cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.809985
title: (Table 2) Organic residue at DSDP Hole 76-534A

description: The kind, sedimentation rate, and diagenesis of organic particles delivered to the North Atlantic seafloor during the Middle Jurassic-Early Cretaceous were responsible for the presence of carbonaceous sediments in Hole 534A. Organic-rich black clays formed from the rapid supply of organic matter; this organic matter was composed of either abundant, well-preserved, and poorly sorted particles of land plants deposited in clays and silty clays within terrigenous turbiditic sequences (tracheal facies) or abundant amorphous debris (xenomorphic facies) generated through the digestive tracts of marine zooplankton and sedimented as fecal pellets. Evidence for the fecal-pellet origin of xenomorphic debris is illustrated. Black clays were also produced in sediments containing less organic matter as a result of the black color of carbonized particles composing all or most of the residues (micrinitic facies). Slowly sedimented hematitic Aptian clays contain very little carbonized, organic debris that survived diagenetic oxidation. In the red calcareous clay sequence of the Late Jurassic, larger amounts of this oxidized debris turned several clay layers black or blackish red. Carbonized debris also dominates the residues recovered in interbedded black and green Albian clays. Carbonization of organic matter in these sediments either turned them black or provided the diagenetic environment for reduced iron. Carbonized debris is also appreciable in burrow-mottled black-green Kimmeridgian clay. The study of Hole 534A organic matter indicates that during the middle Callovian there was a rapid supply of terrigenous organic matter, followed by a late Callovian episode of rapidly supplied xenomorphic debris deposited as fecal pellets. The Late Jurassic-Berriasian was a time of slower sedimentation of organic matter, primarily of a marine dinoflagellate flora in a poorly preserved xenomorphic facies variously affected by diagenetic oxidation. Several intervals of carbonized tracheal tissue in the Oxfordian and Kimmeridgian suggest episodes of oxidized terrigenous matter. The same sequence of Callovian organic events is evident in much of the Early Cretaceous
description: Supplement to: Habib, Daniel (1983): Sedimentation-rate-dependent distribution of organic matter in the North Atlantic Jurassic-Cretaceous. In: Sheridan, RE; Gradstein, FM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 76, 781-794
DOI: 10.1594/pangaea.718189
title: Radiosonde measurements from station Boulder, SURFRAD (2008-02)

description: Start location: Denver, CO; Distance from radiation site: 40 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.957046
title: Ozone measurements from station Lindenberg (2021-06)
DOI: 10.1594/pangaea.957024
title: Ozone measurements from station Tamanrasset (2023-02)
DOI: 10.1594/pangaea.957042
title: Expanded measurements from station Lindenberg (2021-05)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.957020
title: Meteorological synoptical observations from station Tamanrasset (2023-01)
DOI: 10.1594/pangaea.957023
title: Radiosonde measurements from station Tamanrasset (2023-02)

description: Start location: Tamanrasset; Distance from radiation site: 10 km
DOI: 10.1594/pangaea.957025
title: Meteorological synoptical observations from station Tamanrasset (2023-02)
DOI: 10.1594/pangaea.957047
title: Expanded measurements from station Lindenberg (2021-06)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.718166
title: Radiosonde measurements from station Boulder, SURFRAD (2007-09)

description: Start location: Denver, CO; Distance from radiation site: 40 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.835890
title: Pollen profile PS3A, Nahorany, Czech Republic

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.838110
title: Pollen profile DIMA3, Russia

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.904138
title: Seep-bubble measurement codes

description: Matlab codes for measuring bubble sizes and heights above the seafloor from underwater video footage by manually picking bubble axes. The footage must contain the exit point of the bubbles on the seafloor and a known reference distance on the seafloor (usually in the form of two lasers for most underwater cameras). The geometry of the calculations uses Canadian Grids (Wakefield and Genin, 1987, doi:10.1016/0198-0149(87)90148-8) combined with additional geometry (McGovern, 2012 (thesis)). Uncertainties in the bubble sizes and rise heights come from the amount of bubble deviation towards or away from the camera as it rises. Since this deviation can't be measured, the code contains hard-coded deviation distances that increase with rise height. These deviations were originally measured from a selection of seeps along the Hikurangi Margin New Zealand (Higgs, 2019).
DOI: 10.1594/pangaea.718169
title: Ultra-violet measurements from station Boulder, SURFRAD (2007-10)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-09.
DOI: 10.1594/pangaea.956956
title: Other measurements at 10 m from station Payerne (2022-08)
DOI: 10.1594/pangaea.957039
title: Meteorological synoptical observations from station Lindenberg (2021-05)
DOI: 10.1594/pangaea.896550
title: Updated age model for OMEXII-9K based on recalibrated radiocarbon ages
DOI: 10.1594/pangaea.916438
title: 1-Hz PPP displacements at GEONET station 0234 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.895136
title: Functional composition of hard-bottom-communities in the SW Baltic Sea between 2005-2015
DOI: 10.1594/pangaea.896551
title: Stable silicon isotope ratios of sponge spicules from core OMEXII-9K
DOI: 10.1594/pangaea.477548
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_OC_22S/124

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.511761
title: Physical oceanography and CFC measured on water bottle samples at station M59/2_569
DOI: 10.1594/pangaea.833445
title: (Table S4) Globigerinoides sacculifer Mg/Ca data and temperature estimates for ODP Site 165-999A including Mg/Ca-SSTs corrected for changes in Mg/Casw

description: DEPTH, sediment/rock [m] is given in mbsf. The age model is based on a combination of: LR04 benthic stack-derived ages for the interval 5.0-1.7 Myr (Lisiecki & Raymo 2004), two biostratigraphic models (Chaisson & d'Hondt 2000; Kameo & Bralower 2000) for the period 1700-465 ky, a d18O-based orbital solution (Schmidt et al., 2006) for the past 465 kyr.
DOI: 10.1594/pangaea.782936
title: (Table 1) Pollen analysis of clay-gyttja layers obtained in 1966 near Hitzhusen, north Germany

description: Bereits im Jahre 1956 wurde bei Baugrund-Aufschlußbohrungen für das zweite Kurmittelhaus in Bad Bramstedt bei einer Serie von 11 Bohrungen - ausgeführt durch die Firma Fritz Eising K. G. in Hamburg - in drei benachbart gelegenen Bohrpunkten an der südlichen Ecke des Gebäudes in einer Teufe von ca. 10 m u. T. eine offensichtlich organogene Schicht von ca. 2 m Mächtigkeit erbohrt. Eines dieser Bohrprofile hat folgenden Aufbau: -5,8 m Fein-Mittelsand, -7,7 m Mittelsand, Fein-Mittelkies, -10,0 m Mittelsand, wenig Kies, -12,0 m Gyttja, -15,0 m Mittelsand, Grobsand.Die bereits wiedergegebene Teufenangabe ist insofern recht interessant, als im Jahre 1966 bei der Brücke über die Bramau bei Hitzhusen, demnach in der Talaue der Bramau in einer Teufe von 8,55 m ebenfalls eine Gyttja erbohrt wurde. Die Tiefenlagen beider Vorkommen scheinen sich demnach relativ zu entsprechen. Das gesamte Profil bei Hitzhusen ist in einigen Punkten abweichend ausgebildet und enthält vor allem noch ein zweites Gyttja-Band in 11,25 m Teufe. Im Einzelnen wurde hier durch die Bohrfirma Paul Hammers A. G., Hamburg, diese Schichtfolge angetroffen: -1.55 m Fein-Mittelsand, Humus, -3,10 m Mittel-Grobsand, Kies, Steine, etwas Lehm, -4,50 m Mittel-Grobsand, -7,20 m Mittel-Grobsand, Kies, -8,00 m Grobsand, -8,55 m Grobsand, Kies, -8,65 m Schluff-Gyttja, -9,70 m Fein-Grobsand, -10,25 m Mittel-Grobsand, Kies, -10,75 m Mittel-Grobsand, -11,25 m Mittel-Grobsand, Schluffstreifen, -11,40 m Schluff-Gyttja, -12,10 m Mittelsand, -12,30 m Mittel-Grobsand, Kies, -17,85 m Geschiebemergel.Die gewonnenen Proben der Schluff-Gyttjen wurden näher untersucht. Da es sich in beiden Fällen um geringmächtige Lagen handelt (0,1 m resp. 0,15 m), und das Material durchaus als stark feinsandig bis schluffig zu bezeichnen ist (das spricht für eine wesentlich schnellere Sedimentation, als die einer reinen biogenen Gyttja), ist der Effekt einer 'Mischprobe' weitgehend ausgeschlossen. Außerdem lagen die Proben - obgleich wahrscheinlich mit einem Ventilbohrer gefördert - als relativ ungestörte Brocken mit erhaltengebliebener Feinschichtung vor. Auf den Schichtflächen waren gröbere Pflanzenreste erkennbar (in der Tabelle angegeben). Der sehr hohe mineralische Anteil läßt zunächst den Verdacht auf sekundären Pollen aufkommen. Keines der beiden pollenanalytisch ermittelten Vegetationsbilder liefert dagegen irgendeine Bestätigung hierfür.
description: Abundances are given in absolut numbers.
description: Supplement to: Hallik, R (1968): Interstadiale innerhalb der Sander-Sedimente bei Bad Bramstedt? Meyniana, 18, 9-11
DOI: 10.1594/pangaea.913073
title: Gridded bathymetry from EM122 multibeam echosounder of R/V Meteor cruise M141/1

description: Bathymetry data was acquired during R/V Meteor cruise M141/1 in the Atlantic, off the Azores between 08.09.2017 and 03.10.2017. The cruise was designed to identify the age, source, recurrency intervals and eruptive style of large explosive volcanic eruptions on the Azores islands during the last several hundred thousand years, and to investigate possible links to tsunamigenic sector collapses. CI Citation: Paul Wintersteller (seafloor-imaging@marum.de) as responsible party for bathymetry raw data ingest and approval.Description of data source:During the M141/1 cruise, the hull-mounted KONGSBERG EM122 multibeam echosounder (MBES) was utilized to perform bathymetric mapping in medium to deep waters. Two linear transducer arrays in a Mills Cross configuration transmit acoustic signals of a nominal sonar frequency of 12 kHz. With 432 soundings per swath, the emission cone has a dimension of max 150° across track and 1° along track. With a reception obtained from 288 beams, the actual beam footprint is 1° by 2°. Depending on the roughness of the seafloor and the water depth, the swath width on a flat bottom is maximum six times the water depth. For further information on the system, consult https://www.km.kongsberg.com/. The position and depth of the water column is estimated for each beam by using the detected two-way-travel time and the beam, ray-traced through the water column, utilizing a proper sound speed profile. Throughout this cruise, the swath width was mainly set to 120° and did not exceed 130°. Responsible person during this cruise / PI: Laura Frahm (laura.frahm@studium.uni-hamburg.de)Description of data processing:Postprocessing and products were conducted by the Seafloor-Imaging & Mapping group of MARUM/FB5, responsible person Paul Wintersteller (seafloor-imaging@marum.de). The open source software MB-System (Caress, D. W., and D. N. Chayes, MB-System: Mapping the Seafloor, https://www.mbari.org/products/research-software/mb-system, 2017) was utilized for this purpose. Tide corrections were applied to the M141/1 data; but corrections for roll, pitch, sound velocity and heave were not necessary. Using Mbeditviz, artefacts were cleaned manually. NetCDF (GMT) grids of the edited data as well as statistics were created with mbgrid. The published bathymetric EM122 grid of the cruise M141/1 has a resolution of 35 m. No total propagated uncertainty (TPU) has been calculated to gather vertical or horizontal accuracy. A higher resolution is, at least partly, achievable. The grid extended with _num represents a raster dataset with the statistical number of beams/depths taken into account to create the depth of the cell. The extended _sd -grid contains the standard deviation for each cell. The DTMs projections are given in Geographic coordinate system Lat/Lon; Geodetic Datum: WGS84. All grids produced are retrievable through the PANGAEA database (www.pangaea.de).Chief Scientist: T.H. HansteenCR:CSR: https://www.ldf.uni-hamburg.de/meteor/wochenberichte/wochenberichte-meteor/m141-m145/m141-scr.pdf
DOI: 10.1594/pangaea.758109
title: (Table 2) Chemistry of basalts of ODP Hole 119-738C
DOI: 10.1594/pangaea.670264
title: Basic and other measurements of radiation at Neumayer Station (2000-10)
DOI: 10.1594/pangaea.477556
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_OC_22S/46

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.956961
title: Ozone measurements from station Payerne (2022-09)

description: Location: Arosa, Switzerland; Distance from radiation site: 200 km
DOI: 10.1594/pangaea.956970
title: Radiosonde measurements from station Payerne (2022-11)
DOI: 10.1594/pangaea.838165
title: Pollen profile MOLECHAM, United Kingdom

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.747870
title: Meteorological observations during CERES cruise from Downs to Penang started at 1815-04-10
DOI: 10.1594/pangaea.916385
title: 1-Hz PPP displacements at GEONET station 0180 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916386
title: 1-Hz PPP displacements at GEONET station 0181 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.932585
title: Total sea-ice thickness measurements during the ALERT2018 campaign (MAP Last Ice) at station ALERT2018_24

description: Total sea-ice thickness measurements were obtained using a ground-based electromagnetic sound device (EM31-SH, Geonics Limited, Mississauga, ON, Canada) during walking surveys on First-Year-Ice during the ALERT2018 campaign (Multidisciplinary Arctic Program (MAP) - Last Ice) off Alert, Nunavut, Canada in the Lincoln Sea in May 2018. The walks were along a 100 m transect and across an approx. 100 times 100 m wide patch.
DOI: 10.1594/pangaea.916390
title: 1-Hz PPP displacements at GEONET station 0185 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916391
title: 1-Hz PPP displacements at GEONET station 0186 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916394
title: 1-Hz PPP displacements at GEONET station 0189 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916400
title: 1-Hz PPP displacements at GEONET station 0195 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.835775
title: Pollen profile BOITES1, Lac des Boites, France

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.670290
title: Basic and other measurements of radiation at Neumayer Station (2003-04)
DOI: 10.1594/pangaea.670270
title: Basic and other measurements of radiation at Neumayer Station (2001-05)
DOI: 10.1594/pangaea.732915
title: (Table 1) Alkenone and foraminiferal carbon isotopic ratios, alkenone SST, epsilon p37:2 and pCO2 etimates in ODP Hole 165-999A

description: Age determined from composite depth and the orbitally tuned age models of Schmidt et al., (2006, doi:10.1029/2005GC000957) and Haug and Tiedemann (1998, doi:10.1038/31447) and biostratigraphic models (Chaisson and d'Hondt, 2000, doi:10.2973/odp.proc.sr.165.010.2000; Kameo and Bralower, 2000, doi:10.2973/odp.proc.sr.165.012.2000)
DOI: 10.1594/pangaea.956957
title: Other measurements at 30 m from station Payerne (2022-08)
DOI: 10.1594/pangaea.956959
title: Ultra-violet measurements from station Payerne (2022-09)
DOI: 10.1594/pangaea.956960
title: Radiosonde measurements from station Payerne (2022-09)
DOI: 10.1594/pangaea.670272
title: Basic and other measurements of radiation at Neumayer Station (2001-07)
DOI: 10.1594/pangaea.956962
title: Other measurements at 10 m from station Payerne (2022-09)
DOI: 10.1594/pangaea.956963
title: Other measurements at 30 m from station Payerne (2022-09)
DOI: 10.1594/pangaea.956969
title: Ultra-violet measurements from station Payerne (2022-11)
DOI: 10.1594/pangaea.808316
title: Dissolved organic carbon and dissolved nitrogen concentration in sediments associated to deep-sea wood falls (Wood-1 & Wood-5)
DOI: 10.1594/pangaea.908239
title: (Figure 3 c-d-e) Aerosol optical properties at Gruvebadet, Ny-Ålesund, Spitsbergen - July 2015

description: Trends of Aitken, accumulation and coarse mode fractions (a), temperature and relative humidity (b), aerosol scattering at 530 nm (c), absorption coefficients (d), single scattering albedo (SSA) at 530 nm (orange line, right scale) and absorption Angstrom exponent (AAE, grey line, left scale; e) of the aerosol at GVB during the BB event.
DOI: 10.1594/pangaea.477745
title: Hydrochemistry measured on water bottle samples at station SPac_1967_ET_43S/41

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.822616
title: Meteorological measurements in the upper air at station al-Qahira, 1933-07-01 to 1947-02-16, ERA-CLIM ID 4939

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.664452
title: Oceanography at CTD/bottle station IFREMER_1292
DOI: 10.1594/pangaea.666019
title: Oceanography at CTD/bottle station IFREMER_2845
DOI: 10.1594/pangaea.908276
title: (Figure 10) Percent mass fraction of aerosol particles from SEM observations at Gruvebadet, Ny Alesund - July 2015
DOI: 10.1594/pangaea.670292
title: Basic and other measurements of radiation at Neumayer Station (2003-06)
DOI: 10.1594/pangaea.947076
title: Continuous meteorological observations at Neumayer station (2021-04)

description: The meteorological observatory Neumayer continuously acquires meteorological parameters. Measurements are taken on or near the meteorological 10m-mast, located some 300m south-east of the main station building. Co-located there are BSRN (Baseline Surface Radiation Network) measurements taken. The measurement interval of the raw data is approximately 6s. Data is quality controlled: All measurements are checked daily on site and again prior to publication according to BSRN standards. Knowingly affected or erroneous data is removed.
DOI: 10.1594/pangaea.845498
title: Basic and other measurements of radiation at Neumayer Station (2014-11)
DOI: 10.1594/pangaea.947080
title: Continuous meteorological observations at Neumayer station (2021-05)

description: The meteorological observatory Neumayer continuously acquires meteorological parameters. Measurements are taken on or near the meteorological 10m-mast, located some 300m south-east of the main station building. Co-located there are BSRN (Baseline Surface Radiation Network) measurements taken. The measurement interval of the raw data is approximately 6s. Data is quality controlled: All measurements are checked daily on site and again prior to publication according to BSRN standards. Knowingly affected or erroneous data is removed.
DOI: 10.1594/pangaea.838173
title: Pollen profile NAY, France

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.895138
title: Modelled environmental predictors of hard-bottom-communities in the SW Baltic Sea between 2005-2015
DOI: 10.1594/pangaea.484603
title: Hydrochemistry measured on water bottle samples at station SN97/11-1

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.752927
title: Meteorological observations during WORCESTER cruise from Downs to Bombay started at 1767-03-11
DOI: 10.1594/pangaea.477181
title: Hydrochemistry measured on water bottle samples at station NPac_1984_WT_152W/35-1

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.477410
title: Hydrochemistry measured on water bottle samples at station SAtl_1983-84_6N_0E/64-1

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.895137
title: Taxonomic composition of hard-bottom-communities in the SW Baltic Sea between 2005-2015
DOI: 10.1594/pangaea.810150
title: (Table 2) Characteristics of a turbidite flow inferred from physiography and morphology of the margin and the sediment waves

description: This paper presents the morpho-sedimentary characterization and interpretations of the assemblage of landforms of the East Greenland continental slope and Greenland Basin, based on swath bathymetry and sub-bottom TOPAS profiles. The interpretation of landforms reveals the glacial influence on recent sedimentary processes shaping the seafloor, including mass-wasting and turbidite flows. The timing of landform development points to a predominantly glacial origin of the sediment supplied to the continental margin, supporting the scenario of a Greenland Ice Sheet extending across the continental shelf, or even to the shelf-edge, during the Last Glacial Maximum (LGM). Major sedimentary processes along the central section of the eastern Greenland Continental Slope, the Norske margin, suggest a relatively high glacial sediment input during the LGM that, probably triggered by tectonic activity, led to the development of scarps and channels on the slope and debris flows on the continental rise. The more southerly Kejser Franz Josef margin has small-scale mass-wasting deposits and an extensive turbidite system that developed in relation to both channelised and unconfined turbidity flows which transferred sediments into the deep Greenland Basin.
description: Positions approximate. For a more detailed view on the transects see Figure 10 of the article. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
description: Supplement to: García, Marga M; Dowdeswell, Julian A; Ercilla, Gemma; Jakobsson, Martin (2012): Recent glacially influenced sedimentary processes on the East Greenland continental slope and deep Greenland Basin. Quaternary Science Reviews, 49, 64-81
DOI: 10.1594/pangaea.905417
title: Data Set S4 - Offsets applied to cores from IODP Holes 342-U1408A, 342-U1408B, 342-U1408C
DOI: 10.1594/pangaea.838167
title: Pollen profile MONROUX1, Switzerland

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.477413
title: Hydrochemistry measured on water bottle samples at station SAtl_1983-84_6N_0E/67-1

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.