Carbon sequestration and plant community dynamics following reforestation of tropical pasture

• Published in: Ecological applications 2004-08, Vol.14 (4), p.1115-1127
• Main Authors: Silver, Whendee L., Kueppers, Lara M., Lugo, Ariel E., Ostertag, Rebecca, Matzek, Virginia
• Format: Article
• Language: English
• Subjects: biodiversity; biomass; C isotopes; C sequestration; Forest ecology; Forest ecosystems; Forest soils; Luquillo Experimental Forest; Mineral soils; nonnative species; Pastures; productivity; Puerto Rico; Reforestation; Soil ecology; Species; Tropical forests; tropical reforestation; Tropical soils
• ISSN: 1051-0761; 1939-5582
• DOI: 10.1890/03-5123

Conversion of abandoned cattle pastures to secondary forests and plantations in the tropics has been proposed as a means to increase rates of carbon (C) sequestration from the atmosphere and enhance local biodiversity. We used a long-term tropical reforestation project (55-61 yr) to estimate rates of above- and belowground C sequestration and to investigate the impact of planted species on overall plant community structure. Thirteen tree species (nine native and four nonnative species) were planted as part of the reforestation effort in the mid to late 1930s. In 1992, there were 75 tree species (>9.1 cm dbh) in the forest. Overall, planted species accounted for 40% of the importance value of the forest; planted nonnative species contributed only 5% of the importance value. In the reforested ecosystem, the total soil C pool (0-60 cm depth) was larger than the aboveground C pool, and there was more soil C in the forest ($102 \pm 10 Mg/ha$[mean ± 1 SE]) than in an adjacent pasture of similar age ($69 \pm 16 Mg/ha$). Forest soil C ($C_{3}-C$) increased at a rate of$\sim 0.9 Mg\cdot ha^{-1}\cdot yr^{-1}$, but residual pasture C ($C_{4}-C$) was lost at a rate of$0.4 Mg\cdot ha^{-1}\cdot yr^{-1}$, yielding a net gain of 33 Mg/ha as a result of 61 years of forest regrowth. Aboveground C accumulated at a rate of$1.4 \pm 0.05 Mg\cdot ha^{-1}\cdot yr^{-1}$, to a total of$80 \pm 3 Mg/ha$. A survey of 426 merchantable trees in 1959 and 1992 showed that they grew faster in the second 33 years of forest development than in the first 22 years, indicating that later stages of forest development can play an important role in C sequestration. Few indices of C cycling were correlated with plant community composition or structure. Our results indicate that significant soil C can accumulate with reforestation and that there are strong legacies of pasture use and reforestation in plant community structure and rates of plant C sequestration.