Phosphorus rather than nitrogen regulates ecosystem carbon dynamics after permafrost thaw
© 2021 John Wiley & Sons Ltd.
Veröffentlicht in: | Global change biology. - 1999. - 27(2021), 22 vom: 08. Nov., Seite 5818-5830 |
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Weitere Verfasser: | , , , , , , , , , , , |
Format: | Online-Aufsatz |
Sprache: | English |
Veröffentlicht: |
2021
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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... |
Zusammenfassung: | © 2021 John Wiley & Sons Ltd. 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 |
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Beschreibung: | Date Completed 01.11.2021 Date Revised 01.11.2021 published: Print-Electronic Citation Status MEDLINE |
ISSN: | 1365-2486 |
DOI: | 10.1111/gcb.15845 |