cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.984007
title: Magnetic susceptibility of sediment core GeoB25226-1

description: Calibrated, drift-corrected, full core, loop sensor (140 mm) magnetic volume susceptibility measurements in 1 cm steps.
DOI: 10.1594/pangaea.984114
title: Electrical conductivity, porosity and density of sediment core GeoB25201-2
DOI: 10.1594/pangaea.984131
title: Electrical conductivity, porosity and density of sediment core GeoB25201-3
DOI: 10.1594/pangaea.984140
title: Electrical conductivity, porosity and density of sediment core GeoB25202-2
DOI: 10.1594/pangaea.984144
title: Electrical conductivity, porosity and density of sediment core GeoB25206-2
DOI: 10.1594/pangaea.984145
title: Electrical conductivity, porosity and density of sediment core GeoB25212-2
DOI: 10.1594/pangaea.984146
title: Electrical conductivity, porosity and density of sediment core GeoB25212-3
DOI: 10.1594/pangaea.984147
title: Electrical conductivity, porosity and density of sediment core GeoB25217-2
DOI: 10.1594/pangaea.984148
title: Electrical conductivity, porosity and density of sediment core GeoB25219-1
DOI: 10.1594/pangaea.984149
title: Electrical conductivity, porosity and density of sediment core GeoB25221-2
DOI: 10.25574/30638
title: Chandra X-ray Observatory ObsId 30638

description: Probing the power source in narrow-line AGN Green Pea galaxies
DOI: 10.1594/pangaea.984150
title: Electrical conductivity, porosity and density of sediment core GeoB25222-1
DOI: 10.1594/pangaea.984155
title: Electrical conductivity, porosity and density of sediment core GeoB25224-1
DOI: 10.1594/pangaea.905396
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core HU91-45-080P
DOI: 10.1594/pangaea.984156
title: Electrical conductivity, porosity and density of sediment core GeoB25226-2
DOI: 10.1594/pangaea.788787
title: (Table T1) Relative abundance of diatoms in ODP Hole 169-1034B sediments

description: Ocean Drilling Program (ODP) Site 1034 (48°38.000'N, 123°30.000'W) was drilled at a water depth of 200 m in the Saanich Inlet, an anoxic fjord on the southeastern coast of Vancouver Island, British Columbia, to a depth of 118.2 meters below seafloor (mbsf). The uppermost 50 m consists of very well-laminated (triplet varves) diatomaceous muds deposited over the past 7000 yr. Below, sediments become progressively less distinctly laminated and reflect better oxygenated bottom-water conditions. The oldest sediments recovered at Site 1034 were dated as 14 to 15 ka (see Shipboard Scientific Party, 1998, doi:10.2973/odp.proc.ir.169s.1998).Varved sediments recovered during Leg 169S in the Saanich Inlet offer an excellent opportunity to compare the interannual variability of recent climatic elements (e.g., sea-surface temperature, salinity, precipitation) with those of late Quaternary periods that were characterized by climates appreciably different from those of today. A large amount of recent diatom data from Saanich Inlet exists, which can serve as a baseline for such comparisons: Sancetta (1989a, doi:10.1029/PA004i003p00235; 1989b, doi:10.1093/plankt/11.3.503; 1990) investigated modern processes controlling the accumulation of diatoms and spacial and temporal trends of diatom flux in the Inlet; Sancetta and Calvert (1988, doi:10.1016/0198-0149(88)90058-1) documented the annual cycle of sedimentation in the fjord. McQuoid (1995) and McQuoid and Hobson (1997, doi:10.1093/plankt/19.2.173) studied the modern pattern of diatom succession in the Saanich Inlet and analyzed the diatoms in laminae couplets in frozen sediment cores for the years 1900 to 1991 A.D.This report describes the intra-annual variability of the diatom assemblages at Site 1034, during a 8-yr interval near 9 ka. Pollen and dinoflagellates are being studied from the same samples by R. Hebda and P. Mudie (unpubl. data).
description: Diatoms were identified and counted under the light microscope at 1000x. A total of at least 300 valves was counted per sample, with about half of the counts done on one slide and the other half on the other slide.
description: Supplement to: Fourtanier, Elisabeth; Barron, John A (2000): Data Report: Intra-annual variability of the diatom assemblages at Hole 1034B (Saanich Inlet) near 9 ka. In: Bornhold, BD; Firth, JV (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 169S, 1-8
DOI: 10.1594/pangaea.905395
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core HU91/39-012
DOI: 10.1594/pangaea.936779
title: Lipid biomarkers, siliceous microfossil assemblages, biogenic silica and carbon and nitrogen bulk and isotope analyses from IODP Hole 341-U1417D, Gulf of Alaska

description: We analysed IODP Expedition 341 Site U1417 to understand the palaeoceanography in the Gulf of Alaska across the Pliocene and early Pleistocene (4-1.7 Ma). The data submitted here are productivity-related biomarkers (alkenone and brassicasterol accumulation rates), siliceous microfossils (total diatoms and silicoflagellate accumulation rates and diatom assemblages accumulation rates and relative abundance), biogenic silica accumulation rates, bulk carbon and nitrogen accumulation rates and stable isotope ratios (δ13C and δ15N), terrestrial and aquatic n-alkane accumulation rates, the Shannon-Weaver index and preservation value of diatoms (prev. value). The diatom assemblages include pelagic high productivity, pelagic warm water, coastal high productivity, coastal moderate productivity, benthic and freshwater habitats.
DOI: 10.1594/pangaea.905290
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core MD99-2220
DOI: 10.1594/pangaea.905291
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core MD99-2227
DOI: 10.1594/pangaea.863436
title: Physical oceanography during HEINCKE cruise HE429
DOI: 10.1594/pangaea.905394
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core HU90/31-019
DOI: 10.1594/pangaea.863428
title: Physical oceanography during HEINCKE cruise HE418
DOI: 10.1594/pangaea.863430
title: Physical oceanography during HEINCKE cruise HE421
DOI: 10.1594/pangaea.905400
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core MSM05/3_343300
DOI: 10.1594/pangaea.53374
title: (Table 3) Calculated sea surface temperature and paleoproductivity of sediment core D11957P
DOI: 10.1594/pangaea.804559
title: Table 1: Diatom distribution in surface sediments of the Kara Sea

description: Diatom assemblages in 62 surface sediment samples from the outer Ob and Yenisei estuaries and the adjacent inner Kara Sea shelf were examined in relation to environmental conditions. Concentrations of diatoms reflect the biological productivity of surface waters along with specific water mass processes of diatom valve deposition in the zone of intermixing of riverine and marine waters. An inverse relationship between total concentration of diatom valves in sediments and surface water salinity is found. Extremely high abundances of diatom valves (up to 82.4 million valves/g sediment) are observed in the outer Ob and Yenisei estuaries (salinity &lt; 5) and are related to a zone with rapid deposition of riverine organic matter. The overall distribution pattern of freshwater diatoms indicates the inflow of river water onto the shelf and follows the general pattern in surface water salinity. A linear regression between average summer surface water salinity and relative proportions of freshwater diatoms reveals a correlation coefficient of r = 0.86 for a salinity range of ~ 5 to 20. The distribution of sea-ice diatoms in the surface sediments generally reflects the sea-ice conditions during spring and summer time. Steep increases in their relative abundances (&gt;10-20%) correspond to the mean interannual location of the winter polynya corroborating previously obtained results from the Laptev Sea.
description: Supplement to: Polyakova, Ye I (2003): Diatom assemblages in surface sediments of the Kara Sea (Siberian Arctic) and their relationship to oceanological conditions. In: Stein, R; Fahl, K; Fütterer, D K; Galimov, E M & Stepanets, O V (eds.), Siberian River Run-off in the Kara Sea: Characterisation, Quantification, Variability, and Environmental Significance, 488 pp. Proceedings in Marine Sciences, Elsevier, Amsterdam, 6, 375-399
DOI: 10.1594/pangaea.905288
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core HUD2008/29_40
DOI: 10.1594/pangaea.56503
title: Content of different diatom species in sediment core GIK23414-6 and -9
DOI: 10.1594/pangaea.987079
title: Magnetic susceptibility of sediment core GeoB25220-1

description: Calibrated, drift-corrected, full core, loop sensor (85 mm) magnetic volume susceptibility measurements in 1 cm steps. Segment end data are mirror-corrected or overlapped. Section depth (cm) refers to total recovered core length per barrel. Nominal depth (mbsf) is calculated by adding section depth (m) to curated MeBo barrel top depth. Some core segments were liquified and redposited during recovery.
DOI: 10.1594/pangaea.987078
title: Magnetic susceptibility of sediment core GeoB25214-1

description: Calibrated, drift-corrected, full core, loop sensor (85 mm) magnetic volume susceptibility measurements in 1 cm steps. Segment end data are mirror-corrected or overlapped. Section depth (cm) refers to total recovered core length per barrel. Nominal depth (mbsf) is calculated by adding section depth (m) to curated MeBo barrel top depth. Some core segments were liquified and redposited during recovery.
DOI: 10.1594/pangaea.987083
title: Magnetic susceptibility of sediment core GeoB25222-2

description: Calibrated, drift-corrected, full core, loop sensor (85 mm) magnetic volume susceptibility measurements in 1 cm steps. Segment end data are mirror-corrected or overlapped. Section depth (cm) refers to total recovered core length per barrel. Nominal depth (mbsf) is calculated by adding section depth (m) to curated MeBo barrel top depth. Some core segments were liquified and redposited during recovery.
DOI: 10.1594/pangaea.987096
title: Magnetic susceptibility of sediment core GeoB25223-1

description: Calibrated, drift-corrected, full core, loop sensor (85 mm) magnetic volume susceptibility measurements in 1 cm steps. Segment end data are mirror-corrected or overlapped. Section depth (cm) refers to total recovered core length per barrel. Nominal depth (mbsf) is calculated by adding section depth (m) to curated MeBo barrel top depth. Some core segments were liquified and redposited during recovery.
DOI: 10.1594/pangaea.53377
title: Realtive abundance of diatom species in sediment core IK9373-10
DOI: 10.1594/pangaea.905284
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core HU91/45-072
DOI: 10.1594/pangaea.905286
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core HU91/45-085
DOI: 10.1594/pangaea.140491
title: Sea surface temperature reconstruction from sediment core GeoB1309-2
DOI: 10.1594/pangaea.722592
title: (Table DR5) Freshwater diatoms and salinity estimations from ODP Hole 167-1019D data
DOI: 10.1594/pangaea.140494
title: Sea surface temperature reconstruction from sediment core GeoB2204-2
DOI: 10.1594/pangaea.905281
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core HU90-13-013
DOI: 10.1594/pangaea.53378
title: Diatom assemblage in surface sediments of the Laptev Sea
DOI: 10.1594/pangaea.863434
title: Physical oceanography during HEINCKE cruise HE427
DOI: 10.1594/pangaea.849112
title: Summer sea surface temperature and winter sea ice concentration for the EPILOG-LGM time slice in the Pacific Southern Ocean
DOI: 10.1594/pangaea.55660
title: Diatom assemblage of sediment core IOW211660-1
DOI: 10.1594/pangaea.57612
title: Content of different diatom species in sediment core GIK23259-2
DOI: 10.1594/pangaea.905287
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core HUD2003/33-011
DOI: 10.1594/pangaea.743316
title: (Table 7) Paleotemperature estimates for ODP Hole 104-642B
DOI: 10.1594/pangaea.743317
title: (Table 3) Paleotemperature estimates for ODP Hole 105-646B
DOI: 10.15468/dl.c4cf82
title: Occurrence Download

description: A dataset containing 1348 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Cobitis sinensis",
 "HasCoordinate is true",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 1348 records from 19 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0007682-260108223611665/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.905282
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core HU90/31-044
DOI: 10.1594/pangaea.905402
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core TWC04
DOI: 10.1594/pangaea.905283
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core HU91/45-006
DOI: 10.1594/pangaea.905399
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core HUD2008/29-004
DOI: 10.1594/pangaea.56524
title: Content of different diatom species in sediment core GIK23424-3
DOI: 10.1594/pangaea.905289
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core MD95-2033
DOI: 10.34740/kaggle/dsv/14479793
title: BITCOIN Historical Datasets 2018-2026 Binance API
DOI: 10.1594/pangaea.905278
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core HU84/30-21PC
DOI: 10.1594/pangaea.905401
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core Nachvak_602-1
DOI: 10.1594/pangaea.863429
title: Physical oceanography during HEINCKE cruise HE420
DOI: 10.1594/pangaea.863435
title: Physical oceanography during HEINCKE cruise HE428
DOI: 10.1594/pangaea.56462
title: Content of different diatom species in sediment core GIK23071-2 and -3
DOI: 10.1594/pangaea.905434
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core 2004-804-009
DOI: 10.1594/pangaea.693950
title: Trawlings during OCHER cruise OCH1, Part I

description: The fish catches were carried out by the industrial midwater non-closed trawl. There was a small-mesh section with minimum mesh size of 12 mm in the trawl bag. Vertical opening of the trawl made from 35 to 46 m. The trawling duration under catches in the sound-scattering layers made 55 min. to 2 hours and 20 min. Speed of trawling made 4.8-5.7 knots. The catches horizons were determined by the state of sound-scattering layers and fish schools. At night they carried out catches in the upper 2-90 m layer. At the day time they trawled at a range of 32-370 m depths. Each catch was weighted. Fish was determined up to the lowest taxonomic ranks - species, in some cases - genus. Total number and mass of each species in a catch, and average dry mass of one specimen of a species were determined. The standard fish body length (SL) was measured in mm (from the tip of snout to the basement of the middle rays of the caudal fin). The samples were fixed in 10% buffered formaldehyde for further processing in the IBSS laboratories.
DOI: 10.1594/pangaea.693954
title: Trawlings during Professor Vodyanitskiy cruise PV11

description: The fish catches were carried out by the scientific midwater non-closed trawl. There was a small-mesh section with minimum mesh size of 0.14-0.09 mm in the trawl bag. Vertical opening of the trawl made up to 6 m. The trawling duration under catches in the sound-scattering layers made 1 hour. Speed of trawling made 3.0 knots. The catches horizons were determined by the state of sound-scattering layers and they carried out in 30-116 m. Each catch was weighted. Fish was determined up to the lowest taxonomic ranks - species, in some cases - genus. Total number and mass of each species in a catch, and average dry mass of one specimen of a species were determined. The standard fish body length (SL) was measured in mm (from the tip of snout to the basement of the middle rays of the caudal fin). The samples were fixed in 10% buffered formaldehyde for further processing in the IBSS laboratories.
DOI: 10.1594/pangaea.693957
title: Trawlings during Professor Vodyanitskiy cruise PV24, Part III

description: The fish catches were carried out by the scientific midwater non-closed trawl. There was a small-mesh section with minimum mesh size of 0.11-0.07 mm in the trawl bag. Vertical opening of the trawl made up to 6 m. The trawling duration under catches in the sound-scattering layers made 30 min. Speed of trawling made 3.0 knots. The trawling survey has been carried out in the Equatorial zone along 6°, 12°, 18° and 24° W meridians with about 1o intervals by latitude. 56 total catches in the upper 120 m layer (25 at the daytime and 31 in night) have been fulfilled. For sound-scattering layers catching 22 trawlings at the daytime at the 250-425 m depths scale and 37 night trawlings from the surface to 172 m have been carried out. Each catch was weighted. Fish was determined up to the lowest taxonomic ranks - species, in some cases - genus. Total number and mass of each species in a catch, and average dry mass of one specimen of a species were determined. The standard fish body length (SL) was measured in mm (from the tip of snout to the basement of the middle rays of the caudal fin). The samples were fixed in 10% buffered formaldehyde for further processing in the IBSS laboratories.
DOI: 10.1594/pangaea.693955
title: Trawlings during Professor Vodyanitskiy cruise PV24, Part I

description: The fish catches were carried out by the scientific midwater non-closed trawl. There was a small-mesh section with minimum mesh size of 0.11-0.07 mm in the trawl bag. Vertical opening of the trawl made up to 6 m. The trawling duration under catches in the sound-scattering layers made 30 min. Speed of trawling made 3.0 knots. The trawling survey has been carried out in the Equatorial zone along 6°, 12°, 18° and 24° W meridians with about 1o intervals by latitude. 56 total catches in the upper 120 m layer (25 at the daytime and 31 in night) have been fulfilled. For sound-scattering layers catching 22 trawlings at the daytime at the 250-425 m depths scale and 37 night trawlings from the surface to 172 m have been carried out. Each catch was weighted. Fish was determined up to the lowest taxonomic ranks - species, in some cases - genus. Total number and mass of each species in a catch, and average dry mass of one specimen of a species were determined. The standard fish body length (SL) was measured in mm (from the tip of snout to the basement of the middle rays of the caudal fin). The samples were fixed in 10% buffered formaldehyde for further processing in the IBSS laboratories.
DOI: 10.1594/pangaea.693961
title: Trawlings during TITANIT cruise TIT1, Part II

description: The fish catches were carried out by the industrial midwater non-closed trawl. There was a small-mesh section with minimum mesh size of 6.5 mm in the trawl bag. Vertical opening of the trawl made from 26 to 42 m. The trawling duration under catches in the sound-scattering layers made 1 hour, under fish schools catches - from 40 min up to 2 hours and 20 min. Speed of trawling made 3.2-4.2 knots. The catches horizons were determined by the state of sound-scattering layers and fish schools. At night they carried out catches usually in the upper 0-90 m layer, in some cases to 150 m. At the day time they trawled at a range of 15-410 m depths. Each catch was weighted. Fish was determined up to the lowest taxonomic ranks - species, in some cases - genus. Total number and mass of each species in a catch, and average dry mass of one specimen of a species were determined. The standard fish body length (SL) was measured in mm (from the tip of snout to the basement of the middle rays of the caudal fin). The samples were fixed in 10% buffered formaldehyde for further processing in the IBSS laboratories.
DOI: 10.15468/dl.2b9xwk
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{"type":"and","predicates":[{"type":"equals","key":"GADM_LEVEL_2_GID","value":"UZB.12.3_1","matchCase":false},{"type":"equals","key":"CLASS_KEY","value":"212","matchCase":false},{"type":"greaterThanOrEquals","key":"YEAR","value":"2015","matchCase":false},{"type":"not","predicate":{"type":"in","key":"BASIS_OF_RECORD","values":["MATERIAL_CITATION","MATERIAL_SAMPLE","PRESERVED_SPECIMEN"],"matchCase":false}},{"type":"lessThanOrEquals","key":"COORDINATE_UNCERTAINTY_IN_METERS","value":"10000","matchCase":false},{"type":"equals","key":"LICENSE","value":"CC BY 4.0","matchCase":false}]}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0007683-260108223611665/datasets/export for details.
DOI: 10.1594/pangaea.693948
title: Trawlings during NOVOUKRAINKA cruise NOV3, Part I

description: The fish catches were carried out by the industrial midwater non-closed trawl. There was a small-mesh section with minimum mesh size of 6.5 mm in the trawl bag. Vertical opening of the trawl made from 26 to 50 m. The trawling made 30 min up to 2 hour and 30 min. Speed of trawling made 3.2-4.2 knots. The catches horizons were determined by the state of sound-scattering layers and fish schools. At night they carried out catches usually in the upper 0-550 m layer. At the day time they trawled at a range of 60-490 m depths. Each catch was weighted. Fish was determined up to the lowest taxonomic ranks - species, in some cases - genus. Total number and mass of each species in a catch, and average dry mass of one specimen of a species were determined. The standard fish body length (SL) was measured in mm (from the tip of snout to the basement of the middle rays of the caudal fin). The samples were fixed in 10% buffered formaldehyde for further processing in the IBSS laboratories.
DOI: 10.1594/pangaea.693953
title: Trawlings during Professor Vodyanitskiy cruise PV10

description: The fish catches were carried out by the scientific midwater non-closed trawl. There was a small-mesh section with minimum mesh size of 0.14-0.09 mm in the trawl bag. Vertical opening of the trawl made up to 6 m. The trawling duration under catches in the sound-scattering layers made 1 hour. Speed of trawling made 3.0 knots. The catches horizons were determined by the state of sound-scattering layers and they carried out in 20-86 m. Each catch was weighted. Fish was determined up to the lowest taxonomic ranks - species, in some cases - genus. Total number and mass of each species in a catch, and average dry mass of one specimen of a species were determined. The standard fish body length (SL) was measured in mm (from the tip of snout to the basement of the middle rays of the caudal fin). The samples were fixed in 10% buffered formaldehyde for further processing in the IBSS laboratories.