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Relevant bibliographies by topics / Holocene Climatic Optimum

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Journal articles

Academic literature on the topic 'Holocene Climatic Optimum'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Holocene Climatic Optimum"

1

He, Y., Wilfred H. Theakstone, Zhang Zhonglin, et al. "Asynchronous Holocene climatic change across China." Quaternary Research 61, no. 1 (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

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2

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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3

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 (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

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4

Yang, Xunlin, Hong Yang, Baoyan Wang, et al. "Early-Holocene monsoon instability and climatic optimum recorded by Chinese stalagmites." Holocene 29, no. 6 (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 stalagmi

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5

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 (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

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6

Zhang, Jingwei, Xinggong Kong, Kan Zhao, et al. "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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7

Nazarova, L. B., N. G. Razjigaeva, B. Diekmann, et al. "Reconstruction holocene environmental changes in North-Western Pacific in relation to paleorecord from Shikotan Island." Доклады Академии наук 486, no. 2 (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 i

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8

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 (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 char

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9

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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10

Baroni, Carlo, and Giuseppe Orombelli. "The Alpine “Iceman” and Holocene Climatic Change." Quaternary Research 46, no. 1 (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 gl

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