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首页> 外文期刊>Soil Biology & Biochemistry >Laccase activity in Sphagnum-dominated peatland: A study based on a novel measurement of delay dynamics (MDD) for determining laccase activity
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Laccase activity in Sphagnum-dominated peatland: A study based on a novel measurement of delay dynamics (MDD) for determining laccase activity

机译:Sphagnum主导的泥炭地的漆酶活性:基于用于确定LACCASE活动的新型延迟动力学(MDD)的研究

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摘要

The large reservoir of organic carbon in peatland is essential for the global carbon cycle. Laccase, probably the largest class of phenol oxidases in soil, plays an important role in the primary degradation of recalcitrant polyphenolic compounds. However, the traditional method used to test laccase activity may not be suitable for peatland, given that reductive compounds would result in the reduction of chromophore 2,2'-azino-bis (3-ethylbenzo-thiazoline-6-sulfonic acid) radical cation catalyzed by laccase. In this study, the organic and inorganic constituents affecting laccase activity assay in peatland were systematically studied. The experiments indicated that high content of ferrous iron in peatland can significantly affect the measurement of laccase activity by delaying the ABTS(center dot+) absorbance dynamic inflection point, and three typical dynamic changes of ABTS(center dot+) absorbance in Dajiuhu peat samples were found. In this study, we propose a novel method based on delay dynamics (MDD) to determine laccase activity in peatland and applied it to the investigation of Dajiuhu, a Sphagnum-dominated peatland. The results show that the laccase activities measured using MDD (24.45 +/- 10.89 mu mol g(-1).h(-1)) are considerably higher than that measured by the traditional method (12.10 +/- 12.06 mu mol g(-1).h(-1)) in Dajiuhu peatland. In addition, there was no clear evidence that ferrous iron can stimulate laccase activity. Conversely, we found that ferrous iron can even inhibit the catalytic efficiency of laccase. Laccase activities were higher at the depth of 0-10 cm (31.12 +/- 13.36 mu mol g(-1).h(-1)) compared with that at 10-20 cm (18.88 +/- 5.67 mu mol g(-1).h(-1) ), suggesting the sub-optimal conditions for laccase activity with increasing depth in Sphagnum-dominated peatland. In addition, laccase activities decreased significantly with pH increase in Dajiuhu peatland, which is different from the generally positive relationship between soil pH and phenol oxidase activities tested by L-DOPA assay.
机译:泥炭地的大型有机碳库对全球碳循环至关重要。漆酶,可能是土壤中最大的酚氧化酶,在顽钙多酚化合物的初级降解中起重要作用。然而,鉴于还原化合物将导致发色团2,2'-唑胺-6-磺酸)自由基阳离子,可以不适用于测试漆酶活性的传统方法可能不适用于泥炭地。由漆酶催化。在本研究中,系统地研究了影响泥炭地涂层活性测定的有机和无机成分。实验表明,通过延迟ABTS(中心点+)吸光度动态拐点,泥炭地岩石中的含铁铁的高含量可以显着影响漆酶活性的测量,并且发现大学泥浆样品中的ABTS(中心DOT +)吸光度的三种典型动态变化。在这项研究中,我们提出了一种基于延迟动力学(MDD)的新方法,以确定泥炭地的漆晶件活动,并将其应用于Dajiuhu,Sphagnum主导的泥炭地。结果表明,使用MDD测量的漆酶活性(24.45 +/-10.89μmmolg(-1).h(-1))比传统方法测量的(12.10 +/- 12.06 mol g( -1).h(-1))在大羽湖泥炭地。此外,没有明确的证据表明铁铁可以刺激漆酶活性。相反,我们发现铁铁甚至可以抑制漆酶的催化效率。与10-20cm(18.88 +/- 5.67 mm mol g(18.88 +/- 5.67 mm mol g( -1).h(-1)),暗示漆酶活性的次良条件,在斯巴格姆主导的泥炭地中增加深度。此外,大羽湖泥炭地的pH增加,漆酶活性显着降低,这与L-DOPA测定检测的土壤pH与酚氧化酶活性的大致正关系不同。

著录项

  • 来源
    《Soil Biology & Biochemistry》 |2019年第2019期|共8页
  • 作者单位

    China Univ Geosci Sch Earth Sci Hubei Key Lab Crit Zone Evolut Wuhan 430074 Hubei Peoples R China;

    China Univ Geosci Sch Earth Sci Hubei Key Lab Crit Zone Evolut Wuhan 430074 Hubei Peoples R China;

    China Univ Geosci Sch Earth Sci Hubei Key Lab Crit Zone Evolut Wuhan 430074 Hubei Peoples R China;

    China Univ Geosci Sch Earth Sci Hubei Key Lab Crit Zone Evolut Wuhan 430074 Hubei Peoples R China;

    China Univ Geosci Sch Earth Sci Hubei Key Lab Crit Zone Evolut Wuhan 430074 Hubei Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 农业基础科学;
  • 关键词

    Peatland; Laccase; Ferrous iron; Delay dynamics; Carbon cycle;

    机译:泥炭地;漆酶;铁铁;延迟动力学;碳循环;

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