Climate change alters stoichiometry of phosphorus and nitrogen in a semiarid grassland

© 2012 The Authors. New Phytologist © 2012 New Phytologist Trust.

Bibliographische Detailangaben
Veröffentlicht in:The New phytologist. - 1979. - 196(2012), 3 vom: 09. Nov., Seite 807-815
1. Verfasser: Dijkstra, Feike A (VerfasserIn)
Weitere Verfasser: Pendall, Elise, Morgan, Jack A, Blumenthal, Dana M, Carrillo, Yolima, LeCain, Daniel R, Follett, Ronald F, Williams, David G
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2012
Zugriff auf das übergeordnete Werk:The New phytologist
Schlagworte:Journal Article Research Support, Non-U.S. Gov't Research Support, U.S. Gov't, Non-P.H.S. Quaternary Ammonium Compounds Soil Water 059QF0KO0R Carbon Dioxide 142M471B3J Phosphorus mehr... 27YLU75U4W Carbon 7440-44-0 Nitrogen N762921K75
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100 1 |a Dijkstra, Feike A  |e verfasserin  |4 aut 
245 1 0 |a Climate change alters stoichiometry of phosphorus and nitrogen in a semiarid grassland 
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500 |a Citation Status MEDLINE 
520 |a © 2012 The Authors. New Phytologist © 2012 New Phytologist Trust. 
520 |a Nitrogen (N) and phosphorus (P) are essential nutrients for primary producers and decomposers in terrestrial ecosystems. Although climate change affects terrestrial N cycling with important feedbacks to plant productivity and carbon sequestration, the impacts of climate change on the relative availability of N with respect to P remain highly uncertain. In a semiarid grassland in Wyoming, USA, we studied the effects of atmospheric CO(2) enrichment (to 600 ppmv) and warming (1.5/3.0°C above ambient temperature during the day/night) on plant, microbial and available soil pools of N and P. Elevated CO(2) increased P availability to plants and microbes relative to that of N, whereas warming reduced P availability relative to N. Across years and treatments, plant N : P ratios varied between 5 and 18 and were inversely related to soil moisture. Our results indicate that soil moisture is important in controlling P supply from inorganic sources, causing reduced P relative to N availability during dry periods. Both wetter soil conditions under elevated CO(2) and drier conditions with warming can further alter N : P. Although warming may alleviate N constraints under elevated CO(2) , warming and drought can exacerbate P constraints on plant growth and microbial activity in this semiarid grassland 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a Research Support, U.S. Gov't, Non-P.H.S. 
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650 7 |a Soil  |2 NLM 
650 7 |a Water  |2 NLM 
650 7 |a 059QF0KO0R  |2 NLM 
650 7 |a Carbon Dioxide  |2 NLM 
650 7 |a 142M471B3J  |2 NLM 
650 7 |a Phosphorus  |2 NLM 
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650 7 |a 7440-44-0  |2 NLM 
650 7 |a Nitrogen  |2 NLM 
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700 1 |a Pendall, Elise  |e verfasserin  |4 aut 
700 1 |a Morgan, Jack A  |e verfasserin  |4 aut 
700 1 |a Blumenthal, Dana M  |e verfasserin  |4 aut 
700 1 |a Carrillo, Yolima  |e verfasserin  |4 aut 
700 1 |a LeCain, Daniel R  |e verfasserin  |4 aut 
700 1 |a Follett, Ronald F  |e verfasserin  |4 aut 
700 1 |a Williams, David G  |e verfasserin  |4 aut 
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