cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.857213
title: (Table 1, page 1051) Chemical composition of sediment associated with manganese nodules taken from the R/V Vityaz during its Cruise 33 in the Indian Ocean

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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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.808302
title: Physical oceanography measured on water bottle samples during John P. Tully cruise TUL95/7
DOI: 10.1594/pangaea.792606
title: (Table 6) Contributions of grain-size fractions of bottom sediments obtained from the Volga River delta

description: Values given in % biomass.
DOI: 10.1594/pangaea.821671
title: Physical oceanography from BTs to the Arctic Ocean
DOI: 10.1594/pangaea.808245
title: Physical oceanography during John P. Tully cruise IOS-96-01

description: c=beamc-adjc, 1-m pathlength SeaTech transmissometer at 660 nm data are reproducible to better than 0.001 in deep water. Clear water value for c is 0.364.
DOI: 10.1594/pangaea.770348
title: (Table 1) Heavy mineral content in sediments of the southern Mediterranean Ridge, Nile Cone and Egyptian Shelf

description: Petrographic analysis of Quaternary terrigenous sand layers in eastern Mediterranean cores reveals distinct mineralogical differences between the Egyptian Shelf–Nile Cone region and the southern part of the Mediterranean Ridge. A compositionally and texturally immature suite in Ridge cores, mixed with a Nile-derived assemblage, identifies a fresh non-recycled mineral component derived from proximal igneous and metamorphic surface or near-surface exposures, probably in the south–central Ridge area rather than from distal African sources. The presence of such basement terrains would be consistent with a compressive thrust-belt origin for this part of the Mediterranean Ridge.
description: Supplement to: Stanley, Daniel Jean; Sheng, Harrison; Kholief, Mahmoud M (1979): Sand on the southern Mediterranean Ridge: proximal basement and distal African-Nile provenance. Nature, 279(5714), 594-598
DOI: 10.1594/pangaea.797485
title: Record of 7 acritarch taxa from the Miocene, Pliocene and Pleistocene of ODP Site 104-642

description: DEPTH, sediment [m] is given in mbsf. AGE [ka BP] gives the calibrated ages. P = present; R = rare; C = common; A = abundant; F = frequent; ? = questionable assignment, - = not observed.
DOI: 10.1594/pangaea.610115
title: Abundance of lower marine fungi in deep and bottom waters off Portugal (Table 3)
DOI: 10.1594/pangaea.783289
title: XRD raw data from IODP Exp315
DOI: 10.1594/pangaea.884144
title: CTD data from the SWERUS-C3 expedition 2014 in the Arctic Ocean

description: The data set includes CTD data from the SWERUS-C3 (Swedish-Russian-US Arctic Ocean Investigation of Climate-Cryosphere-Carbon Interactions) expedition in 2014 with Swedish icebreaker (IB) Oden. The data was taken August 15 - September 25, 2014 and includes 155 CTD stations mainly located along the Siberian shelf and slope. Parameters in the data file are pressure (dbar), temperature (degC), salinity (PSU), oxygen concentration (µmol/kg) and turbidity (Volts). The quality flags are according to the WHP CTD data quality codes:1. Not calibrated, 2. Acceptable measurement, 3. Questionable measurement, 4. Bad measurement, 5. Not reported, 6. Interpolated over &gt;2 dbar interval, 7. Despiked, 8. Not assigned for CTD data, 9. Not sampled.
description: Supplement to: Björk, Göran; Jakobsson, Martin; Assmann, Karen M; Andersson, Leif; Nilsson, Johan; Stranne, Christian; Mayer, Larry (2018): Bathymetry and oceanic flow structure at two deep passages crossing the Lomonosov Ridge. Ocean Science, 14(1), 1-13
DOI: 10.1594/pangaea.756282
title: (Table 2) Interstitial pore-water chemistry of ODP Leg 115 holes

description: All data have been previously reported by Backman, Duncan, et al. (1988, doi:10.2973/odp.proc.ir.115.1988) with the exception of the Sr2+ concentrations and % recrystallization. The Ca2+ and Mg2+ data have been corrected to account for changes in Sr2+.
DOI: 10.1594/pangaea.788521
title: (Table 1) Stratigraphy, organic carbon, pyrolysis, extract and liquid chromatography at DSDP Holes 95-612 and 95-613
DOI: 10.1594/pangaea.605246
title: Abundance, calculated plasma, and biomass carbon of tinntinids of the western Arabian Sea (Table 4)
DOI: 10.1594/pangaea.744084
title: Physical oceanography at time series station 58NF in 1971
DOI: 10.1594/pangaea.778318
title: (Table 1.15) Composition of glassy basalts from the north part of the Bougault anomaly, Mid-Atlantic Ridge 15°N

description: Structure and composition of sub-surface bottom sediments from the southwest Barents Sea have been under study. The study has revealed heterogeneity of sediment structure resulted from temporal irregularity and variability of sedimentation processes. The study of the heavy minerals from 0.1-0.01 mm grain size fraction has shown prevalence of green hornblende, epidote, garnet, and ilmenite in all types of sediments; these minerals are the basis of terrigenous-mineralogical province. At the same time in different areas local terrigenous-mineralogical associations have been identified. Clay mineral composition of in the sediments was quite uniform: biotite, chlorite, hydromica, smectite. Despite this, a number of features indicating initial stages of clay mineral transformation has been identified. Differences in material composition and structure of the studied sediments are associated with rapid change in paleogeographic situation on the land - ice cover melting on the Kola Peninsula and subsequent Holocene climatic situation.
description: Contents are determined for temperature 1200Â°C in platinum containers. 0 = not found; &gt;0 = traces.
DOI: 10.1594/pangaea.761574
title: (Table 2) Number of species, abundance, and biomass of mesozooplankton in the northern Barents Sea in October 1998
DOI: 10.1594/pangaea.782595
title: (Table 1) Recalculated major element compositions of Pito Deep Rift dikes and lavas

description: Major element values recalculated after converting Fe2O3* to FeO*. Analytical totals have been conserved in the recalcluation.
DOI: 10.1594/pangaea.847797
title: (Table 3) Fractions of straight-chain saturated/unsaturated and iso-/anteiso-branched-chain fatty acids in selected soil samples from Livingston Island, South Shetland Archipelago

description: Fatty acid content is given per gram wet soil.
DOI: 10.1594/pangaea.847798
title: (Table 4) Closest phylogenetic affiliation of sequences and operational taxonomic units in nine soil samples from Livingston Island, South Shetland Archipelago
DOI: 10.1594/pangaea.759105
title: (Table 2) Calculated sedimentation rates based on the constant concentration model and the constant flux model, western flank of the East Pacific Rise at 21°-22°S
DOI: 10.1594/pangaea.760354
title: (Table 3+1) Content of rare earth elements (analyzed by INAA), phosphorus, and iron in phosphorites from Pacific seamounts
DOI: 10.1594/pangaea.807721
title: (Figure 4c) Grain size distributions along the Central Matakana profile

description: Surface sediment samples (uppermost 1 - 5 cm) were collected.Project: INTERCOAST - Integrated Coastal Zone and Shelf Sea Research
DOI: 10.1594/pangaea.838992
title: (Appendix A) Geochemistry of Oligocene sediments of ODP Site 177-1090

description: Ocean Drilling Program (ODP) Site 1090, on the Agulhas Ridge in the South Atlantic sector of the Southern Ocean, is ideally located to capture changes in Southern Ocean circulation patterns. Using samples taken from cored sediments, we construct multiproxy records of productivity (biogenic barium (Baex), opal, and CaCO3 mass accumulation rates (MARs)), nutrient and organic carbon burial (reactive phosphorus (Pr) MARs), and redox conditions (U and Mn enrichments) to investigate hydrographic conditions associated with climatic shifts from the Oligocene through the early Miocene. Orbitally induced cyclicity in U and Mn enrichments (100 kyr) suggests shifts in deepwater characteristics. However, CaCO3 dissolution coincident with low U and Mn enrichments does not indicate low-oxygen, corrosive waters similar to modern conditions. These observations indicate that a well-developed "modern-type" Antarctic Circumpolar Current (ACC) did not yet exist over the period from 30 to 20 Ma, with two potential consequences: The Southern Ocean was not functioning as a silica trap, permitting a broader distribution of silica that may have facilitated organic carbon burial in the ocean in general, and the lack of a deeply mixing ACC may have facilitated organic carbon burial in the Southern Ocean. Both the relative (high opal MARs coincident with low CaCO3 MARs) and absolute (high Pr MARs) burial of organic carbon suggest a powerful mechanism for pCO2 drawdown.
description: Supplement to: Anderson, Linda Davis; Delaney, Margaret Lois (2005): Use of multiproxy records on the Agulhas Ridge, Southern Ocean (Ocean Drilling Project Leg 177, Site 1090) to investigate sub-Antarctic hydrography from the Oligocene to the early Miocene. Paleoceanography, 20(3), PA3011
DOI: 10.1594/pangaea.729239
title: (Table 3d) Oligocene to Eocene calcareous nannofossils in ODP Site 122-762

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.753880
title: (Table 2) Correlation of harmonic 19 mean amplitude values to Krumbein roundness values for endmember saples, OD Leg 113
DOI: 10.1594/pangaea.774418
title: (Table 10) Representative clinopyroxene analyses of ODP Hole 126-791B and Alvin samples

description: Cations based on 6 oxygens.
DOI: 10.1594/pangaea.775974
title: (Appendix A3) Bulk magnetic susceptibility of ODP Site 178-1095A
DOI: 10.1594/pangaea.807664
title: Part of the global DOC versus AOU (dissolved organic carbon/apparent oxygen utilization) data compilation, OACESWOCEP15S170W

description: compilation by Xose Anton Alvarez-Salgado (mailto:xsalgado@iim.csic.es)
DOI: 10.1594/pangaea.733636
title: (Table 10) Trace element contents in pyroxenites and gabbroids

description: X-ray fluorescence analyses have been carried out in the Bronnizy expedition IMGRE under leadership of S.M. Lyapunov.
DOI: 10.1594/pangaea.832846
title: (Table S2) Mapping meters below seafloor to corrected composite depth for ODP Site 138-846

description: DEPTH, sediment/rock [m] gives mbsf.
DOI: 10.1594/pangaea.760068
title: (Table 7b) Azide, ammonium chloride and thiosulfate influences on carbon-14 dioxide assimilation rates in sediments from the Broken Spur and TAG hydrothermal fields
DOI: 10.1594/pangaea.807677
title: Part of the global DOC versus AOU (dissolved organic carbon/apparent oxygen utilization) data compilation, TT053

description: compilation by Xose Anton Alvarez-Salgado (mailto:xsalgado@iim.csic.es)
DOI: 10.1594/pangaea.587441
title: Meteorological observation at CTD stations of Meteor cruise M1, Persian Gulf
DOI: 10.1594/pangaea.682042
title: Phytoplankton abundance in surface water during Akademik Vernadsky cruise AV22
DOI: 10.1594/pangaea.808348
title: Physical oceanography measured on water bottle samples Moana Wave cruise HA-4A

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.770921
title: Physical oceanography during Walther Herwig I cruise WH7
DOI: 10.1594/pangaea.817097
title: Physical oceanography measured on water bottle samples during PELAGIA cruise MERLIM98
DOI: 10.1594/pangaea.735051
title: (Table 11) Composition of nuclei from nodules of Polygon Vityaz-6298

description: Polygon Vityaz-5965 is a part of Polygon Vityaz-6298. Coordinates are polygon buoy position.
DOI: 10.1594/pangaea.684347
title: (Table 1) Age determination of planktonic foraminiferal datums in DSDP Site 94-606 from the North Atlantic

description: Age calculated from age/depth curves based on paleomagnetic data (Clement and Robinson, 1987)
DOI: 10.1594/pangaea.762416
title: (Table 2) Potential-, spring- and summer new primary production and intensities of organic matter production in the Kandalaksha Bay
DOI: 10.1594/pangaea.775215
title: Antarctic coast line in PanMap layer format
DOI: 10.1594/pangaea.811067
title: (Table 2) Daily velocities and travel distances of individual gray whales (Eschrichtius robustus) along the Chukotka Peninsula

description: Satellite transmitter information from Table 1 included. Tagging position of Graywhale_37286 was on land (Latitude: 65.604 Longitude: -171.279), so position was slightly adapted here (Longitude: -171.0).
DOI: 10.1594/pangaea.810942
title: (Table 16) Major element chemistry of clay deposits at DSDP Leg 73 Holes
DOI: 10.1594/pangaea.840546
title: (Tables 9-10) Ratios of heavy metal concentrations between vegetation and soil, and between wood mouse, grass and earthworms from Heteren and Plateaux, The Netherlands

description: Ratios in (mg/kg dry weight)/(mg/kg dry weight).
DOI: 10.1594/pangaea.656462
title: Physical oceanography and hydrochemistry during Arnold Veimer cruise AV86
DOI: 10.1594/pangaea.882161
title: Physical oceanography on section MVP_2016001_10 during CCGS Amundsen cruise MVP_2016001
DOI: 10.1594/pangaea.671545
title: (Table 3) Distribution of tephra layers in Antarctic ice cores
DOI: 10.1594/pangaea.880885
title: (Table 6, pages 450-451) The composition of the hydrogenous component of sediments from DOMES Sites A, B, and C, Pacific Ocean

description: The composition is expressed in percentage of the soluble part in hydroxylamine hydrochloride-acetic 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.819478
title: (Table 2) Chemistry of bulk and &lt;1-µm size fractions of altered volcanic ash, clay vein in basalt, and pelagic clay from DSDP Leg 62 Holes

description: Other elements were scanned, but are below the limits of detection (listed in the parentheses in ppm): Ag (1.0), As (200), Au (10), Bi (10), Cd (2.0), Sb (15), Sn (2.0), Te (50), W (10), Re (50), Tl (10), Hg (500), Se (200). Numbers with &lt; symbol indicate the limit of detection for that particular element. Empty cells mean not analyzed.
DOI: 10.1594/pangaea.797438
title: (Table 11) Major-element compositions of glass shard, glass inclusions in pyroxenes and in plagioclase at DSDP Site 89-585

description: All iron measured as FeO.
DOI: 10.1594/pangaea.762432
title: (Table 6b) 137Cs concentrations in surface layer bottom sediments of the Sea of Japan in 1994 and in 2002

description: Sulfide, S°, and thiosulfate were determined in waters of the Baltic Sea. Microquantities of these compounds were observed in oxic waters. Concentration levels of reduced sulfur compounds in Baltic oxic waters were very close to levels of the Black Sea oxic zone. Thiosulfate and S° were predominate compounds in oxic water whereas sulfide was a predominant compound Baltic waters high in hydrogen sulfide. Conclusion was made that during sedimentation in oxic waters anaerobic microorganisms along with aerobic bacteria take part in mineralization of organic matter. They exist on surfaces and in microniches of particles of organic detritus.
DOI: 10.1594/pangaea.826298
title: (Table 1) Details of Porites specimens analyzed for bio-smoothing

description: Porites species identified by C. Veron, Australian Institute of Marine Science, Townsville, Australia. Orpheus and Nusa Barung coral specimens from Gagan et al. [1998, doi:10.1126/science.279.5353.1014]. Experiments: corals were cultured in the General Environmental Technos Co. Ltd. Laboratory, Japan [Omata et al., 2008, doi:10.1029/2007JG000431] for 519 days at 25.0°C and light intensity of 100 mmol/m2/s with a day/night regime of 12h/12h for 12h-4 and 10h/14h for 10h-4.
DOI: 10.1594/pangaea.778315
title: (Table 1.4) Ratios of petrogenic components in glassy and crystalline basalts from the north part of the Bougault anomaly, Mid-Atlantic Ridge 15°N

description: Structure and composition of sub-surface bottom sediments from the southwest Barents Sea have been under study. The study has revealed heterogeneity of sediment structure resulted from temporal irregularity and variability of sedimentation processes. The study of the heavy minerals from 0.1-0.01 mm grain size fraction has shown prevalence of green hornblende, epidote, garnet, and ilmenite in all types of sediments; these minerals are the basis of terrigenous-mineralogical province. At the same time in different areas local terrigenous-mineralogical associations have been identified. Clay mineral composition of in the sediments was quite uniform: biotite, chlorite, hydromica, smectite. Despite this, a number of features indicating initial stages of clay mineral transformation has been identified. Differences in material composition and structure of the studied sediments are associated with rapid change in paleogeographic situation on the land - ice cover melting on the Kola Peninsula and subsequent Holocene climatic situation.
DOI: 10.1594/pangaea.803830
title: Table 1: Mass budget of Hintereisferner and Kesselwandferner

description: Results of the direct, glaciological determination of the mass budget of Hintereisferner and Kesselwandferner in the Ötztal Alps are summarized for the years 1075/76-1977/78. Tabulations of budget quantities, accumulation and ablation areas are supplemented by graphs of altitudinal, and areal distribution of mass balance and by examples of the seasonal course of ablation.
description: Supplement to: Markl, Gerhard (1979): Neue Massenhaushaltswerte von Hintereisferner und Kesselwandferner 1975/76-1977/78. Zeitschrift für Gletscherkunde und Glazialgeologie, 15(1), 95-99
DOI: 10.1594/pangaea.758908
title: Chemical composition of bottom waters and interstitial waters from the Eastern Mediterranean

description: Chemical composition of bottom waters and interstitial waters and of more than 40 specimens of brines with salinities 50-270 g/kg in cores of bottom sediments up to 5 m long collected during Cruise 2 of R/V Moskovskiy Universitet southeast of the Crete Island are investigated. The brines and high-salinity interstitial waters were investigated in several rift valleys with subzonal orientation (Tyro and Kreteus valleys) associated with the crest of the Mediterranean swell, which is complicated by salt dome tectonics. Increase of salinity in cores containing diatomaceous-sapropelic oozes was accompanied by sulfate reduction and generation of H2S. All water samples and brines belonged to the magnesium subtype of the sulfate category. Two genetic varieties of interstitial waters in the epigenetic class are clearly distinguishable: 1) brines resulting from leaching of halite and mixing with NaCl of seawater, and 2) waters and brines rich in MgCl2. These data indicate that Messinian evaporites have an significant effect on the present-day lithohydrosphere of the Mediterranean.
description: Supplement to: Gurskiy, Yury N (1991): Chemical composition and origin of high-salinity interstitial waters and brines of the Eastern Mediterranean. Oceanology, 31(3), 304-310
DOI: 10.1594/pangaea.811475
title: (Table 6) Latest Oligocene to early Miocene calcareous nannoplankton datum events and their estimated magnetochronology at DSDP Site 72-516
DOI: 10.1594/pangaea.746195
title: (Table 14) Chemical composition of sulfide deposits from the Moose hydrothermal mound, Snake Pit hydrothermal field
DOI: 10.1594/pangaea.831045
title: Coral reef monitoring data during and after a severe bleaching event in 2010 in the Andaman Sea in 15 m water depth

description: CalMarO - Calcification by marine organisms, PEOPLE-2007-1-1-ITN Marie Curie Action: 215157BioAcid - German Ministry for Education and Research Project (Bmbf), Grant number 03F0608B, Bioacid 3.2.3, Coral Calcification in marginal reefsORCAS - Ocean Reef Coupling in the Andaman Sea - German Research Foundation (DFG), Grant number RI 1074/7-1
DOI: 10.1594/pangaea.820998
title: (Table 1) Composition of basal sediments collected at DSDP Holes 59-449 and 59-450

description: This chapter addresses the question of whether backarc spreading centers leave the same fingerprint of metal-enriched sediments that mid-ocean ridge spreading centers are so well known to leave. DSDP Legs 59 and 60 made an east-west traverse across the South Philippine Sea. Samples were collected in the Parece Vela Basin (Sites 449 and 450), the West Mariana Ridge (Site 451), and the Mariana Trough (Sites 452-460). No samples from the West Philippine Basin were analyzed, because original basal sediments had been eroded and replaced with coarse volcaniclastic breccia derived from the igneous basement itself (see Site 447 report, this volume). We analyzed basal-sediment samples from Holes 449 and 450 in the Parece Vela Basin (Leg 59) and from Holes 453, 459B, and 460A (Leg 60) for aluminum, calcium, magnesium, total iron, manganese, copper, colbalt, and nickel. Data and discussion of the results of Leg 59 are included in this report; those for Leg 60 are forthcoming in that volume.
description: Sediment depth is given in mbsf. Although the cored interval is 6.5 meters, 9.0 meters of sediment were recovered.
description: Supplement to: Scott, Martha R; Bolger, George W (1981): Metallogenesis in the Parece Vela Marginal Basin complex of the Philippine Sea, Deep Sea Drilling Project Leg 59. In: Kroenke, L; Scott, R; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 59, 649-652
DOI: 10.1594/pangaea.855414
title: Annotated record of the detailed examination of Mn and phosphate deposits from GOS74 Expedition stations

description: The purpose of the cruise was to map the manganese rich pavements of the Blake Plateau area which had been extensively investigated by ships of the Woods Hole Oceanographic Institution since 1956. From August until September 1965, 112 sites were sampled from R/V Gosnold on a joint USGS-WHOI expedition. At most of the stations on the Blake pavement, large slabs of manganese were recovered along with phosphate rich nodules.
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.763087
title: Tab. 5: Nurrient concentrations in meltstreams from the McMurdo Oasis