cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.tu3gg5
title: Occurrence Download

description: A dataset containing 59 species occurrences available in GBIF matching the query:
{
 "and" : [
 {
 "or" : [
 "BasisOfRecord is Machine Observation",
 "BasisOfRecord is Human Observation"
 ]
 },
 "CoordinateUncertaintyInMeters 0.0-400.0",
 {
 "or" : [
 "DatasetKey is iNaturalist Research-grade Observations",
 "DatasetKey is naturgucker",
 "DatasetKey is Observation.org, Nature data from around the World"
 ]
 },
 "OccurrenceStatus is Present",
 "TaxonKey is Siganus rivulatus Forsskål & Niebuhr, 1775",
 "Year 2010-2022"
 ]
}

 The dataset includes 59 records from 3 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0112468-210914110416597/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25549/pcra-c14-193478
title: Khristiaskiy vestnik = [Christian herald], vol. 19, whole no. 208-210 (1955 January-March)

description: [description english/roman)] The Christian Herald was an informational organ of the Union of Pentecostal churches of "Assemblies of God" in South America. The journal was founded in August 1937 at the founding meeting of the Slavic Pentecostal churches of South America. Believers from Argentina, Paraguay, Uruguay and Brazil were present at the meeting. The purpose of the journal was to "carry unity and communication of the Spirit to the midst of believers in full Gospel". The journal united Pentecostal churches and became a link which connected believers scattered all over the world. Thus, letters of Christians of Evangelical faith from Germany, Belgium, France, the Netherlands, Canada, the United States, Uruguay, Paraguay, the Philippines, China, Australia and other countries were published in the journal journal. The first issue was published in Russia in October 1937. Subsequently, the journal spread to 40 countries where the Slavic diaspora lived. The headquarters of the journal was located in Buenos Aires. Juan Zub-Zolotarow was responsible for the journal. He was a permanent editor for 42 years. The journal was published for offerings of believers. Spiritually-edifying and theological articles of Donald Gee, Alfred Goets, R. Bratslavsky, N. Vodnevsky, D. Bespalov were published in the journal. On the last pages, as a rule, information from local churches and the mission and evangelical fields of North and South America, Canada, Africa, Australia, India, Europe and China was published. Thus the activity of such evangelists as Oral Roberts, Billy Graham, T. Giks, and William Brankham was reported in detail.
DOI: 10.15468/dl.j7nz57
title: Occurrence Download

description: A dataset containing 2097 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is Specimen",
 "Country is Spain",
 "TaxonKey is Quercus pyrenaica Willd."
 ]
}

 The dataset includes 2097 records from 52 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0365943-210914110416597/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.4c9dex
title: Occurrence Download

description: A dataset containing 649 species occurrences available in GBIF matching the query:
{
 "and" : [
 "VerbatimScientificName is Batis orientalis",
 "BasisOfRecord is one of (Machine Observation, Human Observation)",
 "Year 2011-2021",
 "HasCoordinate is true",
 "OccurrenceStatus is Present",
 {
 "not" : {
 "BasisOfRecord" : [
 "is one of (Fossil, Living Specimen, Specimen, Material citation, Material sample)"
 ]
 }
 }
 ]
}

 The dataset includes 649 records from 6 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0063330-230530130749713/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25549/pcra-c14-182636
title: Tserkvi i relihiy̆ni orhanizatsiï Ukraïny v 2001 rotsi: dovidnyk = [Church and religious organizations in Ukraine in 2001: directory], 2002

description: [description english/roman)] State Committee of Ukraine on Religious Matters [Derzhavniy Komitet Ukraini u Spravakh religiy]. Church and religious organizations in Ukraine in 2001: directory [Tserkvi i relihiy̆ni orhanizatsiï Ukraïny v 2001 rotsi: dovidnyk]. Kiev, Ukraine: VIP, 2002.
DOI: 10.25549/pcra-c14-182655
title: Tserkvi i relihiy̆ni orhanizatsiï Ukraïny v 2001 rotsi: dovidnyk = [Church and religious organizations in Ukraine in 2001: directory], 2002

description: [description english/roman)] State Committee of Ukraine on Religious Matters [Derzhavniy Komitet Ukraini u Spravakh religiy]. Church and religious organizations in Ukraine in 2001: directory [Tserkvi i relihiy̆ni orhanizatsiï Ukraïny v 2001 rotsi: dovidnyk]. Kiev, Ukraine: VIP, 2002.
DOI: 10.15468/dl.4t8dgw
title: Occurrence Download

description: A dataset containing 26 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Ecuador",
 "TaxonKey is Gastrotheca psychrophila Duellman, 1974"
 ]
}

 The dataset includes 26 records from 3 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0026958-220831081235567/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.aech9v
title: Occurrence Download

description: A dataset containing 452 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Dendropsophus robertmertensi (Taylor, 1937))",
 "BasisOfRecord is one of (Specimen, Human Observation, Observation, Machine Observation)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 452 records from 19 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0057538-230224095556074/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.qdhhpx
title: Occurrence Download

description: A dataset containing 14023544 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Chinese Taipei",
 "OccurrenceStatus is Present"
 ]
}

 The dataset includes 14023544 records from 1407 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0339601-210914110416597/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.690656
title: (Appendix 1) Stable carbon and oxygen isotope ratios of benthic foraminifera in surface sediments of the South China Sea

description: Given are raw data, for adjustment values are given in Parameter comments. Adjustments of benthic isotope values to that of C. wuellerstorfi follow Shackleton et al. (1995 doi:10.2973/odp.proc.sr.138.117.1995) and Shackleton and Hall (1983 doi:10.2973/dsdp.proc.69.118.1983, 1990 doi:10.2973/odp.proc.sr.115.174.1990)
DOI: 10.5281/zenodo.15009322
title: THEORETICAL BASIS OF THE PRIMARY EDUCATION SYSTEM AND THE EXPERIENCE OF DEVELOPED COUNTRIES
DOI: 10.5281/zenodo.15009323
title: THEORETICAL BASIS OF THE PRIMARY EDUCATION SYSTEM AND THE EXPERIENCE OF DEVELOPED COUNTRIES
DOI: 10.1594/pangaea.67525
title: Stable isotope data of ODP Hole 154-925B (Table A2)
DOI: 10.1594/pangaea.834703
title: Oxygen isotopes of the planktic foraminifer Neogloboquadrina pachyderma (s) in MIS8 of IODP Site 303-1308

description: DEPTH, sediment/rock gives the modified composite splice depth [mcd].
DOI: 10.1594/pangaea.55126
title: Sedimentology of core PS2819-2
DOI: 10.1594/pangaea.912934
title: In-situ reference data for aboveground vegetation traits of pre-Alpine grasslands in southern Germany

description: # = NA
DOI: 10.1594/pangaea.730466
title: (Table 1) Stable oxygen isotope ratios of Cibicidoides wuellerstorfi from sediment core GeoB3935-2
DOI: 10.1594/pangaea.761833
title: Hydrochemistry measured on water bottle samples during POLARSTERN cruise ANT-VIII/2

description: On a section between 72°S and 42°S and a transect between 60°E and 10°E through the Weddell Sea and the southernmost eastern Atlantic Ocean, the water column was sampled on 72 stations, and the stable carbon isotopic composition of total dissolved inorganic carbon (delta13C(SumCO2)) as well as the stable oxygen isotopic composition of seawater (delta18O) was determined. These data were compared with potential temperature, salinity, dissolved oxygen and phosphate data from the same stations. The observed delta13C(SumCO2)/PO4[3-] relationship in the deep Weddell Sea strongly differs from the global Redfield-driven deep water relationship. We attribute this to enhanced thermodynamic fractionation at sites of bottom water formation that decouples the nutrient signal from the delta13C(SumCO2) signal not only in surface and intermediate water masses but also in deep and bottom water. Different, water-mass specific thermodynamic imprints due to different modes of bottom water formation are assumed to cause the observed deviation from the global delta13C(SumCO2)/PO4[3-] relationship in the deep Weddell Sea. The influence of increased photosynthetic fractionation, i.e., a more negative than low-latitude isotopic organic carbon composition, is shown to be minor. As a result, Recent Weddell Sea deep and bottom water delta13C(SumCO2) is by 0.4-0.5 per mil higher than expected if solely biologic fractionation would occur. A discussion of simple hypotheses of Weddell Sea deep and bottom water formation during glacial times reveals that regardless of what scenario is considered, the thermodynamic imprint on Southern Ocean deep water would increase. This makes it difficult to explain low glacial delta13C values observed in benthic foraminifera from the subpolar Southern Ocean as being calcified in Antarctic source bottom water and thus is in support of hypotheses looking for additional sites of deep water formation.
description: Supplement to: Mackensen, Andreas; Hubberten, Hans-Wolfgang; Scheele, Norbert; Schlitzer, Reiner (1996): Decoupling of d13CSUMCO2 and phosphate in recent Weddell Sea deep and bottom water: implications for glacial Southern Ocean paleoceanography. Paleoceanography, 11(2), 203-215
DOI: 10.1594/pangaea.693831
title: Stable isotopes in opal of sediment core PS58/271-1
DOI: 10.1594/pangaea.706927
title: (Table 2) Chemical composition of terrigenous material from sediment core TT013_32
DOI: 10.1594/pangaea.706928
title: (Table 2) Chemical composition of terrigenous material from sediment core TT013_72
DOI: 10.1594/pangaea.706929
title: (Table 2) Chemical composition of terrigenous material from sediment core TT013_83
DOI: 10.1594/pangaea.780636
title: (Table T2) Stable carbon and oxygen isotope ratios of Neogloboquadrina pachyderma (s) from ODP Hole 188-1166A
DOI: 10.1594/pangaea.733457
title: (Figure 5) Stable oxygen isotope ratios on bulk carbonate of sediment core MD03-2698

description: Depth is corrected.
DOI: 10.1594/pangaea.831197
title: (Appendix A) Oxygen isotopes, Mg/Ca ratios and estimated temperatures of sediment core MD01-2378 during Termination I
DOI: 10.1594/pangaea.67527
title: Stable isotope data of ODP Hole 154-925D (Table A2)
DOI: 10.1594/pangaea.690804
title: (Appendix A) Environmental and foraminiferal proxy data of surface sediments from the Chatham Rise

description: Samples are taken from the top few centimetres
DOI: 10.1594/pangaea.54686
title: Figure 2. Stable isotope analysis on sediment core PS2138-1
DOI: 10.1594/pangaea.784148
title: (Table T1) Oxygen and carbon isotope ratios for planktonic foraminifers of ODP Site 184-1143

description: Sediment depth is given in mbsf. Specimens were chosen from the &gt;154 µm fraction.
DOI: 10.1594/pangaea.218144
title: (Appendix 3) Stable oxygen isotope ratios of benthic foraminifera in sediment core MD01-2415

description: Measured on 2-3 species of the endobenthic foraminiferal species Uvigerina auberiana and Uvigerina aktiaensis (Uvigerina peregrina of authors) from the 250-500 um size fraction.
DOI: 10.1594/pangaea.59762
title: (Table 2c) Alkenones, stable isotopes and sea surface temperature from sediment core KC01
DOI: 10.1594/pangaea.59766
title: (Table 2d) Alkenones, stable isotopes and sea surface temperature from sediment core KC01B
DOI: 10.1594/pangaea.614885
title: Sample locations, stratigraphic information and listing of carbon and oxygen isotope data of the measured planktonic foraminifera of surface sediments in the western South Atlantic Ocean (Table 1)

description: We explored the potential to use the stable isotopic compositions of planktonic foraminifera as a proxy for the position of the Brazil-Malvinas Confluence (BMC) in the Argentine Basin. For this purpose, we measured the oxygen and carbon isotopic compositions of Globigerinoides ruber (pink and white varieties measured separately), Globigerinoides trilobus, Globigerina bulloides, Globorotalia inflata and Globorotalia truncatulinoides (left- and right-coiling forms measured separately) from a latitudinal transect of 56 surface sediment samples from the continental slope off Brazil, Uruguay and Argentina between 20 and 48°S. Lowest oxygen isotopes values were found in G. ruber (pink), followed by G. ruber (white) and G. trilobus reflecting the highly stratified near surface water conditions north of the BMC. Globigerina bulloides was present mainly south of the BMC and records subsurface conditions supporting earlier plankton tow studies. Globorotalia inflata and G. truncatulinoides (left and right) were both available over the whole transect and calcify in the depth level with the steepest temperature change across the BMC. Accordingly, the delta18O of these species depict a sharp gradient of 2‰ at the confluence with remarkably stable values north and south of the BMC. Our data show that the oxygen isotopic composition of G. inflata and G. truncatulinoides (left and right) are the most reliable indicators for the present position of the BMC and can therefore be used to define the past migration of the front if appropriate cores are available.
description: The abbreviations of the stratigraphy are defined as follows: IS, isotopic stratigraphy; 14C, 14C AMS dating, calibrated calendar age is given in parentheses; and SBF, stained benthic foraminifera. a This study; b Mollenhauer et al. (2006, doi:10.1016/j.dsr.2006.05.005); c Heil et al. (subm.); d Dürkoop (1998); e Harloff and Mackensen (1997, doi:10.1016/S0377-8398(96)00059-X). / Samples were taken from the uppermost centimeter of 54 multicores and 2 boxcores.
description: Supplement to: Chiessi, Cristiano Mazur; Ulrich, Shannon; Mulitza, Stefan; Pätzold, Jürgen; Wefer, Gerold (2007): Signature of the Brazil-Malvinas Confluence (Argentine Basin) in the isotopic composition of planktonic foraminifera from surface sediments. Marine Micropaleontology, 64(1-2), 52-66
DOI: 10.1594/pangaea.743242
title: (Table 2) Stable carbon and oxygen isotope of station GeoB9908-1
DOI: 10.1594/pangaea.856873
title: Stable isotopic composition of benthic foraminifera in Little Bahamas Banks sediments
DOI: 10.1594/pangaea.711135
title: (Table 1) Rock description and nitrogen concentrations and isotopic compositions of altered oceanic crust samples from ODP Site 185-1149

description: The basement at Site 801 is divided into 4 intervals (the alkaline basalt sills and 3 MORB sections) according to the geochemical characterization of more than 100 communal samples (Plank et al., 2000; http://www-odp.tamu.edu/publications/185_IR/185ir.htm). For each interval, one composite was made for submarine extrusives (FLO) and clastic rocks (VCL) by combing proportional communal samples. FLO and VCL are then combined into the MIX composite in a ratio of 30-70%. The SUPER composite was made for the entire MORB interval by combing the 3 MORB composites. The SED composite was made for the intercalated sediments in the upper 230 m of the basement (mostly in Sequences I, III, and IV, see descriptions by Plank et al. (2000); http://www-odp.tamu.edu/publications/185_IR/185ir.htm; Alt (2003); doi:10.1029/2002GC000400).
DOI: 10.1594/pangaea.831947
title: (Table S1) Carbonate content ans stable isotope record of samples from Farra d'Alpago and Possagno section
DOI: 10.1594/pangaea.788137
title: Stable isotope analyses of sediment core GeoB13602-1
DOI: 10.1594/pangaea.230283
title: (Appendix A7) Stable isotope data of ODP Hole175-1085A-42X to -63X (382.40-594.12 mbsf)

description: Reference depth=logging depth (mbsf) / The Hole was logged with a downhole logging tool string which included the NGT (Natural Gamma Tool) sondes.
DOI: 10.1594/pangaea.817328
title: (Table 1) Nutrient concentrations and carbon isotopes of sea ice segments and brine sampled during Nathaniel B. Palmer cruises NBP98-07 and NBP06-08, Ross Sea

description: We examined controls on the carbon isotopic composition of sea ice brines and organic matter during cruises to the Ross Sea, Antarctica in November/December 1998 and November/December 2006. Brine samples were analyzed for salinity, nutrients, total dissolved inorganic carbon (sum CO2), and the 13C/12C ratio of Sum CO2 (d13C(sum CO2)). Particulate organic matter from sea ice cores was analyzed for percent particulate organic carbon (POC), percent total particulate nitrogen (TPN), and stable carbon isotopic composition (d13C(POC)). Sum CO2 in sea ice brines ranged from 1368 to 7149 µmol/kg, equivalent to 1483 to 2519 µmol/kg when normalized to 34.5 psu salinity (s sum CO2), the average salinity of Ross Sea surface waters. Sea ice primary producers removed up to 34% of the available sum CO2, an amount much higher than the maximum removal observed in sea ice free water. Carbonate precipitation and CO2 degassing may reduce s sum CO2 by a similar amount (e.g., 30%) in the most hypersaline sea ice environments, although brine volumes are low in very cold ice that supports these brines. Brine d13C(sum CO2) ranged from -2.6 to +8.0 per mil while d13C(POC) ranged from -30.5 to -9.2 per mil. Isotopic enrichment of the sum CO2 pool via net community production accounts for some but not all carbon isotopic enrichment of sea ice POC. Comparisons of s sum CO2, d13C(sum CO2), and d13C(POC) within sea ice suggest that epsilon p (the net photosynthetic fractionation factor) for sea ice algae is ~8 per mil smaller than the epsilon p observed for phytoplankton in open water regions of the Ross Sea. These results have implications for modeling of carbon uptake and transformation in the ice-covered ocean and for reconstruction of past sea ice extent based on stable isotopic composition of organic matter in sediment cores.
description: Values given as 'raw' values and normalized to 34.5 psu salinity. Depth-integrated POC represents the mean of all cores at each station. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
description: Supplement to: Munro, David R; Dunbar, Robert B; Mucciarone, David A; Arrigo, Kevin R; Long, Matthew C (2010): Stable isotope composition of dissolved inorganic carbon and particulate organic carbon in sea ice from the Ross Sea, Antarctica. Journal of Geophysical Research, 115(C9), C09005
DOI: 10.1594/pangaea.707184
title: (Table 4, Appendix) Stable carbon isotope composition of bulk sediment from DSDP Hole 74-528
DOI: 10.1594/pangaea.943871
title: Radiosonde measurements in 2019-12 during MOSAiC Legs PS122/1 and PS122/2 (level 3 data)

description: This Level 3 dataset of radiosondes launched during the MOSAiC expedition has been processed by the Global Climate Observing System (GCOS) Reference Upper-Air Network (GRUAN) algorithm for RS41 radiosonde data. The GRUAN processing is based on the extensive characterisation of the sensor properties to produce a traceable reference data product which is free of manufacturer-dependent effects. Uncertainty values are provided for all measured parameters at all height levels. It should be noted that all provided height information is obtained from the GPS measurement. Close to buildings and metal surfaces (such as RV Polarstern) GPS signals are often very noisy, resulting in artifacts in the vertical elevation coordinate close to the surface. In the atmospheric boundary layer, it is therefore recommended to rely on height calculations based on pressure.Please note that the TAB-delimited ascii format data present only a subset of parameters. The complete GRUAN-processed data are available in the linked netCDF files.
DOI: 10.15468/dl.mwgv9p
title: Occurrence Download

description: A dataset containing 6930380 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Ecuador",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "Year 2018-2025"
 ]
}

 The dataset includes 6930380 records from 261 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0003651-250310093411724/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.26952436
title: Conservation genetics of Mahogany Gliders and their complex evolutionary relationship with Squirrel Gliders

description: These are the datasets and analysis scripts for the publication <i>"Conservation genetics of Mahogany Gliders and their complex evolutionary relationship with Squirrel Gliders"</i> submitted to Conservation Genetics 2024.<b>Abstract</b><br>Squirrel Gliders (<i>Petaurus norfolcensis</i>) are widely distributed throughout the woodlands of eastern Australia, while the similar but larger Mahogany Glider (<i>Petaurus gracilis</i>) inhabits the coastal woodlands of the Wet Tropics in northeastern Queensland. The Mahogany Glider is an Endangered species due to habitat loss and fragmentation. This study used single nucleotide polymorphism markers (SNPs) from field and museum-derived samples to investigate genetic relationships within the Squirrel/Mahogany Glider complex and conduct a conservation genetics assessment for the Mahogany Glider. Analyses of genetic structure, phylogenomics, and outlier loci identified four genetic groups: Mahogany Glider and three distinct groups in Squirrel Gliders (North Queensland, Cape Cleveland, and mid-eastern/south-eastern Queensland). We found genetic admixture between these groups, but whether the admixture is historic or current remains unclear. Squirrel Gliders from North Queensland were genetically more similar to Mahogany Gliders in some analyses than to the other two Squirrel Glider groups. Morphological analysis confirmed that Mahogany Gliders are distinguishable from other gliders primarily by their larger body size but did not provide clear differences for the other three genetic groups. We hypothesize that the four genetic groups represent four subspecies of Squirrel Glider, of which the Mahogany Glider is one. This hypothesis can be tested with further field sampling of genetics and morphology, particularly in identified areas of potential contact. When assessing Mahogany Gliders alone, we found a clear north–south split in genetic structuring, with the southern cluster being more structured than the northern cluster. Genetic diversity within Mahogany Gliders was generally comparable to that of Squirrel Gliders, but some sampling localities indicated loss of genetic diversity and low effective population size. Regardless of whether Mahogany Gliders are classified as a species or subspecies, their Endangered status underscores the need for targeted conservation efforts. The genetic findings offer practical pathways for on-ground management to enhance population recovery and connectivity.<br><b>Files in the repository</b>Data folder: data used in the analyses, including morphological data from museum and field specimens and SNPs data derived from DArT analysis.snp_filters.rmd - customized filtering steps for the glider genetics. Output different data formats and filtered status for downstream analyses.structure.rmd - Analyses of genetic structure.diversity_mgsq.rmd - Analyses of genetic diversity focused on the Mahogany and Squirrel Glider datasets.QM_SpeimenData.rmd - Analyses of morphological data from museum specimens.