cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.26631802
title: Additional file 17 of Prediction of musculoskeletal pain after the first intravenous zoledronic acid injection in patients with primary osteoporosis: development and evaluation of a new nomogram

description: Supplementary Material 17
DOI: 10.6084/m9.figshare.26631802.v1
title: Additional file 17 of Prediction of musculoskeletal pain after the first intravenous zoledronic acid injection in patients with primary osteoporosis: development and evaluation of a new nomogram

description: Supplementary Material 17
DOI: 10.6084/m9.figshare.26631805.v1
title: Additional file 18 of Prediction of musculoskeletal pain after the first intravenous zoledronic acid injection in patients with primary osteoporosis: development and evaluation of a new nomogram

description: Supplementary Material 18
DOI: 10.6084/m9.figshare.26631808
title: Additional file 19 of Prediction of musculoskeletal pain after the first intravenous zoledronic acid injection in patients with primary osteoporosis: development and evaluation of a new nomogram

description: Supplementary Material 19
DOI: 10.6084/m9.figshare.26631808.v1
title: Additional file 19 of Prediction of musculoskeletal pain after the first intravenous zoledronic acid injection in patients with primary osteoporosis: development and evaluation of a new nomogram

description: Supplementary Material 19
DOI: 10.6084/m9.figshare.26631811
title: Additional file 20 of Prediction of musculoskeletal pain after the first intravenous zoledronic acid injection in patients with primary osteoporosis: development and evaluation of a new nomogram

description: Supplementary Material 20
DOI: 10.1594/pangaea.112386
title: Total medium sand fraction analysis of sediment core M8_057-2 (Table 3b)
DOI: 10.1594/pangaea.805281
title: (Table 2) Revised stacked record on magnetic susceptibility of ODP Site 162-984 sediments

description: Magnetic field and susceptibility data were collected using the geological high-resolution magnetometer tool string (GHMT) at three sites during Ocean Drilling Program Leg 162. Postcruise processing of the magnetic field data yielded a polarity stratigraphy for Holes 986C and 987E. A magnetic susceptibility record was measured at Hole 984B. Detailed analysis of the core and log susceptibility records at Hole 984B yielded an empirical tool resolution of the susceptibility measurement tool (SUMT) of 53 cm. At Site 984, where sedimentation rates were typically &gt;10 cm/k.y., this gave a resolution of at least ~5000 yr. This data report summarizes the GHMT postcruise processing, method of interpretation, and analysis of the SUMT resolution.
description: Supplement to: Higgins, Sean M; Kreitz, Scott F; King, Terri; Goldberg, David (1999): Data Report: Magnetic polarity and susceptibility measurements from the geological high-resolution magnetometer tool at Sites 984, 986, and 987. In: Raymo, ME; Jansen, E; Blum, P; Herbert, TD (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 162, 1-5
DOI: 10.1594/pangaea.112275
title: Physical oceanography from CTD station EN198_7-5
DOI: 10.1594/pangaea.715016
title: Trace element abundance, and Sr and Nd isotope ratios of dust samples in the Pacific Ocean (Table 2)

description: Eolian dust preserved in deep-sea sediment cores provides a valuable indicator of past atmospheric circulation and continental paleoclimate. In order to identify the provenance of eolian dust, Nd and Sr isotopic compositions and Rb, Sr and rare earth element (REE) concentrations have been determined for the silicate fractions of deep-sea sediments from the north and central Pacific Ocean. Different regions of the Pacific Ocean are characterized by distinct air-borne inputs, producing a large range in epsolin-Nd (-10 to +1), 87Sr/86Sr (0.705-0.721), La/Yb (5-15), EuN/EuN* (0.6-1.0) and Sr/Nd (4-33). The average Nd isotopic composition of Pacific deep-sea sediments (epsilon-Nd = -6), is more radiogenic than the average from the Atlantic (epsilon-Nd = -8). In contrast, the average147Sm/144Nd ratio for Pacific sediments (0.114) is identical to that of Atlantic sediments and to that of global average riverine suspended material. The values of epsilon-Nd and147Sm/144Nd are positively correlated for the Pacific samples but negatively correlated for Atlantic samples, reflecting a fundamental difference between the dominant components in the end members with radiogenic Nd (island-arc components in the Pacific and LREE-enriched intraplate ocean island components in the Atlantic). Samples from the north central Pacific have distinctive unradiogenic epsilon-Nd values of -10, 87Sr/86Sr &gt; 0.715, high La/Yb (&gt; 12), and low EuN/EuN* (0.6) and Sr/Nd (3-6). These data are virtually identical to the values for loess from Asia and endorse the use of these sediments as indicators of Asian paleoclimate and paleowind directions. Island-arc contributions appear to dominate in the northwest Pacific, resulting in higher epsilon Nd (-1 to +1) and lower 87Sr/86Sr (~ 0.705) and La/Yb (~ 5). Sediments from the eastern Pacific tend to have intermediate Sr and Nd isotopic compositions but regionally variable Sr/Nd and REE patterns; they appear to be derived from the west margin of the North and South American continents, rather than from Asia. Our results confirm that dust provenance can be constrained by isotopic and geochemical analyses, which will facilitate reconstructions of past atmospheric circulation and continental paleoclimate.
description: Supplement to: Nakai, Shunichi; Halliday, Alex N; Rea, David K (1993): Provenance of dust in the Pacific Ocean. Earth and Planetary Science Letters, 119(1-2), 143-157
DOI: 10.1594/pangaea.832801
title: Radiosonde PS83/35986 during POLARSTERN cruise PS83 (ANT-XXIX/10) on 2014-03-25 10:57h

description: Height of tropopause 17244 m, precipitable water content 1.3609 cm
DOI: 10.1594/pangaea.222848
title: Carbon analysis of Hole 30-288A
DOI: 10.1594/pangaea.419847
title: Hourly delayed mode sea level from coastal tide gauge station Key_West in 1987
DOI: 10.1594/pangaea.112574
title: Absolute number of siliceous skeletons in sediment core M8_020-2, Ibero-Moroccan shelf (Table 10)
DOI: 10.1594/pangaea.249773
title: Nannofossil abundance of Hole 84-566A

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.320240
title: Water temperature real-time profiles from cruise NTCH90 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.220749
title: Mineral composition of bulk sediment from Hole 44-390
DOI: 10.1594/pangaea.768338
title: (Table S6) Carbon isotope composition of organic carbon of ODP Site 207-1260

description: Sediment depth is given in mcd. Data between 422.2 - 429.6 mcd from Erbacher et al. (2005), for further details see datasets: doi:10.1594/PANGAEA.768350.
DOI: 10.1594/pangaea.322581
title: Water temperature and salinity real-time profiles from cruise 4189200 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.915656
title: Continuous sediment temperature observations at station BEFmate_I7Low (2019-06)
DOI: 10.1594/pangaea.314601
title: Continuous thermosalinograph oceanography along cruise track M12/3
DOI: 10.1594/pangaea.776740
title: (Table T1) Major and trace element concentrations of fine-grained sediments of ODP Hole 210-1276A

description: Inorganic chemical composition and downhole variation of major and trace elements yields useful insights into the sediment provenance and paleoceanography of deep-sea sediments of deepwater continental margins. Here, fine-grained sediments were chemically analyzed at ~10-m intervals from the Eocene to Albian section at Site 1276. These sediments represent a time when background hemipelagic sedimentation was continuously beneath, or near, the calcite compensation depth (CCD). Additional samples were analyzed from the upper Paleocene-middle Eocene time interval to determine whether a volcaniclastic component is present, as suggested by petrographic studies of the coarser size fraction. Sediments recovered near the bottom of the hole show the effects of contact metamorphism adjacent to a sill of alkaline basalt. The overlying thick (~700 m) Albian succession (lithologic Unit 5) is indicative of a dominantly terrigenous source. Redox-sensitive trace elements (e.g., Cu, Ni, V, and Cr) are concentrated in organic-rich layers (black shales) that can be partially correlated with oceanic anoxic Events 1a-1d and 2. Beginning around the Cenomanian/Turonian boundary, a profound change took place to more oxidizing, slowly depositing sediments throughout the North Atlantic, characterized by relative enrichment in Fe, Mn, and related trace metals (e.g., Cu, Ni, and Cr). Similar background conditions persisted until the Eocene when local conditions at Site 1276 became more reducing, as indicated by more subdued colors and lower MnO contents. Moderate upwelling along the Newfoundland continental margin during the Eocene is suggested by the presence of relatively high values of silica coupled with opaline silica. Phosphate and associated trace elements (e.g., Ce and Y) are locally enriched, suggesting relatively high primary productivity. However, productivity was lower than on the conjugate Iberia margin at Deep Sea Drilling Project Site 398. Fine-grained terrigenous sediments at Site 1276 probably were mainly derived from the Grand Banks (e.g., Avalon uplift) and finally accumulated in deep water below the CCD mainly as mud turbidites and hemipelagites.
description: Supplement to: Robertson, Alastair H F (2007): Geochemical evidence for the sedimentary and diagenetic development of the Mesozoic-early Cenozoic Newfoundland rifted margin, northwest Atlantic (Ocean Drilling Program Leg 210, Site 1276). In: Tucholke, BE; Sibuet, J-C; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 210, 1-63
DOI: 10.1594/pangaea.427941
title: Daily sea level from coastal tide gauge station Halifax in 1926 (Research quality database)
DOI: 10.1594/pangaea.801776
title: (Table 2) Mineralogic, elemental, and stable isotopic composition of bulk carbonate sediments from ODP Hole 166-1008A
DOI: 10.1594/pangaea.421344
title: Hourly delayed mode sea level from coastal tide gauge station San_Juan_II in 1985
DOI: 10.1594/pangaea.871111
title: Stable isotopes of ODP Site 154-929

description: CIBKULL C. kullenbergi/C.mundulus [per mil PDB]CWUELL C. wuellerstorfi [per mil PDB]CSPP C. SPP [per mil PDB]CBRA C. bradyii [per mil PDB]CCIC C. cicatricosus [per mil PDB]GLOSUB Globocassidulina subglobosa [per mil PDB]GORB G. orbicularis d18O [per mil PDB]NUMB N. umbonifera [per mil PDB]ORID Oridorsalis spp. [per mil PDB]OUMB O. umbonatus d18O [per mil PDB]PMUR P. murrhina d18O [per mil PDB]UVIG Uvigerina spp. [per mil PDB].
DOI: 10.1594/pangaea.399714
title: (Table 3) Strontium and Neodymium isotope ratios measured on sediment core SU90-38
DOI: 10.1594/pangaea.803853
title: (Table 1) Mineralogy and stable isotopic composition of diagenic carbonates from ODP Leg 164 sites

description: Sediment depth is given in mbsf. In situ temperatures have been deduced from the downhole measurements (Paull, Matsumoto, Wallace, et al., 1996, doi:10.2973/odp.proc.ir.164.1996). The d18O values of dolomite and siderite have been corrected for the differential phosphoric acid fractionation (Sharma and Clayton, 1965, doi:10.1016/0016-7037(65)90011-6; Carothers et al., 1988, doi:10.1016/0016-7037(88)90302-X). The d18O values of the diagenetic waters in equilibrium with the diagenetic dolomite, siderite, and calcite have been deduced from the 18O values of the carbonates and from the alpha values calculated for the in situ temperatures.
DOI: 10.1594/pangaea.801656
title: (Table 1) Thermal conductivities of lithified core samples from ODP Leg 166 sites

description: The geothermal regime of the western margin of the Great Bahama Bank was examined using the bottom hole temperature and thermal conductivity measurements obtained during and after Ocean Drilling Program (ODP) Leg 166. This study focuses on the data from the drilling transect of Sites 1003 through 1007. These data reveal two important observational characteristics. First, temperature vs. cumulative thermal resistance profiles from all the drill sites show significant curvature in the depth range of 40 to 100 mbsf. They tend to be of concave-upward shape. Second, the conductive background heat-flow values for these five drill sites, determined from deep, linear parts of the geothermal profiles, show a systematic variation along the drilling transect. Heat flow is 43-45 mW/m**2 on the seafloor away from the bank and decreases upslope to ~35 mW/m**2. We examine three mechanisms as potential causes for the curved geothermal profiles. They are: (1) a recent increase in sedimentation rate, (2) influx of seawater into shallow sediments, and (3) temporal fluctuation of the bottom water temperature (BWT). Our analysis shows that the first mechanism is negligible. The second mechanism may explain the data from Sites 1004 and 1005. The temperature profile of Site 1006 is most easily explained by the third mechanism. We reconstruct the history of BWT at this site by solving the inverse heat conduction problem. The inversion result indicates gradual warming throughout this century by ~1°C and is agreeable to other hydrographic and climatic data from the western subtropic Atlantic. However, data from Sites 1003 and 1007 do not seem to show such trends. Therefore, none of the three mechanisms tested here explain the observations from all the drill sites. As for the lateral variation of the background heat flow along the drill transect, we believe that much of it is caused by the thermal effect of the topographic variation. We model this effect by obtaining a two-dimensional analytical solution. The model suggests that the background heat flow of this area is ~43 mW/m**2, a value similar to the background heat flow determined for the Gulf of Mexico in the opposite side of the Florida carbonate platform.
description: Supplement to: Nagihara, Seiichi; Wang, Kelin (2000): Geothermal regime of the western margin of the Great Bahama Bank. In: Swart, PK; Eberli, GP; Malone, MJ; Sarg, JF (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 166, 1-8
DOI: 10.1594/pangaea.223403
title: Calcium carbonate bulk analysis of Hole 87-583G
DOI: 10.1594/pangaea.884156
title: Particulate geochemistry of sediment core M107_534-1
DOI: 10.6084/m9.figshare.26631910
title: Additional file 18 of Decoding meningioma heterogeneity and neoplastic cell—macrophage interaction through single-cell transcriptome profiling across pathological grades

description: Additional file 18: Table S8. Function of 33 Cell Communication Signals.
DOI: 10.1594/pangaea.476355
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_AN_26N/208

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.897492
title: (Table S20) Foraminiferal range charts of ODP Site 154-926 (9706-13855 ka)

description: P - indicates taxa present, ? - indicates questionable occurrence, - indicates absence.
DOI: 10.6084/m9.figshare.26629075
title: Additional file 14 of Cross-tissue patterns of DNA hypomethylation reveal genetically distinct histories of cell development

description: Additional file 14: Table S3. Inter-HMR lengths by cell type.
DOI: 10.1594/pangaea.419300
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1999
DOI: 10.1594/pangaea.320490
title: Water temperature from profiling float from cruise 009792 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.322232
title: Water temperature real-time profiles from cruise 6273798 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.322651
title: Water temperature real-time profiles from cruise 4902100 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.884206
title: Porewater geochemistry of sediment core M107_665-1

description: Second Barium parameter --&gt; Boron
DOI: 10.1594/pangaea.476161
title: Hydrochemistry measured on water bottle samples at station NAtl_1957_DS_47N/3511-2

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.771675
title: Physical oceanography during Walther Herwig III cruise WH262
DOI: 10.1594/pangaea.476532
title: Hydrochemistry measured on water bottle samples at station NAtl_1983_6N_37W/47

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.787614
title: (Table T1) Lithologic and ichnologic description of ODP Hole 174-1073A

description: When examined in their sedimentologic and stratigraphic context, ichnofabrics and component ichnofossils can help decipher paleoceanography and sea-level histories from marine deposits (Savrda, 1995, http://www.jstor.org/stable/3515095). Thus far, applications of ichnology in paleoceanographic investigations have been restricted to slowly deposited, predominantly biogenic sediments and/or strata deposited in oxygen-deficient, tectonically active basins. Moreover, ichnologic applications in sequence stratigraphic studies largely have been restricted to strata deposited in relatively shallow-water shelf or foreland basin settings. The limits of previous studies provided impetus for detailed postcruise examination of Quaternary deposits recovered at Ocean Drilling Program (ODP) Site 1073 on the New Jersey margin. These deposits provide the opportunity to assess the sedimentary and ichnofabric record of glacio-eustatic cycles in a passive continental slope setting characterized by relatively rapid accumulation of siliciclastic sediments in an area not far removed from the Laurentide ice margin.The primary purpose of this data report is to present basic sedimentologic and ichnologic observations made at the decimeter scale throughout the Quaternary sequence from Site 1073. Data analysis and interpretation in the context of climate and sea-level histories, as inferred from oxygen isotopic, palynologic, and seismic studies, are ongoing and will be presented in subsequent papers prepared for open literature (e.g., Savrda et al., in press).
description: Sediment depth is given in mbsf. Occurrences: X = present, - = absent, ? = questionable.
description: Supplement to: Savrda, Charles E; Krawinkel, Hannelore (2001): Data report: Decimeter-scale sedimentologic and ichnologic observations on a ~520-m-thick Pleistocene sequence, Site 1073 (Leg 174A), New Jersey Continental Slope. In: Christie-Blick, N; Austin, JA Jr.; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 174A, 1-9
DOI: 10.1594/pangaea.476185
title: Hydrochemistry measured on water bottle samples at station NAtl_1957_DS_47N/3535-2

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.476857
title: Hydrochemistry measured on water bottle samples at station NAtl_1983_OC_51W/252

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.476389
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_AN_37N/103

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.228482
title: Interstitial water chemistry of Hole 85-572D

description: Details given in volume 85, chapter 25
DOI: 10.1594/pangaea.745838
title: Oceanography during Discovery II cruise DISII60
DOI: 10.1594/pangaea.808204
title: Noble gases measured on water bottle samples during L' Atalante cruise EGEE3
DOI: 10.1594/pangaea.847765
title: (Table 1) Depth-age points used for initial chronology and adjusted ages of ODP Site 162-982

description: Ocean Drilling Program (ODP) Site 982 in the North Atlantic contains a complete latest Miocene to early Pliocene section that was tuned to the astronomical timescale by correlating the record of gamma ray attenuation (GRA) bulk density to summer insolation at 65°N and the benthic d18O signal to orbital obliquity for the interval from 4.6 to 7.5 Ma. The astronomical tuning of the Site 982 record permits a direct bed-to-bed correlation to the cyclostratigraphy of Messinian sections in the Mediterranean (Krijgsman et al., 1999a, doi:10.1038/23231, 2001, doi:10.1016/S0037-0738(00)00171-8). The benthic d18O signal at Site 982 records a latest Miocene glacial period that lasted from ~6.26 to 5.50 Ma and consisted of 18 glacial-to-interglacial oscillations that were controlled by the 41-kyr cycle of obliquity. Although the intensification of glaciation at 6.26 Ma may have contributed to the restriction of the Mediterranean, it preceded the depositional onset of the lower evaporite unit at 5.96 Ma by some 300 kyr. The transition from Stage TG12 to TG11 at 5.5 Ma marks the end of the latest Miocene glacial period and precedes the Miocene/Pliocene boundary by 170 kyr. Although benthic d18O values are relatively low and d18O of bulk carbonate reaches a minimum at the Miocene/Pliocene boundary at 5.33 Ma, there is no single "event" that would indicate deglaciation and sea level rise as the cause of the reflooding of the Mediterranean. We conclude that glacioeustatic changes alone were not responsible for either the start or end of evaporite deposition during the Messinian, suggesting that tectonic or local climate changes in the Mediterranean region were the dominant cause(s).
description: Marine isotope stages (MIS) designations follow Shackleton et al. (1995b, doi:10.2973/odp.proc.sr.138.117.1995). The ages for TG20 and TG12 were derived from Site 926 (Shackleton and Crowhurst, 1997, doi:10.2973/odp.proc.sr.154.102.1997), whereas all others were taken from Site 846 (Shackleton et al., 1995b, doi:10.2973/odp.proc.sr.138.117.1995) and adjusted by adding4 1 kyr correspondingto one obliquity cycle. Foraminiferal events are described by Sierro et al. (1993, doi:10.1016/0377-8398(93)90013-N), and the astronomical ages were derived from Hilgen et al. (1995, doi:10.1016/0012-821X(95)00207-S).
description: Supplement to: Hodell, David A; Curtis, Jason H; Sierro, Francisco Javier; Raymo, Maureen E (2001): Correlation of Late Miocene to Early Pliocene sequences between the Mediterranean and North Atlantic. Paleoceanography, 16(2), 164-178
DOI: 10.1594/pangaea.112273
title: Physical oceanography from CTD station EN198_6-4
DOI: 10.1594/pangaea.663661
title: Oceanography at CTD/bottle station IFREMER_0501
DOI: 10.6084/m9.figshare.24439295
title: Additional file 1 of Anti-atherosclerotic effects of naringenin and quercetin from Folium Artemisiae argyi by attenuating Interleukin-1 beta (IL-1β)/ matrix metalloproteinase 9 (MMP9): network pharmacology-based analysis and validation

description: Supplementary Material 1