Tsunami vs storm origin for shell bed deposits in a lagoon enviroment: an example from the Upper Cretaceous of Southern Patagonia, Argentina
The criteria by which the deposits of tsunamis are distiguished from other deposits, including storm surges, have been controversial for more than 10 years. The Mata Amarilla Formation of the lower Upper Cretaceous of Southern Patagonia has excellent outcrops that in its lower section, sedimentary...
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| Format: | Article |
| Language: | English |
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Asociación Argentina de Sedimentología
2021-03-01
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| Series: | Latin American Journal of Sedimentology and Basin Analysis |
| Subjects: | |
| Online Access: | https://lajsba.sedimentologia.org.ar/index.php/lajsba/article/view/168 |
| _version_ | 1797386569956458496 |
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| author | Augusto N. Varela Sebastian Richiano Daniel G. Poiré |
| author_facet | Augusto N. Varela Sebastian Richiano Daniel G. Poiré |
| author_sort | Augusto N. Varela |
| collection | DOAJ |
| description |
The criteria by which the deposits of tsunamis are distiguished from other deposits, including storm surges, have been controversial for more than 10 years. The Mata Amarilla Formation of the lower Upper Cretaceous of Southern Patagonia has excellent outcrops that in its lower section, sedimentary and taphonomic characteristics suggest a tsunami origin. This paper presents details of these aspects, as well as a model of temporal stages that led to their deposition within a lagoon. The sediments are composed of alternating white sandstones and mudstones, with interbedded bioclastic accumulations in the lower section. The depositional environment was characterised by a lagoon bounded by shallow marine bars. These fine-grained sediments are sporadically interrupted by tsunami events represented by coquinas, bioclastic sands and shell pavements with allochthonous and autochthonous mollusk associations from freshwater and marine habitats. Some areas of the lagoon became exposed, thus enabling the development of vegetation on the substrate and pedogenic processes. Subsequently, a forced regression occurred when a fluvial system invaded the lagoon area, representing the beginning of the deposition of the middle section of the Mata Amarilla Formation.
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| first_indexed | 2024-03-08T22:12:21Z |
| format | Article |
| id | doaj.art-6c327711da8b4b0eb18aa1effe9f9193 |
| institution | Directory Open Access Journal |
| issn | 1669-7316 1851-4979 |
| language | English |
| last_indexed | 2024-03-08T22:12:21Z |
| publishDate | 2021-03-01 |
| publisher | Asociación Argentina de Sedimentología |
| record_format | Article |
| series | Latin American Journal of Sedimentology and Basin Analysis |
| spelling | doaj.art-6c327711da8b4b0eb18aa1effe9f91932023-12-19T06:17:26ZengAsociación Argentina de SedimentologíaLatin American Journal of Sedimentology and Basin Analysis1669-73161851-49792021-03-01181Tsunami vs storm origin for shell bed deposits in a lagoon enviroment: an example from the Upper Cretaceous of Southern Patagonia, ArgentinaAugusto N. VarelaSebastian RichianoDaniel G. Poiré The criteria by which the deposits of tsunamis are distiguished from other deposits, including storm surges, have been controversial for more than 10 years. The Mata Amarilla Formation of the lower Upper Cretaceous of Southern Patagonia has excellent outcrops that in its lower section, sedimentary and taphonomic characteristics suggest a tsunami origin. This paper presents details of these aspects, as well as a model of temporal stages that led to their deposition within a lagoon. The sediments are composed of alternating white sandstones and mudstones, with interbedded bioclastic accumulations in the lower section. The depositional environment was characterised by a lagoon bounded by shallow marine bars. These fine-grained sediments are sporadically interrupted by tsunami events represented by coquinas, bioclastic sands and shell pavements with allochthonous and autochthonous mollusk associations from freshwater and marine habitats. Some areas of the lagoon became exposed, thus enabling the development of vegetation on the substrate and pedogenic processes. Subsequently, a forced regression occurred when a fluvial system invaded the lagoon area, representing the beginning of the deposition of the middle section of the Mata Amarilla Formation. https://lajsba.sedimentologia.org.ar/index.php/lajsba/article/view/168Tsunami Deposits, Washover Deposits, Littoral Deposits, Taphonomy, Austral Basin, Mata Amarilla Formation |
| spellingShingle | Augusto N. Varela Sebastian Richiano Daniel G. Poiré Tsunami vs storm origin for shell bed deposits in a lagoon enviroment: an example from the Upper Cretaceous of Southern Patagonia, Argentina Latin American Journal of Sedimentology and Basin Analysis Tsunami Deposits, Washover Deposits, Littoral Deposits, Taphonomy, Austral Basin, Mata Amarilla Formation |
| title | Tsunami vs storm origin for shell bed deposits in a lagoon enviroment: an example from the Upper Cretaceous of Southern Patagonia, Argentina |
| title_full | Tsunami vs storm origin for shell bed deposits in a lagoon enviroment: an example from the Upper Cretaceous of Southern Patagonia, Argentina |
| title_fullStr | Tsunami vs storm origin for shell bed deposits in a lagoon enviroment: an example from the Upper Cretaceous of Southern Patagonia, Argentina |
| title_full_unstemmed | Tsunami vs storm origin for shell bed deposits in a lagoon enviroment: an example from the Upper Cretaceous of Southern Patagonia, Argentina |
| title_short | Tsunami vs storm origin for shell bed deposits in a lagoon enviroment: an example from the Upper Cretaceous of Southern Patagonia, Argentina |
| title_sort | tsunami vs storm origin for shell bed deposits in a lagoon enviroment an example from the upper cretaceous of southern patagonia argentina |
| topic | Tsunami Deposits, Washover Deposits, Littoral Deposits, Taphonomy, Austral Basin, Mata Amarilla Formation |
| url | https://lajsba.sedimentologia.org.ar/index.php/lajsba/article/view/168 |
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