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Freshwater ostracodes from upper Middle Devonian fluvial facies, Catskill Mountains, New York

Published online by Cambridge University Press:  14 July 2015

Gerald M. Friedman  and
Robert F. Lundin
Gerald M. Friedman
Affiliation:
1Northeastern Science Foundation, Inc. affiliated with Brooklyn College, Rensselaer Center of Applied Geology, 15 Third Street, P.O. Box 746, Troy, New York 12181-0746 and Department of Geology, Brooklyn College and Graduate School of the City University of New York, Brooklyn 11210
Robert F. Lundin
Affiliation:
2Department of Geology, P.O. Box 871404, Arizona State University, Tempe 85287-1404
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Abstract

Leperditiocope ostracodes identified as Sollenella? sp. were discovered in the Gilboa Formation (upper Givetian, uppermost Middle Devonian) within the continental Catskill Magnafacies of New York State. The deposits in which the ostracodes were found are meandering-fluvial facies that were part of a vast alluvial plain that sloped westward from the eroding Acadian Mountains. Hence, ostracodes colonized freshwater habitats earlier than heretofore thought. It has been widely accepted that, until now, the oldest known unequivocal occurrences of freshwater ostracodes are of Late Carboniferous age. This new discovery means that the first colonization of freshwater habitats by Ostracoda occurred approximately 60 million years earlier than previously known.

Type
Research Article
Information
Journal of Paleontology , Volume 72 , Issue 3 , May 1998 , pp. 485 - 490
Copyright
Copyright © The Paleontological Society 

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References

Abushik, A. F. 1960. Siluriiskie ostrakod'i Sibirskoi platform'i. Vsesoyuzonogo Nauchno-Issledovatel'skogo Geologiicheskogo Instituta (VSEGEI), new series, 39(6), 131 p.Google Scholar
Allen, J. R. L., and Friend, P. F. 1968. Deposition of the Catskill facies, Appalachian region: With notes on some other Old Red Sandstone basins, p. 21–74. In Klein, G. de V. (ed.), Late Paleozoic and Mesozoic Continental Sedimentation, Northeastern North America, Geological Society of America Special Paper, 106, 309 p.CrossRefGoogle Scholar
Barrell, J. 1913. The Upper Devonian delta of the Appalachian geosyncline. American Journal of Science, 4th series, 36:429–472.CrossRefGoogle Scholar
Berdan, J. M. 1984. Leperditicopid ostracodes from the Ordovician rocks of Kentucky and nearby states and characteristic features of the order Leperditicopida. In United States Geological Survey Professional Paper, 1066J, 40 p.CrossRefGoogle Scholar
Bridge, J. S., and Dingman, L. E. 1981. Depostional environment of the Oneonta Formation (Catskill Facies), near Unadilla, New York. New York State Geological Association Guidebook, 53rd Annual Meeting, Binghamton, p. 255–277.Google Scholar
Bridge, J. S. and Gordon, E. 1985a. Quantitative interpretation of ancient river systems in the Oneonta Formation, Catskill Magnafacies. Geological Society of America Special Paper, 201:163–181.CrossRefGoogle Scholar
Bridge, J. S. and Gordon, E. 1985b. The Catskill Mountain Magnafacies of New York state, p. 3–17. In Flores, R. M. and Harvey, M. (eds.), Field Guidebook to Modern and Ancient Fluvial Systems in the United States. Proceedings of the Third International Fluvial Sedimentology Conference, Fort Collins, Colorado.Google Scholar
Bridge, J. S., and Nickelsen, B. H. 1985. Reanalysis of the Twilight Park Conglomerate, Upper Devonian Catskill Magnafacies, New York State. Northeastern Geology, 7:181–191.Google Scholar
Buttner, P. J. R. 1968. Proximal continental rhythmic sequences in the Genesee Group (Lower upper Devonian) of southeastern New York, p. 109–126. In dev. Klein, G. (ed.), Late Paleozoic and Mesozoic Continental Sedimentation, Northeastern North America. Geological Society of America Special Paper, 106, 309 p.CrossRefGoogle Scholar
Buttner, P. J. R. 1972. Systems analysis and model building, p. 69–86. In Fenner, P. (ed.), Quantitative Geology. Geological Society of America Special Paper, 146, 101 p.CrossRefGoogle Scholar
Carbonel, P., Colin, J. P., Danielopol, D. L., Löffler, H., and Neustrueva, I. 1988. Paleoecology of limnic ostracodes: a review of some major topics. Palaeogeography, Palaeoclimatology, Palaeoecology, 62:413–461.CrossRefGoogle Scholar
Carling, P. A., and Dawson, M. R. (eds.). 1996. Advances in fluvial dynamics and stratigraphy. John Wiley & Sons, New York, 530 p.Google Scholar
Chadwick, G. H. 1936. History and value of the name “Catskill” in geology. New York State Museum Bulletin, 307, 116 p.Google Scholar
Cocks, L. R. M., and Toghill, P. 1973. The biostratigraphy of the Silurian rocks of the Girvan district, Scotland. Journal of the Geological Society, 129:209–243.CrossRefGoogle Scholar
Cooper, G. A. 1934. Stratigraphy of the Hamilton Group of eastern New York. Pt. 2. American Journal of Science, 5th series, 27(157):1–12.Google Scholar
Cooper, G. A. and Williams, J. S. 1935. Tully Formation of New York. Geological Society of America Bulletin, 46:781–868.CrossRefGoogle Scholar
Demicco, R. V., Bridge, J. S., and Cloyd, K. C. 1987. A unique freshwater carbonate from the Upper Devonian Catskill Magnafacies of New York State. Journal of Sedimentary Petrology, 57:327–334.Google Scholar
Dorning, K. J. 1982. Early Wenlock acritarchs from the Knockgardner and Straiton Grit formations of Knockgardner, Ayrshire. Scottish Journal of Geology, 18(4):267–273.CrossRefGoogle Scholar
Fletcher, F. W. 1964. Middle and Upper Devonian stratigraphy of southeastern New York. Unpubulished. , , 197 p.Google Scholar
Fletcher, F. W. 1967. Middle and Upper Devonian clastics of the Catskill front, New York. New York State Geological Association Guidebook, 39:C1–C23.Google Scholar
Friedman, G. M. 1972. “Sedimentary facies”: Products of sedimentary environments in Catskill Mountains, Mohawk Valley, and Taconic sequence, eastern New York state. Society of Economic Paleontologists and Mineralogists, Eastern Section, 48 p.Google Scholar
Friedman, G. M. 1987a. Deep-burial diagenesis: Its implications for vertical movements of the crust, uplift of the lithosphere and isostatic unroofing, a review. Sedimentary Geology, 50:67–94.CrossRefGoogle Scholar
Friedman, G. M. 1987b. Vertical movements of the crust: case histories from the northern Appalachian basin. Geology, 15:1130–1133.2.0.CO;2>CrossRefGoogle Scholar
Friedman, G. M. 1995. Flysch and molasse of the classical Taconian and Acadian orogenies: Models for subsurface reservoir settings, p. 109–143. In Garver, J. I. and Smith, J. A. (eds.), Field Trips for the 67th Annual Meeting of the New York State Geological Association, Union College, Schenectady, New York.Google Scholar
Friedman, G. M., and Chamberlain, J. A. 1995. Archanodon catskillensis (Vanuxem): Fresh-water clams from one of the oldest back-swamp fluvial facies (upper Middle Devonian), Catskill Mountains, New York. Northeastern Geology and Environmental Sciences, 17:431–443.Google Scholar
Friedman, G. M., and Johnson, K. G. 1966. The Devonian Catskill deltaic complex of New York, type example of a “tectonic delta complex'” p. 171-188. In Shirley, M. L. (ed.), Deltas in Their Geologic Framework, Houston Geological Society, 251 p.Google Scholar
Friedman, G. M., and Sanders, J. E. 1982. Time-temperature-burial significance of Devonian anthracite implies former great (∼6.5 km) depth of burial of Catskill Mountains, New York. Geology, 10:93–96.Google Scholar
Friedman, G. M., Sanders, J. E., and Kopaska-Merkel, D. C. 1992. Principles of Sedimentary Deposits: Stratigraphy and Sedimentology. Macmillian Publishing Company, New York/Maxwell Macmillian Canada, Toronto/Maxwell Macmillian International, New York, Oxford, Singapore, Sydney, 717 p.Google Scholar
Friedman, G. M., Sanders, J. E., and Martini, I. P. 1982. Excursion 17A: Sedimentary facies: products of sedimentary environments in a cross section of the classic Appalachian Mountains and adjoining Appalachian basin in New York and Ontario. International Association of Sedimentologists, Eleventh International Congress on Sedimentology, variously paginated.Google Scholar
Gordon, E. A. 1988. Body and trace fossils from the Middle-Upper Devonian Catskill Magnafacies, southeastern New York, U.S.A., p. 139–156. In McMillan, N. J., Embry, A. F. and Glass, D. J. (eds.), The Devonian of the World. Proceedings of the Second International Symposium on the Devonian System, Calgary, Canada. Canadian Society of Petroleum Geologists, Memoir 14, Volume II: Sedimentation, 674 p.Google Scholar
Gordon, E. A. 1989. Fluvial to marine transitional deposits of the Devonian Catskill clastic wedge, New York, U.S.A. Abstracts 4th International Conference on Fluvial Sedimentology, Barcelona, Sitges, Oct. 2, 3, and 4, 1989, p. 140.Google Scholar
Gordon, E. A., and Bridge, E. A. 1987. Evolution of Catskill (Upper Devonian) river systems: intra- and extra-basinal controls. Journal of Sedimentary Petrology, 57:234–249.Google Scholar
Harland, W. B., Armstrong, R. L., Cox, A. V., Craig, L. E., Smith, A. G., and Smith, D. G. 1989. A Geologic Time Scale. Cambridge University Press, Cambridge, 263 p.Google Scholar
Isachsen, Y. W., Landing, E., Lauber, J. M., Rickard, L. V., and Rogers, W. B. (eds.). 1991. Geology of New York: a simplified account. New York State Museum/Geological Survey, The State Education Department, The University of the State of New York, Albany, New York, 283 p.Google Scholar
Johnson, K. G., and Friedman, G. M. 1969. The Tully Clastic Correlative (Upper Devonian) of New York State: a model for recognition of alluvial, dune (?), tidal, nearshore (bar and lagoon), and offshore sedimentary environments in a tectonic delta complex. Journal of Sedimentary Petrology, 39:452–485.Google Scholar
Klapper, G. M. 1981. Review of New York Devonian conodont biostratigraphy, p. 57–66. In Oliver, W. J. Jr. and Klapper, G. M. (eds.), Devonian Biostratigraphy of New York, Part 1, Text, International Union of Geological Sciences, Subcommission on Devonian Stratigraphy, Washington, D.C., 106 p.Google Scholar
Menning, M. 1989. A synopsis of numerical time scales 1917-1986. Episodes, 12(1):3–5.CrossRefGoogle Scholar
Miall, A. D. 1996. The Geology of Fluvial Deposits—Sedimentary Facies, Basin Analysis, and Petroleum Geology. Springer Verlag. New York, 582 p.Google Scholar
Rickard, L. V. 1964. Correlation of the Devonian rocks in New York state. New York State Museum and Science Service Geological Survey Map and Chart Series, 4.Google Scholar
Rickard, L. V. 1975. Correlation of the Silurian and Devonian rocks in New York State. New York State Museum Science Service Map and Chart Series, 24.Google Scholar
Salvador, A. 1985. Chronostratigraphic and geochronometric scales in COSUNA Stratigraphic Correlation Charts of the United States. American Association of Petroleum Geologists Bulletin, 69:181–189.Google Scholar
Sevon, W. D. 1981. The Middle and Upper Devonian clastic wedge in northeastern Pennsylvania. In New York State Geological Association Guidebook for Fieldtrips, 53rd Annual Meeting, Binghamton, p. 31–63.Google Scholar
Shepps, V. C. (ed.). 1963. Symposium on Middle and Upper Devonian stratigraphy of Pennsylvania and adjacent states. Pennsylvania Geological Survey Bulletin, G-39, 301 p.Google Scholar
Siveter, D. J. 1984. Habitats and modes of life of Silurian ostracodes, p. 71–85. In Bassett, M. G. (ed.), Autecology of Silurian organisms. Special Papers in Paleontology, 32, Paleontological Association, London.Google Scholar
Smith, M. L. 1956. Some ostracods from the Middle Devonian Ledyard and Wanakah members of the Ludlowville Formation in western New York. Journal of Paleontology, 30:1–8.Google Scholar
Solle, G. 1935. Die devonischen Ostracoden Spitzbergens; 1, Leperditiidae. Skrifter om Svalbard og Ishavet, 64, 61 p.Google Scholar
Solle, G. 1936. Neu-Benennung von Holtedahlina Solle, 1935. Senckbergiana, 18:282.Google Scholar
Swartz, F. M. 1949. Muscle marks, hinge and overlap features, and classification of some Leperditiidae. Journal of Paleontology, 23:306–327.Google Scholar
Tibert, N. E., and Scott, D. B. 1996. Early Carboniferous ostracodes from the Horton Bluff Formation, Nova Scotia, Canada: a paleoenvironmental interpretation of an ancient marginal-marine ecosystem. Geological Society of America Abstracts with Programs, 28(3):104–105.Google Scholar
Ulrich, E. O., and Bassler, R. S. 1923. Paleozoic Ostracoda: Their morphology, classification and occurrence, p. 271–391. In Swartz, C. K. et al., Maryland Geological Survey, Silurian Volume, 794 p.Google Scholar
Walker, R. G., and Harms, J. C. 1971. The “Catskill Delta”: a prograding muddy shoreline in central Pennsylvania. Journal of Geology, 79:381–399.CrossRefGoogle Scholar
Willis, B. J., and Bridge, J. S. 1988. Evolution of Catskill river systems, New York State, p. 85–106. In McMillan, N. J., Embry, A. F. and Glass, D. J. (eds.), The Devonian of the World. Proceedings of the Second International Symposium on the Devonian System, Calgary, Canada. Canadian Society of Petroleum Geologists, Memoir 14, Volume 2: Sedimentation, 674 p.Google Scholar
Woodrow, D. L., and Ahrnsbrack, W. F. 1973. Paleogeography and paleoclimate at the deposition sites of the Devonian Catskill and Old Red facies. Geological Society of America Bulletin, 83:3051–3064.2.0.CO;2>CrossRefGoogle Scholar