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Reconstruction of an interrupted primary beach plain succession using a geographical information system
This study reports on a primary succession on a beach plain on the Dutch Wadden island of Schiermonnikoog. Vegetation succession started in 1959 when a sand dike was constructed to prevent structural erosion of the area by storm floods. Since then the sandy beach behind the dike has been protected f...
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Published in: | Journal of coastal conservation 1997-12, Vol.3 (1), p.71-78 |
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creator | Veen, A. van der Grootjans, A.P Jong, J. de (Groningen Univ., Haren (Netherlands). Lab. of Plant Ecology) Rozema, J |
description | This study reports on a primary succession on a beach plain on the Dutch Wadden island of Schiermonnikoog. Vegetation succession started in 1959 when a sand dike was constructed to prevent structural erosion of the area by storm floods. Since then the sandy beach behind the dike has been protected from the direct influence of the North Sea. Heavy storms in 1972, however, created a large gap in the dike which has remained open since. Occasional storm floods during winter penetrate deeply into the area and salt water can cover parts of the beach plain for several months. This had a pronounced impact on the vegetation. Vegetation maps for six different years and data from a permanent plot have been used to reconstruct vegetation succession over a 42-yr period. Certain parts of the area seem to have changed little, while others have developed a grassland or scrub cover. The heavy storms and associated processes such as sand blowing, intensive flooding and increased salinity have created a disturbance/stress gradient of progressive and regressive succession across the beach plain. In certain places the vegetation cover has repeatedly been destroyed and succession re-initiated. It is concluded that the different stages of succession and associated diversity of plant species only can persist through the maintenance of the natural dynamics of the area. |
doi_str_mv | 10.1007/bf02908181 |
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Lab. of Plant Ecology) ; Rozema, J</creator><creatorcontrib>Veen, A. van der ; Grootjans, A.P ; Jong, J. de (Groningen Univ., Haren (Netherlands). Lab. of Plant Ecology) ; Rozema, J</creatorcontrib><description>This study reports on a primary succession on a beach plain on the Dutch Wadden island of Schiermonnikoog. Vegetation succession started in 1959 when a sand dike was constructed to prevent structural erosion of the area by storm floods. Since then the sandy beach behind the dike has been protected from the direct influence of the North Sea. Heavy storms in 1972, however, created a large gap in the dike which has remained open since. Occasional storm floods during winter penetrate deeply into the area and salt water can cover parts of the beach plain for several months. This had a pronounced impact on the vegetation. Vegetation maps for six different years and data from a permanent plot have been used to reconstruct vegetation succession over a 42-yr period. Certain parts of the area seem to have changed little, while others have developed a grassland or scrub cover. The heavy storms and associated processes such as sand blowing, intensive flooding and increased salinity have created a disturbance/stress gradient of progressive and regressive succession across the beach plain. In certain places the vegetation cover has repeatedly been destroyed and succession re-initiated. It is concluded that the different stages of succession and associated diversity of plant species only can persist through the maintenance of the natural dynamics of the area.</description><identifier>ISSN: 1400-0350</identifier><identifier>EISSN: 1874-7841</identifier><identifier>DOI: 10.1007/bf02908181</identifier><language>eng</language><publisher>Dordrecht: Opulus Press AB</publisher><subject>BEACHES ; Blowing ; COASTAL PLAINS ; Conservation ; CONTROL DE LA EROSION ; Dikes ; Dunes ; ECOLOGICAL SUCCESSION ; EROSION CONTROL ; Floods ; Geographic information systems ; GEOGRAPHICAL INFORMATION SYSTEMS ; Grasslands ; Levees ; LLANURA COSTERA ; LUTTE ANTIEROSION ; NETHERLANDS ; PAISES BAJOS ; PAYS BAS ; PLAGE ; PLAINE COTIERE ; Plant diversity ; Plant species ; Plants ; PLAYAS ; Saline water ; Sand ; SISTEMAS DE INFORMACION GEOGRAFICA ; Soil salinity ; Soil water ; Species diversity ; Storms ; SUCCESSION ECOLOGIQUE ; SUCESION ECOLOGICA ; SYSTEME D'INFORMATION GEOGRAPHIQUE ; Vegetation ; Vegetation cover</subject><ispartof>Journal of coastal conservation, 1997-12, Vol.3 (1), p.71-78</ispartof><rights>Copyright EUCC</rights><rights>EUCC 1997</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3821-12c418c1edeb46064c1240e92d0d976b2fcd9f63f831f1e06e5cbce7f0a963483</citedby><cites>FETCH-LOGICAL-c3821-12c418c1edeb46064c1240e92d0d976b2fcd9f63f831f1e06e5cbce7f0a963483</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/25098252$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/25098252$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,58238,58471</link.rule.ids></links><search><creatorcontrib>Veen, A. van der</creatorcontrib><creatorcontrib>Grootjans, A.P</creatorcontrib><creatorcontrib>Jong, J. de (Groningen Univ., Haren (Netherlands). Lab. of Plant Ecology)</creatorcontrib><creatorcontrib>Rozema, J</creatorcontrib><title>Reconstruction of an interrupted primary beach plain succession using a geographical information system</title><title>Journal of coastal conservation</title><description>This study reports on a primary succession on a beach plain on the Dutch Wadden island of Schiermonnikoog. Vegetation succession started in 1959 when a sand dike was constructed to prevent structural erosion of the area by storm floods. Since then the sandy beach behind the dike has been protected from the direct influence of the North Sea. Heavy storms in 1972, however, created a large gap in the dike which has remained open since. Occasional storm floods during winter penetrate deeply into the area and salt water can cover parts of the beach plain for several months. This had a pronounced impact on the vegetation. Vegetation maps for six different years and data from a permanent plot have been used to reconstruct vegetation succession over a 42-yr period. Certain parts of the area seem to have changed little, while others have developed a grassland or scrub cover. The heavy storms and associated processes such as sand blowing, intensive flooding and increased salinity have created a disturbance/stress gradient of progressive and regressive succession across the beach plain. In certain places the vegetation cover has repeatedly been destroyed and succession re-initiated. It is concluded that the different stages of succession and associated diversity of plant species only can persist through the maintenance of the natural dynamics of the area.</description><subject>BEACHES</subject><subject>Blowing</subject><subject>COASTAL PLAINS</subject><subject>Conservation</subject><subject>CONTROL DE LA EROSION</subject><subject>Dikes</subject><subject>Dunes</subject><subject>ECOLOGICAL SUCCESSION</subject><subject>EROSION CONTROL</subject><subject>Floods</subject><subject>Geographic information systems</subject><subject>GEOGRAPHICAL INFORMATION SYSTEMS</subject><subject>Grasslands</subject><subject>Levees</subject><subject>LLANURA COSTERA</subject><subject>LUTTE ANTIEROSION</subject><subject>NETHERLANDS</subject><subject>PAISES BAJOS</subject><subject>PAYS BAS</subject><subject>PLAGE</subject><subject>PLAINE COTIERE</subject><subject>Plant diversity</subject><subject>Plant species</subject><subject>Plants</subject><subject>PLAYAS</subject><subject>Saline water</subject><subject>Sand</subject><subject>SISTEMAS DE INFORMACION GEOGRAFICA</subject><subject>Soil salinity</subject><subject>Soil water</subject><subject>Species diversity</subject><subject>Storms</subject><subject>SUCCESSION ECOLOGIQUE</subject><subject>SUCESION ECOLOGICA</subject><subject>SYSTEME D'INFORMATION GEOGRAPHIQUE</subject><subject>Vegetation</subject><subject>Vegetation cover</subject><issn>1400-0350</issn><issn>1874-7841</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1997</creationdate><recordtype>article</recordtype><recordid>eNp90c1rFTEQAPBFLFirF-9C8KIIa2eSbD6OtrQqFApVzyGbnWz3sW-zJruH_vfu81UFD55mYH4zQzJV9QrhAwLo8zYCt2DQ4JPqFI2WtTYSn265BKhBNPCsel7KDoA3phGnVX9HIU1lyWtYhjSxFJmf2DAtlPM6L9SxOQ97nx9YSz7cs3n0w8TKGgKVcmhYyzD1zLOeUp_9fD8EP279MeW9_zWxPJSF9i-qk-jHQi8f41n1_frq2-Xn-ub205fLjzd1EIZjjTxINAGpo1YqUDIgl0CWd9BZrVoeQ2ejEtEIjEigqAltIB3BWyWkEWfV2-PcOacfK5XF7YcSaBz9RGktzoDmuuEaN_nuvxKVRsmFlWqjb_6hu7TmaXuH040UIMAc0PsjCjmVkim6x59zCO5wHHdx_fs4G359xLuypPxH8gas4Q3_W48-Od_nobivV2itAQS1rfwJKW6UUQ</recordid><startdate>19971201</startdate><enddate>19971201</enddate><creator>Veen, A. van der</creator><creator>Grootjans, A.P</creator><creator>Jong, J. de (Groningen Univ., Haren (Netherlands). Lab. of Plant Ecology)</creator><creator>Rozema, J</creator><general>Opulus Press AB</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7SN</scope><scope>7ST</scope><scope>7TN</scope><scope>7U6</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H97</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope><scope>7QH</scope><scope>7UA</scope><scope>H95</scope></search><sort><creationdate>19971201</creationdate><title>Reconstruction of an interrupted primary beach plain succession using a geographical information system</title><author>Veen, A. van der ; Grootjans, A.P ; Jong, J. de (Groningen Univ., Haren (Netherlands). Lab. of Plant Ecology) ; Rozema, J</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3821-12c418c1edeb46064c1240e92d0d976b2fcd9f63f831f1e06e5cbce7f0a963483</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1997</creationdate><topic>BEACHES</topic><topic>Blowing</topic><topic>COASTAL PLAINS</topic><topic>Conservation</topic><topic>CONTROL DE LA EROSION</topic><topic>Dikes</topic><topic>Dunes</topic><topic>ECOLOGICAL SUCCESSION</topic><topic>EROSION CONTROL</topic><topic>Floods</topic><topic>Geographic information systems</topic><topic>GEOGRAPHICAL INFORMATION SYSTEMS</topic><topic>Grasslands</topic><topic>Levees</topic><topic>LLANURA COSTERA</topic><topic>LUTTE ANTIEROSION</topic><topic>NETHERLANDS</topic><topic>PAISES BAJOS</topic><topic>PAYS BAS</topic><topic>PLAGE</topic><topic>PLAINE COTIERE</topic><topic>Plant diversity</topic><topic>Plant species</topic><topic>Plants</topic><topic>PLAYAS</topic><topic>Saline water</topic><topic>Sand</topic><topic>SISTEMAS DE INFORMACION GEOGRAFICA</topic><topic>Soil salinity</topic><topic>Soil water</topic><topic>Species diversity</topic><topic>Storms</topic><topic>SUCCESSION ECOLOGIQUE</topic><topic>SUCESION ECOLOGICA</topic><topic>SYSTEME D'INFORMATION GEOGRAPHIQUE</topic><topic>Vegetation</topic><topic>Vegetation cover</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Veen, A. van der</creatorcontrib><creatorcontrib>Grootjans, A.P</creatorcontrib><creatorcontrib>Jong, J. de (Groningen Univ., Haren (Netherlands). 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Occasional storm floods during winter penetrate deeply into the area and salt water can cover parts of the beach plain for several months. This had a pronounced impact on the vegetation. Vegetation maps for six different years and data from a permanent plot have been used to reconstruct vegetation succession over a 42-yr period. Certain parts of the area seem to have changed little, while others have developed a grassland or scrub cover. The heavy storms and associated processes such as sand blowing, intensive flooding and increased salinity have created a disturbance/stress gradient of progressive and regressive succession across the beach plain. In certain places the vegetation cover has repeatedly been destroyed and succession re-initiated. It is concluded that the different stages of succession and associated diversity of plant species only can persist through the maintenance of the natural dynamics of the area.</abstract><cop>Dordrecht</cop><pub>Opulus Press AB</pub><doi>10.1007/bf02908181</doi><tpages>8</tpages><oa>free_for_read</oa></addata></record> |
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subjects | BEACHES Blowing COASTAL PLAINS Conservation CONTROL DE LA EROSION Dikes Dunes ECOLOGICAL SUCCESSION EROSION CONTROL Floods Geographic information systems GEOGRAPHICAL INFORMATION SYSTEMS Grasslands Levees LLANURA COSTERA LUTTE ANTIEROSION NETHERLANDS PAISES BAJOS PAYS BAS PLAGE PLAINE COTIERE Plant diversity Plant species Plants PLAYAS Saline water Sand SISTEMAS DE INFORMACION GEOGRAFICA Soil salinity Soil water Species diversity Storms SUCCESSION ECOLOGIQUE SUCESION ECOLOGICA SYSTEME D'INFORMATION GEOGRAPHIQUE Vegetation Vegetation cover |
title | Reconstruction of an interrupted primary beach plain succession using a geographical information system |
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