cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.884874
title: Ichthyoplankton composition from SUESTE cruise 3, Southern Brazilian Shelf, in 1984

description: The Departamento de Hidrografia e Navegação (DHN) from the Brazilian Navy in partnership with the Centro de Biologia Marinha (CEM) of the Federal University of Paraná (UFPR) conducted four seasonal cruises covering the coastal, neritic and oceanic regions between 24º06'S and 29º36'S to evaluate the general oceanographic processes present in the region (Brandini, 1990a; 1990b). Each cruise had twelve transects perpendicular to the coastline that were surveyed onboard NOc. Almirante Saldanha resulting in approximately 90 oceanographic stations spaced 30 nautical miles (~ 55 km) apart (Brandini, 1990b). Samples were obtained in the shallow stations (depth &lt;50 m) through horizontal and vertical trawls with a 0.5 m mouth diameter, 250 μm mesh plankton net. Oblique hauls using 0.6 m mouth diameter, 300 μm mesh plankton net were conducted mainly at intermediate depths (&gt; 50 m and &lt;200 m) from 5 m from the bottom to the surface, and from 200 m depth in the deep stations. At selected intermediate and deep stations, stratified vertical hauls with a 0.5 m mouth diameter, 250 μm mesh plankton net were also performed. The net type used has not been determined, except for the use of a Chossi Kid Net in some stations of the 2nd cruise. Volume of filtered water for each trawl is not available and number of eggs and larvae were not standardized (Macedo-Soares, 2015).
DOI: 10.1594/pangaea.891116
title: Meteorological synoptical observations from station Tateno (2018-02)
DOI: 10.1594/pangaea.891119
title: Meteorological synoptical observations from station Tateno (2018-03)
DOI: 10.1594/pangaea.891120
title: Radiosonde measurements from station Tateno (2018-03)
DOI: 10.1594/pangaea.891080
title: Radiosonde measurements from station Southern Great Plains (2016-11)

description: Launches at irregular time intervals. The radiosonde measurements from station Southern Great Plains are used for Billings and E13
DOI: 10.1594/pangaea.891083
title: Basic measurements of radiation at station Billings (2016-12)
DOI: 10.15468/dl.ybehfm
title: Occurrence Download

description: A dataset containing 2040509 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON((46.87903 29.40862,50.94507 23.87381,53.7332 23.23485,55.74685 24.8966,57.21837 26.88221,57.1022 27.53654,53.61703 27.15818,51.25486 29.81263,49.16376 30.88198,46.87903 29.40862))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 2040509 records from 386 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031474-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.891085
title: Basic measurements of radiation at station Billings (2017-01)
DOI: 10.1594/pangaea.891087
title: Basic measurements of radiation at station Billings (2017-03)
DOI: 10.1594/pangaea.891088
title: Basic measurements of radiation at station Billings (2017-04)
DOI: 10.1594/pangaea.891089
title: Basic measurements of radiation at station Billings (2017-05)
DOI: 10.1594/pangaea.874291
title: Pressure and temperature from the borehole observatory of IODP Hole 332-C0010A

description: An Mw 6.0 earthquake struck ~50 km offshore the Kii Peninsula of southwest Honshu, Japan on 1 April 2016. This earthquake occurred directly beneath a cabled offshore monitoring network at the Nankai Trough subduction zone and within 25-35 km of two borehole observatories installed as part of the International Ocean Discovery Program's NanTroSEIZE project. The earthquake's location close to the seafloor and subseafloor network offers a unique opportunity to evaluate dense seafloor geodetic and seismological data in the near field of a moderate-sized offshore earthquake. We use the offshore seismic network to locate the main shock and aftershocks, seafloor pressure sensors, and borehole observatory data to determine the detailed distribution of seafloor and subseafloor deformation, and seafloor pressure observations to model the resulting tsunami. Contractional strain estimated from formation pore pressure records in the borehole observatories (equivalent to 0.37 to 0.15 µstrain) provides a key to narrowing the possible range of fault plane solutions. Together, these data show that the rupture occurred on a landward dipping thrust fault at 9-10 km below the seafloor, most likely on the plate interface. Pore pressure changes recorded in one of the observatories also provide evidence for significant afterslip for at least a few days following the main shock. The earthquake and its aftershocks are located within the coseismic slip region of the 1944 Tonankai earthquake (Mw ~8.0), and immediately downdip of swarms of very low frequency earthquakes in this region, illustrating the complex distribution of megathrust slip behavior at a dominantly locked seismogenic zone.
description: Supplement to: Wallace, L M; Araki, Eiichiro; Saffer, Demian M; Wang, Xiaoming; Roesner, Alexander; Kopf, Achim J; Nakanishi, A; Power, William L; Kobayashi, R; Kinoshita, Chihiro; Toczko, Sean; Kimura, Toshinori; Machida, Shiki; Carr, Stephanie A (2016): Near-field observations of an offshore Mw 6.0 earthquake from an integrated seafloor and subseafloor monitoring network at the Nankai Trough, southwest Japan. Journal of Geophysical Research: Solid Earth, 121(11), 8338-8351
DOI: 10.1594/pangaea.891103
title: Ichthyoplankton composition from MCT-II cruise, Southern Brazilian Shelf, in 2010-2011

description: The MCT-II series is the field component of the project "A Dinâmica das Frentes da Plataforma e Talude Superior no Sul e Sudeste do Brasil e sua Influência nos Fluxos de Carbono entre Oceano e Atmosfera (CO2 SSE)". The cruise was composed of two legs: the first, from December 6 to 22, 2010 between Chuí and Rio de Janeiro; and, the second from January 4 to 11, 2011 between Cabo de São Tomé and Cabo Frio (Ito et al., 2016). A total of 17 transects perpendicular to the coast were carried out on board the Research Vessel (NHo.) Cruzeiro do Sul from the Brazilian Navy (Departamento de Hidrografia e Navegação, DHN) totaling 112 oceanographic stations (Macedo-Soares et al., 2014).Ichthyoplankton samples were obtained through integrated vertical trawls conducted at the stern of the ship, at a speed of approximately 1 m s-1 (2 knots), from the depth of the fluorescence maxima to the surface at deep stations, between the surface and 10 m from the bottom in shallow water stations (up to 20 m) or 10 m above the bottom in stations where the water column was homogeneous (Macedo-Soares et al., 2014). The trawls were made with a conical-cylindrical net (WP-2) with 0.5 m of mouth diameter, 200 μm of mesh opening, equipped with a flowmeter to determine the volume of filtered water in each trawl. The samples were fixed and preserved in formaldehyde solution, buffered with sodium tetraborate, diluted in sea water with a final approximate concentration of 4%. The filtered volume was calculated and used to standardize the abundance of fish eggs and larvae per 100 m3 of filtered water (Macedo-Soares et al., 2014).CORRECTION applied on 2020-07-17: Station MCT-II_74 on 2011-01-06T21:50 the water temperatures were corrected from 53.0°C to 26.6 °C and the salinity was corrected from 73.3 to 36.5.
DOI: 10.1594/pangaea.891135
title: Magnetic volume susceptibility of sediment core GeoB18516-2
DOI: 10.1594/pangaea.891143
title: Ice-rafted detritus counts of sediment core GeoB18514-2
DOI: 10.1594/pangaea.891155
title: Basic measurements of radiation at station Billings (2015-03)

description: SWD values have been removed because it has been found that an incorrect global calibration value had been used. There will be a new version of this dataset (linked to this dataset) once this issue has been solved.
DOI: 10.1594/pangaea.891156
title: Basic measurements of radiation at station Billings (2015-04)

description: SWD values have been removed because it has been found that an incorrect global calibration value had been used. There will be a new version of this dataset (linked to this dataset) once this issue has been solved.
DOI: 10.1594/pangaea.691487
title: Radiolarian abundance of sediment core Y8

description: A high-resolution record of radiolarian faunal changes from Site Y8 south of the Subtropical Front (STF), offshore eastern New Zealand, provides insight into the paleoceanographic history of the last 265 kyrs. Quantitative analysis of radiolarian paleotemperature indicators and radiolarian-based sea surface temperature (SST) estimates reveal distinct shifts during glacial-interglacial (G-I) climate cycles encompassing marine isotope stages (MIS) 8-1. Faunas at Site Y8 are abundant and diverse and consist of a mixture of species typical of the subantarctic, transitional and subtropical zones which is characteristic of subantarctic waters just south of the STF. During interglacials, diverse radiolarian faunas have increased numbers of warm-water taxa (not, vert, similar 15%) while cool-water taxa decrease to not, vert, similar 11% of the assemblage. Warmest climate conditions occurred during MIS 5.5 and the early Holocene Climatic Optimum (HCO) at the onset of MIS 1 where SSTs reach maxima of 12.8 and 12.9 °C, respectively. This suggests that temperatures during the HCO were comparable to the Eemian, one of the warmest interglacial intervals of the Late Quaternary. Glacials are characterized by less diverse radiolarian faunas with cool-water taxa increasing to 49% of the assemblage. Coolest climate conditions occurred in MIS 4 and 2 where SSTs are reduced to 5.4 °C and 4.3 °C, respectively. Radiolarian faunal changes and SST estimates clearly identify major water masses and oceanic fronts in the offshore eastern New Zealand area. During warmest MIS 5.5 and early MIS 1 substantial influence of northern-sourced Subtropical Surface Water (STW) is evident at Site Y8. This implies southward incursions of STW around the eastern crest of Chatham Rise with the STF displaced towards higher latitudes and spinning off eddies as far south as Campbell Plateau. Additionally, increased flow of the Southland Current (SC) might have enhanced the local occurrence of warm-water radiolarians derived from the subtropical Tasman Sea. Coolest glacials are marked by a strong inflow of cool, southern-sourced waters at Site Y8 indicating a more vigorous flow along the Subantarctic Front (SAF).
description: Supplement to: Lüer, Vanessa; Cortese, Giuseppe; Neil, Helen L; Hollis, Christopher J; Willems, Helmut (2009): Radiolarian-based sea surface temperatures and paleoceanographic changes during the Late Pleistocene-Holocene in the subantarctic southwest Pacific. Marine Micropaleontology, 70(3-4), 151-165
DOI: 10.1594/pangaea.841967
title: Flow and suspended sediment concentration fields over tidal bedforms, ADCP profile 11
DOI: 10.1594/pangaea.841973
title: Flow and suspended sediment concentration fields over tidal bedforms, ADCP profile 16
DOI: 10.1594/pangaea.842030
title: Flow and suspended sediment concentration fields over tidal bedforms, ADCP profile 26
DOI: 10.1594/pangaea.891214
title: Basic measurements of radiation at station Cener (2018-05)
DOI: 10.1594/pangaea.877298
title: Deriving Canada-wide soils dataset for use in Soil and Water Assessment Tool (SWAT)

description: The objective of this work was to pre-process the Soil Landscapes of Canada (SLC) database to offer a country-level soils dataset in a format ready to be used in SWAT simulations. A two-level screening process was used to identify critical information required by SWAT and to remove records with information that could not be calculated or estimated. Out of the 14,063 unique soils in the SLC, 11,838 soils with complete information were included in the dataset presented here. Soils with missing records for the required SWAT variables were removed from the analysis. These soils were compiled into a soils list provided as a reference ("incomplete" dataset).
description: Params_Units_Cordeiro_etal_2017.docx: Parameter's unit and abbreviations explanationSLCsoils_Canada_SWAT_Cordeiro-etal_2017.csv: Country-level soils dataset in a format ready to be used in SWAT simulationsSLCsoils_SWAT_Incomplete_Cordeiro-etal_2017.csv: Country-level soils dataset in a format ready to be used in SWAT simulations, incomplete
description: Supplement to: Cordeiro, Marcos R C; Lelyk, Glenn; Kröbel, Roland; Legesse, Getahun; Faramarzi, Monireh; Masud, Mohammad Badrul; McAllister, Tim (2018): Deriving a dataset for agriculturally relevant soils from the Soil Landscapes of Canada (SLC) database for use in Soil and Water Assessment Tool (SWAT) simulations. Earth System Science Data, 10(3), 1673-1686
DOI: 10.1594/pangaea.891274
title: CICE output from Navy Earth System Model (NESM) for 2018060212

description: INITIALIZATION: 2018060212FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.891275
title: CICE output from Navy Earth System Model (NESM) for 2018060312

description: INITIALIZATION: 2018060312FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.891276
title: CICE output from Navy Earth System Model (NESM) for 2018060412

description: INITIALIZATION: 2018060412FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.659149
title: (Table 1) 14C Ages obtained by AMS dating of mixed planktonic foraminifera from ODP Site 202-1233

description: Shown are the calendar ages and resulting linear sedimentation-rates based on the alPal_SFCP_2005 (www.calpal.de) primarily based on the GISP2-synchronised Cariaco basin record (Hughen et al., 2004), INTCAL04 (Reimer et al., 2004), and the most recent Fairbanks U/Th-based calibration curve (Fairbanks et al., 2005). Sample KIA2961 at depth 23.69 m is one dating that is affected by the radiocarbon plateau shown by the CalPal_SFCP_2005 calibration curve (see Fig. 2 and discussion in 3.2.).Samples (primarily Globigerinoides bulloides and Neogloboquadrina pachyderma), performed at the Leibniz-Labor AMS facility in Kiel, Germany.
DOI: 10.1594/pangaea.692155
title: Mesozooplankton biomass during Akademik Kovalevsky cruise AK95, Part II

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 125 µm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-300, 300-500 m) and closed at the upper depth level. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved in 3-4% buffered formaldehyde and processed on return to the laboratory. All of copepods were identified to genus level, other taxonomic groups - to type, class, order and family levels.
DOI: 10.1594/pangaea.891314
title: CICE output from Navy Earth System Model (NESM) for 2018061212

description: INITIALIZATION: 2018061212FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.883093
title: Medium-term sediment characterization of a fetch-limited backbarrier beach (Praia de Faro) located in the Ria Formosa barrier island system within the frame of the BERNA project

description: BERNA (2008). Beach Evolution in Areas of Restricted Fetch:Experimental and Numerical Analysis
DOI: 10.1594/pangaea.891307
title: CICE output from Navy Earth System Model (NESM) for 2018060912

description: INITIALIZATION: 2018060912FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.891309
title: CICE output from Navy Earth System Model (NESM) for 2018061012

description: INITIALIZATION: 2018061012FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.779614
title: Ultra-violet measurements from station Izaña (2012-03)
DOI: 10.1594/pangaea.847902
title: Radiosonde measurements from station Izaña (2015-06)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.891317
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018051712

description: INITIALIZATION: 2018051712FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.891320
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018052012

description: INITIALIZATION: 2018052012FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.891318
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018051812

description: INITIALIZATION: 2018051812FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.891660
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018061412

description: INITIALIZATION: 2018061412FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.736072
title: Ultra-violet measurements from station Izaña (2010-03)
DOI: 10.1594/pangaea.891329
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018052512

description: INITIALIZATION: 2018052512FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.877831
title: (Table 1) Summary of Seheb el Rhassel Group samples from Kess Kess mounds, Anti-Atlas in Morocco
DOI: 10.1594/pangaea.877832
title: (Table 2) Major element contents of Seheb el Rhassel Group (SRG) samples from the Kess Kess mounds, Anti-Atlas in Morocco
DOI: 10.1594/pangaea.877833
title: (Table 2) Trace element concentrations of Seheb el Rhassel Group (SRG) samples from the Kess Kess mounds, Anti-Atlas in Morocco