Soil resistance and recovery during neotropical forest succession

Author:

van der Sande Masha T.1ORCID,Powers Jennifer S.2,Kuyper Thom W.3,Norden Natalia4,Salgado-Negret Beatriz5,Silva de Almeida Jarcilene6,Bongers Frans1,Delgado Diego7,Dent Daisy H.8910,Derroire Géraldine11ORCID,do Espirito Santo Mario Marcos12,Dupuy Juan Manuel13ORCID,Fernandes Geraldo Wilson14,Finegan Bryan7,Gavito Mayra E.15,Hernández-Stefanoni José Luis13,Jakovac Catarina C.1,Jones Isabel L.16,das Dores Magalhães Veloso Maria12,Meave Jorge A.17,Mora Francisco15,Muñoz Rodrigo117,Pérez-Cárdenas Nathalia15ORCID,Piotto Daniel18,Álvarez-Dávila Esteban19,Caceres-Siani Yasmani20,Dalban-Pilon Coralie11,Dourdain Aurélie11,Du Dan V.21,García Villalobos Daniel4,Nunes Yule Roberta Ferreira12ORCID,Sanchez-Azofeifa Arturo22,Poorter Lourens1

Affiliation:

1. Forest Ecology and Forest Management Group, Wageningen University & Research, P.O. Box 47, 6700 AA Wageningen, The Netherlands

2. Department of Ecology, Evolution, & Behavior and Plant & Microbial Biology, University of Minnesota, Saint Paul, MN 55108, USA

3. Soil Biology Group, Wageningen University & Research, P.O. Box 47, 6700 AA Wageningen, The Netherlands

4. Programa Ciencias Básicas de la Biodiversidad, Instituto de Investigación de Recursos Biológicos Alexander von Humbold, Colombia

5. Departamento de Biología, Universidad Nacional de Colombia, Bogotá, Colombia

6. Departamento de Botânica, Centro de Biociências, Universidade Federal de Pernambuco, Recife, Pernambuco CEP 50670-901, Brazil

7. CATIE-Centro Agronómico Tropical de Investigación y Enseñanza, Turrialba, Costa Rica

8. Smithsonian Tropical Research Institute, Roosevelt Ave. 401 Balboa, Ancon, Panama

9. Max Planck Institute for Animal Behaviour, Konstanz, 78315, Germany

10. Department of Environmental Systems Science, ETH Zürich, 8902, Switzerland

11. Cirad, UMR EcoFoG (AgroParistech, CNRS, Inrae, Université des Antilles, Université de la Guyane), Campus Agronomique, Kourou, French Guiana

12. Departamento de Biologia Geral, Universidade Estadual de Montes Claros, Montes Claros-MG CEP 39401-089, Brazil

13. Centro de Investigación Científica de Yucatán A.C. Unidad de Recursos Naturales, Calle 43 # 130(32 y 34, Colonia Chuburná de Hidalgo, C.P. 97205 Mérida, Yucatán, México

14. Departamento de Genética, Ecologia & Evolução, ICB, Universidade Federal de Minas Gerais, 30161-901 Belo Horizonte, Minas Gerais, Brazil

15. Instituto de Investigaciones en Ecosistemas y Sustentabilidad, Universidad Nacional Autónoma de México, CP 58190 Morelia, Michoacán, México

16. Biological and Environmental Sciences, University of Stirling, Stirling FK9 4LA, UK

17. Departamento de Ecología y Recursos Naturales, Facultad de Ciencias, Universidad Nacional Autónoma de México, Coyoacán, Mexico City CP 04510, México

18. Centro de Formação em Ciências Agroflorestais, Universidade Federal do Sul da Bahia, Itabuna-BA 45613-204, Brazil

19. Open and Distance National University, Bogotá, Colombia

20. Wageningen, the Netherlands

21. Department of Soil and Water Systems, University of Idaho, Moscow, ID 83843, USA

22. Department of Earth and Atmospheric Sciences, Centre for Earth Observation Sciences (CEOS), University of Alberta, Edmonton, Alberta, Canada T6G2E3

Abstract

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’.

Funder

Nederlandse Organisatie voor Wetenschappelijk Onderzoek

Publisher

The Royal Society

Subject

General Agricultural and Biological Sciences,General Biochemistry, Genetics and Molecular Biology

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