Abstract True hoppers, consisting of Fulgoromorpha and Cicadomorpha, are plant feeders with very high species-level diversity. A large number of true hopper fossils have been reported from eastern Asia, especially from the Middle to Late Jurassic Yanliao Biota, the Early Cretaceous Jehol Biota and mid-Cretaceous Kachin amber in the last two decades. Herein, true hoppers from the Jurassic and Cretaceous of eastern Asia are reviewed, and combining palaeontological data from other regions of the world and recent advances of molecular studies, the evolutionary history of true hoppers in the mid–late Mesozoic is discussed. Permocicada beipiaoensis Wang, 1987 and Archijassus plurinervis Zhang, 1985 are here excluded from Prosboloidea and Archijassidae, respectively. By the end of 2020, a total of 203 species with definite systematic position had been documented in the Jurassic and Cretaceous of eastern Asia (China, Myanmar, Siberia, Mongolia, Japan and Korea), and were attributed to 116 genera in 22 families and 7 superfamilies. Available fossil data suggest that true hopper components strongly changed in the Cretaceous: primitive groups reduced and went extinct successively, and the origin and/or early diversification of most lineages (family or subfamily level) occurred, likely owing to the displacement of host-plants in the angiosperm floristic revolution.

Abstract China has a rich record of Holocene volcanism that is relatively little known outside the country. It is encountered in large stratovolcanoes in the NE, linked to subduction of the Pacific plate (e.g. Changbaishan), in smaller volcanoes on the Tibetan margin, associated with the collision of India and Eurasia (e.g. Tengchong, Ashishan), and in more isolated centres, possibly resulting from mantle upwelling (e.g. volcanoes in Hainan island). This makes China a natural laboratory for studies of intraplate volcanism, and significant progress in understanding its nature and origins has been made over the past quarter century. Here, we introduce the first publication in English to provide a comprehensive survey of the state of knowledge and research highlights. Accordingly, we provide an overview of the dynamics, geology, geochemistry, volcanic histories and geophysical studies of 14 volcanic areas associated with the Holocene documented thus far. The special publication represents a benchmark reference on the topic but, as importantly, we hope that it will stimulate new, international collaborations aimed at deepening our understanding of the origins, history, hazards and associated risks of China's volcanoes.

Abstract The Changbaishan volcanic field located on the Gaima (Gaema, Gaiman) Plateau has witnessed plateau-forming eruptions along with the uplift of the Gaima Plateau. The Tianchi basaltic lava shield volcano was formed at the main peak of Changbaishan, with cone construction eruptions that formed a huge and steep trachytic composite cone on the gentle lava shield. At the peak of the Millennium Eruption (ME), the height of the eruption column reached 25 km and the bulk volume of tephra was about 120 km 3 . The ME eventually formed Tianchi caldera, after which several eruptions occurred, albeit of a much smaller scale. The magmas involved in the shield-forming eruptions are characterized by both alkalic series trachybasalt and basaltic trachyandesite and subalkalic tholeiite and basaltic andesite. In the cone-construction and ignimbrite-forming eruption stages, the magma is completely composed of alkalic series trachyte and comendite. The largest negative Eu anomalies observed in ME magmas indicate that plagioclase was strongly crystallized and differentiated.

Abstract The Longgang volcanic field (LVF) is a monogenetic volcanic field in China that erupted in the Quaternary, forming more than 100 scoria cones and maars in an area of over 1500 km 2 . The most recent eruption occurred c. 1500–1700 years ago. By summarizing the results of previous and recent research, this paper reviews the geological background, volcano distribution, eruption history, typical volcanoes and geochemical characteristics of the LVF. The volcanic activities in the LVF were structurally controlled by near-EW-, NW- and NE-trending faults. An analysis of typical volcanic edifices reveals that at least two eruptive episodes occurred in the Holocene, and most of the maars in the LVF have characteristics of multiple eruptive styles. It is concluded that the eruption types included effusive eruptions, magma explosive eruptions and phreatomagmatic eruptions. The results of geochemical studies of LVF eruptive products show that most of the rock is trachybasalt and that the magma rarely interacts with crustal rocks. Compared with the previous results for the neighbouring Changbaishan polygenetic volcanic field, the probable origins of their differences in volcanism are discussed.

Abstract China has numerous active volcanoes, and more than 10 erupted in the Quaternary. Although a modern eruption event has not occurred in China, the potential risk from volcanic hazards should be noted. With the development of geodetic technologies including the Global Positioning System (GPS), levelling and interferometric synthetic aperture radar (InSAR), volcanologists can now detect the present-day deformation state of China's active volcanoes. In this paper, we summarize the present-day deformation patterns, magma sources and magma plumbing systems of China's active volcanoes between 1970 and 2013. The results show that the most active volcano in China is the Changbaishan volcano; it showed significant inflation from 2002–03, with the deformation becoming gradually weaker after 2003, indicating that it had been experiencing a magma process during 2000–10. A point source at a depth of c. 10 km was responsible for the observed deformation. The Leiqiong volcanic field showed a trough pattern deformation during 2007–10, which was interpreted as a dyke intrusion model. Fluctuant deformation patterns were shown in the Tengchong volcanic field. The Longgang volcanic field had experienced a volcano-wide uplift during the 1970s and 1990s. Deformation was observed in the Tatun volcanic field from 2006–13, and two shallow sources account for the observed deformation. These volcanoes merit further monitoring given possible evidence of deformation. No obvious deformation related to volcanic activity was observed at the Ashikule volcanic field from 2003–11. The results provide a basic introduction to the deformation state of China's active volcanoes, and may be helpful for evaluating the activity levels of China's volcanoes and mitigating the risks of future volcanic hazards.

Abstract Following decades of geological surveys and studies, 14 active volcanic fields have been identified in China. Evidence for Holocene volcanism in several of these areas highlights the need to understand and monitor volcanic hazards in those regions. Six volcano observatories have thus been established in the past 40 years. This work reviews China's national capability and history of volcano monitoring, with emphasis on the Changbaishan–Tianchi Volcano Observatory and the Tengchong Volcano Observatory. The Changbaishan–Tianchi Volcano Observatory (CTVO) was constructed in 1996 and began monitoring in 1999, with limited recorded observations dating back to 1973. Currently, CTVO is the largest and most advanced observatories in China. The monitoring network of the CTVO incorporates 11 seismic and 15 GPS stations, two levelling routes and three gas geochemistry sampling points. The Changbaishan–Tianchi Volcano experienced unrest during 2002–05, evidenced in elevated levels of seismicity and ground deformation, as well as shifts in gas geochemistry. After 2006, the volcano returned to quiescence, with activities at background levels as recorded in 1973–2001. The monitoring network of Tengchong Volcano Observatory incorporates eight seismic stations, 20 GPS points, 95 levelling points and three gas geochemistry sampling points. The observations made since 1965 indicate significant seismicity, with more than 3000 events recorded in 2011, mostly related to regional tectonics. Tengchong is known for its widespread hot springs, with temperatures up to 105°C recorded at Dagunguo spring. The four other observatories are Longgang Volcano Observatory, Jingbohu Volcano Observatory, Wudalianchi Volcano Observatory and Qiongbei Volcano Observatory. They are equipped with seismic, geodetic and geochemical monitoring equipment. These areas saw only low levels of activity over the past several decades, but related fault systems are relatively active. In a relatively short time, China has gained considerable experience in observatory design and volcano monitoring and has trained up a sizeable task force, laying the foundation for sustained volcano monitoring at the national level. Future efforts must focus on maintaining and expanding observational capacity, as well as gaining better dynamic understanding to inform volcano hazard assessment.

Abstract By synthesizing relevant research findings from China and other countries, this paper discusses the distribution and eruption types of volcanoes in China. An analysis of the spreading characteristics of volcanic ash possibly caused by volcanic eruptions such as those from Changbaishan is presented, and the impact of volcanic ash on aviation flight safety, as well as several key methods of monitoring volcanic ash, are discussed. This paper also outlines the operational process of China's aviation industry in addressing volcanic ash and compares and analyses the handling of volcanic ash by civil aviation industries globally. Further, ways of dealing with volcanic ash are then suggested for China's aviation industry.

Abstract In this study, we collect and translate observations and witness accounts suggestive of volcanic eruptions in ancient and modern China. The documents from the literature covered confirmed volcanic eruptions and suspected volcanic events. Recorded events concerning Tianchi ( c. 946 AD), Wudalianchi (1720, 1721) and Ashikule (1951) volcanoes relate to confirmed volcanic eruptions. Detailed records of Tianchi eruptions in historical documents span from 946 to 1903 AD. The real-time observations of the 1720–21 eruptions recorded by the government are presented. They describe a violent explosion and the development of lava flows at Laoheishan volcano. Evidence for events suggestive of volcanic activity are also presented for Dayingshan (1609, Tengchong), Man'anling (1883, Haikou), Chahayan (Heilongjiang), the South China Sea, Kui-shan Tao (late 1770s, Taiwan) and Penjia Islet (19 May 1916 and 29 June 1927, Taiwan). However, some supposed historical volcanic activities including Helanshan (Ningxia), Datong volcano, Rendagou (Sichuan) and Shizishan (Hunan) remain highly suspect according to their unclear positions and rough geological settings. These events may arise from the spontaneous combustion of coal. Records in Tianshan and Beiting Beishan (Xinjiang) may represent mud volcanoes. One case of an ancient Chinese Fengshui master interpreting geological processes from mythology is helpful when inspecting volcanology-related myths.