cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.810715
title: (Table 1) Moisture content of buried snowpack deposit samples from Pearse Valley, McMurdo Dry Valleys

description: Buried snowpack deposits are found within the McMurdo Dry Valleys of Antarctica, which offers the opportunity to study these layered structures of sand and ice within a polar desert environment. Four discrete buried snowpacks are studied within Pearse Valley, Antarctica, through in situ observations, sample analyses, O-H isotope measurements and numerical modelling of snowpack stability and evolution. The buried snowpack deposits evolve throughout the year and undergo deposition, melt, refreeze, and sublimation. We demonstrate how the deposition and subsequent burial of snow can preserve the snowpacks in the Dry Valleys. The modelled lifetimes of the buried snowpacks are dependent upon subsurface stratigraphy but are typically less than one year if the lag thickness is less than c. 7 cm and snow thickness is less than c. 10 cm, indicating that some of the Antarctic buried snowpacks form annually. Buried snowpacks in the Antarctic polar desert may serve as analogues for similar deposits on Mars and may be applicable to observations of the north polar erg, buried ice at the Mars Phoenix landing site, and observations of buried ice throughout the martian Arctic. Numerical modelling suggests that seasonal snows and subsequent burial are not required to preserve the snow and ice on Mars.
description: Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150
description: Supplement to: Heldmann, J L; Marinova, M; Williams, K E; Lacelle, Denis; McKay, Christopher P; Davila, A; Pollard, W; Andersen, D T (2012): Formation and evolution of buried snowpack deposits in Pearse Valley, Antarctica, and implications for Mars. Antarctic Science, 24(03), 299-316
DOI: 10.1594/pangaea.475978
title: Geochemistry of sediment core M1_MULT202 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.742328
title: (Table 2) Fe and S speciation in bottom sediments of the Black Sea
DOI: 10.1594/pangaea.472312
title: Sediment analyses of surface sediments of the Persian Gulf (Table 12)
DOI: 10.1594/pangaea.815902
title: (Table 2) Metal concentrations in different tissues of Glaucous Gulls (Larus hyperboreus) from Bjørnøya and Jan Mayen

description: All concentrations are given per kg dry weight.
DOI: 10.1594/pangaea.744503
title: (Table 1) Concentrations of Cl and Br in interstitial waters of the Gulf of California
DOI: 10.1594/pangaea.475971
title: Geochemistry of sediment core M1_MULT183 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.762785
title: (Table 1) Water content and grain size composition of surface layer bottom sediments from the Kem' River mixing zone
DOI: 10.1594/pangaea.475974
title: Geochemistry of sediment core M1_MULT187 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.742499
title: (Figure 2) Physical properties, grain size distribution and contents of carbonate and organic carbon of sediment core JR104-GC359

description: Analysed on bulk sediment samples. Further relevant datasets see Hillenbrand et al. (2009): mineralogical analysis of the clay fraction doi:10.1594/PANGAEA.711153, measurement of shear strength doi:10.1594/PANGAEA.711080.
DOI: 10.1594/pangaea.475975
title: Geochemistry of sediment core M1_MULT188 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.757957
title: (Appendix) Physical properties of sediments from the Prydz Bay

description: results of all shipboard analyses
DOI: 10.1594/pangaea.475976
title: Geochemistry of sediment core M1_MULT196 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.820210
title: (Table 2) Tests made on boninite and variolitic basalt sediments at DSDP Hole 60-458
DOI: 10.1594/pangaea.475979
title: Geochemistry of sediment core M1_MULT205 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.793022
title: (Table) Grain size distribution of sediments from core Ak-509, Black Sea continental slope

description: New results of geomorphological, seismoacoustic, and lithological investigations on the upper continental slope off the Arkhipo-Osipovka Settlement are presented. Here, a large submarine slump was discovered by seismic survey in 1998. The assumed slump body, up to 200 m thick, rises 50-60 m above the valley floor that cuts the slope. Recent semiliquid mud that overlies laminated slope sediments with possible slump deformations flows down in the valley thalweg. Radiocarbon age inversion recorded in a Holocene sediment section of shelf facies recovered from the upper slope points to the gravity dislocation of sediments.
description: Supplement to: Moskalenko, V N; Murdmaa, Ivar O; Artemenko, V I; Esin, N V; Levchenko, Oleg V; Platonova, E V (2006): Slumping processes on the Caucasian continental slope of the Black Sea. Lithology and Mineral Resources, 41(2), 187-194
DOI: 10.1594/pangaea.811434
title: (Table 3) Sediment consolidation properties at DSDP Leg 72 Holes
DOI: 10.1594/pangaea.475981
title: Geochemistry of sediment core M1_MULT213 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.818239
title: (Table 1) Physical properties of sediments at DSDP Leg 65 Holes

description: The physical properties of 138 unconsolidated hemipelagic silty clays and turbidites from the mouth of the Gulf of California were analyzed in order to determine their grain size, shear strength, compressional wave velocity, porosity, specific gravity, wet-bulk density, water content, void ratio, and degree of saturation. As at other Deep Sea Drilling Project (DSDP) sites, the wet-bulk density, sonic velocity, and shear strength tended to increase with depth while the porosity and water content decreased in response to increasing compaction. The grain size and clay fraction varied irregularly with depth.The wet-bulk density ranged from 1.34 to 2.58 g/cm**3, while, the shear strength and compressional wave velocity ranged from 0.03 to 1.05 tons/ft.**2 and 1.47 to 4.25 km/s, respectively. The porosity varied between 8 and 79%, while the water content ranged from 28.0 to 175.6%; most samples were effectively 100% saturated. The specific gravity ranged from 1.71 to 3.24 and showed a tendency to be directly related to the wet-bulk density and thus inversely related to porosity.The physical properties of the hemipelagic sediments and turbidites are noticeably different, and the properties of both were modified by diagenesis near the basement.
description: Sediment depth is given in mbsf. Empty cells mean not determined.
description: Supplement to: Gutiérrez-Estrada, Mario; Salisbury, Matthew H (1983): Physical properties of sediments from the mouth of the Gulf of California, Leg 65, Deep Sea Drilling Project. In: Lewis, BTR; Robinson, P; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 65, 675-684
DOI: 10.1594/pangaea.793124
title: (Table) Content of organic compounds in the bottom sediments of the Volga River estuary

description: Materials from different spheres of the Earth are ultimately delivered to bottom sediments, which serve as a natural recorder of the functioning of other spheres and originate as a result of the accumulation of their substances. Sedimentary material and species of river-transported elements are subjected to dramatic reworking in marginal filters, where river and sea waters are mixed. These processes are most important for the Caspian Sea, where runoffs of rivers (especially the Volga River) and the intense development and transportation of hydrocarbon fuel by tankers and pipelines (related to the coastal petroleum industry in the Sumgait and Baku ports, Apsheron Peninsula) are potential sources of hydrocarbon pollution. Previously obtained data showed that the total content of hydrocarbon fraction (i.e., the sum of aliphatic hydrocarbons (AHC) and polycyclic aromatic hydrocarbons (PAH)) in bottom sediments varied within 29-1820 µg/g. The content of petroleum hydrocarbons in the northeastern Caspian region varied from 0.052 to 34.09 µg/g with the maximum content in the Tengiz field. The content of six polyarenes in the Volga delta sediments was no more than 40 ng/g. To determine the recent HC pollution of bottom sediments and trends in the functioning of the Volga marginal filter, in summer of 2003 and 2004 we analyzed bottom sediments (58 samples) in the river waterway; Kirovsk channel; Bakhtemir and Ikryanoe branches; tributaries of the Kizan, Chagan, and other rivers; and the Caspian seashore.
description: Supplement to: Nemirovskaya, Inna A; Brekhovskikh, V F (2006): Hydrocarbons in bottom sediments of the marginal filter of the Volga River. Doklady Earth Sciences, 406(1), 97-102
DOI: 10.1594/pangaea.475950
title: Geochemistry of sediment core MH_7SK from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.475951
title: Geochemistry of sediment core MH_8SK from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.782454
title: (Appendix A2) Chemical composition of sediment core M54/2_11-2
DOI: 10.1594/pangaea.475955
title: Geochemistry of sediment core MH_12SK from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.475956
title: Geochemistry of sediment core MH_21KA from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.475959
title: Geochemistry of sediment core MH_24SK from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.742500
title: (Figure 2) Physical properties, grain size distribution and contents of carbonate and organic carbon of sediment core JR104-GC360

description: Analysed on bulk sediment samples. Further relevant datasets see Hillenbrand et al. (2009): mineralogical analysis of the clay fraction doi:10.1594/PANGAEA.711154, measurement of shear strength doi:10.1594/PANGAEA.711081.
DOI: 10.1594/pangaea.783903
title: (Table 1) Petrological description and consolidation properties of ODP Site 186-1150 and Hole 186-1151A

description: In order to determine the shear parameters of the forearc sedimentary strata drilled during Ocean Drilling Program Leg 186, West Pacific Seismic Network, Japan Trench, eight whole-round samples were selected from different depths in the drilled sections of Sites 1150 and 1151. Whereas Site 1150 lays above the seismically active part of the subduction zone, Site 1151 is situated in an aseismic zone. The aim of the triaxial tests was, apart from determination of the static stress strain behavior of the sediments, to test the hypothesis that the static stress strain parameter could differ for each sites. In order to simulate undrained deformation conditions according to the high clay mineral content of the strata, consolidated undrained shear tests were performed in a triaxial testing setup. Measurements of water content, grain density, organic content, and microtextural investigations under the scanning electron microscope (SEM) accompanied the compression experiments. After the saturation and consolidation stages were completed, failure occurred in the compression stage of the experiments at peak strengths of 280-7278 kPa. The stiffness moduli calculated for each sample from differential stress vs. strain curves show a linear relationship with depth and range between 181 and 5827 kPa. Under the SEM, the artificial fault planes of the tested specimen only show partial alignment of clay minerals because of the high content of microfossils.
description: Supplement to: Roller, Sybille; Pohl, C; Behrmann, Jan-Hinrich (2003): Data report: Triaxial shear strength of sediments and sedimentary rocks from the Japan Trench, ODP Leg 186. In: Suyehiro, K; Sacks, IS; Acton, GD; Oda, M (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 186, 1-19
DOI: 10.1594/pangaea.847796
title: (Table 2) Geochemical and geophysical characteristics of nine soil samples from Livingston Island, South Shetland Archipelago
DOI: 10.1594/pangaea.475960
title: Geochemistry of sediment core MH_26SK from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.823615
title: Moisture and density (MAD) measured on IODP Hole 320-U1331A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.823673
title: Moisture and density (MAD) measured on IODP Hole 320-U1332A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.475965
title: Geochemistry of sediment core MH_37SK from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.849208
title: (Tables, page 17-18) Chemical composition of ferromanganese concretions of the lakes of Northern Savolax in Eastern Finland

description: This paper discusses the occurrence of manganese-rich concretions in the lakes of Northern Savolax in Eastern Finland. The samples were collected in the summer of 1905 and left to dry for 2 months at room temperature. The quantity of H2O mentionned in the analysis was obtained by dessication at 155°C. The amount of Mn is calulated as MnO2 although other valences might be present in the samples. The contents in CO2 and organic substances was not determined. J. Aschan determined that as a general rule, in Finland the manganese rich lake deposits are rather associated with soft bottom sediments while the iron rich deposits are more assocaited with hard or sandy bottoms.
description: Samples have been dried at 155°C in order to evaluate the contents in H2O.Depth of lake see Event(s) information.From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: Aschan, Joh:s (1906): Om några förekomster af manganrik sjömalm i norra Savolax = On occurrences of enrichment in managanese in the lake ores of Savolax (Eastern Finland). original at http://digi.kansalliskirjasto.fi/aikakausi/binding/1122928, Teknikern, 456, 78-80
DOI: 10.1594/pangaea.823702
title: Moisture and density (MAD) measured on IODP Hole 320-U1332B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.475966
title: Geochemistry of sediment core MH_38SK from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.848903
title: Water content of composite core PG2023
DOI: 10.1594/pangaea.475967
title: Geochemistry of sediment core M1_180SK from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.742502
title: (Figure 2) Physical properties, grain size distribution and contents of carbonate and organic carbon of sediment core JR104-GC365

description: Analysed on bulk sediment samples. Further relevant datasets see Hillenbrand et al. (2009): mineralogical analysis of the clay fraction doi:10.1594/PANGAEA.711156, measurement of shear strength doi:10.1594/PANGAEA.711083.
DOI: 10.1594/pangaea.825485
title: Moisture and density (MAD) measured on IODP Hole 329-U1370D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.826476
title: Moisture and density (MAD) measured on IODP Hole 329-U1367F

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.611516
title: Water content of sediment core LD05/AC_37
DOI: 10.1594/pangaea.475969
title: Geochemistry of sediment core M1_182SK from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.767447
title: Tab. 2: Chemical and microbial properties of soils from Casey Station (Wilkes Land) with respect to soil types

description: Mineral constituents and pH were analyzed in water solution (l:5). Soil surfaces are covered by dry moss cushion (sample 1A), moss cushion and microlichens (mainly Candelariella sp.) (2A), moss cushion and microlichens (mainly Buellia sp.) (7A), no visible plant cover (8A), and soil algae (mainly Prasiola crispa and cyanobacteria) (9A). Podzols on leuco gneiss, partly with thin moraine cover: lithic to leptigelic podzols with gelundic phase; leptosols on shist: dystri-gelic leptosols with gelundic phase. Texture of podzols is stony sand, texture of leptosols is gravelly sandy loam.
DOI: 10.1594/pangaea.475972
title: Geochemistry of sediment core M1_MULT185 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.753804
title: (Table 2) Consolidation test results of ODP Leg 112 samples
DOI: 10.1594/pangaea.779749
title: (Table T3) Granulometry of sediments from ODP Leg 190 sites

description: We present the results of grain-size analysis performed on hemipelagic sediment from Sites 1173, 1174, 1175, and 1177 at the Nankai Trough. Analyses of the &lt;63-µm fraction were performed with a laser particle counter, and results were converted to equivalent settling diameters by means of an empirical regression with data from pipette analysis. The relations among grain size, porosity, bulk density, void ratio, and moisture content are influenced by the increasing compaction of sediment with depth as well as facies changes. Thus, departures of bulk density and porosity from normal compaction trends cannot be attributed to grain size on the basis of our laboratory results.
description: Sediment depth is given in mbsf. Porosity, bulk density, void ratio and water content from Shipboard Scientific Party (2001, doi:10.2973/odp.proc.ir.190.101.2001, in Moore et al. (2001)).
description: Supplement to: Steurer, Joan; Underwood, Michael B (2003): Data report: The relation between physical properties and grain-size variations in hemipelagic sediments from Nankai Trough. In: Mikada, H; Moore, GF; Taira, A; Becker, K; Moore, JC; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 190/196, 1-25
DOI: 10.1594/pangaea.848965
title: Chemical composition of a concretion dredged from lake Madüsee (lake Miedwie, Poland)

description: This article describes the bottom sediments, lake ores and limestone bedrock dredged from lake Mad¸see in Pommerania now known as lake Miedwie in Poland.
description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: Weltner, W (1905): Über den Tiefenschlamm, das Seeerz und über Kalksteinaushöhlungen im Madüsee. complete volume at http://www.archive.org/stream/archivfrnaturg7101berl/archivfrnaturg7101berl.pdf, Archiv für Naturgeschichte, I. Band, 277-296
DOI: 10.1594/pangaea.475973
title: Geochemistry of sediment core M1_MULT186 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.772616
title: Fig. 2. Lithology, water and total carbon content, cumulative grain-size distribution, and quartz, feldspar, and mica contents of core sequence Lz1013 from south-western Beaver Lake

description: A 100 cm long sediment sequence was recovered from Beaver Lake in Amery Oasis, East Antarctica, using gravity and piston corers. Sedimentological and mineralogical analyses and the absence of micro and macrofossils indicate that the sediments at the base of the sequence formed under glacial conditions, probably prior to c. 12 500 cal. yr BP. The sediments between c. 81 and 31 cm depth probably formed under subaerial conditions, indicating that isostatic uplift since deglaciation has been substantially less than eustatic sea-level rise and that large areas of the present-day floor of Beaver Lake must have been subaerially exposed following deglaciation. The upper 31 cm of the sediment sequence were deposited under glaciomarine conditions similar to those of today, supporting geomorphic observations that the Holocene was a period of relative sea-level highstand in Amery Oasis.
description: Supplement to: Wagner, Bernd; Hultzsch, Nadja; Melles, Martin; Gore, Damian B (2007): Indications of Holocene sea-level rise in Beaver Lake, East Antarctica. Antarctic Science, 19(1), 125-128
DOI: 10.1594/pangaea.777696
title: (Table 3) Corrected index properties for ODP Leg 128 sites
DOI: 10.1594/pangaea.811435
title: (Table 4) Direct shear properties at DSDP Leg 72 Holes
DOI: 10.1594/pangaea.757956
title: (Tables 1, 2) Geotechnical properties of sediments from the Prydz Bay

description: land-based laboratory analyses of the whole-round core samples
DOI: 10.1594/pangaea.745925
title: (Table 2) Contents of organic compounds in bottom sediments from the southwestern Amur Bay
DOI: 10.1594/pangaea.777695
title: (Table 2) Corrected index properties for ODP Leg 127 sites
DOI: 10.1594/pangaea.784891
title: (Table 2) Carbon, carbonate and water content and bulk density of core GIK-15496

description: 14C ages on marine sediments are probably (50-850 years) too old, see also Wefer et al. (1978).
DOI: 10.1594/pangaea.764064
title: (Table 4a) Geochemical parameters of Kara Sea bottom sediments and chemical composition of interstitial waters, September 2007
DOI: 10.1594/pangaea.785517
title: (Table 2) Thorium and uranium isotopic composition of sediments in core GIK14350
DOI: 10.1594/pangaea.776604
title: A 1.1.1. Harbour sediments: material description - material parameter

description: # = approximately equal (~)
DOI: 10.1594/pangaea.763479
title: Moisture and density (MAD) measured on IODP Hole 325-M0030A
DOI: 10.1594/pangaea.773864
title: Moisture and density (MAD) measured on IODP Hole 316-C0007A

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.611506
title: Water content of sediment core LD05/AC_15
DOI: 10.1594/pangaea.614786
title: Bulk sedimentology on core Lz1010 from Radok Lake, Antarctica
DOI: 10.1594/pangaea.763483
title: Moisture and density (MAD) measured on IODP Hole 325-M0034A
DOI: 10.1594/pangaea.614795
title: Bulk sedimentology on core Lz1012 from Radok Lake, Antarctica
DOI: 10.15468/dl.kmjqup
title: Occurrence Download

description: A dataset containing 160037 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Phalacrocorax brasilianus (Gmelin, 1789)",
 "Year 2011-2015"
 ]
}

 The dataset includes 160037 records from 60 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031504-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.438935
title: Sedimentological bulk parameters of sediment core Lz1019
DOI: 10.1594/pangaea.777005
title: Moisture and density (MAD) measured on IODP Hole 331-C0017D

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.894042
title: Pollen profile of sediment core ERIU, Eriu, Romania

description: This dataset was archived on 2018-09-13 from the EPD database. (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.894021
title: Lithology of sediment core LEZERUMA, Lezerul calimani, Romania

description: This dataset was archived on 2018-09-13 from the EPD database. (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.894025
title: Lithology of sediment core LPA1, Torbiera di Trana, Italy

description: This dataset was archived on 2018-09-13 from the EPD database. (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.894027
title: Lithology of sediment core LUCINA1, Lucina, Romania

description: This dataset was archived on 2018-09-13 from the EPD database. (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.894125
title: Loss on ignition of sediment core OTTTIA, Tiåvatnet, Norway

description: This dataset was archived on 2018-09-14 from the EPD database. (http://www.europeanpollendatabase.net).