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Oecologia

, Volume 187, Issue 4, pp 897–909 | Cite as

Millennial-scale tree-ring isotope chronologies from coast redwoods provide insights on controls over California hydroclimate variability

  • Steven L. Voelker
  • John S. Roden
  • Todd E. Dawson
Special Topic

Abstract

To understand drivers of hydroclimate variability in north-coastal California, we obtained tree cross-sections from eleven coastal redwoods (mean age of 1232 years old) from the northern half of the species range. Tree rings from eight trees were cross-dated and sampled at sub-annual resolution for carbon isotope discrimination (Δ13C) and oxygen isotope composition (δ18O). Tree-ring Δ13C and δ18O, compared to modern climate data, demonstrate these signals primarily record summertime hydroclimate variability—primarily through variables associated with evaporative conditions and/or precipitation. Our 1100-year stable isotope chronologies showed that north-coastal California did not undergo the megadroughts observed elsewhere in California and the western United States. This result implicates extended periods of low winter precipitation, rather than growing season evaporation, as the primary driver of previous megadroughts across California and neighboring regions. Compared to cool conditions prevailing over the Northern Hemisphere during the Little Ice age (1301–1875 of the common era, CE), the frequency of isotopic events of a certain magnitude was greater during periods with warmer Northern Hemisphere temperatures such as the Medieval Climate Anomaly (900–1300 CE) and the modern period (1876 to present). This association between tree-ring isotopic variability and long-term shifts in temperatures is consistent with the expected patterns in mid-latitude hydroclimate variability expected from arctic amplification (i.e., shifts in equator-to-pole temperature differences that modify jet stream speed and amplitude) or amplified quasi-resonant wave activity (i.e., wave-patterns in high-altitude winds that become “trapped” within a certain pattern, thereby producing a longer-duration periods of drought or wetness) across mid-latitudes during the boreal summer.

Keywords

Δ13δ18Arctic amplification Megadrought Climate event frequency Medieval climate anomaly Little ice age 

Notes

Acknowledgements

For processing many thousands of samples, we extend our gratitude to our tree-ring lab managers Ken Olejar and LeAnn Canady, our isotope lab managers Lin Roden, Stefania Mambelli and Wenbo Yang and the many undergraduate student workers at SOU and UCB. For providing access and support in collecting redwood slabs we thank the California Redwood State Parks, Jay Harris, and the trails crews at Humboldt Redwoods and Prairie Creek Redwoods State Parks. We thank Steve Sillett for providing Slab 1 and Allyson Carroll for all of her help in providing tree-ring chronologies that confirmed our cross-dating. This research was supported by the National Science Foundation Paleo Perspectives on Climate Change Grants AGS-1003050 and AGS-1003601. Finally, we thank two anonymous reviewers who provided comments that improved this manuscript greatly.

Author contribution statement

JSR and TED conceived of the research, oversaw and contributed to the research. SLV oversaw data collection, analyzed the data and wrote the manuscript. JSR and TED provided editorial advice.

Supplementary material

442_2018_4193_MOESM1_ESM.docx (6.1 mb)
Supplementary material 1 (DOCX 6277 kb)

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Copyright information

© Springer-Verlag GmbH Germany, part of Springer Nature 2018

Authors and Affiliations

  • Steven L. Voelker
    • 1
  • John S. Roden
    • 2
  • Todd E. Dawson
    • 3
  1. 1.Department of Plants, Soils and ClimateUtah State UniversityLoganUSA
  2. 2.Department of BiologySouthern Oregon UniversityAshlandUSA
  3. 3.Department of Integrative BiologyUniversity of California-BerkeleyBerkeleyUSA

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