cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.891745
title: Diatom density in sediment core from Duluth-Superior Harbor at Minnesota Point, Minnesota, USA

description: Diatom density per dry weight of sediment.
DOI: 10.1594/pangaea.900076
title: Benthic foraminifera of sediment cores HM107-03 and HM107-2732

description: Associated Projects and funding: HOLSMEER and PACLIVA projects funded by the European Commission's 5th Framework Programme (Contracts no. CT-2000-00060 and EVK2-2002-00143); PANIS project (Palaeoenvironments on the North Icelandic shelf); BIOICE project (Benthic Invertebrates of Icelandic Waters). Financial support by the Danish Natural Science Research Council, the Icelandic Research Council and the National Natural Science Foundation of China (Grant no. 40276013)
DOI: 10.1594/pangaea.841892
title: Stable oxygen isotope data of Globorotalia inflata for sediment core GeoB6308-3

description: Composite record GeoB6308 was produced merging the gravity core GeoB6308-3 and the companion multicore GeoB6308-1 [Bleil et al., 2001]. The age model for GeoB6308 is based on previously published [GeoB6308-3; Lantzsch et al., 2014] and new (GeoB6308-1) 14C AMS analyses performed on monospecific samples of the planktonic foraminifer G. inflata.
DOI: 10.1594/pangaea.891747
title: Diatom biovolume in sediment core from Duluth-Superior Harbor at Minnesota Point, Minnesota, USA

description: Diatom biovolume was measured per dry weight of sediment. Additional data on relative biovolume and biovolume accumulation rates can be found under "Further details".
DOI: 10.1594/pangaea.495266
title: Water temperature MBT profiles from cruise U3190215M_1953
DOI: 10.1594/pangaea.842182
title: Stationary profiling of flow and suspended sediment concentration in a bedform field, part 2
DOI: 10.1594/pangaea.495226
title: Water temperature XBT profiles from cruise U18_1975
DOI: 10.1594/pangaea.891752
title: Diatom density in sediment core from north of Clough Island, St. Louis River, Minnesota, USA

description: Diatom density was measured per dry weight of sediment.
DOI: 10.1594/pangaea.823318
title: (Table 4) Geochemistry of three olivine phenocrysts from flow unit 19B at DSDP Hole 55-433C
DOI: 10.1594/pangaea.919413
title: Ultra-violet measurements from station Selegua (2020-04)
DOI: 10.1594/pangaea.664353
title: Oceanography at CTD/bottle station IFREMER_1194
DOI: 10.1594/pangaea.842642
title: Radionuclides activity concentrations of sediment core A2

description: Uncertainties are expressed as 1 standard deviation including counting statistics and detector calibration uncertainty. Values below decision threshold are expressed for 5% type I error probability.
DOI: 10.1594/pangaea.919966
title: Radiosonde measurements from station Budapest (2019-07)
DOI: 10.1594/pangaea.891754
title: Diatom biovolume in sediment core from north of Clough Island, St. Louis River, Minnesota, USA

description: Diatoms biovolume was measured per dry weight of sediment. Additional data on relative biovolume and biovolume accumulation rates can be found under "Further details".
DOI: 10.1594/pangaea.891594
title: Diatom counts in sediment core Billings Park Bay, St. Louis River, Minnesota, USA

description: Additional data on relative abundance and cells accumulation rates of diatoms can be found under "Further details".
DOI: 10.1594/pangaea.691211
title: Nutrient concentrations in water samples collected at Station MARCH-94-GN3619940280101000 in the Aegean Sea
DOI: 10.1594/pangaea.755221
title: (Table 2) Distribution of Bolboforma in ODP Hole 114-699A

description: Abundances: R = rare (&lt;3 %), F = few (3-15 %), C = common (15-30 %) A = abundant (&gt;30 %), - absent, R* = transition B. indistincta to B. lamari.
DOI: 10.1594/pangaea.691259
title: Nutrient concentrations in water samples collected at Station SEPT-94-GN3619940280300920 in the Aegean Sea
DOI: 10.1594/pangaea.763128
title: (Table 3) Major element glass ananlyses of samples from ODP Site 125-786
DOI: 10.1594/pangaea.843627
title: Links to master tracks in different resolutions of HEINCKE cruise HE248, Bremerhaven - Bremerhaven, 2006-05-02 - 2006-05-04
DOI: 10.1594/pangaea.897332
title: Planktic foraminiferal test size and size normalised weight from DSDP Hole 94-610A during the Pliocene
DOI: 10.1594/pangaea.602412
title: Monthly landings from 1991 of Argopecten purpuratus in Independencia Bay, Peru
DOI: 10.1594/pangaea.498330
title: Physical oceanography from BT during cruise U909008467B_1985
DOI: 10.1594/pangaea.671844
title: Basic measurements of radiation at station Regina (2000-05)
DOI: 10.1594/pangaea.820382
title: Lucky Strike record of hydrothermal outflow temperature at vent CY_INC_101014_110705_LN27010

description: The temperature record include ambient temperatures (onboard the ship), water column temperatures (going up and down) and the hydrothermal temperatures.
DOI: 10.1594/pangaea.842645
title: Radionuclides activity concentrations of sediment core HHN2C

description: Uncertainties are expressed as 1 standard deviation including counting statistics and detector calibration uncertainty. Values below decision threshold are expressed for 5% type I error probability.
DOI: 10.1594/pangaea.915115
title: Radiosonde raw data from tandem soundings at Neumayer Station (2019-04), links to files

description: At Neumayer station the transition of sonde type from Vaisala RS92-SGP to RS41-SGP is controlled by tandem soundings starting in July 2018. Each file in this dataset was acquired together with the corresponding data file in doi:10.1594/PANGAEA.915084.
DOI: 10.1594/pangaea.705509
title: (Table 2) Total number of benthic foraminifera below the K/T boundary in DSDP Hole 72-516F
DOI: 10.1594/pangaea.671833
title: Basic measurements of radiation at station Regina (1999-05)
DOI: 10.1594/pangaea.842921
title: Stable nitrogen isotope ratios of mooring Midway samples
DOI: 10.1594/pangaea.809721
title: Dive depth profile of Weddell seal DRE1990_wed_a_m_09 from Drescher Inlet

description: Data processing by HighSEA X students.
DOI: 10.1594/pangaea.750794
title: Meteorological observations during Middelburgs Welvaren cruise from Suriname to Middelburg started at 1756-03-03
DOI: 10.1594/pangaea.855019
title: Trace metal composition of the aerosol at Neumayer Station, Antarctica during the year 2009

description: Aerosol was continuously sampled by sucking ambient air with a flow rate of 120 m**3/h through Whatman 541 filters (diameter 240 mm) using a ventilated electropolished stainless steel inlet stack (total height about 8 m above the snow surface) with a 50% aerodynamic cut-off diameter around 7-10 µm. Trace element analysis was performed by means of inductively coupled plasma - quadrupol mass spectrometry (ICP-QMS, ELAN 6000, Sciex/Perkin Elmer) equipped with a cross-flow nebulizer as sample introduction system. For trace element analyses we chose a total digestion of the samples with a pressurized digestion system (DAS 100, Picotrace) at 200°C in a mixture containing HNO3 (suprapure, 65%, Merck, sub-boiling bi-distilled), HF (suprapure, 40%, Merck, sub-boiling bi-distilled) and H2O2 (suprapure, 30%, Merck). With this device a series of 24 samples could be digested in parallel. Each series included one filter blank and a certified reference sample (NIST 1648 urban particulate matter). For calibration we used commercially available standard solutions (104 ppb multi-element verification standard 1 and 2, Perkin Elmer) which were generally applied in 1 ppb, 10 ppb, and 100 ppb concentrations (1 ppb corresponds to 1 ng of each element in 1 g solute). Each sample was spiked by 10 ppb Rh as internal standard to normalize the signal intensities and compensate instrumental sensitivity variations. We conservatively estimated the method detection limits (MDL) as three times the standard deviation (std) of the overall blank values. Values below the MDL are given as "&lt; respecting MDL value" (e.g.: &lt;0.02) in the table. Concentrations not determined are marked with empty cells. The combined uncertainty of the analyses is approximately between ±8% and ±12% for element concentrations above three times the corresponding MDL. It increased from around ±(15-20)% approaching 3xMDL level to roughly (+50/-100)% close to the MDL. The final atmospheric concentrations (in ng/m**3 = 10**(-9) g/m**3, or pg/m**3 = 10**(-12) g/m**3) were calculated from the blank corrected element amounts and the corrected sampled air volume to standard conditions (273.16 K and 1013 hPa).
DOI: 10.1594/pangaea.915118
title: Radiosonde raw data from tandem soundings at Neumayer Station (2019-07), links to files

description: At Neumayer station the transition of sonde type from Vaisala RS92-SGP to RS41-SGP is controlled by tandem soundings starting in July 2018. Each file in this dataset was acquired together with the corresponding data file in doi:10.1594/PANGAEA.915087.
DOI: 10.1594/pangaea.752575
title: Meteorological observations during UNKNOWN-03 cruise from St. Eustatius to Texel started at 1779-03-26
DOI: 10.1594/pangaea.905376
title: Improving the Climate Hazards Group Infrared Precipitation (CHIRP) using WHU-SGCC method over the Jinsha River Basin from 1990 to 2014

description: A daily precipitation estimation derived from WHU-SGCC method (Wuhan University Satellite and Gauge precipitation Collaborated Correction), blending daily precipitation gauge data and the Climate Hazards Group Infrared Precipitation (CHIRP, daily, 0.05°) satellite-derived precipitation estimates over the Jinsha River Basin during the different seasons from 1990 to 2014.
description: Supplement to: Shen, Gaoyun; Chen, Nengcheng; Wang, Wei; Chen, Zeqiang (2019): WHU-SGCC: a novel approach for blending daily satellite (CHIRP) and precipitation observations over the Jinsha River basin. Earth System Science Data, 11(4), 1711-1744
DOI: 10.1594/pangaea.664236
title: Oceanography at CTD/bottle station IFREMER_1077
DOI: 10.1594/pangaea.915121
title: Radiosonde raw data from tandem soundings at Neumayer Station (2019-10), links to files

description: At Neumayer station the transition of sonde type from Vaisala RS92-SGP to RS41-SGP is controlled by tandem soundings starting in July 2018. Each file in this dataset was acquired together with the corresponding data file in doi:10.1594/PANGAEA.915090.
DOI: 10.1594/pangaea.695206
title: Monthly landings destined for Drying, Chile, 1998
DOI: 10.1594/pangaea.902546
title: Global peat basal ages

description: This database contains the basal ages from peatlands worldwide. See details at Yu et al. 2010.
DOI: 10.1594/pangaea.899140
title: Digital Elevation Model of Mt Etna updated to 18 December 2015

description: We present a Digital Elevation Model (DEM) of Mount Etna obtained from tri-stereo Pléiades data acquired on 18 December 2015. The 3D processing of the tri-stereo Pléiades 1A imagery was performed using the free and open source MicMac photogrammetric library (http://micmac.ensg.eu) developed by the French IGN (Institut Géographique National), and took advantage of Ground Control Points (GCPs) acquired at Mt Etna. The best result obtained is a 4-meter resolution DEM spanning an area of about 16 × 15 km, which covers the summit craters and a portion of the eastern flank of the volcano, including most of the Valle del Bove area. The highest point of 3,367 m is on the south-west rim of the North-East Crater (NEC), while the South-East Crater (SEC) and the New South-East Crater (NSEC) reach an elevation of 3,336 and 3,325 m, respectively. This 2015 DEM was validated against the 1-meter 2005 DEM resulted from digital photogrammetric mapping (Gwinner at al., 2006). The standard deviation of the height difference between the two DEMs in the area not covered by volcanic deposits, emplaced between 2005 and 2015, is 2.95 m. This difference can be partly due to vegetation and/or urbanization. The DEM is provided as GeoTIFF raster (dem_2015_4m.tiff), using the WGS84 datum and the UTM projection, zone 33 North (EPSG 32633). Missing areas are due to snow cover, very low texture and/or terrain shadows. Pléiades data were available through the Space Volcano Observatory with Pléiades (SVOP) project coordinated by Pierre Briole (http://volcano.iterre.fr/svo_projects). We are grateful to Olivier Galland, Luc Girod and Christopher Nuth for their assistance with the use of the MicMac software.This work was developed within the framework of the Laboratory for Technological Advance in Volcano Geophysics (TecnoLab) of the INGV in Catania (Italy) and was partially supported from the "Advanced tools and methods for computational fluid-dynamics"(ATHOS) research programme.
description: Supplement to: Ganci, Gaetana; Cappello, Annalisa; Bilotta, Giuseppe; Hérault, Alexis; Zago, Vito; Del Negro, Ciro (2018): Mapping Volcanic Deposits of the 2011–2015 Etna Eruptive Events Using Satellite Remote Sensing. Frontiers in Earth Science, 6:83
DOI: 10.1594/pangaea.511767
title: Physical oceanography and CFC measured on water bottle samples at station M59/2_576
DOI: 10.1594/pangaea.916959
title: 1-Hz PPP displacements at GEONET station 0778 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.744116
title: Physical oceanography during Argos cruise Argos77/2 to the North Sea
DOI: 10.1594/pangaea.736357
title: Basic and other measurements of radiation at Neumayer Station (2009-02)
DOI: 10.1594/pangaea.736384
title: Basic and other measurements of radiation at Neumayer Station (2009-06)
DOI: 10.1594/pangaea.736386
title: Radiosonde measurements from Neumayer Station (2009-06)
DOI: 10.1594/pangaea.887220
title: Table 2 - Magnesium isotopic composition of pore fluids from ODP Site 189-1171
DOI: 10.1594/pangaea.736423
title: Expanded measurements from Neumayer Station (2009-06)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.902752
title: SO173/2 raw data of EM120 multibeam echosounder (bathymetry & beam time series)

description: Between 08.08.2003 and 02.09.2003, bathymetric data was acquired offshore Guatemala and Costa Rica during the R/V SONNE cruise SO173/2. The expedition comprised geophysical and biological research objectives. One aim was the acquisition of geophysical data for a better understanding of recent and long-term evolution of the Middle America Landbridge and mass flux into the subduction system. Moreover, the cruise was also dedicated to studying the sensory systems of mesopelagic fish, cephalopods, crustaceans and teleosts by using trawl gear and morphometric studies. Bathymetric mapping with the multibeam echosounder (MBES) SIMRAD EM120 was utilized to obtain a full coverage bathymetric map along the El Salvador and Guatemalan continental slope and to complete previous maps by filling gaps along the continental slope and oceanic plate of Nicaragua. Further geophysical instruments, such as the sub-bottom profiler PARASOUND, magnetometer, a dredge and seismic instrumentation, and biological equipment including trawling gear and lab instrumentation, complemented the research equipment. CI Citation: Paul Wintersteller (seafloor-imaging@marum.de) as responsible party for bathymetry raw data ingest and approval. Description of the data source: During the SO173/2 cruise, the hull-mounted multibeam echosounder (MBES) SIMRAD EM120 was utilized to perform bathymetric mapping. It allows to conduct surveys in water depths of up to 11,000 m. Two transducer arrays transmit successive frequency coded acoustic signals (11.25 to 12.6 kHz). Data acquisition is based on successive emission-reception cycles of the signal. While the emission beam has a dimension of 150° across and 2° along track, the reception is obtained from 191 overlapping beams with widths of 2° across and 20° along track. The beam footprint has a dimension of 2° by 2°. The beam spacing can be set to equidistant or equiangular. For further information on the system, consult: https://www.km.kongsberg.com/ Depth is estimated from each beam by using the two-way travel time and the beam angle known from each beam, and taking into account the ray bending due to refraction in the water column by sound speed variations. Combining phase and amplitude is used to provide measurement accuracy practically independent of the beam pointing angle. During the SO173 cruise, the EM120 was used continuously. At the beginning of the cruise, a sound velocity profile was measured to a depth of 2000 m. Responsible person during this cruise / PI: Wilhelm Weinrebe (wweinrebe@ifm-geomar.de) Chief Scientist: Wilhelm Weinrebe (wweinrebe@ifm-geomar.de) CR: http://oceanrep.geomar.de/13407/1/Geomar-Report-116.pdf CSR: https://www2.bsh.de/aktdat/dod/fahrtergebnis/2003/20040060.htm This dataset was published as part of: Geersen, Jacob (2019): Collated bathymetric data from convergent margins that experienced tsunami earthquakes. PANGAEA, https://doi.org/10.1594/PANGAEA.899049
DOI: 10.1594/pangaea.914253
title: Antarctic-Wide Annual Ice Flow Maps from Landsat 8 Imagery between 2013 and 2019

description: This dataset includes annual mosaics of Antarctic ice velocity derived from Landsat 8 images between December, 2013 and April, 2019, which was updated in 2020 in order to produce multi-year annual ice velocity mosaics and improve the quality of products including non-local means (NLM) filter, and absolute calibration using rock outcrops data. The resulting Version 2 of the mosaics offer reduced local errors, improved spatial resolution as described in the README file.
description: Version 202003
DOI: 10.1594/pangaea.694928
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station SEPT-1998-IR72

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.774636
title: Xray-ct-scanner images from IODP Hole 316-C0007C

description: Geocode = [m CSF-A] Top Core depth (below sea floor).Measurements data just above (negative section depth) and below (depth exceed section length) a core section are utilized in the deconvolution (http://en.wikipedia.org/wiki/Deconvolution).
DOI: 10.25345/c5x34n38h
title: MassIVE MSV000095397 - Glycan analysis of HIV envelope protein
title: Analysis of N-linked glycans of envelope protein from Human immunodeficiency virus (HIV-1) via mass spectrometry
DOI: 10.1594/pangaea.694935
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station SEPT-1998-K01

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.777209
title: Section images from IODP Hole 331-C0017B

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.859790
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE430
DOI: 10.1594/pangaea.906973
title: The Arctic sea ice drift simulation from October 2010 to December 2016

description: The simulated sea ice drift data is a by-product from a sea ice thickness assimilation system that generates the Arctic 'Combined Model and Satellite sea ice Thickness (CMST; doi:10.1594/PANGAEA.891475) ' dataset.The data also provide the ocean current velocity where ice free. To obtain the sea ice drift on the geographic coordinate, a transformation must be done as following:uE = AngleCS * SIuice - AngleSN * SIvice;vN = AngleSN * SIuice + AngleCS * SIvice;where uE and vN are two velocity components on the geographic coordinate; AngleCS and AngleSN can be found in 'grid.cdf'; SIuice and SIvice are sea ice velocity on model mesh.
DOI: 10.1594/pangaea.824509
title: Core summary for IODP Hole 318-U1359B
DOI: 10.1594/pangaea.900956
title: Cosmic-ray neutron counts at the Weisssee Snow Research Site
DOI: 10.1594/pangaea.828799
title: Core summary for IODP Hole 339-U1385C
DOI: 10.1594/pangaea.736420
title: Expanded measurements from Neumayer Station (2009-03)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.900957
title: Air pressure at the Weisssee Snow Research Site
DOI: 10.1594/pangaea.900958
title: Relative humidity at the Weisssee Snow Research Site
DOI: 10.1594/pangaea.897614
title: Effective reflectivity, vertical velocity, spectral width and snowfall rate estimates derived from a micro rain radar (MRR) at the Dumont d'Urville station, Adelie Land, East Antarctica

description: Antarctic precipitation is the main positive component in the surface mass balance of the Antarctic ice sheet, thus it is closely related to the evolution of the sea level worldwide. The lack of observations, at both surface and the vertical structure, have hindered the understanding of this important component. Recently a study of the vertical structure of the precipitation in Antarctica have been carried out using micro rain radar (MRR) observations (Durán-Alarcón et al., 2019, TC) at two different sites: Dumont d'Urville (DDU) and Princess Elisabeth (PE) stations. The present collection consists in 2-years of vertical profiles of effective reflectivity (Ze), mean Doppler velocity (W), spectral width (SW) and snowfall rate (S) derived from a K-band vertically-pointing micro rain radar (MRR), obtained at DDU in the framework of the Antarctic Precipitation Remote Sensing from Surface and Space project (APRES3). The observation range of the profiles is between 300 m and 3 km above ground level, with 100m and 1h of vertical and temporal resolutions, respectively. Vertical profiles were separated into surface precipitation and virga (i.e., precipitation that completely sublimes before reaching the surface) to evaluate the impact of virga on the structure of the vertical profiles. The strong katabatic winds blowing at DDU induce a decrease in Ze near to the ground due to the sublimation of the snowfall particles, and the W and SW increases as the height decreases. It was observed that virga is a frequent phenomenon at DDU, since more than a third (36%) of the profiles of precipitation observed with MRR corresponded to virga cases (more details in Durán-Alarcón et al., 2019, TC). This unique dataset of Antarctic precipitation observations in the low troposphere represents a great opportunity to better understand the current numerical models and satellite observations.
description: Supplement to: Durán-Alarcón, Claudio; Boudevillain, Brice; Genthon, Christophe; Grazioli, Jacopo; Souverijns, Niels; van Lipzig, Nicole P M; Gorodetskaya, Irina V; Berne, Alexis (2019): The vertical structure of precipitation at two stations in East Antarctica derived from micro rain radars. The Cryosphere, 13(1), 247-264
DOI: 10.1594/pangaea.759475
title: Basic and other measurements of radiation at Neumayer Station (2010-11)