cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.833266
title: Dead Sea lake level for the last 140 ka

description: In this paper we describe the stratigraphy and sediments deposited in Lake Samra that occupied the Dead Sea basin between ~135 and 75 ka. This information is combined with U/Th dating of primary aragonites in order to estimate a relative lake-level curve that serves as a regional paleohydrological monitor. The lake stood at an elevation of ~340 m below mean sea level (MSL) during most of the last interglacial. This level is relatively higher than the average Holocene Dead Sea (~400±30 m below MSL). At ~120 and ~85 ka, Lake Samra rose to ~320 m below MSL while it dropped to levels lower than ∼380 m below MSL at ~135 and ~75 ka, reflecting arid conditions in the drainage area. Lowstands are correlated with warm intervals in the Northern Hemisphere, while minor lake rises are probably related to cold episodes during MIS 5b and MIS 5d. Similar climate relationships are documented for the last glacial highstand Lake Lisan and the lowstand Holocene Dead Sea. Yet, the dominance of detrital calcites and precipitation of travertines in the Dead Sea basin during the last interglacial interval suggest intense pluvial conditions and possible contribution of southern sources of wetness to the region.
description: Supplement to: Waldmann, Nicolas D; Stein, Mordechai; Ariztegui, Daniel; Starinsky, A (2009): Stratigraphy, depositional environments and level reconstruction of the last interglacial Lake Samra in the Dead Sea basin. Quaternary Research, 72(1), 1-15
DOI: 10.1594/pangaea.861252
title: Sea surface temperature reconstruction for ODP Site 202-1241

description: Dataset was corrected on 2018-05-29, columns for TEX86- and UK'37-temperatures were switched in the old version.
DOI: 10.1594/pangaea.762831
title: (Table 1) Sum concentrations of chlorophyll a plus pheophytin in surface Black Sea waters in 1998-2000
DOI: 10.1594/pangaea.855413
title: Pore depth evolution of a pyrochlore pellet

description: The long-term stability of ceramic materials that are considered as potential nuclear waste forms is governed by heterogeneous surface reactivity. Thus, instead of a mean rate, the identification of one or more dominant contributors to the overall dissolution rate is the key to predict the stability of waste forms quantitatively. Direct surface measurements by vertical scanning interferometry (VSI) and their analysis via material flux maps and resulting dissolution rate spectra provide data about dominant rate contributors and their variability over time. Using pyrochlore (Nd2Zr2O7) pellet dissolution under acidic conditions as an example, we demonstrate the identification and quantification of dissolution rate contributors, based on VSI data and rate spectrum analysis. Heterogeneous surface alteration of pyrochlore varies by a factor of about 5 and additional material loss by chemo-mechanical grain pull-out within the uppermost grain layer. We identified four different rate contributors that are responsible for the observed dissolution rate range of single grains. Our new concept offers the opportunity to increase our mechanistic understanding and to predict quantitatively the alteration of ceramic waste forms.
description: Supplement to: Fischer, Cornelius; Finkeldei, Sarah; Brandt, Felix; Bosbach, Dirk; Lüttge, Andreas (2015): Direct Measurement of Surface Dissolution Rates in Potential Nuclear Waste Forms: The Example of Pyrochlore. ACS Applied Materials & Interfaces, 7(32), 17857-17865
DOI: 10.1594/pangaea.611534
title: Lithology, colour and structural description of sediment profile Kha-1, Appendix 4-2
DOI: 10.1594/pangaea.755741
title: (Table 1k) Nutrient concentrations and primary production at Station Sap-92-2130 in the Bering Sea
DOI: 10.1594/pangaea.722992
title: Ultra-violet measurements from station Rock Springs (2002-01)

description: Version 2, 2009-06-26. 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.855430
title: Observation of manganese deposits in the New England Seamount Chain during Atlantis Cruise 280

description: Reports on ATLANTIS Cruises 280 and 281 to the New England Seamount Chain are combined here. . A continuous bathymetric survey was run on both cruises, with profiles across several seamounts. A series of dredge and camera stations were made. They are dicussed in this report. Also included are photographs representative of each camera lowering and photographs of dredged material.
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.755743
title: (Table 1m) Nutrient concentrations and primary production at Station Sap-92-2134 in the Bering Sea
DOI: 10.1594/pangaea.747604
title: Meteorological observations during BATO cruise from Texel to Kaap de Goede Hoop started at 1802-08-31
DOI: 10.1594/pangaea.755964
title: (Table 7) Accumulation rates for sediments from ODP Hole 115-711A

description: Major element given as oxides.
DOI: 10.1594/pangaea.496177
title: Water temperature MBT profiles from cruise U90X089208M_1977
DOI: 10.1594/pangaea.744061
title: (Table 1) Hydrochemical parameters in the Varna Gulf, Black Sea
DOI: 10.1594/pangaea.901255
title: Apatite fission track (AFT) age analyses of sample MAU-09 from a Precambrian crystalline basement in Mauretania

description: Zeta: Traditionalzeta: 348.18sig zeta: 6.5rho-d (N/cm**2): 1150000Nd: 3443
DOI: 10.1594/pangaea.677165
title: Ozone measurements from station Boulder (2001-03)

description: Location: Boulder, Colorado, USA; Distance from radiation site: 16 km
DOI: 10.1594/pangaea.771210
title: (Table 5) Age control points of ODP Leg 127 sites

description: Sediment depth is given in mbsf. Paleomagnetic data are from Hamano et al. (1992), and biostratigraphic data are from Shipboard Scientific Party (1990) with the exception of the LO of Neodenticula kamtschatica (2.5 Ma control point) in Site 795 which is from Koizumi (1992).
DOI: 10.1594/pangaea.786121
title: Xray-ct-scanner images from IODP Hole 333-C0012C

description: Geocode = [m CSF-A] Top Core depth (below sea floor).Measurements data just above (negative section depth) and below (depth exceed section length) a core section are utilized in the deconvolution (http://en.wikipedia.org/wiki/Deconvolution).
DOI: 10.1594/pangaea.855433
title: (Table 2) Horizontal ice flow velocities, azimuths (relative to true north), and vertical ice-particle velocities in the vicinity of Vostok Station, Antarctica

description: In the austral summer seasons 2001/02 and 2002/03, Global Positioning System (GPS) data were collected in the vicinity of Vostok Station to determine ice flow velocities over Lake Vostok. Ten GPS sites are located within a radius of 30 km around Vostok Station on floating ice as well as on grounded ice to the east and to the west of the lake. Additionally, a local deformation network around the ice core drilling site 5G-1 was installed. The derived ice flow velocity for Vostok Station is 2.00 m/a ± 0.01 m/a. Along the flowline of Vostok Station an extension rate of about 10**-5/a (equivalent to 1 cm/km/a) was determined. This significant velocity gradient results in a new estimate of 28700 years for the transit time of an ice particle along the Vostok flowline from the bedrock ridge in the southwest of the lake to the eastern shoreline. With these lower velocities compared to earlier studies and, hence, larger transit times the basal accretion rate is estimated to be 4 mm/a along a portion of the Vostok flowline. An assessment of the local accretion rate at Vostok Station using the observed geodetic quantities yields an accretion rate in the same order of magnitude. Furthermore, the comparison of our geodetic observations with results inferred from ice-penetrating radar data indicates that the ice flow may not have changed significantly for several thousand years.
description: Supplement to: Wendt, Jens; Dietrich, Reinhard; Fritsche, Mathias; Wendt, Anja; Yuskevich, A V; Kokhanov, Andrey; Senatorov, Anton; Lukin, Valeriy V; Shibuya, Kazuo; Doi, Koichiro (2006): Geodetic observations of ice flow velocities over the southern part of subglacial Lake Vostok, Antarctica, and their glaciological implications. Geophysical Journal International, 166(3), 991-998
DOI: 10.1594/pangaea.892354
title: CICE output from Navy Earth System Model (NESM) for 2018062312

description: INITIALIZATION: 2018062312FORECASTS: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.901823
title: Pan-european, physically consistent simulations from groundwater to the atmosphere with the Terrestrial Systems Modeling Platform, TerrSysMP (1989-2018 daily time-series)

description: Applying the Terrestrial Systems Modeling Platform, TerrSysMP, this study provides the first simulated long-term (1989-2018), high-resolution (~12.5km) terrestrial system climatology over Europe, which comprises variables from groundwater across the land surface to the top of the atmosphere (G2A). The data set offers an unprecedented opportunity to test hypotheses related to short- and long-range feedback processes in space and time between the different interacting compartments of the terrestrial system. The physical consistency of simulated states and fluxes in the terrestrial system constitutes the uniqueness of the data set: while most regional climate models (RCMs) have a tendency to simplify the soil moisture and groundwater representation, TerrSysMP explicitly simulates the full 3D soil- and groundwater dynamics, closing the terrestrial water cycle from G2A. Anthropogenic impacts are excluded, the dataset may serve therefore as a near-natural reference for global change simulations including human water use and climate change. The data set is available as netCDF files.
description: 2019-12-05: 30 Datasets 'vso_EUR-11_ECMWF-ERAINT_evaluation_r1i1p1_FZJ-IBG3-TERRSYSMP11_v1_day_*.nc* deleted
DOI: 10.1594/pangaea.832228
title: Geochemistry of sediment core MD01-2446
DOI: 10.1594/pangaea.897760
title: Other measurements at 30 m from station Payerne (2017-09)
DOI: 10.1594/pangaea.890252
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018050112

description: INITIALIZATION: 2018050112FORECASTS: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.868773
title: Seagrass meadows of the Solomon Islands, derived from field surveys conducted 13 May and 16 June 2004

description: Approximately 6,633 ±1,446 hectares (ha) of predominately intertidal and shallow subtidal seagrass meadows were mapped during the Solomon Islands Rapid Ecological Assessment (SIREA) between 13 May and 16 June 2004. This was the first comprehensive survey of the Solomon Islands and it focused on the main island group from Choiseul Island in the northwest to Makira in the southeast. The survey involved examination of 1,426 field validation sites/points and identified 486 individual meadows. 10 species of seagrass were identified throughout the Solomon Islands.Mapping survey methodologies followed standardised global seagrass research methods (McKenzie et al. 2001, doi:10.1016/B978-044450891-1/50006-2) where observers walked or free-dived to assess survey points. At each survey site/point seagrass % cover and/or above ground biomass (standing crop, grams dry weight (g DW/m**2)) was determined within quadrats (50cm x 50cm) using a non-destructive visual estimates of biomass technique and the seagrass species present identified. Water depth and visual/tactile description of sediment were also recorded at each survey site/point. A differential handheld global positioning system (GPS) was used to locate each survey site/point (accuracy ±5m). Seagrass meadow boundaries were determined based on the positions of survey sites and the presence of seagrass, coupled with depth contours and remote sensing (e.g. aerial photography) where available. The meadow boundary accuracy varied from 7.5m to 500m. The resulting data of each survey point and each seagrass meadow was saved as an ArcMap shapefile and projected to WGS84.Most Solomon Islands seagrasses were found in water shallower than 10m and meadows were monospecific or consisted of multispecies communities; up to 6 species present at a single location. The dominant species encountered were Enhalus acoroides and Thalassia hemprichii. 54% of all seagrass meadows (per hectare basis) were found in Malaita Province. All other provinces each included less than 12% of the seagrass meadows. Seagrass distribution appears to be primarily influenced by the degree of wave action (exposure) and nutrient availability. Solomon Islands' seagrass habitats can be generally categorised into four broad habitats: estuaries (incl. large shallow lagoons), coastal (incl. fringing reef), deep-water and reef (e.g., barrier or isolated).
DOI: 10.1594/pangaea.747444
title: Meteorological observations during AREND cruise from Fort Amsterdam to Hellevoetsluis started at 1780-07-30
DOI: 10.1594/pangaea.777214
title: Xray-ct-scanner images from IODP Hole 331-C0013C

description: Geocode = [m CSF-A] Top Core depth (below sea floor). Measurements data just above (negative section depth) and below (depth exceed section length) a core section are utilized in the deconvolution (http://en.wikipedia.org/wiki/Deconvolution).
DOI: 10.1594/pangaea.891563
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018060412

description: INITIALIZATION: 2018060412FORECASTS: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.895690
title: CICE output from Navy Earth System Model (NESM) for 2018102012

description: INITIALIZATION: 2018102012FORECASTS: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.684698
title: (Appendix) Mg/Ca ratios of ostracodes and bottom-water temperature reconstruction for the Mid-Pliocene of ODP Hole 94-610A in the North Atlantic

description: Age is PRISM-1 age
DOI: 10.1594/pangaea.777127
title: Section images from IODP Hole 331-C0013F

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.892357
title: CICE output from Navy Earth System Model (NESM) for 2018062612

description: INITIALIZATION: 2018062612FORECASTS: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.749505
title: Meteorological observations during Haast U Langzaam cruise from Bramspunt to Middelburg started at 1765-12-11
DOI: 10.1594/pangaea.897761
title: Other measurements at 30 m from station Payerne (2017-10)
DOI: 10.1594/pangaea.892711
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018071612

description: INITIALIZATION: 2018071612FORECASTS: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.898304
title: Sea-bed videos (benthos) from the North Sea along ROV profile HE169/741

description: Positions and depths from the ship's automatic data recording system. The ROV-system sprint 103 was equipped with two video- and one 36mm still camera, lights, flash-lights, compass, and parallel lasers providing a scale in the images, a tether-management system (TMS), a winch, and the board units. All cameras used the same main lens and could be tilted. Videos were recorded in Betacam-format. Videos were uploaded for documentation reasons independently of partly low quality due to a ROV driving strategy responding to varying environmental conditions such as sunlight and turbidity. Photographs along the same ROV-transect are available at https://doi.org/10.1594/PANGAEA.250426. J. Gutt: mailto:Julian.Gutt@awi.de
DOI: 10.1594/pangaea.898306
title: Sea-bed videos (benthos) from the North Sea along ROV profile HE169/759

description: Positions and depths from the ship's automatic data recording system. The ROV-system sprint 103 was equipped with two video- and one 36mm still camera, lights, flash-lights, compass, and parallel lasers providing a scale in the images, a tether-management system (TMS), a winch, and the board units. All cameras used the same main lens and could be tilted. Videos were recorded in Betacam-format. Videos were uploaded for documentation reasons independently of partly low quality due to a ROV driving strategy responding to varying environmental conditions such as sunlight and turbidity. Photographs along the same ROV-transect are available at https://doi.org/10.1594/PANGAEA.250428. J. Gutt: mailto:Julian.Gutt@awi.de
DOI: 10.1594/pangaea.777261
title: Xray-ct-scanner images from IODP Hole 331-C0017C

description: Geocode = [m CSF-A] Top Core depth (below sea floor). Measurements data just above (negative section depth) and below (depth exceed section length) a core section are utilized in the deconvolution (http://en.wikipedia.org/wiki/Deconvolution).
DOI: 10.1594/pangaea.898309
title: Sea-bed videos (benthos) from the North Sea along ROV profile HE169/786

description: Positions and depths from the ship's automatic data recording system. The ROV-system sprint 103 was equipped with two video- and one 36mm still camera, lights, flash-lights, compass, and parallel lasers providing a scale in the images, a tether-management system (TMS), a winch, and the board units. All cameras used the same main lens and could be tilted. Videos were recorded in Betacam-format. Videos were uploaded for documentation reasons independently of partly low quality due to a ROV driving strategy responding to varying environmental conditions such as sunlight and turbidity. Photographs along the same ROV-transect are available at https://doi.org/10.1594/PANGAEA.250431. J. Gutt: mailto:Julian.Gutt@awi.de
DOI: 10.1594/pangaea.898310
title: Sea-bed videos (benthos) from the North Sea along ROV profile HE169/792

description: Positions and depths from the ship's automatic data recording system. The ROV-system sprint 103 was equipped with two video- and one 36mm still camera, lights, flash-lights, compass, and parallel lasers providing a scale in the images, a tether-management system (TMS), a winch, and the board units. All cameras used the same main lens and could be tilted. Videos were recorded in Betacam-format. Videos were uploaded for documentation reasons independently of partly low quality due to a ROV driving strategy responding to varying environmental conditions such as sunlight and turbidity. Photographs along the same ROV-transect are available at https://doi.org/10.1594/PANGAEA.250432. J. Gutt: mailto:Julian.Gutt@awi.de
DOI: 10.1594/pangaea.898314
title: Sea-bed videos (benthos) from the North Sea along ROV profile HE169/800

description: Positions and depths from the ship's automatic data recording system. The ROV-system sprint 103 was equipped with two video- and one 36mm still camera, lights, flash-lights, compass, and parallel lasers providing a scale in the images, a tether-management system (TMS), a winch, and the board units. All cameras used the same main lens and could be tilted. Videos were recorded in Betacam-format. Videos were uploaded for documentation reasons independently of partly low quality due to a ROV driving strategy responding to varying environmental conditions such as sunlight and turbidity. Photographs along the same ROV-transect are available at https://doi.org/10.1594/PANGAEA.250436. J. Gutt: mailto:Julian.Gutt@awi.de
DOI: 10.1594/pangaea.749947
title: Meteorological observations during KEMPHAAN cruise from Vlissingen to Guyana started at 1786-06-09