cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.771369
title: (Table 1) Radiolarian biostratigraphy of ODP Leg 127 sites
DOI: 10.1594/pangaea.808235
title: (Table 2) Mean biomass of protists in water samples from Godthåbsfjord and Kapisigdlit fjord, West Greenland
DOI: 10.1594/pangaea.545216
title: Physical oceanography at CTD station Chip_2003-12-19_11, Chipana, Chile
DOI: 10.1594/pangaea.497166
title: Physical oceanography from BT during cruise M90P100001B_1954
DOI: 10.1594/pangaea.680911
title: Meteorological synoptical observations during Meteor cruise M65

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.548901
title: Nutrients and bacteria measured on water bottle samples at station Chan_2003-01-09_9, Chanavallita, Chile
DOI: 10.1594/pangaea.667150
title: (Table S1) Mapping pairs to adjust particular core sections to the spliced sections / Site 1265 - to adjust Core D4 to splice
DOI: 10.1594/pangaea.497347
title: Physical oceanography from BT during cruise N90XXB_1990
DOI: 10.1594/pangaea.721002
title: Thorium 234 in sediment core 13201-005, subcore 10
DOI: 10.1594/pangaea.758471
title: (Table 10) Distribution of radiolaria in Miocene to Pleistocene sediments of DSDP Hole 7-66A

description: Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent.
DOI: 10.1594/pangaea.722578
title: (Table DR3) Radiogenic isotope data for sediments from ODP Hole 177-1089
DOI: 10.1594/pangaea.750285
title: Meteorological observations during La Venus cruise from La Habana to Canal de Bahama started at 1789-01-18
DOI: 10.1594/pangaea.752343
title: Meteorological observations during STAR cruise from St. Catharine to Table Bay started at 1801-02-02
DOI: 10.1594/pangaea.497713
title: Physical oceanography from BT during cruise U58JH01956B_1981
DOI: 10.1594/pangaea.696123
title: Yearly production of dehydrated marine products in 1992, Chile
DOI: 10.1594/pangaea.776741
title: Core summary for IODP Hole 331-C0014G
DOI: 10.1594/pangaea.496927
title: Physical oceanography from BT during cruise M903800005B_1982
DOI: 10.1594/pangaea.834230
title: Ichthyolith counts and MAR at Gubbio outcrop

description: DEPTH, sediment/rock [m] is given in mbsf. All Ichthyolith counts were collected as part of this study. The primary age model was developed using biostratigraphic and magnetostratigraphic markers (see Gubbio Age model for details) and age datums from GTS 2012. A second age model (a helium age model) was used to test the sensitivity of our conclusions to age models affects. Helium sedimentation rates were directly taken from Figure 2 of Mukhopadhyay et al. (2001). The Gubbio K/Pg boundary is at 347.63 m (GTS 2012 boundary age = 66.04 Ma). MAR were calculated using a constant dry bulk density of 2.7g/cm^3 in both cases.
DOI: 10.1594/pangaea.696124
title: Yearly production of dehydrated marine products in 1993, Chile
DOI: 10.1594/pangaea.696140
title: Yearly production of surimi in 1995, Chile
DOI: 10.1594/pangaea.495500
title: Water temperature XBT profiles from cruise U32X107950_1988
DOI: 10.1594/pangaea.510690
title: Biological samples from Sedlo Seamount at station SEDLOP-03-V04
DOI: 10.1594/pangaea.713789
title: (Table 4) Rare earth element analyses of basement rocks from ODP Hole 126-793B
DOI: 10.1594/pangaea.911952
title: Oxygen and carbon isotopes of benthic foraminifera Melonis barleeanus of ODP Site 202-1242

description: This data includes the oxygen and carbon isotopic measurements carried out in Melonis barleeanus from the 250-350 µm of ODP Site 202-1242. The isotope composition of the foraminifera was measured using a GasBench II coupled to a Delta V mass spectrometer. Values are reported in the conventional delta notation with respect to VPDB.
DOI: 10.1594/pangaea.510691
title: Biological samples from Sedlo Seamount at station SEDLOP-04-O03
DOI: 10.1594/pangaea.747391
title: Meteorological observations during ANDROMEDA cruise from Portsmouth to New York started at 1778-02-25
DOI: 10.1594/pangaea.510698
title: Biological samples from Sedlo Seamount at station SEDLOT-02-V04
DOI: 10.1594/pangaea.690971
title: Documentation of sediment core GIK10092-2
DOI: 10.1594/pangaea.690974
title: Documentation of sediment core GIK12523-1
DOI: 10.1594/pangaea.747958
title: Meteorological observations during COVENTRY cruise from St. Augustins Bay to Madras started at 1775-07-30
DOI: 10.1594/pangaea.477383
title: Hydrochemistry measured on water bottle samples at station SAtl_1983-84_6N_0E/27-1

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.510700
title: Biological samples from Sedlo Seamount at station SEDLOT-04-V04
DOI: 10.1594/pangaea.510704
title: Biological samples from Seine Seamount at station SEINE-03-V03
DOI: 10.1594/pangaea.477955
title: Hydrochemistry measured on water bottle samples at station SAtl_1983-84_6N_44S_33S/60-1

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.911963
title: Stable isotopes of Siphonodosaria lepidula of ODP Site 202-1242

description: This data contains oxygen and carbon isotope measurments on the benthic foraminiferal species Siphonodosaria lepidula of ODP Site 202-1242. Isotopic measurements were carried out on 2 and 3 individuals of Siphonodosaria lepidula from the &gt;400 µm fraction. Samples were measured using a GasBench II coupled to a Delta V mass spectrometer as described in Breitenbach and Bernasconi (2011). Foraminifera were placed in vials and reacted with 104% phosphoric acid at 70ºC. The instrument was calibrated with the internal standards MS2 (δ13C = +2.13 ‰, δ18O = -1.81 ‰) and ETH-4 (δ13C = -10.19 ‰, δ18O = -18.71 ‰) which are calibrated to the international reference materials NBS 19 (δ13C = +1.95‰, δ18O = -2.2‰) and NBS 18 (δ13C = -5.01‰, δ18O = -23.00‰; Bernasconi et al., 2018). Values are reported in the conventional delta notation with respect to VPDB. Long term reproducibility is better than 0.1‰ for both carbon and oxygen isotopes. Measures were carried out in the Geological Institute, ETH Zürich, Switzerland.
DOI: 10.1594/pangaea.494538
title: Physical oceanography during cruise B26AS11108C_1990
DOI: 10.1594/pangaea.888373
title: Carbon isotope of sediment core GS15-198-36-CC in the Denmark Strait
DOI: 10.1594/pangaea.832432
title: Monthly averages of discharge as recorded at the Vernagtbach station for the period 1974 to 2012
DOI: 10.1594/pangaea.883996
title: Snow density of core EG16_LTW4 in snow trench LTW at the EGRIP field site, Greenland
DOI: 10.1594/pangaea.494621
title: Physical oceanography during cruise CUSNS_1994
DOI: 10.1594/pangaea.805006
title: (Table 1) Compressional- and share-wave velocieties at elevated confining pressure of ODP Holes 136-842C and 136-843A

description: Identification of a sediment/basement contact using seismic reflection recordings has proven to be extremely difficult in wide areas of the North Pacific Ocean owing to the presence of massive, highly reflective chert layers within the sediment column. Leg 136 of the Ocean Drilling Program recovered coherent pieces of chert of sufficient size for the first comprehensive laboratory measurements of the seismic properties of this material. Compressional-wave velocities of six samples at 40-MPa confining pressure averaged 5.33 km/s, whereas shear-wave velocities at the same pressure averaged 3.48 km/s. Velocities were independent of porosity, which ranged from 5% to 13%, suggesting that pores within the samples were mostly high aspect ratio vugs as opposed to low aspect ratio cracks. Back-scattered electron images made with a scanning electron microscope confirmed this observation.Acoustic impedances were calculated for the chert samples and from shipboard measurements of the red clay sediment overlying the chert layers. An extremely large compressional-wave reflection coefficient (0.73) characterized the interface between the two lithologies. A synthetic seismogram was calculated using chert and typical pelagic carbonate properties to illustrate the influence of chert layers on a marine seismic-reflection section. Compressional-wave to shear-wave velocity ratios of the chert samples (Vp/Vs =1.53) are close to that of single-crystal quartz in spite of variable porosity. Shear-wave reflection coefficients are estimated to be approximately 0.94. A compressional-wave reflection coefficient for a basement/sediment (carbonate) interface is estimated to be approximately 0.50, significantly less than that of sediment/chert.
description: Supplement to: Wilkens, Roy H; Christensen, Nikolas I; Collins, John A (1993): Seismic properties and reflectivity of North Pacific Ocean cherts. In: Wilkens, RH; Firth, J; Bender, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 136, 99-104
DOI: 10.1594/pangaea.495756
title: Water temperature XBT profiles from cruise U74XX57896_1970
DOI: 10.1594/pangaea.883979
title: Snow density of core CLP_32 in snow trench CLP near Kohnen station, East Antarctica
DOI: 10.1594/pangaea.751216
title: Meteorological observations during PHOENIX cruise from Jamaica to Spithead started at 1770-09-19
DOI: 10.1594/pangaea.822883
title: Meteorological measurements in the upper air at station Allahabad, 1930-07-17 to 1930-09-11, ERA-CLIM ID 5787

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.870178
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_VI_31
DOI: 10.1594/pangaea.751349
title: Meteorological observations during Princess Augusta cruise from Cape to Java started at 1754-03-09
DOI: 10.1594/pangaea.536292
title: Accumalion rate of carbonte free sediment for sediment core GIK12309-2 northern subtropical Atlantic (App. 4)
DOI: 10.1594/pangaea.832431
title: Monthly averages of discharge as recorded at the Vernagtbach station for the period 1974 to 2001
DOI: 10.1594/pangaea.910647
title: Radiocarbon dating of a sediment core from high-elevation lake Bastani
DOI: 10.1594/pangaea.510699
title: Biological samples from Sedlo Seamount at station SEDLOT-03-V04
DOI: 10.1594/pangaea.536293
title: Accumalion rate of carbonte free sediment for sediment core GIK12310-4 northern subtropical Atlantic (App. 4)
DOI: 10.1594/pangaea.747290
title: Meteorological observations during Albrecht Beijling cruise from Brouwershaven to Batavia started at 1849-08-07
DOI: 10.1594/pangaea.510702
title: Biological samples from Seine Seamount at station SEINE-01-V03
DOI: 10.1594/pangaea.748699
title: Meteorological observations during Drie Vrienden cruise started at 1843-03-06
DOI: 10.1594/pangaea.919645
title: Sea ice rafted quartz grains of IODP Site 341-U1421
DOI: 10.1594/pangaea.665147
title: Oceanography at CTD/bottle station IFREMER_1987
DOI: 10.1594/pangaea.744140
title: Physical oceanography during Argos cruise Argos97/2 to the North Sea
DOI: 10.1594/pangaea.665601
title: Oceanography at CTD/bottle station IFREMER_2441
DOI: 10.1594/pangaea.749824
title: Meteorological observations during INTREPID cruise from Cape of Florida to The Downs started at 1796-08-29
DOI: 10.1594/pangaea.664636
title: Oceanography at CTD/bottle station IFREMER_1476
DOI: 10.1594/pangaea.496025
title: Water temperature MBT profiles from cruise U90X000000M_1960
DOI: 10.1594/pangaea.536295
title: Accumalion rate of carbonte free sediment for sediment core GIK12329-6 northern subtropical Atlantic (App. 4)
DOI: 10.1594/pangaea.883982
title: Snow density of core EG16_LTO1 in snow trench LTO at the EGRIP field site, Greenland
DOI: 10.1594/pangaea.913401
title: Natural remanent magnetization of IODP Site 361-U1475
DOI: 10.1594/pangaea.536300
title: Accumalion rate of carbonte free sediment for sediment core GIK13207-3 northern subtropical Atlantic (App. 4)
DOI: 10.1594/pangaea.711598
title: Meteorological synoptical observations from station Tamanrasset (2002-12)
DOI: 10.1594/pangaea.883988
title: Snow density of core EG16_LTO7 in snow trench LTO at the EGRIP field site, Greenland
DOI: 10.1594/pangaea.536301
title: Accumalion rate of carbonte free sediment for sediment core GIK13289-2 northern subtropical Atlantic (App. 4)
DOI: 10.1594/pangaea.815717
title: (Table 1) Chemical composition of rocks from the Odessa and Kazachii Yar quarries and the Zaval'e graphite quarry, Podolia Domain, Ukrainian shield
DOI: 10.1594/pangaea.819821
title: (Table 1) Compressional-wave velocities and anisotropies and wet-bulk densities of calcareous rocks and some cherts at DSDP Holes 62-463 and 62-465A

description: Anisotropy in compressional-wave velocities in sedimentary rocks recovered by DSDP has been recognized by several investigators (Boyce, 1976; Tucholke et al., 1976; Carlson and Christensen, 1977). The anisotropy is also observed at elevated pressures in laboratory experiments, and thus probably persists at depth in some calcareous rocks (Schreiber et al., 1972; Christensen et al., 1973; Carlson and Christensen, 1979). Carlson and Christensen (1979) suggested that the observed velocity anisotropy was produced not by the alignment of cracks but by the alignment of c axes of calcite perpendicular to bedding during compaction, diagenesis, and recrystallization.On DSDP Leg 62, calcareous rocks were recovered from the western Mid-Pacific Mountains (sub-bottom depths of 452-823 m, Site 463) and southern Hess Rise (276-412 m, Site 465). Most of the calcareous rocks are horizontally laminated and color-banded, and ages are early Cenomanian to late Barremian (Site 463 and 465 reports, this volume).The purpose of this study is to confirm the velocity anisotropy in the calcareous rocks and to identify any relationship of anistropy to bulk density, mean velocity, and burial depth.
description: Empty cells = no data.
description: Supplement to: Fujii, Naoyuki (1981): Anisotropy in compressional-wave velocities and wet-bulk densities of calcareous sedimentary rocks, Deep Sea Drilling Project Leg 62. In: Thiede, J; Vallier, TL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 62, 995-998
DOI: 10.1594/pangaea.667148
title: (Table S1) Mapping pairs to adjust particular core sections to the spliced sections / Site 1262 - to adjust Core 13A-6 to splice
DOI: 10.1594/pangaea.883991
title: Snow density of core EG16_LTO10 in snow trench LTO at the EGRIP field site, Greenland
DOI: 10.1594/pangaea.827899
title: Micro-granulometry of sedimentary dykes, Kathmandu basin, Nepal

description: Soft-sediment deformation structures have been analyzed at six sites of the Kathmandu valley. Microgranulometric study (this Supplement and Fig. 3B of Mugnier et al., Tectonophysics, 2011) reveals that silty levels (60 to 80% silt) favor the development of soft-sediment deformation structures, while sandy levels (60 to 80% sand) are passively deformed. Nonetheless well sorted sand levels (more than 80% sand) generate over-fluid pressure during compaction if located beneath a silty cap, leading to fluidization and dike development. 3-D geometry of seismites indicates a very strong horizontal shearing during their development. Using a physical approach based on soil liquefaction during horizontal acceleration, we show that the fluidization zone progressively grows down-section during the shaking, but does not exactly begin at the surface. The comparison of bed-thickness and strength/depth evolution indicates three cases: i) no soft-sediment deformation occurs for thin (few centimeters) silty beds; ii) the thickness of soft-sediment deformation above sandy beds is controlled by the lithological contrast; iii) the thickness of soft-sediment deformation depends on the shaking intensity for very thick silty beds. These 3 cases are evidenced in the Kathmandu basin. We use the 30 cm-thick soft-sediment deformation level formed during the 1833 earthquake as a reference: the 1833 earthquake rupture zone extended very close to Kathmandu, inducing there MMI IX-X damages. A 90 cm-thick sediment deformation has therefore to be induced by an event greater than MMI X. From a compilation of paleo and historic seismology studies, it is found that the great (M ~ 8.1) historical earthquakes are not characteristic of the greatest earthquakes of Himalaya; hence earthquakes greater than M ~ 8.6 occurred. Kathmandu is located above one of the asperities that laterally limits the extent of mega-earthquake ruptures and two successive catastrophic events already affected Kathmandu, in 1255 located to the west of this asperity and in ~ 1100 to the east.
description: Supplement to: Mugnier, Jean-Louis; Huyghe, Pascale; Gajurel, Anata; Upreti, B N; Jouanne, F (2011): Seismites in the Kathmandu basin and seismic hazard in central Himalaya. Tectonophysics, 509(1-2), 33-49
DOI: 10.1594/pangaea.758969
title: (Table 2) Actual and synthetic mass accumulation rate data and their absolute differences for ODP Site 115-707

description: Synthetic mass accumulation rates have been calculated for ODP Site 707 using depth-density and depth-porosity functions to estimate values for these parameters with increasing sediment thickness, at 1 Ma time intervals determined on the basis of published microfossil datums. These datums were the basis of the age model used by Peterson and Backman (1990, doi:10.2973/odp.proc.sr.115.163.1990) to calculate actual mass accumulation rate data using density and porosity measurements. A comparison is made between the synthetic and actual mass accumulation rate values for the time interval 37 Ma to the Recent for 1 Myr time intervals. There is a correlation coefficient of 0.993 between the two data sets, with an absolute difference generally less than 0.1 g/cm**2/kyr. We have used the method to extend the mass accumulation rate analysis back to the Late Paleocene (60 Ma) for Site 707. Providing age datums (e.g. fossil or magnetic anomaly data) are available the generation of synthetic mass accumulation rates can be calculated for any sediment sequence.
description: Supplement to: Sykes, T J S; Ramsay, A T S (1995): Calculation of mass accumulation rates in the absence of density or porosity measurements. Marine Geology, 122(3), 173-179
DOI: 10.1594/pangaea.919729
title: Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of IODP Hole 303-U1306B at the Matuyama-Brunhes boundary
DOI: 10.1594/pangaea.755166
title: (Table 1) Heat flow in the Red Sea rift zone at 18°N

description: New results of geothermal studies at 18°N in the Red Sea rift zone are discussed. It was established that the thermal field of the African plate in this area has a higher than ordinary level, and averages 3.0-3.5 UTF. Heat flow of the Arabian plate is characterized by negative anomalies and is local in character in comparison to adjoining areas of the rift.
description: Supplement to: Verzhbitsky, Evgeny V; Zolotarev, Vladimir G (1980): Studies of the heat flow in the rift zone of the Red Sea. Oceanology, 20(5), 580-583
DOI: 10.1594/pangaea.883992
title: Snow density of core EG16_LTW0 in snow trench LTW at the EGRIP field site, Greenland
DOI: 10.1594/pangaea.919730
title: Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of IODP Hole 303-U1306C at the Matuyama-Brunhes boundary
DOI: 10.1594/pangaea.752873
title: Meteorological observations during WELMEENENDE cruise from Suriname to the Netherlands started at 1774-06-26
DOI: 10.1594/pangaea.883993
title: Snow density of core EG16_LTW1 in snow trench LTW at the EGRIP field site, Greenland
DOI: 10.1594/pangaea.794508
title: (Table 7) Trace elements of glasses of ODP Leg 135 vitrophyric rhyolite samples
DOI: 10.1594/pangaea.484950
title: Sea surface temperature data during cruise Skonort_Nordland_18760422

description: Values of air and water temperature are corrected if corrections are given. If correction value is missing, it is taken 0.0. If correction is given for a range of temperature, particular value is computed by linear interpolation.
DOI: 10.1594/pangaea.881407
title: Basic and other measurements of radiation at station Barrow (2013-09)

description: Please note that relative humidity values might be off and are therefore to be handled with caution.
DOI: 10.1594/pangaea.883994
title: Snow density of core EG16_LTW2 in snow trench LTW at the EGRIP field site, Greenland
DOI: 10.1594/pangaea.883995
title: Snow density of core EG16_LTW3 in snow trench LTW at the EGRIP field site, Greenland
DOI: 10.1594/pangaea.744259
title: Physical oceanography during Håkon Mosby cruise HM06/1 to the North Sea
DOI: 10.1594/pangaea.911564
title: Sea surface temperature reconstructions (TEX86) from samples from DSDP Site 94-610

description: TEX86-based SSTs from DSDP Hole 94-609B
DOI: 10.1594/pangaea.497155
title: Physical oceanography from BT during cruise M90M3B_1989
DOI: 10.1594/pangaea.498853
title: Physical oceanography from BT during cruise U90X007961B_1899
DOI: 10.1594/pangaea.749274
title: Meteorological observations during FALKLAND cruise from Spithead to Fernando Noronha started at 1759-02-18
DOI: 10.1594/pangaea.499122
title: Physical oceanography from BT during cruise U90X008314B_1984
DOI: 10.1594/pangaea.744291
title: Physical oceanography during Johan Hjort cruise JH76/3 to the North Sea
DOI: 10.1594/pangaea.744295
title: Physical oceanography during Johan Hjort cruise JH81/1 to the North Sea
DOI: 10.1594/pangaea.750022
title: Meteorological observations during Koning Willem II cruise from Nederland to Batavia started at 1849-06-25
DOI: 10.1594/pangaea.664981
title: Oceanography at CTD/bottle station IFREMER_1821
DOI: 10.1594/pangaea.744100
title: Physical oceanography during Anton Dohrn cruise AD_02_1984 to the North Sea
DOI: 10.1594/pangaea.883141
title: Meteorological synoptical observations from station Lindenberg (2015-07)
DOI: 10.1594/pangaea.751184
title: Meteorological observations during PHILADELPHIA cruise from Elmina to Suriname started at 1757-04-05
DOI: 10.1594/pangaea.763740
title: Tab. 3: Concentrations of selected chemical species at various depths in Ace Lake

description: This article reviews the history, chemical stratification, biology and biogeochemistry of Ace Lake, which is one of the many marine-derived meromictic (permanently stratified) lakes in the Vestfold Hills, Eastern Antarctica. The lake has an area of 18 ha, a maximum depth of 25 m, and a salinity range from 7 to 43 g l**-1. The lake mixes to a depth of 7 m in late winter as a result of brine freeze out during ice formation. Deeper mixing is precluded by a sharp halocline. The water beneath 12 m is permanently anoxic, The lake was formed approximately 10,800 yr BP as the polar ice cap melted. Sea level rise 7,800 yr BP resulted in invasion of seawater into the initially freshwater lake. Subsequently, sea level dropped, and the now saline lake became isolated from the ocean. The biota of the lake was derived from species trapped when the connection between the lake and the ocean was cut off. The oxic zone above 12 m supports a relatively simple community which includes microbial mats, four major species of phytoplankton (including a picocyanobacterium), two copepod species, and a variety of heterotrophic flagellates and ciliates. The anoxic zone contains populations of photosynthetic sulfur, sulfate reducing, fermentative and methanogenic bacteria, which combine to remineralise organic carbon which sediments from the upper waters. Research on the physics, biology and chemistry of Ace Lake has contributed significantly to knowledge of Antarctic meromictic lakes.
description: Note that the concentrations given for the trace elements in the lake are the sum of dissolved and particulate fractions.
description: Supplement to: Rankin, Lynne M; Gibson, John A E; Franzmann, Peter D; Burton, Harry R (1999): The chemical stratification and microbial communities of Ace Lake, Antarctica: a review of the characteristics of a marine-derived meromictic lake. Polarforschung, 66(1/2), 33-52