cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.868478
title: (Table 1) Apatite fission track (AFT) and (U-Th-Sm)/He (AHe) data of the Eisenhower Range
DOI: 10.1594/pangaea.871862
title: (Table 1a) Age determination of an onshore sediment core from the Miaodao stratigraphic section (MDS) in the northwest region of the Miaodao Archipelago in the Bohai Sea
DOI: 10.1594/pangaea.873693
title: (Table1) AMS radiocarbon dates and calibrated ages of sediment core GeoB12605-3

description: based on Kuhnert et al.(2014).
DOI: 10.1594/pangaea.875722
title: Age determination of sediment core PS69/251-1 derived from 210Pb-dating
DOI: 10.1594/pangaea.875724
title: Age determination of sediment core PS75/160-1 derived from 1C AMS-dating
DOI: 10.1594/pangaea.840549
title: Age determination of sediment core MD99-2303
DOI: 10.1594/pangaea.871343
title: Table S27 - Magnetostratigraphy ODP Site 208-1263
DOI: 10.1594/pangaea.738404
title: (Table 2) Radiocarbon dates and age calibration

description: The high-energy, low-accumulation NW Iberian shelf features three confined Holocene mud depocentres. Here, we show that the evolution of such depocentres follows successive steps. The flooding of inner shelf zones and river catchment areas by the late deglacial sea-level rise provided the precondition for shelf mud deposition. Following this, the Holocene deceleration of the sea-level rise caused a rapid refill of the accommodation space within river valleys. Subsequently, the export of major amounts of fines was initiated. The initial onset and loci of shelf mud deposition were related to deposition-favouring conditions in mid-shelf position or to the presence of morphological highs, which act as sediment traps by providing protection against stronger hydrodynamic energy. The detailed reconstruction of the Holocene depocentre evolution shows for the first time that the expansion of such shelf mud deposits cannot only occur by linear growth off the associated sediment source. Rather, they might develop around centres that are fully disconnected from the source of original sediment supply, and expand later into specific directions. Based on these differences and on the connection of the individual mud depocentres to the material source we propose a conceptual subdivision of the group "mid-shelf mud depocentres".
description: Lab no: Radiocarbon laboratory: KIA = Leibniz Laboratory in Kiel (Germany); Poz = Poznan Radiocarbon Laboratory (Poland).Material: bF = benthic foraminifers; E. crispum = Elphidium crispum (monospecific sample); bv = bivalve; gp = gastropod.Age, minimum/young and Age, maximum/old: For reservoir correction, the conventional age of 400 years is applied using CALIB 5.0.1. (Stuiver et al., 1998).d: Age calibration is based on the function of Bard et al. (1998).
description: Supplement to: Lantzsch, Hendrik; Bender, Vera Barbara; Hanebuth, Till J J (2009): Holocene evolution of mud depocentres on a high-energy, low-accumulation shelf (NW Iberia). Quaternary Research, 72(3), 325-336
DOI: 10.1594/pangaea.848470
title: Age determination of sediment core PS69/849-2
DOI: 10.1594/pangaea.874956
title: Accelerator mass spectrometry radiocarbon dates and calibrated ages of sediment core GeoB13861-1 and GeoB13823-2
DOI: 10.1594/pangaea.787779
title: (Table 2) Radiometric data of sediment core PG1901, Lake Donggi Cona

description: Corrected ages adjusted using the lake reservoir effect determined for a core-top sample. Calibrated ages were calculated with OxCal 4.1 and the IntCal09 calibration curve (Bonk Ramsey, 2009; Reimer et al., 2009). Radiocarbon results regarded as outliers are marked with an asterisk on the laboratory ID number. For age calibration a value of -30 per mil for the d13C of TOC was used.
DOI: 10.1594/pangaea.763824
title: (Table 1) Trace element and age analysis from the Porites coral from IODP Exp 310

description: Climate responses and changes in marine environments during the last deglaciation have been controversial and few paleoceanographic data are available from the tropical South Pacific, though this region is crucial in the investigations of ocean-atmosphere interactions. Integrated Ocean Drilling Program Expedition 310 was conducted to establish the time course of the postglacial sea-level rise at Tahiti in the South Pacific. A principal objective of this expedition was to examine the variation of marine environments during the last deglaciation. As fossil Porites coral is ideal for assessing past marine environments, we selected only Porites specimens from the many coral specimens retrieved, examined them by XRD, and dated them by the 14C method. In all, we obtained 17 pristine Porites specimens composed of only aragonite with ages from 15 to 9 ka. Then, we measured Mg/Ca, Ba/Ca, and U/Ca ratios and Cd contents as proxies for upwelling and sea surface temperature. Higher Ba/Ca ratios and Cd content together with lower reconstructed SSTs using U/Ca ratios in the coral specimens between 12.6 and 9.8 cal ka compared to around 15 cal ka suggest that upwelling and/or entrainment of subsurface water into mixed layer was enhanced around Tahiti during this period. This finding is consistent with previous reports and supports the idea that the South Pacific was characterized by La Niña-like conditions at least from 12.6 to 9.8 cal ka.
description: The authors give for Hole 310-M007A an elevation of -43,2m.
description: Supplement to: Inoue, Mayuri; Yokoyama, Yusuke; Harada, Mariko; Suzuki, Atsushi; Kawahata, Hodaka; Matsuzaki, Hiroyuki; Iryu, Yasufumi (2010): Trace element variations in fossil corals from Tahiti collected by IODP Expedition 310: Reconstruction of marine environments during the last deglaciation (15 to 9 ka). Marine Geology, 271(3-4), 303-306
DOI: 10.1594/pangaea.128924
title: Age determinations and sedimentology from Nagyrn, Lena Delta

description: Ages at elevation of 10.3m; 5.8 m; 4.0 m and 3.4 m are dated by OSL
DOI: 10.1594/pangaea.831618
title: (Table 1) Age determination of sediment core MD01-2430

description: Sediments deposited under lacustrine and marine conditions in the Sea of Marmara hold a Late Quaternary record for water exchange between the Black Sea and the Mediterranean Sea. Here we report a multiproxy data set based on oxygen and strontium isotope results obtained from carbonate shells, major and trace elements, and specific organic biomarker measurements, as well as a micropaleontological study from a 14C-dated sediment core retrieved from the Sea of Marmara. Pronounced changes occurred in d18O and 87Sr/86Sr values at the fresh and marine water transition, providing additional information in relation to micropaleontological data. Organic biomarker concentrations documented the marine origin of the sapropelic layer while changes in n-alkane concentrations clearly indicated an enhanced contribution for organic matter of terrestrial origin before and after the event. When compared with the Black Sea record, the results suggest that the Black Sea was outflowing to the Sea of Marmara from the Last Glacial Maximum until the warmer Bølling-Allerød. The first marine incursion in the Sea of Marmara occurred at 14.7 cal ka B.P. However, salinification of the basin was gradual, indicating that Black Sea freshwaters were still contributing to the Marmara seawater budget. After the Younger Dryas (which is associated with a high input of organic matter of terrestrial origin) both basins were disconnected, resulting in a salinity increase in the Sea of Marmara. The deposition of organic-rich sapropel that followed was mainly related to enhanced primary productivity characterized by a reorganization of the phytoplankton population.
description: Supplement to: Vidal, Laurence; Ménot, Guillemette; Joly, C; Bruneton, H; Rostek, Frauke; Çagatay, M Namik; Major, C; Bard, Edouard (2010): Hydrology in the Sea of Marmara during the last 23 ka: Implications for timing of Black Sea connections and sapropel deposition. Paleoceanography, 25(1), PA1205
DOI: 10.1594/pangaea.894678
title: Age determination of sediment core GeoB3910-2
DOI: 10.1594/pangaea.841032
title: (Table DR1) Radiocarbon ages of sediment cores KR02-06A_MC, KR02-06A_GC and MD01-2421
DOI: 10.1594/pangaea.894679
title: Age determination of sediment core MD09-3257
DOI: 10.1594/pangaea.880818
title: (Table 3) Accelerator mass spectrometry (AMS) radiocarbon dates and calibrated ages

description: °From Rebesco et al. (2016a).*From Rüther et al. (2012).a Radiocarbon laboratory: Poz = Poznan Radiocarbon Laboratory (Poland); TRa = Angström Laboratory Uppsala (Norway).b Material: bv = bivalves; pF = planktic foraminifers; bF = benthic foraminifers.
DOI: 10.1594/pangaea.883581
title: Radiocarbon ages of permafrost cores collected on Sobo-Sise Island and Bykovsky Peninsula
DOI: 10.1594/pangaea.128930
title: Age determinations and sedimentology Sagastyr Island, Lena Delta
DOI: 10.1594/pangaea.128925
title: Age determinations and sedimentology, Kurungnakh, Lena Delta

description: Ages at elevations of 8.8 m; 5.7 m and 4.3 m are dated by OSL
DOI: 10.1594/pangaea.128927
title: Age determinations and sedimentology Samoylov Island, Lena Delta
DOI: 10.1594/pangaea.706067
title: Age determination of sediment core GIK15399-1

description: Measured 14C-ages were probably older due to high input of terrestrial organic matter!
DOI: 10.1594/pangaea.837083
title: (Table 1) Age determination of sediment core MD99-2343

description: Down-core samples of planktonic and benthic foraminifera were analyzed for oxygen and carbon isotopes in International Marine Past Global Changes Study (IMAGES) core MD99-2343 in order to study the interactions between climate change in the Northern Hemisphere and the western Mediterranean thermohaline circulation at times of Heinrich events (HE). Our results confirm the antiphase correlation between enhanced North Atlantic Deep Water formation and low ventilation in the Mediterranean. However, this study reveals that this antiphase relationship in deepwater formation between the North Atlantic and Mediterranean was interrupted during times of HE when the injection of large volumes of water from melting icebergs reached the entrance to the Mediterranean. These events, which lasted less than 1000 years, are represented by pronounced decreases in both planktonic d18O and benthic d13C signals. Lower salinities of Mediterranean surface water resulted in a slowdown of western Mediterranean deepwater overturn even though cold sea surface temperatures and drier climate should have resulted in enhanced deepwater formation.
description: Supplement to: Sierro, Francisco Javier; Hodell, David A; Curtis, Jason H; Flores, José-Abel; Reguera, Maria Isabel; Colmenero-Hidalgo, Elena; Bárcena, María Angeles; Grimalt, Joan O; Cacho, Isabel; Frigola, Jaime; Canals, Miquel (2005): Impact of iceberg melting on Mediterranean thermohaline circulation during Heinrich events. Paleoceanography, 20(2), PA2019
DOI: 10.1594/pangaea.893142
title: Radiocarbon age model of sediment core MD07-3093
DOI: 10.1594/pangaea.810668
title: (Table S1) Globorotalia inflata 14C AMS ages and calibrated calendar year ages for core MD02-2594
DOI: 10.1594/pangaea.833407
title: (Supplementary Table 1) Results of U-Th analysis

description: * Sample ID Dating can be slightly different to the corresponding Sample ID Palaeo (Supplementary Table 2), as the dating sample in some cases is a subsample of a larger coral section that was sampled for palaeoclimate.** Woods Hole Oceanographic Institution (WHOI), Australian National University (ANU), University of Oxford (OX).*** U-Th ages are reported as kyr before the present relative to AD 1950.A, B: U-Th analyses were performed on different parts of the same coral specimen.detr. corr.: Detritial corrected.Results of powder X-ray diffraction (XRD) analysis are shown in Supplementary Table 2.The corals are massive and robust/branching Isopora palifera/cuneata colonies.
DOI: 10.1594/pangaea.413328
title: Age determination of sediment core Gebra-93-1 in the Bransfield Basin (Table 1)
DOI: 10.1594/pangaea.413329
title: Age determination of sediment core Gebra-93-2 in the Bransfield Basin (Table 1)
DOI: 10.1594/pangaea.862015
title: (Supplementary Table S1) Radiocarbon age of sediment core GeoB6518-1

description: Sample 5-15 cm could not be calibrated due to the presence of bomb-derived radiocarbon. Therefore, the core-top was set to zero age.
DOI: 10.1594/pangaea.837739
title: (Table 2) Radiocarbon contents of TOC and alkenone samples

description: Radiocarbon age relationships between co-occurring planktic foraminifera, alkenones, and total organic carbon in sediments from the continental margins of southern Chile, northwest Africa, and the South China Sea were compared with published results from the Namibian margin. Age relationships between the sediment components are site-specific and relatively constant over time. Similar to the Namibian slope, where alkenones have been reported to be 1000-4500 years older than co-occurring foraminifera, alkenones were significantly (~1000 years) older than co-occurring foraminifera in the Chilean margin sediments. In contrast, alkenones and foraminifera were of similar age (within 2 sigma error or better) in the NW African and South China Sea sediments. Total organic matter and alkenone ages were similar off Namibia (age difference TOC alkenones: 200-700 years), Chile (100-450 years), and NW Africa (360-770 years), suggesting minor contributions of preaged terrigenous material. In the South China Sea, total organic carbon is significantly (2000-3000 years) older owing to greater inputs of preaged terrigenous material. Age offsets between alkenones and planktic foraminifera are attributed to lateral advection of organic matter. Physical characteristics of the depositional setting, such as seafloor morphology, shelf width, and sediment composition, may control the age of co-occurring sediment components. In particular, offsets between alkenones and foraminifera appear to be greatest in deposition centers in morphologic depressions. Aging of organic matter is promoted by transport. Age offsets are correlated with organic richness, suggesting that formation of organic aggregates is a key process.
description: Supplement to: Mollenhauer, Gesine; Kienast, Markus; Lamy, Frank; Meggers, Helge; Schneider, Ralph R; Hayes, John M; Eglinton, Timothy Ian (2005): An evaluation of 14C age relationships between co-occurring foraminifera, alkenones, and total organic carbon in continental margin sediments. Paleoceanography, 20(1), PA1016
DOI: 10.1594/pangaea.862118
title: (Table 2) Age determination of sediment core MEDECOS_II_M2
DOI: 10.1594/pangaea.824776
title: (Table 2) Radiocarbon dates and calibrated ages from cores GeoB2107-5 and GeoB6211-1, GeoB6211-2

description: KIA: Leibniz-Laboratory for Radiometric Dating and Stable Isotope Research, Kiel, GermanyPoz: Poznan Radiocarbon Laboratory, Poznan, Poland
DOI: 10.1594/pangaea.746782
title: (Table 2) Radiocarbon ages of bottom sediments from the North Atlantic

description: Late Quaternary paleoceanology of the North Allantic has been studied on the base of radiolaria data.
description: Supplement to: Matul, Alexander G (1995): Late Quaternary paleoceanology of the North Atlantic based on radiolaria analysis data. Oceanology, 34(4), 550-555
DOI: 10.1594/pangaea.846500
title: Scarp points of the Atlantic Coastal Plain between 32° N and 38° N

description: RSL = relative sea level
DOI: 10.1594/pangaea.836020
title: Raw 14C data of sediment core OC437-07_GC68

description: Calibration curve: Marine09.DeltaR: 130 ±25.Calibrations performed using: OxCal P_sequence.k (events/cm): 0.75.
DOI: 10.1594/pangaea.836028
title: Radiocarbon measurements of sediment core OC437-07_GC27

description: Calibration curve: Marine09.DeltaR: 130 ±25.Calibrations performed using: OxCal P_sequence.k (events/cm): 0.75.
DOI: 10.1594/pangaea.836031
title: Radiocarbon measurements of sediment core OC437-07_GC66

description: Calibration curve: Marine09.DeltaR: 130 ±25.Calibrations performed using: OxCal P_sequence.k (events/cm): 0.75.
DOI: 10.1594/pangaea.836032
title: Radiocarbon measurements of sediment core OC437-07_GC68

description: Calibration curve: Marine09.DeltaR: 130 ±25.Calibrations performed using: OxCal P_sequence.k (events/cm): 0.75.
DOI: 10.1594/pangaea.821489
title: (Table 1) Age determination of Atlantic Ocean near-surface sediments
DOI: 10.1594/pangaea.736686
title: (Table 52) K-Ar age of amphibolite, gabbro, and diabase from ophiolite associations of the western Philippine Sea

description: Analyses have been carried out by Yu.G. Lavrentjev and N.L. Dobretsov at the participation of G.N. Savelyeva.
DOI: 10.1594/pangaea.821368
title: (Table 2) Age determination of sediment cores MD97-2106 and RS_147_GC34

description: 14C ages exceed the Marine04 data set (Hughen et al., 2004a). Converted to calendar years using 14C versus GISP2 calendar age calibration curve (Hughen et al., 2004b). 14C dates were reservoir-corrected by 503 yr. This value is the sum of the global average surface ocean reservoir correction of 400 yr (Stuiver and Braziunas, 1993) and Delta R of 103 ± 23 years for the Chatham Islands (Reimer and Reimer, 2001).
DOI: 10.1594/pangaea.846539
title: (Figure 8) Misfit between observations and models for the elevation of the mid-Pliocene shoreline

description: RSL = relative sea level.GIA = glacial isostatic adjustment.
DOI: 10.1594/pangaea.836017
title: Raw 14C data of sediment core OC437-07_GC37

description: Calibration curve: Marine09.DeltaR: 130 ±25.Calibrations performed using: OxCal P_sequence.k (events/cm): 0.75.
DOI: 10.1594/pangaea.890925
title: Supplemental table S3: Dimensional and weight measurements of charred barley grains recovered from cultural layers of the Hamanaka 2 archaeological site, northern Rebun Island, Japan
DOI: 10.15468/dl.yz2c5a
title: Occurrence Download

description: A dataset containing 1049408 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Peru",
 "Geometry POLYGON((-74.41956 -15.55074,-74.20658 -17.66579,-69.98565 -17.75801,-69.88884 -14.89685,-72.17356 -12.60255,-74.41956 -15.55074))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 1049408 records from 511 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0071075-250525065834625/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.m5mnkf
title: Occurrence Download

description: A dataset containing 275 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Stator limbatus (Horn, 1873)",
 "HasGeospatialIssue is false",
 "HasCoordinate is true"
 ]
}

 The dataset includes 275 records from 20 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0009204-250227182430271/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.khgk6x
title: Occurrence Download

description: A dataset containing 1247 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Stenus canaliculatus Gyllenhal, 1827",
 "HasGeospatialIssue is false",
 "HasCoordinate is true"
 ]
}

 The dataset includes 1247 records from 96 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0009118-250227182400228/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.27967104.v1
title: <b>Biometric Indicators, Gelatin Yield, and Functional Properties of Fish Scale Waste from Three Species with Different Trophic Levels</b>

description: Gelatin is a food additive widely used for the ability to form gels and provide an elastic texture in various food products, both for human and animal consumption. Therefore, this study was conducted to evaluate biometric characteristics as well as gelatin physicochemical properties derived from fish scale waste of Puntioplites bulu (herbivore), Cyprinus carpio (omnivore), and Channa lucius (carnivore). The findings demonstrated that the three chosen fish species have morphological variance, with Fulton's condition factors ranging from 1.13 to 3.30. The three species under study exhibited a positive (+) as well as negative allometric (-) growth pattern in the length-weight relationship. The average gelatin yield (dry weight basis) extracted from the scale of P. bulu, C. carpio, and C. lucius was 30.50 ± 2.34, 20.98 ± 0.33, and 18.02 ± 0.20 g/100 g, respectively. The extracted gelatin had an acidic pH ranging from 6.09 to 6.28. Foaming ability (FA) measured based on foam volume, and foam stability ratio (FS) determined based on foam volume loss include P. bulu (613 ± 5.77 and 16.57 ± 0.56 g/100 g), C. carpio (406.67 ± 30.55 and 96.52 ± 0.31 g/100 g), and C. lucius (600 ± 10 and 27.98 ± 1.80 g/100 g). Furthermore, fish scale gelatin’s water holding capacity (WHC) as well as fat binding capacity (FBC) were P. bulu (777.33 ± 23.45 and 98.33 ± 2.51 g/100 g), C. carpio (312 ± 15.71 and 37.66 ± 7.37 g/100 g), and C. lucius (967 ± 59.02 and 207.33 ± 3.08 g/100 g). In conclusion, gelatin made from fish scale waste from three distinct trophic levels displayed a variety of physicochemical and biometric properties
DOI: 10.15468/dl.8ksf4e
title: Occurrence Download

description: A dataset containing 5685 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Continent is North America",
 "OccurrenceStatus is Present",
 "TaxonKey is Helianthus annuus L.",
 "Year 1800-2000"
 ]
}

 The dataset includes 5685 records from 196 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0009206-250227182430271/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.hpqg82
title: Occurrence Download

description: A dataset containing 3 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Stenus capucinus Boheman, 1858",
 "HasGeospatialIssue is false",
 "HasCoordinate is true"
 ]
}

 The dataset includes 3 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0009119-250227182400228/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.pbgf2k
title: Occurrence Download

description: A dataset containing 5685 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Continent is North America",
 "OccurrenceStatus is Present",
 "TaxonKey is Helianthus annuus L.",
 "Year 1800-2000"
 ]
}

 The dataset includes 5685 records from 196 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0009120-250227182400228/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.5281/zenodo.14994639
title: The Effect of GPER1 genetic variants on systolic blood pressure in postmenopausal women in the UK Biobank

description: This dataset contains the summary effect estimates of single nucleotide polymorphisms (SNPs) in the GPER1 gene on systolic blood pressure for postmenopausal women in the UK Biobank. Table S1 shows the SNP effects for each GPER1 variant in all postmenopausal women regardless of parity. Table S2 shows SNP effects for each GPER1 variant in nulliparous women. Table S3 shows SNP effects for each GPER1 variant in multiparous women. Table S4 shows the difference in the SNP effects on mean systolic blood pressure in parous versus nulliparous women.
DOI: 10.15468/dl.zdgw2w
title: Occurrence Download

description: A dataset containing 1378 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Stenus biguttatus (Linnaeus, 1758)",
 "HasGeospatialIssue is false",
 "HasCoordinate is true"
 ]
}

 The dataset includes 1378 records from 116 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0009121-250227182400228/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.