cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.871912
title: Daily temperature measurements in Riobamba, Ecuador in May and August 1872, digitized version

description: The exact date of the observations are unknown only the Month is identified.---The data of this dataset might have been revised during the review process. This might therefore be an old version. To be sure, please check the respective dataset at doi:10.1594/PANGAEA.871480
DOI: 10.1594/pangaea.753637
title: (Appendix B) Interstitial-water samples corrected for admixed surface seawater introduced by drilling, ODP Leg 112
DOI: 10.1594/pangaea.854146
title: (Table 2, page 470), Spectrographic values for the chemical composition of a Pacific Ocean manganese nodule

description: Average quantitative spectrographic data are presented for V, Ti, Zr, Ni, Co, Sc, Cr and La in the following Pacific deep-sea cores: siliceous ooze (3), red clay (6), volcanic mud (3), calcareous ooze (3) and one manganese nodule, and in 23 near-shore cores, mostly from the Gulf of Mexico.
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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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: Young, Edward J (1968): Spectrographic data on cores from the Pacific Ocean and the Gulf of Mexico. Geochimica et Cosmochimica Acta, 32(4), 466-471
DOI: 10.1594/pangaea.853984
title: Basic measurements of radiation at station Cener (2015-07)
DOI: 10.1594/pangaea.759628
title: (Table 2) Stable carbon isotope ratios of benthic foraminifera of ODP Site 121-752

description: Measured on single specimen: Anomalinoides danicus 400-770 µm in diameter; Stensionia beccariiformis 280-580 µm in diameter in the Paleocene to lower Eocene, in Maestrichtian smaller (less than 350 µm) measurement of 10 specimens.
DOI: 10.1594/pangaea.840669
title: Ice-rafted debris in late MIS 35 to MIS 28 samples of ODP Hole 177-1090D
DOI: 10.1594/pangaea.719093
title: Radiosonde measurements from station Bondville (2007-07)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.887240
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2009406

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.911169
title: Basic measurements of radiation at station Billings (2017-10)
DOI: 10.1594/pangaea.816003
title: (Table 2) Major and minor elements in sediments from DSDP Holes 70-507F, 70-507C, and 70-507H
DOI: 10.1594/pangaea.677769
title: Ozone measurements from station South Pole (1997-11)
DOI: 10.1594/pangaea.854336
title: Meteorological synoptical observations from station Tamanrasset (2015-07)

description: This dataset has been updated on the 2016-01-26, as the code had been interpreted wrongly
DOI: 10.1594/pangaea.877477
title: Urban meteorological data of station 2223 for the city of Amsterdam during the summer of 2015
DOI: 10.1594/pangaea.883447
title: Radiosonde measurements from station Barrow (2003-06)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.831271
title: Meteorological measurements in 60 min resolution at oasis of Asrir test site in 2004

description: Dataset created by IMPETUS subproject B3. IMPETUS data set ID: 108
DOI: 10.1594/pangaea.854392
title: (Table 11) Distribution and abundance of conodonts in Devonian/Carboniferous boundary profile at Seiler-Schurf 0
DOI: 10.1594/pangaea.854645
title: Description of ferromanganese concretions from the Jervis Inlet, British Columbia

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.
DOI: 10.1594/pangaea.748888
title: Meteorological observations during El Cortes cruise from La Coruña to La Habana started at 1786-03-10
DOI: 10.1594/pangaea.816057
title: (Table 1) Geochemistry of adjacent nontronite granules from a stratigraphically shallow nontronite DSDP Sample 70-509B-2-1,44-48
DOI: 10.1594/pangaea.839809
title: (Table S1) Offsets between drilling depths (meters below surface, MBS) of Polecat Bench cores A and B used to develop the composite depth scale (meters composite depth, MCD)

description: DEPTH, sediment/rock = Coretop depth (MBS)
DOI: 10.1594/pangaea.854393
title: (Table 6) Distribution and abundance of conodonts in Devonian/Carboniferous boundary profile at Scharfenberg
DOI: 10.1594/pangaea.818821
title: Glacier mass balance Hintereisferner, Ötztal Alps, Austria, 1999/2000
DOI: 10.1594/pangaea.854413
title: Illustrations of nodules and manganese coated rocks from the John Murray Expedition (R/V Mabahiss)

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.
DOI: 10.1594/pangaea.747313
title: Meteorological observations during ALKEMADE cruise from Batavia to Texel started at 1774-11-09
DOI: 10.1594/pangaea.817382
title: (Table 8) Major element composition of olivine DSDP Hole 67-500
DOI: 10.1594/pangaea.733804
title: Meteorological observations during Moana Wave cruise HOT-101
DOI: 10.1594/pangaea.907227
title: Track of GPS very-near surface drifter ISMER_20141024_spot219
DOI: 10.1594/pangaea.810009
title: (Table 2) Carbon, nitrogen, and CaCO3 at DSDP Hole 76-534A, ship-board measurements
DOI: 10.1594/pangaea.675491
title: Specific activity of radionuclides in bottom sediments of the Barents Sea sampled from R/V Geofizik in 2000
DOI: 10.1594/pangaea.808225
title: Dive depth profile of Weddell seal DRE1992_wed_a_f_04 from Drescher Inlet

description: Data processing by HighSEA X students.
DOI: 10.1594/pangaea.777652
title: (Table 1) Rock magnetic properties of the sediment samples from ODP Hole 127-797B

description: Paleomagnetic and rock magnetic studies of the sediment samples from Site 797 were carried out. Thermal demagnetization was found to be more effective in removing secondary overprinting than alternating field demagnetization. Production of new magnetic minerals during the thermal treatment was frequently observed and made thorough demagnetization difficult, however. Thermal demagnetization of orthogonal IRM's suggests that magnetite and pyrrhotite are common magnetic minerals in these sediments. The Lowrie-Fuller test and xARM/x ratio show apparent grain size of the magnetic minerals to be that of single-domain to small multi-domain state. A downcore decrease of rock magnetic parameters such as ARM, IRM, and xARM/x ratio in the upper half of the hole indicates progressive diagenetic dissolution of finer magnetic minerals. In the lower part where igneous rocks intruded, production of magnetic minerals is suggested by discontinuous change of the downcore trend, which may have brought remagnetization of the sediment samples.
description: Supplement to: Torii, Masayuki; Hayashida, Akira; Vigliotti, Luigi; Wippern, Jobst J M (1992): Rock magnetic properties of sediments from Site 797, Japan Sea. In: Tamaki, K; Suychiro, K; Allan, J; McWilliams, M; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 127/128(2), 947-957
DOI: 10.1594/pangaea.808009
title: (Figure 2) Radiolarian range chart of ODP Site 138-845, part I

description: DEPTH, sediment is given in mbsf. Relative abundance of individual species: R = rare (&lt;10 specimens); F = few, (10-100 specimens); C = common (100-200 specimens), and A = abundant (&gt;200 specimens). A- signifies that a species was looked for and not found, small case letters = specimens found that are thought to be reworked, ? = a dubious identification.
DOI: 10.1594/pangaea.867783
title: Radiosonde measurements from station Tamanrasset (2016-10)

description: Start location: Tamanrasset; Distance from radiation site: 10 km
DOI: 10.1594/pangaea.748106
title: Hydrography on standard level calculated from water bottle samples of RV Goyena in 1973
DOI: 10.1594/pangaea.777260
title: (Table 2) Mineralogy of ODP Hole 127-797B

description: Sediment depth is given in mbsf. The XRD analyses were carried out on bulk samples, without any treatment or separation, in the Department of Chemistry of the University of Waterloo. A Cu(Kappa alphy) source was used in a Siemens D500 diffractometer at a scan rate of 0.015°/s, from 8° to 32° (2Theta). "Opal-CT" indicates undifferentiated cristobalite and tridymite. "Zeolites" are undifferentiated zeolite phases, though the most common are clinoptilolite and phillipsite, and analcime and laumontite are not uncommon. The height and width of the peaks frequently prevent the resolution of specific phases. For sections 127-797B-31X-1 through -33X-3, the quartz is detrital in origin, and is flagged with an asterisk (*). References: Finney et al. (1975), Chen et al. (1978), Hawkins et al. (1978), JCPDS (1978), Gottardi and Galli (1985), and Roberts et al. (1990).
DOI: 10.1594/pangaea.839688
title: (Table 1) Pb isotopic composition and concentration for sediments samples of core VNTR01-8PC, ODP Site 138-849A and ashes from Chimborazo
DOI: 10.1594/pangaea.719024
title: Ultra-violet measurements from station Bondville (2006-02)

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 2017-02-09.
DOI: 10.1594/pangaea.719037
title: Radiosonde measurements from station Bondville (2006-05)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.854904
title: Daily polynya area from passive microwave satellite sensors SMMR, SSMI, and SSMIS in the North Water polynya region in 1998/1999
DOI: 10.1594/pangaea.862519
title: GPS-derived precipitable water vapor content calculated for station ZIM2
DOI: 10.1594/pangaea.854819
title: Age - depth relation of Site 208-1262
DOI: 10.1594/pangaea.667946
title: Basic measurements of radiation at station Boulder (1996-05)
DOI: 10.1594/pangaea.733234
title: Physical oceanography during Moana Wave cruise HOT-92 on section PRS2
DOI: 10.1594/pangaea.736242
title: Meteorological synoptical observations from station Lindenberg (2000-06)
DOI: 10.1594/pangaea.494700
title: Physical oceanography during cruise K9007_1963
DOI: 10.1594/pangaea.908872
title: Meteorological synoptical observations from station Lindenberg (2017-10)
DOI: 10.1594/pangaea.846719
title: Basic measurements of radiation at station Boulder (2015-04)
DOI: 10.1594/pangaea.719323
title: Radiosonde measurements from station Bondville (1997-11)

description: Version 2, 2009-06-15; Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.854839
title: Experimental assessment of sediment burial in eelgrass Zostera marina: Biomass
DOI: 10.1594/pangaea.495357
title: Water temperature XBT profiles from cruise U31X047835_1973
DOI: 10.1594/pangaea.862462
title: GPS-derived precipitable water vapor content calculated for station TOUL
DOI: 10.1594/pangaea.494811
title: Physical oceanography during cruise U31X000073C
DOI: 10.1594/pangaea.846950
title: Abundance of mesozooplankton in the western part of the Black Sea in summer 2005 during Phase 2: Leg1 from the GEF Project

description: The sampling area was extended to the Western-South area off the Black Sea coast from Kaliakra cape toward the Bosforous. Samples were collected along four transects. The whole dataset is composed of 17 samples (from 10 stations) with data of mesozooplankton species composition abundance and biomass. Sampling for zooplankton was performed from bottom up to the surface at depths depending on water column stratification and the thermocline depth. These data are organized in the “Control of eutrophication, hazardous substances and related measures for rehabilitating the Black Sea ecosystem: Phase 2: Leg I: PIMS 3065”. Data Report is not published.Zooplankton samples were collected with vertical closing Juday net,diameter - 36cm, mesh size 150 µm. Tows were performed from surface down to bottom meters depths in discrete layers. Samples were preserved by a 4% formaldehyde sea water buffered solution. Sampling volume was estimated by multiplying the mouth area with the wire length.Mesozooplankton abundance: The collected material was analysed using the method of Domov (1959). Samples were brought to volume of 25-30 ml depending upon zooplankton density and mixed intensively until all organisms were distributed randomly in the sample volume. After that 5 ml of sample was taken and poured in the counting chamber which is a rectangle form for taxomomic identification and count. Large (&gt; 1 mm body length) and not abundant species were calculated in whole sample. Counting and measuring of organisms were made in the Dimov chamber under the stereomicroscope to the lowest taxon possible. Taxonomic identification was done at the Institute of Oceanology by Kremena Stefanova using the relevant taxonomic literature (Mordukhay-Boltovskoy, F.D. (Ed.). 1968, 1969,1972). Taxon-specific abundance: The collected material was analysed using the method of Domov (1959). Samples were brought to volume of 25-30 ml depending upon zooplankton density and mixed intensively until all organisms were distributed randomly in the sample volume. After that 5 ml of sample was taken and poured in the counting chamber which is a rectangle form for taxomomic identification and count. Copepods and Cladoceras were identified and enumerated; the other mesozooplankters were identified and enumerated at higher taxonomic level (commonly named as mesozooplankton groups). Large (&gt; 1 mm body length) and not abundant species were calculated in whole sample. Counting and measuring of organisms were made in the Dimov chamber under the stereomicroscope to the lowest taxon possible. Taxonomic identification was done at the Institute of Oceanology by Kremena Stefanova using the relevant taxonomic literature (Mordukhay-Boltovskoy, F.D. (Ed.). 1968, 1969,1972).
DOI: 10.1594/pangaea.854913
title: Daily polynya area from passive microwave satellite sensors SMMR, SSMI, and SSMIS in the North Water polynya region in 2007/2008
DOI: 10.1594/pangaea.706056
title: Age determination of ODP Site 133-820 (Table 4)

description: A detailed pollen record from the Ocean Drilling Program Site 820 core, located on the upper part of the continental slope off the coast of northeast Queensland, was constructed to compare with the existing pollen record from Lynch's Crater on the adjacent Atherton Tableland and allow the production of a regional picture of vegetation and environmental change through the last glacial cycle. Some broad similarities in patterns of vegetation change are revealed, despite the differences between sites and their pollen catchments, which can be related largely to global climate and sea-level changes. The original estimated time scale of the Lynch's Crater record is largely confirmed from comparison with the more thoroughly dated ODP record. Conversely, the Lynch's Crater pollen record has assisted in dating problematic parts of the ODP record. In contrast to Lynch's Crater, which reveals a sharp and sustained reduction in drier araucarian forest around 38,000 yrs BP, considered to have been the result of burning by Aboriginal people, the ODP record indicates, most likely, a stepwise reduction, dating from 140,000 yrs BP or beyond. The earliest reduction shows lack of a clear connection between Araucaria decline and increased burning and suggests that people may not have been involved at this stage. However, a further decline in araucarian forest, possibly around 45,000 yrs BP, which has a more substantial environmental impact and is not related to a time of major climate change, is likely, at least partially, the result of human burning. The suggestion, from the ODP core oxygen isotope record, of a regional sea-surface temperature increase of around 4ºC between about 400,000 and 250,000 yrs BP, may have had some influence on the overall decline in Araucaria and its replacement by sclerophyll vegetation.
description: Oxygen isotope stage boundaries according to the age models of Peerdeman et al. (1993). Further relevant data sets: Peerdeman et al. (1993) doi:10.1594/PANGAEA.706033, Peerdeman and Davies (1993) doi:10.1594/PANGAEA.705538, Kershaw (1976) doi:10.1594/PANGAEA.706055, Wei and Gartner (1993) doi:10.1594/PANGAEA.706054
description: Supplement to: Moss, Patrick T; Kershaw, A Peter (2000): The last glacial cycle from the humid tropics of northeastern Australia: comparison of a terrestrial and a marine record. Palaeogeography, Palaeoclimatology, Palaeoecology, 155(1-2), 155-176
DOI: 10.1594/pangaea.805255
title: (Table 2) Hysteresis properties and Curie temperatures at DSDP Hole 83-504B
DOI: 10.1594/pangaea.854966
title: Annotated record of the detailed examination of Mn deposits from THETA-1 (TH1) Expedition stations

description: The cores described in this list were taken on the THETA-1 (TH1) Expedition in June to September 1956 from the R/V Theta. A total of 19 cores and dredges were recovered and are archived at Scripps for sampling and study.
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.
DOI: 10.1594/pangaea.804882
title: (Table 6) Geochemistry of heulandite at DSDP Hole 83-504B

description: Ti, Fe2+, Fe3+, and Mg also measured but not detected.
DOI: 10.1594/pangaea.718997
title: Radiosonde measurements from station Bondville (2005-07)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.719006
title: Other measurements at 10 m from station Bondville (2005-09)
DOI: 10.1594/pangaea.547872
title: Nutrients measured on water bottle samples at station Bm_1997-09-08_4, Bajo Molle, Chile
DOI: 10.1594/pangaea.750986
title: Meteorological observations during NYMPHE cruise from Table Bay to Madras started at 1779-11-05
DOI: 10.1594/pangaea.821781
title: Length changes of Austrian glaciers 1972/1973
DOI: 10.1594/pangaea.718869
title: Other measurements at 10 m from station Boulder, SURFRAD (2004-11)
DOI: 10.1594/pangaea.748108
title: Hydrography on standard level calculated from water bottle samples of RV General Zapiola from 1962 to 1963
DOI: 10.1594/pangaea.855295
title: (Table II-5) Foraminiferal stable oxygen isotope record of sediment core NH15P
DOI: 10.1594/pangaea.783890
title: Hydrological records from the Vernagtferner Basin - Vernagtbach station, for the year 1993
DOI: 10.1594/pangaea.782895
title: Basic measurements of radiation at station Billings (2010-10)
DOI: 10.1594/pangaea.718912
title: Other measurements at 10 m from station Bondville (2004-05)
DOI: 10.1594/pangaea.859720
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE350
DOI: 10.1594/pangaea.903745
title: Measured coccolith-size data of the Genus Gephyrocapsa in the Quaternary Sequence of the Tropical Indian Ocean, ODP Hole 115-709C

description: Stratigraphic variations in the morphometry of the genus Gephyrocapsa were quantitatively investigated in the Quaternary sequence of ODP Hole 115-709C recovered from the tropical Indian Ocean. This is raw data of the measurement.
description: The first 200 specimens of Gephyrocapsa species were measured for the overall size of the coccolith, the diameter of the central opening, and the angle of the central bridge vs. the long axis of the coccolith. The two lengths were measured to 0.1 µm precision. Because the bridge angle is difficult to measure precisely under a transmission microscope, it was classified into six categories:1 (0° - 15°), 2 (15° - 30°), 3 (30° - 45°), 4 (45° - 60°), 5 (60° - 75°), and 6 (75° - 90°). The angle of the central bridge on 0° means parallel to long axis of the coccolith. For those samples in which the small forms dominated the flora and the large forms were scarce, additional measurements were conducted exclusively for the large forms to obtain a sufficient data set.
description: Supplement to: Matsuoka, Hiromi; Okada, Hisatake (1990): Time-progressive morphometric changes of the genus Gephyrocapsa in the Quaternary sequence of the tropical Indian Ocean, Site 709. In: Duncan, RA; Backmann, J; Peterson, LC; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 115, 255-270
DOI: 10.1594/pangaea.901930
title: Other measurements at 10 m from station Sioux Falls (2018-10)
DOI: 10.1594/pangaea.718930
title: Ultra-violet measurements from station Bondville (2004-10)

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 2017-02-09.
DOI: 10.1594/pangaea.718931
title: Radiosonde measurements from station Bondville (2004-10)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.718938
title: Ultra-violet measurements from station Bondville (2004-12)

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 2017-02-09.
DOI: 10.1594/pangaea.719530
title: Ultra-violet measurements from station Bondville (2002-02)

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.855360
title: Foraminiferal stable isotope ratios of sediment core EW9504-05PC
DOI: 10.1594/pangaea.855361
title: Foraminiferal stable isotope ratios of sediment core EW9504-08PC
DOI: 10.1594/pangaea.603901
title: Hydrographic and chemical measurements at anchor station M8_065-10b of the eastern North Atlantic (Table 1)