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These sediments decrease progressively in grain size, carbonate content and shell debris away from the coast. They differ in the primary and biogenetic structures, degree of bioturbation, lebensspuren and content of fecal pellets.","descriptionType":"Abstract"},{"description":"Supplement to: Reineck, Hans-Erich (1973): Schichtung und Wühlgefüge in Grundproben vor der ostafrikanischen Küste. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C16, 67-81","descriptionType":"Other"}],"geoLocations":[{"geoLocationBox":{"eastBoundLongitude":"54.6666666666666","northBoundLatitude":"11.633","southBoundLatitude":"-2.733","westBoundLongitude":"42.466"}},{"geoLocationPlace":"Western Arabian 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