cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.920918
title: SPM in situ data in Patos Lagoon estuary and adjacent continental shelf - PLATES (1992 - 1993)

description: The project 'Interação Plataforma Continental-Estuário da Lagoa dos Patos - PLATES' established a series of phases for data acquisition from 1992 to 1993. Sampled information consisted of salinity, temperature, current speed and direction and SPM. A series of weekly SPM sampling expeditions in the Rio Grande Channel from March 1992 to January 1993 is presented here. 45 weekly samples were collected at 5 stations along the narrowest section of the navigational channel (about 750 m) of the Patos Lagoon Estuary. Samples were obtained at surface and bottom, filtered using a vacuum pump, and measured following the method described 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.898547
title: Water level and storage changes of Zhuonai 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 EGM96, 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.692919
title: Mesozooplankton abundance during Akademik Kovalevsky cruise AK65, Part III

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 125 µm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-300, 300-500 m) and closed at the upper depth level. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved in 3-4% buffered formaldehyde and processed on return to the laboratory. All of copepods were identified to genus level, other taxanomic groups - to type, class, order and family levels.
DOI: 10.1594/pangaea.898943
title: Temperature percentiles thresholds in Athens, Greece, for the base period 1961-1990
DOI: 10.1594/pangaea.898510
title: Water level and storage changes of Goren Co 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 EGM96, 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.898511
title: Water level and storage changes of Gozha Co 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.898544
title: Water level and storage changes of Yelusu 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 EGM96, 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.901514
title: Beach profile data for the Elwha River Delta, 2012-04-10

description: Data were collected using GNSS survey methods, with a differential GPS operating in Real Time Kinematic (RTK) mode. Data from prior to 2013 were typically collected with a Magellan ProMark 3 traditional RKT-DGPS system (i.e. local base station and rover), with the base station sited on survey control markers installed in 1996, with survey control coordinates referenced to NAD83(CORS91). Starting in 2013 survey data were typically collected with an AshTech ProMark 200 RTK-DGPS system connected to the Washington State Reference Network. Survey data collected between January and November 2013 are referenced to NAD83(CORS96), and after November 2013 to NAD83(2011). Vertical data for surveys in 2012 and 2013 are referenced to NAVD88, presumably using Geoid96 (the survey control documentation does not specific a geoid). For all subsequent surveys the vertical data are referenced to NAVD88(Geoid09). No conversion were applied to these data to account for variations in horizontal or vertical coordinate system adjustments through time, but an error analysis suggests a standard deviation for the elevation data of between 0.03 and 0.05 m across the entire sampling period (2011-2018). All survey data were collected with the GNSS system mounted on a 2.05 m rover pole, held level as a transect line was traced in a cross-shore orientation on the beach. The associated text files include the horizontal (HRMS) and vertical (VRMS) root-mean-square errors estimated by the GNSS system, as well as the RTK-DGPS status reported by the GNSS system at the time each point was collected. Times are referenced to local Pacific time (either PST or PDT).
description: Portions of these data have been published previously, including in Gelfenbaum et al. 2015.
DOI: 10.1594/pangaea.495183
title: Water temperature IBT profiles from cruise U06FI87073I_1987
DOI: 10.1594/pangaea.776197
title: Moisture and density (MAD) measured on IODP Hole 331-C0013E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.898491
title: Radiosonde measurements from station Bondville (2018-12)

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.871653
title: Basic measurements of radiation at station Lerwick (2017-01)

description: Please note that when plotting SWD vs. the calculated global radiation (from DIF and DIR) the slope shows a bias. Please contact the station manager for further information.
DOI: 10.1594/pangaea.933201
title: Tethered balloon-borne meteorological measurements during the Arctic field campaign PAMARCMiP (Balloon_20180322_1156_1353)

description: New version with revised wind speed calibration for the standard meteorology sonde.
DOI: 10.1594/pangaea.901055
title: Modeled climate time series data
DOI: 10.1594/pangaea.901080
title: Other measurements at 10 m from station Rock Springs (2018-01)
DOI: 10.1594/pangaea.933202
title: Tethered balloon-borne meteorological measurements during the Arctic field campaign PAMARCMiP (Balloon_20180322_1542_1652)

description: New version with revised wind speed calibration for the standard meteorology sonde.
DOI: 10.1594/pangaea.956068
title: Gamma ray resolution of core ZK01 from the southern Junggar Basin, Northwestern China
DOI: 10.1594/pangaea.898946
title: Temperature percentiles thresholds in Marseille, France, for the base period 1961-1990
DOI: 10.1594/pangaea.956069
title: Rubidium (Rb) and strontium (Sr) determination of core ZK01 from the southern Junggar Basin, Northwestern China
DOI: 10.1594/pangaea.898509
title: Water level and storage changes of Dung Co 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.898504
title: Water level and storage changes of Cuona 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 EGM96, 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.778792
title: Carbonate analysis from IODP Hole 317-U1354B

description: Geocode = Top depth CSF-A (m). Introduction to shipboard organic geochemistry on the JOIDES Resolution; ODP Technical Note 30: http://www-odp.tamu.edu/publications/tnotes/tn30/TNOTE_30.PDF
DOI: 10.1594/pangaea.956070
title: Paleomagnetic age determination of core ZK01 from the southern Junggar Basin, Northwestern China
DOI: 10.1594/pangaea.778653
title: Gas measurements from IODP Hole 317-U1353B

description: Geocode = Top depth CSF-A (m).Introduction to shipboard organic geochemistry on the JOIDES Resolution; ODP Technical Note 30: http://www-odp.tamu.edu/publications/tnotes/tn30/TNOTE_30.PDF
DOI: 10.1594/pangaea.898505
title: Water level and storage changes of Dagze Co 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 EGM96, T/P, 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.807230
title: (Table 1) Comparison of dive duration and speed of Adélie penguins (Pygoscelis adeliae) equipped with internal and external devices

description: Bio-logging studies suffer from the lack of real controls. However, it is still possible to compare indirect parameters between control and equipped animals to assess the level of global disturbance due to instrumentation. In addition, it is also possible to compare the behaviour of free-ranging animals between individuals equipped with different techniques or instruments to determine the less deleterious approach. We instrumented Adelie Penguins (Pygoscelis adeliae) with internal or external time-depth recorders and monitored them in parallel with a control group during the first foraging trip following instrumentation. Foraging trip duration was significantly longer in the internally-equipped group. This difference was due to a larger number of dives, reflecting a lower foraging ability or a higher food demand, and longer periods of recovery at the surface. These longer recovery periods were likely to be due to a reduced efficiency to ventilate at the surface, probably because the implanted devices pressurised adjacent organs such as air sacs. Moreover, descent and ascent rates were slightly lower in externally-equipped penguins, presumably because external instrumentation increased the bird drag. Looking at our results, implantation appears more disadvantageous - at least for short-term deployment - than external equipment in Adelie Penguins, while this method has been described to induce no negative effects in long-term studies. This underlines the need to control for potential effects due to methodological aspects in any study using data loggers in free-ranging animals, to minimise disturbance and collect reliable data.
description: Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
description: Supplement to: Beaulieu, Michaël; Ropert-Coudert, Yan; Le Maho, Yvon; Ancel, André (2010): Is abdominal implantation of devices a good alternative to external attachment? A comparative study in Adélie penguins. Journal of Ornithology, 151(3), 579-586
DOI: 10.1594/pangaea.934832
title: Age determination of Galvarne Moraine Ridge (GAL) peat core from Tierra del Fuego

description: 14C and 210Pb age determination 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.885044
title: Electrical conductivity from IODP Hole 365-C0010D
DOI: 10.1594/pangaea.898488
title: Other measurements at 10 m from station Bondville (2018-11)
DOI: 10.1594/pangaea.495191
title: Water temperature MBT profiles from cruise U06X026185M_1969
DOI: 10.1594/pangaea.934838
title: Age determination of No Name Creek (NNC) peat core from the USA

description: 14C and 210Pb age determination 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.934834
title: Age determination of Gwaun Nant Ddu (GND) peat core from Wales

description: 14C and 210Pb age determination 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.898506
title: Water level and storage changes of Dogai Coring 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 EGM96, T/P, 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.719596
title: Other measurements at 10 m from station Bondville (2003-06)

description: Version 2, 2009-06-15
DOI: 10.1594/pangaea.719598
title: Ultra-violet measurements from station Bondville (2003-07)

description: Version 2, 2009-06-15. 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.755529
title: Rare earth element concentration EDML ice core
DOI: 10.1594/pangaea.913217
title: Air and ground temperatures at the Crater Lake site during the experiment period (2010)

description: Climate induced warming of permafrost soils is a global phenomenon, with regional and site-specific variations, which are not fully understood. In this context, a 2D automated electrical resistivity tomography (A-ERT) system was installed for the first time in Antarctica at Deception Island, associated to the existing Crater Lake site of the Circumpolar Active Layer Monitoring Network (CALM-S). This set-up aims to I) monitor subsurface freezing and thawing processes on a daily and seasonal basis and to map the spatial and temporal variability of thaw depth, and to II) study the impact of short-lived extreme meteorological events on active layer dynamics. In addition, the feasibility of installing and running autonomous ERT monitoring stations in remote and extreme environments such as Antarctica was evaluated for the first time. Measurements were repeated at 4-hour intervals during a full year, enabling the detection of seasonal trends, as well as short-lived resistivity changes reflecting individual meteorological events. The latter is important to distinguish between (1) long-term climatic trends and (2) the impact of anomalous seasons on the ground thermal regime. The A-ERT.txt file contains all ERT surveys which were performed using Wenner electrode configuration. 20 copper plates, which are connected by buried cables to the active boxes, with an electrode spacing of 0.5 m were used in this experiment. This setup yields 56 individual data points for each monitoring data set at six data levels. All data were saved in the Res2Dinv format. The temperature. xlsx file contains air and ground temperatures data during the experiment period. The Air temperature was measured at 160 cm above the surface and ground temperatures in the shallow borehole S3,3 were measured with ibutton-sensors at depths 2.5, 5, 10, 20, 40, 80 and 160 cm.
DOI: 10.1594/pangaea.926032
title: Trace elements and alkaline-earth metals in Late Pleistocene syngenetic ice wedges in Kular, Yakutia (Russia)

description: Content of trace elements and alkaline-earth metals in Late Pleistocene syngenetic ice wedges from Kular in Northern Yakutia.
description: Analytical measurements of the trace element composition (Mn, Zn, Cu, Co) have been performed on the samples by the method of atomic-absorption spectroscopy at the V.V. Dokuchaev Soil Institute.
DOI: 10.1594/pangaea.807262
title: (Table 1) Retinol (vitamin A) and alpha-tocopherol (vitamin E) concentration in polar bear (Ursus maritimus) kidney

description: Vitamins A and E content of inner organs, among these the kidneys, are increasingly being used as an indicator of adverse effects caused to the organism by e.g. environmental contaminants. In general, only a renal sub sample is used for analyses, and it is thus essential to know which part of the organ to sample in order to get a representative value for this important biomarker. The aim here was to assess the distribution of vitamins A (retinol) and E (alpha-tocopherol) within the polar bear multireniculate kidney (i.e. polar vs. medial position) and also within the cortex vs. medulla of each separate renculi. The results showed no significant difference between the medial and polar renculi with regards to either retinol (p = 0.44) or alpha-tocopherol (p = 0.75). There were, however, significant differences between cortex and medulla for both vitamins (retinol, p = 0.0003; alpha-tocopherol, p&lt;0.0001). The kidney cortex contained higher values of both vitamins than the medulla; on average 29% more retinol and 57% more alpha-tocopherol. Mean concentrations in the medulla was 2.7 mg/kg for retinol and 116 mg/kg for alpha-tocopherol, and in the cortex 3.5 mg/kg for retinol and 182 mg/kg for alpha-tocopherol. These results clearly indicate that one should take precautions when analyzing retinol and alpha-tocopherol in polar bear kidneys. Prior to analysis, the renculi should be separated into medulla and cortex. The results indicated no significant differences between renculi from different parts of the kidney.
description: The kidney of the male polar bear weighed 599.6 g in total and consisted of 47 separate renculi. Ten renculi (7 polar, 3 medial) were divided into cortex and medulla (excl. papilla), which were then analyzed separately for vitamins A (retinol) and E (a-tocopherol) content. The values for polar and medial renculi vitamin concentrations are based on an average of the values found for medulla and cortex in each renculi. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
description: Supplement to: Bechshøft, Thea Ø; Jakobsen, Jette; Sonne, Christian; Dietz, Rune (2011): Distribution of vitamins A (retinol) and E (alpha-tocopherol) in polar bear kidney: Implications for biomarker studies. Science of the Total Environment, 409(18), 3508-3511
DOI: 10.1594/pangaea.888556
title: Meteorological synoptical observations from station Ishigakijima (2018-02)
DOI: 10.1594/pangaea.898483
title: Radiosonde measurements from station Bondville (2018-10)

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.719641
title: Radiosonde measurements from station Desert Rock (2004-02)

description: If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.898498
title: Water level and storage changes of Aqqikkol 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 EGM96, 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.834356
title: Ceilometer raw data measured at Neumayer Station (2011-02), links to files
DOI: 10.1594/pangaea.898499
title: Water level and storage changes of Ayakkum 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.934113
title: Age determination of Bagna and Stazka peat core from Poland

description: 14C and 210Pb age determination 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.814578
title: (Table 3b) Results of K-Ar measurements in Upper Vendian clayey rocks of the Russian Platform from the borehole Kepina_775
DOI: 10.1594/pangaea.904555
title: Table SM-25: ODP Site 138-849 GRA-estimated CaCO3 %
DOI: 10.1594/pangaea.934908
title: Age determination of Mer Bleue (MB) peat core from Canada

description: 14C and 210Pb age determination of a high-resolution peat core from the Past Global Changes - Carbon in Peat on EArth through Time (PAGES_C-PEAT) Project.