cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.9778364
title: A reconnaissance provenance study of Triassic–Jurassic clastic rocks of the Russian Barents Sea

description: Combined U–Pb detrital zircon dating of 21 samples, along with whole-rock chemical composition and Sm–Nd isotopic studies of 39 samples of Triassic and Jurassic rocks from Franz Josef Land and wells in the southern part of the Russian (eastern) Barents Sea, were analyzed for a reconnaissance provenance study. The similarity of detrital zircon age distributions was statistically assessed using the Kolmogorov–Smirnov (K–S) test and points to a common source area for the clastic material of Triassic to Middle Jurassic age. Uralian-age detrital zircons predominate in all samples, with a comparably smaller portion of Caledonian- and Timanian-age detrital zircons. The number of Palaeoproterozoic and Archean grains is very small and becomes significant only in a few Jurassic samples. ε<sub>Nd</sub>(t) values gradually decrease from −1.5 to +2.5 in Lower Triassic rocks, to −2.0 to −8.2 in Jurassic rocks, suggesting an increasing influence of ancient metamorphic basement erosion in the younger Jurassic rocks. High Co/Th ratios, suggesting the erosion of mafic rocks, were mainly recorded in Lower Triassic rocks, whereas increasing Th/Sc ratios, suggesting the erosion of felsic rocks, were recorded only in some uppermost Triassic and Jurassic rocks. We identify the Urals and, in addition during the Triassic, the basement of the West Siberian Basin as the main provenance for the studied clastic rocks. By contrast, only a small volume of fine-grained clastic detritus was derived from basement erosion of the East European Craton, which was characterized by a subdued relief during this time.
DOI: 10.6084/m9.figshare.9778364.v1
title: A reconnaissance provenance study of Triassic–Jurassic clastic rocks of the Russian Barents Sea

description: Combined U–Pb detrital zircon dating of 21 samples, along with whole-rock chemical composition and Sm–Nd isotopic studies of 39 samples of Triassic and Jurassic rocks from Franz Josef Land and wells in the southern part of the Russian (eastern) Barents Sea, were analyzed for a reconnaissance provenance study. The similarity of detrital zircon age distributions was statistically assessed using the Kolmogorov–Smirnov (K–S) test and points to a common source area for the clastic material of Triassic to Middle Jurassic age. Uralian-age detrital zircons predominate in all samples, with a comparably smaller portion of Caledonian- and Timanian-age detrital zircons. The number of Palaeoproterozoic and Archean grains is very small and becomes significant only in a few Jurassic samples. ε<sub>Nd</sub>(t) values gradually decrease from −1.5 to +2.5 in Lower Triassic rocks, to −2.0 to −8.2 in Jurassic rocks, suggesting an increasing influence of ancient metamorphic basement erosion in the younger Jurassic rocks. High Co/Th ratios, suggesting the erosion of mafic rocks, were mainly recorded in Lower Triassic rocks, whereas increasing Th/Sc ratios, suggesting the erosion of felsic rocks, were recorded only in some uppermost Triassic and Jurassic rocks. We identify the Urals and, in addition during the Triassic, the basement of the West Siberian Basin as the main provenance for the studied clastic rocks. By contrast, only a small volume of fine-grained clastic detritus was derived from basement erosion of the East European Craton, which was characterized by a subdued relief during this time.
DOI: 10.6084/m9.figshare.9918518.v2
title: Detrital zircon record of the Mesoproterozoic to Lower Cambrian sequences of NW Russia: implications for the paleogeography of the Baltic interior

description: Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) U–Pb detrital zircon isotope data from Mesoproterozoic to Lower Cambrian strata of the St Petersburg region are used to characterize the paleogeographic and tectonic evolution of the Baltica continent. We dated fifteen samples and divided them into three groups based on their distribution of detrital zircons. The first group (comprising Lower Mesoproterozoic rocks) is dominated by Early Mesoproterozoic and Late Paleoproterozoic zircons, mostly derived from weathering of proximal source region including rapakivi granites exposed across the neighboring Baltic Shield. The second group includes Upper Ediacaran samples (Redkino and Kotlin Regional Stages), with major zircon populations ranging in age between 1970–1850 and 1600–1550 Ma, respectively, correlating with magmatic and metamorphic events within the Svecofennian Orogeny and rapakivi granite igneous activity in the interior of Fennoscandia. The third group of samples, collected from both the uppermost Ediacaran and lowermost Cambrian deposits (Kotlin, Lontova and Dominopol Regional Stages), contains older Paleo-Mesoproterozoic zircons as well as Late Neoproterozoic-earliest Cambrian zircons, indicating a Timanian source area and exhibiting a age spectra similar to spectra for coeval rocks of the Scandinavian Caledonides. Therefore, we conclude that reworking and transport of continental detritus from the Timanian Orogen began during Late Ediacaran, earlier than previously supposed, with transport of Timanian detritus not only to the marginal part of Baltica (known from the Scandinavian Caledonides), but also to the distal interior of Baltica.
DOI: 10.6084/m9.figshare.9918518
title: Detrital zircon record of the Mesoproterozoic to Lower Cambrian sequences of NW Russia: implications for the paleogeography of the Baltic interior

description: Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) U–Pb detrital zircon isotope data from Mesoproterozoic to Lower Cambrian strata of the St Petersburg region are used to characterize the paleogeographic and tectonic evolution of the Baltica continent. We dated fifteen samples and divided them into three groups based on their distribution of detrital zircons. The first group (comprising Lower Mesoproterozoic rocks) is dominated by Early Mesoproterozoic and Late Paleoproterozoic zircons, mostly derived from weathering of proximal source region including rapakivi granites exposed across the neighboring Baltic Shield. The second group includes Upper Ediacaran samples (Redkino and Kotlin Regional Stages), with major zircon populations ranging in age between 1970–1850 and 1600–1550 Ma, respectively, correlating with magmatic and metamorphic events within the Svecofennian Orogeny and rapakivi granite igneous activity in the interior of Fennoscandia. The third group of samples, collected from both the uppermost Ediacaran and lowermost Cambrian deposits (Kotlin, Lontova and Dominopol Regional Stages), contains older Paleo-Mesoproterozoic zircons as well as Late Neoproterozoic-earliest Cambrian zircons, indicating a Timanian source area and exhibiting a age spectra similar to spectra for coeval rocks of the Scandinavian Caledonides. Therefore, we conclude that reworking and transport of continental detritus from the Timanian Orogen began during Late Ediacaran, earlier than previously supposed, with transport of Timanian detritus not only to the marginal part of Baltica (known from the Scandinavian Caledonides), but also to the distal interior of Baltica.
DOI: 10.6084/m9.figshare.9778340
title: Shallow reworking of magmatic zircon grains of latest Neoproterozoic (Timanian) age in serpentinite of the Voykar Massif, Polar Urals: new constraints from U-Pb isotopic data, and first trace elements and Lu-Hf isotopic data

description: The Voykar Massif of the Polar Urals in Russia consists of an ultramafic complex (mantle section) in the northwest, followed by a late Cambrian to Silurian mafic complex (intra-oceanic primitive island arc) and early Devonian intrusive rocks of an evolved island arc to the southeast. These complexes represent tectonic nappes thrust over the East European continental margin during the late Palaeozoic Uralian Orogeny. LA-ICP-MS U-Pb dating of zircon grains (n = 42) from an antigorite-serpentinite lens within the mafic complex yielded a Concordia age of 542 ± 2 Ma with an age range of 549–527 Ma. Additionally, few grains contain inherited domains with ages between ~990 and 3277 Ma. Hafnium isotopic data of the main age group show <sup>176</sup>Hf/<sup>177</sup>Hf<sub>t</sub> from 0.28242 to 028249 and εHf<sub>t</sub> ranging from +1.9 to −6.5. The evolved Hf isotope data and the trace-element composition of the zircon grains point to an involvement of a continental crustal component in the parental magma. The zircon grains originate from igneous rocks formed during the Timanian Orogeny that affected the East European margin in the latest Neoproterozoic. During the Timanian or Uralian Orogeny, the magmatic zircons were eroded and shallowly recycled into the serpentinised mantle above the subduction zone. Finally, Uralian thrusting led to juxtaposition and imbrication of the zircon-bearing serpentinite and intra-oceanic volcanic rocks of the mafic complex.
DOI: 10.6084/m9.figshare.9778394
title: Provenance of the Devonian–Carboniferous clastics of the southern part of the Prikolyma terrane (Verkhoyansk–Kolyma orogen) based on U–Pb dating of detrital zircons

description: U–Pb dating of detrital zircons collected from the Middle–Upper Palaeozoic strata of the Prikolyma terrane (Verkhoyansk–Kolyma orogen) provide the first insight into provenance areas and the Middle–Late Palaeozoic geological history of the Russian Far East. Detrital zircon ages from the Lower–Middle Devonian sandstones group around 395–405 M (Emsian–Eifelian) which correlate well to trachyte of the Uvyazka zone and the Kedon Complex of the North Okhotsk active continental margin located on the Omolon terrane. Precambrian-aged zircons group around 1740–2080 and 2460–2800 Ma, respectively, suggesting possible sources within metamorphic rocks of the basement of the Omolon terrane or the Siberian Craton. The majority of the zircons from the Lower and Upper Carboniferous sandstones group around 333–375 Ma, suggesting that the principle source of the clastics were volcanic rocks and comagmatic felsic intrusions of the Kedon Complex of the North Okhotsk active continental margin. Our new data allow us to evaluate and revise the available palaeotectonic reconstructions of northeast Asia for the Devonian and Carboniferous.
DOI: 10.6084/m9.figshare.9778394.v1
title: Provenance of the Devonian–Carboniferous clastics of the southern part of the Prikolyma terrane (Verkhoyansk–Kolyma orogen) based on U–Pb dating of detrital zircons

description: U–Pb dating of detrital zircons collected from the Middle–Upper Palaeozoic strata of the Prikolyma terrane (Verkhoyansk–Kolyma orogen) provide the first insight into provenance areas and the Middle–Late Palaeozoic geological history of the Russian Far East. Detrital zircon ages from the Lower–Middle Devonian sandstones group around 395–405 M (Emsian–Eifelian) which correlate well to trachyte of the Uvyazka zone and the Kedon Complex of the North Okhotsk active continental margin located on the Omolon terrane. Precambrian-aged zircons group around 1740–2080 and 2460–2800 Ma, respectively, suggesting possible sources within metamorphic rocks of the basement of the Omolon terrane or the Siberian Craton. The majority of the zircons from the Lower and Upper Carboniferous sandstones group around 333–375 Ma, suggesting that the principle source of the clastics were volcanic rocks and comagmatic felsic intrusions of the Kedon Complex of the North Okhotsk active continental margin. Our new data allow us to evaluate and revise the available palaeotectonic reconstructions of northeast Asia for the Devonian and Carboniferous.
DOI: 10.6084/m9.figshare.9778340.v1
title: Shallow reworking of magmatic zircon grains of latest Neoproterozoic (Timanian) age in serpentinite of the Voykar Massif, Polar Urals: new constraints from U-Pb isotopic data, and first trace elements and Lu-Hf isotopic data

description: The Voykar Massif of the Polar Urals in Russia consists of an ultramafic complex (mantle section) in the northwest, followed by a late Cambrian to Silurian mafic complex (intra-oceanic primitive island arc) and early Devonian intrusive rocks of an evolved island arc to the southeast. These complexes represent tectonic nappes thrust over the East European continental margin during the late Palaeozoic Uralian Orogeny. LA-ICP-MS U-Pb dating of zircon grains (n = 42) from an antigorite-serpentinite lens within the mafic complex yielded a Concordia age of 542 ± 2 Ma with an age range of 549–527 Ma. Additionally, few grains contain inherited domains with ages between ~990 and 3277 Ma. Hafnium isotopic data of the main age group show <sup>176</sup>Hf/<sup>177</sup>Hf<sub>t</sub> from 0.28242 to 028249 and εHf<sub>t</sub> ranging from +1.9 to −6.5. The evolved Hf isotope data and the trace-element composition of the zircon grains point to an involvement of a continental crustal component in the parental magma. The zircon grains originate from igneous rocks formed during the Timanian Orogeny that affected the East European margin in the latest Neoproterozoic. During the Timanian or Uralian Orogeny, the magmatic zircons were eroded and shallowly recycled into the serpentinised mantle above the subduction zone. Finally, Uralian thrusting led to juxtaposition and imbrication of the zircon-bearing serpentinite and intra-oceanic volcanic rocks of the mafic complex.
DOI: 10.6084/m9.figshare.9918518.v1
title: Detrital zircon record of the Mesoproterozoic to Lower Cambrian sequences of NW Russia: implications for the paleogeography of the Baltic interior

description: Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) U–Pb detrital zircon isotope data from Mesoproterozoic to Lower Cambrian strata of the St Petersburg region are used to characterize the paleogeographic and tectonic evolution of the Baltica continent. We dated fifteen samples and divided them into three groups based on their distribution of detrital zircons. The first group (comprising Lower Mesoproterozoic rocks) is dominated by Early Mesoproterozoic and Late Paleoproterozoic zircons, mostly derived from weathering of proximal source region including rapakivi granites exposed across the neighboring Baltic Shield. The second group includes Upper Ediacaran samples (Redkino and Kotlin Regional Stages), with major zircon populations ranging in age between 1970–1850 and 1600–1550 Ma, respectively, correlating with magmatic and metamorphic events within the Svecofennian Orogeny and rapakivi granite igneous activity in the interior of Fennoscandia. The third group of samples, collected from both the uppermost Ediacaran and lowermost Cambrian deposits (Kotlin, Lontova and Dominopol Regional Stages), contains older Paleo-Mesoproterozoic zircons as well as Late Neoproterozoic-earliest Cambrian zircons, indicating a Timanian source area and exhibiting a age spectra similar to spectra for coeval rocks of the Scandinavian Caledonides. Therefore, we conclude that reworking and transport of continental detritus from the Timanian Orogen began during Late Ediacaran, earlier than previously supposed, with transport of Timanian detritus not only to the marginal part of Baltica (known from the Scandinavian Caledonides), but also to the distal interior of Baltica.
DOI: 10.5281/zenodo.4384035
title: ENDES2019 Dataset with interpretation on depressive symptomatology in Peruvian adults with HTA

description: ENDES2019 Dataset with interpretation on depressive symptomatology in Peruvian adults with HTA
DOI: 10.5281/zenodo.4384034
title: ENDES2019 Dataset with interpretation on depressive symptomatology in Peruvian adults with HTA

description: ENDES2019 Dataset with interpretation on depressive symptomatology in Peruvian adults with HTA
DOI: 10.6084/m9.figshare.13474920.v1
title: A rare case of long-term complications of squamous cell carcinoma in haemophilia B after arhtrocentesis, and review of the literature

description: The patient is a 53 years old man, who spontaneous joint hemorrhage occurredoccasionally after birth, especially of the knees. But until 1977, when he was age 12years old, he was diagnosed with moderate HB (FⅨ:C 2.8%). Since then, when jointhemorrhages took place, he could only use plasma or cold precipitation replacement treatment, because of the deficient coagulation factorⅨ（FⅨ）. In March 1996, he had a severely IA bleeding of the right knee after traumatic, which the clinical manifestations was severe pain, distension of the joint capsule and flexion antalgic contracture. The orhthopaedic surgeon used knee arthrocentesis to removal of hemarthrosis after about 15 ml/kg day-1plasma transfusion. After the procedure, about 10 ml/kg day-1plasma was infused for 72 hours accompanying a compressive bandage. Although postoperative clinical symptoms improved temporary, the skin around the puncture site of the right joint presented ulceration with purulent exudates with hemorrhage 2 months later.
DOI: 10.48370/ofd/ucu17n
title: Wiechlina łąkowa (Poa pratensis L. s. str.), 2892

description: Herbarium
DOI: 10.25403/upresearchdata.13312682
title: Women leadership in a patriarchal society

description: The datasets were the transcribed interviews. Semi structured interviews for a qualitative study on women leadership in patriarchal society.
DOI: 10.25403/upresearchdata.13312682.v1
title: Women leadership in a patriarchal society

description: The datasets were the transcribed interviews. Semi structured interviews for a qualitative study on women leadership in patriarchal society.
DOI: 10.6084/m9.figshare.6668828
title: Electrical Resistivity Tomography, Time-Domain Electromagnetic and Seismic data from the Pian Grande di Castelluccio basin, epicentral area of the 30 October 2016 Mw 6.5 Norcia earthquake (central Italy)

description: This dataset contains electrical resistivity tomography (ERT), time-domain electromagnetic (TDEM) and passive seismic data we collected on December 2016, March 2017 and June 2017 in the Pian Grande di Castelluccio basin, epicentral area of the 30 October 2016 M<sub>w</sub> 6.5 Norcia earthquake (central Italy). <br>These data represent the core of a research paper by Villani, F., Sapia, V., Baccheschi, P., Civico,R., Di Giulio, G., Vassallo, M., et al. (2019).Geometry and structure of a fault-bounded extensional basin by integrating geophysical surveys and seismic anisotropy across the 30 October 2016 Mw 6.5 earthquake fault(central Italy): The Pian Grande di Castelluccio basin. <i>Tectonics</i>, 38, 26–48.https://doi.org/10.1029/2018TC005205 <br>The dataset is organized into 3 separate compressed folders (.zip format):1) <b>ert_data.zip</b> contains the original raw data (native .bin format of Syscal R2 instrument) of two electrical resistivity profiles T1 and T2, together with absolute elevation of electrodes;2) <b>seismic_data.zip</b> contains several folders, one for each portable seismic station we used (the recordings are in SAC format; location info is reported in a separate txt file);3) <b>tdem_data.zip</b> contains raw TDEM data in .GX7 format. <br>A "Read Me" .txt file is provided in each folder for further details.
DOI: 10.6084/m9.figshare.6668828.v1
title: Electrical Resistivity Tomography, Time-Domain Electromagnetic and Seismic data from the Pian Grande di Castelluccio basin, epicentral area of the 30 October 2016 Mw 6.5 Norcia earthquake (central Italy)

description: This dataset contains electrical resistivity tomography (ERT), time-domain electromagnetic (TDEM) and passive seismic data we collected on December 2016, March 2017 and June 2017 in the Pian Grande di Castelluccio basin, epicentral area of the 30 October 2016 M<sub>w</sub> 6.5 Norcia earthquake (central Italy). Those data represent the core of a research paper by Villani F. et al. submitted to Tectonics (June 2018) and entitled "<i>Geometry and structure of a fault-bounded extensional basin by integrating geophysical surveys and seismic anisotropy across the 30 October 2016 M<sub>w</sub> 6.5 earthquake fault (central Italy): the Pian Grande di Castelluccio basin</i>".<br>The dataset is organized into 3 separate compressed folders (.zip format):1) <b>ert_data.zip</b> contains the original raw data (native .bin format of Syscal R2 instrument) of two electrical resistivity profiles T1 and T2, together with absolute elevation of electrodes;2) <b>seismic_data.zip</b> contains several folders, one for each portable seismic station we used (the recordings are in SAC format; location info is reported in a separate txt file);3) <b>tdem_data.zip</b> contains raw TDEM data in .GX7 format. <br>A "Read Me" .txt file is provided in each folder for further details.
DOI: 10.6084/m9.figshare.13414893.v1
title: Association of dietary and gut microbiota-related metabolites with calcific aortic stenosis

description: Histopathological changes in calcific aortic stenosis (CAS) resemble changes in coronary atherosclerosis. Concerning recent evidence on dietary and gut microbiota-related metabolites representing players in atherosclerosis, we aimed to investigate the link between dietary and gut microbiota-derived metabolites and CAS. We consecutively recruited eligible subjects with moderate-severe CAS (<i>n</i> = 60), aortic sclerosis (ASc) (<i>n</i> = 49) and age and gender-matched control subjects (<i>n</i> = 48) in May 2016-December 2016. Plasma dietary and gut microbiota-related metabolite levels, namely choline, betaine, and trimethylamine N-oxide (TMAO), were measured using ultra-performance liquid chromatography-tandem mass spectroscopy method. Histopathological examinations were performed in patients that underwent aortic valve surgery. Prevalence of traditional cardiovascular risk factors or co-morbidities did not differ among groups (all <i>p</i> &gt; 0.05). CAS patients had higher plasma choline levels compared to both control (<i>p</i> p = 0.006). Plasma betaine and TMAO levels were similar (both <i>p</i> &gt; 0.05). Compared to the lowest quartile choline levels (&lt;11.15 μM), patients with the highest quartile choline levels (≥14.98 μM) had higher aortic valvular (<i>p</i> p = 0.013) calcification scores. Plasma choline levels were independently associated with aortic peak flow velocity (B ± SE:0.165 ± 0.060, <i>p</i> = 0.009). Choline levels were elevated in subjects who had aortic valves with denser lymphocyte infiltration (<i>p</i> p = 0.011), osseous metaplasia (<i>p</i> = 0.004), more severe tissue remodelling (<i>p</i> = 0.002) and calcification (<i>p</i> = 0.002). We found a significant association between choline levels and CAS presence and severity depicted on imaging modalities and histopathological examinations. Our study may open new horizons for prevention of CAS.
DOI: 10.5517/ccdc.csd.cc26w3x4
title: CCDC 2051856: Experimental Crystal Structure Determination

description: Related Article: zhuohao jiao|2020|CSD Communication|||
DOI: 10.48370/ofd/cixmfg
title: Skrzyp zimowy (Equisetum hyemale L.), 9004

description: Herbarium
DOI: 10.6084/m9.figshare.13475193
title: Roaring_model.xlsx

description: Data used to assess the effect of climate on roaring rate of red deer in Doñana National Reserve, accounting for the population density and the opperational sex ratio.
DOI: 10.6084/m9.figshare.13475193.v1
title: Roaring_model.xlsx

description: Data used to assess the effect of climate on roaring rate of red deer in Doñana National Reserve, accounting for the population density and the opperational sex ratio.
DOI: 10.25919/kcya-4485
title: Parkes observations for project P1063 semester 2020APRS_27

description: We propose to use the Parkes UWL receiver for monitoring a small sub-set of the FAST-discovered pulsars, with special properties. The Parkes UWL system provides a unique capability for studying the pulsars over wide bandwidths. The observation proposed will provide significant insight into the special emission properties of these new discoveries and facilitate science.
DOI: 10.6084/m9.figshare.13475310
title: Roaring_model.xlsx

description: Data set used to assess the effect of climate on the roaring rate of red deer in the Doñana Population.
DOI: 10.48370/ofd/hsr8ja/x4omax
title: MRIPAS_coll_1244_LepusEuropaeus_1979_scan.jpg

description: :unav