cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.894342
title: CICE output from Navy Earth System Model (NESM) for 2018090212

description: INITIALIZATION: 2018090212FORECASTS: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.859815
title: Ultra-violet measurements from station Sioux Falls (2009-07)

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.894281
title: Lithology of sediment core VSTANI2, Muntii Stanisoarei, Romania

description: This dataset was archived on 2018-09-17 from the EPD database. (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.859816
title: Other measurements at 10 m from station Sioux Falls (2009-07)
DOI: 10.1594/pangaea.894343
title: CICE output from Navy Earth System Model (NESM) for 2018090312

description: INITIALIZATION: 2018090312FORECASTS: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.860500
title: Permanent open water surfaces in central Siberia from ENVISAT ASAR wide swath data 2003/2004, link to shapefile

description: Permanent water bodies not only store dissolved CO2 but are essential for the maintenance of wetlands in their proximity. From the viewpoint of greenhouse gas (GHG) accounting wetland functions comprise sequestration of carbon under anaerobic conditions and methane release. The investigated area in central Siberia covers boreal and sub-arctic environments. Small inundated basins are abundant on the sub-arctic Taymir lowlands but also in parts of severe boreal climate where permafrost ice content is high and feature important freshwater ecosystems. Satellite radar imagery (ENVISAT ScanSAR), acquired in summer 2003 and 2004, has been used to derive open water surfaces with 150 m resolution, covering an area of approximately 3 Mkm**2. The open water surface maps were derived using a simple threshold-based classification method. The results were assessed with Russian forest inventory data, which includes detailed information about water bodies. The resulting classification has been further used to estimate the extent of tundra wetlands and to determine their importance for methane emissions. Tundra wetlands cover 7% (400,000 km**2) of the study region and methane emissions from hydromorphic soils are estimated to be 45,000 t/d for the Taymir peninsula.
description: Supplement to: Bartsch, Annett; Pathe, Carsten; Wagner, Wolfgang; Scipal, Klaus (2008): Detection of permanent open water surfaces in central Siberia with ENVISAT ASAR wide swath data with special emphasis on the estimation of methane fluxes from tundra wetlands. Hydrology Research, 39(2), 89-100
DOI: 10.1594/pangaea.894322
title: XRF data of sediment core FR1/94-GC3 from the East Tasman Plateau, Australia

description: Model 10kV (Cr) 150 noise (due to negative counts for K at 100 noise the 10kV model was run with 150 noise).Model 30kV thin (sed)
DOI: 10.1594/pangaea.859817
title: Basic measurements of radiation at station Kwajalein (2016-03)
DOI: 10.1594/pangaea.894275
title: Lithology of sediment core VIVERONE, Lago di Viverone, Italy

description: This dataset was archived on 2018-09-17 from the EPD database. (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.859818
title: Radiosonde measurements from station Kwajalein (2016-03)
DOI: 10.1594/pangaea.894344
title: CICE output from Navy Earth System Model (NESM) for 2018090412

description: INITIALIZATION: 2018090412FORECASTS: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.834272
title: Growth rate of Acartia tonsa determined experimentally
DOI: 10.1594/pangaea.834711
title: Maximum ingestion and maximum clearance rate of Acartia tonsa determined experimentally
DOI: 10.1594/pangaea.860504
title: Wetlands in central Siberia from ASAR WS 2003, link to shapefiles

description: An area in central Siberia (partial coverage of Turukhansky und Yeniseysky districts) was investigated using satellite data. It covers freshwater ecosystems of non-forested peatlands in boreal forests. The satellite data represent the growing seasons of 2003/2004.Microwave data were acquired by the Advanced Synthetic Aperture Radar (ASAR) instrument onboard ENVISAT. The multi-temporal capabilities and resolution (150mx150m in WS mode) of the ASAR wide swath mode enabled the detection of dynamic features &gt;2ha over this vast area.Scatterometer (QuikScat) data could be employed to distinguish hydro-periods.Wetland types have been identified on the basis of seasonal changes in backscatter. Results for peatlands have been compared with Russian forest inventory data which contain information on wetland distribution.
description: Supplement to: Bartsch, Annett; Kidd, Richard A; Pathe, Carsten; Scipal, Klaus; Wagner, Wolfgang (2007): Satellite radar imagery for monitoring inland wetlands in boreal and sub-arctic environments. Aquatic Conservation-Marine and Freshwater Ecosystems, 17(3), 305-317
DOI: 10.1594/pangaea.859455
title: (Supplementary Table 1) Locations employed to depict continental environmental conditions at ca. 350 km from the coast

description: Mean annual temperature, precipitation as well as potential evaporation calculated with the WebWIMP Modelling program (Matsuura et al., 2009) and aridity index calculated according to UNEP (1992).
DOI: 10.1594/pangaea.847279
title: Environmental and stand structural characteristics of the European oak species Quercus petraea and Quercus robur

description: Classification of nutrient and water supply level: (NW = high nutrient & high water supply level), (Nw = high nutrient & low water supply level), (nW = low nutrient & high water supply level), (nw = low nutrient & low water supply level).
DOI: 10.1594/pangaea.859909
title: Ultra-violet measurements from station Sioux Falls (2009-08)

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 2017-02-03.
DOI: 10.1594/pangaea.860537
title: Sediment budget and geomorphic process units of the Swedish Kärkevagge, link to ArcInfo E00 files

description: Geomorphic process units have been derived in order to allow quantification via GIS techniques at a catchment scale. Mass movement rates based on existing field measurements are employed in the budget calculations. In the Kärkevagge catchment, Northern Sweden, 80% of the area can be identified either as a source area for sediments or as a zone where sediments are deposited. The overall budget for the slopes beneath the rockwalls in the Kärkevagge is approximately 680 t/a whilst about 150 t a–1 are transported into the fluvial system.
description: The dataset comprises all input data (DEM, NDVI) and the resulting process units (see publication for numbering) as well sedimentbudgets as ArcInfo E00 files.
description: Supplement to: Bartsch, Annett; Gude, Martin; Gurney, Stephen D (2009): Quantifying sediment transport processes in periglacial mountain environments at a catchment scale using geomorphic process units. Geografiska Annaler Series A-Physical Geography, 91(1), 1-9
DOI: 10.1594/pangaea.859910
title: Other measurements at 10 m from station Sioux Falls (2009-08)
DOI: 10.1594/pangaea.894355
title: Pollen profile of sediment core BAIAMAR3, Baia Mare, Romania

description: This dataset was archived on 2018-09-17 from the EPD database. (http://www.europeanpollendatabase.net). Date analyzed: 2000
DOI: 10.1594/pangaea.894443
title: Parameters of a superstatistical distribution of daily precipitation extremes for 20,561 sites in the world

description: This .zip folder contains the parameters of a superstatistical distribution of daily precipitation extremes for 20,561 sites in the world. The details about this distribution are available in the following paper: De Michele, C. and Avanzi, F. (2018): Superstatistical distribution of daily precipitation extremes: A worldwide assessment, Scientific Reports. These parameters were estimated using daily-precipitation data from the Global Historical Climatology Network (GHCN) daily, available at ftp://ftp.ncdc.noaa.gov/pub/data/ghcn/daily/The .zip folder includes one file for each of the 20,561 sites considered in the above paper. The name of each file refers to the station ID of the original site belonging to the Global Historical Climatology Network (GHCN) daily, to which the reader is referred for information regarding the location of each site. The structure of the file is standard as follows:- The first row reports the station ID and the value of the optimal threshold used in the superstatistical distribution (see the above paper for details, unit is mm*10);- All the other rows report estimates of optimal parameters lambda, beta, and p0 for each year with at least 25 days of precipitation. Again, the reader is referred to the above paper for details about these parameters. Each row reports results for one year in the following order: (1) year on which parameters were estimated; (2) number of available precipitation observations; (3) estimated value of beta; (4) estimated value of lambda (unit is mm*10); (5) estimated value of p0. Questions about the dataset should be sent to the following email address: carlo.demichele@polimi.it
description: Supplement to: De Michele, Carlo; Avanzi, Francesco (2018): Superstatistical distribution of daily precipitation extremes: A worldwide assessment. Scientific Reports
DOI: 10.1594/pangaea.892089
title: (Experiment 2) Shell (density, thickness) and soft tissue (somatic tissue weight, gonad index) metrics for eastern oysters Crassostrea virginica reared under variable predation conditions (S. Texas, 2013-14)
DOI: 10.1594/pangaea.894356
title: Pollen profile of sediment core BAIAMAR2, Baia Mare, Romania

description: This dataset was archived on 2018-09-17 from the EPD database. (http://www.europeanpollendatabase.net). Date analyzed: 2000
DOI: 10.1594/pangaea.894357
title: Pollen profile of sediment core BAIAMAR1, Baia Mare, Romania

description: This dataset was archived on 2018-09-17 from the EPD database. (http://www.europeanpollendatabase.net). Date analyzed: 2000
DOI: 10.1594/pangaea.892087
title: (Experiment 1b) Shell crushing force for eastern oysters Crassostrea virginica reared under variable predation conditions (S. Texas, 2013-14)

description: Experimental design: Treatment (2 levels): oysters were reared in the field in cages which did (predator) or did not (control) contain a blue crab predator isolated to prevent consumptionCage (17 levels): the experiment included 17 cages, 9 assigned to control and 8 to predator treatmentsReplicate (5 levels): 5 oysters from each cage were sampled individually
DOI: 10.1594/pangaea.894364
title: Pollen profile of sediment core BISOCLM1, Lacul cu Muschi, Romania
DOI: 10.1594/pangaea.892091
title: (Experiment 3a) Shell weight for eastern oysters Crassostrea virginica reared under variable predation conditions (laboratory study)

description: Date: Summer 2013Experimental design:Treatment (4 levels): oysters were reared in the lab in tanks which never contained crabs (0 hour), or contained crabs 2 hours, 24 hours, or 168 hours per weekMesocosm (8 levels): the experiment included 32 tanks, 8 of which were assigned to each treatmentReplicate (3 levels): 3 oysters were sampled
DOI: 10.1594/pangaea.894365
title: Pollen profile of sediment core BISOCLM2, Lacul cu Muschi, Romania

description: This dataset was archived on 2018-09-19 from the EPD database. (http://www.europeanpollendatabase.net). Date analyzed: 1957
DOI: 10.1594/pangaea.892244
title: (Experiment 1a) Shell weight for eastern oysters Crassostrea virginica reared under variable predation conditions (S. Texas, 2013-14)

description: Experimental design:Treatment (2 levels): oysters were reared in the field in cages which did (predator) or did not (control) contain a blue crab predator isolated to prevent consumptionCage (17 levels): the experiment included 17 cages, 9 assigned to control and 8 to predator treatmentsReplicate (5 levels): 5 oysters from each cage were sampled individually
DOI: 10.1594/pangaea.894467
title: Pollen profile of sediment core SARDORN1, Sarul Domei, Romania

description: This dataset was archived on 2018-09-19 from the EPD database. (http://www.europeanpollendatabase.net). Date analyzed: 1929
DOI: 10.1594/pangaea.892254
title: (Experiment 3b) Shell crushing force for eastern oysters Crassostrea virginica reared under variable predation conditions (laboratory study)

description: Date: Summer 2013Experimental design:Treatment (4 levels): oysters were reared in the lab in tanks which never contained crabs (0 hour), or contained crabs 2 hours, 24 hours, or 168 hours per weekMesocosm (8 levels): the experiment included 32 tanks, 8 of which were assigned to each treatmentReplicate (3 levels): 3 oysters were sampled
DOI: 10.1594/pangaea.859912
title: Ultra-violet measurements from station Sioux Falls (2009-09)

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.859864
title: Culture conditions, mass spectrometric measurements and acclimation carbonate chemistry

description: - A combined increase in seawater [CO2] and [H+] was recently shown to induce a shift from photosynthetic HCO3- to CO2 uptake in Emiliania huxleyi. This shift occurred within minutes, whereas acclimation to ocean acidification (OA) did not affect the carbon source.- To identify the driver of this shift, we exposed low- and high-light acclimated E. huxleyi to a matrix of two levels of dissolved inorganic carbon (1400, 2800 lmol kg-1) and pH (8.15, 7.85) and directly measured cellular O2, CO2 and HCO3 fluxes under these conditions.- Exposure to increased [CO2] had little effect on the photosynthetic fluxes, whereas increased [H+] led to a significant decline in HCO3- uptake. Low-light acclimated cells overcompensated for the inhibition of HCO3- uptake by increasing CO2 uptake. High-light acclimated cells, relying on higher proportions of HCO3- uptake, could not increase CO2 uptake and photosynthetic O2 evolution consequently became carbon-limited.- These regulations indicate that OA responses in photosynthesis are caused by [H+] rather than by [CO2]. The impaired HCO3- uptake also provides a mechanistic explanation for lowered calcification under OA. Moreover, it explains the OA-dependent decrease in photosynthesis observed in high-light grown phytoplankton.
description: Supplement to: Kottmeier, Dorothee; Rokitta, Sebastian D; Rost, Björn (2016): Acidification, not carbonation, is the major regulator of carbon fluxes in the coccolithophore Emiliania huxleyi. New Phytologist, 211(1), 126-137
DOI: 10.1594/pangaea.859913
title: Other measurements at 10 m from station Sioux Falls (2009-09)
DOI: 10.1594/pangaea.859797
title: Description of manganese nodules and crust collected from the Hakurei Maru Cruise GH76-1, January-March, 1976, in the Central Pacific Basin

description: This report of the GH76-1 cruise mainly includes the results of the on-board observations in the survey area of the medial-eastern part of Central Pacific Basin (5 degree -10 degree N, 170 degree -175 degree W) and partly of analytical work at the on-shore laboratory. In addition, the results of some on-board optical and geophysical works along the tracks of Japan-Ogasawara-survey area-Hawaii, are described in appendices. The GH76-1 cruise of the R/V Hakurei-maru was carried out from the 10th January to the 9th March, 1976 as the second phase field work of the Geological Survey of Japan five-year research program of study on the manganese nodule deposits of the Central Pacific Basin and also as a part of the National Research Institute for Pollution and Resources research program of technological study on the exploitation of deep sea mineral resources. The GSJ research program (F.Y. 1974-F.Y. 1978) aims at providing basic information on the manganese nodule distribution and their origin on the deep sea floor of the Central Pacific Basin bounded by the Marshall Ridge to the west, the Christmas Ridge to the east, and the Mid-Pacific Mountains to the north. The first phase of investigation was carried out during the GH74-5 cruise in the eastern part of the area (6 degree -10 degree 30'W, 164 degree 30'-171 degree 30'N)(Mizuno and Chujo, eds., 1975), and the present second phase covered an areas of 5 degree square, just west of the GH74-5 area.
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: Mizuno, Atsuyuki; Moritani, Tomoyuki (1977): Deep Sea Mineral Resources Investigation in the Central-Eastern Part of Central Pacific Basin, January - March 1976 (GH76-1 Cruise). Geological Survey of Japan, Cruise Report, 8, 217 pp
DOI: 10.1594/pangaea.859915
title: Ultra-violet measurements from station Sioux Falls (2009-10)

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.859916
title: Other measurements at 10 m from station Sioux Falls (2009-10)
DOI: 10.1594/pangaea.859825
title: Chemical Analyses of ferromanganese crust from the Alguhas Bank off South-Africa in the Indian Ocean

description: Phosphate-rich sediments are present on modern continental shelves off South West Africa on the Alguhas Bank. They are similar to those found on the Blake Plateau off the Esat coast of the USA. They form phosphatized foraminiferal limestone and glauconite-phosphatic breccia. They are often encrusted with ferromanganese.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.892088
title: (Experiment 1c) Shell amino acid content for eastern oysters Crassostrea virginica reared under variable predation conditions (S. Texas, 2013-14)

description: Experimental design: Treatment (2 levels): oysters were reared in the field in cages which did (predator) or did not (control) contain a blue crab predator isolated to prevent consumptionCage (17 levels): the experiment included 17 cages, 9 assigned to control and 8 to predator treatmentsReplicate: for the first two shell metrics (weight and crushing force), 5 oysters from each cage were sampled individually; due to methodological restrictions, amino acid analysis was conducted on 5 oysters combined
DOI: 10.1594/pangaea.894472
title: Lithology of sediment core SIRIO, Lago di Sirio, Italy

description: This dataset was archived on 2018-09-19 from the EPD database. (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.894353
title: Lithology of sediment core BAIAMAR2, Baia Mare, Romania

description: This dataset was archived on 2018-09-17 from the EPD database. (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.894418
title: CICE output from Navy Earth System Model (NESM) for 2018090812

description: INITIALIZATION: 2018090812FORECASTS: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.894419
title: CICE output from Navy Earth System Model (NESM) for 2018090912

description: INITIALIZATION: 2018090912FORECASTS: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.894420
title: CICE output from Navy Earth System Model (NESM) for 2018091012

description: INITIALIZATION: 2018091012FORECASTS: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" ;