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| 1 | Chinese deserts and sand fields in Last Glacial Maximum and Holocene Optimum显示文摘The Last Glacial Maximum (LGM, c. 26-16 ka) and the Holocene Optimum (HO, c. 9-5 ka) were characterized by cold-dry and warm-wet climates respectively in the recently geological Earth. How Chinese deserts and sand fields responded to these distinctive climatic changes is still not clear, however. To reconstruct environments of the deserts and sand fields during the LGM and HO is helpful to understand the forcing mechanisms of environment change in this arid region, and to test paleoclimatic modeling results. Through our long-term field and laboratory investigations, 400 optically stimulated luminescence (OSL) ages and more than 100 depositional records in the Chinese deserts and sand fields were obtained; on the basis of these data, we reconstruct spatial distributions of the deserts and sand fields during the LGM and HO. Our results show that the sand fields of Mu Us, Hunshandake, Horqin and Hulun Buir in northern and northeastern China had expanded 25%, 37%, 38% and 270%, respectively, during the LGM; the sand fields of Gonghe in the northeastern Qinghai-Tibetan Plateau had expanded 20%, and the deserts of Badain Jaran, Tengger in central northern China had expanded 39% and 29% separately during the LGM; the deserts of Taklimakan, Gurbantünggüt and Kumtag in northwestern China had expanded 10%-20% respectively, compared to their modern areas. On the other hand, all of the sand fields were nearly completely covered by vegetation during the HO; the deserts in northwestern and central northern China were reduced by around 5%-20% in area during this time. Lakes in this arid region were probably expanded during the HO but this conclusion needs more investigation. Compared with the geological distributions of deserts and sand fields, human activity has clearly changed (expanded) the area of active sand dunes at the present time. Our observations show that environmental conditions of Chinese deserts and sand fields are controlled by regional climate together with human activity. | LU HuaYu YI ShuangWen XU ZhiWei ZHOU YaLi ZENG Lin ZHU FangYing FENG Han DONG LiNa ZHUO HaiXin YU KaiFeng MASON Joseph WANG XiaoYong CHEN YingYong LU Qi WU Bo DONG ZhiBao QU JianJun WANG XunMing GUO ZhengTang | 2013 | Chinese Science Bulletin2013，58，23： | 40 |
| 2 | 末次盛冰期和全新世大暖期毛乌素沙地的空间变化显示文摘沙漠/沙地边缘和内部的古风成沙层、砂质古土壤是重建晚第四纪以来地表变化的直接地质证据。位于我国北方半干旱区的毛乌素沙地,其地表过程对气候变化响应敏感。在对毛乌素沙地进行野外拉网式调查以及前人研究的基础上,我们在沙地南部和东部的沙漠-黄土过渡带发现了大量的埋藏古风成沙丘沉积,指示了干冷期沙漠扩张的最南、东界限;沙地内部广泛发育的砂质古土壤则表明在气候相对暖湿期地表植被生长,土壤发育,沙丘基本被固定。对14个典型风成沙/黄土/古土壤沉积剖面进行了光释光年代学样品的采集和测试,结合空间分析和他人研究结果,发现在末次盛冰期(约26~16ka),毛乌素沙地的流动沙丘向南、东扩张,扩张距离现代边界约30~50km,面积扩大至少约10000km^2,占现代沙地面积的25%;在全新世大暖期(约9~5ka),毛乌索沙地大部分被固定,发育了较厚的砂质古土壤。研究结果揭示了毛乌素沙地的地表过程对末次盛冰期和全新世大暖期气候变化的直接响应。 | 徐志伟 鹿化煜 弋双文 周亚利 Joseph A Mason 王晓勇 陈英勇 朱芳莹 张瀚之 翟秀敏 | 2013 | 第四纪研究2013，33，2： | 30 |
| 3 | Optically stimulated luminescence dating of aeolian sand in the Otindag dune field and Holocene climate change显示文摘The dune system in Otindag sand field of northern China is sensitive to climate change, where effective moisture and related vegetation cover play a controlling role for dune activity and stability. Therefore, aeolian deposits may be an archive of past environmental changes, possibly at the millennial scale, but previous studies on this topic have rarely been reported. In this study, thirty-five optically stimulated luminescence (OSL) ages of ten representative sand-paleosol profiles in Otindag sand field are ob-tained, and these ages provide a relatively complete and well-dated chronology for wet and dry varia-tions in Holocene. The results indicate that widespread dune mobilization occurred from 9.9 to 8.2 ka, suggesting a dry early Holocene climate. The dunes were mainly stabilized between 8.0 and 2.7 ka, implying a relatively wet climate, although there were short-term penetrations of dune activity during this wet period. After ~2.3 ka, the region became dry again, as inferred from widespread dune activity. The '8.2 ka' cold event and the Little Ice Age climatic deterioration are detected on the basis of the dune records and OSL ages. During the Medieval Warm Period and the Sui-Tang Warm Period (570-770 AD), climate in Otindag sand field was relatively humid and the vegetation was denser, and the sand dunes were stabilized again. These aeolian records may indicate climate changes at millennial time scale during Holocene, and these climatic changes may be the teleconnection to the climate changes elsewhere in the world. | Joseph MASON James SWINEHART Ronald GOBLE | 2008 | Science China Earth Sciences2008，51，6： | 18 |
| 4 | 青海湖地区冰消期以来气候变化的黄土记录显示文摘青海湖周围堆积着很多黄土和风沙沉积,这些风成沉积序列是过去气候变化的良好记录。相对于湖泊沉积,这些沉积物受到的研究较为薄弱。对青海湖南岸的黄土堆积进行了光释光年代学、磁化率、Fe/Mg值、粒度和有机质含量等气候替代性指标测量。在具有绝对年代标尺控制的基础上,结合气候替代性指标变化特征的分析,表明冰消期以来青海湖地区的古气候经历了多次的冷暖和干湿变化过程:14~9ka间气候前期相对冷干,后期转为凉干,其中可能在11ka左右存在一次暖湿事件;9~2.5ka间气候呈暖湿状态;2.5ka以后的地层扰动较大。黄土和湖泊沉积记录的环境变化过程具有可比性。 | 赵存法 鹿化煜 周亚利 弋双文 Joseph Mason | 2009 | 高校地质学报2009，15，1： | 14 |
| 5 | 便携式粉尘观测仪测定腾格里沙漠和毛乌素沙地PM_(10)释放通量显示文摘中国北方沙漠和沙地是亚洲粉尘释放的重要源区,定量估算这一地区的粉尘释放量有助于评估区域大气环境质量及其气候效应.目前,对中国北方粉尘释放量的估算主要是基于模拟结果,野外直接观测数据很少.利用一种新型的粉尘释放观测仪器——便携式粉尘观测仪(PI-SWERL),测量腾格里沙漠和毛乌素沙地若干典型地表(沙丘、干湖、灌丛沙丘、河流冲积物等)的粉尘释放通量,获得了不同地表潜在粉尘释放量的直接观测数据.结果表明,不同地表的PM10释放通量存在较大差异,但均随摩阻风速的增加而增加.在相同的摩阻风速U*=0.55 m/s条件下,灌丛沙丘的PM10通量最高(0.70~10.23 mg/(m2 s)),河流冲积物次之(0.12~4.97 mg/(m2 s)),干湖湖底、沙丘等地表的通量较小(〈0.5 mg/(m2 s)).对比试验表明,破碎结壳地表释放的PM10通量是未破碎结壳的几倍甚至几十倍;披覆松散沙粒结壳地面的PM10释放通量高出未披覆的1~2个数量级.对比前人研究结果,PI-SWERL可以较好地反映不同源区粉尘释放的差异,对定量评估区域乃至全球的粉尘释放量等具有重要意义. | 崔梦淳 鹿化煜 SWEENEY Mark MASON Joseph 冯晗 徐志伟 | 2015 | 科学通报2015，60，17： | 12 |
| 6 | Crescentic dune migration and stabilization: Implications for interpreting paleo-dune deposits as paleoenvironmental records显示文摘Paleo-dune deposits have been widely used as a proxy indicator of past dune activity, which is further used to reconstruct paleoclimates. However, recent studies have critically examined the reproducibility of dune chronologies and the complexity of paleo-dune deposits as paleoenvironmental records. This paper addresses questions on the paleoenvironmental implications of dune chronostratigraphies that have been raised by those reviews, in the specific case of crescentic dunes, using a case study from the Mu Us dune field, north-central China. The processes of turn-over and stabilization of relatively small crescentic dunes are first investigated by observational evidence. In combination with the analysis of a simplified sand preservation model and stratigraphic records, the effect of dune morphodynamics on sand preservation is demonstrated. It is especially evident that thick, nearly instantaneously deposited sand units record dune stabilization near the very end of a dune activity episode, while thin sand units may signal the preservation of sand deposited earlier in episodes of activity. Interpreting the distribution of luminescence ages that indicate sand deposition over time is not as simple as assumed in some previous work. Low frequency of sand ages could indicate an interval of either dune field stabilization or extensive dune activity but poor sand preservation. A peak of sand age frequency likely represents a shift in dune field activity towards stabilization, not a peak of active dune extent, especially if it partially overlaps with an independently identified interval of stabilization(e.g. one recorded by paleosols). The nature and magnitude of these biases in the distribution of sand ages over time are strongly affected by the magnitude of net sand accumulation, which is in turn related to sand supply, transport capacity and sand availability, and ultimately climate change. Relatively short dune stabilization and turn-over time(10~1 to 10~2 yrs) indicate that dune geomorphic processes can quickly respond to short-term disturbance, but the chronology of that response must be interpreted in light of how those processes influence age distributions. | XU Zhiwei Joseph A. MASON LU Huayu YI Shuangwen ZHOU Yali WU Jiang HAN Zhiyong | 2017 | Journal of Geographical Sciences2017，27，11： | 7 |
| 7 | A preliminary quantitative reconstruction of precipitation in southern Mu Us sandy land at margin of Asian monsoon-dominated region during late Quaternary显示文摘我们在场季风降水的第一个量的评价在在北中国的沙的陆地的迟了的 glacial-Holocene 期间,基于器官的碳从在亩的边缘的一个黄土沙序列的同位素的作文数据我们沙的土地。我们使用在季风降水和碳之间的关系是的现代土壤的同位素的作文类似物与次要的修正,重建降水回到 c。47 ka 以前。初步的结果显示年度季风降水在 8 ka 以后高,与 435 公里的一般水准;并且它与 194 公里的吝啬的价值在 18 和 8 ka 期间减少了。47-18 ka 的降水价值在二之间变化了。我们把重建的降水与另外的记录和 paleoclimatic 建模结果作比较,证明我们的记录同意从另外的来源,的季风降水的重建甚至捕获象更年轻的 Dryas 那样的短气候的事件。我们建议那太阳的发光,高纬度的温度 / 冰体积和本地蒸发一起在沙的陆地的修改潮湿。 | CHEN Yingyong LU Huayu YI Shuangwen ZHANG Enlou XU Zhiwei YU Kaifeng Joseph A. MASON | 2015 | Journal of Geographical Sciences2015，25，3： | 6 |
| 8 | Sand dunes as potential sources of dust in northern China显示文摘While saltation bombardment of sand grains on a fine substrate can produce considerable dust, the well-sorted nature of sand dunes tends to preclude them from consideration as major dust sources. Recent research, however, has revealed that sand dunes can, in some cases, be large sources of dust. We used the PI-SWERL(Portable In-Situ Wind Erosion Laboratory) to measure in the field the potential of sand dunes and other desert landforms to emit particulate matter <10 μm(PM-10) dust in the Tengger, Ulan Buh, and Mu Us deserts of northern China. Combined with high resolution particle size measurements of the dune sand, an assessment of sand dunes as a dust source can be made. Large active transverse dunes tend to contain little to no stored PM-10, yet they produce a low dust flux. Coppice dunes stabilized by vegetation contain appreciable PM-10 and have very high dust emission potential. There is a positive correlation between the amount of PM-10 stored in a dune and its potential dust flux. Saltation liberates loose fines stored in dunes, making them very efficient dust emitters compared to landforms such as dry lake beds and washes where dust particles are unavailable for aeolian transport due to protective crusts or sediment cohesion. In cases where large dunes do not store PM-10 yet emit dust when active, two hypotheses can be considered:(1) iron-oxide grain coatings are removed during saltation, creating dust, and(2) sand grains collide during saltation, abrading grains to create dust. Observations reveal that iron oxide coatings are present on some dune sands. PI-SWERL data suggests that low dust fluxes from dunes containing no stored dust may represent an estimate for the amount of PM-10 dust produced by removal of iron oxide coatings. These results are similar to results from dunes in the United States. In addition, PI-SWERL results suggest that dust-bearing coppice dunes, which cover vast areas of China's sandy deserts, may become major sources of dust in the future if overgrazing, depletion of groundwater, or drought destabilizes the vegetation that now partially covers these dunes. | Mark R SWEENEY LU HuaYu CUI MengChun Joseph A MASON FENG Han XU ZhiWei | 2016 | Science China Earth Sciences2016，59，4： | 2 |
| 9 | The Intracellular Cargo Receptor ERGIC-53 Is Required for the Production of Infectious Arenavirus, Coronavirus, and Filovirus Particles显示文摘 | Joseph P. Klaus Philip Eisenhauer Joanne Russo Anne B. Mason Danh Do Benjamin King Douglas Taatjes Cromwell Cornillez-Ty Jonathan E. Boyson Markus Thali Chunlei Zheng Lujian Liao John R. Yates Bin Zhang Bryan A. Ballif Jason W. Botten | 2013 | Cell Host & Microbe2013，，5： | 1 |
| 10 | Luteal Phase progesterone excretion in ovulatary women with polycystic ovaries显示文摘 | Joseph Home R Mason H Batty S | 2002 | Hum Reprod2002，17，1： | 1 |
| 11 | Growth Kinetics of Renal Masses: Analysis of a Prospective Cohort of Patients Undergoing Active Surveillance显示文摘 | Ross J. Mason Mohamed Abdolell Greg Trottier Christopher Pringle Joseph G. Lawen David G. Bell Michael A.S. Jewett Laurence Klotz Ricardo A. Rendon | 2011 | European Urology2011，，： | 1 |
| 12 | The origins of banking panics : Models, facts, and bank regulation 显示文摘 | Charles Calomiris Joseph Mason | 1991 | University of Chicago Press for the NBER1991，，： | 1 |
| 13 | Contagion and bank failures during the great depression: The June 1932 Chicago banking panic 显示文摘 | Charles Calomiris Joseph Mason | 1997 | American Economic Review1997，，87： | 1 |
| 14 | Holocene climatic changes revealed by aeolian deposits from the Qinghai Lake area (northeastern Qinghai - Tibetan Plateau) and possible forcing mechanisms 显示文摘 | Huayu Lu Cunfa Zhao Joseph Mason | 2010 | The Holocene2010，21，2： | 1 |
| 15 | Limited change in dune mobility in response to a large decrease in wind power in semi-arid northern China since the 1970s显示文摘 | Joseph A. Mason James B. Swinehart Huayu Lu Xiaodong Miao Phueng Cha Yali Zhou | 2008 | Geomorphology2008，，3： | 1 |
| 16 | Herding behavior in Chinese stock markets: An examination of A and B shares显示文摘 | Lin Tan Thomas C. Chiang Joseph R. Mason Edward Nelling | 2007 | Pacific-Basin Finance Journal2007，，： | 1 |
| 17 | Funda- mentals, Panics and Bank Distress during the Depres- sion显示文摘 | Calomiris Charles W Joseph R Mason | 2003 | American Economic Review2003，93，： | 1 |
| 18 | Blood and treasure: ex- iting the Great Depression and lessons for today显示文摘 | Kris James Mitehener Joseph Mason | 2010 | Oxford Review of Economic Policy2010，26，3： | 1 |
| 19 | Summer Scientific Research for Teachers: The Experience and its Effect显示文摘 | Julie F. Westerlund Dana M. García Joseph R. Koke Teresa A. Taylor Diana S. Mason | 2002 | Journal of Science Teacher Education2002，，1： | 1 |
| 20 | Herding Behavior in Chinese Stock Markets: An Examination of A and B Shares 显示文摘 | TAN LIN CHIANG THOMAS C JOSEPH R MASON EDWARD MELLING | 2006 | Pacific -Basin Finance Journal2006，16，： | 1 |
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