cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.911807
title: Photographs of tiles at time series station Liliguapi, Paso Comau, Patagonia, Chile, at 2012-02-04

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). If you intend to work with this data set please do not hesitate to contact the authors to discuss cooperation possibilities.The backside of common tiles was selected as substrate. Tiles have the following dimensions, length:height = 15:15 cm (225 cm²) and are fixed with two screws and washers to a PVC frame. The latter is connected to the wall with a stainless steel bolt. A square pattern on the tiles allows easy analysis of the percentage cover of species. This pattern has a size of 1.75 cm between the middle of adjacent ridges.
DOI: 10.1594/pangaea.911808
title: Photographs of tiles installed at X-Huinay, Comau Fjord, Chile, at 2016-03-31

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). If you intend to work with this data set please do not hesitate to contact the authors to discuss cooperation possibilities.The backside of common tiles was selected as substrate. Tiles have the following dimensions, length:height = 15:15 cm (225 cm²) and are fixed with two screws and washers to a PVC frame. The latter is connected to the wall with a stainless steel bolt. A square pattern on the tiles allows easy analysis of the percentage cover of species. This pattern has a size of 1.75 cm between the middle of adjacent ridges.
DOI: 10.1594/pangaea.911809
title: Photographs of tiles installed at X-Huinay, Comau Fjord, Chile, at 2012-02-07

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). If you intend to work with this data set please do not hesitate to contact the authors to discuss cooperation possibilities.The backside of common tiles was selected as substrate. Tiles have the following dimensions, length:height = 15:15 cm (225 cm²) and are fixed with two screws and washers to a PVC frame. The latter is connected to the wall with a stainless steel bolt. A square pattern on the tiles allows easy analysis of the percentage cover of species. This pattern has a size of 1.75 cm between the middle of adjacent ridges.
DOI: 10.1594/pangaea.911810
title: Photographs of tiles installed at X-Huinay, Comau Fjord, Chile, at 2012-01-27

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). If you intend to work with this data set please do not hesitate to contact the authors to discuss cooperation possibilities.The backside of common tiles was selected as substrate. Tiles have the following dimensions, length:height = 15:15 cm (225 cm²) and are fixed with two screws and washers to a PVC frame. The latter is connected to the wall with a stainless steel bolt. A square pattern on the tiles allows easy analysis of the percentage cover of species. This pattern has a size of 1.75 cm between the middle of adjacent ridges.
DOI: 10.1594/pangaea.911811
title: Photographs of tiles installed at X-Huinay, Comau Fjord, Chile, at 2012-01-31

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). If you intend to work with this data set please do not hesitate to contact the authors to discuss cooperation possibilities.The backside of common tiles was selected as substrate. Tiles have the following dimensions, length:height = 15:15 cm (225 cm²) and are fixed with two screws and washers to a PVC frame. The latter is connected to the wall with a stainless steel bolt. A square pattern on the tiles allows easy analysis of the percentage cover of species. This pattern has a size of 1.75 cm between the middle of adjacent ridges.
DOI: 10.1594/pangaea.911812
title: Photographs of tiles installed at X-Huinay, Comau Fjord, Chile, at 2011-12-10

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). If you intend to work with this data set please do not hesitate to contact the authors to discuss cooperation possibilities.The backside of common tiles was selected as substrate. Tiles have the following dimensions, length:height = 15:15 cm (225 cm²) and are fixed with two screws and washers to a PVC frame. The latter is connected to the wall with a stainless steel bolt. A square pattern on the tiles allows easy analysis of the percentage cover of species. This pattern has a size of 1.75 cm between the middle of adjacent ridges.
DOI: 10.1594/pangaea.911813
title: Photographs of tiles installed at X-Huinay, Comau Fjord, Chile, at 2012-01-18

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). If you intend to work with this data set please do not hesitate to contact the authors to discuss cooperation possibilities.The backside of common tiles was selected as substrate. Tiles have the following dimensions, length:height = 15:15 cm (225 cm²) and are fixed with two screws and washers to a PVC frame. The latter is connected to the wall with a stainless steel bolt. A square pattern on the tiles allows easy analysis of the percentage cover of species. This pattern has a size of 1.75 cm between the middle of adjacent ridges.
DOI: 10.1594/pangaea.911814
title: Photographs of tiles installed at X-Huinay, Comau Fjord, Chile, at 2011-07-08

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). If you intend to work with this data set please do not hesitate to contact the authors to discuss cooperation possibilities.The backside of common tiles was selected as substrate. Tiles have the following dimensions, length:height = 15:15 cm (225 cm²) and are fixed with two screws and washers to a PVC frame. The latter is connected to the wall with a stainless steel bolt. A square pattern on the tiles allows easy analysis of the percentage cover of species. This pattern has a size of 1.75 cm between the middle of adjacent ridges.
DOI: 10.1594/pangaea.911815
title: Photographs of tiles installed at X-Huinay, Comau Fjord, Chile, at 2010-11-12

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). If you intend to work with this data set please do not hesitate to contact the authors to discuss cooperation possibilities.The backside of common tiles was selected as substrate. Tiles have the following dimensions, length:height = 15:15 cm (225 cm²) and are fixed with two screws and washers to a PVC frame. The latter is connected to the wall with a stainless steel bolt. A square pattern on the tiles allows easy analysis of the percentage cover of species. This pattern has a size of 1.75 cm between the middle of adjacent ridges.
DOI: 10.1594/pangaea.911816
title: Photographs of tiles installed at X-Huinay, Comau Fjord, Chile, at 2011-02-24

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de). If you intend to work with this data set please do not hesitate to contact the authors to discuss cooperation possibilities.The backside of common tiles was selected as substrate. Tiles have the following dimensions, length:height = 15:15 cm (225 cm²) and are fixed with two screws and washers to a PVC frame. The latter is connected to the wall with a stainless steel bolt. A square pattern on the tiles allows easy analysis of the percentage cover of species. This pattern has a size of 1.75 cm between the middle of adjacent ridges.
DOI: 10.1594/pangaea.924132
title: Bulk characteristics of sediment core MD-1
DOI: 10.1594/pangaea.918269
title: Mackerel (Scombrus scombrus) diet in iceland during Arni Fridriksson cruise A7/2013
DOI: 10.1594/pangaea.918270
title: Mackerel (Scombrus scombrus) diet in iceland during Arni Fridriksson cruise A6/2014
DOI: 10.1594/pangaea.923725
title: Litter surveys on 24 beaches of 8 Mediterranean islands (2017-2019)

description: Surface area was measured with the “Polygon” tool from Google Earth© between the starting and ending coordinates, the back of the beach and the waterline.
DOI: 10.1594/pangaea.923730
title: Litter abundance and acculmulation rates on 24 beaches of 8 Mediterranean islands (2017-2019)

description: Surface area was measured with the “Polygon” tool from Google Earth© between the starting and ending coordinates, the back of the beach and the waterline.Litter density per 100 m was calculated as litter count * 100 / distance.Litter accumulation rates were either calculated as (1) litter count * 1000 / surface / days elapsed since the last cleaning, or (2) litter count * 1000 / surface / days elapsed since the last monitoring when no cleaning was performed, or (3) litter count * 1000 / surface / days elapsed since the last monitoring for Plastic / polystyrene pieces 0.5 and Pellets.#999.999 = accumulation rate not calculated
DOI: 10.1594/pangaea.924133
title: Bulk characteristics of sediment core MD-2
DOI: 10.1594/pangaea.924134
title: Bulk characteristics of sediment core UD-4
DOI: 10.1594/pangaea.931192
title: Raw XRF data of piston sediment core Lake850-Core2-2019 from Lake 850, Sweden

description: Data contains elemental composition (Al, Si, P, S, Ar, K, Ca, Ti, V, Cr, Mn, Fe, Ni, Cu, Zn, Ge, Se, Br, Rb, Sr, Y, Zr, Nb, Mo, Te, Ba, La, Ce, Nd, Sm, Eu, Tb, Er, Tm, Yb, Hf, Ir, Pt, Au, Pb, Rn och, Rh inc, MS) of the sediment core from 2019 originating from ITRAX CS37 XRF from GLOBE Institute, Copenhagen University.
DOI: 10.1594/pangaea.927292
title: Quaternary deposits map of Yana-Indigirka and Kolyma lowlands tundra zone, R-55-57, based on Landsat imagery

description: The Quaternary geology map was created for the Yana-Indigirka (eastern part) and Kolyma lowlands, tundra and partly forest-tundra zones. The map corresponds to the nomenclature sheet of Government Geological Map R-(55)-57, northern part. The primary goal for creating the map is to enhance current knowledge of Quaternary deposits distribution in Yedoma regions in North-Eastern Siberia due to the lack of the geological maps of large scale for this region. For most area of the region maps of 1:200.000 scale are still not created and only geological maps of 1:1.000.000 scale exist. The Database of Quaternary Deposits from Maps of 1:1.000.000 scale, East and Central Siberia, is available via https://apgc.awi.de (Bryant et al., 2017, https://doi.org/10.5066/F7VT1Q89). The main Quaternary deposits on the Yana-Indigirka and Kolyma lowlands are late Pleistocene ice-rich Yedoma Ice Complex (LIII2-4), corresponded to yedoma uplands, and Holocene Alas Complexes (lbIV) formed in drained thermokarst lake basins (alases) due to the Yedoma IC thawing in the late Pleistocene-Holocene. High ice-rich Yedoma Ice Complex (IC) deposits are very vulnerable to observed climate warming, which lead to the landscape changes such as surface subsidence, thermokarst and thermoerosion processes activation, deepening of the active layer thickness, etc., as well as to remobilization of the buried freezelocked organic matter and contribution to greenhouse gases fluxes to the atmosphere. The map was created using Landsat images that allow the area of the yedoma uplands and alases to be clearly identified. The mapping of Quaternary deposits was done using Landsat TM 5 and 7 ETM+ satellite images acquired from August and July for the 2001-2010 period. Detecting of Quaternary deposits corresponded to landforms were conducted manually using spectral characteristics of satellite images, landform morphology, absolute heights and existing Quaternary Geology map of 1:1.000.000 scale. The working scale of the mapping was 1:30.000. Mapped Quaternary deposits are represented by six types: Yedoma IC, alas complex, alluvial, alluvial-marine, marine, and bedrocks. A comparison of the Quaternary deposit distribution as mapped with the Landsat satellite imagery and the 1:1.000.000 geological map revealed a 2.5-times overestimation of the Yedoma IC deposits extent area at the 1:1.000.000 scale. The Landsat-based map corresponds to 1:200.000 scale and provides important information about the distribution of yedoma uplands and thermokarst development during Holocene and is the basis for the analysis of yedoma-alas landscapes changes under modern climate warming. Detailed information about methods and results can be found in Veremeeva&Glushkova (2016) and Shmelev et al. (2017).
DOI: 10.1594/pangaea.924769
title: Physical oceanography during one part of a ROV dive PS111_117-1 to the grounding zone of the Antarctic ice-sheet
DOI: 10.1594/pangaea.924770
title: Distribution of cryobethic algae during ROV dive PS111_117-1 to the grounding zone of the Antarctic ice-sheet
DOI: 10.1594/pangaea.924772
title: 3D model of the grounding zone of the Antarctic ice-sheet create from ROV dive PS111_117-1
DOI: 10.1594/pangaea.924774
title: Tide level during ROV dive PS111_117-1 to the grounding zone of the Antarctic ice-sheet
DOI: 10.1594/pangaea.924776
title: Video footage highlights of ROV dive PS111_117-1 to the grounding zone of the Antarctic ice-sheet
DOI: 10.1594/pangaea.924815
title: Digitized ice edge form of the grounding zone of the Antarctic ice-sheet on 2018-02-18

description: Projection: EPSG:3031,Ice edge form 18.02.2018,Digitised in QGIS 3.10(64bit) from DLR satellite image:,TSX1_SAR__EEC_RE___SC_S_SRA_20180218T005416_20180218T005438
DOI: 10.1594/pangaea.924820
title: Reverse ice flow calculations based on vector field ice flow data

description: Projection: EPSG:3031Reverse flow based on vector field ice flow data by: Rignot, E et al. (2017)
DOI: 10.1594/pangaea.924821
title: Digitized ice edge form of the grounding zone of the Antarctic ice-sheet on 2015-12-31 with extrapolation into the future using ice edge velocities

description: Projection: EPSG:3031Ice edge form 31.12.2015Digitised in QGIS 3.10(64bit) from DLR satellite image:TDX1_SAR__EEC_RE___SC_S_SRA_20151231T003659_20151231T003728Rignot-et al. (2017)Interpolation of ice edge velocities was done by Rbf function of scipy.interpolate module from Python 3 libraries
DOI: 10.1594/pangaea.924823
title: Physical oceanography during ROV dive PS111_117-1 to the grounding zone of the Antarctic ice-sheet
DOI: 10.1594/pangaea.933053
title: Locations of micro-inclusions identified with Raman spectroscopy in eleven samples (138-1340 m) from the EastGRIP ice core

description: Micro-inclusions in eleven samples from the upper 1340 m of the East Greenland Ice Core Project ice core in North-East Greenland were analysed with Raman spectroscopy. Ice samples were drilled and processed between 2016 and 2019, Raman analysis was performed between January 2020 and December 2020 at the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research. The samples are between 1.0 and 14.1 ka yr old and cover the Holocene, Younger Dryas, and Bolling Allerod. Ice sample sizes are usually 10 x 10 mm; micro-inclusions are only a few micrometers large.The first three or four numbers indicate the samples bag, the number after the underscore implies the section of the respective bag. Yellow dots are located micro-inclusions, colored dots are located and measured (with Raman spectroscopy) micro-inclusions. Images point in the direction of the ice sheet surface, i.e. top is upwards.Grain boundaries and inclusions were not totally counted/analysed for EGRIP2286_3 due to a too large amount of inclusions and thus unreliable data. The same set-up was used by Eichler et al. (2019).
DOI: 10.1594/pangaea.932582
title: High-resolution XRF (Itrax) elemental composition of sediment core YMER80-131

description: Core Number: 131, Core Type: Super Gravity Corer (SGC), Sediment Depth: 349cm, Water Depth: 820m, Latitude: 81° 07' Longitude: 03° 12', Core was taken in September 5th 1980. This is re-evaluated data of 080604\YMER80\YMER80_MG-131_0-64cm_A_Mo\XRF data from 2008-06-18. Core was scanned using the ITRAX XRF core scanner and cores were merged using Corascope.
description: Note: Element counts for silicon for seem to be inconsistent between cores
DOI: 10.1594/pangaea.935986
title: Selected elemental data obtained by X-ray fluorescence (XRF) core scanning (Lagoa Dourada, S Brazil)

description: X-ray fluorescence (XRF) was measured in 2 mm increments with an ITRAX XRF core scanner (Cox Analytics) and Mo tube (30 kV, 50 mA, 5 s).
DOI: 10.1594/pangaea.937086
title: XRF core scanning data of sediment core LV18-B, Lago di Vedana, north-eastern Italy
DOI: 10.1594/pangaea.937965
title: Branched glycerol monoalkyl glycerol tetraethers (brGMGTs) and geochemical proxies in soils, SPM and riverbed sediments in the Godavari River basin (India)

description: Branched Glycerol Monoalkyl Glycerol Tetraethers (brGMGTs) in soils, suspended particulate matter (SPM) and riverbed sediments of the Godavari River basin (India), the largest river of peninsular India that is fed by the Southwest monsoon. Surface soils (0-10 cm) were collected near the Godavari River, and SPM (10-80 L, filtered over 0.7 μm GFF filters) and bulk and fine (≤63 μm) riverbed sediments were collected in a dry (February/March 2015) and wet season (July/August 2015). BrGMGT fractional abundances and concentrations were analysed using ultra high performance liquid chromatography-mass spectrometry. BrGMGT loadings were normalised to Mineral Surface Area (MSA data for soils and dry season sediments from Usman et al., 2018). %TN and C:N were measured in soils and sediments, %TOC was from Kirkels et al. (2021).
DOI: 10.1594/pangaea.942034
title: Physical oceanography from Mooring DS2 in the Denmark Strait Overflow area between August 2005 and July 2006

description: This data set provides quality controlled temperature, conductivity and pressure measurements from moored instrumentation (Seabird Microcat) in the Denmark Strait. Practical salinity was calculated from the measured quantities and is provided as well. Temporal resolution of the time series is 15 minutes. The data was collected from August 2005 to July 2006 at the location of mooring DS2. This mooring is part of the Denmark Strait Overflow array and maintained by the Institute of Oceanography, University Hamburg. The purpose of the array was to monitor the properties and variability of the dense Denmark Strait Overflow.
DOI: 10.1594/pangaea.942046
title: Physical oceanography from Mooring DS2 in the Denmark Strait Overflow area between July 2007 and July 2008

description: This data set provides quality controlled temperature, conductivity and pressure measurements from moored instrumentation (Seabird Microcat) in the Denmark Strait. Practical salinity was calculated from the measured quantities and is provided as well. Temporal resolution of the time series is 10 minutes. The data was collected from July 2007 to July 2008 at the location of mooring DS2. This mooring is part of the Denmark Strait Overflow array and maintained by the Institute of Oceanography, University Hamburg. The purpose of the array was to monitor the properties and variability of the dense Denmark Strait Overflow.
DOI: 10.1594/pangaea.942047
title: Physical oceanography from Mooring DS2 in the Denmark Strait Overflow area between July 2008 and June 2009

description: This data set provides quality controlled temperature, conductivity and pressure measurements from moored instrumentation (Seabird Microcat) in the Denmark Strait. Practical salinity was calculated from the measured quantities and is provided as well. Temporal resolution of the time series is 10 minutes. The data was collected from July 2008 to June 2009 at the location of mooring DS2. This mooring is part of the Denmark Strait Overflow array and maintained by the Institute of Oceanography, University Hamburg. The purpose of the array was to monitor the properties and variability of the dense Denmark Strait Overflow.
DOI: 10.1594/pangaea.942048
title: Physical oceanography from Mooring DS2 in the Denmark Strait Overflow area between June 2009 and July 2010

description: This data set provides quality controlled temperature, conductivity and pressure measurements from moored instrumentation (Seabird Microcat) in the Denmark Strait. Practical salinity was calculated from the measured quantities and is provided as well. Temporal resolution of the time series is 20 minutes. The data was collected from June 2009 to July 2010 at the location of mooring DS2. This mooring is part of the Denmark Strait Overflow array and maintained by the Institute of Oceanography, University Hamburg. The purpose of the array was to monitor the properties and variability of the dense Denmark Strait Overflow.
DOI: 10.1594/pangaea.942049
title: Physical oceanography from Mooring DS2 in the Denmark Strait Overflow area between August 2011 and June 2012

description: This data set provides quality controlled temperature, conductivity and pressure measurements from moored instrumentation (Seabird Microcat) in the Denmark Strait. Practical salinity was calculated from the measured quantities and is provided as well. Temporal resolution of the time series is 10 minutes. The data was collected from August 2011 to June 2012 at the location of mooring DS2. This mooring is part of the Denmark Strait Overflow array and maintained by the Institute of Oceanography, University Hamburg. The purpose of the array was to monitor the properties and variability of the dense Denmark Strait Overflow.
DOI: 10.1594/pangaea.942051
title: Physical oceanography from Mooring DS2 in the Denmark Strait Overflow area between August 2012 and August 2013

description: This data set provides quality controlled temperature, conductivity and pressure measurements from moored instrumentation (Seabird Microcat) in the Denmark Strait. Practical salinity was calculated from the measured quantities and is provided as well. Temporal resolution of the time series is 10 minutes. The data was collected from August 2012 to August 2013 at the location of mooring DS2. This mooring is part of the Denmark Strait Overflow array and maintained by the Institute of Oceanography, University Hamburg. The purpose of the array was to monitor the properties and variability of the dense Denmark Strait Overflow.
DOI: 10.1594/pangaea.942053
title: Physical oceanography from Mooring DS2 in the Denmark Strait Overflow area between August 2013 and July 2014

description: This data set provides quality controlled temperature, conductivity and pressure measurements from moored instrumentation (Seabird Microcat) in the Denmark Strait. Practical salinity was calculated from the measured quantities and is provided as well. Temporal resolution of the time series is 10 minutes. The data was collected from August 2013 to July 2014 at the location of mooring DS2. This mooring is part of the Denmark Strait Overflow array and maintained by the Institute of Oceanography, University Hamburg. The purpose of the array was to monitor the properties and variability of the dense Denmark Strait Overflow.