A submarine canyon as a climate archive - Interaction of the antarctic intermediate water with the mar del plata canyon (southwest atlantic)

The Mar del Plata Canyon is located at the continental margin off northern Argentina in a key intermediate and deep-water oceanographic setting. In this region, strong contour currents shape the continental margin by eroding, transporting and depositing sediments. These currents generate various dep...

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Detalles Bibliográficos
Autores principales: Voigt, I., Henrich, R., Preu, B.M., Piola, A.R., Hanebuth, T.J.J., Schwenk, T., Chiessi, C.M.
Formato: JOUR
Materias:
Antarctic Intermediate Water
Drift deposition
El Niño/Southern Oscillation (ENSO)
Southwest Atlantic
Submarine Canyon
Antarctic intermediate waters
Continuous deposition
Contourite depositional systems
Sedimentation process
Submarine canyon
Upper ocean circulation
Deposits
Sedimentation
Sedimentology
Silt
Submarines
Sediments
bioturbation
continental margin
El Nino-Southern Oscillation
episodic event
Holocene
late glacial
nepheloid layer
paleoceanography
paleoclimate
pelagic deposit
sediment transport
sedimentation
silt
submarine canyon
upper ocean
Argentina
Buenos Aires [Argentina]
Mar del Plata Harbor
Pacific Ocean
Pacific Ocean (Southwest)
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00253227_v341_n_p46_Voigt
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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