Relationships between trophic state, paleosalinity and climatic changes during the first Holocene marine transgression in Rocha Lagoon, southern Uruguay

Journal of Paleolimnology

Volumn 35, Issue 4, 2006, Pages 699-713

  Inda, H ^a   Garcia Rodriguez F ^b   Del Puerto, L ^a   Acevedo, V ^a   Metzeltin, D ^c   Castineira C ^d   Bracco, R ^e   Adams, J B ^b  

^a FACULTAD DE CIENCIAS   (Uruguay)

^b NELSON MANDELA METROPOLITAN UNIVERSITY   (South Africa)

^c GOETHE UNIVERSITY   (Germany)

^d Museo Nacional de Historia Natural y Antropologia   (Uruguay)

^e UNIVERSIDAD DE LA REPÚBLICA   (Uruguay)

Author keywords

Climatic change; Diatoms; Holocene; Opal phytoliths; Sea level change; Trophic state; Uruguay

Indexed keywords

CARBONATE; CLIMATE CHANGE; DIATOM; ESTUARINE ENVIRONMENT; FRESHWATER ENVIRONMENT; HOLOCENE; HUMID ENVIRONMENT; MARINE ENVIRONMENT; MICROFOSSIL; ORGANIC MATTER; PALEOENVIRONMENT; PALEOLIMNOLOGY; PALEOSALINITY; PHYTOLITH; SEA LEVEL CHANGE; TRANSGRESSION; TROPHIC STATUS;

ROCHA [URUGUAY]; ROCHA LAGOON; SOUTH AMERICA; URUGUAY;

BACILLARIOPHYTA; CHRYSOPHYCEAE;

EID: 33745592181     PISSN: 09212728     EISSN: None     Source Type: Journal    
DOI: 10.1007/s10933-005-4841-7     Document Type: Article

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