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Cross-references
Coasts
Estuary, Estuarine Hydrodynamics
Integrated Coastal Zone Management
Marine Evaporites
Marine Sedimentary Basins
Ocean Margin Systems
Reef Coasts
Relative Sea-level (RSL) Cycle
Sea-Level
LAMINATED SEDIMENTS
Alan Kemp
Ocean and Earth Science, National Oceanography Centre
Southampton, University of Southampton Waterfront
Campus, Southampton, UK
Synonyms
Marine varves
Laminated sediments are characterized by the presence of
planar, bed-parallel layers that originate from changes in
particle composition or grain size, with thickness of the
order 1 cm or less. The physical processes involved in
the transport and deposition of sedimentary particles
may produce parallel laminae in sands or silts, but the term
“laminated sediment” is more commonly associated with
the formation of laminae by successive depositional or
“flux” events in hemipelagic or pelagic settings. Such
laminae may be of biogenic origin, formed by the
remains of marine phytoplankton such as diatoms or
coccolithophores, or in marine systems nearer land, may
comprise terrigenous clay and silt particles.
LAMINATED SEDIMENTS
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