cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.21908184
title: Supplementary Material for: Discharge Age and Weight for Very Preterm Infants in Six Countries: 2012–2020

description: <b><i>Background:</i></b> Postmenstrual age for surviving infants without congenital anomalies born at 24–29 weeks’ gestational age from 2005 to 2018 in the USA increased 8 days, discharge weight increased 316 grams, and median discharge weight z-score increased 0.19 standard units. We asked whether increases were observed in other countries. <b><i>Methods:</i></b> We evaluated postmenstrual age, weight, and weight z-score at discharge of surviving infants without congenital anomalies born at 24–29 weeks’ gestational age admitted to Vermont Oxford Network member hospitals in Austria, Ireland, Italy, Switzerland, the UK, and the USA from 2012 to 2020. <b><i>Results:</i></b> After adjustment, the median postmenstrual age at discharge increased significantly in Austria (3.6 days, 99% CI [1.0, 6.3]), Italy (4.0 days [2.3, 5.6]), and the USA (5.4 days [5.0, 5.8]). Median discharge weight increased significantly in Austria (181 grams, 99% CI [95, 267]), Ireland (234 [143, 325]), Italy (133 [83, 182]), and the USA (207 [194, 220]). Median discharge weight z-score increased in Ireland (0.24 standard units, 99% CI [0.12, 0.36]) and the USA (0.15 [0.13, 0.16]). Discharge on human milk increased in Italy, Switzerland, and the UK, while going home on cardiorespiratory monitors decreased in Austria, Ireland, and USA and going home on oxygen decreased in Ireland. <b><i>Conclusions:</i></b> In this international cohort of neonatal intensive care units, postmenstrual discharge age and weight increased in some, but not all, countries. Processes of care at discharge did not change in conjunction with age and weight increases.
DOI: 10.6084/m9.figshare.21908187.v1
title: Supplementary Material for: Examination on Factors Affecting Symptom Change after Drug Withdrawal in Patients with Mild Erosive Gastroesophageal Reflux Disease Undergoing Symptom-Controlled Maintenance Therapy with Acid-Secretion Inhibition Drugs

description: <b><i>Introduction:</i></b> In patients with gastroesophageal reflux disease (GERD) on maintenance therapy with acid-suppressive drugs, it is not clear what background factors allow patients to discontinue the drugs. The aims of this study were to examine the relationship of the changes in the frequency and severity of gastrointestinal symptoms after discontinuation of acid-secretion inhibitors for erosive GERD (eGERD) with possible patient background factors and to identify factors that influence these changes. <b><i>Methods:</i></b> This is a multicenter, open-label, interventional, exploratory study. eGERD patients with mild mucosal injury whose symptoms were under control and who were on maintenance therapy with acid-suppressive drugs were withdrawn from the drug treatment for 4 weeks. We examined the relationship of patient backgrounds (sex, age, body mass index, alcohol consumption, smoking habits), esophageal hiatal hernia, <i>Helicobacter pylori</i> infection, pepsinogen I and II concentrations and I/II ratios, blood gastrin levels before and after drug discontinuation with total score change in Frequency Scale for the Symptoms of GERD (FSSG). <b><i>Results:</i></b> Of the 92 patients whose symptoms could be assessed before and after drug withdrawal, 66 patients (71.7% of the total) had FSSG &lt;8 and no symptom relapse after the withdrawal. Furthermore, patient background factors that may be related to symptom relapse/non-relapse were examined, but no related factors were detected. The maintenance medications before discontinuation in the above 92 patients were a proton pump inhibitor (PPI) and vonoprazan (VPZ, a potassium ion competitive acid blocker). Since PPI and VPZ were administered to about the same number of patients, though incidentally, we additionally examined the relationship between patient background factors and symptom relapse/non-relapse by treatment group. As a result, no relevant background factors were detected in both groups. Although there were no significant differences between the two groups, the severity and frequency of symptom recurrence in the VPZ group tended to be higher than in the PPI group. <b><i>Conclusions:</i></b> Consideration of background factors is unlikely to be required in the discontinuation of maintenance therapy for eGERD. There was no significant difference in the extent of disease or frequency of recurrence during the discontinuation period, regardless of whether the drug before discontinuation was a PPI or VPZ.
DOI: 10.5281/zenodo.7382604
title: Dataset for "A proposed SHCE feature selection method for estimating forest aboveground biomass from multiple satellite data"

description: The data are associated with a submitted manuscript.
DOI: 10.5281/zenodo.7382603
title: Dataset for "A proposed SHCE feature selection method for estimating forest aboveground biomass from multiple satellite data"

description: The data are associated with a submitted manuscript.
DOI: 10.25405/data.ncl.21896055.v1
title: Vallum notebook by Brenda Swinbank

description: The collection consists of a series of scans (produced as pdfs) of the fieldwork notebook of Brenda Heywood (nee Swinbank) that she compiled for her doctoral research on the Vallum of Hadrian's Wall during the course of walking the Wall in May and June of 1950. <br> The notebook provides direct testimony of conditions observable on the ground, along with interpretation. <br> Notes are presented from east to west, with the left margin indicating identifiable sites along the course of the Wall. <br> The notebook was given to Prof. David Breeze by Brenda, and scanned at David's request and with permission.
DOI: 10.25405/data.ncl.21896055
title: Vallum notebook by Brenda Swinbank

description: The collection consists of a series of scans (produced as pdfs) of the fieldwork notebook of Brenda Heywood (nee Swinbank) that she compiled for her doctoral research on the Vallum of Hadrian's Wall during the course of walking the Wall in May and June of 1950. <br> The notebook provides direct testimony of conditions observable on the ground, along with interpretation. <br> Notes are presented from east to west, with the left margin indicating identifiable sites along the course of the Wall. <br> The notebook was given to Prof. David Breeze by Brenda, and scanned at David's request and with permission.
DOI: 10.17031/63c67400b4e58
title: Phytoplankton data from the CPR Survey during the months of Sept,Oct,Nov 2014 - 2018

description: Excel file containing CPR data from the North Atlantic between 2014 and 2020, sample level data (each sample being 1 row, equating to approx. 10 nautical miles of tow, 3m3 of filtered seawater). There are two excel sheets, the first contains the taxa abundance counts, the second contains the taxa names. For each taxa, values indicate abundance (according to standard CPR methodology, see Richardson et al. 2006, Prog in Oceanog 68. 27-74), zero values are absence of taxon, empty cells are when the taxon was not looked for. The excel file consists of samples in rows, with the following information in columns - A: midpoint of sample date and time gmt B: midpoint of sample latitude in decimal degrees C: midpoint of sample longitude in decimal degrees D:chlorophyll index E-onwards:taxa.
DOI: 10.5281/zenodo.4626110
title: A Global Epidemics Dataset (1500-2020)

description: This is a Global Epidemics Dataset analyzed in: Marani, M. , G. Katul, W.H. Pan, A. Parolari, Intensity and frequency of extreme novel epidemics, 2021 The upload includes a revised code that corrects an error and produces revised estimates of the probability of occurrence of global epidemics in the present and in the future.
DOI: 10.5281/zenodo.4626111
title: A Global Epidemics Dataset (1500-2020)

description: This is a Global Epidemics Dataset analyzed in: Marani, M. , G. Katul, W.H. Pan, A. Parolari, Intensity and frequency of extreme novel epidemics, 2021
DOI: 10.5281/zenodo.7543747
title: A Global Epidemics Dataset (1500-2020)

description: This is a Global Epidemics Dataset analyzed in: Marani, M. , G. Katul, W.H. Pan, A. Parolari, Intensity and frequency of extreme novel epidemics, 2021 The upload includes a revised code that corrects an error and produces revised estimates of the probability of occurrence of global epidemics in the present and in the future.
DOI: 10.6084/m9.figshare.19369307
title: U-Pb age of a late Cenozoic ultra-high temperature metamorphic event under Central Mexico, as inferred from granulite xenoliths from Cerro El Toro, Mexico

description: Cerro El Toro, a Pliocene scoria cone that carried abundant lower crust xenoliths to the surface, is located in the Mesa Central (MC), Mexico, where mafic alkalic intra-plate volcanism has occurred since the early Miocene (end of the Sierra Madre Occidental volcanism). Early studies of El Toro xenoliths showed that the feldspathic granulite equilibrated at P = 0.9–1.4 GPa and T = 900−1100°C under anhydrous conditions (ternary feldspars calculations). A young (Oligocene-Quaternary?) pulse of ultra-high temperature (UHT) metamorphism was thus proposed for the region, without a strict age constrain. Zircon crystals recovered from a set of nine xenoliths (7 Grt-Sil bearing metapelites, a Px-bearing meta-quartz diorite, and a Grt-Opx bearing orthogneiss) were selected for LA-(MC)-ICPMS U-Pb geochronology. Palaeozoic to Neoproterozoic zircon crystals are scant, whereas Mesozoic to Cenozoic ages are more abundant. Based on their chondrite-normalized REEs all Neoproterozoic to Mesozoic zircons are interpreted as igneous, whereas those of late Oligocene to late Miocene age (ca. 27–6 Ma) are mostly metamorphic and grew during a protracted pulse of UHT metamorphism in the lower crust. The presence of Cenozoic metasediments in the lower crust under Cerro El Toro is indicative of the action of the subducted Farallon plate, coupled with tectonic erosion of continentally derived sediments, either from a forearc basin and/or an accretionary prism that were relaminated to the lower crust by sediment diapirism. Similarities among the xenolith zircon ages with those from modern sediments belonging to Central Mexico Pacific coast point towards a NW-SE 100 km long coast stretch across Zihuatanejo as a possible sediment source. The paucity of Grenville-age detrital zircon grains in the recovered xenoliths suggests that the El Toro area is not underlain by a Proterozoic basement, thus implying a substantial reduction of Oaxaquia extension beneath Central Mexico and presence of the younger Guerrero terrane.
DOI: 10.6084/m9.figshare.19369307.v1
title: U-Pb age of a late Cenozoic ultra-high temperature metamorphic event under Central Mexico, as inferred from granulite xenoliths from Cerro El Toro, Mexico

description: Cerro El Toro, a Pliocene scoria cone that carried abundant lower crust xenoliths to the surface, is located in the Mesa Central (MC), Mexico, where mafic alkalic intra-plate volcanism has occurred since the early Miocene (end of the Sierra Madre Occidental volcanism). Early studies of El Toro xenoliths showed that the feldspathic granulite equilibrated at P = 0.9–1.4 GPa and T = 900−1100°C under anhydrous conditions (ternary feldspars calculations). A young (Oligocene-Quaternary?) pulse of ultra-high temperature (UHT) metamorphism was thus proposed for the region, without a strict age constrain. Zircon crystals recovered from a set of nine xenoliths (7 Grt-Sil bearing metapelites, a Px-bearing meta-quartz diorite, and a Grt-Opx bearing orthogneiss) were selected for LA-(MC)-ICPMS U-Pb geochronology. Palaeozoic to Neoproterozoic zircon crystals are scant, whereas Mesozoic to Cenozoic ages are more abundant. Based on their chondrite-normalized REEs all Neoproterozoic to Mesozoic zircons are interpreted as igneous, whereas those of late Oligocene to late Miocene age (ca. 27–6 Ma) are mostly metamorphic and grew during a protracted pulse of UHT metamorphism in the lower crust. The presence of Cenozoic metasediments in the lower crust under Cerro El Toro is indicative of the action of the subducted Farallon plate, coupled with tectonic erosion of continentally derived sediments, either from a forearc basin and/or an accretionary prism that were relaminated to the lower crust by sediment diapirism. Similarities among the xenolith zircon ages with those from modern sediments belonging to Central Mexico Pacific coast point towards a NW-SE 100 km long coast stretch across Zihuatanejo as a possible sediment source. The paucity of Grenville-age detrital zircon grains in the recovered xenoliths suggests that the El Toro area is not underlain by a Proterozoic basement, thus implying a substantial reduction of Oaxaquia extension beneath Central Mexico and presence of the younger Guerrero terrane.
DOI: 10.6084/m9.figshare.19329032
title: The nature of the sub-continental lithospheric mantle beneath Thailand: evidence from xenocrysts in Cenozoic basalts

description: Shortly after the cessation of the Cenozoic seafloor spreading in the South China Sea, a period of basaltic magmatism occurred in the Indochina Peninsula. The various types of xenoliths/xenocrysts present in these igneous rocks can provide information about the lithospheric mantle under the Indochina Peninsula. In this study, we present new ages and <i>in situ</i> major and trace element compositions for the xenoliths and olivine xenocrysts from the Wichian Buri and Mae Tha basalt flows in Thailand. The new ages obtained in this study for the Wichian Buri and Mae Tha basalt flows are 9.24 and 2.35 Ma, respectively. Under Thailand, the lithology of the sub-continental mantle lithosphere (SCLM) could be spinel-lherzolite, with a mantle temperature range of 936°C–1096°C. The mantle source of the Cenozoic basalts from Thailand and its adjacent regions could be affect by recycled oceanic crust and carbonates. The origin of spongy textures in clinopyroxene should be resulted from partial melting induced by decompression. SCLM under Thailand were transformed by peridotite-melt interaction, and basaltic melt trapped the mantle xenocryst and xenolith quickly ascended to the surface.
DOI: 10.6084/m9.figshare.19329032.v1
title: The nature of the sub-continental lithospheric mantle beneath Thailand: evidence from xenocrysts in Cenozoic basalts

description: Shortly after the cessation of the Cenozoic seafloor spreading in the South China Sea, a period of basaltic magmatism occurred in the Indochina Peninsula. The various types of xenoliths/xenocrysts present in these igneous rocks can provide information about the lithospheric mantle under the Indochina Peninsula. In this study, we present new ages and <i>in situ</i> major and trace element compositions for the xenoliths and olivine xenocrysts from the Wichian Buri and Mae Tha basalt flows in Thailand. The new ages obtained in this study for the Wichian Buri and Mae Tha basalt flows are 9.24 and 2.35 Ma, respectively. Under Thailand, the lithology of the sub-continental mantle lithosphere (SCLM) could be spinel-lherzolite, with a mantle temperature range of 936°C–1096°C. The mantle source of the Cenozoic basalts from Thailand and its adjacent regions could be affect by recycled oceanic crust and carbonates. The origin of spongy textures in clinopyroxene should be resulted from partial melting induced by decompression. SCLM under Thailand were transformed by peridotite-melt interaction, and basaltic melt trapped the mantle xenocryst and xenolith quickly ascended to the surface.
DOI: 10.6084/m9.figshare.19361619
title: New geochronological and geochemical constraints on the Banke, Dutsen Wai, Guraka, and Zuku alkaline granite complexes from the northcentral Nigerian younger granite province

description: An integrated study was carried out on four anorogenic syenite-granite complexes (i.e. Banke, Dutsen Wai, Guraka, and Zuku) from the Nigerian Younger Granite (NaYG) province, in a bid to constrain their magma sources, rare metal mineralization potentials, and tectonic implications. These four complexes primarily consist of quartz syenite, granite porphyry, arfvedsonite aegirine granite, and biotite granite. The studied rocks are chemically characterized by high alkalis, HFSEs, Ga/Al ratios, and zircon saturation temperature (776–1127°C, average = 932°C), typically of A<sub>1</sub>-type granites. The zircon εHf(t) values of the arfvedsonite aegirine granite (−6.0 to −0.79) are higher than those of the granite porphyry (−9.57 to −7.67) and biotite granite (−9.49 to −5.86) suggesting moderate crustal contamination of mantle-derived melts for the origin of the peralkaline granites. Generation of the biotite granite likely involved inputs of both crustal- and mantle-derived melts and is evidenced by the presence of inherited Pan-African (600–610 Ma) zircons and low whole rock Nb/U and Nb/Ta ratios. Furthermore, input of crustal material likely increased the metal budget of the residual melt and enhanced Nb, Sn, and sulphide mineralization in the Banke granite porphyry and biotite granite and Dutsen Wai biotite granite. Zircon U-Pb dating results constrain the emplacement ages to early Mesozoic era, from the Banke granite porphyry of 180 ± 1 Ma, Dutsen Wai biotite granite of 177 ± 3 Ma, Guraka arfvedsonite aegirine granite of 227 ± 2 Ma and Zuku arfvedsonite granite of 186 ± 2 Ma. These age data indicate a local E-W age migration pattern for the alkaline magma emplacement in northcentral NaYG province. Integrated with other geological evidence, we favour a formation model for the anorogenic NaYG province likely driven by the reactivation of ancient shear zones and structures.
DOI: 10.6084/m9.figshare.19361619.v1
title: New geochronological and geochemical constraints on the Banke, Dutsen Wai, Guraka, and Zuku alkaline granite complexes from the northcentral Nigerian younger granite province

description: An integrated study was carried out on four anorogenic syenite-granite complexes (i.e. Banke, Dutsen Wai, Guraka, and Zuku) from the Nigerian Younger Granite (NaYG) province, in a bid to constrain their magma sources, rare metal mineralization potentials, and tectonic implications. These four complexes primarily consist of quartz syenite, granite porphyry, arfvedsonite aegirine granite, and biotite granite. The studied rocks are chemically characterized by high alkalis, HFSEs, Ga/Al ratios, and zircon saturation temperature (776–1127°C, average = 932°C), typically of A<sub>1</sub>-type granites. The zircon εHf(t) values of the arfvedsonite aegirine granite (−6.0 to −0.79) are higher than those of the granite porphyry (−9.57 to −7.67) and biotite granite (−9.49 to −5.86) suggesting moderate crustal contamination of mantle-derived melts for the origin of the peralkaline granites. Generation of the biotite granite likely involved inputs of both crustal- and mantle-derived melts and is evidenced by the presence of inherited Pan-African (600–610 Ma) zircons and low whole rock Nb/U and Nb/Ta ratios. Furthermore, input of crustal material likely increased the metal budget of the residual melt and enhanced Nb, Sn, and sulphide mineralization in the Banke granite porphyry and biotite granite and Dutsen Wai biotite granite. Zircon U-Pb dating results constrain the emplacement ages to early Mesozoic era, from the Banke granite porphyry of 180 ± 1 Ma, Dutsen Wai biotite granite of 177 ± 3 Ma, Guraka arfvedsonite aegirine granite of 227 ± 2 Ma and Zuku arfvedsonite granite of 186 ± 2 Ma. These age data indicate a local E-W age migration pattern for the alkaline magma emplacement in northcentral NaYG province. Integrated with other geological evidence, we favour a formation model for the anorogenic NaYG province likely driven by the reactivation of ancient shear zones and structures.
DOI: 10.5281/zenodo.7543785
title: Lexicon and example extensions from paper "Lexicon-based comments-oriented news sentiment analyzer system"

description: Lexicon and example extensions for the article "Moreo, Alejandro, et al. "Lexicon-based comments-oriented news sentiment analyzer system." <em>Expert Systems with Applications</em> 39.10 (2012): 9166-9180." Founded by Ministerio de Educación y Ciencia and Junta de Andalucía with Projects: TIN2007-60199, TIC2009-5011 and TIN2007-67984
DOI: 10.5281/zenodo.7543784
title: Lexicon and example extensions from paper "Lexicon-based comments-oriented news sentiment analyzer system"

description: Lexicon and example extensions for the article "Moreo, Alejandro, et al. "Lexicon-based comments-oriented news sentiment analyzer system." <em>Expert Systems with Applications</em> 39.10 (2012): 9166-9180." Founded by Ministerio de Educación y Ciencia and Junta de Andalucía with Projects: TIN2007-60199, TIC2009-5011 and TIN2007-67984
DOI: 10.25442/hku.21907926
title: Aquatic carbon cycle on the Chinese Loess Plateau

description: This dataset includes 1) aquatic greenhouse gas emissions from the Chinese Loess Plateau inland waters (including streams, rivers, lakes, and reservoirs), measured during the period 2015-2019; 2) high-frequency measurement of aquatic carbon export at the Huayuankou hydrologic gauge on the Yellow River in the year of 2018. <br> Three worksheets are included: 1) Stream and river GHG emission: CO2 and CH4 emissions from streams and rivers on the Chinese Loess Plateau (122 sites with coordinate information). <br> 2) Lake and reservoir GHG emission: CO2 and CH4 emissions from lakes and reservoirs on the Chinese Loess Plateau (30 sites with coordinate information). <br> 3) Huayuankou flow, sediment and C: Daily flow and sediment records, and high-frequency (usually at 5 day intervals or shorter) C measurements. For C data, there are dissolved organic carbon (DOC), dissolved inorganic carbon (DIC), and particulate organic carbon (POC).
DOI: 10.25442/hku.21907926.v1
title: Aquatic carbon cycle on the Chinese Loess Plateau

description: This dataset includes 1) aquatic greenhouse gas emissions from the Chinese Loess Plateau inland waters (including streams, rivers, lakes, and reservoirs), measured during the period 2015-2019; 2) high-frequency measurement of aquatic carbon export at the Huayuankou hydrologic gauge on the Yellow River in the year of 2018. <br> Three worksheets are included: 1) Stream and river GHG emission: CO2 and CH4 emissions from streams and rivers on the Chinese Loess Plateau (122 sites with coordinate information). <br> 2) Lake and reservoir GHG emission: CO2 and CH4 emissions from lakes and reservoirs on the Chinese Loess Plateau (30 sites with coordinate information). <br> 3) Huayuankou flow, sediment and C: Daily flow and sediment records, and high-frequency (usually at 5 day intervals or shorter) C measurements. For C data, there are dissolved organic carbon (DOC), dissolved inorganic carbon (DIC), and particulate organic carbon (POC).
DOI: 10.5281/zenodo.7543724
title: raw data for "Two novel CACNA1F gene mutations cause two different phenotypes: Aland Eye Disease and Incomplete Congenital Stationary Night Blindness"

description: DNA and mRNA sequences of two patients affected by CSNB2
DOI: 10.5281/zenodo.7543723
title: raw data for "Two novel CACNA1F gene mutations cause two different phenotypes: Aland Eye Disease and Incomplete Congenital Stationary Night Blindness"

description: DNA and mRNA sequences of two patients affected by CSNB2
DOI: 10.25402/cnc.21908244
title: Supplementary material: A pilot case crossover study of the use of padded headgear in junior Australian football.docx

description: Supplementary material: A pilot case crossover study of the use of padded headgear in junior Australian football
DOI: 10.25402/cnc.21908244.v1
title: Supplementary material: A pilot case crossover study of the use of padded headgear in junior Australian football.docx

description: Supplementary material: A pilot case crossover study of the use of padded headgear in junior Australian football
DOI: 10.5281/zenodo.4271325
title: Nexus database

description: Nexus database associated with the forthcoming publication "<strong>Modelling energy systems across functional scales: an embodied nexus perspective"</strong>