cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.867498
title: Nitrate and ammonium concentration of compost, biochar-amended composts, soil and biochar-amended soil during repeated extractions

description: Repeated extractions of nitrate and ammonium were performed on compost (Con), biochar-amended composts (CB1, CB2, CB3), soil and biochar-amended soil. Data presents the amount of N released during each step of extraction from each replicate of each treatment.
description: Supplement to: Hagemann, Nikolas; Kammann, Claudia I; Schmidt, Hans-Peter; Kappler, Andreas; Behrens, Sebastian (2017): Nitrate capture and slow release in biochar amended compost and soil. PLoS ONE, 12(2), e0171214
DOI: 10.1594/pangaea.867519
title: Daily rainfall data at Danby in the Esk catchment, UK (2007-10)
DOI: 10.1594/pangaea.867521
title: River discharge and suspended sediment concentrations measured at Grosmont on the River Esk, UK (2007-09)
DOI: 10.1594/pangaea.868338
title: Basic and other measurements of radiation at station Tiksi (2014-02)

description: New version (2016-11-11), data recalculated with corrected calibration coefficients
DOI: 10.1594/pangaea.868343
title: Basic and other measurements of radiation at station Tiksi (2014-06)

description: New version (2016-11-11), data recalculated with corrected calibration coefficients
DOI: 10.1594/pangaea.868347
title: Basic and other measurements of radiation at station Tiksi (2014-10)

description: New version (2016-11-11), data recalculated with corrected calibration coefficients
DOI: 10.1594/pangaea.867379
title: (Table 2, 134-135) Point electron microprobe analyses of mineralisations inside micronodules in the brown clay sampled by core NR71 from the NIXO 30 expedition by R/V Le Noroit in the Clarion-Clipperton Zone (CCZ) in the Pacific Ocean

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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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.867518
title: Annotated record of the detailed examination of Mn deposits from DSDP Site 49, Leg 6 (Cores 49A-1, 49-1)

description: At Sites 47 and 48, impenetrable and cherty Upper Cretaceous chalks were found. The upper part of what infer to be lower Cretaceous is even more reflective, and likely to be very cherty (and was found to be cherty in the Vema core). It became clear that basement could only be reached where the Upper Cretaceous and the upper part of the lower Cretaceous are absent. However, west of Site 48, the R/V Argo record showed an area in which the Upper Cretaceous has wedged out down dip, and the Lower Cretaceous is thinning out by loss of the strongly reflective beds at the top. This area appeared to offer the best chance for sampling the lowermost transparent layer. Two holes were drilled: Hole 49.0 and Hole 49.1 after Hole 49.0 stopped at 18 m. Beds near the base of sedimentary sequence revealed by the seismic profiles are found to be of early Cretaceous (Neocomian) or latest Jurassic (Tithonian) age, and of pelagic facies. The crust under the Shatsky Rise is latest Jurassic or older.
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: Heezen, Bruce C; Fischer, A G; Boyce, Robert E; Bukry, David; Douglas, Robert G; Garrison, Robert E; Kling, S A; Krasheninnikov, Valery A; Lisitzin, Alexander P; Pimm, Anthony C (1971): Site 49. In: Fischer, A.G.; et al., Initial Reports of the Deep Sea Drilling Project, 6, Initial Reports of the Deep Sea Drilling Project, 6, U.S. Government Printing Office, VI, 171-194
DOI: 10.1594/pangaea.868936
title: Holocene-length alkenone-based summer temperature record from sediment core HAP0212
DOI: 10.1594/pangaea.868060
title: Meteorological synoptical observations from station Fukuoka (2016-09)
DOI: 10.1594/pangaea.868070
title: Radiosonde measurements from station Sapporo (2016-09)
DOI: 10.1594/pangaea.868764
title: Mineralogy of sediment core COR0503-CL04-36
DOI: 10.1594/pangaea.868953
title: Colour reflectance of sediment core COR0503-CL04-36
DOI: 10.1594/pangaea.868071
title: Other measurements at 10 m from station Desert Rock (2013-04)
DOI: 10.1594/pangaea.867923
title: Annotated record of the detailed examination of Mn deposits from R/V Vema Cruise 18 in the Manihiki Plaeau area, Pacific Ocean

description: The Manihiki Plateau, a 600,000 km2 smooth and nearly flat-topped feature, lies in the west equatorial Pacific. Danger, Nassau, Suvorov and Manihiki Islands rise from the southern part of the plateau. Oceanic depths of about 5500 m surround the 2400-3000 m summit area. The top of the plateau is capped by approximately one kilometer of sediment. The sediment cores to the east and west of the plateau contain red clay but the top of the plateau is covered with foraminiferal ooze. Mineral grains and rock fragments in cores and dredge hauls from the east escarpment indicate that basic igneous rocks underlie a ridge that forms the eastern edge of the plateau north of 13°S. Bottom photographs and dredge hauls below 3000 m on the east scarp of the plateau and in the abyssal hills to the east reveal abundant manganese nodules. Most of the botton photographs show evidence of deep-sea currents. The plateau's shape is apparently controlled by faulting although much evidence of basic vulcanism is present in the cores. The occurrence of Cretaceous fossils on the eastern ridge of the plateau indicates that the bevelling of the plateau must have occurred during or before Cretaceous time. Twenty cores, two dredge hauls, four bottom trawls and fifteen camera stations from the Vema cruise 18.
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: Heezen, Bruce C; Glass, Bill; Menard, H William (1966): The Manihiki Plateau. Deep Sea Research and Oceanographic Abstracts, 13(3), 445-458
DOI: 10.1594/pangaea.868074
title: (Table 1-2 and 3, page 282-284) 10Be, U, Th, 226Ra and 210Pb analyses for layers inside ferromanganese crusts of the Pacific Ocean (ARIES-12D and ARIES-15D)

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.869005
title: Other measurements at 10 m from station Fort Peck (2013-02)
DOI: 10.1594/pangaea.869013
title: Ultra-violet measurements from station Fort Peck (2013-05)

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.869019
title: Ultra-violet measurements from station Fort Peck (2013-07)

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.869023
title: Other measurements at 10 m from station Fort Peck (2013-08)
DOI: 10.1594/pangaea.869031
title: Ultra-violet measurements from station Fort Peck (2013-11)

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.867971
title: Basic and other measurements of radiation at station Tiksi (2011-06)

description: New version (2016-11-10), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.868665
title: Dust-stack 2009 of combined sediment record ELSA

description: The last glacial cycle in Central Europe is dominated by processes of aeolian dust transport and accumulation. These dust deposits are preserved in soils and lake sediments and provide detailed information about the climate variability during cold and dry periods. Especially the transitions from warm into cold periods are characterized by turbulent climate conditions. The main problems of terrestrial paleoclimate reconstructions are the completeness of the core material and a sampling resolution. To detect single dust storms we use a particle detection method, which allows high resolution, sub-annual analyses of sediment structures in undisturbed samples. The ELSA (Eifel Laminated Sediment Archive) stack is a compilation of four different lake sediment cores of the Eifel region (Western Germany) and comprise the period of the last 133 ka. The results of our analyses show high frequencies of dust storm events during the first cold events C24 and C23 after the last warm stage. In opposition, the coldest periods of the last glacial cycle OIS-4 (70-60 ka BP) and OIS-2 (35-14 ka BP) are characterized by stable climate conditions that provide the accumulation of homogenous dust sediments.
description: Sediment core combination: HL2 (Hoher List Lat.: 50.16526, Long.:6.83639, elevation: 402.5, recovery: 104 m, Gauß-Krüger coordinate system: 2559752/5558994) + OW1 (Oberwinkler Maar Lat.: 50.14263, Long.: 6.93954, elevation: 385, recovery: 49.00 m, Gauß-Krüger coordinate system: 2567153/5556565) + DE3 (Dehner Maar Lat.: 50.2944, Long.: 6.50699, elevation: 565, recovery 87 m, Gauß-Krüger coordinate system: 2536122/5573145) + SM3 (Schalkenmehrener Maar Lat.: 50.17115, Long.: 6.85921, elevation 420 m, recovery: 12 m, Gauß-Krüger coordinate system: 2561375/5559668).
description: Supplement to: Seelos, Klemens; Sirocko, Frank; Dietrich, Stephan (2009): A continuous high-resolution dust record for the reconstruction of wind systems in central Europe (Eifel, Western Germany) over the past 133 ka. Geophysical Research Letters, 36(20)
DOI: 10.1594/pangaea.867972
title: Basic and other measurements of radiation at station Tiksi (2011-07)

description: New version (2016-11-10), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.867819
title: Ultra-violet measurements from station Desert Rock (2013-04)

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.867974
title: Basic and other measurements of radiation at station Tiksi (2011-09)

description: New version (2016-11-10), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.868085
title: Basic and other measurements of radiation at station Tiksi (2013-10)

description: New version (2016-11-11), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.867878
title: Basic and other measurements of radiation at station Tiksi (2015-02)
DOI: 10.1594/pangaea.867886
title: Basic and other measurements of radiation at station Tiksi (2015-10)
DOI: 10.1594/pangaea.867957
title: Basic measurements of radiation at station Tiksi (2010-07)

description: New version (2016-11-10), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.867959
title: Basic measurements of radiation at station Tiksi (2010-09)

description: New version (2016-11-10), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.867960
title: Basic measurements of radiation at station Tiksi (2010-10)

description: New version (2016-11-10), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.869421
title: Video observations on predator and prey of gonatid squid in Monterey Bay from 1995-2015
DOI: 10.1594/pangaea.869935
title: Physical oceanography from Seaglider mission CNCY201614913

description: The aim of CNCY201614913 mission presented here (part of the CRELEV-2016 experiment) was to focus on the transport and convection processes occurring in the area of the Eastern Mediterranean Sea. These processes are important for the nutrients injection in the surface waters, the consequent phytoplankton growth and fisheries. The main objective of the CRELEV-2016 cruise was to examine a comprehensive set of parameters in the Eastern Mediterranean Sea in order to quantify variability and trends of physical and biogeochemical properties. These data will be used to better understand the role of natural and anthropogenic pressures. The data were collected with glider SG-149, after being launched from Paphos on 23 March, 2016, and recovered by the R/V Aegaeo near Crete on 6 June 2016. Parameters measured include pressure, temperature, conductivity, dissolved oxygen, optical backscatter at 470 nm, 700 nm, and optical fluorescence at 695 nm at depths up to 1000 m.
description: Find data with quality flags in source datasets in NetCDF format.
DOI: 10.1594/pangaea.869008
title: Other measurements at 10 m from station Fort Peck (2013-03)
DOI: 10.1594/pangaea.869010
title: Ultra-violet measurements from station Fort Peck (2013-04)

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.869020
title: Other measurements at 10 m from station Fort Peck (2013-07)
DOI: 10.1594/pangaea.869516
title: Other measurements at 10 m from station Goodwin Creek (2013-08)
DOI: 10.1594/pangaea.869526
title: Ultra-violet measurements from station Toravere (2016-11)

description: 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 2017-01-17. UVB is measured with Kipp&Zonen CUVB1 narrowband radiometer (bandwidth 306 ± 0.1 nm)
DOI: 10.1594/pangaea.869167
title: Meteorological synoptical observations from station Fukuoka (2016-10)
DOI: 10.1594/pangaea.869171
title: Radiosonde measurements from station Ishigakijima (2016-10)
DOI: 10.1594/pangaea.869174
title: Radiosonde measurements from station Minamitorishima (2016-10)
DOI: 10.1594/pangaea.869210
title: Ozone measurements from station Lindenberg (2008-01)
DOI: 10.1594/pangaea.869213
title: Meteorological synoptical observations from station Lindenberg (2008-02)
DOI: 10.1594/pangaea.869109
title: Basic measurements of radiation at station Camborne (2016-11)
DOI: 10.1594/pangaea.869182
title: Basic measurements of radiation at station Lerwick (2016-11)
DOI: 10.1594/pangaea.869519
title: Basic measurements of radiation at station Cener (2016-06)
DOI: 10.1594/pangaea.869520
title: Basic measurements of radiation at station Cener (2016-07)
DOI: 10.1594/pangaea.869043
title: Documentation of sediment core GIK18375-2
DOI: 10.1594/pangaea.869051
title: Documentation of sediment core GIK18387-2
DOI: 10.1594/pangaea.869055
title: Documentation of sediment core GIK18394-2
DOI: 10.1594/pangaea.869060
title: Documentation of sediment core GIK18399-2
DOI: 10.1594/pangaea.869068
title: Documentation of sediment core GIK18409-3
DOI: 10.1594/pangaea.869071
title: Documentation of sediment core GIK18416-2
DOI: 10.1594/pangaea.869076
title: Documentation of sediment core GIK18422-3
DOI: 10.1594/pangaea.869082
title: Documentation of sediment core GIK18429-2
DOI: 10.1594/pangaea.869529
title: Other measurements at 10 m from station Goodwin Creek (2013-09)
DOI: 10.1594/pangaea.869581
title: Other measurements at 10 m from station Rock Springs (2013-02)
DOI: 10.1594/pangaea.869589
title: Ultra-violet measurements from station Rock Springs (2013-05)

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.869604
title: Ultra-violet measurements from station Rock Springs (2013-10)

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 2017-02-03.
DOI: 10.1594/pangaea.869610
title: Ultra-violet measurements from station Rock Springs (2013-12)

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 2017-02-03.
DOI: 10.1594/pangaea.869200
title: Comparison of Mediterranean pteropod shell biometrics and ultrastructure
DOI: 10.1594/pangaea.869215
title: Ozone measurements from station Lindenberg (2008-02)
DOI: 10.1594/pangaea.869447
title: Ultra-violet measurements from station Carpentras (2016-08)

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 2017-02-09.
DOI: 10.1594/pangaea.869521
title: Basic measurements of radiation at station Cener (2016-08)
DOI: 10.1594/pangaea.869524
title: Basic measurements of radiation at station Cener (2016-11)
DOI: 10.1594/pangaea.869465
title: Challenges in modelling isoprene and monoterpene emission dynamics of arctic plants

description: The Arctic is warming at twice the global average speed, and the warming-induced increases in biogenic volatile organic compounds (BVOCs) emissions from Arctic plants are expected to be drastic. The current global models' estimations of minimal BVOC emissions from the Arctic are based on very few observations and have been challenged increasingly by field data. This study applied a dynamic ecosystem model, LPJ-GUESS, as a platform to investigate short-term and long-term BVOC emission responses to Arctic climate warming. Field observations in a subarctic tundra heath with long-term (13-year) warming treatments were extensively used for parameterizing and evaluating BVOC-related processes (photosynthesis, emission responses to temperature and vegetation composition). We propose an adjusted temperature (T) response curve for Arctic plants with much stronger T sensitivity than the commonly used algorithms for large-scale modelling. The simulated emission responses to 2 °C warming between the adjusted and original T response curves were evaluated against the observed warming responses (WRs) at short-term scales. Moreover, the model responses to warming by 4 and 8 °C were also investigated as a sensitivity test. The model showed reasonable agreement to the observed vegetation CO2 fluxes in the main growing season as well as day-to-day variability of isoprene and monoterpene emissions. The observed relatively high WRs were better captured by the adjusted T response curve than by the common one. During 1999?2012, the modelled annual mean isoprene and monoterpene emissions were 20 and 8 mg C/m**2/yr with an increase by 55 and 57 % for 2 °C summertime warming, respectively. Warming by 4 and 8 °C for the same period further elevated isoprene emission for all years, but the impacts on monoterpene emissions levelled off during the last few years.
description: Supplement to: Tang, Jing; Schurgers, Guy; Valolahti, Hanna; Faubert, Patrick; Tiiva, Päivi; Michelsen, Anders; Rinnan, Riikka (2016): Challenges in modelling isoprene and monoterpene emission dynamics of arctic plants: a case study from a subarctic tundra heath. Biogeosciences, 13, 6651-6667
DOI: 10.1594/pangaea.871280
title: Melt-layer content of the Akademii Nauk ice core (AD 1883-1998)
DOI: 10.1594/pangaea.869222
title: Radiosonde measurements from station Lindenberg (2008-03)
DOI: 10.1594/pangaea.869219
title: Magnetic susceptibility of sediment cores from the Bay of Plenty, New Zealand
DOI: 10.1594/pangaea.869711
title: Other measurements at 10 m from station Sioux Falls (2013-09)
DOI: 10.1594/pangaea.869503
title: Ultra-violet measurements from station Goodwin Creek (2013-04)

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.840719
title: IRD during marine isotope stage 5 of sediment core MD99-2303
DOI: 10.1594/pangaea.869504
title: Other measurements at 10 m from station Goodwin Creek (2013-04)
DOI: 10.1594/pangaea.868759
title: Grain size measurements of sediment core COR0503-CL05-37
DOI: 10.1594/pangaea.868762
title: Geochemistry of sediment core COR0503-CL05-37
DOI: 10.1594/pangaea.869112
title: Radiosonde measurements from station Tamanrasset (2016-11)

description: Start location: Tamanrasset; Distance from radiation site: 10 km
DOI: 10.1594/pangaea.869532
title: Other measurements at 10 m from station Goodwin Creek (2013-10)
DOI: 10.1594/pangaea.868765
title: Mineralogy of sediment core COR0503-CL05-37
DOI: 10.1594/pangaea.869173
title: Meteorological synoptical observations from station Minamitorishima (2016-10)
DOI: 10.1594/pangaea.865416
title: Amazon watershed stream model derived from 1-arcsecond SRTM
DOI: 10.1594/pangaea.869176
title: Meteorological synoptical observations from station Sapporo (2016-10)
DOI: 10.1594/pangaea.869522
title: Basic measurements of radiation at station Cener (2016-09)
DOI: 10.1594/pangaea.869892
title: Meteorological synoptical observations from station Tateno (2016-10)
DOI: 10.1594/pangaea.869893
title: Radiosonde measurements from station Tateno (2016-10)
DOI: 10.1594/pangaea.869229
title: Radiosonde measurements from station Lindenberg (2008-04)
DOI: 10.1594/pangaea.869250
title: Meteorological synoptical observations from station Lindenberg (2008-06)
DOI: 10.1594/pangaea.869170
title: Meteorological synoptical observations from station Ishigakijima (2016-10)
DOI: 10.1594/pangaea.869177
title: Radiosonde measurements from station Sapporo (2016-10)
DOI: 10.1594/pangaea.869208
title: Meteorological synoptical observations from station Lindenberg (2008-01)
DOI: 10.1594/pangaea.870502
title: Ultra-violet measurements from station Carpentras (2016-10)

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.870594
title: Meteorological synoptical observations from station Fukuoka (2016-11)
DOI: 10.1594/pangaea.870598
title: Radiosonde measurements from station Ishigakijima (2016-11)
DOI: 10.1594/pangaea.870603
title: Meteorological synoptical observations from station Sapporo (2016-11)