cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.er6kc2
title: Occurrence Download

description: A dataset containing 1161 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Oligoneuriopsis, Metacnemis, Brachydeutera argentata, Ceriagrion, Diplonychus nepoides, Hydrometra albolineolata, Hydrometra, Mesovelia vittigera, Mesovelia, Naboandelus, Nais communis, Nais, Rhagovelia nigricans, Limnodrilus hoffmeisteri, Mesogomphus, Lestes plagiatus, Macrothrix propinqua, Microcyclops varicans, Microcyclops, Tropocyclops confinis, Bosmina longirostris, Simulium dentulosum, Cloeon elevatum, Daphnia pulex, Dero cooperi, Ecnomus oppidanus, Hydroporus, Alona quadrangularis, Amarodytes, Ilyocypris australiensis, Limnobius, Macrocyclops albidus, Macrocyclops, Paracyclops fimbriatus, Alona guttata, Ceriodaphnia quadrangula, Cyclops agilis, , Cyclops prasinus, Cypretta, Microstomum, Nitocra dubia, Pleuroxus assimilis, Sorocelis, Alona rectangula, Leydigia quadrangularis, Elaphoidella, Haliplus, Presba, Segmentorbis, Prionocera, Allonais inaequalis, Allonais, , Pristina minuta, Atherix variegata, Laccocoris limigenus limigenus, Potamocares, Simulium bequaerti, Alona pulchella, Aulodrilus limnobius, Aulodrilus, Bothrioneurum vejdovskyanum, Bothrioneurum, Eriocera fultonensis, Eriocera, Pleuroxus inermis, Pristina synclites, Stephensoniana trivandrana, Stephensoniana, Alona affinis, Anisops debilis, Anopheles squamosus, Aulodrilus pigueti, , Ranatra emaciata emaciata, Rhagadotarsus hutchinsoni, Rhagadotarsus, Microvelia major, Xiphoveloidea, Eurycercus, Nais elinguis, Eatonica schoutedeni, Eatonica, Burnupia caffra, Burnupia ponsonbyi, Herpetocypris chevreuxi, Herpetocypris, Ptychoptera, Bulinus africanus, Hydaticus servillianus, Eubrianax edwardsii, Halicyclops, Tenagogonus, Ampithoe, Paranais frici, Paranais, Pseudodiaptomus, Limnodrilus udekemianus)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "BasisOfRecord is one of (Specimen, Living Specimen, Observation, Human Observation, Machine Observation, Material sample, Literature Occurrence, Material citation, Occurrence evidence)",
 "Geometry POLYGON ((32.064 -28.9416,32.4847 -28.5786,30.5701 -28.5786,30.5701 -30.7329,30.6252 -30.6659,31.4179 -29.4257,31.8178 -29.0299,32.064 -28.9416))"
 ]
}

 The dataset includes 1161 records from 17 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0020915-250827131500795/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.wjmduz
title: Occurrence Download

description: A dataset containing 539 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Myosotis arvensis",
 "Country is Slovakia",
 "HasCoordinate is true"
 ]
}

 The dataset includes 539 records from 8 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0020917-250827131500795/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.3zz53r
title: Occurrence Download

description: A dataset containing 4989 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Myosotis arvensis",
 "Country is Russian Federation",
 "HasCoordinate is true"
 ]
}

 The dataset includes 4989 records from 48 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0020916-250827131500795/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.8zbkmy
title: Occurrence Download

description: A dataset containing 5 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Nitzschia inconspicua, Nitzschia lancettula, Nitzschia rautenbachiae, Nitzschia siliqua, Nitzschia supralitorea, Nitzschia valdecostata, Planothidium lanceolatum, Tryblionella gracilis, Encyonopsis cesatii, Gomphonema angustatum, Mayamaea atomus, Navicula amphiceropsis, Nitzschia rosenstockii, Planothidium rostratum, Stauroneis submarina, Achnanthes coarctata, Nitzschia angustatula, Pinnularia lundii, Navicula kotschyi)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "BasisOfRecord is one of (Specimen, Living Specimen, Observation, Human Observation, Machine Observation, Material sample, Literature Occurrence, Material citation, Occurrence evidence)",
 "Geometry POLYGON ((15.6372 -28.0032,16.2782 -28.5786,20.509 -28.5786,20.509 -24.0715,15.4933 -24.0715,15.4945 -24.1257,16.0509 -25.6631,15.6372 -28.0032))"
 ]
}

 The dataset includes 5 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0020918-250827131500795/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.rqrrqz
title: Occurrence Download

description: A dataset containing 1930 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON ((-72.53394 11.12291, -72.76648 10.9037, -73.0408 10.58867, -73.24323 10.22612, -73.18691 9.748509, -73.45556 9.264979, -73.3875 9.171993, -73.23003 9.423527, -73.11971 9.581118, -72.98414 9.804667, -72.9871 9.944067, -72.92978 10.21817, -72.89057 10.41909, -72.78545 10.61643, -72.64659 10.88, -72.54651 10.96824, -72.45985 11.122, -72.3422 11.15258, -72.2546 11.145, -72.23976 11.17467, -72.4211 11.21194, -72.53394 11.12291))",
 "TaxonKey is Amphibia"
 ]
}

 The dataset includes 1930 records from 16 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0020919-250827131500795/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.77069
title: Distribution of agglutinated foraminifers in sediment core Well 6406/11-1
DOI: 10.1594/pangaea.940275
title: Air quality data of station Parque Dom Pedro, São Paulo from 2014-2020

description: We compiled criteria pollutants from four air quality monitoring stations in Bogotá, eight in Santiago, and five in São Paulo to characterize the impact of emission changes on air quality during the early Coronavirus-imposed lockdown. Time series include hourly measurements (UTC) of ozone (ppbv), nitric oxide (ppbv), nitrogen dioxide (ppbv), carbon monoxide (ppmv), and PM2.5 (microgram per cubic meter), from 1 January 2014 to 1 June 2020.Specifically, datasets were used to compare the lockdown period (March-May 2020) with the baseline period defined as the multi-year average between 2014 and 2019.São Paulo's air quality data were downloaded from the website of the official monitoring network (https://qualar.cetesb.sp.gov.br). The data provided correspond to the following stations: Congonhas, Ibirapuera, Ponte dos Remedios, Parque Dom Pedro, and Pinheiros.
DOI: 10.1594/pangaea.940280
title: Air quality data of station Ponte dos Remedios, São Paulo from 2014-2020

description: We compiled criteria pollutants from four air quality monitoring stations in Bogotá, eight in Santiago, and five in São Paulo to characterize the impact of emission changes on air quality during the early Coronavirus-imposed lockdown. Time series include hourly measurements (UTC) of ozone (ppbv), nitric oxide (ppbv), nitrogen dioxide (ppbv), carbon monoxide (ppmv), and PM2.5 (microgram per cubic meter), from 1 January 2014 to 1 June 2020.Specifically, datasets were used to compare the lockdown period (March-May 2020) with the baseline period defined as the multi-year average between 2014 and 2019.São Paulo's air quality data were downloaded from the website of the official monitoring network (https://qualar.cetesb.sp.gov.br). The data provided correspond to the following stations: Congonhas, Ibirapuera, Ponte dos Remedios, Parque Dom Pedro, and Pinheiros.
DOI: 10.1594/pangaea.940274
title: Air quality data of station Congonhas, São Paulo from 2014-2020

description: We compiled criteria pollutants from four air quality monitoring stations in Bogotá, eight in Santiago, and five in São Paulo to characterize the impact of emission changes on air quality during the early Coronavirus-imposed lockdown. Time series include hourly measurements (UTC) of ozone (ppbv), nitric oxide (ppbv), nitrogen dioxide (ppbv), carbon monoxide (ppmv), and PM2.5 (microgram per cubic meter), from 1 January 2014 to 1 June 2020.Specifically, datasets were used to compare the lockdown period (March-May 2020) with the baseline period defined as the multi-year average between 2014 and 2019.São Paulo's air quality data were downloaded from the website of the official monitoring network (https://qualar.cetesb.sp.gov.br). The data provided correspond to the following stations: Congonhas, Ibirapuera, Ponte dos Remedios, Parque Dom Pedro, and Pinheiros.
DOI: 10.1594/pangaea.961937
title: Grain size analysis of Laguna Meseta (LME), Central Patagonia

description: Further funding:Environmental and climate reconstruction for Chilean Patagonia - Investigations of lacustrine sediment record at Chile Chico Plateau and its surrounding area, Award: DAAD Doctoral programmes in Germany 2020/21
DOI: 10.1594/pangaea.973009
title: Bulk chemistry measurements and grain size distribution of a composite sediment core from Laguna Vogt, central west Patagonia

description: A 3 m-long sediment composite record was retrieved from Laguna Vogt (46.74º S, central west Patagonia) using a UWITEC gravity corer (for the uppermost 70 cm depth) and a modified Livingstone piston corer (for the remaining depths) during march, 2020. Several analytical techniques were applied to the sediment records. Firstly, X-ray fluorescence and magnetic susceptibility scanning were done at 1 mm and 1 cm resolution, respectively. Afterwards, subsampling was carried out at a 1 cm depth resolution. Exceptionally, the resolution was changed to 0.5 cm for sections with contrasting lithologies. Bulk chemistry measurements for elements C, N, and S were performed on the subsamples at intervals between 4 and 0.5 cm. Finally, grain size distributions for the subsamples were measured using a 4 cm step protocol. Results are presented with respect to depth and age. Ages were derived from an age-depth model based on 9 samples taken for radiocarbon dating from the composite profile.
DOI: 10.1594/pangaea.804889
title: (Table 13) Oxygen and carbon isotopic data for vein minerals at DSDP Holes 70-504B and 83-504B
DOI: 10.1594/pangaea.973023
title: X-ray fluorescence scannings of a composite sediment core from Laguna Vogt, central west Patagonia

description: A 3 m-long sediment composite record was retrieved from Laguna Vogt (46.74º S, central west Patagonia) using a UWITEC gravity corer (for the uppermost 70 cm depth) and a modified Livingstone piston corer (for the remaining depths) during march, 2020. Several analytical techniques were applied to the sediment records. Firstly, X-ray fluorescence and magnetic susceptibility scanning were done at 1 mm and 1 cm resolution, respectively. Afterwards, subsampling was carried out at a 1 cm depth resolution. Exceptionally, the resolution was changed to 0.5 cm for sections with contrasting lithologies. Bulk chemistry measurements for elements C, N, and S were performed on the subsamples at intervals between 4 and 0.5 cm. Finally, grain size distributions for the subsamples were measured using a 4 cm step protocol. Results are presented with respect to depth and age. Ages were derived from an age-depth model based on 9 samples taken for radiocarbon dating from the composite profile.
DOI: 10.1594/pangaea.712350
title: (Table 2) Sr, O and D isotope ratios and water content of altered basement rocks and veins of DSDP Hole 504B
DOI: 10.1594/pangaea.936506
title: Abundances of planktonic items found in southern Patagonia during the austral late-spring 2015

description: Physical and chemical parameters and associated coccolithophores species/Emiliania huxleyi morphotypes abundances and biovolume and co-occurring microplankton abundances recorded in southern Patagonia (~ 50-54 ºS) during the austral late-spring 2015 (at the end of november) and early-spring 2017 (at the end of september). Given the scarcity of data about coccolithophores in Patagonian waters and the impressive nearly a century spring-summer reports of Emiliania huxleyi blooms around the North Sea and Norwegian fjords system we want to observe what happens in this side of the planet. To do that, we collected seawater containing planktonic organisms at the surface and in some stations up to 75 m depth. Inverted microscopy along with SEM analyses were used to identify and quantify the planktonic items.
DOI: 10.1594/pangaea.714977
title: (Table 6) Sr isotope compositions-leaching experiments
DOI: 10.1594/pangaea.112756
title: Thermal conductivity and heat flow measurements from cruise Planet69, 4-21 August 1969, Norwegian Sea

description: This is a report about a joint scientific venture of German and Norwegian Institutes in an area between Latitude = 66°45' N and 68°30' N and Longitude 1.0° E to 7°30' W. The chief scientist's report gives an outline of the cruise. The preliminary contributions by the scientists deal with results of gravity at sea, magnetic and geothermic measurements, the seismic shooting, results of continuous seismic reflection work, some refraction seismic results and with the observations of the ship's weather station.
description: preliminary contributions by the scientist
DOI: 10.1594/pangaea.805064
title: (Table 1) Downhole variation of potassium, apparent K-Ar age, and inert gas abundances at DSDP Holes 69-504B, 70-504B and 83-504B

description: Ne, Ar, Kr, Xe, and K2O were measured in representative samples of holocrystalline basalt from DSDP Hole 504B. No hiatus in inert gas abundance is recognized at the base of the "oxic" alteration zone and the extent rather than the nature of alteration appears to determine these abundances. When the inert gas abundances are separately plotted against K2O, two distinct trends of loss emerge, one for alteration involving K-gain, the other for K-loss.Apparent whole-rock K-Ar ages are anomalous in the upper 50 m of basement, and below 300 m sub-basement. In the intervening zone of basement, celadonization adds sufficient potassium and eliminates enough "primary" 40Ar early in the history of the basalts for "excess" 40Ar to become subordinate to radiogenic 40Ar in basalts showing potassium enrichment greater than 0.2%. Stratigraphically correct K-Ar ages are obtained, therefore, from K-enriched basalts of the oxic alteration zone.
description: Supplement to: Mitchell, John G; Terrell, David J (1985): Downhole variation of potassium, inert gas abundance, and apparent K-Ar age in basalts from the Costa Rica Rift, Hole 504B, Leg 83, Deep Sea Drilling Project. In: Anderson, RN; Honnorez, J; Becker, K; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 83, 305-312
DOI: 10.1594/pangaea.973119
title: Rose Bengal staining status, surface sediment calibrated age, δ18O values, and specimen age of various benthic foraminifera species of surface sediment samples from the Southeast Pacific
DOI: 10.1594/pangaea.56577
title: Sedimentologiccal bulk parameter of core NP94-14SL
DOI: 10.1594/pangaea.973116
title: Benthic foraminifera species abundance of surface sediment samples from the Southeast Pacific
DOI: 10.1594/pangaea.713290
title: (Table 2) Oxygen isotopic composition and calculated temperatures of formation of clay minerals from DSDP Hole 504B

description: Depth, sediment (m) is the sub-basement depth (m), Sample 70-504B-37-1,76-80 calculated after Yeh and Savin (1977, doi:10.1130/0016-7606(1977)88&lt;1321:MOBMOA&gt;2.0.CO;2), sample 83-405B-80-1,106-111 calculated T = 200-250 °C calculated after Wenner and Taylor (1971, doi:10.1007/BF00643332)
DOI: 10.1594/pangaea.223034
title: Carbon analysis of Hole 53-418B
DOI: 10.1594/pangaea.805329
title: (Table 2) Comparisons of dynamic and static Young's moduli of basalt at DSDP Holes 69-504B, 70-504B and 83-504B
DOI: 10.1594/pangaea.944627
title: Morphometric parameters of the Squid Mounds (SQM), Namibian coral mound province

description: Quantitative morphometric analyses were carried out for each mound following the workflows presented by Purkis et al. (2007) The coral mound base was defined following the methodological approach of Correa et al. (2012) using the dip angle map, generated from the digital elevation model (DEM), to extract closed polygons that follow the 3°-contour line. This 3°-cutoff has been qualitatively validated with a comparison between the DEM and the dip angle (Fig. 2). Small-scaled polygons within mound perimeters and resulting from bathymetric artifacts were filtered out. Manual editing was applied to split simple merged mound structures (e.g. twin-peak mounds) based on higher cut-off slope values (4-5°). Furthermore, polygons describing the mound footprint have been corrected to remove unrealistic shapes especially common for the CBM. The DEM was subsequently re-gridded to generate hypothetical bathymetric maps without mounds, for which the vertical relief beneath each removed mound was interpolated from the mound perimeters. The newly interpolated surfaces were then subtracted from the original DEMs to evaluate the volume and heights of the coral mounds. Only features with a footprint area greater than 900 squared meters (corresponding to a two-dimensional array of 3 × 3 DEM grid cells) and with a height of &gt;2 m above the surrounding seafloor (4 × 0.5 m of vertical precision) were considered as coral mounds and quantitatively analyzed.
DOI: 10.1594/pangaea.944595
title: Morphometric parameters of the Coral Belt Mounds (CBM), Namibian coral mound province

description: Quantitative morphometric analyses were carried out for each mound following the workflows presented by Purkis et al. (2007) The coral mound base was defined following the methodological approach of Correa et al. (2012) using the dip angle map, generated from the digital elevation model (DEM), to extract closed polygons that follow the 3°-contour line. This 3°-cutoff has been qualitatively validated with a comparison between the DEM and the dip angle. Small-scaled polygons within mound perimeters and resulting from bathymetry artefacts were filtered out. Manual editing was applied to split simple merged mound structures (e.g. twin-peak mounds) based on higher cut-off slope values (4-5°). Furthermore, polygons describing the mound footprint have been corrected to remove unrealistic shapes especially common for the CBM. The DEM was subsequently re-gridded to generate hypothetical bathymetric maps without mounds, for which the vertical relief beneath each removed mound was interpolated from the mound perimeters. The newly interpolated surfaces were then subtracted from the original DEMs to evaluate the volume and heights of the coral mounds. Only features with a footprint area greater than 900 suared meters (corresponding to a two-dimensional array of 3 × 3 DEM grid cells) and with a height of &gt;2 m above the surrounding seafloor (4 × 0.5 m of vertical precision) were considered as coral mounds and quantitatively analyzed.
DOI: 10.1594/pangaea.934338
title: Lakes with physical, climatological, and isotopic data, located between 38ºS-46ºS along Chile

description: This table contains physical, climatological, and isotope data. All lakes were open lakes. The slope was calculated according to methods/ranges proposed by the United States Department of Agriculture so that each watershed is described with a unitless slope characteristic, with slope gradient classes above 45 indicating steep drainage basins. The land uses were calculated from Chilean vegetative data (methods section) and values represent the proportion (%) of the catchment that is covered with this type of land use. Then, refer it as % snow or glaciers, that means that the zone is covered permanently with this land use. MAT and MAP, are mean annual air temperature and precipitation calculated from a monthly reanalysis product (CR2MET) with a 0.05° horizontal resolution considering the period from 1979 to 2016, and extracting data from the nearest grid point to the lake positions where we collected surface water. All samples were taken during austral spring/summer 2017 to 2019.
DOI: 10.1594/pangaea.934344
title: Lakes with two or more sampling years, located between 38ºS-46ºS along Chile

description: The average standard deviation of H and O isotopes between sampling years for all the lakes in the study is 2.8‰ for δ2H and 0.9 ‰ for δ18O, respectively (additional info in the methods section). All samples were taken during austral spring/summer 2017 to 2019.
DOI: 10.1594/pangaea.961939
title: XRF-elements of Laguna Meseta (LME), Central Patagonia

description: Further funding:Environmental and climate reconstruction for Chilean Patagonia - Investigations of lacustrine sediment record at Chile Chico Plateau and its surrounding area, Award: DAAD Doctoral programmes in Germany 2020/21
DOI: 10.1594/pangaea.222273
title: Grain size analysis of Hole 53-418B
DOI: 10.15468/dl.kghdjn
title: Occurrence Download

description: A dataset containing 16867 species occurrences available in GBIF matching the query:
{
 "and" : [
 "CoordinateUncertaintyInMeters 0.0-989.0",
 "Country is Australia",
 "OccurrenceStatus is Present",
 "StateProvince is Queensland",
 "TaxonKey is Limnodynastes peronii",
 "Year 2022-2025"
 ]
}

 The dataset includes 16867 records from 2 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0020920-250827131500795/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.56576
title: TOC, CaCO3, DBDD, WBD, water content, porosity, grain size, shear strength of Site NP94-11SC
DOI: 10.1594/pangaea.263050
title: Minor-element chemical analyses of Hole 46-396B
DOI: 10.1594/pangaea.753096
title: (Table 3) Datum levels of stratigraphic correlation of ODP Leg 111 and DSDP Leg 69 sites
DOI: 10.1594/pangaea.224878
title: Wet bulk density (GRAPE) of Hole 53-418B
DOI: 10.1594/pangaea.983623
title: Daily meteorological observations of minimum air temperatures for Ambodifotatra, Madagascar

description: Please note that for the daily datasets, the given hour is just allocated by C3S and is not really used when analysing the data by a user, so it is irrelevant.
DOI: 10.1594/pangaea.983624
title: Daily meteorological observations of mean air temperatures for Ambodifotatra, Madagascar

description: Please note that for the daily datasets, the given hour is just allocated by C3S and is not really used when analysing the data by a user, so it is irrelevant.
DOI: 10.1594/pangaea.983745
title: Sub-daily meteorological observations of wind speed for Nosy Varika, Madagascar
DOI: 10.1594/pangaea.983717
title: Daily meteorological observations of precipitation for Morombe, Madagascar

description: Please note that for the daily datasets, the given hour is just allocated by C3S and is not really used when analysing the data by a user, so it is irrelevant.
DOI: 10.1594/pangaea.983621
title: Daily meteorological observations of maximum air temperatures for Ambodifotatra, Madagascar

description: Please note that for the daily datasets, the given hour is just allocated by C3S and is not really used when analysing the data by a user, so it is irrelevant.
DOI: 10.1594/pangaea.983661
title: Sub-daily meteorological observations of precipitation for Ambodifotatra, Madagascar
DOI: 10.1594/pangaea.983619
title: Daily meteorological observations of evaporation for Ambodifotatra, Madagascar

description: Please note that for the daily datasets, the given hour is just allocated by C3S and is not really used when analysing the data by a user, so it is irrelevant.
DOI: 10.1594/pangaea.983620
title: Daily meteorological observations of precipitation for Ambodifotatra, Madagascar

description: Please note that for the daily datasets, the given hour is just allocated by C3S and is not really used when analysing the data by a user, so it is irrelevant.
DOI: 10.1594/pangaea.983662
title: Sub-daily meteorological observations of station level pressure for Ambodifotatra, Madagascar