cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.898324
title: Sea-bed videos (benthos) from the shelf west of Svalbard along ROV profile HE153/1243-3

description: Positions from notes of the principal investigator, depths from the ROV depth sensor. The ROV-system sprint 103 was equipped with two video- and one 36mm still camera, lights, flash-lights, compass, and parallel lasers providing a scale in the images, a tether-management system (TMS), a winch, and the board units. All cameras used the same main lens and could be tilted. Videos were recorded in Betacam-format. Videos were uploaded for documentation reasons independently of partly low quality due to a ROV driving strategy responding to varying environmental conditions such as sunlight and turbidity. Photographs along the same ROV-transect are available at https://doi.pangaea.de/10.1594/PANGAEA.898345. J. Gutt: mailto:Julian.Gutt@awi.de
DOI: 10.1594/pangaea.898300
title: River substrate of the Logie Burn, Scotland (2011 to 2014)

description: Substrate data collected from the restored over 2011 to 2014 and the control reach over 2012 to 2014.
DOI: 10.1594/pangaea.747445
title: Meteorological observations during AREND cruise from Hellevoetsluis to St. Eustacius started at 1780-12-03
DOI: 10.1594/pangaea.892853
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018072812

description: INITIALIZATION: 2018072812FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.897074
title: CICE output from Navy Earth System Prediction Capability (ESPC) for 2018122912

description: INITIALIZATION: 2018122912FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.729628
title: (Table 8) Distribution of radiolarians in ODP Hole 126-792B

description: species abundance: A = abundant, C = common, F = few, R = rare, - = absent
DOI: 10.1594/pangaea.897075
title: CICE output from Navy Earth System Prediction Capability (ESPC) for 2018123012

description: INITIALIZATION: 2018123012FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.806663
title: Basic measurements of radiation at station Cener (2013-01)
DOI: 10.1594/pangaea.650363
title: Description of lithologic section units of Hole 310-M0018A

description: Abbreviations: encr=enrcusting, br=braching, rob=robust, tab=tabular, fol=foliaceous, mas=massive, frags/frag=fragments/fragmented, unident=unidentifies, CAB=coral-algal bindstone, ECR=encrustation, MB=microbiolite, HAL=Halimeda, IS=in situ, UK=unknown, gp=group; DEPTH applies to top depth of section unit
DOI: 10.15468/dl.qsunck
title: Occurrence Download

description: A dataset containing 34 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON((-103.30485 20.88936,-103.48374 20.88379,-103.61951 20.83658,-103.64793 20.69487,-103.59425 20.4791,-103.29746 20.36666,-103.13643 20.42585,-103.06065 20.6151,-103.24694 20.90149,-103.30485 20.88936))",
 "HasGeospatialIssue is false",
 "TaxonKey is Sylvilagus floridanus (J.A.Allen, 1890)"
 ]
}

 The dataset includes 34 records from 4 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031160-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.897076
title: CICE output from Navy Earth System Prediction Capability (ESPC) for 2018123112

description: INITIALIZATION: 2018123112FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.650366
title: Description of lithologic section units of Hole 310-M0021A

description: Abbreviations: encr=enrcusting, br=braching, rob=robust, tab=tabular, fol=foliaceous, mas=massive, frags/frag=fragments/fragmented, unident=unidentifies, CAB=coral-algal bindstone, ECR=encrustation, MB=microbiolite, HAL=Halimeda, IS=in situ, UK=unknown, gp=group; DEPTH applies to top depth of section unit
DOI: 10.1594/pangaea.897077
title: CICE output from Navy Earth System Prediction Capability (ESPC) for 2019010112

description: INITIALIZATION: 2019010112FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.784333
title: Laser profiles of sea ice surface roughness during campaign IRIS 2004 from flight IRIS2004_200403140854
DOI: 10.1594/pangaea.898041
title: Basic measurements of radiation at station Cener (2019-01)
DOI: 10.1594/pangaea.896705
title: CICE output from Navy Earth System Model (NESM) for 2018120112

description: INITIALIZATION: 2018120112FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.752321
title: Meteorological observations during STAG cruise from Portsmouth to Madeira started at 1769-10-01
DOI: 10.1594/pangaea.809967
title: Stomach temperature profile of Weddell seal DRE1992_wed_s_m_01 from Drescher Inlet
DOI: 10.1594/pangaea.831670
title: (Table S1) Qualitative and semi-quantitative abundance of magnetic particles in Paleocene-Eocene sediments

description: On the mid-Atlantic Coastal Plain of the United States, Paleocene sands and silts are replaced during the Paleocene-Eocene Thermal Maximum (PETM) by the kaolinite-rich Marlboro Clay. The clay preserves abundant magnetite produced by magnetotactic bacteria and novel, presumptively eukaryotic, iron-biomineralizing microorganisms. Using ferromagnetic resonance spectroscopy and electron microscopy, we map the magnetofossil distribution in the context of stratigraphy and carbon isotope data and identify three magnetic facies in the clay: one characterized by a mix of detrital particles and magnetofossils, a second with a higher magnetofossil-to-detrital ratio, and a third with only transient magnetofossils. The distribution of these facies suggests that suboxic conditions promoting magnetofossil production and preservation occurred throughout inner middle neritic sediments of the Salisbury Embayment but extended only transiently to outer neritic sediments and the flanks of the embayment. Such a distribution is consistent with the development of a system resembling a modern tropical river-dominated shelf.
description: Where present, numerical counts of putative eukaryotic magnetofossils are based upon the number of particles in a magnetic extract observed under SEM on a single Cu grid within a ~40 micron by 50 micron frame. Observations of conventional magnetofossils are based on TEM. + indicates presence; ++ indicates high abundance; - indicates absence; blanks and ? indicate missing or inconclusive observations.
description: Supplement to: Kopp, Robert E; Schumann, Dirk; Raub, Timothy; Powars, David S; Godfrey, Linda V; Swanson-Hysell, Nicholas L; Maloof, Adam C; Vali, Hojatollah (2009): An Appalachian Amazon? Magnetofossil evidence for the development of a tropical river-like system in the mid-Atlantic United States during the Paleocene-Eocene thermal maximum. Paleoceanography, 24(4), PA4211
DOI: 10.1594/pangaea.806715
title: Ultra-violet measurements from station Izaña (2013-01)
DOI: 10.1594/pangaea.497071
title: Physical oceanography from BT during cruise M90DI00031B_1957
DOI: 10.1594/pangaea.809719
title: Dive depth profile of Weddell seal DRE1990_wed_a_f_08 from Drescher Inlet

description: Data processing by HighSEA X students.
DOI: 10.1594/pangaea.792621
title: (Table 1) Mn, Fe, TOC and CaCO3 concentrations in bottom sediments and silt waters of Kandalaksha Bay, White Sea

description: The redox stratification of bottom sediments in Kandalaksha Bay, White Sea, is characterized by elevated concentrations of Mn (3-5%) and Fe (7.5%) in the uppermost layer, which is two orders of magnitude and one and a half times, respectively, higher than the average concentrations of these elements in the Earth's crust. The high concentrations of organic matter (Corg = 1-2%) in these sediments cannot maintain (because of its low reaction activity) the sulfate-reducing process (the concentration of sulfide Fe is no higher than 0.6%). The clearest manifestation of diagenesis is the extremely high Mn2+ concentration in the silt water (&gt;500 µM), which causes its flux into the bottom water, oxidation in contact with oxygen, and the synthesis of MnO2 oxy-hydroxide enriching the surface layer of the sediments. Such migrations are much less typical of Fe. Upon oxygen exhaustion in the uppermost layer of the sediments, the synthesized oxyhydroxides (MnO2 and FeOOH) serve as oxidizers of organic matter during anaerobic diagenesis. The calculated diffusion-driven Mn flux from the sediments (280 µM/m**2 day) and corresponding amount of forming Mn oxyhydrate as compared to opposite oxygen flux to sediments (1-10 mM/m**2 day) indicates that &gt;10% organic matter in the surface layer of the sediments can be oxidized with the participation of MnO2. The roles of other oxidizers of organic matter (FeOOH and SO4**2-) becomes discernible at deeper levels of the sediments. The detailed calculation of the balance of reducing processes testifies to the higher consumption of organic matter during the diagenesis of surface sediments than it follows from the direct determination of Corg. The most active diagenetic redox processes terminate at depths of 25-50 cm. Layers enriched in Mn at deeper levels are metastable relicts of its surface accumulation and are prone to gradual dissemination.
description: Supplement to: Rozanov, Alexander G; Volkov, Igor I (2009): Bottom sediments of Kandalaksha Bay in the White Sea: the phenomenon of Mn. Geochemistry International, 47(10), 1004-1020
DOI: 10.1594/pangaea.805206
title: (Table 3) Foraminiferal 87Sr/86Sr ratios and ages of ODP Hole 162-986D sediments

description: Site 986 was drilled to 965 meters below seafloor (mbsf) on the western Svalbard margin to record the onset of glaciations and to date and document the glacial evolution in the Svalbard-Barents Sea region during the Pliocene-Pleistocene. In this paper, results of sedimentological analyses are discussed in light of seismic stratigraphy and new age determinations. The latter were difficult to obtain in the glacial deposits, and datums are sparse. Through combined paleomagnetic data, biostratigraphy, and Sr isotopes, however, an overall chronology for the main evolutionary steps is suggested. The cored sequence at Site 986 is younger than 2.6 Ma, and the lower 60 m of the section contains no evidence of a major glacial influence. An initial glaciation is interpreted to have occurred at ~2.3 Ma, resulting in increased sand deposition from debris flows at Site 986 and forming a prominent seismic reflector, R7. However, glaciers probably did not reach the shelf break until ~1.6-1.7 Ma (Reflector R6), after which the depositional environment was dominated by diamictic debris flows. A gradual change in source area from the Barents Sea to Svalbard is recorded primarily by changes in carbonate and smectite content, ~355 mbsf (Reflector R5), at an interpolated age of 1.4-1.5 Ma. During the last ~1 m.y., Site 986 has undergone more distal deposition as the main depocenters have shifted laterally. This has resulted in less frequent debris flows and more turbidites and hemipelagic deposits, with a slight fining upward of the cored sediments.
description: Sediment depth is given in mbsf. See also doi:10.1594/PANGAEA.805084 for a different Sr age determination of ODP Hole 162-986D.
description: Supplement to: Forsberg, Carl Fredrik; Solheim, Anders; Elverhoi, Anders; Jansen, Eystein; Channell, James E T; Andersen, Espen Sletten (1999): The depositional environment of the western Svalbard margin during the late Pliocene and the Pleistocene: sedimentary facies changes at Site 986. In: Raymo, ME; Jansen, E; Blum, P; Herbert, TD (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 162, 1-14
DOI: 10.1594/pangaea.694431
title: Temperature and salinity in the water column of the Aegean Sea at Station FEBR-1999-IR36

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.831481
title: (Fig. 9) Protein carbonyl contents in gills of Mytilus edulis (differenciating between ventral bends and the rest of the tissue) collected in Sylt
DOI: 10.1594/pangaea.806311
title: (Table 3) Representative analyses of zeolites from ODP Holes 140-504B

description: Calculation of structural formula based on 12 oxygen (laumonite) and 18 oxygens (heulandite).
DOI: 10.1594/pangaea.898315
title: Benthic foraminifera from sediment core MSM05/3_343300 off West Greenland
DOI: 10.1594/pangaea.784337
title: Laser profiles of sea ice surface roughness during campaign IRIS 2004 from flight IRIS2004_200403141141
DOI: 10.1594/pangaea.784007
title: Basic measurements of radiation at station Billings (2012-01), Version 1
DOI: 10.1594/pangaea.831233
title: (Table 2) Major and minor element concentration in the Kimmeridge Clay Foramtion, Dorset Coast

description: SECTION, height [m] referes to the height abov datum.
DOI: 10.1594/pangaea.759333
title: Expanded measurements from Neumayer Station (1999-03)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.854801
title: Sea level records and deep ocean temperatures from ODP site 177-1090
DOI: 10.1594/pangaea.805807
title: Geochemistry of sediment core PC-K15, Potter Cove, King George Island
DOI: 10.1594/pangaea.897374
title: Ultra-violet measurements from station Toravere (2018-11)
DOI: 10.1594/pangaea.898530
title: Water level and storage changes of Pung Co lake during 2000‒2017

description: Following information is included:1) Date of the data acquisition time in the form of yyyy-mm-dd.2) Lake water levels are orthometric heights with respect to EGM08, WGS84, in the unit of meter.3) Uncertainty of the lake water level in the unit of meter, if it is altimetry water level. The uncertainty of optical water levels was not calculated and set to 0.4) Lake water storage changes with respect to the baseline (lake water storage of the water level baseline H0, which is a value we do not exactly know; see https://doi.pangaea.de/10.1594/PANGAEA.898409) in the unit of km^3.5) The source of the data, 0 - Landsat, 1 - Envisat, 2 - ICESat, 3 - CryoSat, 4 - Jason-1/2/3.
DOI: 10.1594/pangaea.917426
title: 1-Hz PPP displacements at GEONET station 3076 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.495583
title: Water temperature MBT profiles from cruise U7426246M_1954
DOI: 10.1594/pangaea.898420
title: Radiosonde measurements from station Eastern North Atlantic (2015-04)

description: Launches may be at irregular time intervals
DOI: 10.1594/pangaea.889446
title: Burst performance of Polar cod (Boreogadus saida) under ocean acidification and warming conditions
DOI: 10.1594/pangaea.898533
title: Water level and storage changes of Salt lake during 2000‒2017

description: Following information is included:1) Date of the data acquisition time in the form of yyyy-mm-dd.2) Lake water levels are orthometric heights with respect to EGM96, WGS84, in the unit of meter.3) Uncertainty of the lake water level in the unit of meter, if it is altimetry water level. The uncertainty of optical water levels was not calculated and set to 0.4) Lake water storage changes with respect to the baseline (lake water storage of the water level baseline H0, which is a value we do not exactly know; see https://doi.pangaea.de/10.1594/PANGAEA.898409) in the unit of km^3.5) The source of the data, 0 - Landsat, 1 - Envisat, 2 - ICESat, 3 - CryoSat, 4 - Jason-1/2/3.
DOI: 10.1594/pangaea.786628
title: (Table 2-2) Chemical composition of clinopyroxene from cherty and siliceous-clayey rocks of accretionary complexes in Sikhote Alin
DOI: 10.1594/pangaea.856680
title: (Fig 1, page 350) A manganese nodule in the top part of the CHUBASCO station 17 core taken in the Pacific Ocean

description: The vast extent of pelagic deposits, covering about 70 per cent of the ocean floor, thus about half of the earth, makes them of obvious importance to all Earth Science. All the pelagic (eupelagic) sediments, whether largely of plankton remains or fine inorganic particles, have certain distinctive characteristics to reflect their environment of accumulation. The great segregation of manganese in pelagic sediments presents many problems. It is hypothesized that in the formation of present day nodules a relatively slow accumulation in order to permit deposition of more of the manganese as large nodules, rather than as the disseminated micronodules that are in larger proportion in the Tertiary.
description: 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.
description: Supplement to: Bramlette, M (1961): Pelagic sediments. in: Invited Lectures Presented at the International Oceanographic Congress Held in New York, 31 August-12 September 1959. Presented at the International Oceanographic Congress, 1959, American Association for the Advancement of Science, New York, U.S.A., 345-366
DOI: 10.1594/pangaea.496892
title: Physical oceanography from BT during cruise K90POB_1968
DOI: 10.1594/pangaea.784395
title: Laser profiles of sea ice surface roughness during POL-ICE 2007 field campaign from flight POL-ICE07_200703140839
DOI: 10.1594/pangaea.856738
title: Geochemistry of black shales from Breitbach Creek

description: Lower Cretaceous sediments are frequently characterized by a well expressed cyclicity. While the processes influencing environments above the carbonate compensation depth (CCD) are reasonably well understood, almost nothing is known about the deep ocean. Cretaceous sub-CCD sediments from the Tethys and Atlantic Oceans typically show rhythmic black/green shale successions. To gain insight into the nature of these black/green shale cycles, we performed detailed geochemical analyses (X-ray fluorescence, Rock-Eval and reactive iron analysis) on a 3 m long section of latest Aptian age. The major-element distribution of the analyzed shale sequence indicates a periodic change from a high-productivity and well-oxygenated green shale mode to a low-productivity oxygen-deficient black shale mode. It is proposed here that the preservation of organic matter was dependent on the strength of salinity-driven deepwater generation. Furthermore, the data show that the Corg content covaries with changes in the detrital composition. Therefore we hypothesize that Tethyan deepwater circulation was sensitive to changes in the monsoonal system. Time series analysis suggests that these changes are periodic in nature, although we are currently unable to prove that the dominant periodicity is related to the precession component of the Milankovitch frequencies.
description: Supplement to: Wortmann, Ulrich G; Hesse, Reinhard; Zacher, Katharina (1999): Major-element analysis of cyclic black shales: Paleoceanographic implications for the Early Cretaceous deep western tethys. Paleoceanography, 14(4), 525-541
DOI: 10.1594/pangaea.898628
title: Methane (CH4) data from Barrow, Alaska, 1986-2017

description: Methane (CH4) data and GPS information that was collected at Barrow, Alaska by NOAA's Global Monitoring Division.
DOI: 10.1594/pangaea.908579
title: (Table S2) Coarse fraction accumulation rate of ODP Hole 114-702B
DOI: 10.1594/pangaea.499054
title: Physical oceanography from BT during cruise U90X008240B_1977
DOI: 10.1594/pangaea.807600
title: (Table 5) Globocassidulina subglobosa and Cibicidoides sp. isotope composition for the middle-to-late Pliocene transition at DSDP Hole 80-548
DOI: 10.1594/pangaea.498303
title: Physical oceanography from BT during cruise U902H08766B_1933
DOI: 10.1594/pangaea.898731
title: Ultra-violet measurements from station Boulder, SURFRAD (2018-09)
DOI: 10.1594/pangaea.498624
title: Physical oceanography from BT during cruise U90VD08082B_1985