Holocene
['hɔlәusi:n]
adj. 全新世的;全新统的
n.a.
【地】全新世(的)
Holocene
Holocene['hɔləsi:n]1.■【地质学】adj. 全新世的,全新统的 —n.1.■全新世
HoloceneHolocene[ˈhɔləusi:n]adj.1.■【地质】全新统的, 全新世[纪]的
词性变化Holocene[ˈhɔləusi:n]n.1.■【地质】全新世[纪]
[ˈhɒləsiːn]
adjective
- (Geology)of, relating to, or denoting the present epoch, which is the second epoch in the Quaternary period and followed the Pleistocene
(地质)全新世的,全新统的(第四纪的第二个纪元,在更新世之后)。 亦称 Recent
■[as noun the Holocene]the Holocene epoch or the system of deposits laid down during this time
全新世,全新统;全新世沉积物体系 - The Holocene epoch has lasted from about 10,000 years ago to the present day. It covers the period since the ice retreated after the last glaciation and it is sometimes regarded as just another interglacial period
- late 19th cent.: coined in French from holo- 'whole' + Greek kainos 'new'
Holocene
Holocene
■But high TOC and C/N ratio during MIS 5.1, 3.3 to 3.2 and the Holocene reflect that the terrigenous organic matter input increased during interglacial periods.
2期和全新世高的有机碳含量和C/N比值反映间冰期陆源有机物质输入量的增加.
■Increases in fine-and silt-grained terrigenous components from MIS 5.3 to the Middle Holocene imply that sea ice on the Bering Sea slope extended continuously in a cooling climate.
MIS5.3期至中全新世,不断增加的陆源砂级和粉砂级颗粒组分说明随着气候的逐渐变冷,陆架海冰在不断扩张.
■DENG Qi-dong,WANG Yi-peng,LIAO Yu-hua,et al.1984.Collapse wedges by fault scarps and Holocene history of movement along Helanshan piedmont fault[J].Science Bulletin,29 (9):557-560 (in Chinese).
[1]邓起东,汪一鹏,廖玉华,等.1984.断层崖崩积楔及贺兰山山前断裂全新世活动历史[J].科学通报,29(9):557-560.
■Zhang Peng-xi,Zhang Bao-zhen,Qian Gui-min,Li Hai-jun,Xu Li-ming.The study of paleoclimatic parameter of Qinghai Lake since Holocene[J].Quat Sci,1994,14 (3):225-238 (in Chinese with English abstract).
[22]张彭熹,张保珍,钱桂敏,李海军,徐黎明.青海湖全新世以来古环境参数的研究[J].第四纪研究,1994,14(3):225-238.
■Characteristics of Holocene Sedimentary Provinces in Shanghai Region
上海地区全新世沉积分区及其特征
■Sea Level Changes of Holocene in Shanghai Region
上海地区全新世海平面的变化
■These rapid climate changes occurred in the last glacial stage, but also in the Holocene and the middle and early Pleistocene.
不仅见于末次冰期,也发生在全新世和早、中更新世。
■REGIONAL DIFFERENCE IN HOLOCENE VEGETATIONAL CHANGE AND THE POSSIBLE MIGRATION OF MAJOR TREES IN NE CHINA
东北全新世乔木种类演化的区域差异及其迁移问题
■Holocene Environmental and Climatic Changes from the Information of Peat Bog Sediment in Northeastern China
东北地区以泥炭为信息载体的全新世气候变迁研究进展
■Study on characteristics of new activity and Holocene slip rate along Maqu fault of East Kunlun Active Fault
东昆仑断裂带东段玛曲断裂新活动特征及全新世滑动速率研究
■HOLOCENE SLIP RATE ALONG THE EASTERN SEGMENT OF THE KUNLUN FAULT
东昆仑活动断裂带东段全新世滑动速率研究
■Pollen Record and Forming Process of the Peatland in Late Holocene in the North Bank of the Xingkai Lake, China
中国兴凯湖北岸平原晚全新世花粉记录及泥炭沼泽形成
■Holocene cyclic climate changes and desertifications in northern China
中国北方沙漠地区全新世气候变化的周期性探讨
■M. (2002) Holocene rock uplift and subsidence in coastal area of Taiwan: AGU 2002 Fall meeting.
中国地质学会九十一年年会暨学术研讨会摘要集。
■Variation of sea level along the coast of China during Holocene epoch
中国沿海全新世海平面变化曲线
■The Climatic Record of Organic Matter in the Paleosol from the Yuanbao Holocene Profile
临夏塬堡全新世黄土剖面古土壤有机质碳同位素的气候记录
■Holocene Sediment Texture and Its Environmental Meaning of Donghaizi Lake in Ulan Buh Desert
乌兰布和沙漠东海子湖全新世湖相沉积结构分析及其环境意义
■High-Resolution Holocene Environmental Changes in the Thar Desert,
也许是中全新世的一个决定因素。
■THE RECORDS OF CLIMATIC CHANGE FROM A STALAGMITE DURING THE LATE TIME OF THE MIDDLE HOLOCENE IN NINGLANG AREA, YUNNAN
云南宁蒗地区中全新世晚期气候变化的石笋记录
■The evolution of mangrove forest on the basis of palynological study of Holocene in Hainan Island
从海南岛全新世孢粉研究看海滨红树林的演化
■From the LGM(18 ka BP) to the Holocene transgression(10 ka BP),great changes took place in world climate, including the paleo monsoon activity which occured in the Eastern Asia.
从距今18000年的最后冰期最盛时期到距今10000年开始的全新世海侵,全球气侯发生过急剧的变化。位于亚洲东部的古季风活动也经历了盛衰变化。
■Based on the sedimentary system of Poyang Lake basin from Holocene,the sedimentary system of the margin of Poyang Lake basin presents asymmetry,and shows cyclicity in vertival series.
以全新世以来鄱阳湖盆地沉积体系为基础,发现在鄱阳湖盆地边缘沉积体系呈现不对称性,垂向系列上呈现旋回性。
■Keywords Holocene;Beachrock;Paleoclimate;Lianyungang;
全新世;海滩岩;古气候;连云港;
■Centurial Cycles of Variation of the Holocene East Asian Monsoon
全新世东亚季风变化的百年尺度周期
■Climatic change and environmental characteristic of Holocene in North China
全新世中国北方气候变化及环境特征
■Medial-latter stage of Holocene epoch
全新世中晚期
■warm period of Middle Holocene
全新世中期
■Changes of environment and animal geography of the West Liaohe River Basin since middle Holocene
全新世中期以来西辽河流域动物地理与环境变迁
■middle Holocene transgression
全新世中期海侵
■Evolutionary Process of Hydrologic Cycle and Periodicity of Groundwater Change in North China Plain since Holocene
全新世以来华北平原层圈间水循环演化过程与区域地下水演变周期性
■The main sediments of Holocene sections are clay and sand soil with mini sand layers in North Taklimakan desert.
全新世以来塔克拉玛干北部(以下简称塔干北)主要沉积物组成为亚粘质土、细砂夹杂着粉砂。
■Deposition and forward movement of the coastline in the middle part of Jiangsu since Holocene
全新世以来江苏中部地区海岸的淤进
■Changes of Land and Sea in the Shuoxiang Lake Area Since Holocene
全新世以来硕项湖地区的海陆演变
■River channel evolution of the Yangtze river estuary since Holocene epoch
全新世以来长江河口段河道的演变
■The Northern Boundary of Dry Farming in the North of China During the Typical Period of Holocene Epoch
全新世典型期中国北方旱作农业分布北界
■Studies of Chronology of Millennial Time Scale Climate Oscillations in the Holocene
全新世千年尺度气候振荡的年代学研究
■However,when it came to the end of Holocene Climatic Optimum(5.98-3.67 kaB.P.)
全新世大暖期中期(5.98~3.67 kaB.P.)
■ENVIRONMENTAL EVOLUTION RECORDED BY LAKE SEDIMENTS FROM ERHAI LAKE, YUNNAN PROVINCE IN HOLOCENE MEGATHERMAL
全新世大暖期云南洱海环境演化的湖泊沉积记录
■HOLOCENE SOLUBLE SALT SEDIMENTS OF ANGULINAO LAKE AND ITS ENVIRONMENT
全新世安固里淖易溶盐沉积与环境
■The Holocene intermediate stage was associated with a normal marine environment, with increased oceanic sediments and a warmer and moist climate, indicating a good marine ecological environment.
全新世早-中期为正常海相环境,沉积物中海源物质增加,气候温暖湿润,指示当时海洋生态环境较好;
■The vegetation was dominated by steppe or sparse steppe in the early Holocene,corresponding to a warm and dry climate.
全新世早期气候温凉略干,为草原型植被或稀疏草原型植被;
■A Study on Interaction Between Human Activities and Past Soil and Water Loss in Holocene
全新世时期古水土流失与古人类活动相互影响分析
■The Holocene Epoch or its system of deposits.
全新世时期或该时期的沉积系统
■Decline of Surface Temperature and Salinity in the Western Tropical Pacific Ocean in the Holocene Epoch
全新世时期热带太平洋西部表层温度和盐度的降低
■Sparse woods-grassland of the Late Holocene is dominated by the Arte-misia, Chenopodiaceae, Pinus and Betula, reflecting that the climate was a littlecool and dry similarly to that of the present time.
全新世晚期是以蒿、藜、松和桦为主的疏林-草原,此时气候温凉、略干与现代相近。
■THE LAND USE ARRANGEMENT OF CHINA IN THE HOLOCENE MEGATHERMAL PERIOD AND ITS SIGNIFICANCE
全新世暖期我国土地利用的格局及其意义
■Holocene Climate Change and Desertification in Northern China
全新世气候变化与中国北方沙漠化
■Holocene Climatic Change and Rise and Fall of Prehistoric Civilization in the Yangtze River Delta
全新世气候变化与长江三角洲史前文化兴衰
■Holocene climate and environment
全新世气候环境
■Research on Rivers Change in Luoyang Basin in Holocene
全新世洛阳盆地的水系变迁研究