cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.894656
title: (Table 2) Nannofossil abundances in sediment core MCBR
DOI: 10.1594/pangaea.883263
title: Ozone measurements from station Lindenberg (2016-07)
DOI: 10.1594/pangaea.883264
title: Expanded measurements from station Lindenberg (2016-07)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.883277
title: Ozone measurements from station Lindenberg (2016-09)
DOI: 10.1594/pangaea.882985
title: Expanded measurements from station Lindenberg (2014-01)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.883452
title: Radiosonde measurements from station Barrow (2003-11)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.838564
title: Lithology of sediment core DIMA, Russia

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.894589
title: (Table 1) Nannofossil abundances in sediment core CamDor
DOI: 10.1594/pangaea.883695
title: Meteorological synoptical observations from station Tateno (2017-09)
DOI: 10.1594/pangaea.868444
title: Layer matching
DOI: 10.1594/pangaea.868446
title: Two-way traveltimes of the traced layers
DOI: 10.1594/pangaea.883696
title: Radiosonde measurements from station Tateno (2017-09)
DOI: 10.1594/pangaea.883662
title: Age and body mass of deep-sea squids in Monterey Submarine Canyon
DOI: 10.1594/pangaea.883665
title: Mantle length, body mass and maturity of deep-sea squids in Monterey Submarine Canyon
DOI: 10.1594/pangaea.883300
title: Expanded measurements from station Lindenberg (2016-12)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.883432
title: Radiosonde measurements from station Barrow (2002-03)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.883637
title: Ultra-violet measurements from station Carpentras (2017-10)
DOI: 10.1594/pangaea.883284
title: Surface velocity of the Roi Baudouin Ice Shelf, East Antarctica, from SAR interferometry, link to GeoTIFFs

description: Antarctic ice shelves are buttressed by numerous pinning points attaching to the otherwise freely-floating ice from below. Some of these kilometric-scale grounded features are unresolved in Antarctic-wide datasets of ice thickness and bathymetry, hampering ice flow models to fully capture dynamics at the grounding line and upstream. We investigate the role of an 8.7 km² pinning point at the front of the Roi Baudouin Ice Shelf, East Antarctica.Using ERS interferometry and ALOS-PALSAR speckle tracking, we derive, on a 125 m grid spacing, surface velocities deviating by -5.2 ± 4.5 m/a from 37 on-site global navigation satellite systems-derived velocities. We find no evidence for ice flow changes on decadal time scales and we show that ice on the pinning point virtually stagnates, deviating the ice stream and causing enhanced horizontal shearing upstream. Using the BISICLES ice-flow model, we invert for basal friction and ice rigidity with three input scenarios of ice velocity and geometry. We show that inversion results are the most sensitive to the presence/absence of the pinning point in the bathymetry; surface velocities at the pinning point are of secondary importance. Undersampling of pinning points results in erroneous ice-shelf properties in models initialised by control methods. This may impact prognostic modelling for ice-sheet evolution in the case of unpinning.
description: Supplement to: Berger, Sophie; Favier, Lionel; Drews, Reinhard; Derwael, Jean-Jacques; Pattyn, Frank (2016): The control of an uncharted pinning point on the flow of an Antarctic ice shelf. Journal of Glaciology, 62(231), 37-45
DOI: 10.1594/pangaea.883586
title: Iceberg scour shapefiles from the Naust Formation on the mid-Norwegian margin

description: This data contains a zipped file with digitised records of iceberg scours from five seismic units that comprise the glaciogenic stratigraphy on the mid-Norwegian shelf. These records have been used to investigate iceberg trajectories during the time period covered by each seismic unit.This provides information on the palaeo-oceanography and the dominant ocean currents on the mid-Norwegian shelf during the Pleistocene when the scours were formed.
DOI: 10.1594/pangaea.883636
title: Basic measurements of radiation at station Carpentras (2017-10)
DOI: 10.1594/pangaea.843542
title: MSCL measurements from IODP Hole 348-C0002M

description: Update on 2018-01-19: Parameter 'Susceptibility, volume' has been converted from [10**-5 SI] to [10**-6 SI]. All values were previously given in the wrong unit.
DOI: 10.1594/pangaea.587075
title: Hydrographic observation below 1000 m water depth at site EX_1963_50, equatorial Atlantic
DOI: 10.1594/pangaea.866363
title: Projections for Land Use Change in Brazil: 2000-2050, links to files in ArcGIS shapefile format

description: This data set contains the inputs and the results of the REDD+ Policy Assessment Centre project (REDD-PAC) project (http://www.redd-pac.org), developed by a consortium of research institutes (IIASA, INPE, IPEA, UNEP-WCMC), supported by Germany's International Climate Initiative. Taking a new land use map of Brazil for 2000 as input, the research team used the global economic model GLOBIOM to project land use changes in Brazil up to 2050. Model projections show that Brazil has the potential to balance its goals of protecting the environment and becoming a major global producer of food and biofuels. The model results were taken into account by Brazilian decision-makers when developing the country's intended nationally determined contribution (INDC).
DOI: 10.1594/pangaea.889469
title: Weighted endemism of Cerrado woody plants and related species distribution models

description: This raster provides an overview of endemism of species of woody plants for the Brazilian domain of Cerrado. We compiled information for 174 species and calculated weighted endemism per cel (30 arc seconds) using a function developed by Guerin et al. (2015).
DOI: 10.1594/pangaea.789968
title: Benthic cover map of Heron Reef derived from a high-spatial-resolution multi-spectral satellite image using object based image analysis

description: Providing accurate maps of coral reefs where the spatial scale and labels of the mapped features correspond to map units appropriate for examining biological and geomorphic structures and processes is a major challenge for remote sensing. The objective of this work is to assess the accuracy and relevance of the process used to derive geomorphic zone and benthic community zone maps for three western Pacific coral reefs produced from multi-scale, object-based image analysis (OBIA) of high-spatial-resolution multi-spectral images, guided by field survey data. Three Quickbird-2 multi-spectral data sets from reefs in Australia, Palau and Fiji and georeferenced field photographs were used in a multi-scale segmentation and object-based image classification to map geomorphic zones and benthic community zones. A per-pixel approach was also tested for mapping benthic community zones. Validation of the maps and comparison to past approaches indicated the multi-scale OBIA process enabled field data, operator field experience and a conceptual hierarchical model of the coral reef environment to be linked to provide output maps at geomorphic zone and benthic community scales on coral reefs. The OBIA mapping accuracies were comparable with previously published work using other methods; however, the classes mapped were matched to a predetermined set of features on the reef.
description: A Quickbird-2 multi-spectral image data of Heron Reef taken on July 1, 2007 was used in a multi-scale segmentation and object-based image classification to produce a benthic community map and a geomorphic zone map. These maps are provided in ArcMap shapefile format. Projection used was Universal Transverse Mercator Zone 56 South and Datum used was WGS 84. A map is linked as kmz file to view the the actual spatial extent of the benthic community map and geomorphic zone map in a google-earth map at hdl:10013/epic.40097.d008.
description: Supplement to: Phinn, Stuart R; Roelfsema, Christiaan M; Mumby, Peter John (2012): Multi-scale, object-based image analysis for mapping geomorphic and ecological zones on coral reefs. International Journal of Remote Sensing, 33(12), 3768-3797
DOI: 10.1594/pangaea.669971
title: Basic measurements of radiation at station Kwajalein (2002-02)
DOI: 10.1594/pangaea.705421
title: (Table 2) Occurrence of pollen and spores in sediment core KT05-7_PC-02
DOI: 10.1594/pangaea.756542
title: (Table 2) Major cation elements in the interstitial water at ODP Site 116-718
DOI: 10.1594/pangaea.841033
title: Sea surface alkenone temperatures in the midlatitude North Pacific (KR02-06 St. A MC, KR02-06 St. A GC, and MD01-2421) during the Holocene
DOI: 10.1594/pangaea.509829
title: Grain size distribution of palaeolake sediment core D100, Gobi Desert, NW China
DOI: 10.1594/pangaea.774323
title: (Table 2) Concentrations of total hydrolyzable amino acids in interstitial waters of ODP Sites 126-790 and 126-791
DOI: 10.1594/pangaea.862108
title: Cladocera record in Lake Tiefer See sediments
DOI: 10.1594/pangaea.743921
title: X-ray diffraction analysis of sediment samples from the NW Iberian shelf system
DOI: 10.1594/pangaea.833958
title: Inventory of thermo-erosional valleys and streams in three ice-rich permafrost lowlands adjacent to the Laptev Sea, with links to maps in ArcGIS format

description: This dataset provides an inventory of thermo-erosional landforms and streams in three lowland areas underlain by ice-rich permafrost of the Yedoma-type Ice Complex at the Siberian Laptev Sea coast. It consists of two shapefiles per study region: one shapefile for the digitized thermo-erosional landforms and streams, one for the study area extent. Thermo-erosional landforms were manually digitized from topographic maps and satellite data as line features and subsequently analyzed in a Geographic Information System (GIS) using ArcGIS 10.0. The mapping included in particular thermo-erosional gullies and valleys as well as streams and rivers, since development of all of these features potentially involved thermo-erosional processes. For the Cape Mamontov Klyk site, data from Grosse et al. [2006], which had been digitized from 1:100000 topographic map sheets, were clipped to the Ice Complex extent of Cape Mamontov Klyk, which excludes the hill range in the southwest with outcropping bedrock and rocky slope debris, coastal barrens, and a large sandy floodplain area in the southeast. The mapped features (streams, intermittent streams) were then visually compared with panchromatic Landsat-7 ETM+ satellite data (4 August 2000, 15 m spatial resolution) and panchromatic Hexagon data (14 July 1975, 10 m spatial resolution). Smaller valleys and gullies not captured in the maps were subsequently digitized from the satellite data. The criterion for the mapping of linear features as thermo-erosional valleys and gullies was their clear incision into the surface with visible slopes. Thermo-erosional features of the Lena Delta site were mapped on the basis of a Landsat-7 ETM+ image mosaic (2000 and 2001, 30 m ground resolution) [Schneider et al., 2009] and a Hexagon satellite image mosaic (1975, 10 m ground resolution) [G. Grosse, unpublished data] of the Lena River Delta within the extent of the Lena Delta Ice Complex [Morgenstern et al., 2011]. For the Buor Khaya Peninsula, data from Arcos [2012], which had been digitized based on RapidEye satellite data (8 August 2010, 6.5 m ground resolution), were completed for smaller thermo-erosional features using the same RapidEye scene as a mapping basis. The spatial resolution, acquisition date, time of the day, and viewing geometry of the satellite data used may have influenced the identification of thermo-erosional landforms in the images. For Cape Mamontov Klyk and the Lena Delta, thermo-erosional features were digitized using both Hexagon and Landsat data; Hexagon provided higher resolution and Landsat provided the modern extent of features. Allowance of up to decameters was made for the lateral expansion of features between Hexagon and Landsat acquisitions (between 1975 and 2000).
description: - Geospatial data presentation form: vector data- Native data set environment: ESRI ArcINFO- Access instructions: GIS application needed for viewing files
DOI: 10.1594/pangaea.619018
title: Water temperature profile LD02-1bk
DOI: 10.1594/pangaea.836153
title: Source data for Plos ONE publication Redefining thermal regimes to design reserves for coral reefs in the face of climate change

description: Reef managers cannot fight global warming through mitigation at local scale, but they can use information on thermal patterns to plan for reserve networks that maximize the probability of persistence of their reef system. Here we assess previous methods for the design of reserves for climate change and present a new approach to prioritize areas for conservation that leverages the most desirable properties of previous approaches. The new method moves the science of reserve design for climate change a step forwards by: (1) recognizing the role of seasonal acclimation in increasing the limits of environmental tolerance of corals and ameliorating the bleaching response; (2) including information from several bleaching events, which frequency is likely to increase in the future; (3) assessing relevant variability at country scales, where most management plans are carried out. We demonstrate the method in Honduras, where a reassessment of the marine spatial plan is in progress.
description: Data source: Sea surface temperature from the AVHRR Pathfinder v5.2. Methods: as described in manuscript. Extent: reef areas within the Caribbean basin (8-58N, 58-89W). Reef areas as described by the World Resources Institute (http://www.wri.org/publication/reefs-at-risk-revisited) with a 4 km buffer. File format: geotiff
description: Supplement to: Chollett, Iliana; Enríquez, Susana; Mumby, Peter John: Redefining thermal regimes to design reserves for coral reefs in the face of climate change. PLoS ONE
DOI: 10.1594/pangaea.874948
title: Terrigenous sortable silt of sediment core GeoB13861-1

description: Sortable silt (10 - 63 µm) arithmetical mean size (SSmean in µm) and percentage (SS%) values can be tightly linked to hydrodynamic processes and can be used as a relative flow-strength indicator. Thus, sortable silt proxies give evidence for shifts in water mass circulations strength with low (high) SSmean and SS% indicative for weak (strong) current strength.
DOI: 10.1594/pangaea.707630
title: Meteorological synoptical observations from station Payerne (2002-11)
DOI: 10.1594/pangaea.874952
title: X-ray flourescence FeK of sediment core GeoB13861-1

description: X-ray fluorescence (XRF) scans of the sediment cores were performed at 1 cm intervals. We applied generator settings of 10kV, a current of 0.2 mA directly at the split core surface of the archive halves using the AVAATECH XRF Core Scanner II (AVAATECH Serial No. 2) at the MARUM - University of Bremen.
DOI: 10.1594/pangaea.873859
title: (Table 1) Radiocarbon dating of sediment core GeoB17623-2
DOI: 10.1594/pangaea.805114
title: (Table 1) Paleomagnetism at DSDP Hole 83-504B
DOI: 10.1594/pangaea.894674
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018020212

description: INITIALIZATION: 2018020212FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NPARAMETERS: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.894675
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018022112

description: INITIALIZATION: 2018022112FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ANTu0.08 -- 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.705101
title: Age model of sediment core GeoB7920-2

description: Tie points to stck benthic isotope record of MD95 2042 on GRIP ss09sea timescale: Reference: Absolute calibration of the Greenland time scale: implications for Antarctic time scales and for D14C (N.J Shackleton, R.G Fairbanks, Tzu-chien Chiu, F. Parrenin, Quaternary Science Reviews 23 (2004) 1513-1522), Reference: Phase relationships between millennial scale events 64000 to 24000 years ago (N.J.Shackleton, M.A. Hall and E. Vincent, Paleoceanography, Vol. 15, no. 6, (2000), 565-569)
DOI: 10.1594/pangaea.705111
title: Continental humidity index of sediment core GeoB7920-2
DOI: 10.1594/pangaea.860003
title: Bulk mineralogy of Heihai lake sediment core PG2059-2
DOI: 10.1594/pangaea.705503
title: X-ray fluorescence dry sample measurements on sediment core GeoB7920-2, raw data
DOI: 10.1594/pangaea.855513
title: Individual codes, GenBank accession numbers and GenBank accession links for Mediterranean marine sponge associated actinomycetes
DOI: 10.1594/pangaea.705504
title: X-ray fluorescence wet sample measurements on sediment core GeoB7920-2, raw data
DOI: 10.1594/pangaea.792703
title: (Table 4) Colors of bentonite and DSDP Hole 92-504B mud
DOI: 10.1594/pangaea.860011
title: (Fig. 3b) Membership degrees of Heihai sediment core PG2059-1 to mineralogical cluster C1 to C4
DOI: 10.1594/pangaea.855521
title: Individual codes, GenBank accession numbers and GenBank accession links for Mediterranean sponges

description: Metabolomic analysis has shown the chemical richness of the sponge-associated actinomycetes Streptomyces sp. SBT349, Nonomureae sp. SBT364, and Nocardiopsis sp. SBT366. The genomes of these actinomycetes were sequenced and the genomic potential for secondary metabolism was evaluated. Their draft genomes have sizes of 8.0, 10, and 5.8Mb having 687, 367, and 179 contigs with a GC content of 71.6, 70.7, and 72.7%, respectively. Moreover, antiSMASH 3.0 predicted 108, 149, and 75 secondary metabolite gene clusters, respectively which highlight the metabolic capacity of the three actinomycete species to produce diverse classes of natural products.
description: Supplement to: Horn, Hannes; Cheng, Cheng; Edrada-Ebel, RuAngelie; Hentschel, Ute; Abdelmohsen, Usama Ramadan (2015): Draft genome sequences of three chemically rich actinomycetes isolated from Mediterranean sponges. Marine Genomics
DOI: 10.1594/pangaea.863011
title: Sea surface temperature reconstruction based on TEX86 for sediment core MD98-2195
DOI: 10.1594/pangaea.874941
title: Bulk grain size of sediment core GeoB13823-2
DOI: 10.1594/pangaea.862109
title: Bulk geochemistry of Lake Tiefer See sediments
DOI: 10.1594/pangaea.862114
title: Varve age model of Lake Tiefer See sediments
DOI: 10.1594/pangaea.872076
title: Calcium/Titanium ratios of IODP Hole 339-U1385A
DOI: 10.1594/pangaea.787764
title: Bulk components of sediment core PG1784
DOI: 10.1594/pangaea.806216
title: Evaporation measured on Samoylov Island, 2008
DOI: 10.1594/pangaea.862132
title: Characterization of the defined MDC types and compilation of MDC initiation times (excel-file 19 kB)

description: Mud accumulates on continental shelves under a variety of environmental conditions and results in a diverse formation of mud depocenters (MDCs). Their three-dimensional architectures have been in the focus of several recent studies. Due to some terminological confusion concerning MDCs, the present study sets out to define eight individual MDC types in terms of surface sediment distribution and internal geometry. Under conditions of substantial sediment supply, prodeltas (distal zones off river deltas; triangular sheets), subaqueous deltas (disconnected from deltas by strong normal-to-shore currents; wedge-like clinoforms), and mud patches (scattered distribution) and mud blankets (widespread covers) are formed. Forced by hydrodynamic conditions, mud belts in the strict sense (detached from source; elongated bodies), and shallow-water contourite drifts (detached from source; growing normal to prevailing current direction; triangular clinoforms) develop. Controlled by local morphology, mud entrapments (in depressions, behind morphological steps) and mud wedges (triangular clinoforms growing in flow direction) are deposited. Shelf mud deposition took place (1) during early outer-shelf drowning (~14 ka), (2) after inner-shelf inundation to maximum flooding (9.5-6.5 ka), and (3) in sub-recent times (&lt;2 ka). Subsequent expansion may be (1) concentric, in cases where the depocenter formed near the fluvial source, (2) uni-directional, extending along advective current transport paths, and (3) progradational, forming clinoforms that grow either parallel or normal to the bottom current direction. Classical mud belts may be initiated around defined nuclei, the remote sites of which are determined by seafloor morphology rather than the location of the source. From a stratigraphic perspective, mud depocenters coincide with sea-level highstand-related, shelf-wide condensed sections. They often show a conformable succession from transgressive to highstand systems tract stages.
description: Supplement to: Hanebuth, Till J J; Lantzsch, Hendrik; Nizou, Jean (2015): Mud depocenters on continental shelves—appearance, initiation times, and growth dynamics. Geo-Marine Letters, 35(6), 487-503
DOI: 10.1594/pangaea.787766
title: Bulk components of sediment core PG1900
DOI: 10.1594/pangaea.806202
title: Thaw depth measured on Samoylov Island, 2002-2010
DOI: 10.1594/pangaea.806225
title: Snow density of snow pit 5 on Samoylov Island, 2008
DOI: 10.1594/pangaea.787769
title: Calcium intensity of sediment core PG1784
DOI: 10.1594/pangaea.787770
title: Sr/Ca ratios and Calcium intensity of sediment core PG1900
DOI: 10.1594/pangaea.869662
title: Land cover, land use and human impact control 3

description: LC3c - A third choice for third land cover present if it was difficult and/or we could not agree on third land cover not observed.
DOI: 10.1594/pangaea.787771
title: Sr/Ca ratios and Calcium intensity of sediment core PG1901
DOI: 10.1594/pangaea.619014
title: Hydrometeorological characteristics along the New Siberian Island coast during Expedition LENA 2002 (Table A5.3.4-2)
DOI: 10.1594/pangaea.870082
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_II_07b
DOI: 10.1594/pangaea.872077
title: Calcium/Titanium ratios of IODP Hole 339-U1385B
DOI: 10.1594/pangaea.872079
title: Calcium/Titanium ratios of IODP Hole 339-U1385E
DOI: 10.1594/pangaea.787772
title: Sr/Ca ratios and Calcium intensity of sediment core PG1904
DOI: 10.1594/pangaea.806228
title: Snow density of snow pit 8 on Samoylov Island, 2008
DOI: 10.1594/pangaea.872080
title: Calcium/Titanium ratios of IODP Site 339-U1385
DOI: 10.1594/pangaea.806215
title: Water discharge measured on Samoylov Island, 2006-2011
DOI: 10.1594/pangaea.872081
title: Color reflectance of IODP Site 339-U1385
DOI: 10.1594/pangaea.872066
title: (Table S1) Shipboard composite and corrected composite depths of IODP Site 339-U1385
DOI: 10.1594/pangaea.743920
title: Binocular component analysis performed on the grain-size fraction 250–500 µm on 325 samples from the NW Iberian continental shelf
DOI: 10.1594/pangaea.806222
title: Snow density of snow pit 2 on Samoylov Island, 2008