cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.929737
title: Calibrated ages of Burnt Village (core 1) peat core from Borneo

description: Geochemistry data of a high-resolution peat core from the Past Global Changes - Carbon in Peat on EArth through Time (PAGES_C-PEAT) Project.
DOI: 10.1594/pangaea.805254
title: (Table 1) Remanent magnetic properties at DSDP Hole 83-504B
DOI: 10.1594/pangaea.793263
title: (Appendix B Table 11) Calcareous nannofossil biohorizons of ODP Hole 167-1021B

description: DEPTH, sediment is given in mcd.
DOI: 10.1594/pangaea.930117
title: Calibrated ages of Baie2 peat core from Canada

description: Calibrated ages of a high-resolution peat core from the Past Global Changes - Carbon in Peat on EArth through Time (PAGES_C-PEAT) Project.
DOI: 10.1594/pangaea.693778
title: Mesozooplankton during Professor Vodyanitskiy cruise PV33

description: Standard Judey net
DOI: 10.1594/pangaea.817278
title: Physical oceaongraphy measured on water bottle sample during TYRO cruise NIOP-C1
DOI: 10.1594/pangaea.828785
title: Carbonate analysis from IODP Hole 339-U1386C

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.751055
title: Meteorological observations during PALLAS cruise from Havana to Truvillo started at 1828-05-12
DOI: 10.1594/pangaea.707619
title: Meteorological synoptical observations from station Payerne (2001-12)
DOI: 10.1594/pangaea.805580
title: (Table 2) Geochemistry of magnesiochromite at DSDP Holes 82-556 and 82-562
DOI: 10.1594/pangaea.828053
title: Biomarkers (GDGT) of sediment core POS362-2_33
DOI: 10.1594/pangaea.920904
title: SPM in situ data along Patos Lagoon - 'Espinha de Peixe' Project (1986)

description: This project collected a series of physical, chemical and biological parameters. The data consists of sampling carried out in January 1986, at which sampling cruises were realized in 60 stations. These data are relative to samples in the estuary (6-8 January), in the São Gonçalo Channel area (12-15 January), Tapes (19-22 January), and Pontal da Formiga (29-31 January), the northernmost sampled region. Of these, 17 stations were sampled in the estuarine region, and the remaining were divided in transects E-W and N-S, thus covering all regions of the lagoon. In the E-W direction, data were obtained from margin to margin. Water samples were collected at the surface and near the bottom using a plastic bucket or a 3 l horizontal bottle. SPM analysis were carried out gravimetrically on pre-weighted Gelman GA (0.45 μm pore size) by 'Laboratório de Hidroquímica' at 'Universidade Federal do Rio Grande (FURG)'.
DOI: 10.1594/pangaea.920910
title: SPM in situ data, and SPM estimates from statistical relationships between SPM in situ and turbidity in the estuary of Patos Lagoon - LOCOSTE (2012 - 2019)

description: As an initiative of the 'Laboratório de Oceanografia Costeira e Estuarina - LOCOSTE', at FURG, oceanographic cruises were carried out in the Patos Lagoon estuarine area between 2012 to 2019 in a series of expeditions. The campaigns carried out in 2012 consist of SPM in situ measurements in 7 cruises at 9 stations performed from February to October of that year. Samples were taken along the Patos lagoon estuarine area . A second data set was acquired in 2017 in a 2-day expedition in the Patos Lagoon Estuary. Field measured SPM was acquired following the method by Baumgarten et al. (2010). Further, turbidity and SPM in situ data were gathered from multiple field campaigns carried out in 2014, 2015, 2018, and 2019. Turbidity data were measured using a JFE Advantech™ Rinko-profiler Conductivity, Temperature, and Depth (CTD), while water samples were collected at the surface simultaneously to the CTD vertical profiles using a bucket. The filtration of those samples was performed following the procedures by Loring and Rentala (Loring, D. H. and Rantala, R. T. T.: Manual for the geochemical analyses of marine sediments and suspended particulate matter, Earth-Science Reviews, p. 235–283, 1992). The data made available consists of measured SPM and SPM derived from turbidity samples. The same equation was applied to a set of turbidity data acquired during field campaigns for the Estuarine Physics lectures of the undergraduate course in Oceanography at FURG. The campaigns were carried out on the austral spring years of 2016, 2017, 2018, and 2019 and acquired with the same CTD equipment.
DOI: 10.1594/pangaea.805080
title: Basic measurements of radiation at station Cener (2012-11)
DOI: 10.1594/pangaea.920900
title: SPM in situ data in Camaquã River and Guaíba River - Baisch (1988 - 1990)

description: The objective of this PhD research was to study the environmental behavior and impact of trace metal elements in the Patos Lagoon system (Baisch, P.: Les Oligo-Elements Metallique du Systeme Fluvio-Lagunare dos Patos (Bresil) - Flux et deverir, Ph.D. thesis, L'Université Bordeaux I, 1994). It also aimed to determine SPM, particulate organic carbon and particulate organic nitrogen fluxes from rivers to the lagoon. SPM was obtained from May 1988 to August 1990 for the Camaquã River and from January 1988 to June 1990 for the Guaíba River following the methodology proposed by Aminot and Chaussepied (1983).
DOI: 10.1594/pangaea.747090
title: Meteorological observations during SWALLOW cruise from Monopin Hill started at 1750-08-12
DOI: 10.1594/pangaea.803629
title: (Table 3) Magnetostratigraphy at DSDP Holes 85-574 and 85-574A

description: Sediment depth is given in mbsf. Core 6 to Core 9 data did not allow identification of specific reversals.
DOI: 10.1594/pangaea.496032
title: Water temperature MBT profiles from cruise U90X000000M_1970
DOI: 10.1594/pangaea.920899
title: SPM in situ data in the estuary of Patos Lagoon - ANA (1978 - 2019)

description: The 'Agência Nacional de Águas' (ANA; http://www.snirh.gov.br/hidroweb) is responsible for coordinating a national hydro-meteorological network, a system that gathers about 4,641 monitoring stations in Brazil. Data from a station in the Camaquã River from 1978 to 2019 is shown here. SPM in situ samples were acquired by the Geological Service of Brazil (CPRM) agency.
DOI: 10.1594/pangaea.829349
title: Vane shear strength measurements from IODP Hole 340-U1394B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.917579
title: Expanded measurements from station Ny-Ålesund (2020-03)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.663793
title: Oceanography at CTD/bottle station IFREMER_0633
DOI: 10.1594/pangaea.495655
title: Water temperature MBT profiles from cruise U74X024620M_1955
DOI: 10.1594/pangaea.750555
title: Meteorological observations during MAAS cruise from Suriname to St. Maarten started at 1835-07-11
DOI: 10.1594/pangaea.829133
title: Gas measurements from IODP Hole 340-U1400B

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.753720
title: Meteorological synoptical observations from station Tamanrasset (2010-08)
DOI: 10.1594/pangaea.953829
title: Standardized mineral data of sediment core PG2023 from Lake Kyutyunda (Yakutia, Russia)

description: This data set is part of a larger data harmonization effort to make lake sediment core data machine readable and comparable. Here we standardized mineral data of sediment core PG2023, retrieved in 2010 from Lake Ozero Kyutyunda (Yakutia, Russia) at 2.9 m water depth. The thermokarst lake Ozero Kyutyunda is situated in the coniferous forest area and has one outflow, one inflow and several smaller inflows. It lies at an elevation of ca. 56 m a.s.l. with a surface area of ca. 4.9 km2 and a maximum lake water depth of estimated 3.5 m. The 7.1 m sediment core was retrieved by a UWITEC piston corer during the RU-Land_2010_Lena expedition of the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research (AWI, Germany, Potsdam) in cooperation with the North Eastern Federal State University (NEFU, Russia, Yakutsk). Bulk mineralogy was analysed by x-ray diffractometry (XRD) using a (PHILIPS, Netherlands) PW1820 goniometer.
DOI: 10.1594/pangaea.920903
title: SPM in situ data in Patos Lagoon estuary - ECOSUD (2002 - 2004)

description: This dataset was acquired in a research program funded by the European Commission known as ECOSUD (Estuaries and Coastal Areas: Basis and Tools for a more Sustainable Development). It includes the realization of 4 field campaigns (one every season), where morphologic, meteorological, hydrodynamic, hydrographic, and water quality data were acquired. Sampling campaigns were performed under several salinity conditions in the estuary. The first 2 cruises were conducted in Mangueira Bay and the southern estuarine portion of Patos Lagoon (Rio Grande Channel) in order to obtain contrasting data. Samples were taken in October 2002 (austral spring) and June 2003 (austral winter). 2 additional cruises were then conducted in the remaining seasons: one in December 2003 (austral summer) and the other in April 2004 (austral fall). At each sampling station, the water column was sampled at the surface using a Van Dorn-like bottle. Samples were stored in polyethylene bottles and kept at 5°C until they arrived at the laboratory, where they were either promptly analyzed or preserved. SPM samples were analyzed using the methods described by Baumgarten et al. (Baumgarten, M., Rocha, J., and Niencheski, L.: Manual de Análises em Oceanografia Química, FURG, Rio Grande, Brazil, 1996).
DOI: 10.1594/pangaea.747636
title: Meteorological observations during BELLONA cruise from London to Rio de Janeiro started at 1792-08-14
DOI: 10.1594/pangaea.887210
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2004402

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.803627
title: Ultra-violet measurements from station Toravere (2012-11)

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.494936
title: Physical oceanography during cruise U99X000002C
DOI: 10.1594/pangaea.694937
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station SEPT-1998-K05

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.667487
title: (Table 1) Chemical composition of augite and plagioclase from DSDP Hole 11-100
DOI: 10.1594/pangaea.898543
title: Water level and storage changes of Yamzho Yumco lake during 2000‒2017

description: Following information is included:1) Date of the data acquisition time in the form of yyyy-mm-dd.2) Lake water levels are orthometric heights with respect to EGM08, WGS84, in the unit of meter.3) Uncertainty of the lake water level in the unit of meter, if it is altimetry water level. The uncertainty of optical water levels was not calculated and set to 0.4) Lake water storage changes with respect to the baseline (lake water storage of the water level baseline H0, which is a value we do not exactly know; see https://doi.pangaea.de/10.1594/PANGAEA.898409) in the unit of km^3.5) The source of the data, 0 - Landsat, 1 - Envisat, 2 - ICESat, 3 - CryoSat, 4 - Jason-1/2/3.
DOI: 10.1594/pangaea.495326
title: Water temperature XBT profiles from cruise U31X041797_1971
DOI: 10.1594/pangaea.691215
title: Nutrient concentrations in water samples collected at Station MARCH-94-GN3619940280101100 in the Aegean Sea
DOI: 10.1594/pangaea.719000
title: Ultra-violet measurements from station Bondville (2005-08)

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 2017-02-09.
DOI: 10.1594/pangaea.495050
title: Water temperature XBT profiles from cruise K7441_1992
DOI: 10.1594/pangaea.916503
title: 1-Hz PPP displacements at GEONET station 0301 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.920921
title: SPM in situ data in the Patos Lagoon estuary's access channel (Canal do Rio Grande) and in 'Porto Velho' (Canal do Norte) - 'Porto do Rio Grande' (2000 - 2018)

description: The 'Programa de Monitoramento Ambiental do Porto do Rio Grande' is the network responsible for the data and counts with more than 30 scientists from different laboratory units of the 'Instituto Oceanográfico' at FURG. The sampling program was defined by the Brazilian National Environmental Agency (IBAMA). Annual reports since the year 2000 gather a number of large data sets related to the local aquatic environment covering the lower Patos Lagoon Estuary and the adjacent Atlantic Ocean. It also covered dredging campaigns, and environmental reports of seasonal samplings until the year 2017. Despite the intensive coverage of biological data in the reports, here we present only SPM data. More recent information can be found at the 'Porto do Rio Grande' website http://www.portosrs.com.br/site/responsabilidade_ambiental.php. Data were made available under the Port of Rio Grande data policy. Water samples were obtained on the surface, middle depth and bottom. Water sampling was carried out at sampling stations located along the estuarine access channel (Canal do Rio Grande), and in 'Porto Velho' (Canal do Norte). Water samples were processed following methods proposed by Baumgarten et al. (Baumgarten, M., Rocha, J., and Niencheski, L.: Manual de Análises em Oceanografia Química, FURG, Rio Grande, Brazil, 1996 and Baumgarten, M., Wallner-Kersanach, M., and Niencheski, L.: Manual de Análises em Oceanografia Química, FURG, Rio Grande, Brazil, 2010).
DOI: 10.1594/pangaea.920923
title: SPM in situ data concurrent with Landsat 8/OLI overpass for Guaíba River - UFRGS (2015 - 2017)

description: Two years of field sampling concurrent with Landsat8/OLI overpass was acquired by Scotta (2018; http://hdl.handle.net/10183/184882). 9 field campaigns were carried out onboard a vessel to sample in situ SPM data from November 2015 to March 2017 on the days Landsat8/OLI overpass, when the cloudiness was low or nonexistent. 144 in situ water samples were collected on the surface and later filtered by the gravimetric method in the laboratory to determine SPM following the method described in Baumgarten et al. (Baumgarten, M., Wallner-Kersanach, M., and Niencheski, L.: Manual de Análises em Oceanografia Química, FURG, Rio Grande, Brazil, 2010). Samples were collected at a 2-hour interval before and after the satellite overpass. In the 3 final campaigns, the samplings were conducted throughout the day and the acquisition time exceeded the 2-hour interval due to the larger number of samples. Surface reflectance was extracted from the central pixel correspondent to the samples and from the adjacent pixels so that the results could be compared. Regression analyzes were performed among the SPM data and for the visible, near-infrared (NIR), and two medium infrared bands (SWIR1 and SWIR2). The best-fit model corresponded to the red band (667 nm) in an exponential relationship.
DOI: 10.1594/pangaea.829319
title: Magnetic remanence from IODP Hole 340-U1397A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.953294
title: Standardized diatom data of sediment core PG2023 from Lake Kyutyunda (Yakutia, Russia)

description: This data set is part of a larger data harmonization effort to make lake sediment core data machine readable and comparable. Here we standardized diatom count data of sediment core PG2023, retrieved in 2010 from Lake Ozero Kyutyunda (Yakutia, Russia) at 2.9 m water depth. The thermokarst lake Ozero Kyutyunda is isituated in the coniferous forest area and has one outflow, one inflow and several smaller inflows. It lies at an elevation of ca. 56 m a.s.l. with a surface area of ca. 4.9 km2 and a maximum lake water depth of estimated 3.5 m. The 7.1 m sediment core was retrieved by a UWITEC 60mm piston corer during the RU-Land_2010_Lena expedition of the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research (AWI, Germany, Potsdam) in cooperation with the North Eastern Federal State University (NEFU, Russia, Yakutsk). Diatoms have been counted using a Zeiss AXIO Scope.A1 light microscope with a Plan-Apochromat 100/1.4 Oil Ph3 objective at 1000x magnification.
DOI: 10.1594/pangaea.669986
title: Basic measurements of radiation at station Kwajalein (2003-05)
DOI: 10.1594/pangaea.898540
title: Water level and storage changes of Wulanwula lake during 2000‒2017

description: Following information is included:1) Date of the data acquisition time in the form of yyyy-mm-dd.2) Lake water levels are orthometric heights with respect to EGM08, WGS84, in the unit of meter.3) Uncertainty of the lake water level in the unit of meter, if it is altimetry water level. The uncertainty of optical water levels was not calculated and set to 0.4) Lake water storage changes with respect to the baseline (lake water storage of the water level baseline H0, which is a value we do not exactly know; see https://doi.pangaea.de/10.1594/PANGAEA.898409) in the unit of km^3.5) The source of the data, 0 - Landsat, 1 - Envisat, 2 - ICESat, 3 - CryoSat, 4 - Jason-1/2/3.
DOI: 10.1594/pangaea.497409
title: Physical oceanography from BT during cruise U06XX02220B_1965
DOI: 10.1594/pangaea.718978
title: Other measurements at 10 m from station Bondville (2005-02)
DOI: 10.1594/pangaea.669906
title: Basic measurements of radiation at station Kwajalein (1996-09)
DOI: 10.1594/pangaea.898541
title: Water level and storage changes of Xijir Ulan lake during 2000‒2017

description: Following information is included:1) Date of the data acquisition time in the form of yyyy-mm-dd.2) Lake water levels are orthometric heights with respect to EGM08, WGS84, in the unit of meter.3) Uncertainty of the lake water level in the unit of meter, if it is altimetry water level. The uncertainty of optical water levels was not calculated and set to 0.4) Lake water storage changes with respect to the baseline (lake water storage of the water level baseline H0, which is a value we do not exactly know; see https://doi.pangaea.de/10.1594/PANGAEA.898409) in the unit of km^3.5) The source of the data, 0 - Landsat, 1 - Envisat, 2 - ICESat, 3 - CryoSat, 4 - Jason-1/2/3.
DOI: 10.1594/pangaea.749079
title: Meteorological observations during El Pizarro cruise from La Habana to La Coruña started at 1775-07-06
DOI: 10.1594/pangaea.926031
title: δ¹⁸O in ice wedges, ice lenses and snow from Kular, Yakutia (Russia)

description: Variations of δ¹⁸О in Late Pleistocene ice wedges, in structure-forming ice and segregated ice lenses, as well as in snow and water of Burguat River were determined. The studied section of the yedoma strata has been exposed in an outcrop of the slope sediments on a gentle slope in the foothills of Kular Ridge, nearby Kular Settlement, on the right bank of the Burguat River, 0.5 kilometers from the mouth of the Emis Creek.
description: In the field, the samples of ice wedges for isotope and chemical analysis were sampled out of the axial parts of the wedges from the main outcrop wall with an interval of 0.2 to 0.5 m using the sampling method elaborated by Yu.K. Vasil'chuk (1992). The isotopic composition of ice wedges has been determined at the Tallinn Institute of Geology.
DOI: 10.1594/pangaea.927279
title: Trace elements in Batagay ice wedges, structure ice, Batagaika and Yana River water, North Yakutia, Russia

description: Average content of some trace elements in ice wedges, structure ice, Batagaika and Yana River water. Samples were taken rom the Batagay megaslump, 10 km to south east from Batagay settlement in the Verkhoyansky District of the Yakutia (Sakha) Republic, Russia.The analysis was carried out in samples filtered through the membrane filter (filtered) as well as in samples, that were taken after organic inclusions were precipitated (unfiltered).
description: The content of major and trace elements in ice (water filtered through a membrane filter and also unfiltered), was determined in Moscow, in the laboratory of the All-Russian Research Institute of Mineral Raw Materials named after N.M. Fedorovsky (VIMS) mass spectral (ICP-MS) and atomic emission methods (ICP-AES) with inductively coupled plasma on an iCAP Qc mass spectrometer (Thermo Scientific, USA) and an Optima – 4300 DV atomic emission spectrometer (Perkin Elmer, USA) were used for laboratory analyses, according to certified methods (NSAM 499-AES/MS, 2015) using standard reference materials and blank samples. The VIMS laboratory is accredited in the international accreditation system Analytics (AAS.A.00255), the national accreditation system (RA.RU.21GP11), and also in accordance with the requirements of the International Standards ISO Guide 34: 2009 and ISO/IEC 17025: 2017. Water samples (filtered and unfiltered) in plastic bottles were transferred to the laboratory and then injections of water samples to the chromatograph were made without any special manipulations.#999: below detection limit
DOI: 10.1594/pangaea.666034
title: Oceanography at CTD/bottle station IFREMER_2860
DOI: 10.1594/pangaea.718831
title: Ultra-violet measurements from station Sioux Falls (2009-03)

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.718882
title: Ultra-violet measurements from station Bondville (2003-10)

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 2017-02-09.
DOI: 10.1594/pangaea.848898
title: Diatoms of composite core PG2023
DOI: 10.1594/pangaea.788034
title: (Table 1a) Chemical composition of minerals from crystalline schists of the lower unit of the Khavyven series
DOI: 10.1594/pangaea.496911
title: Physical oceanography from BT during cruise K90XXB_1934
DOI: 10.1594/pangaea.926033
title: Composition and content of water-soluble salts in syngenetic ice wedges in Kular, Yakutia (Russia)

description: Composition and content of water-soluble salts in syngenetic ice wedges from Kular in Northern Yakutia.
description: The chemical composition of water-soluble salts in the Late Pleistocene ice wedges has been determined by titration in the chemical laboratory of the PNIIIS.
DOI: 10.1594/pangaea.927867
title: Trace elements content in soils and soil inclusions in Batagay ice wedges, North Yakutia, Russia

description: Trace elements in soil and soil inclusions of ice wedges from the Batagay megaslump, 10 km to south east from Batagay settlement in the Verkhoyansky District of the Yakutia (Sakha) Republic, Russia.
description: The content of major and trace elements in soils and soil inclusions in ice was determined in Moscow, in the laboratory of the All-Russian Research Institute of Mineral Raw Materials named after N.M. Fedorovsky (VIMS) mass spectral (ICP-MS) and atomic emission methods (ICP-AES) with inductively coupled plasma. iCAP Qc mass spectrometer (Thermo Scientific, USA) and an Optima – 4300 DV atomic emission spectrometer (Perkin Elmer, USA) were used for laboratory analysts, according to certified methods (NSAM 499-AES/MS, 2015) using standard reference materials and blank samples. The VIMS laboratory is accredited in the international accreditation system Analytics (AAS.A.00255), the national accreditation system (RA.RU.21GP11), and also in accordance with the requirements of the International Standards ISO Guide 34: 2009 and ISO/IEC 17025: 2017.
DOI: 10.1594/pangaea.718914
title: Ultra-violet measurements from station Bondville (2004-06)

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 2017-02-09.
DOI: 10.1594/pangaea.823350
title: Feeding, growth and grazing rates of Oxyrrhis marina determined experimentally