Abstract

Compared with other forest systems, research interest in the potential for a stronger ecosystem carbon sequestration of evergreen forests throughout subtropical China has greatly increased. The eddy covariance technique is widely employed to determine accurate forest-atmosphere carbon dioxide (CO2) flux, which is subsequently used to determine forest ecosystem carbon exchange characteristics. The Dinghushan Biosphere Reserve, a subtropical monsoon evergreen broad-leaved forest, is a suitable study area due to its warm and humid climate (compared with other regions within the same latitude), consequently playing a role in the carbon cycle in the region. For this study, we hypothesized that the forest land in this region generally acts as a carbon sink, and that its carbon sequestration capacity increases over time despite the influence of climatic factors. Here, we compared net CO2 flux data derived from the eddy covariance technique over an 8-year study window. Additionally, we ascertained the effects of various environmental factors on net CO2 flux, while also using the Michaelis–Menten model and a physiologically based process model to track and report on ecosystem carbon exchange characteristics. We observed seasonal trends in daily ecosystem flux, indicative of sensitivity to climatic factors, such as air temperature, precipitation, and sunlight. The carbon sequestration capacity of the region exhibited seasonal variability, increasing from October to March (−264 g C m−2 year−1, i.e., 48.4%) while weakening from April to September (−150 g C m−2 year−1, i.e., 40.4%) on average. The net ecosystem exchange (NEE) rate varied from −518 to −211 g C m−2 year−1; ecosystem respiration (Re) varied from 1,142 to 899 g C m−2 year−1; and gross primary production (GPP) varied from 1,552 to 1,254 g C m−2 year−1. This study found that even though the Dinghushan Biosphere Reserve generally acts as a carbon sink, its carbon sequestration capacity did not increase significantly throughout the study period. The techniques (models) used in this study are suitable for application in other ecosystems globally, which can aid in their management and conservation. Finally, the Dinghushan Biosphere Reserve is both an exemplary and a model forest system useful in exploring CO2 absorption and sequestration from the atmosphere.

Highlights

  • Recent research published by the scientific community on climate change has caused a general sense of alarm

  • The results showed that the Dinghushan Biosphere Reserve was a net CO2 sink throughout the year, with a monthly average of 119.84g C m−2 month−1 and an annual sequestration average of −413.2 g C m−2 year−1

  • This study revealed that monsoon evergreen forests, such as the Dinghushan Biosphere Reserve, can be characterized by multiple variables that correlate in a myriad of complex ways

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Summary

Introduction

Recent research published by the scientific community on climate change has caused a general sense of alarm Anthropogenicderived greenhouse gases, such as carbon dioxide (CO2), are driving global climate change through contamination and alterations in atmospheric gaseous composition (Herndon, 2018; Kweku et al, 2018). Research in China has determined that forest systems on the whole function as a carbon sink with an annual net C sequestration rate of 84 to 154 Tg C/year (e.g., 1 Tg = 1012 g) (Lu et al, 2018) Tropical forest systems, such as the Dinghushan Biosphere Reserve in China, can be employed to tackle climate change, whose alterations can transform the entire planet into one which acts to endanger the whole biosphere (Fuss et al, 2021). Given that the Dinghushan Biosphere Reserve is a United Nations Educational, Scientific, and Cultural Organization (UNESCO) world heritage site that has been preserved for hundreds of years, it acts as a uniquely rich research station (Li et al, 2012; Yang et al, 2021)

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