cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.1623178.v1
title: The effect of Invisalign® use on mouth alcohol retention

description: ABSTRACTThree Invisalign®-wearing, alcohol-free subjects were tested for mouth alcohol retention with an Alco-Sensor® IV breath alcohol analyzer (Intoximeters, Inc.). The subjects were given a tolerable amount of beer, wine, or a distilled spirit to swish in their mouths, without swallowing for one minute. The subjects were tested with and without their Invisalign® device in place. In most cases the concentration of alcohol in the mouth was zero 15 minutes post-expectoration in both the controlled and experimental sessions with small to trace amounts of mouth alcohol (≤ 0.016 g/210 L) in several sessions. Based on these findings, Invisalign® use does not significantly affect breath alcohol concentration when a pretest alcohol deprivation period of 15 minutes is performed.
DOI: 10.6084/m9.figshare.1623176.v1
title: Pre-ovipositional and ovipositional behaviour of <i>Lasioseius ometes</i> (Oudemans) and <i>Hypoaspis kargi</i> Costa (Acari: Dermanyssiae: Ascidae, Laelapidae) with notes on egg protection strategies in Mesostigmata

description: Egg deposition by the soil mites <i>Lasioseius ometes</i> (Oudemans, 1903) and <i>Hypoaspis kargi</i> Costa, 1968 was observed using continuous video-monitoring. The process in both species was found to consist of four distinct phases. In Phase 1, both species engage in pre-ovipositional activity prior to the egg being extruded from the genital opening. In <i>L. ometes</i>, the female often selects a substrate depression for egg laying and examines the depression carefully with the gnathosoma and legs I before oviposition. In <i>H. kargi</i>, egg deposition sites are chosen without regard for substrate depressions. Phase 1 lasted approximately 3 minutes for both species. Phase 2 involved egg extrusion and holding of the egg beneath the gnathosoma. Phase 2 lasted approximately 20 times longer in <i>L. ometes</i> (5 minutes) than in <i>H. kargi</i>. Alteration of the egg surface in the form of thorn-like outgrowths was recorded in <i>L. ometes</i>. Egg deposition occurs in Phase 3, and in <i>L. ometes</i> the egg is generally placed at the deposition site using the chelicerae. <i>Hypoaspis kargi</i> also uses the chelicerae for egg manipulation, but also adjusts orientation of the egg with legs I. The sticky nature of egg surface in <i>H. kargi</i> may provide a means for the female to effectively cover the exposed egg with a protective layer of soil particles. Egg deposition in both species occurred in less than 90 seconds. Phase 4 involves egg covering, but behaviour of the female during this last phase differs markedly between the two species. In <i>L. ometes</i>, the female tends to remain close to the egg, whereas in <i>H. kargi</i> the female moves away from the egg to search for substrate particles appropriate for its covering. The average time for Phase 4 in <i>H. kargi</i> was approximately four times longer (80+ minutes) than in <i>L. ometes</i>.
DOI: 10.6084/m9.figshare.1623175.v1
title: The ammonoids from the Late Permian <i>Paratirolites</i> Limestone of Julfa (East Azerbaijan, Iran)

description: The Changhsingian (Late Permian), 4 to 5 m thick <i>Paratirolites</i> Limestone has yielded diverse ammonoid assemblages composed of the genera <i>Neoaganides</i>, <i>Pseudogastrioceras</i>, <i>Dzhulfites</i>, <i>Paratirolites</i>, <i>Julfotirolites</i>, <i>Alibashites</i>, <i>Abichites</i>, <i>Stoyanowites</i> and <i>Arasella</i>. The succession of ammonoid species allows for a subdivision of the rock unit into eight biozones, in ascending order: <i>Dzhulfites zalensis</i> Zone, <i>Paratirolites trapezoidalis</i> Zone, <i>Paratirolites kittli</i> Zone, <i>Stoyanowites dieneri</i> Zone, <i>Alibashites mojsisovicsi</i> Zone, <i>Abichites abichi</i> Zone, <i>Abichites stoyanowi</i> Zone and <i>Arasella minuta</i> Zone. The following 20 new species are described by two of us (DK and AG): <i>Neoaganides ultimus</i> sp. nov., <i>Pseudogastrioceras relicuum</i> sp. nov., <i>Dzhulfites zalensis</i> sp. nov., <i>Dzhulfites hebes</i> sp. nov., <i>Paratirolites coronatus</i> sp. nov., <i>Paratirolites birunii</i> sp. nov., <i>Paratirolites quadratus</i> sp. nov., <i>Paratirolites multiconus</i> sp. nov., <i>Paratirolites serus</i> sp. nov., <i>Julfotirolites kozuri</i> sp. nov., <i>Alibashites ferdowsii</i> sp. nov., <i>Alibashites uncinatus</i> sp. nov., <i>Alibashites stepanovi</i> sp. nov., <i>Abichites subtrapezoidalis</i> sp. nov., <i>Abichites alibashiensis</i> sp. nov., <i>Abichites ariaeii</i> sp. nov., <i>Abichites paucinodus</i> sp. nov., <i>Abichites shahriari</i> sp. nov., <i>Abichites terminalis</i> sp. nov. and <i>Stoyanowites aspinosus</i> sp. nov. After the time-equivalent Chinese occurrences, the material described here is the most diverse assemblage known from the critical interval before the end-Permian mass extinction. http://zoobank.org/urn:lsid:zoobank.org:pub:75D71EE8-27A2-48B1-805B-52E98578A7B8
DOI: 10.6084/m9.figshare.1623171
title: Highly retentive core domains in K-feldspar and their implications for <sup>40</sup>Ar/<sup>39</sup>Ar thermochronology illustrated by determining the cooling curve for the Capoas Granite, Palawan, The Philippines

description: K-feldspar from the late Miocene Capoas Granite on Palawan in The Philippines appears to contain highly retentive diffusion domains that are closed to argon diffusion at near-solidus temperatures during cooling of this ∼7 km-diameter pluton. This is an important result, for K-feldspar is commonly considered not retentive in terms of its ability to retain argon. Closure temperatures for argon diffusion in K-feldspars are routinely claimed to be in the range ∼150–400°C but the release of <sup>39</sup>Ar from irradiated K-feldspar during furnace step-heating experiments <i>in vacuo</i> yields Arrhenius data that imply the existence of highly retentive core domains, with inferred closure temperatures that can exceed ∼500–700°C. These high closure temperatures from the Capoas Granite K-feldspar are consistent with the coincidence of <sup>40</sup>Ar/<sup>39</sup>Ar ages with U–Pb zircon ages at <i>ca</i> 13.5 ± 0.2 Ma. The cooling rate then accelerated, but the rate of change had considerably slowed by <i>ca</i> 12 Ma. Low-temperature (U–Th)/He thermochronology shows that the cooling rate once again accelerated at <i>ca</i> 11 Ma, perhaps owing to renewed tectonic activity.
DOI: 10.6084/m9.figshare.1623172
title: Evidence for 1808–1770 Ma bimodal magmatism, sedimentation, high-temperature deformation and metamorphism in the Aileron Province, central Australia

description: Field relationships and LA-ICP-MS U–Pb geochronology from the Yundurbungu Hills (Aileron Province, central Australia) reveal a record of 1808–1770 Ma bimodal magmatism, sedimentation, high-temperature deformation and metamorphism. Specifically, the data presented here provide the first unequivocal evidence for <i>ca</i> 1774 Ma high-temperature deformation and metamorphism during the 1790–1770 Ma Yambah Event in the southern part of the North Australian Craton. Granitic lithologies were synkinematically emplaced between 1808 and 1770 Ma, with early phases recording D<sub>1</sub> deformation and the youngest phase postdating D<sub>1</sub> deformation. The protolith to a D<sub>1</sub> deformed metasedimentary unit was deposited between 1792 and 1774 Ma, followed by the intrusion and deformation of a composite mafic–felsic magmatic association at <i>ca</i> 1774 Ma. An S<sub>1</sub> migmatitic fabric in the composite mafic–felsic gneiss is truncated by the youngest (<i>ca</i> 1770 Ma) phase of granitic magmatism, constraining the timing of S<sub>1</sub> deformation. A second period of sedimentation appears to post-date D<sub>1</sub> deformation, with deposition occurring sometime after <i>ca</i> 1774 Ma. Subsequent overprinting during the 1590–1550 Ma Chewings Event is recorded by the growth of metamorphic monazite and zircon. This event deformed the <i>ca</i> 1774 Ma S<sub>1</sub> gneissic fabric, producing a composite S<sub>1</sub>/S<sub>2</sub> gneissic fabric in early metasedimentary and magmatic lithologies and a simple S<sub>2</sub>-only fabric in lithologies that were intruded or deposited after <i>ca</i> 1774 Ma. Consistent with previous work, we suggest that localised high-temperature deformation and bimodal magmatism at <i>ca</i> 1774 Ma in the Yundurbungu Hills is consistent with a back-arc setting linked to prolonged north-directed subduction.
DOI: 10.6084/m9.figshare.1623171.v1
title: Highly retentive core domains in K-feldspar and their implications for <sup>40</sup>Ar/<sup>39</sup>Ar thermochronology illustrated by determining the cooling curve for the Capoas Granite, Palawan, The Philippines

description: K-feldspar from the late Miocene Capoas Granite on Palawan in The Philippines appears to contain highly retentive diffusion domains that are closed to argon diffusion at near-solidus temperatures during cooling of this ∼7 km-diameter pluton. This is an important result, for K-feldspar is commonly considered not retentive in terms of its ability to retain argon. Closure temperatures for argon diffusion in K-feldspars are routinely claimed to be in the range ∼150–400°C but the release of <sup>39</sup>Ar from irradiated K-feldspar during furnace step-heating experiments <i>in vacuo</i> yields Arrhenius data that imply the existence of highly retentive core domains, with inferred closure temperatures that can exceed ∼500–700°C. These high closure temperatures from the Capoas Granite K-feldspar are consistent with the coincidence of <sup>40</sup>Ar/<sup>39</sup>Ar ages with U–Pb zircon ages at <i>ca</i> 13.5 ± 0.2 Ma. The cooling rate then accelerated, but the rate of change had considerably slowed by <i>ca</i> 12 Ma. Low-temperature (U–Th)/He thermochronology shows that the cooling rate once again accelerated at <i>ca</i> 11 Ma, perhaps owing to renewed tectonic activity.
DOI: 10.6084/m9.figshare.1623172.v1
title: Evidence for 1808–1770 Ma bimodal magmatism, sedimentation, high-temperature deformation and metamorphism in the Aileron Province, central Australia

description: Field relationships and LA-ICP-MS U–Pb geochronology from the Yundurbungu Hills (Aileron Province, central Australia) reveal a record of 1808–1770 Ma bimodal magmatism, sedimentation, high-temperature deformation and metamorphism. Specifically, the data presented here provide the first unequivocal evidence for <i>ca</i> 1774 Ma high-temperature deformation and metamorphism during the 1790–1770 Ma Yambah Event in the southern part of the North Australian Craton. Granitic lithologies were synkinematically emplaced between 1808 and 1770 Ma, with early phases recording D<sub>1</sub> deformation and the youngest phase postdating D<sub>1</sub> deformation. The protolith to a D<sub>1</sub> deformed metasedimentary unit was deposited between 1792 and 1774 Ma, followed by the intrusion and deformation of a composite mafic–felsic magmatic association at <i>ca</i> 1774 Ma. An S<sub>1</sub> migmatitic fabric in the composite mafic–felsic gneiss is truncated by the youngest (<i>ca</i> 1770 Ma) phase of granitic magmatism, constraining the timing of S<sub>1</sub> deformation. A second period of sedimentation appears to post-date D<sub>1</sub> deformation, with deposition occurring sometime after <i>ca</i> 1774 Ma. Subsequent overprinting during the 1590–1550 Ma Chewings Event is recorded by the growth of metamorphic monazite and zircon. This event deformed the <i>ca</i> 1774 Ma S<sub>1</sub> gneissic fabric, producing a composite S<sub>1</sub>/S<sub>2</sub> gneissic fabric in early metasedimentary and magmatic lithologies and a simple S<sub>2</sub>-only fabric in lithologies that were intruded or deposited after <i>ca</i> 1774 Ma. Consistent with previous work, we suggest that localised high-temperature deformation and bimodal magmatism at <i>ca</i> 1774 Ma in the Yundurbungu Hills is consistent with a back-arc setting linked to prolonged north-directed subduction.
DOI: 10.6084/m9.figshare.1623156
title: Tetraspan cargo adaptors usher GPI-anchored proteins into multivesicular bodies

description: Ubiquitinated membrane proteins are sorted into intralumenal endosomal vesicles on their way for degradation in lysosomes. Here we summarize the discovery of the Cos proteins, which work to organize and segregate ubiquitinated cargo prior to its incorporation into intralumenal vesicles of the multivesicular body (MVB). Importantly, cargoes such as GPI-anchored proteins (GPI-APs) that cannot undergo ubiquitination, rely entirely on Cos proteins for sorting into intralumenal vesicles using the same pathway that depends on ESCRTs and ubiquitin ligases that typical polytopic membrane proteins do. Here we show Cos proteins provide functions as not only adaptor proteins for ubiquitin ligases, but also as cargo carriers that can physically usher a variety of other proteins into the MVB pathway. We then discuss the significance of this new sorting model and the broader implications for this cargo adaptor mechanism, whereby yeast Cos proteins, and their likely animal analogs, provide a ubiquitin sorting signal in <i>trans</i> to enable sorting of a membrane protein network into intralumenal vesicles.
DOI: 10.6084/m9.figshare.1623156.v1
title: Tetraspan cargo adaptors usher GPI-anchored proteins into multivesicular bodies

description: Ubiquitinated membrane proteins are sorted into intralumenal endosomal vesicles on their way for degradation in lysosomes. Here we summarize the discovery of the Cos proteins, which work to organize and segregate ubiquitinated cargo prior to its incorporation into intralumenal vesicles of the multivesicular body (MVB). Importantly, cargoes such as GPI-anchored proteins (GPI-APs) that cannot undergo ubiquitination, rely entirely on Cos proteins for sorting into intralumenal vesicles using the same pathway that depends on ESCRTs and ubiquitin ligases that typical polytopic membrane proteins do. Here we show Cos proteins provide functions as not only adaptor proteins for ubiquitin ligases, but also as cargo carriers that can physically usher a variety of other proteins into the MVB pathway. We then discuss the significance of this new sorting model and the broader implications for this cargo adaptor mechanism, whereby yeast Cos proteins, and their likely animal analogs, provide a ubiquitin sorting signal in <i>trans</i> to enable sorting of a membrane protein network into intralumenal vesicles.
DOI: 10.17632/v2p3th8pb5.2
title: Data for: Failure Analysis of Feed Water Pump Shaft in HRSG of 9F Gas Turbine Generator Unit

description: macrophotograph，fracture morphology，microstructure，mechanical property
DOI: 10.6084/m9.figshare.1623144
title: Analyzing the pyrolysis kinetics of rice straw, bagasse, and mixtures thereof and product energy yield

description: In Taiwan, rice straw and bagasse are major agricultural wastes that are produced in extremely large quantities and volumes and contain high moisture content. Current processing methods remain inadequate; therefore, this study focused on the pyrolysis and relevant analyses of rice straw, bagasse, and mixtures thereof to investigate the feasibility of copyrolyzing rice straw and bagasse for renewable energy generation. Mixtures containing various ratios of bagasse and rice straw were examined through physical, chemical, thermogravimetric, and reaction kinetics analyses. Pyrolysis experiments were conducted to investigate the energy yield of the reaction products. Both bagasse and rice straw contained low ash content, and thermal processing effectively reduced the waste volume and cost of final disposal. A mixture content containing approximately 30 wt% rice straw (potassium content reaching 8.50 g/kg) substantially reduced the activation energies required for copyrolysis reactions, subsequently reducing energies required for thermal processing. The solid char generated from pyrolyzing the bagasse and rice straw mixtures did not decay easily and exhibited high storability and transportability. Moreover, volumetric energy densities substantially increased after pyrolysis. Therefore, copyrolysis is arguably a feasible and effective alternative biofuel conversion method for countries that process large quantities of bagasse and rice straw.
DOI: 10.6084/m9.figshare.1623144.v1
title: Analyzing the pyrolysis kinetics of rice straw, bagasse, and mixtures thereof and product energy yield

description: In Taiwan, rice straw and bagasse are major agricultural wastes that are produced in extremely large quantities and volumes and contain high moisture content. Current processing methods remain inadequate; therefore, this study focused on the pyrolysis and relevant analyses of rice straw, bagasse, and mixtures thereof to investigate the feasibility of copyrolyzing rice straw and bagasse for renewable energy generation. Mixtures containing various ratios of bagasse and rice straw were examined through physical, chemical, thermogravimetric, and reaction kinetics analyses. Pyrolysis experiments were conducted to investigate the energy yield of the reaction products. Both bagasse and rice straw contained low ash content, and thermal processing effectively reduced the waste volume and cost of final disposal. A mixture content containing approximately 30 wt% rice straw (potassium content reaching 8.50 g/kg) substantially reduced the activation energies required for copyrolysis reactions, subsequently reducing energies required for thermal processing. The solid char generated from pyrolyzing the bagasse and rice straw mixtures did not decay easily and exhibited high storability and transportability. Moreover, volumetric energy densities substantially increased after pyrolysis. Therefore, copyrolysis is arguably a feasible and effective alternative biofuel conversion method for countries that process large quantities of bagasse and rice straw.
DOI: 10.6084/m9.figshare.1623129
title: Miocene andesitic lavas of Sierra de Angangueo: a petrological, geochemical, and geochronological approach to arc magmatism in Central Mexico

description: The early and middle Miocene andesitic lavas of the Sierra de Angangueo (MALSA) represent one of the most prominent landforms of intermediate magmatism in Central Mexico. In this paper, we present new petrological, geochemical, thermobarometric, and geochronological data in order to discuss the conditions of MALSA’s emplacement in the lithosphere. MALSA comprises a voluminous eroded early Miocene andesitic structure, emplaced on a Mesozoic basement. MALSA shows a wide variety of textures, from glassy and aphanitic to porphyritic, mainly composed of plagioclase (An<sub>10-55</sub>), clinopyroxene (Wo<sub>60-65</sub>; En<sub>35-40</sub>), amphibole (Mg-hornblende/edenite), and rarely olivine (Fo<sub>75–86</sub>) or orthopyroxene (En<sub>72-80</sub>). Major and trace elements plots follow a typical calc-alkaline trend with relatively increasing fractionation. The <sup>87</sup>Sr/<sup>86</sup>Sr isotopic signatures range between 0.703343 and 0.704459 and εNd values from +1.37 to +4.84; apparently without a significant contribution of an old, thick, or highly radiogenic continental crust. Lead isotope values <sup>206</sup>Pb/<sup>204</sup>Pb vary between 18.68 and 18.83, <sup>207</sup>Pb/<sup>204</sup>Pb from 15.57 to 15.65, and <sup>208</sup>Pb/<sup>204</sup>Pb from 38.39 to 38.67, suggesting contamination of magmas by juvenile crust. Thermodynamic calculations indicate equilibrium conditions at ≤900°C and ~2 kbar and an average log ƒO<sub>2</sub> ≈ −10. Ar–Ar and K–Ar dating carried out on whole rock, matrix, amphibole, and plagioclase phenocrysts yielded ages between 13.0 ± 0.5 and 23.9 ± 0.3 Ma. These dates indicate a series of pulses with maximum magmatic activity between 24 and 18 Ma. The geochemical and petrologic data suggest partial melting processes in the lower or middle crust associated with possible magma mixing during its ascent; such a mechanism could explain a hybrid mantle-lower crust origin of this large volume of andesites. The MALSA, as well as the early to middle Miocene magmatism from Western Mexico, could represent two coeval and independent magmatic arcs prior to the present Trans-Mexican Volcanic Belt (TMVB) in Central Mexico.
DOI: 10.6084/m9.figshare.1623129.v2
title: Miocene andesitic lavas of Sierra de Angangueo: a petrological, geochemical, and geochronological approach to arc magmatism in Central Mexico

description: The early and middle Miocene andesitic lavas of the Sierra de Angangueo (MALSA) represent one of the most prominent landforms of intermediate magmatism in Central Mexico. In this paper, we present new petrological, geochemical, thermobarometric, and geochronological data in order to discuss the conditions of MALSA’s emplacement in the lithosphere. MALSA comprises a voluminous eroded early Miocene andesitic structure, emplaced on a Mesozoic basement. MALSA shows a wide variety of textures, from glassy and aphanitic to porphyritic, mainly composed of plagioclase (An<sub>10-55</sub>), clinopyroxene (Wo<sub>60-65</sub>; En<sub>35-40</sub>), amphibole (Mg-hornblende/edenite), and rarely olivine (Fo<sub>75–86</sub>) or orthopyroxene (En<sub>72-80</sub>). Major and trace elements plots follow a typical calc-alkaline trend with relatively increasing fractionation. The <sup>87</sup>Sr/<sup>86</sup>Sr isotopic signatures range between 0.703343 and 0.704459 and εNd values from +1.37 to +4.84; apparently without a significant contribution of an old, thick, or highly radiogenic continental crust. Lead isotope values <sup>206</sup>Pb/<sup>204</sup>Pb vary between 18.68 and 18.83, <sup>207</sup>Pb/<sup>204</sup>Pb from 15.57 to 15.65, and <sup>208</sup>Pb/<sup>204</sup>Pb from 38.39 to 38.67, suggesting contamination of magmas by juvenile crust. Thermodynamic calculations indicate equilibrium conditions at ≤900°C and ~2 kbar and an average log ƒO<sub>2</sub> ≈ −10. Ar–Ar and K–Ar dating carried out on whole rock, matrix, amphibole, and plagioclase phenocrysts yielded ages between 13.0 ± 0.5 and 23.9 ± 0.3 Ma. These dates indicate a series of pulses with maximum magmatic activity between 24 and 18 Ma. The geochemical and petrologic data suggest partial melting processes in the lower or middle crust associated with possible magma mixing during its ascent; such a mechanism could explain a hybrid mantle-lower crust origin of this large volume of andesites. The MALSA, as well as the early to middle Miocene magmatism from Western Mexico, could represent two coeval and independent magmatic arcs prior to the present Trans-Mexican Volcanic Belt (TMVB) in Central Mexico.