cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.873383
title: (Table 2) Isotope compositions of the fossil brachiopod shell Terebratula scillae
DOI: 10.1594/pangaea.832485
title: Picoheterotrophs in the Hawaiian Islands of the North Atlantic Ocean
DOI: 10.1594/pangaea.873073
title: Annotated record of the detailed examination of Mn deposits from U.S.N.S. Kane 1968 expedition in the Northern Atlantic ocean

description: Five of 34 dredge hauls taken in the Atlantic Ocean recovered a material tentatively described on shipboard as a salmon-colored clay. X-ray diffraction analysis showed the clay material to consist principally of palygorskite. Occurring with the palygorskite are quartz, calcite, and dolomite. It is suggested that the palygorskite (and sepiolite) is the result of chemical precipitation brought about by the reaction of hydrothermal solutions with sea water.
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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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: Bowles, F A; Angino, E A; Hosterman, J W; Galle, O K (1971): Precipitation of deep-sea palygorskite and sepiolite. Earth and Planetary Science Letters, 11(1-5), 324-332
DOI: 10.1594/pangaea.871824
title: (Fig. 3a) Relative spore and pollen abundances in sediment core Messel 2001
DOI: 10.1594/pangaea.873181
title: Annotated record of the detailed examination of Mn deposits observed by the DSV-4 Seacliff submersible in the Guaymas Basin, Gulf of California

description: A submersible dive on a turbidite-covered spreading axis in Guaymas Basin photographed and sampled extensive terraces and ledges of talc. The rock contains siliceous microfossils, smectite, and euhedral pyrrhotite as well as rather pure iron-rich talc. Sulfur and oxygen isotopes indicate precipitation around a hydrothermal vent, at about 280°C.
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: Lonsdale, Peter; Bischoff, James L; Burns, Virginia Mee; Kastner, Miriam; Sweeney, Colm (1980): A high-temperature hydrothermal deposit on the seabed at a gulf of California spreading center. Earth and Planetary Science Letters, 49(1), 8-20
DOI: 10.1594/pangaea.871820
title: Morphometry and biomass of the gastropod Neritina zebra (Bruguière, 1792) at the Mangabeira Beach, Marajó Island, Para state

description: The sampling was done in January 2015.
DOI: 10.1594/pangaea.872934
title: Nutrients in porewater from Elbe Estuary and adjacent Wadden Sea during Ludwig Prandtl cruise LP0903 in March 2009
DOI: 10.1594/pangaea.873033
title: (Table 1) Core drilling site information
DOI: 10.1594/pangaea.872163
title: (Appendix C, page 703) Chemical composition of Mn enriched siderite deposits from DSDP Leg 47 (Hole 398D)

description: Chemical composition was determined after dissolution by hot 1N acetic acid (first treatment), and by 2N acid to which the reducing agent metabisulfate was added (second and third treatments).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.873264
title: Sortable silt paleo-current proxies of sediment core GeoB13862-1 from the Southwest Atlantic

description: Antarctic Intermediate Water (AAIW) is an essential component of the Atlantic meridional overturning circulation (AMOC) contributing to balance the southward flow of North Atlantic Deep Water (NADW). However, the role of AAIW in Holocene abrupt climate changes remains poorly understood. Here we reconstruct changes in the flow strength of AAIW based on a high temporal resolution paleocurrent record from the Southwest Atlantic. Superimposed on a slight increase in AAIW strength at ~ 7 ka BP, a succession of millennial-scale AAIW variations is recognized in our paleocurrent records indicating a highly variable intermediate water circulation throughout the Holocene. Although variations in the strength and position of the Southern Westerlies Winds (SWW) are proposed to greatly influence the formation and circulation of AAIW, we cannot confirm such a potential SWW-AAIW linkage since our records of AAIW flow strength do not correlate to Holocene shifts of the SWW across the Atlantic. However, our data shows a good correspondence with abrupt variations in the AMOC with enhanced (reduced) northward advection of AAIW during periods of reduced (enhanced) NADW circulation. These results provide evidence for a Holocene AAIW-NADW see-saw. Thus, although the exact forcing mechanism remains unresolved, we suggest that Holocene perturbations in AAIW exerted a significant impact on the AMOC.
description: We applied sortable silt paleo-current flow proxies (i.e., sortable silt mean size and percentage) to reconstruct relative changes in intermediate-depth contour current strength, i.e., the Antarctic Intermediate Water flow strength. Both parameters refer to the fraction of the sediment (i.e., terrigenous 10-63 µm) whose size sorting varies in response to hydrodynamic processes, where higher values reflect stronger near-bottom flow and vice versa. Grain-size distributions of the terrigenous fraction were measured with a LS 13320 Laser Diffraction Particle Size Analyzers, resulting in 116 size classes from 0.04 to 2000 µm.
description: Supplement to: Voigt, Ines; Chiessi, Cristiano Mazur; Piola, Alberto R; Henrich, Rüdiger (2016): Holocene changes in Antarctic Intermediate Water flow strength in the Southwest Atlantic. Palaeogeography, Palaeoclimatology, Palaeoecology, 463, 60-67
DOI: 10.1594/pangaea.873506
title: (Table 2, page 1208) Average of 8 partial chemical analyses of opaque mineral grains bordering aragonite veins crossing serpentinized peridotite rocks from the Romanche Fracture Zone, Atlantic Ocean

description: Aragonite mineralization was observed in serpentinized peridotites from the Romanche and Vema Fracture Zones in the Atlantic and the Owen Fracture Zone in the Indian Ocean, either in veins or as radial aggregates in cavities within the serpentinites. Evidence of incipient dissolution of the aragonite crystals was observed in one case. The aragonites tend to have lower Mg content (&lt; 0.03%) and higher Sr content (&gt; 0.95%) relative to other marine aragonites. Their 18O16O, 13C12C and 87Sr86Sr isotopic ratios suggest the aragonite was deposited at ocean floor temperatures from solutions derived from sea water circulating in fissures and fractures within the ultramafic rocks. The 18O16O ratios of the serpentines indicate serpentinization occurred at higher temperatures, probably deeper in the crust. Low-T reactions between circulating seawater and Mg-silicates (primarily serpentine and pyroxenes) caused high pH and enrichment of Mg and Ca in the solution, conditions favoring carbonate precipitation. Aragonite was formed rather than calcite presumably because the high Mg2+ concentration in the solution inhibited calcite precipitation. The high Sr content of the aragonites is probably related, at least in part, to their low temperature of formation. Opaque mineral grains containing over 8% NiO and over 40% MnO were observed concentrated along the margins of some of the aragonite veins, suggesting that Ni is one of the elements mobilized during reactions between ultramafic rocks and circulating seawater.
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: Bonatti, Enrico; Lawrence, James R; Hamlyn, P R; Breger, Dee (1980): Aragonite from deep sea ultramafic rocks. Geochimica et Cosmochimica Acta, 44(8), 1207-1214
DOI: 10.1594/pangaea.856755
title: Pore water geochemistry of sediment core GeoB13824-1
DOI: 10.1594/pangaea.856765
title: Solid phase sulphur concentrations of sediment core GeoB13863-1
DOI: 10.1594/pangaea.856769
title: Pore water methane concentration of sediment core GeoB13863-1
DOI: 10.1594/pangaea.856809
title: Pore water and solid phase sulphur isotopes of sediment core GeoB13863-1
DOI: 10.1594/pangaea.873560
title: Annotated record of the detailed examination of Mn deposits from R/V Eltanin Cruise 9 stations

description: Cores, submarine photography and dredges described in this report were taken during the R/V Eltanin Cruise 9 in 1963 by the Department of Geology, Florida State University. Cores and dredges were recovered for 21 stations along with bottom photography and are available at the Antarctic Research Facility, Florida State University for sampling and study.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.872762
title: Ultra-violet measurements from station Boulder, SURFRAD (2014-09)
DOI: 10.1594/pangaea.872765
title: Ultra-violet measurements from station Boulder, SURFRAD (2014-10)
DOI: 10.1594/pangaea.872771
title: Basic measurements of radiation at station Boulder, SURFRAD (2014-12)
DOI: 10.1594/pangaea.872773
title: Other measurements at 10 m from station Boulder, SURFRAD (2014-12)
DOI: 10.1594/pangaea.873937
title: Mean, minimum and maximum temperature, annual precipitation and runoff in Finland during the period 1962-2014

description: In case of precipitation and runoff, 95th percentile is used instead of maximum, omitting outliers with extremely high values.
DOI: 10.1594/pangaea.873394
title: Other measurements at 10 m from station Fort Peck (2014-01)
DOI: 10.1594/pangaea.873240
title: Macrozoobenthos of the tidal channels in the Sylt-Rømø Bight in the Northern Wadden Sea (North Sea) in September 1996

description: Lister Ley, the largest of 3 tidal channels in Sylt-Rømø bight, was sampled by 270 box cores (0.02 m²) in a stratified random sampling design. The cores were evaluated for Macrozoobenthos (species and abundance) and sediment granulometry. Sampling occurred twice, in September 1996 and again in March 1997 in the same sites.
DOI: 10.1594/pangaea.873718
title: Factor loadings of dead benthic foraminifera of surface sediments of the shelf and upper slope from the Gulf of Guinea
DOI: 10.1594/pangaea.873400
title: Other measurements at 10 m from station Fort Peck (2014-03)
DOI: 10.1594/pangaea.872697
title: CO2 and associated air measurements from the Vancouver Sunset Tower on 2015-05-28 in Vancouver, Canada
DOI: 10.1594/pangaea.873402
title: Ultra-violet measurements from station Fort Peck (2014-04)
DOI: 10.1594/pangaea.873259
title: Flux calculation of short turbulent events in Chersky in the Sakha (Yakutia) Republic, Far Eastern Federal District of Russia (2014-08-02)
DOI: 10.1594/pangaea.873004
title: (Table 4, page 411) Chemical composition of a manganese crust from the Galapagos Spreading Center recovered at DSDP Leg 54 (Hole 424)

description: Sample has been dessicated at 1000°C.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.873193
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 55 (Holes 430, 431, 431A, 432)

description: Leg 55 was conceived as part of the decade-long experiment to test the kinematic hot-spot hypothesis and several of its more imporant corollaries for the origin of the Hawaiian-Emperor chain. Also of particular importance was the question of whether the Hawaiian hot spot has remained fixed in the mantle. The specific primary objectives of Leg 55, were to determine (1) whether the known increase in the age of the volcanoes on the Hawaiian chain with distance from Kilauea continues northward along the Emperor Seamounts; (2) whether the lavas of the Emperor volcanoes are of the same chemical composition and were erupted in the same sequence as those of Hawaiian volcanoes; (3) the latitude of formation of Suiko Seamount as a test of hot-spot fixity; and (4) whether the Emperor Seamounts were once islands and, if so, to determine their post-volcanic and subsidence history.
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.873501
title: Annotated record of the detailed examination of Mn deposits in the Blake Plateau area from R/V Eastward

description: Examination of the surface of freshly collected ferromanganese nodules by scanning electron microscopy revealed the presence of microcolonies of rod- and coccus-shaped bacteria which appeared to be anchored to the nodule surface by slime. The attachment of microcolonies by slime to the surface of freshly collected nodules argues against their being contaminants introduced during nodule collection or processing. These results corroborate cultural and biochemical detection of bacteria on ferromanganese 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.
description: Supplement to: LaRock, P A; Ehrlich, H L (1975): Observations of bacterial microcolonies on the surface of ferromanganese nodules from blake plateau by scanning electron microscopy. Microbial Ecology, 2(1), 84-96
DOI: 10.1594/pangaea.873557
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 58 (Holes 442A, 442B, 443, 444, 444A, 445, 446, 446A)

description: The JOIDES Active Margin Panel for Leg 58 decided that the drilling would occur in the north Philippine Sea, namely, the Shikoku Basin, the Daito Ridge and Basin province. The Shikoku Basin sites were selected to solve several problems concerning back-arc basins formed by ocean-floor spreading. The main objectives were: (1) to determine the age of the oldest sediment, so as to calibrate magnetic-anomaly ages and to provide a test for various spreading models suggested for the basin; (2) to investigate the mineralogy, petrology, and chemistry of basalt samples recovered by drilling, and to compare there basalts with those of midocean ridges, so as to understand the nature and source of magmatic materials in these basins; (3) to determine the distribution of sediment types in time, and to relate that distribution to the tectonic history of the basin.
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: deVries Klein, George; Kobayashi, Kazuo; White, Stan (1980): Initial Reports of the Deep Sea Drilling Project. U.S. Government Printing Office, LVIII, 1013 pp
DOI: 10.1594/pangaea.873576
title: Morphometry of Tortanus discaudatus stage c3 sampled from inshore waters of Scotland between 2013 and 2015
DOI: 10.1594/pangaea.872128
title: Annotated record of the detailed examination of Mn deposits recovered during WHOI R/V Atlantis II Cruise 92

description: This paper summarizes the petrography and major element chemistry of basalt collected by R/V Atlantis II at 23 °N, and compare these data with published data for 22 °N and with the preliminary shipboard data for DSDP Sites 395 and 396, in order to define the regional petrologic setting of the Leg 45 basalts.
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: Bryan, Wilfred B; Sargent, John R (1979): Basalt from 22°23°N, Mid-Atlantic Ridge Median Valley. In: Melson, W.G.; Rabinowitz, P.D.; et al., Initial Reports of the Deep Sea Drilling Project, 45, U.S. Government Printing Office, 45, 653-655
DOI: 10.1594/pangaea.872772
title: Ultra-violet measurements from station Boulder, SURFRAD (2014-12)
DOI: 10.1594/pangaea.873086
title: Annotated record of the detailed examination of Mn deposits from R/V Eltanin Cruise 13 stations

description: Cores, submarine photography and dredges described in this report were taken during the R/V Eltanin Cruise 13 in 1964 by the Department of Geology, Florida State University. Cores and dredges were recovered for 31 stations along with bottom photography and are available at the Antarctic Research Facility, Florida State University 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.
DOI: 10.1594/pangaea.873284
title: Meteorological synoptical observations from station Ishigakijima (2017-01)
DOI: 10.1594/pangaea.873287
title: Meteorological synoptical observations from station Minamitorishima (2017-01)
DOI: 10.1594/pangaea.872450
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 51 (Cores 417A and 417D), DSDP Leg 52 (Core 418A) and DSDP Leg 53 (Core 418B)

description: The JOIDES Paleoenvironment Panel had noted that the Neogene section had only been spot-cored on previous legs in the Western Atlantic (Legs 1, 2, 4, 11, and 43). The Panel accordingly requested that the complete section be recovered on Legs 51 through 53 in order to examine the transition from siliceous, Pacific-type Eocene sedimentation to non-siliceous sedimentation resulting from the gradual emergence of the Central American isthmus. It was also detremined to examine in detail the thick Cretaceous-Tertiary section overlying the basement.
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: Donnelly, Thomas W; Francheteau, Jean; Bryan, Wilfred B; Robinson, Paul T; Flower, Martin F J; Salisbury, Matthew H (1980): Initial Reports of the Deep Sea Drilling Project. Deep Sea Drilling Project, U.S. Government Printing Office, LI, LII, LIII, 1597 pp
DOI: 10.1594/pangaea.873291
title: Radiosonde measurements from station Sapporo (2017-01)
DOI: 10.1594/pangaea.873627
title: Ultra-violet measurements from station Goodwin Creek (2014-05)
DOI: 10.1594/pangaea.873303
title: Radiosonde measurements from station Tateno (2016-12)
DOI: 10.1594/pangaea.873347
title: Ultra-violet measurements from station Desert Rock (2014-03)