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Shifts of demography and growth in limber pine forests of the Great Basin, USA, across 4000 yr of climate variability

Published online by Cambridge University Press:  27 December 2018

Constance I. Millar ,
David A. Charlet ,
Diane L. Delany ,
John C. King  and
Robert D. Westfall
Constance I. Millar*
Affiliation:
Pacific Southwest Research Station, USDA Forest Service, 800 Buchanan St., Albany, California94710, USA
David A. Charlet
Affiliation:
College of Southern Nevada, Department of Biology, 700 College Drive, Henderson, Nevada89002, USA
Diane L. Delany
Affiliation:
Pacific Southwest Research Station, USDA Forest Service, 800 Buchanan St., Albany, California94710, USA
John C. King
Affiliation:
Lone Pine Research, 2604 Westridge Drive, Bozeman, Montana59715, USA
Robert D. Westfall
Affiliation:
Pacific Southwest Research Station, USDA Forest Service, 800 Buchanan St., Albany, California94710, USA
*
*Corresponding author at: Pacific Southwest Research Station, USDA Forest Service, 800 Buchanan St., Albany, California 94710, USA. E-mail address: cmillar@fs.fed.us (C.I. Millar).
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Abstract

Annually dated tree-rings of 509 live and deadwood limber pine (Pinus flexilis) samples from the semi-arid Wassuk Range, Nevada, yielded a 3996-yr record extending from 1983 BC to AD 2013. Correlations of radial growth with climate were positive for water relations and negative for summer temperatures. Long-term trends of ring-width corresponded to climate variability documented from other proxies, including low growth during the Late Holocene Dry Period and Medieval Climate Anomaly (MCA) and elevated growth during cool, wet periods of the Neoglacial and Little Ice Age. Spline fit of the data indicated that growth decrease in the last 20 years was second lowest on record, surpassed by lowest growth at 20 BC—AD 150. Demographics of limber pine by aspect and elevation were not strongly related to long-term climate dynamics, except in the case of extirpations on all but north aspects at the end of the MCA. Pines occurred persistently on north aspects, where a continuous record existed to present. Elevation shifts were not obvious on any aspect, and no evidence existed for migration above current treeline. Non-climatic factors appear to interact with climate to make north slopes refugial for upland pines in semi-arid regions across four millennia.

Keywords

Great BasinLimber pinePinus flexilisLate HoloceneClimate variabilityTree ringsDendroecologyPine demographicsClimate refugia
Type
Research Article
Information
Quaternary Research , Volume 91 , Issue 2 , March 2019 , pp. 691 - 704
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2018 

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References

REFERENCES

Adams, K.D., 2007. Late Holocene sedimentary environments and lake-level fluctuations at Walker Lake, Nevada, USA. Geological Society of America Bulletin 119, 126–139.Google Scholar
Ashcroft, M.B., 2010. Identifying refugia from climate change. Journal of Biogeography 37, 1407–1413.Google Scholar
Baker, B.B., Moseley, R.K., 2007. Advancing treeline and retreating glaciers: implications for conservation in Yunnan, PR China. Arctic, Antarctic, and Alpine Research 39, 200–209.Google Scholar
Barber, A., 2013. Physiology and Early Life-History Associated with Extreme Longevity: An Investigation of Pinus longaeva (Great Basin bristlecone pine). PhD dissertation, University of California, Santa Cruz.Google Scholar
Beckage, B., Osborne, B., Gavin, D.G., Pucko, C., Siccama, T. Perkins, T., 2008. A rapid upward shift of a forest ecotone during 40 years of warming in the Green Mountains of Vermont. Proceedings of the National Academy of Sciences of the United States of America 105, 4197–4202.Google Scholar
Bell, D.M., Bradford, J.B., Lauenroth, W.K., 2014. Mountain landscapes offer few opportunities for high‐elevation tree species migration. Global Change Biology 20, 1441–1451.Google Scholar
Bell, K.L., Johnson, R.E., 1980. Alpine flora of the Wassuk Range, Mineral County, Nevada. Madroño 27, 25–35.Google Scholar
Beniston, M., 2003. Climatic change in mountain regions: a review of possible impacts. Climatic Change 59, 5–31.Google Scholar
Bennett, K.D., Provan, J., 2008. What do we mean by ‘refugia’? Quaternary Science Reviews 27, 2449–2455.Google Scholar
Benson, L.V., Kashgarian, M., Rye, R.O., Lund, S.P., Paillet, F.L., Smoot, J., Kester, C., Mensing, S., Meko, D., Lindstrom, S., 2002. Holocene multidecadal and multicentennial droughts affecting Northern California and Nevada. Quaternary Science Reviews 21, 659–682.Google Scholar
Benson, L.V., Lund, S.P., Smoot, J.P., Kashgarian, M., Burdett, J.W., 2001. Records of climate change from the Owens Lake Basin, California. In: Hershler, R., Madsen, D., Currey, D. (Eds.), Proceedings of the Great Basin Symposium on Glacial and Postglacial Drainage, Smithsonian Institution, Washington, DC.Google Scholar
Bidartondo, M.I., Baar, J., Bruns, T.D., 2001. Low ectomycorrhizal inoculum potential and diversity from soils in and near ancient forests of bristlecone pine (Pinus longaeva). Canadian Journal of Botany 79, 293–299.Google Scholar
Birks, H.J., Willis, K.J., 2008. Alpines, trees, and refugia in Europe. Plant Ecology and Diversity 1, 147–160.Google Scholar
Bowerman, N.D., Clark, D.H., 2011. Holocene glaciation of the central Sierra Nevada, California. Quaternary Science Reviews 30, 1067–1085.Google Scholar
Box, G.E.P., Draper, N.R., 1987. Empirical Model-building and Response Surfaces. J. Wiley Sons, New York.Google Scholar
Brubaker, L.B., Anderson, P.M., Edwards, M.E., Lozhkin, A.V., 2005. Beringia as a glacial refugium for boreal trees and shrubs: new perspectives from mapped pollen data. Journal of Biogeography 32, 833–848.Google Scholar
Bruns, T.D., Peay, K.G., Boynton, P.J., Grubisha, L.C., Hynson, N.A., Nguyen, N.H., Rosenstock, N.P., 2009. Inoculum potential of Rhizopogon spores increases with time over the first 4 yr of a 99‐yr spore burial experiment. New Phytologist 181, 463–470.Google Scholar
Bunn, A.G., 2008. A dendrochronology program library inR (dplR). Dendrochronologia 26, 115–124.Google Scholar
Bunn, A.G., Jansma, E., Korpela, M., Westfall, R.D., Baldwin, J., 2013. Using simulations and data to evaluate mean sensitivity (ζ) as a useful statistic in dendrochronology. Dendrochronologia 31, 250–254.Google Scholar
Bunn, A.G., Waggoner, L.A., Graumlich, L.J., 2005. Topographic mediation of growth in high elevation foxtail pine (Pinus balfouriana Grev. et Balf.) forests in the Sierra Nevada, USA. Global Ecology and Biogeography 14,103–114.Google Scholar
Burns, R.M., Honkala, B.H. (technical coordinators), 1990. Silvics of North America: Volume 1. Conifers. United States Department of Agriculture, Forest Service, Agriculture Handbook 654. Washington, D.C.Google Scholar
Charlet, D.A., 1996. Atlas of Nevada Conifers. A Phytogeographic Reference. University of Nevada Press, Reno.Google Scholar
Collier, F.A., Bidartondo, M.I., 2009. Waiting for fungi: the ectomycorrhizal invasion of lowland heathlands. Journal of Ecology 97, 950–963.Google Scholar
Conlisk, E., Castanha, C., Germino, M.J., Veblen, T.T., Smith, J.M., Kueppers, L.M., 2017. Declines in low-elevation subalpine tree populations outpace growth in high-elevation populations with warming. Journal of Ecology 105, 1347–1357.Google Scholar
Consulting Voortech, 2005. Measure J2X v3.2.1: the tree ring measurement program. Voortech Consulting, Holderness.Google Scholar
Cook, E., Krusic, P., 2014. Program ARSTAN v44h3 (accessed December 15, 2017). http://www.ldeo.columbia.edu/tree-ring-laboratory/resources/software.Google Scholar
Cook, E.R., Kairukstis, L.A. (Eds.), 1990. Methods of Dendrochronology. Kluwer, Dordrecht.Google Scholar
Coughlan, J.C., Running, S.W., 1997. Regional ecosystem simulation: a general model for simulating snow accumulation and melt in mountainous terrain. Landscape Ecology 12, 119–136.Google Scholar
Crimmins, S.M., Dobrowski, S.Z., Greenberg, J.A., Abatzoglou, J.T., Mynsberge, A.R., 2011. Changes in climatic water balance drive downhill shifts in plant species’ optimum elevations. Science 331, 324–327.Google Scholar
Daly, C.R., Neilson, R.P., Phillips, D.L., 1994. A statistical-topographic model for mapping climatological precipitation over mountainous terrain. Journal of Applied Meteorology 33, 140–158.Google Scholar
Davis, M.B., Shaw, R.G., 2001. Range shifts and adaptive responses to Quaternary climate change. Science 292, 673–679.Google Scholar
Dobrowski, S.A., 2011. A climatic basis for microrefugia: the influence of terrain on climate. Global Change Biology 17, 1022–1035.Google Scholar
Dong, S., Ucarkus, G., Wesnousky, S.G., Maloney, J., Kent, G., Driscoll, N., Baskins, R., 2014. Strike-slip faulting along the Wassuk Range of the northern Walker Lane, Nevada. Geosphere 10, 40–48.Google Scholar
Elliott, G.P., 2012. Extrinsic regime shifts drive abrupt changes in regeneration dynamics at upper treeline in the Rocky Mountains, USA. Ecology 93, 1614–1625.Google Scholar
Esper, J., Cook, E.R., Schweingruber, F.H., 2002. Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability. Science 295, 2250–2253.Google Scholar
Felde, V.A., Kapfer, J., Grytnes, J.-A., 2012. Upward shift in elevational plant species ranges in Sikkilsdalen, central Norway. Ecography 35, 922–932.Google Scholar
Feng, X., Epstein, S., 1994. Climatic implications of an 8000-year hydrogen isotope time series from bristlecone pine trees. Science 265, 1079–1081.Google Scholar
Flint, L.E., Flint, A.L., Thorne, J.H., Boynton, R., 2013. Fine-scale hydrologic modeling for regional landscape applications: the California Basin Characterization Model development and performance. Ecological Processes 2, 25.Google Scholar
Fu, P., Rich, P.M., 1999. Design and implementation of the Solar Analyst: an ArcView extension for modeling solar radiation at landscape scales. Proceedings of the Nineteenth Annual ESRI User Conference 1,1–31.Google Scholar
Gentili, R., Baroni, C., Caccianiga, M., Armiraglio, S., Ghiani, A., Citterio, S., 2015. Potential warm-stage microrefugia for alpine plants: Feedback between geomorphological and biological processes. Ecological Complexity 21, 87–99.Google Scholar
Graumlich, L.J., 1993. A 1000-year record of temperature and precipitation in the Sierra Nevada. Quaternary Research 39, 249–255.Google Scholar
Grayson, D.K., 2011. The Great Basin. A Natural Prehistory. University of California Press, BerkeleyGoogle Scholar
Griffin, J.R., Critchfield, W.B., 1976. The Distribution of Forest Trees in California. USDA Forest Service Research Paper PSW-82/1972-supplement 1976. US Department of Agriculture, Washington, D.C.Google Scholar
Grissino-Mayer, H.D., 2001. Evaluating crossdating accuracy: a manual and tutorial for the computer program COFECHA. Tree-Ring Research 57, 205–221.Google Scholar
Haffer, J., 1982. General aspects of the refuge theory. In: Prance, G.T. (Eds.), Biological Diversification in the Tropics. Columbia University Press, New York, pp. 6–24.Google Scholar
Hampe, A., Jump, A.S., 2011. Climate relicts: past, present, and future. Annual Review Ecology, Evolution, and Systematics 42, 313–333.Google Scholar
Hatchett, B.J., Boyle, D.P., Putnam, A.E. Bassett, S.D., 2015. Placing the 2012–2015 California‐Nevada drought into a paleoclimatic context: Insights from Walker Lake, California‐Nevada, USA. Geophysical Research Letters 42, 8632–8640.Google Scholar
Holmes, R.L., 1983. Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bulletin 43, 69–78.Google Scholar
Holmes, R.L., Adams, R.K., Fritts, H.C., 1986. Tree-ring chronologies of western North America: California, Eastern Oregon, and Northern Great Basin with procedures used in the chronology development work including user’s manuals for computer programs COFECHA and ARSTAN. Laboratory of Tree-Ring Research, University of Arizona, Chronology Series VI. Tucson, AZ.Google Scholar
Hughes, M.K., Funkhouser, G., 2003. Frequency-dependent climate signal in upper and lower forest border tree rings in the mountains of the Great Basin. In: Diaz, H. (Ed.) Climate Variability and Change in High Elevation Regions: Past, Present & Future. Springer, Dordrecht, pp. 233–244.Google Scholar
Huntley, B., Birks, J.H., 1983. An Atlas of Past and Present Pollen Maps for Europe 0–13,000 Years Ago. Cambridge University Press, Cambridge.Google Scholar
Huntley, B., Webb, T. III, 1989. Migration: species’ response to climatic variations caused by changes in the earth’s orbit. Journal of Biogeography 16, 5–19.Google Scholar
International Tree-Ring Data Bank (ITRDB), 2017–2018. NOAA National Climate Data Center (accessed February 19, 2018). https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/tree-ring.Google Scholar
Jeffress, M.R., VanGunst, J., Millar, C.I., 2017. A surprising discovery of American pika sites in the northwest Great Basin. Western North American Naturalist 77, 252–268.Google Scholar
Konrad, S.K., Clark, D.H., 1998. Evidence for an early Neoglacial glacier advance from rock glaciers and lake sediments in the Sierra Nevada, California, U.S.A. Arctic and Alpine Research 30, 272–284.Google Scholar
Krusic, P., Cook, E., 2013. ARSTAN40 for Mac OS, v44h2 (accessed August 8, 2017). http://www.ldeo.columbia.edu/res/fac/trl/public/publicSoftware.html.Google Scholar
LaMarche, V. Jr., 1973. Holocene climatic variations inferred from treeline fluctuations in the White Mountains, California. Quaternary Research 3, 632–660.Google Scholar
LaMarche, V. Jr., 1974. Paleoclimatic inferences from long tree-ring records. Science 183, 1043–1048.Google Scholar
LaMarche, V. Jr., Mooney, H.A., 1967. Altithermal treeline advance in western United States. Nature 213, 980–982.Google Scholar
Legendre, P., Legendre, L., 1998. Numerical Ecology. 2nd English ed. Elsevier, New York.Google Scholar
Lenoir, J., Ge’gout, J.C., Guisan, A., Vittoz, P., Wohlgemuth, T., Zimmerman, N.E., Dullinger, S., Pauli, H., Willner, W., Svenning, J.C., 2010. Going against the flow: potential mechanisms for unexpected downslope range shifts in a warming climate. Ecography 33, 295–303.Google Scholar
Lenoir, J., Ge’gout, J.C., Marquet, P.A., Ruffray, P., Brisse, H., 2008. A significant upward shift in plant species optimum elevation during the 20th century. Science 320, 1768–1771.Google Scholar
Lloyd, A.H., Graumlich, L.J., 1997. Holocene dynamics of treeline forests in the Sierra Nevada. Ecology 78, 1199–1210.Google Scholar
Lorenz, T.J., Sullivan, K.A., Bakian, A.V., Aubry, C.A., 2011. Cache-site selection in Clark’s Nutcracker (Nucifraga columbiana). The Auk 128, 237–247.Google Scholar
Louderback, L.A., Rhode, D.E., 2009. 15,000 years of vegetation change in the Bonneville basin: the Blue Lake pollen record. Quaternary Science Review 28, 308–326.Google Scholar
Mensing, S., Benson, L.V., Kashgarian, M., Lund, S., 2004. A Holocene pollen record of persistent droughts from Pyramid Lake, Nevada, USA. Quaternary Research 62, 29–38.Google Scholar
Mensing, S.A., Sharpe, S.E., Tunno, I., Sada, D.W., Thomas, J.M., Starratt, S., Smith, J., 2013. The Late Holocene Dry Period: multiproxy evidence for an extended drought between 2800 and 1850 cal yr BP across the central Great Basin, USA. Quaternary Science Reviews 78, 266–282.Google Scholar
Mensing, S.A., Smith, J., Norman, K.B., Allan, M., 2008. Extended drought in the Great Basin western North America in the last two millennia reconstructed from pollen records. Quaternary International 188, 79–89.Google Scholar
Millar, C.I., Charlet, D.A., Westfall, R.D., King, J.C., Delany, D.L., Flint, A., Flint, L.E., 2018. Do low-elevation ravines provide climate refugia for subalpine limber pine (Pinus flexilis) in the Great Basin, USA? Canadian Journal of Forest Research 48, 663–671.Google Scholar
Millar, C.I., King, J.C., Westfall, R.D., Alden, H.A., Delany, D.L., 2006. Late Holocene forest dynamics, volcanism, and climate change at Whitewing Mountain and San Joaquin Ridge, Mono County, Sierra Nevada, CA, USA. Quaternary Research 66, 273–287.Google Scholar
Millar, C.I., Westfall, R.D., Delany, D.L., 2007. Response of high-elevation limber pine (Pinus flexilis) to multiyear droughts and 20th-century warming, Sierra Nevada, California, USA. Canadian Journal of Forest Research 37, 2508–2520.Google Scholar
Millar, C.I., Westfall, R.D., Delany, D.L., Flint, A.L., Flint, L.E., 2015. Recruitment patterns and growth of high-elevation pines in response to climatic variability (1883–2013), in the western Great Basin, USA. Canadian Journal of Forest Research 45, 1299–1312.Google Scholar
Millar, C.I., Westfall, R.D., Delany, D.L., King, J.C., Graumlich, L.C., 2004. Response of subalpine conifers in the Sierra Nevada, California, U.S.A. to 20th-century warming and decadal climate variability. Arctic, Antarctic, and Alpine Research 36, 181–200.Google Scholar
Miller, J., House, K., Germanoski, D., Tausch, R., Chambers, J., 2004. Fluvial geomorphic responses to Holocene climate change. In: Chambers, J.C., Miller, J.R. (Eds.), Great Basin Riparian Ecosystems: Ecology, Management and Restoration. Island Press, Covelo, pp. 49–87.Google Scholar
Morelli, T.L., Daly, C., Dobrowski, S.Z., Dulen, D.M., Ebersole, J.L., Jackson, S.T., Lundquist, J.D., et al., 2016. Managing climate change refugia for climate adaptation. PLoS One 11, doi.org/10.1371/journal.pone.0159909.Google Scholar
Moritz, C., Patton, J.L., Conroy, C.J., Parra, J.L., White, G.C., Beissinger, S.R., 2008. Impact of a century of climate change on small-mammal communities in Yosemite National Park, USA. Science 322, 261–264.Google Scholar
Osborne, G., Bevis, K., 2001. Glaciation in the Great Basin of the western United States. Quaternary Science Reviews 20, 1377–1410.Google Scholar
R Core Team, 2017. R: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria. https://www.R-project.org/.Google Scholar
Rapacciuolo, G., Maher, S.P., Schneider, A.D., Hammond, T.T., Jabis, M., Walsh, R.E., Iknayan, K.J., et al., 2014. Beyond a warming fingerprint: individualistic biogeographic responses to heterogeneous climate change in California. Global Change Biology 20, 2841–2855.Google Scholar
Reinemann, S.A., Porinchu, S.F., Bloom, A.M., Mark, B.G., Box, J.E., 2009. A multiproxy paleolimnological reconstruction of Holocene climate conditions in the Great Basin, United States. Quaternary Research 72, 347–358.Google Scholar
Rull, V., 2009. Microrefugia. Journal of Biogeography 36, 481–484.Google Scholar
Salzer, M.W., Bunn, A.G., Graham, N.E., Hughes, M.K., 2014. Five millennia of paleotemperature from tree-rings in the Great Basin, USA. Climate Dynamics 42, 1517–1526.Google Scholar
Salzer, M.W., Hughes, M.K., Bunn, A.G., Kipfmueller, K.F., 2009. Recent unprecedented tree-ring growth in bristlecone pine at the highest elevations and possible causes. Proceedings National Academy of Science of the United States of America 106, 20348–20353.Google Scholar
SAS Institute, 2015. SAS Online, Version 12. JMP Statistics and Graphics Guide, Cary.Google Scholar
Scuderi, L.A., 1993. A 2000-year tree ring record of annual temperatures in the Sierra Nevada Mountains. Science 259, 1433–1436.Google Scholar
Serra-Diaz, J.M., Scheller, R.M., Syphard, A.D., Franklin, J., 2015. Disturbance and climate microrefugia mediate tree range shifts during climate change. Landscape Ecology 30, 1039–1053.Google Scholar
Smith, S.E., Read, D.J., 2008. Mycorrhizal Symbiosis. 3rd ed. Academic Press, London.Google Scholar
Steele, R.G.D., Torrie, J.H., 1980. Principles and Procedures of Statistics. McGraw Hill, New York.Google Scholar
Stine, S., 1990. Late Holocene fluctuations of Mono Lake, eastern California. Paleogeography, Palaeoclimatology, Palaeoecology 78, 333–381.Google Scholar
Stine, S., 1994. Extreme and persistent drought in California and Patagonia during mediaeval time. Nature 369, 546–549.Google Scholar
Strachan, S., Daly, C., 2017. Testing the daily PRISM air temperature model on semiarid mountain slopes. Journal of Geophysical Research: Atmospheres 122, 5697–5715.Google Scholar
Surpless, B.E., 2012. Cenozoic tectonic evolution of the central Wassuk Range, western Nevada, USA. International Geology Review 54, 547–571.Google Scholar
Tausch, R., Nowak, C., Mensing, S., 2004. Climate change and associated vegetation dynamics during the Holocene: the paleoecological record. In: Chambers, J.C., Miller, J.R. (Eds.), Great Basin Riparian Ecosystems: Ecology, Management and Restoration. Island Press, Covelo, pp. 24–48.Google Scholar
Thompson, R.S., 1992. Late Quaternary environments in Ruby Valley, Nevada. Quaternary Research 37, 1–15.Google Scholar
Toy, T.J., Foster, G.R., Renard, K.G., 2002. Soil Erosion: Processes, Prediction, Measurement, and Control. John Wiley and Sons, Hoboken, N.J.Google Scholar
Van Gunst, K.J., Weisberg, P.J., Yang, J., Fan, Y., 2016. Do denser forests have greater risk of tree mortality: a remote sensing analysis of density-dependent forest mortality. Forest Ecology and Management 359, 19–32.Google Scholar
Wolfram Research, 2017. Mathematica, Version 11.1. Wolfram Research, Inc., Champaign.Google Scholar
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