cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.901624
title: Beach profile data for the Elwha River Delta, 2017-05-31

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.900819
title: Expanded measurements from Neumayer Station (2018-08), Version 1

description: 99999: No clouds detected; Version 1 with some values missing at 10000m CBH, please use new version (see "Replaced by" reference)
DOI: 10.1594/pangaea.913023
title: Pluviographic observations of rainfall at station WMO_28647
DOI: 10.1594/pangaea.692206
title: Particulate organic carbon and nitrogen concentrations in water samples collected at Station MAY-1995-D4 in the Cretan Sea
DOI: 10.1594/pangaea.778114
title: Meteorological synoptical observations from station Tateno (2012-01)
DOI: 10.1594/pangaea.747379
title: Meteorological observations during AMSTERDAM cruise from Algoa Baai to the Netherlands started at 1818-03-13
DOI: 10.1594/pangaea.729973
title: (Table 18) Distribution of trace elements in sediments from the Galapagos hydrothermal Mound Field
DOI: 10.1594/pangaea.845222
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE355/2, Cuxhaven - Bremerhaven, 2011-04-30 - 2013-05-02
DOI: 10.1594/pangaea.705075
title: Other measurements at 300 m from station Boulder (2006-06)
DOI: 10.1594/pangaea.667954
title: Basic measurements of radiation at station Boulder (1997-01)
DOI: 10.1594/pangaea.677823
title: Ozone measurements from station Tamanrasset (2000-09)
DOI: 10.1594/pangaea.901626
title: Beach profile data for the Elwha River Delta, 2017-07-21

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.778115
title: Radiosonde measurements from station Tateno (2012-01)
DOI: 10.1594/pangaea.901627
title: Beach profile data for the Elwha River Delta, 2017-07-22

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.687211
title: Chlorophyll a in three size fractions from bottle APRIL-2000-K1

description: Separate filtration through polycarbonate Millipore filters having porosities 0.2 (total stock), 1.2 and 3.0µm.
DOI: 10.1594/pangaea.729974
title: (Table 20) Mineral composition of sediments from the Meiji Guyot at DSDP Site 19-192
DOI: 10.1594/pangaea.750217
title: Meteorological observations during La Perla cruise from Cádiz to Cartagena started at 1823-02-10
DOI: 10.1594/pangaea.760021
title: Physical oceanography during HEINCKE cruise HE349
DOI: 10.1594/pangaea.752108
title: Meteorological observations during S-GRAVENHAGE cruise from Batavia to Brouwershaven started at 1848-01-06
DOI: 10.1594/pangaea.843281
title: Other measurements at 10 m from station Darwin (2010-10)

description: Version 2, 2015-02-26
DOI: 10.1594/pangaea.896306
title: North Atlantic Oscillation winter index reconstructed from Lamb weather types over 1781-1996

description: A winter (DJFM) North Atlantic Oscillation index (NAOi) has been reconstructed over the peridod 1781-1996 by calibrating the winter frequencies of Lamb weather types to the winter PC-based NAOi of Hurrell (1995, doi:10.1126/science.269.5224.676).The data file contains 4 columns: year of JFM, NAOi, uncertainty (1 std), number of unclassified days over this winter.The NAOi has no unit since regressed to a normalised index. Note that this index has not been renormalised (to an average value of zero and standard deviation of 1).The number of unclassified days directly affects the reliability and consistency of the NAOi. For instance, Delaygue et al. (2018) require less than 24 unclassified days per winter to consider the NAOi.
DOI: 10.1594/pangaea.706848
title: Basic measurements of radiation at station Kwajalein (2008-02)
DOI: 10.1594/pangaea.749150
title: Meteorological observations during El Rey cruise from La Habana to La Coruña started at 1777-08-12
DOI: 10.1594/pangaea.695020
title: Concentrations of chlorophyll-alpha in water of the Ionian Sea at Station MARCH-2000-IRI15

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.694983
title: Concentrations of particulate organic carbon in water of the Aegean Sea at Station FEBR-1998-IR50
DOI: 10.1594/pangaea.843591
title: Geochemistry of North Sea sediment core JC077-VC10
DOI: 10.1594/pangaea.901643
title: Beach profile data for the Elwha River Delta, 2018-06-12

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.677824
title: Ozone measurements from station Tamanrasset (2000-10)
DOI: 10.1594/pangaea.680299
title: Other measurements at 300 m from station Boulder (2002-08)
DOI: 10.1594/pangaea.705405
title: Basic measurements of radiation at station Boulder (2006-09)
DOI: 10.1594/pangaea.668833
title: Basic measurements of radiation at station Carpentras (1998-07)
DOI: 10.1594/pangaea.749355
title: Meteorological observations during FRANKENDAAL cruise from Rotterdam to Spitsbergen started at 1788-04-29
DOI: 10.1594/pangaea.751956
title: Meteorological observations during Santa Maria Magdalena cruise from Cádiz to Cádiz started at 1779-06-22
DOI: 10.1594/pangaea.877148
title: Continuous water level observations at station BEFmate_I3low (2016-02)
DOI: 10.1594/pangaea.677825
title: Ozone measurements from station Tamanrasset (2000-11)
DOI: 10.1594/pangaea.876856
title: Continuous light intensity observations at station BEFmate_S3low (2016-07)
DOI: 10.1594/pangaea.822465
title: Meteorological measurements in the upper air at station Buhta Varneka, 1937-09-11 to 1938-03-23, ERA-CLIM ID 4723
DOI: 10.1594/pangaea.885775
title: Age at length data for larval African halfbeak Hyporhamphus picarti (Hemiramphidae) in the Sine Saloum estuary, Senegal

description: The African halfbeak Hyporhamphus picarti (Hemiramphidae) is one of the most abundant species within the ichthyoplankton community of the Sine Saloum estuary (Senegal). A year-round occurrence of larvae suggests that the Sine Saloum is an important spawning habitat for this species. Annual fluctuations in water temperature, however, can have severe impacts on the survival probabilities of marine fish larvae. To determine whether temperature has an effect on the growth of H. picarti during its larval development, larval age at length and somatic growth rates were investigated for two contrasting spawning seasons in 2014: February (cold season, 20.8°C) and June (warm season, 26.4°C). H. picarti larvae were sampled at two stations inside the Saloum River using two vertically connected neuston nets (30 × 15 cm, 500 µm mesh size). The nets were attached to a catamaran (Hobie Cat 15), which was towed by a motorboat at a speed of two to three knots. Fish larvae were fixed immediately after the haul with a 30% ethanol/sea water solution and stored in an electric cooling box. At the laboratory, fish larvae were successively transferred to 50% and 70% ethanol. Water temperatures (°C) and salinities (practical salinity scale) were determined at each station with a multiprobe (WTW 3430). Larval standard lengths (SL ± 0.01 mm) were measured using a calibrated stereomicroscope micrometre (Stemi SV 11 and Stemi 2000-C, Zeiss). The sagittal otoliths were dissected and stored in immersion oil for several days. In order to assess the age of H. picarti larvae at a given length, otolith daily growth increments were counted (core to edge) along the otolith's largest diameter using a stereo microscope (Axioskop, Zeiss) at 200-500× magnification. Increments were counted three times by the same reader, and counter read once by an additional reader. If the results of the counts of both persons deviated by more than one increment, the respective otolith was discarded. Otolith diameter was measured using ImageJ 1.49 (Rasband, WS, US National Institutes of Health, Bethesda, MD, http://imagej.nih.gov/ij/).
description: Supplement to: Döring, Julian; Neumann, Sarah Isabel; Sloterdijk, Hans; Ekau, Werner (2018): Seasonal growth differences of larval Hyporhamphus picarti (Hemiramphidae) in the Sine Saloum estuary, Senegal. Journal of Applied Ichthyology, 34(1), 97-102
DOI: 10.1594/pangaea.843616
title: Porewater geochemistry of North Sea sediment core JC077-VC12
DOI: 10.1594/pangaea.777309
title: (Table 1) Major element composition of ODP Sites 127-794 and 127-795 sediments
DOI: 10.1594/pangaea.777388
title: Basic measurements of radiation at station Cener (2011-11)
DOI: 10.1594/pangaea.750072
title: Meteorological observations during La Cantabria cruise from La Coruña to Montevideo started at 1779-04-20
DOI: 10.1594/pangaea.793255
title: (Appendix B Table 3) Calcareous nannofossil biohorizons of ODP Hole 167-1012A

description: DEPTH, sediment is given in mcd.
DOI: 10.1594/pangaea.901584
title: Beach profile data for the Elwha River Delta, 2015-01-30

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.880483
title: Meteorological synoptical observations from station Ishigakijima (2017-07)
DOI: 10.1594/pangaea.786498
title: (Table 1) Age model of DSDP Site 21-210
DOI: 10.1594/pangaea.877145
title: Continuous water level observations at station BEFmate_I3low (2015-11)
DOI: 10.1594/pangaea.842284
title: Other measurements at 10 m from station Darwin (2004-03)

description: Version 3, 2015-02-04
DOI: 10.1594/pangaea.876861
title: Continuous light intensity observations at station BEFmate_S3low (2017-01)
DOI: 10.1594/pangaea.465116
title: Physical properties of sediment core MD03-2685
DOI: 10.1594/pangaea.876777
title: Continuous light intensity observations at station BEFmate_I3pio (2016-02)
DOI: 10.1594/pangaea.756743
title: (Table 5) Biostratigraphic and paleomagnetic events at ODP Hole 117-731A
DOI: 10.1594/pangaea.901605
title: Beach profile data for the Elwha River Delta, 2016-06-08

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.788714
title: (Table 3C) DSDP Site 82-563 age from model 1

description: Unconformity at 270.5 m from age (Ma) 18.4-19.4. Sediment depth is given in mbsf.
DOI: 10.1594/pangaea.843617
title: Porewater geochemistry of North Sea sediment core JC077-VC14
DOI: 10.1594/pangaea.777390
title: Basic measurements of radiation at station Cener (2012-01)
DOI: 10.1594/pangaea.883943
title: Stable isotope record from snow pit South_Pole_S78C
DOI: 10.1594/pangaea.720894
title: Documentation of sediment core GIK23506-1
DOI: 10.1594/pangaea.876862
title: Continuous light intensity observations at station BEFmate_S3low (2017-02)
DOI: 10.1594/pangaea.741105
title: Lithology of sediment core AELBI, Älbi Flue, Switzerland

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.876778
title: Continuous light intensity observations at station BEFmate_I3pio (2016-03)
DOI: 10.1594/pangaea.741135
title: Lithology of sediment core BADENTAR, Badentarbat, United Kingdom

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.741137
title: Lithology of sediment core BALDEGG, Baldeggersee, Switzerland

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.901546
title: Beach profile data for the Elwha River Delta, 2013-07-22

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.