cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.837086
title: (Table 1) Carbon pools in different vegetation components in grazed and ungrazed plots near Ny-Ålesund, Spitzbergen

description: The carbon (C) sink strength of arctic tundra is under pressure from increasing populations of arctic breeding geese. In this study we examined how CO2 and CH4 fluxes, plant biomass and soil C responded to the removal of vertebrate herbivores in a high arctic wet moss meadow that has been intensively used by barnacle geese (Branta leucopsis) for ca. 20 years. We used 4 and 9 years old grazing exclosures to investigate the potential for recovery of ecosystem function during the growing season (July 2007). The results show greater above- and below-ground vascular plant biomass within the grazing exclosures with graminoid biomass being most responsive to the removal of herbivory whilst moss biomass remained unchanged. The changes in biomass switched the system from net emission to net uptake of CO2 (0.47 and -0.77 µmol/m**2/s in grazed and exclosure plots, respectively) during the growing season and doubled the C storage in live biomass. In contrast, the treatment had no impact on the CH4 fluxes, the total litter C pool or the soil C concentration. The rapid recovery of the above ground biomass and CO2 fluxes demonstrates the plasticity of this high arctic ecosystem in terms of response to changing herbivore pressure.
description: Based on C pool data collected at peak biomass in the end of July 2007. Data shown are for grazed (by barnacle geese (Branta leucopsis)) and exclosure plots. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
description: Supplement to: Sjögersten, Sofie; van der Wal, René; Loonen, Maarten J J E; Woodin, Sarah J (2011): Recovery of ecosystem carbon fluxes and storage from herbivory. Biogeochemistry, 106(3), 357-370
DOI: 10.1594/pangaea.610294
title: Underway pCO2 in the Atlantic Ocean of Santa Maria cruise 64SA20060315
DOI: 10.1594/pangaea.821635
title: (Table S1) In situ δ¹⁸O measurements in the basal areas of muricae from ODP Site 143-865

description: Sediment depth is given in mbsf. After ion microprobe measurements, the appearance and location of analysis pits were imaged by SEM. Oxygen isotope data from pits overlapping epoxy resin, cracks, cavities, inclusions, or areas of high porosities (ion yield less than 90% of that obtained in the nonporous standard) are considered as possibly compromised, and data from these measurements were not used for climate reconstruction. However, these measurements are listed in the table.
DOI: 10.1594/pangaea.917309
title: 1-Hz PPP displacements at GEONET station 1146 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.749967
title: Meteorological observations during King George III cruise from Gravesend to York Factory started at 1789-06-24
DOI: 10.1594/pangaea.873503
title: (Table 2-3, page 64) Bulk chemical composition of a Co-rich ferromanganese crust from the Dove Ridge

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.465115
title: Physical properties of sediment core MD03-2683G
DOI: 10.1594/pangaea.749585
title: Meteorological observations during HIND cruise from Plymouth to New York started at 1766-04-12
DOI: 10.1594/pangaea.804626
title: (Table 1) Paleomagnetic of ODP Site 136-842

description: Paleomagnetic studies on sediments recovered during Leg 136 have yielded a polarity reversal sequence that can be compared with the global magnetic reversal time scale to establish a sedimentation rate for Hole 842B. This sedimentation rate is substantially higher than that normally observed in the central Pacific basin probably as a result of the contribution of volcanic ash to the normal pelagic sources of sediment. The basalt samples from the oceanic crust at Site 843 have been used to determine a paleolatitude of 10.2°S for the 110±2 m.y.-old crust from this site. Detailed studies of the polarity transitions yielded few intermediate directions, but these few records provide support for the "Americas" transitional path observed at other continental and marine sites in Europe and North America.
description: Supplement to: Helsley, Charles E (1993): Paleomagnetic results from Leg 136. In: Wilkens, RH; Firth, J; Bender, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 136, 45-50
DOI: 10.1594/pangaea.904729
title: Table SM-4: Splice tie table for ODP Site 138-851

description: This is the splice tie table for Site 851 (originally preferred format for presenting the splice).Each row lists a tie point between consecutive cores, which together form the splice. The table starts with the topmost core and ends with the final core in the splice.TIE indicates where that the core is directly tied to the previous core. The revised m CCSF (revised metres core composite depth below sea floor) depth will be identical between cores at the location of the splice tie point.APPEND indicates where the core is appended to the previous core. The revised m CCSF (revised metres core composite depth below sea floor) depth may not be identical between cores at the location of the append point.
DOI: 10.1594/pangaea.681127
title: Meteorological synoptical observations from station Ny-Ålesund (1994-08)

description: On 2016-07-06 some corrections on the wind speed were made for this dataset. The old version is available at: ftp://ftp.bsrn.awi.de/nya/OldVersions_2016-07-06_oldSYNOPS/
DOI: 10.1594/pangaea.900575
title: Meteorological synoptical observations from station Fukuoka (2019-02)

description: Version 1
DOI: 10.1594/pangaea.767368
title: (Table 1) Boron analyses from ODP Sites 186-1150 and 186-1151

description: Interstitial pore waters from Ocean Drilling Program (ODP) Sites 1150 and 1151, both penetrating ca. 1200 m of sub-seafloor sediment from the upper Japan Trench forearc, were analyzed for B concentrations and d11B isotopes. B concentrations cover a wide range from 329 to 3920 µM (0.8-9.3* seawater) and vary isotopically from +20 to +46 per mil (relative to SRM 951). In general, B concentrations increase more or less steadily with depth. At both sites, the B enrichment and isotopic changes seem to be related to a deep fluid influence, possibly coupled with alteration of volcanic products. Silica diagenesis does not affect the B geochemistry of the waters, as is evident from intact diatom tests and high opal-A contents throughout the holes. The B enrichment is more pronounced at Site 1150 in the seismic portion of the forearc. Here, a large positive anomaly in d11B values is observed, which corresponds with abundant fracturing and two prominent shear zones. At about the same depth range at Site 1151, the d11B values show a negative shift, attesting to an enrichment in 10B in the fluid as a result of B desorption from clay due to burial and tectonic stress. We conclude that B release from clay minerals is the major contributor to pore fluid anomalies, and that fluid flow through permeable out-of-sequence thrust (like the shear zones at Site 1150) may be an efficient mechanism for B backflux from the forearc into the hydrosphere.
description: Sediment depth is given in mbsf. For Alkalinity, pH, Chloride, Magnesium and Sulphate see results from Shipborad analyses (Sacks et al., 2000) ODP Hole 186-1150A dataset: doi:10.1594/PANGAEA.256270), ODP Hole 186-1150B dataset: doi:10.1594/PANGAEA.256271, ODP Hole 186-1151A dataset: doi:10.1594/PANGAEA.256272 and ODP Hole 186-1151C dataset: doi:10.1594/PANGAEA.256273.
description: Supplement to: Deyhle, Annette; Kopf, Achim J (2002): Strong B enrichment and anomalous d11B in pore fluids from the Japan Trench forearc. Marine Geology, 183(1-4), 1-15
DOI: 10.1594/pangaea.770076
title: (Table 1) Hydrocarbon gas composition of sediment and gas hydrate collected in video-guided grabs from Chapopote

description: In the Campeche Knolls, in the southern Gulf of Mexico, lava-like flows of solidified asphalt cover more than 1 square kilometer of the rim of a dissected salt dome at a depth of 3000 meters below sea level. Chemosynthetic tubeworms and bivalves colonize the sea floor near the asphalt, which chilled and contracted after discharge. The site also includes oil seeps, gas hydrate deposits, locally anoxic sediments, and slabs of authigenic carbonate. Asphalt volcanism creates a habitat for chemosynthetic life that may be widespread at great depth in the Gulf of Mexico.
description: Gas hydrate concentrations (Conc.) are reported as parts per million by volume (ppmv) of hydrate gas. Sediment gas concentrations are reported as ppmv of interstitial water. Stable carbon isotopes (d13C) are reported as parts per thousand relative to Pee Dee Belemnite standard.
description: Supplement to: MacDonald, Ian R; Bohrmann, Gerhard; Escobar, E; Abegg, Friedrich; Blanchon, Paul; Blinova, Valentina N; Brueckmann, Warner; Drews, Manuela; Eisenhauer, Anton; Han, X; Heeschen, Katja U; Meier, Felix; Mortera-Gutierrez, Carlos; Naehr, T; Orcutt, B; Bernard, B; Brroks, J; de Farágo, M (2004): Asphalt volcanism and chemosynthetic life, Campache Knolls, Gulf of Mexico. Science, 304(5673), 999-1002
DOI: 10.1594/pangaea.496287
title: Water temperature MBT profiles from cruise U90X089321M_1986
DOI: 10.1594/pangaea.499401
title: Physical oceanography from BT during cruise U90XX07988B_1924
DOI: 10.1594/pangaea.928245
title: Stable oxygen isotopes of ODP Hole 122-761B
DOI: 10.1594/pangaea.904730
title: Table SM-5: Splice tie table for ODP Site 320-U1335

description: This is the splice tie table for Site U1335 (originally preferred format for presenting the splice).Each row lists a tie point between consecutive cores, which together form the splice. The table starts with the topmost core and ends with the final core in the splice.TIE indicates where that the core is directly tied to the previous core. The rmcd (revised metres composite depth) scale will be identical between cores at the location of the splice tie piont.
DOI: 10.1594/pangaea.681219
title: Meteorological synoptical observations from station Ny-Ålesund (2002-04)

description: On 2016-07-06 some corrections on the wind speed were made for this dataset. The old version is available at: ftp://ftp.bsrn.awi.de/nya/OldVersions_2016-07-06_oldSYNOPS/
DOI: 10.1594/pangaea.747388
title: Meteorological observations during ANDROMACHE cruise from Isle of Bec to Cádiz started at 1793-09-17
DOI: 10.1594/pangaea.711162
title: (Fig. 3h) Clay mineral content of sediment core JR104-GC374
DOI: 10.1594/pangaea.905383
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core Qipisarqo_Lake
DOI: 10.1594/pangaea.717871
title: Ultra-violet measurements from station Sioux Falls (2003-12)

description: 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 2017-02-03.
DOI: 10.1594/pangaea.751220
title: Meteorological observations during Piet Heijn cruise from Bramspunt to Bergen started at 1799-03-22
DOI: 10.1594/pangaea.859438
title: Geochemistry of two sediment cores and a reference site from the Orca Basin, northern Gulf of Mexico
DOI: 10.1594/pangaea.477576
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_OC_22S/66

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.707242
title: (Table 2) Oxygen and thorium isotope ratios, and flux data of ODP Hole 138-848B
DOI: 10.1594/pangaea.748540
title: Meteorological observations during DILIGENCIA cruise from Montevideo to La Coruña started at 1779-02-16
DOI: 10.1594/pangaea.497536
title: Physical oceanography from BT during cruise U58GS00111B_1969
DOI: 10.1594/pangaea.912358
title: Blowing snow detection derived from ceilometer measurements at Princess Elisabeth station (East Antarctica) - 2017

description: This dataset contains ceilometer data at the Princess Elisabeth station, East Antarctica (71°57'S - 23°21'E) for 2017.blowing snow code:1=blowing snow +cloud/precipitation2=blowing snow + clear sky3=absence blowing snow + cloud/precipitation4=absence of blowing snow + clear sky5=stormy weather (blowing snow is assumed)FOR DETAILS AND DATA AVAILABILITY, SEE : https://ees.kuleuven.be/hydrant/aerocloud/
DOI: 10.1594/pangaea.495772
title: Water temperature IBT profiles from cruise U90AI76062I_1976
DOI: 10.1594/pangaea.496400
title: Water temperature MBT profiles from cruise U90X121325M_1978
DOI: 10.1594/pangaea.498598
title: Physical oceanography from BT during cruise U90TC09760B_1985
DOI: 10.1594/pangaea.691192
title: Nutrient concentrations in water samples collected at Station MARCH-94-GN3619940280100560 in the Aegean Sea
DOI: 10.1594/pangaea.752786
title: Meteorological observations during Vrouwe Johanna Cores cruise from Axim to Paramaribo started at 1767-11-10
DOI: 10.1594/pangaea.692611
title: Photosynthetic primary production in the euphotic zone of the Aegean Sea at Station JUNE-94-GN3619940280200500
DOI: 10.1594/pangaea.807846
title: (Table 2) Details of laminated intervals of ODP Leg 158 holes

description: Scanning electron microscope (SEM)-based analyses of the laminated diatom oozes encountered during Leg 138 reveal three major laminae types. The first lamina type is composed of multiple layers of ~20-?m-thick diatom mats, which form laminae dominated by assemblages of the pennate diatom, Thalassiothrix longissima. More than one variety/subspecies of T. longissima occurs within these laminae (referred to as the T. longissima Group). The second lamina type is composed of a mixed-assemblage of several species of diatoms (centric and pennate varieties), calcareous nannofossils, and subordinate quantities of radiolarians, silicoflagellates and foraminifers. The third lamina type is dominated by an assemblage of nannofossils and minor amounts of those fossil components mentioned above. This last form of lamination is compositionally similar to the background sediment type, foraminifernannofossil ooze (F-NO). Two lamina associations occur within the laminated intervals; the first comprises alternations of T. longissima Group and mixed-assemblage laminae (average thickness is ~6 mm) and the second is composed of T. longissima and nannofossil-rich laminae (average thickness is ~3.5 mm). The arrangement of laminae probably originates from the deposition of multiple layers of 20-?m-thick mats from one mat-flux episode. The much thinner nannofossil-rich laminae are interpreted to represent periods of more ônormalö deposition between mat-flux episodes. The occurrence of several varieties/subspecies of T. longissima within individual mat layers is consistent with observations of Rhizosolenia diatom mats in the modern world ocean.
description: DEPTH, sediment is given in mbsf.
description: Supplement to: Pearce, Richard B; Kemp, Alan E S; Baldauf, Jack G; King, S C (1995): High-resolution sedimentology and micropaleontology of laminated diatomaceous sediments from the eastern Equatorial Pacific Ocean. In: Pisias, NG; Mayer, LA; Janecek, TR; Palmer-Julson, A; van Andel, TH (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 138, 647-663
DOI: 10.1594/pangaea.891627
title: Radiosonde measurements from station Payerne (2012-12)
DOI: 10.1594/pangaea.691087
title: Nutrient concentrations in water samples collected at Station DEC94-JAN95-GN3619940280400140 in the Aegean Sea
DOI: 10.1594/pangaea.808116
title: (Table 2) Radiolarian species datums and ages of ODP Site 138-844

description: DEPTH, sediment is given in mbsf.
DOI: 10.1594/pangaea.910526
title: Radiosonde measurements from station Bondville (2019-11)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.477544
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_OC_22S/120

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.499089
title: Physical oceanography from BT during cruise U90X008281B_1980
DOI: 10.1594/pangaea.690335
title: Radiosonde M9_R012 during METEOR cruise M9 on 1967-04-21 15:56h

description: Height of tropause 11430 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.900099
title: Sonic anemometer measurements during the Arctic field campaign PASCAL in June 2017 (Balloon_Sonic_20170609_0847_0927)
DOI: 10.1594/pangaea.752581
title: Meteorological observations during UNKNOWN-07 cruise from Soerabaja to Rotterdam started at 1850-11-05
DOI: 10.1594/pangaea.901788
title: Downward spectral solar irradiance as measured in different depths under sea ice (transmitted irradiance) at station ALERT2018_18_1

description: Measurements of transmitted solar radiation under sea ice have been performed on First-Year-Ice (FYI) and Multi-Year-Ice (MYI) during the ALERT2018 campaign (Multidisciplinary Arctic Program (MAP) - Last Ice) off Alert, Nunavut, Canada in the Lincoln Sea between 07 May and 23 May 2018. The radiation measurements have been performed with Ramses spectral radiometes (TriOS, Rastede, Germany). All data are given in full spectral resolution interpolated to 1.0 nm, and integrated over the entire wavelength range (broadband, total: 320 to 950 nm). The irradiance sensor (cos-collector) for energy budget calculations was installed on the ROV. All times are given in UTC.
DOI: 10.1594/pangaea.615989
title: Borehole temperature of Hole LD99-A05-4
DOI: 10.1594/pangaea.668245
title: Physical oceanography of CTD station 100 off Independencia Bay, 2002, Peru
DOI: 10.1594/pangaea.831248
title: Abundance of pteropods in waters of the Aegean Sea during LIA05
DOI: 10.1594/pangaea.695054
title: Concentrations of particulate organic carbon in water of the Ionian Sea at Station MARCH-2000-IRI45
DOI: 10.1594/pangaea.477546
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_OC_22S/122

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.674145
title: Radiosonde measurements from station De Aar (2003-12)
DOI: 10.1594/pangaea.872597
title: Meteorological measurements in Guatemala city, Guatemala from February 1856- December 1859 (gap 1858), digitized version

description: The meteorological measurements were sending it to foreign observatories to give international visibility to the school (Perez, 1897). The geomagnetic observations taken in the observatory from 1857 to 1859 have been recently revisited by Ribeiro et al. (2011). Pérez R. La Compañía de Jesús en Guatemala y Centro América después de su restauración. Valladolid. Imprenta Castellana. 1897/ Ribeiro P., Vaquero J.M., Trigo R.M. 2011. Geomagnetic records of Carrington's storm from Guatemala. Journal of atmospheric and Solar-Terrestrial Physics 73, 308-315./ Canudas A 1864. Tratado elemental de Física por el P. Antonnio Canudas de la Compañía de Jesus.Imprenta de Magriña y Subirana, Barcelona. 384pp.---The data of this dataset might have been revised during the review process. This might therefore be an old version. To be sure, please check the respective dataset at doi:10.1594/PANGAEA.871480
DOI: 10.1594/pangaea.816511
title: Chlorophyll a measured on water bottle samples during AEGAEO cruise LIA-10

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore. 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.872520
title: Meteorological measurements in Buenos Aires, Argentina from January- December 1805, digitized version

description: The observations started the 18th January. The observations were made 4 times a Day (6h, 12h, 18h, 24h). The instruments were in the Cerviño's room, the barometer and one thermometer inside and the other thermometer was outdoors oriented S-SO out of the solar radiation. An important tempest at 6th June is recorded.---The data of this dataset might have been revised during the review process. This might therefore be an old version. To be sure, please check the respective dataset at doi:10.1594/PANGAEA.871480
DOI: 10.1594/pangaea.497521
title: Physical oceanography from BT during cruise U58GJ01036B_1950
DOI: 10.1594/pangaea.747611
title: Meteorological observations during BEAVER cruise from to Dominica started at 1763-05-29
DOI: 10.1594/pangaea.784435
title: (Table T2) Oligocene-Miocene planktonic foraminifer datum levels from ODP Hole 184-1148A

description: DEPTH, sediment is given in mcd.
DOI: 10.1594/pangaea.674131
title: Radiosonde measurements from station De Aar (2002-09)
DOI: 10.1594/pangaea.872521
title: Meteorological measurements in Buenos Aires, Argentina from January- December 1822, digitized version

description: The 22nd September hail, 13th October Hurricane.---The data of this dataset might have been revised during the review process. This might therefore be an old version. To be sure, please check the respective dataset at doi:10.1594/PANGAEA.871480