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Landscape structural analysis of the Lençóis Maranhenses national park: implications for conservation

Autores
Yuri Teixeira Amaral , Edyane Moraes dos Santos , Milton Cézar Ribeiro , Larissa Barreto
Ano de Publicação
2019
Categoria
UNIDADES DE CONSERVAÇÃO
Descrição

Our work evaluated the anthropic effects on the landscape structure of the Lençóis Maranhenses National Park (LMNP) and its Buffer Zone, and proposed strategies for the region’s conservation. LMNP is an important protected area in Brazilian north coast which protects a unique wetland ecosystem composed of sand dunes fields and a coastal vegetation called restinga. Supervised mapping of LMNP and a surrounding buffer of 3 km was carried out through high resolution and fine scale (1:5000) satellite images. The mapped area was subdivided in 1000 ha hexagonal Analysis Units (AU) and the following landscape metrics were calculated for each one of them: cover area (CA) of each soil cover class - dune fields (CA-DUNES), water bodies (CA-WATER), dense restinga (CADENSE), scattered restinga (CA-SCATTER), grassland (CA-SANDY), mangroves (CA-MANG), anthropogenic activity (CA-ANTRO) and, secondary vegetation (CA-SECOND); Landscape Shannon Diversity Index (SHDI), and; percentage of native vegetation cover (NV−COV). Pearson correlations were performed between the CA of each class and SHDI to identify the classes most correlated to CA-ANTRO. Our results showed that anthropic classes (crops, trails, and villages) had a stronger correlation (Pearson Correlation, r ≈ 0.65) with phytophysiognomies of dense restinga, secondary vegetation and SHDI, thus indicating that the land use conversion occurs in dense restinga areas and promotes vegetation secondarization, as well as increasing fragmentation. At least, 42% of the dense restinga habitats was destroyed due to human activities. Five conservation and restoration strategies were proposed in a local scale depending on the percentage of native vegetation cover on each AU, from the most to less conserved: (a) only conservation; (b) conservation with management; (c) management; (d) management and restoration; and, (e) restoration. The implementation of Agroforestry Systems with agro-successional restoration goals was recommended as an alternative for land use.

Keywords:Land use, Territorial planning,Landscape metrics,Conservation strategies


https://reader.elsevier.com/reader/sd/pii/S1617138118303108?token=1E133DD41AB611A5DB97426EFB32BBDABC19DB7AD0359970DA0A6F9EDD129658E32C80E33214545E23956F5A37353057


Tipo de publicação
Publicações periódicas (revistas, jornais, boletins)
Local da publicação
- https://www.sciencedirect.com/sdfe/reader/pii/S1617138118303108/pdf
Nº da edição ou volume
theyareinadequateforagriculture.Analysis of the impacts caused by the traditional land use in theLNMPanditsbufferzoneareimperativetoguideadministrativeactionsatthelocalscalebymanagersanddecision-makersaimingtoproposeadequateconservationstrategiesfortheregion.Thisstudyaimsto:(i)testtheconceptualmodelforlanduseandoccupationintheregion;(ii)evaluatetheeffectoflanduseconversionoverthelandscapestructureofLNMPanditssurroundings;and,(iii)proposeconservationstrategiesfortheregion.2. Methods2.1. StudyareaLençóisMaranhensesNationalPark(LMNP)islocatedattheeasterncoastofMaranhãostate,northeasternBrazil,betweenthecoordinates02°19′ and 2°45′ S; 42°44′ and 43°29′ W (Fig. 1) in an ecotonal areabetween the Amazon, Caatinga, and Cerrado biomes. It comprises anareaof155,000hapartiallyoverlaidbyBarreirinhas,SantoAmarodoMaranhão, and Primeira Cruz municipalities. Climate is of EquatorialZonewithtwomarkedseasonsthroughouttheyear.TherainyseasonextendsfromMarchtoJuneandthedryseasoncoverstherestoftheyear. Annual precipitation is 1800mm and mean temperature is of28.5°Cwitha1.5°Camplitude(IBAMA,2002).Soilsaresandyandrichin quartz of Quaternary origin. Marine transgression and regressionevents occurring since the Pleistocene deposited sediments on thecontinent coast and formed successive dune fields during the last100,000 years (Parteli, Schwaemmle, Herrmann, Monteiro, & Maia,2006). The currently active vegetation-free dune field develops overinactive paleo-dunes from the Pleistocene, which are stabilized by acoastalvegetation(Herrmann,Andrade,Schatz,Sauermann,&Parteli,2005; Luna,de,Parteli,&Herrmann,2012).Restingasarepioneercoastalvegetationformationsthatdeveloponsandy soils with fluviomarine influence and present different phyto-physiognomies related to edaphic features (Santos-Filho, Almeida, &Zickel,2013).InthePleistocenepaleo-duneplateaus,thesclerophyticshrubrestingavegetation occurs in low densities, as scattered bushes,duetolowsoilhumidityandnutrientavailability,withoccurrenceofHumiriabalsamiferaandByrsonimasp.Onvalleyslopes,thesclerophyticwoodyrestingavegetation develops homogenously-distributed withclosedcanopy,butvaryingbetweenshrubsandtrees,withoccurrenceofHymenaeaparvifolia,Anacardiummicrocarpum,andCereusjamacuru.Mauritia flexuosa, Euterpe oleaceaandScripus sp,are commonthroughout the water courses. On the margins of rivers, lakes, andlowlandareas,thatmayormaynotbesubjecttofloodingintherainyseason,herbaceousrestingafieldsdevelop,whichcanbeinterspersedbyshrubsandscatteredtrees(Santos-Filho,Almeida,Soares,dos,&Zickel,2011). In these grasslands are foundCyperussp.,Cassia rotundifolia,Borreriasp.,CopernicapruniferaandAstrocaryumvulgare.Inthecoastalflooding plains typical mangrove forests of the Equatorial Americadevelop, with the occurrence ofRhizophora mangle,AvicenniaschauerianaandLagunculariaracemosa.2.2. MappingMappingofthestudiedareaforthelandscapestructureanalysiswasperformedwith theQuantumGISV.2.14.14software(QGIS DEVELO-PMENTEAM,2016)usingtheOpenLayercomplementwhichprovidesTable 1Resultsofcoverarea(CA)inthebroadandrestrictedclassmaps.BroadclassesArea(ha)%RestrictedclassesArea(ha)%ofbroadclass %oftotalDunesfieldsandlagoons 84,514.9338.08 Dunesfieldsandlagoons84,514.9310038.08CA-DUNESWaterbody46,263.0020.85 Ocean40,509.6287.5618.25CA-WATERRiver3,030.126.541.36Lake2,723.275.881.22Denserestinga23,825.4810.74 Arboreous11,847.7249.725.33CA-DENSEShrubs8,985.3337.314.04Riparianforest1,439.326.040.64Mixofarboreousandshrubs926.663.880.41Mixofarboreous,shrubsandfield 306.811.280.13Palmtreeforest200.280.840.09Spreadarboreous99.420.410.04Litoralrestinga19.890.080.004Restingafields14,481.406.52Openfield(grassland)5792.1339.992.61CA-GRASSMixoffieldandscatteredshrubs4946.6034.152.22Lakesidegrasslands3,406.2423.521.53Meadow317.562.190.14Mixoffieldandpalmtree18.820.0010.003Scatteredrestingashrubs 14,910.906.73Scatteredrestingashrubs14,910.901006.73CA-SCATTERSandysoil12,098.205.45Beach10,210.5084.394.60CA-SANDYSandysoil1,772.0014.640.79Dune67.720.550.03Sandbank47.920.390.02Mangrove7,815.453.52Mangroove6,764.2986.543.04CA-MANGApicum1,051.1613.440.47Antrhopicactivity8,651.353.89Crops5622.0064.982.53CA-ANTROTrails1,141.6813.190.512Village745.438.720.33Pasture419.134.840.18Mixofpastureandscattershrubs290.773.360.13Urbanzone242.522.800.10Exposedsoil189.282.180.08Secondaryvegetation9,158.194.13Intermediarysecondaryvegetation 4,264.4446.561.92CA-SENCONDLatesecondaryvegetation4,003.1343.711.80Pioneersecondaryvegetation890.619.720.40Cloudcover163.990.07Cloudcover163.991000.07Total221,882.88 100221,882.88100Y.T.Amaral,etal.Journal for Nature Conservation 51 (2019) 125725 - https://doi.org/10.1016/j.jnc.2019.125725
Editora
Elsevier - https://www.elsevier.com/locate/jnc
Link