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1

Kramer, Terrill J. "Great Basin National Park: Rationales, Concepts, and Conflicts." Yearbook of the Association of Pacific Coast Geographers 53, no. 1 (1991): 7–34. http://dx.doi.org/10.1353/pcg.1991.0004.

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Ports, Mark A. "Terrestrial Mollusks of Great Basin National Park, the Snake Range, Nevada, USA." Western North American Naturalist 79, no. 2 (2019): 247. http://dx.doi.org/10.3398/064.079.0210.

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3

Carter, Owen, Bradley Kropp, Nastassja Noell, et al. "A Preliminary Checklist of the Lichens in Great Basin National Park, Nevada, USA." Evansia 36, no. 3 (2019): 72. http://dx.doi.org/10.1639/0747-9859-36.3.72.

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4

Šebela, Stanka, Gretchen Baker, and Barbara Luke. "Cave Temperature and Management Implications in Lehman Caves, Great Basin National Park, USA." Geoheritage 11, no. 3 (2019): 1163–75. http://dx.doi.org/10.1007/s12371-019-00367-0.

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5

Houston, Derek D., R. Paul Evans, Jared M. Crowley, and Dennis K. Shiozawa. "Genetic Characterization of Two Populations of Bonneville Cutthroat Trout in Great Basin National Park, USA." Western North American Naturalist 75, no. 2 (2015): 146–56. http://dx.doi.org/10.3398/064.075.0203.

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6

Rickart, Eric A., Shannen L. Robson, and Lawrence R. Heaney. "Mammals Of Great Basin National Park, Nevada: Comparative Field Surveys and Assessment Of Faunal Change." Monographs of the Western North American Naturalist 4, no. 1 (2008): 77–114. http://dx.doi.org/10.3398/1545-0228-4.1.77.

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7

Harris, Thomas R., Jeffrey E. Englin, Shawn W. Stoddard, Thomas R. MacDiarmid, and Gary M. Veserat. "AN ANALYSIS OF VISITATION POTENTIAL AND CORRESPONDING ECONOMIC IMPACTS OF THE GREAT BASIN NATIONAL PARK." Community Development Society. Journal 27, no. 2 (1996): 248–60. http://dx.doi.org/10.1080/15575339609489810.

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8

Szabo, Barney J. "Ages of Travertine Deposits in Eastern Grand Canyon National Park, Arizona." Quaternary Research 34, no. 1 (1990): 24–32. http://dx.doi.org/10.1016/0033-5894(90)90070-2.

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AbstractTravertine deposits in eastern Grand Canyon National Park, Arizona, are inferred to have formed under conditions of effective wetness that were greater than present. Uranium-series dating of 17 samples indicates that the deposits formed at about 15,000, 71,000, 111,000, 171,000, and 338,000 yr B.P. Intervals of travertine deposition are essentially contemporaneous with dated high paleolake levels, montane glacial maxima, and high paleowater-table levels from several Great Basin localities.
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Neff, Keil J., John S. Schwartz, Stephen E. Moore, and Matt A. Kulp. "Influence of basin characteristics on baseflow and stormflow chemistry in the Great Smoky Mountains National Park, USA." Hydrological Processes 27, no. 14 (2012): 2061–74. http://dx.doi.org/10.1002/hyp.9366.

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10

Hamilton, Bryan T., Steve E. Moore, Tod B. Williams, Neal Darby, and Mark R. Vinson. "Comparative Effects of Rotenone and Antimycin on Macroinvertebrate Diversity in Two Streams in Great Basin National Park, Nevada." North American Journal of Fisheries Management 29, no. 6 (2009): 1620–35. http://dx.doi.org/10.1577/m08-178.1.

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Finlayson, Brian J., Rosalie Schnick, Don Skaar, et al. "Comment: Comparative Effects of Rotenone and Antimycin on Macroinvertebrate Diversity in Two Streams in Great Basin National Park, Nevada." North American Journal of Fisheries Management 30, no. 5 (2010): 1126–28. http://dx.doi.org/10.1577/m09-202.1.

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VanCuren, Richard (Tony), and Mae Sexauer Gustin. "Identification of sources contributing to PM2.5 and ozone at elevated sites in the western U.S. by receptor analysis: Lassen Volcanic National Park, California, and Great Basin National Park, Nevada." Science of The Total Environment 530-531 (October 2015): 505–18. http://dx.doi.org/10.1016/j.scitotenv.2015.03.091.

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13

Hamilton, Bryan T., Steve E. Moore, Tod B. Williams, Neal Darby, and Mark R. Vinson. "Comparative Effects of Rotenone and Antimycin on Macroinvertebrate Diversity in Two Streams in Great Basin National Park, Nevada: Response to Comment." North American Journal of Fisheries Management 30, no. 5 (2010): 1129–31. http://dx.doi.org/10.1577/m10-026.1.

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14

Will, Kipling, Riva Madan, and Han Hsu. "Additions to the knowledge of Nevada carabid beetles (Coleoptera: Carabidae) and a preliminary list of carabids from the Great Basin National Park." Biodiversity Data Journal 5 (June 13, 2017): e12250. http://dx.doi.org/10.3897/bdj.5.e12250.

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15

SHEAR, WILLIAM A. "Cave millipeds of the United States. V. The genus Idagona Buckett & Gardner (Chordeumatida, Conotylidae, Idagoninae)." Zootaxa 1463, no. 1 (2007): 1–12. http://dx.doi.org/10.11646/zootaxa.1463.1.1.

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The conotylid milliped subfamily Idagoninae presently includes but a single genus and species, Idagona westcotti Buckett & Gardner, known from lava tubes in Idaho, USA. This study presents new records of the genus Idagona, extending its distribution into Utah and Nevada, its habitat records to limestone caves, and describes two additional species, Idagona lehmanensis, n. sp., from limestone caves in the Great Basin National Park in eastern Nevada, and Idagona jasperi, n. sp., from a high-altitude limestone cave in northern Utah.
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16

Reinemann, Scott A., David F. Porinchu, Amy M. Bloom, Bryan G. Mark, and Jason E. Box. "A multi-proxy paleolimnological reconstruction of Holocene climate conditions in the Great Basin, United States." Quaternary Research 72, no. 3 (2009): 347–58. http://dx.doi.org/10.1016/j.yqres.2009.06.003.

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AbstractA sediment core spanning ∼ 7000 cal yr BP recovered from Stella Lake, a small sub-alpine lake located in Great Basin National Park, Nevada, was analyzed for subfossil chironomids (non-biting midges), diatoms, and organic content (estimated by loss-on-ignition (LOI)). Subfossil chironomid analysis indicates that Stella Lake was characterized by a warm, middle Holocene, followed by a cool “Neoglacial” period, with the last two millennia characterized by a return to warmer conditions. Throughout the majority of the core the Stella Lake diatom-community composition is dominated by small, p
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Stern, Marc J., Robert B. Powell, Kevin D. McLean, Emily Martin, Jennifer M. Thomsen, and Bethany A. Mutchler. "The Difference between Good Enough and Great: Bringing Interpretive Best Practices to Life." Journal of Interpretation Research 18, no. 2 (2013): 79–100. http://dx.doi.org/10.1177/109258721301800205.

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The purpose of this paper is to illuminate in both a quantitative and qualitative sense the practices that distinguish great interpretive programs from those that may merely be adequate to satisfy the visitor's basic desires to learn, be entertained, or spend time with a ranger. Great programs, like great works of art, have the potential to impact audiences in a deeper sense by providing memorable experiences that may influence multiple aspects of visitors’ lives. This paper draws on experiences from three months of fieldwork, observing 376 interpretive programs across 24 units of the U.S. Nat
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Goy, José Luis, Raquel Cruz, Antonio Martínez-Graña, Virginia Valdés, and Mariano Yenes. "Geomorphological Map and Quaternary Landscape Evolution of the Monfragüe Park (Cáceres, Spain)." Sustainability 12, no. 23 (2020): 10099. http://dx.doi.org/10.3390/su122310099.

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From the geomorphological cartography, the geometric and spatial distribution of the quaternary forms and deposits are analyzed, with special relevance to the fluvial terraces that allow obtaining the chronology of the successive landscape changes of the course of the Tagus River attributed to the activity of the Fault of Alentejo-Plasencia (APF). The “Appalachian” relief of Monfragüe National Park, constituting a series of quartzitic combs with direction NW, between which they find slopes, hills and valleys following the same direction, for the dismantlement of the Cenozoic cover that was cov
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19

Becraft, Eric D., Jeremy A. Dodsworth, Senthil K. Murugapiran, et al. "Single-Cell-Genomics-Facilitated Read Binning of Candidate Phylum EM19 Genomes from Geothermal Spring Metagenomes." Applied and Environmental Microbiology 82, no. 4 (2015): 992–1003. http://dx.doi.org/10.1128/aem.03140-15.

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ABSTRACTThe vast majority of microbial life remains uncatalogued due to the inability to cultivate these organisms in the laboratory. This “microbial dark matter” represents a substantial portion of the tree of life and of the populations that contribute to chemical cycling in many ecosystems. In this work, we leveraged an existing single-cell genomic data set representing the candidate bacterial phylum “Calescamantes” (EM19) to calibrate machine learning algorithms and define metagenomic bins directly from pyrosequencing reads derived from Great Boiling Spring in the U.S. Great Basin. Compare
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20

Belkayalı, Nur, and Miraç Aydın. "Küre Dağları Milli Parkı Su Kaynaklarının Rekreasyonel Amaçlı Kullanımı." Turkish Journal of Agriculture - Food Science and Technology 4, no. 10 (2016): 893. http://dx.doi.org/10.24925/turjaf.v4i10.893-902.962.

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Water is a basic need in order to survive all living beings. The functional use of water through the ages of living space formatted directed, has a significant influence on environmental design. In addition to the use of water for various purposes has refreshing climatic features, to create a living suitable environment for all living things and has the visual aesthetics features, to become an indispensable element in the landscape has provided. Despite the abundance of recreational activities, humans are mostly enjoyed water-based recreational activities. Water-based recreation is no doubt th
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21

Burgoyne, Jake, Robin Crepeau, Jacob Jensen, Hayden Smith, Gretchen Baker, and Steven D. Leavitt. "Lampenflora in a Show Cave in the Great Basin Is Distinct from Communities on Naturally Lit Rock Surfaces in Nearby Wild Caves." Microorganisms 9, no. 6 (2021): 1188. http://dx.doi.org/10.3390/microorganisms9061188.

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In show caves, artificial lighting is intended to illuminate striking cave formations for visitors. However, artificial lighting also promotes the growth of novel and diverse biofilm communities, termed lampenflora, that obtain their energy from these artificial light sources. Lampenflora, which generally consist of cyanobacteria, algae, diatoms, and bryophytes, discolor formations and introduce novel ecological interactions in cave ecosystems. The source of lampenflora community members and patterns of diversity have generally been understudied mainly due to technological limitations. In this
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22

Pilic, Sime, Ivanka Buzov, and Gorana Bandalovic. "Rural landscape and preservation of natural environment: Opinions and attitudes of examinees resident within Krka river basin." Sociologija 54, no. 1 (2012): 169–84. http://dx.doi.org/10.2298/soc1201169p.

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This paper includes the presentations of development perspectives of the villages along the right bank of the Krka river that are within, or on the edge of the Krka National park and the results of empirical research of the opinions and attitudes of the local population regarding the preservation and protection of the environment in this area. Using the survey method, we examined the opinions of the adult population of Krka river basin in the rural area of Skradin hinterland. The questions focused on a number of issues regarding preservation and/or threat to the environment. The research is a
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23

Dobek, Mateusz, and Marcin Kozieł. "Geocaching w Roztoczańskim Parku Narodowym." Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia 70, no. 2 (2016): 191. http://dx.doi.org/10.17951/b.2015.70.2.191.

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<p>Geocaching is a type of a field game, which consists in finding caches (ang. Cache) placed earlier in the area. Participants of the game find the approximate location of a hidden "treasure" basing on geographic coordinates and descriptions contained on the website and using GPS. Perceptiveness, creativity and unconventional thinking should be demonstrated to find a cache. There is a so called logbook in a hidden container in which its finding should be recorded, and then this fact must be confirmed on a special website (http://www.geocaching.com, http://www.geocaching.pl). Geocaching
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24

Esquivel M., Alberto, Salvador J. Peris, Rosendo Fraga, et al. "Status of the avifauna of San Rafael National Park, one of the last large fragments of Atlantic Forest in Paraguay." Bird Conservation International 17, no. 4 (2007): 301–17. http://dx.doi.org/10.1017/s095927090700086x.

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AbstractWe provide new information on all birds known from San Rafael National Park, Paraguay. Ornithological records from the period 1997 to 2006 have been reviewed, adding 112 new species to the reserve's avifauna. We provide data on the presence of 405 species in seven basic habitats types, and on their relative abundance. Biogeographically, San Rafael has a mixed avifauna, consisting of 70 Atlantic Forest endemic species, two Mesopotamian Grassland endemics, and many with a wider distribution in South America. At least 12 species are threatened and 16 near-threatened, including important p
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25

Samardzic, Ivan. "Limitations in development of planned and alternative types of tourism in the ”Stara planina” nature park and tourist region." Glasnik Srpskog geografskog drustva 94, no. 2 (2014): 15–30. http://dx.doi.org/10.2298/gsgd1402015s.

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Great Serbian natural resources can be used to develop tourism which follows the principles of sustainable development. Water resources: rivers, lakes, then spas, mountains, etc. can be used in the right way, for development of tourism, local community affirmation as well as the entire country, and of course with the appropriate investments and responsible policy development which can bring huge material use to the entire society. Stara Planina area has defined tourism with emphasis on winter tourism through the planning documents (development of ski centers and appropriate infrastructure). Al
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26

Ji, Zailiang, and Christopher R. Barnes. "Uppermost Cambrian and Lower Ordovician conodont biostratigraphy of the Survey Peak Formation (Ibexian/Tremadoc), Wilcox Pass, Alberta, Canada." Journal of Paleontology 70, no. 5 (1996): 871–90. http://dx.doi.org/10.1017/s0022336000023891.

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The Survey Peak Formation (350 m thick) consists of calcareous shale, mudstone, siltstone, and limestone-pebble conglomerate, and is formally divided into four revised members, successively: Basal Silty Member, Putty Shale Member, Middle Carbonate Member, and Upper Carbonate Member. The Wilcox Pass section, Jasper National Park, Alberta, provides a standard stratigraphic section for the southern Canadian Rocky Mountains and yielded over 4,500 conodonts from 87 samples which are of high species diversity, moderately well preserved, with a conodont Color Alteration Index (CAI) value of 3. Over 5
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Pearson, Ann, Yundan Pi, Weidong Zhao, et al. "Factors Controlling the Distribution of Archaeal Tetraethers in Terrestrial Hot Springs." Applied and Environmental Microbiology 74, no. 11 (2008): 3523–32. http://dx.doi.org/10.1128/aem.02450-07.

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ABSTRACT Glycerol dialkyl glycerol tetraethers (GDGTs) found in hot springs reflect the abundance and community structure of Archaea in these extreme environments. The relationships between GDGTs, archaeal communities, and physical or geochemical variables are underexamined to date and when reported often result in conflicting interpretations. Here, we examined profiles of GDGTs from pure cultures of Crenarchaeota and from terrestrial geothermal springs representing a wide distribution of locations, including Yellowstone National Park (United States), the Great Basin of Nevada and California (
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Mead, Jim I., Larry D. Agenbroad, Arthur M. Phillips, and Larry T. Middleton. "Extinct Mountain Goat (Oreamnos harringtoni) in Southeastern Utah." Quaternary Research 27, no. 3 (1987): 323–31. http://dx.doi.org/10.1016/0033-5894(87)90087-1.

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AbstractThe extinct Harrington's mountain goat (Oreamnos harringtoni Stock) is predominantly known from dry cave localities in the Grand Canyon, Arizona, in addition to two sites in the Great Basin, Nevada, and from San Josecito Cave, Nuevo Leon, Mexico. A dry shelter in Natural Bridges National Monument, on the central Colorado Plateau, southeastern Utah, preserves numerous remains of the extinct mountain goat in addition to pack rat middens. Remains from a 100-cm stratigraphic profile indicate that O. harringtoni lived on the plateau >39,800 yr B.P., the oldest directly dated find of exti
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Knezevic, Milan, Rajko Milosevic, and Olivera Kosanin. "Production potential of the soil and the basic elements of productivity of the most widely spred sessil types in the u. N.P. „Djerdap”." Bulletin of the Faculty of Forestry, no. 102 (2010): 57–67. http://dx.doi.org/10.2298/gsf1002057k.

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This paper is on the results of the soil and its production potential in the types of forests of sessile oaks (Quercus petraea) in the area of the National Park ?Djerdap? in the community units of Zlatica, Djerdap, Strbacko korito, Desna reka and Kozica. There are the most widely spread types of the sprout forests of the sessile oaks in the research area, deep deluvium, luvisoil, eutric cambsoils, and a great number of subtypes of acid brown soil. Considering the fact that the production potential of the defined types of soil depends on the depth, skeleton and other physical characteristics wh
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30

Barden, Lawrence S., and Margaret Lynn Brown. "Great Smoky Mountains National Park, 1900-2000." Ecology 82, no. 12 (2001): 3563. http://dx.doi.org/10.2307/2680175.

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31

Barden, Lawrence S. "Great Smoky Mountains National Park, 1900–2000." Ecology 82, no. 12 (2001): 3563–64. http://dx.doi.org/10.1890/0012-9658(2001)082[3563:gsmnp]2.0.co;2.

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32

Kennedy, B. M., J. H. Reynolds, S. P. Smith, and A. H. Truesdell. "Helium isotopes: Lower Geyser Basin, Yellowstone National Park." Journal of Geophysical Research 92, B12 (1987): 12477. http://dx.doi.org/10.1029/jb092ib12p12477.

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33

Jenkins, Michael A. "Vegetation Communities of Great Smoky Mountains National Park." Southeastern Naturalist 6, sp2 (2007): 35–56. http://dx.doi.org/10.1656/1528-7092(2007)6[35:vcogsm]2.0.co;2.

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34

POGUE, MICHAEL G. "The Plusiinae (Lepidoptera: Noctuidae) of Great Smoky Mountains National Park." Zootaxa 1032, no. 1 (2005): 1. http://dx.doi.org/10.11646/zootaxa.1032.1.1.

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Seventeen species of Plusiinae have been found in Great Smoky Mountains National Park, in Tennessee and North Carolina, USA. These species are documented with adult images, description, flight period, abundance, elevation range, Park and general distribution, and larval hosts from the literature. Maps illustrate the known distribution of each species within the Park. Sixteen of the 17 species occur above 4,000 feet in elevation. The most diverse locality in the Park has 14 species.
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Butler, Jack, and Frank Einhellig. "Exotic Plants in Theodore Roosevelt National Park." UW National Parks Service Research Station Annual Reports 15 (January 1, 1991): 211–16. http://dx.doi.org/10.13001/uwnpsrc.1991.3027.

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The primary objective of the first year of the project was to determine the number and distribution of exotic plant species within the park. A preliminary list of exotics was provided by park personal. A more complete list of exotics found in the park was then generated using Heidel's (1990) list of "Preliminary Vascular Flora of Theodore Roosevelt National Park". The origin of all of the plant species listed in that report were determined from Stevens (1963) and Flora of the Great Plains (Great Plains Association 1986).
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Skeat, A. J. "Wetland management — Kakadu National Park." Australian Journal of Environmental Education 2 (June 1986): 17–20. http://dx.doi.org/10.1017/s0814062600004353.

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AbstractThe wetlands of Kakadu National Park have received national and international recognition. Their significance lies in their large size, the great diversity and high biomass of plants and animals which they support, and the level of protection and management afforded them. The management of these wetlands is influenced by many factors including a uranium mine, a range of alien plants and animals, increasing tourism, an environment subject to change, and Aboriginal ownership of part of the land. Maintaining wetland conservation values appropriate to a major national park and a World Heri
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Vivian, Daniel J., and Daniel S. Pierce. "The Great Smokies: From Natural Habitat to National Park." Environmental History 6, no. 2 (2001): 331. http://dx.doi.org/10.2307/3985105.

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38

Shaver, Christine L., Kathy A. Tonnessen, and Tonnie G. Maniero. "Clearing the Air at Great Smoky Mountains National Park." Ecological Applications 4, no. 4 (1994): 690–701. http://dx.doi.org/10.2307/1942000.

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Linzey, Donald W. "Mammals of Great Smoky Mountains National Park: 2016 Revision." Southeastern Naturalist 15, no. m8 (2016): 1–93. http://dx.doi.org/10.1656/058.015.m801.

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Muise, Charles, Keith R. Langdon, Rebecca P. Shiflett, et al. "Checklist of Odonata from Great Smoky Mountains National Park." Southeastern Naturalist 6, sp2 (2007): 207–14. http://dx.doi.org/10.1656/1528-7092(2007)6[207:coofgs]2.0.co;2.

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Nelson, Diane R., and Bartels Paul J. "“Smoky Bears”—Tardigrades of Great Smoky Mountains National Park." Southeastern Naturalist 6, sp2 (2007): 229–38. http://dx.doi.org/10.1656/1528-7092(2007)6[229:sbogsm]2.0.co;2.

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42

PETERSEN, MATTHEW J., CHARLES R. PARKER, and ERNEST BERNARD. "The crane flies (Diptera: Tipuloidea) of Great Smoky Mountains National Park." Zootaxa 1013, no. 1 (2005): 1. http://dx.doi.org/10.11646/zootaxa.1013.1.1.

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The list of crane flies (Diptera: Ptychopteridae, Tipuloidea, Trichoceridae) known from Great Smoky Mountains National Park is updated. Sampling in association with the All Taxa Biodiversity Inventory of Great Smoky Mountains National Park resulted in the addition of 107 new Park records, bringing the current list to 250 species. This species assemblage is much richer than those of surrounding areas, although similar in composition. Total richness is estimated to be between 450 and 500 species for Great Smoky Mountains National Park.
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Grasby, Stephen E., Robert O. van Everdingen, Jan Bednarski, and Dwayne AW Lepitzki. "Travertine mounds of the Cave and Basin National Historic Site, Banff National Park." Canadian Journal of Earth Sciences 40, no. 11 (2003): 1501–13. http://dx.doi.org/10.1139/e03-058.

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The Cave and Basin National Historic Site is a fan-shaped travertine deposit associated with four thermal spring outlets. Tentative age dating of the travertine mound indicates growth initiated with onset of the late Holocene shift to more humid and cool climate conditions and suggests that the flow of thermal waters was limited during the Hypsithermal, which in turn places constraints on the evolutionary biology of endemic species in the spring system. Two large caves and one collapsed cave structure are developed within the deposit. Cave development is in response to both physical erosion of
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POGUE, MICHAEL G. "The Hadeninae (Lepidoptera: Noctuidae) of Great Smoky Mountains National Park, USA." Zootaxa 2380, no. 1 (2010): 1. http://dx.doi.org/10.11646/zootaxa.2380.1.1.

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Fifty-two species of Hadeninae are recorded from Great Smoky Mountains National Park, Tennessee and North Carolina, USA. Of the six hadenine tribes, five are present in the Park. They include 13 species of Orthosiini, one species of Tholerini, ten species of Hadenini, nine species of Leucaniini, and 19 species of Eriopygini. A total of 160 localities were collected across the Park. The three most diverse localities in the Park were Purchase Knob with 44 species, Big Cove Road with 32 species, and Foothills Parkway with 24 species. The most widespread species in the Park was Pseudorthodes vecor
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Getman, V. "NATIONAL NATURE PARK “DZHARYLGATSKYI”." Bulletin of Taras Shevchenko National University of Kyiv. Geography, no. 70-71 (2018): 50–53. http://dx.doi.org/10.17721/1728-2721.2018.70.8.

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National Natural Park (NPP) “Dzharylgatskyi” was established by Decree of the President of Ukraine from December 11, 2009, on the territory of Skadovsky district of Kherson region. This was preceded by the creation of Dzharylgatskyi botanical reserve of national importance in 1974. According to the physical-geographical zoning of Ukraine, the territory of the NPP “Dzharylgatskyi” refers to the Nizhnedneprovsky terraced-delta landscape of the Black Sea-Pryazovsky dry-steppe region. The main territorial area of the National Park “Dzharylgatskyi” is the Dzharylgach island with a narrow spit in it
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46

van Amerom, Marloes, and Bram Büscher. "Peace parks in Southern Africa: bringers of an African Renaissance?" Journal of Modern African Studies 43, no. 2 (2005): 159–82. http://dx.doi.org/10.1017/s0022278x05000790.

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The pursuit of an African Renaissance has become an important aspect of regional cooperation between South Africa and its neighbours. Transfrontier conservation areas, or ‘Peace Parks’ as they are popularly called, have been identified as key instruments to promote the African Renaissance dream, and are increasingly advocated and justified on this basis. By fostering joint conservation (and tourism) development in Southern Africa's marginalised border regions, Peace Parks are claimed to further international peace, regional cooperation and poverty reduction, and thus serve basic ideals of the
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47

Bernard, Ernest C., and Kelly L. Felderhoff. "Biodiversity Explosion: Collembola (Springtails) of Great Smoky Mountains National Park." Southeastern Naturalist 6, sp2 (2007): 175–82. http://dx.doi.org/10.1656/1528-7092(2007)6[175:becsog]2.0.co;2.

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48

FUNABIKI, Toshiaki, Ryuichi WAKISAKA, and Takahiro SASAKI. "National Memorial and Memorial Park of Great East Japan Earthquake." Journal of The Japanese Institute of Landscape Architecture 85, no. 1 (2021): 6–11. http://dx.doi.org/10.5632/jila.85.6.

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49

Stankovic, Stevan. "The Djerdap national park: The polyfunctional center of the Danube Basin." Geographica Pannonica, no. 6 (2002): 38–44. http://dx.doi.org/10.5937/geopan0206038s.

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50

Glasgow, Benny C., and Paula Pierce. "Freshwater Ribbon Worms (Nemertea) from the Great Smoky Mountains National Park." Journal of North Carolina Academy of Science 130, no. 2 (2014): 60–64. http://dx.doi.org/10.7572/2167-5880-130.2.60.

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Abstract Freshwater ribbon worms collected in the Great Smoky Mountains National Park from 9 June 2007 until 28 September 2010 are reported. All six specimens are identified as genus Prostoma. Species identification is not concluded and also no conclusion is made whether any of the specimens are of a new or undescribed species. Some specimen photographs are provided and a discussion is given on specimen characteristics and their possible identification. Ribbon worms are not previously reported in the Great Smoky Mountains National Park.
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