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Early Holocene Juniper Woodland and Chaparral Taxa in the Central Baja California Peninsula, Mexico

Published online by Cambridge University Press:  20 January 2017

David Rhode
David Rhode*
Affiliation:
Earth and Ecosystem Sciences, Desert Research Institute, 2215 Raggio Parkway, Reno, Nevada, 89512
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Abstract

A packrat midden located in the Sierra San Francisco, Baja California Sur, Mexico, dating to ca. 10,200 14C yr B.P., contains remains of California juniper (Juniperus californica) and other taxa now associated with southern California chaparral. California juniper does not occur in the Sierra San Francisco today, although “relict” populations of a few chaparral taxa still occur at higher elevations. This midden record documents the early Holocene occurrence of Baja California coniferous woodland and chaparral vegetation far south of its present distribution or its previously known extent from other fossil records. Based on modern climatic tolerances of California juniper and other taxa, central Baja California experienced a mild Mediterranean-type climate at least 5°–6°C cooler than the climate of today, with at least twice the winter precipitation the region now receives.

Keywords

Packrat middensNeotomaBaja Californiaearly HolocenechaparralJuniperus californica
Type
Research Article
Information
Quaternary Research , Volume 57 , Issue 1 , January 2002 , pp. 102 - 108
Copyright
University of Washington

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References

Amundson, R., Franco-Vizcaino, E., Graham, R.C., and DeNiro, M. The relationship of precipitation seasonality to the flora and stable isotope chemistry of soils in the Vizcaı́no desert, Baja California, México. Journal of Arid Environments 28, (1994). 265–279.Google Scholar
Axelrod, D.I. California Academy of Sciences Occasional Papers 132, (1979). 1–74.Google 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., Currey, D., Lao, Y., and Hostetler, S. Lake-size variations in the Lahontan and Bonneville basins between 13,000 and 9000 14C yr B.P. Palaeogeography, Palaeoclimatology, Palaeoecology 95, (1992). 19–32.Google Scholar
Betancourt, J.L., Van Devender, T.R., and Martin, P.S. Packrat Middens: The Last 40,000 Years of Biotic Change. (1990). Univ. of Arizona Press, Tucson.Google Scholar
Clark, W.H., and Sankey, J.T. Late Holocene Sonoran Desert arthropod remains from a packrat midden, Cataviña, Baja California Norté, México. Pan-Pacific Entomologist 75, (1999). 183–199.Google Scholar
Cody, M.L., Moran, R., and Thompson, H. The plants. Case, T.J., and Cody, M.L. Island Biogeography in the Sea of Cortéz. (1983). Univ. of California Press, Berkeley. 49–97.Google Scholar
Doose, H., Prahl, F.G., and Lyle, M.W. Biomarker temperature estimates for modern and last glacial surface waters of the California Current system between 33° and 42°N. Paleoceanography 12, (1997). 615–622.Google Scholar
Gardner, J.V., Dean, W.E., and Dartnell, P. Biogenic sedimentation beneath the California Current system for the past 30 kyr and its paleoceanographic significance. Paleoceanography 12, (1997). 207–225.CrossRefGoogle Scholar
Gould, F.W., Moran, R. San Diego Society of Natural History Memoir 12, (1981). 1–140.Google Scholar
Hastings, J. R, and Humphrey, R. R. (1969). Climatological Data and Statistics for Baja California. University of Arizona Institute for Atmospheric Sciences Technical Reports on the Meteorology and Climatology of Arid Regions 18, Univ. of Arizona, Tucson.Google Scholar
Hastings, J.R., and Turner, R.M. Seasonal precipitation regimes in Baja California, Mexico. Geografiska Annaler A 47, (1965). 204–223.Google Scholar
Herbert, T.D., Schuffert, J.D., Andreasen, D., Heusser, L., Lyle, M., Mix, A., Ravelo, A.C., Stott, L.D., and Herguera, J.C. Collapse of the California Current during glacial maxima linked to climate change on land. Science 293, (2001). 71–76.Google Scholar
Heusser, L. 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
Heusser, L.E., and Sirocko, F. Millennial pulsing of environmental change in southern California from the past 24 k. y.: A record of Indo-Pacific ENSO events?. Geology 25, (1997). 243–264.2.3.CO;2>CrossRefGoogle Scholar
Hyland, J.R., and Gutiérrez, M.d.l.L. An obsidian fluted point from central Baja California. Journal of California and Great Basin Anthropology 17, (1995). 126–128.Google Scholar
Keigwin, L.D., and Jones, G.A. Deglacial climatic oscillations in the Gulf of California. Paleoceanography 5, (1990). 1009–1023.Google 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.Google Scholar
Kennett, J.P., and Venz, K. Late Quaternary climatically related planktonic foraminiferal assemblage changes: Hole 893A, Santa Barbara Basin, California. Proceedings of the Ocean Drilling Program, Scientific Results 146, (1995). 281–293.Google Scholar
Markham, C.G. Baja California's climate. Weatherwise 25, (1972). 64–76.Google Scholar
Metcalfe, S.E., O'Hara, S.L., Caballero, M., and Davies, S.J. Records of Late Pleistocene-Holocene climatic change in Mexico—A review. Quaternary Science Reviews 19, (2000). 699–721.Google Scholar
Mikolajewicz, U., Crowley, T.J., Schiller, A., and Voss, R. Modeling teleconnections between the North Atlantic and North Pacific during the younger Dryas. Nature 387, (1997). 384–387.Google Scholar
Mix, A. C., Lund, D. C., Pisias, N. G., Bodén, P., Bornmalm, L., Lyle, M., and Pike, J. (1999). Rapid climate oscillations in the northeast Pacific during the last deglaciation reflect Northern and Southern Hemisphere sources.. In Mechanisms of Global Climate Change at Millennial Time Scales Clark, P. U., Webb, R. S., and Keigwin, L. D., Eds., pp. 127–148. Geophysical Monograph 112, Am. Geophy. Union, Washington, DC.CrossRefGoogle Scholar
Mooney, H. (1977). Southern coastal scrub.. In Terrestrial Vegetation of California Major, J. and Barbour, M., Eds., pp. 471–490. Wiley-Interscience, New York.Google Scholar
Moran, R. (1983). Appendix 4.5: Relictual northern plants on peninsular mountain tops.. In Island Biogeography in the Sea of Cortéz Case, T. J. and Cody, M. L., Eds., pp. 408–410. Univ. of California Press, Berkeley.Google Scholar
Mortyn, P.G., Thunell, R.C., Anderson, D.M., Stott, L.D., and Le, J. Sea surface temperature changes in the southern California borderlands during the last glacial–interglacial cycle. Paleoceanography 11, (1996). 415–430.Google Scholar
Orr, R.T. An analysis of the recent land mammals. Systematic Zoology 9, (1960). 171–179.Google Scholar
Peñalba, M. C, and Van Devender, T. R. (1997). Pollen analysis of late Wisconsin and Holocene packrat (Neotoma) middens from San Fernando and Cataviña, Baja California, Mexico. In, Second Annual Baja California Botanical Symposium, San Diego Natural History Museum, San Diego.Google Scholar
Peñalba, M.C., and Van Devender, T.R. Cambios de vegetación y clima en Baja California, México, durante los últimos 20,000 años. Geologia del Noroeste 2, (1998). 21–31.Google Scholar
Quade, J., Forester, R.M., Pratt, W.L., and Carter, C. Black mats, spring-fed streams, and Late-Glacial-age recharge in the southern Great Basin. Quaternary Research 49, (1998). 129–148.Google Scholar
Reasoner, M., and Jodry, M.A. Rapid response of alpine timberline vegetation to the younger Dryas climate oscillation in the Colorado Rocky Mountains, USA. Geology 28, (2000). 51–54.Google Scholar
Reyes, S., Miranda, F., and Daget, P. (1988). Interannual variability of the rainfall field over Baja California: Middle-latitude versus tropical influences.. In Time Scales and Water Stress: Proceedings of the Fifth International Conference on Mediterranean Ecosystems di Castri, F., Floret, C., Rambal, S., and Roy, J., Eds., pp. 373–380. International Union of Biological Sciences, Paris.Google Scholar
Sankey, J.T., Van Devender, T.R., and Clark, W.H. Late Holocene plants, Cataviña, Baja California. The Southwestern Naturalist 46, (2001). 1–7.Google Scholar
Shreve, F. The transition from desert to chaparral in Baja California. Madroño 3, (1936). 257–264.Google Scholar
Shreve, F. (1951). Vegetation of the Sonoran Desert. Carnegie Inst. of Washington Publication 591, Washington, DC.Google Scholar
Spaulding, W.G., and Graumlich, L. The last pluvial climatic episodes in the deserts of southwestern North America. Nature 320, (1986). 441–444.CrossRefGoogle Scholar
Stuiver, M., and Reimer, P.J. Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon 35, (1993). 215–230.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, F.G., v. d. Plicht, J., and Spurk, M. INTCAL98 radiocarbon age calibration 24,000 – 0 cal BP. Radiocarbon 40, (1998). 1041–1083.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., and Braziunas, T.F. High-precision radiocarbon age calibration for terrestrial and marine samples. Radiocarbon 40, (1998). 1127–1151.Google Scholar
Thompson, R. S., Whitlock, C., Bartlein, P. J., Harrison, S. P., and Spaulding, W. G. (1993). Climate changes in the western United States since 18,000 yr B.P.. In Global Climates Since the Last Glacial Maximum Wright, H. E. Jr., Kutzbach, J. E., Webb, T. III, Ruddiman, W. F., Street-Perrott, F. A., and Bartlein, P. J., Eds., pp. 468–513. Univ. of Minnesota Press, Minneapolis.Google Scholar
Thompson, R.S., Anderson, K.H., Bartlein, P.J. U.S. Geological Survey Professional Paper 1650A. (1999). Google Scholar
Turner, R.M., and Brown, D.E. Sonoran desertscrub. Desert Plants 4, (1982). 181–224.Google Scholar
Turner, R. M, Bowers, J. E, and Burgess, T. L. (1995). Sonoran Desert Plants: An Ecological Atlas. Univ. of Arizona Press, Tucson.Google Scholar
Van Devender, T. R. (1990). Late Quaternary vegetation and climate of the Sonoran Desert, United States and Mexico.. In Packrat Middens: The Last 40,000 Years of Biotic Change Betancourt, J. L., Van Devender, T. R., and Martin, P. S., Eds., pp. 134–165. Univ. of Arizona Press, Tucson.Google Scholar
Van Devender, T. R. (1997). 21,000 years of vegetation change in the northern Vizcaı́no, Baja California. In, Second Annual Baja California Botanical Symposium, San Diego Natural History Museum, San Diego, CA.Google Scholar
Van Devender, T. R., Thompson, R. S., and Betancourt, J. L. (1987). Vegetation history of the deserts of southwestern North America: The nature and timing of the Late. Wisconsin–Holocene transition.. In North America and Adjacent Oceans during the Last Deglaciation Ruddiman, W. F. and Wright, H. E. Jr., Eds. pp. 323–352. The Geology of North America, K-3. Geol. Soc. Am. Boulder, CO.Google Scholar
Van Devender, T. R., Toolin, L. J., and Burgess, T. L. (1990a). The ecology and paleoecology of grasses in selected Sonoran Desert plant communities.. In Packrat Middens: The Last 40,000 Years of Biotic Change Betancourt, J. L., Van Devender, T. R., and Martin, P. S., Eds., pp. 326–349. Univ. of Arizona Press, Tucson.Google Scholar
Van Devender, T.R., Burgess, T.L., Felger, R.S., and Turner, R.M. Holocene vegetation of the Hornaday Mountains of Northwestern Sonora, Mexico. Proceedings of the San Diego Society of Natural History 2, (1990). 1–19.Google Scholar
Van Devender, T.R., Burgess, T.L., Piper, J.C., and Turner, R.M. Paleoclimatic implications of Holocene plant remains from the Sierra Bacha, Sonora, Mexico. Quaternary Research 41, (1994). 99–108.Google Scholar
Wells, P.V. The manzanitas of Baja California, including a new species of Arctostaphylos . Madroño 21, (1972). 268–273.Google Scholar
Wells, P.V. Macrofossil analysis of woodrat, Neotoma, middens as a key to the Quaternary vegetational history of arid America. Quaternary Research 6, (1976). 223–248.Google Scholar
Wells, P. V. (1987). Systematics and distribution of pinyons in the late Quaternary.. In Proceedings—Pinyon-juniper Conference Everett, R. L., Ed., pp. 104–108. USDA Forest Service, Intermountain Research Station, Ogden, UT.Google Scholar
Wiggins, I. L. (1980). Flora of Baja California. Stanford Univ. Press, Stanford, CA.Google Scholar
Zippin, D.B., and Vanderwier, J.M. Scrub community descriptions of the Baja California peninsula, Mexico. Madroño 41, (1994). 85–119.Google Scholar