cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.875334
title: Snow height on sea ice and sea ice drift from autonomous measurements from buoy 2015S35, deployed during POLARSTERN cruise PS94 (ARK-XXIX/3)

description: Snow height was measured by the Snow Depth Buoy 2015S35, an autonomous platform, drifting on Arctic sea ice, deployed during POLARSTERN cruise PS94 (ARK-XXIX/3). The resulting time series describes the evolution of snow depth as a function of place and time between 10 Sep 2015 and 11 Feb 2016 in sample intervals of 1 hour. The Snow Depth Buoy consists of four independent sonar measurements representing the area (approx. 10 m**2) around the buoy. The buoy was installed on first year ice. In addition to snow depth, geographic position (GPS), barometric pressure, air temperature, and an internal ice temperature were measured. Negative values of snow height occur if surface ablation continues into the sea ice. Thus, these measurements describe the position of the sea ice surface relative to the original snow-ice interface. Differences between single sensors indicate small-scale variability of the snow pack around the buoy. The data set has been processed, including the removal of obvious inconsistencies (missing values). Records without any snow depth may still be used for sea ice drift analyses.
DOI: 10.1594/pangaea.899712
title: Basic measurements of radiation at station Palaiseau (2018-10)
DOI: 10.15468/dl.m8tf9p
title: Occurrence Download

description: A dataset containing 47 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Magnolia sinica (Y.W.Law) Noot."
 ]
}

 The dataset includes 47 records from 8 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031407-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.707075
title: (Figure 2) Pollen analysis of sediment core from the Monticchio maar
DOI: 10.1594/pangaea.875292
title: Snow height on sea ice and sea ice drift from autonomous measurements from buoy 2017S47, deployed during POLARSTERN cruise PS103 (ANT-XXXII/2)

description: Snow height was measured by the Snow Depth Buoy 2017S47, an autonomous platform, drifting on Antarctic sea ice, during POLARSTERN cruise PS103 (ANT-XXXII/2). The resulting time series describes the evolution of snow depth as a function of place and time between 10 Jan 2017 and 11 Jan 2017 in sample intervals of 1 hour. The Snow Depth Buoy consists of four independent sonar measurements representing the area (approx. 10 m**2) around the buoy. The buoy was installed on first year ice. In addition to snow depth, geographic position (GPS), barometric pressure, air temperature, and an internal ice temperature were measured. Negative values of snow depth occur if surface ablation continues into the sea ice. Thus, these measurements describe the position of the sea ice surface relative to the original snow-ice interface. Differences between single sensors indicate small-scale variability of the snow pack around the buoy. The data set has been processed, including the removal of obvious inconsistencies (missing values). Records without any snow depth may still be used for sea ice drift analyses.
DOI: 10.1594/pangaea.718487
title: Other measurements at 10 m from station Boulder, SURFRAD (2000-03)

description: Version 2, 2009-06-12
DOI: 10.1594/pangaea.849358
title: Basic measurements of radiation at station Sapporo (2015-07)
DOI: 10.1594/pangaea.718530
title: Radiosonde measurements from station Boulder, SURFRAD (2001-02)

description: Start location: Denver, CO; Distance from radiation site: 40 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown; Version 2, 2009-06-12
DOI: 10.1594/pangaea.857273
title: Radiosonde measurements from station Tamanrasset (2015-10)

description: Start location: Tamanrasset; Distance from radiation site: 10 km
DOI: 10.1594/pangaea.707703
title: Radiosonde measurements from station Payerne (2007-08)

description: Location: Arosa, Switzerland; Distance from radiation site: 200 km
DOI: 10.1594/pangaea.774959
title: Continuous meteorological observations at Neumayer station (1998-09)
DOI: 10.1594/pangaea.875282
title: Sea ice drift, surface temperature, and barometric pressure from autonomous measurements from buoy 2015P6, deployed during POLARSTERN cruise PS89 (ANT-XXX/2)

description: Sea ice drift, surface temperature, and barometric pressure were measured by Surface Velocity Profiler 2015P6 drifting on Antarctic sea ice. The buoy was deployed on first year ice without drogue during POLARSTERN cruise PS89 (ANT-XXX/2). The time series describes the position and additional parameters of the buoy between 17 Jan 2015 and 01 Sep 2016 in sample intervals of 1 hour. The data set has been processed, including the removal of obvious inconsistencies (missing values).
DOI: 10.1594/pangaea.774963
title: Continuous meteorological observations at Neumayer station (1999-01)
DOI: 10.1594/pangaea.841524
title: Radiosonde measurements from station Momote (2010-03)

description: Version 2, 2015-01-14; Launches at irregular time intervals
DOI: 10.1594/pangaea.887808
title: Snow height on sea ice and sea ice drift from autonomous measurements from buoy 2016S36, deployed during POLARSTERN cruise PS101 (ARK-XXX/3)

description: Snow height was measured by the Snow Depth Buoy 2016S36, an autonomous platform, drifting on Arctic sea ice, deployed during POLARSTERN cruise ARK-XXX/3 (PS101). The resulting time series describes the evolution of snow depth as a function of place and time between 15 Sep 2016 and 25 Aug 2017 in sample intervals of 1 hour. The Snow Depth Buoy consists of four independent sonar measurements representing the area (approx. 10 m**2) around the buoy. The buoy was installed on second year ice. In addition to snow depth, geographic position (GPS), barometric pressure, air temperature, and an internal ice temperature were measured. Negative values of snow height occur if surface ablation continues into the sea ice. Thus, these measurements describe the position of the sea ice surface relative to the original snow-ice interface. Differences between single sensors indicate small-scale variability of the snow pack around the buoy. The data set has been processed, including the removal of obvious inconsistencies (missing values). Records without any snow depth may still be used for sea ice drift analyses.
DOI: 10.1594/pangaea.899783
title: Element analyses of clinopyroxenes (electron microprobe) in rock samples from the northern Semail ophiolite (Oman)
DOI: 10.1594/pangaea.841856
title: Radiosonde measurements from station Darwin (2002-07)

description: Version 3, 2015-01-26. Launches at irregular time intervals
DOI: 10.1594/pangaea.870356
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2010/11_19
DOI: 10.1594/pangaea.758462
title: (Table 4) Distribution of radiolaria in Miocene sediments of DSDP Hole 6-55

description: Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent.
DOI: 10.1594/pangaea.673251
title: Basic and other measurements of radiation at station Toravere (2001-01)

description: Please note, that SWD, DIR, DIF and SWU nighttime negatives are set manually to zero (until end of August 2018).
DOI: 10.1594/pangaea.874708
title: Bulk organic isotope geochemistry of sediment core EM_MC
DOI: 10.1594/pangaea.885315
title: Basic and other measurements of radiation at station Barrow (2001-05)

description: Version 2, (2018-01-20), with corrected Short-wave downward (GLOBAL) radiation values.
DOI: 10.1594/pangaea.751085
title: Meteorological observations during PANTER cruise from St. Eustacius to Bonaire started at 1829-01-14
DOI: 10.1594/pangaea.883663
title: Chemical composition of manganese nodules from the Southern Ocean

description: Samples have been air dried and reduced to powder. The analysis is done on the whole content and not on the sole HCL soluble part as in most analyses from other authors.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.722176
title: Ultra-violet measurements from station Goodwin Creek (1996-06)

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.849354
title: Meteorological synoptical observations from station Minamitorishima (2015-07)
DOI: 10.1594/pangaea.887810
title: Snow height on sea ice and sea ice drift from autonomous measurements from buoy 2016S38, deployed during POLARSTERN cruise PS96 (ANT-XXXI/2)

description: Snow height was measured by the Snow Depth Buoy 2016S38, an autonomous platform, drifting on Antarctic sea ice, during POLARSTERN cruise ANT-XXXI/2 (PS96). The resulting time series describes the evolution of snow depth as a function of place and time between 15 Jan 2016 and 08 May 2017 in sample intervals of 1 hour. The Snow Depth Buoy consists of four independent sonar measurements representing the area (approx. 10 m**2) around the buoy. The buoy was installed on multi year ice. In addition to snow depth, geographic position (GPS), barometric pressure, air temperature, and an internal ice temperature were measured. Negative values of snow depth occur if surface ablation continues into the sea ice. Thus, these measurements describe the position of the sea ice surface relative to the original snow-ice interface. Differences between single sensors indicate small-scale variability of the snow pack around the buoy. The data set has been processed, including the removal of obvious inconsistencies (missing values). Records without any snow depth may still be used for sea ice drift analyses.
DOI: 10.1594/pangaea.857319
title: (Fig. 3a) Stable oxygen isotope ratios of benthic foraminifera of sediment core NEAP-18K
DOI: 10.1594/pangaea.905044
title: Eemian iron isotopes from Black Sea sediment cores taken at station 22 during Meteor cruise M72/5
DOI: 10.1594/pangaea.751141
title: Meteorological observations during PENELOPE cruise from Delgada Bay to Halifax started at 1809-07-20
DOI: 10.1594/pangaea.904877
title: Globorotalia crassaformis abundance of core GL-75 from southeastern Brazilian Margin
DOI: 10.1594/pangaea.922549
title: AMS radiocarbon dating of lake sediment cores 14-OM-12A, 14-OM-02B and 14-OM-20B from Omoloy region, north-eastern Siberia
DOI: 10.1594/pangaea.872255
title: Links to master tracks in different resolutions from POLAR 5 flight CryoVEx_ANT_2010_03
DOI: 10.1594/pangaea.724139
title: Other measurements at 10 m from station Southern Great Plains (2003-07)

description: Version 2, 2009-07-07
DOI: 10.1594/pangaea.751165
title: Meteorological observations during PERSEVERENCE cruise from Acheen Head to St. Helena started at 1807-07-13
DOI: 10.1594/pangaea.874538
title: Meteorological synoptical observations from Neumayer Station (2016-07)
DOI: 10.1594/pangaea.763229
title: (Table 3) Abundance of zooplankton near the ice edge in the Pechora Sea
DOI: 10.1594/pangaea.737483
title: (Table 2.2.1.3) Individual length of sympagic meiofauna in sections of sea-ice core IO-5

description: sea-ice core diameter 9 cm; DEPTH ice/snow represents the middle of the ice-core section measured from ice surface; length gives the median of individuals in each ice-core section
DOI: 10.1594/pangaea.845327
title: Homogenized radiosonde record at station Ny-Ålesund, Spitsbergen in 2003

description: Radiosonde data homogenization by Markus Kayser
DOI: 10.1594/pangaea.908883
title: Expanded measurements from station Lindenberg (2017-12)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.751225
title: Meteorological observations during PLANCIUS cruise from Nederland to Batavia started at 1846-03-11
DOI: 10.1594/pangaea.719439
title: Radiosonde measurements from station Bondville (2000-03)

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.753354
title: (Table 5) Radiolarians in ODP Hole 113-690B

description: Species abundances: A = abundant (&gt;50 % of total assemblage), C = common (15-50 %) F = few (3-15 %), R = rare (1-3 %), T = trace (&lt;1 %).
DOI: 10.1594/pangaea.755772
title: (Appendix) Calcium carbonate concentrations of ODP Site 115-710

description: Cores 115-710A-3H,115710A-4H, 115-710B-4H and 115-710B-5H
DOI: 10.1594/pangaea.718440
title: Ultra-violet measurements from station Boulder, SURFRAD (1999-04)

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.870369
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2010/11_32
DOI: 10.1594/pangaea.509422
title: Reflectance of sediment core MD97-2108
DOI: 10.1594/pangaea.848043
title: Radiosonde measurements from station Kwajalein (2012-09)
DOI: 10.1594/pangaea.884388
title: Basic and other measurements of radiation at station Barrow (1998-06)

description: Version 2, (2017-12-21), with corrected Short-wave downward (GLOBAL) radiation values.
DOI: 10.1594/pangaea.722203
title: Ultra-violet measurements from station Goodwin Creek (1997-03)

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.737484
title: (Table 2.2.1.3) Individual length of sympagic meiofauna in sections of sea-ice core IO-6

description: sea-ice core diameter 9 cm; DEPTH ice/snow represents the middle of the ice-core section measured from ice surface; length gives the median of individuals in each ice-core section
DOI: 10.1594/pangaea.675405
title: Radiosonde measurements from station Payerne (1999-12)
DOI: 10.1594/pangaea.751092
title: Meteorological observations during PANTER cruise from Curaçao to Curaçao started at 1830-03-07
DOI: 10.1594/pangaea.855015
title: Trace metal composition of the aerosol at Neumayer Station, Antarctica during the year 2005

description: Aerosol was continuously sampled by sucking ambient air with a flow rate of 120 m**3/h through Whatman 541 filters (diameter 240 mm) using a ventilated electropolished stainless steel inlet stack (total height about 8 m above the snow surface) with a 50% aerodynamic cut-off diameter around 7-10 µm. Trace element analysis was performed by means of inductively coupled plasma - quadrupol mass spectrometry (ICP-QMS, ELAN 6000, Sciex/Perkin Elmer) equipped with a cross-flow nebulizer as sample introduction system. For trace element analyses we chose a total digestion of the samples with a pressurized digestion system (DAS 100, Picotrace) at 200°C in a mixture containing HNO3 (suprapure, 65%, Merck, sub-boiling bi-distilled), HF (suprapure, 40%, Merck, sub-boiling bi-distilled) and H2O2 (suprapure, 30%, Merck). With this device a series of 24 samples could be digested in parallel. Each series included one filter blank and a certified reference sample (NIST 1648 urban particulate matter). For calibration we used commercially available standard solutions (104 ppb multi-element verification standard 1 and 2, Perkin Elmer) which were generally applied in 1 ppb, 10 ppb, and 100 ppb concentrations (1 ppb corresponds to 1 ng of each element in 1 g solute). Each sample was spiked by 10 ppb Rh as internal standard to normalize the signal intensities and compensate instrumental sensitivity variations. We conservatively estimated the method detection limits (MDL) as three times the standard deviation (std) of the overall blank values. Values below the MDL are given as "&lt; respecting MDL value" (e.g.: &lt;0.02) in the table. Concentrations not determined are marked with empty cells. The combined uncertainty of the analyses is approximately between ±8% and ±12% for element concentrations above three times the corresponding MDL. It increased from around ±(15-20)% approaching 3xMDL level to roughly (+50/-100)% close to the MDL. The final atmospheric concentrations (in ng/m**3 = 10**(-9) g/m**3, or pg/m**3 = 10**(-12) g/m**3) were calculated from the blank corrected element amounts and the corrected sampled air volume to standard conditions (273.16 K and 1013 hPa).
DOI: 10.1594/pangaea.673496
title: Radiosonde measurements from station Bermuda (1995-04)

description: Start location: Bermuda; Distance from radiation site: 2 km
DOI: 10.1594/pangaea.753358
title: (Table 2) Definition and depth of stratigraphic datum points of ODP Hole 113-689B
DOI: 10.1594/pangaea.695476
title: Basic and other measurements of radiation at station Barrow (2005-07), Version 1

description: Ellsworth G. Dutton discovered a calibration glitch in the SWD "Short-wave downward (GLOBAL) radiation" data for Barrow, Alaska. SWD data was therefore removed from this dataset. Please refer to the updated Version 2 (see replaced by reference) with correct calibration.
DOI: 10.1594/pangaea.751370
title: Meteorological observations during Princess Augusta cruise started at 1763-12-20
DOI: 10.1594/pangaea.760900
title: (Table 4) Contents and isotopic composition of sulfur compounds in bottom sediments from the area of the Spitsbergen (Svalbard) Archipelago
DOI: 10.1594/pangaea.853739
title: Radiosonde measurements from station Izaña (2015-09)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.753359
title: (Table 3) Definition and depth of stratigraphic datum points of ODP Hole 113-690B
DOI: 10.1594/pangaea.905714
title: Snow height on sea ice and sea ice drift from autonomous measurements from buoy 2018S59, deployed during POLARSTERN cruise PS111

description: Snow height was measured by the Snow Depth Buoy 2018S59, an autonomous platform, drifting on Antarctic sea ice, deployed during POLARSTERN cruise PS111. The resulting time series describes the evolution of snow depth as a function of place and time between 11 February 2018 and 25 April 2019 in sample intervals of 1 hour. The Snow Depth Buoy consists of four independent sonar measurements representing the area (approx. 10 m**2) around the buoy. The buoy was installed on multi year ice. In addition to snow depth, geographic position (GPS), barometric pressure, air temperature, and an internal ice temperature were measured. Negative values of snow height occur if surface ablation continues into the sea ice. Thus, these measurements describe the position of the sea ice surface relative to the original snow-ice interface. Differences between single sensors indicate small-scale variability of the snow pack around the buoy. The data set has been processed, including the removal of obvious inconsistencies (missing values). Records without any snow depth may still be used for sea ice drift analyses.
DOI: 10.1594/pangaea.887821
title: Sea ice drift, surface temperature, and barometric pressure from autonomous measurements from buoy 2016P20, deployed during POLARSTERN cruise PS96 (ANT-XXXI/2)

description: Sea ice drift, surface temperature, and barometric pressure were measured by Surface Velocity Profiler 2016P20 drifting on Antarctic sea ice. The buoy was deployed on multi year ice without drogue during POLARSTERN cruise ANT-XXXI/2 (PS96). The time series describes the position and additional parameters of the buoy between 18 Jan 2016 and 09 Jul 2017 in sample intervals of 1 hour. The data set has been processed, including the removal of obvious inconsistencies (missing values).
DOI: 10.1594/pangaea.897904
title: Ultra-violet measurements from station Toravere (2018-12)
DOI: 10.1594/pangaea.711412
title: Basic measurements of radiation at station Regina (2005-02)
DOI: 10.1594/pangaea.898455
title: Radiosonde measurements from station Bondville (2018-03)

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.719386
title: Ultra-violet measurements from station Bondville (1999-02)

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.899100
title: Other measurements at 10 m from station Desert Rock (2018-05)
DOI: 10.1594/pangaea.849211
title: (Table 3, 4, and 5 - page 458, 460, 470) Optical spectrographic analyses of samples from AMPHITRITE

description: It is stressed that the main difference between quiet and hyaloclastic activity is that in the former the interaction between hot lava and seawater during the eruption is minimal, whereas it is very extensive in the latter. This strong interaction is the cause of the processes which accompany hyaloclastic eruptions, processes which, in their turn, influence the chemistry and mineralogy of wide areas of the Pacific Ocean floor. Admittedly they are not well known yet, but their extensive study seems worthwhile. Two suggestions based on data presented here may be pointed out : 1) Deep-sea basaltic rocks showing breccia and/or ash-like features must not necessarily have erupted under shallow water or above sea level, as is commonly believed. 2) The "altered" or "fresh" appearance of submarine basalts is not necessarily to be ascribed to the relative age or youth of the rock. In fact extensive "alteration" of submarine lavas may commonly take place rapidly at high temperature during the eruption, rather than gradually after emplacement as is generally the case in subaerial formations. Deep-sea waters of the Pacific normally have a pH close to 7 and a rather constant low temperature, close to 0°C. Alteration of igneous minerals after emplacement under such conditions must be exceedingly slow, and concepts of "weathering" as learned in surface geology cannot be applied.
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: Bonatti, Enrico (1967): Mechanisms of deep-sea volcanism in the South Pacific. In: Abelson, P (Ed.) Researches in Geochemistry, Wiley, New York, 2, 453-491
DOI: 10.1594/pangaea.922837
title: Five seismite clusters of sediment core SG-1b
DOI: 10.1594/pangaea.792936
title: Continuous meteorological observations at station Ny-Ålesund (2011-05)
DOI: 10.1594/pangaea.711810
title: Basic measurements of radiation at station Carpentras (2007-04)