Paleoenvironmental changes during the Late Pleistocene in Buenos Aires province (Argentina), using foraminifera fauna as proxy data
This paper describes the lithological and micropaleontological characteristics of a new record corresponding to the last interglacial for Buenos Aires province. Foraminifera were analyzed from an artificial outcrop 4 m thick (36◦34′0.97″ S and 57◦22′54.43″ W), from the quarry situated in the town of...
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| Formato: | Articulo |
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2023
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| Acceso en línea: | http://sedici.unlp.edu.ar/handle/10915/168996 |
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I19-R120-10915-1689962024-08-23T20:04:54Z http://sedici.unlp.edu.ar/handle/10915/168996 Paleoenvironmental changes during the Late Pleistocene in Buenos Aires province (Argentina), using foraminifera fauna as proxy data Petriella, Julieta Bernasconi, Emiliana Fucks, Enrique Eduardo 2023-12-22 2024-08-23T14:42:01Z en Ciencias Naturales Late Pleistocene Benthic foraminifera Puente de Pascua Formation General Conesa site South America This paper describes the lithological and micropaleontological characteristics of a new record corresponding to the last interglacial for Buenos Aires province. Foraminifera were analyzed from an artificial outcrop 4 m thick (36◦34′0.97″ S and 57◦22′54.43″ W), from the quarry situated in the town of General Conesa, Buenos Aires province at an approximate elevation of 4 m a.s.l. Benthic foraminifera fauna was constituted by a predominance of calcareous forms represented mostly by the species Buccella peruviana and Ammonia parkinsoniana. The micropaleontological and lithological characteristics of all the sedimentary units involved in this locality suggest deposits associated with a transition from a low-energy shallow intertidal or subtidal zone to a higher-energy beach or supratidal environment. Although, the topographic height does not enable conclusive assignment of the age of this coastal deposit (>79.500 kyr), the environmental conditions could be correlated with the penultimate transgressive event that occurred at the beginning of the Late Pleistocene (MIS 5), which would have occurred in a shallow environment with changes in the marine influence. These findings provide new information that contributes to better understanding of the paleoenvironmental evolution of this region where two marine transgressions and two wind deposits have been recognized. Centro de Estudios Integrales de la Dinámica Exógena Articulo Articulo http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) application/pdf |
| institution |
Universidad Nacional de La Plata |
| institution_str |
I-19 |
| repository_str |
R-120 |
| collection |
SEDICI (UNLP) |
| language |
Inglés |
| topic |
Ciencias Naturales Late Pleistocene Benthic foraminifera Puente de Pascua Formation General Conesa site South America |
| spellingShingle |
Ciencias Naturales Late Pleistocene Benthic foraminifera Puente de Pascua Formation General Conesa site South America Petriella, Julieta Bernasconi, Emiliana Fucks, Enrique Eduardo Paleoenvironmental changes during the Late Pleistocene in Buenos Aires province (Argentina), using foraminifera fauna as proxy data |
| topic_facet |
Ciencias Naturales Late Pleistocene Benthic foraminifera Puente de Pascua Formation General Conesa site South America |
| description |
This paper describes the lithological and micropaleontological characteristics of a new record corresponding to the last interglacial for Buenos Aires province. Foraminifera were analyzed from an artificial outcrop 4 m thick (36◦34′0.97″ S and 57◦22′54.43″ W), from the quarry situated in the town of General Conesa, Buenos Aires province at an approximate elevation of 4 m a.s.l. Benthic foraminifera fauna was constituted by a predominance of calcareous forms represented mostly by the species Buccella peruviana and Ammonia parkinsoniana. The micropaleontological and lithological characteristics of all the sedimentary units involved in this locality suggest deposits associated with a transition from a low-energy shallow intertidal or subtidal zone to a higher-energy beach or supratidal environment. Although, the topographic height does not enable conclusive assignment of the age of this coastal deposit (>79.500 kyr), the environmental conditions could be correlated with the penultimate transgressive event that occurred at the beginning of the Late Pleistocene (MIS 5), which would have occurred in a shallow environment with changes in the marine influence. These findings provide new information that contributes to better understanding of the paleoenvironmental evolution of this region where two marine transgressions and two wind deposits have been recognized. |
| format |
Articulo Articulo |
| author |
Petriella, Julieta Bernasconi, Emiliana Fucks, Enrique Eduardo |
| author_facet |
Petriella, Julieta Bernasconi, Emiliana Fucks, Enrique Eduardo |
| author_sort |
Petriella, Julieta |
| title |
Paleoenvironmental changes during the Late Pleistocene in Buenos Aires province (Argentina), using foraminifera fauna as proxy data |
| title_short |
Paleoenvironmental changes during the Late Pleistocene in Buenos Aires province (Argentina), using foraminifera fauna as proxy data |
| title_full |
Paleoenvironmental changes during the Late Pleistocene in Buenos Aires province (Argentina), using foraminifera fauna as proxy data |
| title_fullStr |
Paleoenvironmental changes during the Late Pleistocene in Buenos Aires province (Argentina), using foraminifera fauna as proxy data |
| title_full_unstemmed |
Paleoenvironmental changes during the Late Pleistocene in Buenos Aires province (Argentina), using foraminifera fauna as proxy data |
| title_sort |
paleoenvironmental changes during the late pleistocene in buenos aires province (argentina), using foraminifera fauna as proxy data |
| publishDate |
2023 |
| url |
http://sedici.unlp.edu.ar/handle/10915/168996 |
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AT petriellajulieta paleoenvironmentalchangesduringthelatepleistoceneinbuenosairesprovinceargentinausingforaminiferafaunaasproxydata AT bernasconiemiliana paleoenvironmentalchangesduringthelatepleistoceneinbuenosairesprovinceargentinausingforaminiferafaunaasproxydata AT fucksenriqueeduardo paleoenvironmentalchangesduringthelatepleistoceneinbuenosairesprovinceargentinausingforaminiferafaunaasproxydata |
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