cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.2q7m5n
title: Occurrence Download

description: A dataset containing 1832 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Callionymidae",
 "Geometry POLYGON((170 20, 170 50, 120 50, 120 20, 170 20))",
 "HasCoordinate is true"
 ]
}

 The dataset includes 1832 records from 59 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0021043-241107131044228/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.qwj2x9
title: Occurrence Download

description: A dataset containing 8819450 species occurrences available in GBIF matching the query:
{
 "and" : [
 "OccurrenceStatus is Present",
 "TaxonKey is Anura"
 ]
}

 The dataset includes 8819450 records from 7225 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0021031-241107131044228/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.26639938.v1
title: Additional file 12 of The evolution of NLRC3 subfamily genes in Sebastidae teleost fishes

description: Supplementary Material 12
DOI: 10.6084/m9.figshare.26639941
title: Additional file 13 of The evolution of NLRC3 subfamily genes in Sebastidae teleost fishes

description: Supplementary Material 13
DOI: 10.6084/m9.figshare.26639941.v1
title: Additional file 13 of The evolution of NLRC3 subfamily genes in Sebastidae teleost fishes

description: Supplementary Material 13
DOI: 10.6084/m9.figshare.26639944
title: Additional file 14 of The evolution of NLRC3 subfamily genes in Sebastidae teleost fishes

description: Supplementary Material 14
DOI: 10.6084/m9.figshare.26639944.v1
title: Additional file 14 of The evolution of NLRC3 subfamily genes in Sebastidae teleost fishes

description: Supplementary Material 14
DOI: 10.6084/m9.figshare.24564069
title: Additional file 1 of Protein language models can capture protein quaternary state

description: Additional file 1: Supplementary Table SI:  Embeddings.
DOI: 10.6084/m9.figshare.24564069.v1
title: Additional file 1 of Protein language models can capture protein quaternary state

description: Additional file 1: Supplementary Table SI:  Embeddings.
DOI: 10.6084/m9.figshare.24564257
title: Additional file 2 of Protein language models can capture protein quaternary state

description: Additional file 2: Supplementary Table SII:  Model Results.
DOI: 10.6084/m9.figshare.24564257.v1
title: Additional file 2 of Protein language models can capture protein quaternary state

description: Additional file 2: Supplementary Table SII:  Model Results.
DOI: 10.6084/m9.figshare.24564264
title: Additional file 2 of Protecting healthcare workers and patients during the COVID-19 pandemic: a comparison of baseline and follow-up infection prevention and control needs in Nigerian military healthcare facilities delivering HIV services

description: Supplementary Material 2
DOI: 10.6084/m9.figshare.24564264.v1
title: Additional file 2 of Protecting healthcare workers and patients during the COVID-19 pandemic: a comparison of baseline and follow-up infection prevention and control needs in Nigerian military healthcare facilities delivering HIV services

description: Supplementary Material 2
DOI: 10.6084/m9.figshare.24564267
title: Additional file 2 of A novel hypoxia-associated gene signature for prognosis prediction in head and neck squamous cell carcinoma

description: Additional file 2. Details of patients in the TCGA database.
DOI: 10.6084/m9.figshare.24564267.v1
title: Additional file 2 of A novel hypoxia-associated gene signature for prognosis prediction in head and neck squamous cell carcinoma

description: Additional file 2. Details of patients in the TCGA database.
DOI: 10.6084/m9.figshare.24406628
title: Additional file 1 of Hepatozoon spp. infection in wild canids in the eastern United States

description: Additional file 1: Table S1. List of species, capture locality and PCR results. Number of cysts listed for positive cases with available histopathology.
DOI: 10.6084/m9.figshare.26628691
title: Additional file 5 of Percutaneous transvenous coil embolization (PTCE) for treatment of single extrahepatic portosystemic shunt in dogs

description: Additional file 5: Supplementary Table. Diameter of shunt vessel and number and type of implanted coils.
DOI: 10.15468/dl.wjbkja
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "POLYGON ((148.758025 -33.930063, 148.758025 -33.932309, 148.764762 -33.932309, 148.764762 -33.930063, 148.758025 -33.930063))"
 ]
}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069974-240626123714530/datasets/export for details.
DOI: 10.6084/m9.figshare.26628691.v1
title: Additional file 5 of Percutaneous transvenous coil embolization (PTCE) for treatment of single extrahepatic portosystemic shunt in dogs

description: Additional file 5: Supplementary Table. Diameter of shunt vessel and number and type of implanted coils.
DOI: 10.1594/pangaea.719614
title: (Table 2) Chemical composition of basalts from the DSDP Leg 74 Walvis Ridge transect

description: Five sites were drilled along a transect of the Walvis Ridge. The basement rocks range in age from 69 to 71 m.y., and the deeper sites are slightly younger, in agreement with the sea-floor-spreading magnetic lineations. Geophysical and petrological evidence indicates that the Walvis Ridge was formed at a mid-ocean ridge at anomalously shallow elevations. The basement complex, associated with the relatively smooth acoustic basement in the area, consists of pillowed basalt and massive flows alternating with nannofossil chalk and limestone that contain a significant volcanogenic component. Basalts are quartz tholeiites at the ridge crest and olivine tholeiites downslope. The sediment sections are dominated by carbonate oozes and chalks with volcanogenic material common in the lower parts of the sediment columns. The volcanogenic sediments probably were derived from sources on the Walvis Ridge. Paleodepth estimates based on the benthic fauna are consistent with a normal crustal-cooling rate of subsidence of the Walvis Ridge. The shoalest site in the transect sank below sea level in the late Paleocene, and benthic fauna suggest a rapid sea-level lowering in the mid-Oligocene. Average accumulation rates during the Cenozoic indicate three peaks in the rate of supply of carbonate to the sea floor, that is, early Pliocene, late middle Miocene, and late Paleocene to early Eocene. Carbonate accumulation rates for the rest of the Cenozoic averaged 1 g/cm**2/kyr. Dissolution had a marked effect on sediment accumulation in the deeper sites, particularly during the late Miocene, Oligocene, and middle to late Eocene. Changes in the rates of accumulation as a function of depth demonstrate that the upper part of the water column had a greater degree of undersaturation with respect to carbonate during times of high productivity. Even when the calcium carbonate compensation depth (CCD) was below 4400 m, a significant amount of carbonate was dissolved at the shallower sites. The flora and fauna of the Walvis Ridge are temperate in nature. Warmer-water faunas are found in the uppermost Maastrichtian and lower Eocene sediments, with cooler-water faunas present in the lower Paleocene, Oligocene, and middle Miocene. The boreal elements of the lower Pliocene are replaced by more temperate forms in the middle Pliocene. The Cretaceous-Tertiary boundary was recovered in four sites drilled, with the sediments containing well-preserved nannofossils but poorly preserved foraminifera.
DOI: 10.5281/zenodo.13327274
title: Model data for "Melt sensitivity of irreversible retreat of Pine Island Glacier"

description: Model inputs and outputs for the experiments in Reed et al., 2024 "Melt sensitivity of irreversible retreat of Pine Island Glacier".
DOI: 10.6084/m9.figshare.26640121
title: Additional file 6 of The effects of eating frequency on changes in body composition and cardiometabolic health in adults: a systematic review with meta-analysis of randomized trials

description: Additional file 6. Long Data Extraction.
DOI: 10.6084/m9.figshare.26640121.v1
title: Additional file 6 of The effects of eating frequency on changes in body composition and cardiometabolic health in adults: a systematic review with meta-analysis of randomized trials

description: Additional file 6. Long Data Extraction.
DOI: 10.1594/pangaea.711214
title: (Table 2) Calcium isotopic composition of Globigerinoides sacculifer from ODP Site 154-925
DOI: 10.1594/pangaea.704749
title: (Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structurally bound (SBC) fractions of chloride component in serpentinized ultramafic rocks from DSDP Site 566

description: Fractionation was determined using the average value where several values are presented.
DOI: 10.1594/pangaea.746638
title: Magnetostratigraphy of ODP Leg 108 sites

description: This paper presents the magnetostratigraphic results from Leg 108 of the Ocean Drilling Program. Measurements made with the shipboard "pass-through" cryogenic magnetometer on whole cores and archive halves are combined with those made on discrete samples; these measurements constitute the paleomagnetic data base for the Leg 108 cores. Polarity determination on unoriented, low-latitude cores is somewhat subjective; we rely heavily on the available biostratigraphic data and document our line of reasoning where appropriate. The interpretations presented here, therefore, are compatible with the available biostratigraphic information; they are also in substantial agreement with orientation information where available.
description: Supplement to: Tauxe, Lisa; Valet, Jean-Pierre; Bloemendal, Jan (1989): Magnetostratigraphy of Leg 108 advanced hydraulic piston cores. In: Ruddiman, W; Sarnthein, M; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 108, 429-439
DOI: 10.1594/pangaea.789398
title: Organic carbon, calcium carbonate and carbon/nitrogen ratio at DSDP Leg 93 sites

description: A large number of samples of nonlithified and lithified sediments from Leg 93 sites were analyzed for their contents of organic carbon and calcium carbonate. An average of two samples was selected from every core for carbonate determination; organic carbon was measured in most of these samples. Nearly all of these analyses were performed on board Glomar Challenger for samples from Sites 603 and 604. Site 605 samples, plus some of the deeper samples from Hole 603B, were analyzed at the University of Michigan. The procedures used in both cases were virtually the same, and their results compared well. Organic carbon analyses were done using a Hewlett- Packard 185-B CHN Analyzer. Portions of samples selected for calcium carbonate determinations were treated with dilute HC1 to remove carbonate, washed with deionized water, and dried at 110°C. A Cahn Electrobalance was used to weight 20-mg samples of sediment for CHN analysis. Samples were combusted at 1050°C in the presence of an oxidant, and the volumes of the evolved gases determined as measures of the C, H, and N contents of sediment organic matter. Areas of gas peaks were determined and compared to those of rock standards of known carbon and nitrogen contents. These values were used to standardize instrument response so that C/N atomic ratios could be reported. Organic carbon concentrations were calculated on the basis of sediment dry weight. Hydrogen elemental analysis with the procedure used is untrustworthy because of the variable amounts of clay minerals and their hydrates, hence hydrogen values are not reported for samples analyzed by this method.
description: Supplement to: Meyers, Philip A (1987): Appendix II. Organic carbon and calcium carbonate analyses, Deep Sea Drilling Project Leg 93, North American continental rise. In: van Hinte, JE; Wise, SW Jr; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 93, 465-469
DOI: 10.1594/pangaea.261499
title: Paleomagnetic and rock magnetic measurements of igneous and metamorphic rocks of Hole 82-559
DOI: 10.1594/pangaea.263347
title: Minor-element chemical analyses of Hole 17-165A
DOI: 10.1594/pangaea.897976
title: Physical oceanography during PELAGIA cruise PE278

description: Temperature, salinity and oxygen data measured by CTD on the Pelagia cruise PE278.Note: Oxygen is only available for stations 0-5. Chief Scientist: Dagmar Kieke Region: Subpolar Northeastern AtlanticInstrument: SBE 9 plus CTD, SBE 11 plus deck unit, SBE 43 dissolved oxygen sensor
DOI: 10.6084/m9.figshare.26630644
title: Additional file 5 of Transcriptome driven discovery of novel candidate genes for human neurological disorders in the telomer-to-telomer genome assembly era

description: Additional file 5. Differential expression results for novel genes discovered in the analyses of neurological disorders.
DOI: 10.6084/m9.figshare.24564278
title: Additional file 2 of Multi-center, pragmatic, cluster-randomized, controlled trial of standardized peritoneal dialysis (PD) training versus usual care on PD-related infections (the TEACH-PD trial): trial protocol

description: Additional file 2. Funding documents.
DOI: 10.6084/m9.figshare.24564278.v1
title: Additional file 2 of Multi-center, pragmatic, cluster-randomized, controlled trial of standardized peritoneal dialysis (PD) training versus usual care on PD-related infections (the TEACH-PD trial): trial protocol

description: Additional file 2. Funding documents.
DOI: 10.6084/m9.figshare.26630632.v1
title: Additional file 1 of Transcriptome driven discovery of novel candidate genes for human neurological disorders in the telomer-to-telomer genome assembly era

description: Additional file 1. Complete information on the RNAseq studies used for analyses.
DOI: 10.1594/pangaea.788019
title: (Table T2) Diatom biostratigraphy of ODP Core 172-1063D-2H

description: Sediment depth is given in mbsf. Abundance estimate as follows: A = abundant, C = common, F = frequent, R = rare, X = scarce, B = barren, - = not found.
DOI: 10.1594/pangaea.819850
title: Compilation of respiration rate data for marine pelagic organisms

description: The metabolic rate of organisms may either be viewed as a basic property from which other vital rates and many ecological patterns emerge and that follows a universal allometric mass scaling law; or it may be considered a property of the organism that emerges as a result of the organism's adaptation to the environment, with consequently less universal mass scaling properties. Data on body mass, maximum ingestion and clearance rates, respiration rates and maximum growth rates of animals living in the ocean epipelagic were compiled from the literature, mainly from original papers but also from previous compilations by other authors. Data were read from tables or digitized from graphs. Only measurements made on individuals of know size, or groups of individuals of similar and known size were included. We show that clearance and respiration rates have life-form-dependent allometries that have similar scaling but different elevations, such that the mass-specific rates converge on a rather narrow size-independent range. In contrast, ingestion and growth rates follow a near-universal taxa-independent ~3/4 mass scaling power law. We argue that the declining mass-specific clearance rates with size within taxa is related to the inherent decrease in feeding efficiency of any particular feeding mode. The transitions between feeding mode and simultaneous transitions in clearance and respiration rates may then represent adaptations to the food environment and be the result of the optimization of tradeoffs that allow sufficient feeding and growth rates to balance mortality.
DOI: 10.15468/dl.gr3u9m
title: Occurrence Download

description: A dataset containing 519 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Thrips palmi Karny, 1925"
 ]
}

 The dataset includes 519 records from 14 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069975-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.720146
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 30-286

description: Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline quartzP = Plagioclase feldsparK = Potassium feldsparLvo = Other volcanic lithicLvd = Devitrified vitric volcanic lithicLvv = Vitric volcanic lithicLvf = Volcanic lithic with felsitic textureLvmi = Volcanic lithic with microlitic textureLvl = Volcanic lithic with lathwork textureLvp = Pyroclastic volcanic lithicLmv = Metavolcanic lithicLmm = Polycrystalline mica lithicLmt = Quartz-mica tectonite lithicLma = Quartz-feldspar-mica aggregate lithicLmp = Phyllite lithicLsa = Argillite-shale lithicLsc = Sedimentary carbonate lithicLsch = sedimentary chert or cherty argillite lithicLsi = Siltstone sedimentary lithicM = Phyllosilicate mineralsD = Dense mineralsCarb = Carbonate mineralsBio = Bioclastic debris (siliceous and/or carbonate)Misc = Miscellaneous and unidentifiedQ = Total quartzose grainsL = Unstable lithic grainsLm = Metamorphic lithic grainsLv = Volcanic-hypabyssal (and volcaniclastic) lithic grainsLs = Sedimentary lithic grainsLvm = Volcanic-hypabyssal and metavolcanic lithic grainsLsm = Sedimentary and metasedimentary lithic grainsLst = Sedimentary and polycrystalline quartz grainsF = Total feldspar grainsQp = Polycrystalline quartz grainsQ = Qm + Qpw + QptQp = Qpw + QptL = Lm + Lv + LsLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpLm = Lmv + Lmm + Lmt + LmaLsm = Ls + Lmm + Lmt + LmaLvc = Lvf + Lvmi + LvlLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpF = P + KLs = Lsa + LscLvm = Lv + LmvLst = Ls + QpQFL%Q = 100Q/(Q + F + L)QFL%F = 100F/(Q + F + L)QFL%L = 100L/(Q + F + L)QmKP%Qm = 100Qm/(Qm + P + K)QmKP%P = 100P/(Qm + P + K)QmKP%K = 100K/(Qm + P + K)LvfLvmiLvl%Lvf = 100Lvf/LvcLvfLvmiLvl%Lvmi = 100Lmi/LvcLmLvLs%Lm = 100Lm/LLmLvLs%Lv = 100Lv/LLmLvLs%Ls = 100Ls/LQpLvmLsm%Qp = 100Qp/(L + Qp)QpLvmLsm%Lvm = 100Lvm/(L + Qp)QpLvmLsm%Lsm = 100Lsm/(L + Qp)LvfLvmiLvl%Lvl = 100Lvl/Lvc
DOI: 10.1594/pangaea.882144
title: Physical oceanography on section MVP_2015001_03 during CCGS Amundsen cruise MVP_2015001
DOI: 10.1594/pangaea.831741
title: Shipboard natural gamma radiation on the modified composite splice of IODP Site 303-U1308

description: DEPTH, sediment/rock [m] is given in mcd.
DOI: 10.1594/pangaea.835085
title: Maximum ingestion and maximum clearance rate of Cyclosalpa bakeri determined experimentally
DOI: 10.1594/pangaea.97070
title: Sedimentation rates of Hole 44-390

description: compiled and calculated from various DSDP data sources
DOI: 10.1594/pangaea.693949
title: Trawlings during NOVOUKRAINKA cruise NOV3, Part II

description: The fish catches were carried out by the industrial midwater non-closed trawl. There was a small-mesh section with minimum mesh size of 6.5 mm in the trawl bag. Vertical opening of the trawl made from 26 to 50 m. The trawling made 30 min up to 2 hour and 30 min. Speed of trawling made 3.2-4.2 knots. The catches horizons were determined by the state of sound-scattering layers and fish schools. At night they carried out catches usually in the upper 0-550 m layer. At the day time they trawled at a range of 60-490 m depths. Each catch was weighted. Fish was determined up to the lowest taxonomic ranks - species, in some cases - genus. Total number and mass of each species in a catch, and average dry mass of one specimen of a species were determined. The standard fish body length (SL) was measured in mm (from the tip of snout to the basement of the middle rays of the caudal fin). The samples were fixed in 10% buffered formaldehyde for further processing in the IBSS laboratories.
DOI: 10.6084/m9.figshare.24564080
title: Additional file 1 of Unraveling the genetic basis of grain number-related traits in a wheat-Agropyron cristatum introgressed line through high-resolution linkage mapping

description: Additional file 1: Table S1. Marker sequences for map construction and marker-assisted selection.
DOI: 10.6084/m9.figshare.24564080.v1
title: Additional file 1 of Unraveling the genetic basis of grain number-related traits in a wheat-Agropyron cristatum introgressed line through high-resolution linkage mapping

description: Additional file 1: Table S1. Marker sequences for map construction and marker-assisted selection.
DOI: 10.6084/m9.figshare.24564281
title: Additional file 2 of Unraveling the genetic basis of grain number-related traits in a wheat-Agropyron cristatum introgressed line through high-resolution linkage mapping

description: Additional file 2: Table S2. Analysis of variance (ANOVA), the heritability (hB2), and average phenotypic performance for the investigated traits of the recombinant inbred lines (RILs) and their parents in seven environments.
DOI: 10.6084/m9.figshare.24564281.v1
title: Additional file 2 of Unraveling the genetic basis of grain number-related traits in a wheat-Agropyron cristatum introgressed line through high-resolution linkage mapping

description: Additional file 2: Table S2. Analysis of variance (ANOVA), the heritability (hB2), and average phenotypic performance for the investigated traits of the recombinant inbred lines (RILs) and their parents in seven environments.
DOI: 10.1594/pangaea.804665
title: (Table 1) Chemisity of interstitial water at DSDP Leg 66 holes

description: During Leg 66, a transect was drilled across the Middle America Trench off Mexico. In this report, interstitial water analyses for Sites 487 (on oceanic crust), 490, 491, and 492 (continental slope apron), and 493 (upper continental slope) are presented. All sites are characterized by high sedimentation rates, and as a result sulfate reduction and methane generation processes are very important. At Sites 490 through 492 decreases in chlorinity are evidence of the presence of gas hydrates. At Site 493 a sharp increase in dissolved calcium and the complete depletion of dissolved magnesium just above basement indicate that weathering of continental crust is still an ongoing process.
description: DEPTH, sediment [m] is given in mbsf.
description: Supplement to: Gieskes, Joris M; Johnston, Kirk; Boehm, Marcus (1985): Appendix: Interstitial water studies, Leg 66. In: von Heune, R; Aubouin, J; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 84, 961-967
DOI: 10.6084/m9.figshare.26640145
title: Additional file 3 of Unraveling the genetic basis of grain number-related traits in a wheat-Agropyron cristatum introgressed line through high-resolution linkage mapping

description: Additional file 3: Table S3. Summary of unconditional and conditional QTLs for GNS and its component traits.
DOI: 10.6084/m9.figshare.26640145.v1
title: Additional file 3 of Unraveling the genetic basis of grain number-related traits in a wheat-Agropyron cristatum introgressed line through high-resolution linkage mapping

description: Additional file 3: Table S3. Summary of unconditional and conditional QTLs for GNS and its component traits.
DOI: 10.6084/m9.figshare.26640148
title: Additional file 4 of Unraveling the genetic basis of grain number-related traits in a wheat-Agropyron cristatum introgressed line through high-resolution linkage mapping

description: Additional file 4: Table S4. The correlation coefficients between GNS|GNSL, GNS|TSS, GNS|FSS (conditional traits) and GNSL, TSS, FSS (unconditional traits).