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The Long-Term Perspective of Human Impact on Landscape for Environmental Change and Sustainability

A special issue of Sustainability (ISSN 2071-1050). This special issue belongs to the section "Environmental Sustainability and Applications".

Deadline for manuscript submissions: closed (30 September 2018) | Viewed by 79442

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Special Issue Editors


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Guest Editor
Laboratorio di Palinologia e Paleobotanica, Dipartimento di Scienze della Vita, Università di Modena e Reggio Emilia, Viale Caduti in Guerra 127, 41121 Modena, Italy
Interests: palynology; climate change; human impact; cultural landscape; Sahara
Special Issues, Collections and Topics in MDPI journals

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Guest Editor
Laboratorio di Palinologia e Paleobotanica, Dipartimento di Scienze della Vita, Università di Modena e Reggio Emilia, Viale Caduti in Guerra 127, 41121 Modena, Italy
Interests: palynology; archaeological sites; pastoralism; cultural heritage; Southern Italy
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

The knowledge of past environmental history strongly contributes to conscious and efficient environment conservation and management. Therefore, the long-term perspective of the dynamics which govern the human-climate ecosystem is becoming one of the main focuses of paramount interest in biological and earth system sciences. Modern biodiversity is the result of the long-term shaping that humans and climate made on vegetation, soils and landforms. Climate change and human impact are predicted to become significant risks to lose biodiversity.

Multidisciplinary bio-geo-archaeo investigations on the underlying processes of human impact on landscape are crucial to allow us to envisage possible future scenarios of biosphere responses to global warming and biodiversity losses. In particular, palaeoecology and ecology jointly facilitate the understanding of the effects of human impact on ecosystems answering to how plant species have reacted and still react to global changes. Palynology is among the best tools to study high-resolution sequences formed under natural and anthropic (cultural) forces.

This Special Issue seeks to engage an interdisciplinary dialogue on the dynamic interactions between nature and society, focussing on long-term environmental data as essential tool to better-informed landscape management decisions to gain an equilibrium between conservation and sustainable resources exploitation. Studies on environment, global change, archaeobotany, conservation, cultural landscape and human impact, with special focus on the research carried out by botanists in the different fields, are particularly encouraged.

Prof. Dr.  Anna Maria Mercuri
Dr. Assunta Florenzano
Guest Editors

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Keywords

  • Palynology
  • Land use change
  • Landscape transformation
  • Paleoecology
  • Archaeology
  • Palaeoethnobotany
  • Climate change
  • Terrestrial Ecology
  • Restoration planning
  • Environmental Sustainability

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Published Papers (14 papers)

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Editorial

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7 pages, 685 KiB  
Editorial
The Long-Term Perspective of Human Impact on Landscape for Environmental Change (LoTEC) and Sustainability: From Botany to the Interdisciplinary Approach
by Anna Maria Mercuri and Assunta Florenzano
Sustainability 2019, 11(2), 413; https://doi.org/10.3390/su11020413 - 15 Jan 2019
Cited by 12 | Viewed by 4212
Abstract
This is not the first time the Earth has to experience dramatic environmental and climate changes but this seems to be the first time that a living species—humanity—is able to understand that great changes are taking place rapidly and that probably natural and [...] Read more.
This is not the first time the Earth has to experience dramatic environmental and climate changes but this seems to be the first time that a living species—humanity—is able to understand that great changes are taking place rapidly and that probably natural and anthropogenic forces are involved in the process that is under way [...] Full article
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<p>Location map of the study areas (in red) of the 13 research articles included in this Special Issue. For each country, a label showing the first Author names and the time frame of the research has been added (map modified from d-maps.com: free maps).</p>
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Research

Jump to: Editorial

21 pages, 5115 KiB  
Article
The History of Pastoral Activities in S Italy Inferred from Palynology: A Long-Term Perspective to Support Biodiversity Awareness
by Assunta Florenzano
Sustainability 2019, 11(2), 404; https://doi.org/10.3390/su11020404 - 15 Jan 2019
Cited by 37 | Viewed by 5953
Abstract
The present-day Mediterranean landscape is a result of the long-term human–environment–climate interactions that have driven the ecological dynamics throughout the Holocene. Pastoralism had (and still has) an important role in shaping this landscape, and contributes to maintaining the mosaic patterns of the Mediterranean [...] Read more.
The present-day Mediterranean landscape is a result of the long-term human–environment–climate interactions that have driven the ecological dynamics throughout the Holocene. Pastoralism had (and still has) an important role in shaping this landscape, and contributes to maintaining the mosaic patterns of the Mediterranean habitats. Palaeoecological records provide significant multi-proxy data on environmental changes during the Holocene that are linked to human activities. In such research, the palynological approach is especially useful for detailing the complexity of anthropogenically-driven landscape transformations by discriminating past land uses and pastoral/breeding activities. This paper focuses on the palynological evidence for the impact of centuries of grazing on the vegetation of Basilicata, a region of southern Italy where animal breeding and pastoralism have a long tradition. A set of 121 pollen samples from eight archaeological sites (dated from the 6th century BC to the 15th century AD) and five modern surface soil samples were analyzed. The joint record of pollen pasture indicators and spores of coprophilous fungi suggests that continuous and intense pastoral activities have been practiced in the territory and have highly influenced its landscape. The palaeoecological results of this study provide us with better knowledge of the diachronical transformations of the habitats that were exposed to continuous grazing, with a shift toward more open vegetation and increase of sclerophyllous shrubs. The palynological approach gives insights into the vocation and environmental sustainability of this southern Italy region on a long-term basis. Full article
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<p>Study area: (<b>a</b>) Location map of the eight archaeological sites studied for pollen and non-pollen palynomorphs (NPPs) in Basilicata, southern Italy; (<b>b</b>) the current landscapes in which the sites are located.</p>
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<p>Pollen clumps from the archaeological layers of site 7: (<b>a</b>,<b>b</b>) Single-type pollen clumps; (<b>c</b>) mixed-type cluster, including more than one pollen type. The scale bar is 10 μm.</p>
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<p>Percentage pollen diagram (average data from the eight sites, and modern soil samples): Main sums useful for palaeoenvironmental reconstruction, and concentration of coprophilous fungal spores (npp/g/100). The samples are grouped according to their chronology.</p>
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<p>Percentage pollen diagram (average data from the eight sites, and modern soil samples): Mediterranean plants, pollen taxa indicators of (or linked to) pastures, and concentration of coprophilous fungal spores (npp/g/100). The samples are grouped according to their chronology.</p>
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<p>Main pollen and non-pollen palynomorphs indicators of grazing environments from the studied archaeological sites: (<b>a</b>) Cichorieae; (<b>b</b>) <span class="html-italic">Aster</span> type; (<b>c</b>) Poaceae wild grass group; (<b>d</b>) <span class="html-italic">Plantago</span>; (<b>e</b>) <span class="html-italic">Centaurea nigra</span> type; (<b>f</b>) <span class="html-italic">Trifolium</span> type; (<b>g</b>) Chenopodiaceae; (<b>h</b>) <span class="html-italic">Brassica</span> type; (<b>i</b>) <span class="html-italic">Sordaria</span> type; (<b>j</b>) <span class="html-italic">Sporormiella</span> type; (<b>k</b>) <span class="html-italic">Delitschia</span> type; (<b>l</b>) <span class="html-italic">Podospora</span> type. The scale bar is 10 μm.</p>
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17 pages, 1696 KiB  
Article
The Tragedy of Forestland Sustainability in Postcolonial Africa: Land Development, Cocoa, and Politics in Côte d’Ivoire
by Symphorien Ongolo, Sylvestre Kouamé Kouassi, Sadia Chérif and Lukas Giessen
Sustainability 2018, 10(12), 4611; https://doi.org/10.3390/su10124611 - 5 Dec 2018
Cited by 18 | Viewed by 6116
Abstract
Tropical countries are often blamed for not managing their natural resources sustainably. But what if overexploitation is inherent in political structures and policies—rooted in foreign colonial order—and is consistently detrimental in the contemporary use of forestlands? This article argues that post-colonial land development [...] Read more.
Tropical countries are often blamed for not managing their natural resources sustainably. But what if overexploitation is inherent in political structures and policies—rooted in foreign colonial order—and is consistently detrimental in the contemporary use of forestlands? This article argues that post-colonial land development policies and related political interests seriously impede the sustainability of forest ecosystems in Côte d’Ivoire. Methodologically, the study builds on a historic contextualisation of forestland use policies in Sub-Saharan Africa, with Côte d’Ivoire serving as a case study. The results indicate that the increasing development of so-called rent crops clearly follows the historical dynamics of ‘land grabbing’ and a post-colonial agrarian model. This situation benefits agribusiness entrepreneurs and, more recently, sustainability standards. The study discusses the findings based on recent literature and empirical evidence. In conclusion, the post-colonial heritage and the manipulation of the related patterns by elites and policy-makers largely explains the present-day unsustainable forestland conversions in Côte d’Ivoire. Full article
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<p>Evolution of deforestation and forestland cover in Côte d’Ivoire from 1880 to 1991. Source: authors (based on data from [<a href="#B25-sustainability-10-04611" class="html-bibr">25</a>,<a href="#B27-sustainability-10-04611" class="html-bibr">27</a>]).</p>
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<p>Evolution of cocoa production in Côte d’Ivoire from 1961 to 2010. Source: Authors (From [<a href="#B27-sustainability-10-04611" class="html-bibr">27</a>] data).</p>
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<p>Recent trend of forest cover loss in protected areas in Côte d’Ivoire (From [<a href="#B26-sustainability-10-04611" class="html-bibr">26</a>] data).</p>
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<p>Visualisation of the deforestation dynamics in Côte d’Ivoire from 1990 to 2015 (source: adapted from [<a href="#B68-sustainability-10-04611" class="html-bibr">68</a>]).</p>
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21 pages, 4150 KiB  
Article
Forest Landscape Change and Preliminary Study on Its Driving Forces in ?l??a Landscape Park (Southwestern Poland) in 1883–2013
by Piotr Krajewski, Iga Solecka and Karol Mrozik
Sustainability 2018, 10(12), 4526; https://doi.org/10.3390/su10124526 - 30 Nov 2018
Cited by 48 | Viewed by 4870
Abstract
Changes in forest landscapes have been connected with human activity for centuries and can be considered one of the main driving forces of change from a global perspective. The spatial distribution of forests changes along with the geopolitical situation, demographic changes, intensification of [...] Read more.
Changes in forest landscapes have been connected with human activity for centuries and can be considered one of the main driving forces of change from a global perspective. The spatial distribution of forests changes along with the geopolitical situation, demographic changes, intensification of agriculture, urbanization, or changes in land use policy. However, due to the limited availability of historical data, the driving forces of changes in forest landscapes are most often considered in relation to recent decades, without taking long-term analyses into account. The aim of this paper is to determine the level and types of landscape changes and make preliminary study on natural and socio-economic factors on changes in forest landscapes within the protected area, ?l??a Landscape Park, and its buffer zone using long-term analyses covering a period of 140 years (1883–2013). A comparison of historical and current maps and demographic data related to three consecutive periods of time as well as natural and location factors by using the ArcGIS software allows the selected driving forces of forest landscape transformations to be analyzed. We took into account natural factors such as the elevation, slope, and exposure of the hillside and socio-economic drivers like population changes, distances to centers of municipalities, main roads, and built-up areas. Full article
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<p>Location and digital elevation model of the research area.</p>
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<p>Changes in the land cover of the study area between 1883(89) and 2013: (<b>a</b>) map of land cover in 1883(89); (<b>b</b>) map of land cover in 1936(38); (<b>c</b>) map of land cover in 1977; (<b>d</b>) map of land cover in 2013.</p>
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<p>The areas of land cover classes between 1883(89) and 2013.</p>
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<p>Land cover changes in analyzed time intervals.</p>
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<p>Area and number of different landscape changes in analyzed time intervals.</p>
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<p>Maps of the analyzed natural driving forces of landscape change: (<b>a</b>) map of elevation; (<b>b</b>) map of slope grade; (<b>c</b>) map of hillside exposure.</p>
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<p>Population changes in communes of Ślęża Landscape Park (source: population censuses from 1885, 1941, 1978, 2011).</p>
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<p>Maps of the analyzed socioeconomic driving forces of landscape change: (<b>A</b>) map of the distance to a main road; (<b>B</b>) map of the distance to a built-up area; (<b>C</b>) map of the distance to the center of a municipality.</p>
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19 pages, 5058 KiB  
Article
The Impact of Late Holocene Flood Management on the Central Po Plain (Northern Italy)
by Filippo Brandolini and Mauro Cremaschi
Sustainability 2018, 10(11), 3968; https://doi.org/10.3390/su10113968 - 31 Oct 2018
Cited by 20 | Viewed by 8073
Abstract
Fluvial environments have always played a crucial role in human history. The necessity of fertile land and fresh water for agriculture has led populations to settle in floodplains more frequently than in other environments. Floodplains are complex human–water systems in which the mutual [...] Read more.
Fluvial environments have always played a crucial role in human history. The necessity of fertile land and fresh water for agriculture has led populations to settle in floodplains more frequently than in other environments. Floodplains are complex human–water systems in which the mutual interaction between anthropogenic activities and environment affected the landscape development. In this paper, we analyzed the evolution of the Central Po Plain (Italy) during the Medieval period through a multi-proxy record of geomorphological, archaeological and historical data. The collapse of the Western Roman Empire (5th century AD) coincided with a progressive waterlogging of large floodplain areas. The results obtained by this research shed new light on the consequences that Post-Roman land and water management activities had on landscape evolution. In particular, the exploitation of fluvial sediments through flood management practices had the effect of reclaiming the swamps, but also altered the natural geomorphological development of the area. Even so, the Medieval human activities were more in equilibrium with the natural system than with the later Renaissance large-scale land reclamation works that profoundly modified the landscape turning the wetland environment into the arable land visible today. The analysis of fluvial palaeoenvironments and their relation with past human activities can provide valuable indications for planning more sustainable urbanized alluvial landscapes in future. Full article
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<p>The wetlands in the Po Plain before the Renaissance land reclamation works, 1570 AD. Library of the Univerisità degli Studi di Bologna [<a href="#B32-sustainability-10-03968" class="html-bibr">32</a>]. The dashed line indicates the research area.</p>
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<p>Location of the study area. 1—Tagliata Canal; 2—Parmigiana Canal; 3—<span class="html-italic">Crustulus Vetus</span>; 4—Camporainero area; 5—Valle di Gualtieri backswamp; 6—Valle di Novellara backswamp.</p>
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<p>Schematic geomorphic map of the Po plain in the Emilia region (adapted from [<a href="#B47-sustainability-10-03968" class="html-bibr">47</a>,<a href="#B48-sustainability-10-03968" class="html-bibr">48</a>,<a href="#B49-sustainability-10-03968" class="html-bibr">49</a>]). The red dashed line highlights the study area: 1—Valle di Gualtieri; 2—Valle di Novellara.</p>
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<p>Digital Terrain Model elaborated with software QGIS implemented with archaeological records. In the north of the mapped area, the meandering geomorphological feature corresponds to the so-called <span class="html-italic">Po Morto</span> or <span class="html-italic">Dead Po</span>, active in Roman Times.</p>
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<p>The 3D model: altitude checkpoints attribute ×50.</p>
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<p>Application of the soil map [<a href="#B70-sustainability-10-03968" class="html-bibr">70</a>] to the 3D model. Grey and Dark-Grey areas correspond to fine sediments settled after flood events.</p>
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<p>Maximum extension of wetlands before the Renaissance large-scale land reclamation project.</p>
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<p>The Tagliata Canal in the geomorphological map of the Po Plain edited in 1997 [<a href="#B47-sustainability-10-03968" class="html-bibr">47</a>]. The Tagliata Canal is considered a Proto-historic Po ridge characterized by crevasse splays on both sides.</p>
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<p>The distribution of archaeological sites and materials in the study area shows an absence of Bronze Age and Roman Era findings suggesting that the Tagliata Canal ridge developed in medieval times.</p>
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<p>Geomorphological analysis of the Tagliata Canal ridge: crevasse splays and land-fill ridges. 1—Villarotta; 2—Fangaia.</p>
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<p>Medieval historical maps (18th-century copies) that show the environmental situation of the study area before (<b>A</b>), (for more details, see also <a href="#sustainability-10-03968-f012" class="html-fig">Figure 12</a>) and after (<b>B</b>), (for more details, see also <a href="#sustainability-10-03968-f013" class="html-fig">Figure 13</a>) the Renaissance wetland reclamation. The numbers in the schematic box in the center of the image helps to orientate: 1—Tagliata Canal; 2—Parmigiana Canal; 3—Crustulus Vetus; 4—Camporainero area; 5—Valle di Gualtieri backswamp; 6—Valle di Novellara backswamp; 7—Town of Guastalla; 8—Town of Novellara; 9—Town of Gualtieri. (AsMo 52 and 53, XVIIIsec. Modena National Historical Archive—“Congragazione delle Acque e delle Strade, Reggio e Reggiano”) [<a href="#B89-sustainability-10-03968" class="html-bibr">89</a>].</p>
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<p>Detail of the medieval historical map that shows the landscape before the Renaissance land reclamation project (<a href="#sustainability-10-03968-f011" class="html-fig">Figure 11</a>A). (AsMo 52, XVIIIsec. Modena National Historical Archive—“Congragazione delle Acque e delle Strade, Reggio e Reggiano) [<a href="#B89-sustainability-10-03968" class="html-bibr">89</a>]. This map shows the project of artificially diversion on the Crostolo River from the Valle di Novellara to the Po Plain through the Early Medieval <span class="html-italic">Fossa di Roncaglio</span> Canal. a—Town of Guastalla; b—Town of Novellara; c—the so-called <span class="html-italic">Crustulus Vetus</span>, still active at that time; d—the wetland area called <span class="html-italic">Camporainero</span>; e—<span class="html-italic">Fossa di Roncaglio</span> Canal; f—the area of the NNE Crostolo ridge, developed to fill the <span class="html-italic">Camporainero</span> area with Crostolo sediments; g—Valle di Gualtieri wetland; h—Valle di Novellara wetland.</p>
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<p>Detail of the medieval historical map which shows the landscape before the Renaissance land reclamation project (<a href="#sustainability-10-03968-f011" class="html-fig">Figure 11</a>B). (AsMo 53, XVIIIsec. Modena National Historical Archive—“Congragazione delle Acque e delle Strade, Reggio e Reggiano) [<a href="#B89-sustainability-10-03968" class="html-bibr">89</a>]. This map shows the study area after the Renaissance Bonifica Bentivoglio land reclamation project. a—Town of Guastalla; b—Town of Novellara; c—<span class="html-italic">Crostolo Vecchio</span> or <span class="html-italic">Crustulus Vetus</span>, the medieval Crostolo watercourse that flowed into the Valle di Novellara wetland; d—The artificial diversion of the Crostolo River in the Po River; there are no more indications of both <span class="html-italic">Camporainero</span> and <span class="html-italic">Roncaglio</span>; e—Drained area in place of the Valle di Gualtieri wetland; f—Drained area in place of Valle di Novellara wetland; g—<span class="html-italic">Botte Bentivoglio</span> hydraulic device.</p>
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<p>Digital Terrain Model (DTM) of the Crostolo River medieval ridges. 1—NEE Crostolo ridge; 2—NE Crostolo ridge, called <span class="html-italic">Crustulus Vetus</span>; 3—Modern Crostolo River course; 4—Valle di Gualtieri wetland area; 5—Valle di Novellara wetland area; 6—Tagliata Canal ridge; 7—The dashed line indicates the modern Age <span class="html-italic">Fossa Alessandrina</span> Canal, the black square represents the S. Bernardino Church.</p>
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<p>The crossing between the Crostolo River (1) with the <span class="html-italic">Parmigiana Canal</span> (2) in the modern completely drained countryside. The white square highlights the 17th century AD structure of the <span class="html-italic">Botte Bentivoglio</span> hydraulic device (3).</p>
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20 pages, 3840 KiB  
Article
Historical Arable Land Change in an Eco-Fragile Area: A Case Study in Zhenlai County, Northeastern China
by Yuanyuan Yang and Shuwen Zhang
Sustainability 2018, 10(11), 3940; https://doi.org/10.3390/su10113940 - 30 Oct 2018
Cited by 10 | Viewed by 3377
Abstract
Long-term land changes are cumulatively a major driver of global environmental change. Historical land-cover/use change is important for assessing present landscape conditions and researching ecological environment issues, especially in eco-fragile areas. Arable land is one of the land types influenced by human agricultural [...] Read more.
Long-term land changes are cumulatively a major driver of global environmental change. Historical land-cover/use change is important for assessing present landscape conditions and researching ecological environment issues, especially in eco-fragile areas. Arable land is one of the land types influenced by human agricultural activity, reflecting human effects on land-use and land-cover change. This paper selected Zhenlai County, which is part of the farming–pastoral zone of northern China, as the research region. As agricultural land transformation goes with the establishment of settlements, in this research, the historical progress of land transformation in agricultural areas was analyzed from the perspective of settlement evolution, and the historical reconstruction of arable land was established using settlement as the proxy between their inner relationships, which could be reflected by the farming radius. The results show the following. (1) There was little land transformation from nonagricultural areas into agricultural areas until the Qing government lifted the ban on cultivation and mass migration accelerated the process, which was most significant during 1907–1912; (2) The overall trend of land transformation in this region is from northeast to southwest; (3) Taking the topographic maps as references, the spatial distribution of the reconstructed arable land accounts for 47.79% of the maps. When this proxy-based reconstruction method is applied to other regions, its limitations should be noticed. It is important to explore the research of farming radius calculations based on regional characteristics. To achieve land-system sustainability, long-term historical land change trajectories and characteristics should be applied to future policy making. Full article
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<p>Location of the study area, Zhenlai County.</p>
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<p>Advantages and constraints of reconstruction using historical documents.</p>
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<p>Flow path of settlement data capture from the <span class="html-italic">Zhenlai Gazetteer</span>.</p>
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<p>Farming radius calculated by (<b>a</b>) equalization-based method and (<b>b</b>) cultivation–settlement ratio-based method.</p>
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<p>Cumulative curve of the number of villages.</p>
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<p>Spatial distribution of settlements during 1875–1985.</p>
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<p>Sketch map of movement of settlement gravity during 1875–1985.</p>
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<p>Buffer area map with a 1092-m cultivation radius.</p>
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<p>Distribution of arable land and settlements from topographic maps from the 1930s.</p>
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<p>Overlapping arable land between buffer area and topographic map.</p>
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<p>Cultivation and settlement ratio-based buffer area map.</p>
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<p>Overlapping areas of buffer region and topographic maps.</p>
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<p>Arable land reconstruction in 1932 based on settlement distribution and farming radius.</p>
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<p>Overlap analysis map of buffer area and arable land area in the topographic maps.</p>
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27 pages, 12102 KiB  
Article
Analyzing Trends of Dike-Ponds between 1978 and 2016 Using Multi-Source Remote Sensing Images in Shunde District of South China
by Fengshou Li, Kai Liu, Huanli Tang, Lin Liu and Hongxing Liu
Sustainability 2018, 10(10), 3504; https://doi.org/10.3390/su10103504 - 30 Sep 2018
Cited by 17 | Viewed by 4505
Abstract
Dike-ponds have experienced significant changes in the Pearl River Delta region over the past several decades, especially since China’s economic reform, which has seriously affected the construction of ecological environments. In order to monitor the evolution of dike-ponds, in this study we use [...] Read more.
Dike-ponds have experienced significant changes in the Pearl River Delta region over the past several decades, especially since China’s economic reform, which has seriously affected the construction of ecological environments. In order to monitor the evolution of dike-ponds, in this study we use multi-source remote sensing images from 1978 to 2016 to extract dike-ponds in several periods using the nearest neighbor classification method. A corresponding area weighted dike-pond invasion index (AWDII) is proposed to describe the spatial evolution of dike-ponds, both qualitatively and quantitatively. Furthermore, the evolution mechanisms of dike-ponds are determined, which can be attributed to both natural conditions and human factors. Our results show that the total area of dike-ponds in 2016 was significantly reduced and fragmentation had increased compared with the situation in 1978. The AWDII reveals that Shunde District has experienced three main phases, including steady development, rapid invasion and a reduction of invasion by other land use types. Most dike-ponds have now converted into built-up areas, followed by cultivated lands, mainly due to government policies, rural area depopulation, and river networks within Shunde. Our study indicates that the AWDII is applicable towards the evaluation of the dynamic changes of dike-ponds. The rational development, and careful protection, of dike-ponds should be implemented for better land and water resource management. Full article
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<p>Location of the study area.</p>
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<p>Workflow of the research.</p>
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<p>Distribution of dike-pond in Shunde District from 1978 to 2016.</p>
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<p>Changing area of land use types in Shunde District between 1978 and 2016.</p>
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<p>Stacked bar graph of dike-pond area of the 10 towns in Shunde District from 1978 to 2016.</p>
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<p>Two different evolution trends of dike-pond proportion in each town.</p>
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<p>Spatial distribution of the Class A and Class B towns in Shunde.</p>
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<p>Dike-pond expansion/invasion during each period.</p>
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<p>Comparison of dike-pond area proportions in Xingtan and Longjiang from 1978 to 2016.</p>
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<p>The relationship between river network density in 1967 and the dike-pond proportion in each town in 1978.</p>
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<p>The relationship between river network density and dike-pond proportion.</p>
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22 pages, 4511 KiB  
Article
Vegetation History in the Toledo Mountains (Central Iberia): Human Impact during the Last 1300 Years
by Reyes Luelmo-Lautenschlaeger, Sebastián Pérez-Díaz, Francisca Alba-Sánchez, Daniel Abel-Schaad and José Antonio López-Sáez
Sustainability 2018, 10(7), 2575; https://doi.org/10.3390/su10072575 - 23 Jul 2018
Cited by 11 | Viewed by 3725
Abstract
Mid-mountain ecosystems provide a broad diversity of resources, heterogeneous relief, and a mild climate, which are all very useful for human necessities. These features enable different strategies such as the terracing of the slopes as well as wide crop diversification. Their relations lead [...] Read more.
Mid-mountain ecosystems provide a broad diversity of resources, heterogeneous relief, and a mild climate, which are all very useful for human necessities. These features enable different strategies such as the terracing of the slopes as well as wide crop diversification. Their relations lead to a parallel co-evolution between the environment and human societies, where fire and grazing become the most effective landscape management tools. This paper presents the results obtained from a multi-proxy study of the Bermú paleoenvironmental record, which is a minerotrophic mire located in the Quintos de Mora National Hunting Reserve (Toledo Mountains, central Spain). The bottom of this core has been dated in the Islamic period (ca. 711–1100 cal AD), and the study shows how the landscape that was built over time in the Toledo Mountains up to the present day is narrowly linked to human development. This study shows the increasing human pressure on the landscape, as well as the subsequent strategies followed by the plant and human communities as they faced diverse environmental changes. Thus, it is possible to attest the main role played by the humans in the Toledo Mountains, not only as a simple user, but also as a builder of their own reflexion in the environment. Full article
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<p>Map of Bermú mire location in the Toledo Mountains (red star) and other mires mentioned in the text (red points): 1. Las Lanchas; 2. Patateros; 3. La Botija; 4. Valdeyernos.</p>
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<p>Age–depth model of Bermú mire. Lithostratigraphic description according to Aaby and Berglund [<a href="#B41-sustainability-10-02575" class="html-bibr">41</a>].</p>
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<p>Bermú mire trees and shrubs pollen diagram plotted against depth. The black silhouettes show the percentage curves of the taxa; the grey silhouettes show the ×5 exaggeration curves.</p>
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<p>Bermú herbs and non-pollen palynomorphs (NPPs) diagram plotted against depth. The black silhouettes show the percentage curves of the taxa, the grey silhouettes show the ×5 exaggeration curves. Dots represent percentages below 0.5%.</p>
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<p>Synthetic Bermú mire pollen diagram plotted against age. The black silhouettes show the percentage curves of the taxa; the grey silhouettes show the ×5 exaggeration curves. Dots represent percentages below 0.5%. Other riparian trees: <span class="html-italic">Alnus</span>, <span class="html-italic">Fraxinus</span>, <span class="html-italic">Populus</span>, <span class="html-italic">Salix</span>, <span class="html-italic">Ulmus</span>. Anthropogenic-nitrophilous herbs: <span class="html-italic">Aster</span>, <span class="html-italic">Asphodelus albus</span>, Cardueae, <span class="html-italic">Centaurea nigra</span>, Cichorieae, <span class="html-italic">Convovulvus arvensis</span>, <span class="html-italic">Dipsacus fullonum</span>. Anthropozoogenous herbs: Chenopodiaceae, <span class="html-italic">Plantago lanceolata</span>, <span class="html-italic">Urtica dioica</span>. <span class="html-italic">Coprophilous fungi</span>: <span class="html-italic">Sordaria</span> (HdV-55), <span class="html-italic">Sporormiella</span>. Erosive processes indicators: <span class="html-italic">Glomus</span>, <span class="html-italic">Pseudoschizaea.</span> Fire indicators: <span class="html-italic">Chaetomium</span> (HdV-7A).</p>
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<p>Patateros mire synthetic diagram. High-mountain species: <span class="html-italic">Pinus pinaster</span>, <span class="html-italic">Pinus sylvestris</span>, <span class="html-italic">Calluna vulgaris</span>, <span class="html-italic">Erica</span> spp. <span class="html-italic">Cytisus</span> type. Mid-mountain species: Deciduous <span class="html-italic">Quercus</span>, evergreen <span class="html-italic">Quercus</span>, <span class="html-italic">Castanea sativa</span>, <span class="html-italic">Olea europaea</span>, <span class="html-italic">Cistus ladanifer</span>. Anthropic herbs: Aster, <span class="html-italic">Asphodelus albus</span>, Cardueae, <span class="html-italic">Centaurea nigra</span>, Cichorieae, <span class="html-italic">Convolvulus arvensis</span>, <span class="html-italic">Dipsacus fullonum</span>. <span class="html-italic">Coprophilous fungi</span>: <span class="html-italic">Sordaria</span> (HdV-55), <span class="html-italic">Sporormiella</span>.</p>
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<p>Valdeyernos mire synthetic diagram. High-mountain species: <span class="html-italic">Pinus pinaster</span>, <span class="html-italic">Pinus sylvestris</span>, <span class="html-italic">Calluna vulgaris</span>, <span class="html-italic">Erica</span> spp. <span class="html-italic">Cytisus</span> type. Mid-mountain species: Deciduous <span class="html-italic">Quercus</span>, evergreen <span class="html-italic">Quercus</span>, <span class="html-italic">Castanea sativa</span>, <span class="html-italic">Olea europaea</span>, <span class="html-italic">Cistus ladanifer</span>.</p>
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<p>La Botija mire synthetic diagram. High-mountain species: <span class="html-italic">Pinus pinaster</span>, <span class="html-italic">Pinus sylvestris</span>, <span class="html-italic">Calluna vulgaris</span>, <span class="html-italic">Erica</span> spp. <span class="html-italic">Cytisus</span> type. Mid-mountain species: Deciduous <span class="html-italic">Quercus</span>, evergreen <span class="html-italic">Quercus</span>, <span class="html-italic">Castanea sativa</span>, <span class="html-italic">Olea europaea</span>, <span class="html-italic">Cistus ladanifer</span>.</p>
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<p>Las Lanchas mire synthetic diagram. High-mountain species: <span class="html-italic">Pinus pinaster</span>, <span class="html-italic">Pinus sylvestris</span>, and <span class="html-italic">Calluna vulgaris</span>, <span class="html-italic">Erica</span> spp. <span class="html-italic">Cytisus</span> type. Mid-mountain species: Deciduous <span class="html-italic">Quercus</span>, evergreen <span class="html-italic">Quercus</span>, <span class="html-italic">Castanea sativa</span>, <span class="html-italic">Olea europaea</span>, and <span class="html-italic">Cistus ladanifer</span>.</p>
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12 pages, 10185 KiB  
Article
Agricultural Oasis Expansion and Its Impact on Oasis Landscape Patterns in the Southern Margin of Tarim Basin, Northwest China
by Yi Liu, Jie Xue, Dongwei Gui, Jiaqiang Lei, Huaiwei Sun, Guanghui Lv and Zhiwei Zhang
Sustainability 2018, 10(6), 1957; https://doi.org/10.3390/su10061957 - 11 Jun 2018
Cited by 26 | Viewed by 5702
Abstract
Oasis landscape change and its pattern dynamics are considered one of the vital research areas on global land use and landscape change in arid regions. An agricultural oasis is the main site of food security and ecosystem services in arid areas. Recently, the [...] Read more.
Oasis landscape change and its pattern dynamics are considered one of the vital research areas on global land use and landscape change in arid regions. An agricultural oasis is the main site of food security and ecosystem services in arid areas. Recently, the dramatic exploitation of agricultural oases has affected oasis stability, inducing some ecological and environmental issues such as water shortage and land degradation. In this study, the Qira oasis on the southern margin of Tarim Basin, Northwest China, was selected as a study area to examine the spatiotemporal changes in an agricultural oasis and the influence on oasis landscape pattern. Based on the integration of Thematic Mapper, Enhanced Thematic Mapper Plus, and GF-1 images, the agricultural Qira oasis has rapidly increased, with annual change rates of −0.3%, 1.6%, 3.7%, and 1.5% during 1970–1990, 1990–2000, 2000–2013, and 2013–2016, respectively. With the agricultural oasis expansion, the agricultural land has increased from 91.10 km2 in 1970 to 105.04 km2 in 2016. The percentage of farmland area has increased by 15.3% in 2016 compared with that in 1970. The natural vegetation is decreasing owing to the reclamation of desert–oasis ecotone. The oasis landscape change and pattern are mainly affected by agricultural expansion under water-saving technological utilization, land use policy, and regional economic development demand. The expansion of agricultural oasis is alarming due to human overexploitation. Thus, the government should adjust the layout of agricultural development and pay considerable attention to the oasis environment sustainability. This study can provide a valuable reference on the impact of climate change and human activities on a landscape. Full article
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<p>Location of Qira oasis in the southern Tarim Basin (adapted from [<a href="#B24-sustainability-10-01957" class="html-bibr">24</a>]).</p>
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<p>Landscape pattern and agricultural oasis expansion in the Qira oasis from 1970 to 2000.</p>
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<p>Landscape pattern and agricultural oasis expansion in the Qira oasis from 2013 to 2016.</p>
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<p>Changes of desert and oasis landscapes during 1970–2016.</p>
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<p>Land-use changes in the Qira oasis during 1970–2016: (<b>a</b>) farmland area and shrubby grassland area; (<b>b</b>) forestry area and desert area.</p>
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<p>Annual mean temperature and precipitation in the Qira oasis.</p>
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<p>Population and grain yield in the Qira oasis.</p>
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<p>Annual evaporation and runoff in the Qira oasis.</p>
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18 pages, 29239 KiB  
Article
Profiling Human-Induced Vegetation Change in the Horqin Sandy Land of China Using Time Series Datasets
by Lili Xu, Zhenfa Tu, Yuke Zhou and Guangming Yu
Sustainability 2018, 10(4), 1068; https://doi.org/10.3390/su10041068 - 4 Apr 2018
Cited by 17 | Viewed by 3859
Abstract
Discriminating the significant human-induced vegetation changes over the past 15 years could help local governments review the effects of eco-programs and develop sustainable land use policies in arid/semi-arid ecosystems. We used the residual trends method (RESTREND) to estimate the human-induced and climate-induced vegetation [...] Read more.
Discriminating the significant human-induced vegetation changes over the past 15 years could help local governments review the effects of eco-programs and develop sustainable land use policies in arid/semi-arid ecosystems. We used the residual trends method (RESTREND) to estimate the human-induced and climate-induced vegetation changes. Two typical regions in the Horqin Sandy Land of China were selected as study areas. We first detected vegetation dynamics between 2000–2014 using Sen’s slope estimation and the Mann–Kendall test detection method (SMK) based on the Moderate Resolution Imaging Spectroradiometer (MODIS) normalized difference vegetation index (NDVI) time series, then used RESTREND to profile human modifications in areas of significant vegetation change. RESTREND was optimized using statistical and trajectory analysis to automatically identify flexible spatially homogeneous neighborhoods, which were essential for determining the reference areas. The results indicated the following. (1) Obvious vegetation increases happened in both regions, but Naiman (64.1%) increased more than Ar Horqin (16.8%). (2) Climate and human drivers both contributed to significant changes. The two factors contributed equally to vegetation change in Ar Horqin, while human drivers contributed more in Naiman. (3) Human factors had a stronger influence on ecosystems, and were more responsible for vegetation decreases in both regions. Further evidences showed that the primary human drivers varied in regions. Grassland eco-management was the key driver in Ar Horqin, while farming was the key factor for vegetation change in Naiman. Full article
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<p>Location of the Horqin Sandy Land, China and the two study areas.</p>
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<p>Framework of the study.</p>
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<p>Three steps used to find the reference pixel to simulate ideal climate–vegetation relationships.</p>
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<p>Vegetation change (<b>a</b>) and driving forces (<b>b</b>) in the Ar Horqin region.</p>
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<p>Vegetation change (<b>a</b>) and driving forces (<b>b</b>) in the Naiman region.</p>
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<p>Typical change areas in the Ar Horqin region: (<b>a</b>) a typical human-induced vegetation decrease area from the optimized residual trends method (RESTREND) method; (<b>b</b>–<b>e</b>) Landsat false color image maps for (<b>a</b>) on 09/24/2000, 09/06/2005, 09/17/2009, and 09/04/2014, respectively; (<b>f</b>) a typical human-induced vegetation increase area detected by the optimized RESTREND method; (<b>g</b>–<b>j</b>) Landsat false color image maps for (<b>f</b>) on 09/24/2000, 09/06/2005, 09/17/2009, and 09/04/2014, respectively.</p>
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<p>Typical change areas in the Naiman region (<b>a</b>) a typical human-induced vegetation decrease area from the optimized RESTREND method; (<b>b</b>–<b>e</b>) Landsat false color image maps for (<b>a</b>) on 09/24/2000, 09/06/2005, 09/17/2009, and 09/04/2014, respectively; (<b>f</b>) a typical human-induced vegetation increase area detected by the optimized RESTREND method; (<b>g</b>–<b>j</b>) Landsat false color image maps for (<b>f</b>) on 09/24/2000, 09/06/2005, 09/17/2009, and 09/04/2014, respectively.</p>
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<p>Photographs of in situ investigation of the circular grassland in <a href="#sustainability-10-01068-f006" class="html-fig">Figure 6</a>j, collected in August 2015.</p>
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<p>Human-induced changes on different land covers in Ar Horqin region (<b>a</b>) and Naiman region (<b>b</b>).</p>
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<p>(<b>a</b>) Amount of chemical fertilizer and (<b>b</b>) number of livestock at the end of each year in the two regions.</p>
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20 pages, 3617 KiB  
Article
Spatio-Temporal Variation of Land-Use Intensity from a Multi-Perspective—Taking the Middle and Lower Reaches of Shule River Basin in China as an Example
by Libang Ma, Wenjuan Cheng, Jie Bo, Xiaoyang Li and Yuan Gu
Sustainability 2018, 10(3), 771; https://doi.org/10.3390/su10030771 - 11 Mar 2018
Cited by 17 | Viewed by 4207
Abstract
The long-term human activities could influence land use/cover change and sustainability. As the global climate changes, humans are using more land resources to develop economy and create material wealth, which causes a tremendous influence on the structure of natural resources, ecology, and environment. [...] Read more.
The long-term human activities could influence land use/cover change and sustainability. As the global climate changes, humans are using more land resources to develop economy and create material wealth, which causes a tremendous influence on the structure of natural resources, ecology, and environment. Interference from human activities has facilitated land utilization and land coverage change, resulting in changes in land-use intensity. Land-use intensity can indicate the degree of the interference of human activities on lands, and is an important indicator of the sustainability of land use. Taking the middle and lower reaches of Shule River Basin as study region, this paper used “land-use degree (LUD)” and “human activity intensity (HAI)” models for land-use intensity, and analyzed the spatio-temporal variation of land-use intensity in this region from a multi-perspective. The results were as follows: (1) From 1987 to 2015, the land use structure in the study region changed little. Natural land was always the main land type, followed by semi-natural land and then artificial land. (2) The LUD in the study region increased by 35.36 over the 29 years. It increased the most rapidly from 1996 to 2007, and after 2007, it still increased, but more slowly. A spatial distribution pattern of “low land-use degree in east and west regions and high land-use degree in middle region” changed to “high land-use degree in east and middle regions and low land-use degree in west region”. (3) The human activity intensity of artificial lands (HAI-AL) in the study region decreased from 1987 to 1996, and then increased from 1996 to 2015. The human activity intensity of semi-artificial lands (HAL-SAL) in the study region increased over the 29 years, and more rapidly after 1996. (4) 1996–2007 was a transition period for the land-use intensity in the study region. This was related to the implementation of the socio-economy, policies such as “Integrated Development of Agricultural Irrigation and Immigrant Settlement in Shule River Basin (1996–2006)”, and technologies. Full article
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<p>Survey map of the study region.</p>
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<p>Spatial distribution of different land types in the middle and lower reaches of the Shule River Basin (1987–2015).</p>
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<p>Temporal variation of LUD in the middle and lower reaches of the Shule River (1987–2015).</p>
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<p>Spatial distribution of LUD in the middle and lower reaches of the Shule River Basin (1987–2015).</p>
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<p>Spatial distribution of HAL-AL in the middle and lower reaches of the Shule River Basin (1987–2015).</p>
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<p>Spatial distribution of HAL-SAL in the middle and lower reaches of the Shule River Basin (1987–2015).</p>
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14 pages, 1381 KiB  
Article
Modelling Soil Carbon Content in South Patagonia and Evaluating Changes According to Climate, Vegetation, Desertification and Grazing
by Pablo Luis Peri, Yamina Micaela Rosas, Brenton Ladd, Santiago Toledo, Romina Gisele Lasagno and Guillermo Martínez Pastur
Sustainability 2018, 10(2), 438; https://doi.org/10.3390/su10020438 - 8 Feb 2018
Cited by 33 | Viewed by 5711
Abstract
In Southern Patagonia, a long-term monitoring network has been established to assess bio-indicators as an early warning of environmental changes due to climate change and human activities. Soil organic carbon (SOC) content in rangelands provides a range of important ecosystem services and supports [...] Read more.
In Southern Patagonia, a long-term monitoring network has been established to assess bio-indicators as an early warning of environmental changes due to climate change and human activities. Soil organic carbon (SOC) content in rangelands provides a range of important ecosystem services and supports the capacity of the land to sustain plant and animal productivity. The objectives in this study were to model SOC (30 cm) stocks at a regional scale using climatic, topographic and vegetation variables, and to establish a baseline that can be used as an indicator of rangeland condition. For modelling, we used a stepwise multiple regression to identify variables that explain SOC variation at the landscape scale. With the SOC model, we obtained a SOC map for the entire Santa Cruz province, where the variables derived from the multiple linear regression models were integrated into a geographic information system (GIS). SOC stock to 30 cm ranged from 1.38 to 32.63 kg C m?2. The fitted model explained 76.4% of SOC variation using as independent variables isothermality, precipitation seasonality and vegetation cover expressed as a normalized difference vegetation index. The SOC map discriminated in three categories (low, medium, high) determined patterns among environmental and land use variables. For example, SOC decreased with desertification due to erosion processes. The understanding and mapping of SOC in Patagonia contributes as a bridge across main issues such as climate change, desertification and biodiversity conservation. Full article
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Graphical abstract
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<p>Characterization of the study area: (<b>A</b>) location of Argentina (dark grey) and Santa Cruz province (black); (<b>B</b>) Desertification (black = none, very dark grey = slight degraded, dark grey = moderate desertification, grey = moderate to severe desertification, light grey = severe desertification, very light grey = very severe desertification [<a href="#B21-sustainability-10-00438" class="html-bibr">21</a>]; (<b>C</b>) sample sites (black dots) and main water bodies in the zone of the Parcelas de Ecología y Biodiversidad de Ambientes Naturales en Patagonia Austral (PEBANPA) plots; (<b>D</b>) main ecological areas (light grey = dry steppe, grey = humid steppe, medium grey = shrub-lands, dark grey = sub-Andean grasslands, black = forests and alpine vegetation) [<a href="#B22-sustainability-10-00438" class="html-bibr">22</a>].</p>
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<p>Soil organic carbon stock (30 cm depth) in Santa Cruz province, South Patagonia, Argentina.</p>
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14 pages, 235 KiB  
Article
Carbon Neutral by 2021: The Past and Present of Costa Rica’s Unusual Political Tradition
by Julia A. Flagg
Sustainability 2018, 10(2), 296; https://doi.org/10.3390/su10020296 - 24 Jan 2018
Cited by 16 | Viewed by 10365
Abstract
Costa Rica has pledged to become the first nation to become carbon neutral. This event raises the important question of how to understand this contemporary form of climate politics, given that Costa Rica has made an almost negligible contribution to the problem of [...] Read more.
Costa Rica has pledged to become the first nation to become carbon neutral. This event raises the important question of how to understand this contemporary form of climate politics, given that Costa Rica has made an almost negligible contribution to the problem of global climate change. To understand this pledge, a case study spanning about 200 years situates the pledge within the country’s unique historical profile. An analysis of interview data, archival research, and secondary data reveals that the pledge is the latest instance in Costa Rica’s unusual political tradition. This political tradition dates back to the area’s experience as a Spanish colony and as a newly independent nation. Several events, including the abolition of the army, the work on green development, and being awarded a Nobel Peace Prize were all foundational in forming Costa Rica’s tradition as a place that leads by example and stands for peace and protection of nature. The carbon neutral pledge extends the political tradition that has been established through these earlier events. This case highlights the importance of understanding contemporary environmental politics through an analysis of long-term, historical data. Full article
16 pages, 5542 KiB  
Article
Responses of Vegetation Cover to Environmental Change in Large Cities of China
by Kai Jin, Fei Wang and Pengfei Li
Sustainability 2018, 10(1), 270; https://doi.org/10.3390/su10010270 - 20 Jan 2018
Cited by 54 | Viewed by 6715
Abstract
Vegetation cover is crucial for the sustainability of urban ecosystems; however, this cover has been undergoing substantial changes in cities. Based on climate data, city statistical data, nighttime light data and the Normalized Difference Vegetation Index (NDVI) dataset, we investigate the spatiotemporal variations [...] Read more.
Vegetation cover is crucial for the sustainability of urban ecosystems; however, this cover has been undergoing substantial changes in cities. Based on climate data, city statistical data, nighttime light data and the Normalized Difference Vegetation Index (NDVI) dataset, we investigate the spatiotemporal variations of climate factors, urban lands and vegetation cover in 71 large cities of China during 1998–2012, and explore their correlations. A regression model between growing-season NDVI (G-NDVI) and urban land proportion (PU) is built to quantify the impact of urbanization on vegetation cover change. The results indicate that the spatiotemporal variations of temperature, precipitation, PU and G-NDVI are greatly different among the 71 cities which experienced rapid urbanization. The spatial difference of G-NDVI is closely related to diverse climate conditions, while the inter-annual variations of G-NDVI are less sensitive to climate changes. In addition, there is a negative correlation between G-NDVI trend and PU change, indicating vegetation cover in cities have been negatively impacted by urbanization. For most of the inland cities, the urbanization impacts on vegetation cover in urban areas are more severe than in suburban areas. But the opposite occurs in 17 cities mainly located in the coastal areas which have been undergoing the most rapid urbanization. Overall, the impacts of urbanization on G-NDVI change are estimated to be ?0.026 per decade in urban areas and ?0.015 per decade in suburban areas during 1998–2012. The long-term developments of cities would persist and continue to impact on the environmental change and sustainability. We use a 15-year window here as a case study, which implies the millennia of human effects on the natural biotas and warns us to manage landscapes and preserve ecological environments properly. Full article
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<p>Locations of the selected 71 large cities in China and the corresponding urban populations in 1998.</p>
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<p>An example of the extracted urban lands of 1998 and 2012 in the urban area (Z1) and suburban area (Z2) of Nanchang city.</p>
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<p>Spatial distribution of mean annual growing-season temperature (G-T) (<b>a</b>) and growing-season precipitation (G-P) (<b>b</b>) and inter-annual variations of G-T (<b>c</b>) and G-P (<b>d</b>) during 1998–2012 for the selected 71 large cities.</p>
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<p>Spatial distribution of the ΔPU<sub>Z1</sub> (<b>a</b>) and ΔPU<sub>Z2</sub> (<b>b</b>) during 1998–2012 for the selected 71 large cities.</p>
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<p>Spatial distribution of mean annual G-NDVI<sub>Z1</sub> (<b>a</b>) and G-NDVI<sub>Z2</sub> (<b>b</b>) and inter-annual variations of G-NDVI<sub>Z1</sub> (<b>c</b>) and G-NDVI<sub>Z2</sub> (<b>d</b>) during 1998–2012 in the selected 71 large cities.</p>
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<p>The relationship of mean annual G-T, G-P and G-NDVI<sub>Z1</sub> (<b>a</b>) G-NDVI<sub>Z2</sub> (<b>b</b>) of the selected 71 large cities. Each dot in the panel corresponds to three values (i.e., the mean annual G-NDVI, G-T and G-P).</p>
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<p>Correlations between the mean annual G-T and G-NDVI (<b>a</b>) and between the mean annual G-P and G-NDVI (<b>b</b>) of the selected 71 large cities.</p>
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<p>Distributions of the correction coefficients for the inter-annual variation between G-NDVI<sub>Z1</sub> and G-T (<b>a</b>), G-NDVI<sub>Z1</sub> and G-P (<b>b</b>), G-NDVI<sub>Z2</sub> and G-T (<b>c</b>), and G-NDVI<sub>Z2</sub> and G-P (<b>d</b>) in the selected 71 large cities during 1998–2012.</p>
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<p>Trends of G-NDVI<sub>Z1-Z2</sub> for the selected 71 large cities.</p>
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<p>The relationship between trends of G-NDVI<sub>Z1-Z2</sub> and ΔPU<sub>Z1-Z2</sub> for the selected 71 large cities.</p>
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