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Warming combined with more extreme precipitation regimes modifies the water sources used by trees
Author(s) -
Grossiord Charlotte,
Sevanto Sanna,
Dawson Todd E.,
Adams Henry D.,
Collins Adam D.,
Dickman Lee T.,
Newman Brent D.,
Stockton Elizabeth A.,
McDowell Nate G.
Publication year - 2017
Publication title -
new phytologist
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.742
H-Index - 244
eISSN - 1469-8137
pISSN - 0028-646X
DOI - 10.1111/nph.14192
Subject(s) - juniper , environmental science , precipitation , climate change , transpiration , global warming , atmospheric sciences , stomatal conductance , water use , ecology , agronomy , photosynthesis , biology , botany , geography , geology , meteorology
Summary The persistence of vegetation under climate change will depend on a plant's capacity to exploit water resources. We analyzed water source dynamics in piñon pine and juniper trees subjected to precipitation reduction, atmospheric warming, and to both simultaneously. Piñon and juniper exhibited different and opposite shifts in water uptake depth in response to experimental stress and background climate over 3 yr. During a dry summer, juniper responded to warming with a shift to shallow water sources, whereas piñon pine responded to precipitation reduction with a shift to deeper sources in autumn. In normal and wet summers, both species responded to precipitation reduction, but juniper increased deep water uptake and piñon increased shallow water uptake. Shifts in the utilization of water sources were associated with reduced stomatal conductance and photosynthesis, suggesting that belowground compensation in response to warming and water reduction did not alleviate stress impacts for gas exchange. We have demonstrated that predicted climate change could modify water sources of trees. Warming impairs juniper uptake of deep sources during extended dry periods. Precipitation reduction alters the uptake of shallow sources following extended droughts for piñon. Shifts in water sources may not compensate for climate change impacts on tree physiology.