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Paleoecology of a Middle Wisconsin Deposit from Southern California

Published online by Cambridge University Press:  20 January 2017

R. Scott Anderson ,
Mitchell J. Power ,
Susan J. Smith ,
Kathleen Springer  and
Eric Scott
R. Scott Anderson*
Affiliation:
Center for Environmental Sciences & Education and Quaternary Sciences Program, Northern Arizona University, Box 5694, Flagstaff, Arizona, 86011
Mitchell J. Power
Affiliation:
Department of Geography, University of Oregon, Eugene, Oregon, 97403
Susan J. Smith
Affiliation:
Bilby Research Center, Northern Arizona University, Flagstaff, Arizona, 86011
Kathleen Springer
Affiliation:
San Bernardino County Museum, 2024 Orange Tree Lane, Redlands, California, 92374
Eric Scott
Affiliation:
San Bernardino County Museum, 2024 Orange Tree Lane, Redlands, California, 92374
*
1To whom correspondence should be addressed. Fax: (928) 523-7423. E-mail: Scott.Anderson@nau.edu.
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Abstract

Analysis of a buried deposit in the Diamond Valley of southern California has revealed well-preserved pollen, wood, and diatom remains. Accelerator mass spectrometry dates of 41,200±2100 and 41,490±1380 14C yr B.P. place this deposit in marine isotope stage 3. Diatoms suggest a shallow lacustrine environment. Pollen data suggest that several plant communities were present near the site, with grassland, scrub, chaparral, forest, and riparian communities represented. Comparison with modern pollen suggests similarities with montane forests in the nearby San Bernardino and San Jacinto ranges, indicating vegetation lowering by at least 900 m elevation and temperatures 4°–5°C cooler than today. An increase in high-elevation conifer pollen documents climatic cooling near the profile top. Early-profile diatoms are typical of warm water with high alkalinity and conductivity, whereas later diatoms suggest a higher flow regime and input of cooler water into the system. We suggest that the sequence is part of the cooling phase of an interstadial Dansgaard–Oeschger cycle. Records of the middle Wisconsin period are rare in southern California, but the Diamond Valley site is similar to records from Tulare Lake in the San Joaquin Valley and the ODP Site 893A record from Santa Barbara Basin. It is probable that the Diamond Valley assemblage is a local expression of a vegetation type widespread in the ranges and basins of southwestern California during the middle Wisconsin.

Keywords

PaleoecologyCaliforniaplant macrofossilspollen analysisdiatom analysismiddle WisconsinDiamond ValleypaleoenviromentsDansgaard-Oeschger cycles
Type
Research Article
Information
Quaternary Research , Volume 58 , Issue 3 , November 2002 , pp. 310 - 317
Copyright
University of Washington

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References

Adam, D.P., Sarna-Wojcicki, A.M., Rieck, H.J., Bradbury, J.P., Dean, W.E., and Forester, R.M. Tulelake, California: The last 3 million years. Palaeogeography, Palaeoclimatology, Palaeoecology 72, (1989). 89 103.CrossRefGoogle Scholar
Anderson, R.S., Betancourt, J.L., Mead, J.I., Hevly, R.H., and Adam, D.P. Middle- and late-Wisconsin paleobotanic and paleoclimatic records from the southern Colorado Plateau, USA. Palaeogeography, Palaeoclimatology, Palaeoecology 155, (2000). 31 57.CrossRefGoogle Scholar
Anderson, R. S, and Koehler, P. A. (in press), Modern pollen and vegetation relationships in the mountains of Southern California, USA, Grana.Google Scholar
Atwater, B.F., Adam, D.P., Bradbury, J.P., Forester, R.M., Mark, R.K., Lettis, W.R., Fisher, G.R., Gobalet, K.W., and Robinson, S.W. A fan dam for Tulare Lake, California, and implications for the Wisconsin glacial history of the Sierra Nevada. Geological Society of America Bulletin 97, (1986). 97 109.2.0.CO;2>CrossRefGoogle Scholar
Axelrod, D.I. Outline history of the California vegetation. Barbour, M.G., and Major, J. Terrestrial Vegetation of California. (1988). California Native Plant Society, Sacramento. 139 194.Google Scholar
Bartlein, P.J., Anderson, K.H., Anderson, P.M., Edwards, M.E., Mock, C.J., Thompson, R.S., Webb, R.S., Webb, T. III, and Whitlock, C. Paleoclimate simulations for North America over the past 21,000 years: Features of the simulated climate and comparisons with paleoenvironmental data. Quaternary Science Reviews 17, (1998). 549 585.CrossRefGoogle Scholar
Behl, R.J., and Kennett, J.P. Brief interstadial events in the Santa Barbara basin, NE Pacific, during the past 60 kyr. Nature 379, (1996). 243 246.CrossRefGoogle Scholar
Benson, L.V., Burdett, J.W., Kashgarian, M., Lund, S.P., Phillips, F.M., and Rye, R.O. Climatic and hydrologic oscillations in the Owens Lake Basin and adjacent Sierra Nevada, California. Science 274, (1996). 746 749.CrossRefGoogle Scholar
Berger, R., and Libby, W.F. UCLA radiocarbon dates. Radiocarbon 8, (1966). 467 497.CrossRefGoogle Scholar
Blinn, D.W., Hevly, R.H., and Davis, O.K. Continuous Holocene record of diatom stratigraphy, paleohydrology, and anthropogenic activity in a spring-mound in southwestern United States. Quaternary Research 42, (1994). 197 205.CrossRefGoogle Scholar
Bond, G.C., and Lotti, R. Iceberg discharges into the North Atlantic on millennial time scales during the last glaciation. Science 267, (1995). 1005 1010.CrossRefGoogle ScholarPubMed
Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., deMenocal, P., Priore, P., Cullen, H., Hajdas, I., and Bonani, G. A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science 278, (1997). 1257 1266.CrossRefGoogle Scholar
Bradbury, J.P. The late Cenozoic diatom stratigraphy and paleolimnology of Tule Lake, Siskiyou Co. California. Journal of Paleolimnology 6, (1991). 205 255.CrossRefGoogle Scholar
Bradley, R.S. Paleoclimatology; Reconstructing Climates of the Quaternary. (1999). Academic Press, San Diego.Google Scholar
Chaney, R.H., and Mason, H.L. A Pleistocene flora from Santa Cruz Island, California. Carnegie Institution of Washington Publication 415, (1930). 1 24.Google Scholar
Chaney, R.H., and Mason, H.L. A Pleistocene flora from the asphalt deposits at Carpenteria, California. Carnegie Institution of Washington Publication 415, (1934). 47 79.Google Scholar
Clements, F.E. Plant Indicators. (1920). Carnegie Institution of Washington, Washington.Google Scholar
Science 241, (1988). 1043 1052.CrossRefGoogle Scholar
Czarnecki, D.B., and Blinn, D.W. Diatoms of the Colorado River in the Grand Canyon National Park and Vicinity. (1978). J. Cramer, Vadus.Google Scholar
Dansgaard, W., Johnsen, S.J., Clausen, H.B., Dahl-Jensen, D., Gundestrup, N.S., Hammer, C.U., Hvidberg, C.S., Steffensen, J.P., Sveinbjörnsdottir, A.E., Jouzel, J., and Bond, G. Evidence for general instability of past climate from a 250-kyr ice-core record. Nature 364, (1993). 218 220.CrossRefGoogle Scholar
Davis, O.K. Pollen analysis of Tulare Lake, California: Great Basin–like vegetation in central California during the full-glacial and early Holocene. Review of Palaeobotany and Palynology 107, (1999). 249 257.CrossRefGoogle Scholar
Fægri, K., and Iversen, J. Textbook of Pollen Analysis. (1989). John Wiley and Sons, Chichester.Google Scholar
Fergusson, G.J., and Libby, W.F. UCLA radiocarbon dates II. Radiocarbon 5, (1963). 1 22.CrossRefGoogle Scholar
Fergusson, G.J., and Libby, W.F. UCLA radiocarbon dates, III. Radiocarbon 6, (1964). 318 339.CrossRefGoogle Scholar
Frost, F.H. The Pleistocene flora of Rancho La Brea. University of California Publications in Botany 14, (1927). 73 98.Google Scholar
Grimm, E.C. CONISS: A Fortran 77 program for stratigraphically constrained cluster analysis by the method of incremental sum of squares. Computers and Geosciences 13, (1987). 13 35.CrossRefGoogle Scholar
Hamilton, J.G. Changing perceptions of pre-European grasslands in California. Madroño 44, (1997). 311 333.Google Scholar
Heusser, L.E. Marine pollen in Santa Barbara Basin, California: A 12,000-yr record. Geological Society of America Bulletin 89, (1978). 673 678.2.0.CO;2>CrossRefGoogle Scholar
Heusser, L.E. Pollen stratigraphy and paleoecologic interpretation of the 160-K.Y. record from Santa Barbara Basin, Hole 893A. Kennett, J.P., Baldauf, J.G., and Lyle, M. Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 146. (1995). Ocean Drilling Program, College Station. 265 279.Google Scholar
Heusser, L.E. Direct correlation of millennial-scale changes in western North American vegetation and climate with changes in the California Current system over the past ∼60 kyr. Paleoceanography 13, (1998). 252 262.CrossRefGoogle Scholar
Hickman, J.C. The Jepson Manual. (1993). Univ. of California Press, Berkeley.Google Scholar
Holland, R. F. 1986, Preliminary descriptions of the terrestrial natural communities of California, California Department of Fish and Game, Sacramento, 156, p. Unpublished mimeo.Google Scholar
Keigwin, L.D., and Jones, G.A. Deglacial climatic oscillations in the Gulf of California. Paleoceanography 5, (1990). 1009 1023.CrossRefGoogle Scholar
Kennett, J.P., and Ingram, B.L. A 20,000-year record of ocean circulation and climate change from the Santa Barbara basin. Nature 377, (1995). 510 514.CrossRefGoogle Scholar
Kennett, J.P., and Venz, K. Late Quaternary climatically related planktonic foraminiferal assemblage changes: Hole 893A, Santa Barbara Basin, California. Kennett, J.P., Baldauf, J.G., and Lyle, M. Proceedings of the Ocean Drilling Program, Scientific Results. (1995). Ocean Drilling Program, College Station. 281 293.Google Scholar
Küchler, A.W. The map of the natural vegetation of California. Barbour, M.G., and Major, J. Terrestrial Vegetation of California. (1988). California Native Plant Society, Sacramento. 909 928.Google Scholar
Lowe, R. L. 1974, Environmental requirements and pollution tolerance of freshwater diatoms, U.S. Environmental Protection Agency, Cincinatti, OH.Google Scholar
Marcus, L.F., and Berger, R. The significance of radiocarbon dates for Rancho La Brea. Martin, P.S., and Klein, R.G. Quaternary Extinctions. (1984). Univ. of Arizona Press, Tucson. 159 188.Google Scholar
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., Moore, T.C., and Shackleton, N.J. Age dating and the orbital theory of the ice ages: Development of a high resolution 0 to 300,000-year chronostratigraphy. Quaternary Research 27, (1987). 1 29.CrossRefGoogle Scholar
Mason, H.L. A Pleistocene flora from the McKittrick asphalt deposits of California. California Academy of Sciences Proceedings 25, (1944). 221 234.Google Scholar
Mensing, S.A., Michaelsen, J., and Byrne, R. A 560-year record of Santa Ana fires reconstructed from charcoal deposited in the Santa Barbara Basin, California. Quaternary Research 51, (1999). 295 305.CrossRefGoogle Scholar
Merriam, J.C. Preliminary report on the horses of Rancho La Brea. Bulletin of the Department of Geological Sciences 7, (1913). 397 418.Google Scholar
Oeschger, H., Stauffer, B., Finkel, R., Langway, C.C. Jr. Variations of the CO2 concentration of occluded air and of anions and dust in polar ice cores. Sundquist, E.T., and Broecker, W.S. The Carbon Cycle and Atmospheric CO2: Natural Variations Archean to Present. (1985). 132 142.Google Scholar
Patrick, R, and Reimer, C. W. 1966, The diatoms of the United States. Vol. I, Monograph 13, Academy Natural Sciences, Philadelphia.Google Scholar
Patrick, R., and Reimer, C.W. The Diatoms of the United States. (1975). Academy Natural Sciences, Philadelphia.Google Scholar
Reynolds, R.E., and Reynolds, R.L. The Pleistocene beneath our feet: Near-surface Pleistocene fossils in inland southern California basins. Woodburne, M.O., Reynolds, R., and Whistler, D.P. Inland Southern California: The last 70 Million Years. (1991). San Bernardino County Museum Association, Redlands. 41 43.Google Scholar
Magnetic Susceptibility and Anisotropy Instrument Operating Manual and Handbook. (1988). Sapphire Instruments, Ruthven.Google Scholar
Shaw, C.A., and Quinn, J.P. Rancho La Brea: A look at southern California's past. California Geology 39, (1986). 123 133.Google Scholar
Springer, K.B., Scott, E., Murray, L.K., and Spaulding, W.G. Partial skeleton of a large individual of Mammut americanum from the Domenigoni Valley, Riverside County, California. Journal of Vertebrate Paleontology 18, (1998). Google Scholar
Springer, K.B., Scott, E., Sagebiel, J.C., and Scott, K.M. A late Pleistocene lake edge vertebrate assemblage from the Diamond Valley, Riverside County, California. Journal of Vertebrate Paleontology 19, (1999). Google Scholar
Stock, C., and Harris, J.M. Rancho La Brea: A record of Pleistocene life in California. Science Series 37 (1992). Natural History Museum of Los Angeles County, Los Angeles.Google Scholar
Svejkovsky, J. Santa Ana airflow observed from wildfire smoke patterns in satellite imagery. Monthly Weather Review 113, (1985). 902 906.2.0.CO;2>CrossRefGoogle Scholar
Thompson, R.S., Whitlock, C., Bartlein, P.J., Harrison, S.P., and Spaulding, W.G. Climatic changes in the western United States since 18,000 yr B.P. Wright, H.E., Kutzbach, J.E., Webb, T. III, Ruddiman, W.F., Street-Perrott, F.A., and Bartlein, P.J. Global Climates since the Last Glacial Maximum. (1993). Univ. of Minnesota Press, Minneapolis. 468 513.Google Scholar
U.S. Dept. of Commerce, (2002). Available at, www5.ncdc.noaa.gov/climatenormals/clim81/Canorm.Google Scholar
van der Werff, A. A new method of concentrating and cleaning diatoms and other organisms. Verhandlungen der Internationalen Vereinigung fur Theoretische and Angewandte Limnologie 12, (1955). 276 277.Google Scholar
Warter, J.K. Late Pleistocene plant communities—Evidence from the Rancho La Brea Tar Pits. Letting, J. Plant Communities of Southern California. (1976). California Native Plant Society, Berkeley. 32 39.Google Scholar
West, G.J. A late Pleistocene pollen record from San Miguel Island, California: Preliminary results. AMQUA Abstracts with Program 13, (1994). 256 Google Scholar