Littorina Sea

E38554

The Littorina Sea was a post-glacial brackish stage of the Baltic basin that existed after the Ice Age, characterized by higher salinity and sea levels than the modern Baltic Sea.


Statements (47)
Predicate Object
instanceOf paleogeographic water body
post-glacial brackish water stage
chronologicalPosition Holocene
connectedTo North Sea
connectedVia Danish straits
endTime late Holocene
follows Ancylus Lake
formedAfter Weichselian glaciation
last Ice Age
hasCause eustatic sea-level rise
post-glacial isostatic rebound
hasCharacteristicFauna Littorina littorea
marine molluscs
other marine gastropods
hasClimateContext Holocene climatic optimum
hasEvidenceFrom mollusc assemblages
pollen records
raised beaches
shoreline terraces
hasHigherSalinityCause stronger connection to North Sea
wider and deeper Danish straits
hasHydrologicalRelation less marine-influenced than fully marine Baltic stages
more marine-influenced than Ancylus Lake
hasMaximumExtent larger than modern Baltic Sea
hasSalinity higher than modern Baltic Sea
hasSedimentType Littorina transgression deposits
marine-influenced brackish sediments
hasShoreline higher than present Baltic shoreline in many areas
hasTransgression Littorina transgression
hasWaterLevel higher than modern Baltic Sea
hasWaterType brackish water
influencedCoastlineOf Baltic states
Denmark
Finland
Germany
Poland
Sweden
isStageOf Baltic Sea development history
locatedIn Baltic region
locatedOn Northern Europe
namedAfter Littorina littorea
partOf Baltic Sea basin
precedes Limnea Sea
startTime early Holocene
studiedInDiscipline Quaternary geology
marine geology
paleogeography

Referenced by (2)
Subject (surface form when different) Predicate
Ancylus Lake
followedBy
Baltic Sea
precededBy

Please wait…