cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.777612
title: Clay mineralogy on sediment core NBP0602A-6C
DOI: 10.1594/pangaea.761882
title: Radiosonde measurements from station Sede Boqer (2011-01)

description: Start location: Bet-Dagan,Israel; Distance from radiation site: 120 km
DOI: 10.1594/pangaea.777613
title: Clay mineralogy on sediment core NBP0602A-6D
DOI: 10.1594/pangaea.754856
title: Mineral concentration in sediment core HU92045-11P

description: The continental slope in Orphan Basin, northeast of Newfoundland, is underlain by several seaward-thinning debris-flow wedges alternating with acoustically stratified, regionally extensive, mainly hemipelagic sediments. d18O stratigraphy and volcanic ash layers in a 11.67-m core indicate that the uppermost debris-flow wedge formed during the last of several sea-level lowstands in isotopic stages 2–4. Similarly, seismic reflection correlation of dated levels at DSDP Site 111 with the Orphan Basin succession suggests that two deeper debris-flow wedges were deposited during oxygen isotopic stages 6 and 8. The oldest of the debris-flow deposits in at least three of the wedges formed well into the corresponding glacial cycle, after ice sheets had reached the edge of the continental shelf. Slower deposition by hemipelagic processes and ice rafting formed the acoustically stratified units, including Heinrich layers. The youngest three debris-flow wedges each have volumes of 1300–1650 km**3. Approximately two-thirds of this material is attributed to glacial erosion of Mesozoic and Tertiary strata beneath the Northeast Newfoundland Shelf. The remainder is believed to have been derived by glacial erosion of older bedrock that now forms the island of Newfoundland. The observed sediment volumes and the inferred basal and upper ages of the debris-flow wedges imply an average glacial denudation rate of about 0.13 mm/yr for this older bedrock, and an average of about 60 m of glacial bedrock erosion since oxygen isotope stage 22. This denudation rate is similar to estimates from the Barents Sea region off Norway.
description: Supplement to: Hiscott, Richard N; Aksu, Ali E (1996): Quaternary sedimentary processes and budgets in Orphan Basin, Southwestern Labrador Sea. Quaternary Research, 45(2), 160-175
DOI: 10.1594/pangaea.678107
title: Expanded measurements from station Ny-Ålesund (1995-07)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.752168
title: Meteorological observations during SPARTIATE cruise from Plymouth to Funchal started at 1823-09-27
DOI: 10.1594/pangaea.777614
title: Clay mineralogy on sediment core NBP0602A-12A
DOI: 10.1594/pangaea.907282
title: Track of GPS very-near surface drifter ISMER_20150809_spot058
DOI: 10.1594/pangaea.692972
title: Ozone measurements from Neumayer Station (2008-01)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.762150
title: (Table 6) Mineral composition of inorganic fraction of sinking sedimentary material from sediment traps in the northeast Black Sea in September-October 1999

description: + = present; ++ = few.
DOI: 10.1594/pangaea.713498
title: (Table 1) Lithium concentration and isotopic composition of rocks from DSDP/ODP Hole 504B

description: Further d18O data see Alt et al. (1986) datasets: doi:10.1594/PANGAEA.713298 and Alt et al., (1989) datasets: doi:10.1594/PANGAEA.713302
DOI: 10.1594/pangaea.824083
title: Magnetic remanence from IODP Hole 318-U1356A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.785831
title: (Table T5) Datum levels of ODP Site 182-1132

description: DEPTH, sediment is given in mbsf and is here defined as the middle depth between the sample where the taxon occurs and the adjacent sample where it does not occur..
DOI: 10.1594/pangaea.674417
title: Radiosonde measurements from Neumayer Station (1997-09)
DOI: 10.1594/pangaea.790774
title: (Table 1) Revised and corrected composite depth sections of ODP Site 160-964

description: High-resolution color reflectance records of KC01 and KC01B (Calabrian Ridge, Ionian Sea) are presented and compared with a modified spliced high-resolution color reflectance record of Ocean Drilling Program (ODP) Site 964. This comparison revealed that KC01B is characterized by intensive deformation between ~27 and 28.5 m piston depth and that some sapropels are tectonically reduced in thickness. Moreover, the piston coring has caused considerable stretching in the top of KC01 and KC01B. Using a new splice of ODP Site 964 as guide, previous astronomical tuned timescales of KC01B and ODP Site 964 were evaluated. This evaluation resulted in a new sapropel-based astronomical timescale for the last 1.1 Myr. The new timescale implies a much more uniform change in sedimentation rate for the Ionian Sea cores. Two prominent excursions to lighter values in the d18O record of the planktonic foraminiferal species Globigerinoides ruber occur during marine isotopic stages 12 and 16 applying the new timescale. These shifts correspond with maxima in obliquity and are punctuated by minima in the precession cycle. They are absent in global ice volume records and are interpreted as reflecting a (summer) low-salinity surface water lens that floats on top of extremely saline intermediate and deep waters at times of the very low sea levels during these glacial periods. All biostratigraphic and magnetostratigraphic events found in KC01B and ODP Site 964 were re-dated according to the new timescale, and the ages of 33 tephra layers were reviewed. The new ages for the Calabrian Ridge 2 and 3 magnetic events in the Brunhes are concordant with minima in the global Sint800 composite record, derived from worldwide deep-sea records of relative paleointensity and have been attributed to the Big Lost and La Palma excursions, respectively.
description: Supplement to: Lourens, Lucas Joost (2004): Revised tuning of Ocean Drilling Program Site 964 and KC01B (Mediterranean) and implications for the d18O, tephra, calcareous nannofossil, and geomagnetic reversal chronologies of the past 1.1 Myr. Paleoceanography, 19(3), PA3010
DOI: 10.1594/pangaea.695697
title: Meteorological synoptical observations from station Sede Boqer (2007-02)
DOI: 10.1594/pangaea.826008
title: Reflectance spectroscopy and colorimetry from IODP Hole 327-U1362A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.775052
title: Continuous meteorological observations at Neumayer station (2006-06)
DOI: 10.1594/pangaea.707430
title: Meteorological synoptical observations from station Sede Boqer (2007-11)
DOI: 10.1594/pangaea.775128
title: Continuous meteorological observations at Neumayer station (2007-04)
DOI: 10.1594/pangaea.723955
title: Other measurements at 10 m from station Southern Great Plains (1995-11), Version 1

description: Please refer to Version 2 (see Replaced by reference)
DOI: 10.1594/pangaea.828238
title: Spatially explicit estimates of stock size, structure and biomass of North Atlantic albacore tuna (Thunnus alalunga) in the North Atlantic for the period 1975-1984, compiled from statistics about ICCAT fishery region B14

description: The development of the ecosystem approach and models for the management of ocean marine resources requires easy access to standard validated datasets of historical catch data for the main exploited species. They are used to measure the impact of biomass removal by fisheries and to evaluate the models skills, while the use of standard dataset facilitates models inter-comparison. North Atlantic albacore tuna is exploited all year round by longline and in summer and autumn by surface fisheries and fishery statistics compiled by the International Commission for the Conservation of Atlantic Tunas (ICCAT). Catch and effort with geographical coordinates at monthly spatial resolution of 1° or 5° squares were extracted for this species with a careful definition of fisheries and data screening. In total, thirteen fisheries were defined for the period 1956-2010, with fishing gears longline, troll, mid-water trawl and bait fishing. However, the spatialized catch effort data available in ICCAT database represent a fraction of the entire total catch. Length frequencies of catch were also extracted according to the definition of fisheries above for the period 1956-2010 with a quarterly temporal resolution and spatial resolutions varying from 1°x 1° to 10°x 20°. The resolution used to measure the fish also varies with size-bins of 1, 2 or 5 cm (Fork Length). The screening of data allowed detecting inconsistencies with a relatively large number of samples larger than 150 cm while all studies on the growth of albacore suggest that fish rarely grow up over 130 cm. Therefore, a threshold value of 130 cm has been arbitrarily fixed and all length frequency data above this value removed from the original data set.
description: This work was funded in part by the European project EURO-BASIN, funded by Framework Programme 7 (Contract 264933). Special thanks to ICCAT for the access to its public fishing database and Carlos Palma (ICCAT) and Alain Fonteneau (IRD) for their helpful advice on these data.
DOI: 10.1594/pangaea.673444
title: Radiosonde measurements from station Barrow (2002-01)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.835779
title: Pollen profile BREZOVA, Brezová, Czech Republic

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.839146
title: Pollen profile COL2

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.672101
title: Radiosonde measurements from station South Pole (1992-03)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.843141
title: Links to master tracks in different resolutions of HEINCKE cruise HE230, Helgoland - Helgoland, 2005-06-02 - 2005-06-26
DOI: 10.1594/pangaea.876733
title: Marine radiocarbon reservoir ages for the past 50,000 years, links to model results in NetCDF format

description: Radiocarbon (14C) dating calibration for the last glacial period largely relies on cross-dated marine 14C records. However, marine reservoirs are isotopically depleted with respect to the atmosphere, and therefore have to be corrected by the Marine Radiocarbon Ages of surface waters (MRAs), whose temporal variabilities are largely unknown. Here, we present simulations of the spatial and temporal variability in MRAs using a three-dimensional ocean circulation model covering the past 50,000 years. Our simulations are compared to reconstructions of past surface ocean D14C. Running the model with different climatic boundary conditions, we find that low- to mid-latitude MRAs have varied between 400 and 1200 14C years, with values of about 780 14C years at the Last Glacial Maximum. Reservoir ages exceeding 2000 14C years are simulated in the polar oceans. Our simulation results can be used as first order approximation of the MRA variability in future radiocarbon calibration efforts.
description: Version 2, 2017-08-112018-03-20 upload of "Marine Reservoir Age 0-100 m, original temporal resolution" and "Marine Reservoir Age 200-300 m, original temporal resolution" NetCDF files.
description: Supplement to: Butzin, Martin; Köhler, Peter; Lohmann, Gerrit (2017): Marine radiocarbon reservoir age simulations for the past 50,000 years. Geophysical Research Letters, 44(16), 8473-8480
DOI: 10.1594/pangaea.510114
title: Grain size distribution of sediment core M22_103, South Tyrrhenian Sea (Table 2)
DOI: 10.1594/pangaea.874618
title: In-situ measurements of near surface (0-5 cm) soil moisture and temperature in August 2015 on central Yamal (Vaskiny Dachi CALM site)
DOI: 10.1594/pangaea.898584
title: Conquiliometry of Neritina zebra of the Paradise beach in Mosqueiro, state of Pará, northern Brazil (March-May 2018)

description: Samples were collected during the months of March, April, and May. Measuring the length (C), width (L), height (A), length of aperture (Ca) and width of aperture (La).
DOI: 10.1594/pangaea.875402
title: Radiosonde measurements from station Kwajalein (2016-12)
DOI: 10.1594/pangaea.716640
title: Expanded measurements from Neumayer Station (2008-10)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.876711
title: (Table EA2) Experimental parameters in leaching tests
DOI: 10.1594/pangaea.752373
title: Meteorological observations during SUMATRA cruise from St. Eustatius to Curaçao started at 1830-04-07
DOI: 10.1594/pangaea.803345
title: (Table 10) Split-core (archive half) paleomagnetic characteristics of ODP Hole 165-1001B
DOI: 10.1594/pangaea.752375
title: Meteorological observations during SUMATRA cruise from Havannah to Vlissingen started at 1830-05-09
DOI: 10.1594/pangaea.700857
title: Medusae abundance during HEINCKE cruise HE225
DOI: 10.1594/pangaea.752869
title: Meteorological observations during WELMEENENDE cruise from Gulf of Guinea to Paramaribo started at 1770-02-16
DOI: 10.1594/pangaea.676835
title: Clay mineral composition of &lt;0.005 mm grain size fraction of sediments from Hole AMIGE-1993-155 drilled in the Barents Sea

description: Types of rocks and their ages are given in the special data set; see: doi:10.1594/PANGAEA.676843
DOI: 10.1594/pangaea.811087
title: (Table 3) Nannoplankton occurrences in DSDP Hole 90-587

description: Sediment depth is given in mbsf. Species abundance: A = abundant (&gt;50 specimens), C = common (25-49 specimens), and R = rare (&lt;25 specimens) - = absent, obtained by scanning an area measuring approximately 45 mm**2.
DOI: 10.1594/pangaea.707598
title: Meteorological synoptical observations from station Payerne (2000-08)
DOI: 10.1594/pangaea.672136
title: Radiosonde measurements from station South Pole (1995-07)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.785110
title: Photographs of tiles installed at Las Hermanas Island, Palena Bay, Chile, at 2012-06-04 in 21 m water depth

description: This dataset was generated in the frame of the co-operation between the Reserva Anihue (http://www.anihuereserve.cl), the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). If you intend to work with this data set please do not hesitate to contact the authors to discuss cooperation possibilities. Holes were drilled in the bare rock and recruitment plates mount: Polyethylene frames, supported tiles. Each plastic frame has the dimensions 21.5 cm by 17.5 cm (376.25 cm**2). The plastic frame is branded with a number and writing to prevent confusion. One recruitment tile (15.5 cm by 15.5 cm) is held in place by two plastic washers and screws, which root the tile to the hard plastic frame. The tile is composed of a roughed chequered ceramic material. Camera used: Intova IC 12. Under water photographs are taken regularly.
DOI: 10.1594/pangaea.777535
title: ph measured in soil samples from the A.D. 79 level at station Oplontis
DOI: 10.1594/pangaea.777536
title: ph measured in soil samples from the A.D. 79 level at station Pompeii
DOI: 10.1594/pangaea.558163
title: Monthly landings from 1998 of Sciaena deliciosa (Lorna) in San Andres, Pisco, Peru
DOI: 10.1594/pangaea.735838
title: Meteorological synoptical observations from station Lindenberg (1997-03)
DOI: 10.1594/pangaea.823476
title: (Table 11) Trace elements at DSDP Hole 54-424B

description: &lt; = value below detection limit; #1 = element determined in major oxides (%).
DOI: 10.1594/pangaea.828446
title: Interstitial water analysis from IODP Hole 323-U1342A

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.667668
title: Basic measurements of radiation at station Bermuda (1993-10)
DOI: 10.1594/pangaea.672175
title: Radiosonde measurements from station South Pole (1999-01)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.602210
title: Yearly landings from 1998 to 2005 of Mesodesma donacium (Machas) in Tubul, Chile
DOI: 10.1594/pangaea.753050
title: Meteorological observations during Na sa del Rosario cruise from El Callao to El Callao started at 1675-09-21

description: 1676-01-30T00:00: A LAS 3 DE LA TARDE REGRESO EL CHINCHORRO A BORDO Y DIERON RAZON DE LO OBRADO EN TIERRA. QUE LA NOCHE ANTECEDENTE LLEGARON A UNA CALETA QUE FORMABA UNA ISLA EN LA BOCA DE UNA BAHIA MUY GRANDE Y MUY LLENA DE FARALLONES E ISLOTES, QUE A LA MAÑANA SIGUIENTE FUERON A RECONOCER LA TIERRA LA CUAL HALLARON LLANA ALREDEDOR DE LA BAHIA MUY TRATABLE Y JUNTO A UNA PLAYA DE ARENA BLANCA UN ARROYO DE AGUA MUY BUENA QUE SE DESPEÑABA A PROPOSITO PARA LAS AGUADAS, GRABARON EN UN ARBOL EL NOMBRE DE MARIA Y TOMARON POSESION EN NOMBRE DE S.M. CATOLICA DEJANDO UNA BOTIJUELA CON UN TESTIMONIO, SONDARON LA BAHIA Y LA HALLARON DE FONDO PIEDRA SIN SURGIDERO BUENO, LA BAHIA TENIA 4 LEGUAS DE BOCA Y 2 DE ENSENADA DESDE LA PRIMERA ISLA HASTA LA TIERRA QUE PARECIA FIRME AL E, A LA CUAL SE PUSO POR NOMBRE NTRA. SRA. DEL ROSARIO. CONTINUARON CON VIENTO N AL S 1/4 SO A 3 LEGUAS DE TIERRA EN DEMANDA DE CABO CORSO DESCUBRIENDO AL PARECER NO POCAS ENSENADAS QUE PROPASAMOS CON ANIMO DE RECONOCERLAS A LA VUELTA. 1676-02-07T00:00: AMANECIO CON LOS 4 EVANGELIOS, EL VIENTO OSO Y DE MAL CARIZ. ENTRE 7 Y 8 DE LA MAÑANA HABILITARON EL CHINCHORRO CON 16 HOMBRES ESCOGIDOS DE MAR Y GUERRA, UN INDIO CHONO POR INTERPRETE, EL CAPITAN JUAN BAUTISTA ECHAVARRIA Y URQUIZU, EL SARGENTO MAYOR DON PEDRO DE VILLEGAS, EL CAPITAN ANTONIO RUIZ PILOTO Y EL CONTRAMAESTRE FRANCISCO DE ESCORZA... Y POR CABO DE TODOS DON ANTONIO DE IRIARTE, HIJO DEL CAPITAN Y ALFEREZ VIVO DE SU COMPAÑÍA DE MAR Y DE GUERRA, CON ARMAS, INSTRUMENTOS Y TODO LO NECESARIO FUERON A TIERRA PARA TOMAR NUEVA POSESION EN NOMBRE DE S.M. DON CARLOS II CON LA INSCRIPCION QUE SIGUE (LA TRANSCRIBE). ESTABAN A LA SAZON N-S CON LOS EVANGELIOS, ANTIGUAMENTE TENIDA POR TIERRA FIRME, LLAMADA CABO VICTORIA. AL MEDIODIA E-O CON LOS EVANGELIOS, OBSERVARON 52º45 CON 4 PEÑASCOS MAYORES FUERA DE DICHOS PEQUEÑOS CERCA DE ELLOS SITUADOS CASI EN LINEA RECTA AL SE 1/4 AL SSE CON DISTANCIA A LA VISTA DE 7 LEGUAS DEL CABO DESEADO Y TRES DE LAS ISLAS QUE CAEN EN FRENTE DEL CABO VICTORIA
DOI: 10.1594/pangaea.753057
title: Meteorological observations during QUEBEC cruise from Elba to Leghorn started at 1762-07-04

description: 1765-01-09T00:00: SE(...)HALLARON 58 BRAZAS Y DESPUÉS ENTREGANDO LA GUARDIA AL 2º PILOTO CON ORDEN DE SONDAR DE 2 EN 2 HORAS, SE FUE A DORMIR: ESTE SIN HABER VERIFICADO LA ORDEN, DADAS LAS 12, DEJANDO LA GUARDIA AL CONTRAMAESTRE Y AL PILOTÍN HIZO LO MISMO. EL CAPITÁN EN LUGAR DE LEVANTARSE A LA GUARDIA DE LAS 12, NO SE RECORDÓ HASTA LA 1 1/2 QUE LE LLAMÓ EL PILOTÍN Y (LE DIJERON QUE EL 2º PILOTO NO HABÍA SONDADO. EN LUGAR DE SONDAR INMEDIATAMENTE Y CREYENDO VER SOMBRA DE TIERRA, MANDO ARRIBAR. POCO DESPUÉS ESTABA VARADO EL BARCO. TANTO EL CAPITÁN COMO EL SEGUNDO PILOTO ESTABAN CONFUSOS Y NO SABÍAN QUÉ TIERRA ERA LA QUE SE VEÍA, POR LA MUCHA CERRAZÓN. SE MANDÓ ECHAR EL ANCLA AL AGUA Y OTRAS DILIGENCIAS PARA SACAR EL NAVIO, LO QUE SE LOGRÓ. EN ESTE INTERMEDIO DE CUANDO EN CUANDO LA MAREJADA TOCABA EL NAVÍO Y A NOSOTROS NOS ARRANCABA EL CORAZÓN DE DOLOR. (EL NAVÍO HACÍA MUCHO AGUA Y NO PODÍAN ACHICARLA, ASÍ QUE FUE EL BUZO A RECONOCERLO. ESTABA CASI DESCLAVADA LA TABLA PRINCIPAL DE LA APARADURA DE LA QUILLA. ERA IMPOSIBLE SEGUIR EL DESTINO Y EL NAVÍO SE PERDIÓ TOTALMENTE. SACARON VÍVERES, PÓLVORA Y ARMAS Y TODO LO QUE PUDIERON Y SE FUERON A LA PLAYA, CON MUCHAS DIFICULTADES POR LO BRAVO DEL MAR. DURANTE MUCHOS DÍAS ESTUVIERON CONSTRUYENDO UNA EMBARCACIÓN Y TRATANDO CON LOS INDIOS LOCALES)
DOI: 10.1594/pangaea.749880
title: Meteorological observations during JASON cruise from Hellevoetsluis to St. Eustacius started at 1780-01-09
DOI: 10.1594/pangaea.752306
title: Meteorological observations during Stad Utrecht cruise from St. Thomas to Belize started at 1851-11-19
DOI: 10.1594/pangaea.752803
title: Meteorological observations during Walmer Castle cruise from Portsmouth to Bombay started at 1806-03-06
DOI: 10.1594/pangaea.677262
title: Ozone measurements from Neumayer Station (1998-04)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.823471
title: (Table 6) Bulk geochemistry at DSDP Hole 54-424B recalculated on CaO-free basis
DOI: 10.1594/pangaea.753393
title: (Table 1) Activity of strontium-90 in waters of the Northeast Atlantic at the end of 1965 and the beginning of 1966

description: In 1965-1966 R/V Mikhail Lomonosov conducted studies on concentrations of artificial radioactive products in the Northeast Atlantic. Concentration of strontium-90 at the end of 1965 and the beginning of 1966 was higher than the average level for the ocean and reached about 53 dpm/100 l in the surface layer. The most intense transport of artificial radioactive products out of the Irish Sea was detected in the northern and northeastern directions along the Hebrides and the Orkneys. In addition to radioactive fission products from nuclear weapons tests, radioactive wastes of atomic industrial facilities discharged into the ocean are an important source of radioactive contamination of some regions of the world ocean.
description: Supplement to: Baksheyeva, I P; Zemlyanoy, A D; Markelov, V N; Nelepo, Boris A (1971): Radioactivity of the water of the Northeastern part of the Atlantic Ocean. Oceanology, 11, 861-867
DOI: 10.1594/pangaea.828586
title: Magnetic remanence from IODP Hole 323-U1339C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.762652
title: (Table 4) Content and composition of lignin and its derivates in the surface layer of bottom sediments from the Kandalaksha Bay
DOI: 10.1594/pangaea.755810
title: (Table 1o) Concentrations of urea nitrogen in seawater at Station AK22-1949
DOI: 10.1594/pangaea.886244
title: Links to master tracks in different resolutions of HEINCKE cruise HE500, Bremerhaven - Bremerhaven, 2017-10-30 - 2017-11-12
DOI: 10.1594/pangaea.728245
title: (Table 2) Diatom abundance and nannofossil and diatom zonation of ODP Hole 115-708A
DOI: 10.1594/pangaea.752346
title: Meteorological observations during Stirling Castle cruise from to Saugor Roads started at 1813-04-23
DOI: 10.1594/pangaea.756809
title: (Table 2) Stable oxygen isotope ratios of planktonic foraminifera and carbonate from ODP Hole 117-728A
DOI: 10.1594/pangaea.775176
title: (Table 90a) Grain size composition of pelitic bottom sediments from the near Nile province of the Mediterranean Sea
DOI: 10.1594/pangaea.752448
title: Meteorological observations during TERNATE cruise from Rotterdam to Makassar started at 1850-06-19
DOI: 10.1594/pangaea.784386
title: Laser profiles of sea ice surface roughness during POL-ICE 2007 field campaign from flight POL-ICE07_200703131434
DOI: 10.1594/pangaea.615314
title: Description of the soil of core LD98_t7b

description: For the position of the transects t, v, and w see also figure 3-1
DOI: 10.1594/pangaea.751219
title: Meteorological observations during Piet Heijn cruise from Texel to Suriname started at 1796-02-23
DOI: 10.1594/pangaea.825044
title: Natural gamma radiation from IODP Hole 334-U1381A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.752507
title: Meteorological observations during TRAVERS cruise from Diamond Harbour to The Downs started at 1805-07-20
DOI: 10.1594/pangaea.728467
title: (Table 5) Abundance of radiolarian species present at ODP Hole 119-744A

description: Species abundance: X = 1 specimen, R = rare (&lt;5 specimens), F = few (5-10), C = common (10-20), A = abundant (&gt;20), - = absent, ? = questionable
DOI: 10.1594/pangaea.752585
title: Meteorological observations during UNKNOWN-09 cruise from Batavia to Nieuwendiep started at 1845-06-23
DOI: 10.1594/pangaea.752907
title: Meteorological observations during Witte Cornelisz de Wit cruise from Rotterdam to New York started at 1852-10-14
DOI: 10.1594/pangaea.828400
title: Gas measurements from IODP Hole 323-U1342A

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.675379
title: Radiosonde measurements from station Payerne (1997-10)