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Chinese Science Bulletin 1998年第9期43卷 757-761页

作者： Shaoquan Li Jian Liu Shengjie Wang zigeng yang Minist Geol & Mineral Resources Inst Marine Geol Qingdao 266071 Peoples R China

Northwest of Cheju Island in the eastern South Yellow Sea there is an arc patch of muddy deposit which coincides with an anticlokwise eddy and thus is referred to as muddy deposit of eddy. Two drilling wells, the YSDP 102 well and the YSDP 103 well, penetrated the muddy deposit and revelated the sedimentary sequence in the sea area during the last deglaciation and the Holocene. Based on shallow seismic profiles, sedimentary features and dating data, stratigraphic units formed in the eastern South Yellow Sea, documents the path, time and process of the earliest post-glacial transgression in the South Yellow Sea are presented, the formation of the Yellow Sea warm current and its control over the Yellow Sea sedimentation are discussed, and deals with the source of the muddy deposit is dealt with.

关键词： South Yellow Sea sedimentary sequence deposit of eddy environmental evolution

The Sedimentary Sequence and Palaeogeographic Changes of the South Yellow Sea Since the Olduvai Subchron

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Acta Geologica Sinica(English Edition) 1994年第2期68卷 195-207页

作者： yang zigeng Institute of Marine Geology, MGM R, Qingdao, Shandong Institute of Marine Geology MGMR Qingdao Shandong

According to the alternation of terrestrial beds and transgressive beds, the sedimentary sequence of the South Yellow Sea since the Olduvai subchron can be divided into 15 stratigraphical intervals. According to the facies analysis, there are 7 transgressive beds and one bed with transgression marks, and classical transgressive-regressive facies sequence also appears in the major transgressive *** evolution in the shelf area involved 4 periods: (1) 1.70-0.5 Ma B. P. was the stage for the development of the Palaeo-yangtze River alluvial plain and delta. Tide influenced -river channel sediments formed during the Olduvai have been found in borehole QC2. The river mouth was located near 124°E and during the transgressive stage from 0.97-0.73 Ma B.P. to the east of 122.2°E, a large-scale undersea delta was formed. In the regressive stage, the shelf area became an alluvial plain. (2) 0.50-0.75 Ma B.P. was a multi-transgressive fluctuation stage during which 3 transgressive beds (HVI, HV, HIV)developed, being dated as 0.50-0.30 Ma B.P., 0.27-0.20 Ma B.P. and 127-75 Ka B.P. respectively, with the extent of transgression increasing gradually. Influenced by southeast monsoons, the eastern China continent began to have a larger moisture source. (3) 75-14 Ka B.P. was the lower sea-level stage during the last glacial period. The downcutting depth of rivers was up to -133 m. The palaeo-yangtze River system flowed northeastwards into the Sea of Japan through the Sea of Japan through the Tsushima and Korean Straits. The interfluvial area became an eroded, weathered high land. In the cores, two short-lived, relatively high sea-level stages were recorded, corresponding to two interstades in the last glacial period. (4) The period since 14 Ka B.P. is the stage for 'Holocene transgression' and the development of the Yellow River-Huaihe River delta. Before 14 Ka the sea level rose to -68 m, and before 11 Ka to -50 m, and the sea-level was once at a standstill or slight

关键词： South Yellow Sea Quaternary sedimentary sequence palaeogeography

Sedimentary Evolution of the Holocene Subaqueous Clinoform off the Southern Shandong Peninsula in the Western South Yellow Sea

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Journal of Ocean University of China 2014年第5期13卷 747-760页

作者： QIU Jiandong LIU Jian SAITO Yoshiki yang zigeng YUE Baojing WANG Hong KONG Xianghuai College of Marine Geo-Science Ocean University of China The Key Laboratory of Marine Hydrocarbon Resources and Environment Geology Ministry of Land and Resources Qingdao Institute of Marine Geology Ministry of Land and Resources Geological Survey of Japan AIST

Based on the stratigraphic sequence formed since the last glaciation and revealed by 3000 km long high-resolution shallow seismic profiles and the core QDZ03 acquired recently off the southern Shandong Peninsula, we addressed the sedimentary characteristics of a Holocene subaqueous clinoform in this paper. Integrated analyses were made on the core QDZ03, including sedimentary facies, sediment grain sizes, clay minerals, geochemistry, micro paleontology, and AMS 14 C dating. The result indicates that there exists a Holocene subaqueous clinoform, whose bottom boundary generally lies at 15–40 m below the present sea level with its depth contours roughly parallel to the coast and getting deeper seawards. The maximum thickness of the clinoform is up to 22.5 m on the coast side, and the thickness contours generally spread in a banded way along the coastline and becomes thinner towards the sea. At the mouths of some bays along the coast, the clinoform stretches in the shape of a fan and its thickness is evidently larger than that of the surrounding sediments. This clinoform came into being in the early Holocene(about 11.2 cal kyr BP) and can be divided into the lower and upper depositional units(DU 2 and DU 1, respectively). The unit DU 2, being usually less than 3 m in thickness and formed under a low sedimentation rate, is located between the bottom boundary and the Holocene maximum flooding surface(MFS), and represents the sediment of a post-glacial transgressive systems tract; whereas the unit DU 1, the main body of the clinoform, sits on the MFS, belonging to the sediment of a highstand systems tract from middle Holocene(about 7–6 cal kyr BP) to the present. The provenance of the clinoform differs from that of the typical sediments of the Yellow River and can be considered as the results of the joint contribution from both the Yellow River and the proximal coastal sediments of the Shandong Peninsula, as evidenced by the sediment geochemistry of the core. As is control

关键词： subaqueous clinoform Holocene Yellow Sea Shandong Peninsula Yellow River provenance sea-level change sedimentary

THE STRATIGRAPHY AND ENVIRONMENT IN THE LIFE-TIME OF PEKING MAN

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海洋地质与第四纪地质 1983年第4期 75-81页

作者： yang zigeng (Institute of Marine Geology, Ministry of Geology and Mineral Resources)Mu Yunzhi (Lanzhou University)Xie Youyu(Institute of Geography, Academia Sinica) Kong Zhaochen(Institute of Botary, Academia Sinica)

It has been over half a century since the Peking Man(Homo erectus Pekinensis)was discovered,and its academic significance is worldwide notable.A comprehe-nsive survey on the relics of Peking Man was conducted from 1978 to *** the participants and organizers of this project,we are here able to report someresults of it in the aspects of the stratigraphy and environment.

关键词： THE STRATIGRAPHY AND ENVIRONMENT IN THE LIFE-TIME OF PEKING MAN In 谢又予 Man 第四纪地质地质学

Ancient Changjiang channel system in the East China Sea continental shelf during the last glaciation

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Science China Earth Sciences 2005年第11期48卷 1972-1978页

作者： LI Guangxue1,2, LIU Yong1, yang zigeng3, YUE Shuhong4, yang Wenda5 & HAN Xibin1 1. College of Marine Geo-science, Ocean University of China, Qingdao 266003, China 2. Shandong Key Laboratory of Sea Floor Resource and Exploration Technique, Qingdao 266003, China 3. Qingdao Institute of Marine Geology, Qingdao 266071, China 4. College of Marine Environment, Ocean University of China, Qingdao 266003, China 5. First Survey Team of Marine Geology, Shanghai Bureau of Petroleum, Shanghai 201208, China 1. College of Marine Geo-science Ocean University of China 266003 Qingdao China 2. Shandong Key Laboratory of Sea Floor Resource and Exploration Technique 266003 Qingdao China 3. Qingdao Institute of Marine Geology 266071 Qingdao China 4. College of Marine Environment Ocean University of China 266003 Qingdao China 5. First Survey Team of Marine Geology Shanghai Bureau of Petroleum 201208 Shanghai China

Based on the data of high-resolution seismic profiles, an ancient river channel sys-tem of the last glaciation occurred along the Zhedong and Xihu depression in the southeast of Hupijiao rise. The distribution of the channel fill system shows that the ancient Changjiang River went through the Changjiang depression into the low land plain of the outside continental shelf during the low sea level cycle of the last glaciation. The big channel fill into Okinawa Trough is not found due to the depletion of the river kinetic energy in the low land plain. The river discharge dispersal was of an important role to the dilution of the northern Okinawa Trough sea at that time. Six ancient river channel systems (A―F), which are main distributaries of ancient Changjiang in the East China Sea continental shelf during the last glaciation, may be buried off the modern Changjiang estuary. The distribution of these channels coincides with the zonal elevations in the sea floor.

关键词： last glaciation, continental shelf plain, Changjiang River, ancient channel fill

末次冰消期以来黄海海平面变化与黄海暖流的形成

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海洋地质与第四纪地质 1999年第1期19卷 13-24页

作者：刘健李绍全王圣洁杨子赓葛宗诗国土资源部海洋地质研究所韩国资源研究所

ＹＳＤＰ１０２孔和ＹＳＤＰ１０３孔位于南黄海东南侧冷涡所对应的泥质沉积区，它们揭示了自末次冰消期以来的海侵沉积序列：海侵滞留沉积→潮流砂脊／潮坪～海滩沉积→陆架泥质沉积。该沉积序列上部的陆架泥质沉积厚度可达５０余米，... 详细信息

ＹＳＤＰ１０２孔和ＹＳＤＰ１０３孔位于南黄海东南侧冷涡所对应的泥质沉积区，它们揭示了自末次冰消期以来的海侵沉积序列：海侵滞留沉积→潮流砂脊／潮坪～海滩沉积→陆架泥质沉积。该沉积序列上部的陆架泥质沉积厚度可达５０余米，在浅地震剖面上其内部存在一个明显的反射界面，从而将泥质沉积体分为上、下两个单元。泥质沉积体呈灰绿色调，含少量自生黄铁矿，但其内反射界面以上的沉积物含水量高。根据两个钻孔岩心中有孔虫的分布规律、泥质沉积层的化学组分、沉积磁组构特征以及现有测年数据，得到如下结论：（１）黄海暖流形成于大约６ｋａＢ．Ｐ．，（２）泥质沉积层内反射界面以上的沉积物是与黄海暖流伴生的冷涡沉积，（３）黄海地区末次冰消期海侵自略早于１４ｋａＢ．Ｐ．之前开始，至约６ｋａＢ．Ｐ．海平面达到最高位置。从６ｋａＢ．Ｐ．至今，海平面经历了几次波动，即在６～４ｋａＢ．Ｐ．和３～１．９ｋａＢ．Ｐ．海平面超过现今海平面位置；在４～３ｋａＢ．Ｐ．和１．９ｋａＢ．Ｐ．～现代，海平面有所降低，可能与现今海平面高度相当。

关键词：海平面变化黄海暖流末次冰消期全新世

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指套牙刷口腔保健作用的试验观察

实用口腔医学杂志 2002年第4期18卷 353-354页

作者：邱洪晟刘漪杨自更刘爱中刘健张京雷李力兰州军区乌鲁木齐总医院新疆医科大学生理学教研室新疆军区36007部队卫生队北京大学口腔医院

目的 :探讨指套牙刷的口腔保健作用。方法 :用自制硅胶指套牙刷刷当天拔出牙的牙面、标准硬质石膏试件及健康成人口腔牙齿 ,然后检测牙面菌斑去除度、试件表面磨损度及刷后牙刷存菌数。结果 :指套牙刷刷 3～ 5min后 ,牙面菌斑去除度与... 详细信息

目的 :探讨指套牙刷的口腔保健作用。方法 :用自制硅胶指套牙刷刷当天拔出牙的牙面、标准硬质石膏试件及健康成人口腔牙齿 ,然后检测牙面菌斑去除度、试件表面磨损度及刷后牙刷存菌数。结果 :指套牙刷刷 3～ 5min后 ,牙面菌斑去除度与通用牙刷相同 ;试件表面磨损 0度率为 93.3% ( 2 8/ 30 ) ,优于通用牙刷的2 3.3% ( 7/ 30 ) ;刷后牙刷存菌数低于通用牙刷。结论 :指套牙刷可有效去除牙面菌斑 ,牙面磨损少且刷后牙刷存菌数低。

关键词：指套牙刷口腔保健实验研究牙菌斑

Increase in the variability of terrestrial carbon uptake in response to enhanced future ENSO modulation

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Atmospheric and Oceanic Science Letters 2025年第1期18卷 32-38页

作者： Younong Li Li Dan Jing Peng Qidong yang Fuqiang yang Key Laboratory of Regional Climate-Environment for Temperate East Asia Institute of Atmospheric PhysicsChinese Academy of SciencesBeijingChina Key Laboratory of Atmospheric Environment and Processes in the Boundary Layer over the Low-Latitude Plateau Region Department of Atmospheric ScienceYunnan UniversityKunmingChina

El Niño-Southern Oscillation(ENSO)is a major driver of climate change in middle and low latitudes and thus strongly influences the terrestrial carbon cycle through land-air *** the ENSO modulation and carbon flux variability are projected to increase in the future,but their connection still needs further *** investigate the impact of future ENSO modulation on carbon flux variability,this study used 10 CMIP6 earth system models to analyze ENSO modulation and carbon flux variability in middle and low latitudes,and their relationship,under different scenarios simulated by CMIP6 *** results show a high consistency in the simulations,with both ENSO modulation and carbon flux variability showing an increasing trend in the *** higher the emissions scenario,especially SSP5-8.5 compared to SSP2-4.5,the greater the increase in *** flux variability in the middle and low latitudes under SSP2-4.5 increases by 30.9%compared to historical levels during 1951-2000,while under SSP5-8.5 it increases by 58.2%.Further analysis suggests that ENSO influences mid-and low-latitude carbon flux variability primarily through *** occurrence may potentially be attributed to the increased responsiveness of gross primary productivity towards regional temperature fluctuations,combined with the intensified influence of ENSO on land surface temperatures.

关键词： Carbon variability ENSO modulation CMIP6 models

High-temperature-tolerant flexible supercapacitors: Gel polymer electrolytes and electrode materials

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Journal of Energy Chemistry 2025年第1期100卷 426-457页

作者： Chong Peng Xinyi Huang Mingwei Zhao Shuling Liao Quanhong yang Nianjun yang Siyu Yu School of Chemistry & Chemical Engineering Southwest University Nanoyang Group Tianjin Key Laboratory of Advanced Carbon and Electrochemical Energy Storage School of Chemical Engineering and Technology and Collaborative Innovation Center of Chemical Science and Engineering (Tianjin) Tianjin University Department of Chemistry & IMO-IMOMEC Hasselt University

The development of flexible supercapacitors(FSCs) capable of operating at high temperatures is crucial for expanding the application areas and operating conditions of supercapacitors. Gel polymer electrolytes and electrode materials stand as two key components that significantly impact the efficacy of hightemperature-tolerant FSCs(HT-FSCs). They should not only exhibit high electrochemical performance and excellent flexibility, but also withstand intense thermal stress. Considerable efforts have been devoted to enhancing their thermal stability while maintaining high electrochemical and mechanical performance. In this review, the fundamentals of HT-FSCs are outlined. A comprehensive overview of state-of-the-art progress and achievements in HT-FSCs, with a focus on thermally stable gel polymer electrolytes and electrode materials is provided. Finally, challenges and future perspectives regarding HT-FSCs are discussed, alongside strategies for elevating operational temperatures and *** review offers both theoretical foundations and practical guidelines for designing and manufacturing HT-FSCs, further promoting their widespread adoption across diverse fields.

关键词： Flexible supercapacitors High-temperature tolerance Gel polymer electrolytes Electrode materials

Role of the Greenland Sea ice anomaly in the late-spring drought over Northwest China

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Atmospheric and Oceanic Science Letters 2025年第1期18卷 1-5页

作者： yang Liu Huopo Chen Nansen-Zhu International Research Centre Institute of Atmospheric Physics Chinese Academy of SciencesBeijingChina Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters Nanjing University for Information Science and TechnologyNanjingChina

Drought across Northwest China in late spring has exerted a vital effect on the local climate and agricultural production,and has been alleviated during the past *** study explored the influence of the preceding Arctic sea ice on the May drought in Northwest China caused by the precipitation *** analysis indicated that when the Greenland Sea ice concentration is abnormally high during February to April,the dry conditions in Northwest China tend to be *** increase of sea ice in the Greenland Sea can excite a meridional circulation,which causes sea surface temperature(SST)anomalies in the North Atlantic via the sea-air interaction,manifested as significant warm SST anomalies over the south of Greenland and the subtropical North Atlantic,but negative SST anomalies over the west of the *** abnormal SST pattern maintains to May and triggers a zonal wave train from the North Atlantic through Scandinavia and Central Asia to Northwest China,leading to abnormal cyclones in Northwest ***,Northwest China experiences a more humid climate than usual.

关键词： Arctic sea ice Greenland Sea North Atlantic SST Drought Northwest China