Comparison of seasonal soil microbial process in snow-covered temperate ecosystems of northern China.

More than half of the earth's terrestrial surface currently experiences seasonal snow cover and soil frost. Winter compositional and functional investigations in soil microbial community are frequently conducted in alpine tundra and boreal forest ecosystems. However, little information on winte...

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Autores principales: Xinyue Zhang, Wei Wang, Weile Chen, Naili Zhang, Hui Zeng
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Publicado: Public Library of Science (PLoS) 2014
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Acceso en línea:https://doaj.org/article/6915ed5deda64a33b799e97aa82e9dde
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spelling oai:doaj.org-article:6915ed5deda64a33b799e97aa82e9dde2021-11-18T08:26:10ZComparison of seasonal soil microbial process in snow-covered temperate ecosystems of northern China.1932-620310.1371/journal.pone.0092985https://doaj.org/article/6915ed5deda64a33b799e97aa82e9dde2014-01-01T00:00:00Zhttps://www.ncbi.nlm.nih.gov/pmc/articles/pmid/24667929/pdf/?tool=EBIhttps://doaj.org/toc/1932-6203More than half of the earth's terrestrial surface currently experiences seasonal snow cover and soil frost. Winter compositional and functional investigations in soil microbial community are frequently conducted in alpine tundra and boreal forest ecosystems. However, little information on winter microbial biogeochemistry is known from seasonally snow-covered temperate ecosystems. As decomposer microbes may differ in their ability/strategy to efficiently use soil organic carbon (SOC) within different phases of the year, understanding seasonal microbial process will increase our knowledge of biogeochemical cycling from the aspect of decomposition rates and corresponding nutrient dynamics. In this study, we measured soil microbial biomass, community composition and potential SOC mineralization rates in winter and summer, from six temperate ecosystems in northern China. Our results showed a clear pattern of increased microbial biomass C to nitrogen (N) ratio in most winter soils. Concurrently, a shift in soil microbial community composition occurred with higher fungal to bacterial biomass ratio and gram negative (G-) to gram positive (G+) bacterial biomass ratio in winter than in summer. Furthermore, potential SOC mineralization rate was higher in winter than in summer. Our study demonstrated a distinct transition of microbial community structure and function from winter to summer in temperate snow-covered ecosystems. Microbial N immobilization in winter may not be the major contributor for plant growth in the following spring.Xinyue ZhangWei WangWeile ChenNaili ZhangHui ZengPublic Library of Science (PLoS)articleMedicineRScienceQENPLoS ONE, Vol 9, Iss 3, p e92985 (2014)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Xinyue Zhang
Wei Wang
Weile Chen
Naili Zhang
Hui Zeng
Comparison of seasonal soil microbial process in snow-covered temperate ecosystems of northern China.
description More than half of the earth's terrestrial surface currently experiences seasonal snow cover and soil frost. Winter compositional and functional investigations in soil microbial community are frequently conducted in alpine tundra and boreal forest ecosystems. However, little information on winter microbial biogeochemistry is known from seasonally snow-covered temperate ecosystems. As decomposer microbes may differ in their ability/strategy to efficiently use soil organic carbon (SOC) within different phases of the year, understanding seasonal microbial process will increase our knowledge of biogeochemical cycling from the aspect of decomposition rates and corresponding nutrient dynamics. In this study, we measured soil microbial biomass, community composition and potential SOC mineralization rates in winter and summer, from six temperate ecosystems in northern China. Our results showed a clear pattern of increased microbial biomass C to nitrogen (N) ratio in most winter soils. Concurrently, a shift in soil microbial community composition occurred with higher fungal to bacterial biomass ratio and gram negative (G-) to gram positive (G+) bacterial biomass ratio in winter than in summer. Furthermore, potential SOC mineralization rate was higher in winter than in summer. Our study demonstrated a distinct transition of microbial community structure and function from winter to summer in temperate snow-covered ecosystems. Microbial N immobilization in winter may not be the major contributor for plant growth in the following spring.
format article
author Xinyue Zhang
Wei Wang
Weile Chen
Naili Zhang
Hui Zeng
author_facet Xinyue Zhang
Wei Wang
Weile Chen
Naili Zhang
Hui Zeng
author_sort Xinyue Zhang
title Comparison of seasonal soil microbial process in snow-covered temperate ecosystems of northern China.
title_short Comparison of seasonal soil microbial process in snow-covered temperate ecosystems of northern China.
title_full Comparison of seasonal soil microbial process in snow-covered temperate ecosystems of northern China.
title_fullStr Comparison of seasonal soil microbial process in snow-covered temperate ecosystems of northern China.
title_full_unstemmed Comparison of seasonal soil microbial process in snow-covered temperate ecosystems of northern China.
title_sort comparison of seasonal soil microbial process in snow-covered temperate ecosystems of northern china.
publisher Public Library of Science (PLoS)
publishDate 2014
url https://doaj.org/article/6915ed5deda64a33b799e97aa82e9dde
work_keys_str_mv AT xinyuezhang comparisonofseasonalsoilmicrobialprocessinsnowcoveredtemperateecosystemsofnorthernchina
AT weiwang comparisonofseasonalsoilmicrobialprocessinsnowcoveredtemperateecosystemsofnorthernchina
AT weilechen comparisonofseasonalsoilmicrobialprocessinsnowcoveredtemperateecosystemsofnorthernchina
AT nailizhang comparisonofseasonalsoilmicrobialprocessinsnowcoveredtemperateecosystemsofnorthernchina
AT huizeng comparisonofseasonalsoilmicrobialprocessinsnowcoveredtemperateecosystemsofnorthernchina
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