cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.669555
title: (Table 5) Luminescence-dating of sediment core 94-BC20 of the Arctic Ocean
DOI: 10.1594/pangaea.536388
title: Age determination of sediment core GIK13588-3, Banc d'Arguin, off NW Africa (Table 2)

description: Dated on carbonate fraction &gt; 63 µm
DOI: 10.1594/pangaea.873675
title: Radiocarbon ages of sediment core KOT-3, Kotychi Lagoon, Northern Elis, Greece
DOI: 10.1594/pangaea.140720
title: (Table 1) Radiocarbon age determinations on sediment core IWSOE68-037
DOI: 10.1594/pangaea.855354
title: (Table 2) Age determination of sediment cores from the Californian Margin

description: Measuerd on mixed planktonic foraminifera.
DOI: 10.1594/pangaea.140722
title: (Table 1) Radiocarbon age determinations on sediment core IWSOE70-2-19-1
DOI: 10.1594/pangaea.770336
title: (Table 1) Age determination of basalts from DSDP Hole 30-289

description: The Pacific plate has undergone a substantial northward displacement during the late Mesozoic and the Cainozoic. Here we give additional documentation for such motion based on palaeomagnetic measurements of a sequence of sedimentary and basalt samples collected from middle Oligocene to Aptian sections of Deep Sea Drilling Project (DSDP) site 289 (Andrews, 1975; 00° 29.92'S, 158° 30.69'E) drilled on the Ontong Java Plateau.
description: The sample was holocrystallinc with alteration confined to minor oxidation in the groundmass.
description: Supplement to: Hammond, S R; Kroenke, Loren W; Theyer, Fritz; Keeling, D L (1975): Late Cretaceous and Paleogene paleolatitudes of the Ontong Java Plateau. Nature, 255(5503), 46-47
DOI: 10.1594/pangaea.803519
title: (Table 1) Argon ratios and datings of tephra layer biotites from ODP Leg 165 sites
DOI: 10.1594/pangaea.676716
title: (Table 1) Age determination of sediment core Alkor_159_225510

description: Measured on bulk benthic foraminifera. Project: Integrated Baltic Sea Environmental Study (IBSEN); funded by German Ministry of Education and Research (BMBF)
DOI: 10.1594/pangaea.676715
title: (Table 1) Age control points of sediment core GeoB7186-3

description: All ages are corrected for 13C and for a reservoir age of 530 years.
DOI: 10.1594/pangaea.815719
title: (Table 2b) Results of isotope studies of zircons from enderbites of the Odessa quarry, Bug area
DOI: 10.1594/pangaea.767473
title: Lead isotope composition and age determination of zircons in ODP Hole 188-1167A sample 1167 A-22
DOI: 10.5281/zenodo.15751872
title: COVID-19-Hospitalisierungen in Deutschland

description: Im Datensatz 'COVID-19-Hospitalisierungen' werden die aktuellen Zahlen der nach den Vorgaben des Infektionsschutzgesetzes - IfSG - erfassten hospitalisierten COVID-19-Fälle bereitgestellt.
Um den Trend der Anzahl von Hospitalisierungen und der 7-Tage-Hospitalisierungsinzidenz besser bewerten zu können, wird die berichtete Hospitalisierungsinzidenz um eine Schätzung der zu erwartenden Anzahl an verzögert berichteten Hospitalisierungen ergänzt. Neben den Daten der gemeldeten COVID-19-Hospitalisierungen auf Bundes- und Länderebene wird daher ein Nowcasting der Anzahl hospitalisierter Fälle und der 7-Tage-Hospitalisierungsinzidenz auf Bundesebene durchgeführt. Ziel ist die Schätzung der Anzahl von hospitalisierten COVID-19-Fällen mit Meldedatum innerhalb der sieben vorhergehenden Tage - inklusive der noch nicht an das RKI berichteten Hospitalisierungen. Aufbauend auf dem Nowcasting wird eine Schätzung der adjustierten 7-Tage-Hospitalisierungsinzidenz durchgeführt.
DOI: 10.1594/pangaea.879872
title: Age determination of sediment core PS96/079-3
DOI: 10.1594/pangaea.112917
title: Age data and corrections of aragonitic mud of sediment core GIK01177-C, Persian Gulf (Table 3)
DOI: 10.1594/pangaea.744486
title: Radiocarbon ages of sediment profile Co1010
DOI: 10.1594/pangaea.133677
title: Radiocarbon ages of pollen profile WOLFSLO1

description: pollen zones after Firbas VII-X; lowermost 4 samples from parallel profile
DOI: 10.1594/pangaea.793028
title: (Table 1) Radiocarbon ages of Bivalvia shells obtained from core ASV13_1157, Novaya Zemlya Trench

description: It is shown that sediments accumulated in the Southern Novaya Zemlya Trench at both deglaciation and marine stages. Permanent sea ice sheet existed during the deglaciation, and glacier meltwater was intensely delivered to the bottom layer. Along with the dominant sediment supply from the Southern Island of Novaya Zemlya, southern continental sources also played a noticeable role at that stage. Seasonal sea ice freezing led to the formation of cold brines at the marine stage. Like paleoproductivity, these processes were irregular. Dissolution of calcareous benthic foraminiferal tests considerably intensified after about 7 ka BP owing to a stronger Atlantic water advection into the Western Arctic and consequent increase in paleoproductivity, whereas the relative role of southern sedimentary provenances decreased. Sedimentation rates were constant (45 cm/ka) during the entire marine stage.
description: Supplement to: Levitan, Mikhail A; Belyaev, Nikolay A; Burtman, M V; Duplessy, Jean-Claude; Khusid, Tatyana A (2003): Holocene sedimentation history in the Southern Novaya Zemlya Trench. Lithology and Mineral Resources, 38(6), 564-575
DOI: 10.1594/pangaea.846984
title: (Supplementary Table 2) Age determination of sediment core GIK18460-3
DOI: 10.1594/pangaea.767445
title: Radiocarbon age determinations on samples from Delta pingo (Fig. 3)
DOI: 10.1594/pangaea.788691
title: (Table T2) Radionuclide ratios and derived ages of massive sulfides from ODP Leg 139 and Leg 169 sites
DOI: 10.1594/pangaea.77517
title: (Table 1) Age determinations on sediment core GIK13561-2

description: Carbon 14 lab, Kiel, H. Erlenkeuser
DOI: 10.1594/pangaea.847984
title: (Table 1) Age determination of sediment core MD95-2006
DOI: 10.1594/pangaea.755440
title: (Table 1b) Radiocarbon datings of Upper Quaternary bottom sediments from the Mediterranean Sea at Station VITYAZ7910
DOI: 10.1594/pangaea.844929
title: Radiocarbon dating of sediment profile PS2121
DOI: 10.1594/pangaea.527928
title: Age determination of sediment core GIK12358-1, shelf off Mauretania, West Africa (Table1)
DOI: 10.1594/pangaea.693593
title: (Appendix A) 39Ar/40Ar analyses for two volcanic ash layers of DSDP Hole 42-372 in the western Mediterranean Sea

description: Measured on K-feldspar. Sample 42-372-24R-1,5 (No. 1-20) VU51-A2 (04MY272) J = 0.001832 (+/- 0.20%) 200-400 µm ~3 grains per fusion. Sample 42-372-38R-3,0 (No. 21-40) VU51-A6 (04MY274) J = 0.001838 (+/- 0.30%) 200-400 µm ~5 grains per fusion. Sample 42-372-24R-1,5 (No. 41-51) VU51-A3 (05MY107) J = 0.001840 (+/- 0.30%) 120-200 µm ~50 grains per fusion. Sample 42-372-38R-3,0 (No. 52-64) VU51-A6 (A-I) (05MY108) J = 0.001842 (+/- 0.30%) 200-400 µm ~20 grains per fusion, VU51-A7 (J-S) (05MY108) J = 0.001843 (+/- 0.30%) 120-200 µm ~50 grains per fusion
DOI: 10.1594/pangaea.753164
title: (Table 2) U-Pb isotopic dating of zircons from hornfels of the H. Miller Seamount, Amundsen Sea
DOI: 10.1594/pangaea.66874
title: Stacked age determinations of the Ormara sediment cores

description: stacked record of SO90-33KL, SO90-34KG, SO130-245KL, SO130-246KG, SO130-247KA
DOI: 10.1594/pangaea.117009
title: Dated age of sediment core TN041-22G-MC
DOI: 10.1594/pangaea.713014
title: (Table 2) Age determination of sediment core HU77-152
DOI: 10.1594/pangaea.720971
title: (Table 2) K-Ar results from DSDP Hole 34-319A
DOI: 10.1594/pangaea.759528
title: (Table 1) Tie points used for the age model of sediment core MD99-2343

description: Ten 14C-AMS dates were calibrated with the Calib 5.0.1. program (Stuiver and Reimer, 1993) and the MARINE04 calibration curve (Hughen et al., 2004). Prior to 27 ka the age model is based on the correlation with the GISP2 ice core (Grootes et al., 1993, doi:10.1038/366552a0; Meese et al., 1997, doi:10.1029/97JC00269). Four additional tie points were added through the comparison of the G. bulloides d18O from both cores MD99-2343 and MD95-2043 (Cacho et al., 1999, doi:10.1029/1999PA900044; Sierro et al., 2005, doi:10.1029/2004PA001051). The age model was performed with the AnalySeries Version 1.1 (Paillard et al., 1996).
DOI: 10.1594/pangaea.727133
title: (Table 1) Radioisotopic age determinations of igneous rocks from the Vityaz Ridge
DOI: 10.1594/pangaea.735796
title: (Table 2) Age determination of sediment profile PS1535-5/8
DOI: 10.1594/pangaea.704777
title: (Table 3) Results of apatite fission track dating, ODP Site 165-999B
DOI: 10.1594/pangaea.842588
title: (Table 2) Age determination of sediment core HH11-134-BC
DOI: 10.1594/pangaea.375658
title: (Table 1) Age determinations on sediment core V31-135
DOI: 10.1594/pangaea.743233
title: (Tab.2) K-Ar age determination of dredged basalt samples at station PS2693-1
DOI: 10.1594/pangaea.756795
title: (Table a) Radiocarbon ages of bottom sediments from depressions of the Red Sea rift zone
DOI: 10.1594/pangaea.806331
title: (Table 1) Radiocarbon ages for sediment cores MD03-2597, NBP01-01-JPC17B and NBP01-01-KC17B
DOI: 10.1594/pangaea.833131
title: (Table 2) Age determination of sediment cores TTN13-18 and TTN13-19
DOI: 10.1594/pangaea.826079
title: (Table 1) Age determination of Alborian Sea sediment cores

description: Dating on single planktonic foraminifera Globigerina bulloides (&gt;125 µm).
DOI: 10.1594/pangaea.761018
title: (Table 1) Results of 40Ar/39Ar heating experiments of ODP Leg 123 samples
DOI: 10.1594/pangaea.768364
title: (Table 4) Radiocarbon analysis, coralline algae and microbialites from Papeete drill cores

description: Coralline algae and microbialites samples have been dated by radiocarbon AMS at the MALT (University of Tokyo, Japan) and coral samples have been dated by radiocarbon AMS at ARTEMIS (Saclay, France).
DOI: 10.1594/pangaea.141221
title: Lead ratios and zircon ages from tuff samples of Profil Goldisthal, Thüringen
DOI: 10.1594/pangaea.752212
title: Radiocarbon measurements and age calibration of eroded mollusc shells from seafloor sediment samples
DOI: 10.1594/pangaea.745667
title: (Table 3) Results of U-Pb zircon dating of rhyolite from Kytapkai Formation, Okhotsk-Chukotka volcanic belt
DOI: 10.1594/pangaea.802155
title: (Table 1) Age determination of the Holocene section of sediment cores from Lago Calvarne Bog and Laguna Cascada
DOI: 10.1594/pangaea.788995
title: (Table 2) U, Th, and Sm of apatite from rapidly cooled samples

description: Sediment depth is given in mbsf. AGE [ka BP] gives the deposition age.
DOI: 10.1594/pangaea.808554
title: (Table 2) Potassium, argon and K-Ar dates of the Mazagan granodiorite at V30-225, VA79-96KD and DSDP Hole 79-544A, off Moroccan coast
DOI: 10.1594/pangaea.831546
title: 13. 14C-AMS dates from sediment core GeoB3938-1
DOI: 10.1594/pangaea.737919
title: (Table 2) Age determination of sediment cores of the Chilean continental margin
DOI: 10.1594/pangaea.830789
title: (Table 5) Age determination of sediment cores V19-27, V21-40 and V28-238
DOI: 10.1594/pangaea.831191
title: (Table 1) Age determination of sediment core MD01-2378
DOI: 10.1594/pangaea.786463
title: (Table 2) Radiocarbon datings of cryoturbated soil pockets, basal peat and fossil wood along Tulemalu Lake
DOI: 10.1594/pangaea.880963
title: Age deterimination of sediment core GIK18517-2
DOI: 10.1594/pangaea.743506
title: Radiocarbon dating of bottom sediments from the Woodlark and Manus Basins
DOI: 10.1594/pangaea.847459
title: (Table 3) 40Ar-39Ar data of samples from East Antarctica
DOI: 10.1594/pangaea.783519
title: (Table EA2) Individual 40Ar/39Ar analysis of volcanic rocks from Hikurangi and Manihiki Plateaus
DOI: 10.1594/pangaea.786144
title: (Appendix) Radiocarbon ages of peat profiles S52 and S53 obtained southeast of Selwyn Lake, Canada

description: Data source: Environment Canada.
DOI: 10.1594/pangaea.861386
title: Radiocarbon age of sediment core GeoB8331-4
DOI: 10.15468/dl.n8cf9d
title: Occurrence Download

description: A dataset containing 15223 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is India",
 "DatasetKey is India Biodiversity Portal publication grade dataset",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Plantae"
 ]
}

 The dataset includes 15223 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0071076-250525065834625/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.779623
title: Age determination of sediment core MSM05/5_723-2
DOI: 10.1594/pangaea.407091
title: Age determination of sediment core RC11-83
DOI: 10.1594/pangaea.669551
title: (Table 5) Luminescence-dating of sediment core 92-BC17 of the Arctic Ocean
DOI: 10.1594/pangaea.755601
title: (Table 2-3) Radiocarbon datings of organic matter from sediments of Core PSh-4510

description: Core PSh-2510 (4.76 m long) recovered mud and clay of the Baltic Ice Lake and of all subsequent stages of the Baltic Sea. Grain size, mineral and chemical compositions, as well as physical properties of sediments were studied. Biostratigraphic (diatoms and foraminifers), lithostratigraphic, and chemical (26 elements) methods, as well as radiocarbon datings were used to subdivide core sections into stratigraphic units.
description: Supplement to: Emelyanov, Emelyan M; Trimonis, Egidius S; Lukashina, Nadezhda P; Slobodyannik, Vladimir M; Boström, Kurt; Westman, P; Bublitz, G; Leipe, Thomas; Kuptsov, Vladimir M (1995): Stratigraphy and composition of the stratotype core from the Gotland Deep (Baltic Sea). Oceanology, 35(1), 99-104
DOI: 10.1594/pangaea.759578
title: (Table 3) Results of radiocarbon dating of bottom sediments from the Southeast Pacific
DOI: 10.1594/pangaea.134608
title: Age determination of sediment core GIK13289-1
DOI: 10.1594/pangaea.808901
title: (Table 1) Radiocarbon dates of Mytilus edulis shells collected on Drayton Island
DOI: 10.1594/pangaea.848128
title: (Table S1) Age model of sediment core MR0806-PC09
DOI: 10.1594/pangaea.785469
title: (Table 1) Radiocarbon dates from sediment core DA06-139G during DANA cruise in 2006
DOI: 10.1594/pangaea.808902
title: (Table 2) Radiocarbon dates of peat and wood samples collected on Drayton Island
DOI: 10.1594/pangaea.734038
title: (Table 2) Age determination of sediment core INMD-113BX

description: Determinations by Beta-Analysical Laboratorie, Coral Gables, Fla. Bulk CaCO3. Half-life 5568 yr. Years before A.D. 1950 +/- 1 SD
DOI: 10.1594/pangaea.767360
title: (Table 2) Age analysis and aragonite content from different IODP Holes from Exp 310

description: The microbialites are calculated from the midpoint of the 1 sigma range of both raw 14C ages. Coralline algae and microbialites samples have been dated by radiocarbon AMS at the MALT (University of Tokyo, Japan) and most of the corals samples have been dated by radiocarbon AMS at ARTEMIS (Saclay, France) except for samples marked by * which were dated at the MALT. Corals marked by (d) are detailed in Durand et al. (doi:10.2204/iodp.sp.310.2005), submitted for publication. Slopemicrobialites are marked by ** and were not considered for the calculation of the average age offsets.
DOI: 10.1594/pangaea.714368
title: (Table 2) AMS Carbon-14 dating results for ODP Hole 195-1202B
DOI: 10.1594/pangaea.763947
title: Age determination of sediment core Fiavè
DOI: 10.1594/pangaea.742752
title: (Table 2) Age-depth model of ODP Site 167-1016

description: Sediment depth is the composite depth (mcd), 14C measured on bulk organic matter (BOM), below 3.51 mcd d15N correlation.
DOI: 10.1594/pangaea.760145
title: (Table 1) K-Ar age determination of ODP Leg 120 samples

description: lamda epsilon = (0.581 * 10**-10)a**-1; lambda beta = (4.962 10**-10)a**-1; 40K/total K = 1.167 10*-4 mM**-1. The ± figures represent estimations of the analytical precision at the 68% confidence level.
DOI: 10.1594/pangaea.779000
title: (Table 3) Fission track ages of ODP Hole 129-800A samples
DOI: 10.1594/pangaea.786398
title: (Table 1) Radiocarbon ages for permafrost core BY-pond and monoliths BY-hc1-3, Bylot Island
DOI: 10.1594/pangaea.760114
title: (Table 3) Main characteristics of tephra layers recognised in core Lz1120
DOI: 10.1594/pangaea.808060
title: (Table 1) Beryllium 10 production rates and exposure ages of granite erratics near Reedy Glacier
DOI: 10.1594/pangaea.763786
title: Tab. 2: K-Ar ages from the Read Group
DOI: 10.1594/pangaea.705452
title: (Table 1) Fission track age data for zircons from Fish Canyon Tuff standard

description: Age is fission track age, calculated using the zeta calibration method
DOI: 10.1594/pangaea.786663
title: (Appendix A2) Complete results of 40Ar/39Ar dating of hornblende grains from DSDP Hole 28-268

description: Method: Samples were co-irradiated with Mmhb hornblende monitor standard and Cima sanidine (internal standard) for 10 hours in the Cd lined facility at the Oregon State University Reactor, and are referenced to an Mmhb age of 523 Ma (Renne et al., 1998). Single-step CO2 laser fusion 40Ar/39Ar analyses for individual irradiated grains were processed at the Ar geochronology laboratory at Lamont-Doherty Earth Observatory. Reported data are corrected for background based on frequent analysis of the blank and mass discrimination based on frequent measurements of the air pipette. They are also corrected for nuclear interferences using the parameters provided in Renne et al. (1998) for the Oregon State reactor. The "J" values were calculated for the entire irradiation package, as horizontal and vertical gradients were less than the 1% variation of the Mmhb monitor standard measurements. Errors reported are based on the internal precision of the measurement and the 1% variation from measurements of Mmhb (1 sigma). LDEO Ar lab facilities: The LDEO Ar lab consists of a VG5400 noble gas mass spectrometer equipped with a modified Neir ion-source and a 90° sector extended-geometry. The mass spectrometer is operated in static mode and measurements are made on a Balzars multiplier in analogue mode using a high voltage of 1580 V on the multiplier (At these conditions, the 40Ar signal is about 1e-9 amps for 1e-11 moles of atmospheric Ar. A typical background 40Ar signal is approximately 2e-11 Amps). The LDEO Ar lab is entirely automated. Automation of the vacuum valves is achieved by using pneumatically operated valves that are activated by electro-pneumatic solenoid valves. Gasses released from the heating of samples are scrubbed of reactive gases such as H2 CO2, CO and N2 by exposure to Zr-Al sintered metal alloy getters. The remaining inert gasses, principally Ar, are then admitted to the mass spectrometer and the Ar-isotopic ratios are determined using "Mass Spec", an automated data collection software developed by Al Deino of the Berkeley Geochronology Center (http://www.bgc.org/facilities/other_facil.html). Both labs used a CO2 laser for fusing the individual grains.
DOI: 10.1594/pangaea.763669
title: Radiocarbon dates of plant detritus from sedimentary deposits of drill hole Bav-480, Pechora Sea

description: Data obtained during cruises 7, 11, 13, and 14 of R/V Akademik Sergei Vavilov (1990, 1997, and 1998) contributed a lot to reconstruction of paleogeographic environments that existed in the Barents Sea during the last glaciation maximum. This was possible owing to extensive acoustic profiling with Parasound equipment and use of a new approach to study of the upper part of the sedimentary cover. It is established that during the last glaciation maximum the Barents Sea was substantially smaller. It was almost completely surrounded by ice caps that descended to the shelf from glaciation centers on the land. The sea was connected with the World Ocean only by a narrow strait corresponding to the Bear Trough. Sea areas free of bottom glaciers were covered with floating ice: either by old pack ice or by plates of widespread shelf glaciers. Particular glaciomarine sediments accumulated under the floating ice. Destruction of the shelf glaciers during deglaciation resulted in formation of anomalously thick bottom sediment layers. The Pechora Sea shelf appeared to be above the sea level and was eroded by rivers. During entire Late Quaternary and, probably, the earlier epoch, the South Novaya Zemlya Trough represented an area of continuous marine and glaciomarine sedimentation.
description: Supplement to: Pavlidis, Yury A; Bogdanov, Yury A; Levchenko, Oleg V; Murdmaa, Ivar O; Tarasov, Gennadiy A (2005): New data on the natural environment in the Barents Sea at the end of the Valdai glaciation. Translated from Okeanologiya, 2005, 45(1), 92-106, Oceanology, 45(1), 85-98
DOI: 10.1594/pangaea.806942
title: (Table 2) Fission track ages of apatite and sphene from Paleogene sediments at DSDP Hole 81-555

description: Fission track ages of individual crystals of detrital apatite and sphene separated from early Eocene and Paleocene sandstones at Site 555 indicate the contribution of detritus from source rocks of at least three distinct age groups. A major group of Tertiary (56 ± 3 m.y.) apatite ages is compatible with either contemporaneous or near contemporaneous volcanism or rapid unroofing of high level intrusives like those identified previously on Rockall Island (Jones et al., 1972) and Greenland (Gleadow and Brooks, 1979). Cretaceous (100 ± 20 m.y.) apatite ages are consistent with known high level microgabbroic intrusives on Helen's Reef (Roberts et al., 1974). Such apatite ages could also be derived from basement rocks of very ancient terrains, especially around rifted continental margins where low level heating or uplift has affected the fission track ages of apatites (Gleadow, 1978). Minor contributions were also identified from a terrain with apatite ages around 150 to 200 m.y. Similar ages are known from granitic and metamorphic rocks in Greenland (Gleadow, 1978; Gleadow and Brooks, 1979). From experience elsewhere in the North Atlantic Craton (Gleadow, 1978), such apatite ages are also likely in the basement rocks of Rockall, but direct fission track results are lacking. With the identification of at least two nonmetamorphic sources, these data enable a refinement of the source of apatite suggested by heavy mineral studies (Morton, this volume). Two distinct groups of sphene ages of around 60 and 1,380 m.y. are also consistent with sources either on the Rockall Bank (Roberts et al., 1973) or in Greenland (Gleadow, 1978). Apatites from around 900 m depth have a combined age very close to the age of deposition, and they have track length distributions indicating that present temperatures in the hole are at, or close to, the maximum experienced since deposition.
description: Sediment depth is given in mbsf. All track densities expressed as for internal surfaces. Neutron dosimetry for reference glass SRM612: B = 6.005 * 109 neutrons/track, Zeta = 360 ± 10. Equivalent to NBS Cu dosimetry via reference glass SRM962.
description: Supplement to: Duddy, I R; Gleadow, A J W; Keene, John B (1984): Fission track dating of apatite and sphene from Paleogene sediments of Deep Sea Drilling Project Leg 81, Site 555. In: Roberts, DG; Schnittker, D; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 81, 725-729
DOI: 10.1594/pangaea.833370
title: Age determination of sediment core M78/1_235-1
DOI: 10.5281/zenodo.15321333
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/