The hypertidal Santa Cruz–Chico River estuary (South Patagonia, Argentina): A hybrid ria-type system under extreme tides, arid climate and active uplift

The present study focuses on the morphosedimentary organization and sediment infilling stratigraphy of one of the largest estuaries of southern Patagonia in Argentina. With a tidal range up to 12 m, the area is subject to extreme tidal conditions, combined with moderate offshore wave climate, strong...

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Published inSedimentary geology Vol. 471; p. 106728
Main Authors Tessier, Bernadette, Reynaud, Jean-Yves, Cuitiño, Jose I., Scasso, Roberto A., Pancrazzi, Léo, Duperron, Maria, Weill, Pierre, Bout-Roumazeilles, Viviane, du Châtelet, Eric Armynot, Kuinkel, Anjana, Lortie, Thibaud, Dezileau, Laurent
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.09.2024
Elsevier
Subjects
Argentina
arid zones
basins
continental shelf
estuaries
fauna
geochemistry
Geophysics
ground-penetrating radar
Holocene epoch
Holocene stratigraphy
hybrids
Incised-valley
mineralogy
Miocene epoch
Pleistocene epoch
river valleys
rivers
Sciences of the Universe
sea level
Sediment by-pass
sediment transport
sediments
South America
stratigraphy
Tides
Argentina
South America
Sediment by-pass
Incised-valley
Holocene stratigraphy
Tides
Geophysics
icised-valley tides
geophysics
sediment by-pass
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Abstract The present study focuses on the morphosedimentary organization and sediment infilling stratigraphy of one of the largest estuaries of southern Patagonia in Argentina. With a tidal range up to 12 m, the area is subject to extreme tidal conditions, combined with moderate offshore wave climate, strong and constant westerly winds, and contrasted water and sediment discharges from the two tributaries of the estuary, the Santa Cruz and Chico rivers. The estuarine valley is entrenched in the Patagonian coastal plateau due to significant uplift. On the basis of sediment facies (sedimentary structures, grain size, geochemistry, mineralogy), meiofauna (foraminifera and testate amoebae), morphological changes and shallow geophysics (high-resolution seismic reflection, ground-penetrating radar) data, the Santa Cruz–Chico River system is defined as a hybrid system comprising a tide-influenced fluvial mouth (the Santa Cruz River) and a tide-dominated estuary (the Chico River estuary), both converging toward an elongated subtidal ria-type estuarine basin. River-supplied sands and muds by-pass the estuarine basin and are exported offshore where they settle and form an ebb-tidal delta. Sediments in the Santa Cruz–Chico River valley mainly consist of Pleistocene lowstand fluvial gravels resting on the regional Miocene substrate, and thin early Holocene transgressive deposits, deeply incised by a tidal ravinement surface that developed during the highest Holocene sea-level at ca 7500 y. BP. After the maximum stillstand, relative sea level fell and a competition occurred between erosion, promoted by water depth decrease, and deposition, favored by tidal prism reduction. At present, sediment by-passing and offshore sediment export are the dominant processes. The very large size of the ebb-tidal delta, which expands on the continental shelf, suggests that this situation has prevailed for a very long time.
AbstractList The present study focuses on the morphosedimentary organization and sediment infilling stratigraphy of one of the largest estuaries of southern Patagonia in Argentina. With a tidal range up to 12 m, the area is subject to extreme tidal conditions, combined with moderate offshore wave climate, strong and constant westerly winds, and contrasted water and sediment discharges from the two tributaries of the estuary, the Santa Cruz and Chico rivers. The estuarine valley is entrenched in the Patagonian coastal plateau due to significant uplift. On the basis of sediment facies (sedimentary structures, grain size, geochemistry, mineralogy), meiofauna (foraminifera and testate amoebae), morphological changes and shallow geophysics (high-resolution seismic reflection, ground-penetrating radar) data, the Santa Cruz–Chico River system is defined as a hybrid system comprising a tide-influenced fluvial mouth (the Santa Cruz River) and a tide-dominated estuary (the Chico River estuary), both converging toward an elongated subtidal ria-type estuarine basin. River-supplied sands and muds by-pass the estuarine basin and are exported offshore where they settle and form an ebb-tidal delta. Sediments in the Santa Cruz–Chico River valley mainly consist of Pleistocene lowstand fluvial gravels resting on the regional Miocene substrate, and thin early Holocene transgressive deposits, deeply incised by a tidal ravinement surface that developed during the highest Holocene sea-level at ca 7500 y. BP. After the maximum stillstand, relative sea level fell and a competition occurred between erosion, promoted by water depth decrease, and deposition, favored by tidal prism reduction. At present, sediment by-passing and offshore sediment export are the dominant processes. The very large size of the ebb-tidal delta, which expands on the continental shelf, suggests that this situation has prevailed for a very long time.
The present study focuses on the morphosedimentary organization and sediment infilling stratigraphy of one of the largest estuaries of southern Patagonia in Argentina. With a tidal range up to 12 m, the area is subject to extreme tidal conditions, combined with moderate offshore wave climate, strong and constant westerly winds, and contrasted water and sediment discharges from the two tributaries of the estuary, the Santa Cruz and Chico Rivers. The estuarine valley is entrenched in the Patagonian coastal plateau due to significant uplift. On the basis of sediment facies (sedimentary structures, grain size, geochemistry, mineralogy), meiofauna (foraminifera and testate amoebae), morphological changes and shallow geophysics (high-resolution seismic reflection, ground-penetrating radar) data, the Santa Cruz-Chico River system is defined as a hybrid system comprising a tide-influenced fluvial mouth (the Santa Cruz River) and a tide-dominated estuary (the Chico River estuary), both converging towards an elongated subtidal ria-type estuarine basin. River-supplied sands and muds by-pass the estuarine basin and are exported offshore where they settle and form an ebb-tidal delta. Sediments in the Santa Cruz-Chico River valley mainly consists of Pleistocene lowstand fluvial gravels resting on the regional Miocene substrate, and thin early Holocene transgressive deposits, deeply incised by a tidal ravinement surface that developed during the highest Holocene sea-level at ca 7500 yr. BP. After the maximumstillstand, relative sea level fell and a competition occurred between erosion, promoted by water depth decrease, and deposition, favoured by tidal prism reduction. At present, sediment by-passing and offshore sediment export are the dominant processes. The very large size of the ebb-tidal delta, which expands on the continental shelf, suggests that this situation has prevailed for a very long time.
ArticleNumber 106728
Author Tessier, Bernadette
Lortie, Thibaud
Duperron, Maria
Weill, Pierre
Kuinkel, Anjana
du Châtelet, Eric Armynot
Bout-Roumazeilles, Viviane
Pancrazzi, Léo
Reynaud, Jean-Yves
Scasso, Roberto A.
Cuitiño, Jose I.
Dezileau, Laurent
Author_xml – sequence: 1
  givenname: Bernadette
  surname: Tessier
  fullname: Tessier, Bernadette
  email: bernadette.tessier@unicaen.fr
  organization: Université de Caen Normandie, CNRS, Univ Rouen Normandie, Normandie Univ, UMR 6143 M2C, 14000 Caen, France
– sequence: 2
  givenname: Jean-Yves
  surname: Reynaud
  fullname: Reynaud, Jean-Yves
  organization: Univ. Lille, CNRS, Univ. Littoral Côte d'Opale, UMR 8187 LOG, F 59000 Lille, France
– sequence: 3
  givenname: Jose I.
  surname: Cuitiño
  fullname: Cuitiño, Jose I.
  organization: IPGP-CENPAT-CONICET - Puerto Madryn, Chubut, Argentina
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  givenname: Roberto A.
  surname: Scasso
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– sequence: 6
  givenname: Maria
  surname: Duperron
  fullname: Duperron, Maria
  organization: IGeBA, Dpto. de Cs. Geológicas, Universidad de Buenos Aires - CONICET, Argentina
– sequence: 7
  givenname: Pierre
  surname: Weill
  fullname: Weill, Pierre
  organization: Université de Caen Normandie, CNRS, Univ Rouen Normandie, Normandie Univ, UMR 6143 M2C, 14000 Caen, France
– sequence: 8
  givenname: Viviane
  surname: Bout-Roumazeilles
  fullname: Bout-Roumazeilles, Viviane
  organization: Univ. Lille, CNRS, Univ. Littoral Côte d'Opale, UMR 8187 LOG, F 59000 Lille, France
– sequence: 9
  givenname: Eric Armynot
  surname: du Châtelet
  fullname: du Châtelet, Eric Armynot
  organization: Univ. Lille, CNRS, Univ. Littoral Côte d'Opale, UMR 8187 LOG, F 59000 Lille, France
– sequence: 10
  givenname: Anjana
  surname: Kuinkel
  fullname: Kuinkel, Anjana
  organization: Univ. Lille, CNRS, Univ. Littoral Côte d'Opale, UMR 8187 LOG, F 59000 Lille, France
– sequence: 11
  givenname: Thibaud
  surname: Lortie
  fullname: Lortie, Thibaud
  organization: Université de Caen Normandie, CNRS, Univ Rouen Normandie, Normandie Univ, UMR 6143 M2C, 14000 Caen, France
– sequence: 12
  givenname: Laurent
  surname: Dezileau
  fullname: Dezileau, Laurent
  organization: Université de Caen Normandie, CNRS, Univ Rouen Normandie, Normandie Univ, UMR 6143 M2C, 14000 Caen, France
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Keywords South America
Sediment by-pass
Incised-valley
Holocene stratigraphy
Tides
Geophysics
icised-valley tides
geophysics
sediment by-pass
Language English
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Snippet The present study focuses on the morphosedimentary organization and sediment infilling stratigraphy of one of the largest estuaries of southern Patagonia in...
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SubjectTerms Argentina
arid zones
basins
continental shelf
estuaries
fauna
geochemistry
Geophysics
ground-penetrating radar
Holocene epoch
Holocene stratigraphy
hybrids
Incised-valley
mineralogy
Miocene epoch
Pleistocene epoch
river valleys
rivers
Sciences of the Universe
sea level
Sediment by-pass
sediment transport
sediments
South America
stratigraphy
Tides
Title The hypertidal Santa Cruz–Chico River estuary (South Patagonia, Argentina): A hybrid ria-type system under extreme tides, arid climate and active uplift
URI https://dx.doi.org/10.1016/j.sedgeo.2024.106728
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https://hal.science/hal-04777131
Volume 471
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