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Bibliographic Details
Main Authors: Lantzsch, Hendrik, Hanebuth, Till J J, Chiessi, Cristiano Mazur, Schwenk, Tilmann, Violante, Roberto
Format: Dataset Open Access
Language:en
Published: PANGAEA 2014
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.833301
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author Lantzsch, Hendrik
Hanebuth, Till J J
Chiessi, Cristiano Mazur
Schwenk, Tilmann
Violante, Roberto
author_facet Lantzsch, Hendrik
Hanebuth, Till J J
Chiessi, Cristiano Mazur
Schwenk, Tilmann
Violante, Roberto
collection Datos científicos de ciencias marinas y ambientales
contents The continental margin off the La Plata Estuary (SE South America) is characterized by high fluvial sediment supply and strong ocean currents. High-resolution sediment-acoustic data combined with sedimentary facies analysis, AMS-14C ages, and neodymium isotopic data allowed us to reconstruct late Quaternary sedimentary dynamics in relation to the two major sediment sources, the La Plata Estuary and the Argentine margin. Sediments from these two provinces show completely different dispersal patterns. We show that the northward-trending La Plata paleo-valley was the sole transit path for the huge volumes of fluvial material during lower sea levels. In contrast, material from the Argentine margin sector was transported northwards by the strong current system. Despite the large sediment volumes supplied by both sources, wide parts of the shelf were characterized by either persistent non-deposition or local short-term depocenter formation. The location and formation history of these depocenters were primarily controlled by the interplay of sea level with current strength and local morphology. The high sediment supply was of secondary importance to the stratigraphic construction, though locally resulting in high sedimentation rates. Thus, the shelf system off the La Plata Estuary can be considered as a hydrodynamic-controlled end-member.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_833301
institution PANGAEA
language en
publishDate 2014
publisher PANGAEA
record_format pangaea
spellingShingle Neodymium isotopic data, radiocarbon dates and calibrated ages of sediment samples off the La Plata Estuary, southeastern South America
Lantzsch, Hendrik
Hanebuth, Till J J
Chiessi, Cristiano Mazur
Schwenk, Tilmann
Violante, Roberto
Center for Marine Environmental Sciences; MARUM
The continental margin off the La Plata Estuary (SE South America) is characterized by high fluvial sediment supply and strong ocean currents. High-resolution sediment-acoustic data combined with sedimentary facies analysis, AMS-14C ages, and neodymium isotopic data allowed us to reconstruct late Quaternary sedimentary dynamics in relation to the two major sediment sources, the La Plata Estuary and the Argentine margin. Sediments from these two provinces show completely different dispersal patterns. We show that the northward-trending La Plata paleo-valley was the sole transit path for the huge volumes of fluvial material during lower sea levels. In contrast, material from the Argentine margin sector was transported northwards by the strong current system. Despite the large sediment volumes supplied by both sources, wide parts of the shelf were characterized by either persistent non-deposition or local short-term depocenter formation. The location and formation history of these depocenters were primarily controlled by the interplay of sea level with current strength and local morphology. The high sediment supply was of secondary importance to the stratigraphic construction, though locally resulting in high sedimentation rates. Thus, the shelf system off the La Plata Estuary can be considered as a hydrodynamic-controlled end-member.
title Neodymium isotopic data, radiocarbon dates and calibrated ages of sediment samples off the La Plata Estuary, southeastern South America
topic Center for Marine Environmental Sciences; MARUM
url https://doi.org/10.1594/PANGAEA.833301