Abstract

Forest ecosystems play an important role in the global carbon cycle. Therefore, understanding the dynamics of carbon uptake in forest ecosystems is much needed. Pinus cooperi is a widely distributed species in the Sierra Madre Occidental in northern Mexico and future climatic variations could impact these ecosystems. Here, we analyze the variations of trunk carbon in two populations of P. cooperi situated at different elevational gradients, combining dendrochronological techniques and allometry. Carbon sequestration (50% biomass) was estimated from a specific allometric equation for this species based on: (i) variation of intra-annual wood density and (ii) diameter reconstruction. The results show that the population at a higher elevation had greater wood density, basal area, and hence, carbon accumulation. This finding can be explained by an ecological response of trees to adverse weather conditions, which would cause a change in the cellular structure affecting the within-ring wood density profile. The influence of variations in climate on the maximum density of chronologies showed a positive correlation with precipitation and the Multivariate El Niño Southern Oscillation Index during the winter season, and a negative correlation with maximum temperature during the spring season. Monitoring previous conditions to growth is crucial due to the increased vulnerability to extreme climatic variations on higher elevational sites. We concluded that temporal variability of wood density contributes to a better understanding of environmental historical changes and forest carbon dynamics in Northern Mexico, representing a significant improvement over previous studies on carbon sequestration. Assuming a uniform density according to tree age is incorrect, so this method can be used for environmental mitigation strategies, such as for managing P. cooperi, a dominant species of great ecological amplitude and widely used in forest industries.

Highlights

  • The forest growth is one of the most important processes that determine the carbon balance of terrestrial ecosystems [1]

  • These stands are at sites High (H) and Higher (HE), which are in altitude gradients above 2600 msnm, where tree growth was strongly associated with climate in previous research [24]

  • There was a negative correlation between mean series of tree-ring width and maximum density (MXD) (p < 0.01)

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Summary

Introduction

The forest growth is one of the most important processes that determine the carbon balance of terrestrial ecosystems [1]. It is assumed that the density is constant, even though this parameter varies temporally, depending on tree age [16,17,18,19]. This results in differential rates of carbon, with variations occurring among species and ecosystems. We can test the hypothesis that carbon sequestration varies over time and in different ecosystems [20,21] This should help overcome theoretical limitations in understanding carbon fluxes and gaining accurate knowledge of forest productivity

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