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231225s2021 xx |||||o 00| ||eng c |
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|a 10.1111/gcb.15867
|2 doi
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|a pubmed24n1100.xml
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|a (DE-627)NLM330076906
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|a (NLM)34464997
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|a DE-627
|b ger
|c DE-627
|e rakwb
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| 041 |
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|a eng
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| 100 |
1 |
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|a Huang, Wenjuan
|e verfasserin
|4 aut
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| 245 |
1 |
0 |
|a High carbon losses from oxygen-limited soils challenge biogeochemical theory and model assumptions
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| 264 |
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|c 2021
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| 336 |
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|a Text
|b txt
|2 rdacontent
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|a ƒaComputermedien
|b c
|2 rdamedia
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| 338 |
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|a ƒa Online-Ressource
|b cr
|2 rdacarrier
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| 500 |
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|a Date Completed 17.11.2021
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|a Date Revised 17.11.2021
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|a published: Print-Electronic
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|a Citation Status MEDLINE
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| 520 |
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|a © 2021 The Authors. Global Change Biology published by John Wiley & Sons Ltd.
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|a Oxygen (O2 ) limitation contributes to persistence of large carbon (C) stocks in saturated soils. However, many soils experience spatiotemporal O2 fluctuations impacted by climate and land-use change, and O2 -mediated climate feedbacks from soil greenhouse gas emissions remain poorly constrained. Current theory and models posit that anoxia uniformly suppresses carbon (C) decomposition. Here we show that periodic anoxia may sustain or even stimulate decomposition over weeks to months in two disparate soils by increasing turnover and/or size of fast-cycling C pools relative to static oxic conditions, and by sustaining decomposition of reduced organic molecules. Cumulative C losses did not decrease consistently as cumulative O2 exposure decreased. After >1 year, soils anoxic for 75% of the time had similar C losses as the oxic control but nearly threefold greater climate impact on a CO2 -equivalent basis (20-year timescale) due to high methane (CH4 ) emission. A mechanistic model incorporating current theory closely reproduced oxic control results but systematically underestimated C losses under O2 fluctuations. Using a model-experiment integration (ModEx) approach, we found that models were improved by varying microbial maintenance respiration and the fraction of CH4 production in total C mineralization as a function of O2 availability. Consistent with thermodynamic expectations, the calibrated models predicted lower microbial C-use efficiency with increasing anoxic duration in one soil; in the other soil, dynamic organo-mineral interactions implied by our empirical data but not represented in the model may have obscured this relationship. In both soils, the updated model was better able to capture transient spikes in C mineralization that occurred following anoxic-oxic transitions, where decomposition from the fluctuating-O2 treatments greatly exceeded the control. Overall, our data-model comparison indicates that incorporating emergent biogeochemical properties of soil O2 variability will be critical for effectively modeling C-climate feedbacks in humid ecosystems
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|a Journal Article
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| 650 |
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4 |
|a ModEx
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| 650 |
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4 |
|a carbon decomposition
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| 650 |
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4 |
|a carbon stable isotope
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| 650 |
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4 |
|a iron redox
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| 650 |
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4 |
|a methane
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| 650 |
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4 |
|a microbial model
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| 650 |
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4 |
|a mineral-associated carbon
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| 650 |
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4 |
|a oxygen fluctuation
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| 650 |
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7 |
|a Soil
|2 NLM
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| 650 |
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7 |
|a Carbon Dioxide
|2 NLM
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| 650 |
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7 |
|a 142M471B3J
|2 NLM
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| 650 |
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7 |
|a Carbon
|2 NLM
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| 650 |
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7 |
|a 7440-44-0
|2 NLM
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| 650 |
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7 |
|a Methane
|2 NLM
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| 650 |
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7 |
|a OP0UW79H66
|2 NLM
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| 650 |
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7 |
|a Oxygen
|2 NLM
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| 650 |
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7 |
|a S88TT14065
|2 NLM
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| 700 |
1 |
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|a Wang, Kefeng
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Ye, Chenglong
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Hockaday, William C
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Wang, Gangsheng
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Hall, Steven J
|e verfasserin
|4 aut
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| 773 |
0 |
8 |
|i Enthalten in
|t Global change biology
|d 1999
|g 27(2021), 23 vom: 30. Dez., Seite 6166-6180
|w (DE-627)NLM098239996
|x 1365-2486
|7 nnns
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| 773 |
1 |
8 |
|g volume:27
|g year:2021
|g number:23
|g day:30
|g month:12
|g pages:6166-6180
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| 856 |
4 |
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|u http://dx.doi.org/10.1111/gcb.15867
|3 Volltext
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|d 27
|j 2021
|e 23
|b 30
|c 12
|h 6166-6180
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