Edaphic influences on a New Zealand ultramafic ('serpentine') flora: a statistical approach
Ultramafic ("serpentine") soils from and adjacent to the Dun Mountain Ophiolitic Belt, South Island, New Zealand were analysed for 11 elements in order to establish to what degree edaphic factors influenced the character of the overlying vegetation. Using principal components analysis with...
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| Veröffentlicht in: | Plant and soil 1997-01, Vol.188 (1), p.11-20 |
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| creator | Robinson, B.H. (Massey Univ., Palmerston North (New Zealand). Dept. of Soil Science) Brooks, R.R Kirkman, J.H Gregg, P.E.H Varela Alvarez, H |
| description | Ultramafic ("serpentine") soils from and adjacent to the Dun Mountain Ophiolitic Belt, South Island, New Zealand were analysed for 11 elements in order to establish to what degree edaphic factors influenced the character of the overlying vegetation. Using principal components analysis with a mutual plot of the first two principal components, involving the total elemental concentrations in the soils, it was possible to divide the soils into 6 virtually nonoverlapping fields, each of which represented a specific vegetation community. Component 1 was essentially an "ultramafic plot" with heavy loadings from the elements chromium, cobalt, iron, magnesium, manganese, and nickel. Component 2 was a "non ultramafic" plot with heavy loadings from aluminium, copper and zinc. For elements extracted from the soils at pH 5.9, discrimination was somewhat poorer but confirmed the great importance of magnesium and nickel as controlling elements for the serpentine vegetation. It was concluded that the results indicated the overriding importance of edaphic factors in controlling the serpentine vegetation. |
| doi_str_mv | 10.1023/A:1004208230037 |
| format | Article |
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(Massey Univ., Palmerston North (New Zealand). Dept. of Soil Science) ; Brooks, R.R ; Kirkman, J.H ; Gregg, P.E.H ; Varela Alvarez, H</creator><creatorcontrib>Robinson, B.H. (Massey Univ., Palmerston North (New Zealand). Dept. of Soil Science) ; Brooks, R.R ; Kirkman, J.H ; Gregg, P.E.H ; Varela Alvarez, H</creatorcontrib><description>Ultramafic ("serpentine") soils from and adjacent to the Dun Mountain Ophiolitic Belt, South Island, New Zealand were analysed for 11 elements in order to establish to what degree edaphic factors influenced the character of the overlying vegetation. Using principal components analysis with a mutual plot of the first two principal components, involving the total elemental concentrations in the soils, it was possible to divide the soils into 6 virtually nonoverlapping fields, each of which represented a specific vegetation community. Component 1 was essentially an "ultramafic plot" with heavy loadings from the elements chromium, cobalt, iron, magnesium, manganese, and nickel. Component 2 was a "non ultramafic" plot with heavy loadings from aluminium, copper and zinc. For elements extracted from the soils at pH 5.9, discrimination was somewhat poorer but confirmed the great importance of magnesium and nickel as controlling elements for the serpentine vegetation. It was concluded that the results indicated the overriding importance of edaphic factors in controlling the serpentine vegetation.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1023/A:1004208230037</identifier><identifier>CODEN: PLSOA2</identifier><language>eng</language><publisher>Dordrecht: Kluwer Academic Publishers</publisher><subject>Acid soils ; Aluminum ; Animal and plant ecology ; Animal, plant and microbial ecology ; Autoecology ; Biological and medical sciences ; BOTANICAL COMPOSITION ; CHIMIE DU SOL ; Chromium ; Cobalt ; COMPOSICION BOTANICA ; COMPOSITION BOTANIQUE ; EDAPHIC FACTORS ; FACTEUR EDAPHIQUE ; FACTORES EDAFICOS ; Flora ; Forest soils ; Fundamental and applied biological sciences. Psychology ; Magnesium ; Manganese ; METHODE STATISTIQUE ; METODOS ESTADISTICOS ; Mountain soils ; NEW ZEALAND ; Nickel ; NOUVELLE ZELANDE ; NUEVA ZELANDIA ; PLANT SOIL RELATIONS ; Plants ; Plants and fungi ; Principal components analysis ; QUIMICA DEL SUELO ; RELACIONES PLANTA SUELO ; RELATION PLANTE SOL ; Sedimentary soils ; Serpentine ; SERPENTINE SOILS ; SOIL CHEMISTRY ; SOL DE SERPENTINE ; STATISTICAL METHODS ; SUELO DE SERPENTINA ; VEGETACION ; VEGETATION</subject><ispartof>Plant and soil, 1997-01, Vol.188 (1), p.11-20</ispartof><rights>1997 Kluwer Academic Publishers</rights><rights>1997 INIST-CNRS</rights><rights>Kluwer Academic Publishers 1997</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a386t-b18756cd0783a490ec09a841602e0055234f3e49f70819dbd9a09b90bc5ef8053</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/42949372$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/42949372$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,4010,27900,27901,27902,57992,58225</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=2780943$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Robinson, B.H. (Massey Univ., Palmerston North (New Zealand). Dept. of Soil Science)</creatorcontrib><creatorcontrib>Brooks, R.R</creatorcontrib><creatorcontrib>Kirkman, J.H</creatorcontrib><creatorcontrib>Gregg, P.E.H</creatorcontrib><creatorcontrib>Varela Alvarez, H</creatorcontrib><title>Edaphic influences on a New Zealand ultramafic ('serpentine') flora: a statistical approach</title><title>Plant and soil</title><description>Ultramafic ("serpentine") soils from and adjacent to the Dun Mountain Ophiolitic Belt, South Island, New Zealand were analysed for 11 elements in order to establish to what degree edaphic factors influenced the character of the overlying vegetation. Using principal components analysis with a mutual plot of the first two principal components, involving the total elemental concentrations in the soils, it was possible to divide the soils into 6 virtually nonoverlapping fields, each of which represented a specific vegetation community. Component 1 was essentially an "ultramafic plot" with heavy loadings from the elements chromium, cobalt, iron, magnesium, manganese, and nickel. Component 2 was a "non ultramafic" plot with heavy loadings from aluminium, copper and zinc. For elements extracted from the soils at pH 5.9, discrimination was somewhat poorer but confirmed the great importance of magnesium and nickel as controlling elements for the serpentine vegetation. It was concluded that the results indicated the overriding importance of edaphic factors in controlling the serpentine vegetation.</description><subject>Acid soils</subject><subject>Aluminum</subject><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>Autoecology</subject><subject>Biological and medical sciences</subject><subject>BOTANICAL COMPOSITION</subject><subject>CHIMIE DU SOL</subject><subject>Chromium</subject><subject>Cobalt</subject><subject>COMPOSICION BOTANICA</subject><subject>COMPOSITION BOTANIQUE</subject><subject>EDAPHIC FACTORS</subject><subject>FACTEUR EDAPHIQUE</subject><subject>FACTORES EDAFICOS</subject><subject>Flora</subject><subject>Forest soils</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Magnesium</subject><subject>Manganese</subject><subject>METHODE STATISTIQUE</subject><subject>METODOS ESTADISTICOS</subject><subject>Mountain soils</subject><subject>NEW ZEALAND</subject><subject>Nickel</subject><subject>NOUVELLE ZELANDE</subject><subject>NUEVA ZELANDIA</subject><subject>PLANT SOIL RELATIONS</subject><subject>Plants</subject><subject>Plants and fungi</subject><subject>Principal components analysis</subject><subject>QUIMICA DEL SUELO</subject><subject>RELACIONES PLANTA SUELO</subject><subject>RELATION PLANTE SOL</subject><subject>Sedimentary soils</subject><subject>Serpentine</subject><subject>SERPENTINE SOILS</subject><subject>SOIL CHEMISTRY</subject><subject>SOL DE SERPENTINE</subject><subject>STATISTICAL METHODS</subject><subject>SUELO DE SERPENTINA</subject><subject>VEGETACION</subject><subject>VEGETATION</subject><issn>0032-079X</issn><issn>1573-5036</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1997</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp90ElLxDAUAOAgCo7L2ZNQRFwO1ZetSbyJuMGgFwXRQ3mTJtqh09akRfz3RhQFD57Cy_t4GyFbFI4oMH58ekIBBAPNOABXS2RCpeK5BF4sk0n6Yjko87BK1mKcw2dMiwl5Oq-wf6ltVre-GV1rXcy6NsPsxr1ljw4bbKtsbIaAC_SJHexHF3rXDnXr9g8z33QBTxKPAw51HGqLTYZ9Hzq0LxtkxWMT3eb3u07uL87vzq7y6e3l9dnpNEeuiyGfUa1kYStQmqMw4CwY1IIWwByAlIwLz50wXoGmpppVBsHMDMysdF6D5Otk76tuavs6ujiUizpa16TZXTfGkhZMSQE6wYP_IXChKVOcJrrzh867MbRpjVJJyop06iKh3W-EMS3uA7a2jmUf6gWG95IpDUbwxLa_2DwOXfhJC2aE4Yr95j12JT6HVOJmSo3RADQNxD8A2N6Muw</recordid><startdate>199701</startdate><enddate>199701</enddate><creator>Robinson, B.H. 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(Massey Univ., Palmerston North (New Zealand). Dept. of Soil Science) ; Brooks, R.R ; Kirkman, J.H ; Gregg, P.E.H ; Varela Alvarez, H</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a386t-b18756cd0783a490ec09a841602e0055234f3e49f70819dbd9a09b90bc5ef8053</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1997</creationdate><topic>Acid soils</topic><topic>Aluminum</topic><topic>Animal and plant ecology</topic><topic>Animal, plant and microbial ecology</topic><topic>Autoecology</topic><topic>Biological and medical sciences</topic><topic>BOTANICAL COMPOSITION</topic><topic>CHIMIE DU SOL</topic><topic>Chromium</topic><topic>Cobalt</topic><topic>COMPOSICION BOTANICA</topic><topic>COMPOSITION BOTANIQUE</topic><topic>EDAPHIC FACTORS</topic><topic>FACTEUR EDAPHIQUE</topic><topic>FACTORES EDAFICOS</topic><topic>Flora</topic><topic>Forest soils</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Magnesium</topic><topic>Manganese</topic><topic>METHODE STATISTIQUE</topic><topic>METODOS ESTADISTICOS</topic><topic>Mountain soils</topic><topic>NEW ZEALAND</topic><topic>Nickel</topic><topic>NOUVELLE ZELANDE</topic><topic>NUEVA ZELANDIA</topic><topic>PLANT SOIL RELATIONS</topic><topic>Plants</topic><topic>Plants and fungi</topic><topic>Principal components analysis</topic><topic>QUIMICA DEL SUELO</topic><topic>RELACIONES PLANTA SUELO</topic><topic>RELATION PLANTE SOL</topic><topic>Sedimentary soils</topic><topic>Serpentine</topic><topic>SERPENTINE SOILS</topic><topic>SOIL CHEMISTRY</topic><topic>SOL DE SERPENTINE</topic><topic>STATISTICAL METHODS</topic><topic>SUELO DE SERPENTINA</topic><topic>VEGETACION</topic><topic>VEGETATION</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Robinson, B.H. (Massey Univ., Palmerston North (New Zealand). Dept. of Soil Science)</creatorcontrib><creatorcontrib>Brooks, R.R</creatorcontrib><creatorcontrib>Kirkman, J.H</creatorcontrib><creatorcontrib>Gregg, P.E.H</creatorcontrib><creatorcontrib>Varela Alvarez, H</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</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 One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & 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><jtitle>Plant and soil</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Robinson, B.H. (Massey Univ., Palmerston North (New Zealand). Dept. of Soil Science)</au><au>Brooks, R.R</au><au>Kirkman, J.H</au><au>Gregg, P.E.H</au><au>Varela Alvarez, H</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Edaphic influences on a New Zealand ultramafic ('serpentine') flora: a statistical approach</atitle><jtitle>Plant and soil</jtitle><date>1997-01</date><risdate>1997</risdate><volume>188</volume><issue>1</issue><spage>11</spage><epage>20</epage><pages>11-20</pages><issn>0032-079X</issn><eissn>1573-5036</eissn><coden>PLSOA2</coden><abstract>Ultramafic ("serpentine") soils from and adjacent to the Dun Mountain Ophiolitic Belt, South Island, New Zealand were analysed for 11 elements in order to establish to what degree edaphic factors influenced the character of the overlying vegetation. Using principal components analysis with a mutual plot of the first two principal components, involving the total elemental concentrations in the soils, it was possible to divide the soils into 6 virtually nonoverlapping fields, each of which represented a specific vegetation community. Component 1 was essentially an "ultramafic plot" with heavy loadings from the elements chromium, cobalt, iron, magnesium, manganese, and nickel. Component 2 was a "non ultramafic" plot with heavy loadings from aluminium, copper and zinc. For elements extracted from the soils at pH 5.9, discrimination was somewhat poorer but confirmed the great importance of magnesium and nickel as controlling elements for the serpentine vegetation. It was concluded that the results indicated the overriding importance of edaphic factors in controlling the serpentine vegetation.</abstract><cop>Dordrecht</cop><pub>Kluwer Academic Publishers</pub><doi>10.1023/A:1004208230037</doi><tpages>10</tpages></addata></record> |
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| ispartof | Plant and soil, 1997-01, Vol.188 (1), p.11-20 |
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| language | eng |
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| subjects | Acid soils Aluminum Animal and plant ecology Animal, plant and microbial ecology Autoecology Biological and medical sciences BOTANICAL COMPOSITION CHIMIE DU SOL Chromium Cobalt COMPOSICION BOTANICA COMPOSITION BOTANIQUE EDAPHIC FACTORS FACTEUR EDAPHIQUE FACTORES EDAFICOS Flora Forest soils Fundamental and applied biological sciences. Psychology Magnesium Manganese METHODE STATISTIQUE METODOS ESTADISTICOS Mountain soils NEW ZEALAND Nickel NOUVELLE ZELANDE NUEVA ZELANDIA PLANT SOIL RELATIONS Plants Plants and fungi Principal components analysis QUIMICA DEL SUELO RELACIONES PLANTA SUELO RELATION PLANTE SOL Sedimentary soils Serpentine SERPENTINE SOILS SOIL CHEMISTRY SOL DE SERPENTINE STATISTICAL METHODS SUELO DE SERPENTINA VEGETACION VEGETATION |
| title | Edaphic influences on a New Zealand ultramafic ('serpentine') flora: a statistical approach |
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