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(Table 3) Average mound aggradation rates
*: one single age.AR: mound aggradation rate.Average mound aggradation rates (ARø; when available minimum and maximum ARs are given as well) calculated for core records obtained... -
Component analysis of selected sampling stations from the shallow Banc d' Arg...
This dataset has no description
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Radiocarbon measurements and age calibration of eroded mollusc shells from se...
This dataset has no description
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(Table 2) Loose-sediment quantification of seafloor sediment samples as perce...
This dataset has no description
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(Table 1) Details on the Uranium/Thorium age determinations carried out on co...
Cold-water corals are widely distributed along the Atlantic continental margin with varying growth patterns in relation to their specific environment. Here, we investigate the... -
(Tab. XIII.1) TOC content, carbonate content, carbonate mineralogy, percentag...
Modern carbonate sedimentation takes place on the northern Mauritanian shelf (20°N), where typical tropical components (e.g. hermatypic reefs, calcareous green algae) are... -
(Table 1) Quantitative analysis of mollusk taxa from surface sediment samples...
Ecological and taxonomic study of the mollusk-rich fauna of the Golfe d'Arguin, North Mauritania, investigates the various environmental influences affecting this tropical... -
(Table 1) Silt grain-size analysis of sediment surface samples in the Golfe d...
Continental shelf systems are highly dynamic sedimentary environments, where sediments from biogenic production as well as from terrigenous sources are redistributed in the... -
Radiocarbon measurements and loose-sediment quantification of seafloor sedime...
Heterozoan carbonates are typical for extratropical sedimentary systems. However, under mesotrophic to eutrophic conditions, heterozoan carbonates also form in tropical...
