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	<front>
		<journal-meta>
			<journal-id journal-id-type="publisher-id">Pirineos</journal-id>
			<journal-title-group>
				<journal-title>Pirineos</journal-title>
				<abbrev-journal-title>Pirineos</abbrev-journal-title>
			</journal-title-group>
			<issn publication-format="print">0373-2568</issn>
			<issn publication-format="electronic">1988-4281</issn>
			<issn-l>0373-2568</issn-l>
			<publisher>
				<publisher-name>Consejo Superior de Investigaciones Cient&#xed;ficas</publisher-name>
			</publisher>
		</journal-meta>
		<article-meta>
			<article-id pub-id-type="publisher-id">pirineos.2022.177001</article-id>
			<article-id pub-id-type="doi">10.3989/pirineos.2022.177001</article-id>
			<article-categories>
				<subj-group subj-group-type="heading">
					<subject>Art&#xed;culos</subject>
				</subj-group>
			</article-categories>
			<title-group>
				<article-title>Ecosystem services in mountain environments: benefits and threats</article-title>
				<trans-title-group xml:lang="es">
					<trans-title>Servicios ecosist&#xe9;micos en &#xe1;reas de monta&#xf1;a: beneficios y amenazas</trans-title>
				</trans-title-group>
			</title-group>
			<contrib-group>
				<contrib contrib-type="author" corresp="yes">
					<contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-0227-2010</contrib-id>
					<name>
						<surname>Pereira</surname>
						<given-names>Paulo</given-names>
					</name>
					<email xlink:href="pereiraub@gmail.com">pereiraub@gmail.com</email>
					<aff id="aff1"><institution content-type="laboratory">Environmental Management Laboratory</institution>, <institution>Mykolas Romeris University</institution>, <addr-line>Vilnius</addr-line>, <country>Lithuania</country></aff>
				</contrib>
				<contrib contrib-type="author">
					<contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-4917-1287</contrib-id>
					<name>
						<surname>Inacio</surname>
						<given-names>Miguel</given-names>
					</name>
					<email xlink:href="rinacio.miguel@gmail.com">rinacio.miguel@gmail.com</email>
					<aff id="aff2"><institution content-type="laboratory">Environmental Management Laboratory</institution>, <institution>Mykolas Romeris University</institution>, <addr-line>Vilnius</addr-line>, <country>Lithuania</country></aff>
				</contrib>
				<contrib contrib-type="author">
					<contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-8345-458X</contrib-id>
					<name>
						<surname>Bogunovic</surname>
						<given-names>Igor</given-names>
					</name>
					<email xlink:href="igor.bogunovic@gmail.com">igor.bogunovic@gmail.com</email>
					<aff id="aff3"><institution content-type="faculty">Faculty of Agriculture</institution>, <institution>University of Zagreb</institution>, <addr-line>Svetosimunska 25, 10000 Zagreb</addr-line>, <country>Croatia</country></aff>
				</contrib>
				<contrib contrib-type="author">
					<contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-3311-5686</contrib-id>
					<name>
						<surname>Francos</surname>
						<given-names>Marcos</given-names>
					</name>
					<email xlink:href="marcosfrancos91@gmail.com">marcosfrancos91@gmail.com</email>
					<aff id="aff4"><institution content-type="department">Department of Geography</institution>, <institution content-type="faculty">Faculty of Geography and History</institution>, <institution>University of Salamanca</institution>, <addr-line>Cervantes s/n, 37002, Salamanca</addr-line>, <country>Spain</country></aff>
				</contrib>
				<contrib contrib-type="author">
					<contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-8873-0491</contrib-id>
					<name>
						<surname>Barcel&#xf3;</surname>
						<given-names>Dami&#xe0;</given-names>
					</name>
					<email xlink:href="dbcqam@cid.csic.es">dbcqam@cid.csic.es</email>
					<aff id="aff5"><institution>Catalan Institute for Water Research (ICRA-CERCA)</institution>, <addr-line>Girona, Catalonia</addr-line>, <country>Spain</country></aff>
				</contrib>
				<contrib contrib-type="author">
					<contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-5342-354X</contrib-id>
					<name>
						<surname>Zhao</surname>
						<given-names>Wenwu</given-names>
					</name>
					<email xlink:href="zhaoww@bnu.edu.cn">zhaoww@bnu.edu.cn</email>
					<aff id="aff6"><institution content-type="institute">Institute of Land Surface System and Sustainable Development</institution>, <institution content-type="faculty">Faculty of Geographical Science</institution>, <institution>Beijing Normal University</institution>, <addr-line>Beijing 100875</addr-line>, <country>China</country></aff>
				</contrib>
			</contrib-group>
			<pub-date pub-type="epub">
				<day>02</day>
				<month>03</month>
				<year>2022</year>
			</pub-date>
			<pub-date pub-type="collection">
				<month>12</month>
				<year>2022</year>
			</pub-date>
			<volume>177</volume>
			<issue content-type="empty"/>
			<elocation-id>e068</elocation-id>
			<history>
				<date date-type="received">
					<day>06</day>
					<month>11</month>
					<year>2021</year>
				</date>
				<date date-type="accepted">
					<day>18</day>
					<month>01</month>
					<year>2022</year>
				</date>
				<date date-type="pub">
					<day>23</day>
					<month>03</month>
					<year>2022</year>
				</date>
			</history>
			<permissions>
				<copyright-statement>&#xa9;2022 CSIC</copyright-statement>
				<copyright-year>2022</copyright-year>
				<license license-type="open-access" xlink:href="https://creativecommons.org/licenses/by/4.0/">
					<license-p>This is an open-access article distributed under the terms of the Creative Commons Attribution 4.0 International (CC BY 4.0) License.</license-p>
				</license>
			</permissions>
			<self-uri xlink:href="http://pirineos.revistas.csic.es/index.php/pirineos/article/view/XXXX/XXXX"/>
			<abstract>
				<title>Abstract</title>
				<p>Mountain areas have a substantial impact on climate dynamics and are one of the most critical water sources. Mountains were key in human evolution throughout history and supplied essential biotic and abiotic ecosystem services (ES), key for human living. This perspective article will study the importance of mountains to ES supply and the impacts of the different drivers of change, namely habitat change, climate change, overexploitation, pollution, and invasive species. Mountain areas have a high capacity to supply an important number of regulating (global and local climate regulation, air quality regulation, natural hazards regulation, pollination), provisioning (crops, livestock, wild food and fish, biomass for energy and timber, freshwater renewable energy - hydropower, wind, solar and geothermal - and mineral resources) and cultural (recreation and tourism, landscape aesthetics and inspiration, cultural heritage and cultural diversity and knowledge systems). However, changes imposed by habitat change, climate change, overexploitation, pollution, and invasive species can increase the tradeoffs between ES and trigger environmental degradation. Overall, there is a need to balance mountain ES exploitation and reduce the effects of the different drivers of change. </p>
			</abstract>
			<trans-abstract xml:lang="es">
				<title>Resumen</title>
				<p>Las &#xe1;reas de monta&#xf1;a tienen un impacto importante en las din&#xe1;micas clim&#xe1;ticas y son una de las fuentes de agua con condiciones m&#xe1;s cr&#xed;ticas. Las monta&#xf1;as fueron claves en la evoluci&#xf3;n hist&#xf3;rica del ser humano y suministraron servicios ecosist&#xe9;micos (SE) bi&#xf3;ticos y abi&#xf3;ticos esenciales para la vida humana. Este art&#xed;culo de perspectiva estudiar&#xe1; la importancia de las monta&#xf1;as para el suministro de SE y los impactos de los diferentes factores de cambio, a saber, cambios en el h&#xe1;bitat, el cambio clim&#xe1;tico, la sobreexplotaci&#xf3;n, la contaminaci&#xf3;n y las especies invasoras. Las zonas de monta&#xf1;a tienen una gran capacidad para suministrar un n&#xfa;mero importante de recursos reguladores (regulaci&#xf3;n del clima global y local, regulaci&#xf3;n de la calidad del aire, regulaci&#xf3;n de los riesgos naturales, polinizaci&#xf3;n), de aprovisionamiento (cultivos, ganado, alimentos y pesca silvestre, biomasa para energ&#xed;a y madera, energ&#xed;a renovable de agua dulce -hidroel&#xe9;ctrica, e&#xf3;lica, solar y geot&#xe9;rmica- y recursos minerales) y culturales (ocio y turismo, est&#xe9;tica e inspiraci&#xf3;n del paisaje, patrimonio cultural y diversidad cultural y sistemas de conocimiento). Sin embargo, los cambios impuestos por la modificaci&#xf3;n del h&#xe1;bitat, el cambio clim&#xe1;tico, la sobreexplotaci&#xf3;n, la contaminaci&#xf3;n y las especies invasoras pueden aumentar los intercambios entre los SE y desencadenar la degradaci&#xf3;n del medio ambiente. En general, es necesario equilibrar la utilizaci&#xf3;n de los SE de monta&#xf1;a y reducir los efectos de los distintos factores de cambio. </p>
			</trans-abstract>
			<kwd-group>
				<kwd>Mountains</kwd>
				<kwd>biotic</kwd>
				<kwd>abiotic</kwd>
				<kwd>ecosystem services</kwd>
				<kwd>drivers of change</kwd>
			</kwd-group>
			<kwd-group xml:lang="es">
				<kwd>Monta&#xf1;as</kwd>
				<kwd>bi&#xf3;tico</kwd>
				<kwd>abi&#xf3;tico</kwd>
				<kwd>servicios ecosist&#xe9;micos</kwd>
				<kwd>factores de cambio</kwd>
			</kwd-group>
			<funding-group id="fw-01">
				<award-group id="aw1">
					<funding-source>Research Council of Lithuania (LMTLT)</funding-source>
					<award-id>09.3.3-LMT-K-712-01-0104</award-id>
				</award-group>
				<funding-statement>This work was developed within the Lithuanian National Ecosystem Services Assessment and Mapping (LINESAM), which has received funding from European Social Fund project LINESAM no. 09.3.3-LMT-K-712-01-0104 under a grant agreement with the Research Council of Lithuania (LMTLT). Further, we would like to express gratitude to Marius Kalinauskas for providing the photo used in the figure 1.</funding-statement>
			</funding-group>
			<counts>
				<fig-count count="1"/>
				<table-count count="0"/>
				<equation-count count="0"/>
				<ref-count count="270"/>
				<page-count count="18"/>
			</counts>
		</article-meta>
	</front>
	<body>
		<sec id="sec1" sec-type="intro">
			<label>1.</label>
			<title>Introduction</title>
			<p>Mountain areas occupy 40,957,238 km<sup>2</sup>, approximately 30.55% of the global land area. For <xref ref-type="bibr" rid="B92">Kapos (2000)</xref>, they are defined according to the slope, elevation and local relief. However, despite these factors being important, the definition of a mountain is not simple. For instance, absolute elevation is not the best criterion. The degree that slope change in space (ruggedness) is also important (<xref ref-type="bibr" rid="B236">UNEP-WMC, 2002</xref>). <xref ref-type="bibr" rid="B93">Kapos <italic>et al.</italic> (2002)</xref> created criteria to define mountains based on altitude and slope. They divided mountain environments in different classes Class 1: elevation &#x2265; 4 500 m; Class 2: elevation 3 500-4 500 m; Class 3: elevation 2 500-3 500 m; Class 4: elevation 1 500-2 500 m and slope &#x2265; 2&#xb0;; Class 5: elevation 1 000-1 500 m and slope &#x2265; 5&#xb0; or LER &gt; 300 m; Class 6: elevation 300-1 000 m and LER &gt; 300 m (<xref ref-type="bibr" rid="B93">Kapos <italic>et al.,</italic> 2002</xref>; <ext-link ext-link-type="uri" xlink:href="https://www.fao.org/mountain-partnership/about/definitions/en/">https://www.fao.org/mountain-partnership/about/definitions/en/</ext-link>). </p>
			<p>A good discussion about the challenges in the definition of mountain environments was conducted by <xref ref-type="bibr" rid="B100">K&#xf6;rner <italic>et al.</italic> (2011)</xref>. Elevation cannot be the unique criterion for defining mountains since flat areas (plateaus) are located at altitudes around 2000 m (e.g., Central Asia). Also, mountains cannot be defined only by climate. A similar climate is observed in Antarctic and Arctic lowlands. The most common feature in mountain areas is the steepness and ruggedness (<xref ref-type="bibr" rid="B100">K&#xf6;rner <italic>et al.,</italic> 2011</xref>). Recently <xref ref-type="bibr" rid="B101">K&#xf6;rner <italic>et al.</italic> (2021)</xref> discussed the different mountain definitions and their consequences in identifying the area occupied. However, to use a standard definition, we consider a mountain as a <italic>&#x201c;landform that rises prominently above its surroundings, generally exhibiting steep slopes, a relatively confined summit area, and considerable local relief. Mountains generally are understood to be larger than hills, but the term has no standardized geological meaning. Very rarely do mountains occur individually. In most cases, they are found in elongated ranges or chains. When an array of such ranges is linked together, it constitutes a mountain belt&#x201d;</italic> (<ext-link ext-link-type="uri" xlink:href="https://www.britannica.com/science/mountain-landform">https://www.britannica.com/science/mountain-landform</ext-link>). Mountain areas play an essential role in shaping climate and the origin of the large majority of rivers. Also, they have an important influence in the surrounding areas through nutrient runoff and biotic interaction. Mountains are also hotspots and cradles for biodiversity and provide many ecosystem services (ES) essential for humans. Between 400-900 million humans live or depend partly or entirely on mountains (<xref ref-type="bibr" rid="B200">Sayre <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B184">Rahbek <italic>et al.,</italic> 2019a</xref>; <xref ref-type="bibr" rid="B172">Perrigo <italic>et al.,</italic> 2020</xref>). Although mountains are harsh environments, there are multiple records that they have been occupied since pre-historical times and served as an important source of resources and shelter for the humans in America (e.g., <xref ref-type="bibr" rid="B9">Arkush &amp; Arkush, 2021</xref>), Africa (e.g., <xref ref-type="bibr" rid="B175">Phillips <italic>et al.,</italic> 2019</xref>), Asia (e.g., <xref ref-type="bibr" rid="B74">Heydari-Guran &amp; Ghasidian, 2020</xref>), Europe (e.g., <xref ref-type="bibr" rid="B128">Mazzucco <italic>et al.,</italic> 2019</xref>), and Oceania (<xref ref-type="bibr" rid="B213">Slack <italic>et al.,</italic> 2018</xref>). In several mountain areas, humans developed strategies to adapt to rough environments (e.g., terraces) (e.g., <xref ref-type="bibr" rid="B107">Lasanta <italic>et al.,</italic> 2017</xref>). </p>
			<p>It is well known that, mountains provide a multitude of ES (e.g., carbon sequestration, air quality purification, water provisioning, food, recreation) (e.g., <xref ref-type="bibr" rid="B64">Gr&#xea;t-Regamey <italic>et al.,</italic> 2012</xref>; <xref ref-type="bibr" rid="B117">Liu <italic>et al.,</italic> 2019</xref>; <xref ref-type="bibr" rid="B65">Gr&#xea;t-Regamey &amp; Weibel, 2020</xref>). However, they are among the most fragile ecosystems, and several reports highlighted that they are extremely vulnerable to climate change (e.g., <xref ref-type="bibr" rid="B83">Iglesias <italic>et al.,</italic> 2018</xref>). Some biophysical systems started a process of adaptation, as highlighted in <xref ref-type="bibr" rid="B239">Vij <italic>et al.</italic> (2021)</xref>. For instance, according to the latest <xref ref-type="bibr" rid="B84">IPCC (2021)</xref> report, mountain glaciers retreat has been unprecedented in the last 2000 years. Also, the changes in snow cover and the earlier onset of spring melt is changing rivers streamflow seasonality, ecosystem dynamics and water supply in low altitude areas. Permafrost and mountain glaciers are expected to melt for decades or hundreds of years. The permafrost degradation and glacier melting in mountain areas increase slopes instability, and the formation of glacial lakes increases the risk of landslides and glacial lakes outburst floods. Precipitation extremes are expected to rise in all the scenarios in mountain regions, triggering floods and landslides. The temperature changes are also expected to affect mountain habitats, and in recent decades a tremendous change in species abundance and composition has been identified. </p>
			<p>Human pressures in mountains and profound socio-economic changes are affecting ecosystems equilibrium. Activities such as mining (e.g., <xref ref-type="bibr" rid="B21">Bokar <italic>et al.,</italic> 2020</xref>), massive tourism (e.g., <xref ref-type="bibr" rid="B147">Nepal <italic>et al.,</italic> 2020</xref>), intensive agriculture expansion (e.g., <xref ref-type="bibr" rid="B173">Peters <italic>et al.,</italic> 2019</xref>) have a dramatic impact on the ecosystems. On the other hand, mountain areas are suffering from rural exodus in several regions of the world. The abandonment of these areas is changing unprecedently semi-natural habitats created by millennial human activities. Although some benefits from this dynamic are recognised (e.g., rewilding, biodiversity conservation), negative implications occur as well (e.g., loss of semi-natural grassland ecosystems, wildfire risk increase) (e.g., <xref ref-type="bibr" rid="B75">Hinojosa <italic>et al.,</italic> 2019</xref>; <xref ref-type="bibr" rid="B57">Garc&#xed;a-Ruiz <italic>et al.,</italic> 2020</xref>). These socio-economic and environmental changes have a substantial implication on ES supply (<xref ref-type="bibr" rid="B169">Pereira, 2020</xref>). Therefore, it is critical to understand and identify the biotic and abiotic ES supplied by mountain areas and the drivers of change that can affect their quantity and quality. This perspective article aims to assess the regulating, provisioning and cultural ES supplied in mountain areas and the effects of a changing environment.</p>
		</sec>
		<sec id="sec2">
			<label>2.</label>
			<title>Regulating Ecosystem Services</title>
			<p>Mountains have a different climate from the surrounding land. The altitude and the complex topography affect weather, climate, plant and animal distribution, even at small scales (e.g., <xref ref-type="bibr" rid="B86">J&#xe4;hnig <italic>et al.,</italic> 2020</xref>). Therefore, the biodiversity in these environments is high when compared to lowland areas. Even though mountains occupy approximately 30% of the terrestrial area, they host more than 85% of the diversity of mammals, birds and amphibians (<xref ref-type="bibr" rid="B185">Rahbek <italic>et al.,</italic> 2019b</xref>). This high biodiversity is only possible due to the habitat&#x2019;s quality and the presence of well preserved and forests. Several works found that mountain forests have a high capacity for carbon sequestration (global and local climate regulation) (e.g., <xref ref-type="bibr" rid="B210">Sil <italic>et al.,</italic> 2017</xref>; <xref ref-type="bibr" rid="B219">Stritih <italic>et al.,</italic> 2021</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>), and this can be different according to the slope aspect. For instance, <xref ref-type="bibr" rid="B222">Swetnam <italic>et al.</italic> (2017)</xref> found that in the Rocky Mountains (The USA), the carbon storage capacity was higher in the north-facing slopes than in the southern. Similar results were also identified by <xref ref-type="bibr" rid="B52">Fravolini <italic>et al.</italic> (2018)</xref> in the Mediterranean mountains. These differences can also be identified in different mountain ecosystems. For example, forests have a higher capacity than grasslands to store carbon (<xref ref-type="bibr" rid="B260">Yu <italic>et al.,</italic> 2020</xref>). Others found that the implementation of measures that reduce fire risk and increase biodiversity in mountain areas of Ger&#xea;s-Xur&#xe9;s (Portugal and Spain) would be key for carbon sequestration in the long term (<xref ref-type="bibr" rid="B161">Pais <italic>et al.,</italic> 2020</xref>). On the other hand, <xref ref-type="bibr" rid="B203">Seidl <italic>et al.</italic> (2019)</xref> identified that unmanaged forests in the Alps have a high capacity for carbon sequestration and, therefore, climate regulation. Mountains with high biodiversity and forest cover have a high capacity for local and global climate regulation.</p>
			<fig-group id="f1">
					<fig>
						<label>Figure 1</label>
						<caption>
							<title>Mountain ecosystem services supply and the impact of the different drivers of change. </title>
						</caption>
						<graphic id="gra-1" xlink:href="Pirineos-177-e068-gf1.png"/>
					</fig>
					<fig xml:lang="es">
						<label>Figura 1</label>
						<caption>
							<title>Oferta de servicios ecosist&#xe9;micos de monta&#xf1;a e impacto de los diferentes impulsores de cambio.</title>
						</caption>
					</fig>
				</fig-group>
			<p>Vegetation can capture particulate matter (10 and 2.5 mm) and pollutants from the atmosphere (<xref ref-type="bibr" rid="B171">Pereira <italic>et al.,</italic> 2022</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>). Therefore it is expected that forest mountain areas located near cities can reduce air pollution. Most of the studies carried out were focused on urban trees or urban forests (e.g., <xref ref-type="bibr" rid="B258">Yli-Pelkonen <italic>et al.,</italic> 2017</xref>; <xref ref-type="bibr" rid="B153">Nowak <italic>et al.,</italic> 2018</xref>). Few studies were conducted in green areas located in mountain environments using measured data or models (<xref ref-type="bibr" rid="B135">Mengist <italic>et al.,</italic> 2020</xref>). However, <xref ref-type="bibr" rid="B88">Ji-Young <italic>et al.</italic> (2017)</xref> found that in the Gongju City (Korea), the surrounding forests located had a high capacity to capture pollutants. Evergreen coniferous had a high capacity to remove pollutants than evergreen forests. More studies have been developed about the social perception of the role of mountain forests in air purification. However, the results are not conclusive, and some showed that this ES is highly valued (e.g., <xref ref-type="bibr" rid="B72">He <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B167">Pedraza <italic>et al.,</italic> 2020</xref>), while others are not (<xref ref-type="bibr" rid="B165">Paudyal <italic>et al.,</italic> 2018</xref>). </p>
			<p>Mountain forests can filter and regulate water flow (e.g., <xref ref-type="bibr" rid="B120">Locatelli <italic>et al.,</italic> 2017</xref>; <xref ref-type="bibr" rid="B149">Ngwenya <italic>et al.,</italic> 2019</xref>; <xref ref-type="bibr" rid="B122">Ma <italic>et al.,</italic> 2021</xref>), controlling the water quality and quantity that reach the water bodies (<xref ref-type="fig" rid="f1">Figure 1</xref>). They reduce the sediment transport significantly and sustain the fragile mountain soils. Forests are a key for mountains soil conservation, as observed in several works (e.g., <xref ref-type="bibr" rid="B207">Sheng <italic>et al.,</italic> 2017</xref>; <xref ref-type="bibr" rid="B255">Xiao <italic>et al.,</italic> 2017</xref>). This high capacity to retain water and regulate flow is key to reducing peak flow and decreasing the probability of flash floods and landslides after high-intensity precipitation events (e.g., <xref ref-type="bibr" rid="B165">Paudyal <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B31">Costache <italic>et al.,</italic> 2020</xref>; <xref ref-type="bibr" rid="B79">Huber <italic>et al.,</italic> 2020</xref>). Forested catchments can reduce the flood peak from 3 to 70%, especially in small and medium-sized floods (<xref ref-type="bibr" rid="B246">Wahren <italic>et al.,</italic> 2012</xref>). Also, in natural forests, surface microrelief contributes to increasing water retention and decreasing runoff (<xref ref-type="bibr" rid="B237">Valtera &amp; Schaetzl, 2017</xref>). Mountain areas are also known to host a high diversity of pollinators (e.g., <xref ref-type="bibr" rid="B143">Naeem <italic>et al.,</italic> 2020</xref>; <xref ref-type="bibr" rid="B17">Baumann <italic>et al.,</italic> 2021</xref>), essential to agricultural production and the function of rural communities. </p>
		</sec>
		<sec id="sec3">
			<label>3.</label>
			<title>Ecosystem Services Provisioning</title>
			<p>Mountain supply a vast array of food, such as mushrooms, cash crops, berries, vegetables, spices and medicinal plants (<xref ref-type="bibr" rid="B132">McLellan &amp; Brown, 2017</xref>; <xref ref-type="bibr" rid="B234">Ulloa-Mu&#xf1;oz <italic>et al.,</italic> 2020</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>). Other animal-based products are produced from these areas, such as meat, oils, fats, milk, cheese, fish, and shellfish (<xref ref-type="bibr" rid="B125">Martins &amp; Ferreira, 2017</xref>). Numerous works highlight the high capacity of mountain areas for crops, livestock, wild food, and fish supply (e.g., <xref ref-type="bibr" rid="B99">Kokkoris <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B45">Faccione <italic>et al.,</italic> 2019</xref>). Also, they provide a basic income to mountain communities as observed elsewhere (e.g., <xref ref-type="bibr" rid="B209">Shrestha <italic>et al.,</italic> 2019</xref>). Due to the high diversity and food quality, several certification schemes were developed to label mountain regional products and increase consumer trust. This is key to improving mountain rural areas&#x2019; livelihood and sustainability (<xref ref-type="bibr" rid="B127">Mazzocchi &amp; Sali, 2022</xref>). Timber and biomass for energy are also important ES supplied by mountains (e.g., <xref ref-type="bibr" rid="B66">Gurung <italic>et al.,</italic> 2021</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>). In several areas is still one of the most important sources of local communities&#x2019; income and is highly valued in the Alps (<xref ref-type="bibr" rid="B63">Gori <italic>et al.,</italic> 2018</xref>), Carpathians (<xref ref-type="bibr" rid="B134">Melnykovych <italic>et al.,</italic> 2018</xref>), Himalayas (<xref ref-type="bibr" rid="B59">Gentle &amp; Marseni, 2012</xref>) and Africa - Burundi (<xref ref-type="bibr" rid="B145">Ndayizeye <italic>et al.,</italic> 2020</xref>). Mountains are environments that have the highest capacity to provide freshwater. They act as natural water towers and supply approximately 60 to 80% of world freshwater (<ext-link ext-link-type="uri" xlink:href="https://www.fao.org/mountain-partnership/our-work/focusareas/water/en/">https://www.fao.org/mountain-partnership/our-work/focusareas/water/en/</ext-link>). Mountains as water towers are critical in semi-arid and arid areas and have an essential role in supplying water for agriculture, industry, and the growing urban population (<xref ref-type="bibr" rid="B242">Viviroli &amp; Weingartner, 2008</xref>). For instance, approximately 1.5 billion people living in lowlands depend on mountain freshwater (<xref ref-type="bibr" rid="B243">Viviroli <italic>et al.,</italic> 2020</xref>). </p>
			<p>The high presence of water and sloped terrain make mountains key environments for producing hydropower energy. Since ancestral times, humans used water energy (e.g., water mill) to mill cereals and represented an important energy source for rural communities (e.g., <xref ref-type="bibr" rid="B205">Serrano &amp; Gonz&#xe1;lez-Amuchastegui, 2020</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>). Nowadays, hydropower supplies more than 16% of the total electricity production. This energy type is the primary renewable energy resource and is expected to increase in the future (<xref ref-type="bibr" rid="B20">Bilgili <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B82">IEA, 2019</xref>). Mountains also have a high potential to supply wind energy. The wind blows with high velocity in high altitude and high roughness areas (e.g., mountain corridors), therefore, several wind farms were established (e.g., <xref ref-type="bibr" rid="B156">&#xd3;lafsd&#xf3;ttir &amp; S&#xe6;&#xfe;&#xf3;rsd&#xf3;ttir, 2019</xref>; <xref ref-type="bibr" rid="B32">Cunden <italic>et al.,</italic> 2020</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>). After hydropower, wind energy is the energy that contributes the most to renewables production (<xref ref-type="bibr" rid="B82">IEA, 2019</xref>). Several projects have been developed in mountain areas to produce solar energy (e.g., <xref ref-type="bibr" rid="B95">Karpi&#x107; <italic>et al.,</italic> 2019</xref>; <xref ref-type="bibr" rid="B89">Kahl <italic>et al.,</italic> 2019</xref>), which are an option to be considered in the context of the rising energy demand. For instance, solar energy production in the mountains can be 20% higher than at sea level (<ext-link ext-link-type="uri" xlink:href="https://www.fao.org/mountain-partnership/our-work/focusareas/renewableenergy/en/">https://www.fao.org/mountain-partnership/our-work/focusareas/renewableenergy/en/</ext-link>). Solar energy is the highest contributor to renewables production after hydropower and wind energy (<xref ref-type="bibr" rid="B82">IEA, 2019</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>). Finally, in mountainous volcanic areas, there is a great potential for the production of geothermal energy (<xref ref-type="fig" rid="f1">Figure 1</xref>). Worldwide, there are several areas where this type of energy is extensively explored, such as in Iceland (e.g., <xref ref-type="bibr" rid="B216">Spittler <italic>et al.,</italic> 2020</xref>), New Zealand (e.g., <xref ref-type="bibr" rid="B103">Kumar <italic>et al.,</italic> 2021</xref>), United States (e.g., <xref ref-type="bibr" rid="B148">Neves <italic>et al.,</italic> 2021</xref>), Japan (<xref ref-type="bibr" rid="B224">Taghizadeh-Hesary <italic>et al.,</italic> 2020</xref>) and Italy (<xref ref-type="bibr" rid="B168">Pellizzone <italic>et al.,</italic> 2017</xref>). There is an increasing trend of geothermal exploitation (<ext-link ext-link-type="uri" xlink:href="https://www.irena.org/geothermal">https://www.irena.org/geothermal</ext-link>). Geothermal energy, after hydropower, wind energy and solar energy, is the one that contributes more to the total renewable energy production (<xref ref-type="bibr" rid="B82">IEA, 2019</xref>). </p>
			<p>Since historical times, mountain areas have been an essential source of mineral resources such as bronze, iron and gold (e.g., <xref ref-type="bibr" rid="B123">Mariet <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B232">Tolksdorf <italic>et al.,</italic> 2020</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>). More recently, other vital minerals were exploited in the mountains, which are the primary resources for many countries such as diamonds, coal and other raw materials (e.g., Lithium, Tungsten, Cobalt) (e.g., <xref ref-type="bibr" rid="B189">Redondo-Vega <italic>et al.,</italic> 2017</xref>; <xref ref-type="bibr" rid="B2">Ahiakwo <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B71">He <italic>et al.,</italic> 2020</xref>). According to <xref ref-type="bibr" rid="B155">OECD (2015)</xref>, due to human demand, mineral resources are expected to increase. </p>
		</sec>
		<sec id="sec4">
			<label>4.</label>
			<title>Cultural Ecosystem Services</title>
			<p>Mountains are essential areas for recreation and tourism during the different seasons and attract between 15 to 20% of global tourists (<ext-link ext-link-type="uri" xlink:href="https://www.fao.org/mountain-partnership/our-work/focusareas/sustainable-tourism/en/">https://www.fao.org/mountain-partnership/our-work/focusareas/sustainable-tourism/en/</ext-link>). These activities are vital to the economy of several communities is expected to increase in the future (<xref ref-type="bibr" rid="B252">World Tourism Organization, 2018</xref>). For instance, mountains during the winter have a high capacity for skiing activities (e.g., snowboard, skating) during the winter and walking, trekking, biking, rock climbing, paragliding, rafting in spring, summer and autumn (e.g., <xref ref-type="bibr" rid="B139">Mutana &amp; Mukwada 2018</xref>; <xref ref-type="bibr" rid="B151">Noome &amp; Fitchett, 2019</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>). In several mountain environments (e.g., Pyrenees), it is also popular to pick berries and mushrooms (e.g., <xref ref-type="bibr" rid="B134">Melnykovych <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B53">Fuste-Forne, 2020</xref>). Mountain areas are also well known for their high landscape aesthetic value (<xref ref-type="bibr" rid="B73">Hermes <italic>et al.,</italic> 2018</xref>) and are a popular place for sight-seeing, photography or wild animal watching (e.g., <xref ref-type="bibr" rid="B106">Larm <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B85">Ito, 2021</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>). For instance, several mountain areas are considered sacred areas for many indigenous cultures in the Himalayas (<xref ref-type="bibr" rid="B22">Brandt <italic>et al.,</italic> 2013</xref>), Andean (<xref ref-type="bibr" rid="B191">Reinhard, 1985</xref>), Mongolia (<xref ref-type="bibr" rid="B214">Sneath, 2014</xref>), Japan (<xref ref-type="bibr" rid="B131">McGuire, 2013</xref>), North America (<xref ref-type="bibr" rid="B208">Shipek, 1985</xref>) and Norway (<xref ref-type="bibr" rid="B140">Myrvoll, 2017</xref>), therefore with a very high value for spirituality. Since ancestral times, for protection or the abundance of resources, numerous civilizations were developed in mountain areas, some of them reaching a high stage of development (e.g., Incas) (e.g., <xref ref-type="bibr" rid="B62">Gonzales &amp; Bauer, 2021</xref>). Mountain areas are rich in many archaeological sites that are part of our cultural heritage and diversity (e.g., <xref ref-type="bibr" rid="B60">Giannakopoulou &amp; Kaliampakos, 2020</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>). In Europe, one of the good examples is the agricultural terraces that are good evidence of human adaptation to harsh environments for food production (<xref ref-type="bibr" rid="B23">Brown <italic>et al.,</italic> 2021</xref>). Important archaeological sites classified as UNESCO heritage sites are located in mountain areas, such as Historic Sanctuary of Machu Picchu (Peru), Phnom Kulen (Cambodia), Prehistoric Rock Art Sites in the C&#xf4;a Valley and Siega Verde (Portugal), Sacri Monti of Piedmont and Lombardy (Italy) and Archaeological Site of Delphi (Greece) (<ext-link ext-link-type="uri" xlink:href="https://whc.unesco.org/en/list/">https://whc.unesco.org/en/list/</ext-link>). Finally, mountain areas are excellent laboratories to develop cutting edge research and to understand important phenomena such as climate change (e.g., glacier dynamics, <xref ref-type="bibr" rid="B12">Bach <italic>et al.,</italic> 2018</xref>; vegetation processes, <xref ref-type="bibr" rid="B56">Garc&#xed;a-Ruiz <italic>et al.,</italic> 2015</xref>), pre-historical human development (e.g., <xref ref-type="bibr" rid="B38">Dreslerov&#xe1; et al., 2020</xref>), the interaction between past climate change and human expansion, i.e., agriculture and mining (e.g., lake sediments/pollen, <xref ref-type="bibr" rid="B192">Rey et al., 2017</xref>), land degradation (e.g., overgrazing, <xref ref-type="bibr" rid="B235">Umuhoza <italic>et al.,</italic> 2021</xref>) or land abandonment (e.g., rural exodus/vegetation encroachment, <xref ref-type="bibr" rid="B141">Nadal-Romero <italic>et al.,</italic> 2021</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>).</p>
		</sec>
		<sec id="sec5">
			<label>5.</label>
			<title>Drivers of change impacts on ecosystem services</title>
			<p>Drivers of change are defined as any action from humans (e.g., land-use change, political decisions) or natural (e.g., earthquakes, volcanic eruptions) origin that can affect directly or indirectly the ecosystems dynamic. These disturbances can positively or negatively impact the ecosystems (<xref ref-type="bibr" rid="B136">Mik&#x161;a <italic>et al.,</italic> 2020</xref>; <xref ref-type="bibr" rid="B169">Pereira, 2020</xref>). Mountains are subjected to several drivers of change that can dramatically alter ecosystems and their capacity to supply ES in quality and quantity, such as habitat change, climate change, overexploitation, pollution and invasive species. These drivers of change can act alone or combined, increasing the capacity to change the ecosystems (<xref ref-type="bibr" rid="B169">Pereira, 2020</xref>). </p>
			<sec id="sec5.1">
				<label>5.1.</label>
				<title>Habitat change</title>
				<p>Habitat change has been dramatic in some mountain environments and occurs in different forms (e.g., urban and agricultural expansion/land abandonment) (<xref ref-type="fig" rid="f1">Figure 1</xref>). The drivers of change imposed by recreation and tourism are changing mountains dramatically (e.g., land-use change, habitat fragmentation, conflicts with wildlife, noise, air and soil pollution, greenhouse gas emissions, land degradation, i.e., erosion). This has been observed in the Alps (e.g.; <xref ref-type="bibr" rid="B159">Orsi <italic>et al.,</italic> 2020</xref>), Pyrenees (e.g., <xref ref-type="bibr" rid="B13">Badoque <italic>et al.,</italic> 2017</xref>), Himalayas (e.g., <xref ref-type="bibr" rid="B256">Yang <italic>et al.,</italic> 2021</xref>), Tatra mountains (<xref ref-type="bibr" rid="B50">Fidelus-Orzechowska <italic>et al.,</italic> 2021</xref>), to mention some. For instance, Skiing resorts development has a detrimental impact on soil properties, vegetation distribution, biodiversity (<xref ref-type="bibr" rid="B80">Hudek <italic>et al.,</italic> 2020</xref>), geomorphological features (<xref ref-type="bibr" rid="B253">Wro&#x144;ska-Wa&#x142;ach <italic>et al.,</italic> 2019</xref>) and wildlife (<xref ref-type="bibr" rid="B218">Stott <italic>et al.,</italic> 2019</xref>). Another popular activity that is changing mountain habitats is mountaineering (e.g., climbing, trekking, hiking, biking) (<xref ref-type="bibr" rid="B8">Apollo, 2021</xref>). Several works highlighted that the climbers, hikers and bikers are altering land relief and soil (e.g., soil erosion), vegetation and grazers behaviour, animal feeding grounds, and increasing trail degradation, litter and excrement pollution (e.g., <xref ref-type="bibr" rid="B7">Apollo &amp; Andreychouk, 2020</xref>; <xref ref-type="bibr" rid="B44">Evju <italic>et al.,</italic> 2021</xref>). Although recreation and tourism activities are beneficial for local economies, retain people in rural areas and favour the development of outdoor activities important for human wellbeing (<xref ref-type="bibr" rid="B69">Hanna <italic>et al.,</italic> 2019</xref>), there are important tradeoffs associated with the loss of regulating ES, such as global and local climate regulation (<xref ref-type="bibr" rid="B34">Delgado <italic>et al.,</italic> 2007</xref>), air quality regulation, water purification, flow and nutrient regulation (e.g., <xref ref-type="bibr" rid="B193">Ristic <italic>et al.,</italic> 2012</xref>), natural hazards regulation (<xref ref-type="bibr" rid="B10">Arnaud-Fassetta <italic>et al.,</italic> 2005</xref>) and pollination (e.g., grassland flora diversity, <xref ref-type="bibr" rid="B11">Bacchiocchi <italic>et al.,</italic> 2019</xref>). The expansion of ski resorts has a strong impact on the conversion of grasslands and agricultural areas to the urban fabric, decreasing the capacity of these ecosystems to supply biomass for energy and food (<xref ref-type="bibr" rid="B58">Garc&#xed;a-Ruiz &amp; Lasanta, 1993</xref>; <xref ref-type="bibr" rid="B229">Theobald <italic>et al.,</italic> 1996</xref>), respectively. Also, negative impacts were identified on the local cultural activities (<xref ref-type="bibr" rid="B176">Pickering <italic>et al.,</italic> 2003</xref>). </p>
				<p>In several mountains of the world, such as in the Peruvian Andes (<xref ref-type="bibr" rid="B233">Tovar <italic>et al.,</italic> 2013</xref>), Ethiopian highlands (<xref ref-type="bibr" rid="B98">Kidane <italic>et al.,</italic> 2012</xref>) or Thailand (<xref ref-type="bibr" rid="B28">Choenkwan <italic>et al.,</italic> 2014</xref>), the pressure for food security and increasing market demand, are increasing the agriculture area expansion. The agriculture intensification in mountain areas can be profitable in the short term regarding food production and can support recreation and tourism activities. Nevertheless, agriculture intensification may have negative impacts on the ecosystems capacity to regulate the climate and the air quality (e.g., <xref ref-type="bibr" rid="B24">Cai <italic>et al.,</italic> 2019</xref>), water purification, flow, erosion and nutrients (e.g., <xref ref-type="bibr" rid="B197">Rukundo <italic>et al.,</italic> 2018</xref>), natural hazards (e.g., <xref ref-type="bibr" rid="B43">Erena &amp; Worku, 2018</xref>) and pollination (e.g., <xref ref-type="bibr" rid="B194">Ritten <italic>et al.,</italic> 2018</xref>). Although there has been observed a trend in the increase of mountain areas agriculture, others have been affected by land abandonment, a complex socio-ecological phenomenon observed in several mountain areas of Europe (<xref ref-type="bibr" rid="B108">Lasanta <italic>et al.,</italic> 2017</xref>) and Asia (<xref ref-type="bibr" rid="B67">Han &amp; Song 2019</xref>). Land abandonment imposes an important disturbance in mountain ecosystems, which can have positive or negative impacts. Associated with land abandonment is the rewilding process that favours several regulating ES such as global and local climate regulation, through the increase of carbon sequestration (e.g., <xref ref-type="bibr" rid="B18">Bell <italic>et al.,</italic> 2020</xref>) and water purification, erosion and nutrient regulation (e.g., <xref ref-type="bibr" rid="B119">Lizaga <italic>et al.,</italic> 2018</xref>) and biomass for energy and timber (e.g., <xref ref-type="bibr" rid="B178">Pitman &amp; Peace, 2021</xref>). As a consequence of vegetation encroachment, there is an increase in plant water consumption, evapotranspiration, consumption and storage. This reduces water flow and the quantity of water that reaches rivers (<xref ref-type="bibr" rid="B97">Khorchani <italic>et al.,</italic> 2021</xref>) and aquifers (<xref ref-type="bibr" rid="B160">Ouyang <italic>et al.,</italic> 2021</xref>). Afforestation reduces the probability of flash floods and landslides (e.g., <xref ref-type="bibr" rid="B37">Dittrich <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B77">Hu <italic>et al.,</italic> 2021</xref>). On the other hand, land abandonment and vegetation encroachment increase the fuel available and risk wildfire occurrence (<xref ref-type="bibr" rid="B162">Palaiologou <italic>et al.,</italic> 2017</xref>). Regarding the impacts of land abandonment/afforestation on natural hazards regulation, there is an important tradeoff between flood/landslides mitigation and wildfire risk. To mitigate this, it is essential to establish fuel management policies (e.g., prescribed fires) to reduce fire risk without compromising flood regulation (<xref ref-type="bibr" rid="B170">Pereira <italic>et al.,</italic> 2021</xref>). Land abandonment decreases the capacity of mountain areas to provide food. In this process, traditions, cultural activities and landscapes are lost (e.g., <xref ref-type="bibr" rid="B68">Hana&#x10d;ek &amp; Rodr&#xed;guez-Labajos, 2018</xref>). For instance, one of the most evident impacts is the agricultural terraces destruction due to lack of maintenance (<xref ref-type="bibr" rid="B217">Stavi <italic>et al.,</italic> 2018</xref>). The destruction of these structures can trigger soil, water losses, floods and landslides (e.g., <xref ref-type="bibr" rid="B137">Moreno-de-las-Heras <italic>et al.,</italic> 2019</xref>). </p>
				<p>Dam construction for hydropower production dramatically impacts freshwater habitats fragmentation, river ecological function and thermal regimes, nutrient and sediment flux and biodiversity loss (<xref ref-type="bibr" rid="B245">Vuong Pham <italic>et al.,</italic> 2019</xref>; <xref ref-type="bibr" rid="B15">Barbarossa <italic>et al.,</italic> 2020</xref>). Although these infrastructures increase the amount of energy produced from renewable resources, they have profound impacts on fish spawning migratory routes and affect the communities that depend on this resource for food supply (<xref ref-type="bibr" rid="B39">Dugan <italic>et al.,</italic> 2010</xref>). Also, wind farms imposed a high disruption in the environment, and several works highlight that they disturb the natural habitats strongly and negatively affect the different trophic levels (e.g., <xref ref-type="bibr" rid="B228">Thaker <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B48">Fern&#xe1;ndez-Bellon <italic>et al.,</italic> 2019</xref>). These infrastructures have negative impacts on recreation and tourism (<xref ref-type="bibr" rid="B156">&#xd3;lafsd&#xf3;ttir &amp; S&#xe6;&#xfe;&#xf3;rsd&#xf3;ttir, 2019</xref>), landscape aesthetics, noise (<xref ref-type="bibr" rid="B90">Kalinauskas <italic>et al.,</italic> 2021</xref>) and cultural heritage (<xref ref-type="bibr" rid="B144">Nazir <italic>et al.,</italic> 2020</xref>). Finally, as the previous renewable energy resources, solar energy may impose a negative impact on habitats loss and reduce the habitats for pollinators (e.g., <xref ref-type="bibr" rid="B129">McCoshum &amp; Geber, 2020</xref>) and landscape aesthetics (e.g., visual quality) (<xref ref-type="bibr" rid="B36">Dhar <italic>et al.,</italic> 2020</xref>). </p>
			</sec>
			<sec id="sec5.2">
				<label>5.2.</label>
				<title>Climate change</title>
				<p>Climate change (e.g., glacier melting, extreme events, and drought periods) negatively affects mountain ecosystems and their capacity to supply services (<xref ref-type="fig" rid="f1">Figure 1</xref>). Although all ES are predicted to be affected, the most relevant impacts are expected in global and local climate regulation, natural hazards regulation, crops, wild food and fish provisioning, freshwater provisioning, renewable energy, recreation and tourism, landscape aesthetics and cultural heritage and cultural diversity (<xref ref-type="bibr" rid="B163">Palomo, 2017</xref>; <xref ref-type="bibr" rid="B78">Hua <italic>et al.,</italic> 2021</xref>). </p>
				<p>Mountain ecosystems are highly vulnerable to small changes in the climate (e.g., <xref ref-type="bibr" rid="B83">Iglesias <italic>et al.,</italic> 2018</xref>) and, therefore, to ecosystem change (e.g., tree-line upward) (<xref ref-type="bibr" rid="B26">Cazzolla Gatti <italic>et al.,</italic> 2019</xref>). This will likely affect carbon sequestration (global and local climate regulation) (<xref ref-type="bibr" rid="B78">Hua <italic>et al.,</italic> 2021</xref>). As a consequence of glacier and permafrost melting and increase in extreme events, natural hazards (e.g., flash floods, landslides, rockfall) are expected to be more frequent and severe (e.g., <xref ref-type="bibr" rid="B227">Terzi <italic>et al.,</italic> 2019</xref>; <xref ref-type="bibr" rid="B238">Viani <italic>et al.,</italic> 2020</xref>). The increase of wildfires frequency can amplify the high vulnerability to natural hazards, severity and recurrence in a climate change context (e.g., <xref ref-type="bibr" rid="B223">Taboada <italic>et al.,</italic> 2017</xref>; <xref ref-type="bibr" rid="B25">Cassell <italic>et al.,</italic> 2019</xref>). High temperatures and the prevalence of long and frequent drought periods are expected to increase the vulnerability to wildfires. Severe and recurrent wildfires are the ones that impose more ecosystems damage and affect drastically the ecosystems capacity to recover. Therefore, the expected increase of severe wildfires may trigger other natural hazards such as flash floods (e.g., <xref ref-type="bibr" rid="B150">Nolan <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B30">Coscarelli <italic>et al.,</italic> 2021</xref>). </p>
				<p>The alteration of temperature and precipitation patterns due to climate change will affect the water availability (e.g., glacier melting, reduced snow cover, drought periods) for food production in mountain communities (e.g., <xref ref-type="bibr" rid="B180">Poudel &amp; Duex, 2017</xref>), but also in lowland areas that depend on water from glacier and snow melting to irrigate their fields (<xref ref-type="bibr" rid="B81">Huss <italic>et al.,</italic> 2017</xref>). Also, climate change impact on ecosystems shift will affect the distribution of wild foods such as berries (<xref ref-type="bibr" rid="B181">Prev&#xe9;y <italic>et al.,</italic> 2020</xref>) and mushrooms (<xref ref-type="bibr" rid="B257">Yang <italic>et al.,</italic> 2012</xref>). This impact on mushrooms productivity in some mountain ranges (e.g., Prades Mountains, Catalonia-Spain) will be negative (<xref ref-type="bibr" rid="B94">Karavani <italic>et al.,</italic> 2018</xref>). Climate change will also affect adversely mountain grasslands (e.g., afforestation) (<xref ref-type="bibr" rid="B201">Schirpke <italic>et al.,</italic> 2017</xref>). The sensitivity to climate change increases with the increasing altitude (<xref ref-type="bibr" rid="B114">Li <italic>et al.,</italic> 2019a</xref>), which will have implications on their capacity to supply food for cattle. </p>
				<p>Climate change is also expected to negatively impact hydropower energy, mainly due to the snow and ice cover decrease and the reduced glacier volumes that will negatively affect runoff and energy production. These harmful impacts are mainly identified in dry areas, such as central Asia or the tropical Andes, where runoff volume depends on glacier melting (<xref ref-type="bibr" rid="B81">Huss <italic>et al.,</italic> 2017</xref>). Decreases in hydropower production were also observed in other regions such as California (<xref ref-type="bibr" rid="B51">Forrest <italic>et al.,</italic> 2018</xref>), Brazil (<xref ref-type="bibr" rid="B158">Oliveira <italic>et al.,</italic> 2017</xref>) or Portugal (<xref ref-type="bibr" rid="B226">Teot&#xf3;nio <italic>et al.,</italic> 2017</xref>). On the other hand, in regions where precipitation is expected to be high (e.g., Three Gorges Reservoir - China), hydropower energy will increase (<xref ref-type="bibr" rid="B183">Qin <italic>et al.,</italic> 2020</xref>). </p>
				<p>Climate change has a negative and positive impact on mountain recreation and tourism. Winter sports will be negatively affected by the decreasing number of days with snow and ice cover (e.g., <xref ref-type="bibr" rid="B46">Fang <italic>et al.,</italic> 2021</xref>). Several solutions have been established to tackle this problem, such as show snowmaking. However, this solution increases energy and water demand (<xref ref-type="bibr" rid="B195">Rixen <italic>et al.,</italic> 2011</xref>) and has negative impacts on mountain ecosystems (<xref ref-type="bibr" rid="B253">Wro&#x144;ska-Wa&#x142;ach <italic>et al.,</italic> 2019</xref>). Glacier tourism is also being affected since most mountain glaciers are disappearing, bringing substantial losses to this industry (<xref ref-type="bibr" rid="B247">Wang &amp; Zhou, 2019</xref>). Other phenomena related to climate change, such as the wildfire risk increase, discourage tourists from travelling to these areas (<xref ref-type="bibr" rid="B170">Pereira <italic>et al.,</italic> 2021</xref>). However, mountain tourism can benefit during heatwave periods, where people can look for refuges in high altitude areas. Finally, climate change and the impacts on seasonality can affect the time when tourists visit mountain areas (<xref ref-type="bibr" rid="B163">Palomo, 2017</xref>). </p>
				<p>The disappearance of mountain glaciers decreases landscape aesthetics since tourists highly appreciate this landscape, as observed in previous works (e.g., <xref ref-type="bibr" rid="B249">Welling <italic>et al.,</italic> 2020</xref>; <xref ref-type="bibr" rid="B198">Salim <italic>et al.,</italic> 2021</xref>). The increasing wildfire frequency will decrease temporarily landscape quality and the attractiveness of these areas to be visited (<xref ref-type="bibr" rid="B170">Pereira <italic>et al.,</italic> 2021</xref>). Around the world, several mountain landscapes are sacred for different communities located in the Meili Snow Mountains of Yunnan (China), Nepalese Himalaya, Peruvian Andes, Alaska or Canada. The loss of these glaciers will have a detrimental impact on the communities living in these areas (<xref ref-type="bibr" rid="B5">Allison, 2015</xref>; <xref ref-type="bibr" rid="B230">Thornton <italic>et al.,</italic> 2019</xref>). </p>
			</sec>
			<sec id="sec5.3">
				<label>5.3.</label>
				<title>Overexploitation</title>
				<p>Mountain environments are subjected to high overexploitation, threatening biodiversity and ES supply (<xref ref-type="fig" rid="f1">Figure 1</xref>). For instance, hunting and poaching practices cause biodiversity loss in some mountainous areas (e.g., <xref ref-type="bibr" rid="B1">Adhikari <italic>et al.,</italic> 2021</xref>). The mineral resources demand increases the landslides, debris flow, collapse, and ground deformation and subsidence, with severe implications for the populations living in lowland areas (<xref ref-type="bibr" rid="B206">Shao, 2019</xref>). Mineral exploitation imposes a high degradation in the areas where they are established by removing soil and vegetation, drastically hampering these ecosystems&#x2019; capacity to supply regulating, cultural and other provisioning services (e.g., food, freshwater). Overall, these activities impose a high ES value loss (<xref ref-type="bibr" rid="B33">Dawen <italic>et al.,</italic> 2018</xref>). </p>
				<p>Overgrazing is another threat to regulating (e.g., global and local climate regulation, water purification, flow, erosion and nutrient regulation, pollination) and provisioning (e.g., food for livestock) ES (<xref ref-type="fig" rid="f1">Figure 1</xref>). This has been identified in several mountain areas of Ethiopia (<xref ref-type="bibr" rid="B133">Mekonen, 2020</xref>), China (<xref ref-type="bibr" rid="B70">Hao <italic>et al.,</italic> 2018</xref>), Greece (<xref ref-type="bibr" rid="B49">Fetzel <italic>et al.,</italic> 2018</xref>) and Central Asia (<xref ref-type="bibr" rid="B152">Nowak <italic>et al.,</italic> 2020</xref>), to mention some. For instance, overgrazing reduces the grassland capacity to store carbon (e.g., <xref ref-type="bibr" rid="B263">Zhou <italic>et al.,</italic> 2020</xref>), grassland biodiversity (e.g., <xref ref-type="bibr" rid="B152">Nowak <italic>et al.,</italic> 2020</xref>), increases soil and nutrient loss (e.g., <xref ref-type="bibr" rid="B262">Zheng <italic>et al.,</italic> 2017</xref>; <xref ref-type="bibr" rid="B115">Li <italic>et al.,</italic> 2019b</xref>) and reduce pollinators abundance (<xref ref-type="bibr" rid="B142">Naeem <italic>et al.,</italic> 2019</xref>). Mountain Forest overexploitation (e.g., timber production) is also a reality in several environments (e.g., <xref ref-type="bibr" rid="B166">Payne <italic>et al.,</italic> 2020</xref>), imposing a degradation in the capacity of these ecosystems to regulate global and local climate, air quality (<xref ref-type="bibr" rid="B188">Rawat <italic>et al.,</italic> 2021</xref>), water purification, flow, erosion and nutrient regulation (e.g., <xref ref-type="bibr" rid="B146">Negash <italic>et al.,</italic> 2021</xref>), natural hazards and pollination. It also negatively impacts non-timber products (e.g., <xref ref-type="bibr" rid="B215">Soe &amp; Yeo-Chang, 2019</xref>), landscape aesthetics, and cultural heritage (e.g., <xref ref-type="bibr" rid="B261">Zeb <italic>et al.,</italic> 2019</xref>) since several of these areas are considered sacred. </p>
				<p>Agriculture intensification in mountain environments also implies a natural resources overexploitation (e.g., water), and it is responsible for soil quality degradation (e.g., <xref ref-type="bibr" rid="B244">von Westarp <italic>et al.,</italic> 2004</xref>), changes in pedogenesis process (<xref ref-type="bibr" rid="B225">Tang <italic>et al.,</italic> 2019</xref>), erosion (<xref ref-type="bibr" rid="B250">West <italic>et al.,</italic> 2015</xref>) and deforestation (<xref ref-type="bibr" rid="B138">Munwar &amp; Udelhoven, 2020</xref>). Although agriculture intensification and resources overexploitation may have some short-term positive impact on food production, it has crucial tradeoffs related to global and local climate, air quality and regulation (<xref ref-type="bibr" rid="B4">Ali <italic>et al.,</italic> 2017</xref>), water purification, flow, erosion and nutrient regulation (<xref ref-type="bibr" rid="B120">Locatelli <italic>et al.,</italic> 2017</xref>), pollination (<xref ref-type="bibr" rid="B29">Christmann <italic>et al.,</italic> 2021</xref>), freshwater supply (<xref ref-type="bibr" rid="B196">Rolando <italic>et al.,</italic> 2017</xref>), recreation and tourism (<xref ref-type="bibr" rid="B120">Locatelli <italic>et al.,</italic> 2017</xref>), landscape aesthetics and cultural heritage (<xref ref-type="bibr" rid="B3">Albizua <italic>et al.,</italic> 2019</xref>). Mass tourism expansion increases overexploitation (e.g., <xref ref-type="bibr" rid="B55">Ganie <italic>et al.,</italic> 2019</xref>; <xref ref-type="bibr" rid="B126">Mateusz, 2021</xref>). For instance, unregulated tourism harms the overexploitation of medicinal plants (<xref ref-type="bibr" rid="B55">Ganie <italic>et al.,</italic> 2019</xref>), fuelwood (<xref ref-type="bibr" rid="B105">Laiolo <italic>et al.,</italic> 2004</xref>) and water (<xref ref-type="bibr" rid="B212">Singh <italic>et al.,</italic> 2020</xref>) in the Himalaya. In the Mediterranean mountains, mass tourism is causing an increase in groundwater exploitation (<xref ref-type="bibr" rid="B182">Pulido-Bosch <italic>et al.,</italic> 2020</xref>). </p>
			</sec>
			<sec id="sec5.4">
				<label>5.4.</label>
				<title>Pollution</title>
				<p>Mining activities are responsible for high levels of soil and water resources pollution (in the site and off-site) in several mountains of the world, located in Asia (e.g., <xref ref-type="bibr" rid="B248">Wang <italic>et al.,</italic> 2019</xref>), North America (e.g., <xref ref-type="bibr" rid="B111">Lemly, 2019</xref>), Europe (e.g., <xref ref-type="bibr" rid="B104">Kupkov&#xe1; <italic>et al.,</italic> 2018</xref>), Africa (e.g., <xref ref-type="bibr" rid="B96">Khelifi <italic>et al.,</italic> 2021</xref>) and Australia (e.g., <xref ref-type="bibr" rid="B4">Ali <italic>et al.,</italic> 2017</xref>) (<xref ref-type="fig" rid="f1">Figure 1</xref>). The overexploitation of mineral resources is one of the most important causes of land degradation (<xref ref-type="bibr" rid="B54">Gabarr&#xf3;n <italic>et al.,</italic> 2019</xref>). Mining harms all the biotic ES 1) regulating (global and local climate; air quality; natural hazards; pollination) and 2) provisioning (crops, livestock, wild food and fish, biomass for energy and timber and freshwater) since mining exploitation involves vegetation and soil removal (e.g., <xref ref-type="bibr" rid="B109">Lee <italic>et al.,</italic> 2017</xref>; <xref ref-type="bibr" rid="B187">Rajan, 2019</xref>) and increase waterbodies pollution (e.g., <xref ref-type="bibr" rid="B199">Santana <italic>et al.,</italic> 2020</xref>). Also, the mining industry affected negatively cultural heritage in several countries (e.g., Ghana and Western Australia) (<xref ref-type="bibr" rid="B6">Apoh <italic>et al.,</italic> 2017</xref>). Paradox to the above mentioned, there is a growing interest in preserving old mines as part of cultural landscape and history in some regions (e.g., <xref ref-type="bibr" rid="B164">Pardo Abad <italic>et al.,</italic> 2017</xref>). </p>
				<p>Agriculture intensification increases soil and water pollution (e.g., agrochemicals, microplastics) (<xref ref-type="bibr" rid="B42">Ennaji <italic>et al.,</italic> 2020</xref>; <xref ref-type="bibr" rid="B47">Feng <italic>et al.,</italic> 2021</xref>), and this has been observed in several mountain areas (e.g., <xref ref-type="bibr" rid="B254">Wu <italic>et al.,</italic> 2020</xref>; <xref ref-type="bibr" rid="B113">Li <italic>et al.,</italic> 2021</xref>). Although some benefits are obtained from crop production, agriculture intensification and the impacts on soil are decreasing their capacity to regulate nutrients, and there are high losses through overland flow (e.g., <xref ref-type="bibr" rid="B220">Strohmenger <italic>et al.,</italic> 2020</xref>). It is also well known that agrochemicals harm plants flowering and pollinators (e.g., <xref ref-type="bibr" rid="B40">Dupont <italic>et al.,</italic> 2018</xref>), reduce freshwater quality (e.g., <xref ref-type="bibr" rid="B121">Loecke <italic>et al.,</italic> 2017</xref>) and decrease the waterbodies capacity to supply fish due to diffuse pollution (e.g., <xref ref-type="bibr" rid="B61">Godinho <italic>et al.,</italic> 2019</xref>). </p>
				<p>The development of tourist infrastructures in mountain areas increases the pollution and greenhouse gases emission (<xref ref-type="bibr" rid="B87">Jamnongchob <italic>et al.,</italic> 2017</xref>) due road development, traffic increase (<xref ref-type="bibr" rid="B221">Sundriyal <italic>et al.,</italic> 2018</xref>), infrastructure construction, waste production (<xref ref-type="bibr" rid="B204">Semernya <italic>et al.,</italic> 2017</xref>) and litter in wildland environments (<xref ref-type="bibr" rid="B76">Hu <italic>et al.,</italic> 2018</xref>). Although for the region, this can represent an increase in recreation and tourism activities. It will have important tradeoffs on other ES such as air quality regulation, pollination and freshwater supply (<xref ref-type="bibr" rid="B221">Sundriyal <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B91">Kamel, 2020</xref>). </p>
			</sec>
			<sec id="sec5.5">
				<label>5.5.</label>
				<title>Invasive species</title>
				<p>Invasive species in mountain environments are a consequence of multiple human impacts such as land-use change (e.g., plantations), nitrogen deposition and tourism development (e.g., infrastructure development) (<xref ref-type="fig" rid="f1">Figure 1</xref>). Other aspects such as the herbivores abundance, pests and diseases, wildfires or landslides have implications on plants distribution. Climate change has direct (e.g., productivity, competitive balance, phenology) and indirect (e.g., changes in hydrological regime) impacts on plant distribution. Although the invasive species spread in mountain areas is not so easy as in other ecosystems due to climate conditions, when alien species pass this filter, it is complicated to manage and reverse their spread due to the complex topography. Invasive species in mountain environments is a global phenomenon and are mostly of agricultural origin (<xref ref-type="bibr" rid="B130">McDougall <italic>et al.,</italic> 2010</xref>, 2011; <xref ref-type="bibr" rid="B102">Kueffer <italic>et al.,</italic> 2013</xref>). </p>
				<p>For instance, the proliferation of <italic>Eucalyptus</italic> spp. (a native specie from Australia) for timber production in several mountains of the world has dramatic impacts on the environment. This specie is planted in all the continents i.e., Africa (<xref ref-type="bibr" rid="B177">Piiroinen <italic>et al.,</italic> 2018</xref>), America (<xref ref-type="bibr" rid="B41">Dur&#xe1;n <italic>et al.,</italic> 2017</xref>), Europe (<xref ref-type="bibr" rid="B157">Oliveira &amp; Tome, 2017</xref>) and Asia (<xref ref-type="bibr" rid="B27">Chen <italic>et al.,</italic> 2021</xref>). <italic>Eucalyptus</italic> ssp. plantations are well known to have a high-water consumption than the native forests (<xref ref-type="bibr" rid="B251">White <italic>et al.,</italic> 2021</xref>), reduce biodiversity (<xref ref-type="bibr" rid="B35">Deus <italic>et al.,</italic> 2018</xref>), increase soil degradation (<xref ref-type="bibr" rid="B14">Banfield <italic>et al.,</italic> 2018</xref>) and the vulnerability to wildfire risk (<xref ref-type="bibr" rid="B154">Nunes, 2012</xref>). Rubber, palm oil plantations are other invasive species that cause high land degradation in mountain areas (e.g., <xref ref-type="bibr" rid="B110">Leite <italic>et al.,</italic> 2018</xref>; <xref ref-type="bibr" rid="B240">Vijith <italic>et al.,</italic> 2018</xref>).</p>
				<p>Tourism development is an important cause of plant invasion. For example, hiking trails and roadsides are considered major paths of alien plants spread in mountain areas (<xref ref-type="bibr" rid="B116">Liedtke <italic>et al.,</italic> 2020</xref>). Also, the introduction of species of fish (<xref ref-type="bibr" rid="B231">Tiberti <italic>et al.,</italic> 2019</xref>) and herbivores (<xref ref-type="bibr" rid="B124">Mart&#xed;n-Esquivel <italic>et al.,</italic> 2020</xref>) in high lands dramatically impact native fauna. There are several examples where the introduction of non-native herbivores leads to a very high environmental degradation (e.g., sheep in Iceland, <xref ref-type="bibr" rid="B16">Barrio <italic>et al.,</italic> 2018</xref>). </p>
				<p>Finally, climate change is expected to increase invasive species spread in mountain areas. However, this is a more serious problem in low land areas. Since mountain areas have a harsh climate, the alien species spread is difficult. However, climate change may favour the environmental conditions required for non-native species that affect high altitudes (<xref ref-type="bibr" rid="B174">Petitpierre <italic>et al.,</italic> 2016</xref>). In addition, as mentioned previously, with climate change, it is expected that wildfires will be more severe and frequent, increasing the risk for plant invasion, as observed in previous works (e.g., <xref ref-type="bibr" rid="B190">Reilly <italic>et al.,</italic> 2020</xref>). </p>
				<p>Several studies have been developed about the impact of invasive species on ES (e.g., <xref ref-type="bibr" rid="B241">Vil&#xe0; &amp; Hulme, 2017</xref>; <xref ref-type="bibr" rid="B186">Rai &amp; Singh, 2020</xref>). There are several tradeoffs involved in the impacts of invasive species in mountain environments. Forest plantations can have some benefits in the production of biomass for energy and timber. However, they have a low capacity to regulate global and local climate than native forests (<xref ref-type="bibr" rid="B259">Yu <italic>et al.,</italic> 2019</xref>). Therefore, the establishment of non-native species plantations cannot be considered an advantage. Plantations affect the capacity of the ecosystem dramatically to regulate water flow, erosion and nutrients - mainly in young plantations - (e.g., <xref ref-type="bibr" rid="B118">Liu <italic>et al.,</italic> 2017</xref>), pollination (<xref ref-type="bibr" rid="B179">Potts <italic>et al.,</italic> 2010</xref>), freshwater supply (<xref ref-type="bibr" rid="B112">Le&#xf3;n-Mu&#xf1;oz <italic>et al.,</italic> 2017</xref>) and recreation and tourism (<xref ref-type="bibr" rid="B19">Benra <italic>et al.,</italic> 2019</xref>). Climate change impact on invasive species is expected to affect native pollinators negatively (e.g., <xref ref-type="bibr" rid="B202">Schweiger <italic>et al.,</italic> 2010</xref>; <xref ref-type="bibr" rid="B211">Silva <italic>et al.,</italic> 2021</xref>). </p>
			</sec>
		</sec>
		<sec id="sec6" sec-type="conclusions">
			<label>6.</label>
			<title>Conclusion</title>
			<p>Mountains ecosystems are key for human existence and provide many biotic and abiotic ES to the local communities and lowland inhabitants. Although these environments can be inhospitable and challenging to colonise, humans have developed strategies oaf adaptation and established flourishing civilisations in mountain areas throughout history. The ES supply by these environments is immense, though their exploitation can produce different tradeoffs. The excessive exploitation of one determined ES (e.g., mining) can trigger a cascade of adverse effects in all the other ES. Therefore, to maintain the continuous ES supply in quantity and quality, it is vital to rationalising all ES&#x2019;s exploitation to reach the necessary equilibrium in utilising mountain resources. Sustainable approaches are needed in the ES management in mountain environments. This is a challenge for our and future generations.</p>
		</sec>
	</body>
	<back>
		<ack>
			<title>Acknowledgments</title>
			<p>This work was developed within the Lithuanian National Ecosystem Services Assessment and Mapping (LINESAM), which has received funding from European Social Fund project LINESAM no. 09.3.3-LMT-K-712-01-0104 under a grant agreement with the Research Council of Lithuania (LMTLT). Further, we would like to express gratitude to Marius Kalinauskas for providing the photo used in the figure 1.</p>
		</ack>
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