cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.969418
title: Dead Sea density during interglacials MIS 7c, 7a, 5e and 5c measured from halite fluid inclusions, and deduced chemical composition, relative volume and precipitated halite

description: The rain regime in the Eastern Mediterranean is primarily controlled by Mediterranean winter cyclonic systems. The density, chemical composition and relative volume of the Dead Sea responds sensitively to hydrological changes, and can be used to track the evolution of the Mediterranean hydroclimate during the late Quaternary. Halite fluid inclusions are exquisite aliquots of the lake brine, and can therefore be used to reconstruct these variables. Here, we reconstruct the Dead Sea lake density at 25 °C and 1 atmosphere from the measured sound velocity in halite fluid inclusions (FIs) of the deep ICDP core 5017-1-A during Marine Isotope Stages (MIS) 7c, 7a, 5e and 5c. Combining the density data with published pore fluid chemical composition data and evaporation simulations with the software PhreeqC v.3, we reconstruct the lake's chemical composition, relative volume and precipitated halite. The dataset presents values for each FI; averages can be calculated for each sample or group of samples located within a few 10s cm in the core (see paper referenced with this dataset, Guillerm et al., 2023). For each period MIS 7c, 7a, 5e and 5c, the reported lake volume is a value relative to the average of the first (deepest) sample of the given period. Observed and calculated halite thicknesses are cumulated from the beginning of each period MIS 7c, 7a, 5e and 5c.
DOI: 10.1594/pangaea.878108
title: Heat flow data at station SO247_55-7
DOI: 10.1594/pangaea.910809
title: UP10 proxy analysis of sediment core MD99-2343
DOI: 10.1594/pangaea.934575
title: PIP25 indexes and Spring/Summer sea ice concentration (Sp/SuSIC) (Estuarine samples included)

description: The PIP25 indexes calculated by IP25 and phytoplankton biomarkers (Brassicasterol, Dinosterol, HBI-III) in the East Siberian Sea. The calculation methods based on Mueller et al., 2015.
DOI: 10.5281/zenodo.18285847
title: Luziola peruviana Juss. ex J.F.Gmel. In: Marchesi E., Mailhos A. & Bonifacino J.M. (Eds.). Flora Uruguaya: Flora Vascular del Uruguay. ISSN 3121-2050, V. 1.0.

description: Citable snapshot. Includes PDF and CSV of collections. Date: January 13th, 2026 at 16:49
DOI: 10.5281/zenodo.18285848
title: Luziola peruviana Juss. ex J.F.Gmel. In: Marchesi E., Mailhos A. & Bonifacino J.M. (Eds.). Flora Uruguaya: Flora Vascular del Uruguay. ISSN 3121-2050, V. 1.0.

description: Citable snapshot. Includes PDF and CSV of collections. Date: January 13th, 2026 at 16:49
DOI: 10.1594/pangaea.934573
title: Bulk parameters and biomarker data from surface sediment across the East Siberian Sea and the west Chukchi Sea

description: A dataset of 42 collected surface sediment samples from the East Siberian Sea by analysis of Arctic sea ice (IP25) and open water phytoplankton biomarkers (Brassicasterol, Dinosterol, HBI-III and HBI-IV). Terrigenous sterols (campesterol and β-sitosterol) data in this region are also included in the dataset. All biomarkers are based on TOC calculations.
DOI: 10.1594/pangaea.867316
title: Pollen and non-pollen palynomorph counts of sediment core KIN2 from the Sea of Galilee, northern Israel

description: Despite ongoing discussions on hydroclimatic conditions in the southern Levant during the Last Glacial, detailed knowledge about the Levantine paleovegetation, which is an important indicator for the paleoclimate, is limited. To investigate the paleovegetation in northern Israel, we analyzed the pollen assemblage of a sediment core that was drilled at the Ohalo II archaeological site on the southwestern shore of the Sea of Galilee (Lake Kinneret). We refined the lithology and the age-depth model with the help of five new radiocarbon dates. The core comprises a continuous sediment profile of mainly laminated authigenic calcites and detrital material that deposited between ca. 28,000 and 22,500 years before present, when the Sea of Galilee rose above the modern lake level stand and temporarily merged with Lake Lisan, the precursor of the Dead Sea. The well-dated and high-resolution pollen record suggests that steppe vegetation with grasses, other herbs, and dwarf shrubs predominated in northern Israel during the investigated period. In contrast to the Holocene, there was no continuous vegetation belt of the Mediterranean biome in the vicinity of the Sea of Galilee. Mediterranean elements such as deciduous oaks only occurred in limited amounts and were probably patchily distributed. These results disagree with previous pollen-based hypotheses from the region that assumed the spread of Mediterranean forest during glacial periods. While the pollen data may indicate semiarid conditions in northern Israel and give no evidence of increased effective moisture, previous hydroclimatic studies suggested increased precipitation rates that are consistent with high lake levels (Sea of Galilee/Lake Lisan). Thus, we discuss factors influencing the pollen assemblage and the plant cover.
description: Supplement to: Miebach, Andrea; Chen, Chunzhu; Schwab, Markus J; Stein, Mordechai; Litt, Thomas (2017): Vegetation and climate during the Last Glacial high stand (ca. 28-22 ka BP) of the Sea of Galilee, northern Israel. Quaternary Science Reviews, 156, 47-56
DOI: 10.1594/pangaea.887715
title: (Figure 2-4) Physical oceanography, nutrients and lipid biomarkers in surface waters of the northeastern East China Sea and the western Tsushima Strait
DOI: 10.1594/pangaea.910798
title: Stable isotope ratios of benthic foraminifera from sediment core HER_GC_UB06
DOI: 10.1594/pangaea.910804
title: Sedimentation rate of sediment core MD95-2043
DOI: 10.1594/pangaea.910805
title: Sedimentation rate of sediment core MD99-2343
DOI: 10.1594/pangaea.910808
title: TOC content of sediment core MD99-2343
DOI: 10.1594/pangaea.763201
title: Swath sonar bathymetry during SONNE cruise SO182 with links to multibeam raw data files

description: Multibeam data were collected during R/V Sonne cruise SO182 leading to the Transkei Basin, Agulhas Ridge and Agulhas Plateau. Multibeam sonar system was Kongsberg Simrad EM-120. Data are unprocessed and may contain outliers and blunders and should not be used for grid calculations and charting projects without further editing. The raw multibeam sonar data in Simrad multibeam processing format (*.all) were recorded with Simrad SIS software running on UNIX operating system. 1660 files are compressed with GZIP to size of 5.93 GB. One dataset contains a measurement period of half an hour. Simrad data files can be processed using the software packages CARIS HIPS/SIPS or with the open source software package MB-System (http://www.ldeo.columbia.edu/res/pi/MB-System/).
DOI: 10.1594/pangaea.942420
title: Multibeam bathymetry raw data (Kongsberg EM710 entire dataset) of RV SONNE during cruise SO247

description: Multibeam bathymetry raw data using the ship's own Kongsberg EM 710 multibeam echosounder was not continuously recorded during RV SONNE cruise SO247. Data was recorded on 2 days between 2016-03-27 and 2016-04-21. This dataset contains a survey east of New Zealand (North Island) covering parts of the continental slope. The approximate average depth of the entire dataset is around 800m.The data are archived at the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschifffahrt und Hydrographie, BSH) and provided to PANGAEA database for data curation and publication. Ancillary sound velocity profiles (SVP) files from the cruise are archived at the BSH and added to this dataset. However, also data analysis of the multibeam raw data revealed that SVP has been changed during the survey.This publication is conducted within the efforts of the German Marine Research Alliance in the core area "Data management and Digitalization" (Deutsche Allianz Meeresforschung, DAM).Data are unprocessed and therefore contains incorrect depth measurements (artifacts) without further processing. Note that refraction errors can be expected due to the lack of proper SVP. Overall, it appears that the data quality is rather moderate since the gridded hillshade data showed partially some artifacts.Data can be processed e.g. with the open source software package MB-System (Caress, D. W., and D. N. Chayes, MB-System: Mapping the Seafloor, http://www.mbari.org/products/research-software/mb-system/, 2022).
description: These data should not be used for navigational purposes.Data publishing was realized by Daniel Damaske, MARUM - Center for Marine Environmental Sciences (University Bremen).
DOI: 10.1594/pangaea.942421
title: Water column raw data (Kongsberg EM710 entire dataset) of RV SONNE during cruise SO247

description: Water column raw data using the ship's own Kongsberg EM 710 multibeam echosounder was not continuously recorded during RV SONNE cruise SO247. Data was recorded only on 2016-04-21. This dataset contains a survey east of New Zealand (North Island) covering parts of the continental slope.The data are archived at the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschifffahrt und Hydrographie, BSH) and provided to PANGAEA database for data curation and publication. Ancillary sound velocity profiles (SVP) files from the cruise are archived at the BSH and archived at the corresponding multibeam raw dataset https://doi.org/10.1594/PANGAEA.942420.This publication is conducted within the efforts of the German Marine Research Alliance in the core area "Data management and Digitalization" (Deutsche Allianz Meeresforschung, DAM).
description: These data should not be used for navigational purposes.Data publishing was realized by Daniel Damaske, MARUM - Center for Marine Environmental Sciences (University Bremen).
DOI: 10.1594/pangaea.942415
title: Multibeam bathymetry raw data (EM 120 echosounder entire dataset) of RV MARIA S. MERIAN during cruise MSM15/3

description: Multibeam bathymetry raw data using the ship's own Kongsberg (Simrad) EM 120 multibeam echosounder was not continuously recorded during RV MARIA S. MERIAN cruise MSM15/3. Data was recorded on 2 days between 2010-06-25 and 2010-06-27. This dataset contains a survey south of Sicily and an elongated extend of this survey to the east. The approximate average depth of the entire dataset is around 3200m.The data are archived at the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschifffahrt und Hydrographie, BSH) and provided to PANGAEA database for data curation and publication. No ancillary sound velocity profiles (SVP) files from the cruise are archived at the BSH, thus no SVP files are added to this dataset. However, also data analysis of the multibeam raw data revealed that SVP has been changed once during the survey.This publication is conducted within the efforts of the German Marine Research Alliance in the core area "Data management and Digitalization" (Deutsche Allianz Meeresforschung, DAM).Data are unprocessed and therefore contains incorrect depth measurements (artifacts) without further processing. Note that refraction errors can be expected due to the lack of proper SVP. Overall, it appears that the data quality is rather good since the gridded hillshade data showed relatively few obstacles. Nevertheless, it seems that data has been cut off in some areas. Data can be processed e.g. with the open source software package MB-System (Caress, D. W., and D. N. Chayes, MB-System: Mapping the Seafloor, http://www.mbari.org/products/research-software/mb-system/, 2022).
description: These data should not be used for navigational purposes.Data publishing was realized by Daniel Damaske, MARUM - Center for Marine Environmental Sciences (University Bremen).
DOI: 10.1594/pangaea.868449
title: Physical and chemical properties of sediment core GeoB14403-8
DOI: 10.1594/pangaea.910806
title: TOC content of sediment core HER_GC_UB06
DOI: 10.1594/pangaea.910728
title: Benthic foraminiferal raw counts of sediment core MD95-2043
DOI: 10.1594/pangaea.942419
title: Water column raw data (Kongsberg EM 122 entire dataset) of RV SONNE during cruise SO247

description: Water column raw data using the ship's own Kongsberg EM 122 multibeam echosounder was not continuously recorded during RV SONNE cruise SO247. Data was recorded on 22 days between 2016-03-27 and 2016-04-25. This dataset contains a survey east of New Zealand (North Island) covering mostly the continental slope.The data are archived at the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschifffahrt und Hydrographie, BSH) and provided to PANGAEA database for data curation and publication. Ancillary sound velocity profiles (SVP) files from the cruise are archived at the BSH and archived at the corresponding multibeam raw dataset https://doi.org/10.1594/PANGAEA.942418.This publication is conducted within the efforts of the German Marine Research Alliance in the core area "Data management and Digitalization" (Deutsche Allianz Meeresforschung, DAM).
description: These data should not be used for navigational purposes.Data publishing was realized by Daniel Damaske, MARUM - Center for Marine Environmental Sciences (University Bremen).
DOI: 10.1594/pangaea.942418
title: Multibeam bathymetry raw data (Kongsberg EM 122 entire dataset) of RV SONNE during cruise SO247

description: Multibeam bathymetry raw data using the ship's own Kongsberg EM 122 multibeam echosounder was not continuously recorded during RV SONNE cruise SO247. Data was recorded on 25 days between 2016-03-27 and 2016-04-25. This dataset contains a survey east of New Zealand (North Island) covering mostly the continental slope. The approximate average depth of the entire dataset is around 1800m.The data are archived at the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschifffahrt und Hydrographie, BSH) and provided to PANGAEA database for data curation and publication. Ancillary sound velocity profiles (SVP) files from the cruise are archived at the BSH and added to this dataset. However, also data analysis of the multibeam raw data revealed that SVP has been changed during the survey.This publication is conducted within the efforts of the German Marine Research Alliance in the core area "Data management and Digitalization" (Deutsche Allianz Meeresforschung, DAM).Data are unprocessed and therefore contains incorrect depth measurements (artifacts) without further processing. Note that refraction errors can be expected due to the lack of proper SVP. Overall, it appears that the data quality is rather good since the gridded hillshade data showed relatively few obstacles. Data can be processed e.g. with the open source software package MB-System (Caress, D. W., and D. N. Chayes, MB-System: Mapping the Seafloor, http://www.mbari.org/products/research-software/mb-system/, 2022).
description: These data should not be used for navigational purposes.Data publishing was realized by Daniel Damaske, MARUM - Center for Marine Environmental Sciences (University Bremen).
DOI: 10.1594/pangaea.871945
title: Geophysical core log data (MSCL) of volcanoclastic failure surfaces of sediment core GeoB14401-5, NE Gela Basin, Strait of Sicily, Mediterranean Sea
DOI: 10.1594/pangaea.973628
title: 2D single-channel seismic reflection raw data (Sparker source entire dataset) of HSV FISÁLIA cruise in 2020, Southwest Algarve shelf, North Atlantic Ocean

description: This dataset contains raw reflection seismic profiles from the southwestern Algarve shelf, Portugal. The profiles were recorded in January 2020 during a campaign onboard HSV FISÁLIA of the Portuguese Navy for project OnOff "Coupling onshore and offshore tsunami record: complementary tools for a broader perspective on tsunami events", funded by FCT (Portuguese Foundation for Science and Technology) grant PTDC/CTAGEO/28941/2017. The dataset compiles all reflection seismic profiles recorded with a centipede sparker source designed by RCMG at Gent University, Belgium, and a SIG single-channel streamer receiving unit. The center frequency of the signal was around 600 Hz, with a sampling frequency of 16 kHz, a shot interval of 0.5 s, and an approximate vertical resolution of ~50 cm. The dataset contains raw data as .NAV (with coordinates), .PRM and .SEG files.
DOI: 10.21227/kh0x-8h15
title: "Mobile Decision Center-Assisted Cooperative Scheduling of Time-dependent UAVs,Vehicles and Workers for Crowdsensing"

description: "Dataset"
DOI: 10.1594/pangaea.973629
title: 2D single-channel seismic reflection processed data (Sparker source entire dataset) of HSV FISÁLIA cruise in 2020, Southwest Algarve shelf, North Atlantic Ocean

description: This dataset contains processed reflection seismic profiles from the southwestern Algarve shelf, Portugal. The profiles were recorded in January 2020 during a campaign onboard HSV FISÁLIA of the Portuguese Navy for project OnOff "Coupling onshore and offshore tsunami record: complementary tools for a broader perspective on tsunami events", funded by FCT (Portuguese Foundation for Science and Technology) grant PTDC/CTAGEO/28941/2017. The dataset compiles all reflection seismic profiles recorded with a centipede sparker source designed by RCMG at Gent University, Belgium, and a SIG single-channel streamer receiving unit. The center frequency of the signal was around 600 Hz, with a sampling frequency of 16 kHz, a shot interval of 0.5 s, and an approximate vertical resolution of ~50 cm. Basic post-processing included burst noise removal, amplitude correction, bandpass filtering, and top muting. The dataset contains processed data as Label_processed.sgy files with Label_pick.txt files for seafloor picks.
DOI: 10.1594/pangaea.973630
title: Sediment echosounder processed data (Innomar SES-2000 entire dataset) of HSV FISÁLIA cruise in 2020, Southwest Algarve shelf, North Atlantic Ocean

description: This dataset contains processed sub-bottom profiles from the southwestern Algarve shelf, Portugal. The profiles were recorded in January 2020 during a campaign onboard HSV FISÁLIA of the Portuguese Navy for project OnOff "Coupling onshore and offshore tsunami record: complementary tools for a broader perspective on tsunami events", funded by FCT (Portuguese Foundation for Science and Technology) grant PTDC/CTAGEO/28941/2017. The dataset compiles all sub-bottom profiles recorded with an Innomar SES-2000 quattro system. This system consists of four individual transducers functioning as seismic sources and receivers. It was used in single-beam mode with a sampling frequency of 8 kHz. The shot interval during the survey was not set to a specific value but automatically optimized by the system as a function of the water depth. As a result, the ping rate changed slightly around 7-8 pings/s. The theoretical vertical resolution was around 5 cm. Basic post-processing included burst noise removal, amplitude correction, swell filtering, and top muting. The dataset contains processed data as Label_processed.sgy files with Label_pick.txt files for seafloor picks.
DOI: 10.1594/pangaea.878099
title: Heat flow data at station SO247_55-17

description: Depth, sediment = Penetration depth
DOI: 10.1594/pangaea.973631
title: Sediment echosounder raw data (Innomar SES-2000 entire dataset) of HSV FISÁLIA cruise in 2020, Southwest Algarve shelf, North Atlantic Ocean

description: This dataset contains raw sub-bottom profiles from the southwestern Algarve shelf, Portugal. The profiles were recorded in January 2020 during a campaign onboard HSV FISÁLIA of the Portuguese Navy for project OnOff "Coupling onshore and offshore tsunami record: complementary tools for a broader perspective on tsunami events", funded by FCT (Portuguese Foundation for Science and Technology) grant PTDC/CTAGEO/28941/2017. The dataset compiles all sub-bottom profiles recorded with an Innomar SES-2000 quattro system. This system consists of four individual transducers functioning as seismic sources and receivers. It was used in single-beam mode with a sampling frequency of 8 kHz. The shot interval during the survey was not set to a specific value but automatically optimized by the system as a function of the water depth. As a result, the ping rate changed slightly around 7-8 pings/s. The theoretical vertical resolution was around 5 cm. The dataset contains raw data as .txt (with coordinates), .PRM, .raw and .sgy.
DOI: 10.1594/pangaea.844871
title: Major element analysis of selected glass shards from marine marker tephra Y-7 in core GeoB14403-8

description: Geocode is given in composite depth (mcd).
DOI: 10.1594/pangaea.878101
title: Heat flow data at station SO247_55-3

description: Depth, sediment = Penetration depth
DOI: 10.1594/pangaea.878103
title: Heat flow data at station SO247_55-5

description: Depth, sediment = Penetration depth
DOI: 10.1594/pangaea.878096
title: Heat flow data at station SO247_55-14

description: Depth, sediment = Penetration depth
DOI: 10.1594/pangaea.878104
title: Heat flow data at station SO247_55-6

description: Depth, sediment = Penetration depth
DOI: 10.1594/pangaea.820625
title: Physical/chemical properties and stable oxygen and carbon isotope records of sediment core GeoB14403-1
DOI: 10.1594/pangaea.934574
title: PIP25 indexes and Spring/Summer sea ice concentration (Sp/SuSIC) (Estuarine samples excluded)

description: The PIP25 indexes calculated by IP25 and phytoplankton biomarkers (Brassicasterol, Dinosterol, HBI-III) in the East Siberian Sea. To better understand the riverine influence, we compared the data set with and without samples that influenced by riverine input. In this dataset, the estuarine samples (surface salinity &lt; 25) are removed. The calculation methods based on Mueller et al., 2015.
DOI: 10.1594/pangaea.944829
title: Age model of lateglacial ICDP core 5017-1-A

description: This dataset provides the results from Bayesian age depth modelling in OxCal for ICDP core 5017-1-A, retrieved from the deep northern Dead Sea basin in 2010/11, for the last glacial-interglacial transition between ~101 and 88.5 m sediment depth below lake floor (ca. 17-11.5 ka BP). The model was performed in OxCal v.4.4 using a P_Sequence (1,1,C(-2,2)) (Ramsey 2008; Ramsey 2009; Ramsey and Lee 2013) and includes three tephrochronological ages from Neugebauer et al. (2021) and three radiocarbon ages from Kitagawa et al. (2017).
DOI: 10.1594/pangaea.987461
title: Grain size analysis of DSDP Site 10-95
DOI: 10.1594/pangaea.984845
title: AMS radiocarbon dates from Baltic Sea sediment core EMB201/13-4

description: Four radiocarbon samples were taken from the same depth intervals as the identified 1-cm thick cryptotephra isochrons in core EMB201/13-4. The four accelerator mass spectrometer (AMS) 14C ages were obtained from the humic acid fraction of bulk organic matter samples and measured in the Beta Analytic Radiocarbon Dating Laboratory. Uncalibrated and calibrated radiocarbon ages are provided. For comparison with previous studies, calibration followed the published methodology in the Baltic Sea (e.g. Moros et al. 2020) of subtracting the global-average marine reservoir age of 400 years (from IntCal13) before applying OxCal v4.4 (Ramsey, 2009) and IntCal20 (Reimer et al., 2020). Calibrated ages are given as median and with both, 1σ and 2σ uncertainties.