cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.831223
title: Temperature monitoring in the Thai Andaman Sea coral reefs from 2009-12 to 2010-05 - Bon West

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.477693
title: Hydrochemistry measured on water bottle samples at station SPac_1967_ET_28S/182

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.691412
title: Monthly landings in 1998, Puerto Natales, Chile
DOI: 10.1594/pangaea.739120
title: Pollen profile CLAIR, Loch Clair, United Kingdom

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.859022
title: Stem radius change of Pine 484 at Site VISP in 2012
DOI: 10.1594/pangaea.694945
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station SEPT-1998-MNB6

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore filters. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).
DOI: 10.1594/pangaea.728456
title: (Table 7) Distribution of calcareous nannofossils in ODP Hole 119-744B

description: Species abundance: V = very abundant (&gt;40%), A = abundant 10-40%), C = common (1-10%), F = few (0.1-1%), R = rare (&lt;1%), - = absent
DOI: 10.1594/pangaea.711666
title: (Table 1) Basalt density, basement age, and intrusive/extrusive relations from DSDP Site 3-14
DOI: 10.1594/pangaea.728246
title: (Table 2) Diatom abundance and nannofossil and diatom zonation of ODP Hole 115-710A
DOI: 10.1594/pangaea.678111
title: Expanded measurements from station Ny-Ålesund (1995-11)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.666036
title: Oceanography at CTD/bottle station IFREMER_2862
DOI: 10.1594/pangaea.728247
title: (Table 2) Diatom abundance and nannofossil and diatom zonation of ODP Hole 115-712A
DOI: 10.1594/pangaea.746936
title: Meteorological observations during GRIFFIN cruise from Canton River to St. Helena started at 1750-01-28
DOI: 10.1594/pangaea.919627
title: Radiosonde measurements from station Lindenberg (2018-06)
DOI: 10.1594/pangaea.496893
title: Physical oceanography from BT during cruise K90S3B_1959
DOI: 10.1594/pangaea.919629
title: Expanded measurements from station Lindenberg (2018-06)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.675009
title: Radiosonde measurements from station Ny-Ålesund (2002-03)
DOI: 10.1594/pangaea.740676
title: Age determination of sediment core RAC20, Lake Racou, France

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.787641
title: (Table 1) Anisotropy of magnetic susceptibility parameters of ODP Hole 134-833B

description: Ocean Drilling Program (ODP) Sites 832 and 833 were drilled in the intra-arc North Aoba Basin of the New Hebrides Island Arc (Vanuatu). High volcanic influxes in the intra-arc basin sediment resulting from erosion of volcanic rocks from nearby islands and from volcanic activity are associated with characteristic magnetic signals. The high magnetic susceptibility in the sediment (varying on average from 0.005 to more than 0.03 SI) is one of the most characteristic physical properties of this sedimentary depositional environment because of the high concentration of magnetites in redeposited ash flows and in coarse-grained turbidites.Susceptibility data correlate well with the high resolution electrical resistivity logs recorded by the formation microscanner (FMS) tool. Unlike the standard geophysical logs, which have low vertical resolution and therefore smooth the record of the sedimentary process, the FMS and whole-core susceptibility data provide a clearer picture of turbiditic sediment deposition.Measurements of Curie temperatures and low-temperature susceptibility behavior indicate that the principal magnetic minerals in ash beds, silt, and volcanic sandstone are Ti-poor titanomagnetite, whereas Ti-rich titanomagnetites are found in the intrusive sills at the bottom of Site 833. Apart from an increase in the concentration of magnetite in the sandstone layer, acquisition of isothermal and anhysteretic remanences does not show significant differences between sandstone and clayey silts. The determination of the anisotropy of magnetic susceptibility (AMS) in more than 400 samples show that clayey siltstone have a magnetic anisotropy up to 15%, whereas the AMS is much reduced in sandstone layers. The magnetic susceptibility fabric is dominated by the foliation plane, which is coplanar to the bedding plane. Reorientations of the samples using characteristic remanent magnetizations indicate that the bedding planes dip about 10° toward the east, in agreement with results from FMS images.Basaltic sills drilled at Site 833 have high magnetic susceptibilities (0.05 to 0.1 SI) and strong remanent magnetizations. Magnetic field anomalies up to 50 µT were measured in the sills by the general purpose inclinometer tool (GPIT). The direction of the in-situ magnetic anomaly vectors, calculated from the GPIT, is oriented toward the southeast with shallow inclinations which suggests that the sill intruded during a reversed polarity period.
description: Samples of interval 134-833B-83R to 134-833B-91R from basaltic sills, of interval 134-833B-94R to 134-833B-89R from sediments interlayerd with the sills.
description: Supplement to: Roperch, Pierrick; Chabernaud, Thierry; Calza, Francoise (1994): Magnetic properties of a volcanic-rich sedimentary sequence in the intra-Arc Aoba Basin. In: Green, HG; Collot, J-Y; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 134, 491-507
DOI: 10.1594/pangaea.675412
title: Radiosonde measurements from station Payerne (2000-07)
DOI: 10.1594/pangaea.846963
title: Abundance of mesozooplankton in the western part of the Black Sea in spring 1997 during the National Monitoring Programme

description: The “15BO1997001” dataset is based on samples collected in the spring of 1997. The whole dataset is composed of 66 samples (from 27 stations of National Monitoring Sampling Grid) with data of zooplankton species composition, abundance and biomass. Samples were collected in discrete layers 0-10, 0-20, 0-50, 10-25, 25-50, 50-100 and from bottom up to the surface at depths depending on water column stratification and the thermocline depth.Zooplankton samples were collected with vertical closing Juday net,diameter - 36cm, mesh size 150 µm. Tows were performed from surface down to bottom meters depths in discrete layers. Samples were preserved by a 4% formaldehyde sea water buffered solution. Sampling volume was estimated by multiplying the mouth area with the wire length.Mesozooplankton abundance: The collected material was analysed using the method of Domov (1959). Samples were brought to volume of 25-30 ml depending upon zooplankton density and mixed intensively until all organisms were distributed randomly in the sample volume. After that 5 ml of sample was taken and poured in the counting chamber which is a rectangle form for taxomomic identification and count. Large (&gt; 1 mm body length) and not abundant species were calculated in whole sample. Counting and measuring of organisms were made in the Dimov chamber under the stereomicroscope to the lowest taxon possible. Taxonomic identification was done at the Institute of Oceanology by Lyudmila Kamburska using the relevant taxonomic literature (Mordukhay-Boltovskoy, F.D. (Ed.). 1968, 1969,1972).Taxon-specific abundance: The collected material was analysed using the method of Domov (1959). Samples were brought to volume of 25-30 ml depending upon zooplankton density and mixed intensively until all organisms were distributed randomly in the sample volume. After that 5 ml of sample was taken and poured in the counting chamber which is a rectangle form for taxomomic identification and count. Copepods and Cladoceras were identified and enumerated; the other mesozooplankters were identified and enumerated at higher taxonomic level (commonly named as mesozooplankton groups). Large (&gt; 1 mm body length) and not abundant species were calculated in whole sample. Counting and measuring of organisms were made in the Dimov chamber under the stereomicroscope to the lowest taxon possible. Taxonomic identification was done at the Institute of Oceanology by Lyudmila Kamburska using the relevant taxonomic literature (Mordukhay-Boltovskoy, F.D. (Ed.). 1968, 1969,1972).
DOI: 10.1594/pangaea.787645
title: (Table 1) Magnetic characteristic properties of selected samples of ODP Hole 134-831B

description: During Ocean Drilling Program Leg 134 (Vanuatu), geological high sensitivity magnetic tools (GHMT) developed by CEA-LETI and TOTAL were used at two drill sites. GHMT combine two sensors, a proton magnetometer for total magnetic field measurements with an operational accuracy of 0.1 nanoteslas (nT), and a highly sensitive induction tool to measure the magnetic susceptibility with an operational accuracy of a few 10**-6 SI units.Hole 829A was drilled through an accretionary prism and the downhole measurements of susceptibility correlate well with other well-log physical properties. Sharp susceptibility contrasts between chalk and volcanic silt sediment provide complementary data that help define the lithostratigraphic units.At Hole 831B magnetic susceptibility and total field measurements were performed through a 700-m reef carbonate sequence of a guyot deposited on top of an andesitic volcano. The downhole magnetic susceptibility is very low and the amplitude of peak-to-peak anomalies is less than a few 10**-5 SI units. Based on the repeatability of the measurements, the accuracy of the magnetic logging measurements was demonstrated to be excellent. Total magnetic field data at Hole 831B reveal low magnetic anomalies of 0.5 to 5 nT and the measurement of a complete repeat section indicates an accuracy of 0.1 to 0.2 nT. Due to the inclination of the earth's magnetic field in this area (~-40°) and the very low magnetic susceptibility of the carbonate, the contribution of the induced magnetization to the total field measured in the hole is negligible. Unfortunately, because the core recovery was extremely poor (&lt;5%) no detailed comparison between the core measurements and the downhole magnetic data could be made. Most samples have a diamagnetic susceptibility and very low intensity of remanent magnetization (&lt; 10**-4 A/m), but a few samples have a stable remanent magnetization up to 0.005 A/m. These variations of the intensity of the remanent magnetization suggest a very heterogeneous distribution of the magnetization in the carbonate sequence that could explain the magnetic field anomalies measured in these weakly magnetized rocks.
description: Supplement to: Roperch, Pierrick; Barthès, V; Pocachard, J; Collot, Jean-Yves; Chabernaud, Thierry (1994): Magnetic logging and in-situ magnetostratigraphy: a field test. In: Green, HG; Collot, J-Y; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 134, 577-589
DOI: 10.1594/pangaea.858946
title: Experiment on asian green mussels (Perna viridis), West Java, Indonesia (April 2012 - November 2013): hypoxia tolerance in juvenile mussels
DOI: 10.1594/pangaea.787586
title: (Table 3) Chemistry of olivines from ODP Holes 134-828A and 134-832A ash layers
DOI: 10.1594/pangaea.787683
title: (Table 2) Petrography of volcaniclastic sandstones from Unit III of ODP Hole 135-840B
DOI: 10.1594/pangaea.739458
title: Pollen profile LINDENM, Lindenmoos, Austria

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.739962
title: Pollen profile WILDMOOS, Wildmoos, Austria

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.711909
title: Pollen profile KUCUK, Küçük Akgöl, Turkey

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.738955
title: Pollen profile ALETSW2, Aletschwald, Switzerland

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.711904
title: Pollen profile KAZGOLU, Kaz Gölü, Turkey

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.739066
title: Pollen profile BRASPART, Saint Michel de Braspart, France

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.832279
title: Pore water geochemistry of sediment core PC-KX4, Potter Cove, King Georg Island
DOI: 10.1594/pangaea.787518
title: (Table T5) Mineralogy and geochemistry of brown hornblende from ODP Hole 176-735B

description: Sediment depth is given in mbsf. #0.1 = traces.
DOI: 10.1594/pangaea.708386
title: (Table 1) Boron and Beryllium concentrations and isotopic compositions of single tephra particles from ODP Site 135-835

description: Age was erroneously given in Ma, recalculated to ka on 2017-09-28.
DOI: 10.1594/pangaea.751323
title: Meteorological observations during Prince Rupert cruise from Gravesend to Moose started at 1778-06-26
DOI: 10.1594/pangaea.787563
title: (Table 3) Chemistry of pyroxene from ODP Holes 134-832B and 134-833B

description: Calculated on the basis of 6 O.
DOI: 10.1594/pangaea.682040
title: (Table 2) Abundance of Cycladophora davisiana davisiana and isotope stage determination in upper Pliocene and Pleistocene sediments of DSDP Hole 94-611 in the North Atlantic
DOI: 10.1594/pangaea.787468
title: (Table T12) Major element oxides and cations of zeolite from ODP Hole 176-735B veins

description: Number of ions is calculated on the basis of 40 oxygen atoms.
DOI: 10.1594/pangaea.496861
title: Physical oceanography from BT during cruise K90AIB_1960
DOI: 10.1594/pangaea.746662
title: Contents of the main rock-forming chemical elements in basalts from the Mid-Atlantic Ridge sampled at Station 49D
DOI: 10.1594/pangaea.746663
title: Contents of the main rock-forming chemical elements in basalts from the Mid-Atlantic Ridge sampled at Station 67D
DOI: 10.1594/pangaea.746664
title: Contents of the main rock-forming chemical elements in basalts from the Mid-Atlantic Ridge sampled at Station 68D
DOI: 10.1594/pangaea.668010
title: Basic measurements of radiation at station Boulder (2001-09)
DOI: 10.1594/pangaea.777451
title: Compiled seafloor spreading magnetic anomaly isochron positions for the Weddell Sea and Scotia Sea
DOI: 10.1594/pangaea.694818
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station FEBR-1998-MNB1

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore filters. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).
DOI: 10.1594/pangaea.878146
title: Tree-ring width of Pinus uncinata at site CAV
DOI: 10.1594/pangaea.741104
title: Lithology of sediment core AE3, Aegelsee, Switzerland

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.752328
title: Meteorological observations during STAG cruise from Spithead to Funchal started at 1797-04-07
DOI: 10.1594/pangaea.746650
title: Contents of the main rock-forming chemical elements in basalts from the Mid-Atlantic Ridge sampled at Station 15S-19
DOI: 10.1594/pangaea.695570
title: Expanded measurements from station Ny-Ålesund (2007-08)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.770018
title: (Table 2) Abundance of the main groups of planktonic animals in the 250-900 m water layer at the Broken Spur and Lost City sites according to visual counts from the Mir manned submersibles in 2002 and 2005

description: Three dives of the Mir manned submersibles with plankton counts and two vertical plankton hauls with a BR net were carried out above the Lost City (Atlantis underwater massif) and the Broken Spur hydrothermal fields during cruise 50 of R/V Akademik Mstislav Keldysh. Above the Atlantis seamount no significant increase in plankton concentration was found. Above the Lost City field horizontal heterogeneity of plankton distribution in the near-bottom layer and in overlying water layers was shown. Near-bottom aggregations of euphausiids and amphipods previously reported by other scientists seem to be related to attraction of these animals by the submersible's headlights rather than represent a natural phenomenon.
description: Supplement to: Vinogradov, Georgy M; Vereshchaka, Alexander L (2006): Zooplankton distribution above the Lost City (Atlantis massif) and Broken Spur hydrothermal fields in the North Atlantic according to the data of visual observations. Translated from Okeanologiya, 2006, 46(2), 238-248, Oceanology, 46(2), 217-227
DOI: 10.1594/pangaea.526638
title: Relative abundance of amino acids of humic acid in sediment core GIK12379-1, NW African continental margin (Table VIIe)
DOI: 10.1594/pangaea.751774
title: Meteorological observations during RIPPON cruise from Boston to Spithead started at 1769-08-05
DOI: 10.1594/pangaea.696430
title: Concentrations of total organic carbon in waters of the Baltic Sea at Station VA-10_2

description: Not filtered water samples were taken in 10 ml ampoules (sealed immediately after being acidified with phosphoric acid to pH&lt;2, sampling), or 40 ml screw-lid vials, and measured onboard at sampling or next days, or frozen (-20°C) until being acidified and measured in home labs.Carbon measurement was by high-temperature catalytic oxydation in a 10 cm column packed with 5% Pt on aluminum oxide beads at 900°C in a stream of oxygen, and CO2 detection by infrared extinction after the removal of moisture and SO2 by appropriate traps (cold trap, Mg-percarbonate, Na-pyrophosphate, tin, bronze or Sulfix). The apparatus was the dual channel Dimatek 2000 equipped with a Binos 200 detector.
DOI: 10.1594/pangaea.746002
title: (Table 6) Major- and trace-element composition of mainly metalliferous sediments from the Messinian of ODP Hole 107-652A
DOI: 10.1594/pangaea.777204
title: (Table 4) Representative analyses of Cr-spinel, ilmenite and magnetite from ODP Leg 127 samples
DOI: 10.1594/pangaea.695573
title: Expanded measurements from station Ny-Ålesund (2007-11)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.692290
title: Particulate organic carbon and nitrogen concentrations in water samples collected at Station SEPT-1997-GN36199704605MSB06 in the Aegean Sea

description: Seawater samples (1-5 l depending on distance of a station from a coast and depth of sampling) were filtered through Whatman GF/F filters (diameter 2.5 cm). Then the filters were wrapped in aluminium foil and stored at 22°C until analysis according to Hedges and Stern (Hedges, J.I., Stern, J.H. 1984. Carbon and nitrogen determinations of carbonate-containing solids. Limnol. Oceanogr., 29(3), 657-663; http://www.aslo.org/lo/toc/vol_29/issue_3/0657.pdf)
DOI: 10.1594/pangaea.741233
title: Lithology of sediment core CLAP69, Clapeyret, France

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.751226
title: Meteorological observations during PLANCIUS cruise from Nederland to Java started at 1848-03-06
DOI: 10.1594/pangaea.804436
title: (Table 2) Pore fluid pressure at DSDP Leg 84 Sites
DOI: 10.1594/pangaea.741403
title: Lithology of sediment core IVAN5, Ivanovskoye Peat Bog, Russia

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.677517
title: Ozone measurements from station Ny-Ålesund (2005-09)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.691324
title: Mesozooplankton average mass during Akademik Kovalevsky cruise AK7/3, Part II

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 0.145 mm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-500 m) and closed at the upper depth level. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved in 3-4% buffered formaldehyde and processed on return to the laboratory. All of copepods were identified to genus level, other taxanomic groups - to type, class, order and family levels.
DOI: 10.1594/pangaea.496923
title: Physical oceanography from BT during cruise M901JB_1990
DOI: 10.1594/pangaea.741404
title: Lithology of sediment core JAMMERTA, Jammertal, Germany

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.495290
title: Water temperature XBT profiles from cruise U31KN49352_1975
DOI: 10.1594/pangaea.665049
title: Oceanography at CTD/bottle station IFREMER_1889
DOI: 10.1594/pangaea.691342
title: Mesozooplankton average mass during Akademik Kovalevsky cruise AK7/5, Part II

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 0.145 mm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-500 m) and closed at the upper depth level. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved in 3-4% buffered formaldehyde and processed on return to the laboratory. All of copepods were identified to genus level, other taxanomic groups - to type, class, order and family levels.
DOI: 10.1594/pangaea.678097
title: Expanded measurements from station Ny-Ålesund (1994-09)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.678142
title: Expanded measurements from station Ny-Ålesund (1998-08)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.675053
title: Radiosonde measurements from station Ny-Ålesund (2006-01)
DOI: 10.1594/pangaea.776882
title: Headspace-gas measurements from IODP Hole 331-C0017A

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.877133
title: Continuous water level observations at station BEFmate_I1pio (2016-10)
DOI: 10.1594/pangaea.670728
title: Basic and other measurements of radiation at station Ny-Ålesund (2002-05)
DOI: 10.1594/pangaea.670755
title: Basic and other measurements of radiation at station Ny-Ålesund (2004-10)
DOI: 10.1594/pangaea.792584
title: Basic measurements of radiation at station Sapporo (2012-07)
DOI: 10.1594/pangaea.741629
title: Lithology of sediment core PAIDRE, Påidre, Estonia

description: This dataset was archived on 2010-05-11 from the EPD database.