cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.909951
title: Expanded measurements from station Ny-Ålesund (2019-07)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.618972
title: Physical properties of sediments and sedimentary rocks from Kolguev-3 Hole drilled in the Kolguev Island, Barents Sea
DOI: 10.1594/pangaea.753948
title: (Table 2) Interstitial-water chemistry of ODP Site 113-690
DOI: 10.1594/pangaea.693700
title: Yearly production of marine products and its process lines in Tocopilla, Chile, 1998
DOI: 10.1594/pangaea.754588
title: (Appendix) Diatom abundances in ODP Hole 114-704
DOI: 10.1594/pangaea.923795
title: Ultra-violet measurements from station Goodwin Creek (2020-03)
DOI: 10.1594/pangaea.754597
title: (Appendix) Composition of coarse fraction of Leg114 samples
DOI: 10.1594/pangaea.898912
title: Meteorological synoptical observations from Neumayer Station (2009-02)

description: Version 2, 2019-03-01 with some minor corrections to the codes.
DOI: 10.1594/pangaea.674525
title: Radiosonde measurements from station Kwajalein (1992-05)
DOI: 10.1594/pangaea.754005
title: Argon concentration in waters of the Atlantic Ocean

description: Neutron activation analysis was used to determine content of dissolved argon at five points in the Atlantic Ocean at depths of 2 m.
description: Supplement to: Ilichev, O V; Kolobashkin, V M; Novichkov, V P; Piven', N S; Khristoforov, V A (1974): Determination of the argon content in water of the Atlantic Ocean by neutron activation analysis. Oceanology, 14, 914-916
DOI: 10.1594/pangaea.746140
title: (Table S3) Geochemical data and reconstructed sea surface temperatures from Cenomanian-Turonian strata from DSDP site 41-367
DOI: 10.1594/pangaea.783829
title: (Table 3) Isotopic composition of total organic carbon in sediments from Gorgo a Cerbara

description: SECTION, height [m] is from the top of the section decribed by Tejada et al. (2009, doi:10.1130/G25763A.1).
DOI: 10.1594/pangaea.806072
title: Basic measurements of radiation at station Nauru Island (2001-11)

description: Version 3, 2013-01-25
DOI: 10.1594/pangaea.680217
title: Other measurements at 300 m from station Boulder (1995-10)
DOI: 10.1594/pangaea.807817
title: Hydrochemistry measured on water bottle samples during POLARFRONT cruise PF91
DOI: 10.1594/pangaea.783701
title: (Table 6) Chemical composition of rocks from the Disvovery Rise and the Herdman Bank

description: Total Fe espressed as FeO.
DOI: 10.1594/pangaea.680166
title: Other measurements at 30 m from station Solar Village (2002-07)
DOI: 10.1594/pangaea.690295
title: Radiosonde M6_R043 during METEOR cruise M6 on 1966-08-26 05:34h

description: Height of tropause 9520 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.753873
title: (Table 7) Composition of rainwater collected over the Pacific and Indian Oceans in 1955-1960

description: Devoted to chemical interaction between the ocean and the atmosphere in the Pacific and Indian Oceans measured in 1955-1960.
description: Supplement to: Bruevich, Semyon V; Kulik, E Z (1967): Chemical interaction between the ocean and the atmosphere (salt exchange). Oceanology, 7, 279-293
DOI: 10.1594/pangaea.847914
title: (Table 2) Picked maximum velocities from 3 radars (RAY, SHK, and SUM), showing 10 explosions at Erebus volcano, Antarctica, and their respective directivity vectors

description: We used a novel system of three continuous wave Doppler radars to successfully record the directivity of i) Strombolian explosions from the active lava lake of Erebus volcano, Antarctica, ii) eruptions at Stromboli volcano, Italy, and iii) a man-made explosion in a quarry. Erebus volcano contains a convecting phonolite lava lake, presumably connected to a magma chamber at depth. It is one of the few open vent volcanoes that allow a direct observation of source processes during explosions. Its lava lake is the source of frequent violent Strombolian explosions, caused by large gas bubbles bursting at the lake surface. The exact mechanism of these bubble bursts is unclear, as is the mechanism of the creation of the infrasound signal accompanying the explosions. We use the Doppler radar data to calculate the directivity of Strombolian eruptions at Erebus. This allows us to derive information about the expected type of infrasound source pattern (i.e. the role of a dipole in addition to the monopole signature) and the physical structure of the volcano. We recorded 10 large explosions simultaneously with three radars, enabling us to calculate time series of 3D directivity vectors (i.e. effectively 4D), which describe the direction of preferred expansion of the gas bubble during an explosion. Such directivity information allows a comparison to dipole infrasound radiation patterns recorded during similar explosions only a few weeks later. Video observations of explosions support our interpretation of the measurements. We conclude that at Erebus, the directivity of explosions is mainly controlled by random processes. Since the geometry of the uppermost conduit is assumed to have a large effect on the directivity of explosions, the results suggest a largely symmetrical uppermost conduit with a vertical axis of symmetry. For infrasound recordings, a significant dipole signature can be expected in addition to the predominant monopole signature.
description: When the bubble expansion phase lasted for more than 1 s, several directivity vectors were calculated. Error boundaries on the picked velocities were determined manually, and their propagation on the directivity vectors were calculated. Note that errors due to unprecise station locations are negligible compared to errors resulting from picking uncertainties.
description: Supplement to: Gerst, Alexander; Hort, M; Kyle, Philip R; Vöge, Malte (2008): 4D velocity of Strombolian eruptions and man-made explosions derived from multiple Doppler radar instruments. Journal of Volcanology and Geothermal Research, 177(3), 648-660
DOI: 10.1594/pangaea.719090
title: Other measurements at 10 m from station Bondville (2007-06)
DOI: 10.1594/pangaea.907626
title: Stable water isotope composition (δ18O and δD) of firn core FP-4 from King George Island, Antarctica

description: High resolution stable water isotope composition (δ18O and δD) of firn core FP-4 retrieved at King George Island, South Shetland Islands, Antarctica. The core was sampled at 5 cm resolution at the Alfred Wegener Institute (AWI) ice core facilities in Bremerhaven, Germany. Stable water isotopes analysis were carried out at AWI in Potsdam, Germany.
DOI: 10.1594/pangaea.721983
title: Ultra-violet measurements from station Goodwin Creek (2005-07)

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.721476
title: Ultra-violet measurements from station Fort Peck (1999-05)

description: Version 2, 2009-06-19. 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.673337
title: Radiosonde measurements from station Barrow (1993-02)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.677455
title: Ozone measurements from station Ny-Ålesund (2000-05)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.722859
title: Ultra-violet measurements from station Rock Springs (1998-10)

description: Version 2, 2009-06-26. 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.735814
title: Meteorological synoptical observations from station Lindenberg (1995-03)
DOI: 10.1594/pangaea.755579
title: Meteorological synoptical observations from station Lindenberg (2003-09)
DOI: 10.1594/pangaea.687245
title: Egg production rates of copepods from seven SEPT-1999 WP-2 closing net catches

description: Sampling volume was estimated by the net mouth surface and the towing distance. Egg production rates of the dominant calanoid copepods were determined by incubation of fertilised females (eggs female-1 d-1) collected in the 0-100m layer. Copepod egg production was measured for the copepods Temora stylifera, Clausocalanus furcatus, Nannocalanus minor, Paracalanus parvus and Centropages typicus. On board experiments for the estimation of copepod egg production were taken place. For the estimation of copepod production (mgC m-2 d-1), lengths (copepods and eggs) were converted to body carbon (Hopcroft et al., 1998) and production was estimated from biomass and weight-specific egg production rates, by assuming that those rates are representative for juvenile specific growth rates (Berggreen et al., 1988).Berggreen, U., Hansen, B., Kiorboe, T. 1988. Food size spectra, ingestion and growth of copepod Acartia tonsa: implications for the determination of copepod production. Mar. Biol. 99: 341-352.Hopcroft, R.P., Roff J.C., Lombard, D. 1998. Production of tropical copepods in Kingston Harbour, Jamaica: the importance of small species. Mar. Biol. 130: 593-604
DOI: 10.1594/pangaea.718669
title: (Table 2) Oxygen and carbon isotope values for planktonic and benthic foraminifera from DSDP Site 71-511
DOI: 10.1594/pangaea.735618
title: (Table 67) Chemical composition of sediments from Polygon DM2474 and of their part leached by 1% H2SO4
DOI: 10.1594/pangaea.690296
title: Radiosonde M6_R044 during METEOR cruise M6 on 1966-08-26 10:29h

description: Height of tropause 9530 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.681146
title: Meteorological synoptical observations from station Ny-Ålesund (1996-03)

description: On 2016-07-06 some corrections on the wind speed were made for this dataset. The old version is available at: ftp://ftp.bsrn.awi.de/nya/OldVersions_2016-07-06_oldSYNOPS/
DOI: 10.1594/pangaea.868761
title: Geochemistry of sediment core COR0503-CL04-36
DOI: 10.1594/pangaea.548872
title: Physical oceanography at CTD station Chan_2003-10-17_14, Chanavallita, Chile
DOI: 10.1594/pangaea.721591
title: Other measurements at 10 m from station Fort Peck (2002-07)

description: Version 2, 2009-06-19
DOI: 10.1594/pangaea.714820
title: (Table 1) Organic carbon content and stable carbon isotope ratios, and hydrogen and oxygen index of DSDP Site 27-263
DOI: 10.1594/pangaea.821520
title: (Table 5) Nannofossil occurrence at DSDP Holes 57-438B and 57-439

description: Abundance abbreviations: Abundant (A) = 10-100 specimens per field of view; Common (C) =1-10 specimens per field of view; Few (F) = one specimen in 1-10 fields of view; Rare (R) = one specimen in 10-100 fields of view. The preservation states of nannofossils are designated as follows: G = Good preservation, little or no evidence of etching, dissolution, or overgrowth. All specimens readily identifiable. M = Moderately good preservation, slight etching or overgrowth which has destroyed or obscures delicate structures and ornamentation. Most specimens readily identifiable. P = Poor preservation, a majority of specimens strongly etched or overgrown, often fragmented. Diversity is low and species identification often difficult.
DOI: 10.1594/pangaea.718611
title: Other measurements at 10 m from station Boulder, SURFRAD (2002-10)

description: Version 2, 2009-06-12
DOI: 10.1594/pangaea.735085
title: Ultra-violet measurements from station Payerne (2008-11)

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 2017-01-27. UV reflect values might still contain errors.
DOI: 10.1594/pangaea.495134
title: Water temperature XBT profiles from cruise K9084_1986
DOI: 10.1594/pangaea.721176
title: Ultra-violet measurements from station Fort Peck (2005-07)

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.735878
title: Expanded measurements from station Lindenberg (1996-05)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.785526
title: Radiosonde measurements from station Tateno (2011-05)
DOI: 10.1594/pangaea.721224
title: Ultra-violet measurements from station Fort Peck (2006-10)

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.870947
title: Microsatellite marker data for 16 nuclear microsatellite loci for the Dahurian larch (Larix gmelinii) on the Taymyr Peninsula, north-central Siberia

description: The data table contains the biallelic data for 16 loci (LOCUS#: "K241", "K066", "K253", "K211", "d101", "K260", "K056", "K224", "Ld45", "K263", "K228", "K225", "K235", "K189", "Ld56", "Ld42") for 763 Larix individuals from 11 sites located on Taymyr Peninsula, 2 sites located along the Lower Lena and 2 sites along the Kolyma river.
DOI: 10.1594/pangaea.890986
title: Sulfur Isotopic Measurements of Canadian and South African Rivers

description: During a time of negligible atmospheric pO2, Earth's early sulfur cycle generated a spectacular geological signal seen as the anomalous fractionation of multiple sulfur isotopic ratios. The disappearance of this signal from the geologic record has been hypothesized to constrain the timing of atmospheric oxygenation, though interpretive challenges exist. Asymmetry in existing S isotopic data, for example, suggest that the Archean crust was not mass balanced, with the implication that the loss of S isotope anomalies from the geologic record might lag the rise of atmospheric O2. Here, we present new S isotopic analyses of modern surface and groundwaters that drain Archean terrains in order to independently evaluate Archean S cycle mass balance. Natural waters contain sulfur derived from the underlying bedrock and thus can be used to ascertain its S isotopic composition at scales larger than typical geological samples allow. Analyses of 52 water samples from Canada and South Africa suggest that the Archean crust was mass balanced with an average multiple S isotopic composition equivalent to the bulk Earth. Overall, our work supports the hypothesis that the disappearance of multiple S isotope anomalies from the sedimentary record provides a robust proxy for the timing of the first rise in atmospheric O2.
description: Supplement to: Torres, Mark A; Paris, Guillaume; Adkins, Jess F; Fischer, Woodward W (2018): Riverine evidence for isotopic mass balance in the Earth's early sulfur cycle. Nature Geoscience, 11(9), 661-664
DOI: 10.1594/pangaea.756111
title: Physical oceanography during Professor Vodyanitskiy cruise PV5
DOI: 10.1594/pangaea.864031
title: Other measurements at 10 m from station Goodwin Creek (2010-11)
DOI: 10.1594/pangaea.693678
title: Yearly production of marine products and its process lines in Calbuco, Chile, 1998
DOI: 10.1594/pangaea.875466
title: Meteorological synoptical observations from station Lindenberg (2010-06)
DOI: 10.1594/pangaea.693679
title: Yearly production of marine products and its process lines in Caldera, Chile, 1998
DOI: 10.1594/pangaea.670297
title: Basic and other measurements of radiation at Neumayer Station (2003-11)
DOI: 10.1594/pangaea.881218
title: Radiosonde measurements from station Barrow (2011-09)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.910572
title: Table 3. Experimental SSE Parameters

description: Vo = initial slip velocity (cm/yr), r = sample radius (mm)
DOI: 10.1594/pangaea.693687
title: Yearly production of marine products and its process lines in Mejillones, Chile, 1998
DOI: 10.1594/pangaea.881220
title: Radiosonde measurements from station Barrow (2011-10)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.881283
title: Radiosonde measurements from station Barrow (2017-05)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.895078
title: Backward particle trajectories used to estimate the catchment area of sediment traps HG-IV and HG-N deployed in Fram Strait

description: To determine the catchment area of sediment traps deployed in Fram Strait, we used a Lagrangian particle tracking algorithm and computed backward particle trajectories. This was done by reversing the flow field, i.e. particles were treated as if they were rising from the mooring location to the surface with a negative settling velocity, being horizontally displaced with the reversed horizontal velocity (vertical ocean velocities were neglected). Particles were advected with daily averaged horizontal model velocities from the ocean-sea ice model FESOM and a constant settling velocity of either 120 m/day, 60 m/day or 20 m/day. They were released at either 200 m or 2300 m depth, and tracked until they reached the surface. The computation of backward particle trajectories was performed for two locations of moorings equipped with sediment traps in central Fram Strait, HG-N and HG-IV. Particles were released once per day during the time period 2002 to 2009, resulting in 2920 trajectories. Considering the 12 experiments (two mooring positions, two depths of release, three settling velocities), altogether 35040 trajectories were calculated. A time step of 1 hour was used for the trajectory calculation, and thus hourly positions and corresponding temperature and salinity values were stored.
DOI: 10.1594/pangaea.693685
title: Yearly production of marine products and its process lines in Iquique, Chile, 1998
DOI: 10.1594/pangaea.738767
title: Pollen profile DED, Velky Ded, Czech Republic

description: Method: KOH, acetolysis, mostly pretreated with HF.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.881282
title: Basic and other measurements of radiation at station Barrow (2017-05)
DOI: 10.1594/pangaea.714829
title: (Table 2) Organic carbon content and stable carbon isotope ratios, and hydrogen and oxygen index of sediment core BX-5
DOI: 10.1594/pangaea.858630
title: Table 2. Living foraminiferal taxa in the box core PO287-28-1B (no/86cc)
DOI: 10.1594/pangaea.881286
title: Basic and other measurements of radiation at station Barrow (2017-07)
DOI: 10.1594/pangaea.896683
title: Radiosonde measurements from station Sapporo (2018-10)
DOI: 10.1594/pangaea.903031
title: Age determination of core MF4-12 from Mfabeni peatland

description: a: Modern age, expressed as percent modern carbon (pMC), equals –307±23 14C yrs BP.b: Modern age, expressed as percent modern carbon (pMC), equals –143±24 14C yrs BP.
DOI: 10.1594/pangaea.901913
title: Meteorological synoptical observations from station Tateno (2019-03)
DOI: 10.1594/pangaea.904628
title: Skeletal and polypide morphometry of New Zealand stenolaemate bryozoans

description: This dataset provides raw morphometric measurements of the zooids of 13 bryozoan species (Bryozoa: Stenolaemata) collected from 45° 47.89' S, 170° 54.5' E; 46°54.87' S, 168°13.06' E and 47°07.70' S, 168°10.79' E from the depths of 40-90 m. Animals were cultured in isothermic room and feeding polypides with fully extended lophophores were imaged with a camera and a dissecting microscope.I recorded skeletal and soft-body traits. Most are quantitative: length and width of the zooid tube at the level of the orifice, aperture length and width, mouth diameter, tentacle crown diameter, crown height, tentacle number, full tentacle length and tentacle length visible above aperture, as well as length of the longest and shortest tentacles for obliquely-truncated lophophores. Others are qualitative: tentacle crown symmetry and curvature, polypide condition/age and colony growth form. All measurements are reported in micrometers.Morphometric terminology follows Treatise on Invertebrate Paleontology part G (Boardman & Cheetham, 1983).
DOI: 10.1594/pangaea.758852
title: (Table 1) Chemical composition of nodules and crusts from the Sea of Japan
DOI: 10.1594/pangaea.778680
title: Airborne sea ice thickness measurements from the PAMARCMIP field program in spring 2009 from flight HEM_PAM09_05
DOI: 10.1594/pangaea.667978
title: Basic measurements of radiation at station Boulder (1999-01)
DOI: 10.1594/pangaea.822534
title: Meteorological measurements in the upper air at station Alauostari (Petsamo), 1937-06-28 to 1937-08-21, ERA-CLIM ID 4794
DOI: 10.1594/pangaea.912525
title: Basic measurements of radiation at station Cener (2019-05)
DOI: 10.1594/pangaea.828908
title: Pass-through measurements of magnetic susceptibility from IODP Hole 339-U1389C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.881415
title: Radiosonde measurements from station Barrow (2013-12)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.912050
title: Ultra-violet measurements from station Desert Rock (2019-06)
DOI: 10.1594/pangaea.677348
title: Ozone measurements from Neumayer Station (2005-07)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.723632
title: Basic measurements of radiation at station Billings (2002-01)

description: Version 2, 2009-07-02
DOI: 10.1594/pangaea.908514
title: Radiosonde measurements from station Izaña (2019-10)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.855538
title: Basic measurements of radiation at station Carpentras (2015-08)
DOI: 10.1594/pangaea.701423
title: Global radiation during ALKOR cruise AL270
DOI: 10.1594/pangaea.718176
title: Basic measurements of radiation at station Boulder, SURFRAD (2007-12)
DOI: 10.1594/pangaea.719546
title: Ultra-violet measurements from station Bondville (2002-06)

description: Version 2, 2009-06-15. 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.922188
title: Expanded measurements from station Ny-Ålesund (2020-07)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.722234
title: Other measurements at 10 m from station Goodwin Creek (1998-01)

description: Version 2, 2009-06-24
DOI: 10.1594/pangaea.718568
title: Basic measurements of radiation at station Boulder, SURFRAD (2001-12)

description: Version 2, 2009-06-12
DOI: 10.1594/pangaea.714819
title: (Table 1) Organic carbon content and stable carbon isotope ratios, and hydrogen and oxygen index of DSDP Site 27-261
DOI: 10.1594/pangaea.750877
title: Meteorological observations during NAUTILUS cruise from St. Johns to St. Johns started at 1772-07-22
DOI: 10.1594/pangaea.915486
title: Electrical conductivity, porosity and density of sediment core GeoB18549-2
DOI: 10.1594/pangaea.917576
title: Major element geochemistry of volcanic and volcaniclastic rocks from Riverton, Southland, New Zealand

description: Major element geochemical data from tholeiitic basaltic volcanic and volcaniclastic rocks from the Riverton Peninsula and Colac Bay, Southland, New Zealand. These rocks form part of the Permian Brook Street Terrane.