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| 1 | 内蒙古巴丹吉林沙漠成因的粒度分析和热发光测年新证据(英文)显示文摘巴丹吉林沙漠位于中国内蒙古自治区的西部 ,是中国第三大沙漠。过去通常认为该沙漠中沙丘的可能沙源来自附近的各种沉积物和岩石 ,包括弱水河扇的沉积物 ,弱固结的二叠纪页岩、白垩纪砂岩和砾岩以及戈壁阿尔泰的古老岩石。根据对风成砂的粒度观测 ,有证据表明在沙漠内部的风成砂沉积朝东南方向具有较弱的但又确实的变细趋势。这与沙丘横脊线的SW -NE向排列以及坡面的南东指向是一致的。因此 ,可以认为西北部的弱水河冲积扇是巴丹吉林沙漠风成砂的最可能的沙源。在西北部风成床沙覆盖了较老弱水河扇起源的冲积物。这种沉积物的热发光测年范围在 190~ 10 0kaBP之间。由于测量中对沉积物漂白可能不完全以及对其中平均古水含量估算均存在不确定性 ,同时由于对沙漠该地区风成作用开始之前堆积的沉积物进行了测年 ,这一数据范围代表了最大的年龄。另外三个风成砂测年结果分别接近 133 6 6和 2 2ka ,代表有关巴丹吉林沙漠西北部风成作用开始的最小年龄。沙漠的沙丘高度平均为 2 0 0~ 30 0m ,但在东南部偶尔可达 4 5 0m。一些学者曾提出风成床沙覆盖了一个陡峭岛山突起的假说 ,来解释这些异常的空间。本次研究发现 ,在研究区之下是一个产状水平的白垩纪扇砾岩和砂岩的台地 。 | Steffen Mischke | 2005 | 古地理学报2005，7，1： | 26 |
| 2 | Carbon and Oxygen Isotopic Composition of Surface-Sediment Carbonate in Bosten Lake (Xinjiang,China) and its Controlling Factors显示文摘博斯顿·莱克是有在 Tianshan 山融化冰和雪主要供应的水的一个中间纬度的湖。湖的 depositional 环境是空间地由于在湖的西方的部分的主要入口和单个插头的最近不一致。分析结果证明最近的湖沉积的同位素的作文与这特定的湖的 depositional 环境有关并且到结果的碳和氧焦化矿物学。在在 Kaidu 河入口和 Kongqi 河插头之间的西南的湖区域,碳同位素作文(δ
13 C )碳酸盐沉积的价值( −1 ‰ 到 −2 ‰)没有关系到碳酸盐的氧同位素作文(δ
18 O )价值( −7 ‰ 到 8 ‰),与显示出低可变性的两同位素。碳酸盐内容是低的(<20%) 。X 光检查衍射分析的碳酸盐矿物质主要由方解石组成,当霰石没被记录时。湖水的咸度在由于 Kaidu 河流入的河口区域是低的。在比较,碳和氧同位素价值在湖的中间、东方的部分是更高的,与 δ
13 C 价值在之间近似 +0.5 ‰和 +3 ‰,和 δ
18 在 −1 ‰和 −5 ‰之间的 O 价值。在稳定的氧和碳同位素之间有中等关联,与约 0.63 的关联 r 的一个系数。这暗示湖水有一相对短的住处时间。碳酸盐矿物质在湖的中间、东方的区域组成方解石和霰石。霰石和 Mg 方解石在更高的湖水咸度和温度被形成,并且更大的蒸发完成。在在水和相关的碳和氧同位素珍视的大气的公司 2 原因之间的湖和提高的同位素的平衡的中间、东方的区域的更盐的湖水为霰石和 Mg 方解石决定了。蒸发和生物过程是为咸度和在博斯顿·莱克的表面沉积碳酸盐的碳酸盐矿物学影响的主要原因。在空气和水身体之间的湖水住处时间和 CO 2 交换控制碳和碳酸盐沉积的氧同位素作文。另外,有机物污染和分解导致湖表面沉积碳酸盐的反常地低的碳同位素价值。 | Steffen MISCHKE Alexander PROKOPENKO | 2009 | Acta Geologica Sinica(English Edition)2009，83，2： | 14 |
| 3 | Carbon and Oxygen Isotopic Compositions: How Lacustrine Environmental Factors Respond in Northwestern and Northeastern China显示文摘Surface lake sediments,28 from Hoh Xil,24 from northeastern China,99 from Lake Bosten,31 from Ulungur and 26 from Heihai were collected to determine δ13C and δ18O values.Considering the impact factors,conductivity,alkalinity,pH,TOC,C/N and carbonate-content in the sediments,Cl,P,S,and metal element ratios of Mg/Ca,Sr/Ca,Fe/Mn of bulk sediments as environmental variables enable evaluation of their influences on δ13C and δ18O using principal component analysis(PCA) method.The closure and residence time of lakes can influence the correlation between δ13C and δ18O.Lake water will change from fresh to brackish with increasing reduction and eutrophication effects.Mg/Ca in the bulk sediment indicates the characteristic of residence time,Sr/Ca and Fe/Mn infer the salinity of lakes.Carbonate formation processes and types can influence the δ13C–δ18O correlation.δ18O will be heavier from Mg-calcite and aragonite formed in a high-salinity water body than calcite formed in freshwater conditions.When carbonate content is less than 30%,there is no relationship with either δ13C or δ18O,and also none between δ13C and δ18O.More than 30%,carbonate content,however,co-varies highly to δ13C and δ18O,and there is also a high correlation between δ13C and δ18O.Vegetation conditions and primary productivity of lakes can influence the characteristics of δ13C and δ18O,and their co-variance.Total organic matter content(TOC) in the sediments is higher with more terrestrial and submerged plants infilling.In northeastern and northwestern China,when organic matter in the lake sediments comes from endogenous floating organisms and algae,the δ13C value is high.δ13C is in the range of 4‰ to 0‰ when organic matter comes mainly from floating organisms(C/N<6);in the range of 4‰ to 8‰ when organic matter comes from diatoms(C/N=6 to 8);and 8‰ to 4‰ when organic matter comes from aquatic and terrestrial plants(C/N>8). | ZHANG Chengjun FAN Rong LI Jun Steffen MISCHKE laise DEMBELE HU Xiaolan | 2013 | Acta Geologica Sinica(English Edition)2013，87，5： | 13 |
| 4 | Varietal identification of tea(Camellia sinensis)using nanofluidic array of single nucleotide polymorphism(SNP)markers显示文摘Apart from water,tea is the world’s most widely consumed beverage.Tea is produced in more than 50 countries with an annual production of approximately 4.7 million tons.The market segment for specialty tea has been expanding rapidly owing to increased demand,resulting in higher revenues and profits for tea growers and the industry.Accurate varietal identification is critically important to ensure traceability and authentication of premium tea products,which in turn contribute to on-farm conservation of tea genetic diversity.Using a set of single nucleotide polymorphism(SNP)markers developed from the expressed sequence tag(EST)database of Camilla senensis,we genotyped deoxyribonucleic acid(DNA)samples extracted from a diverse group of tea varieties,including both fresh and processed commercial loose-leaf teas.The validation led to the designation of 60 SNPs that unambiguously identified all 40 tested tea varieties with high statistical rigor(p<0.0001).Varietal authenticity and genetic relationships among the analyzed cultivars were further characterized by ordination and Bayesian clustering analysis.These SNP markers,in combination with a high-throughput genotyping protocol,effectively established and verified specific DNA fingerprints for all tested tea varieties.This method provides a powerful tool for variety authentication and quality control for the tea industry.It is also highly useful for the management of tea genetic resources and breeding,where accurate and efficient genotype identification is essential. | Wan-Ping Fang Lyndel W Meinhardt Hua-Wei Tan Lin Zhou Sue Mischke Dapeng Zhang | 2014 | Horticulture Research2014，1，1： | 13 |
| 5 | Exogenous abscisic acid significantly affects proteome in teaplant (Camellia sinensis) exposed to drought stress显示文摘Tea[Camellia sinensis(L.)O.Kuntze]is an important economic crop,and drought is the most important abiotic stress affecting yield and quality.Abscisic acid(ABA)is an important phytohormone responsible for activating drought resistance.Increased understanding of ABA effects on tea plant under drought stress is essential to develop drought-tolerant tea genotypes,along with crop management practices that can mitigate drought stress.The objective of the present investigation is evaluation of effects of exogenous ABA on the leaf proteome in tea plant exposed to drought stress.Leaf protein patterns of tea plants under simulated drought stress[(polyethylene glycol(PEG)-treated]and exogenous ABA treatment were analyzed in a time-course experiment using two-dimensional electrophoresis(2-DE),followed by matrix-assisted laser desorption/ionization time-of-flight(MALDI-TOF)mass spectrometry(MS).Among the 72 protein spots identified by MALDI-TOF MS,16 proteins were downregulated and two were upregulated by exogenous ABA.The upregulated proteins have roles in glycolysis and photosystem II stabilization.Twenty-one protein spots were responsive to drought stress and most participate in carbohydrate and nitrogen metabolism,control of reactive oxygen species(ROS),defense,signaling or nucleic acid metabolism.The combined treatments of exogenous ABA and drought showed upregulation of 10 protein spots at 12 h and upregulation of 11 proteins at 72 h after initiation of drought stress.The results support the importance of the role that ABA plays in the tea plant during drought stress,by improving protein transport,carbon metabolism and expression of resistance proteins. | Lin Zhou Hui Xu Sue Mischke Lyndel W Meinhardt Dapeng Zhang Xujun Zhu Xinghui Li Wanping Fang | 2014 | Horticulture Research2014，1，1： | 12 |
| 6 | High-Resolution Records of the Holocene Paleoenvironmental Variation Reflected by Carbonate and Its Isotopic Compositions in Bosten Lake and Response to Glacial Activities显示文摘The Early Holocene paleoclimate in Bosten Lake on the northern margin of the Tarim Basin, southern Xinjiang, is reconstructed through an analysis of a 953 cm long core (BSTC2000) taken from Bosten Lake. Multiple proxies of this core, including the mineral components of carbonate, carbonate content, stable isotopic compositions of carbonate, Ca/Sr, TOC and C/N and C/S of organic matter, are used to reconstruct the climatic change since 8500 a B.P. The chronology model is made by nine AMS 14C ages of leaves, seeds and organic matter contained in two parallel cores. The climate was cold and wet during 8500 to 8100 a B.P. Temperature increased from 8100 to 6400 a B.P., the climate was warm and humid, and the lake expanded. The lake level was highest during this stage. Then from 6400 to 5100 a B.P., the climate became cold and the lake level decreased slightly. During the late mid-Holocene, the climate was hot and dry from 5100 to 3100 a B.P., but there was a short cold period during 4400 to 3800 a B.P. At this temporal interval, a mass of ice and snow melting water supplied the lake at the early time and made the lake level rise. The second highest lake level stage occurred during 5200 to 3800 a B.P. The climate was cool and wet during 3100 to 2200 a B.P., when the lake expanded with decreasing evaporation. The lake had the last short-term high level during 3100 to 2800 a B.P. After this short high lake level period, the lake shrank because of the long-term lower temperature and reduced water supply. From 2200 to 1200 a B.P., the climate was hot and dry, and the lake shrank greatly. Although the temperature decreased somewhat from 1200 a B.P. to the present, the climate was warm and dry. The lake level began to rise a little again, but it did not reach the river bed altitude of the Konqi River, an outflow river of the Bosten Lake. | ZHANG Chengjun ZHENG Mianping Alexander PROKOPENKO Steffen MISCHKE GOU Xiaohui YANG Qili ZHANG Wanyi FENG Zhaodong | 2009 | Acta Geologica Sinica(English Edition)2009，83，6： | 10 |
| 7 | 内蒙古萨拉乌苏河流域滴哨沟湾全新世早—中期湖相沉积的地球化学古气候响应显示文摘通过对毛乌素沙漠南缘萨拉乌苏河流域滴哨沟湾剖面沉积物粒度、有机碳含量(TOC)、碳酸盐含量、无机碳酸盐碳氧同位素组成等分析测试,在已有的大量年代测定数据基础上,重建了该地区末次冰期晚期到中全新世期间的古环境。分析表明,11 000~9 950aBP滴哨沟湾地区气候干凉,萨拉乌苏河受陕北高原降水和当地冰溶地下水补给;9 950~9 100aBP为全新世初温度、降雨增加时期,有效湿度较高,滴哨沟湾湖泊开始形成;9 100~5 850aBP气温继续上升,降雨增加,但相对湿度减小,该时期是滴哨沟湾湖泊发育最大时期,湖泊水体滞留时间较长;5 850~5 100aBP气温和降水开始下降,湖泊收缩;5 100~4 700aBP期间温度和降水继续下降,湖泊环境逐渐转变为沼泽环境;4 700~4 500aBP期间滴哨沟湾沙漠化,形成了古流动沙丘沙沉积,干旱化加强;而在4 500~4 380aBP时又一次短暂的温湿气候,在沙丘表层钙板隔水层之上形成了短暂的小规模积水;自4 380aBP之后,滴哨沟湾地区沙漠化,干旱状况持续到现在。 | 赵琦 樊荣 李保生 Steffen Mischke 张成君 | 2013 | 海洋地质与第四纪地质2013，33，4： | 9 |
| 8 | 青藏高原东北缘冬给错纳湖全新世湖面波动显示文摘青藏高原处于东亚季风、印度季风和西风环流交互作用区.末次冰消期以来,太阳辐射对该地区的古气候环境产生了重要影响,湖泊随着季风系统的变化发生了明显的水位升降,对湖岸阶地的形成起到了直接作用.本项研究重建了青藏高原东北缘冬给错纳湖湖岸阶地记录的湖面波动历史,试图了解青藏高原季风系统演变过程.通过湖泊北岸265 cm厚湖岸阶地沉积物粒度、碳酸盐、矿物、元素和介形虫古环境指标,结合OSL年代模式,分析表明在约10. 2 ka B. P.之前水体较浅;约10. 2~9. 0 ka B. P.湖面开始上升,气候凉湿;9. 0~8. 5 ka B. P.为印度季风强盛期,湖面明显上升,降雨量增高、温度上升;8. 5~7. 9 ka B. P.湖面降低与气候变冷有关;7. 9~7. 0 ka B. P.印度季风开始减弱,气温、降雨下降,但有效湿度较大,湖面降低;7. 0~6. 1 ka B. P.湖面上升可能与低蒸发作用有关,印度季风仍然影响该地区;6. 1~5. 2 ka B. P.,印度季风衰退,气候逐渐变冷、降雨量减小、水体变浅;5. 2~4. 6 ka B. P.气候冷干,有效湿度减小,湖面进一步下降;4. 6 ka B. P.至今气候干冷,东亚季风衰退,湖面下降,期间也可能受西风环流影响而有短暂的降雨增加时期. | 张菀漪 张静雅 Nusrat Nazir Safarov Khomid 郑淇 Mischke Steffen 张成君 | 2019 | 第四纪研究2019，39，4： | 9 |
| 9 | Developing single nucleotide polymorphism(SNP)markers from transcriptome sequences for identification of longan(Dimocarpus longan)germplasm显示文摘Longan(Dimocarpus longan Lour.)is an important tropical fruit tree crop.Accurate varietal identification is essential for germplasm management and breeding.Using longan transcriptome sequences from public databases,we developed single nucleotide polymorphism(SNP)markers;validated 60 SNPs in 50 longan germplasm accessions,including cultivated varieties and wild germplasm;and designated 25 SNP markers that unambiguously identified all tested longan varieties with high statistical rigor(P<0.0001).Multiple trees from the same clone were verified and off-type trees were identified.Diversity analysis revealed genetic relationships among analyzed accessions.Cultivated varieties differed significantly from wild populations(Fst=0.300;P<0.001),demonstrating untapped genetic diversity for germplasm conservation and utilization.Within cultivated varieties,apparent differences between varieties from China and those from Thailand and Hawaii indicated geographic patterns of genetic differentiation.These SNP markers provide a powerful tool to manage longan genetic resources and breeding,with accurate and efficient genotype identification. | Boyi Wang Hua-Wei Tan Wanping Fang Lyndel W Meinhardt Sue Mischke Tracie Matsumoto Dapeng Zhang | 2015 | Horticulture Research2015，2，1： | 6 |
| 10 | 内蒙古萨拉乌苏河米浪沟湾MIS 5以来生态环境演变特征显示文摘通过对毛乌素沙漠南缘萨拉乌苏河流域米浪沟湾地层中有机质含量(TOC)和饱和烃分布特征,以及沉积物中碳酸盐碳氧同位素组成的分析,讨论了该地区末次间冰期以来生态环境的演变特征和过程。MIS5阶段为森林草原环境,气候比较湿润,河流径流量较大;MIS4和MIS2阶段气候干冷,以沙漠堆积为主,但MIS2在16.9-18.4kaBP期间有一次持续大约1.5ka的古环境适宜时期,森林草原发育;MIS3阶段气候温暖湿润,森林草原环境,湖泊发育;全新世早中期总体上向干旱方向发展,湖泊动荡短暂,为较少森林的草原环境。到晚全新世以沙漠沉积为主,成为与目前生态环境相似的干草原环境。该地区的生态环境演变特征反映出主要受冬夏季风变化控制,但如果西风环流加强时期植被也相对发育。 | 樊荣 赵琦 李保生 温小浩 牛东风 Steffen Mischke 张成君 | 2015 | 干旱区资源与环境2015，29，1： | 5 |
| 11 | A large Middle Pleistocene freshwater to oligohaline lake in the contemporary hyperarid Qaidam Basin (China)显示文摘 | Steffen Mischke Ulrike Herzschuh Naida Sun Zizhen Qiao Zhencheng Sun | 2006 | Episodes2006，29，1： | 4 |
| 12 | Identification of the varietal origin of processed loose-leaf tea based on analysis of a single leaf by SNP nanofluidic array显示文摘Tea is an important cash crop, representing a $40 billion-a-year global market. Differentiation of the tea market has resulted in increasing demand for tea products that are sustainably and responsibly produced. Tea authentication is important because of growing concerns about fraud involving premium tea products. Analytical technologies are needed for protection and value enhancement of high-quality brands. For loose-leaf teas, the challenge is that the authentication needs to be established on the basis of a single leaf, so that the products can be traced back to the original varieties. A new generation of molecular markers offers an ideal solution for authentication of processed agricultural products. Using a nanofluidic array to identify variant SNP sequences, we tested genetic identities using DNA extracted from single leaves of 14 processed commercial tea products. Based on the profiles of 60 SNP markers, the genetic identity of each tea sample was unambiguously identified by multilocus matching and ordination analysis. Results for repeated samples of multiple tea leaves from the same products(using three independent DNA extractions) showed 100% concordance, showing that the nanofluidic system is a reliable platform for generating tea DNA fingerprints with high accuracy. The method worked well on green, oolong, and black teas, and can handle a large number of samples in a short period of time. It is robust and cost-effective, thus showing high potential for practical application in the value chain of the tea industry. | Wanping Fang Lyndel W.Meinhardt Huawei Tan Lin Zhou Sue Mischke Xinghua Wang Dapeng Zhang | 2016 | The Crop Journal2016，4，4： | 4 |
| 13 | 河北泥河湾盆地油房北旧石器地点的发现与研究显示文摘油房北旧石器地点是河北省泥河湾盆地东缘的一处考古新发现,本文对该地点的下部文化层相关情况做了重点介绍。下部文化层的厚度约2.5 m,在3 m2的试掘范围内出土了石制品、动物化石及自然砾石等标本计600余件。石器工业面貌整体上承袭了我国华北地区的小石片石器文化传统。微体古生物化石(介形虫等)研究表明,该文化层自下而上经历了河流阶地到湿地环境的转变。光释光方法测得其年代大约在8.6~10.8万年,相当于深海氧同位素5阶段(MIS5),处于末次间冰期。油房北地点的考古发现增添了末次间冰期古人类活动的新证据,为研究当时古人类的生计方式及人地关系提供了重要实物资料。 | 赵海龙 谭培阳 孙雪峰 Mischke Steffen | 2021 | 第四纪研究2021，41，1： | 3 |
| 14 | 综述:从产业角度看可录光盘的测试和生产工艺 | Wlodek Mischke 袁平 | 2005 | 记录媒体技术2005，0，4： | 3 |
| 15 | Weak Summer Monsoon during the Early Holocene Inferred from the Dingxi Lujiagou Floodplain Lake-Eolian Sand Rhythm due to Solar Impacting显示文摘Objective Precipitation was the highest in the loess plateau during the Early Holocene 10-8 ka BP even to the period 10-3.0 ka BP in the Kesang cave stalagmite westward Tianshan,Xinjiang,based on large numbers of records from paleoclimatic proxies(An et al.,2000;Zhang et al.,2009;Zhang et al.,2018).However,we discovered at first time that floodplain lake-eolian stratigraphical rhythm complex kept in the Lujiagou of Dingxi,Gansu,which was important geological proof to indicate a weak summer monsoon transition period during the Early Holocene in the Chinese Loess Plateau. | ZHANG Wanyi ZHANG Huirong MA Yuan WANG Xiaoyu Steffen MISCHKE ZHANG Chengjun | 2019 | Acta Geologica Sinica(English Edition)2019，93，3： | 3 |
| 16 | Sub-Recent Sexual Populations of Limnocythere inopinata Recorded for the First Time from>3500 m Altitude on the Tibetan Plateau显示文摘The central and northwestern Tibetan Plateau region,also called'Qiangtang Plateau'(30°27'25'-35°39'13'N,83o41'14'-95°10'46'E),is the highest and largest arcticalpine area of the Earth covering approximately 600,000km^2 with altitude ranging from 4600 to 5100 m a.s.l.(Song et al.,2012,Fig.1).Ostracod species | ZHANG Wanyi Steffen MISCHKE ZHANG Chengjun ZHANG Huirong WANG Peng | 2015 | Acta Geologica Sinica(English Edition)2015，89，3： | 2 |
| 17 | 中德联合冬给措纳湖地区寒区环境变迁研究进展显示文摘青藏高原腹地的内陆湖及其湖相沉积物能够较真实地反映气候变化特征,在高原环境变迁研究中备受中外科学家的关注,2006年8月15日~9月10日,中德联合考察小组对青藏高原东北部的冬给措纳湖一带进行了第四纪冻土、地貌和地质学考察,并对湖岸阶地做了初步的数字高程分析,调查了冬给措纳湖底地形、地貌,采集了湖相沉积物样本,在湖的东岸和西岸发现多年冻土,湖泊西北山谷观察到古冰川活动遗迹,初步推测该湖是由断陷沉降形成,为进一步分析湖区气候和环境变迁,联合小组拟定2007年3月份钻取湖芯. | 杨思忠 金会军 Bernhard Diekmann Bernd Wünnemann Steffen Mischke 吉延峻 陈建辉 杨奇丽 | 2006 | 冰川冻土2006，28，6： | 2 |
| 18 | Paleoenvironmental implications of new OSL dates on the formation of the “Shell Bar” in the Qaidam Basin, northeastern Qinghai-Tibetan Plateau显示文摘 | ZhongPing Lai Steffen Mischke David Madsen | 2014 | Journal of Paleolimnology2014，，2： | 2 |
| 19 | Developing single nucleotide polymorphism markers for the identification of pineapple(Ananas comosus)germplasm显示文摘Pineapple(Ananas comosus[L.]Merr.)is the third most important tropical fruit in the world after banana and mango.As a crop with vegetative propagation,genetic redundancy is a major challenge for efficient genebank management and in breeding.Using expressed sequence tag and nucleotide sequences from public databases,we developed 213 single nucleotide polymorphism(SNP)markers and validated 96 SNPs by genotyping the United States Department of Agriculture-Agricultural Research Service pineapple germplasm collection,maintained in Hilo,Hawaii.The validation resulted in designation of a set of 57 polymorphic SNP markers that revealed a high rate of duplicates in this pineapple collection.Twenty-four groups of duplicates were detected,encompassing 130 of the total 170 A cosmos accessions.The results show that somatic mutation has been the main source of intra-cultivar variations in pineapple.Multivariate clustering and a model-based population stratification suggest that the modern pineapple cultivars are comprised of progenies that are derived from different wild Ananas botanical varieties.Parentage analysis further revealed that both A.comosus var.bracteatus and A.comosus var.ananassoides are likely progenitors of pineapple cultivars.However,the traditional classification of cultivated pineapple into horticultural groups(e.g.‘Cayenne’,‘Spanish’,‘Queen’)was not well supported by the present study.These SNP markers provide robust and universally comparable DNA fingerprints;thus,they can serve as an efficient genotyping tool to assist pineapple germplasm management,propagation of planting material,and pineapple cultivar protection.The high rate of genetic redundancy detected in this pineapple collection suggests the potential impact of applying this technology on other clonally propagated perennial crops. | Lin Zhou Tracie Matsumoto Hua-Wei Tan Lyndel W Meinhardt Sue Mischke Boyi Wang Dapeng Zhang | 2015 | Horticulture Research2015，2，1： | 2 |
| 20 | Reconstructing climate variability on the northeastern Tibetan Plateau since the last Lateglacial – a multi-proxy, dual-site approach comparing terrestrial and aquatic signals显示文摘 | Juliane Wischnewski Steffen Mischke Yongbo Wang Ulrike Herzschuh | 2010 | Quaternary Science Reviews2010，，1： | 2 |
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