Geodiversity in Khorat Geopark, Thailand: Approaches to geoconservation and sustainable development

Jaroon Duangkrayom , Pratueng Jintasakul , Wickanet Songtham , Parichat Kruainok , Wilailuck Naksri , Nattinee Thongdee , Paul J. Grote , Tharapong Phetprayoon , Krongkaew Janjitpaiboon , Rapeepan Meepoka
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引用次数: 2

Abstract

This work aims to investigate the geodiversity of the Khorat Geopark area, Northeastern Thailand, and assess the geological sites that are connected to biological and cultural heritage, as well as community activities that enhance geoconservation and sustainable development. The geological diversity of Khorat Geopark dates back to the late Jurassic period and continues to the present day, resulting from the deposition of terrestrial sedimentary rocks from the Khorat Group. The Khorat rock group has been uplifted and eroded to form the Khorat Plateau with a unique landscape and important geological features of the cuesta landform on the western part of the Khorat Geopark. On the four corners of Nakhon Ratchasima City, there are numerous fossils of outstanding Early Cretaceous dinosaurs and other reptiles and Cenozoic fossils of both flora and fauna, mainly mammalian remains and, in particular, ancient elephants. Geological sites in the Khorat Geopark area were weighted and scored based on their scientific value (SV), potential value for education (EV), potential value for tourism (TV), and degradation risk variables (DV). According to the assessment, the Khorat Geopark's 24 geosites are of moderate to high value, with 7 sites having 301–400 scores and 5 sites having a high level of international value. Most of them are related to fossils and cuestas. Thus, the fossil diversity of the Khorat Geopark is of international scientific significance. Khorat Geopark is managed under the conservation, education, and sustainable development initiatives using a bottom-up method with multiple networks, both local communities and local governments, especially through the Home-Temple-School (HTS) model.

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泰国呵叻地质公园的地质多样性:地质保护和可持续发展的途径
这项工作旨在调查泰国东北部呼叻地质公园地区的地质多样性,评估与生物和文化遗产有关的地质遗址,以及加强地质保护和可持续发展的社区活动。可拉特地质公园的地质多样性可以追溯到侏罗纪晚期,并一直持续到今天,这是由于可拉特群陆相沉积岩的沉积造成的。呼拉特岩群被抬升和侵蚀,形成了呼拉特高原,具有独特的景观和重要的地质特征,是呼拉特地质公园西部的cuesta地貌。在那空叻差玛城的四角,有许多杰出的早白垩世恐龙化石和其他爬行动物化石,以及新生代动植物化石,主要是哺乳动物遗骸,特别是古代大象。根据科学价值(SV)、潜在教育价值(EV)、潜在旅游价值(TV)和退化风险变量(DV)对呼拉特地质公园区域内的地质遗址进行加权评分。根据评价结果,呼拉特地质公园共有24处具有中高价值地质点,其中301-400分7处,国际高价值地质点5处。其中大部分与化石和化石有关。因此,呼拉特地质公园的化石多样性具有国际科学意义。可拉特地质公园在保护、教育和可持续发展倡议下进行管理,采用自下而上的方法,包括多个网络,包括当地社区和地方政府,特别是通过家庭-寺庙-学校(HTS)模式。
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来源期刊
International Journal of Geoheritage and Parks
International Journal of Geoheritage and Parks Social Sciences-Urban Studies
CiteScore
6.70
自引率
0.00%
发文量
43
审稿时长
72 days
期刊最新文献
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