cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.728775
title: (Table 8) Miocene-Pleistocene diatom biostratigraphy of ODP Hole 120-748B

description: R = rare ( one specimen of a particular species encountered in 5-20 fields of view using a 40X objective and 10X ocular), F = frequent (one specimen in every 5 fields), C = common (one specimen in every field), A = abundant (more than one species in every field), X = present, - = absent
DOI: 10.1594/pangaea.664755
title: Oceanography at CTD/bottle station IFREMER_1595
DOI: 10.1594/pangaea.668839
title: Basic measurements of radiation at station Carpentras (1999-01)
DOI: 10.1594/pangaea.668383
title: Physical oceanography of CTD station T8 off Independencia Bay, 2007, Peru
DOI: 10.1594/pangaea.816891
title: Quality codes of physical oceanography data during John P. Tully cruise IOS_96-01
DOI: 10.1594/pangaea.825630
title: Gamma ray attenuation bulk density from IODP Hole 329-U1371H

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.713879
title: Chlorophyll and Phaeopigments measured on water bottle samples at station Chipana_EW9Z2_24
DOI: 10.1594/pangaea.744403
title: Physical oceanography during Thetis cruise Thetis73/3 to the North Sea
DOI: 10.1594/pangaea.744416
title: Physical oceanography during Tridens cruise Tridens79/2 to the North Sea
DOI: 10.1594/pangaea.587136
title: Physical oceanography at CTD station M1_CTD252 of the Persian Gulf
DOI: 10.1594/pangaea.744381
title: Physical oceanography during Thalassa cruise Thalassa78/1 to the North Sea
DOI: 10.1594/pangaea.701716
title: Basic measurements of radiation at station Boulder (2005-09)
DOI: 10.1594/pangaea.769689
title: (Table 1) Key boundaries and synthetic seismograms from ODP Sites 161-976, 161-977 and 161-978

description: To constrain the timing of rifting in the western, eastern, and northern parts of the Alboran Sea basin, seismic reflectors, corresponding to biostratigraphic boundaries and unconformities from the Miocene to Recent, are correlated using synthetic seismograms. Regions of adjacent coeval compression and extension are found in the Alboran Sea basin. Normal faulting continues in parts of the eastern Alboran Sea basin later than in the western Alboran Sea basin. Seismic reflection data in the vicinity of ODP Site 976 (western Alboran Sea basin) suggest that rifting ended in the Miocene. Near Site 976 (western Alboran Sea basin), no compressional features affect Miocene and younger sediments. In the eastern Alboran Sea basin north of Al-Mansour Seamount (ODP Site 977), normal faults are observed in Miocene and Early Pliocene sediments. Later folds affect Pleistocene-Recent sediments in the eastern Alboran Sea basin (Site 977). After the folding event, there is evidence for normal faulting in Pleistocene-Recent sediments close to Site 977. South of Al-Mansour Seamount (ODP Site 978), compressional features in the eastern Alboran Sea basin from Miocene to Recent are evidenced by reverse faulting followed by folding. In the northern Alboran Sea basin (Andalucia A-1 well), there is evidence for strike-slip faulting in the Late Miocene that can be related to the Serrata fault system. We envision the development of the Alboran Sea basin through a southeasterly migration of the delaminating continental lithosphere to explain younger extension in the eastern Alboran Sea basin. The rate of the migration of the delamination front is of the range of millimeters-centimeters/year. We see evidence for the migration of the delamination front from Miocene to Recent as tectonic inversion occurs near Site 977. In contradiction to an extensional collapse hypothesis for the formation of the Alboran Sea, rifting did not end in the Late Miocene in the entire Alboran Sea basin. We exclude retreating subduction in a westward direction or a westward continental delamination as a model for Alboran Sea basin development because it would predict younger extension in the western part of the basin.
description: Supplement to: Tandon, Kush; Lorenzo, Juan M; de La Linde Rubio, Joaquin (1998): Timing of rifting in the Alboran Sea basin-correlation of borehole (ODP Leg 161 and Andalucia A-1) to seismic reflection data: implications for basin formation. Marine Geology, 144(4), 275-294
DOI: 10.1594/pangaea.816214
title: (Table 2) Estimated basement temperatures at DSDP Hole 69-504B

description: The achievement of deep penetration (562 m) of seafloor basalts at Hole 504B, near the Costa Rica Rift (1°13.63'N, 83°43.81'W), on DSDP Legs 69 and 70 presented a rare opportunity to examine the structure of young (6 m.y.) oceanic crust. In addition to the recovery of samples for laboratory studies, an extensive suite of downhole logs and experiments was carried out at this site, for two main purposes: (1) to allow reliable deductions about the nature of the entire section of penetrated crust, because recovery of samples was far from complete (-25%); (2) to probe the physical state of rock around the drilled hole on a scale of tens of meters to kilometers. Information on the latter large-scale phenomena at Hole 504B were provided mainly by the oblique seismic experiment, utilizing a bore-hole seismometer (Stephen 1983), and by the large-scale-electrical- resistivity experiment described below.
description: Supplement to: von Herzen, Richard P; Francis, T J G; Becker, Keir (1983): In situ large-scale electrical resistivity of ocean crust, Hole 504B. In: Cann, JR; Langseth, MG; Honnorez, J; Von Herzen, RP; White, SM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 69, 237-244
DOI: 10.1594/pangaea.694435
title: Temperature and salinity in the water column of the Aegean Sea at Station FEBR-1999-IR40

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.744227
title: Physical oceanography during Explorer cruise Explorer76/2 to the North Sea
DOI: 10.1594/pangaea.547855
title: Nutrients measured on water bottle samples at station Bm_1997-09-03_6, Bajo Molle, Chile
DOI: 10.1594/pangaea.905565
title: Closed chamber measurements of net ecosystem exchange of CO2 from Siikaneva bog, Finland: 2015

description: The datasets contains the chamber CO2 measurement and leaf area data of year 2015 used for model validation.
description: Microform column has the following codes: 1=high hummock, 2=hummock, 3=high lawn, 4=lawn, 5=hollow, 6=bare peat
DOI: 10.1594/pangaea.905529
title: Apatite fission track lenghts of in-situ bedrock from site 1111, western Marie Byrd Land, West Antarctica
DOI: 10.1594/pangaea.724462
title: Zooplankton time series at station Point B in 1970
DOI: 10.1594/pangaea.668135
title: Physical oceanography of CTD station 075 off Independencia Bay, 2007, Peru
DOI: 10.1594/pangaea.889392
title: Detailed tritium data of pits drilled at Vostok station, 2006
DOI: 10.1594/pangaea.477551
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_OC_22S/127

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.477595
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_OC_22S/85

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.724459
title: Zooplankton time series at station Point B in 1967
DOI: 10.1594/pangaea.684629
title: Nutrient concentrations in water samples collected at Station MARCH-1997-GN36199704603MNB01 in the Aegean Sea

description: For oxygen determination samples were analysed on board immediately after collection with the Winkler method according to Carpenter (1965a, 1965b). Titration was done with a Metrohm Dosimat 665 automatic burette. Precision of the method is estimated at 0.05 ml O2/l.Apparent oxygen utilisation (AOU) was calculated according to difference of measured oxygen values and oxygen saturation given by the equations of Benson and Krause (1984), which are recommended by Millero (1986).Percentage of oxygen saturation in water was calculated from the following equation (at temperature 0-40ºC and salinity 0-40 promille): %O2 = (O2/O2') X100, where O2 is oxygen concentration in a sample, O2' is oxygen solubility in sea water at the same temperature and salinity as in the sample.Samples for determination of nutrients were collected in 100 ml polyethylene bottles and kept continuously under deep freeze (-20°C ) until analysis in the laboratory. Nitrate and nitrite were analysed by a Bran and Luebbe Autoanalyser II according to the procedure of Treguer and Le Corre (1975). Phosphate was measured by a Perkin Elmer Lambda 2S UV/VIS Spectrometer according to the method described by Murphy and Riley (1962). Precision is estimated at ±0.1 µmol/l for nitrate and ±0.02 µmol/l for phosphate and nitrite. Detection limit was 0.08 µmol/l for nitrate and nitrite and 0.01 µmol/l for phosphate.
DOI: 10.1594/pangaea.739028
title: Pollen profile BEVERA, Lago di Bévera, Italy

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.654403
title: Hydrochemistry measured on water bottle samples during Gunnar Thorson cruise GT90/5
DOI: 10.1594/pangaea.824576
title: Carbonate analysis from IODP Hole 318-U1361A

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.826307
title: P-Wave velocity (PWC) from IODP Hole 330-U1373A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.905536
title: Apatite fission track lenghts of in-situ bedrock from site 1129, western Marie Byrd Land, West Antarctica
DOI: 10.1594/pangaea.690797
title: Mesozooplankton biomass during Professor Vodyanitskiy cruise PV20, Part I

description: Mesozooplankton was sampled by JUDAY net with a 37 cm ring diameter and mesh sizes of 125 µm. Integrated hauls (0-200 m) were usually taken. 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.690800
title: Mesozooplankton biomass during Professor Vodyanitskiy cruise PV21, Part I

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 125 µm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through depths in 0-100 m layer. 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.684630
title: Nutrient concentrations in water samples collected at Station MARCH-1997-GN36199704603MNB02 in the Aegean Sea

description: For oxygen determination samples were analysed on board immediately after collection with the Winkler method according to Carpenter (1965a, 1965b). Titration was done with a Metrohm Dosimat 665 automatic burette. Precision of the method is estimated at 0.05 ml O2/l.Apparent oxygen utilisation (AOU) was calculated according to difference of measured oxygen values and oxygen saturation given by the equations of Benson and Krause (1984), which are recommended by Millero (1986).Percentage of oxygen saturation in water was calculated from the following equation (at temperature 0-40ºC and salinity 0-40 promille): %O2 = (O2/O2') X100, where O2 is oxygen concentration in a sample, O2' is oxygen solubility in sea water at the same temperature and salinity as in the sample.Samples for determination of nutrients were collected in 100 ml polyethylene bottles and kept continuously under deep freeze (-20°C ) until analysis in the laboratory. Nitrate and nitrite were analysed by a Bran and Luebbe Autoanalyser II according to the procedure of Treguer and Le Corre (1975). Phosphate was measured by a Perkin Elmer Lambda 2S UV/VIS Spectrometer according to the method described by Murphy and Riley (1962). Precision is estimated at ±0.1 µmol/l for nitrate and ±0.02 µmol/l for phosphate and nitrite. Detection limit was 0.08 µmol/l for nitrate and nitrite and 0.01 µmol/l for phosphate.
DOI: 10.1594/pangaea.694132
title: Nutrient concentrations in water samples from the Aegean Sea at Station JUNE-1998-IR11
DOI: 10.1594/pangaea.663893
title: Oceanography at CTD/bottle station IFREMER_0734
DOI: 10.1594/pangaea.678086
title: Expanded measurements from station Ny-Ålesund (1993-10)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.744626
title: (Table 2) Trace metal concentrations in ODP Hole 169-1033B

description: We measured the concentrations of redox-sensitive trace metals (Mn, V, Mo, U, Cd and Re) in sediments from ODP Leg 169S Hole 1033B in Saanich Inlet, British Columbia, to determine changes in redox conditions associated with the onset of laminated sediments at ~12.5 kyr. The most striking result is a large peak in authigenic Re along with detrital levels of Mo at the glacial terrigenous clay-diatomaceous sediment transition. In contrast, the underlying glacial terrigenous clay, which extends throughout the bottom section of the core, is chemically similar to detrital concentrations, either Cowichan River particulates or average shale values. These data suggest a period of oxic bottom waters but reducing pore-waters. This could be due to the dramatic transformation of Saanich Inlet during the late deglaciation from an open bay to an inlet, which restricted circulation and slowed bottom water oxygen renewal. A peak and gradual increase in authigenic Mn in younger sediments subsequent to the Re peak suggests that increasingly oxic conditions followed the authigenic enrichment in Re. These conditions could be connected to the Younger Dryas cooling period, which was coincident with an increase in well oxygenated upwelled waters on the west coast of North America that form the bottom waters of Saanich Inlet.Metal concentrations in a gray clay bed (~11 kyr) are similar to their concentrations in the glacial terrigenous clay, implying that they have a common source. Authigenic enrichments of Re with little authigenic Mo and Cd suggest that before the deposition of this bed, bottom waters were oxic and pore-water oxygen was consumed in the top centimeter or less. Laminations above the clay layer suggest anoxic conditions, which are also indicated by higher authigenic Mo and Cd and slightly lower Re/Mo ratios in these sediments. The basin remained mostly anoxic after the gray clay was emplaced, as seen by continuous authigenic enrichment of the redox-sensitive trace metals. These results are consistent with increased stratification of the water column, brought about by an influx of fresh water to the basin by a large flood.
description: Sediment depth given in meters below sea-floor (mbsf).
description: Supplement to: Morford, J L; Russell, Ann D; Emerson, Steven R (2001): Trace metal evidence for changes in the redox environment associated with transition from terrigenous clay to diatomaceous sediment, Saanich Inlet, BC. Marine Geology, 174(1-4), 355-369
DOI: 10.1594/pangaea.477744
title: Hydrochemistry measured on water bottle samples at station SPac_1967_ET_43S/40

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.665237
title: Oceanography at CTD/bottle station IFREMER_2077
DOI: 10.1594/pangaea.825053
title: Vane shear strength measurements from IODP Hole 334-U1381A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.683526
title: Late Pliocene sea-surface temperature record of DSDP Hole 80-548 from the Northeast Atlantic Ocean (Table 1)

description: Application of quantitative micropaleontologic methods of sea-surface temperature (SST) estimation to the planktic foraminiferal faunas at Hole 548 in the northeast Atlantic between 3.5 and 2.0 Ma provide a detailed record of Pliocene surface temperature changes during the onset of major Northern Hemisphere glaciation. SST estimates indicate a relatively warm interval of "enhanced interglacials (warm peaks)" between 3.2 and 2.8 Ma followed by steady cooling with a significant step-like change toward colder temperatures occurring about 2.4 Ma. This record compares well with faunal and SST records from other North Atlantic sites.
description: Factor analysis (varimax) of planktic foraminiferal counts generated by Loubere and Moss (1986)
description: Supplement to: Dowsett, Harry J; Loubere, Paul (1992): High resolution late Pliocene sea-surface temperature record from the Northeast Atlantic Ocean. Marine Micropaleontology, 20(2), 91-105
DOI: 10.1594/pangaea.716588
title: (Appendix A) Gas hydrate anundance in samples of different lithologies of IODP Site 311-U1326
DOI: 10.1594/pangaea.806707
title: (Table 2) Rock-magnetic of ODP Holes 137-504B and 140-504B samples
DOI: 10.1594/pangaea.694460
title: Temperature and salinity in the water column of the Aegean Sea at Station FEBR-1999-MNB2

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.722029
title: Ultra-violet measurements from station Goodwin Creek (2006-10)

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 2017-02-03.
DOI: 10.1594/pangaea.824817
title: P-Wave velocity (PWC) from IODP Hole 324-U1350A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.825052
title: Thermal conductivity of IODP Hole 334-U1381A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.684631
title: Nutrient concentrations in water samples collected at Station MARCH-1997-GN36199704603MNB03 in the Aegean Sea

description: For oxygen determination samples were analysed on board immediately after collection with the Winkler method according to Carpenter (1965a, 1965b). Titration was done with a Metrohm Dosimat 665 automatic burette. Precision of the method is estimated at 0.05 ml O2/l.Apparent oxygen utilisation (AOU) was calculated according to difference of measured oxygen values and oxygen saturation given by the equations of Benson and Krause (1984), which are recommended by Millero (1986).Percentage of oxygen saturation in water was calculated from the following equation (at temperature 0-40ºC and salinity 0-40 promille): %O2 = (O2/O2') X100, where O2 is oxygen concentration in a sample, O2' is oxygen solubility in sea water at the same temperature and salinity as in the sample.Samples for determination of nutrients were collected in 100 ml polyethylene bottles and kept continuously under deep freeze (-20°C ) until analysis in the laboratory. Nitrate and nitrite were analysed by a Bran and Luebbe Autoanalyser II according to the procedure of Treguer and Le Corre (1975). Phosphate was measured by a Perkin Elmer Lambda 2S UV/VIS Spectrometer according to the method described by Murphy and Riley (1962). Precision is estimated at ±0.1 µmol/l for nitrate and ±0.02 µmol/l for phosphate and nitrite. Detection limit was 0.08 µmol/l for nitrate and nitrite and 0.01 µmol/l for phosphate.
DOI: 10.1594/pangaea.889381
title: Total water vapor retrieval data in the Arctic in June 2008 using microwave humidity sounders (TWV12345 retrieval)
DOI: 10.1594/pangaea.690814
title: Mesozooplankton abundance and biomass in waters of the Aegean Sea in September 1997. Station SEPT-1997-GN36199704606MNB02wp2

description: A Stempel pipette has been used for subsamples in taxonomic analysis of zooplankton. Taxonomic identification has been done at the Institute of Oceanography by I. Siokou-Frangou and E. Christou with use of relevant taxonomic literature. Mesozooplankton biomass was estimated as dry-weight (mg/m**3) according to M. Omori and T. Ikeda (Methods in Marine Zooplankton Ecology. New York, John Wiley & Sons. 1984. 311 p.) (1984). A Folsom splitter has been used for biomass and abundance estimations in 4% formaldehyde buffered sub-samples.
DOI: 10.1594/pangaea.690816
title: Mesozooplankton abundance and biomass in waters of the Aegean Sea in September 1997. Station SEPT-1997-GN36199704606MNB04wp2

description: A Stempel pipette has been used for subsamples in taxonomic analysis of zooplankton. Taxonomic identification has been done at the Institute of Oceanography by I. Siokou-Frangou and E. Christou with use of relevant taxonomic literature. Mesozooplankton biomass was estimated as dry-weight (mg/m**3) according to M. Omori and T. Ikeda (Methods in Marine Zooplankton Ecology. New York, John Wiley & Sons. 1984. 311 p.) (1984). A Folsom splitter has been used for biomass and abundance estimations in 4% formaldehyde buffered sub-samples.
DOI: 10.1594/pangaea.663520
title: Oceanography at CTD/bottle station IFREMER_0360
DOI: 10.1594/pangaea.842319
title: Radiosonde measurements from station Darwin (2004-12)

description: Version 3, 2015-02-04; Launches at irregular time intervals
DOI: 10.1594/pangaea.690850
title: Mesozooplankton abundance and biomass in waters of the Aegean Sea in September 1997. Station SEPT-1997-GN36199704605MSB02wp2

description: A Stempel pipette has been used for subsamples in taxonomic analysis of zooplankton. Taxonomic identification has been done at the Institute of Oceanography by I. Siokou-Frangou and E. Christou with use of relevant taxonomic literature. Mesozooplankton biomass was estimated as dry-weight (mg/m**3) according to M. Omori and T. Ikeda (Methods in Marine Zooplankton Ecology. New York, John Wiley & Sons. 1984. 311 p.) (1984). A Folsom splitter has been used for biomass and abundance estimations in 4% formaldehyde buffered sub-samples.
DOI: 10.1594/pangaea.905523
title: Ozone measurements from station Izaña (2019-08)
DOI: 10.1594/pangaea.739078
title: Pollen profile BURG-0, Burgmoos, 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.