<http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2000/01/rdf-schema#label> "Carr (landform)"@en . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Willow> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2002/07/owl#sameAs> <http://nl.dbpedia.org/resource/Broekbos> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Reed_bed> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2000/01/rdf-schema#label> "L\u00F6vsumpskog"@sv . <http://dbpedia.org/resource/Carr_(landform)> <http://xmlns.com/foaf/0.1/depiction> <http://commons.wikimedia.org/wiki/Special:FilePath/Moor_Park_alder_carr.jpg> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2002/07/owl#sameAs> <http://yago-knowledge.org/resource/Carr_(landform)> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2000/01/rdf-schema#comment> "Une for\u00EAt mar\u00E9cageuse ou un carr (terme issu de l'anglais), d\u00E9signe une for\u00EAt claire \u00E0 feuillage caduc, poussant sur un sol constamment humide, riche en mati\u00E8re organique."@fr . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://dbpedia.org/class/yago/Wetland109477890> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2002/07/owl#sameAs> <http://hu.dbpedia.org/resource/L\u00E1perd\u0151> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/abstract> "Une for\u00EAt mar\u00E9cageuse ou un carr (terme issu de l'anglais), d\u00E9signe une for\u00EAt claire \u00E0 feuillage caduc, poussant sur un sol constamment humide, riche en mati\u00E8re organique."@fr . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2000/01/rdf-schema#label> "Carr (zone humide)"@fr . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2000/01/rdf-schema#label> "Broekbos"@nl . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Alder> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2000/01/rdf-schema#label> "Fa\u016Dltarbaro"@eo . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/abstract> "Een broekbos is een permanent nat en af en toe plaatselijk overstroomd bos. Deze natte bossen komen wereldwijd voor. Broekbossen zijn in natte beekdalen en langs laag- en hoogvenen te vinden. Het bostype komt in Europa algemeen voor. Sinds de tweede helft van de 20e eeuw zijn in Vlaanderen en Nederland veel van de traditionele broekbossen verdwenen. De resterende gebieden worden vaak beschermd vanwege de specifieke flora en fauna. Ook vindt natuurherstel plaats. Op laagveengronden nemen elzen- en berkenbroekbossen door veranderd gebruik en beheer toe. In een broekbos wordt de vegetatie bepaald door de hoge stand van het grondwater. \u2018Broek\u2019 betekent laag gelegen moerassig land. Het grootste gedeelte van het jaar staat de waterspiegel tot op of boven het maaiveld. Elzen en berken vormen hierbij de boomlaag. Afhankelijk van de soortensamenstelling vallen broekbossen vegetatiekundig gezien onder de klasse van de berkenbroekbossen (Vaccinio-Betuletea pubescentis) of de klasse van de elzenbroekbossen (Alnetea glutinosae). Er zijn drie verschillende biotopen aan te wijzen waarin broekbossen aanwezig zijn: laagveen, hoogveen en beekdalen. De berkenbroekbossen zijn ontstaan uit hoogvenen en natte heidegebieden. Elzenbroekbossen komen voor in beekdalen en laagveengebieden."@nl . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2000/01/rdf-schema#comment> "L\u00F6vsumpskog, \u00E4ven fuktl\u00F6vskog, \u00E4r en svensk biotop, som best\u00E5r av l\u00F6vtr\u00E4dsdominerad sumpskog med ett best\u00E5nd av l\u00F6vtr\u00E4d understigande 50 % \u00E4dell\u00F6vtr\u00E4d. L\u00F6vsumpskogar \u00E4r v\u00E5tmarksomr\u00E5den som k\u00E4nnetecknas av h\u00F6g f\u00F6rekomst av d\u00F6d ved. Bland tr\u00E4d dominerar glasbj\u00F6rk, klibbal och gr\u00E5al. Aldominerade (\u00F6ver 50 % al) best\u00E5nd kallas alsumpskog. Bland mossarter m\u00E4rks , , terpentinmossa och stubbspretmossa.[k\u00E4lla beh\u00F6vs] Ett exempel p\u00E5 en l\u00F6vsumpskog \u00E4r Uggleviken p\u00E5 Norra Djurg\u00E5rden i Stockholm."@sv . <http://dbpedia.org/resource/Carr_(landform)> <http://purl.org/dc/terms/subject> <http://dbpedia.org/resource/Category:Wetlands> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageID> "11818074"^^<http://www.w3.org/2001/XMLSchema#integer> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Sedge> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/thumbnail> <http://commons.wikimedia.org/wiki/Special:FilePath/Moor_Park_alder_carr.jpg?width=300> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/property/wikiPageUsesTemplate> <http://dbpedia.org/resource/Template:Short_description> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/File:Moor_Park_alder_carr.JPG> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2000/01/rdf-schema#comment> "A carr is a type of waterlogged wooded terrain that, typically, represents a succession stage between the original reedy marsh and the likely eventual formation of forest in a sub-maritime climate. Carrs are wetlands that are dominated by shrubs rather than trees. The carr is one stage in a hydrosere: the progression of vegetation beginning from a terrain submerged by fresh water along a river or lake margin. In sub-maritime regions, it begins with reed-marsh. As the reeds decay, the soil surface eventually rises above the water, creating fens that allow vegetation such as sedge to grow. As this progression continues, riparian trees and bushes appear and a carr landscape is created \u2013 in effect a wooded fen in a waterlogged terrain. At this stage, overall, unlike the overwhelming acidity of"@en . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Shrub> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageInterLanguageLink> <http://sv.dbpedia.org/resource/Sumpskog> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2002/07/owl#sameAs> <http://www.wikidata.org/entity/Q910817> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/property/wikiPageUsesTemplate> <http://dbpedia.org/resource/Template:Wetlands> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Category:Wetlands> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2002/07/owl#sameAs> <http://d-nb.info/gnd/4333508-1> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/abstract> "Ein Bruchwald [\u02C8b\u0281u\u02D0\u03C7-] (Zusammensetzung mit dem Wort Bruch f\u00FCr \u201EFeuchtgebiet\u201C; regional auch Broich, Brook oder Brok) ist ein permanent nasser, \u00F6rtlich \u00FCberstauter, langfristig gefluteter, sumpfiger Wald. Damit l\u00E4sst er sich vom zeitweilig gefluteten Sumpfwald und vom regelm\u00E4\u00DFig gefluteten Auwald abgrenzen; beide sind durch k\u00FCrzere und ausgepr\u00E4gtere Wasserstands\u00E4nderungen gekennzeichnet."@de . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageRevisionID> "1107950091"^^<http://www.w3.org/2001/XMLSchema#integer> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2002/07/owl#sameAs> <http://de.dbpedia.org/resource/Bruchwald> . <http://dbpedia.org/resource/Carr_(landform)> <http://purl.org/linguistics/gold/hypernym> <http://dbpedia.org/resource/Terrain> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://dbpedia.org/class/yago/WikicatSwamps> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://dbpedia.org/ontology/Town> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Ecological_succession> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageLength> "2199"^^<http://www.w3.org/2001/XMLSchema#nonNegativeInteger> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://www.w3.org/2002/07/owl#Thing> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2002/07/owl#sameAs> <http://rdf.freebase.com/ns/m.09g646y> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/abstract> "A carr is a type of waterlogged wooded terrain that, typically, represents a succession stage between the original reedy marsh and the likely eventual formation of forest in a sub-maritime climate. Carrs are wetlands that are dominated by shrubs rather than trees. The carr is one stage in a hydrosere: the progression of vegetation beginning from a terrain submerged by fresh water along a river or lake margin. In sub-maritime regions, it begins with reed-marsh. As the reeds decay, the soil surface eventually rises above the water, creating fens that allow vegetation such as sedge to grow. As this progression continues, riparian trees and bushes appear and a carr landscape is created \u2013 in effect a wooded fen in a waterlogged terrain. At this stage, overall, unlike the overwhelming acidity of decaying reeds, the pH is not too acidic and the soil is not too deficient in minerals, making a habitat for endemic and other wildlife. Characteristic water-tolerant trees include alder and willow."@en . <http://dbpedia.org/resource/Carr_(landform)> <http://xmlns.com/foaf/0.1/isPrimaryTopicOf> <http://en.wikipedia.org/wiki/Carr_(landform)> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Forest> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Fen> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://dbpedia.org/class/yago/PhysicalEntity100001930> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2002/07/owl#sameAs> <http://fr.dbpedia.org/resource/Carr_(zone_humide)> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/PH> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Maritime_climate> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2000/01/rdf-schema#comment> "Een broekbos is een permanent nat en af en toe plaatselijk overstroomd bos. Deze natte bossen komen wereldwijd voor. Broekbossen zijn in natte beekdalen en langs laag- en hoogvenen te vinden. Het bostype komt in Europa algemeen voor. Sinds de tweede helft van de 20e eeuw zijn in Vlaanderen en Nederland veel van de traditionele broekbossen verdwenen. De resterende gebieden worden vaak beschermd vanwege de specifieke flora en fauna. Ook vindt natuurherstel plaats. Op laagveengronden nemen elzen- en berkenbroekbossen door veranderd gebruik en beheer toe."@nl . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2002/07/owl#sameAs> <http://eo.dbpedia.org/resource/Fa\u016Dltarbaro> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://dbpedia.org/class/yago/Swamp109452395> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/abstract> "L\u00F6vsumpskog, \u00E4ven fuktl\u00F6vskog, \u00E4r en svensk biotop, som best\u00E5r av l\u00F6vtr\u00E4dsdominerad sumpskog med ett best\u00E5nd av l\u00F6vtr\u00E4d understigande 50 % \u00E4dell\u00F6vtr\u00E4d. L\u00F6vsumpskogar \u00E4r v\u00E5tmarksomr\u00E5den som k\u00E4nnetecknas av h\u00F6g f\u00F6rekomst av d\u00F6d ved. Bland tr\u00E4d dominerar glasbj\u00F6rk, klibbal och gr\u00E5al. Aldominerade (\u00F6ver 50 % al) best\u00E5nd kallas alsumpskog. Bland mossarter m\u00E4rks , , terpentinmossa och stubbspretmossa.[k\u00E4lla beh\u00F6vs] Ett exempel p\u00E5 en l\u00F6vsumpskog \u00E4r Uggleviken p\u00E5 Norra Djurg\u00E5rden i Stockholm."@sv . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2002/07/owl#sameAs> <http://et.dbpedia.org/resource/Lodumets> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://dbpedia.org/class/yago/YagoGeoEntity> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Acidic> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/property/wikiPageUsesTemplate> <http://dbpedia.org/resource/Template:Reflist> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/property/wikiPageUsesTemplate> <http://dbpedia.org/resource/Template:Authority_control> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageInterLanguageLink> <http://no.dbpedia.org/resource/Sumpskogsmark> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://dbpedia.org/class/yago/Object100002684> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Category:Landforms> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://dbpedia.org/class/yago/YagoPermanentlyLocatedEntity> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://dbpedia.org/class/yago/WikicatWetlands> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Riparian_zone> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2000/01/rdf-schema#comment> "Faultarbaro estas arbaro kiu kreskas sur geologia fa\u016Dlto. \u011Ci estas da\u016Dre malseka kaj partatempe anka\u016D inundata kaj mar\u0109a. \u011Ci diferenci\u011Das de regule inundata , kiu estas karakterizita de rivero kun forta akvonivela dinamiko."@eo . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://dbpedia.org/class/yago/Land109335240> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Old_Norse> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Lake> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2000/01/rdf-schema#comment> "Ein Bruchwald [\u02C8b\u0281u\u02D0\u03C7-] (Zusammensetzung mit dem Wort Bruch f\u00FCr \u201EFeuchtgebiet\u201C; regional auch Broich, Brook oder Brok) ist ein permanent nasser, \u00F6rtlich \u00FCberstauter, langfristig gefluteter, sumpfiger Wald. Damit l\u00E4sst er sich vom zeitweilig gefluteten Sumpfwald und vom regelm\u00E4\u00DFig gefluteten Auwald abgrenzen; beide sind durch k\u00FCrzere und ausgepr\u00E4gtere Wasserstands\u00E4nderungen gekennzeichnet."@de . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/ns/prov#wasDerivedFrom> <http://en.wikipedia.org/wiki/Carr_(landform)?oldid=1107950091&ns=0> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/abstract> "Faultarbaro estas arbaro kiu kreskas sur geologia fa\u016Dlto. \u011Ci estas da\u016Dre malseka kaj partatempe anka\u016D inundata kaj mar\u0109a. \u011Ci diferenci\u011Das de regule inundata , kiu estas karakterizita de rivero kun forta akvonivela dinamiko."@eo . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2002/07/owl#sameAs> <http://sv.dbpedia.org/resource/L\u00F6vsumpskog> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/River> . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2000/01/rdf-schema#label> "Bruchwald"@de . <http://dbpedia.org/resource/Carr_(landform)> <http://www.w3.org/2002/07/owl#sameAs> <https://global.dbpedia.org/id/53oVA> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Marsh> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Tree> . <http://dbpedia.org/resource/Carr_(landform)> <http://dbpedia.org/ontology/wikiPageWikiLink> <http://dbpedia.org/resource/Hydrosere> . <http://dbpedia.org/resource/Carr_(landform)> <http://purl.org/dc/terms/subject> <http://dbpedia.org/resource/Category:Landforms> .