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  • 2020-2024  (7)
Publikationsart
Schlagwörter
Verlag/Herausgeber
Erscheinungszeitraum
Jahr
  • 1
    Publikationsdatum: 2024-03-14
    Beschreibung: Alive and dead colony sections of Madrepora oculata cold-water corals were measured from underwater video transects carried out to characterize benthic communities. Data were collected from 17th to 25th January 2016 off Angola in 6 coral mounds. Video transects were recorded with the Remotely Operated Vehicle SQUID during the ANNA expedition (Hebbeln et al. 2016). The data included in this dataset have been published in Orejas et al. (2021).
    Schlagwort(e): Angola; Coral growth; Coral occurrence; DATE/TIME; Eastern South Atlantic; Event label; GeoB20917-1; GeoB20927-1; GeoB20930-1; GeoB20957-1; iAtlantic; Image analysis NIH ImageJ; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; Length; Location; M122; M122_100-1; M122_110-1; M122_113-1; M122_141-1; Madrepora oculata; Meteor (1986); Remotely operated vehicle SQUID; Remote operated vehicle; ROV; ROV SQUID; Sample code/label; Species; Species, unique identification (Semantic URI); Species, unique identification (URI); Transect
    Materialart: Dataset
    Format: text/tab-separated-values, 270 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Publikationsdatum: 2024-03-14
    Beschreibung: This dataset includes occurrence data for the cold-water coral Madrepora oculata obtained from underwater video transects performed to characterize benthic communities. Data were collected from 17th to 25th January 2016 off Angola on 6 coral mounds. Video transects were carried out with the Remotely Operated Vehicle SQUID during the ANNA expedition (Hebbeln et al. 2016). The information included in this dataset have been published in the paper Orejas et al. (2021).
    Schlagwort(e): Angola; Code; Coral growth; Coral occurrence; DATE/TIME; Eastern South Atlantic; Event label; GeoB20917-1; GeoB20927-1; GeoB20930-1; GeoB20957-1; iAtlantic; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; Location; M122; M122_100-1; M122_110-1; M122_113-1; M122_141-1; Madrepora oculata; Meteor (1986); Remotely operated vehicle SQUID; Remote operated vehicle; ROV; ROV SQUID; Species; Species, unique identification (Semantic URI); Species, unique identification (URI); Time Stamp; Transect; Visual analysis (video)
    Materialart: Dataset
    Format: text/tab-separated-values, 322 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2024-03-14
    Beschreibung: Occurence data and measurements of alive vs. dead colony sections of Madrepora oculata cold-water corals were obtained at six coral mounds off Angola from 17th to 25th January 2016 by recording underwater video transects with the Remotely Operated Vehicle SQUID during the ANNA expedition (Hebbeln et al. 2016). Video transects were primarily performed to characterize benthic communities. The data included in these datasets have been published in Orejas et al. (2021).
    Schlagwort(e): Angola; Coral growth; Coral occurrence; Eastern South Atlantic; GeoB20917-1; GeoB20927-1; GeoB20930-1; GeoB20957-1; iAtlantic; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; M122; M122_100-1; M122_110-1; M122_113-1; M122_141-1; Madrepora oculata; Meteor (1986); Remote operated vehicle; ROV
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2024-02-02
    Beschreibung: Uranium-series age, isotope concentrations and ratios from Lophelia pertusa fragments from the gravity core sample GeoB20531-1 collected during the M122 ANNA cruise off Namibia. *Measured 234U/238U activity ratios (δ234Um) are presented as deviation permil (‰) from the equilibrium value. Decay corrected 234U/238U activity ratios (δ234Ui) are calculated from the given ages and with λ234U: 2.8263 x 10-6 yr-1. Agecor Corrected ages, according to Frank et al. (2004) and Wefing et al., (2017). n.d.: not determinable because lower than the analytical blank (〈0.003 ng/g). For GeoB20572-4 and 20579-1, two L. pertusa fragments were collected from the bulk sample for dating: ' sample 1; '' sample 2.
    Schlagwort(e): Age, dated; Age, dated standard deviation; Aggradation rate; Center for Marine Environmental Sciences; Corrected; dating; DEPTH, sediment/rock; Desmophyllum pertusum; GC; GeoB20531-1; Gravity corer; Laboratory code/label; Lophelia pertusa; M122; M122_026-1; MARUM; Meteor (1986); Namibia; Species; Thorium-232; Thorium-232, standard deviation; Uranium-series; δ234 Uranium; δ234 Uranium, standard deviation
    Materialart: Dataset
    Format: text/tab-separated-values, 217 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Publikationsdatum: 2024-03-15
    Beschreibung: An exceptionally large cold-water coral mound province (CMP) was recently discovered extending over 80 km along the Namibian shelf (offshore southwestern Africa) in water depths of 160–270 m. This hitherto unknown CMP comprises 〉2000 mounds with heights of up to 20 m and constitutes the largest CMP known from the southeastern Atlantic Ocean. Here, the position of the peaks of the Namibian coral mounds is reported.
    Schlagwort(e): Center for Marine Environmental Sciences; CMP; cold-water coral; Coral_mound_province; coral mounds; Depth, water, bottom/maximum; Depth, water, top/minimum; ELEVATION; Identification; LATITUDE; LONGITUDE; Lophelia pertusa; MARUM; Province
    Materialart: Dataset
    Format: text/tab-separated-values, 8060 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Publikationsdatum: 2024-04-20
    Beschreibung: Quantitative morphometric analyses were carried out for each mound following the workflows presented by Purkis et al. (2007) The coral mound base was defined following the methodological approach of Correa et al. (2012) using the dip angle map, generated from the digital elevation model (DEM), to extract closed polygons that follow the 3°-contour line. This 3°-cutoff has been qualitatively validated with a comparison between the DEM and the dip angle (Fig. 2). Small-scaled polygons within mound perimeters and resulting from bathymetric artifacts were filtered out. Manual editing was applied to split simple merged mound structures (e.g. twin-peak mounds) based on higher cut-off slope values (4-5°). Furthermore, polygons describing the mound footprint have been corrected to remove unrealistic shapes especially common for the CBM. The DEM was subsequently re-gridded to generate hypothetical bathymetric maps without mounds, for which the vertical relief beneath each removed mound was interpolated from the mound perimeters. The newly interpolated surfaces were then subtracted from the original DEMs to evaluate the volume and heights of the coral mounds. Only features with a footprint area greater than 900 squared meters (corresponding to a two-dimensional array of 3 × 3 DEM grid cells) and with a height of 〉2 m above the surrounding seafloor (4 × 0.5 m of vertical precision) were considered as coral mounds and quantitatively analyzed.
    Schlagwort(e): 3D relief of the coral mound; 3D relief of the coral mound/coral mound footprint polygon; Bounding area; Circular variance; cold-water coral; Compactness; Convexity; coral mounds; Depth, bottom/max; Depth, difference; Depth, median; Depth, mode; Depth, top/min; DEPTH, water; Dimension, fractal; Direction; Direction of principal axis; Distance from nearest polygon; Elevation, standard deviation; Fractal Span; GeoB20502-1; GeoB20509-1; GeoB20526-1; GeoB20532-1; GeoB20546-1; GeoB20558-1; GeoB20562-1; GeoB20570-1; GeoB20580-1; Grab; GRAB; Height of mound; Identification; LATITUDE; Length of axis ortoghonal to PAX; Length of principal axis; LONGITUDE; Lophelia pertusa; M122; M122_004-1; M122_021-1; M122_027-1; M122_041-1; M122_053-1; M122_057-1; M122_065-1; M122_075-1; M122_1348-1; MB_PS; Meteor (1986); Morphometry; Mound footprint polygon; Mound height/PAX length ratio; Multibeam/Parasound; Nearest polygon identification number; Net area; Number of nodes; Parameter; Perimeter; Principal axes ratio; Ratio between 3D surface and planar surface; Slope; Slope, average, underlying; Slope, average, underlying standard deviation; Slope, maximum underlying; Slope, standard deviation; Slope angle; Volume
    Materialart: Dataset
    Format: text/tab-separated-values, 26999 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Publikationsdatum: 2024-04-20
    Beschreibung: Quantitative morphometric analyses were carried out for each mound following the workflows presented by Purkis et al. (2007) The coral mound base was defined following the methodological approach of Correa et al. (2012) using the dip angle map, generated from the digital elevation model (DEM), to extract closed polygons that follow the 3°-contour line. This 3°-cutoff has been qualitatively validated with a comparison between the DEM and the dip angle. Small-scaled polygons within mound perimeters and resulting from bathymetry artefacts were filtered out. Manual editing was applied to split simple merged mound structures (e.g. twin-peak mounds) based on higher cut-off slope values (4-5°). Furthermore, polygons describing the mound footprint have been corrected to remove unrealistic shapes especially common for the CBM. The DEM was subsequently re-gridded to generate hypothetical bathymetric maps without mounds, for which the vertical relief beneath each removed mound was interpolated from the mound perimeters. The newly interpolated surfaces were then subtracted from the original DEMs to evaluate the volume and heights of the coral mounds. Only features with a footprint area greater than 900 suared meters (corresponding to a two-dimensional array of 3 × 3 DEM grid cells) and with a height of 〉2 m above the surrounding seafloor (4 × 0.5 m of vertical precision) were considered as coral mounds and quantitatively analyzed.
    Schlagwort(e): 3D relief of the coral mound; 3D relief of the coral mound/coral mound footprint polygon; Bounding area; Circular variance; cold-water coral; Compactness; Convexity; coral mounds; Depth, bottom/max; Depth, difference; Depth, median; Depth, mode; Depth, top/min; DEPTH, water; Dimension, fractal; Direction; Direction of principal axis; Distance from nearest polygon; ELEVATION; Elevation, standard deviation; EM1002; EM1002 multibeam echosounder; Fractal Span; GeoB20502-1; GeoB20509-1; GeoB20526-1; GeoB20532-1; GeoB20546-1; GeoB20558-1; GeoB20562-1; GeoB20570-1; GeoB20580-1; Grab; GRAB; Height of mound; Identification; LATITUDE; Length of axis ortoghonal to PAX; Length of principal axis; LONGITUDE; Lophelia pertusa; M122; M122_004-1; M122_021-1; M122_027-1; M122_041-1; M122_053-1; M122_057-1; M122_065-1; M122_075-1; M122_1348-1; Maria S. Merian; MB_PS; Meteor (1986); Morphometry; Mound footprint polygon; Mound height/PAX length ratio; MSM20/014-4-2; MSM20/1; MSM20/1_0_Underway-2; Multibeam/Parasound; Nearest polygon identification number; Net area; Number of nodes; Parameter; Perimeter; Principal axes ratio; Ratio between 3D surface and planar surface; Slope; Slope, average, underlying; Slope, average, underlying standard deviation; Slope, maximum underlying; Slope, standard deviation; Slope angle; Volume; WALPASS
    Materialart: Dataset
    Format: text/tab-separated-values, 22222 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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