cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.25549/one-ouc17551858
title: Mattachine Society, correspondence, Dale Olson (1954-1956)
DOI: 10.6084/m9.figshare.14450033.v1
title: Geochronology and geochemistry of Late Triassic intrusions in the Liaodong Peninsula, eastern North China Craton: implications for post-collisional lithospheric thinning

description: Despite numerous years and avenues of investigation, the timing, evolution, and mechanism of lithospheric thinning of the North China Craton (NCC) are still highly debated. Late Triassic igneous rocks especially mantle derived mafic rocks could provide critical information related to the post-collisional lithospheric thinning of the Liaodong Peninsula in the eastern NCC. Using newly acquired geochronological data points, we determined that the intrusive rocks have emplacement ages of 219–209 Ma, which are typical of Late Triassic magmatism. The studied Qinghekou gabbros have low SiO<sub>2</sub> (49.43–51.86 wt.%), Na<sub>2</sub>O+K<sub>2</sub>O (3.59–7.20 wt.%), high MgO (3.70–8.54 wt.%) and transition metal element contents, with Mg<sup>#</sup> values ranging from 49.2 to 69.3. While these samples are enriched in large ion lithophile elements such as Rb, Ba, and K and light rare earth elements, they are depleted in high field strength elements such as Nb, Ta, Ti, and P and heavy rare earth elements. We conclude that these gabbros samples were formed in a subduction-related tectonic setting, where the primary magmas were derived from partial melting of the lithospheric mantle that experienced metasomatism via slab-related fluids. Our Tongyuanpu granite samples have I-type granite affinity, as indicated by their high SiO<sub>2</sub> (73.60–75.30 wt.%) and low MgO (0.08–0.32 wt.%) contents, as well as the A/CNK values of 0.99–1.25 and the zircon saturated temperature values of 757–832°C, the parental magmas for these granites were generated by partial melting of the lower crust. Combined with the spatio-temporal distribution and rock-assemblages of the Late Triassic intrusive rocks, we conclude that these rocks were formed in an extensional environment characterized by lithospheric thinning caused by lithospheric delamination after the collision between the NCC and the Yangtze Craton. Furthermore, we infer that the initial lithospheric thinning of the eastern NCC occurred during the Late Triassic.
DOI: 10.6084/m9.figshare.7110284
title: Simulation Code from Transitions in synchronization states of model cilia through basal-connection coupling

description: Code used in the simulations (Matlab 2018a version)
DOI: 10.6084/m9.figshare.14450033
title: Geochronology and geochemistry of Late Triassic intrusions in the Liaodong Peninsula, eastern North China Craton: implications for post-collisional lithospheric thinning

description: Despite numerous years and avenues of investigation, the timing, evolution, and mechanism of lithospheric thinning of the North China Craton (NCC) are still highly debated. Late Triassic igneous rocks especially mantle derived mafic rocks could provide critical information related to the post-collisional lithospheric thinning of the Liaodong Peninsula in the eastern NCC. Using newly acquired geochronological data points, we determined that the intrusive rocks have emplacement ages of 219–209 Ma, which are typical of Late Triassic magmatism. The studied Qinghekou gabbros have low SiO<sub>2</sub> (49.43–51.86 wt.%), Na<sub>2</sub>O+K<sub>2</sub>O (3.59–7.20 wt.%), high MgO (3.70–8.54 wt.%) and transition metal element contents, with Mg<sup>#</sup> values ranging from 49.2 to 69.3. While these samples are enriched in large ion lithophile elements such as Rb, Ba, and K and light rare earth elements, they are depleted in high field strength elements such as Nb, Ta, Ti, and P and heavy rare earth elements. We conclude that these gabbros samples were formed in a subduction-related tectonic setting, where the primary magmas were derived from partial melting of the lithospheric mantle that experienced metasomatism via slab-related fluids. Our Tongyuanpu granite samples have I-type granite affinity, as indicated by their high SiO<sub>2</sub> (73.60–75.30 wt.%) and low MgO (0.08–0.32 wt.%) contents, as well as the A/CNK values of 0.99–1.25 and the zircon saturated temperature values of 757–832°C, the parental magmas for these granites were generated by partial melting of the lower crust. Combined with the spatio-temporal distribution and rock-assemblages of the Late Triassic intrusive rocks, we conclude that these rocks were formed in an extensional environment characterized by lithospheric thinning caused by lithospheric delamination after the collision between the NCC and the Yangtze Craton. Furthermore, we infer that the initial lithospheric thinning of the eastern NCC occurred during the Late Triassic.
DOI: 10.6084/m9.figshare.7110419
title: The profiles of soluble adhesion molecules in the “great obstetrical syndromes”*

description: <b>Objective:</b> The objective of this study was to determine the profiles of maternal plasma soluble adhesion molecules in patients with preeclampsia, small-for-gestational-age (SGA) fetuses, acute pyelonephritis, preterm labor with intact membranes (PTL), preterm prelabor rupture of the membranes (preterm PROM), and fetal death. <b>Materials and methods:</b> A cross-sectional study was conducted to determine maternal plasma concentrations of sE-selectin, sL-selectin, and sP-selectin as well as sICAM-1, sVCAM-1, and sPECAM-1 in patients with (1) an uncomplicated pregnancy (control, <i>n</i> = 100); (2) preeclampsia (<i>n</i> = 94); (3) SGA fetuses (in women without preeclampsia/hypertension, <i>n</i> = 45); (4) acute pyelonephritis (<i>n</i> = 25); (5) PTL (<i>n</i> = 53); (6) preterm PROM (<i>n</i> = 24); and (7) fetal death (<i>n</i> = 34). Concentrations of soluble adhesion molecules and inflammatory cytokines (tumor necrosis factor (TNF)-α and interleukin (IL)-8) were determined with sensitive and specific enzyme-linked immunoassays. <b>Results:</b> In comparison to women with a normal pregnancy, (1) women with preeclampsia had higher median concentrations of sE-selectin, sP-selectin, and sVCAM-1, and a lower concentration of sL-selectin (all <i>p</i> values &lt; .001); (2) patients with SGA fetuses had higher median concentrations of sE-selectin, sP-selectin, and sVCAM-1 (all <i>p</i> values &lt; .05); (3) patients with a fetal death had higher median concentrations of sE-selectin and sP-selectin (all <i>p</i> values &lt; .05); (4) patients with acute pyelonephritis had higher median plasma concentrations of sE-selectin, sICAM-1, and sVCAM-1 (all <i>p</i> values &lt; .001); (5) patients with preeclampsia and acute pyelonephritis, plasma concentrations of sVCAM-1, sE-selectin, and sP-selectin correlated with those of the proinflammatory cytokines TNF-α and interleukin (IL)-8 (all <i>p</i> values &lt; .05); (6) patients with PTL had a higher median concentration of sP-selectin and a lower median concentration of VCAM-1 (all <i>p</i> values &lt; .05); and (7) women with preterm PROM had lower median concentrations of sL-selectin and sVCAM-1 (all <i>p</i> values &lt; .05). <b>Conclusions:</b> The results of this study show that endothelial cell activation/dysfunction reflected by the plasma concentration of sE-selectin is not specific to preeclampsia but is present in pregnancies complicated by SGA fetuses, acute pyelonephritis, and fetal death. Collectively, we report that each obstetrical syndrome appears to have a stereotypical profile of soluble adhesion molecules in the peripheral circulation.
DOI: 10.25549/one-ouc17551848
title: Mattachine Society, correspondence, Gonzalo (Tony) Segura, Jr. (1956-1961)
DOI: 10.6084/m9.figshare.20217524.v1
title: Numerical simulation and experimental study of the damage law of EFP warhead charging of cylindrical shells under different angles

description: Abstract In this paper, LS-dyna software was used to simulate the charging process of cylindrical shell when EFP has different angles, and some interesting phenomena and laws were found. Cylindrical elastic wave σr was generated when the cylindrical shell was impacted by EFP. The cylindrical elastic wave σr was correlated with the time required for the cylindrical shell charge to be successfully detonated. When the EFP warhead penetration Angle θ ranges from 0° to 10°, the σr increases linearly with (cosθ)-1/2. With the increase of θ, the tangential velocity vy had an obvious effect on the impact of EFP on the cylindrical shell, and the linear relationship between the elastic wave σr and (cosθ)-1/2 does not change. When the θ was greater than 45°, EFP could not successfully impact and detonate the cylindrical shell charge. The EFP velocity was measured by velocity measurement method with an error of 1.3%. The experimental results have strong similarity with the simulation results, indicating that the parameters of the numerical simulation model have good reliability.
DOI: 10.6084/m9.figshare.19688352
title: Additional file 1 of Self-reported mental health during the COVID-19 pandemic and its association with alcohol and cannabis use: a latent class analysis

description: Additional file 1.
DOI: 10.25549/one-ouc17551851
title: Mattachine Society, correspondence, Dale Olson (1954-1956)
DOI: 10.6084/m9.figshare.19688371.v1
title: Additional file 11 of Research on lncRNA related to drought resistance of Shanlan upland rice

description: Additional file 11: Table S011. The relationship of lncRNA with Mrna.
DOI: 10.6084/m9.figshare.19688392.v1
title: Additional file 5 of Research on lncRNA related to drought resistance of Shanlan upland rice

description: Additional file 5: Table S005. List of differentially expressed miRNAs from the two treatment groups.
DOI: 10.6084/m9.figshare.19688398
title: Additional file 7 of Research on lncRNA related to drought resistance of Shanlan upland rice

description: Additional file 7: Table S007. Function annotion of lncRNAs trans-target gene.
DOI: 10.25549/one-ouc17551854
title: Mattachine Society, correspondence, Dale Olson (1954-1956)
DOI: 10.6084/m9.figshare.19688371
title: Additional file 11 of Research on lncRNA related to drought resistance of Shanlan upland rice

description: Additional file 11: Table S011. The relationship of lncRNA with Mrna.
DOI: 10.25549/one-ouc17551853
title: Mattachine Society, correspondence, Gonzalo (Tony) Segura, Jr. (1956-1961)
DOI: 10.6084/m9.figshare.8159072
title: Inhibition of neddylation causes meiotic arrest in mouse oocyte

description: Mammalian oocyte meiosis is a special form of cell division that provides haploid gametes for fertilization. Unlike in mitosis, post-translational modifications (PTMs) are more crucial during meiosis because of the absence of de novo mRNA transcription. As a classic PTM, protein neddylation is a biological process that mediates protein degradation by modifying cullin proteins and activating the Cullin-Ring E3 ligases. This process plays important roles in various biological processes such as autophagy and tumorigenesis. However, the function of neddylation in germ cells is unknown. In this study, we observed that the inhibition of neddylation by its specific inhibitor MLN4924 significantly arrests mouse oocyte at the stage of metaphase during meiosis. The arrested oocytes display impaired spindles with over-activation of spindle assembly checkpoint (SAC). Accordingly, we identified early mitosis inhibitor 1 (Emi1), a key inhibitor of anaphase-promoting complex/cyclosome (APC/C<sup>Fzr1</sup>), as a substrate of neddylation-mediated protein degradation. Thus, our study uncovered an unknown role of neddylation in female germ cells and suggests that proper neddylation is essential for oocyte maturation.
DOI: 10.6084/m9.figshare.8159072.v1
title: Inhibition of neddylation causes meiotic arrest in mouse oocyte

description: Mammalian oocyte meiosis is a special form of cell division that provides haploid gametes for fertilization. Unlike in mitosis, post-translational modifications (PTMs) are more crucial during meiosis because of the absence of de novo mRNA transcription. As a classic PTM, protein neddylation is a biological process that mediates protein degradation by modifying cullin proteins and activating the Cullin-Ring E3 ligases. This process plays important roles in various biological processes such as autophagy and tumorigenesis. However, the function of neddylation in germ cells is unknown. In this study, we observed that the inhibition of neddylation by its specific inhibitor MLN4924 significantly arrests mouse oocyte at the stage of metaphase during meiosis. The arrested oocytes display impaired spindles with over-activation of spindle assembly checkpoint (SAC). Accordingly, we identified early mitosis inhibitor 1 (Emi1), a key inhibitor of anaphase-promoting complex/cyclosome (APC/C<sup>Fzr1</sup>), as a substrate of neddylation-mediated protein degradation. Thus, our study uncovered an unknown role of neddylation in female germ cells and suggests that proper neddylation is essential for oocyte maturation.
DOI: 10.25549/one-ouc17551857
title: Mattachine Society, correspondence, Gonzalo (Tony) Segura, Jr. (1956-1961)
DOI: 10.25549/one-ouc17555601
title: Mattachine Society, Long Beach (Harbor) Area Council correspondence and memoranda (1953-1956)
DOI: 10.25549/one-ouc17551856
title: Mattachine Society, correspondence, Gonzalo (Tony) Segura, Jr. (1956-1961)
DOI: 10.25549/one-ouc17551855
title: Mattachine Society, correspondence, Donald Stewart Lucas (1956-1965)
DOI: 10.25549/one-ouc17551859
title: Mattachine Society, correspondence, Gonzalo (Tony) Segura, Jr. (1956-1961)
DOI: 10.25549/one-ouc17551869
title: Mattachine Society, correspondence, Wallace O. Maxey (1953-1961)
DOI: 10.25549/one-ouc17551861
title: Mattachine Society, correspondence, Gonzalo (Tony) Segura, Jr. (1956-1961)
DOI: 10.6084/m9.figshare.19688380.v1
title: Additional file 1 of Research on lncRNA related to drought resistance of Shanlan upland rice

description: Additional file 1: Table S001. lncRNA specifically expressed in drought.
DOI: 10.25549/one-ouc17551862
title: Mattachine Society, correspondence, Dale Olson (1954-1956)
DOI: 10.25549/one-ouc17551866
title: Mattachine Society, correspondence, Dale Olson (1954-1956)
DOI: 10.17188/1286599
title: Materials Data on CsCaF3 by Materials Project

description: CsCaF3 is (Cubic) Perovskite structured and crystallizes in the cubic Pm-3m space group. The structure is three-dimensional. Cs1+ is bonded to twelve equivalent F1- atoms to form CsF12 cuboctahedra that share corners with twelve equivalent CsF12 cuboctahedra, faces with six equivalent CsF12 cuboctahedra, and faces with eight equivalent CaF6 octahedra. All Cs–F bond lengths are 3.24 Å. Ca2+ is bonded to six equivalent F1- atoms to form CaF6 octahedra that share corners with six equivalent CaF6 octahedra and faces with eight equivalent CsF12 cuboctahedra. The corner-sharing octahedral tilt angles are 0°. All Ca–F bond lengths are 2.29 Å. F1- is bonded in a distorted linear geometry to four equivalent Cs1+ and two equivalent Ca2+ atoms.
DOI: 10.17188/1286600
title: Materials Data on NdSi2 by Materials Project

description: NdSi2 is Cubic Laves structured and crystallizes in the cubic Fd-3m space group. The structure is three-dimensional. Nd is bonded in a 12-coordinate geometry to twelve equivalent Si atoms. All Nd–Si bond lengths are 3.20 Å. Si is bonded to six equivalent Nd and six equivalent Si atoms to form a mixture of edge, face, and corner-sharing SiNd6Si6 cuboctahedra. All Si–Si bond lengths are 2.73 Å.
DOI: 10.17188/1286601
title: Materials Data on VH21C7N4Cl7 by Materials Project

description: VC3H9(NCl)3(CH3)2NH2(CH2Cl2)2 crystallizes in the monoclinic C2/c space group. The structure is zero-dimensional and consists of sixteen dichloromethane molecules, eight dimethylazanium molecules, and four VC3H9(NCl)3 clusters. In each VC3H9(NCl)3 cluster, V2+ is bonded to three N3- and three Cl1- atoms to form distorted face-sharing VN3Cl3 octahedra. There are a spread of V–N bond distances ranging from 1.90–1.97 Å. There are a spread of V–Cl bond distances ranging from 2.41–2.59 Å. There are three inequivalent C+0.57- sites. In the first C+0.57- site, C+0.57- is bonded to one N3- and three H1+ atoms to form corner-sharing CH3N tetrahedra. The C–N bond length is 1.48 Å. There is one shorter (1.09 Å) and two longer (1.10 Å) C–H bond length. In the second C+0.57- site, C+0.57- is bonded to one N3- and three H1+ atoms to form corner-sharing CH3N tetrahedra. The C–N bond length is 1.47 Å. There is one shorter (1.09 Å) and two longer (1.10 Å) C–H bond length. In the third C+0.57- site, C+0.57- is bonded to one N3- and three H1+ atoms to form corner-sharing CH3N tetrahedra. The C–N bond length is 1.45 Å. There is one shorter (1.08 Å) and two longer (1.10 Å) C–H bond length. There are four inequivalent N3- sites. In the first N3- site, N3- is bonded in a 3-coordinate geometry to two equivalent V2+ and one N3- atom. The N–N bond length is 1.29 Å. In the second N3- site, N3- is bonded in a distorted trigonal planar geometry to two C+0.57- and one N3- atom. In the third N3- site, N3- is bonded in a 3-coordinate geometry to two equivalent V2+ and one N3- atom. The N–N bond length is 1.26 Å. In the fourth N3- site, N3- is bonded in a distorted trigonal planar geometry to two equivalent C+0.57- and one N3- atom. There are nine inequivalent H1+ sites. In the first H1+ site, H1+ is bonded in a single-bond geometry to one C+0.57- atom. In the second H1+ site, H1+ is bonded in a single-bond geometry to one C+0.57- atom. In the third H1+ site, H1+ is bonded in a single-bond geometry to one C+0.57- atom. In the fourth H1+ site, H1+ is bonded in a single-bond geometry to one C+0.57- atom. In the fifth H1+ site, H1+ is bonded in a single-bond geometry to one C+0.57- atom. In the sixth H1+ site, H1+ is bonded in a single-bond geometry to one C+0.57- atom. In the seventh H1+ site, H1+ is bonded in a single-bond geometry to one C+0.57- atom. In the eighth H1+ site, H1+ is bonded in a single-bond geometry to one C+0.57- atom. In the ninth H1+ site, H1+ is bonded in a single-bond geometry to one C+0.57- atom. There are three inequivalent Cl1- sites. In the first Cl1- site, Cl1- is bonded in a single-bond geometry to one V2+ atom. In the second Cl1- site, Cl1- is bonded in a single-bond geometry to one V2+ atom. In the third Cl1- site, Cl1- is bonded in a single-bond geometry to one V2+ atom.
DOI: 10.17188/1286602
title: Materials Data on Er(SiPt)2 by Materials Project

description: ErPt2Si2 crystallizes in the tetragonal I4/mmm space group. The structure is three-dimensional. Er is bonded in a 8-coordinate geometry to eight equivalent Pt and eight equivalent Si atoms. All Er–Pt bond lengths are 3.23 Å. All Er–Si bond lengths are 3.18 Å. Pt is bonded to four equivalent Er and four equivalent Si atoms to form a mixture of distorted edge, corner, and face-sharing PtEr4Si4 tetrahedra. All Pt–Si bond lengths are 2.47 Å. Si is bonded in a 9-coordinate geometry to four equivalent Er, four equivalent Pt, and one Si atom. The Si–Si bond length is 2.31 Å.
DOI: 10.17188/1286603
title: Materials Data on Tm(SiPt)2 by Materials Project

description: Tm(PtSi)2 crystallizes in the tetragonal I4/mmm space group. The structure is three-dimensional. Tm is bonded in a 8-coordinate geometry to eight equivalent Pt and eight equivalent Si atoms. All Tm–Pt bond lengths are 3.22 Å. All Tm–Si bond lengths are 3.17 Å. Pt is bonded to four equivalent Tm and four equivalent Si atoms to form a mixture of distorted edge, face, and corner-sharing PtTm4Si4 tetrahedra. All Pt–Si bond lengths are 2.46 Å. Si is bonded in a 9-coordinate geometry to four equivalent Tm, four equivalent Pt, and one Si atom. The Si–Si bond length is 2.30 Å.
DOI: 10.17188/1286604
title: Materials Data on Lu(SiPt)2 by Materials Project

description: LuPt2Si2 crystallizes in the tetragonal I4/mmm space group. The structure is three-dimensional. Lu is bonded in a 8-coordinate geometry to eight equivalent Pt and eight equivalent Si atoms. All Lu–Pt bond lengths are 3.21 Å. All Lu–Si bond lengths are 3.17 Å. Pt is bonded in a 4-coordinate geometry to four equivalent Lu and four equivalent Si atoms. All Pt–Si bond lengths are 2.46 Å. Si is bonded in a 9-coordinate geometry to four equivalent Lu, four equivalent Pt, and one Si atom. The Si–Si bond length is 2.29 Å.
DOI: 10.17188/1286605
title: Materials Data on CeGa6 by Materials Project

description: CeGa6 crystallizes in the tetragonal P4/nbm space group. The structure is three-dimensional. Ce is bonded to twelve Ga atoms to form a mixture of edge and face-sharing CeGa12 cuboctahedra. There are four shorter (3.13 Å) and eight longer (3.25 Å) Ce–Ga bond lengths. There are two inequivalent Ga sites. In the first Ga site, Ga is bonded in a 4-coordinate geometry to one Ce and three Ga atoms. There are one shorter (2.55 Å) and two longer (2.65 Å) Ga–Ga bond lengths. In the second Ga site, Ga is bonded in a 9-coordinate geometry to four equivalent Ce and five Ga atoms. The Ga–Ga bond length is 2.49 Å.
DOI: 10.17188/1286606
title: Materials Data on Sr2Cu3(SO)2 by Materials Project

description: Sr2Cu3(SO)2 crystallizes in the tetragonal I4/mmm space group. The structure is three-dimensional. Sr2+ is bonded in a 8-coordinate geometry to four equivalent S2- and four equivalent O2- atoms. All Sr–S bond lengths are 3.17 Å. All Sr–O bond lengths are 2.59 Å. There are two inequivalent Cu+1.33+ sites. In the first Cu+1.33+ site, Cu+1.33+ is bonded in a square co-planar geometry to two equivalent S2- and four equivalent O2- atoms. Both Cu–S bond lengths are 3.21 Å. All Cu–O bond lengths are 1.97 Å. In the second Cu+1.33+ site, Cu+1.33+ is bonded to four equivalent S2- atoms to form a mixture of edge and corner-sharing CuS4 tetrahedra. All Cu–S bond lengths are 2.41 Å. S2- is bonded in a 9-coordinate geometry to four equivalent Sr2+ and five Cu+1.33+ atoms. O2- is bonded to four equivalent Sr2+ and two equivalent Cu+1.33+ atoms to form a mixture of face, edge, and corner-sharing OSr4Cu2 octahedra. The corner-sharing octahedral tilt angles are 0°.
DOI: 10.17188/1286607
title: Materials Data on CrAuS2 by Materials Project

description: AuCrS2 crystallizes in the trigonal R-3m space group. The structure is three-dimensional. Cr3+ is bonded to six equivalent S2- atoms to form edge-sharing CrS6 octahedra. All Cr–S bond lengths are 2.40 Å. Au1+ is bonded in a linear geometry to two equivalent S2- atoms. Both Au–S bond lengths are 2.32 Å. S2- is bonded in a 4-coordinate geometry to three equivalent Cr3+ and one Au1+ atom.
DOI: 10.17188/1286609
title: Materials Data on Ho3SnC by Materials Project

description: Ho3SnC is (Cubic) Perovskite structured and crystallizes in the cubic Pm-3m space group. The structure is three-dimensional and consists of one methane molecule and one Ho3Sn framework. In the Ho3Sn framework, Ho is bonded in a linear geometry to two equivalent Sn atoms. Both Ho–Sn bond lengths are 2.79 Å. Sn is bonded to six equivalent Ho atoms to form corner-sharing SnHo6 octahedra. The corner-sharing octahedral tilt angles are 0°.