Hostname: page-component-cd9895bd7-mkpzs Total loading time: 0 Render date: 2024-12-26T09:09:59.938Z Has data issue: false hasContentIssue false
  • English
  • Français

Devils Hole, Nevada, δ18O record extended to the mid-Holocene

Published online by Cambridge University Press:  20 January 2017

Isaac J. Winograd ,
Jurate M. Landwehr ,
Tyler B. Coplen ,
Warren D. Sharp ,
Alan C. Riggs ,
Kenneth R. Ludwig  and
Peter T. Kolesar
Isaac J. Winograd*
Affiliation:
U.S. Geological Survey, 432 National Center, Reston, VA 20192, USA
Jurate M. Landwehr
Affiliation:
U.S. Geological Survey, 432 National Center, Reston, VA 20192, USA
Tyler B. Coplen
Affiliation:
U.S. Geological Survey, 432 National Center, Reston, VA 20192, USA
Warren D. Sharp
Affiliation:
Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709, USA
Alan C. Riggs
Affiliation:
U.S. Geological Survey, Denver Federal Center, MS 413, Lakewood, CO 80225, USA
Kenneth R. Ludwig
Affiliation:
Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709, USA
Peter T. Kolesar
Affiliation:
Department of Geology, Utah State University, Logan, UT 84322, USA
*
⁎Corresponding author. Fax: +1 703 648 5832. E-mail address:[email protected] (I.J. Winograd).
Get access Rights & Permissions [Opens in a new window]

Abstract

The mid-to-late Pleistocene Devils Hole δ18O record has been extended from 60,000 to 4500 yr ago. The new δ18O time series, in conjunction with the one previously published, is shown to be a proxy of Pacific Ocean sea surface temperature (SST) off the coast of California. During marine oxygen isotope stages (MIS) 2 and 6, the Devil Hole and SST time series exhibit a steady warming that began 5000 to > 10,000 yr prior to the last and penultimate deglaciations. Several possible proximate causes for this early warming are evaluated. The magnitude of the peak δ18O or SST during the last interglacial (LIG) is significantly greater (1 per mill and 2 to 3°C, respectively) than the peak value of these parameters for the Holocene; in contrast, benthic δ18O records of ice volume show only a few tenths per mill difference in the peak value for these interglacials. Statistical analysis provides an estimate of the large shared information (variation) between the Devils Hole and Eastern Pacific SST time series from ∼ 41 to ∼ 2°N and enforces the concept of a common forcing among all of these records. The extended Devils Hole record adds to evidence of the importance of uplands bordering the eastern Pacific as a source of archives for reconstructing Pacific climate variability.

Keywords

Late PleistoceneHoloceneSouthwestern U.S.NevadaDevils HolePaleoclimateSSTEastern PacificTropical PacificAtmospheric teleconnection
Type
Research Article
Information
Quaternary Research , Volume 66 , Issue 2 , September 2006 , pp. 202 - 212
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Alley, R.B., and Cuffey, K.M. Oxygen and hydrogen isotopic ratios of water in precipitation: beyond paleothermometry. Valley, J.W., and Cole, D.R. Stable Isotope Geochemistry. Reviews in Mineralogy and Geochemistry vol. 43, (2001). Mineralogical Society of America, Washington, D.C.. 527–553.Google Scholar
Bard, E., Antonioli, F., and Silenzi, S. Sea-level during the penultimate interglacial period based on a submerged stalagmite from Argentarola Cave (Italy). Earth and Planetary Science Letters 196, (2002). 135–146.Google Scholar
Barron, J.A., Heusser, L., Herbert, T., and Lyle, M. High resolution climatic evolution of coastal north California during the past 16,000 years. Paleoceanography 18(1), 20 (2003). 1–19.Google Scholar
Benson, L.V. Western lakes. Gillespie, A.R., Porter, S.C., and Atwater, B.F. The Quaternary Period in the United States. (2004). Elsevier, New York. 185–204.Google Scholar
Bradley, R.S., Vuille, M., Hardy, D., and Thompson, L.G. Low latitude ice cores record Pacific sea surface temperatures. Geophysical Research Letters 30, (4)23 (2003). 1–4.Google Scholar
Broecker, W.S. Upset for Milankovitch theory. Nature 359, (1992). 779–780.Google Scholar
Bull, D., Kemp, A.E.S., and Weedon, G.P. A 160-K.y.-old record of El Nino-Southern Oscillation in marine production and coastal runoff from Santa Barbara Basin, California, USA. Geology 28, (2000). 1007–1010.2.0.CO;2>CrossRefGoogle Scholar
Cayan, D.R., Redmond, K.T., and Riddle, L.G. ENSO and hydrologic extremes in the Western United States. Journal Climate 12, (1999). 2881–2893.Google Scholar
Cheng, H., Edwards, R.L., Hoff, J., Gallup, C.D., Richards, D.A., and Asmerom, Y. The half-lives of uranium-234 and Thorium-230. Chemical Geology 169, (2000). 17–33.Google Scholar
Clark, D.H., (2003). Complex timing and patterns of glaciation in the American Cordillera during Termination I. XVI INQUA Congress Program with Abstracts, Paper 88-4, p. 231.Google Scholar
CLIMAP Project Members The Last Interglacial Ocean. Quaternary Research 21, (1984). 123–225.Google Scholar
Doose, H., Prahl, F.G., and Lyle, M.W. Biomarker temperature estimates for modern and the last glacial surface waters of the California Current System between 33° and 42°N. Paleoceanography 12, (1997). 615–622.Google Scholar
Edwards, R.L., Cheng, H., Murrell, M.T., and Goldstein, S.J. Protactinium-231 dating of carbonates by thermal ionization mass spectrometry: implications for Quaternary climate change. Science 276, (1997). 782–786.Google Scholar
Ely, L.L., Enzel, Y., and Cayan, D.R. Anomalous North Pacific atmospheric circulation and large winter floods in the Southwestern United States. Journal Climate 7, (1994). 977–987.2.0.CO;2>CrossRefGoogle 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 Planetary Science Letters 170, (1999). 181–196.CrossRefGoogle Scholar
Friddel, J.E., Thunell, R.C., and Heusser, L.E. Direct comparison of marine and terrestrial climate variability during marine isotope stages 6 and 5: results from Santa Barbara Basin ODP Hole 893A. Paleoceanography 17, (1)2 (2002). 1–12.CrossRefGoogle Scholar
Friedman, I., Harris, J.M., Smith, G.I., and Johnson, C.R. Stable isotope composition of waters in the Great Basin, United States. 1. Air-mass trajectories. Journal Geophysical Research 107D, (19) ACL14 (2002). 1–14.Google Scholar
Friedman, I., Smith, G.I., and Johnson, C.A. Stable isotope compositions of waters in the Great Basin, United States. 2. Modern precipitation. Journal Geophysical Research 107D, (19) ACL15 (2002). 1–22.Google Scholar
Gallup, C.D., Cheng, H., Taylor, F.W., and Edwards, R.L. Direct determination of the timing of sea level change during Termination II. Science 295, (2002). 310–313.CrossRefGoogle ScholarPubMed
Ganeshram, R.S., and Pedersen, T.F. Glacial–interglacial variability in upwelling and bioproductivity off NW Mexico: implications for Quaternary paleoclimate. Paleoceanography 13, (1998). 634–645.CrossRefGoogle 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.Google Scholar
Henderson, G.M., and Slowey, N.C. Evidence from U–Th dating against Northern Hemisphere forcing of the penultimate deglaciation. Nature 404, (2000). 61–66.Google Scholar
Hendricks, M.B., DePaolo, D.J., and Cohen, R.C. Space and time variation of δ 18O and δ D in precipitation: can temperature be estimated from ice cores?. Global Biogeochemical Cycles 14, (2000). 851–861.CrossRefGoogle Scholar
Hendy, I.L., and Kennett, J.P. Dansgaard–Oeschger cycles and the California Current system: Planktonic foraminiferal response to rapid climate change in Santa Barbara Basin, Ocean Drilling Program Hole 893A. Paleoceanography 15, (2000). 30–42.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.CrossRefGoogle ScholarPubMed
Higgins, R.W., Schemm, J.-K.E., Shi, W., and Leetmaan, A. Extreme precipitation events in the western United States related to tropical forcing. Journal Climate 13, (2000). 793–820.2.0.CO;2>CrossRefGoogle Scholar
Hinrichs, K.-U., Rinna, J., and Rullkotter, T. A 160-kyr record of alkenone-derived sea-surface temperature from Santa Barbara Basin sediments. Naturwissenschaften 84, (1997). 126–128.Google Scholar
Huyer, A. Coastal upwelling in the California Current System. Progress in Oceanography 12, (1983). 259–284.Google Scholar
Imbrie, J. A good year for Milankovitch. Paleoceanography 7, (1992). 687–690.Google Scholar
Imbrie, J., Hays, J.D., Martinson, D.G., McIntyre, A., Mix, A.C., Morley, J.J., Pisias, N.G., Prell, W.L., and Shackleton, N.J. The orbital theory of Pleistocene climate: support from a revised chronology of the marine δ 18O record. Berger, A., Imbrie, J., Hays, J., Kukla, G., and Saltzmann, B. Milankovitch and Climate, Part 1. (1984). Reidel Publishing Company, Boston. 269–305.Google Scholar
Imbrie, J., Mix, A.C., and Martinson, D.G. Milankovitch theory viewed from Devils Hole. Nature 363, (1993). 531–533.CrossRefGoogle Scholar
Johnson, R.G. Last interglacial sea stands on Barbados and an early anomalous deglaciation by differential uplift. Journal Geophysical Research 106C, (2001). 11543–11551.Google Scholar
Kahya, E., and Dracup, J.A. The influence of Type 1 El Nino and La Nina events on streamflows in the Pacific southwest of the United States. Journal Climate 7, (1994). 965–976.Google Scholar
Karner, D.B., and Muller, R.A. A causality problem for Milankovitch. Science 288, (2000). 2143–2144.Google Scholar
Karner, D.B., Levine, J., Medeiros, B.P., and Muller, R.A. Constructing a stacked benthic δ 18O record. Paleoceanography 17, (3)2 (2002). 1–16.Google Scholar
Kerr, R.A. Second clock supports orbital pacing of the ice ages. Science 276, (1997). 680–681.Google Scholar
Kutzbach, J.E., Wright, H.E. Jr. Simulation of the climate of 18,000 years B.P.: results for the North American/North Atlantic/European sector and comparison with the geologic record of North America. Quaternary Science Reviews 4, (1985). 147–187.Google Scholar
Lambeck, K., Yokoyama, Y., and Purcell, T. Into and out of the last glacial maximum: sea level change during oxygen isotope stages 3 and 2. Quaternary Science Reviews 21, (2002). 343–360.CrossRefGoogle Scholar
Landwehr, J.M., and Winograd, I.J. Dating the Vostok ice core record by importing the Devils Hole chronology. Journal of Geophysical Research 106D, (2001). 31853–31861.CrossRefGoogle Scholar
Lea, D.W., Pak, D.K., and Spero, H.J. Climate impact of late Quaternary equatorial Pacific sea surface temperature variations. Science 289, (2000). 1719–1724.Google Scholar
Levine, J., Karner, D.B., and Muller, R.A. Warming at 140 Ka: causality problem for Milankovitch. EOS. Transactions of the American Geophysical Union 82S, (2001). F3 Google Scholar
Licciardi, J.M., Clark, P.U., Brook, E.J., Elmore, D., and Shama, P. Variable responses of Western U.S. glaciers during the last deglaciation. Geology 32, (2004). 81–84.Google Scholar
Ludwig, K.R., Simmons, K.R., Szabo, B.J., Winograd, I.J., Landwehr, J.M., Riggs, A.C., and Hoffman, R.J. Mass-spectrometric 230Th–234U–238U dating of the Devils Hole calcite vein. Science 258, (1992). 284–287.Google Scholar
Lyle, M., Zahn, R., Prahl, F., Dymond, J., Collier, R., Pisias, N., and Suess, E. Paleoproductivity and carbon burial across the California Current: the multitracers transect, 42°N. Paleoceanography 7, (1992). 251–272.Google Scholar
Lyle, M., Koizumi, I., Delaney, M.L., and Barron, J.A. Sedimentary record of the California Current System: middle Miocene to Holocene: a synthesis of 167 results. Proceedings of the Ocean Drilling Program. Scientific Results vol. 167, (2000). Texas A and M University, 341–376.Google Scholar
Lynn, R.J., and Simpson, J.J. The California Current system: the seasonal variability of its physical characteristics. Journal Geophysical Research 92C, (1987). 12947–12966.Google Scholar
Mangelsdorf, K., Guntner, U., and Rullkotter, J. Climatic and oceanographic variations on the California continental margin during the last 160 kyr. Organic Geochemistry 31, (2002). 829–846.CrossRefGoogle Scholar
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., Moore, T.C. Jr., 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.Google Scholar
McCabe, G.J., and Dettinger, M.D. Primary modes and predictability of year-to-year snowpack variations in the western United States from teleconnections with Pacific Ocean climate. Journal Hydrometeorology 3, (2002). 13–25.Google Scholar
McDermott, F. Paleo-climate reconstruction from stable isotope variations in speleothems: a review. Quaternary Science Reviews 23, (2004). 901–918.CrossRefGoogle Scholar
Molina-Cruz, A. Late Quaternary oceanography of the mouth of the Gulf of California: the polycystine connection. Paleoceanography 3, (1988). 447–459.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
Muhs, D.R., and Bettis, E.A. Geochemical variations in Peoria loess of western Iowa indicate paleowinds in midcontinental North America during last glaciation. Quaternary Research 53, (2000). 49–61.Google Scholar
Ortiz, J., Mix, A., Hostetler, S., and Kashgarian, M. The California Current of the last glacial maximum: reconstruction at 42°N based on multiple proxies. Paleoceanography 12, (1997). 191–205.Google Scholar
Paillard, D., Labeyrie, L., and Yiou, P. Macintosh program performs time-series analysis. EOS, Transactions-American Geophysical Union 77, (1996). 379 CrossRefGoogle Scholar
Pandey, G.R., Cayan, D.R., and Georgakakos, K.P. Precipitation structure in the Sierra Nevada of California during winter. Journal Geophysical Research 104D, (1999). 12019–12030.Google Scholar
Plummer, L.N., Busenberg, E., and Riggs, A.C. In-situ growth of calcite at Devils Hole, Nevada: comparison of field and laboratory rates to a 500,000 year record of near-equilibrium calcite growth. Aquatic Chemistry 6, (2000). 257–274.Google Scholar
Pool, D.R. Variations in climate and ephemeral channel recharge in southeastern Arizona, United States. Water Resources Research 41, w11403 (2005). 25 (http://dx.doi.org/10.1029/2004WR003255)Google Scholar
Riggs, A.C., Carr, W.J., Kolesar, P.T., and Hoffman, R.J. Tectonic speleogenisis of Devils Hole, Nevada, and implications for hydrogeology and the development of long continuous paleoenvironmental records. Quaternary Research 42, (1994). 241–254.Google Scholar
Rosenthal, Y., and Broccoli, A.J. In search of paleo-ENSO. Science 304, (2004). 219–221.Google Scholar
Sabin, A.L., and Pisias, N.G. Sea surface temperature changes in the Northeastern Pacific Ocean during the past 20,000 years and their relationship to climate change in Northwestern North America. Quaternary Research 46, (1996). 48–61.Google Scholar
Sancetta, C., Lyle, M., Heusser, L., Zahn, R., and Bradbury, J.P. Late-glacial to Holocene changes in the winds, upwelling, and seasonal production of the Northern California Current System. Quaternary Research 38, (1992). 359–370.Google Scholar
Schaaf, M., and Thurow, J. Two 30,000 year high-resolution grey value time series from the Santa Barbara Basin and Guaymas Basin. Cramp, A., MacLeod, C.J., Lee, S.V., and Jones, E.J.W. Geologic Evolution of Ocean basins: Results from Ocean Drilling Program. Special Publication vol. 131, (1998). Geological Society, London. 101–110.Google Scholar
Schwing, F.B., Murphee, T., de Witt, L., and Green, P.M. The evolution of oceanic and atmospheric anomalies in the northeast Pacific during the El Niño and La Niña events of 1995–2001. Progress in Oceanography 54, (2002). 459–491.Google Scholar
Seki, O., Ishiwatari, R., and Matsumoto, K. Millennial climate oscillations in NE Pacific surface waters over the last 82 Kyr: New evidence from alkenones. Geophysical Research Letters 29, (23) 59 (2002). 1–4.Google Scholar
Simpson, J.J. Response of the Southern California Current system to the mid-latitude North Pacific coastal warming events of 1982–1983 and 1940–1941. Fisheries Oceanography 1, (1992). 57–79.Google Scholar
Speed, R.C., and Cheng, H. Evolution of marine terraces and sea level in the last interglacial, Cave Hill, Barbados. Bulletin of the Geologic Society of America 116, (2004). 219–232.CrossRefGoogle Scholar
Stirling, C.H., Esat, T.M., Lambeck, K., and McCulloch, M.T. Timing and duration of the last interglacial: evidence for a restricted interval of widespread coral reef growth. Earth and Planetary Science Letters 160, (1998). 745–762.Google Scholar
Sweeney, M.R., and Busacca, A.J. Glacial anticyclone recorded in Palouse loess of northwestern United States. Geology 32, (2004). 705–708.Google Scholar
Szabo, B.J., Kolesar, P.T., Riggs, A.C., Winograd, I.J., and Ludwig, K.R. Paleoclimatic inferences from a 120,000-yr calcite record of water-table fluctuations in Browns Room of Devils Hole, Nevada. Quaternary Research 41, (1994). 59–69.Google 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. et al. Global Climates Since the Last Glacial Maximum. (1993). Univ. Minnesota Press, 468–513.Google Scholar
Thunell, R.C., and Mortyn, P.G. Glacial climate instability in the Northeast Pacific Ocean. Nature 376, (1995). 504–506.Google Scholar
Vacco, D.A., Clark, P.U., Mix, A.C., Cheng, H., and Edwards, R.L. A speleothem record of Younger Dryas cooling, Klamath Mountains, Oregon, USA. Quaternary Research 64, (2005). 249–256.Google Scholar
Vuille, M., Bradley, R.S., Healy, K., Werner, M., Hardy, D.R., Thompson, L.G., and Keimig, F. Modeling δ 18O in precipitation over the tropical Americas: 2. Simulation of the stable isotope signal in Andean ice cores. Journal Geophysical Research 108D, (6), ACL 2 (2003). 1–17.Google Scholar
Winograd, I.J. The magnitude and proximate cause of ice-sheet growth since 35,000 yr. B.P.. Quaternary Research 56, (2001). 299–307.Google Scholar
Winograd, I.J., Szabo, B.J., Coplen, T.B., and Riggs, A.C. A 250,000-year climate record from Great Basin vein calcite: implications for Milankovitch Theory. Science 242, (1988). 1275–1280.CrossRefGoogle ScholarPubMed
Winograd, I.J., Coplen, T.B., Landwehr, J.M., Riggs, A.C., Ludwig, K.R., Szabo, B.J., Kolesar, P.T., and Revesz, K.M. Continuous 500,000-year climate record from vein calcite in Devils Hole, Nevada. Science 258, (1992). 255–260.Google Scholar
Winograd, I.J., Coplen, T.B., Ludwig, K.R., Landwehr, J.M., and Riggs, A.C. High resolution δ 18O record from Devils Hole, Nevada, for the period 80 to 19 Ka. EOS. Transactions of the American Geophysical Union 77, 17 (1996). S169 Google Scholar
Winograd, I.J., Landwehr, J.M., Ludwig, K.R., Coplen, T.B., and Riggs, A.C. Duration and structure of the past four interglaciations. Quaternary Research 48, (1997). 141–154.Google Scholar
Winograd, I.J., Riggs, A.C., and Coplen, T.B. The relative contributions of summer and cool-season precipitation to groundwater recharge, Spring Mountains, USA. Hydrogeology Journal 6, (1998). 77–93.Google Scholar
Yamamoto, M., Oba, T., Shimamune, J., and Ueshima, T. Orbital-scale anti-phase variation of sea surface temperature in mid-latitude North Pacific margins during the last 145,000 years. Geophysical Research Letters 31, (2004). L16311 Google Scholar
Yurtsever, V., Gat, J.R., (1981). Atmospheric waters. In: Gat, J.R., Gonfiantini, R. (Eds.), Stable Isotopic Hydrology: Deuterium and Oxygen-18 in the Water Cycle. IAEA Technical Report Series 210, IAEA, Vienna., pp. 103–142.Google Scholar
Supplementary material: File

Winograd et al. Supplementary Material

Supplementary Material

Download Winograd et al. Supplementary Material(File)
File 47.6 KB