Long-term carbon storage in Brazilian Cerrado soils - a conjunction of wildfires, bioturbation, and local edaphic controls on vegetation

Author(s)

Schellekens, Judith ; Justi, Marina ; Macedo, Rodrigo ; Calegari, Marcia Regina ; Buurman, Peter ; Kuyper, Thomas W. ; de Camargo, Plinio Barbosa ; Vidal-Torrado, Pablo

• Document type: Journal article
• Source: PLANT AND SOIL; v. N/A, p. 18-pg., 2022-12-07.

Abstract

Purpose The objective of this study is to improve our understanding of soil organic matter (SOM) stability in Brazilian Cerrado, by interpreting soil properties at the ecosystem scale and elaborating on the interactions of biotic, climatic and edaphic controls. Methods Three 2 m soil profiles with significantly different total organic carbon TOC content but located on the same geomorphological unit were studied for delta C-13 isotopic composition to connect tree-grass patterns to TOC content. To gain insight into soil carbon stability, C/N, delta C-13 and delta N-15 were analysed for functional organic matter (OM) pools: free particulate OM (POM), occluded POM, base-extractable OM, and mineral-associated OM. Results Small but abrupt shifts of delta C-13 with depth reflected simultaneous changes in tree-grass vegetation patterns over the past 10,000 years in all three profiles. These temporal changes were superimposed on spatial differences as indicated by consistent differences in delta C-13 values between the profiles, reflecting that site-specific differences in tree-grass patterns persisted over the past 10,000 years. Profiles with a historically larger contribution from trees (as evidenced by lower delta C-13) had increased charcoal contents. Downward movement of charcoal by intense bioturbation occurred faster in the OM-rich soils as suggested by C-14 dating. Conclusion We found that long-term carbon storage in Brazilian Cerrado soils was a conjunction of wildfires, bioturbation, and local edaphic controls on tree-grass composition. Soils with an OM-rich thick A-horizon had more trees, more charcoal, and a higher activity of soil macrofauna, which was related to local differences in soil water availability. (AU)

• FAPESP's process: 14/23969-0 - Soil organic matter dynamics and its relation to the environment: molecular chemistry (pyrolysis-GC/MS) to understand soil formation in tropical soils
• Grantee: Pablo Vidal Torrado
• Support Opportunities: Regular Research Grants
• FAPESP's process: 14/21128-8 - Organic matter caracterization and pedogenesis in humic latossols under savanna vegetation
• Grantee: Marina Justi
• Support Opportunities: Scholarships in Brazil - Master
• FAPESP's process: 13/03953-9 - Organic matter dynamics in tropical peatlands (Diamantina, Brasil) - development of molecular proxies to reconstruct environmental changes
• Grantee: Judith Schellekens
• Support Opportunities: Scholarships in Brazil - Post-Doctoral