A 15-Year Trend of Carbon Dynamics in Two Massachusetts Forests
Global climate change is driven by human emissions of CO2 and other greenhouse gases. Terrestrial vegetation absorbed approximately 31% of the carbon dioxide emitted by human activities during the most recent decade (2010-2019), slowing the rate of climate change as a result. In this study, we investigate the role that forests, the largest terrestrial carbon sink, play in the carbon balance of a midlatitude forest in north-central Massachusetts, USA. We investigated two forest stands: one (“control”) is a red pine plantation that was established in 1925, the other (“harvest”) is a former red pine plantation harvested in 1990, and is now a naturally regenerating mixed hardwood and white-pine forest. All trees ≥ 5 cm diameter breast height (DBH; 1.3 m) were identified, measured, then tagged, and were surveyed yearly for growth, mortality, and recruitment from 2008-2023.
Using the tree diameter data, we calculated forest carbon sequestration between 2008 and 2023. We found that our control site lost carbon to the atmosphere (from 137 Mg C ha-1 in 2008 to 49 Mg C ha-1 in 2023) due to an ice storm in 2008 and an inferred infestation of red pine scale (a small, invasive insect) in 2022. The harvest site increased carbon storage from 35 Mg C ha-1 in 2008 to 64 Mg C ha-1. Our results underscore the complex carbon dynamics in forested ecosystems and the critical role of episodic disturbances.Research Area | Presenter | Title | Keywords |
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