cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.7188005
title: Depositional age and provenance of the Cobar Supergroup

description: The turbidite-filled, Lower Devonian Cobar Basin is characterised through a detrital zircon study. Uranium–Pb age data for six samples were combined with published data to show the basin has a unique age spectrum characterised by a subordinate Middle Ordovician (<i>ca</i> 470 Ma) peak superimposed on a dominant <i>ca</i> 500 Ma peak. Maximum depositional ages for 3 samples were <i>ca</i> 425 Ma, close to the published Lower Devonian (Lochkovian 419–411 Ma) biostratigraphic ages. A minor <i>ca</i> 1000 Ma zircon population was also identified. The major source of the 500 Ma zircons was probably the local Ordovician metasedimentary basement, which was folded, thickened and presumably exposed during the <i>ca</i> 440 Ma Benambran Orogeny. The <i>ca</i> 470 Ma age peak reflects derivation from Middle Ordovician (Phase 2) rocks of the Macquarie Arc to the east. The I-type Florida Volcanics, located ∼50 km eastward from the Cobar Basin, contains distinctive Middle and Late Ordovician zircon populations, considered to be derived from deeply underthrust Macquarie Arc crust. Protracted silicic magmatism occurred before, during and after Cobar Basin deposition, indicating that the basin formed by subduction-related processes in a back-arc setting, rather than as a continental rift.
DOI: 10.6084/m9.figshare.6264896.v1
title: Mid- to lower-crustal architecture of the northern Lachlan and southern Thomson orogens: evidence from O–Hf isotopes

description: The nature of the substrate below the northern Lachlan Orogen and the southern Thomson Orogen is poorly understood. We investigate the nature of the mid- to lower-crust using O and Lu–Hf isotope analyses of zircons from magmatic rocks that intrude these regions, and focus on the 440–410 Ma time window to minimise temporal effects while focussing on spatial differences. Over the entire region, weighted mean δ<sup>18</sup>O values range from 5.5 to 9.8‰ (relative to VSMOW, Vienna Standard Mean Oceanic Water), and weighted mean ϵHf<sub>t</sub> range from −8.8 to +8.5. In the northern Lachlan Orogen and much of the southern Thomson Orogen, magmatic rocks with unradiogenic ϵHf<sub>t</sub> (∼−7 to −4) and elevated δ<sup>18</sup>O values (∼9 to 10‰) reflect a supracrustal source component that may be common to both orogens. Magmatic rocks intruding the Warratta Group in the western part of the Thomson Orogen also have unradiogenic ϵHf<sub>t</sub> (∼−9 to −6) but more subdued δ<sup>18</sup>O values (∼7‰), indicating a distinct supracrustal source component in this region. Some regions record radiogenic ϵHf and mantle-like δ<sup>18</sup>O values, indicative of either a contribution from arc-derived rocks or a direct mantle input. In the northeast Lachlan Orogen Hermidale Terrane, magmatic rocks record mixing of the supracrustal source component with input from a infracrustal or mantle source component (ϵHf<sub>t</sub> as high as +8.5, δ<sup>18</sup>O values as low as 5.5‰), possibly of Macquarie Arc affinity. Samples in the west-southwestern Thomson Orogen also record some evidence of radiogenic input (ϵHf<sub>t</sub> as high as −0.5, δ<sup>18</sup>O values as low as 6.4‰), possibly from the Mount Wright Arc of the Koonenberry Belt. Overall, our results demonstrate a strong spatial control on isotopic compositions. We find no isotopic differences between the bulk of the Lachlan Orogen and the bulk of the Thomson Orogen, and some indication of similarities between the two.
DOI: 10.6084/m9.figshare.7188005.v1
title: Depositional age and provenance of the Cobar Supergroup

description: The turbidite-filled, Lower Devonian Cobar Basin is characterised through a detrital zircon study. Uranium–Pb age data for six samples were combined with published data to show the basin has a unique age spectrum characterised by a subordinate Middle Ordovician (<i>ca</i> 470 Ma) peak superimposed on a dominant <i>ca</i> 500 Ma peak. Maximum depositional ages for 3 samples were <i>ca</i> 425 Ma, close to the published Lower Devonian (Lochkovian 419–411 Ma) biostratigraphic ages. A minor <i>ca</i> 1000 Ma zircon population was also identified. The major source of the 500 Ma zircons was probably the local Ordovician metasedimentary basement, which was folded, thickened and presumably exposed during the <i>ca</i> 440 Ma Benambran Orogeny. The <i>ca</i> 470 Ma age peak reflects derivation from Middle Ordovician (Phase 2) rocks of the Macquarie Arc to the east. The I-type Florida Volcanics, located ∼50 km eastward from the Cobar Basin, contains distinctive Middle and Late Ordovician zircon populations, considered to be derived from deeply underthrust Macquarie Arc crust. Protracted silicic magmatism occurred before, during and after Cobar Basin deposition, indicating that the basin formed by subduction-related processes in a back-arc setting, rather than as a continental rift.
DOI: 10.6084/m9.figshare.6276215.v1
title: Crustal and thermal structure of the Thomson Orogen: constraints from the geochemistry, zircon U–Pb age, and Hf and O isotopes of subsurface granitic rocks

description: The origin of elevated geothermal gradients in the subsurface Thomson Orogen and the nature of the crustal basement beneath it, whether oceanic or continental, remain enigmatic. Previous studies have demonstrated that a higher crustal radiogenic input is required to explain these anomalous thermal gradients. In this study, we have investigated the nature and age of this crustal input by undertaking geochemical, geochronological and Hf and O isotope analyses of buried granitic rocks as well as evaluating the heat-producing potential of metasedimentary rocks. The mineralogy, composition and Neoproterozoic/Cambrian to Devonian age of the low to moderate heat-producing I- and S-type granitic rocks strongly contrast with the Carboniferous A-type high-heat-producing granites of the Big Lake Suite, which have been suggested to be an important contributor to the elevated geothermal gradients, near the southwest corner of the Thomson Orogen. These differences suggest the Big Lake Suite rocks do not extend into the Queensland part of the temperature anomaly. Heat production of the metasedimentary rocks is also low to moderate. Based on Hf isotope compositions of zircons characterised by mantle-like oxygen signature (ϵ<sub>Hf</sub><sub>(t)</sub> = –12 to +2), we propose the temperature anomaly results from the occurrence of Mesoproterozoic and/or Paleoproterozoic high-heat-producing rocks beneath the Thomson Orogen. Precambrian crust, therefore, lies well east of the Tasman line. The results do not support a Neoproterozoic to Cambrian oceanic crust, as previously suggested, but instead point to a continental substrate for the Thomson Orogen. Hf isotopes indicate an overall trend towards more isotopically juvenile compositions with a progressive reduction in the contribution of older crustal sources to granitic magmas towards the present time. Different Hf isotopic signatures for the Lachlan (ϵ<sub>Hf</sub><sub>(t)</sub> = –13 to +15), Thomson (ϵ<sub>Hf</sub><sub>(t)</sub> = –14 to +5) and Delamerian (ϵ<sub>Hf</sub><sub>(t)</sub> = –7 to +4) orogens highlight lateral variations in the age structures of crustal basement beneath these orogens.
DOI: 10.6084/m9.figshare.6283085.v2
title: Basement geology of the southern Thomson Orogen

description: The diverse geological and geophysical data sets compiled, interrogated and interpreted for the largely undercover southern Thomson Orogen region reveal a Paleozoic terrane dominated by deformed metasedimentary rocks intruded by S- and I-type granites. An interpretive basement geology map and synthesis of geochronological constraints allow definition of several stratigraphic packages. The oldest and most widespread comprises upper Cambrian to Lower Ordovician metasedimentary rocks deposited during the vast extensional Larapinta Event with maximum depositional ages of <i>ca</i> 520 to <i>ca</i> 496 Ma. These units correlate with elements of the northern Thomson Orogen, Warburton Basin and Amadeus Basin. The degree of deformation and metamorphism of these rocks varies across the region. A second major package includes Lower to Middle Devonian volcanic and sedimentary units, some of which correlate with components of the Lachlan Orogen. The region also includes a Middle to Upper Ordovician package of metasedimentary rocks and a Devonian or younger package of intermediate volcaniclastic rocks of restricted extent. Intrusive units range from diatremes and relatively small layered mafic bodies to batholithic-scale suites of granite and granodiorite. S-type and I-type intrusions are both present, and ages range from Ordovician to Triassic, but late Silurian intrusions are the most abundant. Two broad belts of intrusions are recognised. In the east, the Scalby Belt comprises relatively young (Upper Devonian) intrusions, while in the west, the Ella Belt is dominated by intrusions of late Silurian age within a curvilinear, broadly east–west trend. The stratigraphic distributions, characteristics and constraints defined by this interpretive basement mapping provide a basic framework for ongoing research and mineral exploration.
DOI: 10.6084/m9.figshare.12936279
title: Insights into the evolution of the Thomson Orogen from geochronology, geochemistry, and zircon isotopic studies of magmatic rocks

description: Zircon U–Pb ages, εHf(t), and δ<sup>18</sup>O isotopic data together with geochemistry and limited Sm–Nd results from magmatic rocks sampled in deep-basement drill cores from undercover parts of the Thomson Orogen provide strong temporal links with outcropping regions of the orogen and important clues to its evolution and relationship with the Lachlan Orogen. SHRIMP U–Pb zircon ages show that magmatism of Early Ordovician age is widespread across the central, undercover regions of the Thomson Orogen and occurred in a narrow time-window between 480 and 470 Ma. These rocks have evolved εHf(t)<sub>zrn</sub> (−12.18 to −6.26) and εNd (−11.3 to −7.1), and supracrustal δ<sup>18</sup>O<sub>zrn</sub> (7.01–8.50‰), which is in stark contrast to Early Ordovician magmatic rocks in the Lachlan Orogen that are isotopically juvenile. Two samples have late Silurian ages (425–420 Ma), and four have Devonian ages (408–382 Ma). The late Silurian rocks have evolved εHf(t)<sub>zrn</sub> (−6.42 to −4.62) and supracrustal δ<sup>18</sup>O<sub>zrn</sub> (9.26–10.29‰) values, while the younger Devonian rocks show a shift toward more juvenile εHf(t)<sub>zrn</sub>, a trend that is also seen in rocks of this age in the Lachlan Orogen. Interestingly, two early Late Devonian samples have juvenile εHf(t)<sub>zrn</sub> (0.01–1.92) but supracrustal δ<sup>18</sup>O<sub>zrn</sub> (7.45–8.77‰) indicating rapid recycling of juvenile material. Two distinct Hf–O isotopic mixing trends are observed for magmatic rocks of the Thomson Orogen. One trend appears to have incorporated a more evolved supracrustal component and is defined by samples from the northern two-thirds of the Thomson Orogen, while the other trend is generally less evolved and from samples in the southern third of the Thomson Orogen and matches the isotopic character of rocks from the Lachlan Orogen. The spatial association of the Early Ordovician magmatism with the more evolved metasedimentary signature suggests that at least the northern part of the Thomson Orogen is underlain by older pre-Delamerian metasedimentary rocks.
DOI: 10.6084/m9.figshare.12936279.v1
title: Insights into the evolution of the Thomson Orogen from geochronology, geochemistry, and zircon isotopic studies of magmatic rocks

description: Zircon U–Pb ages, εHf(t), and δ<sup>18</sup>O isotopic data together with geochemistry and limited Sm–Nd results from magmatic rocks sampled in deep-basement drill cores from undercover parts of the Thomson Orogen provide strong temporal links with outcropping regions of the orogen and important clues to its evolution and relationship with the Lachlan Orogen. SHRIMP U–Pb zircon ages show that magmatism of Early Ordovician age is widespread across the central, undercover regions of the Thomson Orogen and occurred in a narrow time-window between 480 and 470 Ma. These rocks have evolved εHf(t)<sub>zrn</sub> (−12.18 to −6.26) and εNd (−11.3 to −7.1), and supracrustal δ<sup>18</sup>O<sub>zrn</sub> (7.01–8.50‰), which is in stark contrast to Early Ordovician magmatic rocks in the Lachlan Orogen that are isotopically juvenile. Two samples have late Silurian ages (425–420 Ma), and four have Devonian ages (408–382 Ma). The late Silurian rocks have evolved εHf(t)<sub>zrn</sub> (−6.42 to −4.62) and supracrustal δ<sup>18</sup>O<sub>zrn</sub> (9.26–10.29‰) values, while the younger Devonian rocks show a shift toward more juvenile εHf(t)<sub>zrn</sub>, a trend that is also seen in rocks of this age in the Lachlan Orogen. Interestingly, two early Late Devonian samples have juvenile εHf(t)<sub>zrn</sub> (0.01–1.92) but supracrustal δ<sup>18</sup>O<sub>zrn</sub> (7.45–8.77‰) indicating rapid recycling of juvenile material. Two distinct Hf–O isotopic mixing trends are observed for magmatic rocks of the Thomson Orogen. One trend appears to have incorporated a more evolved supracrustal component and is defined by samples from the northern two-thirds of the Thomson Orogen, while the other trend is generally less evolved and from samples in the southern third of the Thomson Orogen and matches the isotopic character of rocks from the Lachlan Orogen. The spatial association of the Early Ordovician magmatism with the more evolved metasedimentary signature suggests that at least the northern part of the Thomson Orogen is underlain by older pre-Delamerian metasedimentary rocks.
DOI: 10.6084/m9.figshare.6283085.v1
title: Basement geology of the southern Thomson Orogen

description: The diverse geological and geophysical data sets compiled, interrogated and interpreted for the largely undercover southern Thomson Orogen region reveal a Paleozoic terrane dominated by deformed metasedimentary rocks intruded by S- and I-type granites. An interpretive basement geology map and synthesis of geochronological constraints allow definition of several stratigraphic packages. The oldest and most widespread comprises upper Cambrian to Lower Ordovician metasedimentary rocks deposited during the vast extensional Larapinta Event with maximum depositional ages of <i>ca</i> 520 to <i>ca</i> 496 Ma. These units correlate with elements of the northern Thomson Orogen, Warburton Basin and Amadeus Basin. The degree of deformation and metamorphism of these rocks varies across the region. A second major package includes Lower to Middle Devonian volcanic and sedimentary units, some of which correlate with components of the Lachlan Orogen. The region also includes a Middle to Upper Ordovician package of metasedimentary rocks and a Devonian or younger package of intermediate volcaniclastic rocks of restricted extent. Intrusive units range from diatremes and relatively small layered mafic bodies to batholithic-scale suites of granite and granodiorite. S-type and I-type intrusions are both present, and ages range from Ordovician to Triassic, but late Silurian intrusions are the most abundant. Two broad belts of intrusions are recognised. In the east, the Scalby Belt comprises relatively young (Upper Devonian) intrusions, while in the west, the Ella Belt is dominated by intrusions of late Silurian age within a curvilinear, broadly east–west trend. The stratigraphic distributions, characteristics and constraints defined by this interpretive basement mapping provide a basic framework for ongoing research and mineral exploration.
DOI: 10.18157/qogoecdjan20
title: QoG OECD Dataset 2020
DOI: 10.6084/m9.figshare.12936386.v1
title: Additional file 4 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 4.
DOI: 10.6084/m9.figshare.12936383
title: Additional file 3 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 3.
DOI: 10.6084/m9.figshare.12936383.v1
title: Additional file 3 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 3.
DOI: 10.6084/m9.figshare.12936389
title: Additional file 5 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 5.
DOI: 10.6084/m9.figshare.12936395
title: Additional file 7 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 7.
DOI: 10.6084/m9.figshare.12936395.v1
title: Additional file 7 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 7.
DOI: 10.6084/m9.figshare.12936398
title: Additional file 8 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 8.
DOI: 10.6084/m9.figshare.12936389.v1
title: Additional file 5 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 5.
DOI: 10.6084/m9.figshare.12936386
title: Additional file 4 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 4.
DOI: 10.6084/m9.figshare.12936401
title: Additional file 9 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 9.
DOI: 10.6084/m9.figshare.12936381
title: Additional file 11 of Impact of industrial production system parameters on chicken microbiomes: mechanisms to improve performance and reduce Campylobacter

description: Additional file 11: Supplementary S11-Pairwise Differential Analysis.xlsx: Differential analysis of genera that are up/down-regulated between different groups (Adjusted P values ≤0.05) with at least log2 fold change from the base mean abundances for the samples considered in the first column.
DOI: 10.6084/m9.figshare.12936401.v1
title: Additional file 9 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 9.
DOI: 10.6084/m9.figshare.12936392.v1
title: Additional file 6 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 6.
DOI: 10.6084/m9.figshare.12936381.v1
title: Additional file 11 of Impact of industrial production system parameters on chicken microbiomes: mechanisms to improve performance and reduce Campylobacter

description: Additional file 11: Supplementary S11-Pairwise Differential Analysis.xlsx: Differential analysis of genera that are up/down-regulated between different groups (Adjusted P values ≤0.05) with at least log2 fold change from the base mean abundances for the samples considered in the first column.
DOI: 10.6084/m9.figshare.12936392
title: Additional file 6 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 6.
DOI: 10.6084/m9.figshare.12936398.v1
title: Additional file 8 of A novel mouse model expressing human forms for complement receptors CR1 and CR2

description: Additional file 8.
DOI: 10.6084/m9.figshare.12936417.v1
title: Additional file 1 of Detection of deep low-frequency earthquakes in the Nankai subduction zone over 11 years using a matched filter technique

description: Additional file 1. Table of catalog of the template LFEs. Date (Year, Month, Day, Hour, Minute, Second), Latitude, Longitude, Depth and Magnitude.
DOI: 10.6084/m9.figshare.12936417
title: Additional file 1 of Detection of deep low-frequency earthquakes in the Nankai subduction zone over 11 years using a matched filter technique

description: Additional file 1. Table of catalog of the template LFEs. Date (Year, Month, Day, Hour, Minute, Second), Latitude, Longitude, Depth and Magnitude.
DOI: 10.6084/m9.figshare.12936420.v1
title: Additional file 2 of Detection of deep low-frequency earthquakes in the Nankai subduction zone over 11 years using a matched filter technique

description: Additional file 2. Table of catalog of the detected LFEs. Date (Year, Month, Day, Hour, Minute, Second), Latitude, Longitude, Depth and Magnitude.
DOI: 10.6084/m9.figshare.12936420
title: Additional file 2 of Detection of deep low-frequency earthquakes in the Nankai subduction zone over 11 years using a matched filter technique

description: Additional file 2. Table of catalog of the detected LFEs. Date (Year, Month, Day, Hour, Minute, Second), Latitude, Longitude, Depth and Magnitude.
DOI: 10.6084/m9.figshare.12936491
title: Gene database of Paraburkholderia xenovorans LB400

description: <i>Paraburkholderia xenovorans</i> is an aerobic polychlorinated biphenyl degrader which serves an important role as model organism for bioremediation studies. Known to have the largest bacterial genome to date at 9.7 Mb, much remains to be understood of this unique prokaryotic organism which has three distinct chromosomes in its cells. This work sought to provide fundamental information about the genetic repertoire of <i>P. xenovorans</i> LB400 by parsing its annotated genome sequence downloaded from Genbank. Comprising gene name, gene function, and gene sequence, the resource should be useful for functional genomics study seeking to decipher novel functions from genes in the organism or in molecular cloning work seeking to exploit aromatics degrading capability of the organism through heterologous expression in other microbial chassis such as <i>Escherichia coli</i>.
DOI: 10.14284/419
title: Sedimentary and plant carbon, nitrogen and phosphorus measurements of Blakeney salt marsh ponds

description: Carbon, nitrogen and phosphorus concentrations of plant material and pond sediments collected at Blakeney salt marsh, North Norfolk (UK).
description: Carbon, nitrogen and phosphorus concentrations of plant material and pond sediments collected at three seperate visits to Blakeney salt marsh, North Norfolk (UK). In October 2015 and August 2016, 2 replicate cores were collected from one pond with benthic fauna and one pond without benthic fauna. Organic carbon and total nitrogen measurements, as well as sequential phosphorus extractions ('SEDEX') were performed on these pond sediments. In August 2018, 4 ponds with benthic fauna and 4 ponds without benthic fauna (2 replicates each) were sampled. Organic carbon, total nitrogen, total and inorganic phosphorus measurements were performed on these sediments. Plant material was collected in August 2018 and analyzed for total carbon, nitrogen and phosphorus contents.
DOI: 10.6084/m9.figshare.12815585
title: Metadata record for: PPDIST: global 0.1° daily and 3-hourly precipitation probability distribution climatologies for 1979–2018

description: This dataset contains key characteristics about the data described in the Data Descriptor PPDIST: global 0.1° daily and 3-hourly precipitation probability distribution climatologies for 1979–2018. <br> Contents: <br> 1. human readable metadata summary table in CSV format 2. machine readable metadata file in JSON format <br> <br> <br>
DOI: 10.6084/m9.figshare.12815585.v1
title: Metadata record for: PPDIST: global 0.1° daily and 3-hourly precipitation probability distribution climatologies for 1979–2018

description: This dataset contains key characteristics about the data described in the Data Descriptor PPDIST: global 0.1° daily and 3-hourly precipitation probability distribution climatologies for 1979–2018. <br> Contents: <br> 1. human readable metadata summary table in CSV format 2. machine readable metadata file in JSON format <br> <br> <br>