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Dinosaur Breath: Change, Other Kinds of Fossils and Jurassic Park

Published online by Cambridge University Press:  26 July 2017

Diane Bellis*
Affiliation:
U.S. Department of Agriculture, Office of International Cooperation and Development, Research and Exchanges Division, Room 3236 South Building, Washington, D.C. 20250
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Extract

During the latest Cretaceous, before the demise of the last dinosaur, there were ferns, palm trees, and crocodiles in what is now desert in New Mexico, Seymour Island in Antarctica, and the Gobi Desert. Then things changed. Ferns, palm trees, and crocodiles no longer live in New Mexico, Antarctica, or the Gobi Desert because the climate changed. Throughout the 4.6 billion year history of the Earth, internal and external forces have caused changes in the very thin surface layer of the Earth where life exists.

Type
Bring 'em Back Alive
Copyright
Copyright © 1994 Paleontological Society 

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References

References and Further Reading

Barry, T.H. 1932. Natural Varnish Resins. Ernest Benn, London, 294 p.Google Scholar
Bellis, D. 1990. The Characterization of Late Cretaceous (Campanian-Maastrictian) Fossil Resin from the Fossil Forest Study Area, San Juan Basin, New Mexico, unpublished dissertation, 110 p.Google Scholar
Bellis, D. and Wolberg, D.L. 1991. Analysis of gaseous inclusions in fossil resin from a Late Cretaceous stratigraphic sequence. Paleoegeography, Palaeoclimatology, Palaeoecology (Global and Planetary Change Section), 97:6992.CrossRefGoogle Scholar
Berger, A. 1977. Long-term variation of the Earth's orbital elements, Celestial Mechanics, 15:5374.Google Scholar
Berner, R.A. and Landis, G.P. 1988. Gas bubbles in fossil amber as possible indicators of the major composition of ancient air, Science, 239: 14061409.CrossRefGoogle ScholarPubMed
Berner, R.A. and Canfield, D.F. 1989. A new model for atmospheric oxygen of Phanerozoic time, American Journal of Science, 39:333361.Google Scholar
Beck, C.W., 1986. Spectroscopic investigations of amber, Applied Spectroscopy Reviews, 22:57110.Google Scholar
Fraquet, H. 1987. Amber. Butterworths, London, 175 p.Google Scholar
Grimaldi, D. Beck, C.W., and Boon, J.J. 1989. Occurrence, chemical characteristics and paleontology of the fossil resins from New Jersey, American Museum Novitates, 2948, 28 p.Google Scholar
Hays, J.D., Imbrie, J. and Shackleton, N.J. 1976. Variations in the Earth's orbit: Pacemaker of the Ice Ages, Science, 194:11211132.CrossRefGoogle ScholarPubMed
Helm, O. 1891. Uber den Succinit und die ihm verwandten fossilen Harze, Schriften der naturforsch. Geselschaft, Danzig, 7: 189203.Google Scholar
Howes, F.N. 1949. Vegetable Gums and Resins, Chronica Botanica, Waltham, MA, 188p.Google Scholar
Hueber, F.M. 1983. Fossil woods and resin-like substances from the Lee Creek Mine, North Carolina, I. Smithsonian Contributions to Paleobiology, 53, Smithsonian Institution Press, Washington, p. 269285.Google Scholar
Imbrie, J. and Imbrie, K.P. 1979. Ice Ages: Solving the Mystery, Harvard University Press, Cambridge, 223 p.Google Scholar
International Geosphere Biosphere Program: A Study of Global Change, Report # 12. 1990. p. 7121.Google Scholar
Langenheim, J.H. 1964. Present Status of Botanical Studies of Ambers, Harvard University Botanical Museum Leaflet, 20: 225287.Google Scholar
Langenheim, J.H. 1968. Catalogue of Infrarerd Spectra of Fossil Resins (Ambers). I. North and South America, Botanical Museum Leaflets, Harvard University, 22:65120.Google Scholar
Langenheim, J.H. and Beck, C.W. 1965. Infrared spectra as a means of determining botanical sources of amber, Science, 149:5255.Google Scholar
Langenheim, R.L., Smiley, C.J., and Gray, J. 1960. Cretaceous amber from the Arctic coastal plain of Alaska, Bulletin of the Geological Society of America, 72: 13451356.Google Scholar
Nissenbaum, A. 1975. Lower Cretaceous amber from Israel, Naturwissenschaften, 62:34313432.CrossRefGoogle Scholar
Schluter, T. 1983. A fossiliferous resin from the Cenomanian of the Paris and Aquitanian Basins of northwestern France, Cretaceous Research, 4:265269.Google Scholar
White, D. 1913. Resins in Paleozoic plants and in coals of high rank: USGS Professional Paper, 85: 6597.Google Scholar