cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.771885
title: (Table S3) TEX86 and BIT indices and temperature estimation for ODP Site 207-1259

description: Sediment depth is given in mcd, age follows the Ogg et al. (2004) timescale.
DOI: 10.15468/dl.c4fvbm
title: Occurrence Download

description: A dataset containing 8 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is one of (Berlinia hollandii Hutch. & Dalziel)"
 ]
}

 The dataset includes 8 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069932-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.26629084
title: Additional file 16 of Cross-tissue patterns of DNA hypomethylation reveal genetically distinct histories of cell development

description: Additional file 16: Table S5. List of 79 summary statistic files used for S-LDSC analyses.
DOI: 10.1594/pangaea.323748
title: Abundance of broken diatom frustules measured on water bottle samples at station PS58/046-3
DOI: 10.1594/pangaea.834223
title: Ichthyolith counts and MAR at DSDP Hole 74-527

description: DEPTH, sediment/rock [m] is given in mbsf. Tooth counts and sediment mass from Table 7 in Shackleton (1984). All ages were updated using magneto and biostratigraphic tie points as presented in Table 1 and 2 of Shackleton (1984). To re-calculate MAR rates, shipboard wet bulk density, porosity, grain density, porosity, and water content data was taken from Table 6 in Shipboard Scientific Party (1984). Site 527. in Init. Repts. DSDP 74 by Moore et al. (1984). Dry bulk density was then calculated using those factors (wet bulk density, porosity, etc), after a formula (equation 2) in Dadey et al. (1992). Note: All columns marked 'updated' were updated for the present paper as described above.
DOI: 10.6084/m9.figshare.26632585.v1
title: Additional file 3 of The chromatin architectural regulator SND1 mediates metastasis in triple-negative breast cancer by promoting CDH1 gene methylation

description: Additional file 3. Original western blots from Figures 1 to 7. The original, uncropped western blot membranes or film scans are shown. Molecular weight markers are included when available. Figures 1E, 2B, 4B, 4C, 6B, 6F, 7C and Supplementary Fig. S2 included.
DOI: 10.1594/pangaea.744332
title: Physical oceanography during Scotia cruise Scotia10/1 to the North Sea
DOI: 10.1594/pangaea.262862
title: Paleomagnetic measurements with a long-core spinner magnetometer of Hole 71-514
DOI: 10.1594/pangaea.770940
title: Physical oceanography during Walther Herwig I cruise WH36
DOI: 10.6084/m9.figshare.26630395
title: Additional file 3 of Association between fibrosis-related gene polymorphism and long-term allograft outcome in renal transplant recipients

description: Additional file 3: Table S2. Genetic information on SNPs of fibrosis-related genes.
DOI: 10.6084/m9.figshare.26630401
title: Additional file 5 of Association between fibrosis-related gene polymorphism and long-term allograft outcome in renal transplant recipients

description: Additional file 5: Table S4. Results of LD analysis.
DOI: 10.1594/pangaea.434033
title: Hourly sea level from coastal tide gauge station Charleston in 1934 (Research quality database)
DOI: 10.6084/m9.figshare.26742773.v1
title: Additional file 1 of Tissue of origin detection for cancer tumor using low-depth cfDNA samples through combination of tumor-specific methylation atlas and genome-wide methylation density in graph convolutional neural networks

description: Supplementary Material 1
DOI: 10.1594/pangaea.818758
title: (Table 2) Concentrations of particulate components in the water column at Station CATO-I/9 on 18 June 1972
DOI: 10.1594/pangaea.767461
title: (Table 3) Relative depth and age, CaCO3, δ¹⁸O, δ¹³C and Sr/Ca analysis from ODP Leg 130, 154 and 138

description: Interpretations of calcite strontium/calcium records in terms of ocean history and calcite diagenesis require distinguishing the effects on deep-sea calcite sediments of changes in ocean chemistry, of different mixes of calcite-depositing organisms as sediment contributors through time and space, and of the loss of Sr during diagenetic calcite recrystallization. In this paper Sr/Ca and d18O values of bulk calcium carbonate sediments are used to estimate the relative extent of calcite recrystallization in samples from four time points (core tops, 5.6, 9.4, and 37.1 Ma) at eight Ocean Drilling Program sites in the equatorial Atlantic (Ceara Rise) and equatorial Pacific (Ontong Java Plateau and two eastern equatorial Pacific sites). The possibility that site-to-site differences in calcite Sr/Ca at a given time point originated from temporal variations in ocean chemistry was eliminated by careful age control of samples for each time point, with sample ages differing by less than the oceanic residence times of Sr and Ca. The Sr/Ca and d18O values of 5.6- and 9.4-Ma samples from the less-carbonate-rich eastern equatorial Pacific sites and Ceara Rise Site 929 appear to be less diagenetically altered than the Sr/Ca and d18O values of contemporaneous samples from the more carbonate-rich sites. It is evident from these data that both Sr/Ca and d18O in bulk calcite have been diagenetically altered in some samples 5.6 Ma and older. These data indicate that noncarbonate sedimentary components, like clay and biogenic silica, have partially suppressed recrystallization at the lower carbonate sites. Sr/Ca data from the less altered, carbonate-poor sites indicate higher oceanic Sr/Ca relative to today at 5.6 and 9.4 Ma.
description: Sediment depth is given in mbsf. The Parameter AGE are not meant to represent the ''best'' possible age estimates, but to most accurately indicate the relative ages of samples within and between sites.
description: Supplement to: Andreasen, Gretchen Hampt; Delaney, Margaret Lois (2000): Lithologic controls on calcite recrystallization in Cenozoic deep-sea sediments. Marine Geology, 163(1-4), 109-124
DOI: 10.1594/pangaea.61562
title: Stable isotopes measured in sediment profile PS47/089A
DOI: 10.15468/dl.39g2kk
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "MULTIPOLYGON (((146.716594 -33.909851, 146.71884 -33.909851, 146.71884 -33.907605, 146.716594 -33.907605, 146.716594 -33.909851)), ((146.716594 -33.909851, 146.712102 -33.909851, 146.712102 -33.914343, 146.716594 -33.914343, 146.716594 -33.909851)))"
 ]
}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069933-240626123714530/datasets/export for details.
DOI: 10.1594/pangaea.832875
title: d11B and metal/Ca ratios versus size fractions in the Surface and deep dwelling species, ODP Holes 130-806B and 108-664C

description: We have assessed the reliability of several foraminifer-hosted proxies of the ocean carbonate system (d11B, B/Ca, and U/Ca) using Holocene samples from the Atlantic and Pacific oceans. We examined chemical variability over a range of test sizes for two surface-dwelling foraminifers (Globigerinoides sacculifer and Globigerinoides ruber). Measurements of d11B in G. ruber show no significant relationship with test size in either Atlantic or Pacific sites and appear to provide a robust proxy of surface seawater pH. Likewise there is no significant variability in the d11B of our Atlantic core top G. sacculifer, but we find that d11B increases with increasing test size for G. sacculifer in the Pacific. These systematic differences in d11B are inferred to be a consequence of isotopically light gametogenic calcite in G. sacculifer and its preferential preservation during postdepositional dissolution. The trace element ratio proxies of ocean carbonate equilibria, U/Ca and B/Ca, show systematic increases in both G. ruber and G. sacculifer with increasing test size, possibly as a result of changing growth rates. This behavior complicates their use in paleoceanographic reconstructions. In keeping with several previous studies we find that Mg/Ca ratios increase with increasing size fraction in our well-preserved Atlantic G. sacculifer but not in G. ruber. In contrast to previous interpretations we suggest that these observations reflect a proportionally larger influence of compositionally distinct gametogenic calcite in small individuals compared to larger ones. As with d11B this influences G. sacculifer but not G. ruber, which has negligible gametogenic calcite.
description: Supplement to: Ni, Yunyan; Foster, Gavin L; Bailey, Trevor R; Elliott, Tim; Schmidt, Daniela N; Pearson, Paul N; Haley, Brian A; Coath, Chris (2007): A core top assessment of proxies for the ocean carbonate system in surface-dwelling foraminifers. Paleoceanography, 22(3), PA3212
DOI: 10.1594/pangaea.920404
title: Continuous water level observations at station BEFmate_I3upp (2019-06)
DOI: 10.1594/pangaea.920406
title: Continuous water level observations at station BEFmate_I3upp (2019-08)
DOI: 10.1594/pangaea.832151
title: (Table 4) Carbon and nitrogen isotopic ratios of bulk samples from ODP Site 207-1260 and Hole 207-1261A

description: DEPTH, sediment [m] is given in mbsf. The highest d13Corg value (OAE3 samples) is not included in statistic.
DOI: 10.1594/pangaea.734282
title: (Table 2) Cation concentrations in solutions obtained from leaching of serpentinites of ODP Hole 209-1272A

description: Fe (total) below detection limit
DOI: 10.1594/pangaea.691287
title: Benthic foraminiferal number of specimens in Cretaceous samples of various DSDP and ODP Sites (Table 2)

description: Benthic foraminifera from 24 DSDP/ODP sites were investigated to assess their global horizontal and vertical distribution in the deep-sea environment at the end of the Cretaceous period. The samples analyzed are from the late Maastrichtian and within the planktic foraminiferal Abathomphus mayaroensis Zone from a wide range of oceans and paleolatitudes, including the low-latitude Sites 10 and 384 (Atlantic Ocean), 47, 171, 305, and 465 (Pacific Ocean), the mid-latitude Sites 20, 111, 356, 363, 516, 525, 527, 548, and 605 (Atlantic Ocean), 216, 217, and 758 (Indian Ocean), and the high-latitude Sites 208 (Pacific Ocean), 689,698,700,738 and 750 (Southern Ocean).Correspondence analysis, based on the 75 most common taxa, shows a clear biogeographic trend along the first correspondence axis by arranging the sites in paleolatitudinal order. The assemblages from the Tethyan Realm (i.e., low latitudes) are marked by abundant heavily calcified buliminids (such as Bulimina incisa, B. trinitatensis, B. velascoensis, and Reussella szajnochae) and Aragonia spp., whereas high-latitude faunas are characterized by abundant Alabamina creta, Gyroidinoides quadratus, and Pullenia coryelli.The results indicate that the faunas at low and high latitudes, respectively, were influenced by quite different environmental conditions. This is based on the much higher abundance of infaunal morphotypes at low and mid latitudes compared to high latitudes, suggesting that the biogeographic trend found in the data set coincides with the trophic regime at the various sites. The results also provide support for the hypothesis that postulates two simultaneous sources and mechanisms for deep-water formation during the Late Cretaceous, including warm, saline deep water produced by evaporation at low (equatorial) latitudes in contrast to the formation of cold deep waters at high (southern) latitudes.
description: Supplement to: Widmark, Joen G V (1995): Multiple deep-water sources and trophic regimes in the latest Cretaceous deep sea: evidence from benthic foraminifera. Marine Micropaleontology, 26(1-4), 361-384
DOI: 10.1594/pangaea.790820
title: (Table S1) Neodymium isotopes of fish teeth and hydroxylamine hydrochlorite extraction from ODP Site 207-1258

description: Sediment depth is given in mcd. For further Nd values see MacLeod et al. (2008) datasets doi:10.1594/PANGAEA.722613; MacLeod et al. (2011) datasets doi:10.1594/PANGAEA.792572 and Jiménez Berrocoso et al. (2010) datasets: doi:10.1594/PANGAEA.792598.
DOI: 10.1594/pangaea.920424
title: Continuous water level observations at station BEFmate_I4pio (2019-01)
DOI: 10.1594/pangaea.920429
title: Continuous water level observations at station BEFmate_I4pio (2019-06)
DOI: 10.1594/pangaea.920458
title: Continuous water level observations at station BEFmate_I4upp (2019-06)
DOI: 10.1594/pangaea.262668
title: Major-element chemical analyses of Hole 82-557
DOI: 10.1594/pangaea.920440
title: Continuous water level observations at station BEFmate_I10low (2019-02)
DOI: 10.1594/pangaea.920459
title: Continuous water level observations at station BEFmate_I4upp (2019-07)
DOI: 10.1594/pangaea.920478
title: Continuous water level observations at station BEFmate_I10upp (2019-04)
DOI: 10.1594/pangaea.920485
title: Continuous water level observations at station BEFmate_I10upp (2019-12)
DOI: 10.1594/pangaea.920489
title: Continuous water level observations at station BEFmate_S10low (2019-03)
DOI: 10.1594/pangaea.920494
title: Continuous water level observations at station BEFmate_S10low (2019-07)
DOI: 10.1594/pangaea.920503
title: Continuous water level observations at station BEFmate_S3low (2019-04)
DOI: 10.1594/pangaea.894429
title: Sea surface temperature reconstruction for IODP Site 306-U1314

description: Reconstructed with MAT (Prell, 1985) and the MARGO North Atlantic modern dataset, 10 analogs, as published in Alonso-Garcia et al, 2011.
DOI: 10.1594/pangaea.79340
title: Sediment community oxygen consumption at NPac_C_154
DOI: 10.1594/pangaea.920483
title: Continuous water level observations at station BEFmate_I10upp (2019-09)
DOI: 10.1594/pangaea.920540
title: Continuous water level observations at station BEFmate_S10upp (2019-05)
DOI: 10.6084/m9.figshare.24447665
title: Additional file 2 of Metabolism-associated molecular classification of cervical cancer

description: Additional file 2: Tables S1-S9.
DOI: 10.6084/m9.figshare.24447665.v1
title: Additional file 2 of Metabolism-associated molecular classification of cervical cancer

description: Additional file 2: Tables S1-S9.
DOI: 10.1594/pangaea.920534
title: Continuous water level observations at station BEFmate_S10pio (2019-10)
DOI: 10.1594/pangaea.789079
title: (Table 1) Li, B and Sr isotopic composition and concentration in ODP Leg 209 samples

description: Spinel harzburgites from ODP Leg 209 (Sites 1272A, 1274A) drilled at the Mid-Atlantic ridge between 14°N and 16°N are highly serpentinized (50-100%), but still preserve relics of primary phases (olivine &gt;= orthopyroxene &gt;&gt; clinopyroxene). We determined whole-rock B and Li isotope compositions in order to constrain the effect of serpentinization on d11B and d7Li. Our data indicate that during serpentinization Li is leached from the rock, while B is added. The samples from ODP Leg 209 show the heaviest d11B (+29.6 to +40.52 per mil) and lightest d7Li (-28.46 to +7.17 per mil) found so far in oceanic mantle. High 87Sr/86Sr ratios (0.708536 to 0.709130) indicate moderate water/rock ratios (3 to 273, on the average 39), in line with the high degree of serpentinization observed.Applying the known fractionation factors for 11B/10B and 7Li/6Li between seawater and silicates, serpentinized peridotite in equilibrium with seawater at conditions corresponding to those of the studied drill holes (pH: 8.2; temperature: 200 °C) should have d11B of +21.52 per mil and d7Li of +9.7 per mil. As the data from ODP Leg 209 are clearly not in line with this, we modelled a process of seawater-rock interaction where d11B and d7Li of seawater evolve during penetration into the oceanic plate. Assuming chemical equilibrium between fluid and a rock with d11B and d7Li of ODP Leg 209 samples, we obtain d11B and d7Li values of +50 to +60 per mil, -2 to +12 per mil, respectively, for the coexisting fluid. In the oceanic domain, no hydrothermal fluids with such high d11B have yet been found, but are predicted by theoretical calculations. Combining the calculated water/rock ratios with the d7Li and d11B evolution in the fluid, shows that modification of d7Li during serpentinization requires higher water/rock ratios than modification of d11B.Extremely heavy d11B in serpentinized oceanic mantle can potentially be transported into subduction zones, as the B budget of the oceanic plate is dominated by serpentinites. Extremely light d7Li is unlikely to survive as the Li budget is dominated by the oceanic crust, even at small fractions.
description: Supplement to: Vils, Flurin; Tonarini, Sonia; Kalt, Angelika; Seitz, Hans-Michael (2009): Boron, lithium and strontium isotopes as tracers of seawater–serpentinite interaction at Mid-Atlantic ridge, ODP Leg 209. Earth and Planetary Science Letters, 286(3-4), 414-425
DOI: 10.1594/pangaea.52325
title: (Appendix 1) Stable carbon and oxygen isotope ratios of Cibicidoides spp. from sediment core CH72-02
DOI: 10.6084/m9.figshare.26628529
title: Additional file 4 of Unmapped short reads from whole-genome sequencing indicate potential infectious pathogens in German Black Pied cattle

description: Additional file 4: Average assembly and animal sample count information for detected bacteria in DSN cattle.  Arithmetic means are given for assembly size, k-mer depth, number of scaffolds, and genome cover, with standard errors given in parenthesis.
DOI: 10.1594/pangaea.910462
title: (Table S04) Age Model, barium accumulation, and silica accumulation in DSDP Hole 91-596

description: Age/Depth datums from Zhou and Kyte 1992. Table 5 includes age datums. Age was adjusted to GTS 2012 by converting fixed iridium anomaly K/Pg Boundary age of 66.4 (Zhou and Kyte 1992) to 66.04 and shifting the timescale by 0.36 Ma. This compiled table includes data from Table 2 (Barium concentration), Table 3 (Silica concentration), and Table 5 (Age/Sedimentation Model). Data in T2 and T3 did not include ages. The Age (Ma) GTS2012 column includes analyseries-generated ages for these samples.Dry bulk density (DBD) was linearly interpolated for all samples used in this study from the values given below.
DOI: 10.1594/pangaea.229888
title: Sound velocity of Hole 85-572A
DOI: 10.6084/m9.figshare.26630410.v1
title: Additional file 2 of The sucrose non-fermenting-1 kinase Snf1 is involved in fludioxonil resistance via interacting with the high osmolarity glycerol MAPK kinase Hog1 in Fusarium

description: Additional file 2: Table S1. Bases mutation detected by re-sequencing. Table S2. Primers used in this study.
DOI: 10.1594/pangaea.320152
title: Water temperature real-time profiles from cruise NBON90 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.225178
title: Wet bulk density (GRAPE) of Hole 85-571
DOI: 10.1594/pangaea.322944
title: Water temperature BT profiles from cruise 18GA94002 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.225182
title: Wet bulk density (GRAPE) of Hole 85-572C
DOI: 10.1594/pangaea.476617
title: Hydrochemistry measured on water bottle samples at station NAtl_1983_OC_51W/215

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.761650
title: (Table 15) Distribution of planktonic foraminifera in the early to early late Oligocene section of ODP Hole 149-900A

description: Species abundance: R = rare, F = few, C = common, A = abundant, ? = questionable, RW = reworked, - = not present.
DOI: 10.1594/pangaea.322630
title: Water temperature real-time profiles from cruise 4901000 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.476900
title: Hydrochemistry measured on water bottle samples at station NAtl_1983_OC_51W/295

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.322044
title: Water temperature real-time profiles from cruise NBRK99 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.476382
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_AN_26N/235

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.6084/m9.figshare.26763280
title: Genesis of Seismic Gap of the 2008 Wenchuan and 2022&2013 Lushan Earthquakes: Insight from 3d Electrical Structure

description: The files is the dataset for the manuscript entitled 'Genesis of Seismic Gap of the 2008 Wenchuan and 2022&2013 Lushan Earthquakes: Insight from 3d Electrical Structure' by Wang et al., including data file(FullZ_1005.dat), Model file(RHO100.rho), and model covariance file(cov03.cov).
DOI: 10.1594/pangaea.476107
title: Hydrochemistry measured on water bottle samples at station Atlantic_10-13N/18

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.320236
title: Water temperature real-time profiles from cruise NSEM90 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.219993
title: Mineral composition of clay fraction from Hole 9-83A
DOI: 10.1594/pangaea.915620
title: Continuous sediment temperature observations at station BEFmate_I3Low (2019-07)
DOI: 10.1594/pangaea.79359
title: Sediment community oxygen consumption at NPac_SCB_125
DOI: 10.6084/m9.figshare.26629240
title: Additional file 3 of Dual spatially resolved transcriptomics for human host–pathogen colocalization studies in FFPE tissue sections

description: Additional file 3: Table S2. Patient data. Relevant clinical parameters of the 5 patients included in this study are summarized.
DOI: 10.15468/dl.yrug3y
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "POLYGON ((146.808671 -33.909851, 146.808671 -33.914343, 146.810917 -33.914343, 146.810917 -33.909851, 146.808671 -33.909851))"
 ]
}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069934-240626123714530/datasets/export for details.
DOI: 10.6084/m9.figshare.24452465.v1
title: Additional file 1 of Detection and characterization of spike architecture based on deep learning and X-ray computed tomography in barley

description: Additional file 1: Table S1. Image resolution and point cloud clustering parameter of CT images.
DOI: 10.6084/m9.figshare.26633055
title: Additional file 3 of Detection and characterization of spike architecture based on deep learning and X-ray computed tomography in barley

description: Additional file 3: Table S3. Detailed descriptions of phenotype definition.
DOI: 10.6084/m9.figshare.26633055.v1
title: Additional file 3 of Detection and characterization of spike architecture based on deep learning and X-ray computed tomography in barley

description: Additional file 3: Table S3. Detailed descriptions of phenotype definition.
DOI: 10.15468/dl.hfnx5q
title: Occurrence Download

description: A dataset containing 8 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is one of (Berlinia hollandii Hutch. & Dalziel)"
 ]
}

 The dataset includes 8 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069935-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.