cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.2fa4jy
title: Occurrence Download

description: A dataset containing 2835 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Micrurus fulvius (Linnaeus, 1766)"
 ]
}

 The dataset includes 2835 records from 99 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0098122-230530130749713/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.v2pyty
title: Occurrence Download

description: A dataset containing 78437 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Ardeola bacchus (Bonaparte, 1855)"
 ]
}

 The dataset includes 78437 records from 100 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0378957-210914110416597/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.11805342.v1
title: Additional file 3 of Modulation of volatile compound metabolome and transcriptome in grape berries exposed to sunlight under dry-hot climate

description: Additional file 3: Table S2. Concentrations (μg/kg, mean ± SD, n = 6) of detected volatole compounds in harvested grape berries.
DOI: 10.6084/m9.figshare.11805348
title: Additional file 4 of Modulation of volatile compound metabolome and transcriptome in grape berries exposed to sunlight under dry-hot climate

description: Additional file 4: Table S3. Common differentially expressed genes between LR-V and LM-V.
DOI: 10.6084/m9.figshare.11805348.v1
title: Additional file 4 of Modulation of volatile compound metabolome and transcriptome in grape berries exposed to sunlight under dry-hot climate

description: Additional file 4: Table S3. Common differentially expressed genes between LR-V and LM-V.
DOI: 10.6084/m9.figshare.20193930
title: Additional file 2 of Genetic prion diseases presenting as frontotemporal dementia: clinical features and diagnostic challenge

description: Additional file 2: Table S1. The central findings of each patient.
DOI: 10.6084/m9.figshare.20193930.v1
title: Additional file 2 of Genetic prion diseases presenting as frontotemporal dementia: clinical features and diagnostic challenge

description: Additional file 2: Table S1. The central findings of each patient.
DOI: 10.6084/m9.figshare.11805354
title: Additional file 5 of Modulation of volatile compound metabolome and transcriptome in grape berries exposed to sunlight under dry-hot climate

description: Additional file 5: Table S4. KEGG enrichment analysis of differentially expressed genes specially induced by LR-V.
DOI: 10.6084/m9.figshare.11805354.v1
title: Additional file 5 of Modulation of volatile compound metabolome and transcriptome in grape berries exposed to sunlight under dry-hot climate

description: Additional file 5: Table S4. KEGG enrichment analysis of differentially expressed genes specially induced by LR-V.
DOI: 10.6084/m9.figshare.11805357
title: Additional file 6 of Modulation of volatile compound metabolome and transcriptome in grape berries exposed to sunlight under dry-hot climate

description: Additional file 6: Table S5. KEGG enrichment analysis of differentially expressed genes specially induced by LM-V.
DOI: 10.5281/zenodo.10627344
title: Data for "Using shelfedge transport composition and sensitivity experiments to understand processes driving sea level on the Northwest European Shelf"

description: Dataset in support of  and as described in "Using shelfedge transport composition and sensitivity experiments to understand processes driving sea level on the Northwest European Shelf" submitted to JGR:Oceans 11/2023.

Processed data using output from experiments conducted using the AMM7 configuration of NEMO. Monthlys means for year 2006-2015.

exp_sl_residuals_yXX.nc include SSH, Manometric and Steric components of dynamic sea level with linear trend, seasonal and 12-month rolling mean removed.

exp_sl_12m_trends_yXX.nc include 12-month rolling mean of detrended SSH, Manometric and Steric components of dynamic sea level.

along_shelfbreak_windstress_2006_15.nc is the integral of along-shore wind signal as described in the manuscript

exp_vol_tran_2d.nc and exp_vol_tran_3d.nc are cross-shelfedge (200 m isobath) transports as described in the manuscript
DOI: 10.6084/m9.figshare.11805357.v1
title: Additional file 6 of Modulation of volatile compound metabolome and transcriptome in grape berries exposed to sunlight under dry-hot climate

description: Additional file 6: Table S5. KEGG enrichment analysis of differentially expressed genes specially induced by LM-V.
DOI: 10.6084/m9.figshare.11805363
title: Additional file 7 of Modulation of volatile compound metabolome and transcriptome in grape berries exposed to sunlight under dry-hot climate

description: Additional file 7: Table S6. Differentially expressed genes between LM-V and LR-V. The highlighted genes are common DEGs that all appeared at the three tested stages.
DOI: 10.6084/m9.figshare.11805363.v1
title: Additional file 7 of Modulation of volatile compound metabolome and transcriptome in grape berries exposed to sunlight under dry-hot climate

description: Additional file 7: Table S6. Differentially expressed genes between LM-V and LR-V. The highlighted genes are common DEGs that all appeared at the three tested stages.
DOI: 10.6084/m9.figshare.11805366
title: Additional file 8 of Modulation of volatile compound metabolome and transcriptome in grape berries exposed to sunlight under dry-hot climate

description: Additional file 8: Table S7. Genes in each WGCNA module.
DOI: 10.6084/m9.figshare.11805366.v1
title: Additional file 8 of Modulation of volatile compound metabolome and transcriptome in grape berries exposed to sunlight under dry-hot climate

description: Additional file 8: Table S7. Genes in each WGCNA module.
DOI: 10.6084/m9.figshare.20193960.v1
title: Additional file 2 of Deep oncopanel sequencing reveals within block position-dependent quality degradation in FFPE processed samples

description: Additional file 2. A multiple tab Microsoft Excel file of FFPE experiment information, extensive quality check data and analysis results for FFPE samples, and analysis results for free DNA samples.
DOI: 10.6084/m9.figshare.20193960
title: Additional file 2 of Deep oncopanel sequencing reveals within block position-dependent quality degradation in FFPE processed samples

description: Additional file 2. A multiple tab Microsoft Excel file of FFPE experiment information, extensive quality check data and analysis results for FFPE samples, and analysis results for free DNA samples.
DOI: 10.6084/m9.figshare.20193966
title: Additional file 3 of Deep oncopanel sequencing reveals within block position-dependent quality degradation in FFPE processed samples

description: Additional file 3. List of known variants for four participating oncology panels.
DOI: 10.6084/m9.figshare.11805465
title: Additional file 2 of circRIP2 accelerates bladder cancer progression via miR-1305/Tgf-β2/smad3 pathway

description: Additional file 2: Figure S2. Tgf-β2 inhibitor revered cancer promotive role of circRIP2 in bladder cancer cells in vitro. A,B. CCK8 assay was performed to detect cell viability of bladder cancer cells; C,D. Cell potential to replicate and self-renew was reflected by clone formation; E,F. Rate of wound healing assay showed cell potential of migration; scale bar: 100μm. G,H,I,J,K. Trans-well migration and matrigel invasion assay showed cell potential of migration and invasion of bladder cancer cells; scale bar: 25μm.
DOI: 10.6084/m9.figshare.11805465.v1
title: Additional file 2 of circRIP2 accelerates bladder cancer progression via miR-1305/Tgf-β2/smad3 pathway

description: Additional file 2: Figure S2. Tgf-β2 inhibitor revered cancer promotive role of circRIP2 in bladder cancer cells in vitro. A,B. CCK8 assay was performed to detect cell viability of bladder cancer cells; C,D. Cell potential to replicate and self-renew was reflected by clone formation; E,F. Rate of wound healing assay showed cell potential of migration; scale bar: 100μm. G,H,I,J,K. Trans-well migration and matrigel invasion assay showed cell potential of migration and invasion of bladder cancer cells; scale bar: 25μm.
DOI: 10.6084/m9.figshare.12854087
title: Late Palaeozoic–Early Mesozoic southward subduction of the Mongol–Okhotsk oceanic slab: geochronological, geochemical, and Hf isotopic evidence from intrusive rocks in the Erguna Massif (NE China)

description: This study presents new zircon LA-ICP-MS U–Pb ages, zircon Hf isotopes, and whole-rock geochemical compositions for Late Palaeozoic–Early Mesozoic intrusive rocks from the Erguna Massif, Northeast China. Zircon U–Pb dating results indicate that the intrusive rocks were emplaced during the Late Permian–Middle Triassic (ca. 256–234 Ma) and Late Triassic (ca. 210 Ma) in the western and eastern parts of the Erguna Massif, respectively. The Late Permian gabbros and quartz monzodiorites display enrichment in Rb and K, but are depleted in Nb, Ta, and Ti. Their ε<sub>Hf</sub>(t) values (+5.1 to +9.1 and −0.2 to +3.7, respectively) and one-stage Hf model ages (T<sub>DM1</sub> = 544–704 Ma and 764–889 Ma, respectively) indicate that they might be derived from the reworking of the Neoproterozoic lithospheric mantle that was metasomatised by subduction-related fluids. The Late Permian–Early Middle Triassic quartz monzonites, monzogranites, and syenogranites display variable enrichment of rare earth elements (REEs) and large ion lithophile elements (LILEs). They have ε<sub>Hf</sub>(t) values varying from −5.7 to +2.7 with two-stage Hf model ages (T<sub>DM2</sub>) of 1.09–1.69 Ga, implying that they possibly originated from the Mesoproterozoic continental crust. The Late Triassic syenogranites show geochemical signatures of A2-type granites with various enrichment in LILEs and LREEs and depletion in Nb, Ta, and Ti. Combined with regional geological evidence, we conclude that Late Permian to Late Triassic igneous rocks on both sides of the Mongol–Okhotsk suture belt record an active continental margin environment associated with the ongoing bidirectional subduction of the Mongol–Okhotsk Ocean. The eastern Erguna Massif and Xing’an Massif were likely located in a back-arc setting at least since ca. 216 Ma, with long-term southward subduction of the Mongol–Okhotsk oceanic slab spanning from the Late Permian–Early Jurassic.
DOI: 10.6084/m9.figshare.12854087.v1
title: Late Palaeozoic–Early Mesozoic southward subduction of the Mongol–Okhotsk oceanic slab: geochronological, geochemical, and Hf isotopic evidence from intrusive rocks in the Erguna Massif (NE China)

description: This study presents new zircon LA-ICP-MS U–Pb ages, zircon Hf isotopes, and whole-rock geochemical compositions for Late Palaeozoic–Early Mesozoic intrusive rocks from the Erguna Massif, Northeast China. Zircon U–Pb dating results indicate that the intrusive rocks were emplaced during the Late Permian–Middle Triassic (ca. 256–234 Ma) and Late Triassic (ca. 210 Ma) in the western and eastern parts of the Erguna Massif, respectively. The Late Permian gabbros and quartz monzodiorites display enrichment in Rb and K, but are depleted in Nb, Ta, and Ti. Their ε<sub>Hf</sub>(t) values (+5.1 to +9.1 and −0.2 to +3.7, respectively) and one-stage Hf model ages (T<sub>DM1</sub> = 544–704 Ma and 764–889 Ma, respectively) indicate that they might be derived from the reworking of the Neoproterozoic lithospheric mantle that was metasomatised by subduction-related fluids. The Late Permian–Early Middle Triassic quartz monzonites, monzogranites, and syenogranites display variable enrichment of rare earth elements (REEs) and large ion lithophile elements (LILEs). They have ε<sub>Hf</sub>(t) values varying from −5.7 to +2.7 with two-stage Hf model ages (T<sub>DM2</sub>) of 1.09–1.69 Ga, implying that they possibly originated from the Mesoproterozoic continental crust. The Late Triassic syenogranites show geochemical signatures of A2-type granites with various enrichment in LILEs and LREEs and depletion in Nb, Ta, and Ti. Combined with regional geological evidence, we conclude that Late Permian to Late Triassic igneous rocks on both sides of the Mongol–Okhotsk suture belt record an active continental margin environment associated with the ongoing bidirectional subduction of the Mongol–Okhotsk Ocean. The eastern Erguna Massif and Xing’an Massif were likely located in a back-arc setting at least since ca. 216 Ma, with long-term southward subduction of the Mongol–Okhotsk oceanic slab spanning from the Late Permian–Early Jurassic.
DOI: 10.6084/m9.figshare.12854090
title: Geochronology and geochemistry of late Jurassic–Early Cretaceous volcanic rocks in the southern Great Xing’an range, NE China: constraints for late Mesozoic tectono-magmatic evolution

description: Late Mesozoic volcanic rocks are widespread in the Great Xing’an Range (GXR), Northeast (NE) China. However, details of the tectono-magmatic evolution during the Late Mesozoic are poorly understood. In this paper, new zircon U–Pb, Lu–Hf, and whole-rock geochemical data from Late Mesozoic volcanics in the southern GXR, are used to further constrain the tectono-magmatic evolution of the region. Late Mesozoic magmatism in the GXR, eastern Mongolia and southern Transbaikalia occurred during the Early Cretaceous (120–140 Ma) and Late Jurassic (150–163 Ma) periods. Late Jurassic trachyandesites-trachytes show a low rare earth element and moderate light rare earth element (LREE) enrichment with no Eu anomalies. Early Cretaceous trachytes are characterized by an LREE enrichment and negative Eu anomalies. Contemporaneous rhyolites exhibit a significant LREE enrichment, A–type granitoid affinity, and pronounced negative Eu anomalies. Different negative Nb, Ta, and Ti anomalies, and positive zircon ε<sub>Hf</sub>(t) values, indicate that the ~160 Ma trachyandesites-trachytes are derived from partial melting of the lithospheric mantle that was metasomatized by subduction-related fluids. The ~125 Ma trachytes and rhyolites were possibly generated by partial melting of the accreted Meso-Neoproterozoic lower crust. New and previously published geochemical, isotopic and geochronological data from the southern GXR, eastern Mongolia and East-Transbaikalia, suggest that Late Jurassic–Early Cretaceous volcanism in the southern GXR occurred during the post-collisional extension after the closure of the Mongol–Okhotsk Ocean.
DOI: 10.6084/m9.figshare.12854090.v1
title: Geochronology and geochemistry of late Jurassic–Early Cretaceous volcanic rocks in the southern Great Xing’an range, NE China: constraints for late Mesozoic tectono-magmatic evolution

description: Late Mesozoic volcanic rocks are widespread in the Great Xing’an Range (GXR), Northeast (NE) China. However, details of the tectono-magmatic evolution during the Late Mesozoic are poorly understood. In this paper, new zircon U–Pb, Lu–Hf, and whole-rock geochemical data from Late Mesozoic volcanics in the southern GXR, are used to further constrain the tectono-magmatic evolution of the region. Late Mesozoic magmatism in the GXR, eastern Mongolia and southern Transbaikalia occurred during the Early Cretaceous (120–140 Ma) and Late Jurassic (150–163 Ma) periods. Late Jurassic trachyandesites-trachytes show a low rare earth element and moderate light rare earth element (LREE) enrichment with no Eu anomalies. Early Cretaceous trachytes are characterized by an LREE enrichment and negative Eu anomalies. Contemporaneous rhyolites exhibit a significant LREE enrichment, A–type granitoid affinity, and pronounced negative Eu anomalies. Different negative Nb, Ta, and Ti anomalies, and positive zircon ε<sub>Hf</sub>(t) values, indicate that the ~160 Ma trachyandesites-trachytes are derived from partial melting of the lithospheric mantle that was metasomatized by subduction-related fluids. The ~125 Ma trachytes and rhyolites were possibly generated by partial melting of the accreted Meso-Neoproterozoic lower crust. New and previously published geochemical, isotopic and geochronological data from the southern GXR, eastern Mongolia and East-Transbaikalia, suggest that Late Jurassic–Early Cretaceous volcanism in the southern GXR occurred during the post-collisional extension after the closure of the Mongol–Okhotsk Ocean.
DOI: 10.6084/m9.figshare.12854093
title: Origin and tectonic implications of Late Jurassic high-Mg diorites along the Bangong-Nujiang suture zone, Tibet

description: The Shiquanhe-Num Co ophiolitic mélange belt (SNOB) is one of two such belts along the Bangong-Nujiang suture zone (BNSZ) separating the Lhasa and Qiantang terranes of central Tibet. This study reports new geochronological, petrological and geochemical data for high-Mg dioritic dikes intruding the Shiquanhe ophiolitic peridotite. Based on LA-ICP-MS zircon U–Pb dating, dioritic dikes yield a Late Jurassic age of 162.8 ± 1.3 Ma. These are high-Mg diorites (53.0%–56.8% SiO<sub>2</sub>, 7.07%–8.82% MgO) with moderate TiO<sub>2</sub> (0.95%–1.01%), high K<sub>2</sub>O+Na<sub>2</sub>O (6.02%–8.01%), and high contents of Cr (150–182 ppm), Ni (91–145 ppm) and Th (2.8–5.9 ppm). They are very similar to sanukites of the Setouchi volcanic rock belt (SW Japan). Shiquanhe diorites have high Sr/Y ratios (up to 41.3), distinct positive Pb anomalies, negative Nb anomalies and continental crust-like trace element patterns without negative Eu anomalies (average Eu/Eu* = 0.96). These geochemical characteristics indicate that Shiquanhe diorities were derived by partial melting of mantle peridotite as a result of interaction with hydrous melts of subducted sediments. Similar high-Mg magmas are common in the early evolution of a new subduction zone. Integrated with field observations and results from other studies of Late Jurassic high-Mg andesites and diorites along the SNOB, we argue that the Shiquanhe high-Mg diorites formed at an early stage of northward subduction of the Bangong-Nujiang Tethys ocean (BNO) beneath the Qiangtang terrane. Therefore, these results provide critical constraints on the Jurassic tectonic evolution of the Shiquanhe-Num Co ophiolitic mélange belt and are significant for understanding the evolution of the BNO.
DOI: 10.6084/m9.figshare.12854093.v1
title: Origin and tectonic implications of Late Jurassic high-Mg diorites along the Bangong-Nujiang suture zone, Tibet

description: The Shiquanhe-Num Co ophiolitic mélange belt (SNOB) is one of two such belts along the Bangong-Nujiang suture zone (BNSZ) separating the Lhasa and Qiantang terranes of central Tibet. This study reports new geochronological, petrological and geochemical data for high-Mg dioritic dikes intruding the Shiquanhe ophiolitic peridotite. Based on LA-ICP-MS zircon U–Pb dating, dioritic dikes yield a Late Jurassic age of 162.8 ± 1.3 Ma. These are high-Mg diorites (53.0%–56.8% SiO<sub>2</sub>, 7.07%–8.82% MgO) with moderate TiO<sub>2</sub> (0.95%–1.01%), high K<sub>2</sub>O+Na<sub>2</sub>O (6.02%–8.01%), and high contents of Cr (150–182 ppm), Ni (91–145 ppm) and Th (2.8–5.9 ppm). They are very similar to sanukites of the Setouchi volcanic rock belt (SW Japan). Shiquanhe diorites have high Sr/Y ratios (up to 41.3), distinct positive Pb anomalies, negative Nb anomalies and continental crust-like trace element patterns without negative Eu anomalies (average Eu/Eu* = 0.96). These geochemical characteristics indicate that Shiquanhe diorities were derived by partial melting of mantle peridotite as a result of interaction with hydrous melts of subducted sediments. Similar high-Mg magmas are common in the early evolution of a new subduction zone. Integrated with field observations and results from other studies of Late Jurassic high-Mg andesites and diorites along the SNOB, we argue that the Shiquanhe high-Mg diorites formed at an early stage of northward subduction of the Bangong-Nujiang Tethys ocean (BNO) beneath the Qiangtang terrane. Therefore, these results provide critical constraints on the Jurassic tectonic evolution of the Shiquanhe-Num Co ophiolitic mélange belt and are significant for understanding the evolution of the BNO.
DOI: 10.6084/m9.figshare.12854105
title: Mesozoic crustal thickness variations and related hydrothermal Cu mineralization in eastern Heilongjiang and Jilin Provinces, China

description: Ocean-continent subduction drives sequential geologic events, including upwelling of mantle magmas and delamination of thickened lithosphere, which lead to crustal thickness variations and metallic enrichment or depletion at crustal roots. This paper estimates the crustal thickness in eastern Heilongjiang and Jilin Provinces based on La/Yb ratios of crust-derived I-type granites formed by Mesozoic Palaeo-Pacific slab westward subduction beneath Eurasia and assesses the related hydrothermal Cu mineralization. During the flat subduction phase (210–160 Ma), the continental crust dramatically thickened from 32 ± 6 km to 58 ± 6 km, indicating that much mafic magma accumulated under the ancient crust; notably, 210–177 Ma granitoids were generated in the thinner crust because of their normal arc natures, and subsequent remelting of mafic cumulates in the thicker crust formed adakitic magmas (~177–165 Ma) with low MgO (0.03–1.38 wt.%). From 140 to 95 Ma, the steep subduction of the dense slab drove regional decompression and consequent delamination and thinning of the lithosphere from ~58 km to 23 km, inducing explosive volcanic activity along with limited hydrothermal Cu deposition. Most Cu mineralization was associated with normal arc magmas; therefore, we speculate that two key factors were responsible for the small volume of Cu deposition: (1) thinner crust under an extensional setting failed to suppress voluminous pyroclastic eruptions, causing the dissipation of volatiles and preventing a large magma reservoir with long-lasting shallow differentiation; (2) root removal of thickened crust led large volumes of sulphide cumulates, if present, to founder into the mantle rather than remain in the crust, which greatly depleted Cu in the ascending melts.
DOI: 10.6084/m9.figshare.12854105.v1
title: Mesozoic crustal thickness variations and related hydrothermal Cu mineralization in eastern Heilongjiang and Jilin Provinces, China

description: Ocean-continent subduction drives sequential geologic events, including upwelling of mantle magmas and delamination of thickened lithosphere, which lead to crustal thickness variations and metallic enrichment or depletion at crustal roots. This paper estimates the crustal thickness in eastern Heilongjiang and Jilin Provinces based on La/Yb ratios of crust-derived I-type granites formed by Mesozoic Palaeo-Pacific slab westward subduction beneath Eurasia and assesses the related hydrothermal Cu mineralization. During the flat subduction phase (210–160 Ma), the continental crust dramatically thickened from 32 ± 6 km to 58 ± 6 km, indicating that much mafic magma accumulated under the ancient crust; notably, 210–177 Ma granitoids were generated in the thinner crust because of their normal arc natures, and subsequent remelting of mafic cumulates in the thicker crust formed adakitic magmas (~177–165 Ma) with low MgO (0.03–1.38 wt.%). From 140 to 95 Ma, the steep subduction of the dense slab drove regional decompression and consequent delamination and thinning of the lithosphere from ~58 km to 23 km, inducing explosive volcanic activity along with limited hydrothermal Cu deposition. Most Cu mineralization was associated with normal arc magmas; therefore, we speculate that two key factors were responsible for the small volume of Cu deposition: (1) thinner crust under an extensional setting failed to suppress voluminous pyroclastic eruptions, causing the dissipation of volatiles and preventing a large magma reservoir with long-lasting shallow differentiation; (2) root removal of thickened crust led large volumes of sulphide cumulates, if present, to founder into the mantle rather than remain in the crust, which greatly depleted Cu in the ascending melts.