Climate changes in the south part of East Siberia for the last 5.5 ka inferred from multi-proxy sediment records of Lake Frolikha (Northern Baikal area, Russia)

Author(s):  
Andrey Fedotov ◽  
Svetlana Vorobyeva ◽  
Konstantin Vershinin ◽  
Eduard Osipov
Author(s):  
S. Vorobyeva ◽  
◽  
T. Zheleznyakova ◽  
A. Fedotov ◽  
◽  
...  

2008 ◽  
Vol 23 (3) ◽  
pp. n/a-n/a ◽  
Author(s):  
Jun Tian ◽  
Quanhong Zhao ◽  
Pinxian Wang ◽  
Qianyu Li ◽  
Xinrong Cheng

2003 ◽  
Vol 59 (3) ◽  
pp. 470-475 ◽  
Author(s):  
Gunhild C. Rosqvist ◽  
Pernilla Schuber

AbstractThe location of South Georgia (54°S, 36°W) makes it a suitable site for the study of the climatic connections between temperate and polar environments in the Southern Hemisphere. Because the mass balance of the small cirque glaciers on South Georgia primarily responds to changes in summer temperature they can provide records of changes in the South Atlantic Ocean and atmospheric circulation. We use grey scale density, weight-loss-on-ignition, and grain size analyses to show that the proportion of glacially eroded sediments to organic sediments in Block Lake was highly variable during the last 7400 cal yr B.P. We expect that the glacial signal is clearly detectable above noise originating from nonglacial processes and assume that an increase in glacigenic sediment deposition in Block Lake has followed Holocene glacier advances. We interpret proglacial lake sediment sequences in terms of summer climate warming and cooling events. Prominent millennial-scale features include cooling events between 7200 and 7000, 5200 and 4400, and 2400 and 1600 cal yr B.P. and after 1000 cal yr B.P. Comparison with other terrestrial and marine records reveals that the South Georgian record captures all the important changes in Southern Hemisphere Holocene climate. Our results reveal a tentative coupling between climate changes in the South Atlantic and North Atlantic because the documented temperature changes on South Georgia are anti-phased to those in the North Atlantic.


2021 ◽  
pp. 15-32
Author(s):  
Н.Г. Разжигаева ◽  
Л.А. Ганзей ◽  
Т.А. Гребенникова ◽  
В.Б. Базарова ◽  
П.С. Белянин ◽  
...  

Представлены результаты работы лаборатории палеогеографии и геоморфологии ТИГ ДВО РАН в 2017–2020 гг. Приведены новые данные по изучению развития материковых и островных геосистем юга Дальнего Востока и реакции их компонентов на короткопериодные климатические изменения позднего плейстоцена–голоцена. Палеоэкологические изменения с высоким временным разрешением восстановлены в среднегорье Восточного Сихотэ-Алиня. Новые данные получены по развитию геосистем побережья Японского моря, определена роль зональных и азональных природных факторов в их развитии. Выделены этапы развития ландшафтов платобазальтового рода. Реконструированы обстановки осадконакопления и формирования пойменных ландшафтов Приханкайской равнины. Сделаны детальные реконструкции хода развития островных ландшафтов для юга Приморья. Для юга Дальнего Востока проведен синтез изменений ландшафтов в последнее интенсивное потепление – малый оптимум голоцена (VII–XIII вв.). Проанализировано проявление природных катастроф и их пространственно-временной масштаб. Продолжены работы, направленные на оценку цунамиопасности на побережье восточного Приморья. Для Курильских островов выделены наиболее сильные цунами, которые могут быть рассмотрены как кандидаты в мегацунами. Внимание уделено трансформации ландшафтов при освоении территории юга Дальнего Востока древним человеком. Геоархеологические исследования проводились также во внутриконтинентальных районах (Западное Забайкалье, Восточная Монголия). The authors present the results of the researches of the laboratory of paleogeography and geomorphology of PGI FEB RAS in 2017–2020. New data include the study of the development of continental and island geosystems of the South Far East and the response of their components to short-term climate changes in the Late Pleistocene-Holocene. Paleoecological changes with a high temporal resolution have been restored in the middle mountains of the Eastern Sikhote-Alin. New data were obtained on the development of geosystems of the coast of the Sea of Japan, the role of zonal and azonal natural factors in their development was determined. The stages of development of landscapes of the platobasalt genus are highlighted. The conditions of sedimentation and formation of floodplain landscapes of the Khanka Lake plain were reconstructed. Detailed reconstructions of the island landscapes development for the south of Primorye have been made. For the south of the Far East, a synthesis of landscape changes in the last intense warming – Medieval Warm Period of the Holocene (VII-XIII centuries) was made. The manifestation of natural disasters and their space-time scale were analyzed. The investigations aimed at assessment of the tsunami hazard on the coast of eastern Primorye were continued. For the Kuril Islands, the most powerful tsunamis have been identified, which can be considered as candidates for megatsunami. Transformation of landscapes and a human impact on landscapes were also discussed. Geoarchaeological studies were also carried out in the intra-continental regions (Western Transbaikalia, Eastern Mongolia).


2021 ◽  
Vol 13 (18) ◽  
pp. 10402
Author(s):  
Shao Sun ◽  
Qiang Zhang ◽  
Yuanxin Xu ◽  
Ruyue Yuan

Recent decades have witnessed accelerated climate changes across the Qinghai-Tibet Plateau (QTP) and elevated socioeconomic exposure to meteorological hazards. The QTP is called the “the third pole”, exerting remarkable impact on environmental changes in its surrounding regions. While few reports are available for addressing multi-hazard risks over the QTP, we develop an integrated indicator system involving multiple meteorological hazards, i.e., droughts, rainstorms, snowstorms and hailstorms, investigating the spatiotemporal patterns of major hazards over the QTP. The hazard zones of droughts and rainstorms are identified in the southern Gangdise Mountains, the South Tibet Valley, the eastern Nyenchen-Tanglha Mountains, the Hengduan Mountains and West Sichuan Basin. Snowstorm hazard zones distribute in the Himalayas, the Bayan Har Mountains and the central Nyenchen-Tanglha Mountains, while hailstorm hazard zones cluster in central part of the QTP. Since the 21st century, intensified rainstorms are detectable in the densely populated cities of Xining and Lhasa and their adjacent areas, while amplified droughts are observed in grain production areas of the South Tibet Valley and the Hengduan Mountains. Snowstorm hazards show large interannual variations and an increase in pastoral areas, although the overall trend is declining slightly. The frequency of hailstorms gradually decreases in human settlements due to thermal and landscape effects. Mapping meteorological hazards regionalization could help to understand climate risks in the QTP, and provide scientific reference for human adaptation to climate changes in highly sensitive areas.


2017 ◽  
pp. 55-60
Author(s):  
L. M. Kipriyanova

New ass. Cladophoro fractae–Stuckenietum chakas­siensis Kipriyanova ass. nov. hoc loco, referred to the alliance Сladophoro fractae–Stuckenion chakassiensis Kipriyanova all. nov. hoc loco, to the order Ruppietalia maritimae J. Tx. ex Den Hartog et Segal 1964 and to the class Ruppietea maritimae J. Tx. ex Den Hartog et Segal 1964 was described in Siberia. Nomenclature type (holotypus) — relevé 3 (author′s number 5.3) in Table. Dominating diagnostic species is Stuckenia chakassiensis (Kaschina) Klinkova (Flora Nizhnego Povolzhiya, 2006). (Synonyms are Potamogetonpectinatus L. subsp. chakassiensis Kaschina in Krasnob. et Safonova, 1986, Novoe o Fl. Sibiri: 245. — P. chakassiensis (Kaschina) Volob. 1991, Sibir. Biol. Zhurn. 5: 75. — P. chakassiensis var. tenuior Volob. 1993, Sibir. Biol. Zhurn. 3: 57. — P. intramongolicus Ma, 1983, Acta Bot. Bor.-Occid. Sin. 3(1): 8, nom. inval. — P. acifolius Ma, 1983, Acta Bot. Bor.-Occid. Sin. 3(1): 8, nom. inval. — Stuckeniaintramongolica (Ma) Tzvel. 1999, Bot. Zhurn. 84(7): 111, nom. illeg.). The species richness (data of fifteen relevés) is 1–4 per relevé, which is explained by relatively high salinity values. A total of 8 species were registered in association communities. Communities with total cover 20–95 %, occupy quite large (from 20 to more than 100 m2) areas in the studied lakes. The main ­layer — submerged plants — is made by shoots of Stuckenia chakassiensis. There are other species with a wide range of halotolerance (Cladophora species), as well as brackish and saline water species (Ruppia maritima, Chara aspera, C. canescens, C. altaica) and Althenia orientalis, Ruppia drepanensis, R. cirrhosa, Lamprotamnium papulosum, which are much rarer in Western Siberia. Other layers are not expressed, except for the emergent plants represented by reed on the border of belts of submergent and emergent vegetation. Communities of associations were observed only in the brackish (oligohaline, mesohaline, polyhaline) waters of the various classes and groups: mainly sodium-chloride in the south of West Siberia, and sodium-bicarbonate in East Siberia. Not too often they were found in sodium-sulfate and magnesium-bicarbonate waters. Salinity range of association in Transbaikalia was 1.11–9.57 g/dm3. Maximum salinity for Stuckenia chakassiensis communities in the Novosibirsk region was 10.32 g/dm3, in the lakes of Khakassia — 28.8 g/dm3. The pH values varied from 6.55 to 10.50. Special publications (Kipriyanova et al., 2016, 2017) are devoted to a description of the hydrochemical preferences of the S. chakassiensis and some other species of the genus Stuckenia in the lakes of Transbaikalia. According to the obtained data in the brackish waters of the lakes of East Siberia, S. chakassiensis forms thickets with rather high productivity (up to 517.4±89.51 g/m2 abs. dry weight) (Kipriyanova et al., 2017). The association′s area of distribution appears to coincide with the range of the species, which is a southern part of Siberia (Kurgan Region, Novosibirsk Region, Altai Territory, the Republic of Khakassia, the Republic of Buryatia, Trans-Baikal Territory), northern Kazakhstan, northern China, Mongolia, and rarely — the South Eastern Europe: Volgograd Region (Chernyshkovsky district, in the estuaries and lakes of the Tsimlyansky sand massif near the hamlets Tormosin and Morskoy ) (Flora of the Lower Volga region, 2006; Krasnaya..., 2006) and in the Caucasus ­(Tzvelev, 1990). The association quite logically fits into the class Ruppietea and the order Ruppietalia. In addition to the actual cenoses of different Ruppia species, the communities of other aquatic halotolerant plants, such as the association of emergent plant Eleocharitetum parvulae (Christiansen 1934) Gillner 1960, the bryophyte cenoses Rielletum helicophyllae Cirujano et al. 1993, Rielletum notarisii Cirujano et al. 1993 may be included into this class (Rivas-Martínez et al., 2002; and others). Some researchers place into this class the communities of halotolerant charophytes of the Charion canescentis Krausch 1964 alliance, and the ass. Ranunculetum baudotii Br.-Bl. in Br.-Bl. et al. 1952 (Berg et al., 2014). The input of the ass. Cladophoro fractae–Stuckenietum chakassiensis to the Ruppietea class corresponds to principles and methods of the Braun-Blanquet approach (Braun-Blanquet, 1964), since the diagnostic species of the new association is accompanied with different species abundance in the brackish and saline waters: Ruppia maritima, Chara canescens, C. altaica, as well as species with a wide range of halotolerance — Cladophora fracta and others. The character diagnostic species of Сladophoro fractae–Stuckenion chakassiensis alliance are the species specific for continental brackish and saline waters of forest-steppe and steppe zones of Asia such as Stuckenia chakassiensis, S. macrocarpa, Chara altaica.


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