cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.758002
title: Meteorological synoptical observations from station Lindenberg (2005-02)
DOI: 10.1594/pangaea.495447
title: Water temperature XBT profiles from cruise U31XX49258_1974
DOI: 10.1594/pangaea.674418
title: Radiosonde measurements from Neumayer Station (1997-10)
DOI: 10.1594/pangaea.921789
title: Organoleptic qualities (taste, smell, texture and appearance) of the Northern shrimp under combined ocean change drivers (Temp, pH, O₂ saturation)

description: For more details please refer to the method's section "Organoleptic Quality Evaluation (Design B Only)" of Chamel et al. 2020, where scoring and hedonic scale are described.
DOI: 10.1594/pangaea.674498
title: Radiosonde measurements from Neumayer Station (2004-08)
DOI: 10.1594/pangaea.871858
title: Radiosonde measurements from station Izaña (2017-01)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.693010
title: Expanded measurements from Neumayer Station (2007-12)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.757496
title: (Table 2) Concentration of organic carbon in bottom sediments from the Bering Sea
DOI: 10.1594/pangaea.757744
title: Current meter data from mooring M36_A3
DOI: 10.1594/pangaea.884435
title: Basic and other measurements of radiation at station Barrow (1999-11)

description: Version 2, (2017-12-22), with corrected Short-wave downward (GLOBAL) radiation values.
DOI: 10.1594/pangaea.691261
title: Nutrient concentrations in water samples collected at Station SEPT-94-GN3619940280300970 in the Aegean Sea
DOI: 10.1594/pangaea.750176
title: Meteorological observations during La Graciense cruise from Coulon to Martinique started at 1788-09-24
DOI: 10.1594/pangaea.678084
title: Expanded measurements from station Ny-Ålesund (1993-08)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.831488
title: Detection history of Mustela lutreola in northern Spain, 2000-2011

description: two surveys/year (January - March and September - December); 1=species detected; 2=species non detected; 3=site not surveyed
DOI: 10.1594/pangaea.713595
title: Population density of radiolaria at station UT99-15-2
DOI: 10.1594/pangaea.706278
title: Basic and other measurements of radiation at station Barrow (2007-12), Version 1

description: Ellsworth G. Dutton discovered a calibration glitch in the SWD "Short-wave downward (GLOBAL) radiation" data for Barrow, Alaska. SWD data was therefore removed from this dataset. Please refer to the updated Version 2 (see replaced by reference) with correct calibration.
DOI: 10.1594/pangaea.756886
title: Meteorological synoptical observations from station Lindenberg (2004-06)
DOI: 10.1594/pangaea.757778
title: (Table 1) Dissolved and particulate organic carbon, phosphorus, and nitrogen in waters of the Sea of Japan

description: Concentrations of dissolved and particulate organic carbon (DOC and POC, respectively), phosphorus (DP and PP, respectively) and particulate organic nitrogen (PON) were determined at Station VITYAZ6656 in the Sea of Japan in 12 sea water samples collected in June 1972 with a 200-liter sampling bottle. Mean weighted concentrations from the surface to 2000 m were: DOC - 1.58 mg/l, POC - 17.9 µg/l, DP - 13.9 µg/l, PP - 0.185 µg/l, PON - 2.7 µg/l, the ratios were DOC:DP=100:9 and POC:PON:PP=100:14:1. Relation between POC (µg/l)and the light attenuation index "e" (1/m) for the visible part of the spectrum is described by the equation POC = ca. 170e. The maximum of POC in the upper layer correlated with the maxima of phyto- and bacterioplankton and protozoa.
description: 0 = below detection limit
description: Supplement to: Lyutsarev, Sergey V; Romankevich, Evgeny A (1976): Organic carbon, phosphorus and nitrogen in the waters of the Sea of Japan. Oceanology, 16, 178-181
DOI: 10.1594/pangaea.672604
title: Basic and other measurements of radiation at station South Pole (1992-07)
DOI: 10.1594/pangaea.873850
title: Climate model results of various COSMOS Miocene experiments in NetCDF format

description: In this data set we publish the simulated global annual mean sea surface temperature (SST), mixed layer depth (ZMLD), horizontal barotropic streamfunction (PSIUWE), zonal (UKO) and meridional (VKE) velocity in 37 m and 3070 m water depth, respectively, global meridional overturning circulation (GMOC), Atlantic meridional overturning circulation (AMOC) and monthly mean sea-ice concentration over a time period of 100 years retrieved from equilibrium climate simulations for the Miocene ca. 20-10 Myrs ago (MIO). The model data has been utilized in the publication by Huang et al. (2017). The climate data has been produced with COSMOS (ECHAM5/JSBACH/MPIOM/OASIS3), utilized at a resolution of T31 in the atmosphere (19 hybrid sigma-pressure levels) and a resolution of GR30 (bipolar orthogonal curvilinear grid, formal resolution of ~3.0°x1.8°) in the ocean (40 z-coordinate levels). The Miocene model setup is based on the publication of Stärz et al. (2017), including changes in orography, bathymetry, ice sheets, atmospheric CO2 and physical land surface characteristics. This setup has been modified by a regional Weddell Sea bathymetry reconstruction. Details on setup and identifiers of Miocene model simulations can be found in Table 1 of Huang et al. (2017).
description: Supplement to: Huang, Xiaoxia; Stärz, Michael; Gohl, Karsten; Knorr, Gregor; Lohmann, Gerrit (2017): Impact of Weddell Sea shelf progradation on Antarctic bottom water formation during the Miocene. Paleoceanography, 32(3), 304-317
DOI: 10.1594/pangaea.676836
title: Grain size composition of sediments from Hole AMIGE-1993-155 drilled in the Barens Sea

description: Types of rocks and their ages are given in the special data set; see: doi:10.1594/PANGAEA.676843
DOI: 10.1594/pangaea.757598
title: Total biomass of mesoplankton and biomass of Calanus tonsus in the 0-200 m layer at stations in the Southwest Pacific

description: Structure of mesoplankton and distribution of dissolved ammonia in the vicinity of an isolated seamount of the Louisville Ridge in the subantarctic zone of the Pacific Ocean was studied using data obtained in January 1985 in an area 20 x 30 nm. There were areas with both high (20-25 to 139 g/m**2 in the 0-200 m layer) and low biomass values (&lt;10 g/m**2) of mesoplankton. In the areas with high biomass, a single species Calanus tonsus was strongly dominant (&gt;80% of biomass); its population was relatively mature in seasonal terms, with relatively high percentage of individuals containing fat inclusions. Stations with high mesoplankton biomass also had relatively high concentrations of dissolved ammonia. Presence of plankton-rich areas corre¬lated with presence of a quasi-steady-state topographic eddy. Lifetimes of these nonuniformities in the structure of mesoplankton are estimated as 10-30 days.
description: Supplement to: Flint, Mikhail V; Yakushev, E V (1988): Spatial structure of mesoplankton and distribution of dissolved ammonia in the vicinity of Pulkovskaya Seamount. Oceanology, 28(5), 655-660
DOI: 10.1594/pangaea.757783
title: Tab.2+3: Potential of biotic and enzymatic activities and chemical features in different soils from Spitsbergen

description: Chemical analyses showed that on the western coast of Spitsbergen some soils have a very high content of organic matter (2.15-5.63 Ct %) in the top layer while other soils show significantly lower quantities (0.75-0.82 Ct %). With respect to the total nitrogen content (Nt %) a similar situation can be found. Investigations in upper soil horizons, carried out for 5 places in Spitsbergen, showed that one of the soils studied was very little developed with 51,000 colony forming units (cfu) /g dried soil while four soils were more developed with 233,600-695,000 cfu/g dry wt. Heterotrophie, aerobic, non-sporogenous and Gram-negative bacteria are typical for the rhizosphere. Micromycetes, however, were very scarce, soil respiration and cellulolytic potentials were similar to those found in acid and cold soils of Romania (temperate climate). The five soils were enzymatically tested for: catalase, saccharase, urease and total phosphatase potentials. It is important to underline that the biotic and enzymatic potentials of the four more developed soils from Spitsbergen are comparable with the poorer soils from Romania. In Spitsbergen the period with a climate favorable for biological processes is too short (2-3 months) and consequently the organic layer is only 9-12 cm thick.
description: Supplement to: Negoita, Teodor Gheorghe; Stefanic, Gheorghe; Irimescu-Orzan, Mirela Emilia; Palanciuc, Vasilica; Oprea, Georgeta (2002): Microbial, chemical and enzymatic properties in Spitsbergen Soils. Polarforschung, 71(1/2), 41-46
DOI: 10.1594/pangaea.757742
title: Chromatographic fractionation of bitumen from sediments and presence of glycerol ethers in immature sediments (Table 2)

description: Alkanes having unusual saturated isoprenoidal and methyl-branched structures have been isolated from the bitumen of several sediments. The methanogenic biomarkers 2,6,10,15,19-pentamethyleicosane and squalane were found in sediments which also contained bacteriogenic glycerol ethers. However, in one ether-containing sediment, 2,6,10,13,17,21-hexamethyldocosane was tentatively identified and this compound was found in place of the established alkane biomarkers. Other hydrocarbons found were regular C21 and C23 isoprenoid alkanes, compounds which cannot be derived from phytol; two isoprenoids of the type 3,7,11…-polymethylalkane, previously reported only in petroleums; 8-methylheptadecane, a probable biomarker for cyanobacteria and a number of its homologs and other methyl-branched alkanes. Ubiquitous branched-chain alkylbenzenes and a homology of trimethylalkylbenzenes were also isolated. Most, or all, of the compounds reported here are probably not catagenetic products but may represent direct algal or bacterial bioinputs.
description: Supplement to: Vella, Alfred J; Holzer, Gunther (1992): Distribution of isoprenoid hydrocarbons and alkylbenzenes in immature sediments: evidence for direct inheritance from bacterial/algal sources. Organic Geochemistry, 18(2), 203-210
DOI: 10.1594/pangaea.777936
title: Downhole temperature measurement from IODP Hole 317-U1351B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.777913
title: Pass-through measurements of magnetic susceptibility from IODP Hole 317-U1351A

description: Geocode = Depth CSF-A (m).Technical Note 26 Chapter 4: http://www-odp.tamu.edu/publications/tnotes/tn26/CHAP4.PDF
DOI: 10.1594/pangaea.907796
title: Iceberg-rafted debris flux and biogenic silica concentrations in sediment core IN2017_V01-A042-KC14

description: Downcore measurements of iceberg-rafted debris (IBRD) flux and biogenic silica concentrations in kasten core IN2017_V01-A042-KC14 from the continental slope of central Wilkes Land, East Antarctica. The IBRD flux was calculated by multiplying the coarse sand fraction by the linear sedimentation rate and the dry bulk density at each depth interval along the core. All of these values are shown. The biogenic silica concentration is shown as a percentage.
DOI: 10.1594/pangaea.823008
title: (Table 2) Geochemistry recalculated by excluding carbonates, residual materials, water, and salts at DSDP Legs 56-57 Holes
DOI: 10.1594/pangaea.757637
title: TOC, carbonate and bitumen concentrations of DSDP Holes 64-477 and 64-478 (Table 1)

description: The bitumens of a selection of subsurface sediments from Guaymas Basin, Gulf of California, have been analyzed in order to assess the hydrothermal effects on the organic matter and to better delineate the processes influencing the generation, deposition, and alteration of the hydrothermal petroleums at the seabed. Although the thermally generated subsurface bitumens are generally rich in polar/asphaltic materials, as are the seabed oils, the hydrocarbon transformations parallel the extent of hydrothermal alteration as reflected in the downcore mineralogy at DSDP Sites 477 and 478. At Site 477, a progressive change from n-alkane- to aromatic hydrocarbon-dominated patterns in the high resolution gas chromatography-resolvable fractions of the bitumens accompanies decreases in organic carbon and bitumen yields with depth. These transformations are indicative of sequential hydrothermal alteration of the sediments with depth, due to increasing temperature and/or progressive passage of hydrothermal fluid through the sedimentary column. The polycyclic aromatic hydrocarbon (PAH) distributions undergo extensive transformations (e.g. dealkylation) consistent with hydrothermal alterations, are dominant at depth, and have the broadest range as thermal maturation indices. The aliphatic and aromatic components of the seabed oils can be transported to the seabed independently as a result of their generation under different temperature or depth regimes and sequentially over time during pyrolysis. The concentrations of the parent PAH in the thermally altered subsurface bitumens are comparable to those in the seabed oils. The differential dissolution of the more soluble aromatics and selective solidification/condensation of the higher molecular weight PAH out of the high-temperature fluids exiting at the seabed (chimneys) result in aromatic distributions of the oils significantly skewed towards the larger components [e.g. benzo(ghi)perylene] relative to the subsurface bitumens. Comparison of the downcore hydrocarbon distributions with those in the seabed petroleums support the contention that the hydrothermal oils are mixtures of pyrolysates from different depths or thermal regimes and are significantly altered by differential solubilization during transport and at the seabed.
description: Supplement to: Kawka, Orest E; Simoneit, Bernd R T (1994): Hydrothermal pyrolysis of organic matter in Guaymas Basin: I. Comparison of hydrocarbon distributions in subsurface sediments and seabed petroleums. Organic Geochemistry, 22(6), 947-978
DOI: 10.1594/pangaea.923118
title: Endospore concentrations of IODP Hole 370-C0023A

description: m CSF = depth of Core below Sea Floor in meters / m CSF-A: Distance from sea floor to sample within recovered core. This scale allows overlap at core and section boundaries. /m CSF-B: Distance from sea floor to sample within recovered core is compressed, if core recovery &gt; 100%.
DOI: 10.1594/pangaea.761607
title: (Table 2) Phytoplankton biomass in the northeastern the Sea of Okhotsk from March 23 to April 14, 1998
DOI: 10.1594/pangaea.874360
title: Radiosonde measurements from station Minamitorishima (2017-02)
DOI: 10.1594/pangaea.923086
title: Microbial cell abundance of IODP Hole 370-C0023A

description: m CSF = depth of Core below Sea Floor in meters / m CSF-A: Distance from sea floor to sample within recovered core. This scale allows overlap at core and section boundaries. /m CSF-B: Distance from sea floor to sample within recovered core is compressed, if core recovery &gt; 100%.
DOI: 10.1594/pangaea.498619
title: Physical oceanography from BT during cruise U90V207654B_1985
DOI: 10.1594/pangaea.763237
title: (Table 2) Residual magnetization of samples from the Red Sea rift zone
DOI: 10.1594/pangaea.664963
title: Oceanography at CTD/bottle station IFREMER_1803
DOI: 10.1594/pangaea.736619
title: (Table 37) Chemical composition of olivines and pyroxenes from ultrabasic rocks of the Mariana Trench

description: Analyses have been carried out by Yu.G. Lavrentjev and N.L. Dobretsov at the participation of G.N. Savelyeva.
DOI: 10.1594/pangaea.763918
title: (Table 5) Eutrophication factors in the Mamala Bay calculated from maximal biomasses of different planktonic communities and concentations of chlorophyll a in water layers
DOI: 10.1594/pangaea.757446
title: Chemical composition of Fe-Mn nodules and crusts from oceans and seas

description: Fluorine concentrations were determined ionometrically with an error of 0.02% in iron-manganese materials of the ocean. They were: 0.02-0.04% in ocean iron-manganese nodules, with the exception of two specimens (0.08% and 0.20% F); up to 0.02% in iron-manganese nodules of seas; 0.02-1.17% in ore crusts from ocean seamounts; and 0.02% in ore sediments of the Red Sea. Elevated fluorine content of ore crusts is associated with presence of calcium phosphate inclusions in them. Fluorine is not accumulated during iron-manganese nodule mineralization. Its average concentration in the nodules is half that in host deep-sea sediments.
description: Supplement to: Baturin, Gleb N; Korytov, F Ya (1988): Fluorine in iron-manganese materials of the ocean. Oceanology, 28(6), 747-750
DOI: 10.1594/pangaea.777901
title: (Appendix 3A) Principal factor score matrix for benthic foraminifera in eastern equatorial Indian Ocean surface sediments
DOI: 10.1594/pangaea.753826
title: (Table 3b) Biomass of copepods at different depths in the tropical Pacific at Station VITYAZ3689
DOI: 10.1594/pangaea.777902
title: (Appendix 3B) Varimax factor score matrix for benthic foraminifera in eastern equatorial Indian Ocean surface sediments
DOI: 10.1594/pangaea.921630
title: Swimming speed of two phytoplankton species, Rhodomonas salina and Teleaulax sp., and the heterotrophic dinoflagellate Oxyrrhis marina

description: Swimming speed of two phytoplankton species, Rhodomonas salina and Teleaulax sp., grown in nutrient replete F/2 medium and in P-limited conditions, as well as swimming speed of the heterotrophic dinoflagellate Oxyrrhis marina either starved or fed with these four types of phytoplankton individually. In addition to the different culture and feeding conditions, the phytoplankton and dinoflagellates were incubated with the water from differently cultured organisms.
DOI: 10.1594/pangaea.778640
title: (Table T1) Calcareous nannofossil abundance in ODP Hole 194-1193A sediments

description: Sediment depth is given in mbsf. Abundance estimates (1000 x magnification) as follows: F = few, 1 specimen per 11?50 fields of view; R = rare, 1 specimen per 51?200 fields of view; B = barren.
DOI: 10.1594/pangaea.499259
title: Physical oceanography from BT during cruise U90XX00012B_1959
DOI: 10.1594/pangaea.706031
title: (Table 2) Duplicate oxygen-isotope measurements of the planktonic foraminifer Globigerinoides ruber from ODP Hole 133-820A
DOI: 10.1594/pangaea.774380
title: Thermal conductivity of IODP Hole 316-C0008B

description: Geocode = [m CSF-A] Top Core depth (below sea floor). Standard VLQ laboratory probe, source length is 70 mm and source diameter 2 mm. Measuring range 0.1 - 10 Wm-1K-1.
DOI: 10.1594/pangaea.758013
title: Radiosonde measurements from station Lindenberg (2005-04)
DOI: 10.1594/pangaea.510913
title: Radiosonde at Georg-Forster station on 1985-06-19 12:00h

description: Height of tropopause 9458 m
DOI: 10.1594/pangaea.845955
title: Radiosonde measurements from station Kwajalein (2012-05)
DOI: 10.1594/pangaea.847908
title: Radiosonde measurements from station Tamanrasset (2015-06)

description: Start location: Tamanrasset; Distance from radiation site: 10 km
DOI: 10.1594/pangaea.510873
title: Radiosonde at Georg-Forster station on 1990-08-31 00:00h

description: Height of tropopause 17438 m
DOI: 10.1594/pangaea.877793
title: Expanded measurements from station Lindenberg (2012-11)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.823436
title: (Table 4) Mineralogy at DSDP Leg 55 Holes

description: On Leg 55, cores were takenfrom three seamounts in the Emperor Seamount chain: Ojin, Nintoku, and Suiko Seamounts. At the drilling sites the water depth was 1300 to 1700 meters; the maximum thickness of the sediment column was 180 meters at Site 433.
description: &lt;1 = trace, ? = presence uncertain, empty cells = no data.
description: Supplement to: Mann, Ulrich; Müller, German (1980): Mineralogy of the sedimentary sections encountered on Leg 55 (Sites 430 through 433), based on x-ray diffractometry. In: Jackson, ED; Koisumi, I; et al., (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 55, 857-859
DOI: 10.1594/pangaea.611055
title: Abundance of zooplankton in c. 200 m water depth in the Indian Ocean
DOI: 10.1594/pangaea.757370
title: Element data of potassium (K), calcium (Ca), titanium (Ti) and iron (Fe) of IMAGES core MD02-2576

description: The long term history of terrigenous flux to the Gulf of Mexico via the Mississippi River is hardly known. We here present geochemical and sedimentological data to approximate the varying Mississippi River sediment influx into the northeastern Gulf of Mexico (GoM) over the last six glacial-interglacial cycles (MIS 1 to 14). Our study is based on the IMAGES sediment core MD02-2576 that was recovered from the DeSoto Canyon and is located ~ 200 km south to the recent Mississippi River delta and ~ 150 km east of the recent coastline of Florida. Concentrations of siliciclastic elements in bulk sediment samples were estimated from XRF scanning and calibrated by single bulk XRF-analyses. Elemental ratios of the sedimentary record correspond to ratios from the Mississippi River catchment rather than to the core close Alabama and Mobile River catchments. The siliciclastic major element potassium (K) with enhanced surface concentrations in the northwestern Mississippi River catchment shows varying occurrence downcore and here serves as a proxy for Mississippi River sediment discharge variability. Changes in sedimentation rate and magnetic susceptibility further support the variations in Mississippi River influx. Our data were compared with Mississippi River terrestrial archives in the form of loess and terrace deposits that back up our interpretations of enhanced glacial phase Mississippi River influx triggered by strengthened fluvial river runoff and changing fluvial and ice sheet dynamics. Mississippi River influx was at a maximum during glacial MIS 2/3, MIS 8 and MIS 10. Late glacial MIS 6 deviates from this pattern being a period of reduced Mississippi River influx at the core location, probably due to a westward shift of the Mississippi River delta.
description: Elements converted into absolute values by correlation to bulk-XRF measurements
description: Supplement to: Kujau, Ariane; Nürnberg, Dirk; Zielhofer, Christoph; Bahr, André; Röhl, Ursula (2010): Mississippi River discharge over the last ~560,000 years -- Indications from X-ray fluorescence core-scanning. Palaeogeography, Palaeoclimatology, Palaeoecology, 298, 311-318
DOI: 10.1594/pangaea.777900
title: Thermal conductivity of IODP Hole 317-U1351A

description: Geocode = Depth CSF-A (m).Technical Note 26 Chapter 8: http://www-odp.tamu.edu/publications/tnotes/tn26/CHAP8.PDF
DOI: 10.1594/pangaea.836058
title: (Table 7) Ratios of net ecosystem calcification to net community production in three bays in Hurricane Hole, U.S. Virgin Islands
DOI: 10.1594/pangaea.923083
title: Acetate concentration and δ13C acetate values of IODP Hole 370-C0023A

description: m CSF = depth of Core below Sea Floor in meters / m CSF-A: Distance from sea floor to sample within recovered core. This scale allows overlap at core and section boundaries. /m CSF-B: Distance from sea floor to sample within recovered core is compressed, if core recovery &gt; 100%.
DOI: 10.1594/pangaea.675368
title: Radiosonde measurements from station Payerne (1996-11)
DOI: 10.1594/pangaea.727535
title: (Table 4) Sr, Nd, and Pb isotopic composition of chilled glasses from the Mid-Atlantic Ridge segments
DOI: 10.1594/pangaea.923106
title: Methane isotopic composition of IODP Hole 370-C0023A

description: m CSF = depth of Core below Sea Floor in meters / m CSF-A: Distance from sea floor to sample within recovered core. This scale allows overlap at core and section boundaries. /m CSF-B: Distance from sea floor to sample within recovered core is compressed, if core recovery &gt; 100%.
DOI: 10.1594/pangaea.758010
title: Expanded measurements from station Lindenberg (2005-03)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.874535
title: Ozone measurements from Neumayer Station (2016-06)

description: Ozone values are integrated from measured ozone profiles