cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.931721
title: Depth-age model of the B18_2012 firn core

description: Using raw, un-calibrated dielectrical profiling (DEP) data from the field (NEEM Set-up), volcanic tie points were derived. Together with the smoothed density data and the isotopic composition the record was dated by layer counting.
DOI: 10.1594/pangaea.496860
title: Physical oceanography from BT during cruise K90AIB_1959
DOI: 10.1594/pangaea.870351
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2009/10_21
DOI: 10.1594/pangaea.694183
title: Nutrient concentrations in water samples from the Ionian Sea at Station MARCH-2000-IKE1
DOI: 10.1594/pangaea.881353
title: Documentation of sediment core K7905-056GC
DOI: 10.15468/dl.uawa7m
title: Occurrence Download

description: A dataset containing 59 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "TaxonKey is Nymphargus rosada (Ruiz-Carranza & Lynch, 1997)"
 ]
}

 The dataset includes 59 records from 7 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031185-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.924876
title: DMS production and consumption rates (2014.5)
DOI: 10.1594/pangaea.499688
title: Physical oceanography from BT during cruise UXXXX00423B_1975
DOI: 10.1594/pangaea.931704
title: Stable oxygen isotope profile of the B21_2012 firn core, annual means

description: Stable oxygen isotopes (δ18O) were measured on discrete samples using Cavity Ring-Down spectroscopy with an L2120-i and L2130-i by Picarro Instruments. The δ18O concentration with depth is provided with a precision of better than 0.1 per mil. Using raw, un-calibrated dielectrical profiling (DEP) data from the field (NEEM Set-up), volcanic tie points were derived. Together with the smoothed density data and the isotopic composition the record was dated by layer counting. The annual mean values of δ18O were obtained based on this dating.
DOI: 10.1594/pangaea.694212
title: Nutrient concentrations in water samples from the Ionian Sea at Station MARCH-2000-IRI22
DOI: 10.1594/pangaea.870344
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2009/10_14
DOI: 10.1594/pangaea.870337
title: Links to master tracks in different resolutions from POLAR 6 flight WEGAS_1201042601
DOI: 10.1594/pangaea.931722
title: Depth-age model of the B21_2012 firn core

description: Using raw, un-calibrated dielectrical profiling (DEP) data from the field (NEEM Set-up), volcanic tie points were derived. Together with the smoothed density data and the isotopic composition the record was dated by layer counting.
DOI: 10.1594/pangaea.706019
title: Documentation of sediment core GIK15663-2
DOI: 10.1594/pangaea.870341
title: Links to master tracks in different resolutions from POLAR 6 flight WEGAS_1201083101
DOI: 10.1594/pangaea.693626
title: Distribution of calcareous nannofossils in Cretaceous to Paleogene sediments of ODP Hole 208-1262C at Walvis Ridge, South Atlantic Ocean (Appendix A)

description: Site 1262 in the South Atlantic Ocean has provided a stratigraphically continuous deep Cretaceous/Paleogene boundary sequence. High resolution calcareous nannofossil quantitative analyses were carried out across the K/P boundary, and provided a remarkable record of the abrupt and catastrophic extinction. The calcareous nannofossil assemblages are abundant and well preserved allowing to obtain a precise bioevent sequence and to document in detail the survivors and victims and the subsequent recovery across the K/P boundary.Late Maastrichtian diversity and absolute abundance is high and no decrease towards the boundary has been observed. The relative abundance of Cretaceous species does not suffer important changes during the latest Maastrichtian. However, the increase in abundance of cool-water taxa, paralleled with a decrease of warm water taxa in the uppermost 2 cm of the Maastrichtian, revealed a pulse of surface water cooling.The K/P boundary is marked by an important decrease in calcareous nannofossil absolute abundance, the increase of Cretaceous-persistent species such as Cyclagelosphaera reinhardtii together with the dinoflagellate cysts of Thoracosphaera operculata and the appearance of the new-Paleocene taxa Cyclagelosphaera alta and Biantholithus sparsus. These events are followed by the successive relative abundance increases of other Cretaceous survivors as Zeugrhabdotus sigmoides, Markalius inversus and Biscutum recognized as r-selected taxa, adapted to eutrophic and cold water environments. In the early Danian several first occurrences of small new-Paleocene species have been observed: calcareous nannoplankton evolutionary attempts to colonize vacant niches left by the extinct Cretaceous species. Only some forms succeed and become ancestors to the Cenozoic assemblages - the other disappear in few kiloyear. The presence of a reworking/mixing interval above the K/P boundary hampered to unequivocally interpret if the few Cretaceous-vanishing taxa may have survived for a very short time after the K/P extinction.
description: &lt;1 = present
description: Supplement to: Bernaola, Gilen; Monechi, Simonetta (2007): Calcareous nannofossil extinction and survivorship across the Cretaceous-Paleogene boundary at Walvis Ridge (ODP Hole 1262C, South Atlantic Ocean). Palaeogeography, Palaeoclimatology, Palaeoecology, 255(1-2), 132-156
DOI: 10.1594/pangaea.672619
title: Basic and other measurements of radiation at station South Pole (1993-10)
DOI: 10.1594/pangaea.844987
title: The Austrian Glacier Inventory for the Little Ice Age Maximum (GI LIA) in ArcGIS (shapefile) format

description: Groß and Patzelt mapped the glacier areas for the Little Ice Age (LIA) maximum state from the position of the moraines and field surveys based on the orthophotos of the glacier inventory of 1969. As the Austrian federal authorities made LiDAR data available for the major part of Austria, these data have been used for the compilation of a new LIA glacier inventory based on LiDAR DEMs. As the high resolution data allow detailed mapping of LIA moraines, the unpublished maps of Groß have been used as the basis for an accurate mapping of the area and elevation of the LIA moraines, based on the LiDAR DEMs and the ice divides/glacier names used in the inventories 1969 and 1998. The date related to the glacier outlines in this inventory differs from glacier to glacier.
DOI: 10.1594/pangaea.849332
title: Ice thickness measurements on Langenferner, with link to results in ArcGIS format
DOI: 10.1594/pangaea.881363
title: Documentation of sediment core K7905-073BC
DOI: 10.1594/pangaea.881364
title: Documentation of sediment core K7905-074GC
DOI: 10.1594/pangaea.870342
title: Links to master tracks in different resolutions from POLAR 6 flight WEGAS_1201093201
DOI: 10.1594/pangaea.870346
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2009/10_16
DOI: 10.1594/pangaea.548279
title: Physical oceanography at CTD station Bm_1997-08-28_6, Bajo Molle, Chile
DOI: 10.1594/pangaea.881367
title: Documentation of sediment core K7905-079GC
DOI: 10.1594/pangaea.729234
title: (Table 2a) Paleocene calcareous nannofossils in ODP Hole 122-761B

description: species abundance: A = abundant (&gt;10 specimens per field of view at 1000 X), C = common (1-10 specimens), F = few (1 specimen in 2-10 fields), R = rare (1 specimen in 11-100 fields), V = very rare (1 specimen in 101-1000 fields), - = absent
DOI: 10.1594/pangaea.928738
title: Median grain size, water content, total carbon content, and total nitrogen content data in the sediment cores collected from the northern shore, southern shore, and inner lagoon of Dongsha Island (Table 2)
DOI: 10.1594/pangaea.854331
title: Mediterranean copepods' functional traits

description: Information on the functional traits was gathered for the most commonly-sampled copepod species of the Mediterranean Sea. Our database includes 191 species described by 7 traits encompassing diverse ecological functions: minimal and maximal body length (mm), trophic group (Omnivore/Carnivore/Herbivore/Detritivore), feeding type (Cruise-feeding/Filter-feeding/Ambush-feeding), spawning strategy (Sac-spawner/Free-spawner), diel vertical migration (Non-migrant/Weak-migrant/Strong-migrant) and vertical habitat (prefered depth layer). Using cluster analysis in the functional trait space revealed that Mediterranean copepods can be gathered into groups that have different ecological roles.
description: The xlsx file contains data on functional traits of Mediterranean copepods, as well as a list to all referred references. For further details on the methods used and on confidence indices of certain functional traits please refer to the article linked above, as well as its supplementary material. Do not hesitate to contact the first author for any questions (fabio.benedetti [at] obs-vlfr.fr).
description: Supplement to: Benedetti, Fabio; Gasparini, Stéphane; Ayata, Sakina-Dorothée (2016): Identifying copepod functional groups from species functional traits. Journal of Plankton Research, 38(1), 159-166
DOI: 10.1594/pangaea.870354
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2010/11_17
DOI: 10.1594/pangaea.928746
title: Seasonal diel pH, dissolved inorganic carbon, total alkalinity and partial pressure of CO2 data in the seagrass meadows of the inner lagoon and northern shore of Dongsha Island during the 2016–2019 study period (Table 3)
DOI: 10.1594/pangaea.773257
title: Microalgal CO2 Sequestering - Modeling Microalgae Production Costs

description: Microalgae CO2 sequestering facilities might become an industrial reality if microalgae biomass could be produced at cost below $500.00 t-1. We develop a model for estimation of total production costs of microalgae as a function of known production-specific expenses, and incorporate into the model the effects of uncontrollable factors which affect known production-specific expenses. Random fluctuations were intentionally incorporated into the model, consequently into generated cost/technology scenarios, because each and every logically interconnected equipment/operation that is used in design/construction/operation/maintenance of a production process is inevitably subject to random cost/price fluctuations which can neither be eliminated nor a priori controlled. A total of 152 costs/technology scenarios were evaluated to find forty four scenarios in which Predicted Total Production Costs of Microalgae (PTPCM) was in the range $200 to $500 t-1 ha-1 y-1. An additional 24 scenarios were found with PTCPM in the range of $102 to $200 t-1 ha-1 y-1. These findings suggest that microalgae CO2 sequestering and the production of commercial compounds from microalgal biomass can be economically viable venture even today when microalgae production technology is still far from its optimum.
description: Supplement to: Bilanovic, Dragoljub; Holland, Mark; Armon, Robert (2012): Microalgal CO2 sequestering - Modeling microalgae production costs. Energy Conversion and Management, 58, 104-109
DOI: 10.1594/pangaea.792934
title: Continuous meteorological observations at station Ny-Ålesund (2011-03)
DOI: 10.1594/pangaea.792935
title: Continuous meteorological observations at station Ny-Ålesund (2011-04)
DOI: 10.1594/pangaea.694177
title: Nutrient concentrations in water samples from the Ionian Sea at Station MARCH-2000-IAR03
DOI: 10.1594/pangaea.728949
title: (Table 3) Varimax factor loadings from factor analysis of ODP Hole 121-754A
DOI: 10.1594/pangaea.897648
title: Microwave-induced self-organization in mineral systems. III. FeCl3 colloid (200 W; 2.45 GHz; 1 min)

description: Microwave-induced self-organization of membraneous structures with different morphology in hydrolized FeCl3 colloid (200 W, 2.45 GHz,1 min). The local MW treatment conditions and the precoursor layer thickness determine the type of emerging structures.
DOI: 10.1594/pangaea.753172
title: Monthly mean δ¹⁸O values of ice core DML95C07_02 from 1981 to 2007
DOI: 10.1594/pangaea.924938
title: Concentration of sulfur compounds (DMSO) in microlayer in autumn
DOI: 10.1594/pangaea.924935
title: DMS production and consumption rates (2014.11)
DOI: 10.1594/pangaea.924932
title: Concentration of sulfur compounds in surface waters of the Bohai Sea and Yellow Sea in autumn (2014.11)
DOI: 10.1594/pangaea.681355
title: Radiosonde measurements from Georg-von-Neumayer Station (1985-08)
DOI: 10.1594/pangaea.870352
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2009/10_22
DOI: 10.1594/pangaea.871055
title: Quantitative genetic traits of Heracleum sphondylium from three different regions of Germany (Schwäbische Alb, Hainich-Dün, Schorfheide Chorin)
DOI: 10.1594/pangaea.931734
title: Density profile of the B18_2012 firn core

description: Density was measured by micro-focus Computer Tomography with a resolution of 0.1mm and subsequently smoothed with a Gaussian filter with sigma 2 cm.
DOI: 10.1594/pangaea.498725
title: Physical oceanography from BT during cruise U90X007575B_1976
DOI: 10.1594/pangaea.870357
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2010/11_20
DOI: 10.1594/pangaea.933833
title: Lithogenic properties of the spliced record of IODP Site 361-U1476 at the Davie Ridge, Mozambique Channel

description: Records of sortable silt (SS) percentages and means from the spliced record of IODP Site U1476 at the Davie Ridge, Mozambique Channel. The age model of this spliced record is based on benthic oxygen isotopes and biostratigraphy.
DOI: 10.1594/pangaea.706795
title: Documentation of sediment core GeoB9927-2
DOI: 10.1594/pangaea.886891
title: No-Take Zones in the Galapagos Marine Reserve, Zoning plan 2000

description: The Galapagos Marine Reserve (GMR) was created to protect the exceptional marine biodiversity it supports. It is a multi-use protected area where artisanal fishing, tourism and conservation are the main uses. In order to spatially regulate the different uses and ensure the conservation of the biodiversity, the first Zoning plan was created in 2000 classifying the coastline in sectors according to management/use subzones (fishing, tourism and conservation). Yet, no indication was stated as of how to resolve conflictive areas where several uses overlapped. To date, no study has addressed this issue despite the fact that the reserve has been in place for 20 years. This has created confusions in the compliance and enforcement of the reserve boundaries and complicates the calculation and analysis of take and no-take zones within the reserve. Here, I provide an interpretation of the subzoning of the reserve in order to resolve each of the conflictive areas following an objective set of rules which eventually allows the calculation of the areas open to fishing and the no-take zones. The resulting data set is a GIS layer (in ArcGIS shapefile format) of the GMR Zoning 2000 for the No-Take Zones (i.e. tourism and conservation). While a new Zoning plan is about to be effective soon, studies attempting to compare the effect of Take and No-Take Zones on target species and on the conservation of biodiversity during the 16-year period that the Zoning plan 2000 was in place as well as comparing Zoning 2000 with the new Zoning plan will benefit from this Dataset. This publication is contribution number 2194DS of the Charles Darwin Foundation for the Galapagos Islands.
description: This research was conducted on behalf of the Charles Darwin Foundation.
description: Supplement to: Moity, Nicolas (2018): Evaluation of No-Take Zones in the Galapagos Marine Reserve, Zoning Plan 2000. Frontiers in Marine Science, 5
DOI: 10.1594/pangaea.931728
title: Stable oxygen isotope profile of the B18_2012 firn core

description: Stable oxygen isotopes (δ18O) were measured on discrete samples using Cavity Ring-Down spectroscopy with an L2120-i and L2130-i by Picarro Instruments. The δ18O concentration with depth is provided with a precision of better than 0.1 per mil.
DOI: 10.1594/pangaea.924881
title: Concentration of sulfur compounds in surface waters of the Bohai Sea and Yellow Sea in summer (2015.8)
DOI: 10.1594/pangaea.869065
title: Documentation of sediment core GIK18405-3
DOI: 10.1594/pangaea.498602
title: Physical oceanography from BT during cruise U90TP07113B_1958
DOI: 10.1594/pangaea.869069
title: Documentation of sediment core GIK18414-3
DOI: 10.1594/pangaea.497181
title: Physical oceanography from BT during cruise M90PD95211B_1952
DOI: 10.1594/pangaea.690633
title: (Fig. 3) Stratigraphic distribution of upper Cretaceous calcareous nannofossils in the Bottaccione section, Italy

description: Point distance is the sample level (m). Species abundance: A = abundant (&gt;10 %), C = common (1-10 %), F = few (0.1-1 %), R = rare (&lt;0.1 %), - = not present
DOI: 10.1594/pangaea.869073
title: Documentation of sediment core GIK18418-2
DOI: 10.1594/pangaea.924884
title: DMS production and consumption rates (2015.8)
DOI: 10.1594/pangaea.913934
title: X-ray tomography data of columnar joints in starch

description: Columnar jointing is best-known from formations in cooled lava, such as the Giant's Causeway, Devil's Postpile, or Fingal's Cave. However, these crack patterns also arise in other systems, most notably in dried starch. The data published here underlies research into the dynamical ordering of columnar joints, and the process by which they select their size or scale (Goehring and Morris, 2005; Goehring, Morris and Lin, 2006).The data set consists of nine X-ray tomographs of columnar joints in dried starch, presented as both the raw instrument data and as series of reconstructed cross-sectional images throughout the volume of the samples. There is a mixture of samples where the drying rate was monitored but not controlled, which results in columns that grow in size with depth, and samples where the drying rate of the starch was controlled by a feedback technique, which results in columns of constant size. A summary spreadsheet gives metadata associated with each sample, including the instrument settings during data acquisition.This data and the methods of its acquisition will be further detailed in an accompanying data publication, which will also include details of 3D reconstructions of columnar joints in various geophysical settings in the UK and Japan.
DOI: 10.1594/pangaea.931723
title: Depth-age model of the B23_2012 firn core

description: Using raw, un-calibrated dielectrical profiling (DEP) data from the field (NEEM Set-up), volcanic tie points were derived. Together with the smoothed density data and the isotopic composition the record was dated by layer counting.
DOI: 10.1594/pangaea.871054
title: Quantitative genetic traits of Festuca rubra from three different regions of Germany (Schwäbische Alb, Hainich-Dün, Schorfheide Chorin)
DOI: 10.1594/pangaea.870358
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2010/11_21
DOI: 10.1594/pangaea.690673
title: Documentation of sediment core GIK12519-2
DOI: 10.1594/pangaea.496790
title: Physical oceanography from BT during cruise K58SOB_1937
DOI: 10.1594/pangaea.872169
title: Links to master tracks in different resolutions from POLAR 5 flight ANT_2008/09_10
DOI: 10.1594/pangaea.749489
title: Meteorological observations during GUADALOUPE cruise from Plymouth to Madeira started at 1770-04-05
DOI: 10.1594/pangaea.870383
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2010/11_46
DOI: 10.1594/pangaea.931731
title: Stable oxygen isotope profile of the NGRIP_2012 firn core

description: Stable oxygen isotopes (δ18O) were measured on discrete samples using Cavity Ring-Down spectroscopy with an L2120-i and L2130-i by Picarro Instruments. The δ18O concentration with depth is provided with a precision of better than 0.1 per mil.
DOI: 10.1594/pangaea.870386
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2010/11_49
DOI: 10.1594/pangaea.897650
title: Microwave-induced self-organization in mineral systems. IX. Diluted FeOOH sol obtained from FeCl3 and Na2CO3 solutions (2.45 GHz; 450 W; 1 min; check experiment)

description: Microwave-induced self-organization of ferric hydroxide colloids obtained from ferric chloride and sodium carbonate solutions results in the crystallization of different mineral phases, including the excess sodium carbonate, with the crystal morphology depending on the microwave irradiation power and irradiation time.
DOI: 10.1594/pangaea.870361
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2010/11_24
DOI: 10.1594/pangaea.931706
title: Stable oxygen isotope profile of the NGRIP_2012 firn core, annual means

description: Stable oxygen isotopes (δ18O) were measured on discrete samples using Cavity Ring-Down spectroscopy with an L2120-i and L2130-i by Picarro Instruments. The δ18O concentration with depth is provided with a precision of better than 0.1 per mil. Using raw, un-calibrated dielectrical profiling (DEP) data from the field (NEEM Set-up), volcanic tie points were derived. Together with the smoothed density data and the isotopic composition the record was dated by layer counting. The annual mean values of δ18O were obtained based on this dating.
DOI: 10.1594/pangaea.690674
title: Documentation of sediment core GIK12520-1
DOI: 10.1594/pangaea.870362
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2010/11_25
DOI: 10.1594/pangaea.870365
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2010/11_28
DOI: 10.1594/pangaea.737256
title: Sea surface temperature reconstruction from sediment core MD97-2151 using alkenones
DOI: 10.1594/pangaea.752026
title: Meteorological observations during SCIPIO cruise from Hellevoetsluis to Kaapstad started at 1785-12-18

description: 1786-01-02T13:00: DW: HET WEERLIGT ZONDER EENIG VOORBEELD. VMW: DE STORM MEER EN MEER TOENEEMENDE UIJT HET ZW LAGEN MET HET SCHIP ONDER DE ZEE WAAR DOOR CONSIDERABEL VEEL WATER OP HET DEK KREEGEN. MET DE? GL. WOEIJ HET EEN ORCAAN WAAIJENDE HET SCHIP, HOE ZEER OOK BRAMSTENGE EN ONDERRAAS HADDE GESTREEKEN MET DE STUURBOORDSZIJ ONDER WATER, DIT GEVOEGT BIJ TWEE ZWAARE STORTZEEEN DIE TE LOEFWAARD OVERQUAMEN ENDE GANTSCHE KUIJL VOL WATER ZETTEN DEED MIJ ALLE HOOP BENEEMEN VAN WEEDER HET ZULLEN REGTEN, RESOLVEERDE DAAROM SCHIERLIJK (IN DIT UIJTERSTEN) OM HET GESCHUT AAN LIJ OVER BOORD TE WERPEN, HETGEEN VAN DIT GEWENSCHTE GEVOLG WAS DAT NADAT WIJ? STUKKEN? 8 LB EN? DITO? 6 LB QUIJT WAREN HET SCHIP REGTEN WAAROM DOE OOK ORDRES GAF OM GEEN MEER WEG TE SMIJTEN. DES MIDDAGS WAS HET WEER IETS BEETER DOG DE ZEE WAS ZOO AFGRIJSLIJK VERBOLGEN DAT HET ZELVE BIJ MIJN ZONDER VOORBEELD WAS, DE LUIJKEN ALLE TOEGEPRASENNINGD ZIJNDE LEEDEN DE ZIEKEN CONSIDERABEL VEEL EN MAAKTE VOOR DE GEZONDE EEN ZEER ONAANGENAAME EN ONGEZONDE LUGT TUSCHEN DEKS
DOI: 10.1594/pangaea.895570
title: Georeferenced photographs of benthic photoquadrats acquired along transects from Heron Reef flat and slope areas (2009-11)