Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1029/2021JG006492 |
Climatic Controls on Soil Carbon Accumulation and Loss in a Dryland Ecosystems | |
Waring, Bonnie G.; Smith, Kenneth R.; Grote, Edmund E.; Howell, Armin; Reibold, Robin; Tucker, Colin L.; Reed, Sasha C. | |
通讯作者 | Waring, BG (corresponding author),Utah State Univ, Dept Biol, Logan, UT 84322 USA. ; Waring, BG (corresponding author),Utah State Univ, Ctr Ecol, Logan, UT 84322 USA. ; Waring, BG (corresponding author),Imperial Coll London, Grantham Inst Climate Change & Environm, London, England. |
来源期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES
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ISSN | 2169-8953 |
EISSN | 2169-8961 |
出版年 | 2021 |
卷号 | 126期号:12 |
英文摘要 | Arid and semiarid ecosystems drive year-to-year variability in the strength of the terrestrial carbon (C) sink, yet there is uncertainty about how soil C gains and losses contribute to this variation. To address this knowledge gap, we embedded C-depleted soil mesocosms, containing litter or biocrust C inputs, within an in situ dryland ecosystem warming experiment. Over the course of one year, changes in microbial biomass and total soil organic C pools were monitored alongside hourly measurements of soil CO2 flux. We also developed a biogeochemical model to explore the mechanisms that gave rise to observed soil C dynamics. Field data and model simulations demonstrated that water exerted much stronger control on soil biogeochemistry than temperature, with precipitation events triggering large CO2 pulses and transport of litter- and biocrust-derived C into the soil profile. We expected leaching of organic matter would result in steady accumulation of C within the mineral soil over time. Instead, the size of the total organic C pool fluctuated throughout the year, largely in response to microbial growth: increases in the size of microbial biomass were negatively correlated with the quantity of C residing in the top 2 cm, where most biogeochemical changes were observed. Our data and models suggest that microbial responses to precipitation events trigger rapid metabolism of dissolved organic C inputs, which strongly limit accumulation of autotroph-derived C belowground. Accordingly, changes in the magnitude and/or frequency of precipitation events in this dryland ecosystem could have profound impacts on the strength of the soil C sink. |
英文关键词 | biological soil crust desert dryland litter precipitation soil carbon soil respiration warming experiment |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:000734472100024 |
WOS关键词 | ORGANIC-MATTER ; TEMPERATURE SENSITIVITY ; NITROGEN AVAILABILITY ; SEMIARID ECOSYSTEMS ; EXTRACTION METHOD ; RESPIRATION ; DECOMPOSITION ; DYNAMICS ; MOISTURE ; DROUGHT |
WOS类目 | Environmental Sciences ; Geosciences, Multidisciplinary |
WOS研究方向 | Environmental Sciences & Ecology ; Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/375806 |
作者单位 | [Waring, Bonnie G.; Smith, Kenneth R.] Utah State Univ, Dept Biol, Logan, UT 84322 USA; [Waring, Bonnie G.; Smith, Kenneth R.] Utah State Univ, Ctr Ecol, Logan, UT 84322 USA; [Waring, Bonnie G.] Imperial Coll London, Grantham Inst Climate Change & Environm, London, England; [Grote, Edmund E.; Howell, Armin; Reibold, Robin; Tucker, Colin L.; Reed, Sasha C.] US Geol Survey, Southwest Biol Sci Ctr, Moab, UT USA; [Tucker, Colin L.] US Forest Serv, USDA, Northern Res Stn, Houghton, MI USA |
推荐引用方式 GB/T 7714 | Waring, Bonnie G.,Smith, Kenneth R.,Grote, Edmund E.,et al. Climatic Controls on Soil Carbon Accumulation and Loss in a Dryland Ecosystems[J],2021,126(12). |
APA | Waring, Bonnie G..,Smith, Kenneth R..,Grote, Edmund E..,Howell, Armin.,Reibold, Robin.,...&Reed, Sasha C..(2021).Climatic Controls on Soil Carbon Accumulation and Loss in a Dryland Ecosystems.JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES,126(12). |
MLA | Waring, Bonnie G.,et al."Climatic Controls on Soil Carbon Accumulation and Loss in a Dryland Ecosystems".JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES 126.12(2021). |
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