cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.956362
title: Meteorological synoptical observations from station Minamitorishima (2022-12)
DOI: 10.1594/pangaea.956363
title: Radiosonde measurements from station Minamitorishima (2022-12)
DOI: 10.1594/pangaea.910726
title: Modern pollen percentages along the Songpinggou River, eastern Qinghai-Tibetan Plateau
DOI: 10.1594/pangaea.476025
title: Physical oceanography at CTD station AOS94/13-1

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.776632
title: A 2.2.2. Data of the batch experiments with construction waste - main elements
DOI: 10.1594/pangaea.859260
title: RNA/DNA ratio of Scophthalmus maximus first feeding larvae during feeding with beta-glucan (MacroGard)
DOI: 10.1594/pangaea.919700
title: Oxygen (δ¹⁸O) and hydrogen (δ²H) isotope compositions of ice in the core of large lithalsa in Sentsa River valley (Siberia)

description: Oxygen (δ¹⁸O) and hydrogen (δ²H) isotope compositions of ice in core of large lithalsa in Sentsa River valley.Analyses were made at the isotope laboratory of the Geographical Department of moscow University on a Finnigan Delta-V mass spectrometer with the standard gas-bench option (Prof. Yu. Vasil'chuk, Dr. N.Budantseva, Dr. Ju. Chizhova). The δ¹⁸O and δ²H values were expressed per mill (‰) as the deviation of the respective isotope ratios of the measured samples from the Vienna standard mean ocean water VSMOW (δ¹⁸O = 0 ‰, δ²H = 0 ‰) and Greenland Ice Sheet Precipitation GISP (δ¹⁸O = -24.76 ‰, δ²H = -189.5 ‰), as well as IAEA laboratory standards (IAEA 12, δ¹⁸O = -12.10 ‰, δ²H = -85.9 ‰; IAEA 13, δ¹⁸O = -33.35 ‰, δ²H = -257.2 ‰) and the domestic moscow University standard of fresh snow from the Garabashi glacier in the Cuacasus (δ¹⁸O = -15.60 ‰, δ²H = -110.0 ‰). The precision of the measurements was 0.1 ‰ for δ¹⁸O and 0.6 ‰ for δ²H.
DOI: 10.1594/pangaea.477492
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_OC_10S/179

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.762235
title: Counts and mass of different fish species from beam trawl samples in the Eastfrisian Wadden Sea during POLARIS cruise PO0207

description: Depth, water was calculated as mean from bathymetric depths at start/end of trawl
DOI: 10.1594/pangaea.848467
title: Basic measurements of radiation at station Camborne (2009-01)
DOI: 10.1594/pangaea.484358
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_6N_7S_9N/122-1

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.739053
title: Pollen profile BOBROV, Bobrov, Slovakia

description: Method: KOH, acetolysis, samples of the bottom pretreated with HF.The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.887744
title: Continuous meteorological observations at Neumayer station (2017-04)

description: The meteorological observatory Neumayer continuously acquires meteorological parameters. Measurements are taken on or near the meteorological 10m-mast, located some 300m south-east of the main station building. Co-located there are BSRN (Baseline Surface Radiation Network) measurements taken. The measurement interval of the raw data is approximately 6s. Data is quality controlled: All measurements are checked daily on site and again prior to publication according to BSRN standards. Knowingly affected or erroneous data is removed.
DOI: 10.1594/pangaea.720239
title: Ultra-violet measurements from station Desert Rock (2003-08)

description: Version 2, 2009-06-16. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-08.
DOI: 10.1594/pangaea.890189
title: Age determination of Nuikluk_coreNL10-1 peat core
DOI: 10.1594/pangaea.665183
title: Oceanography at CTD/bottle station IFREMER_2023
DOI: 10.1594/pangaea.855026
title: Basic measurements of radiation at station Lerwick (2015-09)
DOI: 10.1594/pangaea.911632
title: CT scans of Lake Cucao sediment cores
DOI: 10.1594/pangaea.878560
title: (Fig. 1-21) Chronostratigraphy of the organic-rich Eagle Ford Group
DOI: 10.1594/pangaea.900410
title: Sandwich Town Neck Beach UAS Aerial Imagery 2018-01-04 (Peter Traykovski, Woods Hole Oceanographic Intitution)

description: Aerial Images from a DJI Phantom 4 with FC330 Camera and Kinematic GPS Marker Flag Locations, in support of coastal morphology studies.
DOI: 10.1594/pangaea.919701
title: Oxygen (δ¹⁸O) and hydrogen (δ²H) isotope compositions of ice in the core of a small lithalsa in Sentsa River valley (Siberia)

description: Oxygen (δ¹⁸O) and hydrogen (δ²H) isotope compositions of ice in core of a small lithalsa in Sentsa River valley.Analyses were made at the isotope laboratory of the Geographical Department of moscow University on a Finnigan Delta-V mass spectrometer with the standard gas-bench option (Prof. Yu. Vasil'chuk, Dr. N.Budantseva, Dr. Ju. Chizhova). The δ¹⁸O and δ²H values were expressed per mill (‰) as the deviation of the respective isotope ratios of the measured samples from the Vienna standard mean ocean water VSMOW (δ¹⁸O = 0 ‰, δ²H = 0 ‰) and Greenland Ice Sheet Precipitation GISP (δ¹⁸O = -24.76 ‰, δ²H = -189.5 ‰), as well as IAEA laboratory standards (IAEA 12, δ¹⁸O = -12.10 ‰, δ²H = -85.9 ‰; IAEA 13, δ¹⁸O = -33.35 ‰, δ²H = -257.2 ‰) and the domestic moscow University standard of fresh snow from the Garabashi glacier in the Cuacasus (δ¹⁸O = -15.60 ‰, δ²H = -110.0 ‰). The precision of the measurements was 0.1 ‰ for δ¹⁸O and 0.6 ‰ for δ²H.
DOI: 10.1594/pangaea.808674
title: Basic measurements of radiation at station Nauru Island (2005-01)

description: Version 3, 2013-03-10
DOI: 10.1594/pangaea.497613
title: Physical oceanography from BT during cruise U58GSXXXXXB_1956
DOI: 10.1594/pangaea.846480
title: Other measurements at 300 m from station Boulder (2014-09)
DOI: 10.1594/pangaea.806717
title: Ozone measurements from station Izaña (2013-01)
DOI: 10.1594/pangaea.823275
title: (Table 3) Trace elements at DSDP Leg 55 Holes

description: Empty cells = not determined. For Samples 55-431-1-1,80-87(c); 55-431-1*-1,103-105; 55-431A-2-2,45-47(a) and (b), trace-element data were not affected, because of the small quantity.
DOI: 10.1594/pangaea.887536
title: Radiosonde measurements from Neumayer Station (2017-03)

description: The meteorological observatory Neumayer typically launches one radiosonde per day around 12UTC. At least weekly the sonde has an ozone sensor attached. Sondes are released from the roof of the station building. The measurement interval of the raw data is typically 1s. Data is quality controlled: Erroneous data is removed (technical issues). Partial pressure ozone is manually validated for plausibility.
DOI: 10.1594/pangaea.818123
title: (Table 2) Chemical composition of gases in basalts from DSDP Leg 65 Holes

description: Basalts from different structural provinces in the ocean basins, such as mid-ocean ridges, island arcs, and oceanic plateaus, show marked differences in major and minor element composition stemming from differences in magma source. In addition, there are variations even within individual provinces, based on such processes as crystal fractionation, secondary alteration, and hydrothermal alteration. It is also known that hydrothermal processes can cause changes in the gas composition of submarine basalts. For example, Zolotarev et al. (1978) have established that hydrothermal alteration frequently causes an increase in the CO2 content of basalts. If the homogeneity in composition and concentration of organic gases in oceanic basalts is associated with degassing during epimagmatic alteration, it would be interesting to investigate the relative abundance of gas phases in young basalts from midoceanic ridges.This chapter deals with the distribution of organic gases and CO2 in young basalts recovered on Leg 65 from the Gulf of California. Our aim was to establish the relationship between gas composition and degree of alteration.
description: Empty cells mean not determined, &lt;0.01 & &lt;0.001 = traces.
description: Supplement to: Zolotarev, Boris P; Starobinets, I S; Voitov, G I (1983): Gases in basalts from the Gulf of California, Deep Sea Drilling Project Leg 65, Holes 482B, 482C, 482D, 482F, 483, 483B, 483C, and 485A. In: Lewis, BTR; Robinson, P; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 65, 667-672
DOI: 10.1594/pangaea.908481
title: (S2) Geochemical data for the CAA-Rivers Project Time Series at the Coppermine River, NU, collected from 2014-2016

description: Coppermine River sampling took place between two locations depending on seasonal site access either by boat, ATV, or from shore. The main sampling site was up river: 67.7633°N, -115.2538°E, and the secondary site was closer to the river mouth: 67.8173°N, -115.0765°E. When travel on the river was dangerous (ice break-up, freeze-up) samples were collected from a shoreline intake for the water plant adjacent to the secondary sampling site (67.8203°N, -115.0848°E).The sample collected on August 22, 2015 appears to have higher dissolved salt concentrations than usual for this river (in particular for Cl and Na). Strong winds required that this sampling event be carried out by ATV, so the sample was collected from shore near the primary site. Although this sample has been included in the presented analyses, it should be treated as potentially contaminated.
DOI: 10.1594/pangaea.830618
title: Section images from IODP Hole 338-C0002H

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.917729
title: δ¹⁸O, δ²H and deuterium excess values in snow from a snow patch in Vorkuta town

description: δ¹⁸O, δ²H and deuterium excess (dexc) values in snow from a snow patch in Vorkuta town (sampled December, 2018) and in the fresh snow (sampled December, 2005) during a single snowfall along a 300 km SW–NE transect (from 66.05 N, 60.366667 E to 67.05 N 65.333333 E).Hydrogen and oxygen isotope ratios (δ¹⁸O and δ²H) in ice and snow (sampled in 2003 and 2004) were measured in the Isotope Laboratory of the Vienna Arsenal Center (Prof. D. Rank, Dr W. Papesch and M. Körner). Analytical precision was ±0.1‰ for δ¹⁸O and ±1‰ for δ²H. Stable isotope ratios in ice and snow sampled in 2018 were analyzed in the stable isotope laboratory of the Geography Faculty of Lomonosov Moscow State University (Prof. Y.Vasil'chuk and Dr. N. Budantseva) using a Finnigan Delta-V Plus mass spectrometer applying equilibration techniques. International water standards (SMOW, GRESP and SLAP) were used for calibration. Analytical precision was ±0.4‰ for δ¹⁸O and ±1‰ for δ2H.
DOI: 10.1594/pangaea.484439
title: Hydrochemistry measured on water bottle samples at station SAVE2/71-1

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.890513
title: Age determination of Stordalen peat core
DOI: 10.1594/pangaea.717618
title: (Table 1) Lithology of DSDP Hole 24-237

description: Depth, sediment (m) is calculated from the depth below MSL, elevation: 1623 m
DOI: 10.1594/pangaea.910429
title: Other measurements at 10 m from station Eastern North Atlantic (2015-08)
DOI: 10.1594/pangaea.720209
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 90-593

description: Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline quartzP = Plagioclase feldsparK = Potassium feldsparLvo = Other volcanic lithicLvd = Devitrified vitric volcanic lithicLvv = Vitric volcanic lithicLvf = Volcanic lithic with felsitic textureLvmi = Volcanic lithic with microlitic textureLvl = Volcanic lithic with lathwork textureLvp = Pyroclastic volcanic lithicLmv = Metavolcanic lithicLmm = Polycrystalline mica lithicLmt = Quartz-mica tectonite lithicLma = Quartz-feldspar-mica aggregate lithicLmp = Phyllite lithicLsa = Argillite-shale lithicLsc = Sedimentary carbonate lithicLsch = sedimentary chert or cherty argillite lithicLsi = Siltstone sedimentary lithicM = Phyllosilicate mineralsD = Dense mineralsCarb = Carbonate mineralsBio = Bioclastic debris (siliceous and/or carbonate)Misc = Miscellaneous and unidentifiedQ = Total quartzose grainsL = Unstable lithic grainsLm = Metamorphic lithic grainsLv = Volcanic-hypabyssal (and volcaniclastic) lithic grainsLs = Sedimentary lithic grainsLvm = Volcanic-hypabyssal and metavolcanic lithic grainsLsm = Sedimentary and metasedimentary lithic grainsLst = Sedimentary and polycrystalline quartz grainsF = Total feldspar grainsQp = Polycrystalline quartz grainsQ = Qm + Qpw + QptQp = Qpw + QptL = Lm + Lv + LsLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpLm = Lmv + Lmm + Lmt + LmaLsm = Ls + Lmm + Lmt + LmaLvc = Lvf + Lvmi + LvlLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpF = P + KLs = Lsa + LscLvm = Lv + LmvLst = Ls + QpQFL%Q = 100Q/(Q + F + L)QFL%F = 100F/(Q + F + L)QFL%L = 100L/(Q + F + L)QmKP%Qm = 100Qm/(Qm + P + K)QmKP%P = 100P/(Qm + P + K)QmKP%K = 100K/(Qm + P + K)LvfLvmiLvl%Lvf = 100Lvf/LvcLvfLvmiLvl%Lvmi = 100Lmi/LvcLmLvLs%Lm = 100Lm/LLmLvLs%Lv = 100Lv/LLmLvLs%Ls = 100Ls/LQpLvmLsm%Qp = 100Qp/(L + Qp)QpLvmLsm%Lvm = 100Lvm/(L + Qp)QpLvmLsm%Lsm = 100Lsm/(L + Qp)LvfLvmiLvl%Lvl = 100Lvl/Lvc
DOI: 10.1594/pangaea.785836
title: Radiosonde measurements from station Izaña (2012-06)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.788821
title: Basic and other measurements of radiation at station Alert (2009-12)
DOI: 10.1594/pangaea.807955
title: Meteorological synoptical observations from station Tamanrasset (2012-11)
DOI: 10.1594/pangaea.890475
title: Geochemistry of E110_core1 peat core
DOI: 10.1594/pangaea.477145
title: Hydrochemistry measured on water bottle samples at station NPac_1974_RY_136E/4473

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.806830
title: Basic measurements of radiation at station Nauru Island (2002-08)

description: Version 3, 2013-02-07
DOI: 10.1594/pangaea.890218
title: Age determination of NW-BG_core2 peat core
DOI: 10.1594/pangaea.871093
title: Swath sonar multibeam bathymetry during HEINCKE cruise HE444 with links to raw data files of bathymetry and water column information

description: Data acquisition was performed using a KONGSBERG EM710 multibeam sonar system. Raw data are delivered within Simrad current multibeam vendor format. SIMRAD raw data can be processed e.g. with the software packages CARIS HIPS/SIPS, Caraibes or with the open source software package MB-System (http://www.ldeo.columbia.edu/res/pi/MB-System/).
DOI: 10.1594/pangaea.904997
title: Broadband radiation measurements (package 1) during the Arctic field campaign PASCAL in June 2017 (Balloon_Balu1_20170605_1706_1835)
DOI: 10.1594/pangaea.753126
title: (Table 1) Stable carbon and oxygen ratios and mineralogy of Cenozoic cements recovered during ODP Leg 112
DOI: 10.1594/pangaea.793197
title: Basic measurements of radiation at station Nauru Island (2000-01)

description: Version 3, 2012-10-25
DOI: 10.1594/pangaea.664402
title: Oceanography at CTD/bottle station IFREMER_1242
DOI: 10.1594/pangaea.908020
title: Mooring measurements from Eidsvåg, Norway, in April 2019

description: This data set contains sensor data from a mooring deployed at the positon 60.4439N, 5.3095E during a SEACRIFOG training workshop. The site is in Eidsvåg, which is a side fjord connected to the larger Byfjorden, off Bergen at the western part of Norway. The mooring was deployed at 3 April 2019 at 9:30 GMT, and retrieved at 5 April 2019 at 08:00 GMT. Ship for deployment was R/V Hans Brattstrom. Attached to the mooring were four instruments:- one AADI Seaguard (serial no. 1804) at approx 21 m depth (pressure measurements in datafile)- one RBR solo T temperature sensor (serial no. 200320) at approx. 33 m depth (12 m deeper than the AADI SeaGuard)- one RBR solo T temperature sensor (serial no. 200321) at approx. 48 m depth (27 m deeper than the AADI SeaGuard)- one SeaBird SBE-37 ctd (serial no. 15045) at approx. 56 m depth (pressure measurements in datafile)The sampling frequency was once every 30 minutes for all instruments. The salinity data has been corrected using discrete salinity samples analysed at a Portasal salinity instrument. The salinity correction was performed by subtracting a constant value which represented the difference between the salinity sensor and the discrete salinity sample at the largest depth. The prescision of the salinity data was 0.002.The dissolved oxygen data has been corrected using Winkler oxygen titration of discrete water samples. The oxygen correction was performed by subtracting a constant value which represented the difference between the oxygen sensor and the discrete oxygen sample at the largest depth. Prescision of the oxygen data was 0.66 umol/kg, accuracy can be determined by comparing uncorrected and corrected oxygen values in the file.
description: Gear ID 1: AADI_SeaGuard; Gear ID 2: RBR_soloT_200320; Gear ID 3: RBR_soloT_200321; Gear ID 4: SBE-37_ctd_15045
DOI: 10.1594/pangaea.955984
title: Changes in oxygen concentration in the outflow of FTR during the anoxic short-term incubation of North Sea sands
DOI: 10.1594/pangaea.663931
title: Oceanography at CTD/bottle station IFREMER_0772
DOI: 10.1594/pangaea.664264
title: Oceanography at CTD/bottle station IFREMER_1105
DOI: 10.1594/pangaea.955987
title: Changes of major parameters (Mn, Fe, P, NH4+, NO3-, DIC, pH, etc.) during the anoxic short-term incubation of North Sea sands
DOI: 10.1594/pangaea.793201
title: Basic measurements of radiation at station Nauru Island (2000-05)

description: Version 3, 2012-10-25
DOI: 10.1594/pangaea.956319
title: Determination of main and trace chemical constituents in manganese nodule samples from the South and North Pacific

description: Manganese nodule samples from the South and North Pacific were selected for the determination of their main and trace constituents. Results obtained by direct atomic-absorption determination of the elements in samples dissolved in 6 M hydrochloric acid (containing 2 % v/v of the hexoneisopropanol-HCl mixture). The following sensitivities for 1 % absorption are obtained: Mn = 0.10 ppm, Cu = 0.12 ppm, Co = 0.22 ppm. and Pb = 0.85 ppm. Uranium cocentration was determined by fluorimetry (Galvanek-Morrison fluorimeter, Mark V (Jarrel-Ash).
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.This dataset represents the digitized Table 3, pp. 89 of the related publication.
DOI: 10.1594/pangaea.751080
title: Meteorological observations during PANTER cruise from Curaçao to Boca Chica started at 1826-08-29
DOI: 10.1594/pangaea.955983
title: Changes in oxygen concentration in the outflow of FTR during the anoxic long-term incubation of North Sea sands
DOI: 10.1594/pangaea.856757
title: Annotated record of the detailed examination of Mn deposits from the H.M.S. Egeria, H.M.S. Fling Fish and H.M.S. Investigator expeditions in the Indian Ocean and Southern Seas

description: Captain Wharton, the Hydrographer of the Admiralty sent to the author a series of the deposit-samples collected in the Indian and Antarctic Oceans during the expeditions in 1887 of H.M.S. Flying Fish, H.M.S. Egeria and H.M.S. Investigator. These deposits were submitted to careful microscopical examination and chemical analysis.
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.
description: Supplement to: Murray, John (1889): On marine deposits in the Indian, Southern, and Antarctic oceans. Scottish Geographical Magazine, 5(8), 405-436
DOI: 10.1594/pangaea.916371
title: 1-Hz PPP displacements at GEONET station 0165 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.694851
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station FEBR-1999-S09

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore filters. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).
DOI: 10.1594/pangaea.720211
title: Ultra-violet measurements from station Desert Rock (2003-01)

description: Version 2, 2009-06-16. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-08.
DOI: 10.1594/pangaea.785532
title: Radiosonde measurements from station Tateno (2011-07)
DOI: 10.1594/pangaea.441527
title: (Table 2) Average major elements composition of smectites of sediment core CRP-2A
DOI: 10.1594/pangaea.895228
title: Middle Miocene benthic Nd isotopes of ODP Hole 130-806B
DOI: 10.1594/pangaea.750063
title: Meteorological observations during La Cantabria cruise from Montevideo to La Coruña started at 1771-11-21
DOI: 10.1594/pangaea.749823
title: Meteorological observations during INTREPID cruise from Bembridge to Carlisle Bay started at 1794-05-23
DOI: 10.1594/pangaea.916457
title: 1-Hz PPP displacements at GEONET station 0253 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.496284
title: Water temperature MBT profiles from cruise U90X089318M_1986