cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.812220
title: Chemostratigraphy (CaCO3, TOC, δ¹³Corg) of Sinemurian black shales

description: The Shales-with-'Beef' and Black Ven Marls of the Charmouth Mudstone Formation (Sinemurian) exposed on the Dorset Coast in southern England (Wessex Basin) show stratigraphic variation in carbonate, organic carbon and organic-carbon isotopes. Little environmental significance is attached to the variation of carbonate except in the case of the tabular and nodular limestones interrupting the sequence that probably record stratigraphic condensation and/or sedimentary stillstands that, in an extreme case, were accompanied by sea-floor erosion to produce the bored and encrusted 'Coinstone'. Relatively high total organiccarbon (TOC) contents are present in the laminated mudstones of the lower turneri Zone (upper brooki and lower birch Subzones) and the obtusum Zone (obtusum and stellare Subzones). Basin stratification related to fresh-water influx was the most likely aid to deoxygenation and enhanced preservation of organic matter. The organic-carbon isotope curve (d13Corg), which shows positive excursions in the upper turneri Zone (upper birchi Subzone) and highest obtusum - raricostatum Zones (highest stellare Subzone, densinodulum and lower raricostatoides Subzones), does not correlate with the TOC stratigraphy and was clearly not controlled by local patterns of organic-matter burial. Long-term (hundreds-of-thousands of years) variations in the carbon-isotope (d13Corg) curve are interpreted as reflecting changing seawater isotopic composition and, in the case of the stratigraphically higher interval, may be related to marine organic-carbon burial on the margins of the proto-Atlantic, as exemplified by the Lusitanian Basin in Portugal. Correlation of the carbon-isotope profile with putative sea-level curves is problematic in detail, although significant local transgressive pulses in the turneri and late raricostatum Zones are approximately coincident with positive d13Corg excursions.
description: Black Ven Marls - samples below Stonebarrow = BVM+206 to BVM-156, below Black Ven = BVM-157 to SWB0. Note gap in sampling between BVM-247 and SWB+38 treated as 10 cm.
description: Supplement to: Jenkyns, Hugh C; Weedon, Graham P (2013): Chemostratigraphy (CaCO3, TOC, d13Corg) of Sinemurian (Lower Jurassic) black shales from the Wessex Basin, Dorset and palaeoenvironmental implications. Newsletters on Stratigraphy, 46(1), 1-21
DOI: 10.1594/pangaea.815883
title: (Appendix A) Paleomagnetic of IODP Site 303-U1305

description: Integrated Ocean Drilling Program (IODP) Expedition 303 to the North Atlantic in 2004 recovered rapidly deposited deep-sea sediments at IODP Site U1305 on Eirik Drift, located south of Greenland at 3460 m water depth, along the path of the Western Boundary Under Current (WBUC). About 200 m of sediment was sampled with u-channels from the composite section, providing a continuous record of paleomagnetic field directions and relative paleointensity (RPI) variations covering the past 1.2 Myr. The age model, based on an oxygen isotope record, is consistent with the fit of the RPI record to a calibrated template, and indicates higher sedimentation rates during interglacials relative to glacial epochs. Magnetite grain-size and concentration proxies indicate higher concentrations of magnetite with larger grain sizes during interglacials. Enhanced interglacial deposition can be attributed to a combination of elevated entrainment of terrigenous detritus into the WBUC due to glacial retreat on continents flanking the upstream path of the WBUC (east Greenland and Iceland), and of increased bottom current (WBUC) vigor leading to elevated transport and deposition at the site during interglacials. This pattern is opposite to observations of flow of the Antarctic circum polar current (ACC) in the south Indian Ocean, which suggests an inter-hemispheric antiphase in marine circulation at the Milankovitch scale, with strong circulation in the deep North Atlantic when the ACC is weak, and vice versa.
description: Sediment depth is given in mcd.
description: Supplement to: Mazaud, Alain; Channell, James E T; Stoner, Joseph S (2012): Relative paleointensity and environmental magnetism since 1.2Ma at IODP site U1305 (Eirik Drift, NW Atlantic). Earth and Planetary Science Letters, 357-358, 137-144
DOI: 10.1594/pangaea.808911
title: Calcium/Strontium ratio at IODP Site U1302-U1303
DOI: 10.1594/pangaea.808912
title: Stable oxygen isotope ratio on N. pachyderma at IODP Site U1302-U1303
DOI: 10.1594/pangaea.808913
title: Declination at IODP Site U1302-U1303
DOI: 10.1594/pangaea.808914
title: GRAPE density at IODP Site U1302-U1303
DOI: 10.1594/pangaea.808915
title: Hysteresis values at IODP Site U1302-U1303
DOI: 10.1594/pangaea.808916
title: Inclination at IODP Site U1302-U1303
DOI: 10.1594/pangaea.808917
title: Susceptibility at IODP Site U1302-U1303
DOI: 10.1594/pangaea.808918
title: Maximum angular deviation at IODP Site U1302-U1303
DOI: 10.1594/pangaea.808919
title: Age model of IODP Site U1302-U1303
DOI: 10.1594/pangaea.808920
title: Paleointensity of IODP Site U1302-U1303
DOI: 10.1594/pangaea.808921
title: Silicon/Strontium ratio of IODP Site U1302-U1303
DOI: 10.1594/pangaea.832891
title: Physical oceanography during Walther Herwig III cruise WH372
DOI: 10.1594/pangaea.829067
title: Groundfish survey data from the German Bight from 1902-08, 1919-23, and 1930-1932 and ICES International Bottom Trawl Survey (IBTS) quarter 3 data from 1991 to 2009

description: Groundfish survey data from the German Bight from 1902-08, 1919-23, and 1930-1932 and ICES International Bottom Trawl Survey (IBTS) quarter 3 data from 1991 to 2009 were analysed with respect to species frequencies, maximum length, trends in catch-per-unit-effort, species richness parameters (SNR) and presence of large fish (Phi40), the latter defined as average presence of species per haul with specimens larger than 40 cm given. Four different periods are distinguished: (a) before 1914 with medium commercial CPUE and low landings, Phi40 approx. 2, high abundance in elasmobranchs and SNR conditions indicating highly diverse assemblages, (b) conditions immediately after 1918 with higher commercial CPUE, recovering landings, Phi40 at &gt; 4 in 1919, and SNR conditions indicating highly diverse assemblages, (c) conditions from 1920 to the early 1930's with decreasing commercial CPUE, increased landings, decreasing Phi40, SNR conditions similar to later years indicating less diverse assemblages, and a decrease in elasmobranchs. In the IBTS series (d), Phi40 remains low indicating an increased rarity of large specimens, and SNR characteristics are similar to the third period. Dab, whiting and grey gurnard have increased considerably in the IBTS series as compared to the historic data. Phi40 is suggested an alternative indicator reflecting community functional diversity when weight based indicators cannot be applied.
description: Supplement to: Fock, Heino O; Kloppmann, Matthias H F; Probst, Wolfgang Nikolaus (2014): An early footprint of fisheries: Changes for a demersal fish assemblage in the German Bight from 1902–1932 to 1991–2009. Journal of Sea Research, 85, 325-335
DOI: 10.1594/pangaea.860274
title: Airborne remote sensing spectral measurements in the short-wave infrared using MAMAP during POLAR 5 flight AIRMETH_11060301
DOI: 10.1594/pangaea.856640
title: Nd and Sm content and isotopic composition of the carbonate-free clay fraction of sediment core HU90-013-013

description: Sm-Nd concentrations and Nd isotopes were investigated in the fine fraction of two Labrador Sea cores to reconstruct the deep circulation patterns through changes in sedimentary supply since the last glacial stage. Three sources are involved: the North American Shield, Palaeozoic rocks from northeastern Greenland, and mid-Atlantic volcanism. The variable input of these sources provides constraints on the relative sedimentary supply, in conjunction with inception of deep currents. During the last glacial stage a persistent but sluggish current occurred inside the Labrador Basin. An increasing discharge of volcanic material driven by the North East Atlantic Deep Water is documented since 14.3 kyr, signaling the setup of a modern-like deep circulation pattern throughout the Labrador, Irminger, and Iceland basins. During the last deglacial stage the isotopic record was punctually influenced by erosion processes related mainly to ice-sheet instabilities, especially 11.4, 10.2, and 9.2 kyr ago.
description: Model ages have been calculated relative to the present Depleted Mantle (147Sm/144Nd = 0.222, 143Nd/144Nd = 0.513114), assuming a one-stage, linear evolution for the Depleted Mantle (Ben Othman et al., 1984). Chondritic Undifferenciated Reservoir (CHUR) parameters are 147Sm/144Nd = 0.1967 (Jacobsen and Wasserburg, 1980), and 143Nd/144Nd = 0.512638 (Wasserburg et al., 1981). Errors on the 143Nd/144Nd ratios are given as 2 sigma. The accuracy of 147Sm/144Nd ratios is better than 2%. Measured Accelerator Mass Spectrometry (AMS) 14C ages (i.e., values in brackets) are normalized to PDB and corrected by -400 years for reservoir effect (Hillaire-Marcel et al., 1994). Ages reported for each sample depth were estimated by direct linear interpolation of available AMS14C ages (Hillaire-Marcel et al., 1994), assuming a constant sedimentation rate. Then these interpolated ages were calibrated using the curve of Stoner et al. (1998). Data for the surface sample 90-013- 017, for which age is estimated at 0, is taken from Innocent et al. (1997).
description: Supplement to: Fagel, Nathalie; Innocent, Christophe; Stevenson, Ross K; Hillaire-Marcel, Claude (1999): Deep circulation changes in the Labrador Sea since the Last Glacial Maximum: New constraints from Sm-Nd data on sediments. Paleoceanography, 14(6), 777-788
DOI: 10.1594/pangaea.833552
title: (Table 2) Radiocarbon and paleomagnetic secular variation tie points for sediment cores MD99-2269 and MD99-2322
DOI: 10.1594/pangaea.833554
title: (Table S1) Paleomagnetic declination and inclination for sediment core MD99-2269
DOI: 10.1594/pangaea.833555
title: (Table S1) Paleomagnetic declination and inclination for sediment core MD99-2322
DOI: 10.1594/pangaea.860275
title: GPS positions during POLAR 5 flight AIRMETH_11060301
DOI: 10.1594/pangaea.860276
title: Airborne remote sensing spectral measurements in the short-wave infrared using MAMAP during POLAR 5 flight AIRMETH_11060401
DOI: 10.1594/pangaea.860277
title: GPS positions during POLAR 5 flight AIRMETH_11060401
DOI: 10.1594/pangaea.862130
title: Physical oceanography during Walther Herwig III cruise WH392
DOI: 10.1594/pangaea.884280
title: Pollen analysis of ODP Site 202-1239
DOI: 10.1594/pangaea.896038
title: Concentrations of n-alkanes C29 and C31, δD nC29 and nC31 values, Artemisia and Chenopodiaceae pollen percentages and calcium carbonate spanning the Mid-Pleistocene Transition on depth and age scales for the SG-1 core
DOI: 10.1594/pangaea.895025
title: Ice-rafted debris weight percents and grains for IODP Site 303-U1307

description: Ice-rafted debris (IRD) data measured for discrete samples between ~117 and 158 revised metres composite depth (rMCD) at IODP Site U1307, Eirik Drift, offshore southern Greenland. Measurements consist of IRD weight percent (wt.%) in the ≥63 and ≥212 μm grain size fractions, and IRD grains per gram in the ≥125 and ≥150 μm grain size fractions. This data is provided against sample IDs, metres below seafloor (MBSF) depths, rMCD depths and age in thousands of years (ka). The time period covered by this dataset is ~2200 to 3200 ka, across the Plio-Pleistocene transition and the intensification of Northern Hemisphere glaciation.
DOI: 10.1594/pangaea.896039
title: Percentages of pollen taxa spanning the Mid-Pleistocene Transition on depth and age scales for the SG-1 core
DOI: 10.1594/pangaea.896133
title: Meteorological forcing data to run land surface models for five high latitude sites. Derived from reanalysis products combined with site observations

description: These data represent five high-latitude sites studied in the PAGE21 project (https://www.page21.eu): Samoylov, Kytalyk, Abisko, Zackenberg and Bayelva. Please see the linked manuscript for details of the sites. These are meteorological driving data, which were prepared using observations from the sites combined with reanalysis data for the grid cell containing the site. For the period 1901-1979, Water and Global Change forcing data (WFD) were used (Weedon et al., 2011). This has half-degree resolution for the whole globe at 3-hourly time resolution from 1901 to 2001. For the period 1979-2014, WATCH-ForcingData-ERA-Interim (WFDEI) was used (Weedon, 2013). For the time periods in which observed data were available, correction factors were generated by calculating monthly biases relative to the WFDEI data. These corrections were then applied to the time series from 1979 to 2014 of the WFDEI data. The WFD before 1979 were then corrected to match these data and the two datasets were joined at 1979 to provide gap-free 3-hourly forcing from 1901 to 2014. Local meteorological station observations were used for all variables except snowfall, which was estimated from the observed snow depth by treating increases in snow depth as snowfall events with an assumed snow density. See linked manuscript for more details.
description: Variables provided: *Air temperature *Specific humidity *Wind speed *Incoming shortwave radiation *Incoming longwave radiation *Surface pressure *Rainfall (both CRU and GPCC) (https://crudata.uea.ac.uk/cru/data/hrg/ ; https://climatedataguide.ucar.edu/climate-data/gpcc-global-precipitation-climatology-centre) *Snowfall (both CRU and GPCC) Both corrected and uncorrected precipitation variables are provided. The data that were used in the linked publication were "Snowf_GPCC_cor" and "Rainf_GPCC_cor".
description: Supplement to: Chadburn, Sarah; Krinner, Gerhard; Porada, Philipp; Bartsch, Annett; Beer, Christian; Belelli Marchesini, Luca; Boike, Julia; Ekici, Altug; Elberling, Bo; Friborg, Thomas; Hugelius, Gustaf; Johansson, Margareta; Kuhry, Peter; Kutzbach, Lars; Langer, Moritz; Lund, Magnus; Parmentier, Frans-Jan W; Peng, Shushi; van Huissteden, Jacobus (Ko); Wang, Tao; Westermann, Sebastian; Zhu, Dan; Burke, Eleanor J (2017): Carbon stocks and fluxes in the high latitudes: using site-level data to evaluate Earth system models. Biogeosciences, 14(22), 5143-5169
DOI: 10.1594/pangaea.896872
title: Magnetic susceptibility in the Blue Lias Formation from St Marys Well Bay, Lavernock, Glamorgan

description: -9999 = missing values, NA = Not applicable or not available.
DOI: 10.1594/pangaea.896874
title: Magnetic susceptibility in the Blue Lias Formation from Quantocks Head, Somerset

description: -9999 = missing values, NA = Not applicable or not available.
DOI: 10.1594/pangaea.896875
title: Magnetic susceptibility in the Blue Lias Formation from Southam Quarry, Warwickshire

description: -9999 = missing values, NA = Not applicable or not available.
DOI: 10.1594/pangaea.896876
title: Magnetic susceptibility in the Blue Lias Formation from St Audries Bay, Somerset

description: -9999 = missing values, NA = Not applicable or not available.
DOI: 10.1594/pangaea.896877
title: Magnetic susceptibility in the Blue Lias Formation from Pinhay Bay to West Cliff Lyme Regis, Dorset

description: -9999 = missing values, NA = Not applicable or not available.
DOI: 10.1594/pangaea.905331
title: Holocene temperature reconstructions for northeastern North America and the northwestern Atlantic, core Lower_Murray_Lake
DOI: 10.1594/pangaea.925262
title: Master track of HEINCKE cruise HE552 in 1 sec resolution (zipped, 2.2 MB)

description: Raw data acquired by position sensors on board RV Heincke during expedition HE552 were processed to receive a validated master track which can be used as reference of further expedition data. Position sensors used during HE552 were the internal navigation system IXSEA PHINS III and the GPS receivers Trimble Marine SPS461 and SAAB R5 SUPREME NAV. Data were downloaded from DAVIS SHIP data base (https://dship.awi.de) with a resolution of 1 sec. Processing and evaluation of the data is outlined in the data processing report found at EPIC repository hdl:10013/epic.e0df8912-61ee-4512-8de8-8c2210ba8a98. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
DOI: 10.15468/dl.7gn2cj
title: Occurrence Download

description: A dataset containing 868691 species occurrences available in GBIF matching the query:
{
 "and" : [
 "DatasetKey is iNaturalist Research-grade Observations",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "Country is one of (Canada, Mexico, United States of America)",
 "EventDate is greater than or equal to 2024-03-23",
 "EventDate is less than or equal to 2024-04-22",
 {
 "not" : {
 "Issue" : [
 "is one of (Basis of record invalid, Coordinate reprojection failed, Coordinate reprojection suspicious, Coordinate precision invalid, Coordinate uncertainty meters invalid, Country mismatch, Country invalid, Geodetic datum invalid, Presumed swapped coordinate, Presumed negated longitude, Presumed negated latitude, Country coordinate mismatch)"
 ]
 }
 }
 ]
}

 The dataset includes 868691 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0021996-240506114902167/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.pnfqyb
title: Occurrence Download

description: A dataset containing 1726 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is one of (Abarema abbottii (Rose & Leonard) Barneby & J.W.Grimes, Abarema acreana (J.F.Macbr.) L.Rico, Abarema adenophora (Ducke) Barneby & J.W.Grimes, Abarema alexandri (Urb.) Barneby & J.W.Grimes, Abarema asplenifolia (Griseb.) Barneby & J.W.Grimes, Abarema auriculata (Benth.) Barneby & J.W.Grimes, Abarema barbouriana (Standl.) Barneby & J.W.Grimes, Abarema barnebyana Iganci & M.P.Lima, Abarema brachystachya (DC.) Barneby & J.W.Grimes)"
 ]
}

 The dataset includes 1726 records from 132 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0022004-240506114902167/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.y8rem9
title: Occurrence Download

description: A dataset containing 23 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Peru",
 "TaxonKey is Hypanus Rafinesque, 1818"
 ]
}

 The dataset includes 23 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0022005-240506114902167/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.25853761
title: Supplementary Material for: Cytomegalovirus Retinitis in an Eye with Unilateral Retinoblastoma: A Case Report

description: Introduction
Cytomegalovirus (CMV) retinitis in the setting of pediatric retinoblastoma is exceedingly unusual. Here, we present the first reported case of CMV retinitis in an enucleated eye with retinoblastoma after chemotherapy in the western hemisphere.
Case Presentation
A two-year-old Hispanic male without a family history of retinoblastoma presented with a three-month history of right exotropia and right eye squinting. Clinical examination revealed dense white vitreous opacities in the right eye. Ocular oncology evaluation unveiled an exudative retinal detachment with vitreous seeds, subretinal seeding, and a tumor emanating from the retina in the superonasal quadrant of the right eye. The patient was diagnosed with unilateral Group D retinoblastoma and RB1 sequencing revealed a pathogenic variant with mosaicism. Treatment involved systemic chemotherapy, intravitreal chemotherapy, and cryotherapy. However, the patient developed a rhegmatogenous retinal detachment with diffuse vitreous hemorrhage and ultimately underwent right eye enucleation. Interestingly, histopathological analysis of the enucleated eye revealed concomitant CMV retinitis alongside retinoblastoma. After consultation with infectious disease, antiviral treatment was not initiated as the patient remained asymptomatic and maintained a recovered immune system. Repeat CMV PCR confirmed viral clearance. The patient received a prosthetic eye and continues to be monitored for retinoblastoma recurrence.
Conclusion 
Clinicians should be aware of the potential for CMV retinitis to develop in retinoblastoma patients receiving chemotherapy, which may complicate clinical decision making and management. Timely identification of CMV retinitis in this setting may improve patient ocular outcomes and overall prognosis.
DOI: 10.15468/dl.y5dv3x
title: Occurrence Download

description: A dataset containing 3 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Peru",
 "TaxonKey is Pteroplatytrygon violacea (Bonaparte, 1832)"
 ]
}

 The dataset includes 3 records from 3 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0022008-240506114902167/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.emqv2x
title: Occurrence Download

description: A dataset containing 7 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Peru",
 "TaxonKey is Echinorhinus cookei Pietschmann, 1928"
 ]
}

 The dataset includes 7 records from 3 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0022010-240506114902167/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.5281/zenodo.11209872
title: Supported data for manuscript NCOMMS-23-54335B: Microdroplets initiate organic-inorganic interactions and mass transfer in thermal hydrous geosystems
DOI: 10.5281/zenodo.11209873
title: Supported data for manuscript NCOMMS-23-54335B: Microdroplets initiate organic-inorganic interactions and mass transfer in thermal hydrous geosystems