cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.901603
title: Beach profile data for the Elwha River Delta, 2016-04-11

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).
DOI: 10.1594/pangaea.759194
title: Physical oceanography during LANCE cruise LA97/3
DOI: 10.1594/pangaea.855245
title: Description of a manganese nodule collected on the Breitgrund flat, Germany

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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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.880028
title: Physical oceanography (CTD) during Meteor cruise M15/1

description: :Conventions = 'CF-1.6, OceanSites Manual-1.3, EGO glider users manual 1.3, ACDD-1.3':netcdf_version = '3.5':GEOMAR_netcdf_version = '6':GEOMAR_po_svn_global_revision_when_writing = 368:Conventions_comment = 'this file is not strict according to OceanSites, EGO, or ACDD':Metadata_Conventions = 'Unidata Dataset Discovery v1.0':format_version = '1.3':standard_name_vocabulary = 'CF-1.6, v19':featureType = 'profile':cdm_data_type = 'Station':coverage_content_type = 'physicalMeasurement':nodc_template_version = 'NODC_NetCDF_Profile_Orthogonal_Template_v1.0'
DOI: 10.1594/pangaea.759188
title: Physical oceanography during Johan Hjort cruise JH98/7
DOI: 10.1594/pangaea.883667
title: Chemical composition of manganese nodules from the Southern Ocean using wet chemical analysis (2)

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.680127
title: Other measurements at 30 m from station Solar Village (1999-04)
DOI: 10.1594/pangaea.780711
title: (Supplement Table 1) Chemical compositions of plagioclase grains in lavas collected from ODP Leg 187 sites

description: Standard deviation always 1 sigma.
DOI: 10.1594/pangaea.855095
title: (Table 2, pages 117), Elemental concentrations of Mn concretions from the sediment surface at site G (Lake Biwa, Japan)

description: Values are based on freeze-dried materials.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.756509
title: Tab. 1: Field measurements of magnetic susceptibility of selected FT samples
DOI: 10.1594/pangaea.855586
title: Mixed layer depth in the global ocean
DOI: 10.1594/pangaea.884031
title: (Table 2) Branched GDGTs in core lipid fractions of lakes in Minnesota and Iowa
DOI: 10.1594/pangaea.680134
title: Other measurements at 30 m from station Solar Village (1999-11)
DOI: 10.1594/pangaea.855403
title: Basic measurements of radiation at station Xianghe (2011-03)
DOI: 10.1594/pangaea.759845
title: (Table 2) Chemical analyses of sapropels from different ODP Leg 107 holes
DOI: 10.1594/pangaea.838333
title: (Table SI-3) Concentrations of alpha- and gamma-hexachlorocyclohexane in high volume air samples during CCGS Amundsen cruises in the Canadian Arctic 2007-2008

description: Please note: exact sample positions could not be obtained.
DOI: 10.1594/pangaea.855598
title: Microplankton fraction in global ocean
DOI: 10.1594/pangaea.892663
title: Pollen counts from short monoliths (FRK III and FRK IV) blanket bog at Connemara National Park, Letterfrack, Co. Galway, Ireland

description: Analyst: Michael O'ConnellLaboratory: Palaeoenvironmental Research Unit, NUI Galway, Galway, IrelandData analysis completed: 1987Sampling in field: 1985-08-20. Sample density: variable; mainly 2 cm intervals.Depths datum = peat/mineral soil interface; nominal depths used to facilitate plottingPollen preparation: Lycopodium spore suspension of know concentration added; acetolysis, mounted in glycerinePollen identification and counting: Cereal-type pollen differentiated using Beug (1961) criteria (37 um taken as cutoff point; but only pollen grains 40 um and greater included in cereal-type). Pollen nomenclature generally follows Moore et al. 1991. &lt;1 = recorded outside the pollen counts (most samples searched for additional taxa). Myrica and Corylus distinguished. Charcoal particles ≥37 um counted during routine pollen counting.
DOI: 10.1594/pangaea.733174
title: Physical oceanography during Wecoma cruise HOT-32 on section PRS2
DOI: 10.1594/pangaea.855404
title: Basic measurements of radiation at station Xianghe (2011-04)
DOI: 10.1594/pangaea.911931
title: Macrofaunal abundance retrieved from 24 subtropical mudflats along south-east Queensland, Australia

description: The datasets represent the observed abundance of macrofauna (retained on a 0.5mm mesh sieve) retrieved from 24 subtropical mudflats along the south-east coast of Australia in 25cm x 25cm box cores and 50cm x 50cm quadrats (to a sediment depth of 11cm). Sites were located between south Deception Bay and Tallebudgera, Gold Coast. Sampling was carried out in winter 2016 (July-August) and summer 2017 (January-February). The summer assemblages contained more species, more individuals and had differing taxonomic composition. The 24 sites were categorised into four land-use sub-catchments e.g. high industry, low industry, residential and peri-urban (see paper for categories and site classifications).
DOI: 10.1594/pangaea.763086
title: Tab. 4: Ranges of nutrient concentrations in Antarctic lakes and ponds
DOI: 10.1594/pangaea.855200
title: Description of manganese nodules collected by HMAS Kimbla during its 1979 Southern Tasman Sea expedition

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.911029
title: Underway CTD data collected during METEOR cruise M131/1
DOI: 10.1594/pangaea.733048
title: Physical oceanography during Moana Wave cruise AC-1

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.884033
title: (Table 3) Branched GDGTs in intact polar lipid fractions of lakes in Minnesota and Iowa
DOI: 10.1594/pangaea.742483
title: (Table 9) Chemical composition of seawater at the Yucatan Polygon
DOI: 10.1594/pangaea.886727
title: Cereal pollen statistics for CRG peat-soil short monoliths

description: Measurements given below in µm (not as no. of divisions on a measuring graticule (d) as in the case of the short monoliths). 1 in size fraction indicates a record but grain size not measured (because grain folded, etc.). #1 indicates a record outside the count
DOI: 10.1594/pangaea.728970
title: Zooplankton abundance measured on Apstein net samples during cruise CISKA2005

description: Apstein net, meshsize 200 µm
DOI: 10.1594/pangaea.757308
title: (Table 4) Analyses of thermogenic gas-hydrated sediments
DOI: 10.1594/pangaea.783658
title: (Table T3) Diatom valve abundance and total organic carbon content of ODP Holes 186-1150B and 186-1151A
DOI: 10.1594/pangaea.759239
title: Chemical compositions of monomineral fractions from Fe-Mn crusts and of their host rocks, seamounts of the Sea of Japan

description: It has been established (with use of analytical electron microscopy) that Fe-Mn crusts from two seamounts of the Sea of Japan consist predominantly of an association of birnessite minerals including Ca-birnessite and clinobirnessite. The latter is represented by twins, which form regular integrowths with 14 Å Ca-birnessite. Ore material from the third seamount (Tarasov submarine volcano) consists only of fibrous todorokite, which forms spherulitic nodules, blocks, and laminar formations. Its chemical composition is close to that of todorokite from the Galapagos rift zone.
description: Supplement to: Gorshkov, Anatoly I; Berezovskaya, V V; Baturin, Gleb N; Sivtsov, Alexander V (1992): The nature of the iron-manganese crusts from seamounts in the Sea of Japan. Oceanology, 32(3), 364-369
DOI: 10.1594/pangaea.771757
title: (Table 10.4.2) Total abundance of bacteria, CO2 assimilation- and methane oxidation rates in water samples collected within the Rainbow hydrothermal field, in the smoke zone above active hydrothermal vents
DOI: 10.1594/pangaea.680155
title: Other measurements at 30 m from station Solar Village (2001-08)
DOI: 10.1594/pangaea.884568
title: Ichthyoplankton composition from SUDEPE cruise 8, Southern Brazilian Shelf, in 1976

description: The cruises of this series were carried out by the "Superintendência de Desenvolvimento da Pesca" (SUDEPE), through the "Grupo Especial para Execução de Pesquisas Marítimas e Lacustres" (GEEPMAL) from the state of Rio Grande do Sul, with support from the "Programa de Desenvolvimento Pesqueiro do Brasil" (PDP). Ichthyoplankton was obtained during 14 exploratory demersal fishing cruises, carried out in 1970, 1971 and 1976 by the Mestre Jerônimo and Cruz Del Sur Research Ships. Because they represent a continuity of sampling during the same time of year, cruises 1, 2 and 3 of 1970 were aggregated in a single cruise (SUDEPE_1, Winter), cruises 7 and 8 of 1970 (SUDEPE_2, Spring), cruises 1 and 2 of 1971 (SUDEPE_3, Winter), cruises 3 and 4 of 1971 (SUDEPE_4, Spring) , and cruises 5 and 6 of 1976 (SUDEPE_8, Winter).In the cruises conducted in 1970 and 1971 two sampling strategies were used. Horizontal trawls of 5 min duration, at 4-5 m depth and at a speed of 3 knots, using Gulf net of 0.18 m of mouth diameter and 500 µm mesh. Vertical trawls with 0.70 m diameter Nansen net and 500 µm mesh, from 50 m depth to the surface, or from the bottom at stations with depths of less than 50 m (Weiss et al. , 1976; Weiss & Souza, 1977). In the cruises made in 1976 the horizontal trawls were obtained at 8 m depth, and only in the first (SUDEPE_5, Summer) were horizontal and vertical trawls conducted. The samples of the cruises 5 and 6 of 1976 (SUDEPE_8) were obtained by the Cruz Del Sur Research Ship through vertical trawls with a conical net of 0.50 m in diameter and 200 µm mesh, from 50 m depth to the surface, or from the bottom at stations with depths less than 50 m (Weiss & Souza, 1977). The volume of filtered water in each trawl was calculated from the measurements obtained from the flowmeter coupled in the nets, and used to standardize the abundance of eggs and fish larvae per 100 m3 of filtered water.
DOI: 10.1594/pangaea.759967
title: (Table 1) Bubble sizes in waters of the Atlantic Ocean from results of measurements aboard R/V Professor Vize
DOI: 10.1594/pangaea.821672
title: Physical oceanography from IBTs to the Arctic Ocean
DOI: 10.1594/pangaea.680143
title: Other measurements at 30 m from station Solar Village (2000-08)
DOI: 10.1594/pangaea.767444
title: Tab. 1: Results of chemical and isotope analyses
DOI: 10.1594/pangaea.855388
title: European lobsters (Homarus gammarus) captured around the rocky island of Helgoland (German Bight, North Sea) in 2008
DOI: 10.1594/pangaea.759280
title: (Table 1) Composition of free fumarole gases of underwater hydrotherms from the Bay of Plenty in 1990
DOI: 10.1594/pangaea.855391
title: European lobsters (Homarus gammarus) captured around the rocky island of Helgoland (German Bight, North Sea) in 2011
DOI: 10.1594/pangaea.759575
title: (Table 1) Content of rare earth elements in standard samples of Fe-Mn ocean ores measured by ICP-MS
DOI: 10.1594/pangaea.902602
title: (Table S1) Representative geochemistry of metamorphic phases from IODP Exp366 samples

description: Cations pfu calculated on the basis of 6 O for Cpx, 14 O for Chl, 11 O for Prh, 12 O for Pmp, 11 O for Ph, 8 O for Lws, 23 O for Gln.Abbreviations: Chl, chlorite; Cpx, clinopyroxene; Gln, glaucophane; Lws, lawsonite; pfu, per formula unit; Ph, phengite; Pmp, pumpellyite; Prh, prehnite.
DOI: 10.1594/pangaea.707900
title: Calcium isotope composition of marine carbonates
DOI: 10.1594/pangaea.855392
title: European lobsters (Homarus gammarus) captured around the rocky island of Helgoland (German Bight, North Sea) in 2012
DOI: 10.1594/pangaea.680171
title: Other measurements at 30 m from station Solar Village (2002-12)
DOI: 10.1594/pangaea.744595
title: (Table 1) Chemical composition of basalts from the rift valley of the Knipovich Ridge
DOI: 10.1594/pangaea.728910
title: (Table T16) Secondary minerals in fine fraction sampled from igneous rocks: Middle Valley, Juan de Fuca Ridge and Escanaba Trough, Gorda Ridge, Legs 139 and 169, X-ray diffraction data
DOI: 10.1594/pangaea.915062
title: Rate- and state-dependent friction parameters from velocity-step tests, Aging law
DOI: 10.1594/pangaea.755372
title: (Table 10) Group composition and yield of methyl esters of oxidation products of humic acids from bottom sediments of the Western Pacific
DOI: 10.1594/pangaea.759494
title: (Table 3) Sr, Pb, and Nd isotopic compositions in ODP Leg 121 samples

description: For Sr and Nd isotopic composition, the measured ratios are given with the 2sigma m (2 sigma on the mean of the measurement), whereas for Pb, the 2 sigma precision is &lt;0.l % for 2 0 6Pb/204Pb and 207Pb/204Pb and &lt;0.15% for 2 08Pb/204Pb. Measured ratios are normalized to 86Sr/88Sr = 0.1194 for Sr isotopic ratios and to 146Nd/144Nd = 0.7219 for Nd isotopic ratios. For Pb, a mass-fractionation correction factor of 0.13% ± 0.04% per atomic mass unit was applied to all the isotopic ratios, on the basis of 72 analyses of the NBS 981 Pb standard. The "initial" ratios were calculated at 38 Ma for Site 756, 58 Ma for Site 757, and 88 Ma for Site 758 (Peirce, Weissel, et al., 1989, doi:10.2973/odp.proc.ir.121.1989; R. A. Duncan, pers. comm., 1990). "Initial" 87Sr/86Sr ratios were calculated for unleached samples on the basis of their XRF-measured Rb and Sr concentrations. Assuming a comparable 87Rb/86Sr range (0 to 0.467) in the acid-leached samples to that in the unleached samples, the corresponding maximum corrections for 38, 58, and 88 Ma are, respectively, 0.00025, 0.00038, and 0.00058 for the 87Sr/86Sr ratios, which is significant, but will not change the general interpretation of the origin of Ninetyeast Ridge. The correction factors are much smaller for Nd because of the longer half-life of 147Sm in comparison with 87Rb (1.53*10**11 and 7.04*10**10yr).
DOI: 10.1594/pangaea.755408
title: (Table 1) Abundance of radiolarians in the surface layer of bottom sediments from the Peru-Chile trench and shelf

description: Two radiolarian assemblages are distinguished: an equatorial sub-assemblage of the tropical assemblage in the East Pacific Ocean, which differs somewhat from association of radiolarians in the western part of the ocean, and an assemblage close to transitional one between the tropical and the boreal. The latter is characterized by presence of considerable number of species typical for cold-water regions. Some criteria are presented for distinguishing radiolarian associations in nearshore regions from similar associations in regions of the open ocean.
description: Supplement to: Kruglikova, Svetlana B (1981): Radiolarians in the surface layer of bottom sediments in the eastern part of the Pacific Ocean's tropical zone. Oceanology, 21(3), 359-363
DOI: 10.1594/pangaea.780632
title: (Table A1) General characteristics of studied samples from IODP Holes 204-U1309D and 305-U1309D
DOI: 10.1594/pangaea.887250
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2011403

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.763980
title: (Table 2) Production characteristics of phytoplankton in the Kara Sea in September 2007
DOI: 10.1594/pangaea.920200
title: 87Sr/86Sr in pore fluids from different Holes of IODP Site 355-U1456 and U1457 in the Arabian Sea Monsoon

description: The radiogenic strontium isotopic composition of pore fluids from two sites drilled during IODP Expedition 355 Arabian Sea Monsoon. We report data from Site U1456 (n=21) and U1457 (n=20). Three distinct zones are identified, similar at both sites.
DOI: 10.1594/pangaea.777524
title: (Table 1) Nd and Sr isotopic analyses of ODP Leg 127 basalts

description: Sr and Nd isotopic compositions are reported for basaltic rocks collected during ODP Leg 127 from the Yamato Basin, a rifted backarc basin in the Japan Sea. The basalts are classified into two groups in terms of Nd isotopic composition: the upper sills at Site 797 are characterized by higher 143Nd/144Nd ratios (0.513083-0.513158, epsilon-Nd = 8.68-10.14) and the basalts from Site 794 and the lower sills at Site 797 have lower 143Nd/144Nd ratios (0.512684-0.512862, epsilon-Nd = 0.90-4.37). All of the basalts show higher Sr isotopic compositions than those of the mantle array, which is attributed to seawater alteration. The basalts with lower Nd isotopic values ranging in age from 20.6 to 17.3 Ma have tapped an enriched subcontinental upper mantle (SCUM) with the minor involvement of a depleted asthenospheric mantle (AM). Subsequent change in composition through the physical replacement of SCUM by AM yielded the basalts of the upper sills of higher Nd isotopic compositions. This event within the upper mantle was associated with the breakup of the overlying lithosphere during the rifting of the Japan Sea backarc basin.
description: epsilon-Sr and epsilon-Nd determined following DePaolo and Wasserburg (1979). 87Sr/86Sr bulk earth = 0.7045 and I(0)CHUR = 0.512638.
description: Supplement to: Nohda, Susumu; Tatsumi, Yoshiyuki; Yamashita, Shigeru; Fujii, Toshitsugu (1992): Nd and Sr isotopic study of Leg 127 basalts: implications for the evolution of the Japan Sea Backarc Basin. In: Tamaki, K; Suychiro, K; Allan, J; McWilliams, M; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 127/128(2), 899-904
DOI: 10.1594/pangaea.811080
title: (Table 2) Cytochrome P450-mediated enzyme activity in liver samples of black-legged kittiwake (Rissa tridactyla) and northern fulmar (Fulmarus glacialis) chicks
DOI: 10.1594/pangaea.771831
title: (Table 1a) Mineral composition of airborne material from yellow snow fallen in the Russian North on March 25-26, 2008
DOI: 10.1594/pangaea.785202
title: (Table 1) Molecular composition and isotope ratios of gases from gas pockets of ODP Site 131-808
DOI: 10.1594/pangaea.772380
title: Hydrochemistry measured on water bottle samples during cruise Gromkii1968

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.858135
title: Body condition indices of Asian green mussels, Perna viridis, from Indonesia

description: While part of a single country, the Indonesian archipelago covers several biogeographic regions, and the high levels of national shipping likely facilitate transfer of non-native organisms between the different regions. Two vessels of a domestic shipping line appear to have served as a transport vector for the Asian green mussel Perna viridis (Linnaeus, 1758) between regions. This species is indigenous in the western but not in the eastern part of the archipelago, separated historically by the Sunda Shelf. The green mussels collected from the hulls of the ferries when in eastern Indonesia showed a significantly lower body condition index than similar-sized individuals from three different western-Indonesian mussel populations. This was presumably due to reduced food supply during the ships' voyages. Although this transportinduced food shortage may initially limit the invasive potential (through reduced reproductive rates) of the translocated individuals, the risk that the species will extend its distributional range further into eastern Indonesia is high. If the species becomes widely established in eastern Indonesia, there will then be an increased risk of incursions to Australia, where the mussel is listed as a high-priority pest species.
description: Mussels were collected between 0.5 m and 2 m depths at all stations.
description: Supplement to: Huhn, Mareike; Zamani, Neviaty P; Lenz, Mark (2015): A ferry line facilitates dispersal: Asian green mussels Perna viridis (Linnaeus, 1758) detected in eastern Indonesia. 4(1), 23-29
DOI: 10.1594/pangaea.771832
title: (Table 1b) Clay mineral composition of airborne material from yellow snow fallen in the Russian North on March 25-26, 2008
DOI: 10.1594/pangaea.772294
title: (Table III.4.4) Sedimentation rate of ferruginous (hydrogoethite-chamosite) shelf sediments of the Atlantic Ocean near the Congo River mouth
DOI: 10.1594/pangaea.736218
title: Meteorological synoptical observations from station Lindenberg (1999-12)