Regrowth of tropical secondary forests following complete or nearly complete removal of forest vegetation actively stores carbon in aboveground biomass, partially counterbalancing carbon emissions from deforestation, forest degradation, burning of fossil fuels, and other anthropogenic sources. We estimate the age and spatial extent of lowland second-growth forests in the Latin American tropics and model their potential aboveground carbon accumulation over four decades. Our model shows that, in 2008, second-growth forests (1 to 60 years old) covered 2.4 million km² of land (28.1% of the total study area). Over 40 years, these lands can potentially accumulate a total aboveground carbon stock of 8.48 Pg C (petagrams of carbon) in aboveground biomass via low-cost natural regeneration or assisted regeneration, corresponding to a total CO₂ sequestration of 31.09 Pg CO₂. This total is equivalent to carbon emissions from fossil fuel use and industrial processes in all of Latin America and the Caribbean from 1993 to 2014. Ten countries account for 95% of this carbon storage potential, led by Brazil, Colombia, Mexico, and Venezuela. We model future land-use scenarios to guide national carbon mitigation policies. Permitting natural regeneration on 40% of lowland pastures potentially stores an additional 2.0 Pg C over 40 years. Our study provides information and maps to guide national-level forest-based carbon mitigation plans on the basis of estimated rates of natural regeneration and pasture abandonment. Coupled with avoided deforestation and sustainable forest management, natural regeneration of second-growth forests provides a low-cost mechanism that yields a high carbon sequestration potential with multiple benefits for biodiversity and ecosystem services.

Resilient secondary tropical forests?: Although deforestation is rampant across the tropics, forest has a strong capacity to regrow on abandoned lands. These “secondary” forests may increasingly play important roles in biodiversity conservation, climate change mitigation, and landscape restoration. Poorteret al. analyzed the patterns of recovery in forest attributes (related to soil, plant functioning, structure, and diversity) in 77 secondary forest sites in the Americas and West Africa. They found that different attributes recovered at different rates, with soil recovering in less than a decade and species diversity and biomass recovering in little more than a century. The authors discuss how these findings can be applied in efforts to promote forest restoration. —AMS

Tropical secondary forests recover quickly (decades) in tree species richness but slowly (centuries) in species composition.

The recovery of soil conditions is crucial for successful ecosystem restoration and, hence, for achieving the goals of the UN Decade on Ecosystem Restoration. Here, we assess how soils resist forest conversion and agricultural land use, and how soils recover during subsequent tropical forest succession on abandoned agricultural fields. Our overarching question is how soil resistance and recovery depend on local conditions such as climate, soil type and land-use history. For 300 plots in 21 sites across the Neotropics, we used a chronosequence approach in which we sampled soils from two depths in old-growth forests, agricultural fields (i.e. crop fields and pastures), and secondary forests that differ in age (1–95 years) since abandonment. We measured six soil properties using a standardized sampling design and laboratory analyses. Soil resistance strongly depended on local conditions. Croplands and sites on high-activity clay (i.e. high fertility) show strong increases in bulk density and decreases in pH, carbon (C) and nitrogen (N) during deforestation and subsequent agricultural use. Resistance is lower in such sites probably because of a sharp decline in fine root biomass in croplands in the upper soil layers, and a decline in litter input from formerly productive old-growth forest (on high-activity clays). Soil recovery also strongly depended on local conditions. During forest succession, high-activity clays and croplands decreased most strongly in bulk density and increased in C and N, possibly because of strongly compacted soils with low C and N after cropland abandonment, and because of rapid vegetation recovery in high-activity clays leading to greater fine root growth and litter input. Furthermore, sites at low precipitation decreased in pH, whereas sites at high precipitation increased in N and decreased in C : N ratio. Extractable phosphorus (P) did not recover during succession, suggesting increased P limitation as forests age. These results indicate that no single solution exists for effective soil restoration and that local site conditions should determine the restoration strategies. This article is part of the theme issue ‘Understanding forest landscape restoration: reinforcing scientific foundations for the UN Decade on Ecosystem Restoration’.

Os objetivos deste estudo foram caracterizar e comparar a composição florística de oito fragmentos de Mata Seca Calcária e Caatinga Arbórea localizados no norte do Estado de Minas Gerais. O levantamento das espécies arbóreas foi realizado através de visitas periódicas aos fragmentos para coleta de material botânico. Nos oito fragmentos foram encontradas 114 espécies arbóreas pertencentes a 40 famílias botânicas. Dentre as 89 espécies encontradas nos fragmentos de Mata Seca, 37 (42%) foram peculiares a essa formação. No entanto, das 75 espécies amostradas nos remanescentes de Caatinga Arbórea, 25 (33%) ocorreram apenas nesses fragmentos. A análise de agrupamento sugere que a composição florística dos fragmentos é afetada pela fitofisionomia e pelas condições bioecológicas locais a que estes fragmentos estão submetidos. Além disso, a relação observada entre a área dos fragmentos e o número de espécies arbóreas, evidenciou que área é um bom indicador da riqueza de espécies arbóreas nos fragmentos florestais. Portanto, os resultados deste estudo indicaram que fatores históricos (fitofisionomia) e ecológicos (área dos fragmentos e ocorrência de perturbações antrópicas) constituem importantes elementos caracterizadores da composição e riqueza de espécies em fragmentos florestais do norte de Minas Gerais.

Myracrodruon urundeuva Allemão, espécie arbórea conhecida como aroeira, constitui-se em um importante componente das Florestas Estacionais Deciduais do norte de Minas Gerais. Apesar disso, a aroeira vem sofrendo um processo de exploração intensa, de forma predatória, o que vem causando a devastação de suas populações naturais. Este trabalho teve como objetivo conhecer os padrões fenológicos reprodutivos e vegetativos, bem como a capacidade germinativa da aroeira, na Área de Preservação da COPASA em Juramento, MG. Foram feitas observações fenológicas quinzenais, no período de janeiro/2002 a novembro/2003, de 20 indivíduos arbóreos, sendo ainda coletadas sementes, submetidas a diferentes tratamentos de escarificação tegumentar (mecânico, térmico, químico e controle). A espécie apresentou as fenofases reprodutivas e vegetativas influenciadas diferencialmente pelas variáveis ambientais de precipitação e temperatura. Na estação seca ocorreram a floração, frutificação e queda foliar, e a estação chuvosa favoreceu o brotamento da espécie. A capacidade germinativa dos diásporos de aroeira variou entre os tratamentos utilizados, com potencial germinativo e velocidade de germinação altos no tratamento-controle, indicando ausência de dormência. Nesse sentido, estudos básicos sobre as espécies florestais ameaçadas podem ser precursores de modelos e mecanismos para manejo e recuperação de suas populações naturais.