cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.8260688.v1
title: Paleoproterozoic A-type granite from the southwestern margin of the North China block: high temperature melting of tonalitic crust in extensional setting

description: Proterozoic igneous rocks in the southern margin of the North China Craton can place constraints on its crustal evolution. This paper reports geochemistry, zircon U-Pb ages, Sr-Nd isotopes and Lu-Hf isotopes for the Proterozoic Angou granite from the southwestern margin of the North China Craton (NCC). The Angou granite has zircon LA-ICP-MS U-Pb age of 1819 ± 14Ma (MSWD = 1.3, n = 37), which is synchronous with the Proterozoic Xiong’er Group in the southeastern margin of the NCC. The granite has A-type granite affinity: (1) high SiO<sub>2</sub> (67.12% to 73.16%) and alkali (Na<sub>2</sub>O+K<sub>2</sub>O = 7.18% to 8.75%) contents, with K<sub>2</sub>O/Na<sub>2</sub>O ratios of 1.04 to 4.78; (2) high FeO<sub>T</sub>/MgO values (4 to 36); (3) significantly negative Eu anomalies (Eu*/Eu = 0.33 to 0.53) and negative Sr anomalies (38.1 to 102ppm); (4) high 10<sup>4</sup>× Ga/Al (2.55 to 4.75, with an average of 3.43) values and Zr+Ce+Nb+Y (634 to 1022ppm) contents; (5) high zircon saturation temperatures (871 to 957°C). In combination with its slightly peraluminous (A/CNK = 1.02 to 1.26) nature, the Angou granite can be classified as slightly peraluminous A-type granite. It displays negative ɛ<sub>Nd</sub>(t) values of −2.0 to −3.9, variable ε<sub>Hf</sub>(t) values (−8.81 to +1.98) with Hf model ages of 2194 to 2721Ma, combined with its high Rb/Sr (1.05 to 3.26) and low Rb/Ba (0.08 to 0.18) ratios, suggesting that the Angou granite was derived from high temperature melting of tonalite in middle-lower crust. The formation of Angou A-type granite is consistent with the mafic dyke swarms and Xiong’er bimodal volcanic rocks in NCC, indicating a Paleoprotozoic extensional setting in the southwestern margin of the NCC.
DOI: 10.15784/601575
title: Weddell seal iron dynamics and oxygen stores across lactation

description: The profound impacts that maternal provisioning of finite energy resources has on offspring survival have been extensively studied across mammals. However, in addition to calories, we tested whether high hemoprotein concentrations in diving mammals necessitates exceptional female-to-pup iron transfer. To answer this question adult female Weddell seals (Leptonychotes weddellii) were handled across the austral summer. This included post-partum females during lactation and post-weaning. To demonstrate that any observed changes in iron dynamics were due to lactation, equivalent skip-breeding females (i.e., that did not produce a pup) were also handled. We measured numerous indices of iron mobilization (ferritin, serum iron, total-iron-binding-capacity, transferrin saturation, milk iron concentration), hemoprotein concentrations, and oxygen stores.
DOI: 10.25345/c5dg9g
title: MassIVE MSV000080636 - MaHPIC Experiment 13: Lipidomics from uninfected Macaca mulatta exposed to pyrimethamine to produce and integrate clinical, hematological, and omics control measures.
title: &lt;p&gt;Uninfected, malaria-naive, male rhesus macaques (&lt;i&gt;Macaca mulatta&lt;/i&gt;), approximately two years of age, were inoculated intravenously with a preparation of salivary gland material derived from non-infected &lt;i&gt;Anopheles dirus&lt;/i&gt; and profiled for clinical, hematological, functional genomic, lipidomic, proteomic, and metabolomic measurements. Samples were generated and analyzed to investigate the effects of the pharmacological intervention with the anti-malarial drug pyrimethamine on normal individuals. The experiment was designed for 100 days plus a follow-up period, with pyrimethamine administered at three different time points to coincide with the predicted treatment days of experimentally infected rhesus macaques. Capillary blood samples were collected daily for the measurement of CBCs and reticulocytes. Capillary blood samples were collected every other day to obtain plasma for metabolomic analysis. Venous blood samples and bone marrow aspirates were collected at seven time points before and after three rounds of drug administration for functional genomic, proteomic, and lipidomic analyses. Within the MaHPIC, this project is known as 'Experiment 13' ('E13'). To access other publicly available results from E13 and other MaHPIC Experiments, including clinical results (specifics on drugs administered, diet, and veterinary interventions), and other omics, visit &lt;a href="http://plasmodb.org/plasmo/mahpic.jsp"&gt;http://plasmodb.org/plasmo/mahpic.jsp&lt;/a&gt;. This dataset was produced by: The MaHPIC Consortium, Monica Cabrera, Jeremy D. DeBarry, Mary G. Galinski, Jay Humphrey, Ebru Karpuzoglu, Jessica C. Kissinger, Regina Joice, Esmeralda Meyer, Alberto Moreno, Vishal Nayak, Mustafa Nural, Suman Pakala, and Sarah Pruett. The experimental design and protocols for this study were approved by the Emory University Institutional Animal Care and Use Committee (IACUC).&lt;/p&gt;
DOI: 10.25739/70ze-8c03
title: Malaria Host Pathogen Interaction Center (MaHPIC) Experiment 25 (E25) Clinical Results

description: Experiment 25: Macaca mulatta infected with Plasmodium cynomolgi strain ceylonensis, in a heterologous challenge, to produce and integrate clinical, hematological, parasitological, and omics measures of acute primary infection and relapses. This clinical results dataset contains measures of disease infection including counts and calucations for: CBCs, reticulocytes, parasitemias, and downstream immunological, functional genomic, lipidomic, proteomic, and metabolomic measurements. Results also include data and metadata from veterinarians on all facets of animal access, including, but not limited to: treatments, hematology, biochemical analyses, parasitology, bacteriology, and surgery statistics, etc. Results also include documentation of data collection and analysis methods and supporting clinical matarials that differentiate between 'Idealized' and 'Actual' disease progression. This is the third in a series of experiments that includes infection of malaria-naïve subjects (Experiment 23, P. cynomolgi B strain) and homologous challenge (Experiment 24, P. cynomolgi B strain) for the individuals from the same cohort. Subjects were cleared of previous infection with P. cynomolgi B strain via treatment with the anti-malarial drugs artemether, chloroquine, and primaquine. Please see the file 'E25M99MEMmCyDaWB_README-PlasmoDB-09262018-V1_MULTIPL.txt' for a full description of this dataset and for instructions on how to access other datasets from this experiment. Please see https://plasmodb.org/plasmo/mahpic.jsp for descriptions and locations of all public MaHPIC datasets.
DOI: 10.25739/h4ej-7691
title: Malaria Host Pathogen Interaction Center (MaHPIC) Experiment 13 (E13) Clinical Results

description: Experiment 13: Uninfected Macaca mulatta exposed to pyrimethamine to produce clinical, hematological, and omics control measures. This clinical results dataset includes infection control measures. Please see the file 'E13M99MEMmXXDpWB_09212018-Readme_MULTIPL.txt' for a full description of this dataset and for instructions on how to access other datasets from this experiment. Please see https://plasmodb.org/plasmo/mahpic.jsp for descriptions and locations of all public MaHPIC datasets.
DOI: 10.25739/zbw6-xk16
title: Malaria Host Pathogen Interaction Center (MaHPIC) Experiment 24 (E24) Clinical Results

description: Experiment 24: Macaca mulatta infected with Plasmodium cynomolgi B strain, in a homologous challenge, to produce and integrate clinical, hematological, parasitological, and omics measures of acute primary infection and relapses. This clinical results dataset contains measures of disease infection including counts and calucations for: CBCs, reticulocytes, parasitemias, and downstream immunological, functional genomic, lipidomic, and metabolomic measurements. Results also include data and metadata from veterinarians on all facets of animal access, including, but not limited to: treatments, hematology, biochemical analyses, parasitology, bacteriology, and surgery statistics, etc. Results also include documentation of data collection and analysis methods and supporting clinical matarials that differentiate between 'Idealized' and 'Actual' disease progression. This is the second in a series of experiments that includes infection of malaria-naïve subjects (Experiment 23, P. cynomolgi B strain) and heterologous challenge (Experiment 25, P. cynomolgi strain ceylonensis) for the individuals from the same cohort. Subjects were cleared of previous infection with P. cynomolgi B strain via treatment with the anti-malarial drugs artemether, chloroquine, and primaquine. Please see the file 'E24M99MEMmCyDaWB_README-PlasmoDB-09242018-V1_MULTIPL.txt for a full description of this dataset and for instructions on how to access other datasets from this experiment. Please see https://plasmodb.org/plasmo/mahpic.jsp for descriptions and locations of all public MaHPIC datasets.
DOI: 10.4121/uuid:41f45b0b-fe19-4007-a4aa-7234e08f40f1
title: Table 1, supplementary data for the paper: Detachment faulting in the Xigazê ophiolite: New constraints on its formation and implications for other ophiolites in the YZSZ, southern Tibet

description: Zircon U-Pb analytical results of the crustal rocks from the Xigaze ophiolite by Laser Ablation – Inductively Coupled Plasma – Mass Spectrometry (LA-ICP-MS) imaging
DOI: 10.5281/zenodo.1157934
title: Polymod Social Contact Data

description: This is the POLYMOD study data.
description: {"references": ["Mossong J, Hens N, Jit M, Beutels P, Auranen K, et al. (2008) Social Contacts and Mixing Patterns Relevant to the Spread of Infectious Diseases. PLOS Medicine 5(3): e74. https://doi.org/10.1371/journal.pmed.0050074"]}
DOI: 10.5281/zenodo.5939805
title: CUPLR features, HMF and PCAWG samples

description: Raw features for the HMF (DR104) and PCAWG cohorts used for training and evaluating the performance of CUPLR
DOI: 10.5281/zenodo.6445460
title: Data for Yamagami et al. (2022)

description: Dataset and python scripts to reproduce main figures in the Yamagami et al (2022). - csv files (.csv) in "data_fig1": Time series and linear trends for figure 1. - netcdf files (.nc) in "data": Linear trends of atmospheric and oceanic variables for figure 2-4. - csv files (.csv) in "data_ht": Linear trends of ocean heat transports for figure 3. - netcdf files (.nc) and csv files (.csv) in "data_nagac": Annual mean potential temperature and ocean velocity for figure 5. - csv files (.csv) in "csv_trends": Linear trends for figure 6. - .py files are python scripts to make figures.
DOI: 10.5291/ill-data.5-41-983
title: Structural refinement of the dimerization in NaFe(WO4)2
DOI: 10.6084/m9.figshare.1181864.v2
title: Crust–mantle interaction triggered by oblique subduction of the Pacific plate: geochronological, geochemical, and Hf isotopic evidence from the Early Cretaceous volcanic rocks of Zhejiang Province, southeast China

description: Large-scale volcanism in the late Mesozoic was a prominent geological event in southeast China. The late Mesozoic volcanic sequences, named the Moshishan Group, are exposed in Zhejiang Province and are predominantly felsic in composition with subordinate mafic magma and rare andesites. To understand the late Mesozoic tectonic evolution of southeast China, we present zircon U–Pb dating, major and trace element analyses, and Hf isotopic compositions from felsic volcanic rocks of the Moshishan Group. Zircon U–Pb dating shows that the Moshishan Group formed between 145 and 129 Ma. The ε<sub>Hf</sub>(<i>t</i>) of the analysed zircons ranges from −16.58 to +6.89, and the <i>T</i><sub>DM2</sub> age ranges from 753 to 2238 Ma with a major peak at ca. 1870 Ma. Hf isotopic compositions of zircons in Early Cretaceous volcanic rocks are more radiogenic than that of the metamorphic basement rocks, indicating a juvenile component in these magmas. Major element concentrations show that the volcanic rocks mainly belong to the high-K calc-alkaline series. Both zircon saturation temperatures and the ε<sub>Hf</sub>(<i>t</i>) values of zircons gradually increased with the evolution of the magma. Trace element data indicates that neither magmatic differentiation of mantle-derived magma nor mixing of magmas from different sources were the predominant magmagenetic processes. Earlier studies suggest that contemporaneous underplating contributed to the heat source that induced crustal melting and to the material origin that inconsistently mixed with the local crustal melts. Magmatic underplating is likely to have occurred because of the southwestward subduction of the Pacific plate with episodic slab rollback. The data obtained in this study suggest that the crust–mantle interaction under the influence of slab rollback played a progressive role in the formation of Early Cretaceous felsic volcanic rocks in southeast China.
DOI: 10.6084/m9.figshare.11889408.v1
title: Neoproterozoic granitoids from the Phan Si Pan Zone, NW Vietnam: geochemistry and geochronology constraints on reconstructing South China – India Palaeogeography

description: Neoproterozoic rocks in the Phan Si Pan Zone, NW Vietnam are considered to be the remnant of the ancient continental crust. They recorded the evolution of the Gondwana supercontinent. A combined study of U-Pb geochronology and Sr-Nd-Hf isotopic geochemistry has been carried out for the Neoproterozoic granites in the Phan Si Pan Zone. Zircon LA-ICP-MS data yield crystallization ages ranging from 758.0 ± 5.0 to 762.0 ± 8.1 Ma. The Neoproterozoic granites have variable (<sup>87</sup>Sr/<sup>86</sup>Sr)<sub>i</sub> ratios of 0.7029 to 0.708 and a wide range of <i>ε</i><sub>Nd</sub>(t) values (−2.02 to 0.04) and of zircon <i>ε</i><sub>Hf</sub>(t) values (−5.1 to 0.0). All these characteristics suggest an origin through partial melting of ancient crustal source rocks with small amount input from the mantle material. Whole-rock Nd and zircon Hf isotopic model ages mostly vary from 1.67 Ga to 1.99 Ga, indicating the existence of the Paleoproterozoic source material in the study area. Neoproterozoic granites in the Phan Si Pan Zone, NW Vietnam have a similar tectonic evolution to those in SW Yangtze, South China.
DOI: 10.6084/m9.figshare.12136878.v1
title: Permian igneous clasts from the Matzitzi Formation, southern Mexico: isotopic constraints on the final amalgamation of Pangea

description: Table A.2. Lu-Hf isotopic data of zircons from four volcanic clasts.
DOI: 10.6084/m9.figshare.12195678.v1
title: Supplement Information for Tectonics (Permian-Triassic magmatic evolution of granitoids from the southeastern Central Asian Orogenic Belt: implications for accretion leading to collision

description: <b>Geochronology, geochemistry, Sr-Nd and Lu-Hf isotopic data of granitoids.</b><br>
DOI: 10.6084/m9.figshare.12202406.v1
title: Geochemistry and tectonic significance of the Fannuj-Maskutan SSZ-type ophiolite (Inner Makran, SE Iran)

description: The nature and geodynamic setting of Inner Makran ophiolites (SE Iran) are controversial and are the focus of a growing debate. The Fannuj-Maskutan ophiolite complex (central Inner Makran) is made up of lherzolites, harzburgites, layered and isotropic gabbros and diabase dikes and basaltic lavas. Here we present new textural description, mineral and whole-rock chemistry of peridotites together with bulk geochemistry of magmatic mafic rocks and U-Pb geochronology and Lu-Hf isotopes of inherited zircons in gabbros, with the aim to reconstruct the petrogenesis of the Fannuj-Maskutan ophiolite. The results indicate to a subduction-metasomatized depleted mantle source experienced 10–20% of partial melting. A transition from IAT-gabbros to E-MORB-basalts is also outlined. We interpret the obtained results as evidence for the Fannuj-Maskutan genesis in a supra-subduction zone (SSZ) basin developed in the Iranian cadomian crust as indicated by the presence of inherited Cadomian zircons (ca. 515 Ma, εHf<sub>(t)</sub>: −13.6 – +11.2). Comparing the Fannuj-Maskutan ophiolites to well-known SSZ-systems such as the South Sandwich SSZ, and integrating with the existing literature on Inner Makran ophiolite belt we interpret the Fannuj-Maskutan ophiolite as a part of a major SSZ-basin opened in the Iranian cadomian crust and evolved during the Neotethys subduction under Central Iran.
DOI: 10.6084/m9.figshare.12205166.v1
title: Mechanism of Paleoarchean continental crust formation as archived in granitoids from northern part of Singhbhum Craton, eastern India

description: Supplemental Table 4: Lu–Hf isotope compositions of zircon grains of granitoids from Saraikela–Hata area, Singhbhum Craton
DOI: 10.6084/m9.figshare.12286616.v1
title: Table S6: Zircon Lu–Hf and O isotope composition of the Paleogene rocks from oceanic tract of NW Iran. The Paleogene Ophiolite Conundrum of the Iran–Iraq Border Region

description: Table S6: Zircon Lu–Hf and O isotope composition of the Paleogene rocks from oceanic tract of NW Iran.
DOI: 10.6084/m9.figshare.1229936.v4
title: New data on detrital zircons from the sandstones of the lower Cambrian Brusov Formation (White Sea region, East-European Craton): unravelling the timing of the onset of the Arctida–Baltica collision

description: The basement of the northeastern periphery of the East-European Craton (ЕЕС) is composed of volcanic-sedimentary sequences, volcanic rocks, granitoids, and rare ophiolite complexes. Geochronological data constrain their age from ca. 750 to 500 Ma, and there is a consensus that these rocks represent relicts of a late Neoproterozoic–Cambrian Pre-Uralides–Timanides orogeny. Combining new integrated isotopic (U-Pb, Lu-Hf) and trace-element data (TerraneChrone<sup>®</sup> approach) on detrital zircons from sandstones of the lower Cambrian Brusov Formation in the Mezen basin (White Sea region in the northeastern periphery of the EEC) with available studies on detrital zircons from Neoproterozoic–middle Cambrian (meta)sedimentary units of the northeastern periphery of the EEC allow us to conclude that (1) the onset of the Arctida–Baltica collision can now be constrained to the time interval between ca. 540 and 510 Ma and (2) the Ediacaran–early Cambrian Mezen sedimentary basin was a basin on the Timanian passive margin of Baltica up to 540 Ma, but was not a foreland basin of the Pre-Uralides–Timanides orogen.
DOI: 10.6084/m9.figshare.12398573.v1
title: Zircon U-Pb ages and Hf isotopes, and whole-rock geochemical compositions

description: Zircon U-Pb ages and Hf isotopes, and whole-rock geochemical compositions for Beishan complex
DOI: 10.6084/m9.figshare.12449579.v1
title: Provenance record of late Mesoproterozoic to early Neoproterozoic units, west Hainan, South China, and implications for Rodinia reconstruction

description: The Supporting Information contains three figures in JPG, three tables in Word and two dataset in Excel file. Details ,<br>Figure S1, Detrital zircon CL images with age and εHf (t) values for the representative samples from the Shilu Group and Shihuiding Formation in west Hainan. Figure S2, <b>P</b>lots of Al2O3 and K2O + Na2O vs. SiO2 (a,b) and (b) TiO2 and Fe2O3T vs. Al2O3 (c,d) for the Shilu Group and Shihuiding Formation samples in west Hainan. The compositions of PAAS (Post Archean Australia Shale, Taylor and McLennan, 1985) and UCC (Upper Continental Crust, Rudnick and Gao, 2003) are also shown diagrams for comparison. Figure S3, Source rock discrimination diagrams for the metasedimentary rocks on (a) 100*TiO2/Al2O3 vs. 100*TiO2/Fe2O3T and (b) (La/Yb)n vs. Eu*/Eu. End members, including average Proterozoic felsic volcanic rocks, andesite, basalt, granite and TTG from Condie, 1993, are plotted for comparison.Table S1, Major oxides and trace elemental analytical results for the represent samples from the Shilu Group and Shihuiding Formation in west Hainan.Table S2, Zircon U–Pb dating results for the representative samples from the Shilu Group and Shihuiding Formation in west Hainan<br>Table S3, Zircon Lu-Hf isotopic composition for the representative samples from the Shilu Group and Shihuiding Formation in west Hainan (A decay constant for <sup>176</sup>Lu of 1.865 ± 0.015 × 10<sup>−11</sup>/year is used for calculating ε<sub>Hf</sub> (t) values and Hf model ages).Data Set S1,Published zircon U-Pb geochronological data of Meso-Neoproterozoic samples from Hainan, the Yangtze Block, India and western Laurentia. Data Set S2, Published zircon Hf isotopic data of Meso-Neoproterozoic samples from Hainan, the Yangtze and Cathaysia Block.<br>
DOI: 10.6084/m9.figshare.12783869.v1
title: Supplementary A: New zircon U-Pb, REE and Lu-Hf data for detrital samples from Paleoproterozoic sequences in Madagascar

description: This includes new zircon U-Pb, REE and Lu-Hf for samples in Madagascar
DOI: 10.6084/m9.figshare.12854117.v1
title: Detrital zircon U-Pb ages of the late Mesoproterozoic–Neoproterozoic Qiaotou formation in the Liao-Ji area of the North China Craton: implications for Rodinia reconstruction

description: The Qiaotou Formation comprises the late Mesoproterozoic to early Neoproterozoic strata in southern Jilin and Liaoning Provinces at the eastern margin of the North China Craton (NCC). The depositional age of the formation is 1.1–0.9 Ga, as constrained from the ages of the youngest detrital zircons and later mafic intrusions. U-Pb age dating of detrital zircons yielded age peaks at 1.16, 1.58, and 1.74 Ga, and a minor peak of 2.47 Ga. The late Neoarchaean to Palaeoproterozoic detrital zircons were derived from the ca. 2.5 Ga Longgang and Liaonan blocks, ca.1.9 Ga magmatic/metamorphic rocks and late Palaeoproterozoic extensional-related magmatic rocks in NCC. The abundance of Mesoproterozoic zircon grains is less easy to explain. The possible source may represent (i) possibly concealed/vanished Grenvillian magmatic rocks in NCC, or (ii) derivation from the Qinling Microcontinent or (iii) Fennoscandian shield, or (iv) São Francisco–Congo Craton.
DOI: 10.6084/m9.figshare.12854147.v1
title: The evolution of the southern Namibian Karoo-aged basins: implications from detrital zircon geochronologic and geochemistry data

description: Detrital U-Pb zircon age dating and grain morphometrics were used for provenance and maximum deposition age determination for the Lower Permian Dwyka and Middle to Upper Permian Ecca groups of southern Namibia’s Aranos and Karasburg basins. Thirteen sedimentary samples and one ash fall sample were analysed using laser ablation – single collector – inductively coupled plasma – mass spectrometry (LA-ICP-MS). The results reveal prominent Cambrian to Neoproterozoic (500–750 Ma), a Lower Neoproterozoic to Mesoproterozoic (950–1300 Ma), and Upper Palaeoproterozoic (1775–1950 Ma) detrital zircon age populations. Multiple evidence (e.g. roundness of investigated zircon grains and <sub>Ɛ</sub>Hf values) suggest the zircon populations are part of a Gondwana-wide recycling system, where basins act as intermediate reservoirs and eventual dispersers. Classic source to sink dynamics do not apply. A Permian age population (ca. 260–296 Ma) consisting of typically euhedral zircon grains is assumed to be derived directly from protolith rocks. Because no felsic Permian rocks are exposed in the southern African region, these findings suggest a significant input by ash fall from an unknown source, which may be linked to the southern Gondwanan arc volcanism during Permian times. The results reveal a ca. 36 Ma duration of the evolution of the Karasburg Basin and a shorter ca. 30 Ma lasting evolution of the Aranos Basin. The stratigraphic oldest datable unit is an ash bed of the Ganigobis Shale Member of the Zwartbas Fm (Dwyka Group) which gave a maximum deposition age of ca. 296 Ma, whereas the Aussenkjer Fm represents the uppermost Namibian Karoo-aged strata with a maximum age of deposition of ca. 260 Ma.