cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.760773
title: (Table 1) Composition of clay minerals in DSDP Hole 75-532

description: An investigation of the quantitative composition of the coarse (&gt; 40 µm) and clay (&lt; 2 µm) fraction of HPC 532, DSDP Leg 75, in 1300 m water depth on the eastern Walvis Ridge off Southwest Africa yielded the following results:(1) The sediments reflect a complete Latest Miocene to Recent depositional history. Sedimentation rates vary between 2.3 and 7.8 cm/ka.(2) Preservation of calcium carbonate is subject to strong variations: short-term (&lt; 100,000 years) and long-term (about 1 m.y.) cycles in carbonate dissolution have been observed, with strongest dissolution occurring during periods of lowered sea level.(3) Upwelling influence from the near-coastal upwelling centre has been detected by means of the opal content: interglacial periods show high opal contents, because the Benguela Current turned westward at about 20°S and carried opal-laden upwelled water to the west. Sediments from glacial periods, however, show opal minima. Besides these short-term cyclic variations in opal content, long-term cycles have been found, with maximum upwelling influence in the latest Pliocene/early Quaternary.(4) Each CaCO3 dissolution minimum (maximum) is correlated with an opal maximum (minimum) throughout the sediment sequence.(5) The oceanographic system off southwest Africa remained essentially unchanged since the latest Miocene: sea level rose and fell periodically on a small and on a large scale, and the Benguela Current flowed southeast-northwest and turned to the west at the latitude of Site 532 during interglacial periods, when sea level was high.(6) The climate in the near-coastal area of southwest Africa in the latitude of Site 532 has probably been arid throughout the investigated period.
description: Supplement to: Diester-Haass, Lieselotte; Rothe, Peter (1987): Plio-Pleistocene sedimentation on the Walvis Ridge, Southeast Atlantic (DSDP Leg 75, Site 532) - Influence of surface currents, carbonate dissolution and climate. Marine Geology, 77(1-2), 53-85
DOI: 10.1594/pangaea.744580
title: (Table 7) Trace element contents and Sr and Nd isotopic characteristics of rocks at ODP Site 209-1275
DOI: 10.1594/pangaea.691030
title: Mesozooplankton average length during Akademik Vernadsky cruise AV9, Part III

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 0.125 mm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-300, 300-500 m) and closed at the upper depth level. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved in 3-4% buffered formaldehyde and processed on return to the laboratory. All of copepods were identified to genus level, other taxanomic groups - to type, class, order and family levels.
DOI: 10.1594/pangaea.746301
title: (Table 7) Distribution of planktonic foraminifers in ODP Hole 108-660A

description: Species abundance: A = abundant (&gt;30%), C = common, (15-30%), F = few (3-15%), R = rare (&lt;3%), X = present, but no abundance estimated, - = absent.
DOI: 10.1594/pangaea.228011
title: Interstitial water chemistry of Hole 12-112A

description: Details given in volume 12, part A, chapter 1
DOI: 10.1594/pangaea.734280
title: (Table 2) Cation concentrations in solutions obtained from leaching of serpentinites of ODP Hole 209-1268A

description: Fe (total) below detection limit
DOI: 10.15468/dl.ze92hp
title: Occurrence Download

description: A dataset containing 83809 species occurrences available in GBIF matching the query:
{
 "and" : [
 "DatasetKey is EOD – eBird Observation Dataset",
 "Geometry POLYGON((-107.38635 51.18486,-103.97403 41.30982,-92.13433 33.86477,-84.22396 32.57222,-81.48377 37.94921,-75.95168 42.49896,-74.60744 45.85958,-82.15589 50.77124,-94.71942 52.6325,-107.38635 51.18486))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Passer montanus (Linnaeus, 1758)",
 "Year 1970-2023"
 ]
}

 The dataset includes 83809 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069716-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.664496
title: Oceanography at CTD/bottle station IFREMER_1336
DOI: 10.1594/pangaea.721882
title: Heat flow ratios of stations from the Iberian abyssal plain (Table 1)

description: New heat flow observations have been made in the Iberia abyssal plain off the Galicia margin along the transeat of Ocean Drilling Program Leg 149 drill sites. in order to investigate the nature of this unusually wide and deep continet-ocean transition region. Our results indicate the presence of three separate zones. Average values of 47.5 +/- 3 mW/m in the westernmost zone III agree with predictions of standard oceanic lithospheric models for its estimated age of 126 Ma. In contrast, the heat flow within zone II is 5-15 mW/m higher than predicted. assuming that the mantle heat flow remains constant across the basin. This region of high values is coincident with the location of a major intra-crustal “S”-type reflector east of ODP Site 900. and the anomaly is consistent with the presence of 2-3 km of primarily upper continental crust above the reflector, with concentrations of radiogenic components similar to those from granodiorite samplles dredged off Galicia Bank. It is not, however, consistent with the low values of heat production measured on gabbroic sanhples from its western end at ODP Site 900. In zone I, detailed measurements across the tilted fault block south of ODP Site 901 show consistent variations which closely match predictions due to the effects of basement structure and sediment deposition. There is no evidence for variations due to vertical convective transport along the dipping basement fault block. Once corrected for these variations. measurements in zone I yield average values that agree quite well with previous measurements across Calicia Bank. indicating no systematic landward increase in heat flow with decreasing amounts of continental, extension.
description: Supplement to: Louden, Keith E; Sibuet, Jean-Claude; Harmegnies, Francois (1997): Variations in heat flow across the ocean-continent transition in the Iberia abyssal plain. Earth and Planetary Science Letters, 151(3-4), 233-254
DOI: 10.1594/pangaea.320523
title: Water temperature real-time profiles from cruise GACA91 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.322293
title: Water temperature and salinity real-time profiles from cruise CGCB95 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.324674
title: Water temperature real-time profiles from cruise ELVX499 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.804226
title: (Table 1) Porosity, and calcium carbonate, scandium and opal content of ODP Hole 164-994C sediments

description: Gas hydrate on the crest of the Blake Ridge is concentrated over two depth zones: between 185 and 260 mbsf, and between 380 and 450 mbsf. Although the abundance of hydrate in the lower zone may be explained by methane cycling across the phase boundary between free gas bubbles and gas hydrate, the upper zone lacks a satisfactory explanation. Chemical analyses of sediment samples from Hole 994C (31º47.139'N, 75º32.753'W) were performed to determine if the relatively high hydrate accumulation between 185 and 260 mbsf coincides with an observable change in sediment composition and microporosity. Our analyses indicate a distinct change in lithology across the upper hydrate zone: the carbonate content decreases from about 25% to about 8% with a corresponding increase in siliceous microfossils and bulk porosity. An increase in the abundance of siliceous microfossils increases the size and roundness of pore spaces. Large and round pores should provide nucleation sites for gas hydrate that are uninhibited by capillary forces between grains. Upward advecting fluids that are supersaturated with methane may deposit gas hydrate as they pass through the diatom-rich depth interval. Results presented here are consistent with the hypothesis that gas hydrate distribution is influenced by sediment lithology and microporosity.
description: Supplement to: Kraemer, Lisa M; Owen, Robert M; Dickens, Gerald Roy (2000): Lithology of the upper gas hydrate zone, Blake Outer Ridge: a link between diatoms, porosity, and gas hydrate. 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, 1-8
DOI: 10.1594/pangaea.690623
title: Mesozooplankton biomass during Mikhail Lomonosov cruise ML14, Part III

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 0.125 mm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-300, 300-500, 500-1000 m) and closed at the upper depth level. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved in 3-4% buffered formaldehyde and processed on return to the laboratory. All of copepods were identified to genus level, other taxanomic groups - to type, class, order and family levels.
DOI: 10.1594/pangaea.322132
title: Water temperature real-time profiles from cruise 4154698 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.772068
title: (Table S1) Stable oxygen isotope record of barite from DSDP Leg 85 sites

description: Oxygen isotopes in marine sulfate (d18O SO4) measured in marine barite show variability over the past 10 million years, including a 5per mil decrease during the Plio-Pleistocene, with near-constant values during the Miocene that are slightly enriched over the modern ocean. A numerical model suggests that sea level fluctuations during Plio-Pleistocene glacial cycles affected the sulfur cycle by reducing the area of continental shelves and increasing the oxidative weathering of pyrite. The data also require that sulfate concentrations were 10 to 20% lower in the late Miocene than today.
description: Supplement to: Turchyn, Alexandra V; Schrag, Daniel P (2004): Oxygen isotope constraints on the sulfur cycle over the past 10 million years. Science, 303(5666), 2004-2007
DOI: 10.1594/pangaea.790399
title: (Table 1) Chemical composition of basalt at DSDP Sample 92-597C-4-5,120-130

description: Empty cells indicate not determined or below detection limit.
DOI: 10.1594/pangaea.804007
title: (Table 3) Noble gas composition of dissociated gas hydrate specimens from ODP Leg 164 sites

description: Fractionation of the noble gases should occur during formation of a Structure I gas hydrate from water and CH4 such that CH4 hydrate is greatly enriched in Xenon. Noble gas concentrations and fractionation factors (F[4He], F[22Ne], F[86Kr], and F[132Xe] as well as R/Ra) were determined for eight gas hydrate specimens collected on Leg 164 to evaluate this theoretical possibility and to assess whether sufficient quantities of Xe are hosted in oceanic CH4 hydrate to account for Xe "missing" from the atmosphere. The simplest explanation for our results is that samples contain mixtures of air and two end-member gases. One of the end-member gases is depleted in Ne, but significantly enriched in Kr and Xe, as anticipated if the source of this gas involves fractionation during Structure I gas hydrate formation. However, although oceanic CH4 hydrate may be greatly enriched in Xe, simple mass balance calculations indicate that oceanic CH4 hydrate probably represents only a minor reservoir of terrestrial Xe. Noble gas analyses may play an important role in understanding the dynamics of gas hydrate reservoirs, but significantly more work is needed than presented here.
description: Noble gas data is presented in terms of F(i) values. An F(i) value is the fractionation factor relative to atmospheric composition, and is defined as: F(i) = [(i/36Ar)sample]/[(i/36Ar)air] where (i) is the concentration of an isotope of a noble gas.
description: Supplement to: Dickens, Gerald Roy; Kennedy, B Mack (2000): Noble gases in methane hydrate from the Blake Ridge. 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, 1-6
DOI: 10.1594/pangaea.262794
title: Major-element chemical analyses of Hole 82-557
DOI: 10.1594/pangaea.263406
title: (Table 5) Analyses of representative tholeiites and tholeiitic ferrobasalts ofthe Pacific Ocean
DOI: 10.1594/pangaea.602544
title: Radium226 concentrations of water samples at site M49_002 of the Northeast Atlantic (Table 7)
DOI: 10.1594/pangaea.720181
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 66-493

description: Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline quartzP = Plagioclase feldsparK = Potassium feldsparLvo = Other volcanic lithicLvd = Devitrified vitric volcanic lithicLvv = Vitric volcanic lithicLvf = Volcanic lithic with felsitic textureLvmi = Volcanic lithic with microlitic textureLvl = Volcanic lithic with lathwork textureLvp = Pyroclastic volcanic lithicLmv = Metavolcanic lithicLmm = Polycrystalline mica lithicLmt = Quartz-mica tectonite lithicLma = Quartz-feldspar-mica aggregate lithicLmp = Phyllite lithicLsa = Argillite-shale lithicLsc = Sedimentary carbonate lithicLsch = sedimentary chert or cherty argillite lithicLsi = Siltstone sedimentary lithicM = Phyllosilicate mineralsD = Dense mineralsCarb = Carbonate mineralsBio = Bioclastic debris (siliceous and/or carbonate)Misc = Miscellaneous and unidentifiedQ = Total quartzose grainsL = Unstable lithic grainsLm = Metamorphic lithic grainsLv = Volcanic-hypabyssal (and volcaniclastic) lithic grainsLs = Sedimentary lithic grainsLvm = Volcanic-hypabyssal and metavolcanic lithic grainsLsm = Sedimentary and metasedimentary lithic grainsLst = Sedimentary and polycrystalline quartz grainsF = Total feldspar grainsQp = Polycrystalline quartz grainsQ = Qm + Qpw + QptQp = Qpw + QptL = Lm + Lv + LsLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpLm = Lmv + Lmm + Lmt + LmaLsm = Ls + Lmm + Lmt + LmaLvc = Lvf + Lvmi + LvlLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpF = P + KLs = Lsa + LscLvm = Lv + LmvLst = Ls + QpQFL%Q = 100Q/(Q + F + L)QFL%F = 100F/(Q + F + L)QFL%L = 100L/(Q + F + L)QmKP%Qm = 100Qm/(Qm + P + K)QmKP%P = 100P/(Qm + P + K)QmKP%K = 100K/(Qm + P + K)LvfLvmiLvl%Lvf = 100Lvf/LvcLvfLvmiLvl%Lvmi = 100Lmi/LvcLmLvLs%Lm = 100Lm/LLmLvLs%Lv = 100Lv/LLmLvLs%Ls = 100Ls/LQpLvmLsm%Qp = 100Qp/(L + Qp)QpLvmLsm%Lvm = 100Lvm/(L + Qp)QpLvmLsm%Lsm = 100Lsm/(L + Qp)LvfLvmiLvl%Lvl = 100Lvl/Lvc
DOI: 10.1594/pangaea.723153
title: (Table 1) Sequential variation of carbonate cycles in DSDP Hole 74-527
DOI: 10.1594/pangaea.734283
title: (Table 2) Cation concentrations in solutions obtained from leaching of serpentinites of ODP Hole 209-1274A

description: Fe (total) below detection limit
DOI: 10.1594/pangaea.743391
title: (Figure 5) Distribution of Upper Cretaceous agglutinated benthic foraminifers in ODP Hole 103-640A

description: Species abundance: r = very rare, R = rare (1-3 specimens), F = few (+/-5), C = common (&gt;10), A = abundant (&gt;50)
DOI: 10.1594/pangaea.881742
title: Compiled linescanner images of sediment core GeoB20302-1
DOI: 10.1594/pangaea.690644
title: Mesozooplankton biomass during Mikhail Lomonosov cruise ML25, Part II

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 125 µm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-300, 300-500 m) and closed at the upper depth level. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved in 3-4% buffered formaldehyde and processed on return to the laboratory. All of copepods were identified to genus level, other taxonomic groups - to type, class, order and family levels.
DOI: 10.1594/pangaea.664461
title: Oceanography at CTD/bottle station IFREMER_1301
DOI: 10.1594/pangaea.668911
title: Basic measurements of radiation at station Chesapeake Light (2003-08)
DOI: 10.1594/pangaea.220735
title: Mineral composition of bulk sediment from Hole 9-83A
DOI: 10.1594/pangaea.659070
title: Frequency distributions of Siphonodictyon siphonum spicule dimensions (de Laubenfels, 1949); sample no. USNM 24107

description: See also doi:10.1594/PANGAEA.658964 for primary data
DOI: 10.1594/pangaea.320157
title: Water temperature real-time profiles from cruise NCQI90 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.762537
title: (Table 3) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-903C

description: X = present, - = absent.
DOI: 10.1594/pangaea.324827
title: Water temperature real-time profiles from cruise ELVX400 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.787673
title: (Table T4) Effective stress and porosity measurements of ODP Sample 174A-1073A-26X-2,76-82

description: Sediment depth is given in mbsf. Diameter was originally given as radius and was converted by multiplying by 2.
DOI: 10.1594/pangaea.322296
title: Water temperature and salinity real-time profiles from cruise CGCB98 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.801633
title: (Table 1) Carbonate aggregate mineralogy at DSDP at DSDP Sample 87-583C-2-1,71-72
DOI: 10.1594/pangaea.787840
title: (Table T1) Planktonic foraminiferal stratigraphy of ODP Hole 173-1065A sediments

description: Sediment depth is given in mbsf. Abundance estimate as follows: A = abundant, C = common, F = few, R = rare, B = barren, - = not found; rw = reworked.
DOI: 10.1594/pangaea.761559
title: (Table 6) Distribution of Pliocene calcareous nannofossils in ODP Hole 149-898A

description: Species abundance: V = very abundant (&gt;10 specimens per field of view at 1560 magnification), A = abundant (1-10 cpescimens per field), C = common (1 specimen per 2-10 fields), F = few (1 specimen per 11-50 fields), R = rare (1 specimen per 51-200 fields), r = reworked, - = not present. Sediment depth is given in mbsf.
DOI: 10.15468/dl.2thvxv
title: Occurrence Download

description: A dataset containing 29 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "POLYGON ((147.954029 -33.80879, 147.954029 -33.815527, 147.960766 -33.815527, 147.960766 -33.80879, 147.954029 -33.80879))"
 ]
}

 The dataset includes 29 records from 2 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069719-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.707328
title: (Table 2A) Composition of metalliferous component of DSDP Hole 92-597A sediments

description: Element contents are given on the salt-free carbonate-free basis. The metalliferous component was leached from the carbonate-free fraction (the carbonate fraction was previously leached by 4 hours treatment by 10% acetic acid) by 3 hours treatment by mixed acid-reducing agent (1 M NH2OH•HCl and 25% acetic acid) and then by 3 hours treatment by hot HCl. Then chemical composition of the leachate was studied.
DOI: 10.1594/pangaea.761633
title: (Table 5) Distribution of planktonic foraminifera in the latest Pliocene to Holocene section of ODP Hole 149-898A

description: Species abundance: R = rare, F = few, C = common, A = abundant, ? = questionable, RW = reworked, - = not present.
DOI: 10.1594/pangaea.761635
title: (Table 6) Distribution of planktonic foraminifera in the late Oligocene to middle Miocene section of ODP Hole 149-898A

description: Species abundance: R = rare, F = few, C = common, A = abundant, ? = questionable, RW = reworked, - = not present.
DOI: 10.1594/pangaea.774880
title: Stable carbon and oxygen isotope record of Cibicidoides wuellerstorfi of ODP Hole 162-982
DOI: 10.1594/pangaea.707337
title: (Table 2A') Accumulation rates of Fe and Mn in sediments from DSDP Hole 92-597A
DOI: 10.1594/pangaea.881749
title: Compiled linescanner images of sediment core GeoB20327-2
DOI: 10.1594/pangaea.707323
title: (Table 1) Element concentrations in the carbonate fraction of DSDP Hole 92-597A sediments

description: Data on the bulk salt-free basis of sediments. The carbonate fraction was leached by 4 hours treatment by 10% acetic acid. Then chemical composition of the leachate was studied.
DOI: 10.1594/pangaea.658963
title: Spicule dimensions of Siphonodictyon rodens (Johnson, 1899); from drawing of spicules of holotype

description: Substrate: Dendrophyllia ramea; Sampled by 'fishermen' and identified by J. Johnson as 'Acca rodens'. All measurements are of mature, fully formed oxeas (from drawing). Small sample size insufficient, does not allow statistical comparison with other samples. Measurements conducted by C. Schönberg on Johnson's Fig. 2. Data are sorted vertically by spicule width.; Johnson, James Y. (1899) Notes on some sponges belonging to the Clionidae obtained at Madeira. Journal of the Royal Microscopical Society, Transactions of the Society 9: 461-463 (S. rodens: p. 162, Fig. 2).
DOI: 10.1594/pangaea.221617
title: Physical properties of Hole 66-493
DOI: 10.1594/pangaea.321250
title: Water temperature real-time profiles from cruise GACA93 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.745547
title: (Table 4) Representative analyses of pyrrhotite of ODP Site 106-649

description: As, Ni, Sb, and Se contents are below detection limits
DOI: 10.1594/pangaea.745550
title: (Table 6) Representative analyses of Fe, Cu sulfides of ODP Site 106-649
DOI: 10.1594/pangaea.322764
title: Water temperature real-time profiles from cruise 6275700 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.358395
title: Stable isotope ratios measured on Cibicidoides spp. from DSDP Hole 40-360
DOI: 10.1594/pangaea.790793
title: (Appendix E) Geochemistry of oxides from DSDP Leg 92 holes
DOI: 10.1594/pangaea.787741
title: (Table T5) Stratigraphic distribution of calcareous nannofossil taxa of ODP Hole 173-1069A

description: Sediment depth is given in mbsf. Abundance estimate as follows: V = very abundant, A = abundant, C = common, F = few, R = rare, B = barren, - = not found.
DOI: 10.1594/pangaea.664517
title: Oceanography at CTD/bottle station IFREMER_1357
DOI: 10.1594/pangaea.320209
title: Water temperature real-time profiles from cruise NMOB90 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.768349
title: Stable organic carbon isotope ratios and total organic carbon content from the Cenomanian-Turonian boundary interval of ODP Site 207-1261
DOI: 10.1594/pangaea.322131
title: Water temperature real-time profiles from cruise 4154598 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.323178
title: Water temperature and salinity real-time profiles from cruise 4154100 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.320528
title: Water temperature real-time profiles from cruise NRCB91 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.802432
title: (Table 3) Magnetization after AF demagnetization of DSDP Hole 86-576