cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.723929
title: Other measurements at 10 m from station Southern Great Plains (1994-05), Version 1

description: Please refer to Version 2 (see replaced by reference) for an updated version.
DOI: 10.1594/pangaea.690274
title: Radiosonde M6_R022 during METEOR cruise M6 on 1966-08-18 23:14h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.722104
title: Ultra-violet measurements from station Goodwin Creek (2008-11)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.890380
title: Age determination of Ennadai_core1 peat core
DOI: 10.1594/pangaea.825400
title: Radiosonde measurements from station Nauru Island (2007-01)

description: Version 2, 2014-01-06. Launches at irregular time intervals.
DOI: 10.1594/pangaea.675094
title: Radiosonde measurements from station Sede Boqer (2005-12)

description: Wind speed was multiplied by a factor of 0.1 (2009-08-28). Start location: Bet-Dagan, Israel; Distance from radiation site: 120 km
DOI: 10.1594/pangaea.856814
title: (Table 1) Bulk geochemistry of sediment cores KH-79-3_L3 and KH-79-3_C3

description: The organic and isotopic geochemical study of two sediment cores (KH-79-3, L-3, and KH-79-3, C-3) from the Oki Ridge in the Japan Sea has revealed that total organic carbon (TOC) mass accumulation rates are extremely high in the 12-11 ka (calendar age) interval and TOC in the sections in the 24-17 ka interval is depleted in 13C by 3.5 per mil relative to Holocene sediments. Alkenone sea surface temperature (SST) shows a decrease from 18° to 14°C from 17.5 to 11.6 ka and a sharp increase from 14° to 19°C from 11.6 to 11.1 ka. The SST changes are associated with the inflow of cold seawater with the vertical water mixing and the inflowof warm Tsushima Current into the Japan Sea. The d13C values for both 24-methylcholesta-5,22-dien-3?-ol (diatom marker) and dinosterol (dinoflagellate marker), are at their minimum from 24 to 17 ka, while those for long-chain alkenones are not. The theoretical considerations on d13C for biomarkers suggest low photosynthetic carbon demand of diatoms and dinoflagellates from 24 to 17 ka.
description: Supplement to: Ishiwatari, Ryoshi; Yamada, Keita; Houtatsu, M; Naraoka, Hiroshi (1999): Organic molecular and carbon isotopic records of the Japan Sea over the past 30 kyr. Paleoceanography, 14(2), 260-270
DOI: 10.1594/pangaea.690340
title: Radiosonde M9_R017 during METEOR cruise M9 on 1967-04-24 10:00h

description: Height of tropause 12380 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.690341
title: Radiosonde M9_R018 during METEOR cruise M9 on 1967-04-24 15:59h

description: Height of tropause 12660 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.890391
title: Age determination of T1_core1 peat core
DOI: 10.1594/pangaea.912781
title: (Supplement 5) Aerosol backscatter coefficient (at 532 nm) measurements in the Atlantic of the 1991 Mt Pinatubo aerosol cloud from Professor Zubov
DOI: 10.1594/pangaea.820244
title: (Table 1) Thermal conductivity at DSDP Site 60-452
DOI: 10.1594/pangaea.926776
title: Trait measurements of Sphagnum moss from northern peatlands
DOI: 10.1594/pangaea.707190
title: Radiosonde measurements from station Sede Boqer (2007-09)

description: Wind speed was multiplied by a factor of 0.1 (2009-08-28). Start location: Bet-Dagan, Israel; Distance from radiation site: 120 km
DOI: 10.1594/pangaea.926779
title: Vascular trait measurements from northern peatlands
DOI: 10.15468/dl.pp7vec
title: Occurrence Download

description: A dataset containing 81 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is one of (China, Chinese Taipei)",
 "TaxonKey is Magnolia lotungensis Chun & C.H.Tsoong"
 ]
}

 The dataset includes 81 records from 11 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031405-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.690343
title: Radiosonde M9_R020 during METEOR cruise M9 on 1967-04-25 16:00h

description: Height of tropause 11530 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.855338
title: (Table 4b) Oxygen and carbon isotopic values of planktonic and benthic foraminifera of sediment core Ulleung_C26
DOI: 10.1594/pangaea.855386
title: European lobsters (Homarus gammarus) captured around the rocky island of Helgoland (German Bight, North Sea) in 2006
DOI: 10.1594/pangaea.690344
title: Radiosonde M9_R021 during METEOR cruise M9 on 1967-04-25 21:56h

description: Height of tropause 11540 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.722038
title: Ultra-violet measurements from station Goodwin Creek (2007-01)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.890533
title: Geochemistry of KAM12-C4_core1 peat core
DOI: 10.1594/pangaea.855387
title: European lobsters (Homarus gammarus) captured around the rocky island of Helgoland (German Bight, North Sea) in 2007
DOI: 10.1594/pangaea.707114
title: (Table 4) Rare earth element contents in basalts from DSDP Hole 65-483B
DOI: 10.1594/pangaea.901686
title: Other measurements at 10 m from station Sioux Falls (2018-02)
DOI: 10.1594/pangaea.761273
title: Tab. 4: The measured above-ground annual production of vascular plants in the recognized vegetation types
DOI: 10.1594/pangaea.856785
title: (Plate 3) Manganese nodules and deep-sea sediment core from Pacific Ocean

description: A synoptic review of the studies of well-known occurrences of palagonite tuffs is presented. Included are palagonite tuffs from Iceland, and pillow-lava palagonite complexes from Columbia River basalts and from the central Oregon coast. Additional petrologic and x-ray defraction data for selected samples are presented. Petrologic evidence shows that basaltic glass of aqueous tuffs and breccias consists of sideromelane, which is susceptible to palagonitization. It is shown that palagonitization is a selective alteration process, involving hydration, oxidation and zeolitization. Some of the manganese nodules dredged from the Pacific Ocean floor contain nucleus of palagonite-tuff breccias or of zeolite. A brief megascopic and microscopic description of nodules from the south Pacific, the Mendocino ridge and the 'Horizon' Nodule from the north Pacific is presented. Petrographic studies of palagonite-tuff breccias of manganese nodules and other palagonites suggest that migration and segregation of metallic elements occur during and subsequent to palagonitization. During the palagonitization of sideromelane, nearly 30 percent of sea water is absorbed. The hydration of sideromelane is also accompanied by oxidation of iron and other elements. These oxides may be released either in colloidal form or in true solution and tend to precipitate first from the unstable palagonite.
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: Nayudu, Y Rammohanroy (1964): Palagonite tuffs (hyaloclastites) and the products of post-eruptive processes. Bulletin of Volcanology, 27(1), 391-410
DOI: 10.1594/pangaea.762293
title: Counts and mass of different fish species from beam trawl samples in the Eastfrisian Wadden Sea during POLARIS cruise PO0894

description: Depth, water was calculated as mean from bathymetric depths at start/end of trawl
DOI: 10.1594/pangaea.707273
title: (Appendix A) Rock magnetic results with indication of the diagenetic setting of ODP Site 204-1251

description: Sulphate zone &lt;3 mbsf, sulphate-methane transition 3-6 mbsf, bottom simulating reflector 193 mbsf
DOI: 10.1594/pangaea.854956
title: Table 1. Pressure, temperature and isotope ratios between H2O and CO2 for all experiments

description: Traditionally, the application of stable isotopes in Carbon Capture and Storage (CCS) projects has focused on d13C values of CO2 to trace the migration of injected CO2 in the subsurface. More recently the use of d18O values of both CO2 and reservoir fluids has been proposed as a method for quantifying in situ CO2 reservoir saturations due to O isotope exchange between CO2 and H2O and subsequent changes in d18OH2O values in the presence of high concentrations of CO2. To verify that O isotope exchange between CO2 and H2O reaches equilibrium within days, and that d18OH2O values indeed change predictably due to the presence of CO2, a laboratory study was conducted during which the isotope composition of H2O, CO2, and dissolved inorganic C (DIC) was determined at representative reservoir conditions (50°C and up to 19 MPa) and varying CO2 pressures. Conditions typical for the Pembina Cardium CO2 Monitoring Pilot in Alberta (Canada) were chosen for the experiments. Results obtained showed that d18O values of CO2 were on average 36.4±2.2 per mil (1 sigma, n=15) higher than those of water at all pressures up to and including reservoir pressure (19 MPa), in excellent agreement with the theoretically predicted isotope enrichment factor of 35.5 per mil for the experimental temperatures of 50°C. By using 18O enriched water for the experiments it was demonstrated that changes in the d18O values of water were predictably related to the fraction of O in the system sourced from CO2 in excellent agreement with theoretical predictions. Since the fraction of O sourced from CO2 is related to the total volumetric saturation of CO2 and water as a fraction of the total volume of the system, it is concluded that changes in d18O values of reservoir fluids can be used to calculate reservoir saturations of CO2 in CCS settings given that the d18O values of CO2 and water are sufficiently distinct.
description: Supplement to: Johnson, Gareth; Mayer, Bernhard (2011): Oxygen isotope exchange between H2O and CO2 at elevated CO2 pressures: Implications for monitoring of geological CO2 storage. Applied Geochemistry, 26(7), 1184-1191
DOI: 10.1594/pangaea.695468
title: Monthly production of frozen marine products, Chile, 1998
DOI: 10.1594/pangaea.761274
title: Tab. 5+6: The percentage of muskox feeding observations per vegetation type
DOI: 10.1594/pangaea.761997
title: (Table 4) Grain size composition of bottom sediments from the West Bay of the Furugelm Island, Sea of Japan
DOI: 10.1594/pangaea.827307
title: Core summary for IODP Hole 329-U1368D
DOI: 10.1594/pangaea.760695
title: (Appendix A) Direction of characteristic magnetization of ODP Hole 122-761B

description: The NRM column represents the initial NRM intensity of each sample, the demagnetization step column refers to the highest step attained during the treatment of each sample.
DOI: 10.1594/pangaea.760697
title: (Appendix A) Directions of characteristic magnetization of Triassic sediments in ODP Hole 122-759B

description: The NRM column represents the initial NRM intensity of each sample, the demagnetization step column refers to the highest step attained during the treatment of each sample.
DOI: 10.1594/pangaea.890217
title: Age determination of NW-BG_core10 peat core
DOI: 10.1594/pangaea.723927
title: Other measurements at 10 m from station Southern Great Plains (1994-04), Version 1

description: Please refer to Version 2 (see replaced by reference) for an updated version.
DOI: 10.1594/pangaea.707319
title: (Appendix A1) Magnetic hysteresis parameters for samples collected across polarity excursions at ODP Site 152-919

description: Sediment depth (m) is composite depth (mcd) after St. John et al. (2004, doi:10.1016/j.margeo.2004.09.004)
DOI: 10.1594/pangaea.854560
title: Glacier mass balance Vernagtferner, Taschachjoch area, Austria, 1977/1978
DOI: 10.1594/pangaea.713195
title: Smear slide analysis of sediment core GeoB6311-1
DOI: 10.1594/pangaea.718756
title: Other measurements at 10 m from station Sioux Falls (2007-02)
DOI: 10.1594/pangaea.900677
title: Other measurements at 10 m from station Goodwin Creek (2019-01)
DOI: 10.1594/pangaea.684677
title: Ciliate abundance and biomass in water samples collected at Station MARCH-1997-GN36199704603MNB07 in the Aegean Sea

description: Ciliate cell sizes were measured and converted into cell volumes using appropriate geometric formulae (Peuto-Moreau, 1991). For biomass estimation the conversion factor 140 fgC µm^-3 was used (Putt and Stoecker, 1989).Borax-buffered formalin (final concentration 2% formaldehyde). Samples for ciliate counting were stored at 4°C in the dark until observation. For ciliate identification and enumeration 100 ml samples were left for 24 h in sedimentation cylinders and then observed under an inverted epifluorescence microscope.
DOI: 10.1594/pangaea.854561
title: Glacier mass balance Vernagtferner, Taschachjoch area, Austria, 1978/1979
DOI: 10.1594/pangaea.854610
title: Glacier mass balance Vernagtferner, Austria, 1986/1987
DOI: 10.1594/pangaea.692275
title: Ciliate abundance and biomass in water samples collected at Station SEPT-1997-GN36199704605MSB03 in the Aegean Sea

description: Borax-buffered formalin (final concentration 2% formaldehyde). Samples for ciliate counting were stored at 4°C in the dark until observation. For ciliate identification and enumeration, 100 ml samples were left for 24 h in sedimentation cylinders and then observed under an inverted epifluorescence microscope. Ciliate cell sizes were measured and converted into cell volumes using appropriate geometric formulae of Peuto-Moreau (Peuto-Moreau M., 1991. Symbiose plastidiale et mixotrophie des cilies planctoniques marins Oligotrichina (Ciliophora). These de Doctorat d' etat, Universite de Nice-Sophia Antipolis). For biomass estimation the conversion factor 140 fgC µm^-3 was used (Putt M., Stoecker D.K., 1989. An experimentally determined carbon: volume ratio for marine oligotrichous ciliates from estuarine and coastal waters. Limnology and Oceanography 34, 1097-1103).
DOI: 10.1594/pangaea.854613
title: Glacier mass balance Vernagtferner, Austria, 1989/1990
DOI: 10.1594/pangaea.820072
title: (Table 1) Chronostratigraphy, depth, carbonate and organic carbon, bitumen composition and OEP at DSDP Leg 60 Holes
DOI: 10.1594/pangaea.918568
title: Basic measurements of radiation at station Sapporo (2020-03)
DOI: 10.1594/pangaea.824453
title: Core summary for IODP Hole 318-U1358B
DOI: 10.1594/pangaea.854503
title: Glacier mass balance Vernagtferner, Brochkogel area, Austria, 2002/2003
DOI: 10.1594/pangaea.723943
title: Other measurements at 10 m from station Southern Great Plains (1994-12), Version 1

description: Please refer to Version 2 (see replaced by reference) for an updated version.
DOI: 10.1594/pangaea.718422
title: Other measurements at 10 m from station Boulder, SURFRAD (1998-11)

description: Version 2, 2009-06-12
DOI: 10.1594/pangaea.902541
title: Other measurements at 10 m from station Payerne (2019-04)
DOI: 10.1594/pangaea.723949
title: Other measurements at 10 m from station Southern Great Plains (1995-03), Version 1

description: Please refer to Version 2 (see Replaced by reference)
DOI: 10.1594/pangaea.828804
title: Core summary for IODP Hole 339-U1386C
DOI: 10.1594/pangaea.735849
title: Ozone measurements from station Lindenberg (1995-07)
DOI: 10.1594/pangaea.819983
title: (Table 1) Minerals of bulk and fine-grained (2 µm) samples from DSDP Hole 60-453

description: Sediment depth is given in mbsf. &lt;1 = trace. Carbonate, clinoptilolite, phillipsite, wairakite, opal-CT, Fe-Mg chlorite, attapulgite and serpentine also looked for but not found.
DOI: 10.1594/pangaea.829126
title: Gas measurements from IODP Hole 340-U1394A

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.854504
title: Glacier mass balance Vernagtferner, Brochkogel area, Austria, 2003/2004
DOI: 10.1594/pangaea.919857
title: Stand-alone soil temperature sensor (Hobo 4) measurements between August 2018 to August 2019 at a boreal forest site in the region of Lena-Viluy in Eastern Siberia

description: For the definition of quality flags see README files ("Further details" reference)
DOI: 10.1594/pangaea.692276
title: Ciliate abundance and biomass in water samples collected at Station SEPT-1997-GN36199704605MSB04 in the Aegean Sea

description: Borax-buffered formalin (final concentration 2% formaldehyde). Samples for ciliate counting were stored at 4°C in the dark until observation. For ciliate identification and enumeration, 100 ml samples were left for 24 h in sedimentation cylinders and then observed under an inverted epifluorescence microscope. Ciliate cell sizes were measured and converted into cell volumes using appropriate geometric formulae of Peuto-Moreau (Peuto-Moreau M., 1991. Symbiose plastidiale et mixotrophie des cilies planctoniques marins Oligotrichina (Ciliophora). These de Doctorat d' etat, Universite de Nice-Sophia Antipolis). For biomass estimation the conversion factor 140 fgC µm^-3 was used (Putt M., Stoecker D.K., 1989. An experimentally determined carbon: volume ratio for marine oligotrichous ciliates from estuarine and coastal waters. Limnology and Oceanography 34, 1097-1103).
DOI: 10.1594/pangaea.854505
title: Glacier mass balance Vernagtferner, Brochkogel area, Austria, 2004/2005
DOI: 10.1594/pangaea.854506
title: Glacier mass balance Vernagtferner, Brochkogel area, Austria, 2005/2006
DOI: 10.1594/pangaea.854498
title: Glacier mass balance Vernagtferner, Brochkogel area, Austria, 1997/1998
DOI: 10.1594/pangaea.898847
title: Other measurements at 10 m from station Boulder, SURFRAD (2018-06)
DOI: 10.1594/pangaea.816357
title: (Appendix) Age-depth relation and red colour reflectance of ODP Site 177-1093

description: Sediment depth is given in mcd.
DOI: 10.1594/pangaea.854499
title: Glacier mass balance Vernagtferner, Brochkogel area, Austria, 1998/1999
DOI: 10.1594/pangaea.922966
title: Cation substitutions in LPEE pedogenic siderites
DOI: 10.1594/pangaea.548986
title: Nutrients measured on water bottle samples at station Chan_2003-08-09_10, Chanavallita, Chile
DOI: 10.1594/pangaea.692280
title: Ciliate abundance and biomass in water samples collected at Station SEPT-1997-GN36199704606MNB02 in the Aegean Sea

description: Borax-buffered formalin (final concentration 2% formaldehyde). Samples for ciliate counting were stored at 4°C in the dark until observation. For ciliate identification and enumeration, 100 ml samples were left for 24 h in sedimentation cylinders and then observed under an inverted epifluorescence microscope. Ciliate cell sizes were measured and converted into cell volumes using appropriate geometric formulae of Peuto-Moreau (Peuto-Moreau M., 1991. Symbiose plastidiale et mixotrophie des cilies planctoniques marins Oligotrichina (Ciliophora). These de Doctorat d' etat, Universite de Nice-Sophia Antipolis). For biomass estimation the conversion factor 140 fgC µm^-3 was used (Putt M., Stoecker D.K., 1989. An experimentally determined carbon: volume ratio for marine oligotrichous ciliates from estuarine and coastal waters. Limnology and Oceanography 34, 1097-1103).
DOI: 10.1594/pangaea.752079
title: Meteorological observations during SEAHORSE cruise from York Factory to Gravesend started at 1790-10-11
DOI: 10.1594/pangaea.706559
title: Basic measurements of radiation at station Carpentras (2005-01)
DOI: 10.1594/pangaea.706562
title: Basic measurements of radiation at station Carpentras (2005-04)

description: Version 2, 2008-11-21
DOI: 10.1594/pangaea.854500
title: Glacier mass balance Vernagtferner, Brochkogel area, Austria, 1999/2000
DOI: 10.1594/pangaea.854501
title: Glacier mass balance Vernagtferner, Brochkogel area, Austria, 2000/2001
DOI: 10.1594/pangaea.692282
title: Ciliate abundance and biomass in water samples collected at Station SEPT-1997-GN36199704606MNB04 in the Aegean Sea

description: Borax-buffered formalin (final concentration 2% formaldehyde). Samples for ciliate counting were stored at 4°C in the dark until observation. For ciliate identification and enumeration, 100 ml samples were left for 24 h in sedimentation cylinders and then observed under an inverted epifluorescence microscope. Ciliate cell sizes were measured and converted into cell volumes using appropriate geometric formulae of Peuto-Moreau (Peuto-Moreau M., 1991. Symbiose plastidiale et mixotrophie des cilies planctoniques marins Oligotrichina (Ciliophora). These de Doctorat d' etat, Universite de Nice-Sophia Antipolis). For biomass estimation the conversion factor 140 fgC µm^-3 was used (Putt M., Stoecker D.K., 1989. An experimentally determined carbon: volume ratio for marine oligotrichous ciliates from estuarine and coastal waters. Limnology and Oceanography 34, 1097-1103).
DOI: 10.1594/pangaea.692284
title: Ciliate abundance and biomass in water samples collected at Station SEPT-1997-GN36199704606MNB06 in the Aegean Sea

description: Borax-buffered formalin (final concentration 2% formaldehyde). Samples for ciliate counting were stored at 4°C in the dark until observation. For ciliate identification and enumeration, 100 ml samples were left for 24 h in sedimentation cylinders and then observed under an inverted epifluorescence microscope. Ciliate cell sizes were measured and converted into cell volumes using appropriate geometric formulae of Peuto-Moreau (Peuto-Moreau M., 1991. Symbiose plastidiale et mixotrophie des cilies planctoniques marins Oligotrichina (Ciliophora). These de Doctorat d' etat, Universite de Nice-Sophia Antipolis). For biomass estimation the conversion factor 140 fgC µm^-3 was used (Putt M., Stoecker D.K., 1989. An experimentally determined carbon: volume ratio for marine oligotrichous ciliates from estuarine and coastal waters. Limnology and Oceanography 34, 1097-1103).
DOI: 10.1594/pangaea.692638
title: Photosynthetic primary production in the euphotic zone of the Cretan Sea at Station SEPTEMBER-1995-D2

description: Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger phytoplankton cells (&gt;5 µm) were preserved in alkaline Lugol solution. Utermoehl, H., 1958. Zur Vervollkommung der quantitativen Phytoplankton-Methodik. Mitt. Int. Ver. Theor. Angew. Limnol., 9:1-38.
DOI: 10.1594/pangaea.816358
title: (Appendix) Age-depth relation and red colour reflectance of ODP Site 177-1094

description: Sediment depth is given in mcd.
DOI: 10.1594/pangaea.696000
title: Ozone measurements from station South Pole (2005-07)
DOI: 10.1594/pangaea.899092
title: Other measurements at 10 m from station Desert Rock (2017-09)