cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.846487
title: Effects of Ocean Acidification on the Ballast of Surface Aggregates Sinking through the Twilight Zone: settling velocity and particle size

description: Incubation SetupThe aggregates were placed inside the settling microcosm. The microcosm was filled with GF/F filtered, artificial seawater (32 psu) with a carbonate chemistry adjusted to the present or future conditions. This reduced the biological activity to the community originally present in the aggregates. The microcosm was continuously pressurized at a rate of 30 MPa/day, until it reached 10 MPa, the equivalent to a depth of 1000 m. The full incubation lasted 80 h. The experiment was triplicated at a pCO2 of 380 µatm and 1100 µatm. Additional incubations of similar duration were done at atmospheric pressure, with triplicates at a pCO2 of 380 µatm and 1100 µatm. These aimed at isolating the effect of the increase in hydrostatic pressure.Determination of Particle Size and Settling Velocity (ws)A Laser In Situ Scattering and Transmissiometry device (LISST-100X) was used to measure the variations in particle size distribution of the model aggregates before and after the incubations. The particle size vs. settling velocity relationship of phytodetrital aggregates was investigated by using a settling column of square cross-section [24]. The particles were back-illuminated and recorded with a digital video camera (Imageworks DFK-41F02) for determination of settling rates and particle sizes. The camera was capable of resolving particles of &gt;11 µm diameter. The analysis of the particle sizes and settling velocities was done using the ImageJ (v.1.61) software. The resulting settling speeds were converted into m day−1 velocities, and the average speed for each of the aggregate size classes was calculated for the equivalent size classes of the LISST analysis (&gt;63 µm, &gt;75 µm, &gt;88 µm, &gt;104 µm, &gt;122 µm, &gt;144 µm, &gt;170 µm, &gt;201 µm, &gt;237 µm, &gt;280 µm, &gt;331 µm, &gt;390 µm, &gt;460 µm).
DOI: 10.1594/pangaea.875620
title: BSIOM model results for the period 1971-2010: Fulton's K condition index of juvenile Baltic cod &lt; 16 cm from the first quarter of the year (Figure 10)

description: ICES subdivisions in the central and eastern Baltic SeaArkona Basin (ICES SD 24)Bornholm Basin (ICES SD 25)Gdansk Deep (ICES SD 26)Gotland Basin (ICES SD 28)
DOI: 10.1594/pangaea.818064
title: (Table 6) Geochemistry of selected plagioclase phenocrysts at DSDP Leg 65 Holes

description: Proportions shown on a basis of 32 oxygen atoms. Empty cells mean data not determined.
DOI: 10.1594/pangaea.913650
title: Geochemical composition of tephra layers from deep sediment core MD99-2284, north of the Faroe-Shetland Channel, eastern Nordic Sea

description: Electron-probe microanalysis (EPMA). These measurements were performed at the Tephrochronological Analytical Unit at the University of Edinburgh using a Cameca SX100 electron microprobe with five vertical wavelength dispersive spectrometers, providing oxide values (wt. %) for 10 major elements (see supplementary information).Beam size: 5Settings:Na, Al, Si, K†, Ca, Fe, Mg :15 keV 2nAMn, P†, Ti: 15 keV 80 nA
DOI: 10.1594/pangaea.860198
title: Average chemical composition by size categories of manganese nodules and crusts collected from the R/V Sonne Cruise SO-06, Sept-Oct, 1978 in the Pacific Ocean

description: Manganese nodules collected from three areas (C, F, and G) on a N-S equatorial Pacific transect at 134° W by R. V. Sonne show differences in size, morphology, surface density and composition which can best be interpreted in terms of the biogenic theory of nodule formation. These data indicate that the biogenic hypothesis is central to an understanding of manganese nodule genesis in the equatorial Pacific and in particular influences the nodule shape, surface texture, rate of growth, composition, and mineralogy. The nodule characteristics in this region are also influenced by the hydrological characteristics of the bottom water, sedimentation rates, local geological and tectonic conditions (including seeding eflects) and topography.
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: Friedrich, G; Glasby, Geoffrey P; Thijssen, Theo; Plüger, W L (1983): Morphological and geochemical characteristics of manganese nodules collected from three areas on an Equatorial Pacific transect by RV Sonne. Marine Mining, 4, 167-253
DOI: 10.1594/pangaea.774121
title: Color data from IODP Hole 331-C0013C

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.774373
title: Fossil occurrence of radiolarians from IODP Hole 316-C0008B

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.905140
title: Archaeological data indicating the upper limit for the shoreline

description: Organizations:Riksantikvarieämbetet (RAÄ) = Swedish National Heritage BoardLänsstyrelsen i Västra Götalands = County Administrative Board of Västra GötalandStatens maritima museer = Swedish National Maritime and Transport MuseumsLänsstyrelsen Dalarna = County Administrative Board of DalarnaJönköpings läns museum = Jönköping County MuseumJamtli = JamtliAlmunga AB = Almunga Co.Länsmuseet Gävleborg = Gävle County Museum
DOI: 10.1594/pangaea.869725
title: (Table 4.2) On-board XRF analytical data on pressed powder pellets and rock slabs, Sonne cruise SO100

description: No unit was given, so it was assumed that the values presented here are XRF raw counts.
DOI: 10.1594/pangaea.891634
title: Pollen density in sediment cores from St. Louis River and Lake Superior, Minnesota, USA

description: Pollen density is measured per dry weight of sediment.TRSHR - Trees & shrubs groupUPHRB - Upland herbs groupWETEM - Wetland emergents groupAQUAT - Aquatics groupPTERI - Pteridophytes groupSPORE - Spore group
DOI: 10.1594/pangaea.907260
title: Track of GPS very-near surface drifter ISMER_20150615_spot028
DOI: 10.1594/pangaea.876800
title: Continuous light intensity observations at station BEFmate_I3upp_pole (2016-09)
DOI: 10.1594/pangaea.664911
title: Oceanography at CTD/bottle station IFREMER_1751
DOI: 10.1594/pangaea.669928
title: Basic measurements of radiation at station Kwajalein (1998-07)
DOI: 10.1594/pangaea.855668
title: (Table 3) Major and minor element concentrations from IODP Hole 343-C0019E

description: # = Elements and element ratios indicating pelagic clays or hydrothermal alteration
DOI: 10.1594/pangaea.902647
title: (Table 3) Carbonate and sulfate Sr and stable isotope geochemistry of IODP Exp366 samples
DOI: 10.1594/pangaea.777633
title: (Table T2) Abundance estimates of Eocene and Neogene radiolarians of ODP Hole 200-1223A sediments

description: Sediment depth is given in mbsf. Radiolarian abundance estimates as follows: T = trace (single specimen per slide), R = rare (2-5 specimens per slide), C = common (6-10 specimens per slide), A = abundant (&gt;10 specimens per slide).
DOI: 10.1594/pangaea.736962
title: (Table 1) Chemical composition of rhyolithic ash in ODP Site 104-642 and Hole 104-643A
DOI: 10.1594/pangaea.824600
title: Natural gamma radiation from IODP Hole 318-U1361B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.806521
title: (Table 1) Mineralogy at DSDP Site 82-558

description: Sediment depth is given in mbsf. &lt;1= trace.
DOI: 10.1594/pangaea.824966
title: P-Wave velocity (PWB) from IODP Hole 334-U1379C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.788611
title: (Table T1) Trace element concentration of interstitial waters from ODP Hole 169-1037B sediments
DOI: 10.1594/pangaea.906105
title: Pore water concentration and isotopes of IODP Hole 334-U137C
DOI: 10.1594/pangaea.746509
title: (Table 101) Chemical composition of samples from hydrothermal sulfide deposits sampled in the North Manus Basin

description: Mineral contents are given in % of crystal phase.
DOI: 10.1594/pangaea.763556
title: (Table 1b) Concentrations of suspended matter and heavy metals in melted ice water from the Barents Sea
DOI: 10.1594/pangaea.904723
title: Table SM-5: Splice interval table for IODP Site 320-U1335

description: This is the splice interval table for SiteU1335 (present day preferred format for presenting the splice).Each row indicates the interval within a core that is included within the revised splice.ANCHOR indicates the core at the top of the splice anchored a the seafloor; TIE indicates where that the core is directly tied to the previous core; APPEND indicates where the core is appended to the previous core.
DOI: 10.1594/pangaea.808522
title: (Table 2) Isotope ratios in evaporite sulfate at DSDP Hole 79-546
DOI: 10.1594/pangaea.837282
title: Hydrochemistry measured on water bottle samples during Ryofu Maru cruise 49RY9201_1 on section PR02

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.776198
title: MSCL measurements from IODP Hole 331-C0013E

description: Update on 2018-01-19: Parameter 'Susceptibility, volume' has been converted from [10**-5 SI] to [10**-6 SI]. All values were previously given in the wrong unit.
DOI: 10.1594/pangaea.776486
title: Electrical conductivity from IODP Hole 331-C0014C

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.811749
title: (Table 1) Trace element content at DSDP Hole 72-516F samples used in the matrix calculation
DOI: 10.1594/pangaea.782653
title: (Table S2) Summary of petrographic charactersitics of Pito Deep samples
DOI: 10.1594/pangaea.824973
title: Vane shear strength measurements from IODP Hole 334-U1379C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.694133
title: Nutrient concentrations in water samples from the Aegean Sea at Station JUNE-1998-IR12
DOI: 10.1594/pangaea.728409
title: (Appendix A, Table 9) Occurrence of stratigraphically important radiolaria species in ODP Hole 117-731A

description: Species occurrence: P = present, + = rare (one or two specimens), - = searched for and found to be absent
DOI: 10.1594/pangaea.787570
title: (Table T1) Magnetic properties of ODP Hole 175-1081C

description: Magnetic properties are reported for samples from sediment cores recovered at Site 1081 on the Walvis Ridge (~20°S) during Leg 175 of the Ocean Drilling Program. Rock magnetic data indicate that the remanence is carried by low-coercivity minerals. Paramagnetic and diamagnetic minerals dominate the susceptibility. Comparison of measurements made aboard ship with those made on shore after the cruise indicate a marked loss of magnetization, probably due to dissolution of some magnetic minerals after core recovery similar to that which has occurred at other Leg 175 sites.
description: Supplement to: Frost, Gina Marie; Yamazaki, Toshitsugu (2001): Data report: Magnetic properties of core sediments from Site 1081 (Walvis Ridge), Leg 175. In: Wefer, G; Berger, WH; Richter, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 175, 1-17
DOI: 10.1594/pangaea.664211
title: Oceanography at CTD/bottle station IFREMER_1052
DOI: 10.1594/pangaea.823276
title: (Table 5) Ratios between principal elements of the sedimentary deposits at DSDP Leg 55 Holes

description: Empty cells = no values of trace-element contents.
DOI: 10.1594/pangaea.811805
title: (Appendix A) Oxygen and carbon isotopic compositions of Globigerinoides ruber at DSDP Hole 72-517
DOI: 10.1594/pangaea.854387
title: (Table 5) Distribution and abundance of conodonts in Devonian/Carboniferous boundary profile at street between Rüthen and Nuttlar (Eulenspiegel-Sattel)
DOI: 10.1594/pangaea.854390
title: (Table 9) Distribution and abundance of conodonts in Devonian/Carboniferous boundary profile at Seiler-Schurf II
DOI: 10.1594/pangaea.854391
title: (Table 10) Distribution and abundance of conodonts in Devonian/Carboniferous boundary profile at Seiler-Schurf I
DOI: 10.1594/pangaea.771208
title: (Table 4) Location of the late Pliocene opal dissolution transition zone in ODP Leg 127 sites
DOI: 10.1594/pangaea.753626
title: (Table 8) Interstitial-water chemistry of ODP Site 112-683
DOI: 10.1594/pangaea.759630
title: (Table 1) Category and total organic carbon of sediment core ABC26

description: PO, postsapropel; OS, oxidised; (Mn), sample from the manganese marker bed; VS, Visible S1; PR, presapropel (*=no organic geochemical data available)
DOI: 10.1594/pangaea.746225
title: (Table 7) Factor loadings of planktonic foraminiferal analyses of ODP Site 108-662A

description: Depth, sediment (m) is composite depth (mcd). Full assemblage counts (second value listed) and quick counts with seven species (first value listed) are given; spliced record.
DOI: 10.1594/pangaea.720817
title: Documentation of sediment core GIK23298-1
DOI: 10.1594/pangaea.784998
title: Visual core description (VCD) from IODP Hole 333-C0012C

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.753090
title: (Table 4) Concentrations of dissolved free amino acids in interstitial-water samples from ODP Hole 111-677A
DOI: 10.1594/pangaea.777105
title: (Table S6) Ebridians, diatoms, radiolarian and actiniscidian abundance in ODP Hole 120-749B
DOI: 10.1594/pangaea.778483
title: Vane shear strength measurements from IODP Hole 317-U1352C

description: Geocode = Depth CSF-A (m).Technical Note 26 Chapter 9: http://www-odp.tamu.edu/publications/tnotes/tn26/CHAP9.PDF
DOI: 10.1594/pangaea.814052
title: Gel particles accumulation in the sea-surface microlayer

description: sml = sea-surface microlayer
DOI: 10.1594/pangaea.831218
title: Framework height data from Thai Andaman Sea coral reefs

description: CalMarO - Calcification by marine organisms, PEOPLE-2007-1-1-ITN Marie Curie Action: 215157BioAcid - German Ministry for Education and Research Project (Bmbf), Grant number 03F0608B, Bioacid 3.2.3, Coral Calcification in marginal reefsORCAS - Ocean Reef Coupling in the Andaman Sea - German Research Foundation (DFG), Grant number RI 1074/7-1
DOI: 10.1594/pangaea.728401
title: (Appendix A, Table 3) Occurrence of stratigraphically important radiolaria species in ODP Hole 117-723A

description: Species occurrence: P = present, + = rare (one or two specimens), - = searched for and found to be absent
DOI: 10.1594/pangaea.884622
title: Elemental ratios and BWT reconstruction for IODP Site 339-U1390
DOI: 10.1594/pangaea.728265
title: (Table 5) Occurrence chart of Paleogene diatom species in ODP Hole 115-714A

description: species abundance: S = singel (&lt;0.1%), R = rare (0.1%-1.0%), F = frequent (1%-10%), C = common (10%-30%), A = abundant (30%-50%), D = dominant (&gt;50%), - = absent
DOI: 10.1594/pangaea.663584
title: Oceanography at CTD/bottle station IFREMER_0424
DOI: 10.1594/pangaea.775950
title: (Table 2) Group composition of organic matter fro black shales collected in DSDP Holes 41-367 and 41-368
DOI: 10.1594/pangaea.776800
title: Core-section summary from IODP Hole 331-C0014F
DOI: 10.1594/pangaea.728686
title: (Table 7, 8) Calcareous nannofossil datum levels in ODP Hole 120-751A
DOI: 10.1594/pangaea.732336
title: (Table 2) Carbon isotope composition in carbonates of deep sea sediments from DSDP Hole 41-368
DOI: 10.1594/pangaea.758294
title: Meteorological data from Jubany Station, King George Island, Western Antarctic Peninsula, 1992
DOI: 10.1594/pangaea.718260
title: (Table 10) δ¹⁸O and δ¹³C data for Planulina wuellerstorfi / Cibicidoides kullenbergi in samples from DSDP Hole 72-518
DOI: 10.1594/pangaea.706055
title: Age determination of Lynch´s Crater, Australia

description: The pollen diagram from Lynch's Crater extends the climatic and vegetation record for the Atherton Tableland back to about 60,000 years B.P. Subtropical rain forest, with abundant Araucaria, was present around the site from before 60,000 B.P. to about 38,000 B.P. and existed under about half the present-day annual rainfall. This was replaced by sclerophyll vegetation between 38,000 and 27,000 B.P. as a result of a decrease in precipitation, a decrease in temperature or the activities of aboriginal man. In any case the agent of rain forest destruction was probably fire. The record for the last 10,000 years or so is probably incomplete and radiocarbon dates unreliable, but changes during this period are in broad agreement with those evidenced from previously described sites within the area. The sequence from Lynch's Crater provides a basis for the interpretation of many problematical features of present-day vegetation distributions.
description: Supplement to: Kershaw, A Peter (1976): A Late Pleistocene and Holocene pollen diagram from Lynch´s Crater, north-eastern Queensland, Australia. New Phytologist, 77(2), 469-498
DOI: 10.1594/pangaea.717809
title: Depth, age, strontium isotopic ratios and trace elemental ratios of samples from DSDP Hole 36-327A

description: Please note, that on 2017-06-09 it was discovered that the age values were given as "ka" alhough the values were "Ma". The data are now recalculated (x1000) to fit the unit.
DOI: 10.1594/pangaea.859985
title: 4.5. Natural remanent magnetization of SLW1 sediment cores

description: Results from the NRM step, which is the very first measurement for all samples, without any prior magnetic treatment (i.e., the 0 mT demagnetization step).
DOI: 10.1594/pangaea.706157
title: (Page 118-119) Physical oceanography of surface and bottom water during the drift of Vessel Varna

description: The Netherlands expedition intended to establish a station at Port Dikson, at the mouth of the Ienissei (Yenisey) river, but their ship was beset in heavy sea ice in the Kara Sea. The Varna, along with the Danish vessel Dijmphna, drifted with the ice for the entire IPY year. A station was built on the sea ice in October, near the two trapped ships. The Varna was crushed and finally sank on July 24, 1883.
DOI: 10.1594/pangaea.723321
title: Description of profile 7140-305
DOI: 10.1594/pangaea.681721
title: Estimate of mid-Pliocene Paleo-pCO2 for ODP Hole 130-806 (Table 1)

description: Three million years ago, prior to the onset of northern hemisphere glaciation, global mean temperatures may have been as much as 3.5 °C warmer than at present. We present evidence, based on the carbon isotopic composition of marine organic matter, that atmospheric CO2 levels at this time were on average only about 35% higher than the preindustrial value of 280 ppm. We also present carbon isotopic evidence for stronger thermohaline circulation in the Atlantic Ocean during the warmest intervals and propose that the North Atlantic “conveyor belt” may act as a positive feedback to global warming by enhancing sea ice retreat and decreasing high latitude albedo. Based on our results, it seems unlikely that the mid Pliocene warm period was a doubled CO, world.
description: Depth is composite depth (mcd), age estimetes are calibrated to timescale of Shackleton et al (1990)
description: Supplement to: Raymo, Maureen E; Grant, B; Horowitz, Michael; Rau, Greg H (1996): Mid-Pliocene warmth: stronger greenhouse and stronger conveyor. Marine Micropaleontology, 27(1-4), 313-326
DOI: 10.1594/pangaea.863359
title: Daily mean meteorology at station ARG, 2001-2011
DOI: 10.1594/pangaea.723348
title: Description of profile 7140-333
DOI: 10.1594/pangaea.733359
title: Documentation of sediment core MSM12/649-4
DOI: 10.1594/pangaea.776943
title: Description and distribution of lithologic units (VCD) from IODP Hole 331-C0015B

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.750578
title: Meteorological observations during MAGDALENA cruise from Calcutta to Batavia started at 1851-02-27
DOI: 10.1594/pangaea.788959
title: Documentation of sediment core M40/4_KL55
DOI: 10.1594/pangaea.667380
title: (Table 4) Chemistry and isotope ratios of glass and palagonite from DSDP Hole 52-418A
DOI: 10.1594/pangaea.615380
title: Description of sediment section MTC-S3
DOI: 10.1594/pangaea.746624
title: Chemical composition of basalt glasses from the Mid-Atlantic Ridge near 15°20'N
DOI: 10.1594/pangaea.673563
title: Radiosonde measurements from station Bermuda (2004-09)

description: Start location: Bermuda; Distance from radiation site: 2 km
DOI: 10.1594/pangaea.746649
title: Contents of the main rock-forming chemical elements in basalts from the Mid-Atlantic Ridge sampled at Station 15S-18
DOI: 10.1594/pangaea.788955
title: Documentation of sediment core M40/4_KL49
DOI: 10.1594/pangaea.774239
title: P-wave velocity anisotropy from IODP Hole 316-C0008A

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.858798
title: Friction measurements of IODP Hole 343-C0019
DOI: 10.1594/pangaea.920111
title: Calcareous nannofossil abundances in ODP Hole 143-865C

description: Preservation: P = poor (specimens severly etched/overgrown, primary features destroyed, fragmented, hard to ID to species and/or genus level) and M = moderate (specimens exhibit some etching/recrystallization but identifiable to species level) Total calcareous nannofossil abundance in the sediment: A = abundant (&gt;50-90% of sediment particles)Abundance of individual calcareous nannofossil taxa used in this study: R= rare (&lt; 1 specimen per 10 fields of view, FOV); F = few (1 specimen per 1-10 FOV); C = common (&gt;1-10 specimens per FOV); A = abundant (&gt;10-100 specimens per FOV and D = dominant (&gt;100 specimens per FOV). For study specific abundance definitions from previously published work see Bralower and Mutterlose (1995). For samples in this study, blank cells indicate that the species was not observed. For selected biostratigraphically important taxa (in bold) a dash is used to indicate where the sample has been inspected in this study or Bralower and Mutterlose (1995) but the species not found. Only abundance data for selected biostratigraphically important taxa have been transcribed here from Bralower and Mutterlose (1995). Datum picks used here are shown in highlighted grey cells. Dictyo. = Dictyococcites; Cr. = Cribrocentrum; Reticulofenestra (Dictyo.) stavensis = R. (Dictyo.) scrippsae in main text
DOI: 10.1594/pangaea.667405
title: (Table 2) Rare-earth elements of basalts from DSDP Hole 53-418A
DOI: 10.1594/pangaea.694225
title: Nutrient concentrations in water samples from the Ionian Sea at Station MARCH-2000-IRI41