cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.749977
title: Meteorological observations during KOERIER cruise from Curacao to St. Eustatius started at 1829-02-10
DOI: 10.1594/pangaea.807765
title: (Table 2) Trace elements at DSDP Hole 80-550
DOI: 10.1594/pangaea.814079
title: Availability of photographs from the Vernagtferner Basin for the year 1984
DOI: 10.1594/pangaea.727680
title: Lithology, colour and structural description of sediment profile Oy7-08-E, Appendix 6.1
DOI: 10.1594/pangaea.901633
title: Beach profile data for the Elwha River Delta, 2018-01-04

description: Data were collected using GNSS survey methods, with a differential GPS operating in Real Time Kinematic (RTK) mode. Data from prior to 2013 were typically collected with a Magellan ProMark 3 traditional RKT-DGPS system (i.e. local base station and rover), with the base station sited on survey control markers installed in 1996, with survey control coordinates referenced to NAD83(CORS91). Starting in 2013 survey data were typically collected with an AshTech ProMark 200 RTK-DGPS system connected to the Washington State Reference Network. Survey data collected between January and November 2013 are referenced to NAD83(CORS96), and after November 2013 to NAD83(2011). Vertical data for surveys in 2012 and 2013 are referenced to NAVD88, presumably using Geoid96 (the survey control documentation does not specific a geoid). For all subsequent surveys the vertical data are referenced to NAVD88(Geoid09). No conversion were applied to these data to account for variations in horizontal or vertical coordinate system adjustments through time, but an error analysis suggests a standard deviation for the elevation data of between 0.03 and 0.05 m across the entire sampling period (2011-2018). All survey data were collected with the GNSS system mounted on a 2.05 m rover pole, held level as a transect line was traced in a cross-shore orientation on the beach. The associated text files include the horizontal (HRMS) and vertical (VRMS) root-mean-square errors estimated by the GNSS system, as well as the RTK-DGPS status reported by the GNSS system at the time each point was collected. Times are referenced to local Pacific time (either PST or PDT).
DOI: 10.1594/pangaea.889233
title: Shipborne visual observations of Arctic sea ice during Louis S. St-Laurent cruise LSL1107
DOI: 10.1594/pangaea.849467
title: Ground-penetrating radar (GPR) point measurements of ice thickness on Oestlicher Wannetferner in 2010
DOI: 10.1594/pangaea.708161
title: (Table 2) Lithium contents and isotopic composition in sediments from ODP Hole 152-918D

description: d6Li data are given relative to a NBS standard L-SVEC.
DOI: 10.1594/pangaea.752592
title: Meteorological observations during UTRECHT cruise from Kaapstad to Batavia started at 1783-12-02
DOI: 10.1594/pangaea.740188
title: Age determination of sediment core BASVILLE, Basse-Ville, France

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.843237
title: Other measurements at 10 m from station Darwin (2010-01)

description: Version 2, 2015-02-25
DOI: 10.1594/pangaea.665546
title: Oceanography at CTD/bottle station IFREMER_2386
DOI: 10.1594/pangaea.750016
title: Meteorological observations during KOMEET cruise from La Guayra to Porto Cabello started at 1820-12-21
DOI: 10.1594/pangaea.780128
title: Biogeochemical analysis in sediments of the Var turbidity system from ENVAR4_MTB_13

description: The data set describes biogeochemical composition of sediment samples from the Var turbidite system.
DOI: 10.1594/pangaea.901924
title: Other measurements at 10 m from station Sioux Falls (2018-08)
DOI: 10.1594/pangaea.758475
title: (Table 13) Distribution of radiolaria in Miocene to Pleistocene sediments of DSDP Hole 30-289

description: Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent.
DOI: 10.1594/pangaea.740225
title: Age determination of sediment core BOSHEI3, Bosscherheide, Netherlands

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.823680
title: The North Sea autumn spawning Herring (Clupea harengus L.) Spawning Component Abundance Index (SCAI)

description: The North Sea autumn-spawning herring (Clupea harengus) stock consists of a set of different spawning components. The dynamics of the entire stock have been well characterized, but although time-series of larval abundance indices are available for the individual components, study of the dynamics at the component level has historically been hampered by missing observations and high sampling noise. A simple state-space statistical model is developed that is robust to these problems, gives a good fit to the data, and proves capable of both handling and predicting missing observations well. Furthermore, the sum of the fitted abundance indices across all components proves an excellent proxy for the biomass of the total stock, even though the model utilizes information at the individual-component level. The Orkney–Shetland component appears to have recovered faster from historic depletion events than the other components, whereas the Downs component has been the slowest. These differences give rise to changes in stock composition, which are shown to vary widely within a relatively short time. The modelling framework provides a valuable tool for studying and monitoring the dynamics of the individual components of the North Sea herring stock.
description: The North Sea Autumn Spawning (NSAS) herring (Clupea harengus L.) spawning component abundance index (SCAI) provides relative indices of the four main sub-components of the NSAS herring stock. This fish stock has been surveyed annually on the main spawning grounds (Orkney/Shetland, Buchan, Banks and Downs, along the east-coast of Great Britain) at spawning time by the International Herring Larval Surveys (IHLS) from 1972 until the present. However, gaps and systematic biases in these surveys are present and limit the usefulness of this data. The SCAI is the output of a state-space statistical model that accounts for these problems in a statistically appropriate manner. The SCAI provides a consistent index of the abundance of the spawning components (at spawning time) relative to each other and over time and is therefore valuable in the study of both the total population of this stock, and of the individual sub-components.
description: Supplement to: Payne, Mark R (2010): Mind the gaps: a state-space model for analysing the dynamics of North Sea herring spawning components. ICES Journal of Marine Science, 67(9), 1939-1947
DOI: 10.1594/pangaea.889162
title: Shipborne visual observations of Arctic sea ice during Arctic Sunrise cruise ArcSun1209
DOI: 10.1594/pangaea.895672
title: Effect of salinity and burial on succinate dehydrogenase and adenosinetriphosphatase in Mya arenaria

description: Bioturbators (such as bivalves, worms, polychaetes), living in a coastal area, experiences frequent changes in salinity. They are often exposed to mechanical disturbances (like wave, currents, storms) forcing them to bury deeper into the sediment to get a better foothold. In nature, these stressors often occurs simultaneously. Osmotic stress negatively affects the burial activity and the physiological performances of soft shell clam, Mya arenaria; however, the mechanism behind this is still unknown. In this dataset we present the effect of different salinity regime on the burial activity of Mya arenaria, as well as the combined effect of osmotic stress and repeated burrowing on the succinate dehydrogenase and ATPase activity in foot muscle of Mya arenaria.
description: We measured the activity of SDH and ATPase in the foot muscle of Mya arenaria by staining the foot cross-section with specific dye (nitroblue tetrazolium and cobalt chloride for SDH and ATPase, respectively). The percentage of area stained in the foot cross-section is equivalent to the activity of these enzymes.
DOI: 10.1594/pangaea.746592
title: Meteorological observations during La Danaé cruise from La Martinique to Brest started at 1765-07-17
DOI: 10.1594/pangaea.748483
title: Meteorological observations during DESCONOCIDO-06 cruise from Buenos Aires to Montevideo started at 1805-04-01
DOI: 10.1594/pangaea.730138
title: (Table 9) Secondary minerals from the main basalt mass of the California Gulf, DSDP Hole 65-485A
DOI: 10.1594/pangaea.740717
title: Age determination of sediment core SANDVIK, Sandvikvatn, Norway

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.748479
title: Meteorological observations during DESCONOCIDO-03 cruise from Montevideo to Isla Del Principe started at 1778-04-17
DOI: 10.1594/pangaea.771088
title: (Table 2) Rock magnetic properties of serpentinize sediments from ODP Leg 125
DOI: 10.1594/pangaea.499674
title: Physical oceanography from BT during cruise UXXXX00131B_1959
DOI: 10.1594/pangaea.739286
title: Pollen profile GUTT, Nowy Gutiski, Ukraine

description: L. Post method.The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.750617
title: Meteorological observations during Maria Elisabeth cruise from Padang to the Netherlands started at 1848-01-19
DOI: 10.1594/pangaea.811485
title: (Tables 1,2) Viability of Poa trivialis seeds transported to Antarctica from different locations

description: Antarctic ecosystems are at risk from the introduction of invasive species. The first step in the process of invasion is the transportation of alien species to Antarctic in a viable state. However, the effect of long-distance human-mediated dispersal, over different time-scales, on propagule viability is not well known. We assessed the viability of Poa trivialis seeds transported to Antarctica from the UK, South Africa and Australia by ship or by ship and aircraft. Following transportation to the Antarctic Treaty area, no reduction in seed viability was found, despite journey times lasting up to 284 days and seeds experiencing temperatures as low as -1.5°C. This work confirms that human-mediated transport may overcome the dispersal barrier for some propagules, and highlights the need for effective pre-departure biosecurity measures.
description: Temperature data refer to transported seeds. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
description: Supplement to: Hughes, Kevin A; Lee, Jennifer E; Ware, Chris; Kiefer, K; Bergstrom, Dana Michelle (2010): Impact of anthropogenic transportation to Antarctica on alien seed viability. Polar Biology, 33(8), 1125-1130
DOI: 10.1594/pangaea.735951
title: (Table 7) Mineralogy of ODP Hole 104-644B

description: &lt;1 = trace, T = trace, P = present, - = absent
DOI: 10.1594/pangaea.761024
title: (Table 2) Sr, Nd, and Pb isotope ratios of ODP Site 123-765 basalts
DOI: 10.1594/pangaea.905027
title: Broadband radiation measurements (package 2) during the Arctic field campaign PASCAL in June 2017 (Balloon_Balu2_20170608_0904_1250)
DOI: 10.1594/pangaea.694814
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station FEBR-1998-IR44

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore filters. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).
DOI: 10.1594/pangaea.749159
title: Meteorological observations during El Rey cruise from La Coruña to Montevideo started at 1795-06-19
DOI: 10.1594/pangaea.748018
title: Meteorological observations during CURACAO cruise from Curacao to Hellevoetsluis started at 1842-05-18
DOI: 10.1594/pangaea.762575
title: Description of lithologic section units of IODP Hole 325-M0032A
DOI: 10.1594/pangaea.726989
title: Particulate organic matter measured in surface sediments at Island Bone Batang, Spermonde Archipelago, Indonesia

description: Samples taken at a mean depth of 0.4 m below spring low water. Along each belt transect three surface sediment samples were taken by usingsmall hand corers while snorkelling (diameter = 6 cm; depth = 5 cm).
DOI: 10.1594/pangaea.817786
title: (Table 3) Quantification of sample disturbance from IODP Sites 317-U1351, 317-U1352, 317-U1353 and 317-U1354

description: DEPTH, sediment/rock = Depth CSFA (m)
DOI: 10.1594/pangaea.751801
title: Meteorological observations during ROTTERDAM cruise from Padang to Batavia started at 1843-02-19
DOI: 10.1594/pangaea.763428
title: (Table 4) Sr, Nd and Pb isotopic variations of the Upper Series magmas from ODP Hole 104-642E
DOI: 10.1594/pangaea.854429
title: (Table 1) Distribution and abundance of conodonts at profile Steinbruch am Hessenkamp

description: + Fauna aus Spaltenfüllung; ++ Fauna aus dem Trägergestein
DOI: 10.1594/pangaea.740720
title: Age determination of sediment core SAVI, Mire Saviku, Estonia

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.754376
title: Organic geochemical parameters in sediment samples from the Weddell Sea (Table 2)

description: Heavy hydrocarbons (~C15 + ) are ubiquitous but minor components in sediment from three sites (692, 693, and 694) drilled during Ocean Drilling Program (ODP) Leg 113. This preliminary report is the first to describe the distribution of some of these hydrocarbons in sediment of the Weddell Sea. Samples from Sites 692 and 693, located on a midslope bench along the margin of Dronning Maud Land, span a time interval from Early Cretaceous to Pleistocene. In our samples from the Tertiary portion of the record, having an average organic-carbon content of about 0.2%, n-alkanes are common and are characterized by populations that indicate both marine and terrigenous sources. The alpha beta-hopanes and aaa-steranes are minor components with isomer ratios indicating partial to full maturity. In contrast, our samples from the Cretaceous portion of the record, having an average organic carbon content of about 4%, contain mixtures of hydrocarbons in which n-alkanes are secondary in abundance to the isoprenoid hydrocarbons, pristane and phytane. Diasterenes, sterenes, and hopenes are present in anomalously high concentrations and indicate immaturity. The Cretaceous hydrocarbons appear to be mainly primary, whereas the Tertiary hydrocarbons contain compounds that indicate that the sediment, along with its organic content, has been recycled. Our samples from Site 694, located in the Weddell Sea on the abyssal plain, range in age from late Miocene to early Pliocene, have an average organic-carbon content of about 0.2%, and contain n-alkanes with a strong terrigenous signature. Isomer ratios of alpha beta-hopanes and aaasteranes indicate intermediate maturity; diasterenes, sterenes, and hopenes are absent. The hydrocarbons at this site are mainly recycled and indicate erosion of previously buried sediment from the continent of Antarctica.
description: Supplement to: Kvenvolden, Keith A; Horstettler, Frances D; Frank, Tamara J (1990): Hydrocarbons in sediment of the Weddell Sea, Antarctica. In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 199-208
DOI: 10.1594/pangaea.774179
title: (Table T3) Sediment concentrations of major and trace elements for ODP Sites 202-1233 and 202-1234

description: The exchange of waters between the Pacific and the Southern Oceans occurs along the eastern boundary of the South Pacific. Because water masses of the Antarctic provide a connection among the world's ocean basins, these water masses maintain the ability to influence changes in ocean circulation and climate (Lynch-Stieglitz et al., 1996, doi:10.1029/95PA03772). One of the primary goals of Ocean Drilling Program (ODP) Leg 202 was to exploit the sediments underlying the southeast Pacific continental margin to ascertain how changes in past ocean circulation (i.e. water mass distributions) have affected global carbon, heat, and nutrient balances.Sediments at Site 1233 are bathed by oxygen-rich Antarctic Intermediate Water at a water depth of 838 m, whereas Pacific Central Water bathes the overlying waters at Site 1234. Site 1234 is located north of Site 1233 at 1015-m water depth. Because of rapid erosion of the high Andes, terrigenous sedimentation rates at these sites are in the range of 1-2 m/k.y. To assess changes in the reducing nature of these sediments through time, a number of geochemical indicators were determined. The solubility of uranium, molybdenum, cadmium, and vanadium decreases under the reducing conditions common along the continental margin seafloor; thus changes in their distribution may signify changes in the reducing character of the surface sediment. A number of other, primarily ancillary, elements were also measured. Most of these elements are used to assess terrigenous inputs.
description: Sediment depth is given in mcd. Samples were prepared using acid hotplate digestion.
description: Supplement to: McManus, James (2006): Data report: major and trace element data for Leg 202 Sites 1233 and 1234. In: Tiedemann, R; Mix, AC; Richter, C; Ruddiman, WF (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 202, 1-9
DOI: 10.1594/pangaea.747058
title: Meteorological observations during SCORPION cruise from Cadiz to Charleston started at 1751-02-11
DOI: 10.1594/pangaea.750936
title: Meteorological observations during Nieuwe Hoop cruise from Middelburg to Kaap Masurado started at 1779-03-29
DOI: 10.1594/pangaea.747419
title: Meteorological observations during ANTHONY cruise from Batavia to Rotterdam started at 1829-04-24
DOI: 10.1594/pangaea.864524
title: Other measurements at 10 m from station Fort Peck (2011-04)
DOI: 10.1594/pangaea.911019
title: Grain size distributions of sand samples from Owens lake site T29-3 in central California, collected in 2016
DOI: 10.1594/pangaea.587149
title: Physical oceanography at CTD station M1_CTD267 of the Persian Gulf
DOI: 10.1594/pangaea.756720
title: (Table 16) Ranges of benthic foraminifers through the Neogene in ODP Hole 115-710A

description: Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because benthic foraminifers are not common in most samples, in many instances the numbers represent their true abundance in a sample. Only the bolivinids reached abundances of 6 or greater.
DOI: 10.1594/pangaea.869032
title: Other measurements at 10 m from station Fort Peck (2013-11)
DOI: 10.1594/pangaea.908845
title: Improved Antarctic-Wide Ice Flow Maps from Landsat 8 Imagery

description: Here, we present a methodology which can automatically calibrate, mosaic, and post-process Landsat images into displacement maps, resulting in seamless, continent-wide, ice velocity products. Using this developed methodology, we have assembled over 200,000 displacement maps to generate Antarctic-wide annual mosaics of ice velocity maps from more than 70,000 Landsat 8 images acquired between December 2013 and April 2019. The new suite of annual Antarctic ice velocity maps at 105-m grid spacing provide the clearest picture of Antarctic-wide ice flow to-date, and error analysis via comparisons with various available prior ice velocity data products and in situ data confirmed the improved accuracy of this new data product.
DOI: 10.1594/pangaea.770482
title: (Table 3) Grain-size analyses for ODP Leg 126 samples
DOI: 10.1594/pangaea.794481
title: (Table 6) δ¹⁸O, carbon composition, bulk densities, accumulation rates and ages of core EW9504-17PC
DOI: 10.1594/pangaea.746922
title: Meteorological observations during FREDEN cruise from Gothenburg to Canton started at 1748-02-19
DOI: 10.1594/pangaea.755854
title: Tab. 2: Ice salinity, flexural strenght, and Young's Modulus
DOI: 10.1594/pangaea.755390
title: (Table 1) Distribution of Quaternary to Eocene calcareous nannofossils in ODP Hole 114-699A

description: Species abundances: A = abundant (&gt;30 %), C = common (30-15 %), F = few (15-3 %), R = rare (&lt;3%), - = not present.
DOI: 10.1594/pangaea.888576
title: Crystal c-axes (fabric analyser G50) of ice core samples (vertical thin sections, full bag measurements) collected from the polar ice core EDML, 2359-2380 m depth (2015)

description: 40 sections measured with Fabric Analyser.Size of thin sections: ca. 6.7 x 9 cm²Resolution: 500 px/cm (FA), images are horizontally mirrored to each other.Measured at Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany.
DOI: 10.1594/pangaea.726086
title: (Table 2) Age model of sediment core CH73-110
DOI: 10.1594/pangaea.899010
title: Radiosonde measurements from station Payerne (2018-10)
DOI: 10.1594/pangaea.900190
title: Other measurements at 10 m from station Fort Peck (2018-10)
DOI: 10.1594/pangaea.752674
title: Meteorological observations during VENUS cruise from Paramaribo to Cayenne started at 1842-05-19
DOI: 10.1594/pangaea.740190
title: Age determination of sediment core BEBR5, Bebrukas Lake, Lithuania

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.720137
title: Radiosonde measurements from station Desert Rock (2002-02)

description: Version 2, 2009-06-16; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.740226
title: Age determination of sediment core BOUARA, Bouara, Syrian Arab Republic

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.726940
title: In vivo growth rates of Pinna muricata at Island Bone Batang, Spermonde Archipelago, Indonesia

description: Samples taken at a mean depth of 0.4 m below spring low water
DOI: 10.1594/pangaea.744147
title: Physical oceanography during Cirolana cruise Cirolana74/2 to the North Sea
DOI: 10.1594/pangaea.740213
title: Age determination of sediment core BJARSJON, Bjarsjon, Sweden

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.747532
title: Meteorological observations during ASTUTO cruise from El Callao de Lima to Cádiz started at 1778-03-13, Version 7
DOI: 10.1594/pangaea.726094
title: (Table 2) Age model of sediment core V27-60
DOI: 10.1594/pangaea.750424
title: Meteorological observations during LESPERANCE cruise from Tongatabou to Nouvelle Caledonie started at 1793-04-10
DOI: 10.15468/dl.h9t76d
title: Occurrence Download

description: A dataset containing 8 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is China",
 "GadmGid is CHN.19_1",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "TaxonKey is Scorzonera sinensis Lipsch. & Krasch."
 ]
}

 The dataset includes 8 records from 2 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031123-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.789347
title: (Table 1) CaCO3, organic carbon, and nitrogen at DSDP Hole 93-603B (shipboard samples)
DOI: 10.1594/pangaea.726095
title: (Table 2) Age model of sediment core V27-86
DOI: 10.1594/pangaea.747244
title: Meteorological observations during AJAX cruise from Boston to Texel started at 1814-10-19
DOI: 10.1594/pangaea.664159
title: Oceanography at CTD/bottle station IFREMER_1000
DOI: 10.1594/pangaea.751533
title: Meteorological observations during PRINCIPE cruise from La Coruña to Montevideo started at 1776-12-15
DOI: 10.1594/pangaea.883902
title: Temperature and pressure measurements from 2014 from mooring SA in the Weddell Sea