Abstract
THEORIES that explain the extinctions characterizing the Cretaceous/Tertiary (K/T) boundary1-3 need to be tested by analyses of thoroughly sampled biotas. Palynological studies are the primary means for stratigraphic placement of the terrestrial boundary and for estimates of plant extinction4-12, but have not been combined with quantitative analyses of fossil leaves (megaflora). Megafloral studies complement palynology by representing local floras with assemblages capable of high taxonomic resolution13, but have previously lacked the sample size and stratigraphic spacing needed to resolve latest Cretaceous floral history5,14-18. We have now combined megafloral data from a 100-m-thick composite K/T boundary section in North Dakota with detailed palynological analysis. Here the boundary is marked by a 30% palynofloral extinction coincident with iridium and shocked-mineral anomalies and lies ∼2 m above the highest dinosaur remains. The megaflora undergoes a 79% turnover across the boundary, and smaller changes 17- and 25-m below it. This pattern is consistent with latest Cretaceous climatic warming preceding a bolide impact.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
References
Alvarez, L. W., Alvarez, W., Asaro, F. & Michel, H. V. Science 208, 1095–1108 (1980).
Hallam, A. Science 238, 1237–1242 (1987).
Officer, C. B., Hallam, A., Drake, C. L. & Devine, J. D. Nature 326, 143–149 (1987).
Orth, C. J. et al. Science 214, 1341–1343 (1981).
Hickey, L. J. Nature 292, 529–531 (1981).
Orth, C. J. et al. Spec. Pap. geol. Soc. Am. 190, 423–433 (1982).
Smit, J. & van der Kaars, S. Science 223, 1177–1179 (1984).
Pillmore, C. L., Tschudy, R. H., Orth, C. J., Gilmore, J. S. & Knight, J. D. Science 223, 1180–1183 (1984).
Bohor, B. F., Foord, E. E., Modreski, P. J. & Triplehorn, D. M. Science 224, 867–869 (1984).
Nichols, D. J., Jarzen, D. M., Orth, C. J. & Oliver, P. Q. Science 231, 714–717 (1986).
Lerbekmo, J. F., Sweet, A. R. & St Louis, R. M. Bull. geol. Socs. Am. 99, 325–330 (1987).
Bohor, B. F., Triplehorn, D. M., Nichols, D. J. & Millard, H. T. Jr Geology 15, 896–899 (1987).
Gray, J. in Late Cenozoic History of the Pacific Northwest (ed. Smiley, C. J.) 185–244 (Pacific Division of the American Association for the Advancement of Science, 1985).
Dorf, E. Publs Carnegie Instn 508, 1–159 (1942).
Hickey, L. J. Spec. Pap. Univ. Mich. Mus. Paleont. 24, 33–49 (1980).
Brown, R. W. Prof. Pap. U.S. geol. Surv. 375 (1962).
Wolfe, J. A. & Upchurch, G. R. Jr Proc. natn. Acad. Sci. U.S.A. 84, 5096–5100 (1987).
Wolfe, J. A. & Upchurch, G. A. Jr Nature 324, 148–151 (1986).
Fastovsky, D. E. Palaios 2, 282–295 (1987).
Belt, E. S. et al. Spec. Publn Int. Ass. Sed. Geol. 177–195 (1984).
Moore, W. Rept Inv. North Dakota geol. Surv. 56 (1976).
Johnson, K. R. thesis, Yale Univ. (1989).
Izett, G. A. Open-File Rept. U.S. geol. Surv. 87–606 (1987).
Tschudy, R. H., Pillmore, C. L., Orth, C. J., Gilmore, J. S. & Knight, J. D. Science 225, 1030–1032 (1984).
Fleming, R. F. & Nichols, D. J. Palynology 12, 238 (1988).
Sweet, A. R. & Lerbekmo, J. F. Eos 69, 301 (1988).
Lee W. T. & knowlton, F. H. Prof. Pap. U.S. geol. Surv. 101, (1917).
Johnson, K. R. & Hickey, L. J. Lunar and Planetary Inst. Contrib. 673, 87 (1988).
Chandrasekharem, A. Paleontographica B147, 1–38 (1974).
Knowlton, F. H. Prof. Pap. U.S. geol. Surv. 155 (1930).
Johnson, K. R. thesis, Univ. Pennsylvania (1985).
Nichols, D. J., Jacobson, S. R. & Tschudy, R. H. in Geologic Studies of the Cordilleran Thrust Belt (ed. Powers, R. B.) 721–733 (Rocky Mountain Association of Geologists. 1982).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Johnson, K., Nichols, D., Attrep, M. et al. High-resolution leaf-fossil record spanning the Cretaceous/Tertiary boundary. Nature 340, 708–711 (1989). https://doi.org/10.1038/340708a0
Received:
Accepted:
Issue date:
DOI: https://doi.org/10.1038/340708a0
This article is cited by
-
The biodiversity crisis and the future of evolution
The Environmentalist (1996)