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Can we set a global threshold age to define mature forests?
Philip Martin1, Martin Jung2, Francis Q Brearley3
1Centre for Conservation Ecology and Environmental Science, Bournemouth University , Bournemouth , United Kingdom.
Peerj
|February 13, 2016
Summary
Global forest biomass density is increasing with age and climate factors like temperature and precipitation. A single threshold age for forest maturity is not feasible due to climate interactions, requiring local assessment.
Area of Science:
- Ecology
- Forestry
- Climate Science
Background:
- Global mature forests show increasing biomass density (BD), with debate on causes like CO2 rise versus land-use legacy.
- Previous studies suggested a 450-year threshold for mature forests but overlooked climate-age interactions.
Purpose of the Study:
- To determine how climate and forest age influence global forest BD.
- To assess if a universal threshold age for forest maturity can be established.
Main Methods:
- Utilized data from published studies to model forest BD using linear mixed-effects models.
- Analyzed dataset representativeness concerning global mature forests, climate space, and forest ages.
- Investigated biases in the dataset, particularly its northern hemisphere and young forest focus.
Main Results:
- Forest BD positively correlated with forest age, mean annual temperature, and annual precipitation.
- The influence of forest age on BD intensified with higher temperatures, while precipitation's effect diminished.
- The dataset exhibited biases towards cooler, drier northern hemisphere forests and those under 250 years old.
Conclusions:
- A single, universal threshold age for forest maturity is not supported; it is locally determined by climate-age interactions.
- Biomass density alone is insufficient to define forest maturity, as biodiversity and tree structure recovery times vary.
- Further research is needed on cost-effective methods for classifying forest maturity.
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