cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.7792241.v1
title: Amplitude-integrated EEG use in neonatal abstinence syndrome: a pilot study

description: <b>Objective:</b> Though central nervous system irritability is a well-established consequence of neonatal drug withdrawal, brain function in infants with neonatal abstinence syndrome (NAS) is not well understood. Amplitude-integrated electroencephalography (aEEG) is a bedside tool used for monitoring brain activity and seizures. We describe the prevalence of abnormal aEEG background patterns in infants with NAS. <b>Methods:</b> In this pilot, observational study primary outcomes were aEEG findings, Finnegan scores, and length of hospital stay in NAS patients. Subjects underwent an initial aEEG and a repeat study following pharmacologic treatment. Two independent reviewers analyzed aEEGs post discharge. <b>Results:</b> Six out of nine infants had abnormal aEEGs demonstrating lack of sleep-wake cycling (SWC) (50%), discontinuity (41.7%), and low voltage (8.3%). Seizures were not detected. NAS scores were lower for infants with continuous aEEGs versus those whose aEEGs were not continuous (5.83 versus 9.17; <i>p</i> = .054). Length of stay was 7.8 ± 4.4 days in infants with continuous aEEGs versus 26 ± 10.5 days in infants without continuous aEEGs (<i>p</i> = .003). <b>Conclusions:</b> Infants exposed to opioids <i>in utero</i> are at increased risk for discontinuity and abnormal SWC detectable on aEEG. Infants with abnormal aEEGs are more likely to have higher NAS scores, require pharmacologic treatment and have longer lengths of stay.
DOI: 10.5281/zenodo.4020328
title: Deadly dormmate: a case study on Bungarus candidus living among a student dormitory with implications for human safety

description: Movement and observation data gained through radio-telemetry of a single Malayan krait (<em>Bungarus candidus</em>) among a suburban landscape (a university dormitory complex) in NE Thailand. Included: movement spatial data .csv file and photographic evidence of foraging observations, a predation event, conflicts with humans, and camera trap footage. B.candidus_observation_data.csv file column headings: folderID: The Zenodo folder ID containing the photographic evidence of events. obvdate: Date of observation (mm/dd/yyyy) obvtime: Time of observation (24hr) easting_utm: UTM easting (UTM Zone 48N; Datum WGS84) northing_utm: UTM northing (UTM Zone 48N; Datum WGS84) gps_accuracy: Accuracy of GPS location (m) notes: Comments and details on events/observations BUCA28_movement_data.csv file column headings: Datetime: Date and time when the snake was located (mm/dd/yyyy hh:mm) Easting: UTM easting (UTM Zone 48N; Datum WGS84) Northing: UTM northing (UTM Zone 48N; Datum WGS84) Behavior: Either the animal’s behavior observed during the location check (sheltering, foraging, or feeding) or type of other significant locations (capture or release sites) Habitat_Type: Land-use type where the snake was located
description: Research is supported by King Cobra Conservancy. We had ethical approval from the Suranaree University of Technology Ethics Committee, and all work was permitted by the National Research Council of Thailand (0002/27; 0402/4367).
DOI: 10.5517/ccdc.csd.cc2412lw
title: CCDC 1967247: Experimental Crystal Structure Determination

description: Related Article: Hiroto Achira|2019|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc260b1m
title: CCDC 2026099: Experimental Crystal Structure Determination

description: Related Article: W. Clegg, R.A. Coxall|2020|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc260b2n
title: CCDC 2026100: Experimental Crystal Structure Determination

description: Related Article: W. Clegg, S.L. Heath|2020|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc260b3p
title: CCDC 2026101: Experimental Crystal Structure Determination

description: Related Article: W. Clegg, R.A. Coxall|2020|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc260b4q
title: CCDC 2026102: Experimental Crystal Structure Determination

description: Related Article: W. Clegg, A.J. Edwards|2020|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc260b6s
title: CCDC 2026104: Experimental Crystal Structure Determination

description: Related Article: W. Clegg, A.J. Edwards|2020|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc260b7t
title: CCDC 2026105: Experimental Crystal Structure Determination

description: Related Article: W. Clegg, A.J. Edwards|2020|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc260b8v
title: CCDC 2026106: Experimental Crystal Structure Determination

description: Related Article: W. Clegg, A.J. Edwards|2020|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc260b9w
title: CCDC 2026107: Experimental Crystal Structure Determination

description: Related Article: W. Clegg, R.A. Coxall|2020|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc260bcy
title: CCDC 2026109: Experimental Crystal Structure Determination

description: Related Article: Arnold L. Rheingold, Daniel Rabinovich and James A. Golen|2020|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc260bdz
title: CCDC 2026110: Experimental Crystal Structure Determination

description: Related Article: Arnold L. Rheingold, Daniel Rabinovich and James A. Golen|2020|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc260bf0
title: CCDC 2026111: Experimental Crystal Structure Determination

description: Related Article: Arnold L. Rheingold, Daniel Rabinovich and James A. Golen|2020|CSD Communication|||
DOI: 10.5517/ccdc.csd.cc248slt
title: CCDC 1974656: Experimental Crystal Structure Determination

description: Related Article: Zhong-Hong Zhu, Hui-Feng Wang, Shui Yu, Hua-Hong Zou, Hai-Ling Wang, Bing Yin, Fu-Pei Liang|2020|Inorg.Chem.|59|11640|doi:10.1021/acs.inorgchem.0c01496
DOI: 10.5281/zenodo.4021333
title: Ozone changes due to the COVID-19 response

description: Based on the emissions scenarios for the effects of the Covid-19 pandemic and society response (see https://github.com/Priestley-Centre/COVID19_emissions) ozone fields are generated using the OsloCTM3 model. The modelled difference between the scenario and the baseline are added to the ozone scenario files from input4MIPS SSP245 (https://esgf-node.llnl.gov/search/input4mips/). Remark, post 2050 the ozone fields in the scenario files are equal to the input4MIP fields. Funding was provided by the European Union’s Horizon 2020 Research and Innovation Programme under grant agreement nos. 820829 (CONSTRAIN) http://constrain-eu.org/
DOI: 10.6084/m9.figshare.6230444.v1
title: Continuation of the Ross–Delamerian Orogen: insights from eastern Australian detrital-zircon data

description: Information on the Paleozoic tectonic evolution of the Tasmanides in eastern Australia is limited due to the presence of an extensive younger sedimentary cover. Based on the spatio-temporal distribution of deformation and magmatism, the Tasmanides have traditionally been subdivided into five domains (Delamerian, Thomson, Lachlan, Mossman and New England). To test the relationships between these domains, we compiled over 10000 published detrital-zircon ages from basement rocks of the Tasmanides. We split the dataset spatially to test postulated connectivity between domains, and temporally to isolate corresponding age populations that can highlight subtle variations between domains. Results show that the Delamerian and Thomson domains originated as a single orogenic belt that likely received detritus from an early Paleozoic continental-scale drainage system. We also recognise a remarkably similar pattern of Paleoproterozoic and Archean ages in the Delamerian, Thomson and New England domains. This similarity indicates that the late Paleozoic development of the New England domain involved recycling of rocks from the Delamerian–Thomson domain(s). These findings shed new light on the crustal architecture of eastern Australia, and the nature of Paleozoic drainage and sediment recycling in eastern Gondwana.
DOI: 10.6084/m9.figshare.7296407
title: Geochronology and geochemistry of the Devonian Gumbardo Formation (Adavale Basin): evidence for cratonisation of the Central Thomson Orogen by the Early Devonian

description: The Devonian subsurface Adavale Basin occupies a central position in the Paleozoic central Thomson Orogen of eastern Australia and records its tectonic setting during this time interval. Here, we have focussed on the basal volcanics of the Gumbardo Formation to clarify the tectonic setting of the basin. The approach has been to undertake stratigraphic logging, LA-ICP-MS U–Pb zircon geochronology and whole-rock geochemical analysis. The data indicate that basin initiation was rapid occurring at <i>ca</i> 401 Ma. The volcanic rocks are dominated by K-feldspar phyric rhyodacitic ignimbrites. The whole-rock geochemical data indicate little evidence for extensive fractional crystallisation, with the volcanic suite resembling the composition of the upper continental crust and exhibiting transitional I- to A-type tectonomagmatic affinities. One new U–Pb zircon age revealed an Early Ordovician emplacement age for a volcanic rock previously interpreted to be part of the Early Devonian Gumbardo Formation, and older basement age is consistent with seismic interpretations of uplifted basement in this region of the western Adavale Basin. Five ignimbrites dated from different stratigraphic levels within the formation yield similar emplacement ages with a pooled weighted age of 398.2 ± 1.9 Ma (mean square weighted deviation = 0.94, <i>n</i> = 93). Significant zircon inheritance in the volcanic rocks records reworking of Ordovician and Silurian silicic igneous basement from the Thomson Orogen and provides insight into the crustal make-up of the Thomson Orogen. Collectively, the new data presented here suggest the Adavale Basin is a cover-type basin that developed on a stabilised Thomson Orogen after the major Bindian deformation event in the late Silurian.
DOI: 10.6084/m9.figshare.7296407.v1
title: Geochronology and geochemistry of the Devonian Gumbardo Formation (Adavale Basin): evidence for cratonisation of the Central Thomson Orogen by the Early Devonian

description: The Devonian subsurface Adavale Basin occupies a central position in the Paleozoic central Thomson Orogen of eastern Australia and records its tectonic setting during this time interval. Here, we have focussed on the basal volcanics of the Gumbardo Formation to clarify the tectonic setting of the basin. The approach has been to undertake stratigraphic logging, LA-ICP-MS U–Pb zircon geochronology and whole-rock geochemical analysis. The data indicate that basin initiation was rapid occurring at <i>ca</i> 401 Ma. The volcanic rocks are dominated by K-feldspar phyric rhyodacitic ignimbrites. The whole-rock geochemical data indicate little evidence for extensive fractional crystallisation, with the volcanic suite resembling the composition of the upper continental crust and exhibiting transitional I- to A-type tectonomagmatic affinities. One new U–Pb zircon age revealed an Early Ordovician emplacement age for a volcanic rock previously interpreted to be part of the Early Devonian Gumbardo Formation, and older basement age is consistent with seismic interpretations of uplifted basement in this region of the western Adavale Basin. Five ignimbrites dated from different stratigraphic levels within the formation yield similar emplacement ages with a pooled weighted age of 398.2 ± 1.9 Ma (mean square weighted deviation = 0.94, <i>n</i> = 93). Significant zircon inheritance in the volcanic rocks records reworking of Ordovician and Silurian silicic igneous basement from the Thomson Orogen and provides insight into the crustal make-up of the Thomson Orogen. Collectively, the new data presented here suggest the Adavale Basin is a cover-type basin that developed on a stabilised Thomson Orogen after the major Bindian deformation event in the late Silurian.
DOI: 10.6084/m9.figshare.6230444
title: Continuation of the Ross–Delamerian Orogen: insights from eastern Australian detrital-zircon data

description: Information on the Paleozoic tectonic evolution of the Tasmanides in eastern Australia is limited due to the presence of an extensive younger sedimentary cover. Based on the spatio-temporal distribution of deformation and magmatism, the Tasmanides have traditionally been subdivided into five domains (Delamerian, Thomson, Lachlan, Mossman and New England). To test the relationships between these domains, we compiled over 10000 published detrital-zircon ages from basement rocks of the Tasmanides. We split the dataset spatially to test postulated connectivity between domains, and temporally to isolate corresponding age populations that can highlight subtle variations between domains. Results show that the Delamerian and Thomson domains originated as a single orogenic belt that likely received detritus from an early Paleozoic continental-scale drainage system. We also recognise a remarkably similar pattern of Paleoproterozoic and Archean ages in the Delamerian, Thomson and New England domains. This similarity indicates that the late Paleozoic development of the New England domain involved recycling of rocks from the Delamerian–Thomson domain(s). These findings shed new light on the crustal architecture of eastern Australia, and the nature of Paleozoic drainage and sediment recycling in eastern Gondwana.
DOI: 10.6084/m9.figshare.7296392
title: The age and tectonic significance of the Warraweena Volcanics and related rocks, southern Thomson Orogen

description: Magmatic-textured zircon from medium- to high-K calc-alkaline Warraweena Volcanics (WV) in two drill holes have yielded concordant U–Pb dates of 417 ± 3.5 and 414 ± 4.0 Ma and are interpreted as maximum emplacement ages. The Warraweena volcanics were previously considered to be either Neoproterozoic or Macquarie arc equivalents. Whole-rock εNd<sub>t</sub> values of these volcanics are +4.5 and +4.8. Along strike of the drill holes, Devonian zircon U–Pb ages (411 ± 5.5 Ma) were obtained from coherent S-type rhyolite flows that have highly negative εNd<sub>t</sub> values (–7.9 and –7.8). These are a component of the Oxley volcanics. The ages of the Warraweena and Oxley volcanics are identical within uncertainty. The Oxley volcanics (OV) are interbedded with predominantly fine- to medium-grained metasedimentary and so imply a Lower Devonian deposition age for these host rocks. Based on their geophysical characteristics, the metasediments are widely distributed. These metasedimentary rocks yield a wide range of maximum depositional ages, from Early Devonian to earliest Ordovician–latest Cambrian, similar to the Cobar Basin. The absence of complex fabric development typical of Ordovician supracrustal rocks in the region, and conformity with the OV where observable suggest the widespread sedimentation was synchronous with rift-related volcanism in the Early Devonian. Regionally, the WV is temporally, geochemically and isotopically (εNd values) similar to the calc-alkaline Louth Volcanics located over 100 km to the southwest of the WV. Louth Volcanics define a complexly folded belt in geophysical data. Other potentially correlative Early Devonian igneous rocks occur in the nearby Cobar Superbasin and elsewhere in the eastern Lachlan Orogen and are considered to represent the products of a post-orogenic, nascent continental back-arc rift system.
DOI: 10.6084/m9.figshare.6276215
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
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.7296392.v2
title: The age and tectonic significance of the Warraweena Volcanics and related rocks, southern Thomson Orogen

description: Magmatic-textured zircon from medium- to high-K calc-alkaline Warraweena Volcanics (WV) in two drill holes have yielded concordant U–Pb dates of 417 ± 3.5 and 414 ± 4.0 Ma and are interpreted as maximum emplacement ages. The Warraweena volcanics were previously considered to be either Neoproterozoic or Macquarie arc equivalents. Whole-rock εNd<sub>t</sub> values of these volcanics are +4.5 and +4.8. Along strike of the drill holes, Devonian zircon U–Pb ages (411 ± 5.5 Ma) were obtained from coherent S-type rhyolite flows that have highly negative εNd<sub>t</sub> values (–7.9 and –7.8). These are a component of the Oxley volcanics. The ages of the Warraweena and Oxley volcanics are identical within uncertainty. The Oxley volcanics (OV) are interbedded with predominantly fine- to medium-grained metasedimentary and so imply a Lower Devonian deposition age for these host rocks. Based on their geophysical characteristics, the metasediments are widely distributed. These metasedimentary rocks yield a wide range of maximum depositional ages, from Early Devonian to earliest Ordovician–latest Cambrian, similar to the Cobar Basin. The absence of complex fabric development typical of Ordovician supracrustal rocks in the region, and conformity with the OV where observable suggest the widespread sedimentation was synchronous with rift-related volcanism in the Early Devonian. Regionally, the WV is temporally, geochemically and isotopically (εNd values) similar to the calc-alkaline Louth Volcanics located over 100 km to the southwest of the WV. Louth Volcanics define a complexly folded belt in geophysical data. Other potentially correlative Early Devonian igneous rocks occur in the nearby Cobar Superbasin and elsewhere in the eastern Lachlan Orogen and are considered to represent the products of a post-orogenic, nascent continental back-arc rift system.
DOI: 10.6084/m9.figshare.6264896
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.