Response of soil organic carbon to land-use change in central Brazil: a large-scale comparison of Ferralsols and Acrisols

verfasst von
S. Strey, J. Boy, R. Strey, O. Weber, G. Guggenberger
Abstract

Background and aims: The southeastern part of the Amazon region is one of the largest agricultural frontiers in the world, leading to extensive land-use change. This paper provides evidence for the impacts of land-use change on soil organic carbon (OC) stocks along a large scale for Ferralsols and Acrisols including subsoil. Methods: We took soil samples to 100 cm depth for native vegetation, pasture and crop-field along a 1000 km agricultural transect in central Brazil to determine OC stocks and, by using a stable isotope approach, losses of forest-derived OC. Results: At the scale of individual plots, soil OC stocks indicate a highly heterogeneous response to land-use change (e.g. in Ferralsols in 0–30 cm from −45 % to +57 % Mg OC ha−1 after conversion to pasture), but relatively minor responses when considering the complete transect (i.e. no significant OC changes for similar land-use type). Acrisols evidenced a slower decline of forest-derived OC and simultaneously a faster accumulation of pasture-derived OC than Ferralsols. Surprisingly, the impact of land-use change was more pronounced in the subsoil. Conclusion: Our results emphasize the role of subsoils on carbon cycling which has been previously underestimated, but may also raise doubts whether OC stocks in soil is an appropriate parameter to assess the impacts of land-use conversion on climate change.

Organisationseinheit(en)
Institut für Bodenkunde
Externe Organisation(en)
Universidade Federal de Mato Grosso
Typ
Artikel
Journal
Plant and soil
Band
408
Seiten
327-342
Anzahl der Seiten
16
ISSN
0032-079X
Publikationsdatum
11.2016
Publikationsstatus
Veröffentlicht
Peer-reviewed
Ja
ASJC Scopus Sachgebiete
Bodenkunde, Pflanzenkunde
Ziele für nachhaltige Entwicklung
SDG 13 – Klimaschutzmaßnahmen, SDG 15 – Lebensraum Land
Elektronische Version(en)
https://doi.org/10.1007/s11104-016-2901-6 (Zugang: Geschlossen)