cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.858981
title: Radiosonde measurements from station Kwajalein (2015-12)
DOI: 10.1594/pangaea.858982
title: Basic measurements of radiation at station Kwajalein (2016-01)
DOI: 10.1594/pangaea.858983
title: Radiosonde measurements from station Kwajalein (2016-01)
DOI: 10.1594/pangaea.858984
title: Basic measurements of radiation at station Kwajalein (2016-02)
DOI: 10.1594/pangaea.826963
title: (Table 4) Duplicate elemental and Pb isotopic measurements from total, detrital, and leachable fractions from sediment core JM06-WP-16-MCB
DOI: 10.1594/pangaea.858985
title: Radiosonde measurements from station Kwajalein (2016-02)
DOI: 10.1594/pangaea.858987
title: Radiosonde measurements from station Boulder (2015-11)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.858972
title: Basic and other measurements of radiation at station South Pole (2015-12)
DOI: 10.1594/pangaea.858974
title: Basic and other measurements of radiation at station South Pole (2016-01)
DOI: 10.1594/pangaea.858976
title: Basic and other measurements of radiation at station South Pole (2016-02)
DOI: 10.1594/pangaea.759148
title: (Table 5) Chemistry of microtektites in ODP Hole 121-758B
DOI: 10.1594/pangaea.858986
title: Basic measurements of radiation at station Boulder (2015-11)
DOI: 10.1594/pangaea.858988
title: Basic measurements of radiation at station Boulder (2015-12)
DOI: 10.1594/pangaea.882474
title: Physical properties and X-ray fluorescence of sediment core MSM09/2_455-13 (GeoTü SL 170)
DOI: 10.1594/pangaea.759581
title: (Table 3) Nannofossil datum levels of ODP Site 121-752

description: The age of the LO of Reinhardtites levis is not well constrained and is roughly estimated here at 70.4 Ma.
DOI: 10.1594/pangaea.848468
title: Decade Wind and Wave Data for NW Iberia, Cabo Sillerio

description: Seafloor sediment mobilization on the inner Northwest Iberian continental shelf is caused largely by ocean surface waves. The temporal and spatial variability in the wave height, wave period, and wave direction has a profound effect on local sediment mobilization, leading to distinct sediment mobilization scenarios. Six grain-size specific sediment mobilization scenarios, representing seasonal average and storm conditions, were simulated with a physics-based numerical model. Model inputs included meteorological and oceanographic data in conjunction with seafloor grain-size and the shelf bathymetric data. The results show distinct seasonal variations, most importantly in wave height, leading to sediment mobilization, specifically on the inner shelf shallower than 30 m water depth where up to 49% of the shelf area is mobilized. Medium to severe storm events are modeled to mobilize up to 89% of the shelf area above 150 m water depth. The frequency of each of these seasonal and storm-related sediment mobilization scenarios is addressed using a decade of meteorological and oceanographic data. The temporal and spatial patterns of the modeled sediment mobilization scenarios are discussed in the context of existing geological and environmental processes and conditions to assist scientific, industrial and environmental efforts that are directly affected by sediment mobilization. Examples, where sediment mobilization plays a vital role, include seafloor nutrient advection, recurrent arrival of oil from oil-spill-laden seafloor sediment, and bottom trawling impacts.
description: Supplement to: Oberle, Ferdinand K; Storlazzi, Curt D; Hanebuth, Till J J (2014): Wave-driven sediment mobilization on a storm-controlled continental shelf (Northwest Iberia). Journal of Marine Systems, 139, 362-372
DOI: 10.1594/pangaea.858996
title: Physical oceanography from Seaglider mission CNCY200914907

description: Find data with quality flags in source datasets in NetCDF format.
DOI: 10.1594/pangaea.859191
title: Basic measurements of radiation at station Camborne (2013-08)
DOI: 10.1594/pangaea.859176
title: Basic and other measurements of radiation at station South Pole (2015-11)
DOI: 10.1594/pangaea.859184
title: Basic measurements of radiation at station Camborne (2016-02)
DOI: 10.1594/pangaea.839124
title: (Table 1) Age and lithological description of sediment core MD99-2227

description: For bulk mineralogy, semiquantitative estimation was obtained by applying correction factors to the measured intensity of the reflections as follows: I3.34 Å * 1 for quartz, I3.03Å * 1.92 for calcite, I3.18Å and I3.20Å * 2 for feldspars, and I4.4Å * 20 for total clay (Boski et al., 1998). Semiquantitative estimations (±5 *10%; Biscaye (1965)) of the main clay species were based on the height of specific reflections, generally measured on EG runs. The intensities were corrected by a weight factor and values were added up to total 100%. The relative intensity of the main clay species was calculated according to I10ÅEG * 1 for illite, (I10ÅH-I10ÅEG) * 1 for smectites, I14ÅEG * 0.4 for chlorite, and I12ÅEG * 0.4 for illite-chlorite mixed layers (10 * 14c), I7ÅEG * 0.7 * [I3.57ÅEG/(I3.57ÅEG+I3.54ÅEG)] (see Fagel et al. (2003) for details). For grain-size data, mean and sorting were calculated according to Folk and Ward (1957).
DOI: 10.1594/pangaea.859198
title: Continuous air temperature measurement at Schwingbachtal Studienlandschaft, Germany (growing season 2013-2014)
DOI: 10.1594/pangaea.859201
title: Continuous groundwater level measurement at Schwingbachtal Studienlandschaft, Germany (growing season 2013-2014)
DOI: 10.1594/pangaea.859207
title: Continuous solar radiation measurement at Schwingbachtal Studienlandschaft, Germany (growing season 2013-2014)
DOI: 10.1594/pangaea.893247
title: Magnetic susceptibility from sediment core XC05 from the Xingu River, Brazil
DOI: 10.1594/pangaea.858712
title: (Table 13-2) Ground temperature data (annual mean, minimum, maximum) of the polygon wall POK-01
DOI: 10.1594/pangaea.859210
title: Observation of manganese crusts recovered during the R/V Thomas Washington cruise 1965-1 in December 1965 in the Atlantic Ocean

description: The petrology of the mid-Atlantic ridge between 22° and 23°N latitude may be typical of those portions of the ridge characterized by a linear topography parallel to the axis, a well-developed median valley, and an absence of volcanic cones. Submarine basalt lavas dredged at fifteen stations on the crest of the ridge are of three eruptive facies, all derived from essentially identical magmas; (1) pillow lavas, (2) sideromelane-rich tuffs, and (3) massive, mainly holocrystalline basalts. This association is well known from continental exposures of ancient submarine lavas. Chemically, the lavas are oceanic tholeiites and thus support the view that these low-potassium olivine basalts are by far the dominant eruptive on the deep-sea floor. In the 22° area, they are probably the product of voluminous fissure eruptions. The oceanic tholeiite is evidently the counterpart of the continental flood basalts, but it differs compositionally from these, especially in a lower potassium content. As a further characterization of the basalts, seven new analyses of major, minor, and trace elements are presented. Post-cooling hydrothermal metamorphism under some overburden has transformed some of these basalts into greenschists and lower-grade metamorphic rocks. New data indicate that faulting and shearing along the median valley combined with the introduction of hot, probably saline solutions were major agents in the metamorphism.
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: Melson, William G; Thompson, Geoffrey; van Andel, Tjeerd H (1968): Volcanism and metamorphism in the Mid-Atlantic Ridge, 22°N latitude. Journal of Geophysical Research, 73(18), 5925-5941
DOI: 10.1594/pangaea.859008
title: Description of manganese nodules and crust collected from the R/V Sonne Cruise SO-06, Pacific 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.859141
title: (Tables 1b, page 210) Chemical composition of manganese nodules and crusts recovered from the Pacific 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.859009
title: Average chemical composition by size categories of manganese nodules and crusts collected from the R/V Sonne Cruise SO-06, Pacific 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.859142
title: (Tables 2, page 210) Multiple measurements of the chemical composition of manganese nodules and crusts recovered from the Pacific 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.859145
title: Illustrations of typical manganese deposits recovered from the Pacific 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.859010
title: Average chemical composition of manganese micronodules from cores collected during the R/V Sonne Cruise SO-06, Pacific 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.859150
title: Annotated record of the detailed examination of Mn deposits from R/V Atlantis - Cruise 151 (Dec. 1947) in the Atlantic Ocean

description: One of the objectives of WHOI Atlantis Cruise 151, covering the period from 7 December 1947 to 18 June 1948, was to obtain as complete a sampling of the sea bottom of the Meditterranean and Aegean Seas as was compatible with the remainder of the scientific program. It was furthermore planned to make concurrent bottom photographs as a means for studying the correlation between bottom sediments and the morphology of the sea floor. The photographs also held the possibility of determining the presence of bottom fauna. The underwater camera used for this work was loaned to us by Dr. Maurice Ewing of Columbia University. As it was fitted with a one foot long coring tube at the base of its pole a majority of the bottom samples were obtained by the camera itself. On the way to Gibraltar, several bottom photos were taken in the Atlantic ocean. One of them was the deepest underwater photograph ever taken at the tima (3026 fathoms) showing a cluster of objects, some as much as 5 inches across on a clay bottom. These appeared to be manganese nodules, judging from their rounded and bulbous shape, especially the potato-like form of some of them. A core sample obtained at the same spot with a corer attached to the camera stand contained abundant manganese grains.
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: Owen, D M (1949): Atlantis Cruise 151 to Mediterranean area - scientific report No. 2 - bottom samples and underwater photography. Woods Hole Oceanographic Institution; http://www.ngdc.noaa.gov/mgg/geology/data/atlantis_ii/02025011/02025011.pdf, 49-08, 31 pp
DOI: 10.1594/pangaea.858713
title: (Table 14-1) Bedrock description of samples from the Pokhodskaya Yedoma
DOI: 10.1594/pangaea.859152
title: (Table, Page 194) Measurements of radium inside ferromanganese nodules in the Pacific Ocean

description: The author studies in what state the radioactive matter exists in the sea water and in the sediments. The material dealt with in the present experiments are partly from the 'Challenger' and partly from the 'Albatross' collections of Sir John Murray, F.R.S. It includes sediment samples and manganese nodules.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.858714
title: (Table 14-2) Cryotexture, sediment description and selected ice content of samples from the Pokhodskaya Yedoma Island

description: Ice content is the amount of ice contained in frozen or partially frozen soil or rock.- absolute ice content: the ratio of the mass of the ice in a sample to the mass of the frozen sample- gravimetric ice content: the ratio of the mass of the ice in a sample to the mass of the dry sample (the gravimetric ice content can greatly exceed 100 percent)
DOI: 10.1594/pangaea.859012
title: Annotated record of the detailed examination of manganese nodules from the Kara Sea and a lake in Karelia

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.859153
title: Description of manganese nodules collected in a metamorphic slate Silurian formation near the Tweed River, New South Wales, Australia

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.759144
title: (Table 1) Carbonate concentration in ODP Hole 121-758C
DOI: 10.1594/pangaea.859154
title: Chemical composition of manganese nodules collected in a metamorphic slate Silurian formation near the Tweed River, New South Wales, Australia

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.759587
title: (Table 8) Magnetic chron boundaries in ODP Leg 121 holes
DOI: 10.1594/pangaea.859156
title: Observation of manganese crusts recovered during the CHAIN 44 cruise in October 1964 in the Atlantic Ocean

description: In October 1964, a detailed geophysical and sampling survey was made of the central part of the Mid-Atlantic Ridge between 22° and 23° north latitude. The results indicate a large difference in age between the relief of the crest and that of the flanks of the Ridge and suggest that the crest portion is very young. Detailed surveys of two sediment-filled valleys on the upper western flank of the Ridge reveal different sedimentary sequences in the two valleys and indicate the probable existence of a locally controlled depositional regime and a significant local supply of sediment.
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: van Andel, T H; Bowen, V T; Sachs, P L; Siever, R (1965): Morphology and Sediments of a Portion of the Mid-Atlantic Ridge. Science, 148(3674), 1214-1216
DOI: 10.1594/pangaea.859148
title: Meteorological data, stem radius measurements (SR) and derivates of SR of the three Swiss forest sites Visp, Davos and Lägeren

description: - Separating continuously measured stem radius (SR) fluctuations into growth-induced irreversible stem expansion (GRO) and tree water deficit-induced reversible stem shrinkage (TWD) requires a concept to decide on potential growth processes during periods of shrinking and expanding SR below a precedent maximum. Here we investigated two physiological concepts: the linear growth (LG) concept assuming linear growth vs. the zero growth (ZG) concept assuming no growth during periods of shrunken stems. - We evaluated the physiological mechanisms underlying these two concepts and assessed the respective plausibility with SR data obtained from 15 deciduous and evergreen trees. - The LG concept showed steady growth rates, whereas the ZG concept showed strongly varying growth rates over time, more in accordance with mechanistic expectations. Further, growth increased for maximally 120 min after periods of shrunken stems, indicating limited growth activity during that period. However, the fraction of this extra growth was found to be small. Furthermore, TWD of the ZG concept was better explained by a hydraulic plant model than TWD of the LG concept. - We conclude that periods of shrunken stems allow for very little growth in the four tree species investigated. However, further studies should focus on obtaining independent growth data to ultimately validate these findings.
description: Supplement to: Zweifel, Roman; Haeni, Matthias; Buchmann, Nina; Eugster, Werner (2016): Are trees able to grow in periods of stem shrinkage? NPH-MS-2015-21113, New Phytologist, 211(3), 839-849
DOI: 10.1594/pangaea.859194
title: Zr/Al ratios of IODP Hole 339-U1387C
DOI: 10.1594/pangaea.859195
title: Grain size composition of IODP Hole 339-U1387C
DOI: 10.1594/pangaea.796236
title: Calcium and strontium content of IODP Hole 303-U1305C

description: Sediment depth is given in mcd.
DOI: 10.1594/pangaea.859196
title: Planktonic foraminifera of IODP Hole 339-U1387C
DOI: 10.1594/pangaea.859065
title: Basic measurements of radiation at station Boulder, SURFRAD (2009-07)
DOI: 10.1594/pangaea.859348
title: Meteorological synoptical observations from station Tateno (2016-01)
DOI: 10.1594/pangaea.859066
title: Ultra-violet measurements from station Boulder, SURFRAD (2009-07)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-09.