Rüggeberg, Andres; Dullo, Wolf-Christian; Dorschel, Boris; Hebbeln, Dierk (2007): Benthic foraminifera, stable isotope ratios and carbon concentrations of sediment cores from Propeller Mound and Porcupine Srabight. PANGAEA, https://doi.org/10.1594/PANGAEA.711838, Supplement to: Rüggeberg, A et al. (2007): Environmental changes and growth history of a cold-water carbonate mound (Propeller Mound, Porcupine Seabight). International Journal of Earth Sciences, 96(1), 57-72, https://doi.org/10.1007/s00531-005-0504-1
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On- and off-mound sediment cores from Propeller Mound (Hovland Mound province, Porcupine Seabight) were analysed to understand better the evolution of a carbonate mound. The evaluation of benthic foraminiferal assemblages from the off-mound position helps to determine the changes of the environmental controls on Propeller Mound in glacial and interglacial times. Two different assemblages describe the Holocene and Marine Isotope Stage (MIS) 2 and late MIS 3 (~31 kyr BP). The different assemblages are related to changes in oceanographic conditions, surface productivity and the waxing and waning of the British Irish Ice Sheet (BIIS) during the last glacial stages. The interglacial assemblage is related to a higher supply of organic material and stronger current intensities in water depth of recent coral growth. During the last glaciation the benthic faunas showed high abundances of cassidulinid species, implying cold bottom waters and a reduced availability of organic matter. High sedimentation rates and the domination of Elphidium excavatum point to shelf erosion related to sea-level lowering (~50 m) and the progradation of the BIIS onto the shelf. A different assemblage described for the on-mound core is dominated by Discanomalina coronata, Gavelinopsis translucens, Planulina ariminensis, Cibicides lobatulus and to a lower degree by Hyrrokkin sarcophaga. These species are only found or show significantly higher relative abundances in on-mound samples and their maximum contribution in the lower part of the record indicates a higher coral growth density on Propeller Mound in an earlier period. They are less abundant during the Holocene, however. This dataset portrays the boundary conditions of the habitable range for the cold-water coral Lophelia pertusa, which dominates the deep-water reefal ecosystem on the upper flanks of Propeller Mound. The growth of this ecosystem occurs during interglacial and interstadial periods, whereas a retreat of corals is documented in the absence of glacial sediments on-mound. Glacial conditions with cold intermediate waters, a weak current regime and high sedimentation rates provide an unfavourable environmental setting for Lophelia corals to grow. A Late Pleistocene decrease is observed in the mound growth for Propeller Mound, which might face its complete burial in the future, as it already happened to the buried mounds of the Magellan Mound province further north.
Dorschel, Boris (2003): Late Quaternary Development of a deep-water Carbonate Mound in the northeast Atlantic. PhD Thesis, Elektronische Dissertationen an der Staats- und Universitätsbibliothek Bremen, Germany, urn:nbn:de:gbv:46-diss000006917
Dorschel, Boris; Hebbeln, Dierk; Rüggeberg, Andres; Dullo, Wolf-Christian (2007): Carbonate budget of a cold-water coral carbonate mound: Propeller Mound, Porcupine Seabight. International Journal of Earth Sciences, 96(1), 73-83, https://doi.org/10.1007/s00531-005-0493-0
Dorschel, Boris; Hebbeln, Dierk; Rüggeberg, Andres; Dullo, Wolf-Christian; Freiwald, André (2005): Growth and Erosion of a Cold-Water Coral Covered Carbonate Mound in the Northeast Atlantic during the Late Pleistocene and Holocene. Earth and Planetary Science Letters, 233(1-2), 33-44, https://doi.org/10.1016/j.epsl.2005.01.035
Rüggeberg, Andres; Dorschel, Boris; Dullo, Wolf-Christian; Hebbeln, Dierk (2005): Sedimentary patterns in the vicinity of a carbonate mound in the Hovland Mound Province, northern Porcupine Seabight. In: Freiwald, A & Roberts, JM (eds.), 2005, Cold-water Corals and Ecosystems, Springer-Verlag, Berlin, Heidelberg, Part I, 87-112, https://doi.org/10.1007/3-540-27673-4_5
Median Latitude: 52.153175 * Median Longitude: -12.769100 * South-bound Latitude: 52.147683 * West-bound Longitude: -12.771367 * North-bound Latitude: 52.158667 * East-bound Longitude: -12.766833
Date/Time Start: 2000-09-24T09:35:00 * Date/Time End: 2000-09-24T17:34:00
GeoB6725-1 (POS485-1) * Latitude: 52.158667 * Longitude: -12.766833 * Date/Time: 2000-09-24T09:35:00 * Elevation: -820.0 m * Recovery: 4.5 m * Location: Porcupine Seabight * Campaign: POS265 * Basis: Poseidon * Method/Device: Gravity corer (Kiel type) (SL)
Datasets listed in this publication series
- Rüggeberg, A; Dullo, W-C; Dorschel, B et al. (2007): (Fig. 4) Assemblage of benthic foraminifera in sediment core GeoB6725-1. https://doi.org/10.1594/PANGAEA.351603
- Rüggeberg, A; Dullo, W-C; Dorschel, B et al. (2007): (Fig. 3) Carbonate analyses of sediment core GeoB6725-1. https://doi.org/10.1594/PANGAEA.134614
- Rüggeberg, A; Dullo, W-C; Dorschel, B et al. (2007): (Fig. 6) Assemblage of benthic foraminifera in sediment core GeoB6730-1. https://doi.org/10.1594/PANGAEA.351671
- Rüggeberg, A; Dullo, W-C; Dorschel, B et al. (2007): (Fig. 5) Carbonate analyses of sediment core GeoB6730-1. https://doi.org/10.1594/PANGAEA.134617