This data set is the hydrogen isotope data of leaf wax from 10 m core of Qinghai Lake in Tengchong, Southeast of Qinghai Tibet Plateau. Tengchong Qinghai Lake is a small crater lake in Gaoligong Mountain, Southwest China. Core samples were collected at about 4m in the center of the lake in 2017. Ams-14c dating was used to establish the age series. The n-alkane leaf wax hydrogen isotope was determined and analyzed by Agilent 6890 GC gas chromatograph and Deltaplus XL type chromatography isotope mass spectrometry. The data reflect the information of atmospheric precipitation isotope in this area, and play an important role in the study of monsoon precipitation changes in southwest monsoon region in the past 40000 years. Data acquisition, pre-processing extraction and instrument testing were completed in strict accordance with the relevant operating procedures.
Lake sediment is important archive for reconstructing the past climate change, in which the chronological framework of sediments is the basis. Varve is a kind of sedimentary lamina formed in pairs in lake sediments, usually with one year as a cycle. Supported by the projects the Strategic Priority Research Program of Chinese Academy of Sciences “Pan-Third Pole Environment Study for a Green Silk Road (Pan-TPE)” and The Second Tibetan Plateau Scientific Expedition and Research, the authors obtained a 1-meter long sediment gravity core from Jiangco in the central Tibet Plateau, and found well preserved varves. Subsequently, core thin sections were made, and the varve and its thickness were counted and measured to obtain the chronological sequence from 81 A.D. to 2015. The precipitation in this area in the past 2000 years has been reconstructed by using the percentage of coarse-grained layer thickness in the total varve thickness, which represents the precipitation. High resolution and high-precision chronology and precipitation records can provide reliable background of climate and environmental change, and provide reference for paleoclimate simulation and the rise and fall of ancient civilization.
Pollen and spores extracted from sediment are considered as the important proxy in reconstructing past vegetation and climate, and which plays essential role in investigating environmental evolution during the Quaternary. Accurate identification of pollen and spore is the base for palynological research, which determines it is quite necessary to establish modern atlas for pollen and spore. Supported by the projects the Strategic Priority Research Program of Chinese Academy of Sciences “Pan-Third Pole Environment Study for a Green Silk Road (Pan-TPE)” and The Second Tibetan Plateau Scientific Expedition and Research, authors completed the vegetation and soil surveys in 2018 for the alpine meadow in the east Tibetan Plateau (including Yushu Prefecture, Changdu City, Ganzi prefecture, Naqu City) and alpine forest in the southeast Tibetan Plateau (Linzhi City) , and collected 401 specimens for anther of flowering plants and sporangium of ferns. Pollen and spores were extracted and from these specimens using the standard acid-alkali approach and acetolysis (9:1 mixture of acetic anhydride and sulphuric acid) treatment, and further were refrigerated in glycerin. More than two photographs were took for each pollen and spore type, using the LEICA-dm-2500 optical microscope and its imaging system with scale. The atlas of pollen and spore morphology will be a valuable reference for palynology research and teaching.
CAO Xianyong TIAN Fang LI Kai NI Jian
Data content: Standard ring-width chronology derived from Wilson juniper shrub around the northern shore of the Nam Co Lake; May-June SZI (Standardized Moisture Anomaly Index) drought reconstruction for the Nam Co region. Time span: 1605 to 2010. Temporal resolution: Yearly. Application and prospects: Hydroclimate study on the south-central Tibetan Plateau.
LU Xiaoming HUANG Ru WANG Yafeng ZHANG Baoqing ZHU Haifeng CAMARERO J. Julio LIANG Eryuan*
Data set contains tree age of trees growing at different glacier moraines in the central Himalayas. The data were obtained using tree ring samples. Cores samples were collected (almost near to the ground level to estimate the minimum age of the related moraine) using an increment borer. Samples were processed by using standard dendrochronological techniques.
SIGDEL Shalik Ram ZHNAG Hui ZHU Haifeng MUHAMMAD Sher MUHAMMAD Sher MUHAMMAD Sher MUHAMMAD Sher MUHAMMAD Sher LIANG Eryuan*
By archaeological investigation and excavation in Tibetan Plateau and Hexi corridor, we discovered more than 40 Neolithic and Bronze Age sites, including Zongri, Sanjiaocheng, Huoshiliang, Ganggangwa, Yigediwonan, Shaguoliang, Guandi, Maolinshan, Dongjicuona, Nuomuhong, Qugong, Liding and so on. In this dataset, there are some basic informations about these sites, such as location, longitude, latitude, altitude, material culture and so on. On this Basis, we identified animal remains, plant fossil, selected some samples for radiocarbon dating, optically stimulated luminescence dating, stable carbon, nitrogen isotopes, polle, fungal sporen and environmental proxies. This dataset provide important basic data for understanding when and how prehistoric human lived in the Tibetan Plateau during the Neolithic and Bronze Age.
DONG Guanghui YANG Xiaoyan Lü Hongliang LIU Xiangjun HOU Guangliang
Black carbon is an important light absorbing substance, which has an important impact on climate change. This data set contains the data of black carbon concentration and sedimentation flux in the core of six lakes (gun Yong lake, Tanggula lake, linggecuo, Ranwu lake, gokyo, gosainkunda) on the Qinghai Tibet Plateau and the south slope of the Himalayas. The carbon concentration of Huxin black was determined by digestion filtration thermoluminescence method. This dataset is an excel file, which can be opened directly by using Excel. This data set is helpful to study the history of atmospheric black carbon deposition in the Qinghai Tibet Plateau and its surrounding areas and to further analyze the sources of atmospheric black carbon. It can be used as the basic data for the study of atmospheric black carbon transport and climate effect assessment.
Guided by the theories of plate tectonics, paleogeography, petroliferous basin analysis and sedimentary basin dynamics, we have collected a large number of data and achievements of geological research and oil-gas geological research in Pan third pole in recent years, including basic materials such as stratum, sedimentation, paleontology, paleogeography, paleoenvironment, paleoclimate, structure, oil-gas (potash) geology, especially paleomagnetism and paleogenesis On the basis of zircon and geochemical data, combined with the results of typical measured stratigraphic sections, the lithofacies and climate palaeogeographic pattern of Jurassic period are restored and reconstructed, and the paleogeographic map of lithofacies and climate of Pan third extremely early, middle and late Jurassic (3 sheets) and pan third extremely early, middle and late Jurassic (3 sheets) are obtained, aiming to discuss paleogeography and paleostructure The control and influence of paleoclimate on oil and gas (including potash) resources, in order to reveal the geological conditions and resource distribution rules of oil and gas formation, and provide scientific basis and technical support for overseas and domestic oil and gas exploration and deployment in China.
Cenozoic sedimentary strata, which have been extensively developed in the low Himalaya region of western Nepal, provide an opportunity to study the dynamics of plateau uplift and the effects of climate and environment. According to a detailed field explored in the region nearly 10 sections, we found that a typical Cenozoic strata in the area is mainly composed of passive continental margin sedimentary of India's Tansen group and the Himalayas of foreland basin of Siwalik group, thickness of the Tansen group of 2000-3000 m, bottom-up Cenozoic strata, including the Amile group (Amile), and Bhainskati group (Bhainskati), Dumri group (Dumri); The Siwalik group, up to 4000m-6000m, is mainly composed of the lower, middle and upper west Siwalik. Cenozoic strata in Butwal section (309 m, including Amile and upper Bhainskati formation), Tulsipur section (357 m, including the top of Amile group and Bhainskati group formation) and Kalyan section (1161 m, including upper Bhainskati group formation and Dumri formation) are well exposed. High precise (with 1 m spacing) paleomagnetic chronology and environmental proxies samples collected in those three sections. By giving the precise stratigraphic age and paleoenvironmental data, it is of great significance to explore whether the north-south monsoon and drought events on the plateau are coupled and synchronized, and to reveal their relationship with the tectonic uplift of the Tibetan Plateau and global change.
1) Data content: this data is the DNA data of the paleoenvironmental sediments generated from the study of four archaeological sites in the downstream of Yarlung Zangbo River in the Qinghai Tibet Plateau, including Changguogou, Liding, Liena and, Qugong. It includes the sequence of Hiseqx metagenomic data of 10 samples of the paleoenvironmental sediments in four archaeological sites. It can be used to study the research methods and feasibility of the ancient environment DNA in the archaeological sites of the Tibet Plateau and its possible important role in the research of the ancient agricultural development processes. 2) Data source and processing method: it is the own data of our research group, and the data is detected by using the pair-end library building method and Illumina Hiseqx sequencing method. 3) Data quality: 279M data volume, Q30 > 85%. 4) Achievements and prospects of data application: data are used to reveal the ancient agriculture in the Tibet Plateau at the level of ancient environmental DNA.
This magnetic susceptibility data set of the XS loess section at Ganzi in the eastern Tibet Plateau. We analyzed the magnetic susceptibility of the top part of the loess sequence at 5cm intervals, and obtained 200 sets of magnetic susceptibility data. The experimental analysis was completed in the Key Laboratory of Western China's Environmental Systems（Ministry of Education), Lanzhou University. Air-dried and grind the samples were put it into a non-magnetic cubic box, and measured by the British Bartington MS2. The result indicates the varations of the low frequency magnetic susceptibility of the Loess sequence since the Last Interglacial at Ganzi area, which is of great importance for understanding past environment changes in the eastern Tibet Plateau.
This data is the grain size data set of the XS loess section at Ganzi in the east of Qinghai Tibet Plateau. The whole section is 10 meters thick, and the grain size analysis is carried out according to the interval of 2.5cm. A total of 398 groups of grain size data are obtained. The grain size analysis was carried out at the Key Laboratory of Western China's Environmental Systems（Ministry of Education), Lanzhou University. Before the measurement, the organic matter and carbonate in the sample were removed by H2O2 and hydrochloric acid, then adding the sodium hexago-hydrophosphate and vibrating for about 10 min to disperse samples by using ultrasonic apparatus. All measurements are conducted by using the Mastersizer 2000. This data reflects variations of the loess grain size since the last interglacial, which is of great importance for understanding past evionroment changes in the eastern Tibet Plateau.
The climate model used is a fast air sea coupled model (famous) developed jointly by the British meteorological agency and the University of England. In the famous model, the horizontal resolution of the atmospheric model is 5 °× 7.5 ° and there are 11 layers in the vertical direction; the horizontal resolution of the ocean model is 2.5 °× 3.75 ° and there are 20 layers in the vertical direction. The atmosphere and the ocean are coupled once a day without flux adjustment
The data set integrated glacier inventory data and 426 Landsat TM/ETM+/OLI images, and adopted manual visual interpretation to extract glacial lake boundaries within a 10-km buffer from glacier terminals using ArcGIS and ENVI software, normalized difference water index maps, and Google Earth images. It was established that 26,089 and 28,953 glacial lakes in HMA, with sizes of 0.0054–5.83 km2, covered a combined area of 1692.74 ± 231.44 and 1955.94 ± 259.68 km2 in 1990 and 2018, respectively.The current glacial lake inventory provided fundamental data for water resource evaluation, assessment of glacial lake outburst floods, and glacier hydrology research in the mountain cryosphere region
This dataset includes few pollen data and high-resolution microcharcoal dataset in a ~4000 m-thick sedimentary outcrops retrieved from the Huatutou, Qaidam Basin. Pollen data from the sediment are rare, only 15 samples got enough pollen grains for pollen assemblages division and analysis, the results indicates that during the early period, the vegetation are favor a relatively warm and wet climate correlated with the global warming stages (only ice-sheet accumulated in the Antarctic), then along with the global cooling, the xerophytic taxa increased and the vegetation types became similar than before. Sedimentary microcharcoals from fine grains (e.g., mudstone, siltstone and sandstone) are one of the typical wildfire proxies commonly used in paleoclimatic studies, as they have the potential to record past variations in wildfire history related with the vegetation and precipitation. The sediment samples were grounded and treated with 10% HCl and 40% HF to remove carbonates and silica. Separation of the microcharcoals from the residue was accomplished using a 10-lm nylon sieve. Finally, they were mounted in glycerin jelly. Based on the data of outcrops in the Qaidam Basin, the evolution history of wildfire and arid environment together vegetation in the west Qaidam Basin since the early Oligocene can be reconstructed, allowing further exploring of trends, variability and mechanisms of vegetation and wildfire history.
This data set comes from shallow marine carbonate sections at Tingri and Gamba, south Tibet. The age of these samples is about 56 Ma (at the Paleocene-Eocene boundary). At Tingri, we studied two parallel sections (13ZS section and 10-11TM section), and at Gamba, we studied one section (11TMG). From the 13ZS section, we analyzed carbon and oxygen isotopic compositions and calcium carbonate content of the whole carbonate rock, as well as the in-situ carbon isotopic compositions and element contents of the foraminifera shell. From the 10-11TM section, we analyzed carbon, oxygen and strontium isotopic compositions of the whole rock. From the 11TMG section, we analyzed carbon and oxygen isotopic compositions of the whole carbonate rock. Carbon and oxygen isotopic compositions of the whole rock were measured by gas isotope mass spectrometer (MAT251), strontium isotope by thermal ionization mass spectrometry (TIMS), calcium carbonate content by acid dissolution, in-situ carbon isotopic compositions by SIMS, and in-situ element contents by LA-ICPMS. Among these data, in-situ carbon isotope data were obtained from the laboratory of Professor John Valley at the University of Wisconsin-Madison in the United States, and the rest are from the relevant laboratories of the Department of Geosciences at the University of Bremen in Germany. Based on these data, we published three peer-reviewed papers on Journals of Gondwana Research, GSA Bulletin, and Global and Planetary Change.
The data of triode ice core mainly comes from NOAA (National Oceanic and Atmospheric Administration, https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/ice-core). The original data is mainly in text format, which is provided by relevant units and researchers voluntarily. The data mainly includes the original observation data such as oxygen isotope, greenhouse gas concentration, ice core age, etc., as well as the historical temperature, carbon dioxide concentration and methane concentration produced by the researchers according to the observation data. The data are mainly divided into Antarctic, Arctic, Greenland and the third polar region. The database includes drilling address, time, derivative products, corresponding observation site data, references and other elements. Derivative products include product name, type, time and other elements. The space location is divided into the south pole, the north pole and the third pole, including Alaska, Canada, Russia, Greenland and other regions. After sorting and post-processing the collected data, the ice core database is established by using the access database management system of Microsoft office. According to the Antarctic, Arctic, Greenland and the third pole, it is divided into four sub databases. The first table in each database is readme, which contains information and references of each data table.
This project is based on the data of bioactive elements such as Fe in miaergou ice core (94 ° 19 ′ e, 43 ° 03 ′ n, 4518 m) of the East Tianshan Mountains, and rebuilt the metal element history of 1956-2004. Data content: 1956-2004 ice core metal elements (including Fe, CD, Pb, as, Ba, Al, s, Mn, CO and Ni); data source, through ICP-MS test; data quality: blank sample is significantly lower than sample value, with better quality; data application results and prospects: data has been published, see Du, Z., Xiao, C., Zhang, W., Handley, M. J., mayewski, P. A., Liu, Y., & Li, X. (20. 19). Iron record associated with sandstorms in a central Asian shallow ice core spanning 1956-2004. Atmospheric environment, 203, 121-130. It can provide comparative study of other ice cores in Central Asia.
This data was reconstructed based on the history of perchlorate from 1956 to 2004 in Miaoergou ice core (94°19 'E,43°03 'N, 4518 m) in east Tianshan mountain. Data content: perchlorate from 1956 to 2004 (including: Cl-, NO3- and SO42-). Data was measured by ESI-MS/MS; Data quality: the blank sample was significantly lower than the sample values, and the quality was good. Data application result and prospect: The data has been published, the detailed information can be found in the published paper. Zhiheng Du, Cunde Xiao, Vasile I. Furdui C,Wangbin Zhang. (2019). The perchlorate record during 1956–2004 from Tienshan ice core, East Asia. Science of the Total Environment. Time range and resolution: 1956-2004 AD, and annual resolution.
Luanhaizi Borehole (LHZ18) was acquired by Huang Xiaozhong Research Group of Lanzhou University in August 2018. This data is 0-859 cm grain size data of the core of Luanhaizi Lake in Qilian Mountains. Grain size analysis was carried out at 0-4 m according to one sample, and grain size analysis was carried out at on ssample interval at the depth of 4-8.6 m, totaling 390 data were obtained. The experiment was completed in the Key Laboratory of the Ministry of Environmental Education of Lanzhou University, and grain size analysis was carried out with Mastersizer 2000 instrument. The data reflected the grain size change of the lake sediment, which is very important for the study of long-time series eolian activities in the Qinghai-Tibet Plateau.
HUANG Xiaozhong ZHANG Jun WANG Jiale REN Xiuxiu SUN Mingjie XIANG Lixiong