cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.547745
title: Delta 44/40 Ca, Mg/Ca and Sr/Ca record of Globigerinoides sacculifer and calculated temperatures and salinity changes of ODP Hole 165-999A

description: The delta18O values of planktonic foraminifera increased in the Caribbean by about 0.5‰ relative to the equatorial East Pacific values between 4.6 and 4.2 Ma as a consequence of the closure of the Central American Gateway (CAG). This increase in delta18O can be interpreted either as an increase in Caribbean sea surface (mixed layer) salinity (SSS) or as a decrease in sea surface temperatures (SST). This problem represents an ideal situation to apply the recently developed paleotemperature proxy delta44/40Ca together with Mg/Ca and d18O on the planktic foraminifer Globigerinoides sacculifer from ODP Site 999. Although differences in absolute temperature calibration of delta44/40Ca and Mg/Ca exist, the general pattern is similar indicating a SST decrease of about 2-3 8C between 4.4 and 4.3 Ma followed by an increase in the same order of magnitude between 4.3 and 4.0 Ma. Correcting the delta18O record for this temperature change and assuming that changes in global ice volume are negligible, the salinity-induced planktonic delta18O signal decreased by about 0.4‰ between 4.4 and 4.3 Ma and increased by about 0.9‰ between 4.3 and 4.0 Ma in the Caribbean. The observed temperature and salinity trends are interpreted to reflect the restricted exchange of surface water between the Caribbean and the Pacific in response to the shoaling of the Panamanian Seaway, possibly accompanied by a southward shift of the Intertropical Convergence Zone (ITCZ) between 4.4 and 4.3 Ma. Differences in Mg/Ca- and delta44/40Ca-derived temperatures can be reconciled by corrections for secular variations of the marine Mg/Ca[sw] and delta44/40Ca, a salinity effect on the Mg/Ca ratio and a constant temperature offset of ~2.5 °C between both SST proxy calibrations.
description: Supplement to: Gussone, Nikolaus; Eisenhauer, Anton; Tiedemann, Ralf; Haug, Gerald H; Heuser, Alexander; Bock, Barbara; Nägler, Thomas F; Müller, A (2004): Reconstruction of Caribbean Sea surface temperature and salinity fluctuations in response to the Pliocene closure of the Central American gateway and radiative forcing, using d44/40Ca, d18O and Mg/Ca ratios. Earth and Planetary Science Letters, 227(3-4), 201-214
DOI: 10.1594/pangaea.821993
title: (Table 1) Typical trace-fossil occurrences in DSDP Holes 56-436 and 56-435A

description: Trace fossils are in places abundant in cores from DSDP Leg 56 sites. They are particularly rich in the pelagic-clay sequence at Site 436. Some significant trace fossils, including Zoophycos, Teichichnus, Chondrites, rind and solid burrows, and pellet-armored rods, are described. The ichnofauna, except for pellet-armored rods in diatomaceous mudstone of the landward trench slope, is characterized by cosmopolitan bathyal to abyssal forms.
description: Supplement to: Okada, Hakuyu (1980): Trace fossils in Cores from Deep Sea Drilling Project Sites 434, 435, and 436 (Japan Trench Transect). In: Scientific Party, Initial Reports of the Deep Sea Drilling Project, 56/57 (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 56-57, 911-919
DOI: 10.1594/pangaea.747165
title: Meteorological observations during ADDER cruise from Curaçao to Suriname started at 1849-06-14
DOI: 10.1594/pangaea.693816
title: Zoobenthos in surface sediments during Professor Vodyanitskiy cruise PV32

description: The Ocean grab was taken at each station using a 0.25 m**2. The samples were sieved through a creen with 1 mm mesh size and were preserved in 40% alcohol, for subsequent sorting and identifing in the laboratory. On the basis of taxon scores, the means of total zoobenthos abundance and total benthos biomass were calculated.
DOI: 10.1594/pangaea.818808
title: Glacier mass balance Hintereisferner, Ötztal Alps, Austria, 1986/1987
DOI: 10.1594/pangaea.760698
title: (Appendix B) Directions of characteristic magnetization of Triassic sediments in ODP Hole 122-760A

description: The NRM column represents the initial NRM intensity of each sample, the demagnetization step column refers to the highest step attained during the treatment of each sample.
DOI: 10.1594/pangaea.804537
title: (Table 1) Diatom biostratigraphy in ODP Site 164-997 sediments

description: Ocean Drilling Program Site 997 is located on the Blake Ridge, which underlies a periphery of the subtropical central gyre and is under the profound influence of the warm saline Gulf Stream as well as the Western Boundary Undercurrent (WBUC), which carried the clastic materials to the Blake Ridge as sediment drift. The shipboard study of nannofossils and sedimentary particles revealed a downward increase in sedimentation rate and a higher concentration of diatoms in three stratigraphic intervals (Shipboard Scientific Party, 1996). Thus, the stratigraphic change in diatom accumulation rate is important to understand the paleoceanographic and depositional history of this region. We have been studying the time-progressive change of diatom flora at Site 997 by quantitatively observing the flora in 141 samples selected from the entire sequence recovered from Holes 997A and 997B. These samples were chosen to represent a time interval of 50 k.y. Some of the results currently obtained through this study are presented in this data report.
description: Sediment depth is given in mbsf. All diatoms were identified and counted under a light microscope with magnification of 600? until the total number exceeded 200 (resting spores of Chaetoceros spp. were not included).
description: Supplement to: Ikeda, Akihiro; Okada, Hisatake; Koizumi, Itaru (2000): Data Report: Late Miocene to Pleistocene diatoms from the Blake Ridge, Site 997. In: Paull, CK; Matsumoto, R; Wallace, PJ; Dillon, WP (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 164, 1-12
DOI: 10.1594/pangaea.811481
title: (Table S1) Coverage, growth traits and leaf chemistry of five Arctic tundra plant species at Alexandra Fiord

description: For several variables, not all species were sampled in all plots.
DOI: 10.1594/pangaea.820073
title: (Table 2) Composition of n-alkanes and the isoprenoids pristane and phytane at DSDP Leg 60 Holes

description: #1 = Marine/terrestrial n-alkanes is given by S = (n-C21 + n-C22)/(n-C28 + n-C29) (Philippi, 1974).
DOI: 10.1594/pangaea.917278
title: 1-Hz PPP displacements at GEONET station 1112 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.704855
title: Radiosonde measurements from station Kwajalein (2005-12)
DOI: 10.1594/pangaea.819739
title: (Table 3) Rare-earth elements, barium, and scandium abundances at DSDP Hole 62-465A

description: Empty cells mean no data.
DOI: 10.1594/pangaea.855013
title: Trace metal composition of the aerosol at Neumayer Station, Antarctica during the year 2003

description: Aerosol was continuously sampled by sucking ambient air with a flow rate of 120 m**3/h through Whatman 541 filters (diameter 240 mm) using a ventilated electropolished stainless steel inlet stack (total height about 8 m above the snow surface) with a 50% aerodynamic cut-off diameter around 7-10 µm. Trace element analysis was performed by means of inductively coupled plasma - quadrupol mass spectrometry (ICP-QMS, ELAN 6000, Sciex/Perkin Elmer) equipped with a cross-flow nebulizer as sample introduction system. For trace element analyses we chose a total digestion of the samples with a pressurized digestion system (DAS 100, Picotrace) at 200°C in a mixture containing HNO3 (suprapure, 65%, Merck, sub-boiling bi-distilled), HF (suprapure, 40%, Merck, sub-boiling bi-distilled) and H2O2 (suprapure, 30%, Merck). With this device a series of 24 samples could be digested in parallel. Each series included one filter blank and a certified reference sample (NIST 1648 urban particulate matter). For calibration we used commercially available standard solutions (104 ppb multi-element verification standard 1 and 2, Perkin Elmer) which were generally applied in 1 ppb, 10 ppb, and 100 ppb concentrations (1 ppb corresponds to 1 ng of each element in 1 g solute). Each sample was spiked by 10 ppb Rh as internal standard to normalize the signal intensities and compensate instrumental sensitivity variations. We conservatively estimated the method detection limits (MDL) as three times the standard deviation (std) of the overall blank values. Values below the MDL are given as "&lt; respecting MDL value" (e.g.: &lt;0.02) in the table. Concentrations not determined are marked with empty cells. The combined uncertainty of the analyses is approximately between ±8% and ±12% for element concentrations above three times the corresponding MDL. It increased from around ±(15-20)% approaching 3xMDL level to roughly (+50/-100)% close to the MDL. The final atmospheric concentrations (in ng/m**3 = 10**(-9) g/m**3, or pg/m**3 = 10**(-12) g/m**3) were calculated from the blank corrected element amounts and the corrected sampled air volume to standard conditions (273.16 K and 1013 hPa).
DOI: 10.1594/pangaea.673369
title: Radiosonde measurements from station Barrow (1995-10)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.673517
title: Radiosonde measurements from station Bermuda (1998-12)

description: Start location: Bermuda; Distance from radiation site: 2 km
DOI: 10.1594/pangaea.705531
title: Late Eocene to Early Oligocene magnetostratigraphic chron boundaries of ODP Hole 119-744A (Table 1)

description: The earliest Oligocene (~33.5 Ma) is marked by a major step in the long-term transition from an ice-free to glaciated world. The transition, characterized by both cooling and ice-sheet growth, triggered a transient but extreme glacial period designated Oi-1. High-resolution isotope records suggest that Oi-1 lasted for roughly 400,000 yr (the duration of magnetochron 13N) before partially abating, and that it was accompanied by an ocean-wide carbon isotope anomaly of 0.75‰. One hypothesis relates the carbon isotope anomaly to enhanced export production brought about by climate-induced intensification of wind stress and upwelling, particularly in the Southern Ocean. To understand how this climatic event affected export production in the Southern Ocean, biogenic silica (opal) and carbonate accumulation rates were computed for the sub-polar Indian Ocean using deep-sea cores from ODP Site 744, Kerguelen Plateau. Our findings suggest that net productivity in this region increased by several fold in response to the Oi-1 glaciation. In addition, calcareous primary producers dominant in the Late Eocene were partially replaced by opaline organisms suggesting a trend toward seasonally greater surface divergence and upwelling in this sector of the Southern Ocean. We attribute these changes to intensification of atmospheric=oceanic circulation brought about by high-latitude cooling and the appearance of a full-scale continental ice-sheet on East Antarctica. Higher terrigenous sediment accumulation rates support the idea that wind-induced changes in regional productivity were augmented by an increased supply of glacial dust and debris that provided limiting micro-nutrients (e.g., iron-rich dust particles). We speculate that the rapid changes in biogenic sediment accumulation in the Southern Ocean and other upwelling-dominated regions contributed to the ocean-wide positive carbon isotope anomaly by temporarily increasing the burial rate of organic carbon relative to carbonate carbon. The changes in burial rates, in turn, may have produced a positive feedback on climate by briefly drawing down atmospheric pCO2 .
description: Supplement to: Salamy, Karen A; Zachos, James C (1999): Latest Eocene-Early Oligocene climate change and Southern Ocean fertility: inferences from sediment accumulation and stable isotope data. Palaeogeography, Palaeoclimatology, Palaeoecology, 145(1-3), 61-77
DOI: 10.1594/pangaea.665038
title: Oceanography at CTD/bottle station IFREMER_1878
DOI: 10.1594/pangaea.829295
title: Reflectance spectroscopy and colorimetry from IODP Hole 340-U1395B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.819974
title: (Table 2) Mineralogy at DSDP Holes 59-450 and 59-451

description: Sediment depth is given in mbsf. &lt;0.5 = trace; #1.5 = 1-2; #1 = about 1. Phillipsite, chlorite and kaolinite also searched for but not found.
DOI: 10.1594/pangaea.828787
title: Carbonate analysis from IODP Hole 339-U1387C

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.746705
title: Snow temperature time series at station P3 near Ny-Ålesund, Svalbard, Norway

description: Snow temperatures measured at three heights above ground
DOI: 10.1594/pangaea.854089
title: Radiosonde measurements from station South Pole (2015-09)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.819529
title: (Table 3) Mass-accumulation rates for the non-authigenic, inorganic, crystalline, eolian component of sediments recovered at DSDP Hole 62-466

description: Sediment depth is given in mbsf. Empty cells mean no data.
DOI: 10.15468/dl.vkwrqs
title: Occurrence Download

description: A dataset containing 1138 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is Human Observation",
 "CoordinateUncertaintyInMeters 0.0-10000.0",
 "Geometry POLYGON((-124.52953 25.08509,-97.65265 25.08509,-97.65265 40.49449,-124.52953 40.49449,-124.52953 25.08509))",
 "TaxonKey is Scantius aegyptius (Linnaeus, 1758)"
 ]
}

 The dataset includes 1138 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031242-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.819986
title: (Table 4) Minerals of bulk and fine-grained (2 µm) samples from DSDP Hole 60-456A

description: Sediment depth is given in mbsf. &lt;1 = trace. Phillipsite, wairakite, opal-CT, chlorite, attapulgite and serpentine also looked for but not found. A = abundant, P = present, T = trace, - = not found.
DOI: 10.1594/pangaea.819991
title: (Table 8) Minerals of bulk and fine-grained (2 µm) samples from DSDP Hole 60-460A

description: Sediment depth is given in mbsf. &lt;1 = trace. Carbonate, alkaline feldspar, clinoptilolite, analcime, illite chlorite, Fe-Mg chlorite, attapulgite and serpentine also looked for but not found.. A = abundant, P = present, T = trace, - = not found.
DOI: 10.1594/pangaea.915419
title: Other measurements at 10 m from station Rock Springs (2019-11)
DOI: 10.1594/pangaea.689994
title: Radiosonde M69_R001 during METEOR cruise M69 on 1984-07-20 08:25h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.819239
title: (Table 3) Clay minerals and their assemblages in Miocene through Quaternary sediments at DSDP Hole 63-470
DOI: 10.1594/pangaea.858119
title: Field temperatures along Taita Hills, Farm Mbangang-ombe
DOI: 10.1594/pangaea.858444
title: Time series of atmospheric water vapour at station UNSA_S1
DOI: 10.1594/pangaea.752294
title: Meteorological observations during Stad Utrecht cruise from Batavia to Padang started at 1840-04-22
DOI: 10.1594/pangaea.819412
title: (Table 6) Composition of carotenoid assemblages isolated from DSDP Leg 64 core samples

description: Sediment depth is given in mbfs. &lt;1 = indicated.
DOI: 10.1594/pangaea.735090
title: Other measurements at 30 m from station Payerne (2008-11)
DOI: 10.1594/pangaea.819312
title: (Table 1) Organic- and carbonate-carbon values and extract data for DSDP Hole 63-467
DOI: 10.1594/pangaea.818540
title: (Table 4) Chemical composition bulk solids at DSDP Leg 64 Holes
DOI: 10.1594/pangaea.818541
title: (Table 5) Bulk sediment atomic elemental ratios to aluminum at DSDP Leg 64 Holes

description: Blank spaces indicate that no data were obtained.
DOI: 10.1594/pangaea.819380
title: (Table 5) Distribution and abundance of calcareous-nannoplankton species in the Cretaceous sediments of DSDP Hole 62-465A

description: Sediment depth is given in mbsf. A = abundant, C= common, F = few, R = rare, VR = very rare, G = good, M = moderate, P = poor, + = present, X = cf., ? = questionable, - = not present, * = reworking/contamination, (+) = down-hole contamination, (x) = aff.
DOI: 10.1594/pangaea.818543
title: (Table 7) Protodolomite and dolomite geochemistry at DSDP Leg 64 Holes

description: Sediment depth is given in mbsf. Blank spaces indicate that no data were obtained.
DOI: 10.1594/pangaea.818974
title: (Table 3) Kerogen chemistry at DSDP Leg 64 Holes
DOI: 10.1594/pangaea.818102
title: (Table 2) Geochemistry of groundmass plagioclases from DSDP Hole 64-478

description: Cations per 8 oxygens.
DOI: 10.1594/pangaea.673981
title: Radiosonde measurements from station Boulder (1998-02)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.818257
title: (Table 2) Grain sizes of sediments from DSDP Leg 65 Holes

description: Sediment depth is given in mbsf. Empty cells mean not determined.
DOI: 10.1594/pangaea.677124
title: Ozone measurements from station Boulder (1997-10)

description: Location: Boulder, Colorado, USA; Distance from radiation site: 16 km
DOI: 10.1594/pangaea.818984
title: (Table 1) Amount of organic carbon and hydrocarbon yield at DSDP Leg 64 Holes
DOI: 10.1594/pangaea.776558
title: CNS-analysis from IODP Hole 331-C0014E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.846327
title: Potential of RapidEye image data from 2011-07-11 for sediment monitoring of the German tidal flats

description: This sediment classification is based on a preprocessed RapidEye data of 2011-07-11. The preprocessing steps comprises an atmospheric correction with ENVI's FLAASH, a Fast Fourier Transformation and a Maximum Noise Fraction Transform. The classification itself is a hierarichal decision tree with customized reflectance parameters. The overall accuracy is 66.85 % with a Kappa coefficient of 0.26. This classification was created within the project WiMo at the Institute for Geoinformatics and Remote Sensing (IGF) in Osnabrück.
DOI: 10.1594/pangaea.719062
title: Other measurements at 10 m from station Bondville (2006-11)
DOI: 10.1594/pangaea.494761
title: Physical oceanography during cruise M90BY000563
DOI: 10.1594/pangaea.719500
title: Other measurements at 10 m from station Bondville (2001-06)

description: Version 2, 2009-06-15
DOI: 10.1594/pangaea.775628
title: Continuous meteorological observations at station Ny-Ålesund (2004-08)
DOI: 10.1594/pangaea.817803
title: (Table 1) Bulk chemical compositions of basalts at DSDP Hole 66-487

description: Analyst, H. Haramura.
DOI: 10.1594/pangaea.817871
title: (Table 4) Geochemistry of basaltic glass and hyaloclastites at DSDP Holes 65-485A and 65-483
DOI: 10.1594/pangaea.818640
title: Feeding assays, direct grazing, fresh algae

description: Control: ungrazed piece of Ascophyllum nodosum; Treatment: previously grazed piece of Ascophyllum nodosum
DOI: 10.1594/pangaea.818070
title: (Table 1) Geochemistry and minerals of glass selvedges at DSDP Leg 65 Holes
DOI: 10.1594/pangaea.900553
title: Other measurements at 10 m from station Goodwin Creek (2018-11)
DOI: 10.1594/pangaea.611240
title: Grain size analysis of sediment core Lz1010 (Table A7)
DOI: 10.1594/pangaea.611261
title: Clay mineral composition of sediment core Lz1013 (Table A15)
DOI: 10.1594/pangaea.854617
title: Glacier mass balance Vernagtferner, Austria, 1993/1994
DOI: 10.1594/pangaea.665948
title: Oceanography at CTD/bottle station IFREMER_2774
DOI: 10.1594/pangaea.752692
title: Meteorological observations during VENUS cruise from St. Juan de Porte Rico to Curaçao started at 1850-05-09
DOI: 10.1594/pangaea.611083
title: Geochemistry from core profile Lz1005 (Table A24)
DOI: 10.1594/pangaea.818077
title: (Table 1) Samples studied and their lithologic units at DSDP Site 65-483
DOI: 10.1594/pangaea.758301
title: Meteorological data from Jubany Station, King George Island, Western Antarctic Peninsula, 1998
DOI: 10.1594/pangaea.748329
title: Hydrography on standard level calculated from water bottle samples of RV Islas Orcadas in 1978
DOI: 10.1594/pangaea.670266
title: Basic and other measurements of radiation at Neumayer Station (2000-12)
DOI: 10.1594/pangaea.854508
title: Glacier mass balance Vernagtferner, Brochkogel area, Austria, 2007/2008
DOI: 10.1594/pangaea.748863
title: Meteorological observations during El Colon cruise from La Coruña to La Habana started at 1775-11-04
DOI: 10.1594/pangaea.750005
title: Meteorological observations during KOERIER cruise from Nederland to Suriname started at 1852-03-05
DOI: 10.1594/pangaea.736126
title: Meteorological synoptical observations from station Lindenberg (1998-02)
DOI: 10.1594/pangaea.558180
title: Monthly landings from 1998 of Sardinops sagax sagax (Sardina) in San Andres, Pisco, Peru
DOI: 10.1594/pangaea.806611
title: (Table 1) Platinum group elements, copper and nickel concentrations in diabases of ODP Hole 140-504B
DOI: 10.1594/pangaea.858764
title: Habitat characteristics for Asian green mussels (Perna viridis), West Java, Indonesia (April 2012 - November 2013): nutritional status of mussels
DOI: 10.1594/pangaea.680178
title: Other measurements at 300 m from station Boulder (1992-07)
DOI: 10.1594/pangaea.748650
title: Meteorological observations during DORDRECHT cruise from Curacao to the Netherlands started at 1848-05-06
DOI: 10.1594/pangaea.916666
title: 1-Hz PPP displacements at GEONET station 0470 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.863111
title: Local geomagnetic K indices at station COI in 2010
DOI: 10.1594/pangaea.875867
title: Expanded measurements from station Lindenberg (2011-12)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.881523
title: Radiosonde measurements from station Barrow (2015-03)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.667731
title: Basic measurements of radiation at station Bermuda (1999-01)
DOI: 10.1594/pangaea.917064
title: 1-Hz PPP displacements at GEONET station 0888 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.669849
title: Basic measurements of radiation at station Ilorin (1997-12)

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.707678
title: Meteorological synoptical observations from station Payerne (2006-11)
DOI: 10.1594/pangaea.803171
title: Basic measurements of radiation at station Regina (2011-09)
DOI: 10.1594/pangaea.883233
title: Meteorological synoptical observations from station Lindenberg (2017-01)
DOI: 10.1594/pangaea.750428
title: Meteorological observations during LESPERANCE cruise from Bouton to Surabaya started at 1793-10-04
DOI: 10.1594/pangaea.923441
title: Hourly electricity generation of Loy Yang B coal power plant, Australia, 2010 - 2019
DOI: 10.1594/pangaea.674491
title: Radiosonde measurements from Neumayer Station (2004-01)
DOI: 10.1594/pangaea.912860
title: Other measurements at 10 m from station Fort Peck (2019-10)
DOI: 10.1594/pangaea.858804
title: Ozone measurements from Neumayer Station (2015-02)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.692318
title: Concentrations of chlorophyll-alpha in sea water from the euphotic zone at Station MARCH-94-GN3619940280100590 in the Aegean Sea

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).
DOI: 10.1594/pangaea.817196
title: Core summary for IODP Hole 343-C0019E
DOI: 10.1594/pangaea.611468
title: Some properties of the studied lakes in Central and North-east Yakutia, Appendix 2-2