Peer-Reviewed Journal Details
Mandatory Fields
Creamer, CA;de Menezes, AB;Krull, ES;Sanderman, J;Newton-Walters, R;Farrell, M
2015
January
Soil Biology & Biochemistry
Microbial community structure mediates response of soil C decomposition to litter addition and warming
Published
Altmetric: 1WOS: 30 ()
Optional Fields
ORGANIC-MATTER DECOMPOSITION CARBON-USE EFFICIENCY HOME-FIELD ADVANTAGE 16S RIBOSOMAL-RNA TEMPERATURE SENSITIVITY THEORETICAL-MODEL CLIMATE-CHANGE ELEVATED CO2 STOICHIOMETRIC CONTROLS NITROGEN LIMITATION
80
175
188
Microbial activity has been highlighted as one of the main unknowns controlling the fate and turnover of soil organic matter (SUM) in response to climate change. How microbial community structure and function may (or may not) interact with increasing temperature to impact the fate and turnover of SUM, in particular when combined with changes in litter chemistry, is not well understood. The primary aim of this study was to determine if litter chemistry impacted the decomposition of soil and litter-derived carbon (C), and its interaction with temperature, and whether this response was controlled by microbial community structure and function. Fresh or pre-incubated eucalyptus leaf litter (C-13 enriched) was added to a woodland soil and incubated at 12, 22, or 32 degrees C. We tracked the movement of litter and soil-derived C into CO2, water-extractable organic carbon (WEOC), and microbial phospholipids (PLFA). The litter additions produced significant changes in every parameter measured, while temperature, interacting with litter chemistry, predominately affected soil C respiration (priming and temperature sensitivity), microbial community structure, and the metabolic quotient (a proxy for microbial carbon use efficiency [CUE]). The direction of priming varied with the litter additions (negative with fresh litter, positive with pre-incubated litter) and was related to differences in the composition of microbial communities degrading soil-C, particularly gram-positive and gram-negative bacteria, resulting from litter addition. Soil-C decomposition in both litter treatments was more temperature sensitive (higher Q(10)) than in the soil-only control, and soil-C priming became increasingly positive with temperature. However, microbes utilizing soil-C in the litter treatments had higher CUE, suggesting the longer-term stability of soil-C may be increased at higher temperature with litter addition. Our results show that in the same soil, the growth of distinct microbial communities can alter the turnover and fate of SUM and, in the context of global change, its response to temperature. (C) 2014 Elsevier Ltd. All rights reserved.
0038-0717
10.1016/j.soilbio.2014.10.008
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