cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.738394
title: (Table 13) Composition of chrome-spinellids from peridotites of the Doldrums Fault
DOI: 10.1594/pangaea.917256
title: 1-Hz PPP displacements at GEONET station 1086 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.673518
title: Radiosonde measurements from station Bermuda (1999-01)

description: Start location: Bermuda; Distance from radiation site: 2 km
DOI: 10.1594/pangaea.789289
title: (Table 2A) Geochemistry at DSDP Hole 93-603
DOI: 10.1594/pangaea.678082
title: Expanded measurements from station Ny-Ålesund (1993-06)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.806377
title: Continuous meteorological observations at SIMA station Xingó reservoir in 2013

description: Quality flags: ? = questionable; / = not valid
DOI: 10.1594/pangaea.842315
title: Radiosonde measurements from station Darwin (2004-10)

description: Version 3, 2015-02-04; Launches at irregular time intervals
DOI: 10.1594/pangaea.857535
title: Lithogenic flux and grain size distribution from sediment trap M3_1, 21 sample cups

description: 21 sample cups
DOI: 10.1594/pangaea.830432
title: Color data from IODP Hole 338-C0002L

description: Geocode = [m CSF-A]
DOI: 10.1594/pangaea.857573
title: A foraminiferal δ¹⁸O record of sediment core GT90-3 covering the last 2,200 years

description: For many years the Torino Cosmogeophysics group has been studying sediment cores drilled from the Gallipoli Terrace in the Gulf of Taranto (Ionian Sea) and deposited in the last millennia. The gravity core GT90-3, in which the 18O series was measured, was drilled from the Gallipoli Terrace in the Gulf of Taranto (Ionian Sea) at 39°45'53''N, 17°53'33''E. It was extracted at a depth of 178 m and its length is 3.57 m. Thanks to its geographical location, the Gallipoli Terrace is a favourable site for climatic studies based on marine sediments, because of its closeness to the volcanically active Campanian area, a region that is unique in the world for its detailed historical documentation of volcanic eruptions. Tephra layers corresponding to historical eruptions were identified along the cores, thus allowing for accurate dating and determination of the sedimentation rate. The measurements performed in different cores from the same area showed that the sedimentation rate is uniform across the whole Gallipoli Terrace. We measured the oxygen isotope composition d18O of planktonic foraminifera. These measurements provided a high-resolution 2,200-year-long record. We sampled the core using a spacing of 2.5 mm corresponding to 3.87 years. Each sample of sediment (5 g) was soaked in 5% calgon solution overnight, then treated in 10% H2O2 to remove any residual organic material. Subsequently it was washed with a distilled-water jet through a sieve with a 150 µm mesh. The fraction &gt; 150 µm was kept and oven-dried at 5°C. The planktonic foraminifera Globigerinoides ruber were picked out of the samples under a microscope. For each sample, 20-30 specimens were selected from the fraction comprised between 150 µm and 300 µm. The use of a relatively large number of specimens for each sample reduces the isotopic variability of individual organisms, giving a more representative d18O value. The stable isotope measurements were performed using a VG-PRISM mass spectrometer fitted with an automated ISO-CARB preparation device. Analytical precision based on internal standards was better than 0.1 per mil. Calibration of the mass spectrometer to VPDB scale was done using NBS19 and NBS18 carbonate standards. The strategic location of the drilling area makes this record a unique tool for climate and oceanographic studies of the Central Mediterranean.
DOI: 10.1594/pangaea.726792
title: (Enclosure 2) Carbon and nitrogen content of exposure Fluderbach C, Samerberg

description: Horizontal sample surface 6 cm x 6 cm. Zero at the base of the profile.
DOI: 10.1594/pangaea.726793
title: (Enclosure 2) Carbon and nitrogen content of exposure Fluderbach I, Samerberg

description: Horizontal sample surface 6 cm x 6 cm. Zero at the base of the profile. Hiatus at 0.17 m, 0.27 m, most likely also at 0.2 m.
DOI: 10.1594/pangaea.729529
title: (Table 2) Radiolarians from ODP Hole 125-784A

description: abundances: A = abundant, C = common, F = few, R = rare, - = absent
DOI: 10.1594/pangaea.720406
title: Documentation of sediment core GIK16317-2
DOI: 10.1594/pangaea.862456
title: GPS-derived precipitable water vapor content calculated for station TIXG
DOI: 10.1594/pangaea.887191
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2001403

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.829348
title: Vane shear strength measurements from IODP Hole 340-U1394A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.729486
title: (Table T121) Secondary minerals in igneous rocks of Yamato Basin, Japan Sea, Leg 127, Hole 797C
DOI: 10.1594/pangaea.494777
title: Physical oceanography during cruise N58LA98802C
DOI: 10.1594/pangaea.846601
title: Radiosonde measurements from station Boulder (2014-10)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.846602
title: Other measurements at 300 m from station Boulder (2014-10)
DOI: 10.1594/pangaea.733189
title: Physical oceanography during New Horizon cruise HOT-47 on section PRS2
DOI: 10.1594/pangaea.718327
title: Ultra-violet measurements from station Boulder, SURFRAD (1996-12)

description: Version 2, 2009-06-12. 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.917340
title: 1-Hz PPP displacements at GEONET station 1179 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.670842
title: Basic measurements of radiation at station Lerwick (2006-01)
DOI: 10.1594/pangaea.808678
title: Basic measurements of radiation at station Nauru Island (2005-03)

description: Version 3, 2013-03-10
DOI: 10.1594/pangaea.854677
title: Glacier mass balance Vernagtferner, Austria, 2009/2010
DOI: 10.1594/pangaea.729246
title: (Table 4g) Lower Paleocene calcareous nannofossils in ODP Hole 122-762C

description: species abundance: A = abundant (&gt;10 specimens per field of view at 1000 X), C = common (1-10 specimens), F = few (1 specimen in 2-10 fields), R = rare (1 specimen in 11-100 fields), V = very rare (1 specimen in 101-1000 fields), - = absent
DOI: 10.1594/pangaea.693759
title: Chlorophyll a, phaeopigments, and primary production in surface water during Professor Vodyanitskiy cruise PV41

description: Chlorophyll a and phaeopigments where measured fluorometrically by use of laboratory fluorometer constracted on the base of spectrophotometer Specol, fitted with a red sensitive photomultiplier, blue lamp, blue filter and red filter. Accuracy: lower limit = 0.01 mg/m**3 and the error of Chl and Phaeo determination is 10-15% (calculated from 10-15 repeatings).
DOI: 10.1594/pangaea.818839
title: Elevation zones Hintereisferner, Ötztal Alps, Austria, 1952/1953
DOI: 10.1594/pangaea.727182
title: (Table 3) Stable carbon and oxygen isotope ratios of planktonic foraminifera from DSDP Hole 94-609
DOI: 10.1594/pangaea.829266
title: P-Wave velocity (PWC) from IODP Hole 340-U1401A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.748117
title: Hydrography on standard level calculated from water bottle samples of RV Investigator from 1964 to 1965
DOI: 10.1594/pangaea.842156
title: (Table 1) Age determination of sediment cores EW9302-JPC1 and EW9302-JPC2

description: Results from two deep sea cores from northeast of Newfoundland at 1251 and 2527 m water depth, respectively, indicate that during the time period from 160,000 to 10,000 years BP, ice rafting events in the Labrador Sea were accompanied by rapid variations in deep and surface water circulation. Twelve ice-rafting events occurred, each coinciding with high concentrations of detrital carbonate and oxygen isotopic depletion of both surface and bottom waters. Eleven of these can be correlated with the North Atlantic Heinrich events H1–H11. The remaining very conspicuous ice-rafting event took place early in MIS substage 5e, at a time when the planktic faunal assemblage suggests marked warming of the sea surface. In the shallower core, benthic d13C values rise from a minimum during the deglaciation to peak substage 5e values following the last ice-rafting event, indicating that the ventilation of intermediate depths was renewed after the deglaciation was complete and continued throughout substage 5e. The benthic foraminifera suggest that this well-ventilated water mass was comparable to the modern Labrador Sea Water (LSW). The benthic faunas suggest that a relatively warm intermediate water mass entered the SE Labrador Sea during Heinrich events. Generally low benthic d13C values indicate that this water mass was poorly ventilated and rich in inorganic nutrients. Isotope data and benthic faunal distributions indicate that North Atlantic Deep Water (NADW) formed in the Norwegian-Greenland Sea reached the SE Labrador Sea between the Heinrich events.
description: Supplement to: Rasmussen, Tine Lander; Oppo, Delia W; Thomsen, Erik; Lehman, Scott J (2003): Deep sea records from the southeast Labrador Sea: ocean circulation changes and ice-rafting events during the last 160,000 years. Paleoceanography, 18(1), 1018
DOI: 10.1594/pangaea.818869
title: Elevation zones Hintereisferner, Ötztal Alps, Austria, 1982/1983
DOI: 10.1594/pangaea.829039
title: Magnetic remanence from IODP Hole 339-U1388C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.695525
title: Radiosonde measurements from station Ny-Ålesund (2007-11)

description: The Ny-Ålesund radiosonde program is part of the GCOS Reference Upper-Air Network (GRUAN). Please consider using the Ny-Alesund reference radiosonde data with higher temporal resolution and uncertainty values for all height levels, available via http://www.gruan.org.
DOI: 10.1594/pangaea.828761
title: P-Wave velocity (PWL) from IODP Hole 336-U1384A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.828483
title: Pass-through measurements of magnetic susceptibility from IODP Hole 323-U1343E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.828831
title: Gas measurements from IODP Hole 339-U1389A

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.724225
title: Other measurements at 10 m from station Southern Great Plains (2006-03)
DOI: 10.1594/pangaea.818870
title: Elevation zones Hintereisferner, Ötztal Alps, Austria, 1983/1984
DOI: 10.1594/pangaea.835525
title: Radiosonde measurements from station Momote (2002-03)

description: Version 3, 2014-09-04. Launches at irregular time intervals
DOI: 10.1594/pangaea.846473
title: Other measurements at 300 m from station Boulder (2014-07)
DOI: 10.1594/pangaea.860384
title: Ultra-violet measurements from station Desert Rock (2009-08)

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 2017-02-08.
DOI: 10.1594/pangaea.832907
title: Structure of seven dominant vegetation types in the rainy season 2002 in the Aguima Catchment, Benin
DOI: 10.1594/pangaea.494833
title: Physical oceanography during cruise U58X001300C
DOI: 10.1594/pangaea.835931
title: Pollen profile TYR1, Tyre, Lebanon

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.917088
title: 1-Hz PPP displacements at GEONET station 0913 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.667760
title: Basic measurements of radiation at station Bermuda (2001-06)
DOI: 10.1594/pangaea.723462
title: Basic measurements of radiation at station Billings (1996-04)

description: Version 2, 2009-07-02
DOI: 10.1594/pangaea.494814
title: Physical oceanography during cruise U31X010241C
DOI: 10.1594/pangaea.733212
title: Physical oceanography during Moana Wave cruise HOT-70 on section PRS2
DOI: 10.1594/pangaea.816004
title: (Table 3) Major and minor elements in sediments from DSDP Hole 70-509B
DOI: 10.1594/pangaea.691476
title: Monthly landings in 1998, Tocopilla, Chile
DOI: 10.1594/pangaea.748220
title: Hydrography on standard level calculated from water bottle samples of RV Patriot from 1981 to 1989
DOI: 10.1594/pangaea.818774
title: Glacier mass balance Hintereisferner, Ötztal Alps, Austria, 1952/1953
DOI: 10.1594/pangaea.849075
title: (page 121) Observation of manganese nodules in the Kara Sea

description: This work describes the Dutch participation to the first International Polar Year, 1882-1883. The main objective of the expedition was to take meteorological and other scientific observations and assess the navigability of the Kara sea during the winter. It was undertaken on the steamship Varna along with the Danish Polar Expedition abord the Dymphna.
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: Snellen, M; Ekama, H (1910): Rapport sur l'expédition Néerlandaise qui a hiverné dans la Mer de Kara en 1882/83. J. van Boekhoven, Utrecht, 275 pp
DOI: 10.1594/pangaea.826069
title: Gamma ray attenuation bulk density from IODP Hole 327-U1363D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.826104
title: Reflectance spectroscopy and colorimetry from IODP Hole 327-U1363F

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.893164
title: Monthly 2-meter temperature observations at Evangelistas (1901 - 2016), southern South America

description: 3- or 6-hourly 2-meter temperature observations were recorded at Evangelista in the southern South America region. These were retrieved from the Navy Weather Service of Chile and then digitized and condensed into monthly means.
DOI: 10.1594/pangaea.825992
title: P-Wave velocity (PWL) from IODP Hole 329-U1366E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.835812
title: Pollen profile HALAMKY, Halámky, Czech Republic

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.826286
title: Thermal conductivity of IODP Hole 330-U1372A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.826347
title: Natural gamma radiation from IODP Hole 330-U1377A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.826348
title: P-Wave velocity (PWC) from IODP Hole 330-U1377A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.672605
title: Basic and other measurements of radiation at station South Pole (1992-08)
DOI: 10.1594/pangaea.825290
title: Reflectance spectroscopy and colorimetry from IODP Hole 329-U1368F

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.719146
title: Other measurements at 10 m from station Bondville (2008-08)
DOI: 10.1594/pangaea.707657
title: Meteorological synoptical observations from station Payerne (2005-02)
DOI: 10.1594/pangaea.672814
title: Basic and other measurements of radiation at station South Pole (1999-05)
DOI: 10.1594/pangaea.721464
title: Ultra-violet measurements from station Fort Peck (1999-01)

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.822332
title: (Table 3) Amorphous silica at DSDP Legs 56-57 Holes
DOI: 10.1594/pangaea.824725
title: Natural gamma radiation from IODP Hole 324-U1347A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.735829
title: Meteorological synoptical observations from station Lindenberg (1996-06)
DOI: 10.1594/pangaea.824089
title: Reflectance spectroscopy and colorimetry from IODP Hole 318-U1356A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.672211
title: Radiosonde measurements from station South Pole (2002-01)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.823309
title: (Table 1) Petrographic summary of DSDP Hole 55-433C tholeiitic basalts

description: #1 = &lt;&lt;1.
DOI: 10.1594/pangaea.835799
title: Pollen profile CV8A, Suchdol, Czech Republic

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.715035
title: Magnetic properties of the oceanic igneous rocks (Table 1)

description: Hysteresis measurements have been carried out on a suite of ocean-floor basalts with ages ranging from Quaternary to Cretaceous. Approximately linear, yet separate, relationships between coercivity (Bc) and the ratio of saturation remanence/saturation magnetization (Mrs/Ms) are observed for massive doleritic basalts with low-Ti magnetite and for pillow basalts with multi-domain titanomagnetites (with x= 0.6). Even when the MORB has undergone lowtemperature oxidation resulting in titanomaghemite, the parameters are still distinguishable, although offset from the trend for unoxidized multidomain titanomagnetite. The parameters for these iron oxides with different titanium content reveal contrasting trends that can be explained by the different saturation magnetizations of the mineral types. This plot provides a previously underutilized and non-destructive method to detect the presence of low-titanium magnetite in igneous rocks, notably MORB.
description: Supplement to: Wang, Daming; Van der Voo, Rob (2004): The hysteresis properties of multidomain magnetite and titanomagnetite/titanomaghemite in mid-ocean ridge basalts. Earth and Planetary Science Letters, 220(1-2), 175-184
DOI: 10.1594/pangaea.825256
title: Reflectance spectroscopy and colorimetry from IODP Hole 329-U1368E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.825258
title: Thermal conductivity of IODP Hole 329-U1368E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.676701
title: Radiosonde measurements from station Payerne (2007-04)
DOI: 10.1594/pangaea.822303
title: (Table 3) d(101) spacing of silica minerals from DSDP Leg 57 Holes

description: Sediment depth is given in mbsf. Internal standard: quartz. Radiation: CuK-alpha; scan speed: 0.5°/min.; chart speed: 400 mm/hr.; the values ford(101) spacing of Opal-CT and low cristobalite are the mean of 2 measurements; error is ±0.005 but ±0.01 for the values with two decimal places.
DOI: 10.1594/pangaea.758819
title: Basic and other measurements of radiation at station Ny-Ålesund (1993-03)

description: Version 2, 2011-04-01
DOI: 10.1594/pangaea.824728
title: Reflectance spectroscopy and colorimetry from IODP Hole 324-U1347A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.824779
title: Gamma ray attenuation bulk density from IODP Hole 324-U1349A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.676959
title: Expanded measurements from Neumayer Station (1993-01)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.825984
title: Gamma ray attenuation bulk density from IODP Hole 329-U1366E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.748044
title: Hydrography on standard level calculated from water bottle samples of RV Antares from 1967 to 1968
DOI: 10.1594/pangaea.823477
title: (Table 12) Trace elements at DSDP Hole 54-424C

description: &lt; = value below detection limit; #1 = element determined in major oxides (%).
DOI: 10.1594/pangaea.823354
title: (Table 4) Geochemistry in Fe-Ti oxide at DSDP Leg 55 Holes

description: Cations, oxygen = 3 and 4.
DOI: 10.1594/pangaea.835795
title: Pollen profile CV23A, Doupe, Czech Republic

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.835797
title: Pollen profile CV4A, Horní Pole, Czech Republic

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.835798
title: Pollen profile CV6A, Stálkov, Czech Republic

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.736353
title: (Table 2) Stable carbon and oxygen isotope ratios of Neogloboquadrina pachyderma from ODP Hole 104-643A
DOI: 10.1594/pangaea.822141
title: (Table 2) Weight-loss ratio at 125°C from the results of DTA-TG at DSDP Legs 56 and 57 Holes
DOI: 10.1594/pangaea.821306
title: (Table 1) Grain-size at DSDP Leg 58 Holes
DOI: 10.1594/pangaea.821335
title: (Table 6) Geochemistry, recalculated by excluding carbonates, residual materials, water, and salts at DSDP Hole 58-442A
DOI: 10.1594/pangaea.821344
title: (Table 2) Organic carbon and nitrogen at DSDP Hole 58-443
DOI: 10.1594/pangaea.780732
title: (Table T2) Bulk rock chemistry of altered basalts from Leg 187 sites

description: Altered basalts were selected on shore for whole-rock analysis using ICP-AES and ICP-MS. Samples chosen were free of glass, veins containing secondary minerals, and any other foreign material.
DOI: 10.1594/pangaea.804475
title: Heavy mineral analyses of sediment samples from the San Francisco Bay coastal system

description: Heavy or high-specific gravity minerals make up a small but diagnostic component of sediment that is well suited for determining the provenance and distribution of sediment transported through estuarine and coastal systems worldwide. By this means, we see that surficial sand-sized sediment in the San Francisco Bay Coastal System comes primarily from the Sierra Nevada and associated terranes by way of the Sacramento and San Joaquin Rivers and is transported with little dilution through the San Francisco Bay and out the Golden Gate. Heavy minerals document a slight change from the strictly Sierran-Sacramento mineralogy at the confluence of the two rivers to a composition that includes minor amounts of chert and other Franciscan Complex components west of Carquinez Strait. Between Carquinez Strait and the San Francisco Bar, Sierran sediment is intermingled with Franciscan-modified Sierran sediment. The latter continues out the Gate and turns southward towards beaches of the San Francisco Peninsula. The Sierran sediment also fans out from the San Francisco Bar to merge with a Sierran province on the shelf in the Gulf of the Farallones. Beach-sand sized sediment from the Russian River is transported southward to Point Reyes where it spreads out to define a Franciscan sediment province on the shelf, but does not continue southward to contribute to the sediment in the Golden Gate area.
description: Sediment samples were selected from the 0.063 and 0.25-mm size fraction (or, if not enough sample was available, from the 0.25 to 0.50 mm size fraction) for heavy mineral analysis. Samples were separated in tetrabromoethane diluted to a specific gravity of 2.90; both the light and heavy (floating and sinking, respectively) grains were retrieved. The heavy grains were microsplit to about 1000 grains and mounted on glass slides. Grains were identified and counted by optical properties determined on a petrographic microscope for 42 samples. The counts were normalized as percent of total non-opaque grains and a cluster analysis was applied.
description: Supplement to: Wong, Florence L; Woodrow, Donald L; McGann, Mary L (2013): Heavy mineral analysis for assessing the provenance of sandy sediment in the San Francisco Bay Coastal System. Marine Geology, 345, 170-180
DOI: 10.1594/pangaea.824819
title: Reflectance spectroscopy and colorimetry from IODP Hole 324-U1350A

description: Geocode = Depth CSF-A (m)