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Cherrapunji, India: a land of waterfalls and speleothems, and the right place to become a UNESCO Global Geopark 印度切拉蓬吉:瀑布和岩浆之地,成为联合国教科文组织全球地质公园的理想之地
Pub Date : 2024-11-26 DOI: 10.1111/gto.12497
Krishanu Datta

Here, I propose that Cherrapunji, one of the wettest places on the planet, should be a potential site as a UNESCO Global Geopark. This location is not only associated with numerous majestic waterfalls, karst topography and multiple natural caves and speleothems with global scientific value, but is also of great significance to local people. These features have made this place an important area for geoscience research, as well as an important area for the development of geotourism. Cherrapunji is also the source of the ‘Meghalayan Age’, the most recent age in the geological timescale, defined by the International Commission on Stratigraphy (ICS) in 2018, for the past 4200 years of the Holocene. This article calls on researchers, government officials as well as the local people to take all the necessary steps to make Cherrapunji a UNESCO Global Geopark.

在此,我建议将地球上最潮湿的地方之一 Cherrapunji 作为联合国教科文组织全球地质公园的潜在地点。这个地方不仅拥有众多雄伟的瀑布、喀斯特地貌和多个具有全球科学价值的天然洞穴和岩浆,而且对当地人民也具有重要意义。这些特点使这里成为地质科学研究的重要地区,也是发展地质旅游的重要地区。Cherrapunji 还是 "梅加拉亚时代 "的源头,"梅加拉亚时代 "是国际地层学委员会(ICS)于 2018 年为全新世过去 4200 年定义的地质年代表中的最新时代。本文呼吁研究人员、政府官员以及当地人民采取一切必要措施,将切拉蓬吉建成联合国教科文组织全球地质公园。
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引用次数: 0
Geodigest Geodigest
Pub Date : 2024-11-26 DOI: 10.1111/gto.12493
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引用次数: 0
Can a 62-million-year-old ‘hyperthermal’ event hold the clues to our uncertain future climate? 6200 万年前的 "高热 "事件能否为我们不确定的未来气候提供线索?
Pub Date : 2024-11-26 DOI: 10.1111/gto.12495
James Barnet

Climate change has been rising to an ever-increasing prominence in the news headlines in recent years, as local and global temperature records are obliterated, and extreme weather events occur with increasing frequency and severity. Preparing for an uncertain future climate represents one of the biggest challenges humans have ever faced. Here, I take you back 62 million years ago (Ma) to a poorly studied short-lived global warming event known as the Latest Danian Event (LDE), which may represent a good analogue for current human-induced climate change. I discuss evidence for changes in temperature and pH of the oceans during the LDE, using novel geochemical proxies on the calcite shells of zooplankton to prove that the LDE was the first global ‘hyperthermal’ event of the Cenozoic. I also delve into the potential forcing mechanisms behind the event, outlining the critical outstanding questions which palaeoclimatologists are yet to answer. Most importantly, I highlight the lessons we can learn from the LDE about our future climate, allowing us to better plan, prepare and adapt.

近年来,气候变化在新闻头条中的地位日益突出,当地和全球的气温记录荡然无存,极端天气事件发生的频率和严重程度也与日俱增。为不确定的未来气候做好准备,是人类有史以来面临的最大挑战之一。在这里,我将带您回到 6200 万年前(Ma)一个研究不足的短期全球变暖事件,即最新达尼安事件(LDE),它可能是当前人类引起的气候变化的一个很好的类比。我讨论了 LDE 期间海洋温度和 pH 值变化的证据,利用浮游动物方解石外壳上的新型地球化学代用指标证明 LDE 是新生代第一次全球 "过热 "事件。我还深入探讨了这一事件背后的潜在作用机制,概述了古气候学家尚未回答的关键问题。最重要的是,我强调了我们可以从 LDE 事件中吸取的有关未来气候的经验教训,以便我们更好地规划、准备和适应。
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引用次数: 0
Messages from the past: the petroglyphs of El Hierro Island, Canary Islands 来自过去的信息:加那利群岛埃尔希耶罗岛的岩画
Pub Date : 2024-11-26 DOI: 10.1111/gto.12496
Mario Guglielmi, Valentin R. Troll, Joerg Foest, Juan Carlos Carracedo

Ancient cultures have frequently made use of stone surfaces to carve and engrave symbols, letters and messages for others. These petroglyphs usually have a lasting character and are frequently preserved well beyond the survival of the culture that produced the petroglyphs. In this article, we focus on the written and pictorial testimony of the pre-Hispanic era of the island of El Hierro (Canary Islands, Spain), which exploited a series of volcanic rock features to create a written testimony of their presence and their way of life. This specific cultural heritage has been adapted to the specific geological features on the island and the emerging stone masonry skill of the aboriginal culture of the original islanders, creating a unique and lasting record of their ability to use geological elements for cultural development.

古代文化经常利用石头表面为他人雕刻符号、字母和信息。这些岩画通常具有持久的特征,其保存时间往往远远超过了产生岩画的文化的存续时间。在这篇文章中,我们将重点介绍埃尔希耶罗岛(西班牙加那利群岛)前西班牙时代的文字和图像见证,他们利用一系列火山岩地貌创造了他们存在和生活方式的文字见证。这种特殊的文化遗产适应了岛上特定的地质特征和原住民文化中新兴的石砌技术,为他们利用地质元素促进文化发展的能力创造了独特而持久的记录。
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引用次数: 0
Rock climbing sites as locations for geoheritage and geoscience engagement in mountains 作为山区地质遗产和地质科学参与地点的攀岩地点
Pub Date : 2024-11-26 DOI: 10.1111/gto.12494
Jasper Knight, Irene Maria Bollati

Outdoor activities including trekking and hiking are commonly undertaken in mountains and in other environments where bedrock surfaces or bedrock-controlled landforms are present and where users can enjoy the fresh air and the physical landscape. Information boards and leaflets are often used by scientists and environmental managers in these environments to communicate geoscience issues to the general public along hiking and trekking trails. Rock climbing sites are also prime locations where rock surfaces are exposed and where specific user groups interact with the physical landscape. Here, we describe the relationship between rock climbing and the nature of rock outcrops and the opportunity that this affords for more innovative ways of communicating geoscience information to a physically active and engaged public. As such, rock climbing sites can be considered geoheritage sites, where they represent sites of importance for people and communities (cultural heritage) as well as for their geological and educational value (geological heritage). The characteristics of rock climbing sites as geoheritage sites are discussed in this feature, as are the potential threats to the integrity of these sites.

包括徒步旅行和远足在内的户外活动通常在山区和其他存在基岩表面或基岩控制地貌的环境中进行,使用者可以享受新鲜空气和自然景观。在这些环境中,科学家和环境管理者经常使用信息板和传单向远足和徒步路径沿线的公众宣传地球科学问题。攀岩地点也是岩石表面裸露的主要地点,也是特定用户群体与自然景观互动的地方。在这里,我们将描述攀岩与岩石露头性质之间的关系,以及这为以更创新的方式向身体活跃、参与性强的公众传播地球科学信息提供的机会。因此,攀岩地点可被视为地质遗产地,它们代表着对人类和社区具有重要意义的地点(文化遗产),以及具有地质和教育价值的地点(地质遗产)。本专题讨论了攀岩地点作为地质遗产地的特点,以及对这些地点完整性的潜在威胁。
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引用次数: 0
Geology of the Tour de France: taking a sports audience by surprise 环法自行车赛的地质学:让体育观众大吃一惊
Pub Date : 2024-09-24 DOI: 10.1111/gto.12489
Douwe J.J. Van Hinsbergen, Mark B. Carpenter, José Been, Marjolein N. Naudé

Every year, tens of millions of cycling enthusiasts watch and read about the Tour de France, one of the largest sports events of the year. For hours on end, they wait in anticipation of the climax of the race, and these hours are filled by commentators and journalists with background information about riders, the course, history, cuisine, culture and architecture. Little do they realize that every day the peloton is actually setting out on a beautiful excursion through what is one of the most geologically and geographically diverse regions in the world. The Geo-Sports project provides journalists, readers, and viewers with accessible excursion guides, in written and video format, on websites and social media. In this article, we explain the rationale and background of the project, and we hope you will join us in lifting the veil to expose the beauty of the natural world and its role in our society.

每年,数以千万计的自行车爱好者观看和阅读环法自行车赛,这是一年中最大的体育赛事之一。在这些时间里,解说员和记者为他们提供有关车手、赛道、历史、美食、文化和建筑的背景信息。他们很少意识到,实际上每天车队都在穿越世界上地质和地理环境最多样化的地区之一,开始一次美丽的旅行。Geo-Sports 项目通过网站和社交媒体,为记者、读者和观众提供文字和视频形式的游览指南。在这篇文章中,我们将解释该项目的原理和背景,希望您能加入我们的行列,揭开自然世界之美及其在我们社会中的作用的面纱。
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引用次数: 0
Geodigest Geodigest
Pub Date : 2024-09-24 DOI: 10.1111/gto.12488
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引用次数: 0
Peridotites and other ultramafic rocks 橄榄岩和其他超基性岩
Pub Date : 2024-09-24 DOI: 10.1111/gto.12491
Kent Brooks

Peridotites are a group within the category of ultramafic rocks. These are usually dark-coloured rocks rich in magnesium, poor in silica and lacking feldspars. Earth's mantle, which makes up 83 percent by volume and 67 percent by weight of the planet, consists largely of peridotite, which, although relatively sparse at the surface, therefore, is Earth's most abundant rock type. Unfortunately, the mantle, which lies on average at >7 km under the oceans and >35 km under the continents, is not directly accessible for observation and our information comes largely from seismic studies, inclusions in volcanic rocks and sections of the ocean floor which have been tectonically emplaced into the crust: the ophiolite complexes and abyssal peridotites of the oceans. Such rocks also occur when mafic minerals, such as olivine, pyroxene and spinel, accumulate in magma chambers. An unusual occurrence of ultramafic rocks is the lava called komatiite, representing ultramafic liquids, which are largely restricted to Precambrian environments.

橄榄岩是超基性岩中的一类。这些岩石通常呈深色,富含镁,硅含量低,缺乏长石。地幔占地球体积的 83%,重量的 67%,主要由橄榄岩组成,虽然在地表相对稀少,但却是地球上最丰富的岩石类型。遗憾的是,地幔平均位于大洋下 7 千米和大陆下 35 千米处,无法直接观测,我们的信息主要来自地震研究、火山岩中的包裹体以及构造作用下沉积到地壳中的洋底剖面:蛇绿岩复合体和海洋深海橄榄岩。当橄榄石、辉石和尖晶石等黑云母矿物在岩浆室中堆积时,也会形成此类岩石。超基性岩中一种不常见的现象是被称为 "komatiite "的熔岩,它代表了超基性液体,主要局限于前寒武纪环境。
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引用次数: 0
North York Moors and Yorkshire Wolds: Landscape and Geology by Tony Waltham. Ramsbury, Marlborough: Crowood Press, 2024. 160pp. ISBN: 978-0-7198-4374-7 [paperback] £18.99 北约克沼泽和约克郡沃尔德:景观与地质》,托尼-沃尔瑟姆著。马尔堡拉姆斯伯里:克劳德出版社,2024 年。 160pp.ISBN: 978-0-7198-4374-7 [平装] £18.99
Pub Date : 2024-09-24 DOI: 10.1111/gto.12492
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引用次数: 0
Land subsidence in Iran: an omnipresent geohazard 伊朗的土地沉降:无处不在的地质灾害
Pub Date : 2024-09-24 DOI: 10.1111/gto.12473
Houshang Khairy, Mehdi Sarfi

As a result of several factors including overpopulation of the Earth and the ever-expanding search for groundwater resources, land subsidence is slowly becoming a global challenge. In fact, a 2021 study of 41 countries around the globe demonstrated the severity of the problem. However, land subsidence in Iran is accompanied by other issues which further complicate the problem.

由于地球人口过剩和对地下水资源的不断开采等多种因素,土地沉降正逐渐成为一项全球性挑战。事实上,2021 年对全球 41 个国家进行的一项研究表明了这一问题的严重性。然而,伊朗的土地沉降伴随着其他问题,使问题更加复杂。
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Geology Today
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