Title
Adaptation of soil microbial growth to temperature: Using a tropical elevation gradient to predict future changes
Date Issued
01 March 2019
Access level
open access
Resource Type
journal article
Author(s)
Nottingham A.T.
Bååth E.
Reischke S.
Meir P.
Publisher(s)
Blackwell Publishing Ltd
Abstract
Terrestrial biogeochemical feedbacks to the climate are strongly modulated by the temperature response of soil microorganisms. Tropical forests, in particular, exert a major influence on global climate because they are the most productive terrestrial ecosystem. We used an elevation gradient across tropical forest in the Andes (a gradient of 20°C mean annual temperature, MAT), to test whether soil bacterial and fungal community growth responses are adapted to long-term temperature differences. We evaluated the temperature dependency of soil bacterial and fungal growth using the leucine- and acetate-incorporation methods, respectively, and determined indices for the temperature response of growth: Q 10 (temperature sensitivity over a given 10oC range) and T min (the minimum temperature for growth). For both bacterial and fungal communities, increased MAT (decreased elevation) resulted in increases in Q 10 and T min of growth. Across a MAT range from 6°C to 26°C, the Q 10 and T min varied for bacterial growth (Q 10–20  = 2.4 to 3.5; T min  = −8°C to −1.5°C) and fungal growth (Q 10–20  = 2.6 to 3.6; T min  = −6°C to −1°C). Thus, bacteria and fungi did not differ significantly in their growth temperature responses with changes in MAT. Our findings indicate that across natural temperature gradients, each increase in MAT by 1°C results in increases in T min of microbial growth by approximately 0.3°C and Q 10–20 by 0.05, consistent with long-term temperature adaptation of soil microbial communities. A 2°C warming would increase microbial activity across a MAT gradient of 6°C to 26°C by 28% to 15%, respectively, and temperature adaptation of microbial communities would further increase activity by 1.2% to 0.3%. The impact of warming on microbial activity, and the related impact on soil carbon cycling, is thus greater in regions with lower MAT. These results can be used to predict future changes in the temperature response of microbial activity over different levels of warming and over large temperature ranges, extending to tropical regions.
Start page
827
End page
838
Volume
25
Issue
3
Language
English
OCDE Knowledge area
Investigación climática Biología celular, Microbiología Ciencia del suelo
Scopus EID
2-s2.0-85059587397
PubMed ID
Source
Global Change Biology
ISSN of the container
13541013
Sponsor(s)
This study was led with support from the UK Natural Environment Research Council (NERC), NE/G018278/1 and NE/N006852/1 to PM and also by an Australian Research Council (ARC) grant DP170104091 to PM and a European Union Marie-Curie Fellowship FP7-2012-329360 to ATN. We thank the Asociación para la Conservación de la Cuenca Amazónica (ACCA) in Cusco and the Instituto Nacional de Recursos Naturales (INRENA) in Lima for access to the study sites. For their logistical support, we thank Dr. Eric Cosio and Eliana Esparza Ballón at Pontificia Universidad Católica del Perú (PUCP). For field support, we thank Walter H. Huasco and Adan J. Q. Ccahuana. This study an output of the Andes Biodiversity and Ecosystem Research Group consortium (www.andesconservation.org) and part of LUCCI (Lund University Centre for studies of Carbon Cycle and Climate Interactions).
Sources of information: Directorio de Producción Científica Scopus