cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.936585
title: Age determination of Joey_core12 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.
DOI: 10.1594/pangaea.762088
title: (Table 4) Chemistry of plagioclase from ODP Site 124-770 basement rocks

description: Sediment depth is given in mbsf. Fe3+/Fe2+ partitioning according to Papike et al. (1974)
DOI: 10.1594/pangaea.822774
title: Meteorological measurements in the upper air at station Ilmala, 1934-09-10 to 1935-06-20, ERA-CLIM ID 5505
DOI: 10.1594/pangaea.819740
title: (Table 4) Abundances of elements enhanced by over a factor of 100 in the pyrite-containing fractions, relative to the Cretaceous calcareous at DSDP Hole 62-465A

description: Empty cells mean no data.
DOI: 10.1594/pangaea.819794
title: Radiocarbon dating of profile ETO
DOI: 10.1594/pangaea.755187
title: Physical properties of sediment core JR141_VC428
DOI: 10.1594/pangaea.833143
title: Physical oceanography during HEINCKE cruise HE203/1
DOI: 10.1594/pangaea.901488
title: Beach profile data for the Elwha River Delta, 2011-03-20

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.901493
title: Beach profile data for the Elwha River Delta, 2011-05-18

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).
description: Portions of these data have been published previously, including in Gelfenbaum et al. 2015.
DOI: 10.1594/pangaea.667658
title: Basic measurements of radiation at station Bermuda (1992-12)
DOI: 10.1594/pangaea.497719
title: Physical oceanography from BT during cruise U58JR01990B_1982
DOI: 10.1594/pangaea.819710
title: (Table 4) Diagenetic characteristics of radiolarians and foraminifers at DSDP Leg 62 Holes

description: Sediment depth is given in mbsf. Empty cells and - mean no data.
DOI: 10.1594/pangaea.495169
title: Water temperature MBT profiles from cruise U0639276M_1971
DOI: 10.1594/pangaea.838245
title: (Table 1) Total length, lipid content and liver siloxane concentrations in Atlantic cod (Gadus morhua) and shorthorn sculpin (Myxocephalus scorpius) sampled around Svalbard in 2009
DOI: 10.1594/pangaea.819711
title: (Table 5) Chemistry of cherts, porcellanites, and siliceous carbonates of DSDP Leg 62 Holes

description: Other elements were scanned, but are below the limits of detection (in parentheses in ppm): As (&lt; 100), Au(&lt; 7), Be (&lt;0.7), Bi (&lt;7), Cd (&lt;7), La(&lt;7), Nb (&lt;7), Pb (&lt;7), Pd (
DOI: 10.1594/pangaea.938369
title: Freshwater cultured pearls from Kentucky Lake - Table S2

description: This Dataset serves as supplementary table S2 for our publication (Farfan et al, 2021). It contains all of the mineralogical, oxygen isotope, and Kentucky Lake environmental data compiled for the study, set into nacre-transect space defined by the SIMS-pits taken during oxygen isotope analyses.
description: The pearls are cut in half and the data is sub-sampled from those timeframes. The pearls themselves were collected at the latest 'Approximate Date' for each transect, namely 1996-10-16 for Pearl 1, 1996-09-30 for Pearl 2, 2002-11-25 for Pearl 3."T:L" in last 4 columns relates to Translational (T) and Librational (L) Raman spectroscopy modes in carbonates.
DOI: 10.1594/pangaea.746881
title: Meteorological observations during ASSURANCE cruise started at 1752-05-17
DOI: 10.1594/pangaea.667791
title: Basic measurements of radiation at station Bermuda (2004-01)
DOI: 10.1594/pangaea.704865
title: (Table 3) Stable oxygen and carbon isotope ratios of benthic foraminifera from ODP Hole 167-1014A

description: Age model folows Lyle et al. (1998, doi:10.2973/odp.proc.ir.167.1997). Size fraction of benthic foraminifera &gt;150 µm
DOI: 10.1594/pangaea.659131
title: Benthic foraminifera distribution of sediment core BP01-62/06
DOI: 10.1594/pangaea.786570
title: (Table 1) Stable isotope ratios of Globigerinoides ruber and pore water, and Cl measurement at ODP Hole 133-817C

description: The oxygen isotopic composition of pore waters squeezed from sediments in Hole 817C co-varies with the oxygen isotopic composition of Globigerinoides ruber below 8 mbsf. The magnitude of the variation in the pore water d18O is approximately 30% of the variation in the foraminifers. Overall, the d18O of the pore waters increases down the core, a trend that is also present in the Cl- concentrations. The variations in the d18O of pore waters may be the result of either of two phenomena. First, these may reflect original variations in the waters, the magnitude of which has been subsequently reduced by process of diffusion. Second, these may reflect recrystallization of the precursor sediment and isotopic exchange between the fluids and the recrystallized sediment. At the moment data are not available to ascertain which process is responsible although the correlation between the Cl- and the d18O data suggests that these values reflect the original composition modified by diffusion.
description: Supplement to: Swart, Peter K (1993): Comparisons between the oxygen isotopic composition of pore water and Globigerinoides ruber in sediments from Hole 817C. In: McKenzie, JA; Davies, PJ; Palmer-Julson, A; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 133, 481-487
DOI: 10.1594/pangaea.497128
title: Physical oceanography from BT during cruise M90IEB_1990
DOI: 10.1594/pangaea.819826
title: (Table 1) Compressional-wave velocities at DSDP Hole 62-465A
DOI: 10.1594/pangaea.777467
title: (Table T4) Mineral and foraminifer composition of sediments across the Paleocene/Eocene Thermal Maximum of ODP Hole 198-1211C
DOI: 10.1594/pangaea.659080
title: Frequency distributions of Siphonodictyon cruzi spicule dimensions (Schönberg, in review); sample no. ZMA POR 05194 (holotype)

description: See also doi:10.1594/PANGAEA.658974 for primary data
DOI: 10.1594/pangaea.887820
title: Sea ice drift, surface temperature, and barometric pressure from autonomous measurements from buoy 2016P18, deployed during POLARSTERN cruise PS96 (ANT-XXXI/2)

description: Sea ice drift, surface temperature, and barometric pressure were measured by Surface Velocity Profiler 2016P18 drifting on Antarctic sea ice. The buoy was deployed on multi year ice without drogue during POLARSTERN cruise ANT-XXXI/2 (PS96). The time series describes the position and additional parameters of the buoy between 18 Jan 2016 and 22 Aug 2017 in sample intervals of 1 hour. The data set has been processed, including the removal of obvious inconsistencies (missing values).
DOI: 10.1594/pangaea.752028
title: Meteorological observations during SCIPIO cruise from Colombo to Batavia started at 1786-12-01
DOI: 10.1594/pangaea.939859
title: Plio-Pleistocene environmental magnetic data from ODP Site 967, Eastern Mediterranean

description: Here we present a bulk sediment isothermal remanence magnetism record (“IRM900@120mT”) from ODP site 967, measured using a 2-G Enterprises cryogenic magnetometer. The IRM900@120mT proxy represents isothermal remanence magnetism after imparting a 900 mT induction in a direct current field, followed by alternating field (AF) demagnetization in a peak 120 mT field. The record spans the last 5 million years at high sampling resolution (every 1 cm downcore).
description: Caution values in sediment slump interval in Hole A sections 6H5-110 to 7H4-60 and in Hole B sections 7H4-114 to 7H5-63 (equivalent to 62.83 to 63.82 metres CCSF-offspl depth).
DOI: 10.1594/pangaea.659129
title: Daily precipitation sums from meteorological station Waru, Indonesia

description: Project: The Impact of ENSO on Sustainable Water Management and the Decision-Making Community at a Rainforest Margin in Indonesia (IMPENSO), http://www.gwdg.de/~impenso, subproject C: The socio-economic impact of ENSO; funded by German Ministry of Education and Research (BMBF) within the framework of the German Climate Research Program DEKLIM, http://www.deklim.de
DOI: 10.1594/pangaea.752540
title: Meteorological observations during TRYAL cruise from St. Augustine to Charlestown started at 1764-05-09
DOI: 10.1594/pangaea.744254
title: Physical oceanography during Helland Hansen cruise HH72/1 to the North Sea
DOI: 10.1594/pangaea.772274
title: (Table A5) Geochemistry of amphibole of ODP Leg 125 peridotites

description: Further geochemical data see Ishii et al., 1992, dataset: doi:10.1594/PANGAEA.770907
DOI: 10.1594/pangaea.663408
title: Oceanography at CTD/bottle station IFREMER_0248
DOI: 10.1594/pangaea.875276
title: Sea ice drift, surface temperature, and barometric pressure from autonomous measurements from buoy 2015P17, deployed during POLARSTERN cruise PS96 (ANT-XXXI/2)

description: Sea ice drift, surface temperature, and barometric pressure were measured by Surface Velocity Profiler 2015P17 drifting on Antarctic sea ice. The buoy was deployed on first year ice without drogue during POLARSTERN cruise PS96 (ANT-XXXI/2). The time series describes the position and additional parameters of the buoy between 23 Dec 2015 and 02 Sep 2016 in sample intervals of 1 hour. The data set has been processed, including the removal of obvious inconsistencies (missing values).
DOI: 10.1594/pangaea.901523
title: Beach profile data for the Elwha River Delta, 2012-07-17

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.848315
title: Basic measurements of radiation at station Xianghe (2014-04)
DOI: 10.1594/pangaea.692344
title: Concentrations of chlorophyll-alpha in sea water from the euphotic zone at Station JUNE-94-GN3619940280200560 in the Aegean Sea

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore. 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.692369
title: Concentrations of chlorophyll-alpha in sea water from the euphotic zone at Station SEPT-94-GN3619940280300960 in the Aegean Sea

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore. 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.747099
title: Meteorological observations during SWALLOW cruise started at 1751-09-01
DOI: 10.1594/pangaea.844520
title: (Table 2) Quantitative analyses of planktonic foraminifera in sediment core UM94PC31
DOI: 10.1594/pangaea.666072
title: Oceanography at CTD/bottle station IFREMER_2898
DOI: 10.1594/pangaea.747805
title: Meteorological observations during CARYSFORT cruise from Jamaica to Spithead started at 1773-05-24
DOI: 10.1594/pangaea.934448
title: Age determination of Harberton Bog (PAT-HB-2010) peat core from Patagonia

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) Projec
DOI: 10.1594/pangaea.658980
title: Spicule dimensions of Siphonodictyon sp.; sample no. MNHN DT 2533

description: dentified by E. Topsent as 'Cliona nodosa'. Recognised as a new species and tentatively identified as S. minakestrum by C. Schönberg. All measurements are of mature, fully formed oxeas, but smaller sample size does not allow statistical comparison with other samples. Measurements conducted by C. Schönberg on tissue preparation made by E. Topsent. Data are sorted vertically by spicule width.
DOI: 10.1594/pangaea.849072
title: Annotated record of the detailed examination of Mn deposits from the HMS Challenger stations

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.
DOI: 10.1594/pangaea.824036
title: Reflectance spectroscopy and colorimetry from IODP Hole 320-U1336A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.901520
title: Beach profile data for the Elwha River Delta, 2012-05-22

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.
DOI: 10.1594/pangaea.870444
title: Temperature and current measurements in the Weddell Sea at mooring site D2

description: Additional information in:Østerhus, S., and R. A. Krause (1990), Ausbringung und Bergung von ozeanographischen Verankerungen. Die Expedition ANTARKTIS-V mit FS ''Polarstern'' 1986/87, Berichte zur Polarforschung, 57.Nordlund, N. (1992), Bottom currents at the Continental slope in the Southern Weddell Sea (in Norwegian), Cand.Sci. thesis, Univ. of Bergen, Bergen.
DOI: 10.1594/pangaea.827193
title: Spatially explicit estimates of length and biomass of Clupea harengus (Norwegian spring spawning herring) from acoustic and trawl surveys in the North-East Atlantic in May 2007

description: Acoustic estimates of herring and blue whiting abundance were obtained during the surveys using the Simrad ER60 scientific echosounder. The allocation of NASC-values to herring, blue whiting and other acoustic targets were based on the composition of the trawl catches and the appearance of echo recordings. To estimate the abundance, the allocated NASC -values were averaged for ICES-squares (0.5° latitude by 1° longitude). For each statistical square, the unit area density of fish (rA) in number per square nautical mile (N*nm-2) was calculated using standard equations (Foote et al., 1987; Toresen et al., 1998). To estimate the total abundance of fish, the unit area abundance for each statistical square was multiplied by the number of square nautical miles in each statistical square and then summed for all the statistical squares within defined subareas and over the total area. Biomass estimation was calculated by multiplying abundance in numbers by the average weight of the fish in each statistical square then summing all squares within defined subareas and over the total area. The Norwegian BEAM soft-ware (Totland and Godø 2001) was used to make estimates of total biomass.
description: The research leading to these results received (partial/full) funding from the European Commission FP7 EURO-BASIN (European Basin-Scale Anal ysis, Synthesis, and Integration; Grant Agreement 264 933).
DOI: 10.1594/pangaea.737106
title: (Figure 12) Concentration of fish debris in the sand fraction from ODP SITE 175-1085
DOI: 10.1594/pangaea.773474
title: (Table 1) Summary of horizon, lithology, and paleomagnetic of ODP Hole 126-791B basaltic mousse samples

description: A paleomagnetic study was made on the highly vesiculated basaltic tuff breccia (the basaltic mousse) drilled by Ocean Drilling Program Leg 126 from the Izu-Bonin backarc, Sumisu Rift, to estimate the mode of its emplacement. Thirty-four 10-cm**3 minicore samples were collected from almost all the horizons of the basaltic mousse. Stepwise thermal and alternating-field demagnetization experiments show that the natural remanent magnetizations of many samples are mainly composed of a single stable component. Although remanence inclinations are not expected to be disturbed by rotary drilling, the measured inclinations of remanence show a random directional distribution as a whole. The remanence inclinations, however, show directional consistency on a smaller scale. High-density sampling and measurements from a limited interval of drilled cores, and the measurement of small disks cut from a single minicore sample show that there is directional consistency over several centimeters. Strong and stable remanent magnetization, the existence of remanence direction consistency, and the fresh lithology of the samples suggest the thermal origin of remanence. Combining the paleomagnetic results with other geological, petrographical, and paleontological characters, the Hole 791B basaltic mousse can be interpreted as a subaqueous explosion breccia produced by deep-sea pyroclastic fountaining.
description: Supplement to: Koyama, Masato; Cisowski, Stanley M; Gill, James B (1992): Paleomagnetic estimate of emplacement mechanisms of deep basaltic volcaniclastic rocks in the Sumisu Rift, Izu-Bonin Arc. In: Taylor, B; Fujioka, K; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 126, 371-379
DOI: 10.1594/pangaea.749175
title: Meteorological observations during El Septentrión cruise from St. Cathalina to Montevideo started at 1777-10-26
DOI: 10.1594/pangaea.819009
title: (Figure 3 and Figure 7) X-ray fluorescence scanning of sediment core GeoB13832-2
DOI: 10.1594/pangaea.737109
title: (Figure 13) Contribution of terrigenous material in ODP Site 175-1085
DOI: 10.1594/pangaea.737110
title: (Figure 13) Contribution of terrigenous material in ODP Hole 175-1086A
DOI: 10.1594/pangaea.737114
title: (Figure 14) Concentration of glauconite in ODP Hole 175-1087C