cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.887561
title: Radiosonde measurements from Neumayer Station (2017-11)

description: The meteorological observatory Neumayer typically launches one radiosonde per day around 12UTC. At least weekly the sonde has an ozone sensor attached. Sondes are released from the roof of the station building. The measurement interval of the raw data is typically 1s. Data is quality controlled: Erroneous data is removed (technical issues). Partial pressure ozone is manually validated for plausibility.
DOI: 10.1594/pangaea.659133
title: Coverage of organisms associated to Macrocystis integrifolia off Chile in 2001, Regions I to IV
DOI: 10.1594/pangaea.863353
title: Basic measurements of radiation at station Lerwick (2011-11)
DOI: 10.1594/pangaea.907150
title: Dissolved methane and nitrous oxide concentrations measured on discrete bottle samples in Cambridge Bay, Nunavut, Canada from 2018
DOI: 10.1594/pangaea.918839
title: Measurements of sensor 2 during fixed-wing unmanned aerial vehicle flight 1.04 on 2020-02-28
DOI: 10.1594/pangaea.917354
title: 1-Hz PPP displacements at GEONET station 3007 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.863412
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE443
DOI: 10.1594/pangaea.809842
title: Sulphate reduction and Methane oxidation rates of Amsterdam mud volcano sediments measured at station MSM13/4_1007-1
DOI: 10.1594/pangaea.755867
title: Basic measurements of radiation at station Cener (2009-08)
DOI: 10.1594/pangaea.863354
title: Basic measurements of radiation at station Lerwick (2011-12)
DOI: 10.1594/pangaea.902582
title: Monthly sea temperature in 20 m water depth derived from in situ observations offshore L'Estartit (NW Mediterranean) since 1974

description: In-situ sea temperatures have been obtained using two Richter and Wiese protected reversing thermometers mounted on a Nansen bottle. Temperature readings, after correction according to the thermometer's calibration certificates are averaged if the temperature difference among thermometers is lower than 0.2°C and repeated otherwise, so that the accuracy can be set to be lower than 0.2°C. Thermometers are periodically controlled at facilities of the Marine Research Institute (ICM) in Barcelona against a high precision Pt100. which, in turn is annually controlled using Ga and pure H2O melting points.
DOI: 10.1594/pangaea.918841
title: Measurements of sensor 1 during fixed-wing unmanned aerial vehicle flight 1.05 on 2020-02-28
DOI: 10.1594/pangaea.739012
title: Pollen profile BELATE05, Puerto de Belate, Spain

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.805713
title: (Table 5) Trace element anbundances of partial melt of ODP Hole 140-504B samples
DOI: 10.1594/pangaea.547891
title: Nutrients measured on water bottle samples at station Bm_1997-09-13_3, Bajo Molle, Chile
DOI: 10.1594/pangaea.902589
title: Monthly sea temperature in 80 m water depth derived from in situ observations offshore L'Estartit (NW Mediterranean) since 1974

description: In-situ sea temperatures have been obtained using two Richter and Wiese protected reversing thermometers mounted on a Nansen bottle. Temperature readings, after correction according to the thermometer's calibration certificates are averaged if the temperature difference among thermometers is lower than 0.2°C and repeated otherwise, so that the accuracy can be set to be lower than 0.2°C. Thermometers are periodically controlled at facilities of the Marine Research Institute (ICM) in Barcelona against a high precision Pt100. which, in turn is annually controlled using Ga and pure H2O melting points.
DOI: 10.1594/pangaea.865165
title: Ultra-violet measurements from station Fort Peck (2012-11)

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 2017-02-03.
DOI: 10.1594/pangaea.752372
title: Meteorological observations during SUMATRA cruise from Rio de Janeiro to St. Eustatius started at 1830-03-04
DOI: 10.1594/pangaea.901530
title: Beach profile data for the Elwha River Delta, 2012-10-15

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.881839
title: Chemical composition of manganese nodules from the Pacific Ocean using X-ray Emission Analysis (XES)

description: Chemical compositions have been corrected to 110° C drying (see, https://doi.pangaea.de/10.1594/PANGAEA.854202).From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis..) not present in the NOAA-MMS database.
DOI: 10.1594/pangaea.866352
title: Other measurements at 10 m from station Sioux Falls (2012-11)
DOI: 10.1594/pangaea.779358
title: (Table T3) Density and porosity characteristics of basalts from several ODP Leg 192 sites
DOI: 10.1594/pangaea.945078
title: Meteorological synoptical observations from station Tamanrasset (2022-05)
DOI: 10.1594/pangaea.497870
title: Physical oceanography from BT during cruise U58X001117B_1928
DOI: 10.1594/pangaea.696201
title: Organic carbon and nitrogen concentrations in waters of the Arabian Sea at Station M32/3_238
DOI: 10.1594/pangaea.548323
title: Physical oceanography at CTD station Bm_1997-09-09_1, Bajo Molle, Chile
DOI: 10.1594/pangaea.547865
title: Nutrients measured on water bottle samples at station Bm_1997-09-07_3, Bajo Molle, Chile
DOI: 10.1594/pangaea.708057
title: (Table 2) Sulphur contents and partition of iron in ODP Hole 112-681 sediments
DOI: 10.1594/pangaea.762462
title: (Table 4-I-C) Chemical analyses and structural formulas of feldspar of ODP Site 124-769
DOI: 10.1594/pangaea.945101
title: Radiosonde measurements from station Abashiri (2022-03)
DOI: 10.1594/pangaea.904897
title: (Dataset 1) Pliocene alkenone unsaturation index (Uk37) and SST anomalies of ODP site 165-999

description: *** Change history *** in September 2021 it was found, that the ages in all "Dataset 1" datasets were declared here as being in "ka BP" but they were actually in "Ma". To correct this error all ages were recalculated (*1000) to fit the unit "ka BP".
DOI: 10.1594/pangaea.778033
title: (Table T8) Tie points used to create the revised composite depth section for ODP Site 198-1211
DOI: 10.1594/pangaea.887418
title: Soil organic carbon storage and organic layer depth for the Stordalen catchment, Abisko, Sweden

description: Soil organic carbon (SOC) stored in northern peatlands and permafrost-affected soils are key components in the global carbon cycle. This dataset provides SOC storage and organic layer depth for 47 soil pedons located in the Stordalen catchement. Stordalen is a sub-arctic mountainous peatland environment in the discontinuous permafrost zone in Abisko, northern Sweden. The data is provided as total SOC storage (SOCTot) including wetland pedons processed to a reference depth of 1.5 m and non-wetland pedons processed to a reference depth of 1 m. If the pedon did not reach that depth it was extrapolated based on a trend in the pedon or similar pedons or set to zero if the lithic contact was reached. Other extracted depth intervals are the SOC stored in the organic surface layer (SOCOL),in the permafrost layer (SOCPF), the SOC stored for the top 30 cm (SOC0to30) and the SOC for the top 100 cm (SOC0to100). SOC values are in kg C m-2 . The depth of the organic layer (OLdepth) in cm is also provided.The location of each pedon is provided as XY coordinates projected in WGS 84 / UTM zone 33N (EPSG: 32633). Altitude is provided from a GPS reading.More information on how the soil data was collected and processed can be found in the linked article (Open Access).
DOI: 10.1594/pangaea.913900
title: Species-adjusted stable oxygen isotope record of ODP Site 130-806
DOI: 10.1594/pangaea.809215
title: Sulphate reduction rates of Amon mud volcano sediments measured at station MSM13/3_968-1_PUC8
DOI: 10.1594/pangaea.929690
title: Organic geochemistry of sediment core EN18218 from Arctic glacial lake Rauchuagytgyn, Chukotka, Russia
DOI: 10.1594/pangaea.669945
title: Basic measurements of radiation at station Kwajalein (1999-12)
DOI: 10.1594/pangaea.497649
title: Physical oceanography from BT during cruise U58JH01016B_1955
DOI: 10.1594/pangaea.939705
title: Rare earth elements, suspenden particulate matter,dissolved organic carbon, Neodymium/Ytterbium ratio and Neodymium isotopes data along the salinity gradient in the Changjiang estuary

description: Surface seawater samples from the Changjiang Estuary were collected during the high discharge season in August 2015. The sampling locations focused on the Changjiang River Estuary area from ~32ºN to ~29ºN . Soon after their recovery, all of the samples were filtered through a 0.40-μm Whatman membrane onboard the vessel. The samples were then acidified to a pH of ~2 with high-purity HCl . From each sample, 15-20 L was placed in acid-cleaned bottles for Nd isotope composition analysis, and 500 mL was collected to determine the REE concentration. The filter membranes were cryopreserved for the determination of SPM. REE concentrations and Nd isotope compositions determined in these filtered waters were treated as dissolved-phase measurements (Nd&lt;0.45μm). An unfiltered water sample was directly acidified to a pH &lt;2 with hydrochloric acid after sample collection and then filtered through a 0.40-μm Whatman membrane in a cleanroom to determine the acid-soluble REEs (Nd&gt;0.45μm)The data on dissolved REE concentrations were measured by ICP-MS (Thermo iCAP-Q) with a precision of better than 4% and a reagent blank of less than 2%, based on the results of replicated measurements. Nd isotope measurements were made on Nu plasma I and II instruments at the Key Laboratory of Environmental Geochemistry. Corrections were made for instrumental mass bias using a value of ¹⁴³Nd/¹⁴⁴Nd = 0.7219. The ¹⁴³Nd/¹⁴⁴Nd ratios of the samples were normalized using the accepted value from the literature of 0.512115±0.000006 (Tanaka et al., 2000) for JNdi-1 (Geological Survey of Japan). Blank values were ≤700 pg (representing an average of 2% of the sampled signal). The Nd isotopic compositions can be expressed by ε~Nd~ = ¹⁴³Nd/¹⁴⁴Nd[measured] / ¹⁴³Nd/¹⁴⁴Nd[CHUR]-1)×10000, where CHUR stands for the Chondritic Uniform Reservoir, with a value is 0.512638 (Wasserburg et al., 1981), and ¹⁴³Nd/¹⁴⁴Nd[measured] represents the measured value.
DOI: 10.1594/pangaea.693614
title: Mesozooplankton average length during Mikhail Lomonosov cruise ML27, Part III

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 0.125 mm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-300, 300-500 m) and closed at the upper depth level. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved in 3-4% buffered formaldehyde and processed on return to the laboratory. All of copepods were identified to genus level, other taxanomic groups - to type, class, order and family levels.
DOI: 10.1594/pangaea.943599
title: D: GISP2 temperature anomalies from δ15N fitting using Schwander et al. (1997) firn model and Goujon et al. (2003) firn model reconstructed using stabilized temperature from 70 to 1000 yr b2k

description: GISP2 temperature anomalies from d15N fitting using Schwander et al. (1997) firn model and Goujon et al. (2003) firn model reconstructed using stabilized temperature from 70 to 1000 a b2k (Figure 4 and Supplement p. 6 in Döring and Leuenberger 2022, QSR). Ages from 70 to 1000 a b2k not recommend for climatic interpretation. Uncertainty is 2sigma = 0.80...0.88 K for the Schwander et al. (1997) firn model reconstruction and 2sigma = 0.86...0.94 K for the Goujon et al. (2003) firn model reconstruction. The uncertainty is based on mean isotope data resolution of 17.8 a.
DOI: 10.1594/pangaea.939706
title: Dissolved Neodymium data in the rainwater in the coastal East China Sea

description: Samples were filtered through a 0.40-μm Whatman membrane. The samples were then acidified to a pH of ~2 with high-purity HCl . From each sample, 15-20 L was placed in acid-cleaned bottles for Nd isotope composition analysis, and 500 mL was collected to determine the REE concentration. The filter membranes were cryopreserved for the determination of SPM. REE concentrations and Nd isotope compositions determined in these filtered waters were treated as dissolved-phase measurements (Nd&lt;0.45μm). An unfiltered water sample was directly acidified to a pH &lt;2 with hydrochloric acid after sample collection and then filtered through a 0.40-μm Whatman membrane in a cleanroom to determine the acid-soluble REEs (Nd&gt;0.45μm).
DOI: 10.1594/pangaea.943600
title: E: Modelled Isotopes and firn parameters using the Schwander et al. (1997) firn model with temperature (dataset D, column 2) and 200 km ice sheet margin retreat accumulation rate scenario (dataset Q, column 4) as inputs
DOI: 10.1594/pangaea.705564
title: Documentation of sediment core GIK10867-1
DOI: 10.1594/pangaea.509768
title: Physical oceanography at station Rigel-7 from date 2005-10-03, Chipana, Chile
DOI: 10.1594/pangaea.811244
title: (Appendix) Planktonic foraminifera counts in different size fractions of DSDP Hole 48-401
DOI: 10.1594/pangaea.845348
title: Radiosonde measurements from station Kwajalein (2011-05)
DOI: 10.1594/pangaea.943613
title: O: Modelled Isotopes and firn parameters using the Schwander et al. (1997) firn model with temperature (dataset N, column 2) and 200 km ice sheet margin retreat accumulation rate scenario (dataset Q, column 4) as inputs
DOI: 10.1594/pangaea.678452
title: Bitumen in sedimentary rocks from Hole VNIIO-1983-21 drilled in the Barents Sea

description: Types of rocks and their ages are given in the special data set; see: doi:10.1594/PANGAEA.678454
DOI: 10.1594/pangaea.943607
title: J: GISP2 temperature anomalies from δ15Nexcess fitting using Schwander et al. (1997) firn model and Goujon et al. (2003) firn model

description: GISP2 temperature anomalies from δ15Nexcess fitting using Schwander et al. (1997) firn model and Goujon et al. (2003) firn model (Figure 4 and Supplement p. 6 in Döring and Leuenberger 2022, QSR). Not recommended for climatic interpretation.
DOI: 10.1594/pangaea.939708
title: Dissolved Neodymium data in the well water of JiangYin

description: Samples were filtered through a 0.40-μm Whatman membrane. The samples were then acidified to a pH of ~2 with high-purity HCl . From each sample, 15-20 L was placed in acid-cleaned bottles for Nd isotope composition analysis, and 500 mL was collected to determine the REE concentration. The filter membranes were cryopreserved for the determination of SPM. REE concentrations and Nd isotope compositions determined in these filtered waters were treated as dissolved-phase measurements (Nd&lt;0.45μm). An unfiltered water sample was directly acidified to a pH &lt;2 with hydrochloric acid after sample collection and then filtered through a 0.40-μm Whatman membrane in a cleanroom to determine the acid-soluble REEs (Nd&gt;0.45μm).
DOI: 10.1594/pangaea.943612
title: N: GISP2 temperature anomalies from hybrid approach using Schwander et al. (1997) firn model and Goujon et al. (2003) firn model
DOI: 10.1594/pangaea.945059
title: Environmental data of coral stations A-F in Comau Fjord, Chile
DOI: 10.1594/pangaea.705573
title: Documentation of sediment core GIK11881-1
DOI: 10.1594/pangaea.945061
title: Porewater concentrations of ammonium, nitrite, nitrate, sulfate, hydrogen sulfide, dissolved iron and dissolved manganese at 5 sites along a water depth transect in the Gulf of Mexico (Louisiana continental shelf)

description: Porewater samples for NH4+, NO3- , and NO2- were analyzed on board with Quattro gas-segmented continuous flow analysers using the indophenolblue method (NH+4), and the sulphanyl-amide method (NOx). Porewater sulfide was determined spectrophotometrically using phenylenediamine and ferric chloride. Porewater samples for SO4 2- were analyzed by ion-chromatography. Dissolved Fe and Mn were analyzed by Inductively Coupled Plasma Optical Emission Spectroscopy (ICP-OES; Spectro Arcos). Porewater concentrations were around or below the detection limit (0.5 and 0.8 μmol L−1, respectively) and are therefore not presented.
DOI: 10.1594/pangaea.945066
title: Biomass of Desmophyllum dianthus at stations A-F in Comau Fjord, Chile
DOI: 10.1594/pangaea.943594
title: A: GISP2 temperature anomalies from δ15N fitting using Schwander et al. (1997) firn model and Goujon et al. (2003) firn model

description: Uncertainty is 2sigma = 0.80...0.88 K for the Schwander et al. (1997) firn model reconstruction and 2sigma = 0.86...0.94 K for the Goujon et al. (2003) firn model reconstruction. The uncertainty is based on mean isotope data resolution of 17.8 a.
DOI: 10.1594/pangaea.670814
title: Basic measurements of radiation at station Lerwick (2003-08)
DOI: 10.1594/pangaea.943614
title: P: Modelled Isotopes and firn parameters using the Goujon et al. (2003) firn model with temperature (dataset N, column 4) and 200 km ice sheet margin retreat accumulation rate scenario (dataset Q, column 4) as inputs
DOI: 10.1594/pangaea.740469
title: Age determination of sediment core KOZLI, Kozli, Czech Republic

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.945064
title: Solid phase concentrations in the sediment at 5 sites along a water depth transect in the Gulf of Mexico (Louisiana continental shelf)

description: All sediments were freeze-dried and the porosity was determined from the weight loss upon freeze drying. To determine the total elemental concentrations of aluminum (Al), Co, Fe, Mn, Ni, and S, ca. 125 mg of sediment was digested in 2.5 ml mixed acid (HNO3:HClO4; 2:3) and 2.5 ml 40% HF at 90◦C. After fuming off the acids, the residue was redissolved in 4.5% HNO3. The solutions were subsequently analyzed on an ICP-OES. The analytical uncertainty based on duplicates and triplicates was &lt;1% for Al, &lt;4.2% for Co, &lt;1.6% for Fe, &lt;2.5% for Mn, &lt;2.3% for Ni, and &lt;1.7% for S. A subsample of circa 300 mg was decalcified with 2 wash steps of 1M HCl and subsequently dried, powdered and analyzed for carbon (C) using an elemental analyser (Fisons Instrumentsmodel NA 1500 NCS). Organic C content was determined after correction for the weight loss following decalcification. The analytical uncertainty based on duplicates and triplicates was &lt;0.07 wt%.
DOI: 10.1594/pangaea.945065
title: Concentration of total dissolvable and total iron, manganese, cobalt and nickel in the water column at 5 sites along a water depth transect in the Gulf of Mexico (Louisiana continental shelf)

description: The concentration of Fe in water column samples was determined by flow injection chemiluminescence with preconcentration detection. Total dissolvable Fe concentrations were determined 3 months after sample collection. All samples per station were analyzed in triplicate in the same run. The blank of acidified ultrapure water (pH = 1.8) was 32 ± 39 pmol L−1 (n = 194). The average limit of detection (LOD), calculated as the standard deviation of the analysis of oligotrophic seawater with known trace metal concentrations, multiplied by 3, was 86 ± 120 pmol L−1 (n = 19). The concentrations of Co, Mn, and Ni were determined by Inductively Coupled Plasma Mass Spectrometry (ICP-MS; Nexion ICP-MS (Perkin Elmer)) after pre-concentration with an SC-DX SeaFAST S2 (Elemental Scientific). Total dissolvable Co, Mn, and Ni were determined 7 months after sample collection. The LOD values for Co, Mn, and Ni were 0.027 ± 0.004, 0.11 ± 0.024, and 0.99 ± 0.12 nmol L−1 (n=5), respectively, and the values of the oligotrophic seawater were 0.77 ± 0.9, 0.9 ± 0.5, and 4.41 ± 0.52 nmol L−1 (n=40), respectively.
DOI: 10.1594/pangaea.777044
title: Nematode 13C isotope values from in situ feeding experiments in the Nazare Canyon conducted with sediments from ROV push-core JC10-112-PUC07

description: Nematode 13C isotope values (ca. 100 ind., per mil relative to PVDB standard)
DOI: 10.1594/pangaea.943604
title: G: GISP2 temperature anomalies from δ40Ar fitting using Schwander et al. (1997) firn model and Goujon et al. (2003) firn model reconstructed using stabilized temperature from 70 to 1000 yr b2k

description: GISP2 temperature anomalies from δ40Ar fitting using Schwander et al. (1997) firn model and Goujon et al. (2003) firn model reconstructed using stabilized temperature from 70 to 1000 a b2k (Figure 4 and Supplement p. 6 in Döring and Leuenberger 2022, QSR). Ages from 70 to 1000 a b2k not recommend for climatic interpretation. Uncertainty is 2sigma = 1.14...1.95 K for the Schwander et al. (1997) firn model reconstruction and 2sigma = 1.30...2.05 K for the Goujon et al. (2003) firn model reconstruction. The uncertainty is based on mean isotope data resolution of 17.8 a.
DOI: 10.1594/pangaea.829227
title: Natural gamma radiation from IODP Hole 340-U1394B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.904113
title: Oxygen isotope ratio and reconstructed temperature record from the Agassiz ice cap, Greenland
DOI: 10.1594/pangaea.943605
title: H: Modelled Isotopes and firn parameters using the Schwander et al. (1997) firn model with temperature (dataset G, column 2) and 200 km ice sheet margin retreat accumulation rate scenario (dataset Q, column 4) as inputs
DOI: 10.1594/pangaea.775663
title: Continuous meteorological observations at station Ny-Ålesund (2007-06)
DOI: 10.1594/pangaea.757189
title: (Table 7) Carbohydrates in sediments of ODP Site 117-723

description: Ages are calculated on biostratigraphical and magnetostratigraphical data from the shipboard party (1989, doi:10.2973/odp.proc.ir.117.110.1989).