cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.708709
title: (Table 6) Selenium isotopic composition of sediment samples from ODP Site 185-1149

description: Multiple-collector inductively coupled plasma mass spectrometry has been used for the precise measurement of the isotopic composition of Se in geological samples. Se is chemically purified before analysis by using cotton impregnated with thioglycollic acid. This preconcentration step is required for the removal of matrix-interfering elements for hydride generation, such as transitional metals, and also for the quantitative separation of other hydride-forming elements, such as Ge, Sb, and As. The analyte is introduced in the plasma torch with a continuous-flow hydride generation system. Instrumental mass fractionation is corrected with a “standard-sample bracketing” approach. By use of this new technique, the minimum Se required per analysis is lowered to 10 ng, which is one order of magnitude less than the amount needed for the N-TIMS technique. The estimated external precision calculated for the 82Se/76Se isotope ratio is 0.25‰ (2 sigma), and the data are reported as delta notation (‰) relative to our internal standard (MERCK elemental standard solution). Measurements of Se isotopes are presented for samples of standard solutions and geological reference materials, such as silicate rocks, soils, and sediments. The Se isotopic composition of selected terrestrial and extraterrestrial materials are also presented. An overall Se isotope variation of 8‰ has been observed, suggesting that Se isotopes fractionate readily and are extremely useful tracers of natural processes.
DOI: 10.1594/pangaea.497489
title: Physical oceanography from BT during cruise U58AA02063B_1984
DOI: 10.1594/pangaea.824462
title: P-Wave velocity (PWL) from IODP Hole 318-U1358B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.780474
title: (Table T1) Calcium carbonate content, brightness and reflectance for discrete color bands in ODP Site 188-1165 and Hole 188-1167A

description: Sediment depth is given in mbsf. Factors scores were calculated using entire spectral range (250-850 nm).
DOI: 10.1594/pangaea.828467
title: Pass-through measurements of magnetic susceptibility from IODP Hole 323-U1339D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.477364
title: Hydrochemistry measured on water bottle samples at station SAtl_1983-84_6N_0E/1-1

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.828472
title: Pass-through measurements of magnetic susceptibility from IODP Hole 323-U1341A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.828696
title: Interstitial water analysis from IODP Hole 336-U1383E

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.497796
title: Physical oceanography from BT during cruise U58X000041B_1959
DOI: 10.1594/pangaea.499152
title: Physical oceanography from BT during cruise U90X008371B_1984
DOI: 10.1594/pangaea.668225
title: Basic measurements of radiation at station Camborne (2006-10)
DOI: 10.1594/pangaea.872172
title: Links to master tracks in different resolutions from POLAR 5 flight WEGAS_2009/10_03
DOI: 10.1594/pangaea.821790
title: Length changes of Austrian glaciers 1981/1982
DOI: 10.1594/pangaea.827373
title: Spatially explicit estimates of length and biomass of Micromesistius poutassou (Blue Whiting) from acoustic and trawl surveys in the North-East Atlantic in May 2005

description: Acoustic estimates of herring and blue whiting abundance were obtained during the surveys using the Simrad ER60 scientific echosounder. The allocation of NASC-values to herring, blue whiting and other acoustic targets were based on the composition of the trawl catches and the appearance of echo recordings. To estimate the abundance, the allocated NASC -values were averaged for ICES-squares (0.5° latitude by 1° longitude). For each statistical square, the unit area density of fish (rA) in number per square nautical mile (N*nm-2) was calculated using standard equations (Foote et al., 1987; Toresen et al., 1998). To estimate the total abundance of fish, the unit area abundance for each statistical square was multiplied by the number of square nautical miles in each statistical square and then summed for all the statistical squares within defined subareas and over the total area. Biomass estimation was calculated by multiplying abundance in numbers by the average weight of the fish in each statistical square then summing all squares within defined subareas and over the total area. The Norwegian BEAM soft-ware (Totland and Godø 2001) was used to make estimates of total biomass.
description: The research leading to these results received (partial/full) funding from the European Commission FP7 EURO-BASIN (European Basin-Scale Anal ysis, Synthesis, and Integration; Grant Agreement 264 933).
DOI: 10.1594/pangaea.526628
title: Amino acid analysis of the sediment in sediment core GIK12379-1, NW African continental margin (Table VIIb)
DOI: 10.1594/pangaea.664649
title: Oceanography at CTD/bottle station IFREMER_1489
DOI: 10.1594/pangaea.827191
title: Spatially explicit estimates of length and biomass of Clupea harengus (Norwegian spring spawning herring) from acoustic and trawl surveys in the North-East Atlantic in May 2005

description: Acoustic estimates of herring and blue whiting abundance were obtained during the surveys using the Simrad ER60 scientific echosounder. The allocation of NASC-values to herring, blue whiting and other acoustic targets were based on the composition of the trawl catches and the appearance of echo recordings. To estimate the abundance, the allocated NASC -values were averaged for ICES-squares (0.5° latitude by 1° longitude). For each statistical square, the unit area density of fish (rA) in number per square nautical mile (N*nm-2) was calculated using standard equations (Foote et al., 1987; Toresen et al., 1998). To estimate the total abundance of fish, the unit area abundance for each statistical square was multiplied by the number of square nautical miles in each statistical square and then summed for all the statistical squares within defined subareas and over the total area. Biomass estimation was calculated by multiplying abundance in numbers by the average weight of the fish in each statistical square then summing all squares within defined subareas and over the total area. The Norwegian BEAM soft-ware (Totland and Godø 2001) was used to make estimates of total biomass.
description: The research leading to these results received (partial/full) funding from the European Commission FP7 EURO-BASIN (European Basin-Scale Anal ysis, Synthesis, and Integration; Grant Agreement 264 933).
DOI: 10.1594/pangaea.827192
title: Spatially explicit estimates of length and biomass of Clupea harengus (Norwegian spring spawning herring) from acoustic and trawl surveys in the North-East Atlantic in May 2006

description: Acoustic estimates of herring and blue whiting abundance were obtained during the surveys using the Simrad ER60 scientific echosounder. The allocation of NASC-values to herring, blue whiting and other acoustic targets were based on the composition of the trawl catches and the appearance of echo recordings. To estimate the abundance, the allocated NASC -values were averaged for ICES-squares (0.5° latitude by 1° longitude). For each statistical square, the unit area density of fish (rA) in number per square nautical mile (N*nm-2) was calculated using standard equations (Foote et al., 1987; Toresen et al., 1998). To estimate the total abundance of fish, the unit area abundance for each statistical square was multiplied by the number of square nautical miles in each statistical square and then summed for all the statistical squares within defined subareas and over the total area. Biomass estimation was calculated by multiplying abundance in numbers by the average weight of the fish in each statistical square then summing all squares within defined subareas and over the total area. The Norwegian BEAM soft-ware (Totland and Godø 2001) was used to make estimates of total biomass.
description: The research leading to these results received (partial/full) funding from the European Commission FP7 EURO-BASIN (European Basin-Scale Anal ysis, Synthesis, and Integration; Grant Agreement 264 933).
DOI: 10.1594/pangaea.917452
title: Fig. 3 (2008): Susc_Vol., Susc_freq; ARM; "SIRM"; against depth; Dating of a Last Glacial loess sequence by relative geomagnetic palaeointensity: A case study from the Middle Danube Basin (Süttö, Hungary)

description: A thorough rock- and palaeomagnetic investigation of an almost 13-m-thick Upper Pleistocene loessepalaeosol sequence (LPSS) outcropping near the village of Süttö in northern Hungarywas conducted to obtain rock magnetic and palaeomagnetic-based chronostratigraphies. The low-field susceptibility (Klf), the frequency-dependent susceptibility (Kfd), the ARM and the “S”IRM of the LPSS at Sütt}o are shown together in Fig. 3 as a function of the profile depth. The very high values at the top of the profile characterise recent soil (unit 1). With the beginning of the uppermost pure loess layer (unit 2), the susceptibility signal drops considerably and then slowly increases with increasing depth (age). Apart from the clearly higher susceptibility values that unambiguously correlate with the identified soils, there appears to be a quasi-linear increasing susceptibility trend in the uppermost loess section (unit 2), which is also weakly present in the frequency-dependent susceptibility (Kfd) and in the “S”IRM, but is not visible in the ARM. Generally, the primarily concentration-dependent parameters Klf, ARM and “S”IRM show a similar course with depth. The upper part of the sand unit at a depth of approximately 8 m is characterised by high susceptibility, no elevated frequency dependence and missing higher values for ARM but somewhat higher “S”IRM. The Max/Min variation in Klf and “S”IRM is less than one order of magnitude incontrast to the ARM, which has variations of more than one order of magnitude (Fig. 3).
DOI: 10.1594/pangaea.484574
title: Hydrochemistry measured on water bottle samples at station SAVE4/212-2

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.827197
title: Spatially explicit estimates of length and biomass of Clupea harengus (Norwegian spring spawning herring) from acoustic and trawl surveys in the North-East Atlantic in May 2011

description: Acoustic estimates of herring and blue whiting abundance were obtained during the surveys using the Simrad ER60 scientific echosounder. The allocation of NASC-values to herring, blue whiting and other acoustic targets were based on the composition of the trawl catches and the appearance of echo recordings. To estimate the abundance, the allocated NASC -values were averaged for ICES-squares (0.5° latitude by 1° longitude). For each statistical square, the unit area density of fish (rA) in number per square nautical mile (N*nm-2) was calculated using standard equations (Foote et al., 1987; Toresen et al., 1998). To estimate the total abundance of fish, the unit area abundance for each statistical square was multiplied by the number of square nautical miles in each statistical square and then summed for all the statistical squares within defined subareas and over the total area. Biomass estimation was calculated by multiplying abundance in numbers by the average weight of the fish in each statistical square then summing all squares within defined subareas and over the total area. The Norwegian BEAM soft-ware (Totland and Godø 2001) was used to make estimates of total biomass.
description: The research leading to these results received (partial/full) funding from the European Commission FP7 EURO-BASIN (European Basin-Scale Anal ysis, Synthesis, and Integration; Grant Agreement 264 933).
DOI: 10.1594/pangaea.664162
title: Oceanography at CTD/bottle station IFREMER_1003
DOI: 10.1594/pangaea.822430
title: Meteorological measurements in the upper air at station Tashkent, 1958-07-03 to 1958-07-24, ERA-CLIM ID 4687
DOI: 10.1594/pangaea.827221
title: Spatially explicit estimates of length and biomass of Clupea harengus (Norwegian spring spawning herring) from acoustic and trawl surveys in the North-East Atlantic in May 2009

description: Acoustic estimates of herring and blue whiting abundance were obtained during the surveys using the Simrad ER60 scientific echosounder. The allocation of NASC-values to herring, blue whiting and other acoustic targets were based on the composition of the trawl catches and the appearance of echo recordings. To estimate the abundance, the allocated NASC -values were averaged for ICES-squares (0.5° latitude by 1° longitude). For each statistical square, the unit area density of fish (rA) in number per square nautical mile (N*nm-2) was calculated using standard equations (Foote et al., 1987; Toresen et al., 1998). To estimate the total abundance of fish, the unit area abundance for each statistical square was multiplied by the number of square nautical miles in each statistical square and then summed for all the statistical squares within defined subareas and over the total area. Biomass estimation was calculated by multiplying abundance in numbers by the average weight of the fish in each statistical square then summing all squares within defined subareas and over the total area. The Norwegian BEAM soft-ware (Totland and Godø 2001) was used to make estimates of total biomass.
description: The research leading to these results received (partial/full) funding from the European Commission FP7 EURO-BASIN (European Basin-Scale Anal ysis, Synthesis, and Integration; Grant Agreement 264 933).
DOI: 10.1594/pangaea.495271
title: Water temperature MBT profiles from cruise U3190217M_1954
DOI: 10.1594/pangaea.664156
title: Oceanography at CTD/bottle station IFREMER_0997
DOI: 10.1594/pangaea.496760
title: Physical oceanography from BT during cruise K58GSB_1967
DOI: 10.1594/pangaea.827190
title: Spatially explicit estimates of length and biomass of Clupea harengus (Norwegian spring spawning herring) from acoustic and trawl surveys in the North-East Atlantic in May 2004

description: Acoustic estimates of herring and blue whiting abundance were obtained during the surveys using the Simrad ER60 scientific echosounder. The allocation of NASC-values to herring, blue whiting and other acoustic targets were based on the composition of the trawl catches and the appearance of echo recordings. To estimate the abundance, the allocated NASC -values were averaged for ICES-squares (0.5° latitude by 1° longitude). For each statistical square, the unit area density of fish (rA) in number per square nautical mile (N*nm-2) was calculated using standard equations (Foote et al., 1987; Toresen et al., 1998). To estimate the total abundance of fish, the unit area abundance for each statistical square was multiplied by the number of square nautical miles in each statistical square and then summed for all the statistical squares within defined subareas and over the total area. Biomass estimation was calculated by multiplying abundance in numbers by the average weight of the fish in each statistical square then summing all squares within defined subareas and over the total area. The Norwegian BEAM soft-ware (Totland and Godø 2001) was used to make estimates of total biomass.
description: The research leading to these results received (partial/full) funding from the European Commission FP7 EURO-BASIN (European Basin-Scale Anal ysis, Synthesis, and Integration; Grant Agreement 264 933).
DOI: 10.1594/pangaea.818011
title: (Table 1) Organic geochemistry of sediments recovered from DSDP Leg 65 Holes

description: Pliocene-Pleistocene marls, muds, and hemipelagic clays with some beds of silt and sand were recovered on Leg 65 near the crest of the East Pacific Rise at the mouth of the Gulf of California. The organic matter in the sediments is mainly of marine origin for the upper Pleistocene sediments (0-0.61 m.y.), while the lower Pleistocene deposits (0.61- 1.80 m.y.) are characterized by continental organic matter except near the bottom of the sediment section in Hole 483A, where marine organic matter was found. The sediments belong to an early stage of geochemical evolution, except in Hole 482D, where hydrothermal effects are invoked to explain the maturity of the organic matter above the basement.
description: Sediment depth is given in mbsf. Empty cells mean not determined.
description: Supplement to: Deroo, Gerard; Herbin, Jean-Paul (1983): The nature, origin, and distribution of organic material at Deep Sea Drilling Sites 482 through 485, Leg 65, in the Gulf of California. In: Lewis, BTR; Robinson, P; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 65, 431-438
DOI: 10.1594/pangaea.917055
title: 1-Hz PPP displacements at GEONET station 0879 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.917057
title: 1-Hz PPP displacements at GEONET station 0881 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.917060
title: 1-Hz PPP displacements at GEONET station 0884 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.828603
title: Magnetic remanence from IODP Hole 323-U1344B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.916768
title: 1-Hz PPP displacements at GEONET station 0577 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.917247
title: 1-Hz PPP displacements at GEONET station 1077 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.477143
title: Hydrochemistry measured on water bottle samples at station NPac_1974_RY_136E/4471

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.744440
title: Physical oceanography during W. Beukelsz cruise WB71/2 to the North Sea
DOI: 10.1594/pangaea.824852
title: Magnetic remanence from IODP Hole 334-U1378B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.902963
title: Calcareous nannofossils absolute abundance and accumulation rates from DSDP Site 80-549 and 80-551
DOI: 10.1594/pangaea.477631
title: Hydrochemistry measured on water bottle samples at station SPac_1967_ET_28S/120

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.826432
title: Natural gamma radiation from IODP Hole 329-U1367C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.663871
title: Oceanography at CTD/bottle station IFREMER_0711
DOI: 10.1594/pangaea.826468
title: P-Wave velocity (PWB) from IODP Hole 329-U1367E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.477765
title: Hydrochemistry measured on water bottle samples at station SPac_1967_ET_43S/5

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.494768
title: Physical oceanography during cruise N58LA00003C
DOI: 10.1594/pangaea.477816
title: Hydrochemistry measured on water bottle samples at station SPac_1968_HH_170W/2-2

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.826479
title: Natural gamma radiation from IODP Hole 329-U1367F

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.477313
title: Hydrochemistry measured on water bottle samples at station NPac_1985_TT_47Na/53-1

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.484577
title: Hydrochemistry measured on water bottle samples at station SAVE4/215-2

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.723325
title: Description of profile 7140-310
DOI: 10.1594/pangaea.900844
title: Stable isotope ratios of Planulina wuellerstorfi of IODP Site 353-U1443

description: Isotope values were first specified with one decimal place, corrected to 3 decimal places (2020-01-21).
DOI: 10.1594/pangaea.733265
title: Physical oceanography during Kaimikai O Kanaloa cruise HOT-115 on section PRS2
DOI: 10.1594/pangaea.751121
title: Meteorological observations during PEGASUS cruise from St. Maarten to Suriname started at 1832-12-09
DOI: 10.1594/pangaea.758800
title: Oxygen and carbon isotope measurements of North Atlantic from IODP Hole 307-U1317E

description: Recent deep-ocean exploration has revealed unexpectedly widespread and diverse coral ecosystems in deep water on continental shelves, slopes, seamounts, and ridge systems around the world. Origin and growth history of these cold-water coral mounds are poorly known, owing to a lack of complete stratigraphic sections through them. Here we show high-resolution oxygen isotope records of planktic foraminifers from the base to the top of Challenger Mound, southwest of Ireland, which was drilled during Integrated Ocean Drilling Program Expedition 307. Challenger Mound began to grow during isotope stage 92 (2.24 million years ago (Ma)), immediately after the onset of Northern Hemisphere glaciation and the initiation of modern stratification in the northeast Atlantic. Mound initiation was likely due to reintroduction of Mediterranean Outflow Water (MOW) and ensuing development of a density gradient with overlying northeastern Atlantic water (NEAW), where organic matter was prone to be stagnated and fueled the coral ecosystem. Coral growth continued for 11 glacial-interglacial cycles until isotopic stage 72 (1.82 Ma) with glacial siliciclastic input from the continental margin. After a long hiatus that separates the lower mound and the upper mound, coral growth restored for a short time in isotope stages 19-18 (0.8-0.7 Ma) in which sediments were either eroded or not deposited during a full glacial stage. The development pattern of the water mass interface between MOW and NEAW might have changed, because of the fluctuations of the MOW production which is responsible for the amplitude in ice volume oscillations from the low-amplitude 41 ka cycles for the lower mound to the high-amplitude 100 ka cycles for the upper mound. The average sedimentation and CaCO3 production rates of the lower mound were evaluated 27 cm/ka and 31.1 g/cm2/ka, respectively.
description: Supplement to: Sakai, Saburo; Kano, Akihiro; Abe, Kohei (2009): Origin, glacial-interglacial responses, and controlling factors of a cold-water coral mound in NE Atlantic. Paleoceanography, 24(2), PA2213
DOI: 10.1594/pangaea.498543
title: Physical oceanography from BT during cruise U90PO07115B_1957