cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.691196
title: Nutrient concentrations in water samples collected at Station MARCH-94-GN3619940280100740 in the Aegean Sea
DOI: 10.1594/pangaea.751036
title: Meteorological observations during PALLAS cruise from Spithead to Plymouth started at 1825-05-28
DOI: 10.1594/pangaea.924025
title: Water content of sediment core LR398
DOI: 10.1594/pangaea.663852
title: Oceanography at CTD/bottle station IFREMER_0692
DOI: 10.1594/pangaea.668505
title: Basic and other measurements of radiation at station Barrow (1999-10), Version 1

description: Ellsworth G. Dutton discovered a calibration glitch in the SWD "Short-wave downward (GLOBAL) radiation" data for Barrow, Alaska. SWD data was therefore removed from this dataset. Please refer to the updated Version 2 (see replaced by reference) with correct calibration.
DOI: 10.1594/pangaea.924026
title: Water content of sediment core LR400
DOI: 10.1594/pangaea.926759
title: Age model of sediment core M72/5_620-1
DOI: 10.1594/pangaea.838713
title: Lithology of sediment core NABAHNE, Na bahne, Czech Republic

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.845696
title: Radiosonde measurements from station Sapporo (2015-02)
DOI: 10.1594/pangaea.784854
title: (Appendix 1) Stable isotope ratios of planktonic foraminifers in sediment core POS287-06-3G obtained during Poseidon cruise POS287
DOI: 10.1594/pangaea.696447
title: (Table 3) Stable oxygen and carbon isotope ratios of benthic foraminifera from ODP Site 138-846 in the eastern equatorial Pacific

description: DEPTH, sediment [m] is given in mbsf. Adjustment factors for delta18O, using Uvigerina as standard, and for delta13C using Cibicidoides wuellerstorfi as standard. Uvigerina sp., d18O = 0.00, d13C = 0.90. Hoeglundina elegans, d18O = -0.40, d13C = -1.30. Cibicidoides wuellerstorfi, d18O = 6.64, d13C = 0.00. C. kullenbergi, d18O = 0.64, d13C = 0.00. Oridorsalis sp., d18O = 0.00, d13C = 1.00. Globocassidulina subglobosa, d18O = -0.10, d13C = 0.50. C. kullenbergi and C. wuellerstorfi, d18O = 0.64, d13C = 0.00. Nuttalides sp., d18O = 0.35, d13C = 0.00. Nuttalides and Cibicidoides sp., d18O = 0.40, d13C = 0.00. Sphaeroidina bulloides, d18O = -0.10, d13C = -0.10. Cibicidoides spp., d18O = 0.50, d13C = 0.00. Gyroidina sp., d18O = 0.00, d13C = 0.00. Globobulimina pacifica, d18O 0.00, d13C = NA.
DOI: 10.1594/pangaea.922143
title: Age determination of profile MAM_III
DOI: 10.1594/pangaea.720516
title: Documentation of sediment core GIK16560-1
DOI: 10.1594/pangaea.922142
title: Pollen content of MAM_III

description: Pollen analyst: Chun Chang HuangLaboratory: Palaeoenvironmental Research Unit, NUI Galway, Galway, IrelandDate pollen analysis completed 1992Sampling in the field: MAM IIIb, c (duplicate cores) sampled using 5 cm diameter Livingstone corer in 1 m drives; top-sediment (1 m) sampled (MAM IIIa) by Mackereth 1-m pneumatic corer. MAM III consists of MAM IIIa (0 to 86 cm; Mackereth core) & IIIc (86-420)"Stratigraphy: Mineral-rich (inorganic content &gt;50% throughout) dark gyttja; basal 20 cm silt/clay (end of YD)Length of core (Holocene only) (m): 4.3 mProfile SHE III (in cm): 0-418Pollen sampling details: sampling density: variable; varies between 2 to 12 cm; average 6 cm; samples 1 cm thick. Pollen preparation: Lycopodium spore suspension of known concentration added; acetolysis, mounted in glycerinePollen identification and counting: Cereal-type pollen differentiated using Beug (1961) criteria but 40 um (rather than 38 µm) taken as cutoff point. Pollen nomenclature generally follows Moore et al. 1991. &lt;1 = recorded outside the pollen counts (most samples searched for additional taxa). Distinction between Myrica and Corylus made Charcoal particles ≥37 um counted during routine pollen counting
DOI: 10.1594/pangaea.756727
title: (Table 20) Ranges of benthic foraminifers from the late Neogene through the Pleistocene in ODP Hole 115-709A

description: Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because benthic foraminifers are not common in most samples, in many instances the numbers represent their true abundance in a sample. Only the bolivinids reached abundances of 6 or greater.
DOI: 10.1594/pangaea.924016
title: Bulk density of sediment core LR398

description: Measured on the unopened cores using the Geotek MSCL scanner, and represents the gamma density (g/cm³) from the Gamma Ray Attenuation Porosity Evaluator.
DOI: 10.1594/pangaea.779819
title: Hradec Králové total ozone assimilated time series from 1961 to 2010

description: Homogenized data series of total ozone measurements taken by the regularly and well calibrated Dobson and Brewer spectrophotometers at Hradec Králové (Czech) and the data from the re-analyses ERA-40 and ERA-Interim were assimilated and combined to investigate differences between the particular data sets over Central Europe, the NH mid-latitudes. The Dobson-to-Brewer transfer function and the algorithm for approximation of the data from the re-analyses were developed, tested and applied for creation of instrumentally consistent and completed total ozone data series of the 50-year period 1961-2010 of observations. The assimilation has reduced the well-known seasonal differences between Dobson and Brewer data below the 1% calibration limit of the spectrophotometers. Incorporation of the ERA-40 and ERA-Interim total ozone data on days with missing measurements significantly improved completeness and reliability of the data series mainly in the first two decades of the period concerned. Consistent behaviour of the original and assimilated data sets was found in the pre-ozone-hole period (1961-1985). In the post-Pinatubo (1994-2010) era the data series show seasonal differences that can introduce uncertainty in estimation of ozone recovery mainly in the winter-spring season when the effect of the Montreal Protocol and its Amendments is expected. All the data sets confirm substantial depletion of ozone also in the summer months that gives rise to the question about its origin. The assimilated and completed data series of total ozone will be further analyzed to quantify chemical ozone losses and contribution of natural atmospheric processes to the ozone depletion over the region. This case study points out importance of selection and evaluation of the quality and consistency of the input data sets used in estimation of long-term ozone changes including recovery of the ozone layer over the selected areas.
description: Project: Long-term Changes of the Ozone Layer Over the Territory of the Czech Republic. The Czech Grant Agency, Project No. P209/10/0058, 2010-2012. Global Atmosphere Watch Programme (GAW), http://www.wmo.int/pages/prog/arep/gaw/gaw_home_en.html
DOI: 10.1594/pangaea.922144
title: Macrofossils of profile MAM_III
DOI: 10.1594/pangaea.926760
title: Paleomagnetic results of sediment core M72/5_620-1
DOI: 10.1594/pangaea.664889
title: Oceanography at CTD/bottle station IFREMER_1729
DOI: 10.1594/pangaea.845762
title: Meteorological synoptical observations from station Ny-Ålesund (2014-06)

description: On 2016-07-06 some corrections on the wind speed were made for this dataset and a decimal was added to the atmospheric pressure value. The old version is available at: ftp://ftp.bsrn.awi.de/nya/OldVersions_2016-07-06_oldSYNOPS/
DOI: 10.1594/pangaea.924017
title: Bulk density of sediment core LR400

description: Measured on the unopened cores using the Geotek MSCL scanner, and represents the gamma density (g/cm³) from the Gamma Ray Attenuation Porosity Evaluator.
DOI: 10.1594/pangaea.926053
title: LOI of profile MAM_III
DOI: 10.1594/pangaea.926063
title: Physical properties of profile MAM_III
DOI: 10.1594/pangaea.870139
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_IX_05
DOI: 10.1594/pangaea.496057
title: Water temperature MBT profiles from cruise U90X000990M_1980
DOI: 10.1594/pangaea.805240
title: Basic measurements of radiation at station Sapporo (2012-10)
DOI: 10.1594/pangaea.926826
title: Plant species composition from northern peatlands
DOI: 10.1594/pangaea.921566
title: (Supplement 1) Phytoplankton and dinoflagellate stoichiometry in the FlowCam experiment

description: This dataset comprises data from two experiments analysed with two different tools, a FlowCam and a microscope. The heterotrophic dinoflagellate Oxyrrhis marina was subjected to different feeding treatments (starved, or fed with either F/2 nutrient reach, nitrogen-limited, or phosphorus-limited phytoplankton of the species Rhodomonas salina). The carbon:nitrogen:phosphorus stoichiometry of the different phytoplankton and dinoflagellate cultures was measured. The nitrogen-limited and phosphorus-limited phytoplankton were mixed and the mixture was offered as food to the dinoflagellates previously fed on either nitrogen-limited, or phosphorus-limited phytoplankton. The selective feeding of the dinoflagellate on the two mixed algal qualities was measured.
DOI: 10.1594/pangaea.895008
title: Sea surface temperature measurements during typhoon Morakot in 2009 at Suao Buoy
DOI: 10.1594/pangaea.728672
title: (Table 5) Varimax Principal Component scores of live associations &gt;125 µm
DOI: 10.1594/pangaea.921567
title: (Supplement 2) Phytoplankton and dinoflagellate stoichiometry in the Microscopy experiment

description: This dataset comprises data from two experiments analysed with two different tools, a FlowCam and a microscope. The heterotrophic dinoflagellate Oxyrrhis marina was subjected to different feeding treatments (starved, or fed with either F/2 nutrient reach, nitrogen-limited, or phosphorus-limited phytoplankton of the species Rhodomonas salina). The carbon:nitrogen:phosphorus stoichiometry of the different phytoplankton and dinoflagellate cultures was measured. The nitrogen-limited and phosphorus-limited phytoplankton were mixed and the mixture was offered as food to the dinoflagellates previously fed on either nitrogen-limited, or phosphorus-limited phytoplankton. The selective feeding of the dinoflagellate on the two mixed algal qualities was measured.
DOI: 10.1594/pangaea.688789
title: Radiosonde M16_R007 during METEOR cruise M16 on 1969-01-27 21:04h

description: Height of tropause 19070 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.510891
title: Radiosonde at Georg-Forster station on 1990-11-06 00:00h

description: Height of tropopause 10937 m, total ozone 155.9 DU
DOI: 10.1594/pangaea.695213
title: Monthly landings destined for Smoking, Chile, 1998
DOI: 10.1594/pangaea.747945
title: Meteorological observations during CONWAY cruise from Panama to Acapulco started at 1822-02-07
DOI: 10.1594/pangaea.750393
title: Meteorological observations during Le Saumon cruise from Guadeloupe to Brest started at 1786-07-13
DOI: 10.1594/pangaea.815947
title: (Table 3) Relative contribution of diatom size fractions in water samples obtained near Point Barrow 2005-2006
DOI: 10.1594/pangaea.752041
title: Meteorological observations during SCOURGE cruise from Falmouth to Demerara started at 1797-06-08
DOI: 10.1594/pangaea.818805
title: Glacier mass balance Hintereisferner, Ötztal Alps, Austria, 1983/1984
DOI: 10.1594/pangaea.926773
title: (Supplement 4) Selective feeding of dinoflagellate in the Microscopy experiment

description: This dataset comprises data from two experiments analysed with two different tools, a FlowCam and a microscope. The heterotrophic dinoflagellate Oxyrrhis marina was subjected to different feeding treatments (starved, or fed with either F/2 nutrient reach, nitrogen-limited, or phosphorus-limited phytoplankton of the species Rhodomonas salina). The carbon:nitrogen:phosphorus stoichiometry of the different phytoplankton and dinoflagellate cultures was measured. The nitrogen-limited and phosphorus-limited phytoplankton were mixed and the mixture was offered as food to the dinoflagellates previously fed on either nitrogen-limited, or phosphorus-limited phytoplankton. The selective feeding of the dinoflagellate on the two mixed algal qualities was measured.
DOI: 10.1594/pangaea.926772
title: (Supplement 3) Selective feeding of dinoflagellate in the FlowCam experiment

description: This dataset comprises data from two experiments analysed with two different tools, a FlowCam and a microscope. The heterotrophic dinoflagellate Oxyrrhis marina was subjected to different feeding treatments (starved, or fed with either F/2 nutrient reach, nitrogen-limited, or phosphorus-limited phytoplankton of the species Rhodomonas salina). The carbon:nitrogen:phosphorus stoichiometry of the different phytoplankton and dinoflagellate cultures was measured. The nitrogen-limited and phosphorus-limited phytoplankton were mixed and the mixture was offered as food to the dinoflagellates previously fed on either nitrogen-limited, or phosphorus-limited phytoplankton. The selective feeding of the dinoflagellate on the two mixed algal qualities was measured.
DOI: 10.1594/pangaea.858020
title: Radiosonde measurements from station Minamitorishima (2015-12)
DOI: 10.1594/pangaea.779658
title: Regional surface soil moisture and freeze/thaw timing remote sensing products with links to geotiff images

description: The SAR Surface Soil Moisture (SSM) product is derived from the ENVISAT ASAR sensor operating in Global Monitoring (GM) mode (Pathe et al. 2009) based on the approach of Wagner et al. (1999). The SAR SSM product is delivered as weekly mean composites at the 1 km spatial resolution. The version 2 release of the data covers the years 2005 through 2011 for the regional sites Ob Estuary, Alaska, Mackenzie and Central Yakutia. For the Laptev Sea Coast site the product is provided for 2005 through 2010. Product availability is limited to availability of ASAR GM data (Sabel et al. 2012).The SAR Surface Soil Moisture parameter represents a relative measure of the soil moisture in the top layer of the soil, scaled between references corresponding approximately to wilting level (0%) and field capacity (100%) (Wagner et al. 1999).In addition to the SSM maps, quality indicator maps provide information on the number of individual SSM retrievals that were averaged in order to achieve the corresponding weekly SSM composites. Furthermore, for each region, the mask applied to the SSM maps is supplied in a GeoTIFF file.More information about the SSM part of dataset can be found in hdl:10013/epic.39180.d001.The Synthetic Aperture Radar (SAR) Freeze/Thaw (F/T) product is as well derived from data acquired by the ENVISAT ASAR sensor operating in Global Monitoring (GM) mode (Park et al. 2010).The SAR F/T product represents timing (day of year) of ground surface freeze-up and thawing at a resolution of 1 km. The version 2 release of the data covers the years 2005 through 2010 for the regional sites Ob Estuary, Alaska, Mackenzie, Laptev Sea Coast and Central Yakutia. Product quality and geographical coverage is strongly dependent on the availability of ASAR GM data. Therefore information of available number of measurements per year is supplied with the dataset.Overview figures:- Thawing in 2010, regional product, Canada: hdl:10013/epic.39181.d002- Freezing in 2010, regional product, Canada: hdl:10013/epic.39181.d003Product guides:- ESA DUE Permafrost SAR Surface Soil Moisture v2 product guide: hdl:10013/epic.39180.d001- ESA DUE Permafrost SAR Freeze/Thaw v2 product guide: hdl:10013/epic.39181.d001This dataset is part of the ESA Data User Element (DUE) Permafrost Full Product Set (doi:10.1594/PANGAEA.780111).
DOI: 10.1594/pangaea.871973
title: Radiosonde measurements from station Ishigakijima (2016-12)
DOI: 10.1594/pangaea.818859
title: Elevation zones Hintereisferner, Ötztal Alps, Austria, 1972/1973
DOI: 10.1594/pangaea.779580
title: (Table 5) Pb isotopic ratios of ODP Leg 130 basalts

description: Pb isotopic ratios are present-day values, corrected for fractionation using the NBS 981 standard values of Todt et al. (1984); the total ranges measured for NBS 981 are +0.008 for 206Pb/2O4Pb, ±0.008 for 207Pb/204Pb, and ±0.030 for 208Pb/2O4Pb. Within-run uncertainties (2 sigma m) on the isotopic data above are generally less than these values, and in all cases less than ±0.012, ±0.012, and ±0.038. Estimated uncertainty on Pb abundances is
DOI: 10.1594/pangaea.759950
title: Radiosonde measurements from station Minamitorishima (2011-01)
DOI: 10.1594/pangaea.870134
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_IV_25
DOI: 10.1594/pangaea.810263
title: Brachiopods in Early Carboniferous

description: Changes in Mississippian global paleogeography derived from the reconfiguration of the continents, a reversal in ocean currents and global cooling. Although the tectonic and climatic changes are well-documented, their effects on the distribution of brachiopod fauna are poorly documented. Here we present systematic quantitative analyses on global paleobiogeography based on a global brachiopod database from the Mississippian (i.e., Tournaisian, Visean, and Serpukhovian). The dataset consists of 2123 species of 344 brachiopod genera from 1156 localities. Our results reveal that global provincialism was not evident during the Tournaisian and Visean Stages. Two realms, i.e., the Gondwanan and Paleoequatorial Realms, are recognized during the Tournaisian. The Paleoequatorial Realm dominates during the Visean Stage, whereas the Gondwanan Realm is not documented due to the absence of data points. In contrast to the early and middle Mississippian stages, faunal provincialism is greatly enhanced in the Serpukhovian Stage with Paleotethyan and North American realms easily distinguished. This indicates that the Rheic Ocean was closed before the Serpukhovian due to the collision between Gondwana and Laurussia, that disrupted faunal interchange between the Paleotethys and North America. In addition, the paleolatitude-related thermal gradient was enhanced and the Boreal Realm was distinguished from the Paleotethyan Realm during the onset of the Late Palaeozoic Ice Age (LPIA) in the Serpukhovian. The paleolatitude diversity gradient pattern further shows a distinct shift of diversity center from the southern tropic zone in the Tournaisian and Visean to the northern tropic zone in the Serpukhovian.
description: Supplement to: Qiao, Li; Shen, Shu-zhong (2014): Global paleobiogeography of brachiopods during the Mississippian—Response to the global tectonic reconfiguration, ocean circulation, and climate changes. Gondwana Research, 26(3-4), 1173-1185
DOI: 10.1594/pangaea.848431
title: Radiosonde measurements from station Minamitorishima (2015-05)
DOI: 10.1594/pangaea.849360
title: Meteorological synoptical observations from station Sapporo (2015-07)
DOI: 10.1594/pangaea.494575
title: Physical oceanography during cruise CUSNS_1947
DOI: 10.1594/pangaea.688766
title: Meteorology at radiosonde positions during METEOR cruise M49

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.688769
title: Meteorology at radiosonde positions during METEOR cruise M6

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.871979
title: Radiosonde measurements from station Sapporo (2016-12)
DOI: 10.1594/pangaea.870208
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_VII_25
DOI: 10.1594/pangaea.899322
title: Meteorological synoptical observations from station Sapporo (2019-01)
DOI: 10.1594/pangaea.723851
title: Radiosonde measurements from station Southern Great Plains (2008-05)

description: Launches at irregular time intervals. The radiosonde measurements from station Southern Great Plains are used for Billings and E13
DOI: 10.1594/pangaea.695636
title: Radiosonde measurements from station Sede Boqer (2006-11)

description: Wind speed was multiplied by a factor of 0.1 (2009-08-28). Start location: Bet-Dagan, Israel; Distance from radiation site: 120 km
DOI: 10.1594/pangaea.810236
title: (Table 1) Organic carbon isotopic composition in Cretaceous sediments at DSDP Hole 75-530A

description: Cretaceous sediments from DSDP Site 530 have been analyzed for organic carbon isotopic composition. The d13C values in the sediments decrease from -22.7 per mil to -27.5 per mil in the following order: light-olive green mudstone/claystone, dark brown-red mudstone/siltstone/claystone, and black shale. This large range is primarily the result of variation in the relative amounts of terrestrial organic carbon superimposed on that derived from marine organisms.The black shales have an average d13C value of -25.9 per mil (range is from -23.7 per mil to -27.5 per mil). These values indicate that they originated primarily in terrigenous organic materials.The average d13C value present throughout the Cretaceous suggests that a large amount of terrestrial organic matter was supplied into this paleoenvironment, except during the Campanian, when an average d13C of -23.9 per mil is found near the marine end of the range.
description: Supplement to: Nohara, Masato; Ishizuka, Toshio; Gieskes, Joris M (1984): Organic carbon isotopic composition in Cretaceous sediments, Angola Basin, southeastern Atlantic, Deep Sea Drilling Project Site 530. In: Hay, WW; Sibuet, J-C; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 75, 1051-1054
DOI: 10.1594/pangaea.780335
title: Radiosonde measurements from station Minamitorishima (2012-02)
DOI: 10.1594/pangaea.902945
title: Meteorological synoptical observations from station Minamitorishima (2019-03)

description: Version 2, 2019-06-29, Error in metadata about instruments corrected
DOI: 10.1594/pangaea.845396
title: Horizon at station Fukuoka (after 2014-12)
DOI: 10.1594/pangaea.691095
title: Nutrient concentrations in water samples collected at Station DEC94-JAN95-GN3619940280400261 in the Aegean Sea
DOI: 10.1594/pangaea.869952
title: Links to master tracks in different resolutions from POLAR 2 flight ANT_2005/06_01
DOI: 10.1594/pangaea.911837
title: Meteorological synoptical observations from station Fukuoka (2019-11)
DOI: 10.1594/pangaea.810268
title: (Table 1) Near surface water chemistry of south Patagonian waters during spring and winter

description: Both the biomass of autotrophic dinoflagellates and its contribution to total chlorophyll were found to increase significantly with seawater temperature and the level of stratification in southern Patagonian waters during spring and winter. The highest peak of biomass corresponded to a single species, Prorocentrum minimum (Pavillard) Schiller, and was detected in middle shelf waters, coinciding with the primary productivity and CO2 uptake maxima reported for the area under spring conditions.
description: Wind speed was originally given in knots and was converted into m/s by multiplying by 0.51444. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
description: Supplement to: Gómez, Maréa Inés; Piola, Alberto R; Kattner, Gerhard; Alder, Viviana A (2011): Biomass of autotrophic dinoflagellates under weak vertical stratification and contrasting chlorophyll levels in subantarctic shelf waters. Journal of Plankton Research, 33(8), 1304-1310
DOI: 10.1594/pangaea.899303
title: Meteorological synoptical observations from station Fukuoka (2019-01)
DOI: 10.1594/pangaea.913543
title: Radiosonde measurements from station Ishigakijima (2020-01)
DOI: 10.1594/pangaea.870382
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2010/11_45
DOI: 10.1594/pangaea.665041
title: Oceanography at CTD/bottle station IFREMER_1881
DOI: 10.1594/pangaea.901897
title: Radiosonde measurements from station Ishigakijima (2019-03)
DOI: 10.1594/pangaea.747367
title: Meteorological observations during AMSTEL cruise from Curacao to Rio de Janeiro started at 1827-02-01