cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.t6sn2t
title: Occurrence Download

description: A dataset containing 68 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Physalia physalis (Linnaeus, 1758)",
 "HasGeospatialIssue is false",
 "Geometry POLYGON((-114.90 15.81,-114.90 31.78,-87.34 31.78,-87.34 15.81,-114.90 15.81))"
 ]
}

 The dataset includes 68 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0085731-160910150852091/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.xj8vex
title: Occurrence Download

description: A dataset containing 48 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Syzygium laxiflorum (Blume) DC."
 ]
}

 The dataset includes 48 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0038465-200613084148143/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.mh9mbn
title: Occurrence Download

description: A dataset containing 298 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON((-7.71556 37.67704,-4.38044 37.67704,-4.38044 41.12988,-7.71556 41.12988,-7.71556 37.67704))",
 "HasCoordinate is true",
 "OccurrenceStatus is Present",
 "TaxonKey is Botaurus stellaris (Linnaeus, 1758)"
 ]
}

 The dataset includes 298 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0018281-240229165702484/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.dbdev4
title: Occurrence Download

description: A dataset containing 3377 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON((-87.92885 40.22258,-69.75895 40.22258,-69.75895 43.49382,-87.92885 43.49382,-87.92885 40.22258))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "TaxonKey is Ambystoma maculatum (Shaw, 1802)"
 ]
}

 The dataset includes 3377 records from 33 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0038487-200613084148143/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.xfj3hq
title: Occurrence Download

description: A dataset containing 303950 species occurrences available in GBIF matching the query:
{
 "and" : [
 {
 "or" : [
 "BasisOfRecord is Human Observation",
 "BasisOfRecord is Machine Observation",
 "BasisOfRecord is Living Specimen"
 ]
 },
 "Country is Namibia",
 "Year 2005-2017",
 "DatasetKey is SAFRING: Historical Bird Ringing Records (2005-2009)"
 ]
}

 The dataset includes 303950 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0085735-160910150852091/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.2qjpdp
title: Occurrence Download

description: A dataset containing 12538 species occurrences available in GBIF matching the query:
{
 "and" : [
 "OccurrenceStatus is Present",
 "TaxonKey is Scaphyglottis Poepp. & Endl."
 ]
}

 The dataset includes 12538 records from 288 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0007772-231002084531237/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dd.kjkqws
title: Test for derived dataset

description: This data was filtered using a fake protocol
DOI: 10.15468/dd.wau3zn
title: Test for derived dataset

description: This data was filtered using a fake protocol
DOI: 10.15468/dd.f35yw7
title: Test for derived dataset

description: This data was filtered using a fake protocol
DOI: 10.15468/dd.wckr29
title: Current State of Knowledge of Páramo Amphibians in Colombia: Spatio Temporal Trends and Information Gaps to Be Strengthened for Effective Conservation

description: Summary of GBIF data used in (study)[https://doi.org/10.1177/19400829231169984]
DOI: 10.15468/dd.getpr3
title: A multi-dimensional selective landscape drives adaptive divergence between and within closely related Phlox species

description: Summary of the datasets used in the [study](https://doi.org/10.1101/2023.04.18.537324)
DOI: 10.15468/dd.u4ycxv
title: Test for derived dataset

description: This data was filtered using a fake protocol
DOI: 10.15468/dd.9afnas
title: Test for derived dataset

description: This data was filtered using a fake protocol
DOI: 10.15468/dd.y57pua
title: DEPOBIO

description: DEPOBIO
DOI: 10.1594/gfz.sddb.1301
title: Supplementary material to Mangili et al. (2010): Climatic implications of annual to decadal resolution stable isotope data from calcite varves of the Piànico interglacial lake record, Southern Alps

description: Stable oxygen isotope analyses at annual, 2-, 5-, 10- and 20-varve sample resolutions were carried out on two selected varve intervals from the interglacial sediment record of the Pianico palaeolake. These sediments are particularly suitable for ultra-high-resolution isotope analyses on lacustrine endogenic calcite because of the exceptionally well-preserved varve structure. A bias through detrital contamination can be excluded because microscopically controlled sampling enabled selecting detritus-free samples. The studied sediment intervals comprise 352 and 88 continuous varve series formed during periods of rapid climate change at the onset and end of a marked millennial-scale cool interval during the Pianico Interglacial. The most intriguing result is a pronounced short-term oscillation in the bi-annually resolved isotope record superimposed on the general decreasing and increasing delta-18O trends at the climatic transitions that is recorded at lower sample resolution. Spectral analyses of the bi-annual time series reveal periodicities indicating solar and NAO controls on the delta-18O record. Multiple delta-18O measurements from endogenic calcite of individual varves showed variations of up to 0.6 per mill, thus larger than the observed inter-annual variability and most likely explained by seasonal effects.
DOI: 10.1594/gfz.sddb.1311
title: Electrical Resistivity of Mini Cores (Plugs) of the KTB Main Hole HB1

description: In general, four-electrode devices are used to measure the resistivity on original (unprepared) cores and on mini cores drilled from these original cores. The in-phase and the out-of-phase signal is measured and therefore the complex resistivity is determined. All measurements are performed under surface conditions (room temperature and atmospheric pressure). Mini cores of 25.4 mm diameter and approximately 50 mm length are drilled from original cores. Anisotropy information is obtained by different core orientations. The complex resitivity is measured in an 4-electrode elctrolytic cell by use of a lock-in-amplifier. The applied frequency ranges from 0.5 Hz to 120 kHz.
The samples are first evacuated and back-saturated with destilled water. In this case, mainly sigmas and sigmam contribute to the rock resistivity. A second cycle of evacuating and back-saturating with 0.1 molar NaCl solution leads to sigmav (Rauen 1994).
DOI: 10.1594/gfz.sddb.1314
title: Electrical Resistivity of Mini Cores (Plugs) of the KTB Main Hole HB1g

description: In general, four-electrode devices are used to measure the resistivity on original (unprepared) cores and on mini cores drilled from these original cores. The in-phase and the out-of-phase signal is measured and therefore the complex resistivity is determined. All measurements are performed under surface conditions (room temperature and atmospheric pressure).Mini cores of 25.4 mm diameter and approximately 50 mm length are drilled from original cores. Anisotropy information is obtained by different core orientations. The complex resitivity is measured in an 4-electrode elctrolytic cell by use of a lock-in-amplifier. The applied frequency ranges from 0.5 Hz to 120 kHz.
The samples are first evacuated and back-saturated with destilled water. In this case, mainly sigmas and sigmam contribute to the rock resistivity. A second cycle of evacuating and back-saturating with 0.1 molar NaCl solution leads to sigmav (Rauen 1994).
DOI: 10.1594/gfz.sddb.1315
title: Natural Gamma-ray Activity of Cuttings of the KTB Pilot Hole VB1

description: In the laboratory, the gamma radiation is measured by a sodium iodtite (NaI) scintillation detector (cores and cuttings) and by a germanium (Ge) semiconductor detector (cuttings).
The cuttings are measured in air tight Marinelli-beakers with a volume of 250 cm3. For the core measurements a special, automatically operating equipment with three NaI detectors is used. A description of this apparatus is given in Wienand et al. (1989). The principle of measurements with the Ge-detector is described by Bücker et al. (1991).The measured spectra are calibrated by a standard of Luvarovite (NIM-L, South African Bureau of Standards). The influence of the local terrestrial radiation on the measurements has been corrected. Especially for the core measurements a calibration procedure has been performed for geometric corrections (core diameter and length). In general, a measuring time of 12 h for the NaI-detector and 2 h for the Ge-detector was chosen.
DOI: 10.1594/gfz.sddb.1316
title: Natural Gamma-ray Activity of Cuttings of the KTB Pilot Hole VB1a

description: In the laboratory, the gamma radiation is measured by a sodium iodtite (NaI) scintillation detector (cores and cuttings) and by a germanium (Ge) semiconductor detector (cuttings). The cuttings are measured in air tight Marinelli-beakers with a volume of 250 cm3. For the core measurements a special, automatically operating equipment with three NaI detectors is used. A description of this apparatus is given in Wienand et al. (1989). The principle of measurements with the Ge-detector is described by Bücker et al. (1991).The measured spectra are calibrated by a standard of Luvarovite (NIM-L, South African Bureau of Standards). The influence of the local terrestrial radiation on the measurements has been corrected. Especially for the core measurements a calibration procedure has been performed for geometric corrections (core diameter and length). In general, a measuring time of 12 h for the NaI-detector and 2 h for the Ge-detector was chosen.
DOI: 10.1594/gfz.sddb.1318
title: Natural Gamma-ray Activity of Cuttings of the KTB Main Hole HB1 (measurements with Germanium detector only)

description: In the laboratory, the gamma radiation is measured by a sodium iodtite (NaI) scintillation detector (cores and cuttings) and by a germanium (Ge) semiconductor detector (cuttings).The cuttings are measured in air tight Marinelli-beakers with a volume of 250 cm3. For the core measurements a special, automatically operating equipment with three NaI detectors is used. A description of this apparatus is given in Wienand et al. (1989). The principle of measurements with the Ge-detector is described by Bücker et al. (1991). The measured spectra are calibrated by a standard of Luvarovite (NIM-L, South African Bureau of Standards). The influence of the local terrestrial radiation on the measurements has been corrected. Especially for the core measurements a calibration procedure has been performed for geometric corrections (core diameter and length). In general, a measuring time of 12 h for the NaI-detector and 2 h for the Ge-detector was chosen.
DOI: 10.1594/gfz.sddb.1319
title: Natural Gamma-ray Activity of Cuttings of the KTB Main Hole HB1a (measurements with Germanium detector only)

description: In the laboratory, the gamma radiation is measured by a sodium iodtite (NaI) scintillation detector (cores and cuttings) and by a germanium (Ge) semiconductor detector (cuttings).The cuttings are measured in air tight Marinelli-beakers with a volume of 250 cm3. For the core measurements a special, automatically operating equipment with three NaI detectors is used. A description of this apparatus is given in Wienand et al. (1989). The principle of measurements with the Ge-detector is described by Bücker et al. (1991). The measured spectra are calibrated by a standard of Luvarovite (NIM-L, South African Bureau of Standards). The influence of the local terrestrial radiation on the measurements has been corrected. Especially for the core measurements a calibration procedure has been performed for geometric corrections (core diameter and length). In general, a measuring time of 12 h for the NaI-detector and 2 h for the Ge-detector was chosen.
DOI: 10.1594/gfz.sddb.1320
title: Natural Gamma-ray Activity of Cuttings of the KTB Main Hole HB1d (measurements with Germanium detector only)

description: In the laboratory, the gamma radiation is measured by a sodium iodtite (NaI) scintillation detector (cores and cuttings) and by a germanium (Ge) semiconductor detector (cuttings).The cuttings are measured in air tight Marinelli-beakers with a volume of 250 cm3. For the core measurements a special, automatically operating equipment with three NaI detectors is used. A description of this apparatus is given in Wienand et al. (1989). The principle of measurements with the Ge-detector is described by Bücker et al. (1991). The measured spectra are calibrated by a standard of Luvarovite (NIM-L, South African Bureau of Standards). The influence of the local terrestrial radiation on the measurements has been corrected. Especially for the core measurements a calibration procedure has been performed for geometric corrections (core diameter and length). In general, a measuring time of 12 h for the NaI-detector and 2 h for the Ge-detector was chosen.
DOI: 10.1594/gfz.sddb.1321
title: Supplementary material to Lauterbach et al. (2010): Multi-proxy evidence for early to mid-Holocene environmental and climatic changes in northeastern Poland

description: We investigated the sedimentary record of Lake Hancza (northeastern Poland) using a multi-proxy approach, focusing on early to mid-Holocene climatic and environmental changes. AMS 14C dating of terrestrial macrofossils and sedimentation rate estimates from occasional varve thickness measurements were used to establish a chronology. The onset of the Holocene at c. 11 600 cal. a BP is marked by the decline of Lateglacial shrub vegetation and a shift from clastic-detrital deposition to an autochthonous sedimentation dominated by biochemical calcite precipitation. Between 10 000 and 9000 cal. a BP, a further environmental and climatic improvement is indicated by the spread of deciduous forests, an increase in lake organic matter and a 1.7% rise in the oxygen isotope ratios of both endogenic calcite and ostracod valves. Rising d18O values were probably caused by a combination of hydrological and climatic factors. The persistence of relatively cold and dry climate conditions in northeastern Poland during the first one and a half millennia of the Holocene could be related to a regional eastern European atmospheric circulation pattern. Prevailing anticyclonic circulation linked to a high-pressure cell above the retreating Scandinavian Ice Sheet might have blocked the influence of warm and moist Westerlies and attenuated the early Holocene climatic amelioration in the Lake Hancza region until the final decay of the ice sheet.
DOI: 10.6084/m9.figshare.30450923
title: The Role of Fear in Harm Reduction: Replication Package

description: Background: Misinformation about fentanyl exposure risks may affect first responders’ will-ingness to administer naloxone. This study examines its impact in New York State, focusing onbehavioral changes after a widely publicized event promoting the false belief that brief contactwith fentanyl is lethal.Methods This study examines quarterly naloxone administration data (2015–2019) in UpstateNew York, sourced from the New York State Department of Health. It categorizes adminis-trations by law enforcement, emergency medical services, and community programs. Using adifferences-in-differences quasi-experimental approach, it compares administration rate changesacross responder types before and after the misinformation event.Results Findings indicate a significant decline in naloxone administration by law enforcementofficers following the media event, suggesting increased hesitancy to render aid due to unfoundedfears of fentanyl exposure. No comparable decline is observed among harm reduction profession-als, highlighting the selective impact of misinformation on responder behavior.Conclusions These results underscore the potential adverse effects of misinformation on publichealth outcomes, particularly in emergency overdose response. The findings provide a new per-spective on the inconsistent empirical results regarding harm reduction policies and emphasizethe need for targeted education and training initiatives to counteract misinformation among firstresponders.
DOI: 10.6084/m9.figshare.30450923.v1
title: The Role of Fear in Harm Reduction: Replication Package

description: Background: Misinformation about fentanyl exposure risks may affect first responders’ will-ingness to administer naloxone. This study examines its impact in New York State, focusing onbehavioral changes after a widely publicized event promoting the false belief that brief contactwith fentanyl is lethal.Methods This study examines quarterly naloxone administration data (2015–2019) in UpstateNew York, sourced from the New York State Department of Health. It categorizes adminis-trations by law enforcement, emergency medical services, and community programs. Using adifferences-in-differences quasi-experimental approach, it compares administration rate changesacross responder types before and after the misinformation event.Results Findings indicate a significant decline in naloxone administration by law enforcementofficers following the media event, suggesting increased hesitancy to render aid due to unfoundedfears of fentanyl exposure. No comparable decline is observed among harm reduction profession-als, highlighting the selective impact of misinformation on responder behavior.Conclusions These results underscore the potential adverse effects of misinformation on publichealth outcomes, particularly in emergency overdose response. The findings provide a new per-spective on the inconsistent empirical results regarding harm reduction policies and emphasizethe need for targeted education and training initiatives to counteract misinformation among firstresponders.
DOI: 10.1594/gfz.sddb.1335
title: Natural Gamma-ray Activity of Cuttings of the KTB Main Hole HB1a  (measurements with NaI-detector only)

description: In the laboratory, the gamma radiation is measured by a sodium iodtite (NaI) scintillation detector (cores and cuttings) and by a germanium (Ge) semiconductor detector (cuttings).
The cuttings are measured in air tight Marinelli-beakers with a volume of 250 cm3. For the core measurements a special, automatically operating equipment with three NaI detectors is used. A description of this apparatus is given in Wienand et al. (1989). The principle of measurements with the Ge-detector is described by Bücker et al. (1991).The measured spectra are calibrated by a standard of Luvarovite (NIM-L, South African Bureau of Standards). The influence of the local terrestrial radiation on the measurements has been corrected. Especially for the core measurements a calibration procedure has been performed for geometric corrections (core diameter and length). In general, a measuring time of 12 h for the NaI-detector and 2 h for the Ge-detector was chosen.
DOI: 10.1594/gfz.sddb.1340
title: Natural Gamma-ray Activity of Cores of the KTB Main Hole HB1a

description: In the laboratory, the gamma radiation is measured by a sodium iodtite (NaI) scintillation detector (cores and cuttings) and by a germanium (Ge) semiconductor detector (cuttings). The cuttings are measured in air tight Marinelli-beakers with a volume of 250 cm3. For the core measurements a special, automatically operating equipment with three NaI detectors is used. A description of this apparatus is given in Wienand et al. (1989). The principle of measurements with the Ge-detector is described by Bücker et al. (1991).The measured spectra are calibrated by a standard of Luvarovite (NIM-L, South African Bureau of Standards). The influence of the local terrestrial radiation on the measurements has been corrected. Especially for the core measurements a calibration procedure has been performed for geometric corrections (core diameter and length). In general, a measuring time of 12 h for the NaI-detector and 2 h for the Ge-detector was chosen.
DOI: 10.1594/gfz.sddb.1341
title: Natural Gamma-ray Activity of Cores of the KTB Main Hole HB1g

description: In the laboratory, the gamma radiation is measured by a sodium iodtite (NaI) scintillation detector (cores and cuttings) and by a germanium (Ge) semiconductor detector (cuttings). The cuttings are measured in air tight Marinelli-beakers with a volume of 250 cm3. For the core measurements a special, automatically operating equipment with three NaI detectors is used. A description of this apparatus is given in Wienand et al. (1989). The principle of measurements with the Ge-detector is described by Bücker et al. (1991).The measured spectra are calibrated by a standard of Luvarovite (NIM-L, South African Bureau of Standards). The influence of the local terrestrial radiation on the measurements has been corrected. Especially for the core measurements a calibration procedure has been performed for geometric corrections (core diameter and length). In general, a measuring time of 12 h for the NaI-detector and 2 h for the Ge-detector was chosen.
DOI: 10.1594/gfz.sddb.1342
title: Natural Remanent Magnetisation of Cores of the KTB Pilot Hole VB1

description: Natural Remanent Magnetisation of Cores of the KTB Pilot Hole VB1
DOI: 10.1594/gfz.sddb.1344
title: Natural Remanent Magnetisation of Cores of the KTB Main Hole HB1

description: Natural Remanent Magnetisation of Cores of the KTB Main Hole HB1
DOI: 10.1594/gfz.sddb.1345
title: Natural Remanent Magnetisation of Cores of the KTB Main Hole HB1a

description: Natural Remanent Magnetisation of Cores of the KTB Main Hole HB1a
DOI: 10.1594/gfz.sddb.1347
title: Permeability of Mini Cores of the KTB Pilot Hole VB1

description: In the KTB field laboratory, porosity, internal surface and permeability were determined on identical mini cores with 25.4 mm in diameter and approximately 50 mm in length. These samples were drilled either axial or radial with respect to the drill core, or parallel or perpendicular with respect to the foliation. In the KTB field laboratory, the stationary sArcy method was used with nitrogen gas as the streaming medium. The measurements were made at a constant confining pressure of 5 MPa to 6.5 MPa. The nitrogen pressure gradient was up to 2 MPa at the inflow side minus atmospheric pressure at the outflow side of the sample. Because of the low pore pressures during the measurements (max 2 MPa) the data had to be corrected for the effect of gas friction along the matrix wall, the so called Klinkenberg effect (Huenges et al. 1990). Further details, regarding equipment and evaluation are given by Pusch et al. (1986).