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Stable isotopes of tree rings reveal seasonal-to-decadal patterns during the emergence of a megadrought in the Southwestern US

  • SPECIAL ISSUE: IN HONOR OF RUSSELL K. MONSON
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Abstract

Recent evidence has revealed the emergence of a megadrought in southwestern North America since 2000. Megadroughts extend for at least 2 decades, making it challenging to identify such events until they are well established. Here, we examined tree-ring growth and stable isotope ratios in Pinus ponderosa at its driest niche edge to investigate whether trees growing near their aridity limit were sensitive to the megadrought climatic pre-conditions, and were capable of informing predictive efforts. During the decade before the megadrought, trees in four populations revealed increases in the cellulose δ13C content of earlywood, latewood, and false latewood, which, based on past studies are correlated with increased intrinsic water-use efficiency. However, radial growth and cellulose δ18O were not sensitive to pre-megadrought conditions. During the 2 decades preceding the megadrought, at all four sites, the changes in δ13C were caused by the high sensitivity of needle carbon and water exchange to drought trends in key winter months, and for three of the four sites during crucial summer months. Such pre-megadrought physiological sensitivity appears to be unique for trees near their arid range limit, as similar patterns were not observed in trees in ten reference sites located along a latitudinal gradient in the same megadrought domain, despite similar drying trends. Our results reveal the utility of tree-ring δ13C to reconstruct spatiotemporal patterns during the organizational phase of a megadrought, demonstrating that trees near the arid boundaries of a species’ distribution might be useful in the early detection of long-lasting droughts.

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All data for this manuscript will be posted in the International Tree-Ring Database (ITRDB).

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Acknowledgements

This manuscript is to be published as part of a Special Issue honoring Russell K. Monson. We appreciate particularly Russ’ extensive contributions in plant ecology. We also thank C. Niel, A. Thomas, L. Wells, F. Moreno, M. Twitty, A. Spencer, C. Monteleone, and E. Bergman for their assistance in blue reflectance tree-ring and cellulose sample processing. This work was supported by a grant from the Ecosystems Program in the Division of Environmental Biology (NSF Award 1754430). FB acknowledges support from project ‘Inside out’ (#POIR.04.04.00–00-5F85/18–00) funded by the HOMING program of the Foundation for Polish Science co-financed by the European Union under the European Regional Development Fund.

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WEW, SB, FB, PS, and RKM conceived the ideas and designed methodology. PS, SB, and WEW collected the data. PS, SB, and FB analyzed the data. PS and RKM led the writing of the manuscript. All authors contributed critically to the drafts and gave final approval for publication.

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Correspondence to Paul Szejner.

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The authors declare that they have no conflict of interest.

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Communicated by Christiane Roscher .

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Szejner, P., Belmecheri, S., Babst, F. et al. Stable isotopes of tree rings reveal seasonal-to-decadal patterns during the emergence of a megadrought in the Southwestern US. Oecologia 197, 1079–1094 (2021). https://doi.org/10.1007/s00442-021-04916-9

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  • DOI: https://doi.org/10.1007/s00442-021-04916-9

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