cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.830932
title: Satellite-based lake surface water temperatures from Lake_Iseo, 1989-2013

description: Lake Surface Water Temperature (LSWT) has been extracted from a 3x3 pixel array at the center of the lake. See "Event(s)" for Lake/pixel co-ordinates.
DOI: 10.1594/pangaea.741438
title: Lithology of sediment core KOYCEGIZ, Köycegiz Gölü, Turkey

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.843252
title: Other measurements at 10 m from station Darwin (2010-08)

description: Version 2, 2015-02-25
DOI: 10.1594/pangaea.956259
title: Ultra-violet measurements from station Desert Rock (2021-09)
DOI: 10.1594/pangaea.808159
title: (Table S2) Molar gas ratios and stable oxygen and nitrogen gas isotopes of air entrapped in glacier ice, North America
DOI: 10.1594/pangaea.902568
title: Shoreline survey data collected at Rialto Beache, Washington State, 2019-03-18

description: Data were collected using GNSS survey methods, with a differential GPS operating in Real Time Kinematic (RTK) mode. All data were collected with an AshTech ProMark 200 RTK-DGPS system connected to the Washington State Reference Network. Horizontal positions are referenced to NAD83(2011) and the vertical data are referenced to NAVD88(Geoid09). All survey data were collected with the GNSS system mounted on a 2.05 m rover pole, held level as a transect line was traced in a cross-shore orientation on the beach.The associated text files include the horizontal (HRMS) and vertical (VRMS) root-mean-square errors estimated by the GNSS system, as well as the RTK-DGPS status reported by the GNSS system at the time each point was collected. Times are referenced to local Pacific time (either PST or PDT).Most data in these files are intended to be used to calculate beach profiles, but two other data types were collected during each survey:1) Grain size photos, the locations of which were surveyed in the field and denoted in the "Description" field. The photos are currently available by request.2) The location of the most seaward presence of large wood on the profile.These data were collected as part of a one year project intended to characterize seasonal shoreline position variability on the complex shoreline of Washington's Olympic coast. The project was jointly supported by the North Pacific Coast Marine Resources Committee, Washington Sea Grant, and Peninsula College.
DOI: 10.1594/pangaea.476045
title: Physical oceanography at CTD station AOS94/22-1

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.741628
title: Lithology of sediment core PADULE, Lago Padule, Italy

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.741631
title: Lithology of sediment core PALLUNG, Palü Lunga ob Ramosch, Switzerland

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.956269
title: Ultra-violet measurements from station Desert Rock (2021-12)
DOI: 10.1594/pangaea.741451
title: Lithology of sediment core LAGOAJO, Lago de Ajo, Spain

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.956263
title: Ultra-violet measurements from station Desert Rock (2021-10)
DOI: 10.1594/pangaea.878147
title: Earlywood width of Pinus sylvestris at site DAL
DOI: 10.1594/pangaea.956264
title: Other measurements at 10 m from station Desert Rock (2021-10)
DOI: 10.1594/pangaea.741698
title: Lithology of sediment core SALDROPO, Saldropo, Spain

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.956266
title: Ultra-violet measurements from station Desert Rock (2021-11)
DOI: 10.1594/pangaea.712500
title: Geochemistry of sediment core GeoB3718-4
DOI: 10.1594/pangaea.956267
title: Other measurements at 10 m from station Desert Rock (2021-11)
DOI: 10.1594/pangaea.741297
title: Lithology of sediment core EGR2A, Etang de la Gruère, Switzerland

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.743337
title: (Table 3) Sediment accumulation rates of the Baffin Bay
DOI: 10.1594/pangaea.895657
title: Oxygen isotopic composition of sediment core CEUTA10PC08, last 25 kyr
DOI: 10.1594/pangaea.680889
title: Meteorological synoptical observations during Meteor cruise M44

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.691467
title: Radiosonde measurements from station Lindenberg (1994-10)
DOI: 10.1594/pangaea.804213
title: (Table 1) Major elements and CIPW norms at DSDP Hole 84-567A basalts compared with an orogenic basalt from Hole 67-494A

description: The CIPW norms are calculated with 85% total iron as FeO and 15% as Fe2O3.
DOI: 10.1594/pangaea.875536
title: Observation of manganese deposits in the Kane Fractue Zone of the Mid-Atlantic Ridge

description: Seven Alvin dives (14 km total) and numerous deep-towed camera traverses using ANGUS and NOAA camera systems provide dense coverage of a 12-km2 portion of the eastern wall of the Mid-Atlantic Ridge in the TAG area (26°N lat.). These data, in conjunction with recent Soviet Mir submersible data, provide important constraints on the tectonic, magmatic, and hydrothermal history of this spreading center segment. Active hydrothermal venting occurs near the junction of the median valley floor and eastern median valley wall and appears to be tectonically controlled by the intersection of major fault zones. An east-west fault-line scarp interpreted as an accommodation zone intersects escarpments associated with 020°-trending (ridge-parallel) normal faults that bound the median valley floor. The accommodation zone permits differential extension and rotation between major crustal blocks to the north and south. On the basis of the distribution of tilted chalk beds and geochemical anomalies in sediments, this fault zone has been intermittently active for at least 5x104 yr. The accommodation zone has apparently provided a conduit of high permeability oriented at a high angle to the ridge axis. Observations and samples from areas surrounding active and inactive vent sites provide evidence for three distinct episodes for hydrothermal outflow driven by separate magmatic events. The geometry of this active system may have implications for the location of hydrothermal systems in active spreading regimes and for massive sulfide exploration in ophiolite terranes.
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: Karson, Jeffrey A; Rona, Peter A (1990): Block-tilting, transfer faults, and structural control of magmatic and hydrothermal processesin the TAG area, Mid-Atlantic Ridge 26°N. Bulletin of the Geological Society of America, 102(12), 1635-1645
DOI: 10.1594/pangaea.949197
title: Biomarker test on the springtail Folsomia candida exposed via artificial test soils in a laboratory experiment

description: In a laboratory experiment, the soil invertebrate Folsomia candida (Collembola) was exposed to CuCl2 or copper oxide nanoparticles (CuO-NP) for 6 days. The animals were exposed via artificial test soil which varied in the size (19 or 30% of total mass) or the clay type of their clay fraction (kaolin or montmorillonite). The test substances were dissolved (CuCl2) or dispersed (CuO-NP) in pure miliQ water and stirred into the dry test soils to end up with test concentrations of 1, 3, 10 and 32 mg Cu/kg and a water content of 50% of the maximum water holding capacity of the respective soils. As a control, soil with miliQ water only was tested. At the beginning of the experiment, around 220 animals at the age of 10-12 days were inserted into the test vessels containing the spiked test soil. After 6 days, all animals were extracted by floatation of the test soils with tap water. 50 and 150 animals were collected for catalase and metallothionein analysis, respectively. The endpoints survival, reproduction and dry mass per individual were referred to the average values of the negative control. All endpoints were statistically compared to the control by a linear model.
description: Funded by :Hans‐Böckler‐Stiftung within the framework of the graduate school NanoCompetence (PK041). Open Access funding enabled and organized by Projekt DEAL.
DOI: 10.1594/pangaea.956210
title: Chemical concentration of metal and rare reath elements (REE) in manganese nodules and crusts

description: Manganese nodules and crusts samples analyzed in this work were chosen to represent a range of marine environments both oceanic and epicontinental. They were analysed by atomic-absorption spectrometry and optical-emission spectrometry to display a range of chemical compositions.
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.This dataset represents the digitized Table 1, pp. 107 of the related publication.
DOI: 10.1594/pangaea.860934
title: Ultra-violet measurements from station Boulder, SURFRAD (2010-12)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-09.
DOI: 10.1594/pangaea.828687
title: Gamma ray attenuation bulk density from IODP Hole 336-U1382A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.949653
title: Average composition of metalliferous sediment layers from Nereus Deep

description: Nereus Deep is situated within the NW-SE trending median valley of the Red Sea and is divided along its length by a saddle into two parallel basins. Each basin contains a number of distinct depressions which either contain brine pools, or show evidence of having contained them in the past. Geochemical analysis of unwashed samples of sediment cores from the Deep has been undertaken for Fe, Mn, Zn, Cu, Pb, Ni, Co, Cr, Hg and Ca using atomic absorption techniques. This has confirmed the observed presence of several metalliferous layers within the sediments.
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.This dataset represents digitized Table 1, pp. 128 of the related publication.
DOI: 10.1594/pangaea.843983
title: Cenozoic high latitude marine benthic δ¹⁸O stack
DOI: 10.1594/pangaea.949199
title: Moulting test on the springtail Folsomia candida exposed via artificial test soils in a laboratory experiment

description: In a laboratory experiment, the soil invertebrate Folsomia candida (Collembola) was exposed to CuCl2 or copper oxide nanoparticles (CuO-NP) for 6 days. The animals were exposed via artificial test soil which varied in the size (19 or 30% of total mass) or the clay type of their clay fraction (kaolin or montmorillonite). The test substances were dissolved (CuCl2) or dispersed (CuO-NP) in pure miliQ water and stirred into the dry test soils to end up with test concentrations of 1, 3, 10 and 32 mg Cu/kg and a water content of 50% of the maximum water holding capacity of the respective soils. As a control, soil with miliQ water only was tested. For all soils, two tests with 5 replicates per treatment were conducted. At the beginning of the experiment, 30 animals at the age of 10-12 days were inserted into the test vessels containing the spiked test soil. After 6 days, all animals were extracted by floatation of the test soils with tap water and transferred to a Paris-plaster culture plate. After 2, 5 and 7 days, the exuviae shed by the animals were collected under a binocular and analysed for their total Cu content (not per biomass as mass of exuviae is too little to be measured) via atomic absorption spectroscopy (AAS). The number of shed exuviae per animal was calculated for each time point and statistically compared to the control by a linear mixed-effect model considering the two test runs as random factor. The Cu contents of the samples were analysed by an ordinal regression with respect to their ability to exceed the limit of detection or quantification in the AAS.
description: Funded by :Hans‐Böckler‐Stiftung within the framework of the graduate school NanoCompetence (PK041). Open Access funding enabled and organized by Projekt DEAL.
DOI: 10.1594/pangaea.844022
title: Cenozoic low latitude marine benthic δ¹⁸O stack
DOI: 10.1594/pangaea.949200
title: Reproduction test on the springtail Folsomia candida exposed via artificial test soils in a laboratory experiment

description: In a laboratory experiment, the soil invertebrate Folsomia candida (Collembola) was exposed to CuCl2 or copper oxide nanoparticles (CuO-NP) for 28 days. The animals were exposed via artificial test soil which varied in the size (19 or 30% of total mass) or the clay type of their clay fraction (kaolin or montmorillonite). The test substances were dissolved (CuCl2) or dispersed (CuO-NP) in pure miliQ water and stirred into the dry test soils to end up with test concentrations of 1, 3, 10 and 32 mg Cu/kg and a water content of 50% of the maximum water holding capacity of the respective soils. As a control, soil with miliQ water only was tested. At the beginning of the experiment, 5 animals at the age of 10-12 days were inserted into the test vessels containing the spiked test soil. After 28 days, the previously inserted adult animals and the juvenile animals produced within the last 28 days were extracted by floatation of the test soils with tap water. The water surface was photographed and the number of produced juveniles was counted manually with the computer programme ImageJ to assess the reproductive output of the animals and their survival rate. The adult animals were collected from the water surface and further analysed for dry mass and Cu body concentration. The endpoints survival, reproduction and dry mass per individual were referred to the average values of the negative control. All endpoints were statistically compared to the control by a linear model.
description: Funded by :Hans‐Böckler‐Stiftung within the framework of the graduate school NanoCompetence (PK041). Open Access funding enabled and organized by Projekt DEAL.
DOI: 10.1594/pangaea.680896
title: Meteorological synoptical observations during Meteor cruise M51

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.949663
title: Accumation rates of manganese in pelagic sediments using 130Th activity

description: For 7 pelagic sediment cores, the decrease in unsupported 130Th activity with depth in the core was used to establish the mean accumulation rate over the last 300 000 years. Because CaCO3 is a Mn-free diluent, the Mn concentration results and the sediment accumulation rate results are given on a carbonate-free basis. CaCO3 content ofcores raised from below the carbonate compensation level is taken as zero. The in situ density of water-free deep-sea cores was assumed to be 0.7 g/cm³ , this could lead in some cases to an error.
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.This dataset represents the digitized Table 1 - Part 2, pp. 144 of the related publication.
DOI: 10.1594/pangaea.834355
title: Ceilometer raw data measured at Neumayer Station (2011-01), links to files
DOI: 10.1594/pangaea.872761
title: Basic measurements of radiation at station Boulder, SURFRAD (2014-09)
DOI: 10.1594/pangaea.762230
title: Counts and mass of different fish species from beam trawl samples in the Eastfrisian Wadden Sea during POLARIS cruise PO0206

description: Depth, water was calculated as mean from bathymetric depths at start/end of trawl
DOI: 10.1594/pangaea.825332
title: Radiosonde measurements from station Nauru Island (2003-04)

description: Version 4, 2014-01-06. Launches at irregular time intervals.
DOI: 10.1594/pangaea.497343
title: Physical oceanography from BT during cruise N90XXB_1986
DOI: 10.1594/pangaea.721185
title: Ultra-violet measurements from station Fort Peck (2005-10)

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.735287
title: Other measurements at 30 m from station Payerne (2009-01)
DOI: 10.1594/pangaea.733157
title: Physical oceanography during Kaimalino cruise HOT-14 on section PRS2
DOI: 10.1594/pangaea.828228
title: Spatially explicit estimates of stock size, structure and biomass of North Atlantic albacore tuna (Thunnus alalunga) in the North Atlantic for the period 1967-1986, compiled from statistics about ICCAT fishery region L4

description: The development of the ecosystem approach and models for the management of ocean marine resources requires easy access to standard validated datasets of historical catch data for the main exploited species. They are used to measure the impact of biomass removal by fisheries and to evaluate the models skills, while the use of standard dataset facilitates models inter-comparison. North Atlantic albacore tuna is exploited all year round by longline and in summer and autumn by surface fisheries and fishery statistics compiled by the International Commission for the Conservation of Atlantic Tunas (ICCAT). Catch and effort with geographical coordinates at monthly spatial resolution of 1° or 5° squares were extracted for this species with a careful definition of fisheries and data screening. In total, thirteen fisheries were defined for the period 1956-2010, with fishing gears longline, troll, mid-water trawl and bait fishing. However, the spatialized catch effort data available in ICCAT database represent a fraction of the entire total catch. Length frequencies of catch were also extracted according to the definition of fisheries above for the period 1956-2010 with a quarterly temporal resolution and spatial resolutions varying from 1°x 1° to 10°x 20°. The resolution used to measure the fish also varies with size-bins of 1, 2 or 5 cm (Fork Length). The screening of data allowed detecting inconsistencies with a relatively large number of samples larger than 150 cm while all studies on the growth of albacore suggest that fish rarely grow up over 130 cm. Therefore, a threshold value of 130 cm has been arbitrarily fixed and all length frequency data above this value removed from the original data set.
description: This work was funded in part by the European project EURO-BASIN, funded by Framework Programme 7 (Contract 264933). Special thanks to ICCAT for the access to its public fishing database and Carlos Palma (ICCAT) and Alain Fonteneau (IRD) for their helpful advice on these data.
DOI: 10.1594/pangaea.904459
title: Table SM-20: IODP Site 321-U1338 XRF data

description: NMS refers to normalized median scaled data, which is not calibrated. Calibrated data are listed as wt%.
DOI: 10.1594/pangaea.825604
title: Magnetic remanence from IODP Hole 329-U1371F

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.855817
title: Basic and other measurements of radiation at station Alert (2014-04)
DOI: 10.1594/pangaea.854078
title: Basic measurements of radiation at station Boulder (2015-09)
DOI: 10.1594/pangaea.782620
title: (Appendix 2) Contents, coefficients of roundness and flatness and their variations of rock fragments in 5-10 mm size fraction from shelf bottom sediments of the Sea of Okhotsk
DOI: 10.1594/pangaea.855818
title: Radiosonde measurements from station Alert (2014-04)

description: Start location: Alert, Nunavut, CA; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.875535
title: Seismic locations, geochemical variations, attenuation anomalies, geomorphological structures for the 1983-84 unrest at Campi Flegrei caldera

description: Despite their importance for eruption forecasting the causes of seismic rupture processes during caldera unrest are still poorly reconstructed from seismic images. Seismic source locations and waveform attenuation analyses of earthquakes in Campi Flegrei area (Southern Italy) during the 1982-1984 unrest have revealed a 4-4.5 km deep NW-SE striking aseismic zone of high attenuation offshore Pozzuoli. The lateral features and principal axis of the attenuation anomaly correspond to the main source of ground uplift during the unrest. The seismic swarms correlate in space and time with fluid injections from a deep hot source, inferred to represent geochemical and temperature variations at Solfatara. These injections struck a high-attenuation 3-4 km deep reservoir of supercritical fluids/foams under Pozzuoli and migrated towards a shallower aseismic deformation source under Solfatara. The reservoir became aseismic for two months just after the main seismic swarm (April 1, 1984) due to a SE-to-NW directed input from the high-attenuation domain, likely a dyke emplacement. The unrest ended after fluids migrated from Pozzuoli to the location of the last caldera eruption (Mt. Nuovo, 1538 AD). The results show that a single source controls the largest monitored seismic, deformation, and geochemical unrest at the caldera.
description: The dataset proposed here is the result of this interdisciplinary study. Inside the zipped folder a readme.txt file explains the meaning of each observation.
description: Supplement to: De Siena, Luca; Chiodini, Giovanni; Vilardo, Giuseppe; Del Pezzo, Edoardo; Castellano, Mario; Colombelli, Simona; Tisato, Nicola; Ventura, Guido (2017): Source and dynamics of a volcanic caldera unrest: Campi Flegrei, 1983–84. Scientific Reports, 7(1)