Phosphorus rather than nitrogen regulates ecosystem carbon dynamics after permafrost thaw

© 2021 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 27(2021), 22 vom: 08. Nov., Seite 5818-5830
1. Verfasser: Yang, Guibiao (VerfasserIn)
Weitere Verfasser: Peng, Yunfeng, Abbott, Benjamin W, Biasi, Christina, Wei, Bin, Zhang, Dianye, Wang, Jun, Yu, Jianchun, Li, Fei, Wang, Guanqin, Kou, Dan, Liu, Futing, Yang, Yuanhe
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2021
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article carbon cycle carbon fluxes carbon-climate feedback climate warming nutrient availability thermokarst Phosphorus 27YLU75U4W Carbon mehr... 7440-44-0 Nitrogen N762921K75
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520 |a Ecosystem carbon (C) dynamics after permafrost thaw depends on more than just climate change since soil nutrient status may also impact ecosystem C balance. It has been advocated that nitrogen (N) release upon permafrost thaw could promote plant growth and thus offset soil C loss. However, compared with the widely accepted C-N interactions, little is known about the potential role of soil phosphorus (P) availability. We combined 3-year field observations along a thaw sequence (constituted by four thaw stages, i.e., non-collapse and 5, 14, and 22 years since collapse) with an in-situ fertilization experiment (included N and P additions at the level of 10 g N m-2  year-1 and 10 g P m-2  year-1 ) to evaluate ecosystem C-nutrient interactions upon permafrost thaw. We found that changes in soil P availability rather than N availability played an important role in regulating gross primary productivity and net ecosystem productivity along the thaw sequence. The fertilization experiment confirmed that P addition had stronger effects on plant growth than N addition in this permafrost ecosystem. These two lines of evidence highlight the crucial role of soil P availability in altering the trajectory of permafrost C cycle under climate warming 
650 4 |a Journal Article 
650 4 |a carbon cycle 
650 4 |a carbon fluxes 
650 4 |a carbon-climate feedback 
650 4 |a climate warming 
650 4 |a nutrient availability 
650 4 |a thermokarst 
650 7 |a Phosphorus  |2 NLM 
650 7 |a 27YLU75U4W  |2 NLM 
650 7 |a Carbon  |2 NLM 
650 7 |a 7440-44-0  |2 NLM 
650 7 |a Nitrogen  |2 NLM 
650 7 |a N762921K75  |2 NLM 
700 1 |a Peng, Yunfeng  |e verfasserin  |4 aut 
700 1 |a Abbott, Benjamin W  |e verfasserin  |4 aut 
700 1 |a Biasi, Christina  |e verfasserin  |4 aut 
700 1 |a Wei, Bin  |e verfasserin  |4 aut 
700 1 |a Zhang, Dianye  |e verfasserin  |4 aut 
700 1 |a Wang, Jun  |e verfasserin  |4 aut 
700 1 |a Yu, Jianchun  |e verfasserin  |4 aut 
700 1 |a Li, Fei  |e verfasserin  |4 aut 
700 1 |a Wang, Guanqin  |e verfasserin  |4 aut 
700 1 |a Kou, Dan  |e verfasserin  |4 aut 
700 1 |a Liu, Futing  |e verfasserin  |4 aut 
700 1 |a Yang, Yuanhe  |e verfasserin  |4 aut 
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773 1 8 |g volume:27  |g year:2021  |g number:22  |g day:08  |g month:11  |g pages:5818-5830 
856 4 0 |u http://dx.doi.org/10.1111/gcb.15845  |3 Volltext 
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