cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.822486
title: Meteorological measurements in the upper air at station Mys Zhelania, 1939-08-17 to 1940-05-31, ERA-CLIM ID 4744
DOI: 10.1594/pangaea.875868
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 94 (Holes 608, 609, 610A, 610B, 611)

description: Leg 94 represents the last of four transects of sites set up by the Ocean Paleoenvironment Panel to examine climatic and oceanographic changes in the Pacific and Atlantic oceans. During this leg, a transect of six holes aligned roughly in a south-southwest/north-northeast direction were drilled in the North Atlantic from 37° to 53°N. The principal objective of this transect was to document the magnitude and spectral character of the surface-ocean response to high-latitude climatic change in the northern hemisphere during the Neogene.
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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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.719629
title: Other measurements at 10 m from station Desert Rock (2003-11)
DOI: 10.1594/pangaea.926863
title: XRF-derived elemental intensities and ratios from IODP Site 353-U1443
DOI: 10.1594/pangaea.719911
title: Other measurements at 10 m from station Desert Rock (2009-04)
DOI: 10.1594/pangaea.927134
title: Light intensity time series from 16 locations in Løgstør Bredning, Limfjorden, Denmark, at 3 m above seabed, 7-March-2017

description: Field studies were conducted in two different areas of the Limfjorden, in Lovns Bredning (26th February to 4th March 2017) and in Løgstør Bredning (6-10th March 2017). In each sampling area, 16 fixed-position moorings were deployed in two circular sensor arrays around a mussel dredging area to investigate possible effects of dredging related sediment plumes (Pastor et al, 2020). The inner array (stations 1 - 8) had a diameter of 200 m and the outer array (stations 9 - 16) was set up with a diameter of 600 m. Integrated temperature and light loggers (HOBO Pendant Temperature/Light 64K Data Logger) were mounted on each mooring in the two circular arrays at three different water depths (0.5, 1.5 and 3.0 m above seabed). The 48 loggers (3 depths and 16 stations) were deployed in each area over a period of four days and light intensity time series were collected with a sampling interval of 30 seconds. Five loggers in the Lovns area did not provide any data due to technical problems (two near-surface loggers and three loggers at 1.5 m above the seabed). However, only one bottom logger at Løgstør Bredning failed to provide data. Each time series was filtered using a 3-minute moving average for removing the largest outliers, but retaining sharp changes in light intensity associated with short-lived sediment plumes caused by experimental mussel dredging.
DOI: 10.1594/pangaea.927136
title: Light intensity time series from 16 locations in Løgstør Bredning, Limfjorden, Denmark, at 1.5 m above seabed, 8-March-2017

description: Field studies were conducted in two different areas of the Limfjorden, in Lovns Bredning (26th February to 4th March 2017) and in Løgstør Bredning (6-10th March 2017). In each sampling area, 16 fixed-position moorings were deployed in two circular sensor arrays around a mussel dredging area to investigate possible effects of dredging related sediment plumes (Pastor et al, 2020). The inner array (stations 1 - 8) had a diameter of 200 m and the outer array (stations 9 - 16) was set up with a diameter of 600 m. Integrated temperature and light loggers (HOBO Pendant Temperature/Light 64K Data Logger) were mounted on each mooring in the two circular arrays at three different water depths (0.5, 1.5 and 3.0 m above seabed). The 48 loggers (3 depths and 16 stations) were deployed in each area over a period of four days and light intensity time series were collected with a sampling interval of 30 seconds. Five loggers in the Lovns area did not provide any data due to technical problems (two near-surface loggers and three loggers at 1.5 m above the seabed). However, only one bottom logger at Løgstør Bredning failed to provide data. Each time series was filtered using a 3-minute moving average for removing the largest outliers, but retaining sharp changes in light intensity associated with short-lived sediment plumes caused by experimental mussel dredging.
DOI: 10.1594/pangaea.822512
title: Meteorological measurements in the upper air at station Mys Zhelania, 1948-01-02 to 1948-06-30, ERA-CLIM ID 4770
DOI: 10.1594/pangaea.669528
title: Horizon at station Xianghe
DOI: 10.1594/pangaea.869271
title: Radiosonde measurements from station Lindenberg (2008-09)
DOI: 10.1594/pangaea.822495
title: Meteorological measurements in the upper air at station Uelen, 1944-08-03 to 1945-04-11, ERA-CLIM ID 4753
DOI: 10.1594/pangaea.822504
title: Meteorological measurements in the upper air at station Ostrov Dikson, 1946-01-03 to 1947-12-31, ERA-CLIM ID 4762
DOI: 10.1594/pangaea.822508
title: Meteorological measurements in the upper air at station Buhta Tihaya, 1947-12-31 to 1948-06-29, ERA-CLIM ID 4766
DOI: 10.1594/pangaea.775410
title: Headspace-gas measurements from IODP Hole 331-C0013B

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.666862
title: Rare-earth element concentration of anhydrite vein separated from ODP Site 1188 (Table 2)

description: Ocean Drilling Program (ODP) leg 193 successfully drilled four deep holes (126 to 386 m) into basement underlying the active dacite-hosted Pacmanus hydrothermal field in the eastern Manus Basin. Anhydrite is abundant in the drill core material, filling veins and vesicles, cementing breccias, and occasionally replacing igneous material. We report rare-earth element (REE) contents of anhydrite from a site of diffuse venting (Site 1188) which show extreme variability, in terms of both absolute concentrations (e.g., 0.08–28.3 ppm Nd) and pattern shape (LaN/SmN=0.08–3.78, SmN/YbN=0.48–23.1, Eu/Eu*=0.59–6.1). The range of REE patterns in anhydrite includes enrichments in the middle and heavy REEs and variable Eu anomalies. The patterns differ markedly from those of anhydrite recovered during ODP Leg 158 from the TAG hydrothermal system at the Mid-Atlantic Ridge which display uniform LREE-enriched patterns with positive Eu anomalies, very similar to TAG vent fluid patterns. As the system is active, the host-rock composition is uniform, and the anhydrite veins appear to relate to the same hydrothermal stage, we can rule out predominant host-rock and transport control. Instead, we propose that the variation in REE content reflects waxing and waning input of magmatic volatiles (HF, SO2) and variable complexation of REEs in the fluids. REE speciation calculations suggest that increased fluoride and possibly sulfate concentrations at Pacmanus may affect REE complexation in fluids, whereas at TAG only chloride and hydroxide complexes play a significant role. The majority of the anhydrites do not show positive Eu anomalies, suggesting that the fluids were more oxidizing than in typical mid-ocean ridge hydrothermal systems. We use other hydrothermal fluids from the Manus Basin (Vienna Woods and Desmos), which bracket the Pacmanus fluids in terms of acidity and ligand concentrations, to examine the dependence of REE complexation on fluid composition. Geochemical modeling reveals that under the prevailing conditions at Pacmanus (pH=3.5, T=250–300 °C), Eu oxidation state and the relative importance of fluoride versus chloride complexing are very sensitive to small variations in oxygen fugacity, temperature, and pH. Patterns with extreme mid-REE enrichment may reflect speciation effects (free-ion abundance) coupled with crystal chemical control. We conclude that the great variability in REE concentrations and pattern shape is likely due to variable fluid composition and REE complexation in the fluids.
description: Supplement to: Bach, Wolfgang; Roberts, Stephen; Vanko, David A; Binns, Raymond A; Yeats, Chris J; Craddock, Paul R; Humphris, Susan E (2003): Controls of fluid chemistry and complexation on rare earth element contents of anhydrite from the PACMANUS subseafloor hydrothermal system, Manus Basin, Papua New Guinea. Mineralium Deposita, 38(8), 916-935
DOI: 10.1594/pangaea.822501
title: Meteorological measurements in the upper air at station Mys Shmidta, 1946-08-02 to 1947-12-28, ERA-CLIM ID 4759
DOI: 10.1594/pangaea.822502
title: Meteorological measurements in the upper air at station Mys Zhelania, 1946-01-02 to 1947-12-30, ERA-CLIM ID 4760
DOI: 10.1594/pangaea.826278
title: Pass-through measurements of magnetic susceptibility from IODP Hole 330-U1372A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.618847
title: Water temperature profile LD99-CR19b
DOI: 10.1594/pangaea.876402
title: Other measurements at 10 m from station Desert Rock (2015-07)
DOI: 10.1594/pangaea.822510
title: Meteorological measurements in the upper air at station Mys Cheliuskin, 1948-06-04 to 1948-06-29, ERA-CLIM ID 4768
DOI: 10.1594/pangaea.925269
title: Pollen content of profile No 84/41 of gravel pit Northeim_PitA

description: The pollen spectra belong to Pollen zone III or /IV (late Younger Dryas/Early Preboreal).Radiocarbon ages:lens 41a: wood of Salix, Hv-13278, 9890+/-100 BP; calibrated: 9462+/-163 calBClens 41b: wood of Populus, Hv-13277, 9985+/-175 BP; calibrated: 9642+/-294 calBC
DOI: 10.1594/pangaea.822515
title: Meteorological measurements in the upper air at station Amderma, 1949-07-10 to 1949-12-31, ERA-CLIM ID 4773
DOI: 10.1594/pangaea.666872
title: (Table 3) Major element composition of silicic and mafic glasses from ODP Site 180-1115
DOI: 10.1594/pangaea.673276
title: Basic and other measurements of radiation at station Toravere (2003-03)

description: Please note, that SWD, DIR, DIF and SWU nighttime negatives are set manually to zero (until end of August 2018).
DOI: 10.1594/pangaea.924007
title: Physical oceanography from mooring KPO_1169

description: GEOMAR moorings are typically equipped with instruments recording pressure, temperature, conductivity, dissolved oxygen and current velocity. Instruments with pressure, temperature, conductivity and oxygen sensors were calibrated in situ immediately prior to and after a mooring deployment period by attaching them to the CTD frame during CTDO casts. Correction terms were then developed from the difference between the sensor readings and the calibrated CTDO data during several minute long calibration stops. These correction terms were then applied to the full deployment periods. This ensured best data quality with recognition of potential sensor drifts and also allowed for the estimation of calibration and measurement errors (Hahn et al. 2014, Bittig et al. 2018, Berx et al. 2019). Moored Acoustic Doppler Current Profiler bin depths were corrected using the sound speed at instrument depth following the approach by Shcherbina et al. (2005). Velocities were not corrected, but respective measurement errors were assumed as described in Hahn et al. (2014). For all instruments within a mooring that did not record pressure, full deployment pressure time series were estimated by linearly interpolating between the instruments having a pressure sensor.
description: instrument = Label:kpo_1169_02 File:kpo_1169_instr_02.nc Type:Teledyne RDI LongRanger 75 SN:02290instrument = Label:kpo_1169_03 File:kpo_1169_instr_03.nc Type:Seabird MicroCat 37-IM mit P SN:10653instrument = Label:kpo_1169_04 File:kpo_1169_instr_04.nc Type:Seabird MicroCat 37-SM SN:02618instrument = Label:kpo_1169_05 File:kpo_1169_instr_05.nc Type:Nortek Aquadopp Seriell SN:P26209-20instrument = Label:kpo_1169_06 File:kpo_1169_instr_06.nc Type:Seabird MicroCat 37-SM SN:01583comment = flag_meaningscomment = 0:unknowncomment = 1:good_datacomment = 2:probably_good_datacomment = 3:potentially_correctable_bad_datacomment = 4:bad_datacomment = 5:not_usedcomment = 6:not_usedcomment = 7:nominal_valuecomment = 8:interpolated_valuecomment = 9:missing_value
DOI: 10.1594/pangaea.925271
title: Pollen content of profile No 84/3 of gravel pit Northeim_PitA

description: The pollen spectra belong to Pollen zones IV (Preboreal) to VIII (Subboreal). Radiocarbon age of peat (depth 1.39-1.45 m): Hv-13279: 9100+/- 220 BP; calibrated: 8286+/-314 calBC
DOI: 10.1594/pangaea.802529
title: Meteorological synoptical observations from station Tateno (2012-09)
DOI: 10.1594/pangaea.884873
title: Ichthyoplankton composition from SUESTE cruise 2, Southern Brazilian Shelf, in 1983

description: The Departamento de Hidrografia e Navegação (DHN) from the Brazilian Navy in partnership with the Centro de Biologia Marinha (CEM) of the Federal University of Paraná (UFPR) conducted four seasonal cruises covering the coastal, neritic and oceanic regions between 24º06'S and 29º36'S to evaluate the general oceanographic processes present in the region (Brandini, 1990a; 1990b). Each cruise had twelve transects perpendicular to the coastline that were surveyed onboard NOc. Almirante Saldanha resulting in approximately 90 oceanographic stations spaced 30 nautical miles (~ 55 km) apart (Brandini, 1990b). Samples were obtained in the shallow stations (depth &lt;50 m) through horizontal and vertical trawls with a 0.5 m mouth diameter, 250 μm mesh plankton net. Oblique hauls using 0.6 m mouth diameter, 300 μm mesh plankton net were conducted mainly at intermediate depths (&gt; 50 m and &lt;200 m) from 5 m from the bottom to the surface, and from 200 m depth in the deep stations. At selected intermediate and deep stations, stratified vertical hauls with a 0.5 m mouth diameter, 250 μm mesh plankton net were also performed. The net type used has not been determined, except for the use of a Chossi Kid Net in some stations of the 2nd cruise. Volume of filtered water for each trawl is not available and number of eggs and larvae were not standardized (Macedo-Soares, 2015).
DOI: 10.1594/pangaea.802530
title: Radiosonde measurements from station Tateno (2012-09)
DOI: 10.1594/pangaea.845293
title: Ultra-violet measurements from station Toravere (2015-03)

description: 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 2017-01-17. UVB is measured with Kipp&Zonen CUVB1 narrowband radiometer (bandwidth 306 ± 0.1 nm)
DOI: 10.1594/pangaea.772125
title: Table 1: Parameters of 21 samples from core III of Vernagtferner

description: The purpose of this study was: (1) To make an attempt at finding a stratification of the snowpack in order to help remove ambiguities in dating the snowlayers by standard methods. (2) To verify the depth at which the transition between firn and ice occurs.Clearly the first goal was missed, the structural information in a temperate firn being strongly smoothed out in time. Interesting details like horizontal ice lenses and layers of "cold snow" however, were revealed. In spite of strong variations of density, gravimetric density PG and ice density PI, computed from point density, are identical for the firn pack between Z = 2.0 m and 6.0 m. p(ice) = 0.522 ± 0.034 x 10**3 kg/m**3. The ice density of 0.8 x 10**3 kg/m**3, the assumed transition between firn and ice, was found to occur at a depth of Z= 19 m. Even at this level, rather important variations in density may be localized. Between Z= 19 m and 21 m, the ice density varies from 0.774 x 10**3 to 0.860 x 10**3 kg/m**3.
description: Supplement to: Good, Walter (1982): Structural investigations of snow and ice on core III from the drilling on Vernagtferner, Austria, in 1979. Zeitschrift für Gletscherkunde und Glazialgeologie, 18(1), 53-64
DOI: 10.1594/pangaea.773716
title: Headspace-gas measurements from IODP Hole 316-C0006F

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.836981
title: Properties of seawater from a Sea-Bird TSG temperature and conductivity sensor mounted on the continuous surface water sampling system during campaign TARA_20110626Z of the Tara Oceans expedition 2009-2013

description: The Tara Oceans Expedition (2009-2013) sampled the world oceans on board a 36 m long schooner, collecting environmental data and organisms from viruses to planktonic metazoans for later analyses using modern sequencing and state-of-the-art imaging technologies. Tara Oceans Data are particularly suited to study the genetic, morphological and functional diversity of plankton. The present data publication contains measurements from the Continuous Surface Sampling System [CSSS] made during one campaign of the Tara Oceans Expedition. Water was pumped at the front of the vessel from ~2m depth, then de-bubbled and circulated to a Sea-Bird TSG temperature and conductivity sensor. System maintenance (instrument cleaning, flushing) was done approximately once a week and in port between successive legs. All data were stamped with a GPS.
DOI: 10.1594/pangaea.925709
title: Magnetization intensities of redeposited Black Sea sediment from the last glacial

description: This data publication provides data on redeposition experiments with mud collected during paleomagnetic sampling of various cores from the Arkhangelsky Ridge, SE Black Sea, recovered during marine expedition M72/5 of German research vessel RV METEOR in 2007 and expedition MSM33 of German research vessel RV Maria S. Merian in 2013. The collected silici-clastic mud mostly originates from glacial sediments deposited during marine isotope stages (MIS) 2 to 4, and 6. The material (bulk/mixed sample) originates from 208m to 847m water depth, 41° 28.66'N to 42° 13.57'N in latitude, and 36° 29.53'E to 37° 11.68'E in longitude. Experiments were performed in order to check the (non-) linearity of the detrital remanent magnetization (DRM) of Black Sea sediments acquired in different magnetic fields.
description: Component(s) of the ambient magnetic field set by the coils system. H - horizontal componentV – vertical componentvibr. - vibrating platformstill – still platform
DOI: 10.1594/pangaea.879857
title: Other measurements at 10 m from station Boulder, SURFRAD (2016-10)
DOI: 10.1594/pangaea.495761
title: Water temperature XBT profiles from cruise U74XX79424_1974
DOI: 10.1594/pangaea.925348
title: Macroremain content of profile No 85/3 of gravel pit Northeim_SiteC
DOI: 10.1594/pangaea.707135
title: Ultra-violet measurements from station Toravere (2008-10)

description: 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 2017-01-17. UVB is measured with Kipp&Zonen CUVB1 narrowband radiometer (bandwidth 306 ± 0.1 nm)
DOI: 10.1594/pangaea.822672
title: Meteorological measurements in the upper air at station Soesterberg, 1911-06-09 to 1920-06-14, ERA-CLIM ID 5003B
DOI: 10.1594/pangaea.880246
title: Time series of hydrofluorocarbon HFC-125 concentration at MaceHead in 2011
DOI: 10.1594/pangaea.880835
title: Other measurements at 10 m from station Bondville (2017-05)
DOI: 10.1594/pangaea.858813
title: Radiosonde measurements from Neumayer Station (2015-04)
DOI: 10.1594/pangaea.822536
title: Meteorological measurements in the upper air at station Ny Alesund, 1937-07-07 to 1937-08-04, ERA-CLIM ID 4796
DOI: 10.1594/pangaea.881096
title: Other measurements at 10 m from station Goodwin Creek (2017-06)
DOI: 10.1594/pangaea.822540
title: Meteorological measurements in the upper air at station Royal Center, 1918-07-12 to 1918-12-31, ERA-CLIM ID 4800

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.822542
title: Meteorological measurements in the upper air at station Fort Omaha, 1915-05-08 to 1915-05-09, ERA-CLIM ID 4802

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.881963
title: Basic and other measurements of radiation at station Barrow (2007-08)

description: Version 2, 2017-10-18 with corrected Short-wave downward (GLOBAL) radiation values. Please note that relative humidity values might be off and are therefore to be handled with caution.
DOI: 10.1594/pangaea.495496
title: Water temperature XBT profiles from cruise U32X107798_1988
DOI: 10.1594/pangaea.771134
title: (Table 4.3.5) Integrated formation- and consumption rates of methane in surface layer bottom sediments of the Batabano Bay
DOI: 10.1594/pangaea.771135
title: (Table 4.3.6) Consumption of organic carbon in microbial processes in bottom sediments of the Batabano Bay
DOI: 10.1594/pangaea.880274
title: Ultra-violet measurements from station Fort Peck (2016-07)
DOI: 10.1594/pangaea.880837
title: Ultra-violet measurements from station Bondville (2017-06)
DOI: 10.1594/pangaea.925286
title: Macroremain content of profile No 85/2 of gravel pit Northeim_PitB
DOI: 10.1594/pangaea.881215
title: Basic and other measurements of radiation at station Barrow (2011-08)

description: Please note that relative humidity values might be off and are therefore to be handled with caution.
DOI: 10.1594/pangaea.920902
title: SPM derived data using a local established statistical relationship between turbidity and SPM in situ in Guaíba River - DMAE (2003 - 2013)

description: The 'Departamento Municipal de Águas e Esgotos - DMAE' data were acquired at the Guaíba River mouth from 2003 to 2013 on a daily basis. The data set was assembled gathering daily river discharge data from the main rivers that contribute to the Guaíba River and water turbidity data recorded at 30 minutes interval. The turbidity data were converted to SPM concentration throughout calibration procedures in laboratory following standard procedures. The SPM-turbidity relationship was determined with a r = 0.98. Daily averaged SPM data is available in this dataset.
DOI: 10.1594/pangaea.880838
title: Other measurements at 10 m from station Bondville (2017-06)
DOI: 10.1594/pangaea.920911
title: SPM in situ data along Patos Lagoon - 'Lagoa dos Patos' Project (1987 - 1989)

description: The 'Lagoa dos Patos' project goal was to assess geological, chemical, physical, biological and socio-economic parameters along the lagoon in order to advise on the best approach for exploration of the Patos Lagoon resources at the time. The Project was composed of monthly expeditions studying distribution and behavior of properties affecting water quality: salinity, water temperature and SPM among other parameters and the dynamics of sediments in the Patos Lagoon, although only Suspended Particulate Matter (SPM) is available here. SPM data were acquired between December 1987 and December 1988 in 19 stations along the lagoon. A total of 13 monthly cruises were carried out from North to South of the lagoon. Stations were located in the navigational canal and samples were obtained at the surface, mid water column, and bottom. All SPM samples were acquired using the methodology by Aminot and Chaussepied (Aminot, A. and Chaussepied, M.: Manuel des Analyses Chimiques en milieu Matin, CNEXO, Bres, p. 396, 1983).
DOI: 10.1594/pangaea.920913
title: SPM in situ data along Patos Lagoon - 'Pró-Mar de Dentro' Project (1998 - 2000)

description: The most comprehensive study of Patos Lagoon was carried out by the 'Pró-Mar de Dentro' Project. During the period between February 1999 to January 2000, 11 sampling expeditions were performed, where 8 stations were established in the Patos Lagoon main axis, 3 stations on the main tributaries (Guaíba River, Camaquã River, and São Gonçalo Channel), and 1 station on the inner continental shelf, just after the Patos Lagoon inlet. During sampling procedures, a variety of chemical, physical, and biological parameters were analyzed. Data and results were reported in the year 2000 by a partnership with 'Japan International Cooperation Agency' (JICA), the project sponsor.