Divergent climate impacts on C3 versus C4 grasses imply widespread 21st century shifts in grassland functional composition

被引:17
|
作者
Havrilla, Caroline A. [1 ]
Bradford, John B. [2 ]
Yackulic, Charles B. [2 ]
Munson, Seth M. [2 ]
机构
[1] Colorado State Univ, Dept Forest & Rangeland Stewardship, Ft Collins, CO 80523 USA
[2] US Geol Survey, Southwest Biol Sci Ctr, Flagstaff, AZ USA
关键词
C-3; grass; C-4; climate change; grassland; habitat suitability; perennial grass; species distribution modelling (SDM); SEASONAL WATER AVAILABILITY; SPECIES DISTRIBUTION MODELS; DESERT GRASSLAND; RELATIVE ABUNDANCE; RESPONSES; PRECIPITATION; PRODUCTIVITY; TEMPERATURE; CONSEQUENCES; TRANSITION;
D O I
10.1111/ddi.13669
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Aim: Grasslands cover a third of Earth's landmass and provide critical ecosystem services. Anticipating how perennial C-3 (cool-season) and C-4 (warm-season) grasses respond to climate change will be key to predicting future composition and functioning of grasslands. Here, we evaluate environmental drivers of C-3 and C-4 perennial distributions and assess how C-3 and C-4 grass distributions shift in response to future climate change. Location: Western United States. Methods: We developed integrated species distribution models to identify climate and soil drivers of relative abundance of C-3 and C-4 perennial grasses. We then created projections of species abundances under future climate and evaluated when and where projected shifts in relative abundance were robust across climate models. Results: Historically, C-3 grasses occupied areas with lower temperature and more variable precipitation regimes, while C-4 grasses occupied areas of higher temperature, greater temperature variability and greater warm-season precipitation. C-4 species also occupied narrower soil texture niches. In response to future climate change, C-3 grass abundance declined across 74% of areas, while C-4 abundance increased across 66% of areas. C-3 grasses expanded in mid- to higher-latitude areas with increasing temperature and decreasing seasonality of precipitation. In contrast, C-4 grasses increased in higher-latitude regions, but declined in lower-latitude, dryer regions. Results were surprisingly robust across climate scenarios, suggesting high confidence in the direction of these future changes. Main Conclusions: Findings imply C-3 and C-4 perennial grasses will have highly divergent responses to climate change that may result in grassland functional compositional changes. Increasing temperatures and precipitation variability may favour some C-4 grasses, but C-4 habitat expansion may be constrained by soil conditions in western USA. Results provide actionable insights for anticipating the impacts of climate change on grass-dominated and co-dominated ecosystems and improving large-scale conservation and restoration efforts.
引用
收藏
页码:379 / 394
页数:16
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