Thermal adaptation of soil microbial respiration to elevated temperature.

Abstract:

:In the short-term heterotrophic soil respiration is strongly and positively related to temperature. In the long-term, its response to temperature is uncertain. One reason for this is because in field experiments increases in respiration due to warming are relatively short-lived. The explanations proposed for this ephemeral response include depletion of fast-cycling, soil carbon pools and thermal adaptation of microbial respiration. Using a > 15 year soil warming experiment in a mid-latitude forest, we show that the apparent 'acclimation' of soil respiration at the ecosystem scale results from combined effects of reductions in soil carbon pools and microbial biomass, and thermal adaptation of microbial respiration. Mass-specific respiration rates were lower when seasonal temperatures were higher, suggesting that rate reductions under experimental warming likely occurred through temperature-induced changes in the microbial community. Our results imply that stimulatory effects of global temperature rise on soil respiration rates may be lower than currently predicted.

journal_name

Ecol Lett

journal_title

Ecology letters

authors

Bradford MA,Davies CA,Frey SD,Maddox TR,Melillo JM,Mohan JE,Reynolds JF,Treseder KK,Wallenstein MD

doi

10.1111/j.1461-0248.2008.01251.x

subject

Has Abstract

pub_date

2008-12-01 00:00:00

pages

1316-27

issue

12

eissn

1461-023X

issn

1461-0248

pii

ELE1251

journal_volume

11

pub_type

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