cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.13502234.v1
title: Comparison of proteomic profiles from the testicular tissue of males with impaired and normal spermatogenesis

description: In this study, we aimed to explore the potential differences in proteomic profiles from the testicular tissue of azoospermatic men with impaired spermatogenesis and normal spermatogenesis. Isobaric tags for relative and absolute quantitation (iTRAQ) labeled technology and LC-MS/MS technology were used to identify differentially expressed proteins. Potential functions of differentially expressed proteins were predicted using gene ontology (GO) and the Kyoto encyclopedia of genes and genomes (KEGG). Immunohistochemistry (IHC) and western blot (WB) were used to verify the differentially expressed proteins. A protein–protein interaction (PPI) network was built to outline the regulatory network of differentially expressed proteins. A total of 3,945 proteins were identified in men with normal and impaired spermatogenesis. Of these, 116 proteins were differentially expressed in men with impaired spermatogenesis: 39 were upregulated and 77 were downregulated. Furthermore, we found that these differentially expressed proteins were mainly involved in the cellular component, which may be mainly associated with the spliceosome, ribosome, and thyroid hormone synthesis signaling pathways. The spliceosome- and ribosome-associated proteins YBX1, FBL, and HNRNPU were downregulated. And the proteomic profile of testicular tissue in men with impaired spermatogenesis is different from that of men with normal spermatogenesis. For this reason, differentially expressed proteins such as YBX1, FBL and HNRNPU might be involved in the pathology of spermatogenesis dysfunction. <b>Abbreviations:</b> iTRAQ: Isobaric tags for relative and absolute quantitation;GO: Gene ontology; KEGG: Kyoto encyclopedia of genes and genomes; IHC: Immunohistochemistry; WB: Western blot; PPI: Protein–protein interaction; ICSI: Intracytoplasmic sperm injection; BP: Biological process; CC: Cellular components; MF: Molecular function; snoRNA: Small nucleolar RNA; snRNA: Small nuclear RNA; LC-MS/MS: Liquid chromatography and MS/MS analysis; BSA: Bovine serum albumin; SD: Spermatogenic dysfunction; micro-TESE: Testicular microscopic sperm extraction
DOI: 10.6084/m9.figshare.13502234
title: Comparison of proteomic profiles from the testicular tissue of males with impaired and normal spermatogenesis

description: In this study, we aimed to explore the potential differences in proteomic profiles from the testicular tissue of azoospermatic men with impaired spermatogenesis and normal spermatogenesis. Isobaric tags for relative and absolute quantitation (iTRAQ) labeled technology and LC-MS/MS technology were used to identify differentially expressed proteins. Potential functions of differentially expressed proteins were predicted using gene ontology (GO) and the Kyoto encyclopedia of genes and genomes (KEGG). Immunohistochemistry (IHC) and western blot (WB) were used to verify the differentially expressed proteins. A protein–protein interaction (PPI) network was built to outline the regulatory network of differentially expressed proteins. A total of 3,945 proteins were identified in men with normal and impaired spermatogenesis. Of these, 116 proteins were differentially expressed in men with impaired spermatogenesis: 39 were upregulated and 77 were downregulated. Furthermore, we found that these differentially expressed proteins were mainly involved in the cellular component, which may be mainly associated with the spliceosome, ribosome, and thyroid hormone synthesis signaling pathways. The spliceosome- and ribosome-associated proteins YBX1, FBL, and HNRNPU were downregulated. And the proteomic profile of testicular tissue in men with impaired spermatogenesis is different from that of men with normal spermatogenesis. For this reason, differentially expressed proteins such as YBX1, FBL and HNRNPU might be involved in the pathology of spermatogenesis dysfunction. <b>Abbreviations:</b> iTRAQ: Isobaric tags for relative and absolute quantitation;GO: Gene ontology; KEGG: Kyoto encyclopedia of genes and genomes; IHC: Immunohistochemistry; WB: Western blot; PPI: Protein–protein interaction; ICSI: Intracytoplasmic sperm injection; BP: Biological process; CC: Cellular components; MF: Molecular function; snoRNA: Small nucleolar RNA; snRNA: Small nuclear RNA; LC-MS/MS: Liquid chromatography and MS/MS analysis; BSA: Bovine serum albumin; SD: Spermatogenic dysfunction; micro-TESE: Testicular microscopic sperm extraction
DOI: 10.35080/data.c.2020.p36
title: 1∶50 000 Mineral Geological Map Database of the Zhaochuan Map-sheet in Zhangjiakou area, Hebei Province

description: The Zhaochuan Map-sheet (K50E020006) area is located in the eastern part ofZhangjiakou–Xuanhua region of Hebei province and the middle section of the northern marginof the North China craton. It is one of the important gold fields in China. The 1∶50 000mineral geological map database of the Zhaochuan Map-sheet was compiled in accordancewith the Technical Requirements of Solid Mineral Geological Survey (1∶50 000) (DD2019−02) and other applicable industrial standards. The survey work involves specificgeological mapping covering an area of 379.93 km2, measured geological routes totalingapproximately 315 km in length, ore spot checks and anomaly checks at about 15 points, threegroups of U–Pb ages (390–370 Ma, 234 Ma and 140–120 Ma), and six groups of whole-rockanalytical data. Through comprehensively analysing field measurement data of geologicalpoints, geological routes and geological boundaries, and previous regional geological surveyrecords, the boundaries of geological units were redelineated, and the corresponding featurelayers were established. Meanwile, the Meso–Neoarchean, Mesoproterozoic and Mesozoicstrata in the Zhaochuan Map-sheet were redivided, the Archean to Mesozoic magmatic rockswere generalized, the spatio-temporal evolution sequence of the magmatic rocks andmetallogenesis was determined, and a “three-in-one” ore prospecting prediction geologicalmodel and an integrated geological, geochemical, geophysical and remote-sensing oreprospecting prediction model were then established. The database has a high reference valuefor the deployment of mineral exploration activities in the area, and could also provide servicefor the local natural resource departments in the field of the land space planning and ecologicalcivilization.
DOI: 10.35080/data.c.2020.p32
title: Database of 1∶50 000 Mineral Geological Map of the Suolong Map-sheet in Zhaishang–Mawu Gold Deposit, Minxian County, Gansu Province

description: The 1∶50 000 mineral geological map of the Suolong Map-sheet (I48E010011) inZhaishang–Mawu Gold Deposit in Minxian County, Gansu Province was developed inaccordance with the Technical Requirements of Solid Mineral Geological Survey (1∶50 000)and other unified standards and requirements in the geological industry, during which theresults obtained from previous 1∶50 000-scale regional geological surveys and 1∶50 000-scale regional mineral surveys were fully utilized. Meanwhile, the digital mapping system wasadopted for field geology-specific mapping, and indoor map compilation was conducted alongwith field mapping. In this map, the sedimentary suite types of the pre-Devonian Wujiashanand Dacaotan Formations, Carboniferous Badu Formation, and Permian Shilidun Formationare reclassified, the formation epochs of the intrusions are classified into Late Triassic andEarly Permian, and the evolutionary sequence of magmatic rocks is established. The goldmetallogenesis in this Map-sheet is closely related to Permian strata, and most deposits (oreoccurrences) occurred in clastic rocks of the Shilidun Formation with relatively developedfissures. The database of the 1∶50 000 mineral geological map (also referred to as theDatabase) includes the data of seven stratigraphic units and two stages of magmatic rocks, andcovers 212 polished thin sections, 192 chemical samples, 486 bedrock spectra, 2 793 soilsamples, two samples for Ar/Ar dating, eight samples for fluid inclusion thermometry, and 15samples for petrochemical analysis. Meanwhile, three gold ore bodies and one goldmineralized point were newly discovered in the study area, with estimated (334) gold of 5.32tonnes. Having a data size of about 17.4 MB, the Database fully reflects the demonstrationresults of 1∶50 000 mineral geological surveys, and could provide references for mineralresource research and energy exploration in this Map-sheet area.
DOI: 10.35080/data.c.2020.p31
title: 1∶50 000 Mineral Geological Map Database of the Huangzhuguan Map-sheet in the Xicheng Pb-Zn Orefield, Gansu

description: The 1∶50 000 mineral geological map of the Huangzhuguan Map-sheet, Gansu(I47E013015) is compiled in accordance with the Technical Requirements of Solid MineralGeological Survey (DD 2019–02) and unified industrial standards and requirements. On thebasis of existing 1∶50 000 and 1∶250 000 regional geological survey results, the work wasperformed through field geology-specific mapping both outdoors and indoors with the help ofdigital mapping systems. The Huangzhuguang mineral geological map redivides the formationtypes of the Devonian Xihanshui Group, and establishes three formation units of the Devonianlead and zinc-forming period, including lead-zinc-bearing carbonate rock formation (D1a1a),lead-zinc-rich carbonate rock formation (D1a1c), and lead-zinc-poor phyllite with limestoneformation (D1a2). The map also establishes the EW fold–fault structure systems within themap-sheet area, highlights the lead-zinc ore-bearing formations and the special lithologic layersclosely related to the metallogenesis of lead and zinc, and innovatively presents geologicalfeatures related to the metallogenesis of lead and zinc in the exhalation sedimentation periodand hydrothermal reformation period supplemented by a lithofacies paleogeographic sketchmap and a tectonic outline map. The database contains 16 stratigraphic units, five stages ofintrusive rocks, three stages of structures, four isotopic ages, 12 pieces of whole-rock analyticaldata, and 30 pieces of mineral deposit data, with a data volume of 30.6 MB. The database givesa full presentation of the demonstrative results of 1∶50 000 mineral geological survey and canprovide reference for other similar areas.
DOI: 10.35080/data.c.2020.p35
title: Database of 1∶50 000 Mineral Geological Map of the Hongshi Map-sheet in Kalatage Copper (-Zinc) Deposit, Hami, Xinjiang

description: The database of 1∶50 000 mineral geological map of Hongshi Map-sheet(K46E009008) in Kalatage Copper (-Zinc) Deposit, Hami, Xinjiang (also referred to as theDatabase) was developed through field geology-specific mapping using the digital mappingsystem in accordance with the Technical Requirements of Solid Mineral Geological Survey(1∶50 000) (DD2019-02) and other standards and requirements in the geological industry.Meanwhile, the results of previous 1∶200 000 and 1∶50 000 regional geological surveyswere fully utilized, and indoor and outdoor mapping/compilation was also carried out duringdatabase building. In this database, the suites of the Daliugou Formation of Middle-UpperOrdovician Huangcaopo Group as well as Lower Silurian Hongliuxia and Kalatage formationswere reclassified. Moreover, the formation time of intrusive rocks in the map-sheet area wasdetermined as Silurian, Devonian, and Permian, and the evolutionary sequence of magmaticrocks was established. There are eight large, medium and small mineral deposits and oreoccurrences in the map-sheet area, the metallogenic epoch of which is concentrated in theSilurian and Carboniferous. The ore-hosted wall rocks are pyroclastic and subvolcanic rocks.The dominant mineral resources in this area are copper, zinc and gold, and their deposit typesare mainly VMS type and subvolcanic hydrothermal vein type, which are distributed in thesoutheastern zone of the map-sheet area. In addition to metallic minerals, there are bentonitedeposits with good prospecting potential. With a data size of about 15.1 MB, this databasecontains the data of five stratigraphic units and three stages of magmatic rocks. These datafully reflect the demonstration results of 1∶50 000 mineral geological survey of this mapsheetand provide references for the research and exploration of mineral resources in the surveyarea.
DOI: 10.35080/data.c.2020.p22
title: Database of 1∶50 000 Mineral Geological Map of the Shiren Town Map-sheet, Jilin Province

description: The 1∶50 000 mineral geological map of the Shiren Town map-sheet(K52E013003) in Jilin Province was prepared by adopting indoor and field mapping(compilation) according to the Technical Requirement of 1∶50 000 Solid Mineral GeologicalSurvey (DD 2019-02), during which the results of previous 1∶50 000 regional geologicalsurveys were fully utilized. With mineralization types as the main line, this project focused onmineral and geology-specific mapping based on a preliminary study and mainly researchedmetallogenic factors. Meanwhile, the presentation of geology-specific mapping results wasactively explored and innovated, the stratigraphic sequences of the Shiren Town map-sheetwere basically ascertained, and the sedimentary rock suites, intrusion suites, and metamorphicrock suites were determined in detail. The map was completed by adding geographic data andmineral resource information to the suite-tectonic map, highlighting the expression ofmetallogenic information. The database of the map (also referred to as the Database) contains amineral geological vector map in MapGIS format, whole-rock petrogeochemical data of sevensamples, petrogeochemical data of major, trace, and rare earth elements of 20 samples, andzircon U–Pb isotopic dating data of 16 samples. Besides, it includes the data of 13 gold andpolymetallic deposits, whose genetic types are quartz vein and alteration types. The totalamount of resource reserves is 1 098.41 ×104 t, and that of gold is 49 989 kg, with the averageAu grade of 4.55 g/t. With a data size of about 80.70 MB, the database fully reflects the resultsof 1∶50 000 mineral and geology-specific mapping, thus providing basic geological bases andprospecting direction for future strategic actions on prospecting breakthroughs.
DOI: 10.35080/data.c.2020.p24
title: Database of 1∶50 000 Mineral Geological Map of Changtuxilesitai Map-sheet, Inner Mongolia

description: In this paper, the database of 1∶50 000 mineral geological map of ChangtuxilesitaiMap-sheet (L50E015021), Inner Mongolia (also referred to as the Database) was establishedon the basis of digital geological mapping system, achieving the digitalization of the wholeprocess of early data preparation → field geological mapping → indoor comprehensive datacollation → the presentation of final results. Meanwhile, various relevant data were effectivelydescribed, stored, organized and utilized in an integrated way. The mapping method of“volcanic structure–lithology and lithofacies–volcanic strata” was adopted during theestablishment of the Database. As a result, the volcanic strata were determined again, and thevolcanic lithofacies as well as eruption cycles and their association types were classified indetail. Furthermore, the relationship of volcanics, volcanic structures and volcanic activitieswith mineralization were ascertained, and the geological conditions and metallogenic rule ofmetal minerals in Mesozoic volcanic areas were summarized. The Database contains eightstratigraphic units, four phases of volcanic eruption cycles, eight mineralization prospectingareas and six prospecting target areas. In addition, it also contains analytical data on 1 170pieces of rock samples and 261 pieces of samples for geochemistry, 108 pieces of samples forpetrochemistry, 222 pieces of thin slice samples for petrography, 35 pieces of S and Pbisotopes, ten pieces of H and O isotopes, as well as four zircon U–Pb ages. The newlydiscovered Changtuxili Ag-Pb-Zn-Mn deposits in the map-sheet area have a roughly identifiedresource of 1 028.35 tonnes of 3341 Ag, 112 500 tonnes of Pb, 93 600 tonnes of Zn and 552 400tonnes of Mn, belonging to a large-scale silver polymetallic deposit. The Database is detailedand accurate in contents and boasts high utility, providing important basic data for furthersurvey and assessment of mineral resources, as well as the exploration and development ofmetal minerals in the area of Mesozoic volcanic rocks in the middle–southern section of the DaHinggan Mountains.
DOI: 10.35080/data.c.2020.p27
title: 1∶50 000 Mineral and Geological Map Database of Zangjiazhuang Map-sheet, Shandong Province

description: The 1∶50 000 mineral and geological map of Zangjiazhuang Map-sheet(J51E016004), Shandong Province was prepared according to applicable industry standardssuch as Technical Requirement of 1∶50 000 Solid Mineral Geological Survey (DD 2019-02)and Spatial Database for Digital Geological Map (DD 2006-06), during which the results ofrelevant 1∶50 000- and 1∶200 000-scale regional geological surveys were fully adopted. Inaddition, a digital mapping system was applied to acquire data in the field, and indoor mappreparation was conducted in combination with field survey of key survey sites. The data in the1∶50 000 mineral and geological map database of Zangjiazhuang Map-sheet, ShandongProvince (also referred to as the Database) was individually stored according to four types ofclasses, namely feature classes, complex classes, object classes and independent featureclasses. In this paper, a new polymetallic metallogenic belt located in Qixia, Yantai City wasproposed, i.e., the Gaojia–Xiangkuang–Xingjiashan polymetallic metallogenic belt. Thismetallogenic belt, with Mesozoic acid intrusions as metallogenic intrusions, is under thecontrol of the intersection of the EW- and NNE-trending faults. LA-ICP-MS zircon U-Pbdating of the metallogenic intrusions in typical Xiangkuang polymetallic deposits indicates thatthe metallogenic age of the metallogenic intrusions is 127.91±0.58 Ma, providing new credibledata for research into the metallogenic ages and rules of the polymetallic deposits inZangjiazhuang Map-sheet. The Database covers the data of five ages and 25 mineral deposits,including two copper ore occurrences and one gold mineralized point that were newlydiscovered. Meanwhile, two prospecting target areas were determined and six predictedminimum prospecting target areas were delineated. Furthermore, the resources of Au, Ag, Pband Zn in the new polymetallic metallogenic belt were predicted to be 10 962 kg, 499.638 t,141 437 t and 230 011 t, respectively. The Database could provide basic data for the geologicalprospecting in Zangjiazhuang Map-sheet, as well as data sources for information- and network-oriented construction of geology.
DOI: 10.35080/data.c.2020.p29
title: 1∶50 000 Mineral Geological Map Database of the Bazang Map-sheet, Gansu

description: The 1∶50 000 mineral geological map database of the Bazang Map-sheet(I48E013009), Gansu was compiled under the guidance of the Guide for Compiling Maps ofMineral Geological Survey Results (draft for discussion) and the three-in-one ore prospectingprediction geological model. The collected data include the previous 1∶50 000 regionalgeological survey primitive data maps, mineral investigation reports, scientific researchreports, academic papers, and gathered data in the 1∶50 000 specific mapping. Data recordsinclude 811 entries on attitude, 102 on geological boundary, 5 on isotopic age, 2 on fossil, 21on mineral information, 22 on mineralization alteration, 86 on fault, 111 on fold, and 65 onformation. The map face is a combination of the master map and corner maps to give a full,objective presentation of the regional geological boundaries, rock formations, eras, faults, foldaxial traces, joints, cleavages, wrinkle lineations, mullion structures, fault plane striations,mineralization alterations, mineral information, and the metallogenic geology of typicaldeposits, covering the Caledonian storm deposits and fold deformations, Early Carboniferousferruginous nodules, and a series of new discoveries and new understandings. In the attributesof the “formation-structure” layer, ore-bearing formations and mineralization alterations areemphasized. In the “fault” layer and “fold” structure layer, ore-forming structures areemphasized. The database provides basic data for the investigation and research of regionalmetallogenesis as well as engineering geology and environmental geology, and can beretrieved by users whenever so needed. The data volume of the Bazang Map-sheet isapproximately 90.2 MB for the MapGIS spatial database and 2.51 MB for the Access database.
DOI: 10.5281/zenodo.4686358
title: Depth of Martian Magnetization From Localized Power Spectrum Analysis

description: Supplementary data to the article Gong, S. and Wieczorek, M. (2021) Depth of Martian Magnetization From<br> Localized Power Spectrum Analysis, J. Geophys. Res. Planets This archive contains the final inversion results for the employed magnetized<br> caps model using a magnetic field that expanded to degree and order 134. For<br> each localized analysis, the bandwidth and angular radius of the window were<br> 17 and 20 degrees, respectively, which yields 8 localization windows that<br> concentrated more than 70% of the power with the region of interest. The<br> analyses were performed at 150 km altitude and on an equally spaced grid with a<br> spacing corresponding to 10 degrees of latitude. FILE DESCRIPTIONS 20_17_8_134_150.dat This file contains the best fitting values and the corresponding reduced<br> chi^2 value of the inversion. The first two columns correspond to the<br> latitude and longitude, and the third to sixth columns correspond to the<br> best fitting values of the angular radii (in km) of the magnetized caps,<br> the magnetization depth (in km), the square root of the metric N&lt;M^2&gt;V^2<br> (in A m^2), and the reduced chi^2 value of the best fitting model at each<br> location, respectively. 20_17_8_134_150_lower.dat<br> 20_17_8_134_150_upper.dat These two files contain the 1-sigma lower and upper limits of the<br> parameters. For each file, the first two columns correspond to the latitude<br> and longitude, and the third to fifth columns correspond to the 1-sigma<br> lower or upper limits of the angular radii (in km) of the magnetized caps,<br> the magnetization depth (in km), the square root of the metric N&lt;M^2&gt;V^2<br> (in A m^2), respectively. The last column corresponds to the 1-sigma<br> confidence level of the reduced chi^2 that were obtained from Monte Carlo<br> simulations. The 1-sigma lower and upper limits were set to -1e+100 when the<br> minimum reduced chi^2 value of the best fitting model was above this 1-sigma<br> confidence level.