Relevant bibliographies by topics / Holocene Climatic Optimum

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Holocene Climatic Optimum'

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Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Holocene Climatic Optimum"

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He, Y., Wilfred H. Theakstone, Zhang Zhonglin, Zhang Dian, Yao Tandong, Chen Tuo, Shen Yongping, and Pang Hongxi. "Asynchronous Holocene climatic change across China." Quaternary Research 61, no. 1 (January 2004): 52–63. http://dx.doi.org/10.1016/j.yqres.2003.08.004.

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A review of Holocene climatic variations in different parts of China shows that they were asynchronous. Proxy data from ice cores, pollen, loess, lacustrine sediments, and changes of sea and lake levels demonstrate that many warm and cold oscillations have occurred in China during the Holocene, including a most important climatic event known as the “Holocene optimum,” a milder and wetter period, and that the duration and amplitude of the optimum period, as well as its start and end times, differed in different parts of China. Uplift of the Tibetan plateau over the past millions of years led to the development of the monsoon climate and to complex atmospheric circulation over continental China during the Holocene. As a result, the Holocene optimum began and terminated earlier in high-altitude regions of western China than at lower elevations in eastern China, and the amplitude of the variations was lower in the east. This suggests that the western higher-altitude areas were more sensitive to climatic change than were the eastern lower-altitude areas. Holocene climatic records in the Dunde and Guliya ice cores do not correspond. Inverse δ18O variations between the two cores indicate that the effects of climate and atmospheric processes on the stable isotopes at the two sites differed. The correlation between the isotopic composition of carbonates in lake deposits in western China and climatic variations is similar to that in the ice cores. The climatic resolution in ice cores and lake sediments is higher than that in other media. The lack of precise correspondence of climatic records constructed on the basis of proxy data from different parts of China is a result of the different locations and elevations of the sampling sites, the different resolutions of the source material, and the varied climatic conditions within China. Further work is needed to confirm both the conclusions and the inferences presented here.
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Weidick, A. "Jakobshavn Isbræ area during the climatic optimum." Rapport Grønlands Geologiske Undersøgelse 155 (January 1, 1992): 67–72. http://dx.doi.org/10.34194/rapggu.v155.8183.

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The GGU glaciological investigations related to hydropower planning north (Pakitsoq) and south (Tiningnilik) of Jakobshavn Isbræ have, together with finds and dating of marine subfossils, furnished information on the history of the ice margin changes during and since the Holocene climatic optimum. The paper attempts to reconstruct the ice margin conditions and surroundings during the Holocene climatic optimum on the basis of this information.
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NIELSEN, LISBETH T., GUðFINNA AÐALGEIRSDÓTTIR, VASILEIOS GKINIS, ROMAN NUTERMAN, and CHRISTINE S. HVIDBERG. "The effect of a Holocene climatic optimum on the evolution of the Greenland ice sheet during the last 10 kyr." Journal of Glaciology 64, no. 245 (May 22, 2018): 477–88. http://dx.doi.org/10.1017/jog.2018.40.

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ABSTRACTThe Holocene climatic optimum was a period 8–5 kyr ago when annual mean surface temperatures in Greenland were 2–3°C warmer than present-day values. However, this warming left little imprint on commonly used temperature proxies often used to derive the climate forcing for simulations of the past evolution of the Greenland ice sheet. In this study, we investigate the evolution of the Greenland ice sheet through the Holocene when forced by different proxy-derived temperature histories from ice core records, focusing on the effect of sustained higher surface temperatures during the early Holocene. We find that the ice sheet retreats to a minimum volume of ~0.15–1.2 m sea-level equivalent smaller than present in the early or mid-Holocene when forcing an ice-sheet model with temperature reconstructions that contain a climatic optimum, and that the ice sheet has continued to recover from this minimum up to present day. Reconstructions without a warm climatic optimum in the early Holocene result in smaller ice losses continuing throughout the last 10 kyr. For all the simulated ice-sheet histories, the ice sheet is approaching a steady state at the end of the 20th century.
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Yang, Xunlin, Hong Yang, Baoyan Wang, Li-Jung Huang, Chuan-Chou Shen, R. Lawrence Edwards, and Hai Cheng. "Early-Holocene monsoon instability and climatic optimum recorded by Chinese stalagmites." Holocene 29, no. 6 (February 28, 2019): 1059–67. http://dx.doi.org/10.1177/0959683619831433.

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The timing and duration of the Holocene East Asian summer monsoon (EASM) maximum and the interpretation of Chinese stalagmite δ18O records have long been disputed. Notably, interpretations of Holocene EASM variations are frequently based on a single record or study area and are often contradictory. In this study, we conducted stable isotope analyses of four Holocene stalagmites from Chongqing, southwest China. The results reveal differences in the timing of the Holocene EASM maximum and to try to resolve the inconsistency we analyzed and statistically integrated a total of 16 Holocene stalagmite records from 14 caves in the EASM region. The resulting synthesized Holocene stalagmite δ18O (δ18Osyn) record is in agreement with other EASM records and confirms that stalagmite δ18O records are a valid indicator of EASM intensity, rather of local precipitation amount. The δ18Osyn record shows that the EASM intensified rapidly from the onset of the early Holocene; notably, however, there were distinct EASM oscillations in the early Holocene, consisting of three abrupt millennial-scale events. This indicates that, contrary to several previous interpretations, the early Holocene EASM was unstable. Subsequently, during 8–6 kyr BP, the EASM was relatively stable and strong, with the strongest monsoon occurring during 8–7 kyr BP. This evidence of a stable and strong mid-Holocene EASM in eastern China is in accord with the classical view of a mid-Holocene Optimum in China.
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Jin, Zhang-Dong, Yanhong Wu, Xiaohui Zhang, and Sumin Wang. "Role of late glacial to mid-Holocene climate in catchment weathering in the central Tibetan Plateau." Quaternary Research 63, no. 2 (March 2005): 161–70. http://dx.doi.org/10.1016/j.yqres.2004.09.012.

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The lightness (L*) and concentrations of Rb, Sr and organic carbon (Corg) have been measured in the age-constrained lake sediment cores recovered from Co Ngoin in the central Tibetan Plateau. Dissolved Sr flux is a dominant control on the variation of Rb/Sr ratios in the sediments. Variations in color and geochemical proxies of Co Ngoin sediments display a continuous history of late glacial to mid-Holocene chemical versus physical weathering intensity in response to past climatic changes between approximately 13,500 and 4500 cal yr B.P. A lower chemical weathering under a late glacial climate was followed by a higher weathering during the Holocene Optimum. Weathering intensity in the central Tibetan Plateau catchment also responds to well-known climatic events, such as the Younger Dryas (YD), and possibly the Holocene Event 5 (HE-5). Although there are differences in time or duration of the climatic events, many of the well-known late glacial to mid-Holocene events occurred in high-elevation Co Ngoin where atmospheric circulation might play a hemispherical role in climatic forcing. The sediment hiatus since c. 4200 14C yr B.P. in the Co Ngoin indicates a period of desiccation that was probably associated with a sharp decrease in summer monsoon strength. Our lascustrine results not only imply catchment weathering variations in response to late glacial to mid-Holocene climatic conditions in the central plateau, but also provide further evidence for global connections between regional climates.
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Zhang, Jingwei, Xinggong Kong, Kan Zhao, Yongjin Wang, Shushuang Liu, Zhenjun Wang, Jianwei Liu, Hai Cheng, and R. Lawrence Edwards. "Centennial-scale climatic changes in Central China during the Holocene climatic optimum." Palaeogeography, Palaeoclimatology, Palaeoecology 558 (November 2020): 109950. http://dx.doi.org/10.1016/j.palaeo.2020.109950.

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Nazarova, L. B., N. G. Razjigaeva, B. Diekmann, Т. А. Grebennikova, L. А. Ganzey, N. I. Belyanina, K. А. Arslanov, et al. "Reconstruction holocene environmental changes in North-Western Pacific in relation to paleorecord from Shikotan Island." Доклады Академии наук 486, no. 2 (May 27, 2019): 212–16. http://dx.doi.org/10.31857/s0869-56524862212-216.

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Results of a paleolimnological investigated of a well-dated lake sediment section from Shikotan Island (Southern Kurils) showed that from ca 8.0 to 5.8 cal ka BP warm and humid period corresponding to middle Holocene optimum took place. Cooling thereafter corresponds to Neoglacial. A reconstructed from ca 0.9 to ca 0.58 cal ka BP warm period can be correlated to a Medieval Warm Period. Cooling after 0.58 cal ka BP can be correlated with the LIA. Marine regression stages were identified at ca 6.2-5.9, 5.5-5.1 and 1.07-0.36 cal ka BP. The general chronology of major climatic events of Holocene in the island is in accordance with the climate records from the North Pacific region. Revealed spatial differences in timing and magnitude of the Late Holocene climatic episodes (LIA, MWP) within region needs further investigations.
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Janz, Lisa, Arlene M. Rosen, Dashzeveg Bukhchuluun, and Davaakhuu Odsuren. "Zaraa Uul: An archaeological record of Pleistocene-Holocene palaeoecology in the Gobi Desert." PLOS ONE 16, no. 4 (April 8, 2021): e0249848. http://dx.doi.org/10.1371/journal.pone.0249848.

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Environmentally-based archaeological research at Zaraa Uul, including zooarchaeology, phytolith analysis, and radiocarbon dating, is the first of its kind in Mongolia and presents critical new insight on the relationship between periods of occupational intensity and climatic amelioration from the earliest anatomically modern humans to the adoption of pastoralism. The palaeoenvironmental and faunal record of Zaraa Uul show that Early-Middle Holocene hydrology and species distributions were distinct from all other periods of human occupation. Holocene hunter-gatherers inhabited an ecosystem characterized by extensive marshes, riparian shrub and arboreal vegetation along the hill slopes and drainages. The exploitation of species associated with riparian and wetland settings supports the hypothesis of, but suggests an earlier timing for, oasis-based logistical foraging during the Early-Middle Holocene of arid Northeast Asia. The onset of wetter conditions at 8500 cal BP agrees with other regional studies, but multiple lines of evidence present the first integrated field- and laboratory-based record of human-environment relationships in arid East Asia during the Holocene Climatic Optimum. We compare it to Late Pleistocene climatic amelioration, and highlight specific responses of the hydrological, vegetative and faunal communities to climate change in arid Northeast Asia.
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Nahm, Wook-Hyun, Jin Kwan Kim, Ju-Yong Kim, Sangheon Yi, Jaesoo Lim, and Jin Cheul Kim. "The Holocene climatic optimum in Korea: Evidence from wetland records." Palaeogeography, Palaeoclimatology, Palaeoecology 376 (April 2013): 163–71. http://dx.doi.org/10.1016/j.palaeo.2013.02.033.

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Baroni, Carlo, and Giuseppe Orombelli. "The Alpine “Iceman” and Holocene Climatic Change." Quaternary Research 46, no. 1 (July 1996): 78–83. http://dx.doi.org/10.1006/qres.1996.0046.

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The finding of a prehistoric mummified corpse at the upper edge of the accumulation area of an alpine glacier, together with its unique set of artifacts, provided new information on glacier dimensions during the little-known phases of major glacier shrinkage that characterized the warmest parts of the Holocene. The sudden burial of the corpse in a permanent snow cover occurred 5300–5050 cal yr B.P., indicating a significant climatic change that induced glacier expansion at the beginning of Neoglaciation. New geomorphologic data and two AMS 14C ages from buried soils suggest that the present glacier size, following over 100 yr of shrinkage, is comparable to that immediately preceding Neoglaciation. Therefore, we can deduce that the current global climatic warming may have interrupted the environmental conditions prevailing in the Alps during Neoglacial time, restoring characteristics similar to those prevailing during the climatic optimum that were never achieved during the second half of the Holocene.
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Dissertations / Theses on the topic "Holocene Climatic Optimum"

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Nordhoff, Peter. "Stable isotope investigations on speleothems from different cave systems in Germany." Doctoral thesis, [S.l.] : [s.n.], 2005. http://webdoc.sub.gwdg.de/diss/2005/nordhoff.

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Books on the topic "Holocene Climatic Optimum"

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A, McKinnon Neil, Stuart Glenn S. L. 1959-, University of Calgary. Archaeological Association., and University of Calgary. Dept. of Archaeology., eds. Man and the mid-Holocene climatic optimum: Proceedings of the Seventeenth Annual Conference of the Archaeological Association of the University of Calgary. Calgary, Alta., Canada: University of Calgary, Archaeological Association, 1987.

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University of Calgary Archaeological Association. Conference. Man and the Mid-holocene climatic optimum: Proceedings of the seventeenth annual Conference of the Archaeological Association of the University of Calgary. Calgary, Alta: University of Calgary Archaeological Association, 1987.

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University of Calgary. Archaeological Association. Conference. Man and the mid-holocene climatic optimum: Proceedings of the seventeenth annual conference of the Archaeological Association of the University of Calgary. Calgary: The University of Calgary Archeaological Association, 1987.

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Book chapters on the topic "Holocene Climatic Optimum"

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"Holocene Climatic Optimum." In Encyclopedic Dictionary of Archaeology, 604. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58292-0_80325.

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McMichael, Anthony. "Spread of Farming, New Diseases, and Rising Civilizations: Mid- Holocene Optimum." In Climate Change and the Health of Nations. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780190262952.003.0010.

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As The Earth Warmed after the last glacial maximum, temperatures fluctuated. About 9700 B.C.E., temperatures rose again suddenly and began to stabilize, marking the beginning of a new geological epoch, the Holocene. The landscape continued to change, but not so fast that a single generation of humans would have noticed. Ice- sheets and tundra were receding in Eurasia, and over time human groups, both hunter- gatherers and then early farmer- pastoralist communities, adjusted their ways of living to warmer conditions and different rainfall patterns. Small- scale farming and herding emerged on all nonpolar con­tinents during the period 8500 to 6000 B.C.E., predominantly in the northern hemisphere, while human numbers were creeping up. These great changes in environmental conditions and subsequent cultural practices had a profound influence on the foundations of human health and survival: food sufficiency and quality, water sup­plies, contacts with infectious agents, modes of settlement, and social relations. A new era in human ecology was looming. Farming increased food production, but the switch to dependency on a few staples decreased diversity of diets and created an annual agricul­tural regime more susceptible to climate shifts. Close contact with animals, standing water in irrigated environments, and denser set­tlements provided opportunities for microbes, pathogens, viruses, and parasites to cross species barriers and infect and spread among human populations. During the Early Holocene, from about 9700 B.C.E. to 6000 B.C.E., the earth was subjected to the competing stresses of high solar influ­ence and still massive melting ice- sheets. From around 6000 B.C.E., the majority of ice- sheet melting had abated, allowing the stabiliza­tion of the Earth’s climate into what can be called the Mid- Holocene Climatic Optimum (approx. 6000 to 3000 B.C.E.). This was a change in climate that spanned 3,000 to 4,000 years. Warming was most evi­dent in the northern hemisphere, influenced by the peaking of solar radiation at higher northern latitudes as the 23,000- year Milankovitch “wobble” cycle maximized northern sun exposure for several millen­nia. The Milankovitch cycle also drew the rain- bearing Inter- Tropical Convergence Zone (ITCZ) further north.
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McMichael, Anthony. "Eurasian Bronze Age: Unsettled Climatic Times." In Climate Change and the Health of Nations. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780190262952.003.0011.

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The Story Now Moves beyond the mid- Holocene. By around 4000 B.C.E., viable agrarian settlements had appeared in many parts of the world. Not only could larger populations be supported, but surplus food produced by toiling farmers enabled the differentiation of labour and social status. Settlements expanded, made trading connections, and formed larger collective polities. Hierarchical authority and power began to replace horizontal flows of local information and decision- making. The vagaries of climate, however, lurked on the horizon. Agrarian societies, with their increasing dependence on harvest staples, were painting themselves into a corner. Also, as populations grew and settle­ments coalesced, mutant strains of animal- hosted microbes that made a successful crossing from livestock or urban pests to humans took ad­vantage of larger, intermingling host populations. A few of these adven­turers, such as the measles virus, not only initiated new epidemics but continued circulating, between outbreaks, as endemic “crowd diseases.” Measles, a microbial success story, is still with us today. The advent of property, food stores, and occupied land in nearby populations stimulated both war and conquest, each having diverse, debilitating, and often bloody consequences for health and survival. Climatic conditions in Sumer, sitting at the meteorological crossroads of the Middle East, began changing about 3600 B.C.E., one- third of the way into the fourth millennium B.C.E. . There was a general cooling and drying in the northern hemisphere as the first phase of the Holocene Climatic Optimum waned and as the Icelandic Low and Siberian (Asiatic) High circulations intensified, funnelling colder air southwards. Rainfall declined in southern Mesopotamia, compounded by a southerly drift of the rain- bearing Inter- Tropical Convergence Zone and the regional monsoon. Further west, the Sahara was changing from green to brown, and Egyptian agriculture was faltering. As rainfall declined and arrived later in the year, farming became more difficult; farmers now needed to make a year- round effort, with double- cropping and shorter fallow periods. By extending their irrigation systems, the Sumerians compounded an­other problem: several centuries of overirrigation and deforestation had already begun to turn the soil saline.
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Gusick, Amy E., and Jon M. Erlandson. "Paleocoastal Landscapes, Marginality, and Early Human Settlement of the California Islands." In An Archaeology of Abundance, 59–97. University Press of Florida, 2019. http://dx.doi.org/10.5744/florida/9780813056166.003.0003.

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If the California Islands were marginal for human settlement, why were several of them occupied more or less continuously since Terminal Pleistocene or Early Holocene times? The earliest human history of California's Islands is clouded by sea level rise, coastal erosion, dune building, and differential research intensity. Nonetheless, Paleocoastal sites are abundant on the Northern Channel Islands and Cedros Island, suggesting that they were optimal habitat for early hunter-gatherers, with ample food, freshwater, mineral, and other resources to sustain permanent settlement. Worldwide on islands where late Pleistocene or early Holocene human colonization occurred, climate shifts and massive landscape changes caused by postglacial sea level rise require detailed reconstructions of paleogeography and paleoecology to assess the potential productivity or marginality of islands or archipelagos.
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Holman, J. Alan. "Herpetological Population Adjustments in the Pleistocene of Britain and Europe." In Pleistocene Amphibians and Reptiles in Britain and Europe. Oxford University Press, 1998. http://dx.doi.org/10.1093/oso/9780195112320.003.0011.

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Compared to herpetological population adjustment patterns in North America (sec Holman, 1995c), the patterns in Britain and central and northern Europe seem to be rather straightforward. Basically, (1) very few herpetological species were present in ice-free areas during full glacial times, and (2) formerly glaciated areas were reinvaded by species from the south during warming cycles. Moreover, during climatic optimal warm times, several southern species existed well north of their present ranges. The invasion of southern Europe by northern populations in cold times is taken for granted (e.g., Rocek, 1995), although, as addressed in this chapter, it is difficult to document this in the fossil record. As indicated by geological and fossil evidence, the British Islands were connected to continental Europe during much of the Pleistocene. Although sea level changes in the British late Pleistocene arc a subject of some controversy (Stuart, 1982), it is generally agreed that Britain first separated from Ireland and then from the continent early in the Holocene. The classic idea is that the very depauperate British heretofauna of the cold part of the Devensian (last glacial stage) became somewhat, but not fully enriched by herpetological species during a warming trend that began about 10,000 ybp and lasted until about 8,500 ybp. The fact that Ireland has a much poorer modern herpetofauna (Triturus vulgaris, the rare Bufo calamita, Rana temporaria, and Lacerta vivipara) than Britain, which has six native species of amphibians and six native species of reptiles (Fra/,er, 1983; Smith, 1964), is attributed to Ireland's early separation from Britain. The Irish herpetofauna suggests that this separation occurred rather soon after the final withdrawal of the Devensian (last glacial) ice sheet. One of the most common questions asked about snakes, especially near St. Patrick's Day, is, "Have there ever been any snakes in Ireland?" No fossil snakes have ever been found in Ireland. But since Ireland lacks a terrestrial fossil record during most of the time that snakes have existed, it would seem that snakes could have lived in Ireland during some part of geological time. As far as I am aware, the few Pleistocene deposits containing herpetological remains in Ireland represent very late Devensian (last glacial) times.
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Conference papers on the topic "Holocene Climatic Optimum"

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Белянин, П. С., and Н. И. Белянина. "THE LATE HOLOCENE HISTORY OF VEGETATION OF THE ACCUMULATIVE PLAIN IN THE INNER PART OF THE USSURI BAY." In Геосистемы Северо-Восточной Азии. Crossref, 2021. http://dx.doi.org/10.35735/tig.2021.43.79.012.

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На основе палинологических данных, восстановлена история развития природной среды аккумулятивной равнины в кутовой части Уссурийского залива за последние 5350 кал. л. Определены особенности структуры растительного покрова в завершающую фазу оптимума голоцена, а также при разнонаправленных климатических флуктуациях позднего голоцена. В завершающую фазу оптимума голоцена широколиственные растения в горном обрамлении были распространены более широко, чем в настоящее время. На аккумулятивной равнине преобладали мелколиственные растительные сообщества с доминированием березы обыкновенной, гибридных берез и ольхи. Похолодание, начавшееся в конце среднего и продолжившееся в начале позднего голоцена, привело к сокращению в растительности широколиственных растений и более широкому распространению мелколиственных. В конце позднего голоцена в кутовой части Уссурийского залива сложились природные условия, обусловившие формирование современной структуры растительности. Based on the palynological data, the history of vegetation on the accumulative plain in the inner part of the Ussuri Bay was reconstructed. Features of the structure of the vegetation cover during the final phase of the Holocene optimum and at multidirectional climatic fluctuations in the Late Holocene were identified. Broad-leaf plants in the final phase of the Holocene were more widely-spread on the surrounding mountain than at present. On the accumulative plains grassy meadows with small-leaf plant communities dominated. Deterioration of natural conditions during the transition to the Late Holocene caused a decrease in vegetation of broad- leaved plants and in an increase in the role of small-plants. At the end of the Late Holocene natural conditions developed in the inner part of the Ussuri Bay, that conditioned the formation of the modern structure of vegetation.
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Demkina, Tatiana, Tatiana Khomutova, and Aleksandr Borisov. "STEPPE SOILS AT THE PERIODS OF CLIMATIC CRISES AND OPTIMUMS OF THE HOLOCENE: PRECIPITATION PATTERN IN COLD AND WARM PERIODS OF YEAR." In 20th International Multidisciplinary Scientific GeoConference Proceedings SGEM 2020. STEF92 Technology, 2020. http://dx.doi.org/10.5593/sgem2020/3.1/s13.073.

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