cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.694554
title: Temperature and salinity in the water column of the Ionian Sea at Station MARCH-2000-IRI38

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.694560
title: Temperature and salinity in the water column of the Ionian Sea at Station MARCH-2000-IRI42

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.782534
title: (Table 2) Geochemistry of pore waters from sediments obtained during Tender Oste research cruise, Baltic Sea

description: Assumption was made that gamma/l is equal to µg/l.
DOI: 10.1594/pangaea.821382
title: (Table 2) Geochemistry and minerals at DSDP Hole 58-442A

description: Normative values based on Fe2O3/FeO ratio of 0.15. Empty cells mean no data.
DOI: 10.1594/pangaea.908565
title: (Figure 4) Annually averaged and smoothed ICP-MS Fe measurements (1780-2006) on ice core KCC from Colle Gnifetti

description: Dataset corresponds to Figure 4 in the final manuscript. Annually averaged ICP-MS Fe measurements from 1780-2006 C.E. and smoothed ICP-MS Fe measurements.
DOI: 10.1594/pangaea.804705
title: Basic measurements of radiation at station Tiksi (2010-11), Version 2

description: Version 2, 2013-01-04, please refer to new version from 2016 (see "Replaced by" reference)
DOI: 10.1594/pangaea.666060
title: Oceanography at CTD/bottle station IFREMER_2886
DOI: 10.1594/pangaea.671789
title: Basic measurements of radiation at station Regina (1995-09)
DOI: 10.1594/pangaea.819726
title: (Table 2) Bulk geochemistry of sediments at DSDP Hole 62-464

description: # = Value below detection limit; total iron was calculated as Fe2O3, and total manganese as Mn3O4; CaCO3 was calculated using the total CaO.
DOI: 10.1594/pangaea.870506
title: Geochemistry of loess-paleosol sequence Zilly
DOI: 10.1594/pangaea.672126
title: Radiosonde measurements from station South Pole (1994-09)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.821338
title: (Table 9) Geochemistry, recalculated by excluding carbonates, residual materials, water, and salts at DSDP Hole 58-444
DOI: 10.1594/pangaea.694543
title: Temperature and salinity in the water column of the Ionian Sea at Station MARCH-2000-IRI30

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.858579
title: Average composition manganese concretions in the Oacoma manganese deposit in South Dakota

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.819738
title: (Table 2) Major-element, bromine, and strontium abundances at DSDP Hole 62-465A

description: Empty cells mean no data.
DOI: 10.1594/pangaea.694727
title: Temperature and salinity in the water column of the Ionian Sea at Station MARCH-2000-IKE6A

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.671625
title: Nutrients measured on water bottle samples off Chipana, Chile, winter 2006
DOI: 10.1594/pangaea.859277
title: (Table 3, page 158-159), Electron microprobe data for the oxide matrix of Fe-Mn micronodules from the Alpha Ridge, Central Arctic Ocean

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.671790
title: Basic measurements of radiation at station Regina (1995-10)
DOI: 10.1594/pangaea.884092
title: XRF, carbon and CaCO3 data from the loess-paleosol sequence Süttö, Hungary

description: This study provides a detailed geochemical record of one of the most detailed loess-paleosol sequence (LPS) in Hungary covering Marine Isotope Stage (MIS) 6 to MIS 2. Süttő is situated in the northwestern Carpathian Basin at the transition between oceanic and continental climate. We investigated weathering intensity, dust provenance and sedimentation dynamics by high-resolution X-ray fluorescence (XRF) scanning of discrete samples in comparison with quantitative XRF and other published proxy data such as grain-size, magnetic susceptibility and micromorphology. Multivariate statistics unravel pedogenesis in terms of decalcification and grain-size dynamics as processes controlling the elemental composition. Furthermore, high-resolution chemostratigraphy indicates geochemical homogeneity for mature MIS 5 paleosols and the modern soil. Together with the A-CN-K plot providing no hint for K-feldspar weathering, semi-arid continental paleoenvironmental conditions are considered as prevailing. Dust provenance is studied by geochemical reference literature data from potential ultimate dust source areas, Th/metal ratios and comparison with the composition of the upper continental crust (UCC). Results indicate a felsic rock composition and a stable dust source, albeit immediate (adjacent Danube floodplains) and ultimate dust sources (surrounding mountain belts) need to be distinguished. According to the Sr-K-Rb plot, the Austroalpine cover nappes area northwest of Süttő might be the dominant ultimate dust source. The weathering-resistant elements Al, Ti and Zr as well as Zr/metal ratios indicate Zr addition and thus strongest sediment sorting and/ or recycling during MIS 6. Since Al, Ti and Zr show minimal correlations with grain-size, we suggest a cascade-alike transport pathway from ultimate source to sink involving multiple sediment recycling and sorting cycles in both fluvial and eolian domains. Therefore, this study highlights how high-resolution qualitative geochemical data contributes to a better understanding of paleoenvironmental and sedimentation dynamics at LPS. Application of such a versatile geochemical screening tool is of broad interest to the scientific community working on (terrestrial) paleoenvironmental archives that are commonly discretely sampled.
description: Supplement to: Profe, Jörn; Neumann, Lena; Novothny, Ágnes; Barta, Gabriella; Rolf, Christian; Frechen, Manfred; Ohlendorf, Christian; Zolitschka, Bernd (2018): Paleoenvironmental conditions and sedimentation dynamics in Central Europe inferred from geochemical data of the loess-paleosol sequence at Süttő (Hungary). Quaternary Science Reviews, 196, 21-37
DOI: 10.1594/pangaea.704454
title: (Appendix I) Stable carbon and oxygen isotope ratios of Cibicidoides spp. from ODP Site 177-1088 in the sub-Antarctic South Atlantic

description: Age based on calcareous nannofossil biostratigraphic datums (Gersonde et al., 1999, doi:10.2973/odp.proc.ir.177.1999) reported to Berggern et al. (1995) time scale. Depth is composite depth (mcd)
DOI: 10.1594/pangaea.805245
title: Hydrochemistry measured on water samples from Samoylov Island, Lena Delta, northeastern Siberia, in 2008
DOI: 10.1594/pangaea.670624
title: Basic and other measurements of radiation at station Ny-Ålesund (1992-11)
DOI: 10.1594/pangaea.843621
title: Porewater geochemistry of North Sea sediment core JC077-VC23
DOI: 10.1594/pangaea.907570
title: (Table S1a) εNd composition of weakly cleaned foraminifera for MIS M2 from ODP Site 165-999A

description: (a) Composite depth, De Schepper et al. (2013)(b) Age model De Schepper et al. (2013)(c) corrected to Tanaka et al. (2000)(d) corrected for ingrowth of 143Nd, using average Sm/Nd ratio of 0.139 for uncleaned foraminifera (Osborne et al., 2017)
DOI: 10.1594/pangaea.672185
title: Radiosonde measurements from station South Pole (1999-11)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.902219
title: Trace element analyses on single glass shards of tephra OH-DP-2669

description: Uncertainty at a 95% confidence level.NIST SRM 610 refernce values according to Jochum, et al., 2011, doi:10.1111/j.1751-908X.2011.00120.x.T1-G + ATHO-G reference values according to Jochum et al., 2006, doi:10.1029/2005GC001060.
DOI: 10.1594/pangaea.726414
title: (Table 3) Thin section description and mineralogy of ODP Hole 113-692B

description: Mineral percents are based on visual percentages (Terry and Chilingarian, 1955). Size designations are: Major (M) 65%-35%, Common (C), 35%-5%, and Trace (T) &lt;5%
DOI: 10.1594/pangaea.672210
title: Radiosonde measurements from station South Pole (2001-12)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.694524
title: Temperature and salinity in the water column of the Ionian Sea at Station MARCH-2000-IRI14

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.694531
title: Temperature and salinity in the water column of the Ionian Sea at Station MARCH-2000-IRI18

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.690478
title: (Appendix III) Neogene radiolarian events of DSDP Hole 30-289 in the western equatorial Pacific
DOI: 10.1594/pangaea.757072
title: Hydrochemistry measured on water bottle samples during Akademik Vernadsky cruise AV5
DOI: 10.1594/pangaea.671810
title: Basic measurements of radiation at station Regina (1997-06)
DOI: 10.1594/pangaea.784997
title: Thermal conductivity of IODP Hole 333-C0012C

description: Geocode = [m CSF-A] Top Core depth (below sea floor). VLQ laboratory probe, source length is 60 mm and source diameter 2 mm. Measuring range 0.1 - 10 Wm-1K-1.
DOI: 10.1594/pangaea.767626
title: (Table 4) Geochemistry of plagioclase in ODP Site 125-786
DOI: 10.1594/pangaea.664421
title: Oceanography at CTD/bottle station IFREMER_1261
DOI: 10.1594/pangaea.671820
title: Basic measurements of radiation at station Regina (1998-04)
DOI: 10.1594/pangaea.779950
title: (Table 5) Quaternary calcareous nannofossil datums in ODP Hole 130-805C
DOI: 10.1594/pangaea.713730
title: (Table 3) Radiogenic isotope ratios of ODP Site 126-790

description: Pleistocene - Quaternary back-arc rifts. Samples were leached in 3 M HCl for 2 h
DOI: 10.1594/pangaea.670775
title: Physical oceanography of CTD station T7 off Independencia Bay, 2000, Peru
DOI: 10.1594/pangaea.785750
title: (Table 1) Sr-isotope values of representative sediment samples from ODP sites at the Costa Rica margin

description: Two sealed borehole hydrologic observatories (CORKs) were installed in two active hydrogeochemical systems at the Costa Rica subduction zone to investigate the relationship between tectonics, fluid flow, and fluid composition. The observatories were deployed during Ocean Drilling Program (ODP) Leg 205 at Site 1253, ~ 0.2 km seaward of the trench, in the upper igneous basement, and at Site 1255, ~ 0.5 km landward of the trench, in the décollement. Downhole instrumentation was designed to monitor formation fluid flow rates, composition, pressure, and temperature. The two-year records collected by this interdisciplinary effort constitute the first co-registered hydrological, chemical, and physical dataset from a subduction zone, providing critical information on the average and transient state of the subduction thrust and upper igneous basement. The continuous records at ODP Site 1253 show that the uppermost igneous basement is highly permeable hosting an average fluid flow rate of 0.3 m/yr, and indicate that the fluid sampled in the basement is a mixture between seawater (~ 50%) and a subduction zone fluid originating within the forearc (~ 50%). These results suggest that the uppermost basement serves as an efficient pathway for fluid expelled from the forearc that should be considered in models of subduction zone hydrogeology and deformation. Three transients in fluid flow rates were observed along the décollement at ODP Site 1255, two of which coincided with stepwise increases in formation pressure. These two transients are the result of aseismic slip dislocations that propagated up-dip from the seismogenic zone over the course of ~ 2 weeks terminating before reaching ODP Site 1255 and the trench. The nature and temporal behavior of strain and the associated hydrological response during these slow slip events may be an analog for the response of the seaward part of the subduction prism during or soon after large subduction zone earthquakes.
description: Sediment depth is given in mbsf. 87Sr/86Sr of modern seawater = 0.70916.
description: Supplement to: Solomon, Evan A; Kastner, Miriam; Wheat, C Geoffrey; Jannasch, Hans W; Robertson, Gretchen; Davis, Earl E; Morris, Julie (2009): Long-term hydrogeochemical records in the oceanic basement and forearc prism at the Costa Rica subduction zone. Earth and Planetary Science Letters, 282(1-4), 240-251
DOI: 10.1594/pangaea.671847
title: Basic measurements of radiation at station Regina (2000-08)
DOI: 10.1594/pangaea.670782
title: Physical oceanography of CTD station T7 off Independencia Bay, 2007, Peru
DOI: 10.1594/pangaea.672215
title: Radiosonde measurements from station South Pole (2004-04)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.887273
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2012402

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.475953
title: Geochemistry of sediment core MH_10SK from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.818316
title: (Table 1) Sound velocity, wet-bulk density, and acoustic impedance of some indurated sediment from DSDP Leg 64 Holes

description: The Pliocene-Quaternary sediments that we drilled at eight sites in the Gulf of California consist of silty clays to clayey silts, diatomaceous oozes, and mixtures of both types. In this chapter I have summarized various measurements of their physical properties, relating this information to burial depth and effective overburden pressure. Rapid deposition and frequent intercalations of mud turbidites may cause underconsolidation in some cases; overconsolidation probably can be excluded. General lithification begins at depths between 200 and 300 meters sub-bottom, at porosities between 55 and 60% (for silty clays) and as high as 70% (for diatomaceous ooze). Diatom-rich sediments have low strength and very high porosities (70-90%) and can maintain this state to a depth of nearly 400 meters (where the overburden pressure = 1.4 MPa). The field compressibility curves of all sites are compared to data published earlier. Where sediments are affected by basaltic sills, these curves clearly show the effects of additional loading and thermal stress (diagenesis near the contacts). Strength measurements on well-preserved hydraulic piston cores yielded results similar to those obtained on selected samples from standard drilling. Volumetric shrinkage dropped to low values at 100 to 400 meters burial depth (0.3 to 2.0 MPa overburden pressure). Porosity after shrinkage depends on the composition of sediments.
description: Supplement to: Einsele, Gerhard (1982): Mass physical properties of Pliocene to Quaternary sediment in the Gulf of California, Deep Sea Drilling Project Leg 64. In: Curray, JR; Moore, DG; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 64, 529-542
DOI: 10.1594/pangaea.690469
title: Mesozooplankton biomass during Akademik Kovalevsky cruise AK7/5, Part I

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 0.145 mm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-500 m) and closed at the upper depth level. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved in 3-4% buffered formaldehyde and processed on return to the laboratory. All of copepods were identified to genus level, other taxanomic groups - to type, class, order and family levels.
DOI: 10.1594/pangaea.663537
title: Oceanography at CTD/bottle station IFREMER_0377
DOI: 10.1594/pangaea.782989
title: Radiosonde measurements from station Southern Great Plains (2012-01)

description: Launches at irregular time intervals. The radiosonde measurements from station Southern Great Plains are used for Billings and E13
DOI: 10.1594/pangaea.901582
title: Beach profile data for the Elwha River Delta, 2015-01-07

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.694541
title: Temperature and salinity in the water column of the Ionian Sea at Station MARCH-2000-IRI27

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.888372
title: Magnesium, iron, manganese and aluminium to calcium ratio and benthic temperature estimate of sediment core GS15-198-36-CC in the Denmark Strait
DOI: 10.1594/pangaea.804681
title: (Table 2) Experimental phase assemblage and CIPW phase proportions of ODP Holes 152-917A, 152-918D and 163-989B
DOI: 10.1594/pangaea.805342
title: (Table 4) Mineral composition of clays from ODP Hole 161-977A
DOI: 10.1594/pangaea.777852
title: Downhole temperature measurement from IODP Hole 317-U1351A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.897621
title: Geochemical and lithological investigations of sediment core Zuckerfabrik 2
DOI: 10.1594/pangaea.671787
title: Basic measurements of radiation at station Regina (1995-07)