cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.21258/1833705
title: Swiss national forest inventory - Result table No. 1190362
DOI: 10.21258/1833706
title: Swiss national forest inventory - Result table No. 1190367
DOI: 10.21258/1833707
title: Swiss national forest inventory - Result table No. 1190371
DOI: 10.21258/1833708
title: Swiss national forest inventory - Result table No. 1190373
DOI: 10.21258/1833709
title: Swiss national forest inventory - Result table No. 1190376
DOI: 10.21258/1833710
title: Swiss national forest inventory - Result table No. 1190381
DOI: 10.1594/pangaea.915425
title: Susceptibility of sediment core GeoB18529-2
DOI: 10.21258/1833678
title: Swiss national forest inventory - Result table No. 1195543
DOI: 10.21258/1833679
title: Swiss national forest inventory - Result table No. 1195727
DOI: 10.21258/1833680
title: Swiss national forest inventory - Result table No. 1195753
DOI: 10.21258/1833681
title: Swiss national forest inventory - Result table No. 1195852
DOI: 10.21258/1833682
title: Swiss national forest inventory - Result table No. 1192712
DOI: 10.21258/1833683
title: Swiss national forest inventory - Result table No. 1192857
DOI: 10.21258/1833684
title: Swiss national forest inventory - Result table No. 1192928
DOI: 10.21258/1833685
title: Swiss national forest inventory - Result table No. 1193039
DOI: 10.21258/1833686
title: Swiss national forest inventory - Result table No. 1193138
DOI: 10.21258/1833687
title: Swiss national forest inventory - Result table No. 1193155
DOI: 10.21258/1833688
title: Swiss national forest inventory - Result table No. 1193160
DOI: 10.21258/1833689
title: Swiss national forest inventory - Result table No. 1193246
DOI: 10.21258/1833690
title: Swiss national forest inventory - Result table No. 1193392
DOI: 10.21258/1833691
title: Swiss national forest inventory - Result table No. 1193597
DOI: 10.21258/1833692
title: Swiss national forest inventory - Result table No. 1193707
DOI: 10.21258/1833693
title: Swiss national forest inventory - Result table No. 1193714
DOI: 10.21258/1833694
title: Swiss national forest inventory - Result table No. 1190244
DOI: 10.1594/pangaea.904636
title: Magnetic susceptibility of the late Eocene-early Oligocene interval, southwestern Neotethys margin (northeastern Tunisia)
DOI: 10.1594/pangaea.915573
title: Susceptibility values of high resolution magnetic susceptibility record of the (penultimate and) last glacial cycles at the Süttő loess section, in Hungary in 2008

description: 0.026 mean
DOI: 10.21258/1833662
title: Swiss national forest inventory - Result table No. 1202302
DOI: 10.21258/1833663
title: Swiss national forest inventory - Result table No. 1202362
DOI: 10.21258/1833664
title: Swiss national forest inventory - Result table No. 1202807
DOI: 10.21258/1833665
title: Swiss national forest inventory - Result table No. 1202877
DOI: 10.21258/1833666
title: Swiss national forest inventory - Result table No. 1203159
DOI: 10.21258/1833667
title: Swiss national forest inventory - Result table No. 1203181
DOI: 10.21258/1833668
title: Swiss national forest inventory - Result table No. 1203190
DOI: 10.21258/1833669
title: Swiss national forest inventory - Result table No. 1203200
DOI: 10.21258/1833670
title: Swiss national forest inventory - Result table No. 1194976
DOI: 10.21258/1833671
title: Swiss national forest inventory - Result table No. 1195322
DOI: 10.21258/1833672
title: Swiss national forest inventory - Result table No. 1195368
DOI: 10.21258/1833673
title: Swiss national forest inventory - Result table No. 1195441
DOI: 10.21258/1833674
title: Swiss national forest inventory - Result table No. 1195459
DOI: 10.21258/1833675
title: Swiss national forest inventory - Result table No. 1195470
DOI: 10.21258/1833676
title: Swiss national forest inventory - Result table No. 1195518
DOI: 10.21258/1833677
title: Swiss national forest inventory - Result table No. 1195524
DOI: 10.21258/1833645
title: Swiss national forest inventory - Result table No. 1200253
DOI: 10.21258/1833646
title: Swiss national forest inventory - Result table No. 1200254
DOI: 10.21258/1833647
title: Swiss national forest inventory - Result table No. 1200264
DOI: 10.21258/1833648
title: Swiss national forest inventory - Result table No. 1200267
DOI: 10.21258/1833649
title: Swiss national forest inventory - Result table No. 1200387
DOI: 10.21258/1833650
title: Swiss national forest inventory - Result table No. 1200603
DOI: 10.21258/1833651
title: Swiss national forest inventory - Result table No. 1200843
DOI: 10.21258/1833652
title: Swiss national forest inventory - Result table No. 1200918
DOI: 10.21258/1833653
title: Swiss national forest inventory - Result table No. 1199634
DOI: 10.21258/1833654
title: Swiss national forest inventory - Result table No. 1199648
DOI: 10.21258/1833655
title: Swiss national forest inventory - Result table No. 1199762
DOI: 10.21258/1833656
title: Swiss national forest inventory - Result table No. 1199808
DOI: 10.21258/1833657
title: Swiss national forest inventory - Result table No. 1199908
DOI: 10.21258/1833658
title: Swiss national forest inventory - Result table No. 1199934
DOI: 10.21258/1833659
title: Swiss national forest inventory - Result table No. 1202236
DOI: 10.21258/1833660
title: Swiss national forest inventory - Result table No. 1202272
DOI: 10.21258/1833661
title: Swiss national forest inventory - Result table No. 1202295
DOI: 10.1594/pangaea.915439
title: Susceptibility of sediment core GeoB18557-2
DOI: 10.21258/1833633
title: Swiss national forest inventory - Result table No. 1206544
DOI: 10.21258/1833634
title: Swiss national forest inventory - Result table No. 1206550
DOI: 10.21258/1833635
title: Swiss national forest inventory - Result table No. 1206551
DOI: 10.21258/1833636
title: Swiss national forest inventory - Result table No. 1206567
DOI: 10.21258/1833637
title: Swiss national forest inventory - Result table No. 1206568
DOI: 10.21258/1833638
title: Swiss national forest inventory - Result table No. 1199951
DOI: 10.21258/1833639
title: Swiss national forest inventory - Result table No. 1200004
DOI: 10.21258/1833640
title: Swiss national forest inventory - Result table No. 1200010
DOI: 10.21258/1833641
title: Swiss national forest inventory - Result table No. 1200065
DOI: 10.21258/1833642
title: Swiss national forest inventory - Result table No. 1200107
DOI: 10.21258/1833643
title: Swiss national forest inventory - Result table No. 1200138
DOI: 10.21258/1833644
title: Swiss national forest inventory - Result table No. 1200241
DOI: 10.1594/pangaea.915426
title: Susceptibility of sediment core GeoB18530-1
DOI: 10.1594/pangaea.915441
title: Susceptibility of sediment core GeoB18559-2
DOI: 10.21258/1833629
title: Swiss national forest inventory - Result table No. 1206532
DOI: 10.21258/1833630
title: Swiss national forest inventory - Result table No. 1206537
DOI: 10.21258/1833631
title: Swiss national forest inventory - Result table No. 1206541
DOI: 10.21258/1833632
title: Swiss national forest inventory - Result table No. 1206542
DOI: 10.1594/pangaea.915430
title: Susceptibility of sediment core GeoB18534-1
DOI: 10.1594/pangaea.915427
title: Susceptibility of sediment core GeoB18531-1
DOI: 10.1594/pangaea.885413
title: Time series of hydrographic, chemical and primary production variables for a shelf station off A Coruña (NW Spain): 1989-2016

description: Water column discrete observations of temperature, salinity, density, irradiance, dissolved nutrients (nitrate, nitrite, phosphate, ammonium, silicate), oxygen, chlorophyll-a, primary production (carbon uptake) rates, and particulate organic carbon and nitrogen (NW Spain) from samples collected monthly at a shelf station off A Coruña between 1989 and 2016.These series are part of the long-term observational project RADIALES (Instituto Español de Oceanografía, IEO, Spain).
description: Method comment:1) Chla: filtration (Millipore cellulose acetate 0.8 µm pore-size until 1992; Whatman GF/F filters from 10992 onwards), extraction in 90% acetone overnight (-20°C) and measured fluorometrically (until 2000) or espectrofluorometrically (from 2000 onwards). Intercallibration adjustments between methods were made to ensure the compatibility of the series for the entire sampling period. References: Parsons et al. 1984; Neveux and Panouse 1987.2) PP: 14C-bicarbonate uptake.in situ-simulated incubations for 2h at noon. Reference: Bode et al. (2011).3) POC, PON, C:N: Filtration (Whatman GF/C filters until 1996; GF/F from 1996 onwards), drying (60°C) and combustion in elemental analyzer (Parsons et al. 1984)
description: Supplement to: Bode, Antonio; Álvarez, Marta; Ruiz-Villarreal, Manuel; Varela, Marta M (2019): Changes in phytoplankton production and upwelling intensity off A Coruña (NW Spain) for the last 28 years. Ocean Dynamics, 69(7), 861-873
DOI: 10.1594/pangaea.915429
title: Susceptibility of sediment core GeoB18533-2
DOI: 10.1594/pangaea.901409
title: Magnetic susceptibility in sediments of the Yaodian section from the Gansu Group, China
DOI: 10.1594/pangaea.901408
title: Rubidium and Strontium concentration in sediments of the Yaodian section from the Gansu Group, China
DOI: 10.1594/pangaea.946680
title: Video footage of the benthos and accompanying oceanographic CTD data recorded along a transect at station 37-10 of RV Meteor cruise M179/2 in the Paso Goree (Tierra del Fuego, Chile)

description: A custom-built observation frame (ROVOS) based on Ocean Module V8Sii ROV (Remotely Operated Vehicle) technology was launched from RV Meteor and towed along a 183 m transect in the Goree Passage, in a depth of 32 m. The shallow seabed is partly covered by algae and inhabited by crustaceans.The instrument was equipped with three cameras with different perspectives: one HD camera (Kongsberg oe14-502, 720p50) pointed isometrically forward at an angle of 22.5° to the horizon, the second 4k camera (SubC Imaging Mk6, 2160p25) was oriented downward and an observation camera (Bowtech L3C-650-L, 240p24) provided a low-resolution view forward. Environmental data was recorded with a CTD (RBR Maestro), which included sensors for chlorophyll a, turbidity, oxygen, pH and PAR in addition to standard instruments for conductivity, temperature and pressure. Additional CTD data are available from water profiles (Schwalfenberg, in preparation). The position of the ROVOS was recorded with the ship's own Posidonia USBL. The global orientation with respect to magnetic north was determined with an internal IMU device. To determine the true image scale on the high-resolution footage, a series of reference lasers indicating 10 cm were used in addition to an altimeter (Tritech) providing acoustically measured heights from the SubC camera to the seabed (see metadata).
DOI: 10.1594/pangaea.950707
title: Raw data of two lake sediment cores from southern Norway to reconstruct the frequency of palaeo floods

description: The data is from two separate sediment cores (LYP118 and LYG118) retrieved in November 2018 from the same coring location in Lake Lygne, southern Norway. LYP118 was retrieved using a piston corer equipped with a 6 m PCV-tube, whereas LYG118 was retrieved using a a UWITEC gravity corer equipped with a 2 m plastic tube. The purpose was to reconstruct palaeo floods from the Lygna river system by identifying flood layers in the sediment record. The sediment cores were stored in a refrigerated room (4 degrees C) prior to analysis. The attached data includes continuous magnetic susceptibility (MS) data measured at 0.2 cm intervals and continuous x-ray fluorescence (XRF) data measured at 0.05 cm intervals. Additionally, there are three images from a CT-scan, highlighting layers of low (0-5th percentile) and high (90-100th percentile) density. The grainsize, dry bulk density (DBD), and loss-on-ignition (LOI) data are from 1 cm samples collected at specific depth intervals (see column I for depth interval).
DOI: 10.1594/pangaea.946682
title: Video footage of the benthos and accompanying oceanographic CTD data recorded along a transect at station 41-12 of RV Meteor cruise M179/2 in the Boca de la Bahia Yendegaia (Tierra del Fuego, Chile)

description: A custom-built observation frame (ROVOS) based on Ocean Module V8Sii ROV (Remotely Operated Vehicle) technology was launched from RV Meteor and towed along a 211 m transect in the mouth of the Yendegaia Bay, in a depth of 298 m. The barren and muddy sea floor is covered with brittle stars, occasional drop stones provide a substrate for gorgonians and other sessile organisms.The instrument was equipped with three cameras with different perspectives: one HD camera (Kongsberg oe14-502, 720p50) pointed isometrically forward at an angle of 22.5° to the horizon, the second 4k camera (SubC Imaging Mk6, 2160p25) was oriented downward and an observation camera (Bowtech L3C-650-L, 240p24) provided a low-resolution view forward. Environmental data was recorded with a CTD (RBR Maestro), which included sensors for chlorophyll a, turbidity, oxygen, pH and PAR in addition to standard instruments for conductivity, temperature and pressure. Additional CTD data are available from water profiles (Schwalfenberg, in preparation). The position of the ROVOS was recorded with the ship's own Posidonia USBL. The global orientation with respect to magnetic north was determined with an internal IMU device. To determine the true image scale on the high-resolution footage, a series of reference lasers indicating 10 cm were used in addition to an altimeter (Tritech) providing acoustically measured heights from the SubC camera to the seabed (see metadata).
DOI: 10.1594/pangaea.946685
title: Video footage of the benthos and accompanying oceanographic CTD data recorded along a transect at station 44-11 of RV Meteor cruise M179/2 in the Fiordo Garibaldi Sur (Tierra del Fuego, Chile)

description: A custom-built observation frame (ROVOS) based on Ocean Module V8Sii ROV (Remotely Operated Vehicle) technology was launched from RV Meteor and towed along a 118 m transect in the southern part of the Garibaldi Fjord, in a depth of 92 m. The extreme barren sea floor is only home to only very few crustaceans.The instrument was equipped with three cameras with different perspectives: one HD camera (Kongsberg oe14-502, 720p50) pointed isometrically forward at an angle of 22.5° to the horizon, the second 4k camera (SubC Imaging Mk6, 2160p25) was oriented downward and an observation camera (Bowtech L3C-650-L, 240p24) provided a low-resolution view forward. Environmental data was recorded with a CTD (RBR Maestro), which included sensors for chlorophyll a, turbidity, oxygen, pH and PAR in addition to standard instruments for conductivity, temperature and pressure. Additional CTD data are available from water profiles (Schwalfenberg, in preparation). The position of the ROVOS was recorded with the ship's own Posidonia USBL. The global orientation with respect to magnetic north was determined with an internal IMU device. To determine the true image scale on the high-resolution footage, a series of reference lasers indicating 10 cm were used in addition to an altimeter (Tritech) providing acoustically measured heights from the SubC camera to the seabed (see metadata).
DOI: 10.1594/pangaea.950940
title: Magnetic susceptibility of sediment core LV53-27 (Sea of Japan, 2010)
DOI: 10.1594/pangaea.915436
title: Susceptibility of sediment core GeoB18554-1
DOI: 10.1594/pangaea.915434
title: Susceptibility of sediment core GeoB18552-1
DOI: 10.1594/pangaea.938205
title: Pedogenic carbonate carbon isotope determination from the Jiaxian Section on the Chinese Loess Plateau
DOI: 10.1594/pangaea.937813
title: Geochemical, sedimentological and micropaleontological data of the LAR sediment core

description: Bulk organic geochemistry, stable carbon isotopes, biogenic opal, calcium carbonate, geometric mean grain size, C37 alkenones, and freshwater vs. marine diatoms analyzed at a 10 to 20 cm interval.
DOI: 10.1594/pangaea.937817
title: Density data of the LAR sediment core

description: Wet and dry bulk density were measured on 1 cm thick slices (2.9 ± 0.7 cm3) every 20 cm.
DOI: 10.1594/pangaea.937818
title: Magnetic susceptibility of the LAR sediment core

description: Continuous high-resolution logging of magnetic susceptibility was accomplished using a Bartington MS2E spot sensor integrated into an automatic logging system. Measurements were performed on the split cores in steps of 1 mm with drift correction every 10 mm using readings in air. The gravity and piston cores were correlated using the magnetic susceptibility data, resulting in a composite core length of 9.20 m.
DOI: 10.1594/pangaea.937820
title: Fractions of lithogenic particles &gt;63 µm and &gt;150 µm of the LAR sediment core

description: The lithogenic fractions &gt;63 µm and &gt;150 µm were separated through wet-sieving. Five (30.5 – 680.5 cm) or 10 g (680.5 – 910.5 cm) of freeze-dried sediment was used for analysis. Organic matter was removed through loss-on-ignition by heating the samples in a muffle furnace at 750 °C for four hours. Inorganic carbon and biogenic silica were removed with acetic acid (5 mL, 100%) and boiling NaOH (5 mL, 2N), respectively. Results are presented in dry weight percentages.
DOI: 10.1594/pangaea.937821
title: Mean ages calculated by the bayesian age-depth model

description: The age model of the LAR sediment core was produced with the BACON 2.4.3 software, using 11 radiocarbon ages. The table contains the mean age of the sediment at a 1mm resolution.
DOI: 10.1594/pangaea.915582
title: Susceptibility values of high resolution magnetic susceptibility record of the (penultimate and) last glacial cycles at the Süttő loess section, in Hungary 2009

description: 0.026 mean value
DOI: 10.1594/pangaea.938206
title: Occluded organic matter carbon isotope from the Jiaxian Section on the Chinese Loess Plateau
DOI: 10.1594/pangaea.938207
title: Magnetic susceptibility (Chi) determination from the Jiaxian Section on the Chinese Loess Plateau
DOI: 10.1594/pangaea.938210
title: Age model calibration from the Jiaxian Section on the Chinese Loess Plateau
DOI: 10.1594/pangaea.915431
title: Susceptibility of sediment core GeoB18549-2
DOI: 10.1594/pangaea.932448
title: Integrated Stratigraphy of the Middle-Late Eocene Souar Formation (Tunisia): Implications for the Expression of the Middle Eocene Climatic Optimum (MECO) in the SW Neo-Tethys

description: The Middle Late Eocene relatively poorly known from the southwestern Neo-Tethys settings since no integrated study is presented so far. The Souar section (604 m, 36°13'27.07N, 10° 1'23.77E) from the Tunisian dorsale (Zaghouan, Tunisia) provide the needed stratigraphic, chronological, and paleoenvironmental constraints for a reference section in the southern Neo-Tethys. We generate new high-resolution biostratigraphic, magnetic susceptibility, stable isotope and X-ray fluorescence (XRF) records spanning the Lutetian to lower Priabonian (~36.7 to 45.8 Ma). Quantitative calcareous microfossil has been performed (94 samples, ~6 m resolution) to identify the major biostratigraphic horizons (Base, base common, top, and top common) following the work of Agnini et al., 2014. Calcareous nannofossils zones extends from CNE9 to CNE18. The high-quality XRF and XRD records highlight the potential enhanced biosiliceous productivity during the lower Bartonian. This indicates the development of upwelling zone causing the observed drastic reduce of in situ calcareous nannoplankton and carbonate productivity. A correlation between the δ13Corg of the Souar section and other published reference sections (Pacific and Neo-Tethys) suggests the identification of the δ13C pre-MECO local maximum at ~40.5 Ma, of the δ13C MECO minimum at ~40 Ma, as well as a potential δ13C maximum at ~37.4 Ma. The Bartonian-Priabonian boundary is placed at the base of Reticulofenestra erbae (37.89 Ma) and coincides with major variations in calcareous nannofossil abundance, calcium carbonate content, and magnetic susceptibility indicating profound changes in hemipelagic carbonate production and the source of siliciclastic material, likely related to the late Eocene climate change and palaeoceanographic restriction of the Neo-Tethys.
DOI: 10.1594/pangaea.919985
title: Photospectrometic down-core scanning profiles of sediment cores from the East Frisian Wadden Sea, Germany
DOI: 10.1594/pangaea.969092
title: Isothermal remanent magnetization (IRM) gradient of Palouse loess at site CLY-2, eastern Washington, USA

description: These data are from samples gathered in 2016 from the CLY-2 site in eastern Washington, USA (Location: 46.3131, -118.4874, WGS84). The CLY-2 is a roadcut exposing a vertical face of the Palouse loess containing carbonate paleosol horizons and tephras. The samples were collected from a set of three stepped trenches into the roadcut about 10-20 m apart. Each trench was excavated to a depth of about a meter to expose a fresh surface; the final ~10 cm was excavated with non-ferrous digging tools. Other magnetic properties were measured at Western Washington University's Pacific Northwest Paleomagnetism Laboratory. To make isothermal remanent magnetization (IRM) gradient acquisition curves, we loaded a subset of sample pots into gel capsules and measured the samples' response to a magnetic field in a Princeton Micromag 3900 vibrating sample magnetometer, which provided fields up to 2.2 tesla. To detect the presence of high-coercivity components such as goethite, we subjected a subset of samples to higher fields (stepwise up to 5 tesla), using an ASC Scientific Model IM-10-30 Impulse Magnetizer, and measured the IRM in a liquid He-cooled, 3-axis superconducting magnetometer (2G Enterprises Model 755) with a sensitivity of 0.001 mA/m, in a field-free room, demagnetizing the sample between measurements.
DOI: 10.1594/pangaea.946679
title: Video footage of the benthos and accompanying oceanographic CTD data recorded along a transect at station 23-8 of RV Meteor cruise M179/2 in the Canal Beagle / Fiordo Garibaldi (Tierra del Fuego, Chile)

description: A custom-built observation frame (ROVOS) based on Ocean Module V8Sii ROV (Remotely Operated Vehicle) technology was launched from RV Meteor and towed along a 207 m transect in the Beagle Channel in front of the Garibaldi Fjord, in a depth of 193 m. The mainly muddy seabed is home to only very few sessile sea cucumbers and brittle stars.The instrument was equipped with three cameras with different perspectives: one HD camera (Kongsberg oe14-502, 720p50) pointed isometrically forward at an angle of 22.5° to the horizon, the second 4k camera (SubC Imaging Mk6, 2160p25) was oriented downward and an observation camera (Bowtech L3C-650-L, 240p24) provided a low-resolution view forward. Environmental data was recorded with a CTD (RBR Maestro), which included sensors for chlorophyll a, turbidity, oxygen, pH and PAR in addition to standard instruments for conductivity, temperature and pressure. Additional CTD data are available from water profiles (Schwalfenberg, in preparation). The position of the ROVOS was recorded with the ship's own Posidonia USBL. The global orientation with respect to magnetic north was determined with an internal IMU device. To determine the true image scale on the high-resolution footage, a series of reference lasers indicating 10 cm were used in addition to an altimeter (Tritech) providing acoustically measured heights from the SubC camera to the seabed (see metadata).