Soil microbial community, dissolved organic matter and nutrient cycling interactions change along an elevation gradient in subtropical China
To identify possible dominating processes involved in soil microbial community assembly, dissolved organic matter (DOM) and multi-nutrient cycling (MNC) interactions and contribute to understanding of climate change effects on these important cycles, we investigated the interaction of soil chemistry...
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Veröffentlicht in: | Journal of environmental management 2023-11, Vol.345, p.118793-118793, Article 118793 |
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creator | Wang, Shuzhen Heal, Kate V. Zhang, Qin Yu, Yuanchun Tigabu, Mulualem Huang, Shide Zhou, Chuifan |
description | To identify possible dominating processes involved in soil microbial community assembly, dissolved organic matter (DOM) and multi-nutrient cycling (MNC) interactions and contribute to understanding of climate change effects on these important cycles, we investigated the interaction of soil chemistry, DOM components and microbial communities in five vegetation zones - ranging from evergreen broad-leaved forest to alpine meadow - along an elevation gradient of 290–1960 m in the Wuyi Mountains, Fujian Province, China. Soil DOM composition and microbial community assembly were characterized using Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) and Illumina MiSeq high-throughput sequencing, respectively. Sloan's neutral model and the modified stochasticity ratio were used to infer community assembly processes. Key microbial drivers of the soil MNC index were identified from partial least squares path models. Our results showed that soil DOM composition is closely related to the vegetation types along an elevation gradient, the structure and composition of the microbial community, and soil nutrient status. Overall, values of the double bond equivalent (DBE), modified aromaticity index (AImod) increased, and H/C ratio and molecular lability boundary (MLBL) percentage decreased with elevation. Lignins/CRAM-like structures compounds dominated soil DOM in each vegetation type and its relative abundance decreased with elevation. Aliphatic/protein and lipids components also decreased, but the relative abundance of aromatic structures and tannin increased with elevation. The alpha diversity index of soil bacteria gradually decreased with elevation, with deterministic processes dominating the microbial community assembly in the highest elevation zone. Bacterial communities were conducive to the decomposition of labile degradable DOM compounds (H/C ≥ 1.5) at low elevation. In the cooler and wetter conditions at higher-elevation sites the relative abundance of potentially resistant soil DOM components (H/C |
doi_str_mv | 10.1016/j.jenvman.2023.118793 |
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[Display omitted]
•Relative abundance of DOM tannin and aromatic structures increased with elevation•Deterministic processes dominated microbial community assembly at high elevation•Bacteria promote decomposition of potentially labile DOM compounds at low elevation•Fungal community Shannon index and multi-nutrient cycling index negatively related</description><identifier>ISSN: 0301-4797</identifier><identifier>ISSN: 1095-8630</identifier><identifier>EISSN: 1095-8630</identifier><identifier>DOI: 10.1016/j.jenvman.2023.118793</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>alpine meadows ; altitude ; bioavailability ; carbon sequestration ; carbon sinks ; China ; climate change ; deciduous forests ; Dissolved organic matter (DOM) ; ecosystem management ; environmental management ; Environmental Sciences ; FT-ICR MS ; Labile components ; Markvetenskap ; mass spectrometry ; microbial communities ; Microbial community assembly ; Miljövetenskap ; organic matter ; Refractory components ; soil ; soil microorganisms ; Soil multi-nutrient cycling ; soil nutrients ; Soil Science ; species diversity</subject><ispartof>Journal of environmental management, 2023-11, Vol.345, p.118793-118793, Article 118793</ispartof><rights>2023 Elsevier Ltd</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c461t-f311bb472ca69fb5fa72fed2669514d62125b9af549a777d4a86e7a887987f783</citedby><cites>FETCH-LOGICAL-c461t-f311bb472ca69fb5fa72fed2669514d62125b9af549a777d4a86e7a887987f783</cites><orcidid>0000-0003-2471-1168 ; 0000-0002-1019-748X</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.jenvman.2023.118793$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,314,778,782,883,3539,27907,27908,45978</link.rule.ids><backlink>$$Uhttps://res.slu.se/id/publ/126423$$DView record from Swedish Publication Index$$Hfree_for_read</backlink></links><search><creatorcontrib>Wang, Shuzhen</creatorcontrib><creatorcontrib>Heal, Kate V.</creatorcontrib><creatorcontrib>Zhang, Qin</creatorcontrib><creatorcontrib>Yu, Yuanchun</creatorcontrib><creatorcontrib>Tigabu, Mulualem</creatorcontrib><creatorcontrib>Huang, Shide</creatorcontrib><creatorcontrib>Zhou, Chuifan</creatorcontrib><creatorcontrib>Sveriges lantbruksuniversitet</creatorcontrib><title>Soil microbial community, dissolved organic matter and nutrient cycling interactions change along an elevation gradient in subtropical China</title><title>Journal of environmental management</title><description>To identify possible dominating processes involved in soil microbial community assembly, dissolved organic matter (DOM) and multi-nutrient cycling (MNC) interactions and contribute to understanding of climate change effects on these important cycles, we investigated the interaction of soil chemistry, DOM components and microbial communities in five vegetation zones - ranging from evergreen broad-leaved forest to alpine meadow - along an elevation gradient of 290–1960 m in the Wuyi Mountains, Fujian Province, China. Soil DOM composition and microbial community assembly were characterized using Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) and Illumina MiSeq high-throughput sequencing, respectively. Sloan's neutral model and the modified stochasticity ratio were used to infer community assembly processes. Key microbial drivers of the soil MNC index were identified from partial least squares path models. Our results showed that soil DOM composition is closely related to the vegetation types along an elevation gradient, the structure and composition of the microbial community, and soil nutrient status. Overall, values of the double bond equivalent (DBE), modified aromaticity index (AImod) increased, and H/C ratio and molecular lability boundary (MLBL) percentage decreased with elevation. Lignins/CRAM-like structures compounds dominated soil DOM in each vegetation type and its relative abundance decreased with elevation. Aliphatic/protein and lipids components also decreased, but the relative abundance of aromatic structures and tannin increased with elevation. The alpha diversity index of soil bacteria gradually decreased with elevation, with deterministic processes dominating the microbial community assembly in the highest elevation zone. Bacterial communities were conducive to the decomposition of labile degradable DOM compounds (H/C ≥ 1.5) at low elevation. In the cooler and wetter conditions at higher-elevation sites the relative abundance of potentially resistant soil DOM components (H/C < 1.5) gradually increased. Microbial community diversity and composition were important predictors of potential soil nutrient cycling. Although higher elevation sites have higher nutrient cycling potential, soil DOM was assessed to be a more stable carbon store, with apparent lower lability and bioavailability than at lower elevation sites. Overall, this study increases understanding of the potential linkage between soil microbial community, multiple nutrient cycling and DOM fate in subtropical mountain ecosystems that can help predict the effect of climate change on soil carbon sequestration and thus inform ecosystem management.
[Display omitted]
•Relative abundance of DOM tannin and aromatic structures increased with elevation•Deterministic processes dominated microbial community assembly at high elevation•Bacteria promote decomposition of potentially labile DOM compounds at low elevation•Fungal community Shannon index and multi-nutrient cycling index negatively related</description><subject>alpine meadows</subject><subject>altitude</subject><subject>bioavailability</subject><subject>carbon sequestration</subject><subject>carbon sinks</subject><subject>China</subject><subject>climate change</subject><subject>deciduous forests</subject><subject>Dissolved organic matter (DOM)</subject><subject>ecosystem management</subject><subject>environmental management</subject><subject>Environmental Sciences</subject><subject>FT-ICR MS</subject><subject>Labile components</subject><subject>Markvetenskap</subject><subject>mass spectrometry</subject><subject>microbial communities</subject><subject>Microbial community assembly</subject><subject>Miljövetenskap</subject><subject>organic matter</subject><subject>Refractory components</subject><subject>soil</subject><subject>soil microorganisms</subject><subject>Soil multi-nutrient cycling</subject><subject>soil nutrients</subject><subject>Soil Science</subject><subject>species diversity</subject><issn>0301-4797</issn><issn>1095-8630</issn><issn>1095-8630</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNqFkc2O1DAQhCMEEsPCIyD5yIEE23Fi54TQiD9ppT0AZ6vjdGY9cuzBdgbNO_DQOMxqr3vqQ9XX3aqqqreMNoyy_sOxOaI_L-AbTnnbMKbk0D6rdowOXa36lj6vdrSlrBZykC-rVykdKaUtZ3JX_f0RrCOLNTGMFhwxYVlWb_PlPZlsSsGdcSIhHsBbQxbIGSMBPxG_5mjRZ2Iuxll_INYXCUy2wSdi7sEfkIALRQFP0OEZNokcIkz_OetJWsccw8macnd_bz28rl7M4BK-eZg31a8vn3_uv9W3d1-_7z_d1kb0LNdzy9g4CskN9MM8djNIPuPE-37omJh6zng3DjB3YgAp5SRA9ShBlViUnKVqb6rmujf9wdM66lO0C8SLDmB1cusIcRs6oWa8F7wtwLsrcIrh94op68Umg86Bx7Am3VJBBVe0Y09aueqkElyozdpdrSX8lCLOj48wqrdm9VE_NKu3ZvW12cJ9vHJYMjpbLN-akqnByUY0WU_BPrHhHwgVsqU</recordid><startdate>20231101</startdate><enddate>20231101</enddate><creator>Wang, Shuzhen</creator><creator>Heal, Kate V.</creator><creator>Zhang, Qin</creator><creator>Yu, Yuanchun</creator><creator>Tigabu, Mulualem</creator><creator>Huang, Shide</creator><creator>Zhou, Chuifan</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope><scope>7S9</scope><scope>L.6</scope><scope>ADTPV</scope><scope>AOWAS</scope><orcidid>https://orcid.org/0000-0003-2471-1168</orcidid><orcidid>https://orcid.org/0000-0002-1019-748X</orcidid></search><sort><creationdate>20231101</creationdate><title>Soil microbial community, dissolved organic matter and nutrient cycling interactions change along an elevation gradient in subtropical China</title><author>Wang, Shuzhen ; Heal, Kate V. ; Zhang, Qin ; Yu, Yuanchun ; Tigabu, Mulualem ; Huang, Shide ; Zhou, Chuifan</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c461t-f311bb472ca69fb5fa72fed2669514d62125b9af549a777d4a86e7a887987f783</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>alpine meadows</topic><topic>altitude</topic><topic>bioavailability</topic><topic>carbon sequestration</topic><topic>carbon sinks</topic><topic>China</topic><topic>climate change</topic><topic>deciduous forests</topic><topic>Dissolved organic matter (DOM)</topic><topic>ecosystem management</topic><topic>environmental management</topic><topic>Environmental Sciences</topic><topic>FT-ICR MS</topic><topic>Labile components</topic><topic>Markvetenskap</topic><topic>mass spectrometry</topic><topic>microbial communities</topic><topic>Microbial community assembly</topic><topic>Miljövetenskap</topic><topic>organic matter</topic><topic>Refractory components</topic><topic>soil</topic><topic>soil microorganisms</topic><topic>Soil multi-nutrient cycling</topic><topic>soil nutrients</topic><topic>Soil Science</topic><topic>species diversity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Shuzhen</creatorcontrib><creatorcontrib>Heal, Kate V.</creatorcontrib><creatorcontrib>Zhang, Qin</creatorcontrib><creatorcontrib>Yu, Yuanchun</creatorcontrib><creatorcontrib>Tigabu, Mulualem</creatorcontrib><creatorcontrib>Huang, Shide</creatorcontrib><creatorcontrib>Zhou, Chuifan</creatorcontrib><creatorcontrib>Sveriges lantbruksuniversitet</creatorcontrib><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><collection>AGRICOLA</collection><collection>AGRICOLA - Academic</collection><collection>SwePub</collection><collection>SwePub Articles</collection><jtitle>Journal of environmental management</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Shuzhen</au><au>Heal, Kate V.</au><au>Zhang, Qin</au><au>Yu, Yuanchun</au><au>Tigabu, Mulualem</au><au>Huang, Shide</au><au>Zhou, Chuifan</au><aucorp>Sveriges lantbruksuniversitet</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Soil microbial community, dissolved organic matter and nutrient cycling interactions change along an elevation gradient in subtropical China</atitle><jtitle>Journal of environmental management</jtitle><date>2023-11-01</date><risdate>2023</risdate><volume>345</volume><spage>118793</spage><epage>118793</epage><pages>118793-118793</pages><artnum>118793</artnum><issn>0301-4797</issn><issn>1095-8630</issn><eissn>1095-8630</eissn><abstract>To identify possible dominating processes involved in soil microbial community assembly, dissolved organic matter (DOM) and multi-nutrient cycling (MNC) interactions and contribute to understanding of climate change effects on these important cycles, we investigated the interaction of soil chemistry, DOM components and microbial communities in five vegetation zones - ranging from evergreen broad-leaved forest to alpine meadow - along an elevation gradient of 290–1960 m in the Wuyi Mountains, Fujian Province, China. Soil DOM composition and microbial community assembly were characterized using Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) and Illumina MiSeq high-throughput sequencing, respectively. Sloan's neutral model and the modified stochasticity ratio were used to infer community assembly processes. Key microbial drivers of the soil MNC index were identified from partial least squares path models. Our results showed that soil DOM composition is closely related to the vegetation types along an elevation gradient, the structure and composition of the microbial community, and soil nutrient status. Overall, values of the double bond equivalent (DBE), modified aromaticity index (AImod) increased, and H/C ratio and molecular lability boundary (MLBL) percentage decreased with elevation. Lignins/CRAM-like structures compounds dominated soil DOM in each vegetation type and its relative abundance decreased with elevation. Aliphatic/protein and lipids components also decreased, but the relative abundance of aromatic structures and tannin increased with elevation. The alpha diversity index of soil bacteria gradually decreased with elevation, with deterministic processes dominating the microbial community assembly in the highest elevation zone. Bacterial communities were conducive to the decomposition of labile degradable DOM compounds (H/C ≥ 1.5) at low elevation. In the cooler and wetter conditions at higher-elevation sites the relative abundance of potentially resistant soil DOM components (H/C < 1.5) gradually increased. Microbial community diversity and composition were important predictors of potential soil nutrient cycling. Although higher elevation sites have higher nutrient cycling potential, soil DOM was assessed to be a more stable carbon store, with apparent lower lability and bioavailability than at lower elevation sites. Overall, this study increases understanding of the potential linkage between soil microbial community, multiple nutrient cycling and DOM fate in subtropical mountain ecosystems that can help predict the effect of climate change on soil carbon sequestration and thus inform ecosystem management.
[Display omitted]
•Relative abundance of DOM tannin and aromatic structures increased with elevation•Deterministic processes dominated microbial community assembly at high elevation•Bacteria promote decomposition of potentially labile DOM compounds at low elevation•Fungal community Shannon index and multi-nutrient cycling index negatively related</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.jenvman.2023.118793</doi><tpages>1</tpages><orcidid>https://orcid.org/0000-0003-2471-1168</orcidid><orcidid>https://orcid.org/0000-0002-1019-748X</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | alpine meadows altitude bioavailability carbon sequestration carbon sinks China climate change deciduous forests Dissolved organic matter (DOM) ecosystem management environmental management Environmental Sciences FT-ICR MS Labile components Markvetenskap mass spectrometry microbial communities Microbial community assembly Miljövetenskap organic matter Refractory components soil soil microorganisms Soil multi-nutrient cycling soil nutrients Soil Science species diversity |
title | Soil microbial community, dissolved organic matter and nutrient cycling interactions change along an elevation gradient in subtropical China |
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