Kathryn M. Gregory-Wodzicki
Lamont-Doherty Earth Observatory of Columbia
University, Box 1000,
61 Route 9W
Palisades, NY 10964-8000
USA
gregory@ldeo.columbia.edu
My
research centers on using botanically-based indicators of climate to
study
the topographic evolution of the North American and Andean
Cordilleras.
PUBLICATIONS:
Andes
| Western US
| Leaf
morphologic method | CO2 | Fossil
tree
rings
CONFERENCES:
Segundo
Encuentro
de Investigaciones Fitolíticas del Cono Sur
COURSES: Introduccion a Paleoclima y
Paleoecologia
new!
WEB RESOURCES
c 1999 Tony Kraps
5. Gregory-Wodzicki, K.M, Velasquez, K., and McIntosh, W.C., 1998, Paleoclimate and paleoelevation of the late Miocene Jakokkota flora, Bolivian Altiplano: Journal of South American Earth Sciences, v. 11, p. 533-560. [PDF] [Photos, leaf fossils]
6. Gregory-Wodzicki, K.M., Graham, A., and Hinojosa, L.F., 2000, Dos floras del Mioceno tardio de Bolivia: implicaciones climáticas y tectónicas de los Andes Centrales, XI Congreso de Paleobotanica de Argentina. [Resumen]
Also, see: Gregory-Wodzicki, K.M., 2000, Relationships between leaf morphology and climate, Bolivia: Implications for estimating paleoclimate from fossil floras: Paleobiology, v. 26, p. 668-688. [Abstract] [PDF file] new!
Image processed by Cornell Andes Project
1. Chase, C.G., Gregory-Wodzicki, K.M., Parrish-Jones, J.T., DeCelles, P., 1998, Topographic history of the western Cordillera of North America and controls on climate, in Crowley, T.J., and Burke, K., Tectonic Boundary Conditions for Climate Model Simulations: Oxford Monographs on Geology and Geophysics, Oxford University Press, 73-99. [Abstract] [Summary diagram, uplift history of the western US]
2. Gregory, K.M., 1997, The late Eocene House Range Flora, Sevier Desert, Utah: Paleoclimate and paleoelevation: PALAIOS, v. 12, p. 552-567. [Abstract] [Press release on related article]
3. Gregory, K.M., 1994, Palaeoclimate and palaeoelevation of the 35 Ma Florissant flora, Front Range, Colorado: Palaeoclimates, v.1, p 23-57.
4. Gregory, K.M., and Chase, C.G., 1992, Tectonic significance of paleobotanically estimated climate and altitude of the late Eocene erosion surface, Colorado: Geology, v. 20, p.581-585.
5. Gregory, K.M., and Chase, C.G., 1994, Stable isotope study of fluid inclusions in fluorite from Idaho: Implications for continental climates during the Eocene COMMENT: Geology, v.22, p. 275-276.
6. Gregory, K.M., and Chase, C.G., 1994, Tectonic and climatic significance of a late Eocene low-relief, high-level geomorphic surface, Colorado: JGR, v. 99, no. B10, p 20,141-20,160.
7. Gregory, K. M., and McIntosh, W. C., 1996, Paleoclimate and paleoelevation of the Oligocene Pitch-Pinnacle flora, Sawatch Range, Colorado: GSA Bulletin, v. 108, p. 545-561. [Abstract] [Data Repository material]
8. Wolfe, J.A.,
Gregory-Wodzicki, K.M., Molnar, P., and
Mustoe, G., 1999, Paleobotanical
evidence for the development of high altitudes
during the early Eocene in
northwestern North America [abs.]: Goteborg,
Sweden. [Abstract] [Meeting
summary]
2. Gregory, K.M., 1994, New prospects in old bubbles: Nature, v. 372, p. 407-408.
3. Gregory, K.M., 1996, Are
paleoclimate estimates biased
by foliar physiognomic response to elevated
atmospheric CO2?: Palaeo-3,
v. 124, p. 39-51.
[Abstract] [PDF
file] new!
On fossil tree rings
and climate:
1. Gregory, K.M., in press, Paleoclimatic Implications of Tree-ring Growth Characteristics of 35 Ma Sequoia affinis from Florissant, Colorado as Compared to Modern Coast Redwood and Giant Sequoia, in Evanoff, E., ed. Proceedings of the Denver Natural History Museum. [Abstract]
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Last modified: April 27, 2001