cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.741833
title: Lithology of sediment core WAXECK, Waxeckalm, Austria

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.741806
title: Lithology of sediment core UITBERG, Uitbergen, Belgium

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.955766
title: Radiosonde measurements from station Barrow (2021-10)

description: Start location: Point Barrow; Distance from radiation site: 8 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.749237
title: Meteorological observations during EURIDICE cruise from West Indies to Vlissingen started at 1819-04-01
DOI: 10.1594/pangaea.939716
title: High-resolution non-sea-salt sulphur and sea-salt sodium data of firn core OH-12 from Plateau Laclavere, northern Antarctic Peninsula

description: The firn core OH-12 was retrieved from Plateau Laclavere, a small ice cap on the northernmost end of the Antarctic Peninsula at about 1090 m above sea level in January 2016. The core was drilled down to 19.93 m depth. Glacio-chemical parameters (hydrogen peroxide, sulphur, sodium, black carbon) were determined in summer 2017 using a Continuous Flow Analysis (CFA) system as described by Röthlisberger et al. (2000) and McConnell et al. (2002, 2007). Sulphur and sodium concentrations were measured using two Thermo Finnigan Element2 High Resolution-Inductively Coupled Plasma-Mass Spectrometry (HR-ICP-MS) instruments. Values of sea-salt sodium (ssNa) and non-sea-salt sulphur (nssS) were calculated from sodium and sulphur concentrations applying the approach of Röthlisberger et al. (2002) and Sigl et al. (2013) and using relative abundances from Bowen (Bowen, 1979). The core was dated using annual layer counting of hydrogen peroxide measurements. We additionally accounted for precipitation intermittency at the drill site by using precipitation data from the European Centre for Medium-Range Weather Forecasts (ECMWF) ERA5 Reanalysis extracted from the grid point closest to the firn-core drill site. The core covers the period from July 2011 to January 2016. The data has been used for investigating recent climate and environmental changes in the northern Antarctic Peninsula region providing the basis for the retrieval and analysis of a deeper ice core from the same site.
DOI: 10.1594/pangaea.955767
title: Basic and other measurements of radiation at station Barrow (2021-11), Version 1

description: Old Version with errors, please use new version (see Replaced by reference).
DOI: 10.1594/pangaea.511030
title: Radiosonde at Georg-Forster station on 1986-11-23 12:00h

description: Height of tropopause 9029 m, total ozone 256.1 DU
DOI: 10.1594/pangaea.792607
title: (Table 7) Heavy and light mineral composition of the coarse silt fraction of sediments obtained from the Volga River delta

description: Without preliminary recalculation, the average contents of opaque minerals are 26.6 and 23.5%, respectively; the average contents of altered rocks and minerals are 21.6 and 22.2%, respectively.
DOI: 10.1594/pangaea.881324
title: Documentation of sediment core K7905-001BC
DOI: 10.1594/pangaea.955768
title: Radiosonde measurements from station Barrow (2021-11)

description: Start location: Point Barrow; Distance from radiation site: 8 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.932845
title: Basic measurements of radiation at station Cener (2021-05)
DOI: 10.1594/pangaea.939717
title: High-resolution hydrogen peroxide data of firn core OH-12 from Plateau Laclavere, northern Antarctic Peninsula

description: The firn core OH-12 was retrieved from Plateau Laclavere, a small ice cap on the northernmost end of the Antarctic Peninsula at about 1090 m above sea level in January 2016. The core was drilled down to 19.93 m depth. Subsamples for stable water isotope analysis were obtained from the core at 5 cm resolution. Glacio-chemical parameters (hydrogen peroxide, sulphur, sodium, black carbon) were determined in summer 2017 using a Continuous Flow Analysis (CFA) system as described by Röthlisberger et al. (2000) and McConnell et al. (2002, 2007). The core was dated using annual layer counting of hydrogen peroxide measurements. We additionally accounted for precipitation intermittency at the drill site by using precipitation data from the European Centre for Medium-Range Weather Forecasts (ECMWF) ERA5 Reanalysis extracted from the grid point closest to the firn-core drill site. The core covers the period from July 2011 to January 2016. The data has been used for investigating recent climate and environmental changes in the northern Antarctic Peninsula region providing the basis for the retrieval and analysis of a deeper ice core from the same site.
DOI: 10.1594/pangaea.496564
title: Water temperature XBT profiles from cruise U99X115774_1994
DOI: 10.1594/pangaea.750834
title: Meteorological observations during Na sa de Aranzazu cruise from Noka to Monterrey started at 1792-10-03
DOI: 10.1594/pangaea.752058
title: Meteorological observations during SEAHORSE cruise started at 1756-08-05
DOI: 10.1594/pangaea.747066
title: Meteorological observations during SHOREHAM cruise from Spithead to Madeira started at 1753-05-24
DOI: 10.1594/pangaea.936487
title: Calcium/titanium ratio in sediment core KN18

description: The elemental composition (log (Ca/Ti) ratio) was measured in 0.5 cm resolution.
DOI: 10.1594/pangaea.499583
title: Physical oceanography from BT during cruise U90XX08719B_1968
DOI: 10.1594/pangaea.747898
title: Meteorological observations during CHICHESTER cruise from Spithead to Barbados started at 1803-05-20
DOI: 10.1594/pangaea.783424
title: (Table 2) Oxygen isotope composition of authigenic and detrital phosphates from ODL Leg 201 sites

description: Many (bio)geochemical processes that bring about changes in sediment chemistry normally begin at the sediment-water interface, continue at depth within the sediment column and may persist throughout the lifetime of sediments. Because of the differential reactivity of sedimentary phosphate phases in response to diagenesis, dissolution/precipitation and biological cycling, the oxygen isotope ratios of phosphate (d18OP) can carry a distinct signature of these processes, as well as inform on the origin of specific P phases. Here, we present results of sequential sediment extraction (SEDEX) analyses combined with d18OP measurements, aimed at characterizing authigenic and detrital phosphate phases in continental margin sediments from three sites (Sites 1227, 1228 and 1229) along the Peru Margin collected during ODP Leg 201. Our results show that the amount of P in different reservoirs varies significantly in the upper 50 m of the sediment column, but with a consistent pattern, for example, detrital P is highest in siliciclastic-rich layers. The d18OP values of authigenic phosphate vary between 20.2 per mil and 24.8 per mil and can be classified into at least two major groups: authigenic phosphate precipitated at/near the sediment-water interface in equilibrium with paleo-water oxygen isotope ratios (d18Ow) and temperature, and phosphate derived from hydrolysis of organic matter (Porg) with subsequent incomplete to complete re-equlibration and precipitated deeper in the sediments column. The d18OP values of detrital phosphate, which vary from 7.7-15.4 per mil, suggest two possible terrigenous sources and their mixtures in different proportions: phosphate from igneous/metamorphic rocks and phosphate precipitated in source regions in equilibrium with d18Ow of meteoric water. More importantly, original isotopic compositions of at least one phase of authigenic phosphates and all detrital phosphates are not altered by diagenesis and other biogeochemical changes within the sediment column. These findings help to understand the origin and provenance of P phases and paleoenvironmental conditions at/near the sediment-water interface, and to infer post-depositional activities within the sediment column.
description: Supplement to: Jaisi, Deb P; Blake, Ruth E (2010): Tracing sources and cycling of phosphorus in Peru Margin sediments using oxygen isotopes in authigenic and detrital phosphates. Geochimica et Cosmochimica Acta, 74(11), 3199-3212
DOI: 10.1594/pangaea.936490
title: Geochemical data of sediment core KN18

description: Total organic carbon (TOC), total nitrogen, bulk δ^13^C~TOC~, δ^15^N and biogenic silica were measured in 2 cm resolution.
DOI: 10.1594/pangaea.722892
title: Other measurements at 10 m from station Rock Springs (1999-07)

description: Version 2, 2009-06-26
DOI: 10.1594/pangaea.610266
title: Physical oceanography at station SO177/2-78
DOI: 10.1594/pangaea.665211
title: Oceanography at CTD/bottle station IFREMER_2051
DOI: 10.1594/pangaea.610269
title: Physical oceanography at station SO177/2-86
DOI: 10.1594/pangaea.722901
title: Other measurements at 10 m from station Rock Springs (1999-10)

description: Version 2, 2009-06-26
DOI: 10.1594/pangaea.748754
title: Meteorological observations during ECHO cruise from Plymouth to Newfoundland started at 1783-07-10
DOI: 10.1594/pangaea.747344
title: Meteorological observations during AMBUSCADE cruise from Spithead to Barbados started at 1796-05-19
DOI: 10.1594/pangaea.910668
title: (Table S05) Ichthyolith abundance in ODP Hole 113-689B

description: Ichthyolith counts (&gt;38µm) and calculated ichthyolith accumulation rates determined in this study. Age model after Mackensen and Ehrmann 1992. (Table 2). Adjusted to GTS 2012; See Table S6 (this study doi:10.1594/PANGAEA.910669). Sediment dry bulk density (DBD) from: Faul and Delany 2010 (Table S2b), data: doi:10.1594/PANGAEA.831403. Variable DBD does not make a significant difference in calcualations of IAR (See supplement to: Sibertet al. 2014). 64695 Used varibale dry bulk density values in figures.
DOI: 10.1594/pangaea.751261
title: Meteorological observations during POLLUX cruise from Batavia to Texel started at 1827-04-01
DOI: 10.1594/pangaea.771026
title: (Table 5) Diatom zonation of samples from ODP Leg 127
DOI: 10.1594/pangaea.509792
title: Physical oceanography at station Rigel-7 from date 2005-11-24, Chipana, Chile
DOI: 10.1594/pangaea.496791
title: Physical oceanography from BT during cruise K58SOB_1939
DOI: 10.1594/pangaea.770945
title: (Table 3) Distribution of radiolarians from ODP Hole 128-798C

description: Species abundance: A = abundant, C = common, F = few, R = rare, - = absent.
DOI: 10.1594/pangaea.932710
title: CDOM dynamics in the presence of inorganic (silica gel) versus polystyrene plastic particles: a laboratory study - oxygen concentrations

description: The present dataset relates to a study that explored dissolved organic matter dynamics under three scenarios: a particle-free environment, a particle-enriched system with polystyrene microplastics, and a particle-enriched system with inorganic particles (water insoluble SiO₂). In part 1 of the experiment, natural marine organic matter was obtained by culturing a non-axenic strain of Chaetoceros socialis in 2 L flasks under each of three scenarios (1C = control, 2PS = polystyrene, 3S = silica). Dissolved oxygen concentration was used as a proxy for bacterial activity. Oxygen was measured in each cuvette of all of the three scenarios 1C, 2PS and 3S with a FireSting Oxygen needle-type optical probe and temperature sensor, PyroScience® (Aachen, Germany), at the beginning of part 2 (day 7, t7).
DOI: 10.1594/pangaea.708398
title: (Table 2) Isotopic analyses and carbon contents of C-O-H fluids in ODP Hole 118-735B extracted by step-heating at temperatures &gt;1000°C
DOI: 10.1594/pangaea.891356
title: Meteorological synoptical observations from station Payerne (2011-12)
DOI: 10.1594/pangaea.747512
title: Meteorological observations during ASIA cruise from Madagascar to Table Bay started at 1780-07-28
DOI: 10.1594/pangaea.916841
title: 1-Hz PPP displacements at GEONET station 0653 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.808025
title: (Figure 9) Radiolarian range chart of ODP Site 138-852, part I

description: DEPTH, sediment is given in mbsf. Relative abundance of individual species: R = rare (&lt;10 specimens); F = few, (10-100 specimens); C = common (100-200 specimens), and A = abundant (&gt;200 specimens). A- signifies that a species was looked for and not found, small case letters = specimens found that are thought to be reworked, ? = a dubious identification.
DOI: 10.1594/pangaea.788695
title: Basic and other measurements of radiation at station Alert (2005-06)
DOI: 10.1594/pangaea.547839
title: Nutrients measured on water bottle samples at station Bm_1997-09-01_2, Bajo Molle, Chile
DOI: 10.1594/pangaea.722888
title: Other measurements at 10 m from station Rock Springs (1999-06)

description: Version 2, 2009-06-26
DOI: 10.1594/pangaea.835099
title: SIRGAS reference frame realization SIR11P01: Multi-year solution for 230 GNSS station positions and linear velocities, including weekly residual time series, link to data files in zip archive

description: This solution is available in SINEX format (SIR11P01.SNX; including station positions and velocities) and in different text files containing station positions (SIR11P01.CRD), station velocities (SIR11P01.VEL) and residual time series (SIR11P01.PLT).
DOI: 10.1594/pangaea.477772
title: Hydrochemistry measured on water bottle samples at station SPac_1967_ET_43S/66

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.895646
title: (Table 2) Linear equations for hydrogen isotope correlation
DOI: 10.1594/pangaea.916880
title: 1-Hz PPP displacements at GEONET station 0695 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.932509
title: Processed hourly current meter data from Mooring EB3/2 2017-2018

description: This data set contains current meter measurement data from deep-sea mooring EB3/2 deployed in the North Atlantic Eastern Boundary (EB) region at Goban Spur from June 2017 to April 2018. The mooring is part of an array that represents the eastern extension of the basin-wide "North Atlantic Changes" (NOAC) ocean observatory deployed along 47°N. Data were interpolated on a regular hourly time grid.
DOI: 10.1594/pangaea.509794
title: Physical oceanography at station Rigel-9 from date 2005-11-24, Chipana, Chile
DOI: 10.1594/pangaea.916853
title: 1-Hz PPP displacements at GEONET station 0666 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.907773
title: XRD diffractograms of silt samples from lake sediment core HAP0212
DOI: 10.1594/pangaea.916863
title: 1-Hz PPP displacements at GEONET station 0677 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.665347
title: Oceanography at CTD/bottle station IFREMER_2187
DOI: 10.1594/pangaea.758897
title: (Table 1) Benthic foraminifer and ostracode stable carbon and oxygen isotope ratios of ODP Site 120-748

description: Size fraction &gt;150 µm.
DOI: 10.1594/pangaea.499586
title: Physical oceanography from BT during cruise U90XX08724B_1968
DOI: 10.1594/pangaea.747025
title: Meteorological observations during PHILADELPHIA cruise from Guinea to Suriname started at 1753-10-27
DOI: 10.1594/pangaea.761114
title: (Table 2) Color and chemical composition of earliest Cretaceous sediments off nortwestern Australia

description: All major elements calculated for LOI-free, assuming that most of LOI corresponds to smectite-bound H2O (11%-19%). Samples were not desalinated (Na2O values may be too high-an assumption not confirmed by SEM investigations).
DOI: 10.1594/pangaea.855252
title: Basic measurements of radiation at station Xianghe (2015-09)
DOI: 10.1594/pangaea.747533
title: Meteorological observations during ASTUTO cruise from El Callao de Lima to Cádiz started at 1778-03-13, Version 8

description: 1778-06-28T14:00: AYER SE VIERON VOLADORES, Y HOY RABIJUNCOS, ALGÚN SARGAZO Y VOLADORES., MAR LLANA, VTO GALENO HASTA LAS 5 QUE SE EMPEZÓ A SENTIR ALGUNA MAR DEL O (...) A LAS 9 1/2 DE LA NOCHE EMPEZAMOS A PERCIBIRE POR LA PARTE DEL N UNA GRAN CLARIDAD QUE SE FUE EXTENDIENDO DESDE EL NNO HASTA EL NE DE LA AGUJA INCENDIÁNDOSE CASI REPENTINAMENTE EL CIELO CON UNA FAJAS QUE CAÍAN COMO DE LOS 45º HASTA CERCA DEL HORIZONTE Y AUNQUE AL PRINCIPIO ERAN BLANCAS O CLARAS SEN ENCENDIABAN INMEDIATAMENTE CON MÁS VIVEZA QUE EL RESTO; CONOCIMOS SER AURORA BOREAL Y A LAS 10 SÓLO QUEDABA ALGUNA POCA DE CLARIDAD QUE CONTINUÓ DESDE LAS 11 AVIVÁNDOSE Y A LAS 11 1/2 VOLVIÓ A INCENDIARSE EL CIELO COMO ANTES, PERO CON LA DIFERENCIA DE QUE SE EXTENDIÓ DESDE EL NNO HASTA EL NO. QUEDÓ TAMBIÉN CLARA AQUELLA PARTE DESDE LA UNA EN QUE SE DISIPÓ LA INCENDIADA HASTA LAS DOS Y A DICHA HORA POR TERCERA VEZ VOLVIÓ A INCENDIARSE AL NO, AUNQUE NO CON TANTA VIVEZA: A LAS 3 1/2 ESTANDO BASTANTE CLARA EL ALBA SE DISIPÓ ENTERAMENTE. AMANECIÓ CLARO, VTO. FRESQUITO CON MAREJADA DEL ONO.
DOI: 10.1594/pangaea.897651
title: Microwave-induced self-organization in mineral systems. V. FeCl3 colloid (800 W; 2.45 GHz; 30 sec.)

description: Microwave-induced self-organization in FeCl3 colloids under high irradiation power (800 W) is strongly dependent on the layer thickness of the precursor (saturated ferric chloride solution) and results in less diversity of membraneous structure morphologies because of the too fast water evaporation preventing hydrolytic polycondensation and favoring simple crystallization of the mineral phases.
DOI: 10.1594/pangaea.783187
title: Meteorological synoptical observations from Neumayer Station (2011-05)
DOI: 10.1594/pangaea.694357
title: Nutrient concentrations in water samples from the Ionian Sea at Station SEPT-2000-IKO8
DOI: 10.1594/pangaea.932500
title: Processed hourly current meter data from Mooring EB1/2 2017-2018

description: This data set contains current meter measurement data from deep-sea mooring EB1/2 deployed in the North Atlantic Eastern Boundary (EB) region at Goban Spur from June 2017 to April 2018. The mooring is part of an array that represents the eastern extension of the basin-wide "North Atlantic Changes" (NOAC) ocean observatory deployed along 47°N. Data were interpolated on a regular hourly time grid.
DOI: 10.1594/pangaea.901227
title: Mean and 1s of quantities derived from the five GISS-E2.1 ensemble members used to calculate D36,trop
DOI: 10.1594/pangaea.880251
title: Model outputs, related figures and input data for inversions of HFC-125, HFC-134a and SF6 emissions over Europe
DOI: 10.1594/pangaea.695035
title: Concentrations of particulate organic carbon in water of the Aegean Sea at Station MAY-1997-IR06

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore filters. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).
DOI: 10.1594/pangaea.830919
title: Abundance of pteropods in the Aegean Sea during LIA07, LIA08, LIA09 and LIA10
DOI: 10.1594/pangaea.751126
title: Meteorological observations during PEGASUS cruise from Suriname to Curaçao started at 1834-03-30
DOI: 10.1594/pangaea.901572
title: Beach profile data for the Elwha River Delta, 2014-08-14

description: Data were collected using GNSS survey methods, with a differential GPS operating in Real Time Kinematic (RTK) mode. Data from prior to 2013 were typically collected with a Magellan ProMark 3 traditional RKT-DGPS system (i.e. local base station and rover), with the base station sited on survey control markers installed in 1996, with survey control coordinates referenced to NAD83(CORS91). Starting in 2013 survey data were typically collected with an AshTech ProMark 200 RTK-DGPS system connected to the Washington State Reference Network. Survey data collected between January and November 2013 are referenced to NAD83(CORS96), and after November 2013 to NAD83(2011). Vertical data for surveys in 2012 and 2013 are referenced to NAVD88, presumably using Geoid96 (the survey control documentation does not specific a geoid). For all subsequent surveys the vertical data are referenced to NAVD88(Geoid09). No conversion were applied to these data to account for variations in horizontal or vertical coordinate system adjustments through time, but an error analysis suggests a standard deviation for the elevation data of between 0.03 and 0.05 m across the entire sampling period (2011-2018). All survey data were collected with the GNSS system mounted on a 2.05 m rover pole, held level as a transect line was traced in a cross-shore orientation on the beach. The associated text files include the horizontal (HRMS) and vertical (VRMS) root-mean-square errors estimated by the GNSS system, as well as the RTK-DGPS status reported by the GNSS system at the time each point was collected. Times are referenced to local Pacific time (either PST or PDT).
description: Portions of these data have been published previously, including in Gelfenbaum et al. 2015.
DOI: 10.1594/pangaea.845749
title: Water quality observations from a fixed monitoring station at the Guadiana Estuary, 2012-2013

description: Hourly probe (YSI 6600) records of temperature, chlorophyll, salinity, dissolved oxygen, turbidity, and pH at a water depth of 1 m.
DOI: 10.1594/pangaea.893605
title: 03. Annual glacier elevation change rate raster dataset, South American Andes, Outer Tropics (Bolivia) 2000 and 2011-2015

description: The dataset is a mosaic of several dh/dt fields for the region '03 Outer Tropics (Bolivia)' according the nomenclature of regions taken from Nature Climate Change Paper 'Glacier elevation and mass changes over entire South America between 2000 and 2011–15'. The product is derived from differencing of TanDEM-X and SRTM Digital Elevation Models. All TanDEM-X products were processed by the authors (cf. referenced paper for methods description).
DOI: 10.1594/pangaea.864936
title: Ultra-violet measurements from station Boulder, SURFRAD (2012-08)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-09.
DOI: 10.1594/pangaea.932563
title: Daily volume transport time series from North Atlantic Eastern Boundary near Goban Spur based on current meter measurements and extended with satellite altimetry

description: This data set contains volume transport time series derived from deep-sea moorings deployed in the North Atlantic Eastern Boundary (EB) region at Goban Spur. The moorings are part of an array that represents the eastern extension of the basin-wide "North Atlantic Changes" (NOAC) ocean observatory deployed along 47°N. The first time series (observed) is obtained from 10-day low-pass filtered current meter measurments at mooring EB1 and EB3 from 2017 to 2019. The second time series (regressed) is extendend to the period 1993 to 2019 applying a multi-linear regression model on geostrophic surface velocities derived from satellite altimetry.
description: In Sverdrup. Positive values indicate poleward along-slope transport.
DOI: 10.1594/pangaea.864938
title: Basic measurements of radiation at station Boulder, SURFRAD (2012-09)
DOI: 10.1594/pangaea.879932
title: Other measurements at 10 m from station Bondville (2016-09)
DOI: 10.1594/pangaea.664988
title: Oceanography at CTD/bottle station IFREMER_1828