cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.498932
title: Physical oceanography from BT during cruise U90X008074B_1984
DOI: 10.1594/pangaea.666006
title: Oceanography at CTD/bottle station IFREMER_2832
DOI: 10.1594/pangaea.864232
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE467, Bremerhaven - Bremerhaven, 2016-07-08 - 2016-07-17
DOI: 10.1594/pangaea.909219
title: Cosmic-ray neutron (CRN) height profiles for Voulund Farmland, Harrild Heathland and Gludsted Plantation, Denmark, in 2013-2015

description: Cosmic-ray neutron (CRN) height profiles (of thermal and epithermal neutron energies) were estimated from bare and moderated detector measurements at three field site locations in the western part of Denmark. The measurements were collected in the period 2013-2015 and the field sites represent the three main land cover types in the catchment (i.e. agriculture "Voulund Farmland", forest "Gludsted Plantation" and heathland "Harrild Heathland"). The procedure to estimate thermal and epithermal neutrons from measurements of bare and moderated detectors is described in Andreasen et al (submitted). One neutron height profile was measured directly using a cadmium shielded moderated neutron detector.
DOI: 10.1594/pangaea.817776
title: (Table 3) Clinopyroxenes in basalts at DSDP Hole 66-487

description: Cations on 6 Oxygen.
DOI: 10.1594/pangaea.498265
title: Physical oceanography from BT during cruise U74X009303B_1981
DOI: 10.1594/pangaea.878917
title: Major elements geochemistry of manganese nodules from the DOMES C site in the Pacific Ocean using X-ray emission spectroscopy

description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
DOI: 10.1594/pangaea.864234
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE469, Bremerhaven - Bremerhaven, 2016-08-02 - 2016-08-13
DOI: 10.1594/pangaea.499198
title: Physical oceanography from BT during cruise U90X008696B_1967
DOI: 10.1594/pangaea.819872
title: (Table 1) Sample description, carbon and tetrapyrrole pigments at DSDP Hole 61-462

description: Six core-samples from DSDP/IPOD Site 462 in the Central Nauru Basin were examined for tetrapyrrole pigment content. Samples ranged from Pliocene to middle Cretaceous, and were recovered from 25 to 551 meters sub-bottom. The fate of chlorophyll in an open ocean environment was to be the prime objective of this study. Leg 61 is viewed as an extension of tetrapyrrole pigment studies in the western and southwestern Pacific which included the Japan Trench sites of Legs 56-57 (Louda et al., in press; Baker and Louda, in press a), the Shikoku Basin and Daito Ridge sites of Leg 58 (Baker and Louda, 1980), and the Mariana Basin and Trench sites of Leg 60 (Baker and Louda, in press b). Throughout these studies, we have detected tetrapyrrole pigments which by their quantity and quality could be related to the overall productivity of overlying waters, depositional environments, and certain geologic events, such as reworking. The more-oceanic position of Site 462 and suspected turbidite deposition in the deep ocean basin in which it is situated seemed favorable for relating rate of pigment loss to oxic diagenesis.
description: Sediment depth is given in mbsf. Empty cells mean no data.
description: Supplement to: Baker, Earl W; Louda, William (1981): Geochemistry of chlorophyll derivatives: Deep Sea Drilling Project Leg 61, Site 462, northern Nauru Basin. In: Larson, RL; Schlanger, SO; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 61, 619-620
DOI: 10.1594/pangaea.707101
title: Other measurements at 300 m from station Boulder (2008-08)
DOI: 10.1594/pangaea.672272
title: Input-output parameters for the steady-state model of Independencia Bay in 1996, Peru
DOI: 10.1594/pangaea.817778
title: (Table 5) Titanomagnetite in basalts DSDP Hole 66-487

description: The determination of the unit cell dimension of magnetic ore mineral from Sample 66-487-20-1,113-115 cm, performed by M. T. Dmitrieva, shows that according to the value of this parameter, a = 8.405 ± 0.005 Å, the mineral is almost pure magnetite (a = 8.395-8.40 Å).
DOI: 10.1594/pangaea.677736
title: Ozone measurements from station South Pole (1994-07)
DOI: 10.1594/pangaea.701711
title: (Table 2) Stable oxygen and carbon isotope ratios of Inoceramus and paleotemperture reconstruction from DSDP Hole 22-217 in the Indian Ocean

description: Late Campanian-Early Maastrichtian
DOI: 10.1594/pangaea.494988
title: Water temperature MBT profiles from cruise K7401M_1950
DOI: 10.1594/pangaea.817804
title: (Table 2) Chemical composition of plagioclase at DSDP Hole 66-487
DOI: 10.1594/pangaea.494872
title: Physical oceanography during cruise U90XX00013C_1986
DOI: 10.1594/pangaea.817685
title: (Table 1) Uncompacted and compacted sedimentation rate values corrected for bedding attitudes at DSDP Leg 66 Holes

description: Sediment accumulation rates, computed using agesediment thickness curves obtained from DSDP cores, are rarely corrected for compaction or bedding attitude to better approximate true sediment accumulation rates (c.f. van Andel et al., 1975; Davies et al., 1977; and Whitman and Davies, 1979). Variations with depth in either of these factors can hinder interpreting relative rates of sedimentary processes associated with a particular depositional environment. This problem becomes particularly relevant for convergent margin sediments, which often display variable bedding attitudes and pronounced changes in porosity, bulk density, and other parameters related to the compaction process at shallow depth. These rapid shallow changes render correlation of sedimentation rates within a single transect of holes very difficult. Two techniques have been applied to data collected from a transect of holes along the southwestern Mexico continental margin, DSDP Leg 66 (Fig. 1), to correct sediment accumulation rates for variations in compaction and bedding attitude. These corrections should help resolve true fluctuations in accumulation rates and their implications regarding convergent margin processes.
description: Sediment thickness drilled is the apparent thickness penetrated by drilling. True sediment thickness is corrected for bedding attitude.
description: Supplement to: Shephard, Les E; McMillen, Kenneth J (1982): Sedimentation rates of the southern Mexico Continental Margin, Deep Sea Drilling Project Leg 66. In: Watkins, JS; Casey Moore, J; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 66, 445-452
DOI: 10.1594/pangaea.477681
title: Hydrochemistry measured on water bottle samples at station SPac_1967_ET_28S/170

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.761749
title: Hydrochemistry measured on water bottle samples during KAPITAN DRANITSYN cruise Transdrift-III to the Laptev Sea, Arctic Ocean

description: The TRANSDRIFT III expedition was part of the joint Russian-German cooperation and the Laptev Sea System project. The Arctic and Antarctic Research Institute (AARI) in St. Petersburg and the GEOMAR Research Center for Marine Geosciences were jointly responsible for the organization and coordination of the TRANSDRIFT III expedition, which was funded by the Russian Ministry for Research and Technology and the German Ministry for Research and Technology.The TRANSDRIFT III expedition was carried out aboard the Russian icebreaker KAPITAN DRANITSYN in the Laptev Sea from October 1 to 30, 1995. In this shelf region a multi-disciplinary working program investigated the causes and effects of annual freeze-up. Unlike our previous expeditions to the Laptev Sea, which focused on oceanographical, hydrochemical, ecological and sedimentological processes during the brief ice-fee period in summer, this expedition studied these processes during the extreme physical change through the onset of ice formation in autumn. This was the first study of its kind under these conditions, and gave important clues to the rapid (14 to 40 days) freeze-up, which has significant year-round effects on the Laptev Sea and global environment.The working program was carried out in bilateral cooperation. CTD data were retrieved at a total number of 75 positions in the Laptev Sea. Hydrochemical sampling with oxygen, silicate and phosphate analysis was carried out at 65 of these stations.
DOI: 10.1594/pangaea.691079
title: Nutrient concentrations in water samples collected at Station DEC94-JAN95-GN3619940280400050 in the Aegean Sea
DOI: 10.1594/pangaea.672223
title: Radiosonde measurements from station South Pole (2004-12)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.818012
title: (Table 1) Water-extractable and acid-extractable carbohydrates in DSDP Leg 65 samples

description: Selected parts of ten frozen core samples from Holes 482A, 482B, 483A, and 485A, Leg 65 of the Deep Sea Drilling Project (DSDP), were analyzed for residual carbohydrates in order to determine the provenance and history of the organic material in the sediments. The samples, which represented silty-clay, shale, and nannofossil- chalk sediments, were analyzed for water-soluble monosaccharides, acid-soluble monosaccharides, and for starch and cellulose. Most samples yielded positive results for acid-extractable (polymeric) arabinose, fucose, xylose, mannose, galactose, and glucose. Amylose was detected in seven of the samples, whereas cellulose was found in only one. Possible explanations for the relatively high levels of free sugars are suggested in the conclusions to this chapter.
description: Empty cells mean not determined.
description: Supplement to: Swain, Frederick M; Bratt, Judy M (1983): Carbohydrate residues in core samples from the mouth of 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, 439-440
DOI: 10.1594/pangaea.750237
title: Meteorological observations during La Perle cruise from Coastal started at 1769-05-02
DOI: 10.1594/pangaea.707098
title: Other measurements at 300 m from station Boulder (2008-07)
DOI: 10.1594/pangaea.817767
title: (Table 5) Geochemistry of amphiboles at DSDP Sample 66-489A-1-CC
DOI: 10.1594/pangaea.835710
title: Nutrients measured in surface water during CHALLENGER cruise CH128B
DOI: 10.1594/pangaea.484942
title: Sea surface temperature data during cruise Polarstjernen_18700416

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.819732
title: (Table 1) Sr isotopes on carbonates at DSDP Hole 62-463

description: Study of 12 carbonate oozes from Deep Sea Drilling Project Hole 463, in the Mid-Pacific Mountains, suggests mean values of 0.70690 ± 0.00029 (2-sigma) and 0.70712 ± 0.00030 (relative to 0.71014 for the NBS 987 Sr isotope standard) as representing the Sr isotope composition of the Barremian and early Aptian seas, respectively. Two additional values of less than 0.7064 are the least radiogenic values known from the Phanerozoic and may be a consequence of the introduction of Sr depleted in the heavy isotope from massive submarine volcanic activity, which followed the initiation of the latest oceanic spreading episode in the Oxfordian.
description: Supplement to: Clauer, Norbert (1981): 87Sr/86Sr ratios of the Barremian and early Aptian Seas. In: Thiede, J; Vallier, TL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 62, 781-783
DOI: 10.1594/pangaea.817774
title: (Table 1) Modal composition of basalts at DSDP Hole 66-487

description: &lt;1= rare grains; #0= in matrix.
DOI: 10.1594/pangaea.663589
title: Oceanography at CTD/bottle station IFREMER_0429
DOI: 10.1594/pangaea.773657
title: Sea-floor videos along ROV profile B08-05 from the Bay of Biscay with links to files
DOI: 10.1594/pangaea.495342
title: Water temperature XBT profiles from cruise U31X044927_1974
DOI: 10.1594/pangaea.825372
title: Magnetic remanence from IODP Hole 329-U1369B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.826387
title: Pass-through measurements of magnetic susceptibility from IODP Hole 329-U1366C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.879235
title: (Table 2) Concentration of CL brGDGTs and crenarchaeol for soils and marine surface sediments
DOI: 10.1594/pangaea.707080
title: (Table 1) Analyses of halite samples from DSDP Hole 23-225

description: Sample 23-225-29-3,40-45: Rb content is 0.00037 weight-% per total sample or 0.0014 weight-% Rb per pure polyhalite
DOI: 10.1594/pangaea.819741
title: (Table 5) Abundances of other elements enhanced by over a factor of 10 in the pyrite-containing fractions, relative to the Cretaceous calcareous at DSDP Hole 62-465A

description: Empty cells mean no data.
DOI: 10.15468/dl.qqwm48
title: Occurrence Download

description: A dataset containing 163115 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "TaxonKey is Sterna hirundo Linnaeus, 1758",
 "Year 2019-2019"
 ]
}

 The dataset includes 163115 records from 288 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031255-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.707050
title: (Figure 1) Chronology of sediment core from the Monticchio maar
DOI: 10.1594/pangaea.707052
title: (Table 1) Major element abundances in boninite and tholeiite from DSDP Hole 60-458
DOI: 10.1594/pangaea.879236
title: (Table 3) Concentration of CL and IPL-brGDGTs and crenarchaeol for river SPM samples
DOI: 10.1594/pangaea.741904
title: SeaWiFS total absorption results except pure water measured at 555 nm

description: Monthly coverage, 18 km on equal angle resolution.
DOI: 10.1594/pangaea.818037
title: Coral δ¹³C record from the Northern Gulf of Aqaba, sample Aq-19A
DOI: 10.1594/pangaea.807090
title: (Table 1) Trace elements at DSDP Leg 81 Holes
DOI: 10.1594/pangaea.918913
title: Halo Doppler Lidar measurements on Hailuoto Island during campaign HAOS in February/March 2020
DOI: 10.1594/pangaea.819706
title: (Appendix) Occurrence and abundance of chert and porcellanite in cores recovered during DSDP Leg 62

description: Sediment depth is given in mbsf. The abundance of chert in the core is a qualitative estimate based on the amount and type of recovered sediment, the drilling time, torque and pump pressure of coring as determined from the drilling log, experience of the drilling crew, and discussions with the drilling crew during coring attempts. Rare (R) generally means the recovery of only a few fragments of chert (&lt; 1%) within a high-recovery calcareous sediment core, or the recovery of a few fragments when other factors indicate the near absence of chert (fast drill time, low torque, low pump pressure). Common (C) shows a higher percentage of chert in the core (1-10%) and (or) high drill time, high and steady torque, and possibly high pump pressure. Abundant (A) generally indicates that at least 10% of a drilled sequence consists of chert, as shown by high chert percentages in the recovered sediment, and high drill time, torque, and pump pressure. A dash indicates the absence of chert.
DOI: 10.1594/pangaea.830939
title: Satellite-based lake surface water temperatures from Lake_Neusiedler, 1989-2013

description: Lake Surface Water Temperature (LSWT) has been extracted from a 3x3 pixel array at the center of the lake. See "Event(s)" for Lake/pixel co-ordinates.
DOI: 10.1594/pangaea.818454
title: (Table 7) Geochemistry of spinel from DSDP Hole 64-474A
DOI: 10.1594/pangaea.901215
title: Firn-air O2 isotopic data for the LOCK-IN site
DOI: 10.1594/pangaea.907497
title: Organic carbon, nitrogen, sulfur content and stable carbon isotopes for sediment core PG1169
DOI: 10.1594/pangaea.818794
title: Glacier mass balance Hintereisferner, Ötztal Alps, Austria, 1972/1973
DOI: 10.1594/pangaea.907498
title: Organic carbon, nitrogen, sulfur content and stable carbon isotopes for sediment core PG1170
DOI: 10.1594/pangaea.784677
title: Composition of sulfides from the Sierra Leone Fracture Zone (Central Atlantic Ocean)

description: An analysis of data on the location of hydrothermal fields, seismicity, and satellite altimetry evidences that in mid-ocean ridges with low spreading rate hydrothermal fields tend to be grouped in areas with generally low seismic activity and at intersections of discontinuities and rift zones. Based on this assumption, the Sierra Leone Fracture Zone was studied in 2000 during Cruise 22 of R/V Akademik Nikolaj Strakhov. A study of gabbrodolerite and dolerite showed that sulfide ore minerals in them were formed both by hydrothermal and magmatic processes. An analysis of melt inclusions demonstrated that magmatic complexes formed from a high-temperature (1210-1255°C) low-potassium melt of the N-MORB type. Investigations of fluid inclusions revealed that gabbro and dolerite formed under influence of an active hydrothermal system at temperature 205-226°C. Thus, the Sierra Leone Fracture Zone is considered to be perspective for a discovery of a new hydrothermal field.
description: Supplement to: Mazarovich, Alexander O; Simonov, Vladimir A; Peive, Aleksandr V; Kovyazin, S V; Tret'yakov, G A; Raznitsin, Yury N; Savel'eva, G N; Skolotnev, Sergey G; Sokolov, S Yu; Turko, Natalia N (2001): Hydrothermal mineralization in the Sierra Leone Fracture Zone (Central Atlantic Ocean). Translated from Litologiya i Poleznye Iskopaemye, 2001, 5, 526-533, Lithology and Mineral Resources, 36(5), 460-466
DOI: 10.1594/pangaea.909437
title: Benthic foraminifera in surface sediments, small fraction
DOI: 10.1594/pangaea.666033
title: Oceanography at CTD/bottle station IFREMER_2859
DOI: 10.1594/pangaea.834347
title: Ceilometer raw data measured at Neumayer Station (2010-05), links to files
DOI: 10.1594/pangaea.674528
title: Radiosonde measurements from station Kwajalein (1992-08)
DOI: 10.1594/pangaea.674487
title: Radiosonde measurements from Neumayer Station (2003-08)
DOI: 10.1594/pangaea.867854
title: Broadband albedo transects in the lower ablation zone of southwest Greenland on 2013-06-16
DOI: 10.1594/pangaea.496471
title: Water temperature IBT profiles from cruise U999981011I_1980
DOI: 10.1594/pangaea.818298
title: (Fig. 4) Concentrations P2O5, K, and Fe in peat ash with peat age in the Kyzyltun (Bokarevskii) ryam bog

description: Data were digitized from the plot.
DOI: 10.1594/pangaea.811546
title: (Table 1) Age model of ODP Site 189-1172

description: Sediment depth is given in mcd.
DOI: 10.1594/pangaea.867857
title: Broadband albedo transects in the lower ablation zone of southwest Greenland on 2013-06-25
DOI: 10.15468/dl.usaq56
title: Occurrence Download

description: A dataset containing 502 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Continent is South America",
 "TaxonKey is Macrocoma tenuis (Hook. & Grev.) Vitt"
 ]
}

 The dataset includes 502 records from 50 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031270-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.747614
title: Meteorological observations during BEAVER cruise from Barbados to Halifax started at 1768-03-31
DOI: 10.1594/pangaea.860865
title: Physical oceanography from Seaglider mission CNCY201314911, links to files in NetCDF format
DOI: 10.1594/pangaea.633946
title: Sea-bed images of permanent plots of rocky benthos at Medes, site Pota de Llop, plot L6E

description: Area monitored at each permanent plot: 310 cm²
DOI: 10.1594/pangaea.633998
title: Sea-bed images of permanent plots of rocky benthos at Marseille, site Riou Sud, plot R5E

description: Area monitored at each permanent plot: 310 cm²
DOI: 10.1594/pangaea.921916
title: NAO proxy-based reconstruction from Iberian Peninsula (-150 to 2010 CE)

description: We present a quantitative NAO reconstruction for the central Iberian Peninsula (IP) over the last two millennia, along with its uncertainties, by applying a Bayesian approach.
DOI: 10.1594/pangaea.874404
title: Microbiota diversity of common lizards (Zootoca vivipara) as a function of climatic treatment, link to supplementary data

description: Climate change is now considered as the greatest threat to biodiversity and ecological networks, but its impacts on the bacterial communities associated with plant or animals remain largely unknown. Here, we studied the consequences of climate warming on gut bacterial communities of an ectotherm, the common lizard (Zootoca vivipara), using a semi-natural experimental approach. We found that +2/3°C warmer climates cause a 34% loss of populations' microbiota diversity, with possible negative consequences for host survival.
description: Version 2 (2017-06-28)
description: Supplement to: Bestion, Elvire; Jacob, Staffan; Zinger, Lucie; Di Gesu, Lucie; Richard, Murielle; White, Joël; Cote, Julien (2017): Climate warming reduces gut microbiota diversity in a vertebrate ectotherm. Nature Ecology & Evolution, 1(6), 0161
DOI: 10.1594/pangaea.886793
title: Figure 4: Iron characteristics of surface sediments in the Mustionjoki estuary transect September 2014
DOI: 10.1594/pangaea.714262
title: Meteorological synoptical observations from station Payerne (2008-09)
DOI: 10.1594/pangaea.818793
title: Glacier mass balance Hintereisferner, Ötztal Alps, Austria, 1971/1972
DOI: 10.1594/pangaea.818928
title: (Table 2) Relative content of alkanes at DSDP Leg 64 Holes
DOI: 10.1594/pangaea.745632
title: Statistics for grain size analysis of surface sediments off Sylt collected during HEINCKE cruise HE236
DOI: 10.1594/pangaea.682706
title: (Table 4) Principal component analysis, paleotemperatures and distribution of infaunal benthic foraminifera in Late Quaternary sediments of core RC09-150 in the southeast Indian Ocean
DOI: 10.1594/pangaea.702142
title: (Appendix 1) Estimated sea-surface temperatures of DSDP Hole in the western Pacific Ocean

description: FP-12E is the planktonic foraminiferal transfer function developed by Thompson (1981, doi:10.1016/0031-0182(81)90099-7) for the western Pacific. Time-slice: 1 = 1.8-2.0 Ma, 2 = 2.4-2.6 Ma, 3 = 2.8-3.0 Ma. 4 = 3.5-3.7 Ma, 5 = 4.2-4.4 Ma. 6 = 4.8-5.0 Ma. Time-interval: 1 = 0.0-2.0, 2 = 1.8-2.6, 3 = 2.4-3.0, 4 = 2.8-3.7, 5 = 3.5-4.4, 6 = 4.2-5.0, 7 = &gt;4.8
DOI: 10.1594/pangaea.894263
title: CICE output from Navy Earth System Model (NESM) for 2018082712

description: INITIALIZATION: 2018082712FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;