cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.868835
title: (Table 1) CaCO3 and He concentrations in sediment core TTN13-72

description: The availability of CaCO3 and 3He content results for core TT 13-72 from 4.3 km depth in the equatorial Pacific (Marcantonio et al., 1996, doi:10.1038/383705a0) allows the magnitude of the excess (i.e., over ambient) CaCO3 dissolution at the onset of marine glacial stages 10, 8, and 6 to be estimated. These three events are remarkably similar; during each an integrated loss of about 28 g CaCO3 per cm² occurred. While the magnitude of this loss is consistent with that expected from the interglacial to glacial pH shifts reconstructed based on boron isotope measurements on benthic foraminifera (Sanyal et al., 1995, doi:10.1038/373234a0), measurements at a number of other locations and water depths will be required before this approach can be used to evaluate the global toll of these dissolution events.
description: Supplement to: Broecker, Wallace S; Sanyal, A (1997): Magnitude of the CaCO3 dissolution events marking the onset of times of glaciation. Paleoceanography, 12(4), 530-532
DOI: 10.1594/pangaea.869863
title: Zostera marina wasting disease index of Labyrinthula zosterae inoculated plants at two nutrient levels
DOI: 10.1594/pangaea.869896
title: Results of a hydrodynamic model coupled with a Lagrangian particle tracking technique for survival and dispersal variability of pelagic eggs and yolk-sac larvae of central and eastern Baltic flounder (Platichthys flesus)

description: A hydrodynamic model coupled with a Lagrangian particle tracking technique was utilized to simulate spatially and temporally resolved long-term environmentally-related i) size of habitat suitable for reproduction, ii) egg/yolk-sac larval survival, iii) separation of causes of mortality, and iv) connectivity between spawning areas of Baltic flounder with pelagic eggs. Information on reproduction habitat requirements and mortality sources were obtained from field or laboratory studies. In our modelling study we only quantified physical processes generating heterogeneity in spatial distribution of eggs and yolk sac larvae, as e.g. predation is not accounted for. The spatial extent of eggs and larvae represented as modelled particles is primarily determined by oxygen and salinity conditions. The reproduction habitat most suitable was determined for the Gdansk Deep, followed by the Bornholm Basin. Relatively low habitat suitability was obtained for the Arkona Basin and the Gotland Basin. The model runs also showed yolk sac larval survival to be to a large extent affected by sedimentation. Eggs initially released in the Arkona Basin and Bornholm Basin are strongly affected by sedimentation compared to those released in the Gdansk Deep and Gotland Basin. Highest relative survival of eggs occurred in the Gdansk Deep and in the Bornholm Basin. Relatively low survival rates in the Gotland Basin were attributable to oxygen-dependent mortality. Oxygen content had almost no impact on survival in the Arkona Basin. For all spawning areas mortality caused by lethally low temperatures was only evident after severe winters. Buoyancy of eggs and yolk-sac larvae in relation to topographic features appear as a barrier for the transport of eggs and yolk sac larvae and potentially limits the connectivity of early life stages between the different spawning areas.
description: Supplement to: Hinrichsen, Hans-Harald; Petereit, Christoph; Nissling, Anders; Wallin, Isa; Ustups, Didzis; Florin, Ann-Britt (2016): Survival and dispersal variability of pelagic eggs and yolk-sac larvae of central and eastern Baltic flounder (Platichthys flesus): application of biophysical models. ICES Journal of Marine Science, fsw163
DOI: 10.1594/pangaea.869312
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 27 (Sites 259, 261, 263)

description: During Leg 27 five sites were drilled in the eastern Indian Ocean, four in abyssal plains near the western margin of Australia and one in the Timor Trough. Abyssal plain sediments are divided into two major units: (1) a lower, acoustically transparent layer of relatively uniform thickness draped over basaltic basement and (2) a horizontally layered sequence of highly variable thickness filling low areas on the surface of the transparent layer. The transparent layer, ranging in age from Upper Jurassic to Upper Cretaceous, consists chiefly of dark gray, siliceous clays and claystones with minor zeolitic clay and nannofossil ooze. Sedimentation rates are between 5 and 30 m/m.y. being highest in the Lower Cretaceous. Upper Cretaceous sediment are sparse or absent. The relatively high sedimentation rates for pelagic clay are probably due to the proximity of the Australian continent. The layered unit consists of calcareous oozes and lesser zeolitic clay and radiolarian ooze, all of Cenozoic age. Many of the oozes contain shallow-water foraminifers and graded sequences suggesting deposition by mass transport.
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: Robinson, Paul T; Thayer, Julie A; Cook, Peter J; McKnight, Brian K (1974): Lithology of Mesozoic and Cenozoic Sediments of the Eastern Indian Ocean, Leg 27, Deep Sea Drilling Project. In: Veevers, J.J.; Heirtzler, J.R.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXVII, 1001-1047
DOI: 10.1594/pangaea.869482
title: Tab. 15 Isotope ratios of fracture Calcite
DOI: 10.1594/pangaea.881796
title: Biomass determination from 2012 to 2015 from experimental plots in the Jena Experiment (Germany)
DOI: 10.1594/pangaea.936676
title: Fluorescent Particles over the central Pacific Ocean in March 2019

description: Number concentration of fluorescent and total particles retrieved from a Wideband Integrated Bioaerosol Sensor Model 4A (WIBS-4A, Droplet Measurement Technologies) during cruise MR18-06 Leg4 of RV Mirai in March 2019.
DOI: 10.1594/pangaea.936677
title: Ozone and carbon monoxide over the central Pacific Ocean in March 2019

description: Ozone and carbon monoxide mixing ratios retrieved from an Ozone Analyzer (Model 49C, Thermo Fisher Scientific) and a CO Analyzer (Model 48C, Thermo Fisher Scientific) during cruise MR18-06 Leg4 of RV Mirai in March 2019.
DOI: 10.1594/pangaea.772054
title: (Table S1) Mg/Ca and stable oxygen isotope ratios of Globigerina bulloides from ODP Hole 189-1171C
DOI: 10.1594/pangaea.936673
title: Marine biological indicators over the central Pacific Ocean in March 2019

description: Marine biological indicators measured during cruise MR18-06 Leg4 of RV Mirai in March 2019. This dataset contains the abundance of transparent exopolymer particles (TEP), coomassie stainable particles (CSP), bacteria, chlorophyll a, nitrate, phosphate, and ammonium.
DOI: 10.1594/pangaea.954525
title: Major and minor elements of marine ferromanganese nodules

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.This dataset represents the digitized Table 2, pp. 519 of the related publication.
DOI: 10.1594/pangaea.773783
title: Fossil occurrence of calcareous nannofossils from IODP Hole 316-C0006F

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.759937
title: (Table 1) Elemental abundances across the K/T boundary in ODP Hole 122-761C

description: Sediment depth is given in mbsf.1-sigma uncertainties are 1%-3% for Fe, Sc, Th, Ce, Cr, Co, Eu; 3%-5% for CaCO3, Si, Sr, Cs, Zn, Hf, Tb, Yb, La, Sm; 5%-10% for Ba, Rb, Lu; and 10%-15% for Al, Mg, Ni, Nd.
DOI: 10.1594/pangaea.914849
title: Meteorological synoptical observations from station Toravere (2020-01)
DOI: 10.1594/pangaea.834362
title: Ceilometer raw data measured at Neumayer Station (2011-08), links to files
DOI: 10.1594/pangaea.900922
title: Tethered balloon-borne turbulence measurements during the Arctic field campaign PAMARCMiP (Balloon_20180327_1106_1556)

description: This dataset was not imported into the relational system due to its size.
DOI: 10.1594/pangaea.834335
title: Ceilometer raw data measured at Neumayer Station (2009-05), links to files
DOI: 10.1594/pangaea.914855
title: Radiosonde measurements from station Izaña (2020-03)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.868668
title: Flood-stack of combined sediment record ELSA

description: This study reconstructs the main flood phases in central Europe from event layers in sediment cores from Holocene Eifel maar lakes and Pleistocene dry maar structures. These reconstructions are combined with recent gauge time-series to cover the entire precipitation extremes of the last 60 000 years. In general, Eifel maar sediments are perfectly suited for the preservation of event layers since the deep water in the maar lakes is seasonal anoxic and therefore, bioturbation is low. However, the preservation of annual lamination is only preserved in Holzmaar and Ulmener Maar; the other cores are dated by 14C, magnetostratigraphy, tephra markers and ice core tuning. The cores were drilled in the Eifel region of central western Germany, which represents a climatic homogenous region from Belgium to Poland and all across Central Europe.A total of 233 flood layers over 7.5 mm were detected in all analysed cores. The stratigraphic classification of the flood events follows the newly defined Landscape Evolution Zones (LEZ). The strongest events in the Holocene have occurred during LEZ 1 (0?6000 b2k) in the years 658, 2800 and 4100 b2k. Flood layers in the LEZ 2 (6000-10 500 b2k) are not as frequent as during the LEZ 1, nevertheless, the floods cluster between 6000 and 6500 b2k. Twenty flood layers are found in the LEZ 3 (10 500?14 700 b2k); 11 in LEZ 4 (14 700-21 000 b2k); 15 in LEZ 5 (21 000-28 500 b2k); 34 in LEZ 6 (28 500?36 500 b2k); 8 in LEZ 7 (36 500-49 000 b2k); zero in LEZ 8 (49 000-55 000 b2k) and LEZ 9 (55 000-60 000 b2k). The maximum flood phases during the Pleistocene are at 11 500-17 500 (late glacial and Younger Dryas), 23 000-24 000 (before Greenland Interstadial (GI) 2), 29 000-35 000 (especially between GI 5 and 4) and 44 000-44 500 b2k (transition from GI 12 to 11).The variations in flood dynamics are climatically driven and mainly associated with climate transitions and colder periods, combined with light vegetation. It turns out that low vegetation coverage related to both Greenland Stadial phases and anthropogenic impacts since late Holocene is the main cause for the development of flood layers in maar sediments. The precipitation itself, plays only a secondary role. This interpretation is based on the current climate understanding of cold phases and several studies of fluvial erosion related to vegetation coverage.
description: Sediment core combination: AU2 (Aueler Maar Lat.: 50.28383, Long.: 6.59574. elevation: 453, recovery: 123 m, Gauß-Krüger coordinate system: 2542455/5572017) + HM1 (Holzmaar Lat.: 50.1203, Long.: 6.87963, elevation: 425, recovery: 10 m, Gauß-Krüger coordinate system: 2562900/5554030)
description: Supplement to: Brunck, Heiko; Sirocko, Frank; Albert, Johannes (2016): The ELSA-Flood-Stack: A reconstruction from the laminated sediments of Eifel maar structures during the last 60000 years. Global and Planetary Change, 142, 136-146
DOI: 10.1594/pangaea.663186
title: Oceanography at CTD/bottle station IFREMER_0025
DOI: 10.1594/pangaea.822721
title: Meteorological measurements in the upper air at station Jabalpur, 1938-12-31 to 1942-03-31, ERA-CLIM ID 5444

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.885697
title: Pollen and spores counts at site CRG_L5-a

description: Analyst: Michael O'ConnellLaboratory: Palaeoenvironmental Research Unit, NUI Galway, IrelandData analysis completed: 1983Sampling in field: When sampling in the field, monoliths from Location 5 were referred to as L5.1 and L5.2 (50 cm apart; L5.2 taken so as to sample peat/mineral soil interface). These have been referred to as L5.a and L5.bPollen sampling details: sampling density &lt;= 4 cm intervals. Depths originally recorded in cm (cited here in m) with respect to the mineral/soil interface (as in all samples from Carrownaglogh); negative values indicate above the mineral/peat interface. Uppermost depth cited as the depth of the sample (standard PRU practice); e.g. 1 cm = 1-2 cm below the mineral/peat horizonPollen preparation: Lycopodium tablets (Stockmarr) added; acetolysis, HF for basal (minerogenic) samples; mounted in glycerinePollen identification and counting: -5 cm and -25 cm counted by Michael O'Connell. Other spectra counted in Majella Coleman in the context of a BSc (Hons) project 1979; i.e. in reality these are preliminary counts. Counts for these 2 spectra (-5 and -25 cm) are also included in profile 5.b in dataset doi:10.1594/PANGAEA.885699. Cereal-type pollen differentiated using Beug (1961) criteria (37 µm taken as cutoff point; this differs from PRU practice in later years when 40 µm was taken as the cut off size). Pollen nomenclature generally follows Moore et al. 1991. &lt;1 = recorded outside the pollen counts.
DOI: 10.1594/pangaea.868594
title: Annotated record of the detailed examination of Mn deposits from DSDP Site 75, Leg 8 (Core 75-9)

description: Site 75 is located 300 miles southeast of the Marquesas Islands; 400 miles south of Site 74. It is the southernmost of the sites along the N-S line drilled during Leg 8 to investigate the east-west trending accumulation of sediments centered about 2°N near 140°W. This site is a replacement for the site at 31°S originally chosen by the JOIDES Pacific Advisory Panel (PAP Site 27). The original site was not drilled since a preliminary R/V Argo SCAN survey indicated insufficient sediment thickness.
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: Tracey, J I; Sutton, George H; Nesteroff, Wladimir D; Galehouse, J S; von der Borch, Christopher C; Moore, T; Lipps, J; Haq, Bilal U; Beckmann, Jean-Pierre (1971): Site 75. In: Tracey, J.I.Jr.; et al., Initial Reports of the Deep Sea Drilling Project, 8, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, VIII, 675-709
DOI: 10.1594/pangaea.756068
title: (Table 5) Occurrence of calcareous nannofossils observed in the upper to middle Eocene samples from ODP Hole 115-707C

description: Specimens not identifiable to known species are excluded. Distribution chart: Numbers = calculated percentage in the indigenous flora, figures below the decimals are omitted; F = few (&gt;0.1% and &lt; 1% of indigenous forms); R = rare (&lt;0.1% of indigenous forms); c = common reworked occurrence (&gt; 1% and &lt; 10% of the total flora), f = few reworked occurrence (&gt;0.1% and &lt; 1% of the total flora); r = rare reworked occurrence (&lt;0.1% of the total flora), - = not present.
DOI: 10.1594/pangaea.822908
title: Meteorological measurements in the upper air at station Madras (Chennai), 1933-01-06 to 1936-12-30, ERA-CLIM ID 5812

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.832033
title: Hydrological records from the Vernagtferner Basin - Vernagtbach station, for the year 2012
DOI: 10.1594/pangaea.868430
title: Sea ice calculations for two sectors off East Antarctica

description: A discontinuous record of monthly sea ice area is calculated from a series of satellite-based sensors, covering the period from 1974 to 2015 with missing years for 1975, 1977 and 1978. Sea ice area for the period 1973 to 1977 was determined from daily brightness temperatures monitored by the ESMR instrument mounted on the NIMBUS-5 satellite (Parkinson et al., 2004). For the period January 1979 to May 2015, sea ice observations were obtained from the SMMR and SSM/I and SSMIS instruments mounted on various satellite platforms (Cavalieri et al., 1996, updated yearly). These data are freely available from the US National Snow and Ice Data Centre (NSIDC) website (Cavalieri et al., 1999; Fetterer et al.).
DOI: 10.1594/pangaea.885698
title: Pollen and spores counts at site CRG_LM

description: Analyst: Michael O'ConnellLaboratory: Palaeoenvironmental Research Unit, NUI Galway, IrelandData analysis completed: 1983Sampling in field: Monolith, in two 1-m lengths, removed from a freshly cut peat face. Blanket bog peat (this [so-called Long Monolith] and all other monoliths relating to Carrownaglogh project)Pollen sampling details: sampling density &lt;= 4 cm intervals. Depths cited in m (originally recorded in cm) with respect to the mineral/soil interface (as in all samples from Carrownaglogh); negative values indicate above the mineral/peat interface.Surface of bog somewhat disturbed, i.e. youngest peat (uppermost cms) disturbed (not analysed)Uppermost depth cited as the depth of the sample (standard PRU practice); e.g. 1 cm = 1-2 cm below the mineral/peat horizonPollen preparation: Lycopodium tablets (Stockmarr) added; acetolysis, HF for basal (minerogenic) samples; mounted in glycerinePollen identification and counting: Cereal-type pollen differentiated using Beug (1961) criteria (37 um taken as cutoff point; this differs from PRU practice in later years when 40 um was taken as the cut off size). Pollen nomenclature generally follows Moore et al. 1991. &lt;1 = recorded outside the pollen counts.
DOI: 10.1594/pangaea.495953
title: Water temperature IBT profiles from cruise U90PO76102I_1976
DOI: 10.1594/pangaea.876086
title: A new flow-through bioassay for testing low-emission antifouling coatings: Fig 4
DOI: 10.1594/pangaea.868420
title: Neunkirch, Switzerland (field station): Long-term forest meteorological data from the Long-term Forest Ecosystem Research Programme (LWF), from 1997-2016

description: High quality meteorological data are needed for long-term forest ecosystem research, particularly in the light of global change. The long-term data series published here comprises almost 20 years of two meteorological stations in Neunkirch in Switzerland where one station is located within a natural deciduous forest stand (NEB) with European beech (Fagus sylvatica; 160 yrs), sycamore maple (Acer pseudoplatanus; 160 yrs) and lime trees (Tilia sp.; 110 yrs) as main tree species. A second station is situated in the very vicinity outside of the forest (field station, NEF). The meteorological time series are presented in hourly time resolution of air temperature, relative humidity, precipitation, photosynthetically active radiation (PAR) and wind speed. Neunkirch is part of the Long-term Forest Ecosystem research Programme (LWF) established and maintained by the Swiss Federal Research Institute WSL. For more information see PDF under 'Further Details'.
DOI: 10.1594/pangaea.663538
title: Oceanography at CTD/bottle station IFREMER_0378
DOI: 10.1594/pangaea.743908
title: Grain size analysis on Site 208-1262
DOI: 10.1594/pangaea.936358
title: Expanded measurements from station Lindenberg (2001-07)

description: 99999: No clouds detected; Version 2, 2021-09-27 with some previously missing values for 10000m CBH inserted
DOI: 10.1594/pangaea.497602
title: Physical oceanography from BT during cruise U58GS01972B_1982
DOI: 10.1594/pangaea.936364
title: Expanded measurements from station Lindenberg (2005-06)

description: 99999: No clouds detected; Version 2, 2021-09-27 with some previously missing values for 10000m CBH inserted
DOI: 10.1594/pangaea.886428
title: Physical oceanography from mooring KPO_0906

description: instrument = Label:kpo_0906_01, File:kpo_0906_instr_01.nc, Type:Seabird MicroCat 37-SM, SN:00056 depth/pressure data was derived not measuredinstrument = Label:kpo_0906_02, File:kpo_0906_instr_02.nc, Type:Sontek Argonaut, SN:182 depth/pressure data was derived not measuredinstrument = Label:kpo_0906_03, File:kpo_0906_instr_03.nc, Type:GEOMAR, TD-Logger, SN:17instrument = Label:kpo_0906_04, File:kpo_0906_instr_04.nc, Type:Seabird MicroCat 37-SM, SN:00054 depth/pressure data was derived not measuredinstrument = Label:kpo_0906_05, File:kpo_0906_instr_05.nc, Type:Aanderaa RCM 8, SN:09933instrument = Label:kpo_0906_06, File:kpo_0906_instr_06.nc, Type:Seabird SeaCat 16, SN:1307 depth/pressure data was derived not measuredinstrument = Label:kpo_0906_07, File:kpo_0906_instr_07.nc, Type:Sontek Argonaut, SN:183 depth/pressure data was derived not measuredinstrument = Label:kpo_0906_08, File:kpo_0906_instr_08.nc, Type:Sontek Argonaut, SN:188 depth/pressure data was derived not measuredinstrument = Label:kpo_0906_09, File:kpo_0906_instr_09.nc, Type:Seabird SeaCat 16, SN:0941 depth/pressure data was derived not measuredinstrument = Label:kpo_0906_10, File:kpo_0906_instr_10.nc, Type:Sontek Argonaut, SN:038 depth/pressure data was derived not measuredinstrument = Label:kpo_0906_11, File:kpo_0906_instr_11.nc, Type:Aanderaa RCM 8, SN:09349 depth/pressure data was derived not measured
DOI: 10.1594/pangaea.897080
title: The comparison between calving front variations and bed elevation of Branch A in Jakobshavn Isbræ

description: In this movie, we show the bed elevation at the calving front of Branch A and the comparison between bed elevation and calving front variation in terms of area change. Figure a shows the calving front variation expressed by area change. Figure b shows the bed elevation along the profile. The profile is shown in figure c by the green line. The red star shows the cross section between the calving front and the profile.
DOI: 10.1594/pangaea.886161
title: Geochemistry of individual-oxide grains in Hawaiian lavas, sample HW-6
DOI: 10.1594/pangaea.707930
title: Basic measurements of radiation at station Carpentras (2005-08)
DOI: 10.1594/pangaea.867890
title: Basic and other measurements of radiation at station Tiksi (2016-02)
DOI: 10.1594/pangaea.936362
title: Expanded measurements from station Lindenberg (2003-09)

description: 99999: No clouds detected; Version 2, 2021-09-27 with some previously missing values for 10000m CBH inserted
DOI: 10.1594/pangaea.936363
title: Expanded measurements from station Lindenberg (2003-10)

description: 99999: No clouds detected; Version 2, 2021-09-27 with some previously missing values for 10000m CBH inserted
DOI: 10.1594/pangaea.877576
title: Georeferenced photographs of benthic photoquadrats acquired along transects from Vicki Harriott Reef in the Cairns to Cooktown region of the Great Barrier Reef (2017-05)
DOI: 10.1594/pangaea.889166
title: Shipborne visual observations of Arctic sea ice during Lance cruise LA1208