Journal
FRONTIERS IN ECOLOGY AND THE ENVIRONMENT
Volume 7, Issue 4, Pages 185-189Publisher
WILEY
DOI: 10.1890/080016
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Funding
- Los Alamos National Lab (Environmental Restoration and LDRDDR)
- National Science Foundation [DEB0443526, EAR-9876800]
- Arizona Agricultural Experiment Station [126-580]
- DOE NICCR [FC02-06ER64159]
- Office of Science (BER), Department of Energy [DE-FG0207ER 64393]
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Global climate change is projected to produce warmer, longer, and more frequent droughts, referred to here as global change-type droughts, which have the potential to trigger widespread tree die-off. However, drought-induced tree mortality cannot be predicted with confidence, because long-term field observations of plant water stress prior to, and culminating in, mortality are rare, precluding the development and testing of mechanisms. Here, we document plant water stress in two widely distributed, co-occurring species, pinon pine (Pinus edulis) and juniper (Juniperus monosperma), over more than a decade, leading up to regional-scale die-off of pinon pine trees in response to global change-related drought. Pinon leaf water potentials remained substantially below their zero carbon assimilation point for at least 10 months prior to dying, in contrast to those of juniper, which rarely dropped below their zero-assimilation point. These data suggest that pinon mortality was driven by protracted water stress, leading to carbon starvation and associated increases in susceptibility to other disturbances (eg bark beetles), a finding that should help to improve predictions of mortality during drought.
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