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Development of sedimentary strata in Eckernförde Bay, southwestern Baltic Sea (1996)

Bentley, S. J. ; Nittrouer, C. A. ; Sommerfield, C. K.

Springer

Geo-marine letters 16 (1996), S. 148-154

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ISSN: 1432-1157

Source: Springer Online Journal Archives 1860-2000

Topics: Geosciences

Notes: Abstract Sediment in central Eckernförde Bay is characterized by beds of clay-sized material, with slightly coarser laminations (~ 10% silt and sand). Excess234Th activity indicates that mixing is limited to the upper 1 cm. Accumulation rates (210Pb geochronology) range from 3 to over 10 mm yr−1. Relatively high accumulation rates and absence of a significant mixed layer in the central bay allow fluctuations of sedimentological processes to be recorded in detail. Sediment-transport studies suggest that the laminations are caused by alternating deposition of storm-suspended sediments from adjacent shallow-water and fair-weather supply of fine suspended material advected from Kiel Bight.

Type of Medium: Electronic Resource

URL: http://dx.doi.org/10.1007/BF01204502

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