cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.688833
title: Radiosonde M16_R216 during METEOR cruise M16 on 1969-02-20 21:31h

description: Height of tropause 17280 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.779934
title: Sea surface temperature estimation (Uk37) of several sediment cores in the eastern North Atlantic
DOI: 10.1594/pangaea.229890
title: Sound velocity of Hole 85-572C
DOI: 10.1594/pangaea.52454
title: (Table 4) Stable carbon and oxygen isotope ratios of foraminifera in sediment core PAR87A-10
DOI: 10.1594/pangaea.688807
title: Radiosonde M16_R079 during METEOR cruise M16 on 1969-02-07 08:57h

description: Height of tropause 15030 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.688811
title: Radiosonde M16_R098 during METEOR cruise M16 on 1969-02-09 09:02h

description: Height of tropause 15370 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.688813
title: Radiosonde M16_R108 during METEOR cruise M16 on 1969-02-10 08:52h

description: Height of tropause 15240 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.810448
title: (Table 1) Ooze/chalk cycles: frequency of occurrence at DSDP Leg 74 Sites

description: Shallow- to deep-water environments are represented by the sediments and rocks recovered from the Walvis Ridge- Angola Basin transect. These calcareous oozes, chalks, limestones, and volcaniclastic sedimentary rocks are used to define and correlate four lithostratigraphic units. The sediments were deposited in cycles which represent recurring tectonic or Oceanographic events and may be related to climatic fluctuations and orbital perturbations.Turbidites are the most common and easily identified sedimentary cycle. They are Late Cretaceous to Paleocene in age and are repeated in intervals ranging from thousands to tens of thousands of years. They are also found interbedded between basalt layers. Turbidites are easily distinguished from the other cycles present by their sedimentary structures, mineral composition, alteration products, and physical properties (GRAPE) data. Large-scale turbidites, debris, or slump breccias are found at or just above the Cretaceous/Tertiary boundary and indicate an event of considerable energy possibly related to intense tectonic activity.Diagenetic cycles, interpreted as small-scale dissolution cycles or sequences produced by biogenic activity, occur in early Paleocene chalks. The recurrence intervals average -20,000 y. but have a wide range of values. Variations in CaCO3 content, color, gradational boundaries, and trace fossil content characterize these sediments. These cycles reflect bottom-water conditions.Ooze-chalk cycles occur in upper Oligocene to upper Paleocene sediments and represent conditions that once existed at the sediment/water interface where they obtained their diagenetic potential. These oscillations are repeated over tens of thousands of years and may have no modern analogs.Color variations in sediments at the Cretaceous/Tertiary boundary indicate local fluctuations in oxygen content within the sediments or the water column. This situation lasted for several hundred thousand years and is not repeated elsewhere in the sequence.Large dissolution cycles are recorded in the sediments at Site 527 that are of middle Miocene and early Oligocene to middle Eocene age. During this time the seafloor at this site appears to have been located at or subsided to a depth occupied by a fluctuating CCD and lysocline.
description: Supplement to: Borella, Peter E (1984): Sedimentology, petrology, and cyclic sedimentation patterns, Walvis Ridge Transect, Leg 74, Deep Sea Drilling Project. In: Moore, TC Jr; Rabinowitz, PD; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 74, 645-662
DOI: 10.1594/pangaea.664518
title: Oceanography at CTD/bottle station IFREMER_1358
DOI: 10.1594/pangaea.688792
title: Radiosonde M16_R015 during METEOR cruise M16 on 1969-01-29 08:10h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.688798
title: Radiosonde M16_R034 during METEOR cruise M16 on 1969-02-02 08:59h

description: Height of tropause 15970 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.688823
title: Radiosonde M16_R158 during METEOR cruise M16 on 1969-02-15 09:34h

description: Height of tropause 15680 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.754215
title: Radiosonde PS76/31630 during POLARSTERN cruise ARK-XXV/3 on 2010-10-03 11:00h

description: Height of tropopause 10004 m, precipitable water content 1.4022 cm
DOI: 10.1594/pangaea.924451
title: Compilation of swath-mapping bathymetry from oceanic transform fault systems - a global approach

description: Bathymetric data from oceanic transform faults and their associated fracture zones were compiled, providing high-resolution gridded seafloor topography. Data used in this compilation were open and archived at US American National Oceanographic and Atmospheric Administration (https://maps.ngdc.noaa.gov/viewers/bathymetry), Japan Agency for Marine-Earth Science and Technology (http://www.godac.jamstec.go.jp/darwin/e), and the German Datacenter for bathymetric data (https://www.bsh.de/EN/DATA/Oceanographic_Data_Center/Surveying_data/surveying_data_node). Data were processed and gridded using Multibeam System (https://www.mbari.org/products/research-software/mb-system) and can be displayed using Generic Mapping Tools (https://gmt.soest.hawaii.edu). All grids are in netCDF format. The compilation includes transform faults and fracture zones from the Northern and Southern East Pacific Rise, the Cosos-Nazca spreading center, Chile Rise and the Pacific Antarctic Ridge, the Southwest Indian Ridge, Central Indian Ridge and Southeast Indian Ridge as well as the Mid-Atlantic Ridge.
DOI: 10.1594/pangaea.536195
title: Relatiev abundance of benthic foraminifera in surface sediments of the NW African continental margin (Table 5)
DOI: 10.1594/pangaea.810329
title: (Table 1) Sand, silt and clay at DSDP Leg 75 Holes

description: The distribution of sand, silt, and clay was determined on 10-cm**3 sediment samples collected at the time the cores were split and described. The sediment classification used here is that of Shepard (1954), with the sand, silt, and clay boundaries based on the Westbrook (1922) scale. Thus, the sand, silt, and clay fractions are composed of particles whose diameters range, respectively, from 2000 to 62.5 µm, 62.5 to 3.91 µm, and less than 3.91 µm. This classification is applied regardless of sediment type and origin; therefore, the sediment names used in this table may differ from those used elsewhere in this volume, e.g., a slit composed of nannofossils in this table may be called a nannofossil ooze in a site summary chapter. Standard sieve and pipette methods were used to determine the grain-size distribution. The sediment sample was dried and dispersed in a Calgon solution. If a sediment sample failed to disaggregate, it was treated with a sonic probe and, if necessary, hydrogen peroxide. Sediment samples which resisted this treatment were not analyzed.
description: Supplement to: Bode, Gerald W (1984): Appendix I. Grain-size analyses. In: Hay, WW; Sibuet, J-C; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 75, 1301-1303
DOI: 10.1594/pangaea.434029
title: Hourly sea level from coastal tide gauge station Charleston in 1930 (Research quality database)
DOI: 10.1594/pangaea.434075
title: Hourly sea level from coastal tide gauge station Charleston in 1976 (Research quality database)
DOI: 10.1594/pangaea.824124
title: Carbonate measurements during the GEOSECS Atlantic expedition
DOI: 10.1594/pangaea.434073
title: Hourly sea level from coastal tide gauge station Charleston in 1974 (Research quality database)
DOI: 10.1594/pangaea.920396
title: Continuous water level observations at station BEFmate_I3low (2019-06)
DOI: 10.1594/pangaea.434048
title: Hourly sea level from coastal tide gauge station Charleston in 1949 (Research quality database)
DOI: 10.1594/pangaea.665467
title: Oceanography at CTD/bottle station IFREMER_2307
DOI: 10.1594/pangaea.434051
title: Hourly sea level from coastal tide gauge station Charleston in 1952 (Research quality database)
DOI: 10.1594/pangaea.434052
title: Hourly sea level from coastal tide gauge station Charleston in 1953 (Research quality database)
DOI: 10.1594/pangaea.755286
title: (Table 5) Vertical distribution of biomass of Euphausiacea, Amphipoda, Mysidacea, and Ostracoda in the Sea of Japan at Station VITYAZ7519
DOI: 10.1594/pangaea.664102
title: Oceanography at CTD/bottle station IFREMER_0943
DOI: 10.1594/pangaea.688817
title: Radiosonde M16_R126 during METEOR cruise M16 on 1969-02-12 09:27h

description: Height of tropause 17160 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.434034
title: Hourly sea level from coastal tide gauge station Charleston in 1935 (Research quality database)
DOI: 10.1594/pangaea.434035
title: Hourly sea level from coastal tide gauge station Charleston in 1936 (Research quality database)
DOI: 10.1594/pangaea.688719
title: (Appendix B1) Diversity, abundance and preservation of calcareous nannofossils from the Paleocene-Eocene Thermal Maximum of ODP Hole 207-1260B in the equatorial Atlantic

description: Counting with cross-polarized light at magnification of x1250. &lt;1 = species present
DOI: 10.1594/pangaea.434038
title: Hourly sea level from coastal tide gauge station Charleston in 1939 (Research quality database)
DOI: 10.1594/pangaea.434042
title: Hourly sea level from coastal tide gauge station Charleston in 1943 (Research quality database)
DOI: 10.1594/pangaea.434045
title: Hourly sea level from coastal tide gauge station Charleston in 1946 (Research quality database)
DOI: 10.1594/pangaea.665490
title: Oceanography at CTD/bottle station IFREMER_2330
DOI: 10.1594/pangaea.805681
title: Physical oceanography at time series station BATS in 1996
DOI: 10.6084/m9.figshare.24532310
title: Additional file 2 of A model-based clustering via mixture of hierarchical models with covariate adjustment for detecting differentially expressed genes from paired design

description: Additional file 2: Table S1.Gene list of 6 UE transcripts detected by limma.
DOI: 10.1594/pangaea.779348
title: (Appendix A) Major element composition of serpentine, brucite, Fe- and Cl-rich hydroxide pseudomorphs and vein fillings of DSDP Hole 84-566C serpentinite

description: Sample S021 = 84-566C-6-1,9-12 piece 1, 117.3 to 117.6 mbsf.
DOI: 10.1594/pangaea.927328
title: M162 GLORIA-FLOW, Heat flow data at station HF2015

description: Heat flow data, taken with the 6 m Bremen heat probe during M162 in the Gulf of Cadiz. Heat flow data were measured across fault zones to support the idea of fluid transport along leaking faults.
DOI: 10.6084/m9.figshare.24355149
title: Additional file 2 of Estimated indirect costs of haemodialysis versus peritoneal dialysis from a patients’ perspective at an Academic Hospital in Pretoria, South Africa

description: Additional file 2.
DOI: 10.1594/pangaea.920291
title: Continuous water level observations at station BEFmate_I3upp (2017-11)
DOI: 10.1594/pangaea.922859
title: Lowered ADCP data at 47°N in the subpolar North Atlantic

description: Current measurements from a total of 14 cruises that were carried out in the subpolar North Atlantic between 2003 and 2017. The data set comprises 525 stations along a line that, from west to east, crosses Flemish Cap at about 47° N and reaches the European continental slope at about 49° N. Two Teledyne RDI 300 kHz Workhorse Monitor acoustic Doppler current profiler (ADCPs), one upward and one downward looking, were mounted into the water sampler to measure velocities during CTD casts. The raw data were processed to yield full depth profiles of horizontal velocity with a vertical resolution of 10 m. Barotropic tidal velocity was obtained from the global TPXO model at each station and was then subtracted from the lowered ADCP velocity profiles.
DOI: 10.1594/pangaea.404794
title: Water temperature and current velocity from surface drifter SVP_9300691
DOI: 10.1594/pangaea.927319
title: M162 GLORIA-FLOW, Heat flow data at station HF2006

description: Heat flow data, taken with the 6 m Bremen heat probe during M162 in the Gulf of Cadiz. Heat flow data were measured across fault zones to support the idea of fluid transport along leaking faults.
DOI: 10.1594/pangaea.920289
title: Continuous water level observations at station BEFmate_I3upp (2017-09)
DOI: 10.1594/pangaea.663444
title: Oceanography at CTD/bottle station IFREMER_0284
DOI: 10.1594/pangaea.689146
title: Radiosonde M2_R177 during METEOR cruise M2 on 1965-10-03 18:56h

description: Height of tropause 15790 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.665718
title: Oceanography at CTD/bottle station IFREMER_2544
DOI: 10.6084/m9.figshare.24531938
title: Additional file 1 of Omic horizon expression: a database of gene expression based on RNA sequencing data

description: Additional file 1: Brief information of 2,762 samples based on the sequencing run data. Rat strain, age, sex and the associated PubMed IDs are indicated when the information is available on the NCBI web pages
DOI: 10.6084/m9.figshare.24531938.v1
title: Additional file 1 of Omic horizon expression: a database of gene expression based on RNA sequencing data

description: Additional file 1: Brief information of 2,762 samples based on the sequencing run data. Rat strain, age, sex and the associated PubMed IDs are indicated when the information is available on the NCBI web pages
DOI: 10.1594/pangaea.315446
title: (Table 1) Range table of planktonic foraminifers from ODP Hole 166-1006A sediments
DOI: 10.1594/pangaea.601810
title: Meteorological observation at anchor station Meteor366 in the Westafrican area of upwelling
DOI: 10.1594/pangaea.665479
title: Oceanography at CTD/bottle station IFREMER_2319
DOI: 10.1594/pangaea.920298
title: Continuous water level observations at station BEFmate_I3upp (2018-06)
DOI: 10.1594/pangaea.844145
title: Hydrochemistry measured on water bottle samples in the North Atlantic subpolar gyre during SURATLANT cruise AGSK20070203
DOI: 10.6084/m9.figshare.24531999
title: Additional file 1 of Clinical characteristics of hospitalized patients with Nocardia genus detection by metagenomic next generation sequencing in a tertiary hospital from southern China

description: Additional file 1: Supplementary table 1. Patients characterics of ND.
DOI: 10.6084/m9.figshare.24531999.v1
title: Additional file 1 of Clinical characteristics of hospitalized patients with Nocardia genus detection by metagenomic next generation sequencing in a tertiary hospital from southern China

description: Additional file 1: Supplementary table 1. Patients characterics of ND.
DOI: 10.1594/pangaea.761103
title: (Table 3) Mineral composition of aerosols sampled over the North Atlantic in August 1995

description: &gt;0 = traces.
DOI: 10.1594/pangaea.915662
title: Continuous sediment temperature observations at station BEFmate_I7Low (2019-12)
DOI: 10.1594/pangaea.820766
title: Downwelling spectral irradiance as measured in different depths at radiometer station PS73/038-2
DOI: 10.6084/m9.figshare.24532319.v1
title: Additional file 2 of Management of links of interest in European Union expertise authorities dealing with plant protection products: comparative analysis and recommendations

description: Additional file 2. Selected criteria, filled in for the investigated competent authorities; detailed method used for data collection.
DOI: 10.1594/pangaea.917589
title: S27. Age model of ODP Site 207-1258
DOI: 10.1594/pangaea.805548
title: Total flux, particulate carbon and nitrogen from surface-tethered sediment traps at time series station BATS in 1993
DOI: 10.1594/pangaea.432668
title: Daily sea level from coastal tide gauge station Virginia_Key in 2000 (Research quality database)
DOI: 10.1594/pangaea.805547
title: Total flux, particulate carbon and nitrogen from surface-tethered sediment traps at time series station BATS in 1992
DOI: 10.1594/pangaea.432664
title: Daily sea level from coastal tide gauge station Virginia_Key in 1996 (Research quality database)
DOI: 10.1594/pangaea.432669
title: Daily sea level from coastal tide gauge station Virginia_Key in 2001 (Research quality database)
DOI: 10.1594/pangaea.744327
title: Physical oceanography during Scotia cruise Scotia05/2 to the North Sea
DOI: 10.1594/pangaea.844114
title: Hydrochemistry measured on water bottle samples in the North Atlantic subpolar gyre during SURATLANT cruise AGSK20030426
DOI: 10.1594/pangaea.800071
title: (Table 1) Anisotropy of magnetic susceptibility of basalts at DSDP Hole 89-462A

description: Measurements of the anisotropy of magnetic susceptibility (AMS) in basalts cored from 1070 to 1209 m sub-bottom depth in Hole 462A reveal that samples with a high ratio of maximum (K1) to minimum (K3) principal susceptibility show a prolate type of anisotropy in which K1 axes are nearly vertical. For other prolate types, K1 axes vary widely. Although the oblate type of AMS is less common among these basalts, K3 axes are nearly vertical in the upper units and horizontal in the lower units. The anisotropy of compressional wave velocities measured for the same specimen shows no correlation with the degree and type of AMS. This finding indicates that AMS could have been caused by variations in flows but not by compressive stress. Processes of emplacement of basaltic sills and flows must have been complex, because directions of principal axes of AMS vary from unit to unit.
description: Supplement to: Fujii, Naoyuki; Hamano, Yozo (1986): Anisotropy of basalts, Hole 462A, Nauru Basin, Deep Sea Drilling Project Leg 89. In: Moberly, R; Schlanger, SO; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 89, 647-650
DOI: 10.1594/pangaea.663710
title: Oceanography at CTD/bottle station IFREMER_0550
DOI: 10.1594/pangaea.784610
title: Radiosonde PS79/33502 during POLARSTERN cruise ANT-XXVIII/5 on 2012-05-01 10:50h

description: Height of tropopause 16954 m, precipitable water content 3.3108 cm
DOI: 10.1594/pangaea.792732
title: (Table 3) Stratigraphy, sedimentation rates, and mass accumulation rates from DSDP Leg 92 holes

description: The Glomar Challenger crossed the East Pacific Rise at 19°S on Leg 92 during the austral fall of 1983. The intent of the cruise was to recover sediments and rocks that would reveal the geologic history of seafloor hydrothermal activity as determined by the geochemistry and sedimentation history of hydrothermal material, the advection of sediment pore waters, the nature and history of alteration of seafloor basalt, and the paleoceanography of the southeast Pacific. Results show that the composition of hydrothermal material is determined by its source and modified by exposure to seawater during transport in the water column. The flux of hydrothermal sediment appears to increase during episodes of tectonic activity and ridge jumps but to be independent of spreading rate. Pore water advection in sediment may occur early in the depositional history of a site, but it does not appear to continue for more than 1 or 1.5 m.y. The basaltic rocks recovered are mostly low-olivine tholeiites, but those recovered at two sites contain ferrobasalt and alkali basalt. Hole 597C is the deepest penetration by the Deep Sea Drilling Project of fast-spreading crust. Basalts from that hole reveal three stages of alteration: an early deuteric stage, a reducing stage, and a later oxidative stage. K/Ar dates of alteration minerals suggest that alteration continues for 9 to 15 m.y. after the formation of crust. Paleoceanographic studies have defined the Neogene history of the compensation depth and lysocline, the timing of important changes in atmospheric transport processes, and the nature and age of significant intervals of reworking in the abyssal sediments.
description: Supplement to: Rea, David K; Leinen, Margaret W (1986): Neogene controls on hydrothermal activity and paleoceanography of the Southeast Pacific Ocean. In: Leinen, M; Rea DK; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 92, 597-617
DOI: 10.1594/pangaea.913717
title: In situ observational data of chlorophyll a of central-southern Chile

description: This dataset contains total and size-fractionated chlorophyll a samples in the micro-, nano- and pico-phytoplankton range collected in the upper layer (0, 5, 10, 15, 20, 30, and 40 m depth).
DOI: 10.1594/pangaea.789820
title: (Table 1) Bulk elemental composition at DSDP Holes 92-597, 92-598, and 92-599

description: The major element composition of Leg 92 sediments reflects the input of hydrothermal precipitates from the East Pacific Rise and extinct Mendoza Rise plus minor amounts of terrigenous detritus. The basal sediments are a mixture of hydrothermally precipitated ferromanganese oxyhydroxides and carbonates. In present and ancient sediments deposited 200 km or more from the rise crest, however, the amount of hydrothermal precipitates in the sediments decreases markedly. The distal deposits of hydrothermal particulates are also richer in iron because of fractionation by sedimentation processes. Slowly accumulating aluminosilicate detritus becomes a more important fraction of the sediments far from the rise crest as a result of the decrease of hydrothermal sedimentation.
description: Supplement to: Lyle, Mitchell W (1986): Major element composition of Leg 92 sediments. In: Leinen, M; Rea DK; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 92, 355-370
DOI: 10.1594/pangaea.805549
title: Total flux, particulate carbon and nitrogen from surface-tethered sediment traps at time series station BATS in 1994
DOI: 10.1594/pangaea.789695
title: (Table 1) Calcium carbonate and &lt;2 µm fractions of bulk sample and insoluble residue at DSDP Hole 92-597

description: Particles of red brown to yellow brown semiopaque oxides (RSO) dominate the insoluble residue fraction of the sediments at Site 597. Unlike the X-ray amorphous particles in the Bauer Deep sediments, these particles are composed of mainly goethite; the amount of X-ray amorphous ferric hydroxide and poorly crystalline ferromanganese oxyhydroxides is generally small relative to the amount of goethite. A qualitative goethite crystallinity index was established. The variations observed in the crystallinity of goethite with increasing depth and changes in lithology suggest that aging and long-term exposure to seawater in a high water/sediment regime influence and increase the rate of recrystallization of the Fe-oxyhydroxides of the RSO particles. The percentage of organic carbon is low in these sediments; it varies primarily between 0.2 and 0.4 wt.%. Phillipsite is present throughout the sediment column and is more concentrated in the youngest clay layer and in the oldest basal sediments.
description: Supplement to: Kastner, Miriam (1986): Mineralogy and diagenesis of sediments at Site 597: Preliminary results. In: Leinen, M; Rea DK; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 92, 345-349
DOI: 10.1594/pangaea.805550
title: Total flux, particulate carbon and nitrogen from surface-tethered sediment traps at time series station BATS in 1995
DOI: 10.1594/pangaea.846711
title: Basic measurements of radiation at station Chesapeake Light (2015-05)