气候变化领域集成服务门户

The muted wood isotopic signal in slow-growing trees of unthinned stands indicates lower responsiveness to changing environmental conditions compared to fast-growing trees in thinned stands.

To examine the physiological processes associated with higher growth rates after thinning, we analyzed the oxygen isotopic values in wood (delta O-18(w)) of 12 ponderosa pine (Pinus ponderosa) trees from control, moderately, and heavily thinned stands and compared them with wood-based estimates of carbon isotope discrimination (a dagger C-13), basal area increment (BAI), and gas exchange. We found that (heavy) thinning led to shifts and increased inter-annual variability of both stable carbon and oxygen isotope ratios relative to the control throughout the first post-thinning decade. Results of a sensitivity analysis suggested that both an increase in stomatal conductance (g (s)) and differences in source water among treatments are equally probable causes of the delta O-18(w) shift in heavily thinned stands. We modeled inter-annual changes in delta O-18(w) of trees from all treatments using environmental and physiological data and found that the significant increase in delta O-18(w) inter-annual variance was related to greater delta O-18(w) responsiveness to changing environmental conditions for trees in thinned stands when compared to control stands. Based on model results, the more muted climatic response of wood isotopes in slow-growing control trees is likely to be the consequence of reduced carbon sink strength causing a higher degree of mixing of previously stored and fresh assimilates when compared to faster-growing trees in thinned stands. Alternatively, the muted response of delta O-18(w) to climatic variation of trees in the control stand may result from little variation in the control stand in physiological processes (photosynthesis, transpiration) that are known to affect delta O-18(w).