cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.901537
title: Beach profile data for the Elwha River Delta, 2013-04-01

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.901545
title: Beach profile data for the Elwha River Delta, 2013-07-12

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).
description: Portions of these data have been published previously, including in Gelfenbaum et al. 2015.
DOI: 10.1594/pangaea.747174
title: Meteorological observations during Admiraal Evertsen cruise from Coastal East India to Coastal East India started at 1816-09-04
DOI: 10.1594/pangaea.751952
title: Meteorological observations during Santa María de la Caveza cruise from Cádiz to Estrecho de Magallanes started at 1785-10-10
DOI: 10.1594/pangaea.663809
title: Oceanography at CTD/bottle station IFREMER_0649
DOI: 10.1594/pangaea.495222
title: Water temperature XBT profiles from cruise U18X121124_1978
DOI: 10.1594/pangaea.498877
title: Physical oceanography from BT during cruise U90X007995B_1925
DOI: 10.1594/pangaea.746975
title: Meteorological observations during Le Chariot Royal cruise from Rochefort to Québec started at 1751-06-27
DOI: 10.1594/pangaea.751075
title: Meteorological observations during PALLAS cruise from St. Eustatius to St. Maarten started at 1830-10-18
DOI: 10.1594/pangaea.810047
title: (Table 2) Geochronology at DSDP Hole 44-391
DOI: 10.1594/pangaea.810336
title: (Table 2) Lipid class compositions of the arctic ctenophore Mertensia ovum from Kongsfjorden, Svalbard

description: Percentages are mass % of total lipids.
DOI: 10.1594/pangaea.750035
title: Meteorological observations during La Belle Poule cruise from Brest to Cádiz started at 1771-06-20
DOI: 10.1594/pangaea.750774
title: Meteorological observations during MERSEY cruise from Bermuda to Staten Island started at 1821-05-08
DOI: 10.1594/pangaea.750500
title: Meteorological observations during LOISEAU cruise from Simons Bay to Madras started at 1797-06-28
DOI: 10.1594/pangaea.816208
title: EPS, rbar and associated statistics
DOI: 10.1594/pangaea.477885
title: Hydrochemistry measured on water bottle samples at station SPac_1971_HH_150-100W/27

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.690392
title: (Table 4) Middle Eocene to Oligocene radiolarian bioevents of ODP Hole 120-749B from the southern Indian Ocean

description: Based on raw data of Takemura (1992) doi:10.2973/odp.proc.sr.120.177.1992, data sets: doi:10.1594/PANGAEA.690423
DOI: 10.1594/pangaea.871373
title: Table S10 - Bulk stable isotope data ODP Site 208-1263
DOI: 10.1594/pangaea.869223
title: Ozone measurements from station Lindenberg (2008-03)
DOI: 10.1594/pangaea.725352
title: (Table 3) Mineralogy of Fe-Mn segregations from island arcs in the West Pacific
DOI: 10.1594/pangaea.751790
title: Meteorological observations during ROMNEY cruise from Road Torn Tortola to Nore started at 1804-06-27
DOI: 10.1594/pangaea.497242
title: Physical oceanography from BT during cruise M90TC00034B_1989
DOI: 10.1594/pangaea.498356
title: Physical oceanography from BT during cruise U90A208086B_1986
DOI: 10.1594/pangaea.751103
title: Meteorological observations during PANTHER cruise from Plymouth to St. Johns started at 1771-06-14
DOI: 10.1594/pangaea.746743
title: Analyses of gashydrates from DSDP Sites 76-533 and 84-568 (Table 1)

description: Two sites of the Deep Sea Drilling Project in contrasting geologic settings provide a basis for comparison of the geochemical conditions associated with marine gas hydrates in continental margin sediments. Site 533 is located at 3191 m water depth on a spit-like extension of the continental rise on a passive margin in the Atlantic Ocean. Site 568, at 2031 m water depth, is in upper slope sediment of an active accretionary margin in the Pacific Ocean. Both sites are characterized by high rates of sedimentation, and the organic carbon contents of these sediments generally exceed 0.5%. Anomalous seismic reflections that transgress sedimentary structures and parallel the seafloor, suggested the presence of gas hydrates at both sites, and, during coring, small samples of gas hydrate were recovered at subbottom depths of 238m (Site 533) and 404 m (Site 568). The principal gaseous components of the gas hydrates wer methane, ethane, and CO2. Residual methane in sediments at both sites usually exceeded 10 ml/l of wet sediment. Carbon isotopic compositions of methane, CO2, and SumCO2 followed parallel trends with depth, suggesting that methane formed mainly as a result of biological reduction of oxidized carbon. Salinity of pore waters decreased with depth, a likely result of gas hydrate formation. These geochemical characteristics define some of the conditions associated with the occurrence of gas hydrates formed by in situ processes in continental margin sediments.
description: Supplement to: Kvenvolden, Keith A (1985): Comparison of marine gas hydrates in sediments of an active and passive continental margin. Marine and Petroleum Geology, 2(1), 65-71
DOI: 10.1594/pangaea.756744
title: (Table 6) Biostratigraphic and paleomagnetic events at ODP Hole 117-723A
DOI: 10.1594/pangaea.762100
title: (Table 4) Trace-element chemistry of the basaltic rocks from ODP Hole 124-768C
DOI: 10.1594/pangaea.862194
title: GPS-derived precipitable water vapor content calculated for station CALL
DOI: 10.1594/pangaea.496293
title: Water temperature MBT profiles from cruise U90X097099M_1975
DOI: 10.1594/pangaea.780457
title: (Table T4) Reworked diatoms and sponge spicules in ODP Hole 188-1165B sediments

description: Sediment depth is given in mbsf. Abundance estimate as follows: F = few, R = rare, X = present, - = absent. Abundance letter followed by 'r' = out of known biostratigraphic range and interpreted as reworked.
DOI: 10.1594/pangaea.499652
title: Physical oceanography from BT during cruise U99XX00369B_1973
DOI: 10.1594/pangaea.836620
title: Velocity measurements of the Äußeres Hochebenkar (Ötztal, Tyrolian Alps, Austria), link to appendix
DOI: 10.1594/pangaea.809979
title: (Table 2) Geochemistry at DSDP Hole 76-534A

description: One analysis of the Miocene nannofossil carbonates of the Great Abaco Member and three of the Upper Cretaceous black shales from the Hatteras Formation are included for comparison.
DOI: 10.1594/pangaea.680290
title: Other measurements at 300 m from station Boulder (2001-11)
DOI: 10.1594/pangaea.496550
title: Water temperature XBT profiles from cruise U99X115577_1994
DOI: 10.1594/pangaea.750811
title: Meteorological observations during MIÑO cruise from Cádiz to Cádiz started at 1794-10-08
DOI: 10.1594/pangaea.901535
title: Beach profile data for the Elwha River Delta, 2013-02-05

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.497840
title: Physical oceanography from BT during cruise U58X001013B_1953
DOI: 10.1594/pangaea.664378
title: Oceanography at CTD/bottle station IFREMER_1219
DOI: 10.1594/pangaea.496336
title: Water temperature MBT profiles from cruise U90X110056M_1986
DOI: 10.1594/pangaea.494638
title: Physical oceanography during cruise INW31NWIXXC
DOI: 10.1594/pangaea.495316
title: Water temperature MBT profiles from cruise U31X022194M_1968
DOI: 10.1594/pangaea.476141
title: Hydrochemistry measured on water bottle samples at station IndianOcean_1979_9W_12S/16

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.680262
title: Other measurements at 300 m from station Boulder (1999-07)
DOI: 10.1594/pangaea.664200
title: Oceanography at CTD/bottle station IFREMER_1041
DOI: 10.1594/pangaea.901526
title: Beach profile data for the Elwha River Delta, 2012-08-28

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.901534
title: Beach profile data for the Elwha River Delta, 2013-01-11

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.863066
title: Annotated record of the detailed examination of Mn deposits from ARA Islas Orcadas Cruise 7 core stations

description: The purpose of this volume, the seventh in a series of similar publications (Goodell, 1964, 1965, 1968; Frakes 1971, 1973 ; Cassidy et al., 1977), is to continue a presentation to the research community of sediment core descriptions and attendant data of cored and otherwise obtained sediments retrieved in waters of the Southern Ocean aboard the research vessel, ARA Islas Orcadas (formerly, USNS Eltanin), as a part of the circumpolar survey begun by Eltanin in 1962 (see issue of Antarctic Journal of the United States, Vol. 8, No. 3, 1973). The data presented herein are concerned with the results of coring activities aboard cruise 0775 of Islas Orcadas, the second marine geology coring cruise of this vessel under the terms of the present United States-Argentine agreement. The core descriptions are organised as follows: 1) a brief summary of the coring objectives of the cruise, together with a discussion of core recovery; 2) a table and map of station location data for materials retrieved; 3) a table of tentative age-dates for each piston core; 4) an explanation of the laboratory procedures and descriptive criteria used in the description of the sediments, and 5) lithologic descriptions of the piston and trigger cores, and the piston and trigger core bag samples.
description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: Cassidy, D S; Ciesielski, Paul F; Kaharoeddin, F A; Sherwood, WW; Zemmels, I (1977): ARA Islas Orcadas Cruise 0775 Sediment descriptions. Antartic Research Facility, Department of Geology, Florida Sate University, Tallahassee, Florida, Contribution No. 45, 82 pp
DOI: 10.1594/pangaea.663183
title: Oceanography at CTD/bottle station IFREMER_0022
DOI: 10.1594/pangaea.758905
title: (Table 6) Age model of ODP Site 120-748
DOI: 10.1594/pangaea.664417
title: Oceanography at CTD/bottle station IFREMER_1257
DOI: 10.1594/pangaea.733186
title: Physical oceanography during Cromwell cruise HOT-44 on section PRS2
DOI: 10.1594/pangaea.665363
title: Oceanography at CTD/bottle station IFREMER_2203
DOI: 10.1594/pangaea.857388
title: (Table 1) Cd/Ca and Mn/Ca ratios of benthic foraminifera of sediment core V30-49
DOI: 10.1594/pangaea.778229
title: (Table 1) Geothermal measurements during ODP Legs 127 and 128

description: Sediment depth gives the deepest temperature point used to calculate gradients.
DOI: 10.1594/pangaea.753680
title: (Table 3) Comparison of hydrocarbon gas concentrations at ODP 104-644A

description: ODP = results from shipboard laboratory, USGS = results from US Geology Survey shore-base laboratory.
DOI: 10.1594/pangaea.680261
title: Other measurements at 300 m from station Boulder (1999-06)
DOI: 10.1594/pangaea.821801
title: Length changes of Austrian glaciers 1992/1993
DOI: 10.1594/pangaea.901512
title: Beach profile data for the Elwha River Delta, 2012-03-05

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.901513
title: Beach profile data for the Elwha River Delta, 2012-03-15

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.