cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.963461
title: Physical oceanography from mooring KPO_1237

description: GEOMAR moorings are typically equipped with instruments recording pressure, temperature, conductivity, dissolved oxygen and current velocity. Instruments with pressure, temperature, conductivity and oxygen sensors were calibrated in situ immediately prior to and after a mooring deployment period by attaching them to the CTD frame during CTDO casts. Correction terms were then developed from the difference between the sensor readings and the calibrated CTDO data during several minute long calibration stops. These correction terms were then applied to the full deployment periods. This ensured best data quality with recognition of potential sensor drifts and also allowed for the estimation of calibration and measurement errors (Hahn et al. 2014, Bittig et al. 2018, Berx et al. 2019).
description: instrument = Label:kpo_1237_03 File:kpo_1237_instr_03.nc Type:Teledyne RDI QuarterMaster 150 SN:21861instrument = Label:kpo_1237_04 File:kpo_1237_instr_04.nc Type:GEOMAR TD-Logger SN:57instrument = Label:kpo_1237_05 File:kpo_1237_instr_05.nc Type:Teledyne RDI LongRanger 75 SN:17570instrument = Label:kpo_1237_06 File:kpo_1237_instr_06.nc Type:Seabird MicroCat 37-SM mit P SN:10689instrument = Label:kpo_1237_07 File:kpo_1237_instr_07.nc Type:Aanderaa Optode 3830 SN:01074 depth/pressure data was at least partially derived and not directly measured, consult quality flags for detailsinstrument = Label:kpo_1237_09 File:kpo_1237_instr_09.nc Type:Seabird MicroCat 37-SM mit P SN:06858instrument = Label:kpo_1237_10 File:kpo_1237_instr_10.nc Type:Aanderaa Optode 3830 SN:00219 depth/pressure data was at least partially derived and not directly measured, consult quality flags for detailsinstrument = Label:kpo_1237_11 File:kpo_1237_instr_11.nc Type:Seabird MicroCat 37-IM SN:07417 depth/pressure data was at least partially derived and not directly measured, consult quality flags for detailsinstrument = Label:kpo_1237_13 File:kpo_1237_instr_13.nc Type:Nortek Aquadopp Seriell SN:P26209-34instrument = Label:kpo_1237_14 File:kpo_1237_instr_14.nc Type:McLane Profiler MMP SN:11617instrument = Label:kpo_1237_15 File:kpo_1237_instr_15.nc Type:Nortek Aquadopp Seriell SN:P26209-24instrument = Label:kpo_1237_16 File:kpo_1237_instr_16.nc Type:Nortek Aquadopp Seriell SN:P27523instrument = Label:kpo_1237_17 File:kpo_1237_instr_17.nc Type:Seabird MicroCat 37-SM SN:08947 depth/pressure data was at least partially derived and not directly measured, consult quality flags for details
DOI: 10.1594/pangaea.663313
title: Oceanography at CTD/bottle station IFREMER_0153
DOI: 10.1594/pangaea.963540
title: Radiosonde measurements from station Budapest (2023-09)
DOI: 10.1594/pangaea.665584
title: Oceanography at CTD/bottle station IFREMER_2424
DOI: 10.1594/pangaea.859202
title: Continuous nitrate measurements at Schwingbachtal Studienlandschaft, Germany (growing season 2013-2014)
DOI: 10.1594/pangaea.663862
title: Oceanography at CTD/bottle station IFREMER_0702
DOI: 10.1594/pangaea.663939
title: Oceanography at CTD/bottle station IFREMER_0780
DOI: 10.1594/pangaea.664749
title: Oceanography at CTD/bottle station IFREMER_1589
DOI: 10.1594/pangaea.665138
title: Oceanography at CTD/bottle station IFREMER_1978
DOI: 10.1594/pangaea.963587
title: Radiosonde measurements from station Barrow (2018-01)

description: Start location: Point Barrow; Distance from radiation site: 8 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.963591
title: Radiosonde measurements from station Barrow (2018-11)

description: Start location: Point Barrow; Distance from radiation site: 8 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.665997
title: Oceanography at CTD/bottle station IFREMER_2823
DOI: 10.1594/pangaea.963592
title: Radiosonde measurements from station Barrow (2018-12)

description: Start location: Point Barrow; Distance from radiation site: 8 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.666007
title: Oceanography at CTD/bottle station IFREMER_2833
DOI: 10.1594/pangaea.963588
title: Basic and other measurements of radiation at station Barrow (2018-01)
DOI: 10.1594/pangaea.665167
title: Oceanography at CTD/bottle station IFREMER_2007
DOI: 10.1594/pangaea.963593
title: Basic and other measurements of radiation at station Barrow (2018-11)
DOI: 10.1594/pangaea.963543
title: Water record of Magallana angulata F1 generation during laboratory experiments in 2020/2021

description: The basic observed water characteristics (pH, temperature, salinity and total alkalinity (TA)) and calculated water carbonate chemistry of Magallana angulata (also known as Crassostrea angulata) F1 generation from larval stage to adult in the hatchery located in Zhanjiang, China (21.07°N, 110.74°E) for around one year. These F1 larvae were acquired by artificial fertilization of matured F0 generation (F0_8.1 and F0_7.4). Embryos from F0_8.1 were separated into two pH levels: F1_8.1-8.1 and F1_8.1-7.4. Likewise, embryos from F0_7.4 were separated into two pH levels: F1_7.4-8.1 and F1_7.4-7.4. Thus, there were four treatments for F1 generation, and each treatment had three independent 500L tank replicates (A, B, and C). F1 generation continued to be reared to the next year till most of them reached the first year of gonad maturation to test the transgenerational low pH effect on oyster biological responses. Low pH was driven by bubbling of CO2-enriched air mixed with ambient air into filter seawater in the treatment tanks. pH and temperature were monitored daily with pH meter (Mettler Toledo InLab®, Switzerland) calibrated with NBS standards. Salinity was monitored using a dual-scale refractometer (MingRui, China). The seawater was utterly changed every two days during larval stage and every week for juvenile stage. About 50 mL of seawater was preserved with HgCl2 for total alkalinity (TA) measurement. The TA was measured using an alkalinity titrator (Mettler Toledo G20S Compact Titrator, Switzerland), and pCO2, CO32-, saturation states of calcite and aragonite were calculated by CO2SYS program with equilibrium constants K2 and KSO4 (Millero, F. J., Graham, T. B., Huang, F., Bustos-Serrano, H., & Pierrot, D. (2006). Dissociation constants of carbonic acid in seawater as a function of salinity and temperature. Marine Chemistry, 100(1), 80-94. https://doi.org/10.1016/j.marchem.2005.12.001
DOI: 10.1594/pangaea.665203
title: Oceanography at CTD/bottle station IFREMER_2043
DOI: 10.1594/pangaea.963544
title: Water record of immune response to transgenerational ocean acidification in Magallana angulata F2 generation during laboratory experiments in 2021/2022

description: The basic observed water characteristics (pH, temperature, salinity) of Magallana angulata (also known as Crassostrea angulata) F2 generation from larval stage to adult in the hatchery located in Zhanjiang, China (21.07°N, 110.74°E) for around one year. The F2 larvae were acquired by artificial fertilization of matured F1 generation (F1_8.1-8.1 and F1_7.4-7.4). Embryos from F1_8.1-8.1 were separated into two pH levels: F2_8.1-8.1-8.1 and F2_8.1-8.1-7.4. The embryos from F1_7.4-7.4 were separated into two pH levels: F2_7.4-7.4-8.1 and F2_7.4-7.4-7.4. There were four treatments for F2 generation and reared till 2022 to test the transgenerational OA effects on oyster biological and immunological responses. Low pH was driven by bubbling of CO2-enriched air mixed with ambient air into filter seawater in the treatment tanks. pH and temperature were monitored daily with pH meter (Mettler Toledo InLab®, Switzerland) calibrated with NBS standards. Salinity was monitored using a dual-scale refractometer (MingRui, China). The seawater was utterly changed every two days during larval stage and every week for juvenile stage.
DOI: 10.1594/pangaea.664818
title: Oceanography at CTD/bottle station IFREMER_1658
DOI: 10.1594/pangaea.665247
title: Oceanography at CTD/bottle station IFREMER_2087
DOI: 10.1594/pangaea.665293
title: Oceanography at CTD/bottle station IFREMER_2133
DOI: 10.1594/pangaea.664871
title: Oceanography at CTD/bottle station IFREMER_1711
DOI: 10.1594/pangaea.665091
title: Oceanography at CTD/bottle station IFREMER_1931
DOI: 10.1594/pangaea.664915
title: Oceanography at CTD/bottle station IFREMER_1755
DOI: 10.1594/pangaea.665875
title: Oceanography at CTD/bottle station IFREMER_2701
DOI: 10.1594/pangaea.665907
title: Oceanography at CTD/bottle station IFREMER_2733
DOI: 10.1594/pangaea.665549
title: Oceanography at CTD/bottle station IFREMER_2389
DOI: 10.1594/pangaea.665942
title: Oceanography at CTD/bottle station IFREMER_2768
DOI: 10.1594/pangaea.477211
title: Hydrochemistry measured on water bottle samples at station NPac_1984_WT_152W/62-1

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.665876
title: Oceanography at CTD/bottle station IFREMER_2702
DOI: 10.1594/pangaea.958737
title: Nature of pastoral activities and main trees in Lake Gers catchment over the last 4600 years

description: Method used to produce the sedimentary DNA datasets: DNA sequences were produced by using g (5'-GGGCAATCCTGAGCCAA-3') and h (5'-CCATTGAGTCTCTGCACCTATC-3') primers for plants and MamP007F (5'-CGAGAAGACCCTATGGAGCT-3') and MamP007R (5'-CCGAGGTCRCCCCAACC-3') primers and the human-blocking primer (5'-GGAGCTTTAATTTATTAATGCAAACAGTACCC-3') for mammals. The sequences have been produced by the Illumina technology (HiSeq instrument). The bioinformatic treatment of the sequences was operated applying the Obitool program (Boyer, F. et al. OBITOOLS:aUNIX-inspired software package for DNA metabarcoding. Mol. Ecol. Resour. 16, 176–182 (2016)) and following the procedure described in Giguet-Covex et al. New insights on lake sediment DNA from the catchment: importance of taphonomic and analytical issues on the record quality. Scientific Reports. 9, 14676 (2019) (DOI https://doi.org/10.1038/s41598-019-50339-1). Then, other filtering processing were performed as also described in Giguet-Covex et al. 2019. These second treatments allow for removing 1) taxa assigned to a reference taxon at &lt;95 % of sequence identity, 2) potential contaminations (based on sampling, extraction and PCR controls, and recognition of exotic taxa) and 3) stochastic detections. Several analytical replicates by samples were performed (8 for both, the plants and mammals). Data are presented in number of positive replicates by sample. A replicate is considered as positive if more than 5 sequences are detected.
DOI: 10.1594/pangaea.958744
title: Sporormiella spore concentration in Lake Gers sediments over the last 4600 years
DOI: 10.1594/pangaea.963633
title: Ozone measurements from station Izaña (2023-09)
DOI: 10.1594/pangaea.963448
title: Expanded measurements from station Ny-Ålesund (2023-09)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.963449
title: Expanded measurements from station Ny-Ålesund (2023-10)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.963634
title: Ultra-violet measurements from station Izaña (2023-09)
DOI: 10.1594/pangaea.905362
title: Sea surface temperature calculations from sediment core GEOFAR KF16 upper 2 m
DOI: 10.1594/pangaea.963635
title: Radiosonde measurements from station Izaña (2023-09)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.963636
title: Meteorological synoptical observations from station Izaña (2023-10)
DOI: 10.1594/pangaea.905364
title: Foraminifer composition of sediment core KF16 upper 2 m
DOI: 10.1594/pangaea.910544
title: Foraminifer composition of sediment core KF16 in 5-124m depth
DOI: 10.1594/pangaea.963616
title: Abundance of sclerobionts and presence of malformation on Middle Devonian brachiopods from Skały, Poland (Dobruchna Member, Skały Formation)

description: Brachiopod shells were collected from a large heap adjacent to the Semav Stones Skała Quarry in Skały (Holy Cross Mountains, Poland) in order to describe sclerobiont diversity, abundance and colonization patterns. All specimens derive from the Dobruchna Brachiopod Shale Member of the shaly-calcareous Skały Formation (ensensis conodont Zone, Eifelian). Both articulated shells and isolated valves were sampled, but fragmentary specimens were excluded. Each brachiopod specimens (separately dorsal and ventral valves) was inspected under a binocular microscope for the presence of sclerobionts and shell malformations. Each sclerobiont was determined to the lowest possible taxonomic level and counted. Well-separated colonies of clonal epibionts were treated as separate specimens. Only brachiopod specimens with at least one sclerobiont or malformation are included in the dataset.
DOI: 10.1594/pangaea.747657
title: Meteorological observations during BLANCHE cruise from St. Johns to Woodmans Bay Dominica started at 1793-04-11
DOI: 10.1594/pangaea.747660
title: Meteorological observations during BLANCHE cruise from Halifax to Basse Terre started at 1794-09-22
DOI: 10.1594/pangaea.963637
title: Ozone measurements from station Izaña (2023-10)
DOI: 10.1594/pangaea.963638
title: Ultra-violet measurements from station Izaña (2023-10)
DOI: 10.1594/pangaea.958764
title: Nature of pastoral activities in Lake Verney catchment over the last 4600 years from sedimentary DNA and Sporormiella spores

description: Method used to produce the sediment DNA datasets: DNA sequences were generated using g (5'-GGGCAATCCTGAGCCAA-3') and h (5'-CCATTGAGTCTCTGCACCTATC-3') primers for plants and MamP007F (5'-CGAGAAGACCCTATGGAGCT-3') and MamP007R (5'-CCGAGGTCRCCCCAACC-3') primers and the human-blocking primer (5'-GGAGCTTTAATTTATTAATGCAAACAGTACCC-3') for mammals. The sequences have been produced by the Illumina technology (HiSeq instrument). The bioinformatic treatment of the sequences was operated applying the Obitool program (Boyer, F. et al. OBITOOLS:aUNIX-inspired software package for DNA metabarcoding. Mol. Ecol. Resour. 16, 176–182 (2016)) and following the procedure described in Giguet-Covex et al. New insights on lake sediment DNA from the catchment: importance of taphonomic and analytical issues on the record quality. Scientific Reports. 9, 14676 (2019) (DOI https://doi.org/10.1038/s41598-019-50339-1). Further filtering treatments were then applied, as also described in Giguet-Covex et al. 2019. These second treatments allow the removal of 1) taxa assigned to a reference taxon at &lt;95 % of sequence identity, 2) potential contaminations (based on sampling, extraction and PCR controls, and recognition of exotic taxa) and 3) stochastic detections. Several analytical replicates by samples were performed (12 for both, the plants and mammals). Data are presented in number of positive replicates by sample. A replicate is considered as positive if more than 5 sequences are detected.
DOI: 10.1594/pangaea.749913
title: Meteorological observations during JUNO cruise from Vlissingen to Batavia started at 1783-03-03
DOI: 10.1594/pangaea.666002
title: Oceanography at CTD/bottle station IFREMER_2828
DOI: 10.1594/pangaea.963639
title: Radiosonde measurements from station Izaña (2023-10)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.476132
title: Hydrochemistry measured on water bottle samples at station IndianOcean_1976_AN_18S/2269

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.825568
title: Reflectance spectroscopy and colorimetry from IODP Hole 329-U1371D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.825571
title: Thermal conductivity of IODP Hole 329-U1371D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.958701
title: Nature of pastoral activities and trees in Lake Anterne catchment over the Holocene

description: Method used to produce the sediment DNA datasets: DNA sequences were generated using g (5'-GGGCAATCCTGAGCCAA-3') and h (5'-CCATTGAGTCTCTGCACCTATC-3') primers for plants and MamP007F (5'-CGAGAAGACCCTATGGAGCT-3') and MamP007R (5'-CCGAGGTCRCCCCAACC-3') primers and the human-blocking primer (5'-GGAGCTTTAATTTATTAATGCAAACAGTACCC-3') for mammals. The sequences have been produced by the Illumina technology (HiSeq instrument). The bioinformatic treatment of the sequences was operated applying the Obitool program (Boyer, F. et al. OBITOOLS:aUNIX-inspired software package for DNAmetabarcoding. Mol. Ecol. Resour. 16, 176–182 (2016)) and following the procedure described in Giguet-Covex et al. New insights on lake sediment DNA from the catchment: importance of taphonomic and analytical issues on the record quality. Scientific Reports. 9, 14676 (2019) (DOI https://doi.org/10.1038/s41598-019-50339-1). Further filtering treatments were then applied, as also described in Giguet-Covex et al. 2019. These second treatments allow the removal of 1) taxa assigned to a reference taxon at &lt;95 % of sequence identity, 2) potential contaminations (based on sampling, extraction and PCR controls, and recognition of exotic taxa) and 3) stochastic detections. Several analytical replicates by samples were performed (8 for both, the plants and mammals). Data are presented in number of positive replicates by sample. A replicate is considered as positive if more than 5 sequences are detected.
DOI: 10.1594/pangaea.963664
title: Radiosonde measurements from station Budapest (2023-07)
DOI: 10.1594/pangaea.963279
title: Continuous water temperature, salinity and oxygen data in front of GEOMAR Pier, Kiel, Germany (2020-2022)

description: From January 2020 to January 2022, temperature, salinity, and oxygen (only July 2020 - April 2021) data were logged with an AANDERAA oxygen sensor 3835 and a SEABIRD SBE 37-SI MicroCAT CT(D) in 10-minutes intervals at GEOMAR (Kiel, Germany) pier at 54°19'48.8N 10°08'59.6E. The sensor system is mounted to a floating platform such that a continuous depth of 1 m is ensured at any time. Oxygen data were corrected for salinity, temperature and depth following the manual for Aanderaa Optodes using the salinity and temperature measurements from the SEABIRD SBE 37-SI MicroCAT CT(D) sensor. After cleaning and other re-boots of the sensor package, temperature, salinity and oxygen data tend to deviate from true values. Hence, 60 minutes of data after any re-boot (after sensor servicing with re-deployment, data download or power failure) were deleted. Two major data gaps (January 2020 – July 2020, April 2021 – June 2021) are due to longer periods when the sensors were serviced in the workshop.
DOI: 10.1594/pangaea.963280
title: Water temperature, salinity and oxygen data in front of GEOMAR Pier, Kiel, Germany (2020-2021)

description: From January 2020 to October 2021, seawater temperature and salinity data were measured repeatedly by a hand-held salinity probe (WTW Handheld ProfiLine Multi 3320 with conductivity measuring cell TetraCon 325) at GEOMAR (Kiel, Germany) pier at 54°19'48.8N 10°08'59.6E. The seawater was continuously pumped from 1m depth to a container on the 'Kiel Outdoor Benthocosm' (KOB) platform in which the measurement took place. The sensor was calibrated prior to each measurement.
DOI: 10.1594/pangaea.963632
title: Meteorological synoptical observations from station Izaña (2023-09)
DOI: 10.1594/pangaea.963281
title: Continuous water temperature and salinity data in front of GEOMAR Pier, Kiel, Germany (2022-2023)

description: From January 2022 to May 2023, temperature and salinity (only until March 2023) data were logged with a SEABIRD SBE 37-SMP MicroCAT CT in 2-minutes intervals at GEOMAR (Kiel, Germany) pier at 54°19'48.8N, 10°08'59.6E. The sensor system is mounted to a floating platform to ensure a continuous depth of 1 m at any time. After cleaning and other re-boots of the sensor package, temperature and salinity data tend to deviate from true values. Hence, 60 minutes of data after any re-boot (after sensor servicing with re-deployment, data download or power failure) were deleted. Due to massive fouling the conductivity sensor caused false salinity data during the last two months of this measurement period which were, hence, also deleted from the data set.
DOI: 10.1594/pangaea.963282
title: Water temperature and salinity data in front of GEOMAR Pier, Kiel, Germany (2022-2023)

description: From June 2022 to May 2023, seawater temperature and salinity data were measured repeatedly by a hand-held salinity probe (WTW Handheld ProfiLine Multi 3320 with conductivity measuring cell TetraCon 325) at GEOMAR (Kiel, Germany) pier at 54°19'48.8N 10°08'59.6E. The seawater was continuously pumped from 1m depth to a container on the 'Kiel Outdoor Benthocosm' (KOB) platform in which the measurement took place. The sensor was calibrated prior to each measurement.
DOI: 10.1594/pangaea.904082
title: Stable water isotope data of ice wedges at the Adycha River (Figure 6)
DOI: 10.1594/pangaea.904083
title: Stable water isotope data of ice wedges at the Batagay megaslump (Figure 6)
DOI: 10.1594/pangaea.904084
title: 16. Spatial comparison of stable water isotope data of ice wedges at Batagay
DOI: 10.1594/pangaea.904085
title: 09. Spatial comparison of stable water isotope data of ice wedges at New Siberian Islands, Belkovsky
DOI: 10.1594/pangaea.747783
title: Meteorological observations during BURFORD cruise from Gibraltar to Plymouth started at 1768-04-06
DOI: 10.1594/pangaea.750351
title: Meteorological observations during LASCELLES cruise from Gravesend to Madras started at 1787-01-22
DOI: 10.1594/pangaea.476579
title: Hydrochemistry measured on water bottle samples at station NAtl_1983_6N_37W/96

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.904087
title: 08. Spatial comparison of stable water isotope data of ice wedges at Buor Khaya
DOI: 10.1594/pangaea.904091
title: 11. Spatial comparison of stable water isotope data of ice wedges at New Siberian Islands, Kotel'ny
DOI: 10.1594/pangaea.548143
title: Nutrients and bacteria measured on water bottle samples at station Chip_2003-11-27_07, Chipana, Chile
DOI: 10.1594/pangaea.904088
title: 06. Spatial comparison of stable water isotope data of ice wedges at Bykovsky
DOI: 10.1594/pangaea.904089
title: 15. Spatial comparison of stable water isotope data of ice wedges at Duvanny Yar
DOI: 10.1594/pangaea.904086
title: 12. Spatial comparison of stable water isotope data of ice wedges at New Siberian Islands, Bol'shoy Lyakhovsky Island
DOI: 10.1594/pangaea.904090
title: 03. Spatial comparison of stable water isotope data of ice wedges at Lena Delta, Khardang
DOI: 10.1594/pangaea.904093
title: 01. Spatial comparison of stable water isotope data of ice wedges at Mamontov Klyk
DOI: 10.1594/pangaea.477881
title: Hydrochemistry measured on water bottle samples at station SPac_1971_HH_150-100W/23

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.496946
title: Physical oceanography from BT during cruise M909E00006B_1987
DOI: 10.1594/pangaea.477348
title: Hydrochemistry measured on water bottle samples at station NPac_1985_TT_47Na/85-1

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.904094
title: 18. Spatial comparison of stable water isotope data of ice wedges at Central Yakutia, Mamontova Gora
DOI: 10.1594/pangaea.750448
title: Meteorological observations during LILLY cruise from Halifax to Bermuda started at 1800-10-26