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  • 1
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    Geological map of northern XU-Fjella, Heimefrontfjella, Dronning Maud Land, Antarctica (Scale 1:25,000) (2008)
    PANGAEA
    In:  Department of Geosciences, Bremen University
    Details
    Publication Date: 2023-03-13
    Description: The geological map shows the northeastern part of the polyphase deformed Sivorg Terrane in the Heimefrontfjella/Dronning Maud Land. The basement was affected by late Mesoproterozoic and Cambrian deformation and metamorphism. Geological mapping was carried out during the Antarctic Expedition 2000/01 of the Alfred Wegener Institute for Polar and Marine Research. Topographic data were obtained through stereoscopic aerial photo interpretation. The photogrammetric photo flights were undertaken in 1986 by the Institut für Angewandte Geodäsie, Frankfurt/M. Horizontal ground control points required for aerial photo interpretation were determined by means of Doppler satellite observation during the 2nd German Neuschwabenland Expedition 1985/86. Vertical ground control points were taken from unpublished map drafts at 1:100 000 scale by Norsk Polarinstitutt, Oslo. The elevation above mean sea level was transferred to Heimefrontfjella barometrically. For this reason assertions concerning the absolute elevation (referred to sea level) are uncertain. Contours and spot heights presented on the map were obtained from the photogrammetric evaluation of the photography taken in 1986; relative elevation data (height differences) are accurate to approximately ±10 m. Published by Fachbereich Geowissenschaften, Universität Bremen & Geologisches Institut, RWTH Aachen.
    Keywords: File format; File size; Geological mapping; GEOMAP; Heimefrontfjella, Antarctica; ORDINAL NUMBER; Uniform resource locator/link to raw data file; XU-FJELLA
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 2
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    Geological map of HANSSONHORNA, Heimefrontfjella, Dronning Maud Land, Antarctica, 2nd revised Edition (Scale 1:25,000) (2008)
    PANGAEA
    In:  Geologisches Institut, RWTH Aachen
    Details
    Publication Date: 2023-03-13
    Description: The geological map shows the border area between the polyphase (late Mesoproterozoic and Cambrian) deformed Sivorg Terrane and the Kottas Terrane where a pervasive Cambrian tectonometamorphic overprints is lacking. Geological revision mapping was carried out during the Antarctic Expedition 2000/01 of the Alfred Wegener Institute for Polar and Marine Research. Topographic data were obtained through stereoscopic aerial photo interpretation. The photogrammetric photo flights were undertaken in 1986 by the Institut für Angewandte Geodäsie, Frankfurt. Horizontal ground control points required for aerial photo interpretation were determined by means of Doppler satellite observation during the 2nd German Neuschwabenland Expedition 1985/86. Vertical ground control points were taken from unpublished map drafts at 1:100 000 scale by Norsk Polarinstitutt, Oslo. The elevation above mean sea level was transferred to Heimefrontfjella barometrically. For this reason assertions concerning the absolute elevation (referred to sea level) are uncertain. Contours and spot heights presented on the map were obtained from the photogrammetric evaluation of the photography taken in 1986; relative elevation data (height differences) are accurate to approximately ±10 m. Published by Geologisches Institut der RWTH Aachen & Fachbereich Geowissenschaften, Bremen.
    Keywords: File format; File size; Geological mapping; GEOMAP; HANSSONHORNA; Heimefrontfjella, Antarctica; ORDINAL NUMBER; Uniform resource locator/link to raw data file
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 3
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    Geological map of Heimefrontfjella, Dronning Maud Land, Antarctica (Scale 1:250,000) (2009)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Description: The geological overview map was compiled from 15 geological maps (1 : 25,000) and is based on Jacobs et al. 1996. The topographic basemaps were adapted from unpublished 1:250,000 provisional topographic maps, Institut f. Angewandte Geodäsie, Frankfurt, 1983. Part of the contour lines are from Radarsat (Liu et al. 2001).
    Keywords: Glaciers Austria; Heimefrontfjella; Heimefrontfjella, Antarctica
    Type: Dataset
    Format: application/pdf, 919.1 kBytes
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  • 4
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    Tab.1: Composition of salt crusts and host rocks (2011)
    PANGAEA
    In:  Supplement to: Bauer, Wilfried; Fitzner, Bernd (2005): Salt crusts on bedrock exposures in Dronning Maud Land, East Antarctica. Polarforschung, 73(1), 1-4, hdl:10013/epic.29906.d001
    Details
    Publication Date: 2023-01-13
    Description: Gypsum and calcite crusts were found on many outcrops of the metamorphic basement and on moraines in Dronning Maud Land. For the first time the copper mineral connellite was found in such crusts. Salt crust and efflorescences indicate an important role of chemical weathering even in a cold and arid climate such as the Antarctic interior. Findings of salt efflorescenees few centimetres beneath the rock surface suggest the contribution of salt crystallization to the formation of the typical Antarctic cavernous or honeycomb weathering features.
    Keywords: B22.1.94; Description; Event label; Geological sample; GEOS; Heimfront-fjella, Antarctica; KB102a; KB102b; KB146; KB147; Latitude of event; Location of event; Longitude of event; Major components/lithology; Minor components/lithology; Mühlig-Hofmann-Gebirge, Antarctica; WB208; WB209; WB255; WB256
    Type: Dataset
    Format: text/tab-separated-values, 27 data points
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    DATA PANGAEA
  • 5
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    Data of the Garchinger Heide 1984-1993-2018: processed data species (2022)
    PANGAEA
    Details
    Publication Date: 2023-01-13
    Keywords: Bavaria, Germany; BM; Botanical mapping; Botany; Ecology & Environment; Garchinger_Heide_X03M01; Garchinger_Heide_X03M02; Garchinger_Heide_X03M03; Garchinger_Heide_X03M04; Garchinger_Heide_X03M05; Garchinger_Heide_X03M06; Garchinger_Heide_X03M07; Garchinger_Heide_X03M08; Garchinger_Heide_X03M09; Garchinger_Heide_X03M10; Garchinger_Heide_X03M11; Garchinger_Heide_X03M12; Garchinger_Heide_X03M13; Garchinger_Heide_X03M14; Garchinger_Heide_X03M15; Garchinger_Heide_X03M16; Garchinger_Heide_X03M17; Garchinger_Heide_X03M18; Garchinger_Heide_X03N01; Garchinger_Heide_X03N02; Garchinger_Heide_X03N03; Garchinger_Heide_X03N04; Garchinger_Heide_X03N05; Garchinger_Heide_X03N06; Garchinger_Heide_X03S01; Garchinger_Heide_X03S02; Garchinger_Heide_X03S03; Garchinger_Heide_X03S04; Garchinger_Heide_X03S05; Garchinger_Heide_X03S06; Garchinger_Heide_X03S07; Garchinger_Heide_X03S08; Garchinger_Heide_X03S09; Garchinger_Heide_X03S10; Garchinger_Heide_X03S11; Garchinger_Heide_X03S12; Garchinger_Heide_X03S13; Garchinger_Heide_X03S14; Garchinger_Heide_X03S15; Garchinger_Heide_X03S16; Garchinger_Heide_X03S17; Garchinger_Heide_X03S18; Garchinger_Heide_X18I1; Garchinger_Heide_X18I10; Garchinger_Heide_X18I11; Garchinger_Heide_X18I12; Garchinger_Heide_X18I13; Garchinger_Heide_X18I14; Garchinger_Heide_X18I15; Garchinger_Heide_X18I16; Garchinger_Heide_X18I17; Garchinger_Heide_X18I18; Garchinger_Heide_X18I19; Garchinger_Heide_X18I2; Garchinger_Heide_X18I20; Garchinger_Heide_X18I21; Garchinger_Heide_X18I22; Garchinger_Heide_X18I23; Garchinger_Heide_X18I24; Garchinger_Heide_X18I25; Garchinger_Heide_X18I26; Garchinger_Heide_X18I27; Garchinger_Heide_X18I3; Garchinger_Heide_X18I4; Garchinger_Heide_X18I5; Garchinger_Heide_X18I6; Garchinger_Heide_X18I7; Garchinger_Heide_X18I8; Garchinger_Heide_X18I9; Garchinger_Heide_X18II1; Garchinger_Heide_X18II14; Garchinger_Heide_X18II2; Garchinger_Heide_X18II3; Garchinger_Heide_X18II4; Garchinger_Heide_X18II5; Garchinger_Heide_X18II6; Garchinger_Heide_X18II7; Garchinger_Heide_X18II8; Garchinger_Heide_X18III1; Garchinger_Heide_X18III16; Garchinger_Heide_X18III2; Garchinger_Heide_X18III3; Garchinger_Heide_X18M01; Garchinger_Heide_X18M02; Garchinger_Heide_X18M03; Garchinger_Heide_X18M04; Garchinger_Heide_X18M05; Garchinger_Heide_X18M06; Garchinger_Heide_X18M07; Garchinger_Heide_X18M08; Garchinger_Heide_X18M09; Garchinger_Heide_X18M10; Garchinger_Heide_X18M11; Garchinger_Heide_X18M12; Garchinger_Heide_X18M13; Garchinger_Heide_X18M14; Garchinger_Heide_X18M15; Garchinger_Heide_X18M16; Garchinger_Heide_X18M17; Garchinger_Heide_X18M18; Garchinger_Heide_X18N01; Garchinger_Heide_X18N02; Garchinger_Heide_X18N03; Garchinger_Heide_X18N04; Garchinger_Heide_X18N05; Garchinger_Heide_X18N06; Garchinger_Heide_X18S01; Garchinger_Heide_X18S02; Garchinger_Heide_X18S03; Garchinger_Heide_X18S04; Garchinger_Heide_X18S05; Garchinger_Heide_X18S06; Garchinger_Heide_X18S07; Garchinger_Heide_X18S08; Garchinger_Heide_X18S09; Garchinger_Heide_X18S10; Garchinger_Heide_X18S11; Garchinger_Heide_X18S12; Garchinger_Heide_X18S13; Garchinger_Heide_X18S14; Garchinger_Heide_X18S15; Garchinger_Heide_X18S16; Garchinger_Heide_X18S17; Garchinger_Heide_X18S18; Garchinger_Heide_X73I1; Garchinger_Heide_X73I10; Garchinger_Heide_X73I11; Garchinger_Heide_X73I12; Garchinger_Heide_X73I13; Garchinger_Heide_X73I14; Garchinger_Heide_X73I15; Garchinger_Heide_X73I16; Garchinger_Heide_X73I17; Garchinger_Heide_X73I18; Garchinger_Heide_X73I19; Garchinger_Heide_X73I2; Garchinger_Heide_X73I20; Garchinger_Heide_X73I21; Garchinger_Heide_X73I22; Garchinger_Heide_X73I23; Garchinger_Heide_X73I24; Garchinger_Heide_X73I25; Garchinger_Heide_X73I26; Garchinger_Heide_X73I27; Garchinger_Heide_X73I3; Garchinger_Heide_X73I4; Garchinger_Heide_X73I5; Garchinger_Heide_X73I6; Garchinger_Heide_X73I7; Garchinger_Heide_X73I8; Garchinger_Heide_X73I9; Garchinger_Heide_X73II1; Garchinger_Heide_X73II14; Garchinger_Heide_X73II2; Garchinger_Heide_X73II3; Garchinger_Heide_X73II4; Garchinger_Heide_X73II5; Garchinger_Heide_X73II6; Garchinger_Heide_X73II7; Garchinger_Heide_X73II8; Garchinger_Heide_X73III1; Garchinger_Heide_X73III16; Garchinger_Heide_X73III2; Garchinger_Heide_X73III3; Garchinger_Heide_X84I1; Garchinger_Heide_X84I10; Garchinger_Heide_X84I11; Garchinger_Heide_X84I12; Garchinger_Heide_X84I13; Garchinger_Heide_X84I14; Garchinger_Heide_X84I15; Garchinger_Heide_X84I16; Garchinger_Heide_X84I17; Garchinger_Heide_X84I18; Garchinger_Heide_X84I19; Garchinger_Heide_X84I2; Garchinger_Heide_X84I20; Garchinger_Heide_X84I21; Garchinger_Heide_X84I22; Garchinger_Heide_X84I23; Garchinger_Heide_X84I24; Garchinger_Heide_X84I25; Garchinger_Heide_X84I26; Garchinger_Heide_X84I27; Garchinger_Heide_X84I3; Garchinger_Heide_X84I4; Garchinger_Heide_X84I5; Garchinger_Heide_X84I6; Garchinger_Heide_X84I7; Garchinger_Heide_X84I8; Garchinger_Heide_X84I9; Garchinger_Heide_X84II1; Garchinger_Heide_X84II14; Garchinger_Heide_X84II2; Garchinger_Heide_X84II3; Garchinger_Heide_X84II4; Garchinger_Heide_X84II5; Garchinger_Heide_X84II6; Garchinger_Heide_X84II7; Garchinger_Heide_X84II8; Garchinger_Heide_X84III1; Garchinger_Heide_X84III16; Garchinger_Heide_X84III2; Garchinger_Heide_X84III3; Garchinger_Heide_X93I1; Garchinger_Heide_X93I10; Garchinger_Heide_X93I11; Garchinger_Heide_X93I12; Garchinger_Heide_X93I13; Garchinger_Heide_X93I14; Garchinger_Heide_X93I15; Garchinger_Heide_X93I16; Garchinger_Heide_X93I17; Garchinger_Heide_X93I18; Garchinger_Heide_X93I19; Garchinger_Heide_X93I2; Garchinger_Heide_X93I20; Garchinger_Heide_X93I21; Garchinger_Heide_X93I22; Garchinger_Heide_X93I23; Garchinger_Heide_X93I24; Garchinger_Heide_X93I25; Garchinger_Heide_X93I26; Garchinger_Heide_X93I27; Garchinger_Heide_X93I3; Garchinger_Heide_X93I4; Garchinger_Heide_X93I5; Garchinger_Heide_X93I6; Garchinger_Heide_X93I7; Garchinger_Heide_X93I8; Garchinger_Heide_X93I9; Garchinger_Heide_X93II1; Garchinger_Heide_X93II14; Garchinger_Heide_X93II2; Garchinger_Heide_X93II3; Garchinger_Heide_X93II4; Garchinger_Heide_X93II5; Garchinger_Heide_X93II6; Garchinger_Heide_X93II7; Garchinger_Heide_X93II8; Garchinger_Heide_X93III1; Garchinger_Heide_X93III16; Garchinger_Heide_X93III2; Garchinger_Heide_X93III3; Plant species frequency: countings after Raunkiaer (1918); Ratio; Species
    Type: Dataset
    Format: text/tab-separated-values, 14036 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 6
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    Fly-through movie for the reconstructed folds in the onset region of the Petermann Glacier, North Greenland (2016)
    PANGAEA
    In:  Supplement to: Bons, Paul D; Jansen, Daniela; Mundel, Felicitas; Bauer, Catherine C; Binder, Tobias; Eisen, Olaf; Jessell, Mark W; Llorens, Maria-Gema; Steinbach, Florian; Steinhage, Daniel; Weikusat, Ilka (2016): Converging flow and anisotropy cause large-scale folding in Greenland's ice sheet. Nature Communications, 7, 11427, https://doi.org/10.1038/ncomms11427
    Details
    Publication Date: 2023-02-06
    Description: The increasing catalogue of high-quality ice-penetrating radar data provides a unique insight in the internal layering architecture of the Greenland ice sheet. The stratigraphy, an indicator of past deformation, highlights irregularities in ice flow and reveals large perturbations without obvious links to bedrock shape. In this work, to establish a new conceptual model for the formation process, we analysed the radar data at the onset of the Petermann Glacier, North Greenland, and created a three-dimensional model of several distinct stratigraphic layers. We demonstrate that the dominant structures are cylindrical folds sub-parallel to the ice flow. By numerical modelling, we show that these folds can be formed by lateral compression of mechanically anisotropic ice, while a general viscosity contrast between layers would not lead to folding for the same boundary conditions. We conclude that the folds primarily form by converging flow as the mechanically anisotropic ice is channelled towards the glacier.
    Keywords: North Greenland; Petermann_Glacier; RADAR; Radar profile
    Type: Dataset
    Format: video/quicktime, 20.3 MBytes
    Location Call Number Expected Availability
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  • 7
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    Effects of artifical light at night (ALAN) on three benthic grazer species (Arbacia lixula, Paracentrotus lividus, Cerithium spp.) from the Adriatic Sea (June - August 2021): time-lapse experiment 1 (2022)
    PANGAEA
    Details
    Publication Date: 2023-02-02
    Description: This data set shows the day-/night feeding behaviour of Arbacia lixula, Cerithium spp. and Paracentrotus lividus under artificial light at night (ALAN), derived from time-lapse photography, with acclimation.
    Keywords: Adriatic Sea; Arbacia lixula; Artificial Light at Night; benthic invertebrates; Cerithium; feeding rates; Flag; Food consumption rates; GAME; Global Approach by Modular Experiments; Mediterranean; Paracentrotus lividus; Replicate; Species; time-lapse photography; Time point, descriptive; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 92625 data points
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  • 8
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    Effects of artifical light at night (ALAN) on three benthic grazer species (Arbacia lixula, Paracentrotus lividus, Cerithium spp.) from the Adriatic Sea (June - August 2021): time-lapse experiment 2 (2022)
    PANGAEA
    Details
    Publication Date: 2023-02-02
    Description: This data set shows the day-/night feeding behaviour of Arbacia lixula, Cerithium spp. and Paracentrotus lividus under artificial light at night (ALAN), derived from time-lapse photography, no acclimation.
    Keywords: Adriatic Sea; Arbacia lixula; Artificial Light at Night; benthic invertebrates; Cerithium; feeding rates; Flag; Food consumption rates; GAME; Global Approach by Modular Experiments; Mediterranean; Paracentrotus lividus; Replicate; Species; time-lapse photography; Time point, descriptive; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 77755 data points
    Location Call Number Expected Availability
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  • 9
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    Effects of artifical light at night (ALAN) on three benthic grazer species (Arbacia lixula, Paracentrotus lividus, Cerithium spp.) from the Adriatic Sea (June - August 2021): consumption rates experiment 1 (2022)
    PANGAEA
    Details
    Publication Date: 2023-02-02
    Description: This data set shows the consumption rates of Arbacia lixula, Cerithium spp. and Paracentrotus lividus under artificial light at night (ALAN), with acclimation.
    Keywords: Adriatic Sea; Arbacia lixula; Artificial Light at Night; benthic invertebrates; Cerithium; Diameter; Dry mass; feeding rates; Food consumption; Food consumption rates; Food pellet, consumed; Food pellet, dry mass; Food pellet, fresh mass; GAME; Global Approach by Modular Experiments; Mediterranean; Paracentrotus lividus; Replicate; Species; time-lapse photography; Treatment; Wet mass
    Type: Dataset
    Format: text/tab-separated-values, 2220 data points
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  • 10
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    Effects of artifical light at night (ALAN) on three benthic grazer species (Arbacia lixula, Paracentrotus lividus, Cerithium spp.) from the Adriatic Sea (June - August 2021): consumption rates experiment 2 (2022)
    PANGAEA
    Details
    Publication Date: 2023-02-02
    Description: This data set shows the consumption rates of Arbacia lixula, Cerithium spp. and Paracentrotus lividus under artificial light at night (ALAN), no acclimation.
    Keywords: Adriatic Sea; Arbacia lixula; Artificial Light at Night; benthic invertebrates; Cerithium; Diameter; Dry mass; feeding rates; Food consumption; Food consumption rates; Food pellet, consumed; Food pellet, dry mass; Food pellet, fresh mass; GAME; Global Approach by Modular Experiments; Mediterranean; Paracentrotus lividus; Replicate; Species; time-lapse photography; Treatment; Wet mass
    Type: Dataset
    Format: text/tab-separated-values, 1836 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
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