cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.728426
title: (Appendix B) Communality and factor loadings for sediment core RC27-4
DOI: 10.1594/pangaea.811101
title: (Table 3) Rare-earth-elements of basalts at DSDP Leg 73 Holes
DOI: 10.1594/pangaea.811023
title: (Table 2) Minerals of modal analyses at DSDP Leg 73 Holes
DOI: 10.1594/pangaea.838224
title: Pollen profile WINNEYS, United Kingdom

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.728129
title: (Table 2) Major element analyses of glass particles from sediment cores HM79-6.2 and HM79-4
DOI: 10.1594/pangaea.727172
title: (Table 2b) Sand content of sediment core ERDC-124P
DOI: 10.1594/pangaea.838586
title: Lithology of sediment core EXBRIDGE, United Kingdom

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.671349
title: Basic measurements of radiation at station Sede Boqer (2005-01)
DOI: 10.1594/pangaea.811127
title: (Table 3) Numerical ages of foraminiferal datum levels at DSDP Leg 73 Holes
DOI: 10.1594/pangaea.784649
title: (Table T2) Depths and ages of calcareous nannofossil events at ODP Sites 184-1147 and 184-1148

description: DEPTH, sediment is given in mcd.
DOI: 10.1594/pangaea.884011
title: Radiosonde measurements from station Fukuoka (2017-10)
DOI: 10.1594/pangaea.784650
title: (Table T3) Depths and ages of calcareous nannofossil events at ODP Site 184-1146

description: DEPTH, sediment is given in mcd.
DOI: 10.1594/pangaea.785229
title: (Table 4) Geochemistry of basement basaltic rocks from ODP Hole 131-808C
DOI: 10.1594/pangaea.726439
title: (Table 1) Organic carbon content of ODP Site 113-689
DOI: 10.1594/pangaea.784802
title: (Table T1) Geochemical composition of ODP Site 184-1143 late Pliocene sediments

description: Pliocene core intervals from Ocean Drilling Program Site 1143 located in the southern part of the South China Sea were measured for their major and minor element composition at ~2-k.y. resolution. Changes in sediment composition parallel glacial-interglacial changes as indicated by the corresponding oxygen isotope record of benthic foraminifers. Carbonate contents are lower during glacial stages and higher during interglacial stages. This is attributed to dilution by a higher contribution of terrigenous detrital matter during glacial intervals and to enhanced biological productivity during interglacials as indicated by enrichments in barium. The terrigenous detrital matter fraction shows small but distinct changes in composition. These variations may be explained by multiple processes, including changes in provenance and weathering caused by monsoonal climate variability and sea level fluctuations. Gradual or long-term changes in sediment composition also occur during the investigated interval. There is a shift toward lower TiO2 (carbonate-free basis; cfb) values at around 2.9 Ma and an increase in Al2O3 (cfb) variations at around 2.55 Ma. These changes can be explained in both cases by an increasing contribution from the Mekong River, delivering material with low TiO2 (cfb)/Al2O3 (cfb) ratios, followed by a gradual increase in weathering, causing higher Al2O3 (cfb) (probably reflecting kaolinite) contents. Both may be the result of an enhanced summer monsoon. The manganese and phosphate geochemistry of Site 1143 sediments seem to be strongly dominated by biological productivity and a high burial flux of carbonate, which acts as an adsorbing agent and/or substrate. During strong interglacials and corresponding times of enhanced productivity, Mn may be remobilized from continental margin sediments deposited within an oxygen minimum zone and subsequently exported into the pelagic region, where it oxidizes and settles to form Mn-enriched layers in the sediment.
description: Sediment depth is given in mcd. Elemental contents were calculated on a carbonate-free basis.
description: Supplement to: Wehausen, Rolf; Tian, Jun; Brumsack, Hans-Jürgen; Cheng, Xinrong; Wang, Pinxian (2003): Geochemistry of Pliocene sediments from ODP Site 1143 (southern South China Sea). In: Prell, WL; Wang, P; Blum, P; Rea, DK; Clemens, SC (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 184, 1-25
DOI: 10.1594/pangaea.785244
title: (Table 1) Results of permeability testing of sediments from ODP Site 131-808A

description: Coring at ODP Site 808 successfully recovered a sequence of accreted and subducted sediments from the toe of the Nankai convergent margin. Detailed physical properties measurements revealed a systematic downhole consolidation trend, punctuated by two main offsets: a thrust fault at 365 mbsf and a décollement near 950 mbsf. Sediment dewatering during the accretion and subduction processes are strongly influenced by the permeability of the sediments. Results of over 60 permeability measurements made on subsamples of Site 808 cores reveal coefficients of permeability ranging from 10**-5 to 10**-10 cm/s (10**-14 to 10**-19 m**2) in horizontal and vertical directions. The generally low permeability of sediments at the depth of the décollement must influence the stress-strain behavior of this major structural horizon.
description: Supplement to: Taylor, Elliott; Fisher, Andrew T (1993): Sediment permeability at the Nankai accretionary prism, Site 808. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 235-245
DOI: 10.1594/pangaea.727193
title: (Table 5) Model 10Be/9Be ages of ODP Hole 181-1121B sediments
DOI: 10.1594/pangaea.783552
title: (Table T2) Minerals and major element oxides of authigenic carbonates from ODP Site 186-1150

description: Sediment depth is given in mbsf. Element composition is given in mol %.
DOI: 10.1594/pangaea.785264
title: (Table 2) Vertical effective stress and pore pressure parameter for ODP Site 131-808
DOI: 10.1594/pangaea.784118
title: (Table T1) Wet and dry resistivity along three orthogonal directions of ODP Hole 185-801C

description: Sediment depth is given in mbsf. Resistivity values of &gt;9999 = above detection limit of 9999.9 Ohm m.
DOI: 10.1594/pangaea.755865
title: Radiosonde measurements from station Tamanrasset (2010-12)

description: Start location: Tamanrasset; Distance from radiation site: 10 km
DOI: 10.1594/pangaea.784119
title: (Table T2) Wet and dry resistivity along three orthogonal directions of ODP Hole 185-1149B

description: Sediment depth is given in mbsf. Lithology and lithologic units are as defined during Leg 185 (Shipboard Scientific Party, 2000, doi:10.2973/odp.proc.ir.185.104.2000).
DOI: 10.1594/pangaea.784130
title: (Table T5) New combined 40Ar/39Ar and magnetostratigraphic chronostratigraphy of ODP Sites 185-1149 and 191-1179
DOI: 10.1594/pangaea.816583
title: (Table 1) Compressional-wave and shear-wave velocities and elastic constants from DSDP Legs 69 and 70

description: Shear-wave and compressional-wave velocities of 26 basalt samples collected at Site 504 during Deep Sea Drilling Project Legs 69 and 70 were measured at elevated confining pressures. The young basalts have higher velocities than average DSDP basalts, because of their lack of alteration. Measurements of sample porosity are combined with laboratory and in situ velocity measurements to yield estimates of total crustal porosity: 13% at the top of Layer 2, and very low porosity below a depth of 2.0 km.
description: Supplement to: Wilkens, Roy H; Christensen, Nikolas I; Slater, L (1983): High-pressure seismic studies of Leg 69 and 70 basalts. In: Cann, JR; Langseth, MG; Honnorez, J; Von Herzen, RP; White, SM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 69, 683-686
DOI: 10.1594/pangaea.785285
title: (Table 2) TOC, maceral composition, and vitrinit reflectance of two vitrinite populations in sediments of ODP Site 131-808

description: Sediment depth is given in mbsf. A minor amount of cutinite was observed in Sample 131-808C-10R-3,26-28.
DOI: 10.1594/pangaea.783924
title: (Table 1) Silicoflagellate abundance in ODP Hole 186-1149A sediments

description: Silicoflagellate assemblages have been studied from Hole 1149A (northwestern Pacific, Ocean Drilling Program Leg 185) in a continuous record of pelagic clay from lithologic Unit I. The biostratigraphic framework of D. Bukry, adapted in this work, is calibrated to tropical and subtropical fossil floras. Four biozones and three subzones have been recognized (from the lower Pliocene Dictyocha fibula Zone to the Quaternary Dictyocha aculeata aculeata Zone), and their zonal boundaries have been calibrated to the magnetostratigraphic scale. In particular, the boundary between the Dictyocha perlaevis delicata and the Dictyocha perlaevis ornata Subzones approximates the Pliocene/Pleistocene boundary.The identification of three closely spaced climatic events (the asperoid/fibuloid reversal at 75.11 meters below seafloor [mbsf], the sharp decrease in abundance of Distephanus sp. at 70.05 mbsf, and the last occurrence of Distephanus boliviensis at 68.46 mbsf) indicates the increased strength of the warm Kuroshio Current in the interval between 3.3 and 2.8 Ma, due to the final closure of the Central American Seaway and leading to the present-day hydrodynamic regime. The beginning of the acme of Mesocena quadrangula at 37.01 mbsf (~1.1 Ma) also shows a sharp warming in surface waters.
description: Sediment depth is given in mbsf. Sample observation was performed under a polarizing light microscope at 400x magnification. Abundance estimate as follows: A = abundant, C = common, F = few, R = rare, VR = very rare, - not found.
description: Supplement to: Lozar, Francesca; Mussa, Massimo (2003): Silicoflagellate biostratigraphy, Hole 1149A (ODP Leg 185, Nadezhda Basin, northwestern Pacific). In: Ludden, JN; Plank, T; Escutia, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 185, 1-18
DOI: 10.1594/pangaea.910503
title: Ultra-violet measurements from station Bondville (2019-06)
DOI: 10.1594/pangaea.819284
title: (Table 3) Geochemistry of clinopyroxene at DSDP Leg 63 Holes

description: Formula basis = 6 oxygens.
DOI: 10.1594/pangaea.825073
title: Age determination results from site Aschersleben
DOI: 10.1594/pangaea.740586
title: Age determination of sediment core MOSFELL, Mosfell, Iceland

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.783926
title: (Table 1) Calcareous nannofossil abundance in ODP Hole 185-1149B sediments

description: Sediment depth is given in mbsf. Abundance estimate as follows: A = abundant, C = common, F = few, R = rare, VR = very rare, B = barren, - not found.
DOI: 10.15468/dl.jpxps2
title: Occurrence Download

description: A dataset containing 78 species occurrences available in GBIF matching the query:
{
 "and" : [
 "GadmGid is PAK",
 "TaxonKey is Neophron percnopterus (Linnaeus, 1758)"
 ]
}

 The dataset includes 78 records from 4 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031399-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.785276
title: (Table 1) Heavy metal concentration of surface sediments from Neustadt lagoon, north Germany
DOI: 10.1594/pangaea.728288
title: (Table 2) Organic matter, pyrite, sand and foraminifera content of ODP Hole 116-717C

description: A = abundant, C = common, R = rare
DOI: 10.1594/pangaea.783927
title: (Table 2) Calcareous nannofossil abundance in ODP Hole 185-1149C sediments

description: Sediment depth is given in mbsf. Abundance estimate as follows: A = abundant, C = common, F = few, R = rare, - not found.
DOI: 10.1594/pangaea.818017
title: (Table 1) Abundance, refractive indices, color, and shape of glass shards in ash layers from DSDP Leg 65 Holes

description: Empty cells mean not determined.
DOI: 10.1594/pangaea.918434
title: Radiocarbon dates of organic material from sediments in the third terrace of the Seyaha River, Bovanenkovo

description: Radiocarbon dates of organic material from sediments including massive ice body (body 1) in the third terrace of the Seyaha River, Bovanenkovo. Samples of organic material for radiocarbon age analyses have been selected in surrounding sediments of massive ice. ¹⁴C ages have been obtained in Radiocarbon Laboratory of GIN RAS (L.D.Sulerzhitsky).
DOI: 10.1594/pangaea.511144
title: Radiosonde at Georg-Forster station on 1988-09-25 12:00h

description: Height of tropopause 11334 m, total ozone 303.3 DU
DOI: 10.1594/pangaea.783928
title: (Table 3) Calcareous nannofossil abundance in ODP Hole 185-1149D sediments

description: Sediment depth is given in mbsf. Abundance estimate as follows: A = abundant, C = common, F = few, R = rare, VR = very rare, T = trace, B = barren, - not found.
DOI: 10.1594/pangaea.728143
title: (Table 3) Stratigraphic range chart for radiolaria in ODP Hole 104-642C

description: Species abundance: - = not present (0 specimens per longitudinal traverse), T = trace (&lt;1), R = rare (1), S = sparce (2-4), C = common (5-9), A = abundant (10-15), VA = very abundant (16-20), D = dominant (21-49), VD = very dominant (50-100) F = flood (&gt;100)
DOI: 10.1594/pangaea.787876
title: Ionic composition of snow from snow pit SP_NMsued030107 excavated near Neumayer Station
DOI: 10.1594/pangaea.817273
title: Hydochemistry measured on water bottle samples during TYRO cruise NIOP-D3
DOI: 10.1594/pangaea.723469
title: Radiosonde measurements from station Southern Great Plains (1996-07)

description: Version 2, 2009-07-02; Launches at irregular time intervals. The radiosonde measurements from station Southern Great Plains are used for Billings and E13
DOI: 10.1594/pangaea.726175
title: Rock eval analysis of organic material from DSDP Hole 76-534A
DOI: 10.1594/pangaea.728289
title: (Table 2) Organic matter, pyrite, sand and foraminifera content of ODP Hole 116-718C

description: A = abundant, C = common, R = rare
DOI: 10.1594/pangaea.783456
title: (Table 3) Contents of major rock-forming elements, trace elements, and rare earth elements in basalts from ODP Hole 183-1137A
DOI: 10.1594/pangaea.783457
title: (Table 4) Contents of major rock-forming elements, trace elements, and rare earth elements in basalts from ODP Hole 183-1138A
DOI: 10.1594/pangaea.816582
title: (Table 1) Physical properties of basalts from DSDP Legs 69 and 70

description: Physical properties of basalts from Deep Sea Drilling Project Sites 504 and 505, south of the Costa Rica Rift, including wet-bulk density, water content, sonic velocity, and thermal conductivity, were measured on board D/V Glomar Challenger during Legs 69 and 70. The mean wet-bulk density is 2.90±0.06 g/cm**3, porosity 5.0±2.2%, sonic velocity 5.75±0.30 km/s, and thermal conductivity 1.67±0.09 W/m°K.Basalts from this young ocean crust (5.9 m.y.) have relatively low porosity and consequently high density and sonic velocity, as compared to average DSDP basalts.Some systematic trends in depth variation of physical properties were found: down to Core 40 in Hole 504B, grain densities were lower than those deeper in the hole, whereas porosity in the upper section was higher. This can be attributed either to differences in the flow type or in the nature of alteration of basalts at the different levels in the hole.
description: Supplement to: Karato, Shun-ichiro; Wilkens, Roy H; Langseth, Marcus G (1983): Shipboard physical-properties measurements of basalts from the Costa Rica Rift, Deep Sea Drilling Project Legs 69 and 70. In: Cann, JR; Langseth, MG; Honnorez, J; Von Herzen, RP; White, SM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 69, 675-681
DOI: 10.1594/pangaea.668179
title: Basic measurements of radiation at station Camborne (2002-12)
DOI: 10.1594/pangaea.783656
title: (Table T1) Major element oxides of bulk samples from ODP Holes 186-1150B and 186-1151A
DOI: 10.1594/pangaea.719408
title: Other measurements at 10 m from station Bondville (1999-07)

description: Version 2, 2009-06-15
DOI: 10.1594/pangaea.728158
title: (Table 3) Distribution of middle Eoecen-lowest Miocene calcareous nannofossils in ODP Hole 120-748B

description: V = very abundand, A = abundant, C = common, F = few, R = rare, r = rare reworked specimens, F = few reworked specimens, - = absent. The high-latitude zonation of Wei and Wise (1990 doi:10.2973/odp.proc.sr.113.125.1990) is used with the erection of the LO of Reticulofenestra bisecta as the marker for the Oligocene/Miocene boundary.
DOI: 10.1594/pangaea.740351
title: Age determination of sediment core FOUGS948, Fougères, France

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.816913
title: Physical oceanography during John P. Tully cruise IOS_97-11
DOI: 10.1594/pangaea.740649
title: Age determination of sediment core PANBRI, Pannel Bridge, United Kingdom

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.819296
title: (Table 1) Geochemistry of clinopyroxene at DSDP Holes 63-469 and 63-471

description: Formula basis = 6 oxygens.
DOI: 10.21227/s9rj-af80
title: Acoustic Holograms Dataset

description: To address the issue of insufficient real training data for acoustic holography, the Angular Spectrum Method (ASM) was used to synthesize an adequate amount of training data. This involved simulating a set of phase information on the holographic plane to provide ample training material for deep learning. During the training process, a custom learning rate scheduler was specifically employed to optimize the neural network's weight parameters, facilitating faster learning and enhancing network performance. This section also provides a detailed introduction to the deep learning approach of the IU-Net architecture, which is designed to more effectively process acoustic data and improve the quality of acoustic hologram reconstruction.
DOI: 10.6084/m9.figshare.26342119.v1
title: Supplementary Material for: Delivery Room Handling of the Newborn. Filling the Gaps

description: Background
Newborn resuscitation algorithms have since the turn of the century been more evidence-based. In this review, we discuss the development of American Heart Association (AHA) and the International Liaison Committee on Resuscitation (ILCOR)’s algorithm for newborn resuscitation from 1992-2024. We have also aimed to identify the remaining gaps in non-evidenced practice.
Summary
Of the 22 procedures reviewed in the 2020 ILCOR recommendations, the evidence was either low, very low, or non-existing. The strength of recommendation is weak or non-existing for most topics discussed. Several knowledge gaps are also summarized. The special challenge for low and middle income countries (LMIC) is discussed specifically.
Key messages
Newborn resuscitation is still not evidence-based although great progress has been achieved the recent years. We have identified several knowledge gaps which should be prioritized in future research. The challenge of obtaining evidence-based knowledge from LMIC should be focused on in future research.
DOI: 10.1594/pangaea.787101
title: (Table T1) Porosity and permeability of samples from ODP Leg 180 sites

description: Woodlark Basin, an area of continental extension, is an ideal location to study the evolution of permeability and the development of overpressures within an active rift basin. In this investigation, we measured sediment permeabilities of cores from Woodlark Basin and used numerical modeling to determine if pore fluid overpressures are likely at the base of the rift basin. Constant-rate flow tests were conducted on cores from Site 1108, located in the rift basin, and Sites 1115 and 1118, located on the northern margin of the basin. Results of the laboratory tests indicated permeabilities that range from 1.5 x 10**-18 to 1 x 10**-16 m**2. Results of the numerical modeling of Site 1108 suggest that overpressures due to sedimentation are unlikely.
description: Sediment depth is given in mbsf. Please note that depth of sample 180-1118A-56R (denoted as 180-1118C-56R in the article) might be wrong.
description: Supplement to: Kemerer, Amy; Screaton, Elizabeth J (2001): Permeabilities of sediments from Woodlark Basin: implications for pore pressures. In: Huchon, P; Taylor, B; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 180, 1-14
DOI: 10.1594/pangaea.785273
title: (Table 3) Total phosphorus concentration of sediment cores from Neustadt lagoon, north Germany
DOI: 10.1594/pangaea.903253
title: Calcareous nannofossils absolute abundance and accumulation rates from sediment core HTM-102, France
DOI: 10.1594/pangaea.726959
title: (Table 2) Corrected ages of sediment core V23-81
DOI: 10.1594/pangaea.903049
title: Calcareous nannofossils absolute abundance and accumulation rates from L'Arboudeysse, France
DOI: 10.15468/dl.4pjm4f
title: Occurrence Download

description: A dataset containing 1092 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is one of (China, Chinese Taipei)",
 "TaxonKey is Vaccinium mandarinorum Diels"
 ]
}

 The dataset includes 1092 records from 36 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031400-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.726983
title: (Table 2) Occurrence of sapropels
DOI: 10.1594/pangaea.819109
title: (Supplement 2) Phytoplankton concentrations in water samples obtained during R/V Natsushima (JAMSTEC) cruise to the Kuroshio Extension Front in October 2009
DOI: 10.1594/pangaea.721805
title: (Table DR1) Trace element concentrations in zircons from ODP Hole 147-894G
DOI: 10.1594/pangaea.717996
title: Radiosonde measurements from station Boulder, SURFRAD (2006-05)

description: Start location: Denver, CO; Distance from radiation site: 40 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.782438
title: (Appendix) Calcium carbonate content in OD Hole 130-806B

description: Geochemical well logs were obtained in sediment at Sites 805 and 806 of Ocean Drilling Program Leg 130. Corrections have been applied to the logs to account for variations in bore-hole size, drilling-fluid composition, and drill-pipe attenuation. Oxide and calcium carbonate weight percentages were calculated from the logs and are compared with available carbonate measurements from core. Log-derived CaCO3 values from Hole 805C, though lower than shipboard CaCO3 core measurements, show a similar variation in character. In Hole 806B, log and shipboard CaCO3 sample values have a similar mean and variance. The CaCO3 high-resolution sample values from Hole 806B, however, have a similar mean but a lower variance than the CaCO3 logs. It is probable that discrepancies result from gamma-ray spectrometry tool malfunctions experienced throughout the logging operations of this leg as well as from chlorine-induced interference in the calcium yield. Because the amplitude of CaCO3 variations was extremely low (standard deviation of 1.38 on high-resolution samples), the tool, which has a sensitivity of roughly 2% for Ca, probably would not have been able to detect these variations, even if the tool had been working properly.
description: Supplement to: Pratson, Elizabeth Lewis; Lyle, Mitchell W; Tivy, Jennifer (1993): Data report: Geochemical well logs through Cenozoic sediments from Sites 805 and 806. In: Berger, WH; Kroenke, LW; Mayer, LA; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 130, 775-788
DOI: 10.1594/pangaea.821677
title: Physical oceanography from CTDs during Professor Multanovskiy cruise E90CT