Stable nitrogen isotope ratio in wood substrates and xylotrophic fungi in forest ecosystems of Western Siberia
It has been shown that wood substrates are the main source of nitrogen for xylotrophic fungi, which have almost the same isotopic signature as their substrate. This fact and a strong positive correlation in nitrogen isotope composition between the substrates and fungi provide evidence for a closed t...
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Published in | Russian journal of ecology Vol. 45; no. 6; pp. 539 - 546 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
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Moscow
Springer-Verlag
01.11.2014
Pleiades Publishing Springer Nature B.V |
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Abstract | It has been shown that wood substrates are the main source of nitrogen for xylotrophic fungi, which have almost the same isotopic signature as their substrate. This fact and a strong positive correlation in nitrogen isotope composition between the substrates and fungi provide evidence for a closed type of nitrogen turnover in the wood-fungus system that is based on retention and repeated utilization of this element. Its isotope composition in the fungi depends on that in the substrate, which is enriched in the heavy isotope in deciduous wood and in the light isotope in coniferous wood. The nitrogen isotope composition in the fungi and wood substrates does not depend on the degree of wood mineralization or climatic conditions, and δ¹⁵N is not an indicator of fungal physiological activity or wood decomposition rate but rather a marker of the isotopic composition of nitrogen sources for the fungi. |
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AbstractList | It has been shown that wood substrates are the main source of nitrogen for xylotrophic fungi, which have almost the same isotopic signature as their substrate. This fact and a strong positive correlation in nitrogen isotope composition between the substrates and fungi provide evidence for a closed type of nitrogen turnover in the wood-fungus system that is based on retention and repeated utilization of this element. Its isotope composition in the fungi depends on that in the substrate, which is enriched in the heavy isotope in deciduous wood and in the light isotope in coniferous wood. The nitrogen isotope composition in the fungi and wood substrates does not depend on the degree of wood mineralization or climatic conditions, and delta super(15)N is not an indicator of fungal physiological activity or wood decomposition rate but rather a marker of the isotopic composition of nitrogen sources for the fungi. It has been shown that wood substrates are the main source of nitrogen for xylotrophic fungi, which have almost the same isotopic signature as their substrate. This fact and a strong positive correlation in nitrogen isotope composition between the substrates and fungi provide evidence for a closed type of nitrogen turnover in the wood-fungus system that is based on retention and repeated utilization of this element. Its isotope composition in the fungi depends on that in the substrate, which is enriched in the heavy isotope in deciduous wood and in the light isotope in coniferous wood. The nitrogen isotope composition in the fungi and wood substrates does not depend on the degree of wood mineralization or climatic conditions, and δ¹⁵N is not an indicator of fungal physiological activity or wood decomposition rate but rather a marker of the isotopic composition of nitrogen sources for the fungi. It has been shown that wood substrates are the main source of nitrogen for xylotrophic fungi, which have almost the same isotopic signature as their substrate. This fact and a strong positive correlation in nitrogen isotope composition between the substrates and fungi provide evidence for a closed type of nitrogen turnover in the wood-fungus system that is based on retention and repeated utilization of this element. Its isotope composition in the fungi depends on that in the substrate, which is enriched in the heavy isotope in deciduous wood and in the light isotope in coniferous wood. The nitrogen isotope composition in the fungi and wood substrates does not depend on the degree of wood mineralization or climatic conditions, and δ 15 N is not an indicator of fungal physiological activity or wood decomposition rate but rather a marker of the isotopic composition of nitrogen sources for the fungi. It has been shown that wood substrates are the main source of nitrogen for xylotrophic fungi, which have almost the same isotopic signature as their substrate. This fact and a strong positive correlation in nitrogen isotope composition between the substrates and fungi provide evidence for a closed type of nitrogen turnover in the wood-fungus system that is based on retention and repeated utilization of this element. Its isotope composition in the fungi depends on that in the substrate, which is enriched in the heavy isotope in deciduous wood and in the light isotope in coniferous wood. The nitrogen isotope composition in the fungi and wood substrates does not depend on the degree of wood mineralization or climatic conditions, and δ^sup 15^N is not an indicator of fungal physiological activity or wood decomposition rate but rather a marker of the isotopic composition of nitrogen sources for the fungi.[PUBLICATION ABSTRACT] |
Author | Mukhin, V. A Ignat’ev, A. V Velivetskaya, T. A Voronin, P. Yu |
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Cites_doi | 10.1093/treephys/25.11.1437 10.1134/S1067413614010093 10.1046/j.1469-8137.2003.00838.x 10.1046/j.1469-8137.1999.00373.x 10.1046/j.1469-8137.1999.00508.x 10.1080/10256010701360256 10.1111/j.1461-0248.2008.01265.x 10.1017/CBO9780511550522.008 10.1134/S1067413607010043 10.1016/j.soilbio.2012.01.014 10.1134/S0012496613060082 10.1016/S1360-1385(01)01889-1 10.1016/S0169-5347(00)02098-X |
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Keywords | stable isotopes xylotrophic fungi Western Siberia nitrogen wood pool forest ecosystems |
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References | Watkinson, Bebber, Darrah, Gadd (CR20) 2006 Mukhin (CR12) 1993 Vanin (CR19) 1934 Tiunov (CR18) 2007 CR7 Gebauer, Taylor (CR3) 1999; 142 Mukhin, Voronin (CR13) 2007; 38 Mukhin, Voronin, Velivetskaya, Ignat’ev (CR15) 2014; 45 Mayor, Schuur, Henkel (CR9) 2009; 12 Mezentsev, Karnatsevich (CR11) 1969 Hobbie, Sánchez, Rygiewicz (CR4) 2012; 48 Kohzu, Miyajima, Tateishi (CR6) 2007; 43 Menyailo, Khangeit (CR10) 2006; 408 Robinson (CR16) 2001; 16 Evans (CR2) 2001; 6 Kohzu, Yoshioka, Ando (CR5) 1999; 144 Martinelli, Piccolo, Townsend (CR8) 1999; 46 Taylor, Fransson, Högberg (CR17) 2003; 159 Elhani, Guehl, Nys (CR1) 2005; 25 Mukhin, Voronin, Velivetskaya, Ignat’ev, Kuznetsov (CR14) 2013; 453 S Elhani (7485_CR1) 2005; 25 AFS Taylor (7485_CR17) 2003; 159 RD Evans (7485_CR2) 2001; 6 OV Menyailo (7485_CR10) 2006; 408 G Gebauer (7485_CR3) 1999; 142 7485_CR7 A Kohzu (7485_CR6) 2007; 43 JR Mayor (7485_CR9) 2009; 12 A Kohzu (7485_CR5) 1999; 144 EA Hobbie (7485_CR4) 2012; 48 VA Mukhin (7485_CR12) 1993 S Watkinson (7485_CR20) 2006 AV Tiunov (7485_CR18) 2007 SI Vanin (7485_CR19) 1934 VA Mukhin (7485_CR13) 2007; 38 VA Mukhin (7485_CR15) 2014; 45 VS Mezentsev (7485_CR11) 1969 D Robinson (7485_CR16) 2001; 16 VA Mukhin (7485_CR14) 2013; 453 LA Martinelli (7485_CR8) 1999; 46 |
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SubjectTerms | Biomedical and Life Sciences climatic factors decayed wood Ecology Environment forest ecosystems Forests Fungi Isotopes Life Sciences mineralization Nitrogen Russian Academy of Sciences Terrestrial ecosystems This Number of the Journal is Dedicated to the 70th Anniversary of Institute of Plant and Animal Ecology Ural Branch Wood |
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Title | Stable nitrogen isotope ratio in wood substrates and xylotrophic fungi in forest ecosystems of Western Siberia |
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