Scholar
Benson, R. H. in press . Giuliano Ruggieri in the 60's and 70's: from an American friend's point of view. Paleontologica Italica, 13 p.Google Scholar
Benson, R. H. and Collinson, C. 1958. Three ostracode faunas from Lower and Middle Mississippian Strata in Southern Illinois. Illinois State Geological Survey, circular 255: 126.Google Scholar
Benson, R. H., Chapman, R. E., and Deck, L.T. 1985. Evidence from the Ostracoda of Major Events in the South Atlantic and World wide over the Past 80 Million Years, Proceedings of the First International Conference on Paleoceanography, Zurich, 1983, p. 325350. In Hsüu, K. J. and Weissert, H. J. (eds.), South Atlantic_Paleoceanography, Cambridge Univ. Press.Google Scholar
Benson, R. H., Hayek, L.-A., Hodell, D. A., and Rakic-El Bied, K. 1995. Extending the climatic precession curve back into the late Miocene by template signature comparison. Paleoceanography, 10(1): 520.Google Scholar
Benson, R. H., Rakic- El Bied, K., and Bonaduce, G. 1991. An important current reversal (influx) in the Rifian Corridor (Morocco) at the Tortonian-Messinian Boundary. Paleoceanography, 6(1): 164192.Google Scholar
Benson, R. H., and Rakic-El Bied, K. 1991. Biodynamics, saline giants and Late Miocene catastrophism. Carbonates & Evaporites, 6(2): 127168.CrossRefGoogle Scholar
Benson, R. H., and Ruggieri, G. 1974. The end of the Miocene, time of crisis in Tethys-Mediterranean history. Annals of the Geological Survey of Egypt, 4: 237250.Google Scholar
Benson, R. H., and Sylvester-Bradley, P. C. 1971. Deep-sea ostracodes and the transformation of ocean to sea in the Tethys. Bulletin Centre Recherch Pau-SNPA, 5: 6391.Google Scholar
Hodell, D. A., Benson, R. H., Kent, D.V., Boersma, A., and Rakic-El Bied, K. 1994. Magnetostratigraphic, biostratigraphic, and stable isotope stratigraphy of an upper Miocene drill-core sequence from the Sale Briqueterie (northwestern Morocco): A high-resolution chronology for the Messinian Stage. Paleoceanography, 9: 835855.Google Scholar
Krömmelbein, K. 1966. On “Gondwana Wealden” Ostracoda from NE Brazil and West Africa, Proceedings of the Second West African Micropaleontological Colloquium, (Ibadan, 1965): 113119.Google Scholar
Sylvester-Bradley, P. C. and Benson, R. H. 1971. Terminology for surface features in ornate ostracodes. Lethaia, 4: 249286.CrossRefGoogle Scholar