Soil warming alters microbial substrate use in alpine soils

© 2013 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 20(2014), 4 vom: 04. Apr., Seite 1327-38
1. Verfasser: Streit, Kathrin (VerfasserIn)
Weitere Verfasser: Hagedorn, Frank, Hiltbrunner, David, Portmann, Magdalena, Saurer, Matthias, Buchmann, Nina, Wild, Birgit, Richter, Andreas, Wipf, Sonja, Siegwolf, Rolf T W
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2014
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article Research Support, Non-U.S. Gov't Larix decidua Pinus mugo continuous 13C labeling free air CO2 enrichment (FACE) fungi gram negative bacteria gram positive bacteria phospholipid fatty acids (PLFA) mehr... soil warming Fatty Acids Phospholipids Soil Carbon 7440-44-0
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520 |a Will warming lead to an increased use of older soil organic carbon (SOC) by microbial communities, thereby inducing C losses from C-rich alpine soils? We studied soil microbial community composition, activity, and substrate use after 3 and 4 years of soil warming (+4 °C, 2007-2010) at the alpine treeline in Switzerland. The warming experiment was nested in a free air CO2 enrichment experiment using depleted (13)CO2 (δ(13)C = -30‰, 2001-2009). We traced this depleted (13)C label in phospholipid fatty acids (PLFA) of the organic layer (0-5 cm soil depth) and in C mineralized from root-free soils to distinguish substrate ages used by soil microorganisms: fixed before 2001 ('old'), from 2001 to 2009 ('new') or in 2010 ('recent'). Warming induced a sustained stimulation of soil respiration (+38%) without decline in mineralizable SOC. PLFA concentrations did not reveal changes in microbial community composition due to soil warming, but soil microbial metabolic activity was stimulated (+66%). Warming decreased the amount of new and recent C in the fungal biomarker 18:2ω6,9 and the amount of new C mineralized from root-free soils, implying a shift in microbial substrate use toward a greater use of old SOC. This shift in substrate use could indicate an imbalance between C inputs and outputs, which could eventually decrease SOC storage in this alpine ecosystem 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a Larix decidua 
650 4 |a Pinus mugo 
650 4 |a continuous 13C labeling 
650 4 |a free air CO2 enrichment (FACE) 
650 4 |a fungi 
650 4 |a gram negative bacteria 
650 4 |a gram positive bacteria 
650 4 |a phospholipid fatty acids (PLFA) 
650 4 |a soil warming 
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650 7 |a Phospholipids  |2 NLM 
650 7 |a Soil  |2 NLM 
650 7 |a Carbon  |2 NLM 
650 7 |a 7440-44-0  |2 NLM 
700 1 |a Hagedorn, Frank  |e verfasserin  |4 aut 
700 1 |a Hiltbrunner, David  |e verfasserin  |4 aut 
700 1 |a Portmann, Magdalena  |e verfasserin  |4 aut 
700 1 |a Saurer, Matthias  |e verfasserin  |4 aut 
700 1 |a Buchmann, Nina  |e verfasserin  |4 aut 
700 1 |a Wild, Birgit  |e verfasserin  |4 aut 
700 1 |a Richter, Andreas  |e verfasserin  |4 aut 
700 1 |a Wipf, Sonja  |e verfasserin  |4 aut 
700 1 |a Siegwolf, Rolf T W  |e verfasserin  |4 aut 
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773 1 8 |g volume:20  |g year:2014  |g number:4  |g day:04  |g month:04  |g pages:1327-38 
856 4 0 |u http://dx.doi.org/10.1111/gcb.12396  |3 Volltext 
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