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Paleoclimatic Reconstruction Using the Correlation in δ18O of Hackberry Carbonate and Environmental Water, North America

Published online by Cambridge University Press:  20 January 2017

A. Hope Jahren ,
Ronald Amundson ,
Carol Kendall  and
Peter Wigand
A. Hope Jahren
Affiliation:
Department of Earth and Planetary Sciences, The Johns Hopkins University, Baltimore, Maryland, 21218,, E-mail: jahren@jhu.edu
Ronald Amundson
Affiliation:
Division of Ecosystem Sciences, Department of Environmental Science, Policy and Management, University of California, Berkeley, California, 94720
Carol Kendall
Affiliation:
Water Resources Division, United States Geological Survey, Menlo Park, California, 94025
Peter Wigand
Affiliation:
Great Basin and Mojave Paleoenvironmental Consulting, Reno, Nevada, 89506
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Abstract

Celtis sp. (commonly known as “hackberry”) fruits were collected from 101 North American sites located in 13 states and one Canadian province between the years of 1979–1994. The biomineralized carbonate endocarp of the hackberry, which is a common botanical fossil found throughout the Quaternary sediments of the Great Plains, was analyzed for its δ18O value and plotted against the δ18O value of site environmental water to demonstrate the potential of the hackberry as a paleoclimate indicator. This correlation was reinforced by intensive studies on extracted tissue-water δ18O value and hackberry endocarp carbonate δ18O value from three trees in Sterling, Colorado. The observed correlation in the large data set between hackberry endocarp carbonate δ18O value and environmental water is [endocarp δ18O=38.56+0.69×environmental water δ18O] (R=0.88; R2=0.78; p value<0.0001). The relation of the hackberry carbonate to temperature in the Great Plains was the following: (average daily-maximum growing season temperature [°C])=6.33+0.67 (δ18O of endocarp carbonate) (R=0.73; R2=0.54; p value=0.0133). The δ18O value of early Holocene fossil hackberry carbonate in the Pintwater Cave, southern Nevada, suggested precipitation δ18O values more positive than today (∼−4‰ early Holocene vs ∼−9 to −10‰ today). This shift, combined with paleobotanical data, suggests an influx of summer monsoonal moisture to this region in the early Holocene. Alternatively, the more positive δ18O values could be viewed as suggestive of warmer temperatures, although the direct use of Great Plains hackberry/temperature relationships to the Great Basin is of debatable value.

Keywords

oxygen isotopepaleoclimatehackberry carbonate
Type
Research Article
Information
Quaternary Research , Volume 56 , Issue 2 , September 2001 , pp. 252 - 263
Copyright
University of Washington

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References

Abell, P.I Oxygen isotope data in modern African gastropod shells: A data base for paleoclimatology. Chemical Geology (Isotope Geoscience Section) 58, (1985). 193–193.Google Scholar
Amundson, R, Chadwick, O.A, Kendall, C, Wang, Y, and DeNiro, M Isotopic evidence for shifts in atmospheric circulation patterns during the late Quaternary in North America. Geology 24, (1996). 23 26.Google Scholar
Brown, W.J, Wells, S.G, Enzel, Y, Anderson, R.Y, McFadden, L.D, and Reynolds, J The late Quaternary history of Lake Mojave and the evolution of the lower Mojave River drainage basin, Southern California. Abstracts of Papers Presented at the Mojave Desert Quaternary Research Center Fourth Annual Symposium. (1990). p. 23 Google Scholar
Buck, P.E, Hockett, B, Nials, F, and Wigand, P.E Prehistory and Paleoenvironment at Pintwater Cave, Nevada: Results of Field Work During the 1996 Season. (1997). Desert Research Institute, Reno/Las Vegas. p. 101 Google Scholar
Coleman, M.L, Shepard, T.J, Durham, J.J, Rouse, J.E, and Moore, G.R Reduction of water with zinc for hydrogen isotope analysis. Analytical Chemistry 54, (1982). 993 995.Google Scholar
Condon, A.G, Richards, R.A, and Farquhar, G.D Relationships between carbon isotope discrimination, water use efficiency and transpiration efficiency for dryland wheat. Australian Journal of Agricultural Research 44, (1993). 1693 1711.Google Scholar
Cowan, M.R, Gabel, M.L, Jahren, A.H, and Tieszen, L.L Growth and biomineralization of Celtis occidentalis (Ulmaceae) pericarps. American Midland Naturalist 137, (1997). 266 273.CrossRefGoogle Scholar
Craig, H Isotopic variations in meteoric waters. Science 133, (1961). 1702 1703.CrossRefGoogle ScholarPubMed
Dansgaard, W Stable isotopes in precipitation. Tellus 16, (1964). 436 468.Google Scholar
Dawson, T.E, and Ehleringer, J.R Streamside trees that do not use stream water. Nature 350, (1991). 335 337.CrossRefGoogle Scholar
DeBolt, A.M The Ecology of Celtis reticulata Torr. (Netleaf Hackberry) in Idaho. (1992). Oregon State University, p. 161 Google Scholar
Ehleringer, J.R, and Dawson, T.E Water uptake by plants: Perspectives from stable isotope composition. Plant, Cell and Environment 15, (1992). 1073 1082.Google Scholar
Elias, T.S The Complete Trees of North America. (1980). Times Mirror Magazines, New York. p. 948 Google Scholar
Epstein, S, and Mayeda, T Variations of 18O content of water from natural sources. Geochimica et Cosmochimica Acta 54, (1953). 1845 1846.Google Scholar
Farquhar, G.D, O'Leary, M.H, and Berry, J.A On the relationship between carbon isotope discrimination and the intercellular carbon dioxide concentration in leaves. Australian Journal of Plant Physiology 9, (1982). 121 137.Google Scholar
Flanagan, L.B, and Ehleringer, J.R Stable isotope composition of stem and leaf water: Applications to the study of plant water use. Functional Ecology 5, (1991). 270 277.Google Scholar
Fricke, H.C, and O'Neil, J.R The correlation between 18O/16O ratios of meteoric water and surface temperature: Its use in investigating terrestrial climate change over geologic time. Earth and Planetary Science Letters 170, (1999). 181 196.Google Scholar
Friedman, I, Smith, G.I, Gleason, J.D, Warden, A, and Harris, J.M Stable isotope composition of Waters in southeastern California. 1. Modern precipitation. Journal of Geophysical Research 97, (1992). 395 400.Google Scholar
Gat, J.R The isotopes of hydrogen and oxygen in precipitation. Fritz, P, and Fontes, J.C Handbook of Environmental Isotope Geochemistry. (1981). Elsevier, Amsterdam. 21 47.Google Scholar
Harvey, A.M, Wigand, P.E, and Wells, S.G Response of alluvial fan systems to the late Pleistocene to Holocene climatic transition: Contrasts between the margins of pluvial Lakes Lahontan and Mojave, Nevada and California, U.S.A. Caten 36, (1999). 255 281.CrossRefGoogle Scholar
Jahren, A.H The Stable Isotope Composition of the Hackberry (Celtis) and Its Use as a Paleoclimate Indicator. (1996). University of California at Berkeley, p. 136 Google Scholar
Jahren, A.H, Gabel, M.L, and Amundson, R Biomineralization in seeds: Developmental trends in isotopic signatures of hackberry. Palaeogeography, Palaeoclimatology, Palaeoecology 138, (1998). 259 269.CrossRefGoogle Scholar
Kendall, C, and Coplen, T Distribution of Oxygen-18 and Deuterium in river waters across the United States. Hydrological Processes 15, (2001). 1363 1393.CrossRefGoogle Scholar
Little, E. L. (1971). Atlas of United States Trees: Volume 1: Conifers and Important Hardwoods, U. S. Department of Agriculture. Forest Service, Division of Timber Management Research, Washington, D.C., Miscellaneous Publication 1146, 200, maps.Google Scholar
Little, E.L Atlas of United States Trees: Volume 3: Minor Western Hardwoods. (1976). U.S. Department of Agriculture. Forest Service, Division of Timber Management Research, Washington. p. 210 Google Scholar
McCrea, J.M On the isotopic chemistry of carbonates and a paleotemperature scale. Journal of Chemical Physics 18, (1950). 849 857.Google Scholar
Nativ, R, and Riggio, R Precipitation in the southern high plains: Meteorological and isotopic features. Journal of Geophysical Research 95, (1990). 559 564.CrossRefGoogle Scholar
O'Neil, J.R, and Clayton, R.N Oxygen isotope geothermometry. Craig, H, Miller, S.L, and Wasserburg, G.J Isotopic and Cosmic Chemistry. (1964). 157 168.Google Scholar
Quade, J, Chivas, A.R, and McCulloch, M.T Strontium and carbon isotope tracers and the origins of soil carbonate in South Australia and Victoria. Palaeogeography, Palaeoclimatology, Palaeoecology 113, (1995). 103 117.CrossRefGoogle Scholar
Quade, J, Forester, R.M, Pratt, W.L, and Carter, C Black mats, spring-fed streams, and late-glacial-age recharge in southern Great Basin. Quaternary Research 49, (1998). 129 148.Google Scholar
Ramesh, R, Bhattacharya, S.K, and Gopalan, K Climatic correlations in the stable isotope records of silver fir (Abies pindrow) trees from Kashmir, India. Earth and Planetary Science Letters 79, (1986). 66 74.Google Scholar
Smith, R.A, and Alexander, R.B Estimating baseline water quality at unmeasured stream locations based on data from national network monitoring stations. International Union of Geodesy and Geophysics, General Assembly 19, (1987). 995 Google Scholar
Spangler, W. M. L, and Jenne, R. L. (1990). Dataset TD-9641 (U.S. Monthly Normals of Temperature and Precipitation). in, World Monthly Surface Station Climatology and Associated Datasets, (1994). ed, World Weather Disc Associates, Seattle.Google Scholar
Spaulding, W.G Vegetational and climatic development of the Mojave Desert; the last glacial maximum to the present. 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. 166 199.Google Scholar
Spaulding, W.G, and Reynolds, J Mid-postglacial environments of the Mojave Desert; understanding the effects of climatic warming. Abstracts from Proceedings; the 1994 Desert Research Symposium. (1994). p. 29–30.Google Scholar
Spaulding, W.G Paleohydrologic Investigations in the Vicinity of Yucca Mountain: Late Quaternary Paleobotanical and Palynological Records. (1994). p. 80 Google Scholar
Spaulding, W.G, and Graumlich, L.J The last pluvial climatic episodes in the deserts of southwestern North America. Nature 320, (1986). 441 444.CrossRefGoogle Scholar
Thomasson, J.R Sediment-borne “seeds” from Sand Creek, northwestern Kansas: taphonomic significance and paleoecological and paleoenvironmental implications. Paleogeography, Paleoclimatology, Paleoecology 85, (1991). 213 225.Google Scholar
Thompson, R. S, Anderson, K. H, and Bartlein, P. J. (2000b). ), Atlas of Relations Between Climatic Parameters and Distributions of Important Trees and Shrubs in North America (Hardwoods). U.S. Geological Survey. U.S. Geological Survey Professional Paper 1650-B, 415, pp.Google Scholar
Wang, Y, Jahren, A.H, and Amundson, R Potential for 14-C dating of biogenic carbonate in hackberry (Celtis) endocarps. Quaternary Research 47, (1997). 337 343.CrossRefGoogle Scholar
Wigand, P.E, Hemphill, M.L, Sharpe, S.E, Patra. S, Waugh, W.J Great Basin woodland dynamics during the Holocene. in Proceedings of the Workshop-Climate Change in the Four Corners and Adjacent Regions: Implications for Environmental Restoration and Land-Use Planning. (1995). U.S. Department of Energy, Grand Junction.Google Scholar
Wigand, P. E, and Rhode, D. (in press), Great Basin vegetation history and aquatic systems: The last 150,000 years. Smithsonian Contributions to Earth Sciences.Google Scholar
Williamson, G.J, and Coston, C.D The relationship among root growth, shoot growth and fruit growth of peach. Journal of the American Society of Horticultural Science 114, (1989). 180 183.Google Scholar
Yu, Z, McAndrews, J.H, and Eicher, U Middle Holocene dry climate caused by change in atmospheric circulation patterns: Evidence from lake levels and stable isotopes. Geology 25, (1997). 251 254.Google Scholar
Yurtsever, Y. (1975). Worldwide survey of stable isotopes in precipitation. Report, Section on Isotopic Hydrology, International Atomic Energy Agency, Vienna., November 1975, 40, pp.Google Scholar