cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.902176
title: CuO lignin, and bulk decomposition data of a 75-day anoxic Phragmites australis litter decomposition experiment in soil substrates from three northeast German wetlands

description: Leaf and rhizome litter was anaerobically decomposed in the soil substrates of three NE_German wetlands. The decomposition time was 75 days. Leaf litter from all sites was decomposed in all substrates, rhizome litter only in its home substrate. The decomposition experiment was done in the laboratory at room temperature by placing litterbags at the bottom of polyethylene containers (80 x 60 x 43 cm) filled with the specific soil substrates. The dataset contains litter CN-data, determined with an elemental analyzer, mass loss data, determined gravimetrically, data on the peak intensity of the proteinaceous bands Amide I and Amide II, determined via peak fitting of the vector normalized FTIR spectra (Origin Peak Analyzer), the increase of the asymmetric phosphodiester band due to litter decomposition, determined as the peak height of the second derivative difference spectra at 1220 cm-1, as well as, lignin phenol concentrations, determined by gas chromatography mass spectrometry after alkaline CuO oxidation of litter and soil substrates.
DOI: 10.1594/pangaea.919059
title: Geochemical, lithological, and geochronological characteristics of sediment samples from Yedoma deposits in Siberia and Alaska 1998-2016
DOI: 10.1594/pangaea.759999
title: (Table 2) Daily rations and total consumption of phytoplankton by Calanus pacificus and Calanus australis
DOI: 10.1594/pangaea.671406
title: Basic measurements of radiation at station Solar Village (2000-01)
DOI: 10.1594/pangaea.772397
title: Hydrochemistry measured on water bottle samples during cruise Lena1957

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.759824
title: (Table 2) Mineral compositions of surface and buried micronodules from the Guatemala Basin
DOI: 10.1594/pangaea.671438
title: Basic measurements of radiation at station Solar Village (2002-09)
DOI: 10.1594/pangaea.772507
title: Hydrochemistry measured on water bottle samples during cruise Storm1959

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.772598
title: Hydrochemistry measured on water bottle samples during cruise WOD98_49_12228

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.759838
title: (Table 1) Hydrophysical and hydrochemical parameters of Black Sea waters important for phytoplankton production measured in autumn 1992
DOI: 10.1594/pangaea.772295
title: (Table III.4.5) Chemical composition of interstitial waters from surface layer bottom sediments of the Atlantic Ocean in the Angola Basin and off the Congo River mouth

description: 0 = not found.
DOI: 10.1594/pangaea.744417
title: Physical oceanography during Tridens cruise Tridens80/2 to the North Sea
DOI: 10.1594/pangaea.759839
title: (Table 2) Hydrolytic enzyme activity and some production characteristics of phytoplankton in the Black Sea in autumn 1992
DOI: 10.1594/pangaea.772367
title: Hydrochemistry measured on water bottle samples during cruise DUGMS1979

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.772480
title: Hydrochemistry measured on water bottle samples during cruise SEVER19

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.770801
title: (Table 3) Stratigraphic distribution of calcareous nannofossils at ODP Site 127-795

description: Species abundances: A = Abundant, C = common, M = many, F = few, R = rare
DOI: 10.1594/pangaea.771504
title: Physical oceanography during Walther Herwig II cruise WH078
DOI: 10.1594/pangaea.688866
title: Radiosonde M16_R288 during METEOR cruise M16 on 1969-03-14 18:00h

description: Height of tropause 17590 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.820174
title: (Table 11) Representative major and trace element analyses of basement rocks at DSDP Leg 60 Holes

description: Empty cells = no data.
DOI: 10.1594/pangaea.918711
title: Solomon Islands Local Ecological Knowledge of Marine Fishes 2014-2015, names and characteristics per group

description: This dataset contains all species names listed by respondents in the different focus groups, as well as the characteristics assigned to each species when sorting them into different groups. Samples are in rows, and factors/characteristics in columns. The columns comprise a sample identifier, gender, age and community of the respective focus group, local species names, and up to seven characteristics for each species. Samples are in rows, factors/characteristics in columns.
DOI: 10.1594/pangaea.759876
title: (Table 1) Mineral composition of aerosols sampled by nets above the West Pacific water surface

description: 0 = not found; &gt;0 = traces.
DOI: 10.1594/pangaea.772489
title: Hydrochemistry measured on water bottle samples during cruise SEVER30

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.744583
title: (Table 3) REE contents in basalts from pillow lavas of the Sierra Leone fault site, MAR 5-7°N
DOI: 10.1594/pangaea.759903
title: (Table 4) Catches of marked Greenland halibut far from places of marking

description: Parameters: ''Latitude'', ''Longitude'', and ''Date/Time of event'' show positions and dates of tag points; parameters: ''Latitude of event 2'', ''Longitude of event 2'', and ''Date/Time of event 2'' show positions and dates of recaptures.
DOI: 10.1594/pangaea.694101
title: Nutrient concentrations in water samples from the Aegean Sea at Station FEBR-1999-IR34
DOI: 10.1594/pangaea.772252
title: Hydrochemistry measured on water bottle samples during cruise AF00

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.706558
title: (Appendix 1) Biostratigraphy and Sr isotopic composition of sediments from DSDP Leg 14
DOI: 10.1594/pangaea.804376
title: (Table 3) Isotopic compositions and hydrocarbon isomer ratios of core gases at DSDP Site 84-567
DOI: 10.1594/pangaea.671420
title: Basic measurements of radiation at station Solar Village (2001-03)
DOI: 10.1594/pangaea.772255
title: Hydrochemistry measured on water bottle samples during cruise TI74

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.707374
title: (Table 2) Al203 of tephra and clay fractions in noncarbonate matter of sediments at DSDP Site 72-516
DOI: 10.1594/pangaea.772474
title: Hydrochemistry measured on water bottle samples during cruise SEVER02

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.744625
title: Composition of subalkali basalts from the Jan Mayen Fracture Zone, Jan Mayen Ridge, and alkali rocks from the Southern Seamount in the Greenland Sea
DOI: 10.1594/pangaea.855518
title: Table 2 & Appendix A. Properties of operations injecting CO2 into saline aquifers

description: The experience from CO2 injection at pilot projects (Frio, Ketzin, Nagaoka, US Regional Partnerships) and existing commercial operations (Sleipner, Snøhvit, In Salah, acid-gas injection) demonstrates that CO2 geological storage in saline aquifers is technologically feasible. Monitoring and verification technologies have been tested and demonstrated to detect and track the CO2 plume in different subsurface geological environments. By the end of 2008, approximately 20 Mt of CO2 had been successfully injected into saline aquifers by existing operations. Currently, the highest injection rate and total storage volume for a single storage operation are approximately 1 Mt CO2/year and 25 Mt, respectively. If carbon capture and storage (CCS) is to be an effective option for decreasing greenhouse gas emissions, commercial-scale storage operations will require orders of magnitude larger storage capacity than accessed by the existing sites. As a result, new demonstration projects will need to develop and test injection strategies that consider multiple injection wells and the optimisation of the usage of storage space. To accelerate large-scale CCS deployment, demonstration projects should be selected that can be readily employed for commercial use; i.e. projects that fully integrate the capture, transport and storage processes at an industrial emissions source.
description: Supplement to: Michael, K; Golab, A; Shulakova, V; Ennis-King, J; Allinson, G; Sharma, S; Aiken, T (2010): Geological storage of CO2 in saline aquifers—A review of the experience from existing storage operations. International Journal of Greenhouse Gas Control, 4(4), 659-667
DOI: 10.1594/pangaea.671432
title: Basic measurements of radiation at station Solar Village (2002-03)
DOI: 10.1594/pangaea.846154
title: Nematoda communities in sediments at Panarea shallow CO2 seeps during cruise ECO2-3
DOI: 10.1594/pangaea.762456
title: (Table 1) Petrographic, chemical, and mineralogical description of ODP Leg 124 tephra samples
DOI: 10.1594/pangaea.671434
title: Basic measurements of radiation at station Solar Village (2002-05)
DOI: 10.1594/pangaea.761608
title: (Table 1) Distribution of phytoplankton pigments (chlorophylls a, b, c and carotenoids) in the northeastern Sea of Okhotsk from March 23 to April 14, 1998
DOI: 10.1594/pangaea.780575
title: (Table T2) Spectral reflectance record for ODP Site 188-1165

description: Two main alternating facies were observed at Ocean Drilling Program (ODP) Site 1165, drilled in 3357 m water depth into the Wild Drift (Cooperation Sea, Antarctica): a dark gray, laminated, terrigenous one (interpreted as muddy contourites) and a greenish, homogeneous, biogenic and coarse fraction-bearing one (interpreted as hemipelagic deposits with ice rafted debris [IRD]). These two cyclically alternating facies reflect orbitally driven changes (Milankovitch periodicities) recorded in spectral reflectance, bulk density, and magnetic susceptibility data and opal content changes. Superimposed on these short-term variations, significant uphole changes in average sedimentation rates, total clay content, IRD amount, and mineral composition were interpreted to represent the long-term lower to upper Miocene transition from a temperate climate to a cold-climate glaciation. The analysis of the short-term variations (interpreted to reflect ice sheet expansions controlled by 41-k.y. insolation changes) requires a quite closely spaced sampled record like that provided by the archive multisensor track. Among those, cycles are best described by spectral reflectance data and, in particular, by a parameter calculated as the ratio of the reflectivity in the green color band and the average reflectivity (gray). In this data report a numerical evaluation of spectral reflectance data was performed and substantiated by correlation with core photos to provide an objective description of the color variations within Site 1165 sediments. The resulting color description provides a reference to categorize the available samples in terms of facies and, hence, a framework for further analyses. Moreover, a link between visually described features and numerical series suitable for spectral analyses is provided.
description: Supplement to: Rebesco, Michele (2003): Data report: Numerical evaluation of diffuse spectral reflectance data and correlation with core photos, ODP Site 1165, Wild Drift, Cooperation Sea, Antarctica. In: Cooper, AK; O'Brien, PE; Richter, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 188, 1-27
DOI: 10.1594/pangaea.912780
title: (Supplement 5) Aerosol backscatter coefficient (at 532 nm) measurements in the Atlantic of the 1991 Mt Pinatubo aerosol cloud from Professor Vize
DOI: 10.1594/pangaea.548183
title: Nutrients and bacteria measured on water bottle samples at station Chip_2004-01-09_15, Chipana, Chile
DOI: 10.1594/pangaea.737441
title: (Table 3) Representative analyses of orthopyroxenes and clinopyroxenes of peridotites from the eastern part of the Romanche Fracture Zone

description: Analyses have been carried out in TsNIGRI by M.V. Shavyrina.
DOI: 10.1594/pangaea.855515
title: Table 1. pH, Temperature, conductivity and hydrochemistry of samples

description: Carbon dioxide deep geological storage, especially in deep saline aquifers, is one of the preferred technological options to mitigate the effects of greenhouse gases emissions. Thus, in the last decade, studies characterising the behaviour of potential CO2 deep geological storage sites along with thorough safety assessments have been considered essential in order to minimise the risks associated with these sites. The study of natural analogues represents the best source of reliable information about the expected hydrogeochemical processes involved in the CO2 storage in such deep saline aquifers.In this work, a comprehensive study of the hydrogeochemical features and processes taking place at the natural analogue of the Alicún de las Torres thermal system (Betic Cordillera) has been conducted. Thus, the main water/CO2/rock interaction processes occurring at the thermal system have been identified, quantified and modelled, and a principle conclusion is that the hydrogeochemical evolution of the thermal system is controlled by a global dedolomitization process triggered by gypsum dissolution. This geochemical process generates a different geochemical environment to that which would result from the exclusive dissolution of carbonates from the deep aquifer, which is generally considered as the direct result of CO2 injection in a deep carbonate aquifer. Therefore, discounting of the dedolomitization process in any CO2 deep geological storage may lead to erroneous conclusions. This process will also influence the porosity evolution of the CO2 storage formation, which is a very relevant parameter when evaluating a reservoir for CO2 storage. The geothermometric calculation performed in this work leads to estimate that the thermal water reservoir is located between 650 and 800 m depth, which is very close to the minimum required to inject CO2 in a deep geological storage.It is clear that the proper characterisation of the features and hydrogeochemical processes taking place at a natural system analogous to a man-made deep geological storage will provide useful conceptual, semi-quantitative and even quantitative information about the processes and consequences that may occur at the artificial storage system.
description: Supplement to: Prado-Pérez, Antonio; Pérez del Villar, Luís (2011): Dedolomitization as an analogue process for assessing the long-term behaviour of a CO2 deep geological storage: The Alicún de las Torres thermal system (Betic Cordillera, Spain). Chemical Geology, 289(1-2), 98-113
DOI: 10.1594/pangaea.720311
title: Documentation of sediment core GIK13973-3
DOI: 10.1594/pangaea.803994
title: (Table 6) Amphiboles from gabbros and amphibolites at DSDP Holes 84-567A and 84-569

description: Formula basis: 23 oxygens.
DOI: 10.1594/pangaea.761454
title: (Table 3) Major and minor element composition of ferromanganese nodules and crusts

description: All sample concentrations expressed in weight percent on 110°C dried basis.
DOI: 10.1594/pangaea.808142
title: (Table 1) Geochemistry at DSDP Leg 80 Holes
DOI: 10.1594/pangaea.733642
title: (Table 14) Chemical composition of harzburgites from the Cape Verde fault

description: Analyses have been carried out in the Bronnizy expedition IMGRE.
DOI: 10.1594/pangaea.744790
title: (Table 7) Composition of spinels from basalts the Bouvet triple junction
DOI: 10.1594/pangaea.745091
title: (Table 3) Representative analyses of pyroxenes in rocks from the Sierra Leone segment of the Mid-Atlantic Ridge
DOI: 10.1594/pangaea.770804
title: (Table 6) Summary of calcareous nannofossil events of ODP Leg 127
DOI: 10.1594/pangaea.818538
title: (Table 2) Interstitial water chemistry at DSDP Leg 64 Holes

description: Blank spaces indicate that no data were obtained.
DOI: 10.1594/pangaea.809825
title: (Table 2) Major and minor element composition of the insoluble residues at DSDP Site 76-533 sediments
DOI: 10.1594/pangaea.921650
title: (Table 5) Fourier Transformed Infrared Spectroscopy inference for biogenic silica and TOC of sediment core PET09P2 from Lake Petit (Southern French Alps)
DOI: 10.1594/pangaea.855828
title: (Table, page 395) Chemistry of fossil manganese rich concretions from the Cambrian formations of Conception Bay and Trinity Bay, Newfoundland

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.774561
title: (Table T1) Carbonate mineralogy and carbonate content of several ODP Leg 204 sites

description: Carbonate mineralogy and carbonate content were determined on 65 samples from Sites 1244-1252, which were drilled on southern Hydrate Ridge and in an adjacent slope basin at the Cascadia accretionary prism. X-ray diffraction analyses data indicate varying carbonate compositions. Pure calcites are rare but were found at Sites 1246 and 1252. Low- and high-magnesium calcites are the dominant carbonate mineralogies and occur at all sites. The presence of dolomite is characteristic for the slope basin sites. The sampling depth of the carbonates varies from near seafloor to deep within the accretionary complex, suggesting different modes of carbonate formation. The summit, flank, and slope basin sites show characteristic carbonate compositions with different carbonate contents in distinct depth intervals.
description: Supplement to: Teichert, Barbara M A; Bohrmann, Gerhard (2006): Data report: Composition of authigenic carbonates in sediments of the Cascadia accretionary prism, ODP Leg 204. In: Tréhu, AM; Bohrmann, G; Torres, ME; Colwell, FS (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 204, 1-8
DOI: 10.1594/pangaea.858104
title: Field temperatures along Mt. Kilimanjaro, Farm Kirua
DOI: 10.1594/pangaea.497609
title: Physical oceanography from BT during cruise U58GS02070B_1984
DOI: 10.1594/pangaea.856628
title: Shipboard acoustic doppler current profiling during Maria S. Merian cruise MSM15/4, link to NetCDF file
DOI: 10.1594/pangaea.828466
title: Pass-through measurements of magnetic susceptibility from IODP Hole 323-U1339C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.815350
title: (Table 5) Geochemistry of the clay fraction (&lt;2 µm) of hydrothermal sediments at DSDP Leg 70 Holes
DOI: 10.1594/pangaea.882208
title: Grain sizes of Omongwa Pan sediment sequence (Omaheke Region, Namibia) by Horiba Scattering Particle Size Distribution Analyzer LA-950
DOI: 10.1594/pangaea.497813
title: Physical oceanography from BT during cruise U58X000092B_1962
DOI: 10.1594/pangaea.747849
title: Meteorological observations during Catharina Johanna cruise from Banjouwangie to Nieuwediep started at 1843-11-21
DOI: 10.1594/pangaea.680170
title: Other measurements at 30 m from station Solar Village (2002-11)
DOI: 10.1594/pangaea.817228
title: (Table 2) Geochemistry of glasses in ashes from DSDP Holes 67-497 and 67-496
DOI: 10.1594/pangaea.729886
title: (Table 6) Distribution of trace element contents in sediments at DSDP Site 65-483
DOI: 10.1594/pangaea.815446
title: (Table 7) Fe**3+/Fe**2+ ratios in selected nontronite samples at DSDP Leg 70 Holes

description: Since its discovery in 1974 (Klitgord and Mudie, 1974), the Galapagos mounds hydrothermal field has received much attention. Sediment samples were taken during Leg 54 of the Deep Sea Drilling Project (DSDP) and by other expeditions to the area (e.g., Corliss et al., 1978). While a hydrothermal origin for the mounds sediments has been generally accepted, several different theories of origin for the mounds themselves have been proposed (e.g., Corliss et al., 1978; Natland et al., 1979; Williams et al., 1979). One of the aims of DSDP Leg 70 was to return to the mounds field and, using the new hydraulic piston cor er described elsewhere in this volume, to obtain more complete recovery of mounds sediments than had previously been possible. It was our hope that this would help in our understanding of the nature and origin of these deposits. In this chapter, we describe the results of chemical analysis of over 250 sediment samples taken during the course of Leg 70.
description: Supplement to: Moorby, S A; Cronan, David S (1983): Chemical composition of sediments from Sites 506, 507, 508, and 509, Leg 70, Deep Sea Drilling Project. In: Honnorez, J; Von Herzen, RP; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 70, 269-275
DOI: 10.1594/pangaea.730124
title: (Table 64) Distribution of trace element contents in sediments from the Central American Trench at DSDP Site 67-494
DOI: 10.1594/pangaea.828551
title: P-Wave velocity (PWL) from IODP Hole 323-U1343D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.775783
title: (Table 1b) Chemical composition of bottom aleuroargillites from the Philippine Sea
DOI: 10.1594/pangaea.856622
title: Annotated record of the detailed examination of Mn deposits from WAHINE Expedition stations

description: The cores described in this report were taken on the WAHINE Expedition in February to March 1965 by the Scripps Institution of Oceanography from the R/V Spencer F. Baird. A total of 54 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 (1965): WAHINE (1965) Expedition, Core List, R/V Spencer F. Baird. Scripps Institution of Oceanography, UC San Diego, unpublished, 67 pp
DOI: 10.1594/pangaea.499529
title: Physical oceanography from BT during cruise U90XX08329B_1985
DOI: 10.1594/pangaea.744725
title: (Table 4) Rare earth element contents in selected basalts from the Sierra Leone Fracture Zone region
DOI: 10.1594/pangaea.817870
title: (Table 3) Bulk geochemistry of terrigenous hemipelagic sediments from DSDP Sites 65-483 and 65-485
DOI: 10.1594/pangaea.808281
title: Basic measurements of radiation at station Cener (2013-02)
DOI: 10.1594/pangaea.694807
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station FEBR-1998-IR08

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).