cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.898507
title: Water level and storage changes of Dogaicoring Qangco 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.901509
title: Beach profile data for the Elwha River Delta, 2012-01-27

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.901522
title: Beach profile data for the Elwha River Delta, 2012-07-05

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.879221
title: (Figure 3) Dust flux determined from peat core MOHOS in the Eastern Carpathians, Romania
DOI: 10.1594/pangaea.898508
title: Water level and storage changes of Donggei 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 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.495928
title: Water temperature MBT profiles from cruise U90M_1970
DOI: 10.1594/pangaea.901608
title: Beach profile data for the Elwha River Delta, 2016-08-18

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).
DOI: 10.1594/pangaea.901547
title: Beach profile data for the Elwha River Delta, 2013-07-23

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.898514
title: Water level and storage changes of Hoh Xil 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.898518
title: Water level and storage changes of Langa 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.753533
title: Documentation of sediment core GeoB14615-1
DOI: 10.1594/pangaea.898523
title: Water level and storage changes of Memar 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.898532
title: Water level and storage changes of Rola 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.900374
title: Tethered balloon-borne turbulence measurements during the Arctic field campaign PAMARCMiP (Balloon_20180403_1657_2044)
DOI: 10.1594/pangaea.760161
title: Curie temperatures and cell edges of ODP Leg 120 samples (Table 1)

description: Basalt samples recovered on Ocean Drilling Program Leg 120 from the Kerguelen Plateau were investigated by thermomagnetic analysis, X-ray diffraction, and ore microscopy. The basement samples could be divided into two groups based on Curie temperatures, cell-edge parameters, and optical magnetic mineralogy. Samples from Sites 748 and 750 underwent only low-temperature oxidation and displayed Curie temperatures for the titanomaghemites that ranged from 340° to 395°C. The basalts from Sites 747 and 749 mainly experienced high-temperature oxidation. High-temperature oxidation produced titanium-poor titanomagnetites with ilmenite-exsolution lamellae. Curie temperatures of the deuterically oxidized titanomaghemites varied from 490° to 620°C.
description: Supplement to: Heider, Franz; Geiss, Christoph; Dunlop, David J; Inokuchi, Hiroo (1992): Rock-Magnetic investigation of basalts from the southern Kerguelen Plateau (Leg 120). In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 79-87
DOI: 10.1594/pangaea.898538
title: Water level and storage changes of Tu 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.898539
title: Water level and storage changes of Urru 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.898931
title: Effect of atorvastatin on the neutral red retention of blue mussels, Mytilus edulis

description: Increasing concentration of biologically active pharmaceutical compounds can affect marine organisms. The bioavailability and environmental stability of these compounds make them potential threat to these organisms, specially the sessile organisms. We have examined the effects of atorvastatin, a globally prescribed drug, on the blue mussels – Mytilus edulis. In this data set, we presents the effect of atorvastatin (ATO) on the membrane properties, detoxification and biotransformation enzyme activities of Mytilus edulis.
DOI: 10.1594/pangaea.903336
title: Calcareous nannofossils absolute abundance and accumulation rates from Cabo Mondego, Portugal
DOI: 10.1594/pangaea.904650
title: Pollen record of surface samples from mire Pastlingsee in Niederlausitz, Brandenburg, Germany
DOI: 10.1594/pangaea.548102
title: Nutrients and bacteria measured on water bottle samples at station Chip_2003-09-13_14, Chipana, Chile
DOI: 10.1594/pangaea.552444
title: Physical oceanography at stations E1 and E2, Atenas, Independence Bay, Peru (2004)
DOI: 10.1594/pangaea.904899
title: (Dataset 1) Pliocene alkenone unsaturation index (Uk37) and SST anomalies of ODP site 167-1012

description: *** Change history *** in September 2021 it was found, that the ages in all "Dataset 1" datasets were declared here as being in "ka BP" but they were actually in "Ma". To correct this error all ages were recalculated (*1000) to fit the unit "ka BP".
DOI: 10.1594/pangaea.904913
title: (Dataset 1) Pliocene alkenone unsaturation index (Uk37) and SST anomalies of DSDP site 90-593

description: *** Change history *** in September 2021 it was found, that the ages in all "Dataset 1" datasets were declared here as being in "ka BP" but they were actually in "Ma". To correct this error all ages were recalculated (*1000) to fit the unit "ka BP".
DOI: 10.1594/pangaea.900622
title: High resolved snow height measurements at Neumayer Station, Antarctica, 2018

description: At Neumayer-Station in Antarctica snow height is permanently monitored with a laser distance meter. The instrument measures continuously since 2013-01-01 and is located in the vicinity of the Air Chemical Observatory Neumayer. By design, the sample area of the surface is on the order of a few millimetre in diameter. Long-term trends of the measured snow height are strongly correlated with accumulation on the ice shelf at a horizontal scale of several kilometres. Short-term trends reflect dynamic changes of the surface and can be used to deduce information on surface roughness.
DOI: 10.1594/pangaea.691305
title: Stable carbon and oxygen istotope ratios of Oligocene foraminifera from ODP Hole 121-758A of the northern Ninetyeast Ridge, Indian Ocean (Appendix 1)

description: An Oligocene-basal Miocene (Zones P19-P22/N4) oxygen and carbon isotope stratigraphy is presented based on mixed benthic foraminiferal faunas and different species of planktic foraminifers from Eastem Indian Ocean ODP Hole 758A. Lack of covariance in planktic and benthic delta18O ratios indicates that many Oligocene sea level fluctuations, including the major fall at 30 Ma, are not of glacio-eustatic origin. Delta18O values suggest that test morphology is a poor indicator of preferred depth habitat of Oligocene planktic foraminifers. Also, some groups show considerable shifts in preferred depth habitat. Reconstructed surface water temperature was nearly constant during the investigated period, but even assuming a large Antarctic icecap, values are unrealistically low, 18°-20°C. Most likely, water masses with markedly different oxygen isotopic composition existed, this poses great problems for quantitative temperature reconstructions.Planktic foraminiferal species show similar delta13C ratios, indicating well-mixed surface waters. This contrasts with the strong oxygen isotopic gradient, which suggests well-stratified surface waters. During the Oligocene the difference in delta13C ratio between the average ratio of planktic foraminiferal species and the benthic foraminifers (Delta delta13C P-B') shows an inverse relation with the known circulation intensity record and thus with productivity. This Delta delta13C pattern is interpreted as being caused by the presence of younger bottom waters at this site during periods with lower temperatures and/or larger Antarctic ice sheets.
description: Test sizes &gt;250 µm, plus some important 125-250 µm species from selected samples.
description: Supplement to: van Eijden, AJM; Ganssen, Gerald M (1995): An Oligocene multi-species foraminiferal oxygen and carbon isotope record from ODP Hole 758A (Indian Ocean): paleoceanographic and paleo-ecologic implications. Marine Micropaleontology, 25(1), 47-65
DOI: 10.1594/pangaea.805705
title: (Table 8) Major and trace element compositions of chilled margins from ODP Hole 140-504B

description: Cations calculated on the basis of 6 oxygens.
DOI: 10.1594/pangaea.826406
title: Magnetic remanence from IODP Hole 329-U1366F

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.904925
title: (Dataset 2) Pliocene sea-surface temperature anomalies of the mid-latitudes
DOI: 10.1594/pangaea.902590
title: Monthly sea surface temperature derived from in situ observations offshore L'Estartit (NW Mediterranean) since 1974

description: In-situ sea temperatures have been obtained using two Richter and Wiese protected reversing thermometers mounted on a Nansen bottle. Temperature readings, after correction according to the thermometer's calibration certificates are averaged if the temperature difference among thermometers is lower than 0.2°C and repeated otherwise, so that the accuracy can be set to be lower than 0.2°C. Thermometers are periodically controlled at facilities of the Marine Research Institute (ICM) in Barcelona against a high precision Pt100. which, in turn is annually controlled using Ga and pure H2O melting points.
DOI: 10.1594/pangaea.903700
title: Respiration and grazing rates in the estuarine eelgrass sea hare, Phyllaplysia taylori
DOI: 10.1594/pangaea.496980
title: Physical oceanography from BT during cruise M90B300042B_1987
DOI: 10.1594/pangaea.748197
title: Hydrography on standard level calculated from water bottle samples of RV New Liscard in 1962
DOI: 10.1594/pangaea.903701
title: Defecation rates in the estuarine eelgrass sea hare, Phyllaplysia taylori
DOI: 10.1594/pangaea.902604
title: Monthly sea level anomaly based on 2h data from L'Estartit meteorological station II (NW Mediterranean) since 1990

description: Sea Level is obtained by a mechanical sea gauge device attached to a continuous graphical recorder. The record is digitized at 2h intervals and the originals preserved for detailed analyses if necessary. The position is periodically georeferenced by the Catalan Cartographic Institute (ICC) every ~5 years and data is backwards linearly corrected for each period.
DOI: 10.1594/pangaea.727670
title: Lithology, colour and structural description of sediment profile L7-15, Appendix 6.1
DOI: 10.1594/pangaea.902644
title: Monthly averaged air temperature based on ~8h data from L'Estartit meteorological station I (NW Mediterranean) since 1971

description: Atmospheric parameters (air temperature and precipitation) have been measured in a meteorological box with standard instruments certified and regularly checked by the Spanish Meteorological Office (AEMET). These observations have been included in the official AEMET weather observation network. Readings are reported every 8h.
DOI: 10.1594/pangaea.902793
title: Ice nucleating particle data from winter 2018 at Jungfraujoch

description: Immersion INP spectra from snow, cloud rime, and time- and size-resolved aerosol samples collected during the Ice Nucleation Characterization in the Alps of Switzerland (INCAS) study which took place from 15 February to 11 March 2018 in the Sphinx observatory at Jungfraujoch (46.55 N, 7.98 E; 3580 m above sea level (m a.s.l.).
description: Supplement to: Creamean, Jessie; Mignani, Claudia; Bukowiecki, Nicolas; Conen, Franz (2019): Using freezing spectra characteristics to identify ice-nucleating particle populations during the winter in the Alps. Atmospheric Chemistry and Physics, 19(12), 8123-8140
DOI: 10.1594/pangaea.817562
title: (Table 1) Composition of dispersed organic matter (fauna excluded) at DSDP Leg 67 Hole

description: Empty cells = not observed.
DOI: 10.1594/pangaea.745996
title: (Table 6) Chemical composition of glasses from ODP Hole 107-650A
DOI: 10.1594/pangaea.754622
title: (Table 3) Stable carbon and oxygen isotopic composition of the fine fraction of ODP Site 114-704

description: Fine fraction = &lt;63 µm.
DOI: 10.1594/pangaea.908406
title: Continuous sediment temperature observations at station BEFmate_S3low (2018-01)