cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.6570261
title: Elnusa Community Service Data Description of Informants and Interviews

description: The raw data is a brief description of informants in Elnusa village; it will use as the <br> preliminary issue for a community service proposal to be presented to the Ambon <br> State Christian Institute's Research and Community Development Institute (LP2M). <br> As a result, resources written in Bahasa, such as personal information descriptions <br> and interview footage.
description: COPE REGULATION RESTRICTS SELLING AND REUSING THIS DATA FOR INDIVIDUAL AND GROUP INTEREST, SO ANY ENGAGEMENT THAT VIOLATES THIS REGULATION WILL BE CHARGED BY THE LAW AND SCIENTIFIC REGULATION.
DOI: 10.5281/zenodo.6570262
title: Elnusa Community Service Data Description of Informants and Interviews

description: The raw data is a brief description of informants in Elnusa village; it will use as the <br> preliminary issue for a community service proposal to be presented to the Ambon <br> State Christian Institute's Research and Community Development Institute (LP2M). <br> As a result, resources written in Bahasa, such as personal information descriptions <br> and interview footage.
description: COPE REGULATION RESTRICTS SELLING AND REUSING THIS DATA FOR INDIVIDUAL AND GROUP INTEREST, SO ANY ENGAGEMENT THAT VIOLATES THIS REGULATION WILL BE CHARGED BY THE LAW AND SCIENTIFIC REGULATION.
DOI: 10.6084/m9.figshare.21922211.v1
title: Table S1: Physiological selectivity and plant–environment feedbacks during Middle and Late Pennsylvanian plant community transitions

description: List of fossils used in this study, including collection location.
DOI: 10.6084/m9.figshare.21922211
title: Table S1: Physiological selectivity and plant–environment feedbacks during Middle and Late Pennsylvanian plant community transitions

description: List of fossils used in this study, including collection location.
DOI: 10.6084/m9.figshare.21922215
title: Supplementary Material for: Effects of a Sound Intervention on Physical and Emotional Well-Being in Patients with Cancer: A Prospective Randomized Trial

description: <b><i>Aim:</i></b> Cancer remains a disease with a significant impact on morbidity and mortality but also on quality of life. This prospective randomized pilot study investigated the effects of a sound intervention on physical and emotional well-being in outpatients with cancer. <b><i>Methods:</i></b> Two self-applied sound interventions were used for this purpose, either <i>active</i> “music playing” with a body monochord or <i>passive</i> sound intervention with headphones to listen to a given music compilation. Interventions were carried out over a period of 4 weeks for at least 15 min in the evening before bedtime. The following self-assessment questionnaires were completed both at baseline and after 4 weeks to evaluate the response: the Pittsburgh Sleep Quality Index (PSQI), the European Organization for Research and Treatment of Cancer (EORTC) Quality of Life Questionnaire (QLQ-C30), Visual Analogue Scale (VAS) for pain and fatigue, and the Fear of Progression (FoP) questionnaire. Primary endpoint of this exploratory trial was to describe the rate of patients with improvement in at least one dimension without worsening of any other. <b><i>Results:</i></b> 73 patients (29 male, 44 female) were included in the study and randomized to either <i>active</i> (<i>n</i> = 34, 47%) or <i>passive</i> sound intervention (<i>n</i> = 39, 53%). Median age was 52.0 years (range 21–79). Fourteen patients (19%) stated that they were musically active. The sound intervention was carried out on a median of 26 days (range 5–28). A higher percentage of patients in the passive group reached the primary endpoint: <i>n</i> = 15 (39%) versus <i>n</i> = 9 (27%). Response differences in favour of the passive group were seen with the VAS fatigue and with QLQ-30 questionnaires. Overall, an improvement in QLQ-30 questionnaire was seen in 12 patients (31%) in the passive group versus 3 patients (9%). Moreover, sound intervention significantly improved social functioning and shortness of breath in the passive group according to QLQ-C30. Significant improvements were also noticed in the passive group in terms of affective reactions as a domain of the FoP questionnaire. No effects on pain or sleep quality could be observed. <b><i>Conclusion:</i></b> A 4-week self-administered sound intervention was feasible in outpatients suffering from cancer. Using a panel of 5 questionnaires, passive sound interventions appeared to be more likely to positively influence patient-reported outcomes. In particular, a positive impact was documented in social functioning and fatigue.
DOI: 10.6084/m9.figshare.19500829
title: Post-UHP tectonic evolution of the East Kunlun Orogenic Belt, northern Tibetan Plateau: insight from the regional-scale crustal anatexis

description: Extensive crustal anatexis is common during the decompressional exhumation of deeply subducted continental crust and the delamination of a collision‐thickened orogenic lithosphere, indicating that determining the timing of partial melting can provide insights into the possible tectonic evolution during orogenic processes. An integrated study of petrology, zirconology and whole-rock geochemical compositions from migmatites and pegmatites in the Nageng, Langmuri and Wulonggou area of the East Kunlun Orogenic Belt, is presented in this study. The protoliths of these migmatites include Tonian sedimentary rocks and ca. 440 Ma arc-related dioritic rock. Together with previous studies, an extensive crustal anatexis event recorded by anatectic zircons occurred after ca. 410 Ma. In addition, hafnium isotope analyses indicate that the anatectic zircons may or may not inherit their Hf isotope compositions from protolith zircons during partial melting, depending on whether or not the garnet Hf contributes to the Hf budget of anatectic melt. Thus, the most reasonable method to trace the source of granite is to compare the Hf isotope composition of anatectic zircon in migmatite and magmatic zircon in contemporaneous granite. By such method, anatectic melt produced by migmatites in this study could account for both penecontemporaneous A- and I-type granites with high magmatic zircon ε<sub>Hf</sub>(t) values and S-type granites with low magmatic zircon ε<sub>Hf</sub>(t) values. As the extensive crustal anatexis is later than both metamorphic peak and amphibole-facies retrogression of high-pressure and ultrahigh-pressure (HP-UHP) metamorphic rocks, it is reasonable that post-collision orogenic collapse of the collision‐thickened orogenic lithosphere as a result of delamination and asthenospheric upwelling occurred after ca. 410 Ma, which is also supported by contemporaneous granulite-facies metamorphism, molasse deposition, and magmatic events including Xiarihamu mafic-ultramafic intrusions, A-type granites, and mafic dykes formed in the continental rifting setting.
DOI: 10.6084/m9.figshare.19500829.v2
title: Post-UHP tectonic evolution of the East Kunlun Orogenic Belt, northern Tibetan Plateau: insight from the regional-scale crustal anatexis

description: Extensive crustal anatexis is common during the decompressional exhumation of deeply subducted continental crust and the delamination of a collision‐thickened orogenic lithosphere, indicating that determining the timing of partial melting can provide insights into the possible tectonic evolution during orogenic processes. An integrated study of petrology, zirconology and whole-rock geochemical compositions from migmatites and pegmatites in the Nageng, Langmuri and Wulonggou area of the East Kunlun Orogenic Belt, is presented in this study. The protoliths of these migmatites include Tonian sedimentary rocks and ca. 440 Ma arc-related dioritic rock. Together with previous studies, an extensive crustal anatexis event recorded by anatectic zircons occurred after ca. 410 Ma. In addition, hafnium isotope analyses indicate that the anatectic zircons may or may not inherit their Hf isotope compositions from protolith zircons during partial melting, depending on whether or not the garnet Hf contributes to the Hf budget of anatectic melt. Thus, the most reasonable method to trace the source of granite is to compare the Hf isotope composition of anatectic zircon in migmatite and magmatic zircon in contemporaneous granite. By such method, anatectic melt produced by migmatites in this study could account for both penecontemporaneous A- and I-type granites with high magmatic zircon ε<sub>Hf</sub>(t) values and S-type granites with low magmatic zircon ε<sub>Hf</sub>(t) values. As the extensive crustal anatexis is later than both metamorphic peak and amphibole-facies retrogression of high-pressure and ultrahigh-pressure (HP-UHP) metamorphic rocks, it is reasonable that post-collision orogenic collapse of the collision‐thickened orogenic lithosphere as a result of delamination and asthenospheric upwelling occurred after ca. 410 Ma, which is also supported by contemporaneous granulite-facies metamorphism, molasse deposition, and magmatic events including Xiarihamu mafic-ultramafic intrusions, A-type granites, and mafic dykes formed in the continental rifting setting.
DOI: 10.6084/m9.figshare.19500829.v1
title: Post-UHP tectonic evolution of the East Kunlun orogenic belt, northern tibetan plateau: insight from the regional-scale crustal anatexis

description: Extensive crustal anatexis is common during the decompressional exhumation of deeply subducted continental crust and the delamination of a collision‐thickened orogenic lithosphere, indicating that determining the timing of partial melting can provide insights into the possible tectonic evolution during orogenic processes. An integrated study of petrology, zirconology and whole-rock geochemical compositions from migmatites and pegmatites in the Nageng, Langmuri and Wulonggou area of the East Kunlun orogenic belt, is presented in this study. The protoliths of these migmatites include Tonian sedimentary rocks and ca. 440 Ma arc-related dioritic rock. Together with previous studies, an extensive crustal anatexis event recorded by anatectic zircons occurred after ca. 410 Ma. In addition, hafnium isotope analyses indicate that the anatectic zircons may or may not inherit their Hf isotope compositions from protolith zircons during partial melting, depending on whether or not the garnet Hf contributes to the Hf budget of anatectic melt. Thus, the most reasonable method to trace the source of granite is to compare the Hf isotope composition of anatectic zircon in migmatite and magmatic zircon in contemporaneous granite. By such method, anatectic melt produced by migmatites in this study could account for both penecontemporaneous A- and I-type granites with high magmatic zircon ε<sub>Hf</sub>(t) values and S-type granites with low magmatic zircon ε<sub>Hf</sub>(t) values. As the extensive crustal anatexis is later than both metamorphic peak and amphibole-facies retrogression of high-pressure and ultrahigh-pressure (HP-UHP) metamorphic rocks, it is reasonable that post-collision orogenic collapse of the collision‐thickened orogenic lithosphere as a result of delamination and asthenospheric upwelling occurred after ca. 410 Ma, which is also supported by contemporaneous granulite-facies metamorphism, molasse deposition, and magmatic events including Xiarihamu mafic-ultramafic intrusions, A-type granites, and mafic dykes formed in the continental rifting setting.
DOI: 10.6084/m9.figshare.19581477
title: Neoproterozoic pre-collisional events recorded in the Sergipano belt, Southern Borborema Province, West Gondwana

description: The Canindé Domain is crucial for understanding the pre-collisional events in Sergipano Belt, Borborema Province, especially during the Late Stenian/Early Tonian (740–680 Ma). We present thermobarometric, geochronology, and isotopic studies of the metavolcanosedimentary rocks of the Novo Gosto unit. The calculated metamorphic conditions resulted in a range of T: 600–740°C and P: 3.5–10.0 kbar for non-mylonitic amphibolites and values of T: 636–808°C and P: 7.0–12.0 kbar for mylonites, both of amphibolite facies. The minimum metamorphic conditions imprint in these rocks are T: 390°C and P: 2.5 kbar, indicating retrometamorphism in greenschist facies. The probable age of the peak metamorphic event was obtained in zircon rims from a quartzite at 692 ± 8.5 Ma. U-Pb detrital zircon and Nd model ages of the metasedimentary rocks point out Early Tonian as primary source rocks. Subordinate contributions of Mesoproterozoic, Paleoproterozoic, and Neoarchean sources were also recognized. These primary sources are related to Cariris Velhos event rocks, whereas the subordinate sources are from the Pernambuco-Alagoas superterrane. Early Tonian and Late Stenian ages were recognized for the first time in the Canindé Domain, with U-Pb zircon ages of 1005 ± 3 and 989 ± 6 Ma in amphibolites and mylonitized granites, mostly outcropping at the southwestern limit of the area. New ages were also obtained in the Novo Gosto surrounding intrusions: Canindé Layered Gabbroic Intrusion (~718 Ma), Garrote (~715 Ma) and Curralinho/Boa Esperança (~708 Ma) metagranites, and Gentileza metavolcanic rock (~700), which integrate the early pre-collisional magmatism of the Sergipano Belt (~740-680 Ma). Finally, U-Pb zircon ages were obtained in the Poço Redondo Domain, potential source area of the Novo Gosto metasedimentary rocks, resulting in ages of 957 ± 11 and 988 ± 15 Ma. The new data bring perspective to future correlations with adjacent belts and the understanding of the structuration of West Gondwana during the Brasiliano-Pan-African Orogeny.
DOI: 10.6084/m9.figshare.19581477.v1
title: Neoproterozoic pre-collisional events recorded in the Sergipano belt, Southern Borborema Province, West Gondwana

description: The Canindé Domain is crucial for understanding the pre-collisional events in Sergipano Belt, Borborema Province, especially during the Late Stenian/Early Tonian (740–680 Ma). We present thermobarometric, geochronology, and isotopic studies of the metavolcanosedimentary rocks of the Novo Gosto unit. The calculated metamorphic conditions resulted in a range of T: 600–740°C and P: 3.5–10.0 kbar for non-mylonitic amphibolites and values of T: 636–808°C and P: 7.0–12.0 kbar for mylonites, both of amphibolite facies. The minimum metamorphic conditions imprint in these rocks are T: 390°C and P: 2.5 kbar, indicating retrometamorphism in greenschist facies. The probable age of the peak metamorphic event was obtained in zircon rims from a quartzite at 692 ± 8.5 Ma. U-Pb detrital zircon and Nd model ages of the metasedimentary rocks point out Early Tonian as primary source rocks. Subordinate contributions of Mesoproterozoic, Paleoproterozoic, and Neoarchean sources were also recognized. These primary sources are related to Cariris Velhos event rocks, whereas the subordinate sources are from the Pernambuco-Alagoas superterrane. Early Tonian and Late Stenian ages were recognized for the first time in the Canindé Domain, with U-Pb zircon ages of 1005 ± 3 and 989 ± 6 Ma in amphibolites and mylonitized granites, mostly outcropping at the southwestern limit of the area. New ages were also obtained in the Novo Gosto surrounding intrusions: Canindé Layered Gabbroic Intrusion (~718 Ma), Garrote (~715 Ma) and Curralinho/Boa Esperança (~708 Ma) metagranites, and Gentileza metavolcanic rock (~700), which integrate the early pre-collisional magmatism of the Sergipano Belt (~740-680 Ma). Finally, U-Pb zircon ages were obtained in the Poço Redondo Domain, potential source area of the Novo Gosto metasedimentary rocks, resulting in ages of 957 ± 11 and 988 ± 15 Ma. The new data bring perspective to future correlations with adjacent belts and the understanding of the structuration of West Gondwana during the Brasiliano-Pan-African Orogeny.
DOI: 10.6084/m9.figshare.19761421
title: The 1800-1770 Ma Colider silicic large igneous province in the Amazonian craton: crustal evolution using zircon in situ REE compositions, U-Pb ages and Hf isotope analyses

description: This paper presents zircon U-Pb, REE and Hf data for Paleoproterozoic felsic volcanic rocks from the Colíder Group with outcrops in the southwestern Amazonian Craton. It is estimated that these rocks cover an area of 85,000 km<sup>2</sup> with a volume of 2.7 × 10<sup>6</sup> km<sup>3</sup>. The Colíder volcanics are comprised of basalts, andesites and a variety of felsic rocks. The felsic rocks are characterized by rhyolite, andesite and dacite lavas with frequent intercalated pyroclastic and epiclastic deposits. Effusive and pyroclastic rocks are intruded in places by hypabyssal porphyritic rocks. The U-Pb ages obtained for the northeastern domain (1782–1776 Ma) are younger than the ages obtained for the southern domain (1800–1787 Ma). The NE volcanic facies show Hf T<sub>DM</sub> ages between 2.3 and 2.5 Ga (ε<sub>Hf</sub> from +1 to −3) and greater fractionation (Ce/Yb – 0.03–0.06) than the younger facies that has T<sub>DM</sub> from 2.4 to 2.7 Ga (ε<sub>Hf</sub> from −3 to −6) with Ce/Yb values of 0.025–0.030. The Hf isotope compositions, REE contents and U-Pb analyses suggest geographic (north-south) variations in composition, crystallization ages, and T<sub>DM</sub> age zonation during the generation of the Colíder large igneous province.
DOI: 10.6084/m9.figshare.19761421.v1
title: The 1800-1770 Ma Colider silicic large igneous province in the Amazonian craton: crustal evolution using zircon in situ REE compositions, U-Pb ages and Hf isotope analyses

description: This paper presents zircon U-Pb, REE and Hf data for Paleoproterozoic felsic volcanic rocks from the Colíder Group with outcrops in the southwestern Amazonian Craton. It is estimated that these rocks cover an area of 85,000 km<sup>2</sup> with a volume of 2.7 × 10<sup>6</sup> km<sup>3</sup>. The Colíder volcanics are comprised of basalts, andesites and a variety of felsic rocks. The felsic rocks are characterized by rhyolite, andesite and dacite lavas with frequent intercalated pyroclastic and epiclastic deposits. Effusive and pyroclastic rocks are intruded in places by hypabyssal porphyritic rocks. The U-Pb ages obtained for the northeastern domain (1782–1776 Ma) are younger than the ages obtained for the southern domain (1800–1787 Ma). The NE volcanic facies show Hf T<sub>DM</sub> ages between 2.3 and 2.5 Ga (ε<sub>Hf</sub> from +1 to −3) and greater fractionation (Ce/Yb – 0.03–0.06) than the younger facies that has T<sub>DM</sub> from 2.4 to 2.7 Ga (ε<sub>Hf</sub> from −3 to −6) with Ce/Yb values of 0.025–0.030. The Hf isotope compositions, REE contents and U-Pb analyses suggest geographic (north-south) variations in composition, crystallization ages, and T<sub>DM</sub> age zonation during the generation of the Colíder large igneous province.
DOI: 10.5281/zenodo.7185806
title: Data for: Mercury contamination challenges the behavioral response of a keystone species to Arctic climate change

description: Combined effects of multiple, climate change-associated stressors are of mounting concern, especially in Artic ecosystems. Elevated mercury (Hg) exposure in Arctic animals could affect behavioural responses to changes in foraging landscapes linked to climate change, generating interactive effects on behaviour and population resilience. We investigated this hypothesis in the little auk (<em>Alle alle</em>), a keystone Artic seabird. We compiled behavioural data using accelerometers, and quantified blood mercury and environmental conditions (sea surface temperature (SST), sea ice coverage (SIC)) across multiple years. These datasets contain the behavioral, blood Hg and environmental data (SST, SIC) used in our analyses. Details about the datasets are found in the accompanying word document.
DOI: 10.5281/zenodo.7185805
title: Data for: Mercury contamination challenges the behavioral response of a keystone species to Arctic climate change

description: Combined effects of multiple, climate change-associated stressors are of mounting concern, especially in Artic ecosystems. Elevated mercury (Hg) exposure in Arctic animals could affect behavioural responses to changes in foraging landscapes linked to climate change, generating interactive effects on behaviour and population resilience. We investigated this hypothesis in the little auk (<em>Alle alle</em>), a keystone Artic seabird. We compiled behavioural data using accelerometers, and quantified blood mercury and environmental conditions (sea surface temperature (SST), sea ice coverage (SIC)) across multiple years. These datasets contain the behavioral, blood Hg and environmental data (SST, SIC) used in our analyses. Details about the datasets are found in the accompanying word document.
DOI: 10.5281/zenodo.7550320
title: socialmedia

description: Small Bits of Social Media Data
DOI: 10.5281/zenodo.7550319
title: socialmedia

description: Small Bits of Social Media Data
DOI: 10.5281/zenodo.7053991
title: Size spectrum values in stream fish communities

description: Size spectrum values and the main predictors
DOI: 10.5281/zenodo.7053992
title: Size spectrum values in stream fish communities

description: Size spectrum values and the main predictors
DOI: 10.6084/m9.figshare.21922235.v1
title: Mid-Ordovician stratigraphy and volcanism in the Hølonda area, Scandinavian Caledonides: complex tectonomagmatic development following arc–continent collision near the Laurentian margin of Iapetus

description: Table S1. Whole-rock geochemical data (Excel table), including isotopes.
DOI: 10.6084/m9.figshare.21922235
title: Mid-Ordovician stratigraphy and volcanism in the Hølonda area, Scandinavian Caledonides: complex tectonomagmatic development following arc–continent collision near the Laurentian margin of Iapetus

description: Table S1. Whole-rock geochemical data (Excel table), including isotopes.
DOI: 10.6084/m9.figshare.21922238
title: Mid-Ordovician stratigraphy and volcanism in the Hølonda area, Scandinavian Caledonides: complex tectonomagmatic development following arc–continent collision near the Laurentian margin of Iapetus

description: Table S5. U–Pb TIMS data Nonsåsen volcanic unit (Excel table).
DOI: 10.6084/m9.figshare.21922238.v1
title: Mid-Ordovician stratigraphy and volcanism in the Hølonda area, Scandinavian Caledonides: complex tectonomagmatic development following arc–continent collision near the Laurentian margin of Iapetus

description: Table S5. U–Pb TIMS data Nonsåsen volcanic unit (Excel table).
DOI: 10.6084/m9.figshare.21922247.v1
title: Mid-Ordovician stratigraphy and volcanism in the Hølonda area, Scandinavian Caledonides: complex tectonomagmatic development following arc–continent collision near the Laurentian margin of Iapetus

description: Table S6. LA–ICP–MS detrital zircon data (Excel table).
DOI: 10.6084/m9.figshare.21922247
title: Mid-Ordovician stratigraphy and volcanism in the Hølonda area, Scandinavian Caledonides: complex tectonomagmatic development following arc–continent collision near the Laurentian margin of Iapetus

description: Table S6. LA–ICP–MS detrital zircon data (Excel table).
DOI: 10.5519/qd.b18eaeai
title: Query on the Natural History Museum Data Portal (data.nhm.ac.uk) (5416765 records)
DOI: 10.6084/m9.figshare.21922272
title: Student Communications Surveys - meta-analysis

description: Analysis of the student communications survey data