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
|
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 |