cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.880096
title: Scalloped hammerhead shark (Sphyrna lewini) tracking records in the Red Sea (dive extraction)
DOI: 10.1594/pangaea.778588
title: Natural gamma radiation from IODP Hole 317-U1353A

description: Geocode = Depth CSF-A (m).Natural gamma radiation principles and system implementation notes; Technical Note 26 Chapter 5: http://www-odp.tamu.edu/publications/tnotes/tn26/CHAP5.PDF
DOI: 10.1594/pangaea.494705
title: Physical oceanography during cruise K9007_1976
DOI: 10.1594/pangaea.676850
title: Clay mineral composition of &lt;0.001 mm grain size fraction of sedimentary rocks from Hole VNIIO-1985-Arct-01 drilled in the Barents Sea

description: Types of rocks and their ages are given in the special data set; see: doi:10.1594/PANGAEA.676854
DOI: 10.1594/pangaea.820203
title: (Table 4) Geochemistry of glasses in boninite pillow fragments at DSDP Hole 60-458

description: CIPW norms computed assuming Fe**2+ /Fe**2+ + Fe**3+ = 0.86.
DOI: 10.1594/pangaea.676863
title: Clay mineral composition of &lt;0.001 mm grain size fraction of sedimentary rocks from Hole VNIIO-1985-Kur-01 drilled in the Barents Sea

description: Types of rocks and their ages are given in the special data set; see: doi:10.1594/PANGAEA.676866
DOI: 10.1594/pangaea.893130
title: Record of the Mg/Ca ratio in G. bulloides from sediment core MD07-3076
DOI: 10.1594/pangaea.816911
title: Physical oceanography during John P. Tully cruise IOS_96-18
DOI: 10.1594/pangaea.679339
title: Clay mineral composition of &lt;0.005 mm grain size fraction of sedimentary rocks from Hole VNIIO-1989-27 drilled in the Barents Sea
DOI: 10.1594/pangaea.680757
title: Clay mineral composition of &lt;0.005 mm grain size fraction of sediments from Hole VNIIO-1983-Bel-01 drilled in the Kara Sea

description: Types of rocks and their ages are given in the special data set; see: doi:10.1594/PANGAEA.680748
DOI: 10.1594/pangaea.745704
title: (Table 2) Major element and CIPW norms of volcanic rocks from ODP Holes 107-655A and 107-654A

description: Norms and MgV calculated assuming Fe2O3/FeO = 0.15. Analyses with FeO carried out at Dip. Scienze della Terra (University of Pisa); others with total iron as Fe203, averages of analyses performed at DST, Universities of Bologna and Pisa.
DOI: 10.1594/pangaea.816678
title: Hydrochemistry measured on water bottle samples during HUDSON cruise HUD92/37
DOI: 10.1594/pangaea.711152
title: (Supp. Fig.) Clay mineral content of sediment core JR104-GC358
DOI: 10.15468/dl.gcq96z
title: Occurrence Download

description: A dataset containing 125 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is Human Observation",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "StateProvince is Utah",
 "TaxonKey is Bombus nevadensis Cresson, 1874",
 "Year 2014-2024"
 ]
}

 The dataset includes 125 records from 2 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031371-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.835808
title: Pollen profile GAI1, Gaienhofen, Germany

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.774415
title: (Table 8) Modal phenocryst mineralogy of rift basement ODP Leg 126 samples

description: Phenocrysts are &gt;0.5 mm except for magnetite where &gt;0.1 mm. X indicates &gt;5% by volume; &lt; indicates 1%-5%; - indicates not present. N indicates that the silicate phenocrysts were tabulated in Sites 790/791, table 11 of Taylor, Fujioka, et al. (1990, doi:10.2973/odp.proc.ir.126.1990), but the thin sections were unavailable for further study. Parentheses indicate some alteration. Units are the shipboard igneous stratigraphic units (Taylor, Fujioka, et al., 1990).
DOI: 10.1594/pangaea.887218
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2006408

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.527960
title: Clay mineralogy of sediments of the deep sea sediment trap LB-1, Norwegian Sea (Appendix A1.7, A5.2.8)
DOI: 10.1594/pangaea.711159
title: (Supp. Fig.) Clay mineral content of sediment core JR104-GC370
DOI: 10.1594/pangaea.759212
title: Physical oceanography during Magnus Heinason cruise MH99/2
DOI: 10.1594/pangaea.723757
title: Nematoda size spectra analysis of sediment core 13077-021, subcore A
DOI: 10.1594/pangaea.887147
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN1997403

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.729627
title: (Table 7) Distribution of radiolarians in ODP Hole 126-792A

description: species abundance: A = abundant, C = common, F = few, R = rare, - = absent
DOI: 10.1594/pangaea.887239
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2009404

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.834688
title: (Table S1) Hematite stained grains, Icelandic glass, and detritic carbonate in MIS4-2 of DSDP Site 94-609, fine sand fraction

description: DEPTH, sediment/rock gives meters below seafloor [mbsf]. AGE [ka BP] gives the age before 2000.
DOI: 10.1594/pangaea.847829
title: (Table 1, page 1124), Chemical composition of Lake Michigan manganese nodules

description: Manganese nodules containing up to 22 percent manganese oxide were found in Green Bay and the western and northern parts of Lake Michigan. The chemical composition of these nodules resembles that of shallow-water lacustrine and marine nodules. The manganese content of interstitial water is in some places enriched as much as 4000 times over that of lake water.
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: Rossmann, Ronald; Callender, Edward (1968): Manganese Nodules in Lake Michigan. Science, 162(3858), 1123-1124
DOI: 10.1594/pangaea.711493
title: (Table 2) Magnetic properties and oxidation state of titanomagnetite in MORB older than 100 Ma, ODP Hole 129-802A
DOI: 10.1594/pangaea.494589
title: Physical oceanography during cruise CUSNS_1961
DOI: 10.1594/pangaea.774805
title: (Table T2) Rock magnetic properties of ODP Hole 204-1245B

description: Sediment depth is given in mbsf. All magnetic properties are normalized by the dry weight of the samples.
DOI: 10.1594/pangaea.774814
title: (Table T9) Rock magnetic properties of ODP Hole 204-1252A

description: Sediment depth is given in mbsf. All magnetic properties are normalized by the dry weight of the samples.
DOI: 10.1594/pangaea.905840
title: Underway CTD data collected during METEOR cruise M120

description: Version = PO-GLOBAL-SVN = 277Matlab = 8.3.0.532 (R2014a)Release = 3
DOI: 10.1594/pangaea.707058
title: (Table 1ab) Chemical and mineral compositions of basalts from DSDP Hole 65-483B
DOI: 10.1594/pangaea.494942
title: Physical oceanography during cruise UXXXX09999C_1982
DOI: 10.1594/pangaea.887227
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2006410

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.711494
title: (Table 2) Magnetic properties and oxidation state of titanomagnetite in MORB older than 100 Ma, DSDP Hole 26-257
DOI: 10.1594/pangaea.729005
title: (Table T49) Secondary minerals in fine fraction sampled from basalts of tholeiitic series from Emperor Seamount chain, Leg 55, Hole 433C (Suiko seamount), X-ray diffraction data
DOI: 10.1594/pangaea.885780
title: Lake-groundwater exchange at Laguna La Conceja (Ruidera, Spain) during 2009
DOI: 10.1594/pangaea.711513
title: (Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 63-469
DOI: 10.1594/pangaea.751373
title: (Table 1) Mineral associations of ODP Hole 111-504B

description: + = present, - = absent
DOI: 10.1594/pangaea.756587
title: (Table 3A) Clay mineralogy of ODP Hole 116-717C

description: Data are from Lille (Bouquillon et al., 1990).
DOI: 10.1594/pangaea.862337
title: GPS-derived precipitable water vapor content calculated for station MDVJ
DOI: 10.1594/pangaea.494537
title: Physical oceanography during cruise B26AS11104C
DOI: 10.1594/pangaea.876035
title: Net photosynthesis of large benthic foraminifera holobionts

description: Net oxygen production.
DOI: 10.1594/pangaea.711514
title: (Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 65-483B
DOI: 10.1594/pangaea.774812
title: (Table T7) Rock magnetic properties of ODP Hole 204-1250C

description: Sediment depth is given in mbsf. All magnetic properties are normalized by the dry weight of the samples.
DOI: 10.1594/pangaea.807703
title: (Table 2) Clay-mineral characteristics at DSDP Hole 80-548A
DOI: 10.1594/pangaea.774182
title: P-wave velocity anisotropy from IODP Hole 316-C0007D

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.784914
title: XRF-core logger measurements from IODP Hole 333-C0011D

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.704241
title: Temperature, salinity, and concentrations of nutrients and chlorophyll a in the Gulf of Naples and the Gulf of Salerno in March 1987

description: Before analysing samples have been frozen at -20°C.
DOI: 10.1594/pangaea.774813
title: (Table T8) Rock magnetic properties of ODP Hole 204-1251B

description: Sediment depth is given in mbsf. All magnetic properties are normalized by the dry weight of the samples.
DOI: 10.1594/pangaea.808214
title: (Table 1) Lithofacies, chronostratigraphy, and minerals at DSDP Hole 80-548A
DOI: 10.1594/pangaea.906104
title: Size classes of Hemigrapsus takanoi in the Kiel Fjord, Western Baltic Sea during 2017
DOI: 10.1594/pangaea.811104
title: (Table 6) Normative mineralogy of basalts at DSDP Hole 73-520
DOI: 10.1594/pangaea.811108
title: (Table 10) Normative mineralogy of basalts from lower part of DSDP Hole 73-524
DOI: 10.1594/pangaea.779057
title: (Table T2) Mineral composition of altered felsic volcanic rocks from ODP Hole 193-1189A

description: Sediment depth is given in mbsf. The analyses were conducted on samples taken directly from the cores and on the powders produced for onboard X-ray diffraction analyses (XRD powder).
DOI: 10.1594/pangaea.810641
title: (Table 2) Minerals and rock types at DSDP Holes 74-525A and 74-528

description: D = dominant, A = abundant, P = present, ? = unknown.
DOI: 10.1594/pangaea.819088
title: (Appendix C) Minerals at DSDP Hole 64-478

description: Sediment depth is given in mbsf. Between depths 203.5 and 241.3 as well as between 253.3 and 256.9 is sill. After depth 338.92 is thick sill. tr. = traces, X = common, XX = abundant, - = not determined.
DOI: 10.1594/pangaea.820140
title: (Table 1) Geochemistry of gabbros at DSDP Hole 60-453

description: Empty cells = no data. CIPW norms are calculated assuming Fe**2+ /Fe**2+ + Fe**3+ = 0.86.
DOI: 10.1594/pangaea.862199
title: GPS-derived precipitable water vapor content calculated for station CFAG
DOI: 10.1594/pangaea.887164
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN1999403

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.733206
title: Physical oceanography during Maurice Ewing cruise HOT-64 on section PRS2
DOI: 10.1594/pangaea.733226
title: Physical oceanography during Moana Wave cruise HOT-84 on section PRS2
DOI: 10.1594/pangaea.733259
title: Physical oceanography during Kaimikai O Kanaloa cruise HOT-109 on section PRS2
DOI: 10.1594/pangaea.494648
title: Physical oceanography during cruise IXXXXKVTXXC
DOI: 10.1594/pangaea.494945
title: Physical oceanography during cruise UXXXX09999C_1987
DOI: 10.1594/pangaea.494853
title: Physical oceanography during cruise U90XX00004C_1980
DOI: 10.1594/pangaea.494807
title: Physical oceanography during cruise U18X009210C
DOI: 10.1594/pangaea.704310
title: Temperature, salinity, and concentrations of oxygen, nutrients and chlorophyll a in the Gulf of Naples and the Gulf of Salerno in November 1985

description: Before analysing samples have been frozen at -20°C.
DOI: 10.1594/pangaea.816924
title: Hydrochemistry measured on water bottle samples during John P. Tully cruise IOS_94-02
DOI: 10.1594/pangaea.848297
title: (Table 2, Annex), Manganese crusts and manganese coated rocks recovered from study area (lat 26°N)

description: An asymmetric tectonic fabric was delineated by narrow-beam bathymetric profiles in a 180-km2 area of the Mid-Atlantic Ridge crest at lat 26°N. Features of the tectonic fabric are a continuous rift valley offset by small (&lt;10-km) transform faults and minor fracture zones expressed as valleys with intervening ridges that trend normal and oblique to the two sides of the rift valley. The discharge zone of a postulated sub-sea-floor hydrothermal convection system is focused by faults on the southeast wall of the rift valley and driven by intrusive heat sources beneath the rift valley. The rift valley has a double structure consisting of linear segments, bounded by ridges, and basins at the intersections of the minor fracture zones. The double structure of the rift valley acts like a template that programs the reproduction of the tectonic fabric. The minor fracture zones form an asymmetric V about the rift valley at variance with the symmetric small circles formed by major fracture zones. To reconcile the asymmetry of minor fracture zones with the symmetry of major fracture zones, it is proposed that the minor fracture zones have been preferentially reoriented by an external stress field attributed to interplate and intraplate motions. Major fracture zones remain symmetric under the same stress field owing to differential stability between minor and major structures of oceanic lithosphere.
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: Rona, Peter A; Harbison, Reginald N; Bassinger, Bobby G; Scott, Robert B; Nalwalk, Andrew J (1976): Tectonic fabric and hydrothermal activity of Mid-Atlantic Ridge crest (lat 26°N). Geological Society of America Bulletin, 87, 661-674
DOI: 10.1594/pangaea.831536
title: Physical oceanography during HEINCKE cruise HE168/2
DOI: 10.1594/pangaea.687241
title: Nutrients from bottle profile SEPT-1999-K9
DOI: 10.1594/pangaea.785193
title: Basic measurements of radiation at station Eureka (2011-04)
DOI: 10.1594/pangaea.733177
title: Physical oceanography during Wecoma cruise HOT-35 on section PRS2
DOI: 10.1594/pangaea.816684
title: Nutrients measured on water bottle samples during HUDSON cruise HUD92/53
DOI: 10.1594/pangaea.835481
title: Hydrochemistry measured on water bottle samples during HEINCKE cruise HE201
DOI: 10.1594/pangaea.816912
title: Physical oceanography during John P. Tully cruise IOS_97-02
DOI: 10.1594/pangaea.494884
title: Physical oceanography during cruise U90XX00023C
DOI: 10.1594/pangaea.495787
title: Water temperature IBT profiles from cruise U90BR86112I_1986
DOI: 10.1594/pangaea.817264
title: Hydochemistry measured on water bottle samples during TYRO cruise NIOP-A1
DOI: 10.1594/pangaea.494684
title: Physical oceanography during cruise K9006_1960
DOI: 10.1594/pangaea.784880
title: Physical oceanography during Le Noroit curise ECOMARGE2
DOI: 10.1594/pangaea.494928
title: Physical oceanography during cruise U90XX00157C
DOI: 10.1594/pangaea.494948
title: Physical oceanography during cruise UZZX000005C
DOI: 10.1594/pangaea.494799
title: Physical oceanography during cruise P67CEAREX_1994
DOI: 10.1594/pangaea.733051
title: Physical oceanography during Moana Wave cruise HA-3

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.494802
title: Physical oceanography during cruise P67CEAREX_1997
DOI: 10.1594/pangaea.495764
title: Water temperature XBT profiles from cruise U74XX79427_1977
DOI: 10.1594/pangaea.726475
title: Physical oceanography during cruise 64PE306 at CTD station 64PE306-2
DOI: 10.1594/pangaea.887596
title: Basic measurements of radiation at station Gandhinagar (2014-06)

description: Short-wave nighttime values were artificially set to 0, this will be changed in February 2019.
DOI: 10.1594/pangaea.687233
title: Nutrients from bottle profile SEPT-1999-K1
DOI: 10.1594/pangaea.687235
title: Nutrients from bottle profile SEPT-1999-K3
DOI: 10.1594/pangaea.722936
title: Ultra-violet measurements from station Rock Springs (2000-07)

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.723016
title: Ultra-violet measurements from station Rock Springs (2002-09)

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.726204
title: (Table 2) Stable carbon and oxygen isotope ratios of Globigerinoides ruber from sediment core RC12-344
DOI: 10.1594/pangaea.723606
title: Radiosonde measurements from station Southern Great Plains (2001-04)

description: Version 2, 2009-07-02; Launches at irregular time intervals. The radiosonde measurements from station Southern Great Plains are used for Billings and E13
DOI: 10.1594/pangaea.722284
title: Ultra-violet measurements from station Goodwin Creek (1999-06)

description: Version 2, 2009-06-24. 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.724349
title: Radiosonde measurements from station Desert Rock (2009-06)

description: If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.722514
title: Silicic acid concentration of sediment core 12930-075
DOI: 10.1594/pangaea.687231
title: Total organic carbon from bottle APRIL-2000-K6

description: The samples (10 ml) were obtained in pre-combusted (480oC, 12 h) glass ampoules, acidified with HCl to 0.1% by volume and flame - sealed immediately on board. High Temperature Catalytic Oxidation HTCO using a Shimadzu 5000 TOC analyzer. Sugimura, Y & Y. Suzuki, 1988. Cauwet, G., 1994.
DOI: 10.1594/pangaea.723799
title: Radiosonde measurements from station Southern Great Plains (2006-03)

description: Launches at irregular time intervals. The radiosonde measurements from station Southern Great Plains are used for Billings and E13
DOI: 10.1594/pangaea.726465
title: (Table 1) 137Cs and 90Sr concentrations, salinity, and temperature in waters of the southeastern Baltic Sea on October 16, 2001

description: An analysis of variations in 137Cs and 90Sr concentrations in Baltic Sea surface waters after the accident at the Chernobyl nuclear power plant was performed. Instability of 137Cs concentrations during the short-term observations was found, when they differed 2- to 3-fold. Concentrations of 90Sr appeared to be more stable; meanwhile, their deviations sometimes exceeded ranges of experimental errors. By variations in the monthly average values of radionuclide concentrations in surface waters of the Baltic Sea in 1989-1995, no trend of water self-purification was observed. Theoretical results obtained confirmed a potential of formation and propagation of patches with increased concentrations of 137Cs in the southeastern Baltic Sea. The most reliable factor that controlled the process of self-purification of Baltic Sea water appeared to be the mean annual value of radionuclide concentration. Pronounced divergences were obtained between the measured and calculated mean annual concentrations of 137Cs and 90Sr in surface waters of the Baltic Sea in 1989-2001. These divergences are explained by potential influence of waters from the Gulf of Bothnia and by other additional supplies of radionuclides to marine environment, which were not included into mathematical models.
description: Supplement to: Styro, D; Morkuniene, R; Vdovinskiene, S (2006): The process of self-purification of the Baltic Sea waters from artificial radionuclides. Oceanology, 46(3), 358-367
DOI: 10.1594/pangaea.773877
title: Structure description (VCD) from IODP Hole 316-C0007A

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.722291
title: Other measurements at 10 m from station Goodwin Creek (1999-08)

description: Version 2, 2009-06-24
DOI: 10.1594/pangaea.723319
title: Description of profile 7140-303
DOI: 10.1594/pangaea.726466
title: (Table 1) Properties of grab sampled sediments from the Nha Trang Bay

description: General characteristics of macrobenthos of muddy sediments of the subtidal (19-24 m) zone in the Nha Trang Bay (South Vietnam) were described based on the survey performed in April-May 2002. The mean abundance of organisms was 637 ind/m**2 and the mean biomass was 2.3 g/m**2. Sixty-seven macrobenthic species were found during the study. The main structural features of the macrobenthos were high species diversity, low species recurrence, and high evenness of species structure with the absence of clearly manifested dominants. The number of species encountered regularly increased with the increase in the total area sampled from 210 to 5000 cm**2, though the relation did not reach saturation. Similarities and differences between the macrobenthos structures in the Nha Trang Bay and those in some tropical and boreal soft-bottom communities are discussed.
description: Supplement to: Udalov, S S; Britaev, T A; Than, N T H (2006): Features of the soft-bottom subtidal macrobenthos in Nha Trang Bay (Vietnam, South China Sea). Oceanology, 46(4), 483-491
DOI: 10.1594/pangaea.723343
title: Description of profile 7140-328
DOI: 10.1594/pangaea.859689
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE314
DOI: 10.1594/pangaea.930067
title: Age determination of sediment core Ghats_BOP

description: Most radiocarbon dates were published in Bhagwat et al., 2012; 2014.