Hostname: page-component-848d4c4894-mwx4w Total loading time: 0 Render date: 2024-06-22T11:07:25.942Z Has data issue: false hasContentIssue false

James H. Stitt: A Dedicated Professor and Exemplary Biostratigrapher

Published online by Cambridge University Press:  20 May 2016

John F. Taylor*
Affiliation:
Geoscience Department, Indiana University of Pennsylvania, Indiana, PA 15705
Rights & Permissions [Opens in a new window]

Extract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

On Friday September 17 Jim Stitt died quietly in his sleep, ending a long and characteristically tenacious battle with cancer. His passing leaves a void of great magnitude in the geological sciences and in the lives of the many people whom he influenced as family, friends, or colleagues. I was Jim's first Ph.D. student at the University of Missouri, where he spent the past 31 years as a pillar of the geology program, serving at various times as Chair and Graduate Student Advisor. Jim is well known and respected for an impressive body of meticulously crafted taxonomic and biostratigraphic studies on trilobites and brachiopods. His three monographs on faunas in the Arbuckle and Wichita Mountains of Oklahoma (Stitt, 1971a, 1977, 1983) established that area as a standard for correlation of Upper Cambrian and Lower Ordovician strata in North America. This “Oklahoma trilogy” is a treasure trove of taxonomic and biostratigraphic data that has been drawn upon heavily in numerous subsequent biostratigraphic and paleobiologic studies. It provides a biozonation of unparalleled precision for carbonate platform facies of that interval, ironically assembled in an area where rocks of that age yield their fossils only reluctantly. Jim took great pride in extracting useful information from difficult rocks. He passed that laudable attitude on to his academic offspring, along with the sense of satisfaction he derived from seeing his data put to good use in solving geologic or paleobiologic problems, in his own work and in that of others. At the same time, he was always complimentary and supportive of more theoretical or abstract research, an attitude sadly lacking in some practitioners with a bent toward applied paleontology.

Type
Memorial
Copyright
Copyright © The Paleontological Society 2000

References

Brezinski, D. K., and Stitt, J. H. 1982. Ditomopyge scitula (Meek and Worthen) from the Lower Pennsylvanian of central Missouri and central Texas: Journal of Paleontology, 56:12421250.Google Scholar
Hart, W. D., Stitt, J. H., Hohensee, S. R. and Ethington, R. L. 1987. Geological implications of Late Cambrian trilobites from the Collier Shale, Jessieville area, Arkansas: Geology, 15:447450.Google Scholar
Hohensee, S. R. and Stitt, J. H. 1989. Redeposited Elvinia Zone (Upper Cambrian) trilobites from the Collier Shale, Ouachita Mountains, west-central Arkansas. Journal of Paleontology, 63:857879.CrossRefGoogle Scholar
Miller, J. F., and Stitt, J. H. 1997. Stratigraphic position and significance of Jujuyaspis and lapetognathus in the Wilberns Formation, Texas, p. 105108. In Cooper, J. D., Droser, M. L., and Finney, S. C. (eds.), Ordovician Odyssey: Short papers for the Seventh International Symposium on the Ordovician System, Pacific Section, Society for Sedimentary Geology.Google Scholar
Perfetta, P. J., Shelton, K. L., and Stitt, J. H. 1999. Carbon isotope evidence for deep water invasion at the Marjumiid-Pterocephaliid Biomere boundary, Black Hills, USA: common origin for biotic crises on Late Cambrian shelves. Geology, 27:403406.2.3.CO;2>CrossRefGoogle Scholar
Stitt, J. H. 1971a. Late Cambrian and earliest Ordovician trilobites: Timbered Hills and Lower Arbuckle Groups, western Arbuckle Mountains, Murray County, Oklahoma. Oklahoma Geological Survey Bulletin, 110:183Google Scholar
Stitt, J. H. 1971b. Repeating evolutionary pattern in Late Cambrian trilobite biomeres. Journal of Paleontology, 45:178181.Google Scholar
Stitt, J. H. 1975. Adaptive radiation, trilobite paleoecology, and extinction, Ptychaspid Biomere, Late Cambrian of Oklahoma. Fossils and Strata, 4:381390.Google Scholar
Stitt, J. H. 1976. Functional morphology and life habits of the Late Cambrian trilobite Stenopilus pronus Raymond. Journal of Paleontology, 50:561576.Google Scholar
Stitt, J. H. 1977. Late Cambrian and earliest Ordovician trilobites, Wichita Mountains area, Oklahoma. Oklahoma Geological Survey Bulletin, 124:179.Google Scholar
Stitt, J. H. 1983. Trilobites, biostratigraphy, and lithostratigraphy of the Mackenzie Hill Limestone (Lower Ordovician), Wichita and Arbuckle Mountains, Oklahoma. Oklahoma Geological Survey Bulletin, 134:154.Google Scholar
Stitt, J. H. 1998. Trilobites from the Cedarina dakotaensis Zone, lowermost part of the Deadwood Formation (Marjuman Stage, Upper Cambrian), Black Hills, South Dakota. Journal of Paleontology, 72:10301046.CrossRefGoogle Scholar
Stitt, J. H., and Miller, J. F. 1987. Jujuyaspis borealis and associated trilobites and conodonts from the Lower Ordovician of Texas and Utah. Journal of Paleontology, 61:112121.CrossRefGoogle Scholar
Stitt, J. H., and Straatmann, W. M. 1997. Trilobites from the upper part of the Deadwood Formation (Upper Franconian and Trempealeauan Stages, Upper Cambrian), Black Hills, South Dakota. Journal of Paleontology, 71:86102.CrossRefGoogle Scholar