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Bivalve Species Duration, Areal Extent and Population Size in a Cretaceous Sea

Published online by Cambridge University Press:  08 February 2016

Carl F. Koch*
Affiliation:
Department of Geophysical Sciences, Old Dominion University, Norfolk, Virginia 23508

Abstract

Geographic distribution, species duration, and population size of 41 bivalve species which coexisted during the uppermost biozone (Sciponoceras gracile zone) of the Cenomanian were measured. Average species duration and correlation between geographic distribution, species duration, and population size were computed for five groups: total, infaunal, epifaunal, cemented epifaunal, and uncemented epifaunal bivalves.

Average species duration for all bivalves is less than 2 Myr. Infaunal bivalves averaged slightly higher, epifaunal slightly lower. Positive correlation was measured between species duration and geographic distribution for all five groups and statistical significance of the relationships was demonstrated for all but infaunal forms. In general no correlation was found between species duration and population size, and between population size and geographic distribution with the following exceptions: species duration and population size were significantly correlated for infaunal bivalves and uncemented epifaunal bivalves, and population size and geographic distribution were correlated for uncemented bivalves. Because these 41 fossil species coexisted at the same time and were distributed in the same space, differences in the relationships of species duration, geographic distribution and population among the various life habits indicate differences in ecological strategy and the evolutionary consequences of that difference.

Type
Articles
Copyright
Copyright © The Paleontological Society 

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References

Literature Cited

Berggren, W. A. and van Couvering, J. A. 1974. The Late Neogene. Palaeogeogr., Palaeoclimatol., Palaeoecol. 16:1216.Google Scholar
Boucot, A. J. 1975a. Standing diversity of fossil groups in successive intervals of geologic time viewed in the light of changing levels of provincialism. J. Paleontol. 49:11051111.Google Scholar
Boucot, A. J. 1975b. Evolution and Extinction Rate Controls. 427 pp. Elsevier; New York.Google Scholar
Coates, A. G. and Kauffman, E. G. 1973. Stratigraphy, paleontology and paleoenvironments of a Cretaceous coral thicket, Lamy, New Mexico. J. Paleontol. 47:953968.Google Scholar
Cobban, W. A. 1951. Colorado shale of central and northwestern Montana and equivalent rocks of the Black Hills. Bull. Am. Assoc. Petrol. Geol. 35:21702198.Google Scholar
Cobban, W. A. 1971. New and little known Ammonites from the Upper Cretaceous (Cenomanian and Turonian) of the Western Interior of the United States. U.S. Geol. Surv. Prof. Pap. 699, 24 pp.CrossRefGoogle Scholar
Cobban, W. A. and Reeside, J. B. Jr. 1952. Correlation of the Cretaceous formations of the Western Interior of the United States. Bull. Geol. Soc. Am. 63:10111044.Google Scholar
Cobban, W. A. and Scott, G. R. 1972. Stratigraphy and ammonite fauna of the Graneros Shale and the Greenhorn Limestone near Pueblo, Colorado. U.S. Geol. Surv. Prof. Pap. 645. 108 pp.Google Scholar
Hallam, A. 1977. Jurassic bivalve biogeography. Paleobiology. 3:5873.Google Scholar
Hansen, T. A. 1978. Larval dispersal and species longevity in Lower Tertiary gastropods. Science. 199:885887.CrossRefGoogle ScholarPubMed
Hattin, D. E. 1975. Stratigraphy and depositional environment of the Greenhorn Limestone (Upper Cretaceous) of Kansas. Kans. Geol. Surv. Bull. 209. 128 pp.Google Scholar
Hazel, J. E. 1969. Cytheris eaglefordensis Alexander. 1929. A guide fossil for deposits of latest Cenomanian age in the Western Interior and Gulf Coast regions of the United States. U.S. Geol. Surv. Prof. Pap. 650-D:155158.Google Scholar
Hazel, J. E. 1971. Ostracode biostratigraphy of the Yorktown Formation (upper Miocene and lower Pliocene) of Virginia and North Carolina. U.S. Geol. Surv. Prof. Pap. 704. 13 pp.Google Scholar
Hose, R. K. 1955. Geology of the Crazy Woman Creek area, Johnson County, Wyoming, U.S. Geol. Surv. Bull. 1027-B:33118.Google Scholar
Jackson, J. B. C. 1974. Biogeographic consequences of eurytopy and stenotopy among marine bivalves and their evolutionary significance. Am. Nat. 104:541560.Google Scholar
Jefferies, R. P. S. 1961. The palaeoecology of the Actinocamax plenus Subzone (lowest Turonian) in the Anglo-Paris basin. Palaeontol. 4:609647.Google Scholar
Jefferies, R. P. S. 1963. The stratigraphy of the Actinocamax plenus Subzone (Turonian) in the Anglo-Paris basin. Proc. Geol. Assoc. 74:123.CrossRefGoogle Scholar
Jeletsky, J. A. 1970. Cretaceous macrofaunas. Pp. 649662. In: Geology and Economic Minerals of Canada, Economic Geology Report 1 (5th ed.). Dept. of Energy, Mines and Resources; Canada.Google Scholar
Jeletsky, J. A. 1971. Marine Cretaceous biotic provinces and palaeogeography of western and Arctic Canada: illustrated by a detail study of ammonites. Pap. Geol. Surv. Can. 70–22:192.Google Scholar
Kauffman, E. G. 1967. Coloradoan macroinvertebrate assemblages, Central Western Interior, United States. In: Paleoenvironments of the Cretaceous Seaway in the Western Interior. Colo. School of Mines; Golden, Colo.Google Scholar
Kauffman, E. G. 1975. Dispersal and biostratigraphic potential of Cretaceous benthonic bivalvia in the Western Interior. Geol. Assoc. Can. Spec. Pap. 13:163194.Google Scholar
Kauffman, E. G. 1976. South African Middle Cretaceous Inoceramidae. Annales Du Muséum D'Histoire Naturelle de Nice -Tome IV.XVIII.1-XVIII.6.Google Scholar
Kauffman, E. G. 1977. Systematic, biostrategraphic, and geographic relationship between Middle Cretaceous Euramerican and North Pacific Inoceramidae. Paleont. Soc. Japan, Special Pap. No. 21:169212.Google Scholar
Kauffman, E. G., Powell, J. D., and Hattin, D. E. 1969. Cenomanian-Turonian facies across the Raton Basin. Mt. Geol. 6:93118.Google Scholar
Kennedy, W. J. and Juignet, P. 1973. Observations on the lithostratigraphy and ammonite succession across the Cenomanian-Turonian boundary in the environs of Le Mans (Sarthe, N.W. France). Neswl. Stratigr. 2, 4:189202.Google Scholar
Koch, C. F. 1978. Bias in the published fossil record. Paleobiology. 4:367372.CrossRefGoogle Scholar
Koch, C. F. 1980. The Sciponoceras gracile Biozone (Cenomanian, Cretaceous): A reference time plane for the Western Interior, North America. In: Hattin, D. E. and Kauffman, E. G., eds. Marine Cretaceous of the North Temperate Realm. Dowden, Hutchinson, and Ross, Inc.; Stroudsburg, Pa.Google Scholar
Landis, E. R., Dane, C. H., and Cobban, W. C. 1973. Stratigraphic terminology of the Dakota Sandstone and Mancos Shale, West-central New Mexico. U.S. Geol. Surv. Bull. 1372-J.Google Scholar
Moreman, W. L. 1942. Paleontology of the Eagleford Group of North and Central Texas. J. Paleontol. 16:192220.Google Scholar
Nicol, D. 1953. Period of existence of some late Cenozoic pelecypods. J. Paleontol. 27:706707.Google Scholar
Nicol, D. 1954. Growth and decline of populations and the distribution of marine pelecypods. J. Paleontol. 28:2225.Google Scholar
Obradovich, J. D. and Cobban, W. A. 1975. A time scale for the Late Cretaceous of the Western Interior of North America. Geol. Assoc. Can. Spec. Pap. 13:3154.Google Scholar
Powell, J. D. 1965. Late Cretaceous platform-basin facies, Northern Mexico and adjacent Texas. Bull. Am. Assoc. Petrol. Geol. 49(5):511525.Google Scholar
Reeside, J. F. Jr. 1957. Paleoecology of the Cretaceous Seas of the Western Interior of the United States. Geol. Soc. Am. Mem. 67. 2:505542.Google Scholar
Repenning, C. A. and Page, H. G. 1956. Late Cretaceous stratigraphy of Black Mesa, Navajo and Hopi Indian reservations, Arizona. Am. Assoc. Petrol. Geol. Bull. 40:255295.Google Scholar
Scott, G. R. 1962. Geology of the Littleton Quadrangle, Jefferson, Douglas, and Arapahoe Counties, Colorado. U.S. Geol. Surv. Bull. 1121-L. 53 pp.Google Scholar
Stanley, S. M. 1977. Trends, rates, and patterns of evolution in the bivalvia. Pp. 209250. In: Hallam, A., ed. Patterns of Evolution, as Illustrated by the Fossil Record. Elsevier; Amsterdam.Google Scholar
Stanton, T. W. 1893. The Colorado Formation and its invertebrate fauna. U.S. Geol. Surv. Bull. 106. 299 pp. (1894).Google Scholar
Stephenson, L. W. 1952. Larger invertebrate fossils of the Woodbine Formation (Cenomanian) of Texas. U.S. Geol. Surv. Prof. Pap. 242. 226 pp.Google Scholar
Swenson, A. J. 1962. Anisoceratidae and Hammitidae (Ammonoidea) from the Cretaceous of Texas and Utah. Brigham Young Univ. Geol. Studies. 9:5382. (1963).Google Scholar
Thayer, C. W. 1974. Environmental and evolutionary stability in bivalve mollusks. Science. 186:828830.CrossRefGoogle ScholarPubMed
Ward, L. W. and Blackwelder, B. W. 1975. Chesapecten, a new genus of Pectinidae (Mollusca: bivalvia) from the Miocene and Pliocene of Eastern North America. U.S. Geol. Surv. Prof. Pap. 861. 24 pp. 7 pl.CrossRefGoogle Scholar