Nitrogen deposition and soil carbon content affect nitrogen mineralization during primary succession in acid inland drift sand vegetation

Background and aims Two inland dunes in the Netherlands receiving low (24) and high (41 kg N ha⁻¹ yr⁻¹) nitrogen (N) deposition were compared for N dynamics and microbial activity to investigate the potential effect of N on succession rate of the vegetation and loss of pioneer habitats. Methods Prim...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Plant and soil 2013-03, Vol.364 (1/2), p.219-228
Hauptverfasser: Sparrius, Laurens B., Kooijman, Annemieke M.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 228
container_issue 1/2
container_start_page 219
container_title Plant and soil
container_volume 364
creator Sparrius, Laurens B.
Kooijman, Annemieke M.
description Background and aims Two inland dunes in the Netherlands receiving low (24) and high (41 kg N ha⁻¹ yr⁻¹) nitrogen (N) deposition were compared for N dynamics and microbial activity to investigate the potential effect of N on succession rate of the vegetation and loss of pioneer habitats. Methods Primary succession stages were sampled, including bare sand, and vegetation dominated by Polytrichum piliferum, Campylopus introflexus, lichens and grasses respectively, representing a series of vegetation types in undisturbed drift sand sites with succession starting on bare sand containing virtually no organic matter. Microbial characteristics and potential N mineralization were analysed in a laboratory experiment. Results Organic matter accumulated during succession, resulting in a lower pH and in higher microbial biomass (bacteria and fungi), respiration and net N mineralization. The increase in respiration and N mineralization was largely due to the development of an ectorganic layer in the middle stages of succession. The observed effects of N deposition were (1) decrease of microbial biomass, (2) higher net N mineralization per m², (3) higher levels of free nitrogen in the soil, and (4) a higher microbial N:P ratio. Conclusions Elevated N deposition leads to higher N availability which may cause accelerated succession.
doi_str_mv 10.1007/s11104-012-1351-z
format Article
fullrecord <record><control><sourceid>gale_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_1291611912</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A375816210</galeid><jstor_id>42953453</jstor_id><sourcerecordid>A375816210</sourcerecordid><originalsourceid>FETCH-LOGICAL-c483t-895b5c1b738be96c55efddea2fd0b6211e5f965d1d47328e72d1fc8a99ab7ccc3</originalsourceid><addsrcrecordid>eNp9kc2KFDEUhYMo2LY-gAuhQAQ3NeYmlarKchj8g0E3Cu5CKrlp0lQnbZIW7DfwrU1NtYO4kCySm5zvcMgh5DnQK6B0eJMBgHYtBdYCF9CeH5ANiIG3gvL-IdlQyllLB_ntMXmS854uM_Qb8uuTLynuMDQWjzH74mNodLBNjn5ujE5TnU0MBUNptHNoShP-IAcfMOnZn_UdZk_Jh11zTP6g088mn4zBnJcXXz2Nt3WfF2-bvCtNXo4_cIflDn9KHjk9Z3x22bfk67u3X24-tLef33-8ub5tTTfy0o5STMLANPBxQtkbIdBZi5o5S6eeAaBwshcWbDdwNuLALDgzain1NBhj-Ja8Xn2PKX4_YS7q4LPBuSbDeMoKmIQeQAKr0pf_SPfxlEJNV1Wj4IwKCVV1tap2ekblg4slaVOXxYOvX4fO1_trPogRakBaAVgBk2LOCZ26fJkCqpY21dqmqm2qpU11rsyrSxSdjZ5d0sH4fA-yaj52NdKWsFWXj0sZmP6K_B_zFyu0zyWme9OOScE7wflvczi8Wg</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1285320591</pqid></control><display><type>article</type><title>Nitrogen deposition and soil carbon content affect nitrogen mineralization during primary succession in acid inland drift sand vegetation</title><source>JSTOR Archive Collection A-Z Listing</source><source>SpringerLink Journals - AutoHoldings</source><creator>Sparrius, Laurens B. ; Kooijman, Annemieke M.</creator><creatorcontrib>Sparrius, Laurens B. ; Kooijman, Annemieke M.</creatorcontrib><description>Background and aims Two inland dunes in the Netherlands receiving low (24) and high (41 kg N ha⁻¹ yr⁻¹) nitrogen (N) deposition were compared for N dynamics and microbial activity to investigate the potential effect of N on succession rate of the vegetation and loss of pioneer habitats. Methods Primary succession stages were sampled, including bare sand, and vegetation dominated by Polytrichum piliferum, Campylopus introflexus, lichens and grasses respectively, representing a series of vegetation types in undisturbed drift sand sites with succession starting on bare sand containing virtually no organic matter. Microbial characteristics and potential N mineralization were analysed in a laboratory experiment. Results Organic matter accumulated during succession, resulting in a lower pH and in higher microbial biomass (bacteria and fungi), respiration and net N mineralization. The increase in respiration and N mineralization was largely due to the development of an ectorganic layer in the middle stages of succession. The observed effects of N deposition were (1) decrease of microbial biomass, (2) higher net N mineralization per m², (3) higher levels of free nitrogen in the soil, and (4) a higher microbial N:P ratio. Conclusions Elevated N deposition leads to higher N availability which may cause accelerated succession.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1007/s11104-012-1351-z</identifier><identifier>CODEN: PLSOA2</identifier><language>eng</language><publisher>Dordrecht: Springer</publisher><subject>Agronomy. Soil science and plant productions ; Animal, plant and microbial ecology ; Biochemistry and biology ; Biogeochemistry ; Biological and medical sciences ; Biomedical and Life Sciences ; Campylopus ; Carbon content ; Chemical, physicochemical, biochemical and biological properties ; Ecological succession ; Ecology ; Forest soils ; Fundamental and applied biological sciences. Psychology ; General agronomy. Plant production ; Lichens ; Life Sciences ; Microbial activity ; Microbiology ; Mineral soils ; Mineralization ; Nitrogen ; Organic matter ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; Plant Physiology ; Plant populations ; Plant Sciences ; Plants ; Polytrichum piliferum ; Regular Article ; Respiration ; Sand ; Sand &amp; gravel ; Soil air ; Soil microbiology ; Soil microorganisms ; Soil organic matter ; Soil science ; Soil Science &amp; Conservation ; Soil-plant relationships. Soil fertility ; Soil-plant relationships. Soil fertility. Fertilization. Amendments ; Soils ; Vegetation</subject><ispartof>Plant and soil, 2013-03, Vol.364 (1/2), p.219-228</ispartof><rights>2013 Springer</rights><rights>The Author(s) 2012</rights><rights>2014 INIST-CNRS</rights><rights>COPYRIGHT 2013 Springer</rights><rights>Springer Science+Business Media Dordrecht 2013</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c483t-895b5c1b738be96c55efddea2fd0b6211e5f965d1d47328e72d1fc8a99ab7ccc3</citedby><cites>FETCH-LOGICAL-c483t-895b5c1b738be96c55efddea2fd0b6211e5f965d1d47328e72d1fc8a99ab7ccc3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/42953453$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/42953453$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,27924,27925,41488,42557,51319,58017,58250</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=27588485$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Sparrius, Laurens B.</creatorcontrib><creatorcontrib>Kooijman, Annemieke M.</creatorcontrib><title>Nitrogen deposition and soil carbon content affect nitrogen mineralization during primary succession in acid inland drift sand vegetation</title><title>Plant and soil</title><addtitle>Plant Soil</addtitle><description>Background and aims Two inland dunes in the Netherlands receiving low (24) and high (41 kg N ha⁻¹ yr⁻¹) nitrogen (N) deposition were compared for N dynamics and microbial activity to investigate the potential effect of N on succession rate of the vegetation and loss of pioneer habitats. Methods Primary succession stages were sampled, including bare sand, and vegetation dominated by Polytrichum piliferum, Campylopus introflexus, lichens and grasses respectively, representing a series of vegetation types in undisturbed drift sand sites with succession starting on bare sand containing virtually no organic matter. Microbial characteristics and potential N mineralization were analysed in a laboratory experiment. Results Organic matter accumulated during succession, resulting in a lower pH and in higher microbial biomass (bacteria and fungi), respiration and net N mineralization. The increase in respiration and N mineralization was largely due to the development of an ectorganic layer in the middle stages of succession. The observed effects of N deposition were (1) decrease of microbial biomass, (2) higher net N mineralization per m², (3) higher levels of free nitrogen in the soil, and (4) a higher microbial N:P ratio. Conclusions Elevated N deposition leads to higher N availability which may cause accelerated succession.</description><subject>Agronomy. Soil science and plant productions</subject><subject>Animal, plant and microbial ecology</subject><subject>Biochemistry and biology</subject><subject>Biogeochemistry</subject><subject>Biological and medical sciences</subject><subject>Biomedical and Life Sciences</subject><subject>Campylopus</subject><subject>Carbon content</subject><subject>Chemical, physicochemical, biochemical and biological properties</subject><subject>Ecological succession</subject><subject>Ecology</subject><subject>Forest soils</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General agronomy. Plant production</subject><subject>Lichens</subject><subject>Life Sciences</subject><subject>Microbial activity</subject><subject>Microbiology</subject><subject>Mineral soils</subject><subject>Mineralization</subject><subject>Nitrogen</subject><subject>Organic matter</subject><subject>Physics, chemistry, biochemistry and biology of agricultural and forest soils</subject><subject>Plant Physiology</subject><subject>Plant populations</subject><subject>Plant Sciences</subject><subject>Plants</subject><subject>Polytrichum piliferum</subject><subject>Regular Article</subject><subject>Respiration</subject><subject>Sand</subject><subject>Sand &amp; gravel</subject><subject>Soil air</subject><subject>Soil microbiology</subject><subject>Soil microorganisms</subject><subject>Soil organic matter</subject><subject>Soil science</subject><subject>Soil Science &amp; Conservation</subject><subject>Soil-plant relationships. Soil fertility</subject><subject>Soil-plant relationships. Soil fertility. Fertilization. Amendments</subject><subject>Soils</subject><subject>Vegetation</subject><issn>0032-079X</issn><issn>1573-5036</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kc2KFDEUhYMo2LY-gAuhQAQ3NeYmlarKchj8g0E3Cu5CKrlp0lQnbZIW7DfwrU1NtYO4kCySm5zvcMgh5DnQK6B0eJMBgHYtBdYCF9CeH5ANiIG3gvL-IdlQyllLB_ntMXmS854uM_Qb8uuTLynuMDQWjzH74mNodLBNjn5ujE5TnU0MBUNptHNoShP-IAcfMOnZn_UdZk_Jh11zTP6g088mn4zBnJcXXz2Nt3WfF2-bvCtNXo4_cIflDn9KHjk9Z3x22bfk67u3X24-tLef33-8ub5tTTfy0o5STMLANPBxQtkbIdBZi5o5S6eeAaBwshcWbDdwNuLALDgzain1NBhj-Ja8Xn2PKX4_YS7q4LPBuSbDeMoKmIQeQAKr0pf_SPfxlEJNV1Wj4IwKCVV1tap2ekblg4slaVOXxYOvX4fO1_trPogRakBaAVgBk2LOCZ26fJkCqpY21dqmqm2qpU11rsyrSxSdjZ5d0sH4fA-yaj52NdKWsFWXj0sZmP6K_B_zFyu0zyWme9OOScE7wflvczi8Wg</recordid><startdate>20130301</startdate><enddate>20130301</enddate><creator>Sparrius, Laurens B.</creator><creator>Kooijman, Annemieke M.</creator><general>Springer</general><general>Springer Netherlands</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7SN</scope><scope>7ST</scope><scope>7T7</scope><scope>7X2</scope><scope>88A</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>LK8</scope><scope>M0K</scope><scope>M7P</scope><scope>P64</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>RC3</scope><scope>SOI</scope><scope>7U6</scope><scope>M7N</scope></search><sort><creationdate>20130301</creationdate><title>Nitrogen deposition and soil carbon content affect nitrogen mineralization during primary succession in acid inland drift sand vegetation</title><author>Sparrius, Laurens B. ; Kooijman, Annemieke M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c483t-895b5c1b738be96c55efddea2fd0b6211e5f965d1d47328e72d1fc8a99ab7ccc3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Agronomy. Soil science and plant productions</topic><topic>Animal, plant and microbial ecology</topic><topic>Biochemistry and biology</topic><topic>Biogeochemistry</topic><topic>Biological and medical sciences</topic><topic>Biomedical and Life Sciences</topic><topic>Campylopus</topic><topic>Carbon content</topic><topic>Chemical, physicochemical, biochemical and biological properties</topic><topic>Ecological succession</topic><topic>Ecology</topic><topic>Forest soils</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>General agronomy. Plant production</topic><topic>Lichens</topic><topic>Life Sciences</topic><topic>Microbial activity</topic><topic>Microbiology</topic><topic>Mineral soils</topic><topic>Mineralization</topic><topic>Nitrogen</topic><topic>Organic matter</topic><topic>Physics, chemistry, biochemistry and biology of agricultural and forest soils</topic><topic>Plant Physiology</topic><topic>Plant populations</topic><topic>Plant Sciences</topic><topic>Plants</topic><topic>Polytrichum piliferum</topic><topic>Regular Article</topic><topic>Respiration</topic><topic>Sand</topic><topic>Sand &amp; gravel</topic><topic>Soil air</topic><topic>Soil microbiology</topic><topic>Soil microorganisms</topic><topic>Soil organic matter</topic><topic>Soil science</topic><topic>Soil Science &amp; Conservation</topic><topic>Soil-plant relationships. Soil fertility</topic><topic>Soil-plant relationships. Soil fertility. Fertilization. Amendments</topic><topic>Soils</topic><topic>Vegetation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sparrius, Laurens B.</creatorcontrib><creatorcontrib>Kooijman, Annemieke M.</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Agricultural Science Collection</collection><collection>Biology Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>Proquest Central</collection><collection>Natural Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Biological Science Collection</collection><collection>Agricultural Science Database</collection><collection>Biological Science Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Genetics Abstracts</collection><collection>Environment Abstracts</collection><collection>Sustainability Science Abstracts</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><jtitle>Plant and soil</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sparrius, Laurens B.</au><au>Kooijman, Annemieke M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Nitrogen deposition and soil carbon content affect nitrogen mineralization during primary succession in acid inland drift sand vegetation</atitle><jtitle>Plant and soil</jtitle><stitle>Plant Soil</stitle><date>2013-03-01</date><risdate>2013</risdate><volume>364</volume><issue>1/2</issue><spage>219</spage><epage>228</epage><pages>219-228</pages><issn>0032-079X</issn><eissn>1573-5036</eissn><coden>PLSOA2</coden><abstract>Background and aims Two inland dunes in the Netherlands receiving low (24) and high (41 kg N ha⁻¹ yr⁻¹) nitrogen (N) deposition were compared for N dynamics and microbial activity to investigate the potential effect of N on succession rate of the vegetation and loss of pioneer habitats. Methods Primary succession stages were sampled, including bare sand, and vegetation dominated by Polytrichum piliferum, Campylopus introflexus, lichens and grasses respectively, representing a series of vegetation types in undisturbed drift sand sites with succession starting on bare sand containing virtually no organic matter. Microbial characteristics and potential N mineralization were analysed in a laboratory experiment. Results Organic matter accumulated during succession, resulting in a lower pH and in higher microbial biomass (bacteria and fungi), respiration and net N mineralization. The increase in respiration and N mineralization was largely due to the development of an ectorganic layer in the middle stages of succession. The observed effects of N deposition were (1) decrease of microbial biomass, (2) higher net N mineralization per m², (3) higher levels of free nitrogen in the soil, and (4) a higher microbial N:P ratio. Conclusions Elevated N deposition leads to higher N availability which may cause accelerated succession.</abstract><cop>Dordrecht</cop><pub>Springer</pub><doi>10.1007/s11104-012-1351-z</doi><tpages>10</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0032-079X
ispartof Plant and soil, 2013-03, Vol.364 (1/2), p.219-228
issn 0032-079X
1573-5036
language eng
recordid cdi_proquest_miscellaneous_1291611912
source JSTOR Archive Collection A-Z Listing; SpringerLink Journals - AutoHoldings
subjects Agronomy. Soil science and plant productions
Animal, plant and microbial ecology
Biochemistry and biology
Biogeochemistry
Biological and medical sciences
Biomedical and Life Sciences
Campylopus
Carbon content
Chemical, physicochemical, biochemical and biological properties
Ecological succession
Ecology
Forest soils
Fundamental and applied biological sciences. Psychology
General agronomy. Plant production
Lichens
Life Sciences
Microbial activity
Microbiology
Mineral soils
Mineralization
Nitrogen
Organic matter
Physics, chemistry, biochemistry and biology of agricultural and forest soils
Plant Physiology
Plant populations
Plant Sciences
Plants
Polytrichum piliferum
Regular Article
Respiration
Sand
Sand & gravel
Soil air
Soil microbiology
Soil microorganisms
Soil organic matter
Soil science
Soil Science & Conservation
Soil-plant relationships. Soil fertility
Soil-plant relationships. Soil fertility. Fertilization. Amendments
Soils
Vegetation
title Nitrogen deposition and soil carbon content affect nitrogen mineralization during primary succession in acid inland drift sand vegetation
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-24T18%3A07%3A11IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Nitrogen%20deposition%20and%20soil%20carbon%20content%20affect%20nitrogen%20mineralization%20during%20primary%20succession%20in%20acid%20inland%20drift%20sand%20vegetation&rft.jtitle=Plant%20and%20soil&rft.au=Sparrius,%20Laurens%20B.&rft.date=2013-03-01&rft.volume=364&rft.issue=1/2&rft.spage=219&rft.epage=228&rft.pages=219-228&rft.issn=0032-079X&rft.eissn=1573-5036&rft.coden=PLSOA2&rft_id=info:doi/10.1007/s11104-012-1351-z&rft_dat=%3Cgale_proqu%3EA375816210%3C/gale_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1285320591&rft_id=info:pmid/&rft_galeid=A375816210&rft_jstor_id=42953453&rfr_iscdi=true