cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.739386
title: Pollen profile KOLMILAT, Lake Kolmilaträsk, Finland

description: Method: KOH, HF, acetolysis, KOH.The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.829377
title: (Figure 5a) Potential impact of DOM accumulation on fCO2 and carbonate ion computations in ocean acidification experiments

description: The paper is a theoretical and modelling study. We note that the data provided through this reposity are output from models described in the paper and do not constitute in situ measurements or experimental data.
DOI: 10.1594/pangaea.722764
title: Other measurements at 10 m from station Rock Springs (2007-06)
DOI: 10.1594/pangaea.829373
title: (Figure 4a) Potential impact of DOM accumulation on fCO2 and carbonate ion computations in ocean acidification experiments

description: The paper is a theoretical and modelling study. We note that the data provided through this reposity are output from models described in the paper and do not constitute in situ measurements or experimental data.
DOI: 10.1594/pangaea.495235
title: Water temperature XBT profiles from cruise U18_1986
DOI: 10.1594/pangaea.884740
title: Holocene pollen record from Lake Kinneret (Sea of Galilee), Israel

description: Lake Kinneret, also known as the Sea of Galilee and Lake Tiberias, is located in the northeast of Israel. At a lake level of 211 m b.s.l. (below mean sea level), the central basin is 43 m deep. The maximum length of the lake is 21 km (N-S) and its maximum width is 12 km (W-E). Lake Kinneret's surface area is 166 166 km². A new 17.8 m long sedimentary core was drilled in 2010. Here, we present the entire palynological record from it, which covers the last ~ 9,000 years. Special emphasis is given to the natural and human-influenced vegetation history of Galilee in comparison to that of the more southerly Dead Sea region. Significant signs of human impact are the first Olea (olive) increase during the beginning of the Chalcolithic period between 7,000 and 6,500 years ago, as well as the prominent Olea phase during the Hellenistic/Roman/Byzantine period between 2,300 and 1,500 years ago. Mediterranean macchia and bathas scrub vegetation, as known in the area today, has developed in the southern Levant under human impact since the last ca. 1,500 years.
description: Supplement to: Schiebel, Vera; Litt, Thomas (2018): Holocene vegetation history of the southern Levant based on a pollen record from Lake Kinneret (Sea of Galilee), Israel. Vegetation History and Archaeobotany, 27(4), 577-590
DOI: 10.1594/pangaea.905629
title: Radiosonde measurements from station Fukuoka (2019-05)
DOI: 10.1594/pangaea.829378
title: (Figure 6) Potential impact of DOM accumulation on fCO2 and carbonate ion computations in ocean acidification experiments

description: The paper is a theoretical and modelling study. We note that the data provided through this reposity are output from models described in the paper and do not constitute in situ measurements or experimental data.
DOI: 10.1594/pangaea.829362
title: Vane shear strength measurements from IODP Hole 340-U1400C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.694495
title: Temperature and salinity in the water column of the Ionian Sea at Station MARCH-2000-IKE4

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.722752
title: Other measurements at 10 m from station Rock Springs (2007-02)
DOI: 10.1594/pangaea.694500
title: Temperature and salinity in the water column of the Ionian Sea at Station MARCH-2000-IKE8

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.829363
title: Vane shear strength measurements from IODP Hole 340-U1401A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.829372
title: (Figure 2,3,5b) Potential impact of DOM accumulation on fCO2 and carbonate ion computations in ocean acidification experiments

description: The paper is a theoretical and modelling study. We note that the data provided through this reposity are output from models described in the paper and do not constitute in situ measurements or experimental data.
DOI: 10.1594/pangaea.832023
title: Hydrological records from the Vernagtferner Basin - Vernagtbach station, for the year 2002
DOI: 10.1594/pangaea.832024
title: Hydrological records from the Vernagtferner Basin - Vernagtbach station, for the year 2003
DOI: 10.1594/pangaea.722758
title: Other measurements at 10 m from station Rock Springs (2007-04)
DOI: 10.1594/pangaea.761497
title: (Table 3) Clinopyroxene and plagioclase analyses from DSDP Hole 26-250
DOI: 10.1594/pangaea.832026
title: Hydrological records from the Vernagtferner Basin - Vernagtbach station, for the year 2005
DOI: 10.1594/pangaea.722761
title: Other measurements at 10 m from station Rock Springs (2007-05)
DOI: 10.1594/pangaea.832032
title: Hydrological records from the Vernagtferner Basin - Vernagtbach station, for the year 2011
DOI: 10.1594/pangaea.829342
title: Thermal conductivity of IODP Hole 340-U1398B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.829344
title: Thermal conductivity of IODP Hole 340-U1399B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.739554
title: Pollen profile MONTCARR, Mont Carré, Hérémence, Switzerland

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.843624
title: Links to master tracks in different resolutions of HEINCKE cruise HE240, Kiel - Kiel, 2005-09-29 - 2005-10-07
DOI: 10.1594/pangaea.893987
title: Pollen profile of sediment core KILOLIT, Litlvatnet, Norway

description: This dataset was archived on 2018-09-13 from the EPD database. (http://www.europeanpollendatabase.net). Date analyzed: 1994
DOI: 10.1594/pangaea.893993
title: Pollen profile of sediment core KILOMYR, Myrvatnet, Norway

description: This dataset was archived on 2018-09-13 from the EPD database. (http://www.europeanpollendatabase.net). Date analyzed: 1994
DOI: 10.1594/pangaea.822741
title: Meteorological measurements in the upper air at station Port Blair, 1938-12-31 to 1942-03-12, ERA-CLIM ID 5464

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.829346
title: Thermal conductivity of IODP Hole 340-U1400C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.894178
title: Pollen profile of sediment core SETESI, Isbenttjønn, Norway

description: This dataset was archived on 2018-09-14 from the EPD database. (http://www.europeanpollendatabase.net). Date analyzed: 1998
DOI: 10.1594/pangaea.835168
title: Pollen profile from sediment core De_U

description: Analysed by Helmut Müller 1999
DOI: 10.1594/pangaea.757845
title: Ozone measurements from station Barrow (1998-03)
DOI: 10.1594/pangaea.835819
title: Pollen profile HUZ1, Huzenbacher See, Germany

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.835924
title: Pollen profile SVARCENB, Svarcenberk, Czech Republic

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.694358
title: Nutrient concentrations in water samples from the Ionian Sea at Station SEPT-2000-IPA1
DOI: 10.1594/pangaea.905966
title: Expanded measurements from station Lindenberg (2017-06)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.835140
title: Basic measurements of radiation at station Momote (2000-10)

description: Version 3, 2014-08-26
DOI: 10.1594/pangaea.696324
title: Basic measurements of radiation at station Ilorin (1999-10)

description: Some additional quality control will be performed during summer 2013 for the LW data. For further infos contact Rachel T. Pinker
DOI: 10.1594/pangaea.835110
title: Maximum ingestion and maximum clearance rate of Euphausia pacificus determined experimentally
DOI: 10.1594/pangaea.669850
title: Basic measurements of radiation at station Ilorin (1998-01)

description: Some additional quality control will be performed during summer 2013 for the LW data. For further infos contact Rachel T. Pinker
DOI: 10.1594/pangaea.707670
title: Meteorological synoptical observations from station Payerne (2006-03)
DOI: 10.1594/pangaea.822828
title: Meteorological measurements in the upper air at station Yaounde, 1953-08-01 to 1956-12-31, ERA-CLIM ID 5571

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.717151
title: Documentation of sediment core JR104-BC361
DOI: 10.1594/pangaea.720139
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 19-186

description: Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline quartzP = Plagioclase feldsparK = Potassium feldsparLvo = Other volcanic lithicLvd = Devitrified vitric volcanic lithicLvv = Vitric volcanic lithicLvf = Volcanic lithic with felsitic textureLvmi = Volcanic lithic with microlitic textureLvl = Volcanic lithic with lathwork textureLvp = Pyroclastic volcanic lithicLmv = Metavolcanic lithicLmm = Polycrystalline mica lithicLmt = Quartz-mica tectonite lithicLma = Quartz-feldspar-mica aggregate lithicLmp = Phyllite lithicLsa = Argillite-shale lithicLsc = Sedimentary carbonate lithicLsch = sedimentary chert or cherty argillite lithicLsi = Siltstone sedimentary lithicM = Phyllosilicate mineralsD = Dense mineralsCarb = Carbonate mineralsBio = Bioclastic debris (siliceous and/or carbonate)Misc = Miscellaneous and unidentifiedQ = Total quartzose grainsL = Unstable lithic grainsLm = Metamorphic lithic grainsLv = Volcanic-hypabyssal (and volcaniclastic) lithic grainsLs = Sedimentary lithic grainsLvm = Volcanic-hypabyssal and metavolcanic lithic grainsLsm = Sedimentary and metasedimentary lithic grainsLst = Sedimentary and polycrystalline quartz grainsF = Total feldspar grainsQp = Polycrystalline quartz grainsQ = Qm + Qpw + QptQp = Qpw + QptL = Lm + Lv + LsLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpLm = Lmv + Lmm + Lmt + LmaLsm = Ls + Lmm + Lmt + LmaLvc = Lvf + Lvmi + LvlLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpF = P + KLs = Lsa + LscLvm = Lv + LmvLst = Ls + QpQFL%Q = 100Q/(Q + F + L)QFL%F = 100F/(Q + F + L)QFL%L = 100L/(Q + F + L)QmKP%Qm = 100Qm/(Qm + P + K)QmKP%P = 100P/(Qm + P + K)QmKP%K = 100K/(Qm + P + K)LvfLvmiLvl%Lvf = 100Lvf/LvcLvfLvmiLvl%Lvmi = 100Lmi/LvcLmLvLs%Lm = 100Lm/LLmLvLs%Lv = 100Lv/LLmLvLs%Ls = 100Ls/LQpLvmLsm%Qp = 100Qp/(L + Qp)QpLvmLsm%Lvm = 100Lvm/(L + Qp)QpLvmLsm%Lsm = 100Lsm/(L + Qp)LvfLvmiLvl%Lvl = 100Lvl/Lvc
DOI: 10.1594/pangaea.829315
title: Magnetic remanence from IODP Hole 340-U1395B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.694253
title: Nutrient concentrations in water samples from the Aegean Sea at Station MAY-1997-IR34
DOI: 10.1594/pangaea.829329
title: Magnetic remanence from IODP Hole 340-U1401B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.829331
title: Magnetic remanence from IODP Hole 340-U1401D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.544651
title: Hydrography and plankton abundance of vertical plankton haul profile GIK15666-8, off NW Africa (Table 1c)
DOI: 10.1594/pangaea.694268
title: Nutrient concentrations in water samples from the Aegean Sea at Station MAY-1997-IR62
DOI: 10.1594/pangaea.694314
title: Nutrient concentrations in water samples from the Aegean Sea at Station SEPT-1998-IR55
DOI: 10.1594/pangaea.829322
title: Magnetic remanence from IODP Hole 340-U1398B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.829317
title: Magnetic remanence from IODP Hole 340-U1396B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.760895
title: (Table 5) Major and trace element composition of representative alteration halos and adjacent groundmass of ODP Hole 123-765D
DOI: 10.1594/pangaea.711575
title: Ozone measurements from station Tamanrasset (2008-10)
DOI: 10.1594/pangaea.869239
title: Expanded measurements from station Lindenberg (2008-05)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.842039
title: Basic measurements of radiation at station Darwin (2003-05)

description: Version 3, 2015-01-28
DOI: 10.1594/pangaea.720410
title: Documentation of sediment core GIK16322-1
DOI: 10.1594/pangaea.835086
title: Maximum ingestion and maximum clearance rate of Meganyctiphanes norvegica determined experimentally
DOI: 10.1594/pangaea.693756
title: Chlorophyll a and primary production in surface water during Professor Vodyanitskiy cruise PV25

description: Chlorophyll a and phaeopigments were measured fluorometrically by use of laboratory fluorometer constracted on the base of spectrophotometer Specol, fitted with a red sensitive photomultiplier, blue lamp, blue filter and red filter. Accuracy: lower limit = 0.01 mg/m**3 and the error of Chl and Phaeo determination is 10-15% (calculated from 10-15 repeatings). Primary production was measured by C14 simulated in situ method. Accuracy: 20 %, from experimens.
DOI: 10.1594/pangaea.906061
title: Stable carbon and oxygen isotopes of the Miocene alluvial-lacustrine Aktau succession in south-east Kazakhstan

description: The Aktau succession is located at 44.03°N and 79.30°E in the Ili Basin, south-east Kazakhstan. The dataset contains measurement results from the Middle to early Late Miocene part of the succession (total height: 372 m, lowermost sample: 0.29 m, uppermost sample: 370.94 m). Stable carbon and oxygen istopes were derived from bulk rock measurements.
DOI: 10.1594/pangaea.693808
title: Nano- and microphytoplankton during cruise Yalta_Bay_1982

description: Nucleopore filtration. Accuracy: 20%. Nonfixed samples were processed.
DOI: 10.1594/pangaea.734424
title: (Table 2.1.1.1) Vertical temperature and brine salinity profiles of sea-ice core IO-3

description: sea-ice core diameter 9 cm; DEPTH ice/snow measured from ice surface
DOI: 10.1594/pangaea.822274
title: Meteorological measurements in the upper air at station Kirnsk, 1954-10-19 to 1955-04-22, ERA-CLIM ID 4620
DOI: 10.1594/pangaea.752865
title: Meteorological observations during WEAZLE cruise started at 1776-03-01
DOI: 10.1594/pangaea.906030
title: Bulk sediment 14C ages of sediment core PC54 at Chatham Rise, Canterbury Shelf and Inner Bounty Trough, New Zealand
DOI: 10.1594/pangaea.751758
title: Meteorological observations during RHIJN cruise from Wijnkopers Baai to Nieuwediep started at 1842-10-18
DOI: 10.1594/pangaea.744139
title: Physical oceanography during Argos cruise Argos96/2 to the North Sea
DOI: 10.1594/pangaea.707082
title: (Table 2) Analyses of anhydrite samples from DSDP Hole 23-225
DOI: 10.1594/pangaea.806231
title: Concentration and isotope ratios of gases in porewater of the North Alex Mud Volcano

description: Sediment depth of PO362-2_36 is corrected depth [m].
DOI: 10.1594/pangaea.751282
title: Meteorological observations during Prince Edward cruise from Plymouth to Jamaica started at 1763-12-12
DOI: 10.1594/pangaea.908690
title: Photophysiological data of the arctic picoeukaryote Micromonas pusilla
DOI: 10.1594/pangaea.829299
title: Reflectance spectroscopy and colorimetry from IODP Hole 340-U1397A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.782396
title: (Table S9) Trace element distribution coefficients between garnet and allanite of sample VT08102

description: #0 = below detection limit.
DOI: 10.1594/pangaea.829289
title: P-Wave velocity (PWL) from IODP Hole 340-U1401C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.726488
title: (Table 1) Results of core-NCR (Non-Contact Resistivity) data analyses from ODP Leg 204

description: As part of Ocean Drilling Program Leg 204 at southern Hydrate Ridge off Oregon we have monitored changes in sediment electrical resistivity during controlled gas hydrate dissociation experiments. Two cores were used, each filled with gas hydrate bearing sediments(predominantly mud/silty mud). One core was from Site 1249 (1249F-9H3), 42.1 m below seafloor (mbsf) and the other from Site 1248 (1248C-4X1), 28.8 mbsf. At Site 1247, a third experiment was conducted on a core without gas hydrate (1247B-2H1, 3.6 mbsf). First, the cores were imaged using an infra-red (IR) camera upon recovery to map the gas hydrate occurrence through dissociation cooling. Over a period of several hours, successive runs on the multi-sensor track (includes sensors for P-wave velocity, resistivity, magnetic susceptibility and gamma-ray density) were carried out complemented by X-ray imaging on core 1249F-9H3. After complete equilibration to room temperature (17-18 8C) and complete gas hydrate dissociation, the final measurement of electrical resistivity was used to calculate pore-water resistivity and salinities. The calculated pore-water freshening after dissociation is equivalent to a gas hydrate concentration in situ of 35-70% along core 1249F-9H3 and 20-35% for core 1248C-4X1 assuming seawater salinity of in situ pore fluid. Detailed analysis of the IR scan, X-ray images and split-core photographs showed the hydrate mainly occurred disseminated throughout the core. Additionally, in core 1249F-9H3, a single hydrate filled vein, approximately 10 cm long and dipping at about 658, was identified. Analyses of the logging-while-drilling (LWD) resistivity data revealed a structural dip of 40-808 in the interval between 40 and 44 mbsf. We further analyzed all resistivity data measured on the recovered core during Leg 204. Generally poor data quality due to gas cracks allowed analyses to be carried out only at selected intervals at Sites 1244, 1245, 1246, 1247, 1248, 1249, and 1252. With a few exceptions, data from these intervals yield low to no gas hydrate concentration, which corresponds to estimates from downhole resistivity logs. However, since the gas cracking may be the result of gas hydrate dissociation, this is a biased sampling. Cores that had contained some gas hydrate may have been excluded.
description: Supplement to: Riedel, Michael; Long, Philip E; Collett, Tim S (2006): Estimates of in situ gas hydrate concentration from resistivity monitoring of gas hydrate bearing sediments during temperature equilibration. Marine Geology, 227(3-4), 215-225
DOI: 10.1594/pangaea.834899
title: (Table 1) Age determination of sediments of the Straits of Florida

description: The salinity and temperature of the Florida Current are key parameters affecting the transport of heat into the North Atlantic, yet little is known about their variability on centennial timescales. Here we report replicated, high-resolution foraminiferal records of Florida Current surface hydrography for the last millennium from two coring sites, Dry Tortugas and the Great Bahama Bank. The oxygen isotopic composition of Florida Current surface water (d18Ow) near Dry Tortugas increased 0.4‰ during the course of the Little Ice Age (LIA) (~1200–1850 A.D.), equivalent to a salinity increase of 0.8–1.5. On the Great Bahama Bank, where surface waters are influenced by the North Atlantic subtropical gyre, d18Ow increased by 0.3‰ during the last 200 years. Although a portion (~0.1 per mil) of this shift may be an artifact of anthropogenically driven changes in surface water SumCO2, the remaining d18Ow signal implies a 0.4–1 increase in salinity after 200 years B.P. The simplest explanation of the d18Ow data is southward migration of the Atlantic Hadley circulation during the LIA. Scaling of the d18Ow records to salinity using the modern low-latitude d18Ow-S slope produces an unrealistic reversal in the salinity gradient between the two sites. Only if d18Ow is scaled to salinity using a high-latitude d18Ow-S slope can the records be reconciled. Variable atmospheric 14C paralleled Dry Tortugas d18Ow, suggesting that solar irradiance paced centennial-scale migration of the Inter-Tropical Convergence Zone and changes in Florida Current salinity during the last millennium.
description: Core tops contain more radiocarbon than expected in modern samples, indicating contamination with bomb 14C and post-1950 A.D. deposition ages. We calibrated the down-core raw 14C values to calendar ages using CALIB 4.3 (Stuiver et al.,1998) and a reservoir age of 400 years. Each date is based on G. ruber from the &gt;250 µm size fraction. Average sedimentation rate is 25 cm/kyr and average sampling interval is 20 years for core W167-79GGC. See Lund and Curry (2004) for the W167-79GGC age model.
description: Supplement to: Lund, David C; Curry, William B (2006): Florida Current surface temperature and salinity variability during the last millennium. Paleoceanography, 21(2), PA2009
DOI: 10.1594/pangaea.829259
title: P-Wave velocity (PWC) from IODP Hole 340-U1398A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.829260
title: P-Wave velocity (PWC) from IODP Hole 340-U1398B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.710763
title: (Table 3) Molecular and isotopic properties of hydrate-bound gases from ODP Site 204-1245

description: Gas concentrations are given as volume parts of natural gases. Zero values = not detected.
DOI: 10.1594/pangaea.848057
title: (Tables 1+4) Sample site substratum and morphometrics and damage levels of different populations of Laternula elliptica around Antarctica

description: We document differences in shell damage and shell thickness in a bivalve mollusc (Laternula elliptica) from seven sites around Antarctica with differing exposures to ice movement. These range from 60% of the sea bed impacted by ice per year (Hangar Cove, Antarctic Peninsula) to those protected by virtually permanent sea ice cover (McMurdo Sound). Patterns of shell damage consistent with blunt force trauma were observed in populations where ice scour frequently occurs; damage repair frequencies and the thickness of shells correlated positively with the frequency of iceberg scour at the different sites with the highest repair rates and thicker shells at Hangar Cove (74.2% of animals damaged) compared to the other less impacted sites (less than 10% at McMurdo Sound). Genetic analysis of population structure using Amplified Fragment Length Polymorphisms (AFLPs) revealed no genetic differences between the two sites showing the greatest difference in shell morphology and repair rates. Taken together, our results suggest that L. elliptica exhibits considerable phenotypic plasticity in response to geographic variation in physical disturbance.
description: Supplement to: Harper, Elizabeth M; Clark, Melody S; Hoffman, Joseph I; Philipp, Eva E R; Peck, Loyd S; Morley, Simon A (2012): Iceberg Scour and Shell Damage in the Antarctic Bivalve Laternula elliptica. PLoS ONE, 7(9), e46341
DOI: 10.1594/pangaea.870153
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_IX_18a
DOI: 10.1594/pangaea.829261
title: P-Wave velocity (PWC) from IODP Hole 340-U1399A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.494672
title: Physical oceanography during cruise K58_1994
DOI: 10.1594/pangaea.870207
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_VII_24