Literature DB >> 10407310

Molecular insight into soil carbon turnover.

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Abstract

Curie-point pyrolysis-gas chromatography coupled on-line to mass spectrometry (Py-GC/MS) and isotope ratio mass spectrometry (Py-GC/IRMS) were used to determine the individual turnover rate of specific carbohydrates, lignin, lipids and N-containing compounds from French arable soils. The analysed soils were cultivated, either continuously with a C3 plant (wheat delta(13)C-value = -25.2 per thousand), or transferred to a C4 plant (maize delta(13)C-value = -11.4 per thousand) cropping 23 years ago. Most pyrolysis products identified were related to carbohydrates (furans), lipids (hydrocarbons and derivatives of benzene), proteins (nitriles and pyrrole) and lignins (phenols). The relative yield of all individual pyrolysis products was similar in the samples from the maize and control wheat soil. The isotopic enrichment between identical pyrolysis products from the two soils varied from 1 to 12 delta (delta) units, indicating that after 23 years of cultivation 7 to 90% of their C was derived from maize. This suggests a slow mean turnover time varying from 9 to 220 years. Based on the differences in isotopic enrichment of chemical structures after vegetation change the pyrolysis products could be divided into three groups: (i) pyrolysis products with a nearly complete C4 signal, e. g. phenol, derived from lignin degradation products, (ii) pyrolysis products with an intermediate isotopic enrichment of 6-8 per thousand, most likely to be a composite of remaining (possibly physically protected) fragments derived from both maize and native wheat, and (iii) pyrolysis products showing only low enrichments in (13)C of 1-3 per thousand. Most of their precursors were found to be proteinaceaous materials. This indicates that proteins or peptides are indeed preserved during decomposition and humification processes occurring in the soil. Our study highlights the potential of Py-GC/MS-C-IRMS to further novel insights into the dynamics of soil organic constituents. Copyright 1999 John Wiley & Sons, Ltd.

Entities:  

Year:  1999        PMID: 10407310     DOI: 10.1002/(SICI)1097-0231(19990715)13:13<1278::AID-RCM649>3.0.CO;2-N

Source DB:  PubMed          Journal:  Rapid Commun Mass Spectrom        ISSN: 0951-4198            Impact factor:   2.419


  6 in total

1.  Isotopic evidences for microbiologically mediated and direct C input to soil compounds from three different leaf litters during their decomposition.

Authors:  M Rubino; C Lubritto; A D'Onofrio; F Terrasi; C Kramer; G Gleixner; M F Cotrufo
Journal:  Environ Chem Lett       Date:  2008-02-15       Impact factor: 9.027

2.  An isotopic method for testing the influence of leaf litter quality on carbon fluxes during decomposition.

Authors:  Mauro Rubino; C Lubritto; A D'Onofrio; F Terrasi; G Gleixner; M F Cotrufo
Journal:  Oecologia       Date:  2007-07-31       Impact factor: 3.225

3.  The pyrolytic profile of lyophilized and deep-frozen compact part of the human bone.

Authors:  Jolanta Lodowska; Daniel Wolny; Sławomir Kurkiewicz; Ludmiła Węglarz
Journal:  ScientificWorldJournal       Date:  2012-04-24

4.  Isotope fractionation and 13C enrichment in soil profiles during the decomposition of soil organic matter.

Authors:  Björn Boström; Daniel Comstedt; Alf Ekblad
Journal:  Oecologia       Date:  2007-03-31       Impact factor: 3.298

5.  The molecular composition of dissolved organic matter in forest soils as a function of pH and temperature.

Authors:  Vanessa-Nina Roth; Thorsten Dittmar; Reinhard Gaupp; Gerd Gleixner
Journal:  PLoS One       Date:  2015-03-20       Impact factor: 3.240

6.  DNA Stable-Isotope Probing Delineates Carbon Flows from Rice Residues into Soil Microbial Communities Depending on Fertilization.

Authors:  Yali Kong; Yakov Kuzyakov; Yang Ruan; Junwei Zhang; Tingting Wang; Min Wang; Shiwei Guo; Qirong Shen; Ning Ling
Journal:  Appl Environ Microbiol       Date:  2020-03-18       Impact factor: 4.792

  6 in total

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