cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.15113139
title: Temperate macroalgae BSi concentrations

description: This is a dataset for biogenic silica concentrations (%BSi by dry weight) from macroalgae from two temperate estuaries: Waquoit Bay (MA, USA) and Narragansett Bay (RI, USA). Additional data on %C, del13C, and collection information is also provided. <br>The del13C data were previously published: Oczkowski, A., Schmidt, C., Santos, E., Miller, K., Hanson, A., Cobb, D., Krumholz, J., Pimenta, A., Heffner, L., Robinson, S. and Chaves, J., 2018. How the distribution of anthropogenic nitrogen has changed in Narragansett Bay (RI, USA) following major reductions in nutrient loads. <i>Estuaries and Coasts</i>, <i>41</i>(8), pp.2260-2276.
DOI: 10.6084/m9.figshare.15113139.v1
title: Temperate macroalgae BSi concentrations

description: This is a dataset for biogenic silica concentrations (%BSi by dry weight) from macroalgae from two temperate estuaries: Waquoit Bay (MA, USA) and Narragansett Bay (RI, USA). Additional data on %C, del13C, and collection information is also provided. <br>The del13C data were previously published: Oczkowski, A., Schmidt, C., Santos, E., Miller, K., Hanson, A., Cobb, D., Krumholz, J., Pimenta, A., Heffner, L., Robinson, S. and Chaves, J., 2018. How the distribution of anthropogenic nitrogen has changed in Narragansett Bay (RI, USA) following major reductions in nutrient loads. <i>Estuaries and Coasts</i>, <i>41</i>(8), pp.2260-2276.
DOI: 10.23729/115c138d-145f-4d96-b53a-47bdbe7a8ecf
title: Combining instrument inversions for sub-10 nm aerosol number size-distribution measurements: package aeroinverter and research data

description: Aeroinverter package for python and julia aerosol size-distribution inversions corresponding to the GitLab repository https://version.helsinki.fi/stolzenb/aeroinverter on August 17th 2021, the submission date of the revised version to the Journal of Aerosol Science.
DOI: 10.6073/pasta/cb0787f0816305ab9a0d620f61e7d43f
title: Long-Term Field Research Sites at Harvard Forest since 1937

description: The Harvard Forest is an iconic field station, hosting hundreds of field-based studies since it was founded in 1907. Site-based, long-term research increased sharply starting in 1988, when Harvard Forest became a Long-Term Ecological Research Site. This dataset documents the locations of most long-term research studies initiated since 1988; a few studies that began earlier and are still active are also included. Short-term studies, or studies that focus on sampling individual organisms, are not included.
DOI: 10.17028/rd.lboro.15180207
title: Supplementary Information files for The impact of news consumption on anti-immigration attitudes and populist party support in a changing media ecology

description: Supplementary Information files for The impact of news consumption on anti-immigration attitudes and populist party support in a changing media ecology<br>Democracies around the world are facing a rising wave of right-wing populism and new nationalism, which often relies on strategic exploitation of anti-immigration sentiments. While media have long been acknowledged as important channels of anti-immigration rhetoric, the evidence of the actual impact of news consumption on attitudes tomigration and support for populist parties is still inconclusive, and largely limited to pre-digital media ecologies. Combining a representative twowave panel survey (N=819), digital tracking of real-time electronic measurement of television, radio and online media exposure, and an analysis of news content, this study explores the effect of news consumption on anti-immigration attitudes and electoral behaviour during the EP2019 election campaign in the Czech Republic. Our analysis reveals that being exposed to news about migration – particularly on websites and on commercial television stations – increases the likelihood of voting for populist parties, while exposure to public service media leads to less negative attitudes towards immigration. At the same time, being exposed to more news sources intensifies, rather than reduces, anti-immigrant attitudes. This result challenges the assumption that a more diverse news media diet could serve as an antidote to selective exposure and “echo chambers”, commonly linked with radicalization of political views.
DOI: 10.17028/rd.lboro.15180207.v1
title: Supplementary Information files for The impact of news consumption on anti-immigration attitudes and populist party support in a changing media ecology

description: Supplementary Information files for The impact of news consumption on anti-immigration attitudes and populist party support in a changing media ecology<br>Democracies around the world are facing a rising wave of right-wing populism and new nationalism, which often relies on strategic exploitation of anti-immigration sentiments. While media have long been acknowledged as important channels of anti-immigration rhetoric, the evidence of the actual impact of news consumption on attitudes tomigration and support for populist parties is still inconclusive, and largely limited to pre-digital media ecologies. Combining a representative twowave panel survey (N=819), digital tracking of real-time electronic measurement of television, radio and online media exposure, and an analysis of news content, this study explores the effect of news consumption on anti-immigration attitudes and electoral behaviour during the EP2019 election campaign in the Czech Republic. Our analysis reveals that being exposed to news about migration – particularly on websites and on commercial television stations – increases the likelihood of voting for populist parties, while exposure to public service media leads to less negative attitudes towards immigration. At the same time, being exposed to more news sources intensifies, rather than reduces, anti-immigrant attitudes. This result challenges the assumption that a more diverse news media diet could serve as an antidote to selective exposure and “echo chambers”, commonly linked with radicalization of political views.
DOI: 10.5285/64a60b58-6de5-4909-a321-91ca90bb9251
title: Volcanological data for the Echo Canyon Eruption, Ascension Island, South Atlantic: size, abundance, density, vesicle texture and composition of pumice and lava clasts, collected between 2018 and 2020

description: Compositional and volcanological data from a small-volume explosive-effusive volcanic eruption on Ascension Island, South Atlantic. Multiple samples of pumice and lava spanning the whole eruption sequence were collected from several locations in the area surrounding NE-Bay on Ascension Island. This dataset includes compositional, clast size, abundance, clast density and vesicle texture data for the products of the Echo Canyon eruption. Data was collected between the 12th June 2018 and the 30th August 2020 on Ascension Island and at the University of East Anglia, UK. Compositional data was collected using X-ray fluorescence (XRF), density of pumice clasts using the Archimedes suspension method and textural data by visual inspection of sample vesicle shape and size, all at the University of East Anglia, UK. Clast size and abundance was semi-quantitatively estimated in the field on Ascension Island and later checked against photographs. This data provides a framework through which changes to eruption style were reconstructed and is useful to any persons wishing to study or compare small-volume eruption deposits which record eruptive transitions. The data supports and forms the basis of Davies et al., (2021) (DOI : 10.1007/s00445-021-01480-1) and forms part of B V Davies’ Natural Environment Research Council funded PhD project investigating eruption controls on Ascension Island. Bridie V Davies collected and interpreted the data with assistance from Jane H Scarrow and Richard J Brown on Ascension Island, and Jenni Barclay at the University of East Anglia, Bertrand Leze performed XRF on prepared samples. All data collected is included in this resource.
DOI: 10.6084/m9.figshare.12854132.v1
title: Late Neoproterozoic evolution of the southwestern margin of the Siberian Craton: evidence from sedimentology, geochronology and detrital zircon analysis

description: Sedimentary successions and igneous rocks exposed in Eastern Sayan provide an important geological record on the tectonic evolution of the southwestern margin of the Siberian Craton during the Neoproterozoic. Here we present sedimentological and detrital zircon provenance data from key stratigraphic units, complemented by a new U-Pb zircon age of 718 ± 6 Ma from the mafic Nersa magmatic complex. Sedimentological and provenance data from the lower part of the stratigraphic succession (Karagasy Group) show that these rocks were deposited in a passive margin setting after 750 Ma and before the emplacement of the Nersa magmatic complex. The upper part of the stratigraphic succession (Oselok Group) consists of Cryogenian and Ediacaran glaciogenic deposits and associated cap carbonates, overlain by mid to late Ediacaran sequences of dominantly shallow-marine and fluvial siliciclastic rocks. Provenance data indicate that rocks from the Tuva-Mongolia and Zavkhan terranes provided a significant input of detrital material into the sedimentary basin that was the source of the glacial deposits. Orogenic processes during the late Ediacaran (<i>ca</i> 570–540 Ma) in Eastern Sayan were likely associated with the accretion of the Tuva-Mongolia terrane, as indicated by the detrital zircon data.
DOI: 10.6084/m9.figshare.12854132
title: Late Neoproterozoic evolution of the southwestern margin of the Siberian Craton: evidence from sedimentology, geochronology and detrital zircon analysis

description: Sedimentary successions and igneous rocks exposed in Eastern Sayan provide an important geological record on the tectonic evolution of the southwestern margin of the Siberian Craton during the Neoproterozoic. Here we present sedimentological and detrital zircon provenance data from key stratigraphic units, complemented by a new U-Pb zircon age of 718 ± 6 Ma from the mafic Nersa magmatic complex. Sedimentological and provenance data from the lower part of the stratigraphic succession (Karagasy Group) show that these rocks were deposited in a passive margin setting after 750 Ma and before the emplacement of the Nersa magmatic complex. The upper part of the stratigraphic succession (Oselok Group) consists of Cryogenian and Ediacaran glaciogenic deposits and associated cap carbonates, overlain by mid to late Ediacaran sequences of dominantly shallow-marine and fluvial siliciclastic rocks. Provenance data indicate that rocks from the Tuva-Mongolia and Zavkhan terranes provided a significant input of detrital material into the sedimentary basin that was the source of the glacial deposits. Orogenic processes during the late Ediacaran (<i>ca</i> 570–540 Ma) in Eastern Sayan were likely associated with the accretion of the Tuva-Mongolia terrane, as indicated by the detrital zircon data.
DOI: 10.6084/m9.figshare.12854135.v1
title: New ages from the Shackleton Glacier area and their context in the regional tectonomagmatic evolution of the Ross orogen of Antarctica

description: The Ross orogenic belt in Antarctica is one of several Neoproterozoic-early Palaeozoic orogens that crisscrossed Gondwana and are associated with Gondwana’s assembly. We present new age data from the Queen Maud Mountains, Ross orogen, from areas that hitherto have lacked precise ages from the local plutonic rocks. The zircon U-Pb igneous crystallization ages (n = 7) and a hornblende <sup>40</sup>Ar/<sup>39</sup>Ar cooling age (n = 1) constrain plutonism to primarily lie within the Cambrian to Ordovician. Cumulative zircon U-Pb crystallization age data yield polymodal age distributions (516 Ma, 506–502 Ma, and 488 Ma age peaks) that are similar to other areas of the Queen Maud-Horlick Mountains, consistent with regional magmatic flare-ups along the Pacific-Gondwana margin during these times. The ages of deformed plutons constrain deformation to the Cambrian (Series 2) to Ordovician (Lower), with some regions indicating a transition to post-tectonic magmatism and cooling at ~509-470 Ma. Collectively, the data indicate that the Queen Maud-Horlick Mountains share a similar petrotectonic history with other regions of the Pacific-Gondwana margin, providing new evidence that this tectonostratigraphic province is part of and not exotic to the larger igneous-sedimentary successions developed in the peri-Gondwana realm under a broadly convergent margin setting.
DOI: 10.6084/m9.figshare.12854138.v1
title: A unique blueschist facies metapelite with Mg-rich chloritoid from the Badajoz-Córdoba Unit (SW Iberian Massif): correlation of Late Devonian high-pressure belts along the Variscan Orogen

description: The Badajoz-Córdoba Unit (BCU, SW Iberian Massif) is a Variscan high-P unit mainly constituted by metapelites, metagreywackes, orthogneisses, Grt-amphibolites, and retrogressed eclogites (high-P metamorphism at c. 377 Ma). Discovery of rare metapelites with well-preserved high-P mineral assemblages, including large garnets up to 1 cm in diameter with abundant inclusions, chloritoid (up to X<sub>Mg</sub> = 0.32), kyanite, staurolite, chlorite, phengite (up to Si = 3.16 apfu), paragonite, margarite, and rutile, allows detailed determination of the tectonothermal evolution of the unit. Pseudosection modelling of representative samples indicates that this mineral assemblage formed in blueschist facies (near eclogite facies transition) at P conditions higher than 20 kbar at c. 525°C and that it underwent a subsequent severe exhumation and moderate heating. The lithological composition of the BCU, the age of high-P metamorphism and the characteristics of the high-P mineral assemblages are similar to those found in other high-P and low to intermediate-T units of the Variscan Orogen. All these units form part of a single blueschist-eclogite facies metamorphic belt formed during Late Devonian subduction of the external margin of Gondwana.
DOI: 10.6084/m9.figshare.12854138
title: A unique blueschist facies metapelite with Mg-rich chloritoid from the Badajoz-Córdoba Unit (SW Iberian Massif): correlation of Late Devonian high-pressure belts along the Variscan Orogen

description: The Badajoz-Córdoba Unit (BCU, SW Iberian Massif) is a Variscan high-P unit mainly constituted by metapelites, metagreywackes, orthogneisses, Grt-amphibolites, and retrogressed eclogites (high-P metamorphism at c. 377 Ma). Discovery of rare metapelites with well-preserved high-P mineral assemblages, including large garnets up to 1 cm in diameter with abundant inclusions, chloritoid (up to X<sub>Mg</sub> = 0.32), kyanite, staurolite, chlorite, phengite (up to Si = 3.16 apfu), paragonite, margarite, and rutile, allows detailed determination of the tectonothermal evolution of the unit. Pseudosection modelling of representative samples indicates that this mineral assemblage formed in blueschist facies (near eclogite facies transition) at P conditions higher than 20 kbar at c. 525°C and that it underwent a subsequent severe exhumation and moderate heating. The lithological composition of the BCU, the age of high-P metamorphism and the characteristics of the high-P mineral assemblages are similar to those found in other high-P and low to intermediate-T units of the Variscan Orogen. All these units form part of a single blueschist-eclogite facies metamorphic belt formed during Late Devonian subduction of the external margin of Gondwana.
DOI: 10.6084/m9.figshare.12854135
title: New ages from the Shackleton Glacier area and their context in the regional tectonomagmatic evolution of the Ross orogen of Antarctica

description: The Ross orogenic belt in Antarctica is one of several Neoproterozoic-early Palaeozoic orogens that crisscrossed Gondwana and are associated with Gondwana’s assembly. We present new age data from the Queen Maud Mountains, Ross orogen, from areas that hitherto have lacked precise ages from the local plutonic rocks. The zircon U-Pb igneous crystallization ages (n = 7) and a hornblende <sup>40</sup>Ar/<sup>39</sup>Ar cooling age (n = 1) constrain plutonism to primarily lie within the Cambrian to Ordovician. Cumulative zircon U-Pb crystallization age data yield polymodal age distributions (516 Ma, 506–502 Ma, and 488 Ma age peaks) that are similar to other areas of the Queen Maud-Horlick Mountains, consistent with regional magmatic flare-ups along the Pacific-Gondwana margin during these times. The ages of deformed plutons constrain deformation to the Cambrian (Series 2) to Ordovician (Lower), with some regions indicating a transition to post-tectonic magmatism and cooling at ~509-470 Ma. Collectively, the data indicate that the Queen Maud-Horlick Mountains share a similar petrotectonic history with other regions of the Pacific-Gondwana margin, providing new evidence that this tectonostratigraphic province is part of and not exotic to the larger igneous-sedimentary successions developed in the peri-Gondwana realm under a broadly convergent margin setting.
DOI: 10.6084/m9.figshare.10048319
title: Land degradation assessment in an African dryland context based on the Composite Land Degradation Index and mapping method

description: Increasing environmental and socioeconomic transformations in African drylands are driving land degradation. Using the Composite Land Degradation Index, this study assessed physical, chemical and biological degradation by determining their extent and severity. Palapye, an agro-pastoral region in eastern Botswana was used as a case study. Land degradation maps (status and indicators) were created with data from the field, soil chemical properties and image interpretation. Areas in the vicinity of settlements with Luvisols at elevations between 773 and 893 m were most degraded, implying impacts from human activities. This study developed a comprehensive list of of land degradation indicators for Botswana and created additional symbols for mapping indicators. Creation of these reference data for 2015 will facilitate the monitoring of land degradation in Palapye. The integrative and spatially explicit procedure utilized in this study can be adapted for assessing and validating local-level land degradation baseline and estimates towards operationalizing Land Degradation Neutrality in all countries.
DOI: 10.6084/m9.figshare.10048319.v1
title: Land degradation assessment in an African dryland context based on the Composite Land Degradation Index and mapping method

description: Increasing environmental and socioeconomic transformations in African drylands are driving land degradation. Using the Composite Land Degradation Index, this study assessed physical, chemical and biological degradation by determining their extent and severity. Palapye, an agro-pastoral region in eastern Botswana was used as a case study. Land degradation maps (status and indicators) were created with data from the field, soil chemical properties and image interpretation. Areas in the vicinity of settlements with Luvisols at elevations between 773 and 893 m were most degraded, implying impacts from human activities. This study developed a comprehensive list of of land degradation indicators for Botswana and created additional symbols for mapping indicators. Creation of these reference data for 2015 will facilitate the monitoring of land degradation in Palapye. The integrative and spatially explicit procedure utilized in this study can be adapted for assessing and validating local-level land degradation baseline and estimates towards operationalizing Land Degradation Neutrality in all countries.
DOI: 10.15139/s3/pde4ss
title: CMAQ Model Version 5.3, 5.3.1, 5.3.2, 5.3.3 Output Data -- 7/1/2016 - 7/14/2016 12km Southeast US

description: Data Summary: CMAQv5.3+ output data for a 07/01/2016 - 07/14/2016 simulation over the Southeast US. Note:The datasets are on a Google Drive. The metadata associated with this DOI contain the link to the Google Drive folder and instructions for downloading the data.
DOI: 10.6073/pasta/0bb709dddb0ba6fe7024e2537c7a0046
title: PBG07 Grasshopper species abundances in the Patch-Burn Grazing experiment at Konza Prairie

description: ‘PBG’ datasets are associated with a long-term, large-scale study that is addressing the effects of fire-grazing interactions in the context of a Patch-Burn Grazing management system designed to promote grassland heterogeneity. Effects of patch-burn grazing management on plant and animal diversity and the nature and variety of wildlife habitat are being assessed in two replicate management units, each consisting of three pastures (watersheds) designated C03A/C03B/C03C and C3SA/C3SB/C3SC. In each patch-burn grazing unit, one watershed is burned and two that are left unburned in a given year. The burning treatments are rotated annually so that each pasture is burned every third year. Each patch-burn grazing unit is paired with an annually-burned pasture for comparison with traditional grazing systems (C01A and C1SB). All grazing units are stocked with cow/calf pairs from approximately 1 May until 1 Oct at a stocking density equal to 3.2 ha per cow/calf. To examine the impact of patch burning and grazing in all 8 units, we monitor changes in plant species composition, residual biomass, grassland bird populations, insect populations, small mammal populations, soil nutrients, and stream water quality1(1C3SA/C3SB/C3SC unit only). The KSU Department of Animal Science monitors cattle performance, including weight gain and body condition to assess the economic feasibility of using patch-burn management on a widespread basis.
DOI: 10.5281/zenodo.5211945
title: (Cot)2Yb98%Tm2%(K(18-c-6)2)

description: This contains the dataset of (Cot)2Yb98%Tm2%(K(18-c-6)2)
DOI: 10.5281/zenodo.5211944
title: (Cot)2Yb98%Tm2%(K(18-c-6)2)

description: This contains the dataset of (Cot)2Yb98%Tm2%(K(18-c-6)2)
DOI: 10.5281/zenodo.5211933
title: (Cot)2LnK2(thf)4_Yb98%Tm2%

description: This contains the dataset of (Cot)2LnK2(thf)4_Yb98%Tm2%
DOI: 10.5281/zenodo.5211932
title: (Cot)2LnK2(thf)4_Yb98%Tm2%

description: This contains the dataset of (Cot)2LnK2(thf)4_Yb98%Tm2%
DOI: 10.5281/zenodo.5211890
title: ((Cot)2TmK)2(µ-K)K(thf)4

description: This contains the dataset of ((Cot)2TmK)2(µ-K)K(thf)4
DOI: 10.5281/zenodo.5211889
title: ((Cot)2TmK)2(µ-K)K(thf)4

description: This contains the dataset of ((Cot)2TmK)2(µ-K)K(thf)4
DOI: 10.5281/zenodo.5211859
title: biscyclooctatrienylthulium bispotassium-18-crown-6, (Cot)2Tm(K(18-c-6)2)

description: This contains the dataset of (Cot)2Tm(K(18-c-6)2)
DOI: 10.5281/zenodo.5211858
title: biscyclooctatrienylthulium bispotassium-18-crown-6, (Cot)2Tm(K(18-c-6)2)

description: This contains the dataset of (Cot)2Tm(K(18-c-6)2)
DOI: 10.5281/zenodo.5211785
title: biscyclooctatrienylthulium bispotassium tetrakis(tetrahydrofuran), (Cot)2TmK2(thf)4

description: This contains the dataset for (Cot)2TmK2(thf)4