Respiratory Acclimation of Tropical Forest Roots in Response to In Situ Experimental Warming and Hurricane Disturbance

被引:3
|
作者
Tunison, Rob [1 ]
Wood, Tana E. [2 ]
Reed, Sasha C. [3 ]
Cavaleri, Molly A. [1 ]
机构
[1] Michigan Technol Univ, Coll Forest Resources & Environm Sci, Houghton, MI 49931 USA
[2] USDA Forest Serv, Int Inst Trop Forestry, Rio Piedras, PR USA
[3] US Geol Survey, Southwest Biol Sci Ctr, Moab, UT USA
基金
美国国家科学基金会;
关键词
acclimation; climate change; disturbance; experimental warming; root respiration; tropical plants; TRACE; THERMAL-ACCLIMATION; PLANT RESPIRATION; CARBON; TEMPERATURE; LEAF; DYNAMICS; CLIMATE;
D O I
10.1007/s10021-023-00880-y
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Climate projections predict higher temperatures and more frequent hurricanes in the tropics. Tropical plants subjected to these stresses may respond by acclimating their physiology. We investigated tropical forest root respiration in response to in situ experimental warming and hurricane disturbance in eastern Puerto Rico. We measured mass-normalized root specific respiration, root biomass, and root traits at the Tropical Responses to Altered Climate Experiment (TRACE), where understory vegetation is warmed + 4 degrees C above ambient. Our measurements span 5 years, including before and after two major hurricanes, to quantify root contributions to ecosystem carbon fluxes. Experimental warming did not affect root specific respiration at a standard temperature of 25 degrees (RSR25, mean = 3.89 nmol CO2 g(-1) s(-1)) or the temperature sensitivity of root respiration (Q(10), mean = 1.75), but did result in decreased fine-root biomass, thereby decreasing area-based estimations of ecosystem-level root respiration in warmed plots by similar to 35%. RSR25 of newer roots, which increased with increasing root nitrogen, showed greater rates 6 months after the hurricanes, but subsequently decreased after 12 months. Root specific respiration did not acclimate to higher temperatures, based on lack of adjustments in either Q(10) or RSR25 in the warmed plots; however, decreased root biomass indicates the root contribution to soil carbon dioxide efflux was overall lower with warming. Lower root biomass may also limit nutrient and water uptake, having potential negative effects on carbon assimilation. Our results show that warming and hurricane disturbance have strong potential to affect tropical forest roots, as well as ecosystem carbon fluxes.
引用
收藏
页码:168 / 184
页数:17
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