Nitrogen and phosphorus supply controls soil organic carbon mineralization in tropical topsoil and subsoil

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Title:Main Title: Nitrogen and phosphorus supply controls soil organic carbon mineralization in tropical topsoil and subsoil
Description:Abstract: Nitrogen (N) deposition to soils is globally rising, but its effect on soil organic carbon (SOC) turnover is still uncertain. Moreover, common theories of stoichiometric decomposition and microbial N mining predict opposing effects of N supply on SOC turnover. We hypothesized that the effect of N deposition on SOC turnover depends on initial soil nutrient conditions. Thus, we sampled tropical forests and rubber gardens with pronounced gradients of nutrient availability from the topsoil to the deep subsoil (up to 400 cm) and measured substrate-induced respiration (SIR) for 30 days in four treatments (C, CN, CP, CNP additions). A natural 13C abundance approach was conducted to quantify priming effects (PE) of the added C on SOC mineralization. For this purpose we assessed the 13CO2 isotope composition after adding a C4 sugar to the C3 soil; to correct for isotopic fractionation a treatment with C3 sugar additions served as control. We found that nutrient additions to topsoil did neither alter cumulative CO2 release within 30 days (SIRacc) nor PE (PE = 1.6, i.e., sugar additions raised the release of SOC-derived CO2 by a factor of 1.6). In the upper subsoil (30-100 cm), however, both CN and CP additions increased SIRacc (by 239% and 92%, respectively) and the PE (PE = 5.2 and 3.3, respectively) relative to the treatments that received C only (PE = 1.7), while CNP additions revealed the largest increase of SIRacc (267%) and PE (PE = 6.0). In the deep subsoil (>130 cm depth), only the CNP addition consistently increased SIRacc (by 871%) and PE (PE = 5.2) relative to only C additions (PE = 2.0). We conclude that microbial activity was not limited by nutrients in the topsoil but was co-limited by both N and P in the subsoil. The results imply that microbes mine nutrients from previously unavailable pools under the conditions that 1) deficiency actually exists, 2) co-limitation is alleviated, and 3) nutrient reserves are present. Yet, as opposed to microbial nutrient mining theories, we showed that the subsoil PE is highest when nutrient supply matches microbial demand. As a result also N deposition might exert variable effects on SOC turnover in tropical soils: it might have no effect in nutrient-rich topsoils and in co-limited subsoils without P reserves but might increase SOC turnover in co-limited subsoils with potentially acquirable P reserves.
Identifier:10.1016/j.soilbio.2018.01.024 (DOI)
Responsible Party
Creators:Nele Meyer (Author), Gerd Welp (Author), Andrei Rodionov (Author), Nils Borchard (Author), Christopher Martius (Author), Wulf Amelung (Author)
Publisher:Elsevier
Publication Year:2018
Topic
TR32 Topic:Soil
Related Subproject:B3
Subjects:Keywords: Soil Respiration, Soil Organic Matter, CO2
File Details
Filename:Meyer_2018_SBB.pdf
Data Type:Text - Article
File Size:639 KB
Date:Accepted: 23.01.2018
Mime Type:application/pdf
Data Format:PDF
Language:English
Status:Completed
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Download Permission:Only Project Members
General Access and Use Conditions:According to the TR32DB data policy agreement.
Access Limitations:According to the TR32DB data policy agreement.
Licence:[TR32DB] Data policy agreement
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Publication Status:Published
Review Status:Peer reviewed
Publication Type:Article
Article Type:Journal
Source:Soil Biology and Biochemistry
Volume:119
Number of Pages:10 (152 - 161)
Metadata Details
Metadata Creator:Nele Meyer
Metadata Created:06.02.2018
Metadata Last Updated:06.02.2018
Subproject:B3
Funding Phase:3
Metadata Language:English
Metadata Version:V50
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