Research |
Paleolimnology & Paleoclimatology
In the US Great Basin
We have an active research program studying the history
of lakes associated with the US Basin and Range Province. Much of
the information we have obtained about this history is derived from
scientific drilling campaigns, which have yielded long sediment cores
from old lake deposits. Primary study areas for this work have been
the Great Salt Lake/Lake Bonneville & Bear Lake, Utah, and Summer
Lake, Oregon.
Great Salt Lake/Lake Bonneville & Bear Lake,
Utah
We have studied drilling and seismic records of the
Great Salt Lake (GSL) basin collected by AMOCO to interpret basin
history, paleolimnology, and palynology over the last 10 million
years (Davis and Moutoux, 1998; Kowalewska and Cohen, 1998; Davis,
2002). Using the dedicated Global Lakes Drilling system, the GLAD800,
our colleagues at the USGS, the University of Minnesota's Limnological
Research Center, and the UA have obtained a series of cores (the
longest being over 120m) spanning the last ~270,000 years of pluvial
lake history from the Great
Salt Lake and Bear Lake (Dean et al., 2002; Balch, 2003
and in prep.). Neogene records of the basin indicate it was occupied
by a series of extensive marshes over much of its history, linked
with the Paleolake Idaho drainage to the north, with the GSL Basin
as the terminus of the drainage system. Extensive lakes only began
to evolve in the Quaternary. The GSL record is also notable for providing
evidence of major cyclical crashes in lake level and salinity crises
in the lake at the even/odd oxygen isotope stage boundaries, following
several major lake high stands in the late parts of OIS 6, 4 and
2.
Balch, D., 2003 and in prep. "Quaternary ostracode
paleoecology and its link to climate change in the Bonneville Basin:
A detailed study of the GLAD800 core GSL00-4, Great Salt Lake, Utah." MS
Thesis, Univ. of Arizona.
Davis, O.K., 2002. "Late Neogene environmental
history of the Northern Bonneville Basin: A review of palynological
studies." In Herschler, R., Madsen, D.B. and Currey, D.R. (eds.) "Great
Basin Aquatic Systems History Smithsonian Contributions to Earth." Sciences 33:295-308.
Davis, O.K. and Moutoux, T., 1998. "Tertiary
and Quaternary vegetation history of the Great Salt Lake. Jour." Paleolimnology 19:417-427.
Dean, W., Rosenbaum, J., Haskell, B., Kelts, K.,
Schnurrenberger, D., Valero-Garces, B., Cohen, A.S., Davis, O.K.,
Dinter, D., and Nielson, D., 2002. "Progress in global lake
drilling holds potential for global change research." EOS 83:85,
90-91.
Kowalewska, A. and Cohen, A.S., 1998. "Reconstruction
of paleoenvironments of the Great Salt Lake Basin during the late
Cenozoic." Jour. Paleolimnology 20:381-407.
Summer Lake, Oregon
At Summer Lake, we have obtained a 250,000 year record
of climate change in the northwestern Great Basin, where it meets
the Cascade Mountains (Palacios-Fest et al., 1993; Cohen et al.,
2000 and Negrini et al, 2000). A combination of sedimentologic, paleoecologic,
environmental magnetic, and geochemical data indicates fluctuations
in the levels and salinity of Summer Lake and its predecessor, Lake
Chewaucan, in synchrony with the marine oxygen isotope record of
global glacial advances. The Summer Lake record is notable for providing
clear evidence of the power of using minor element ratios in ostracode
crustacean shells for the quantitative inference of paleolimnological
parameters, especially the use of Mg/Ca ratios to infer paleotemperatures.
Cohen, A.S., Palacios-Fest, M. R., Negrini, R., Wigand,
P. and Erbes, D., 2000. "A paleoclimate record for the past
250,000 years from Summer Lake, Oregon, USA II Sedimentology, paleontology
and geochemistry." Jour. Paleolimnology 24:151-182.
Negrini, R.M., Erbes, D., Faber, K., Herrera, A.M.,
Roberts, A.P., Cohen, A.S., Wigand, P.E., and Foit, F.F., 2000. "A
paleoclimate record for the past 250,000 years from Summer Lake,
Oregon, USA I Chronology and magnetic proxies for lake level." Jour.
Paleolimnology 24:125-149.
Palacios-Fest, M.R., Cohen, A.S., Ruiz, J. and Blank,
B., 1993. "Comparative paleoclimatic interpretations from nonmarine
ostracodes using faunal assemblages, trace element shell chemistry
and stable isotope data." In Swart, P.K. et al. (eds.) "Climate
Change in Continental Isotopic Records AGU Geophys." Monogr.
78:179-190. |