Taphonomic modes on fluvial deposits of the Monte Hermoso Formation (early Pliocene), Buenos Aires province, Argentina
The sedimentary deposits of the Monte Hermoso Formation, outcropping at its type locality (Farola Monte Hermoso, Buenos Aires province, Argentina), accumulated through fluvial processes acting on highly sinuous rivers. The Monte Hermoso Formation comprises a rich vertebrate fauna corresponding to th...
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2013
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| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00310182_v369_n_p282_Tomassini http://hdl.handle.net/20.500.12110/paper_00310182_v369_n_p282_Tomassini |
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paper:paper_00310182_v369_n_p282_Tomassini2023-06-08T14:56:40Z Taphonomic modes on fluvial deposits of the Monte Hermoso Formation (early Pliocene), Buenos Aires province, Argentina Argentina Fluvial deposits Monte Hermoso Formation Pliocene Taphonomic modes Vertebrates depositional environment floodplain fluvial deposit fossil assemblage outcrop paleoenvironment Pliocene taphonomy Argentina Buenos Aires [Argentina] Vertebrata Zanclea The sedimentary deposits of the Monte Hermoso Formation, outcropping at its type locality (Farola Monte Hermoso, Buenos Aires province, Argentina), accumulated through fluvial processes acting on highly sinuous rivers. The Monte Hermoso Formation comprises a rich vertebrate fauna corresponding to the Montehermosan Stage/Age (early Pliocene), which includes numerous and diverse vertebrate remains. Comparative taphonomic analysis indicated that the faunal assemblages coming from two different fossiliferous levels, FL 1 and FL 2, recognized in floodplain deposits and channel deposits respectively, are composed of remains affected by diverse taphonomic processes and therefore representing distinct taphonomic histories. The variations recorded between both fossiliferous levels, with respect to their taphonomic attributes and sedimentary context, allowed the recognition of two distinct taphonomic modes: floodplain in the FL 1 and channel-lag in the FL 2. These taphonomic modes represent different conditions within the range of taphonomic histories for the Monte Hermoso Formation assemblage formed by attritional accumulation of remains. At the moment, continental systems linked to fluvial environments have been poorly analyzed for the South American Neogene; this study contributes new information on taphonomic and paleoenvironmental characteristics of this type of deposit. © 2012 Elsevier B.V. 2013 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00310182_v369_n_p282_Tomassini http://hdl.handle.net/20.500.12110/paper_00310182_v369_n_p282_Tomassini |
| institution |
Universidad de Buenos Aires |
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I-28 |
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R-134 |
| collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
| topic |
Argentina Fluvial deposits Monte Hermoso Formation Pliocene Taphonomic modes Vertebrates depositional environment floodplain fluvial deposit fossil assemblage outcrop paleoenvironment Pliocene taphonomy Argentina Buenos Aires [Argentina] Vertebrata Zanclea |
| spellingShingle |
Argentina Fluvial deposits Monte Hermoso Formation Pliocene Taphonomic modes Vertebrates depositional environment floodplain fluvial deposit fossil assemblage outcrop paleoenvironment Pliocene taphonomy Argentina Buenos Aires [Argentina] Vertebrata Zanclea Taphonomic modes on fluvial deposits of the Monte Hermoso Formation (early Pliocene), Buenos Aires province, Argentina |
| topic_facet |
Argentina Fluvial deposits Monte Hermoso Formation Pliocene Taphonomic modes Vertebrates depositional environment floodplain fluvial deposit fossil assemblage outcrop paleoenvironment Pliocene taphonomy Argentina Buenos Aires [Argentina] Vertebrata Zanclea |
| description |
The sedimentary deposits of the Monte Hermoso Formation, outcropping at its type locality (Farola Monte Hermoso, Buenos Aires province, Argentina), accumulated through fluvial processes acting on highly sinuous rivers. The Monte Hermoso Formation comprises a rich vertebrate fauna corresponding to the Montehermosan Stage/Age (early Pliocene), which includes numerous and diverse vertebrate remains. Comparative taphonomic analysis indicated that the faunal assemblages coming from two different fossiliferous levels, FL 1 and FL 2, recognized in floodplain deposits and channel deposits respectively, are composed of remains affected by diverse taphonomic processes and therefore representing distinct taphonomic histories. The variations recorded between both fossiliferous levels, with respect to their taphonomic attributes and sedimentary context, allowed the recognition of two distinct taphonomic modes: floodplain in the FL 1 and channel-lag in the FL 2. These taphonomic modes represent different conditions within the range of taphonomic histories for the Monte Hermoso Formation assemblage formed by attritional accumulation of remains. At the moment, continental systems linked to fluvial environments have been poorly analyzed for the South American Neogene; this study contributes new information on taphonomic and paleoenvironmental characteristics of this type of deposit. © 2012 Elsevier B.V. |
| title |
Taphonomic modes on fluvial deposits of the Monte Hermoso Formation (early Pliocene), Buenos Aires province, Argentina |
| title_short |
Taphonomic modes on fluvial deposits of the Monte Hermoso Formation (early Pliocene), Buenos Aires province, Argentina |
| title_full |
Taphonomic modes on fluvial deposits of the Monte Hermoso Formation (early Pliocene), Buenos Aires province, Argentina |
| title_fullStr |
Taphonomic modes on fluvial deposits of the Monte Hermoso Formation (early Pliocene), Buenos Aires province, Argentina |
| title_full_unstemmed |
Taphonomic modes on fluvial deposits of the Monte Hermoso Formation (early Pliocene), Buenos Aires province, Argentina |
| title_sort |
taphonomic modes on fluvial deposits of the monte hermoso formation (early pliocene), buenos aires province, argentina |
| publishDate |
2013 |
| url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00310182_v369_n_p282_Tomassini http://hdl.handle.net/20.500.12110/paper_00310182_v369_n_p282_Tomassini |
| _version_ |
1768545867533385728 |