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Holocene evolution of coastal wetlands in wet-tropical northeastern AustraliaCentre for Palynology and Palaeoecology, Department of Geography and Environmental Science, Monash University, Clayton 3168, Australia
Geology Department, James Cook University of North Queensland, Townsville 4811, Australia Pollen in sediments drilled from the Innisfail coastal plain, northeast Queensland, Australia, was examined to reconstruct the evolution of Holocene wetlands in a wet-tropical environment. In contrast to monsoonal Australia, stable environmental conditions created by year-round rainfall and low tidal range caused abrupt, unidirectional transitions in wetland zonation as marine influence changed. This has enabled a detailed reconstruction of the marine transgression and subsequent progradation. Mangroves colonized in response to marine transgression at c. 7400 BP, as riverine mangroves of low salt tolerance migrated up the Mulgrave River. These were replaced around 7000 BP by extensive Rhizophora-dominated mangroves, coinciding with the development of a Rhizophora-dominated community in Wyvuri embayment. Mangroves reached their greatest extent as sea-level rise slowed towards 6000 BP, with a stillstand indicated by a brief return to terrestrial conditions at one site. High freshwater input depressed salt intrusion in the upper reaches of the Mulgrave estuary and prevented the development of hypersalinity in the upper tidal zone. Drainage conditions then controlled whether mangroves were succeeded by freshwater swamp or swamp-forest.
Key Words: Holocene • mangroves • pollen • sea-level history • tropics • vegetation history • wetlands • Australia.
The Holocene, Vol. 5, No. 4,
385-399 (1995) This article has been cited by other articles:
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