cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.56084
title: Table 1. Radiocarbon dated samples from lake basin cores from the Nikel-Kirkenes area

description: The marine-lacustrine transition (isolation contact) in sediment cores from eight lake basins situated 13.5–72 m a.s.l., in the Norwegian-Russian border area north of Nikel, northwest Russia, was identified based on lithological and diatom analysis, radiocarbon dated, and used to construct a relative sea-level (RSL) curve for the Holocene. All the lakes except one (interpreted as having an unconformable slumped transition) show a regressive I-II-III (marine-transitional-lacustrine) facies succession, indicating a postglacial history of continuous emergence. The RSL curve shows rapid emergence between 10 000 and 8000 BP, very slow emergence between 7000 and 5000 BP, increased rate of emergence between 4500 and 4000 BP, and a moderate rate of emergence after 3500 BP. The low rate of emergence around 6000 BP correlates with the Tapes transgression of more coastal regions, but corresponding sea level, at 25–26 ma. present s.l., lies 5–10 m lower than the elevation predicted based on existing isobase maps for the region. The discrepancy suggests a need for further work in order to more rigorously define and map the Tapes transgression and associated shoreline complex in the northern Fennoscandian-Kola region.
description: Supplement to: Corner, Geoffrey D; Yevzerov, Vladimir Y; Kolka, Vasili V; Møller, Jakob J (1999): Isolation basin stratigraphy and Holocene relative sea-level change at the Norwegian-Russian border north of Nikel, northwest Russia. Boreas, 28(1), 146-166
DOI: 10.1594/pangaea.837323
title: (Table 1) Age determination of ODP Hole 117-723A

description: We have carried out a high-resolution study of fluctuations in upwelling intensity along the Oman Margin, western Arabian Sea, through the last 19,130 years based on several marine microfossil indices of upwelling. We document a periodicity of 2,200 years in the upwelling indices, which would be governed by the south-west (SW) monsoon with such a periodicity. Our data further demonstrate greater amplitude in the variability of the SW monsoon during the Holocene than during the last glacial period. Our reported 2,200 years periodicity has two implications (1) oceanic circulation changes partly influence monsoon strength at sub-Milankovitch cycles (2) previously documented 2,300 years periodicity in atmospheric 14C might be induced by oceanic circulation changes.
DOI: 10.1594/pangaea.650327
title: Age determination of profile Helambu_1
DOI: 10.1594/pangaea.732383
title: (Table 1) Age determination on sediment core 87-144PC
DOI: 10.1594/pangaea.722547
title: (Table 2) Ar-Ar results for minerals from ODP Hole 173-1070A
DOI: 10.1594/pangaea.815886
title: (Supplementary Table 1) Concentrations of 14C, radiocarbon and calibrated ages obtained on planktonic foraminifera from core SO130-289KL from the northeastern Arabian Sea

description: Depth is given as average depth.ETH: AMS facility at Hönggerberg Zürich, Switzerland.KIA: Leibnitz-Laboratory for Radiometric Dating and Isotope Research at the Christian-Albrechts University in Kiel, Germany.
DOI: 10.1594/pangaea.57386
title: tab 3
DOI: 10.1594/pangaea.904057
title: Isotope ratios across Paleocene-Eocene Thermal Maximum of ODP Site 198-1209
DOI: 10.1594/pangaea.763782
title: Tab. 1: Rb-Sr data of Read Group rocks, basement of the Read Window (A. Höhndorf, P. Müller, N. Roland)
DOI: 10.1594/pangaea.763935
title: Tab. 1: Age of biogene material from the ice margin, Kofoed-Hansen Bræ and Storstrømmen

description: Early Holocene recession of the ice cover over Germania Land in North-East Greenland 7.5 ka B.P. brought the Inland Ice margin back to a position close to the present. Continued recession after that time lead to the formation of a "Storstrømmen Sound" which separated Germania Land from mainland Greenland in the period from about 6 to 1 ka B.P. The present filling of the approximately 100 km long sound by the glaciers of Storstrømmen and Kofoed-Hansen Bræ must therefore have taken place during the Little lce Age. In an archaeological sense this implies deterioration of the living conditions of Neo-Eskimos compared to those of Palaeo-Eskimos.The neoglacial re-formation and present existence of the glaciers as a Little Ice Age relict may imply a present-day instability in their dynamics, as demonstrated by the pulsations (surge-like behaviour) in the last part of the 20th century. An earlier Little Ice Age advance might possibly have had the same amplitude as that documented from the 20th century but its exact age and character is not known.The glacio-isostatic response of the earth's crust to the variations in the Holocene glacier load implies a relatively slow and slight emergence and subsequent submergence. The shift from emergence to submergence must have taken place between about 2 and 1 ka B.P.
description: Position digitized from map. No further information available.
description: Supplement to: Weidick, Anker; Andreasen, Claus; Oerter, Hans; Reeh, Niels (1996): Neoglacial glacier changes around Storstremmen, North-East Greenland. Polarforschung, 64(3), 95-108
DOI: 10.1594/pangaea.422408
title: (Table 1a) Age control points of sediment core GeoB7622-2 and GeoB7622-3, Black Sea

description: Calibrated Age, Calendar Years B.P.: 0=modern age
DOI: 10.1594/pangaea.720974
title: (Table 3) K-Ar results from DSDP Hole 35-323
DOI: 10.1594/pangaea.823418
title: (Table S1) Age horizons given by varve-independent age markers compared to varve age-depth model of Lake Ledro

description: Age control: earthquake see Rovida et al., 2011; Simonneau et al., 2013; begin of hydrological modifications see Casellato and Caneva, 1994.
DOI: 10.5281/zenodo.15751841
title: GPXV Manuscript Supplementary Materials

description: The supplementary file includes four tables, two gb files, and a txt file. The first table lists the viruses used for phylogenetic comparison with GPXV, including their ICTV formal names, common names, natural hosts, and accession numbers. The second table shows a list of all the annotated GPXV genes along with their start coordinates, end coordinates, and strand listed. The third table provides the genomic coordinates of ORFs 8, 9, 50, and 73 within the GPXV genome. The fourth table depicts a genomic comparison of GPXV and GPHLV proteins. The gb files are the raw, complete genome of GPXV and GPHLV. The txt file is the annotated GPXV genome.
DOI: 10.5281/zenodo.15751842
title: GPXV Manuscript Supplementary Materials

description: The supplementary file includes four tables, two gb files, and a txt file. The first table lists the viruses used for phylogenetic comparison with GPXV, including their ICTV formal names, common names, natural hosts, and accession numbers. The second table shows a list of all the annotated GPXV genes along with their start coordinates, end coordinates, and strand listed. The third table provides the genomic coordinates of ORFs 8, 9, 50, and 73 within the GPXV genome. The fourth table depicts a genomic comparison of GPXV and GPHLV proteins. The gb files are the raw, complete genome of GPXV and GPHLV. The txt file is the annotated GPXV genome.
DOI: 10.1594/pangaea.735790
title: (Table 2) Age determination of sediment core OD-041-04
DOI: 10.1594/pangaea.732362
title: (Table 1) Age determination of sediment core 88-PCM-4

description: some dates were published previous in Svendsen et al. (1992)
DOI: 10.1594/pangaea.732363
title: (Table 1) Age determination of sediment core 90-01-PC1
DOI: 10.1594/pangaea.732365
title: (Table 1) Age determination of sediment core 90-24-PC1
DOI: 10.1594/pangaea.788593
title: (Table S2) B/Ca ratios Oridorsalis umbonatus from Holocene sediments

description: Size fraction of benthic foraminifera = 150-250 µm.
DOI: 10.1594/pangaea.871459
title: Table S45 - Combined magnetostratigraphy for the Ypresian from ODP Sites 207-1258, 208-1262, 208-1263, 208-1265, 208-1267
DOI: 10.1594/pangaea.357054
title: Paleoecological investigation of Hessische Senke at site Rau-1
DOI: 10.1594/pangaea.867858
title: AMS 14C data of sediment core GRV_13-2
DOI: 10.1594/pangaea.778835
title: Table 1 : AMS-14C data used for the reconstruction of the Wismar Bay shoreline displacement curve

description: The Baltic coast of Mecklenburg-Vorpommern is located in the transition Zone between the region of Fennoscandian Uplift and the Central European Depression. In relation to the eustatic sea-level rise, the northeast coast shows a slower inundation, while for the southwestern area a faster transgression is indicated, which can be attributed to crustal movements. To determine the spatial and temporal differences since the onset of the Littorina Transgression, three relative sea-level curves have been established along a transect parallel to the gradient of upliftlsubsidence. The Wismar Bay area is one endpoint of the transect demonstrating today 10 Abb., 2 Tab. a relative sea-level rise of 1.4 mm/a. To determine the relative sea-level curve for the Wismar Bay, two sites were investigated on Rustwerder Spit (Poel) and Redentin. They provided reliable depth-age data, while the stratigraphy was additionally supported by lithological/geochemical, pollen, diatom and macrofossil data. Additional evidence was provided by archaeological submarine surveys and excavations. Comparing the new relative sea-level curve with a curve from the Vorpommern coast, it can be shown that for the period from 4000 cal BC until present, the differences between the two curves are caused by a constant neotectonic movement, while for the older periods an increasing isostatic component must be taken into account.
description: R - Rustwerder, GT - Großes Tief, JG - Jäckelgrund, JB - Jäckelberg, T - Timmendorf
description: Supplement to: Lampe, Reinhard; Endtmann, Elisabeth; Janke, Wolfgang; Meyer, Hinrich; Lübke, Harald; Harff, Jan; Lemke, Wolfram (2005): A new relative sea-level curve for the Wismar Bay, N-German Baltic coast. Meyniana, 57, 5-35
DOI: 10.5281/zenodo.15751835
title: Game Character Art Comparison: Human vs. AI

description: This is the dataset of a questionnaire collecting the perception and anticipated player experience towards game character design, with a a 2×2 factorial design to explore the effects of (1) actual creator and (2) labeled creator on multiple dimensions of player perception, including aesthetic appeal and anticipated psychological experience.
DOI: 10.1594/pangaea.357057
title: Paleoecological investigation of Hessische Senke at site RKS_13_14
DOI: 10.1594/pangaea.357059
title: Paleoecological investigation of Hessische Senke at site RKS_17_18
DOI: 10.5281/zenodo.15751834
title: Game Character Art Comparison: Human vs. AI

description: This is the dataset of a questionnaire collecting the perception and anticipated player experience towards game character design, with a a 2×2 factorial design to explore the effects of (1) actual creator and (2) labeled creator on multiple dimensions of player perception, including aesthetic appeal and anticipated psychological experience.
DOI: 10.1594/pangaea.124318
title: Age determination on sediment core BP01-62/06
DOI: 10.1594/pangaea.376353
title: Age determinations on peat profile Kunyok
DOI: 10.1594/pangaea.720972
title: (Table 2) K-Ar results from DSDP Hole 34-321
DOI: 10.1594/pangaea.912805
title: Optically stimulated luminescence (OSL) dating results for sediment core KK12-2, Lake Karakul, Tajikistan
DOI: 10.1594/pangaea.726787
title: (Table 1) Age determination of profiles from Labaz Lake area
DOI: 10.1594/pangaea.856905
title: (Table 3) AMS Radiocarbon ages of South Pacific sediment cores

description: For prediction of range of 14C ages, we assigned the following l4C ages to the P. wuellerstorfi found at the core depth from which the radiocarbon sample was taken. 4.5 ka to the Holocene, an average age of sediment mixed layer (Penget al., 1979), 18 ka to LGM, 11 ka to deglacial stage, and 40 ka to marine isotopic stage 3. P. wuellerstorfi with intermediate d18OO values could not be classified as either Holocene or LGM and were assumed to be of deglacial age or stage 3 age. Two sets of calculations were done: one with all intermediate value P. wuellerstorfi assumed to be from deglacial stage (this gives the lower age limit) and another with all assumed to be from stage 3 (the upper limit). Radiocarbon measurements were made on shells larger than 300 ftm at the National Science Foundation-Arizona Accelerator Mass Spectrometer (AMS) Facility at the University of Arizona. All dates are reservoir- age corrected using the natural 14C reservoir ages of Pacific surface waters (Bard, 1988).
DOI: 10.1594/pangaea.865053
title: Age determinations of Witpan sediment sequence (Northern Cape, South Africa) by 14C dating of TOC bulk samples
DOI: 10.1594/pangaea.794521
title: (Table 2) Phosphorus components, CaCO3 and biogenic opal in sediments of ODP Hole 167-1011B
DOI: 10.1594/pangaea.650330
title: Age determination of profile Langtang_3
DOI: 10.1594/pangaea.856936
title: (Table 1) Age determination of sediment cores of the Labrador Sea

description: A close look at the sedimentology of Heinrich event 4 from the northwest Labrador Sea indicates that an extended ice margin, perhaps greater than before Heinrich events 1 or 2 (H-1 and H-2), existed in the Hudson Strait region pre-Heinrich event 4 (H-4) and, that on the basis of characteristics of the sediment unit, Heinrich event-4 was different than Heinrich events 1 or 2 (i.e., larger ice sheet collapse(?), longer duration(?), "dirtier" icebergs(?)). Other data from across the southern and eastern margin of the Laurentide Ice Sheet, as well as Greenland and the North Atlantic, support this interpretation, possibly indicating a relative mid-Wisconsin glacial maximum pre-Heinrich event 4. Many of these data also indicate that Heinrich event 4 (35 ka) resulted in serious climatic and oceanographic reorganizations. We suggest that Heinrich event 4 gutted the Hudson Strait, leaving it devoid of ice for Heinrich event 3. We further hypothesize that Heinrich event 3 did not originate from axial ice transport along the Hudson Strait; thus Heinrich event 3 may be more analogous to the proposed northward advancing ice from Ungava Bay during Heinrich event 0 than to the more typical down-the-strait flow during H-1, H-2, and H-4. Consequently, the climatic and oceanographic impacts resulting from Heinrich events are highly susceptible to the type, origin, and magnitude of ice sheet collapse, something which varied per Heinrich event during the last glacial period.
description: Dates are from Manley and Jennings (1996).
description: Supplement to: Kirby, Mathew E; Andrews, John T (1999): Mid-Wisconsin Laurentide ice sheet growth and decay: Implications for Heinrich events 3 and 4. Paleoceanography, 14(2), 211-223
DOI: 10.1594/pangaea.55293
title: Radiocarbon age determinations of coral and reef cores from the Philippines off North Bohol and Olango

description: Nine holes were drilled with a submersible hydraulic drill into the slopes and reef flats of the Caubyan and Calituban reefs as well as of Olango Flat. The maximum depth of core penetration was 11 m. 14C ages showed that the Caubyan and Calituban reefs were formed within the last 6,000 years. Corals settled on a pre-existing relief parallel to the island of Bohol, building a framework for other carbonate-producing organisms. The reef flat south of Olango has a different structure. Formation took place during a Pleistocene high sea level, e.g. 125,000 years ago.
description: Supplement to: Grobe, Hannes; Willkomm, Horst; Wefer, Gerold (1985): Internal structure and origin of the Double Reefs of North Bohol and the Olango Reef Flat (Philippines). The Philippine Scientist, 22, 83-94
DOI: 10.1594/pangaea.865040
title: Age determinations of Omongwa Pan sediment sequence (Omaheke Region, Namibia) by 14C dating of TOC bulk samples
DOI: 10.1594/pangaea.59562
title: Stable isotope analysis on sediment core GIK23055-2
DOI: 10.1594/pangaea.740901
title: Age determination of sediment core VEAU, Tourbière les Veaux, Switzerland

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.735799
title: (Table 2) Age determination of sediment profile PS2837-5/6

description: dated material: Neogloboquadrina pachyderma (s.)
DOI: 10.1594/pangaea.745669
title: (Table 3) Radiocarbon ages of Laptev Sea sediments from marine biogenic calcite of bivalves
DOI: 10.1594/pangaea.835443
title: (Table 2) Age determination of sediment core JR179_GC479
DOI: 10.1594/pangaea.835442
title: (Table 2) Age determination of sediment core JR179_GC475
DOI: 10.1594/pangaea.87367
title: (Table 2) Age determination of sediment core PS51/141-2
DOI: 10.1594/pangaea.87366
title: (Table 2) Age determination of sediment core PS51/135-4
DOI: 10.1594/pangaea.389056
title: (Table 1) Age determinations on sediment core DF79.009-GB
DOI: 10.1594/pangaea.860314
title: (Table 1) Radiocarbon dates as obtained from the Bacon modeling of sediment core GeoB13813-4
DOI: 10.1594/pangaea.357142
title: Paleoecological investigation of Hessische Senke at site RKS_15_16
DOI: 10.1594/pangaea.124634
title: Dated age of sediment core TT013_88
DOI: 10.1594/pangaea.385641
title: Age determinations on sediment core PG1200
DOI: 10.1594/pangaea.186272
title: Radiocarbon age determinations on sediment core V23-82
DOI: 10.1594/pangaea.323490
title: Age determination of sediment core GT04-388GC
DOI: 10.1594/pangaea.89471
title: (Table 1) Age determinations on sediment core M44/1 GeoTü KL71

description: reservoir age correction 346+/-60 years
DOI: 10.1594/pangaea.808699
title: Carbon14 and Pb210 ages of sediment core GeoB12309-5
DOI: 10.1594/pangaea.87364
title: (Table 2) Age determination of sediment core PS51/118-2
DOI: 10.1594/pangaea.735800
title: (Table 2) Age determination of sediment profile PS2876-1/2

description: dated material: Neogloboquadrina pachyderma (s.)
DOI: 10.1594/pangaea.761269
title: Radiocarbon datings of mollusk shells, sedimentation rates and accumulation rates of sediment matter in core PS2718-6

description: A bottom sediment core about 8 m long sampled in the eastern Kara Sea near the entrance to the Vil'kitsky Strait was studied. An age model was constructed based on four 14C datings obtained from by thy accelerating mass spectrometry method. Results of grain size, chemical, mineralogical, and foraminiferal analyses were adjusted to the model. A paleoceanological interpretation of these data together with paleoclimatic data on the Bol'shevik Island located in the neighborhood was performed.
description: Supplement to: Levitan, Mikhail A; Arnold, M; Burtman, M V; Ivanova, Elena V; Marina, Mariya M (2000): On the Holocene sedimentation history of the eastern Kara Sea. Translated from Okeanologiya, 2000, 40(4), 614-620, Oceanology, 40(4), 577-582
DOI: 10.1594/pangaea.422569
title: (Table 1c) Age control points of sediment core GeoB5804-4, Gulf of Aqaba, Northern Red Sea

description: Calibrated Age, Calendar Years B.P.: 0=after A.D. 1950
DOI: 10.1594/pangaea.823115
title: (Supplementary Table S2) Compiled radiocarbon data. Planktic and benthic radiocarbon dates, B-P offset and Delta14C estimates from core MD07-3088
DOI: 10.1594/pangaea.835437
title: (Table 2) Age determination of sediment core JR179_BC472
DOI: 10.1594/pangaea.117015
title: Dated age of sediment core TN047-7B-MC
DOI: 10.1594/pangaea.847814
title: (Table 2) Age determination of sediment cores from the continental shelf of Mac Roberston Land, East Antarctica

description: Geochemical records are presented for five sediment cores from basins on the continental shelf of Mac. Robertson Land, East Antarctica. The cores contain 2-4 m thick sequences of hemipelagic, siliceous mud and ooze (SMO) deposited under seasonally open marine conditions. The inner and middle shelf SMO sequences are massive dark olive green material, whereas the outer shelf SMO sequences are dark olive material interspersed with light olive green layers ~1-10 cm thick. The biogenic material is dominated by marine diatoms including Fragilariopsis curta, Fragilariopsis cylindrus, and Chaetoceros spp. in the dark-colored SMO and Corethron criophilum in the light-colored layers. Radiocarbon dates suggest that the cores provide continuous accumulation records extending from &lt; 1 kyr before present (B.P.) back as far as 4-15 kyr B.P., with estimated accumulation rates of 0.07-5 mm/yr. The three core records from the middle and outer shelf suggest six episodes of increased accumulation of biogenic material at ~5.5 kyr B.P. (all three cores), 1, 2, and 6.2 kyr B.P. (two of the three cores), and 3.8 and 10.8 kyr B.P. (one core), most of which coincide with Corethron layers. We interpret these features as the result of enhanced diatom production over the outer shelf, possibly related to climatic warm periods. The absence of such features in the inner shelf core records is thought to reflect a relatively constant level of seasonal diatom production in adjacent waters maintained by a coastal polynya.
description: Supplement to: Sedwick, Peter; Harris, Peter Townsend; Robertson, Lisette G; McMurtry, Gary M; Cremer, Maximilian D (2001): Holocene sediment records from the continental shelf of Mac. Robertson Land, East Antarctica. Paleoceanography, 16(2), 212-225
DOI: 10.1594/pangaea.133673
title: Radiocarbon ages of pollen profile SAUBORST

description: pollen zones after Firbas V-X
DOI: 10.1594/pangaea.847652
title: (Appendix I) Stable isotope measurements of benthic and planktonic foraminifera in sediment core MD99-2269

description: Isotopic analysis was performed at the Leibniz-Laboratory for radiometric dating and stable isotope research at Christian-Albrechts-University Kiel, Germany using a Finnigan MAT 251 mass spectrometer with an on-line coupled Kiel Carbon device. First 13 columns are raw data as reported from the Kiel laboratory, samples with warnings and/or remarks are " shown with full remarks at the end of this Appendix. The ± errors in the data sheets is the internal error. Each sample is measured ten times (in a succession of reference gas, sample gas, reference gas, sample gas etc.). The internal error is the SD of the ten measurements of the sample gas. If the sample size is very" small then the internal error will be increased. The external error (also called the analytical error) measures how accurately carbonate standards can be reproduced (by comparison of the resulting values which base each on ten internal measurements). Different carbonates are used as standards and measured regularly each day in the lab and results checked for performance of the mass spec, but generally not sent to the customers. For a sample &gt; 15 µg the external error is better than 0.04 per mil (13C) and 0.06 per mil (18O). For smaller sizes the error is higher, going up to 0.2 per mil for &lt; 8 µg. However, these small sample sizes are signed with warnings in the data sheets. For the earliest sample batch of Nps two morphotypes were run separately; Nps quadrate form (Npsq) and Nps normal form (Npsn). Sample depth is shown on both original depth scale (cm*) and void corrected depth scale (cm). For depths with multiple measurements an average was used for data analysis, the average is not shown in this Appendix, only the separate original values.