cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.15321334
title: Data on Swedish perceptions of MBSE adoption

description: This is a repository contatining additional information for a publication under review. The repository will be updated based on feedback on the main manuscript during this process. 

The publication discusses three industrial cases, and we provide additional information in this repository regarding the evaluation. Three related publications are linked at the end of this repository, and for the tools themselves we offer the following links;

The implementation for case 1 can be accessed at the following GitHub: https://github.com/AIDOaRt-VCE-Team/Solution-framework

The implementation for case 2 can be accessed at the following GitHub: https://github.com/lolakkalol/Papyrus-Impact-Plugin

The tool used for case 3 can be found at: https://sparxsystems.com/products/ea/
DOI: 10.1594/pangaea.704775
title: (Table 3) Results of apatite fission track dating, DSDP Site 43-386
DOI: 10.1594/pangaea.785345
title: (Table T4) Argon 40 - Argon 39 incremental heating ages from Neogene ash layers in ODP Hole 183-1138A

description: Sediment depth is given in mbsf. All ages calculated relative to neutron fluence monitor FCT-2 biotite (28.04 ± 0.12 Ma), decay and abundance constants le = 0.581 x 10**-10/yr; lb = 4.961 x 10**-10/yr; 40K/K = 1.17 x 10**-4, and corrected for 37Ar decay (half-life = 35.1 days) and interfering isotopes 36Ar/37Ar[Ca] = 2.64 x 10**-4, 39Ar/37Ar[Ca] = 6.73 x 10**-4, 40Ar/39Ar[K] = 1.0 x 10**-3.
DOI: 10.1594/pangaea.756114
title: (Table 1a) Radiocarbon dating of bottom sediments from Station AK26A-2573
DOI: 10.1594/pangaea.82259
title: (Table 2) Age determination of sediment core GeoB3911-3

description: Measurement of monospecific carbonate samples (globigerina sacculifer in the fraction 250-500 µm). Ages were corrected for a reservoir effect of 400 yr (Bard, 1988, doi:10.1029/PA003i006p00635) and calibrated using the method of Bard et al. (1993)
DOI: 10.1594/pangaea.816010
title: (Table 2) Radiochemistry in the upper sediments at DSDP Hole 70-509B
DOI: 10.1594/pangaea.841738
title: (Table 3) Age determination of eastern equatorial Pacific sediment cores

description: Sediment depth is given in mbsf. Measured on Neogloboquadrina dutertrei &gt;200 µm. 14C results were calibrated to calendar ages considering a one standard deviation uncertainty (1 s confidence interval) for all ages and applying a 400 years reservoir effect correction. Ages were obtained using CALIB 4.2 (Stuiver et al. , 1998) or the polynomial of Bard et al. (1998).
DOI: 10.1594/pangaea.830814
title: Additional information for previously unpublished age records
DOI: 10.1594/pangaea.831280
title: (Table 1) Age determination of sediment cores M31/2_17KL and M5/2_9KL
DOI: 10.1594/pangaea.57541
title: Age determination, and physical properties of sediment core PS2647-5
DOI: 10.1594/pangaea.763233
title: Appendix A: SIMS zircon U-Pb isotopic analysis of the Beiwu, Linong and Lunong intrusions
DOI: 10.1594/pangaea.715255
title: (Table 1) 40Ar/39Ar plateau and isochron ages from DSDP Leg 15 holes

description: AGE is the plateau age
DOI: 10.1594/pangaea.782407
title: (Table S15) U-Th-Pb analyses of titanites of sample VT08122

description: Uncertainties at 1 s level.
DOI: 10.1594/pangaea.838966
title: (Table 4) Age determination of sediment cores from the north Queensland margin
DOI: 10.1594/pangaea.832497
title: (Table 1) Age determination of sediment core LINK17

description: A number of short-lasting warm periods (interstadials) interrupted the otherwise cold climate of the last glacial period. These events are supposedly linked to the inflow of the warm Atlantic surface water to the Nordic seas. However, previous investigations of planktonic foraminifera from the Nordic seas have not been able to resolve any significant difference between the interstadials and intervening cold stadials, as the faunas are continuously dominated by the polar species Neogloboquadrina pachyderma s. Here we examine the planktonic foraminifera assemblages from a high-resolution core, LINK17, taken at 1500 m water depth off northern Scotland below the warmest part of the inflowing Atlantic water. The core comprises the time period 34–10 calibrated ka B.P., the coldest period of the last glaciation and the deglaciation. The results reveal a hitherto unknown faunistic variability indicating significant fluctuations in both surface water inflow and in summer sea surface temperatures. During the interstadials, relatively warm Atlantic surface water (4–7°C) flowed north into the eastern Norwegian Sea. During the stadials and Heinrich events the surface inflow stopped and the temperatures in the study area dropped to &lt;2°C. The Last Glacial Maximum was nearly as warm as the interstadials, but the inflow was much more unstable. The data reveal two previously unrecognized warming events each lasting more than 1600 years and preceding Heinrich events HE3 and HE2, respectively. By destabilizing the ice sheets on the shelves the warmings may have played a crucial role for the development of Heinrich events HE2 and HE3.
description: Supplement to: Rasmussen, Tine Lander; Thomsen, Erik (2008): Warm Atlantic surface water inflow to the Nordic seas 34-10 calibrated ka B.P. Paleoceanography, 23(1), PA1201
DOI: 10.1594/pangaea.841266
title: (Table 2) Age determination of bulk fraction of sediment core MD99-2201

description: PMC (corrected) is the proportion of modern (1950 AD) carbon (%), corrected with the d13C value for mass fractionation.
DOI: 10.1594/pangaea.741966
title: (Table 1) Radiocarbon dating of Upper Quaternary sediments from the Black Sea, Cruise 8 of R/V Vityaz-2
DOI: 10.1594/pangaea.788023
title: (Table 5) K-Ar age of leucocratic epidote-mica crystalline schists from the lower unit of the Khavyven Formation
DOI: 10.1594/pangaea.792590
title: (Table 4) K-Ar determinations for celadonite and proto-celadonite from DSDP Site 92-597 altered basalts

description: Sub-basement depth [m]. Ages were calculated from the following decay and abundance constants: lambda-e = 0.581x10**-10 /yr ; lambda-beta = 4.962 x 10**-10/yr.; 40K/K = 1.167x10**-4 mol/mol.
DOI: 10.1594/pangaea.831610
title: (Table 1) Age determination of sediment core RAPiD-15-4P

description: Radiocarbon ages were converted to calendar ages using Calib 5.1 IntCal (Reimer et al., 2004). Years B.P., years before A.D. 1950. By using the assigned stratigraphic age (converted to years B.P.), the contemporaneous age difference (Rsurf) between the atmosphere 14C age (calculated using IntCal04) and the measured 14C age of the surface marine sample (planktonic foraminifera samples) can be calculated. Error estimates for DR include lab error in 14C measurement, uncertainty in the 14C calibration curve, error in NGRIP age, and an estimate of error for picking midpoints/tephra layers based on sedimentation rates and modeled mixing intervals.
DOI: 10.1594/pangaea.834962
title: (Table 1) Age determination of sediment core SONK_11_D

description: Sediment depth is given in composite depth (mcd). Conventional 14C ages were calibrated using OxCal 4.1 (Ramsey, 1995, 2001, 2009) with the IntCal09 calibration data set (Reimer et al., 2009). Conventional 14C ages obtained from aquatic material and bulk sediment OM were corrected by -150 years before calibration to consider the hardwater effect. Samples down to 0.215 mcd were not considered for age modeling.
DOI: 10.1594/pangaea.786917
title: (Table T3) Ages and two-way traveltimes of ODP Site 180-1118

description: Sediment depth is given in mbsf. Event numbers correspond to those presented in Takahashi et al. (2001, doi:10.2973/odp.proc.sr.180.152.2001). Two-way traveltimes of non-MCS events have had 18 ms added to move the event to the location corresponding to the point at which the first positive peak of a corresponding reflector would appear. The TWTT for each event has been added, in addition to the depth, age, and TWTT of key reflectors in the MCS data. Data are adapted from Takahashi et al. (2001, doi:10.2973/odp.proc.sr.180.152.2001).
DOI: 10.1594/pangaea.787118
title: (Table 3) Dose rates, uranium and thorium content, and IRSL ages of soil profiles obtained in the Kyichu River catchment
DOI: 10.1594/pangaea.855321
title: (Table 1) Age determination of sediment core RC14-31TW
DOI: 10.1594/pangaea.745118
title: (Table 9) U-Pb isotopic dating of zircons from cataclased hornblende gabbronorite of the Markov depression, Central Atlantic
DOI: 10.1594/pangaea.66313
title: Age model and sedimentation rates of core GEOFAR KF09
DOI: 10.1594/pangaea.755002
title: (Table 1) Age of basalts from the Norwegian Sea
DOI: 10.1594/pangaea.735795
title: (Table 2) Age determination of sediment profile PS1906-1/2

description: dated material: Neogloboquadrina pachyderama (s.)
DOI: 10.1594/pangaea.839281
title: Radiocarbon dates and their calendar age conversions for sediment cores from the Indo-Pacific and Eastern Equatorial Pacific
DOI: 10.1594/pangaea.816518
title: Table A. LA-ICP-MS zircon U-Pb dating results of Jurassic granitoid rocks
DOI: 10.1594/pangaea.763900
title: Age determination of sediment core Bondone
DOI: 10.5281/zenodo.15665866
title: Data and code to reproduce analyses in Li et al, "Assessment of enzyme diversity in the fermented food microbiome".

description: This datasets archives the data and code to reproduce analyses for the article Li et al, "Assessment of enzyme diversity in the fermented food microbiome".

Among them, the prok_mag_orf_enzyme_sequence.fasta and euk_mag_orf_enzyme_sequence.fasta files contain the enzyme sequences of MAGs predicted to be from prokaryotes or eukaryotes, respectively.

The metadata.csv file contains the CLEAN prediction annotation results and sample-food category mapping information.

The cfmd_reset.Rmd file is the code used to reproduce this work.

The two files cfmd_reset.tar.gz and cfmd_copy.tar.gz contain the process files generated in our analysis.
DOI: 10.1594/pangaea.759804
title: Table 1 Control points for the age model for core MD972151

description: Accelerator mass spectrometry (AMS) C-14 ages were obtained for nine samples using calcareous tests of single species of the planktonic foraminifer G. sacculifer. Marine isotope stage boundaries were identified using the d18O curve of benthic foraminifer shown in Fig. 3 and ages of Martinson et al. (1987), doi:10.1016/0033-5894(87)90046-9 are followed with a modification of MIS 3.1 as suggested by Grootes and Stuvier (1997), doi:10.1029/97JC00880.
DOI: 10.1594/pangaea.80224
title: (Table 1) Age determination of sediment core GIK18287-3
DOI: 10.1594/pangaea.822110
title: (Table S2) Age determination of corals from the Tasmanian Seamounts
DOI: 10.1594/pangaea.883845
title: (Table S2) Uranium/Thorium isotopic composition of in situ Porites microatolls in French Polynesia

description: Uranium/Thorium isotopic composition of 72 in situ Porites microatolls from five islands in French Polynesia. Recommendations of Dutton et al. were followed for the presentation of U/Th age data. All statistical errors are two standard deviations of the mean (2 sigma mean). All samples have been corrected for initial 230Th by using a 230Th/232Th activity ratio of 0.66 ± 0.2. Non-reported data consist of 230 Th/232 Th ratios which became negative due to background corrections. 238U Concentrations are not corrected for the background.
DOI: 10.1594/pangaea.726216
title: (Table 7) Age determination of sediment core MD73-025
DOI: 10.1594/pangaea.707170
title: 14C age determinations of peat from profile Kakitu
DOI: 10.1594/pangaea.755171
title: (Table S1) Age determination of sediment core MSM05/5_712-1
DOI: 10.1594/pangaea.722615
title: (Table DR1) 40Ar-39Ar incremental heating ages for ODP Hole 198-1213B basalts
DOI: 10.1594/pangaea.133671
title: Radiocarbon ages of profile Kolbermoor1 for pollen zone Ia

description: Pollen zone after Firbas Ia-III
DOI: 10.1594/pangaea.68880
title: (Table 1) Age determination of sediment core SO82_5-1
DOI: 10.1594/pangaea.725358
title: (Table 2) Radiocarbon ages of basement fluids from transect of east flank of Juan de Fuca Ridge, ODP Leg 168

description: AGE is the radiocarbon age. Samples are near-basement porewaters; ages from Site 1026 are on duplicate samples collected by downhole sampler. Ages for porewater samples were corrected for 'dead' organic carbon; this mostly affects Site 168-1024 and also Site 168-1023
DOI: 10.1594/pangaea.841265
title: (Table 1) Age determination of Globigerinoides sacculifer of sediment core MD99-2201

description: Calendar year ranges represent 95% probability (2 sigma. PMC (corrected) is the proportion of modern (1950 AD) carbon (%), corrected with the d13C value for mass fractionation.
DOI: 10.15468/dl.cud7dw
title: Occurrence Download

description: A dataset containing 7269 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Sison amomum L., Sisymbrium altissimum L., Sisymbrium irio L., Sisymbrium loeselii L., Sisymbrium officinale (L.) Scop., Sisymbrium orientale L., Sixalix atropurpurea (L.) Greuter & Burdet, Smilax aspera L., Smyrnium olusatrum L., Solanum angustifolium Houst. ex Mill., Solanum carolinense L., Solanum dulcamara L., Solanum nigrum L., Solanum nitidibaccatum Bitter, Solanum physalifolium Rusby, Solanum sarrachoides Sendtn., Solanum tuberosum L., Solidago altissima L., Solidago canadensis L., Solidago gigantea Aiton, Solidago nemoralis Aiton, Solidago virgaurea L., Sonchus arvensis L., Sonchus asper (L.) Hill, Sonchus oleraceus L., Sonchus palustris L., Sonchus tenerrimus L., Sorbaria sorbifolia (L.) A.Braun, Sorbus aucuparia L., Sorghum bicolor (L.) Moench, Sorghum halepense (L.) Pers., Sparganium emersum Rehmann, Sparganium erectum L., Spartium junceum L., Spergula arvensis L., Spergularia rubra (L.) J.Presl & C.Presl, Spiraea alba Du Roi, Spiraea douglasii Hook., Spiraea tomentosa L., Spiranthes spiralis (L.) Chevall., Spirodela polyrhiza (L.) Schleid., Sporobolus alterniflorus (Loisel.) P.M.Peterson & Saarela, Sporobolus anglicus (C.E.Hubb.) P.M.Peterson & Saarela, Sporobolus indicus (L.) R.Br., Stachys alpina L., Stachys annua (L.) L., Stachys arvensis (L.) L., Stachys byzantina K.Koch, Stachys germanica L., Stachys palustris L., Stachys recta L., Stachys sylvatica L., Stellaria alsine Grimm, Stellaria apetala Bernardino, Stellaria graminea L., Stellaria media (L.) Vill., Stellaria neglecta (Lej.) Weihe, Stellaria palustris (Murray ex Ehrh.) Hoffm., Stenocactus crispatus (DC.) A.Berger, Stenocactus multicostatus (Hildm.) A.Berger, Stratiotes aloides L., Struthiopteris spicant (L.) Weiss, Succisa pratensis Moench, Symphoricarpos albus (L.) K.Koch, Symphyotrichum lanceolatum (Willd.) G.L.Nesom, Symphyotrichum novae-angliae (L.) G.L.Nesom, Symphyotrichum novi-belgii (L.) G.L.Nesom, Symphyotrichum pilosum (Willd.) G.L.Nesom, Symphyotrichum squamatum (Spreng.) G.L.Nesom, Symphytum officinale L., Symphytum tuberosum L., Symphytum ×uplandicum Nyman, Symplocarpus foetidus (L.) Salisb. ex W.P.C.Barton, Syringa vulgaris L., Taeniatherum caput-medusae (L.) Nevski)",
 "Country is New Zealand",
 "BasisOfRecord is one of (Human Observation, Observation, Occurrence evidence, Material citation, Living Specimen)",
 "CoordinateUncertaintyInMeters is less than or equal to 10000",
 "HasCoordinate is true"
 ]
}

 The dataset includes 7269 records from 8 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0071079-250525065834625/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.847590
title: (Table 2, page 458), Isotopic data on manganese oxide crust U23-1 from the south-west Pacific island arc

description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
DOI: 10.1594/pangaea.707390
title: (Table 2) Age determinations of sediment core PS1726-1

description: Vedde ash at 0.58 m sediment depth
DOI: 10.1594/pangaea.725950
title: (Table 2) Age determination of sediment core GIK16017-2
DOI: 10.1594/pangaea.707254
title: (Table 1) Uranium and thorium mass spectrometric results for stalagmite 1s
DOI: 10.1594/pangaea.733308
title: (Table 1) Chronostratigraphic model for sediment core MD95-2040
DOI: 10.1594/pangaea.787454
title: (Table 1) Radiocarbon dates for sediment core T89-16
DOI: 10.1594/pangaea.711749
title: (Table 2) Age determination of sediment core GeoB3129-1

description: Measurement of monospecific carbonate samples (globigerina sacculifer in the fraction 250-500 µm). Ages were corrected for a reservoir effect of 400 yr (Bard, 1988, doi:10.1029/PA003i006p00635) and calibrated using the method of Bard et al. (1993)
DOI: 10.1594/pangaea.763136
title: (Table A1) Age determination of cores St-11, DR-16 and DR-13 from the Bering Sea

description: Ages are calculated from total organic carbon
DOI: 10.1594/pangaea.823144
title: (Table S1) Age determination of sediment core MD03-2607

description: Age determination at the core depth at which the strong increase in %C3 was observed.
DOI: 10.1594/pangaea.753108
title: (Table 1) Results of age determinations of volcaniclastic rocks from the Sea of Japan
DOI: 10.1594/pangaea.823772
title: Age determination of North Atlantic sediment cores

description: Available overwash records from coastal barrier systems document significant variability in North Atlantic hurricane activity during the late Holocene. The same climate forcings that may have controlled cyclone activity over this interval (e.g., the West African Monsoon, El Niño-Southern Oscillation (ENSO)) show abrupt changes around 6000 yrs B.P., but most coastal sedimentary records do not span this time period. Establishing longer records is essential for understanding mid-Holocene patterns of storminess and their climatic drivers, which will lead to better forecasting of how climate change over the next century may affect tropical cyclone frequency and intensity. Storms are thought to be an important mechanism for transporting coarse sediment from shallow carbonate platforms to the deep-sea, and bank-edge sediments may offer an unexplored archive of long-term hurricane activity. Here, we develop this new approach, reconstructing more than 7000 years of North Atlantic hurricane variability using coarse-grained deposits in sediment cores from the leeward margin of the Great Bahama Bank. High energy event layers within the resulting archive are (1) broadly correlated throughout an offbank transect of multi-cores, (2) closely matched with historic hurricane events, and (3) synchronous with previous intervals of heightened North Atlantic hurricane activity in overwash reconstructions from Puerto Rico and elsewhere in the Bahamas. Lower storm frequency prior to 4400 yrs B.P. in our records suggests that precession and increased NH summer insolation may have greatly limited hurricane potential intensity, outweighing weakened ENSO and a stronger West African Monsoon-factors thought to be favorable for hurricane development.
description: Supplement to: Toomey, Michael R; Curry, William B; Donnelly, Jeffrey P; vam Hengstum, Peter J (2013): Reconstructing 7000 years of North Atlantic hurricane variability using deep-sea sediment cores from the western Great Bahama Bank. Paleoceanography, 28(1), 31-41
DOI: 10.1594/pangaea.802550
title: (Table 2) Radiocarbon ages of sediment core GeoB9532-2, GeoB9533-2/3, and GeoB9534-5
DOI: 10.1594/pangaea.743076
title: (Table 1) Radiocarbon age dates and calibrated ages of sediment core GeoB9503-5

description: Calibrated ages were estimated using CALIB 5.0.2 and are based on the Intcal04 calibration curve (Reimer et al. 2004; Stuiver et al. 2005).
DOI: 10.1594/pangaea.832474
title: (Table 2) AMS-14C ages and calibrated ages of sediment core GeoB10065-7

description: NOSAMS: Measured at the National Ocean Sciences Accelerator Mass Spectrometry Facility, Woods Hole, United States of America. UCIAMS: Measured at the Keck Carbon Cycle Accelerator Mass Spectrometry Facility, Earth System Science Department, University of California, Irvine, United States of America. NOSAMS-OS-64679: Invalid age for the marine13.14c calibration curve. *: A regional reservoir correction (DR) of þ130 35 years have been applied (Southon et al., 2013).
DOI: 10.1594/pangaea.722548
title: (Table 3) U-Th-Pb analyses of zircons from ODP sample 210-1277-9R-7,50-53
DOI: 10.1594/pangaea.860743
title: Age determination of sediment core PS75/073-2
DOI: 10.1594/pangaea.705255
title: (Table 3) Age determination of ODP Site 181-1119

description: Laboratory determinations were provided by the Australian Nuclear Science and Technology Organisation. Dates were corrected for marine reservoir age after the data provided by Sikes et al. (2000, doi: doi:10.1038/35014581), and converted to calendar year estimates using CALPAL (CALPAL, 2003, http://www.calpal.de/) and the INTCAL98 age model (Stuiver et al.,1998).
DOI: 10.1594/pangaea.82025
title: (Table 1) Age model of sediment core MD95-2039
DOI: 10.1594/pangaea.605205
title: K-Ar ages from Berg Mountains and Archangel Mountains, northern Victoria Land, Antarctica (Table 4.6-1)
DOI: 10.1594/pangaea.140247
title: (Table T2) 40Ar-39Ar data on milligram-sized fractions, ODP Hole 178-1097A

description: 178-1097A-27R-1,35-58, (6.8 mg) J = 0.0006101
DOI: 10.1594/pangaea.744986
title: (Table 1) Results of radiochemical analyses of sulfide ore samples collected from the Rainbow and Logachev-2 hydrothermal fields
DOI: 10.1594/pangaea.875298
title: (Table S1) Raw AMS 14C data and calibrated ages of sediment cores GeoB16206–1 and M35003-4
DOI: 10.1594/pangaea.718620
title: (Table 1) Argon dating of ash layers from DSDP Hole 18-178

description: Ash layers from Deep Sea Drilling Project site 178 in the northeast Pacific Ocean have been dated by the 40Ar-39Ar stepwise heating technique to resolve published discrepancies concerning the length of time explosive volcanism has affected the eastern Aleutian arc and Alaskan Peninsula. The results of the investigation indicate that the record of ash-fall deposition at site 178 extends back at least 6.5 m.y. Assuming that 6.5 m.y. ago marks the onset of renewed calc-alkalic volcanism of the volcanic arc, proposed models of continuous and discontinuous motion between the Pacific and North American lithospheric plates can be evaluated. If appreciable time elapsed between the onset of subduction and the onset of arc volcanism, the 6.5-m.y. record of ash-fall deposition in the north-east Pacific is most compatible with models of continuous plate motion throughout late Cenozoic time.