cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.854176
title: (Table 2, page 22), Dithionite-soluble Fe and Al in different type and size classes of lake ores

description: After extraction with acid ammonium oxalate, Fe and Al in the residue were extracted using the dithionite-citrate-bicarbonate method.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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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: 10.48577/jpl.lgw4gv
title: 2023-07-25 OGC - Dynamic Information Acquisition as part of the Earth System Digital Twins Framework

description: No abstract available.
DOI: 10.1594/pangaea.789967
title: (Table 5) Concentrations of trace elements in wetland waters, lower Tom basin

description: Positions were obtained from Figure 1. When no exact position could be obtained an approximate was made - see sample comment.
DOI: 10.1594/pangaea.694995
title: Concentrations of particulate organic carbon in water of the Aegean Sea at Stations JUNE-1998-S03, JUNE-1998-S06, JUNE-1998-IR03, and JUNE-1998-IR06
DOI: 10.1594/pangaea.807185
title: (Table 3) Average of annual chemical fluxes during specific event intervals in Svalbard ice cores
DOI: 10.1594/pangaea.755375
title: Age of bottom sediments from the Indian Ocean

description: It has been found that oxygen-isotope and paleotemperature curves based on types of planktonic foraminiferal thanatocenoses in three sediment cores, from the tropical, southern temperate, and southern glacial zones of the Indian Ocean can be readily correlated with each other. The sediment cores revealed three epochs of cold climate during the past 700 ky; these are probably connect with worldwide epochs of cooling during Pleistocene that led to advance of ice sheets during continental glaciations in the northern hemisphere.
description: Supplement to: Lisitzin, Alexander P; Nikolaev, Vladimir I; Blyum, Natalia S (1978): The temperatures of the Indian Ocean in the Brunhes paleomagnetic epoch. Oceanology, 18(1), 58-61
DOI: 10.1594/pangaea.764067
title: (Table 1) Physiographic province, age and lithologic descriptions from different DSDP Holes in the Indian Ocean

description: Sediment depth is given in msbf.
DOI: 10.1594/pangaea.854657
title: Separation between acid insoluble and soluble parts from Mn nodules from the Challenger expedition

description: After drying at 110°C the fine powder was treated with concentrated hydrochloric acid.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.854659
title: (Table 6, page 476-477) Composition of acid-soluble fraction from manganese

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.824062
title: RNA and DNA measured during Marion Dufresne cruise ANTARES-IV
DOI: 10.1594/pangaea.857280
title: Annotated record of the detailed examination of Mn deposits from the Southern Borderland (SOB) Expedition stations

description: The cores and dredges described in this report were taken on the Southern Borderland (SOB) Expedition in February-March 1960 by the Scripps Institution of Oceanography from the R/V Spencer F. Baird. A total of 34 cores and dredges were recovered and are available at Scripps for sampling and study.
description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: SCRIPPS Institution of Oceanography (1960): Southern Borlerland (SOB) Expedition, Core List, R/V Spencer F. Baird. Scripps Institution of Oceanography, UC San Diego, unpublished, 4 pp
DOI: 10.1594/pangaea.756964
title: (Table 4A) Trace element concentrations in high-latitude diatoms
DOI: 10.1594/pangaea.810341
title: (Table 1) Salinity, dissolved organic carbon and absorption characteristics of surface river waters around Hudson Bay

description: Composition and concentration of colored dissolved organic matter (CDOM) have been determined in Hudson Bay and Hudson Strait by excitation emission matrix spectroscopy (EEM) and parallel factor analysis (PARAFAC). Based on 63 surface samples, PARAFAC identified three fluorescent components, which were attributed to two humic- and one protein-like components. One humic-like component was identified as representing terrestrial organic matter and showed a conservative behaviour in Hudson Bay estuaries. The second humic-like component, traditionally identified as peak M, originated both from land and produced in the marine environment. Component 3 had spectra resembling protein-like material and thought to be plankton-derived. The distribution and composition of CDOM were largely controlled by water mass mixing with protein-like component being the least affected. Distinctive fluorescence patterns were also found between Hudson Bay and Hudson Strait, suggesting different sources of CDOM. The optically active fraction of DOC (both absorbing and fluorescing) was very high in the Hudson Bay (up to 89%) suggesting that fluorescence and absorbance can be used as proxies of the DOC concentration.
description: Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
description: Supplement to: Guéguen, Celine; Granskog, Mats A; McCullough, G; Barber, David G (2011): Characterisation of colored dissolved organic matter in Hudson Bay and Hudson Strait using parallel factor analysis. Journal of Marine Systems, 88(3), 423-433
DOI: 10.48577/jpl.qqk47g
title: On-orbit Thermal Performance of the JWST Mid-Infrared Instrument

description: No abstract available.
DOI: 10.1594/pangaea.757820
title: (Table 1) Composition of dredged samples of the Atlantis II Fracture Zone
DOI: 10.1594/pangaea.787322
title: (Table 2) Nannofossil biohorizons for ODP Sites 133-812 through 133-818
DOI: 10.1594/pangaea.810369
title: (Table 17) Distrubution of calcareous nannofossil taxa in the Pleistocene-Pliocene interval at ODP Site 138-848

description: Sediment depth is given in mbsf. Species abundance: A = abundant (usually &gt;10 specimens observed per field), C = common (1-10 specimens per field), F = few (1 specimen per 1-10 fields), R = rare (
DOI: 10.1594/pangaea.823507
title: XRD raw data from IODP Exp329
DOI: 10.1594/pangaea.757186
title: (Table 5) Amino acids and amino sugars in sediments of ODP Site 117-723

description: Ages are calculated on biostratigraphical and magnetostratigraphical data from the shipboard party (1989, doi:10.2973/odp.proc.ir.117.110.1989).
DOI: 10.1594/pangaea.757827
title: (Table 2) Elemental and protein nitrogen contents of ODP Leg 112 samples
DOI: 10.1594/pangaea.759234
title: (Table 2) Biomass of nannoplankton infusoria at abundance peaks in the California region
DOI: 10.1594/pangaea.788881
title: Bacterial single cell number measurements during METEOR cruise M76/3b at the REGAB seep site in 2008

description: Project: DFG-Research Center/Excellence Cluster The Ocean in the Earth System (MARUM) and the Max Planck Institute for Marine Microbiology, Bremen, Germany.
DOI: 10.1594/pangaea.772370
title: Hydrochemistry measured on water bottle samples during cruise DUGMS1982

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.830835
title: Presence of plant species at IMPETUS Testsites in the Drâa Catchment

description: Dataset created by IMPETUS subproject B3. IMPETUS data set ID: 113
DOI: 10.1594/pangaea.763352
title: (Table 1) Mass spectra of free-base, nickel and nicke-plus-copper porphyrins isolated from DSDP Leg 64 holes

description: Normalized within cach class. viz. free-base or metalloporphyrin (Ni or Ni/Cu). Average low-voltage (14 eV) mass spectra normalized and isotopically corrected.
DOI: 10.1594/pangaea.772470
title: Hydrochemistry measured on water bottle samples during cruise Priboy1964

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.744421
title: Physical oceanography during Tridens cruise Tridens84/1 to the North Sea
DOI: 10.1594/pangaea.745654
title: (Table 4) Chemical composition of bottom sediments from the Clarion Fracture Zone
DOI: 10.1594/pangaea.755197
title: Distribution of tripylean radiolarians from ODP Leg 114 (Table 2)

description: The occurrence of tripylean radiolarians is reported for the first time from subsurface sediments of the subantarctic Atlantic Ocean. Although their occurrence is rare as well as sporadic, seven species belonging to four genera are recognized from Upper Cenozoic sediments drilled at Sites 699, 700, and 701 of ODP Leg 114 in 1987.
description: Taxa abundance: + = single specimen; R = rare (2-5 specimens), F = few (6-10 specimens), - = absent.
description: Supplement to: Ling, Hsin Yi (1991): Tripylean radiolarians from the Subantarctic Atlantic. In: Ciesielski, PF; Kristoffersen, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 114, 311-315
DOI: 10.1594/pangaea.755205
title: (Table 1) Accumulation of glucose by populations of microorganisms in the Black Sea
DOI: 10.1594/pangaea.760616
title: (Table 2) Fluxes of dissolved metals from bottom sediments to water in the Amur and Zolotoy Rog bays
DOI: 10.1594/pangaea.755659
title: Abundance and biomass of benthic foraminifera in bottom sediments from the Sea of Okhotsk and the Pacific Ocean

description: A study of distribution of live individuals of benthic foraminifera in sediments of the Sea of Okhotsk and of the Northwestern Basin of the Pacific Ocean shows that they can be present in sediments up to depth of 30 cm and probably can live there for long periods, sometimes forming high concentrations. Living individuals in the subsurface layer often account for more than 50% of total biomass, which varies from 1 to 21 g/m**2 in different morphological structures. The largest biomass values are attained in underwater rises embedded in relatively warm, oxygen-saturated Pacific waters. Minimum total biomass concentrations occur in deep-water depressions where stagnation phenomena are observed. Foraminifera biomass everywhere decreases gradually with increasing depth from the surface of sediments regardless of relief, depth, and nature of sediments.
description: Supplement to: Basov, Ivan A; Khusid, Tatyana A (1983): Biomass of benthic foraminifera in sediments of the Sea of Okhotsk. Oceanology, 23(4), 489-495
DOI: 10.1594/pangaea.768328
title: (Table 2b) Total phytoplankton biomass in the fluorescence maximum layer and contributions of dominant species to its value in the Western Arctic in July-August 2003
DOI: 10.1594/pangaea.788030
title: (Table 3) Chemical composition of micas from epidote-mica-amphibole green schists in the upper unit of the Khavyven Highland
DOI: 10.1594/pangaea.807344
title: (Table 4) Individual lifetime energy budgets of ocean quahog (Arctica islandica)

description: Energy values were originally given in kJ and were converted to cal by dividing by 4.1868 and multiplying by 1000.
DOI: 10.15468/dl.b79c9x
title: Occurrence Download

description: A dataset containing 201 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is Human Observation",
 "Country is Korea, Republic of",
 "OccurrenceStatus is Present",
 "PublishingOrg is one of (ce3cfcc0-6d56-11db-a819-b8a03c50a862, 6f2da4d9-8bd9-4f4f-852b-22cde4a43a01, d6aeeb7c-db16-436f-98bb-f0d7e2c7a0db, eb07eeb0-3db9-11d9-8439-b8a03c50a862)",
 "TaxonKey is one of (Platycladus orientalis (L.) Franco, Zabelia tyaihyoni (Nakai) Hisauti & H.Hara, Hylotelephium ussuriense (Kom.) H.Ohba, Rhododendron micranthum Turcz.)",
 "Year 1990-2024"
 ]
}

 The dataset includes 201 records from 3 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031482-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.836297
title: (Figures 1, 6, 7) Original FORC data and original AC data

description: View dataset as HTML below will open a table with links to data files.
DOI: 10.1594/pangaea.857465
title: Colored dissolved organic matter (cDOM) absorption measurements on Fildes Peninsula (King George Island, West Antarctica) - Bellingshausen Station, Russia, in 2013
DOI: 10.1594/pangaea.785958
title: (Table T2) Sedimentation rates of ODP Leg 182 sites
DOI: 10.1594/pangaea.806606
title: (Table 2) Fluid inclusion analyses of ODP Holes 137-504B and 140-504B
DOI: 10.1594/pangaea.695034
title: Concentrations of particulate organic carbon in water of the Ionian Sea at Station MARCH-2000-IRI44

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.828782
title: Dissolved inorganic carbon and sulphate concentrations in the pore water of sediment at the rim of a vesicomyd clam colony in the Japan Deep Sea Trench (dive 955)
DOI: 10.1594/pangaea.847625
title: (Table 2) Chlorophyll content, chlorophyll a/b ratio, number of algal cells per mg dry weight and chlorophyll content per photobiont cell of the lichen Cetraria aculeata

description: All data given per (milli)gram dry weight (DW).
DOI: 10.1594/pangaea.716571
title: (Table 1) Trace element concentrations and Nd and Pb isotope ratios of DSDP Site 78-543

description: Nd isotope ratios are relative to the value recommended by Chauvel and Blichert-Toft (2001, doi:10.1016/S0012-821X(01)00379-X) for the Rennes Nd standard (143Nd/144Nd = 0.511961, which corresponds to a La Jolla value of 0.511856). Uncertainties reported on the Nd isotope ratios are in-run errors (2 sigma), where sigma is the standard deviation and n the number of measured 143Nd/144Nd ratios, generally 60). The Rennes Nd standard was run every second sample and its reproducibility (2sigma) calculated on each analyses session (~20 analyses) is typically 30 ppm. Reproducibility calculated using complete duplicate analyses of 7 samples is 1.2 * 10**-5 (2 sigma) on the measured 143Nd/144Nd ratio (25 ppm) and is better than the average in-run errors. Pb isotope ratios are relative to NBS 981 values of 206Pb/204Pb = 16.9405, 207Pb/204Pb = 15.4963 and 208Pb/204Pb = 36.7219 (Galer and Abouchami, 1998). The NBS 981 standard was run every second sample and its reproducibility (2 sigma) calculated on the entire period of analyses is 150, 180 and 200 ppm for 206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb ratios respectively (106 analysis). Reproducibility calculated using complete duplicate analyses of 8 samples, excluding the 4 duplicates of black shales (Site 144 - Unit 3), is 0.007 (370 ppm), 0.002 (130 pm) and 0.011 (300 ppm) for 206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb ratios respectively (2 sigma). The reproducibility of the black shale duplicates is not as good probably because of the strong heterogeneities of these samples.
DOI: 10.1594/pangaea.760749
title: (Table 3) Diatom valve fluxes and composition for the developments BO1 and PF3 (upper traps)
DOI: 10.1594/pangaea.880544
title: (Table 2, page 71) Major elements geochemistry of manganese nodules and ferromanganese crusts from the Pacific Ocean, samples dried at 110°C for 24 hours

description: The samples were wet-ground to powders and kept in artificial seawater. After drying samples were dissolved in 15ml of I:2HCl+1:5NH3OHCl at 75°C for chemical analysis by atomic absorption spectrometry.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: 10.48577/jpl.c8eqfl
title: Spectral responses of the SPHEREx telescope

description: The Spectro-Photometer for the History of the Universe, Epoch of Reionization, and Ices Explorer (SPHEREx) is an upcoming all-sky near-infrared spectroscopic survey satellite designed to address all three primary science goals of NASA’s Astrophysics Division. SPHEREx employs a series of Linear Variable Filters (LVFs) to create 102 spectral channels across the wavelength range of 0.75 to 5 μm, with spectral resolutions R between 35 and 120. This paper presents the spectral calibration setup used for SPHEREx and discusses the various challenges encountered during the measurement process. Ultimately, we demonstrate the spectral responses for all 25 million pixels in SPHEREx.
DOI: 10.1594/pangaea.882292
title: Monitoring of spatial and temporal variability in bottom water oxygen levels on the Southern Benguela continental shelf, from 2014 to 2017

description: There is increasing evidence for a global trend towards lower seawater dissolved oxygen levels, which poses a threat to marine ecosystem health. A particular concern is upwelling areas, such as the Benguela Upwelling System, that is predisposed to low oxygen levels with occasional catastrophic consequences for fisheries resources. In the Southern Benguela Upwelling System, the lowest seawater O2 levels are typically found in inshore bottom waters at relatively shallow depths on the shelf. In order to better understand the factors inducing low oxygen conditions, temporal trends, and to provide input to the Department of Environmental Affairs' annual State of the Oceans and Coasts Report, oxygen data had been collected approximately 3-monthly along 4 transects, since 2014. To this dataset had been added data collected on a random sampling grid in the vicinity of the monitoring lines. The dissolved oxygen, temperature and salinity data represent stations at a maximum depth of about 500 m, for cruises conducted on the R/V Algoa in: August 2014 (AUG14), October 2014 (OCT14), February 2015 (FEB15), May 2015 (MAY15), September 2015 (SEP15), November 2015 (NOV15), February 2016 (FEB16), May 2016 (MAY16), August 2016 (AUG16), November 2016 (NOV16), February 2017 (FEB17) and May 2017 (MAY17).
DOI: 10.1594/pangaea.696182
title: Organic carbon and nitrogen concentrations in surface waters of the Arabian Sea along 65°E during the intermonsoon period of 1995

description: Not filtered water samples were taken in 10 ml ampoules (sealed immediately after being acidified with phosphoric acid to pH&lt;2, sampling), or 40 ml screw-lid vials, and measured onboard at sampling or next days, or frozen (-20°C) until being acidified and measured in home labs.Carbon measurement was by high-temperature catalytic oxydation in a 10 cm column packed with 5% Pt on aluminum oxide beads at 900°C in a stream of oxygen, and CO2 detection by infrared extinction after the removal of moisture and SO2 by appropriate traps (cold trap, Mg-percarbonate, Na-pyrophosphate, tin, bronze or Sulfix). The apparatus was the dual channel Dimatek 2000 equipped with a Binos 200 detector. Nitrogen was measured by chemoluminescence detection of NO2 in the combustion gases after leaving the Binos detector in one of the two channels of the setup. Most measurements of samples containing high nitrate were discarded, when data were inconsistent. The nature of nitrate interference is not clear.
DOI: 10.1594/pangaea.733267
title: Physical oceanography during Kaimikai O Kanaloa cruise HOT-117 on section PRS2
DOI: 10.1594/pangaea.676639
title: Contents of tricyclic terpanes in bottom sediments of the Barents Sea sampled from R/V Ivan Petrov in 2005
DOI: 10.1594/pangaea.786269
title: (Table 1) Content and composition of chloroform bitumoids in organic matter from bottom sediments of the northeast Black Sea
DOI: 10.1594/pangaea.808109
title: (Table 1) Interstitial water chemistry at DSDP Leg 80 Holes

description: Interstitial water studies of sediments recovered during DSDP Leg 80 (Goban Spur transect) indicate a well-developed dissolved-sulfate minimum at Site 548 resulting from increased sulfate reduction in the rapidly deposited Pleistocene sediment section. Changes in the concentration of dissolved strontium at each site must be related to carbonate recrystallization processes.
description: Supplement to: Gieskes, Joris M; Johnston, Kirk (1985): Interstitial water studies, Leg 80. In: De Graciansky, PC; Poag, CW; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Gov. Printing Office), 80, 1047-1053
DOI: 10.1594/pangaea.837004
title: Hydrochemistry measured on water bottle samples during SHOYO cruise 492SSY9607_1 on section P08N

description: For definition of quality flags see hdl:10013/epic.31518.d001