Paleoenvironment of the Toropí Formation (Upper Pleistocene), Corrientes province (Mesopotamian region, Argentina): A phytolith approach
Two Pleistocene sedimentary units are recognized in the Corrientes province, Argentina: the Toropí and Yupoí formations. These sediments have proven productive for fossil vertebrates, but few macrofossils have been recovered. To remedy this situation, plant silica (phytoliths) were extracted from th...
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Autores principales: | , , , , |
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Formato: | Articulo Preprint |
Lenguaje: | Inglés |
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2013
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Acceso en línea: | http://sedici.unlp.edu.ar/handle/10915/96375 https://ri.conicet.gov.ar/11336/76276 |
Aporte de: |
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I19-R120-10915-96375 |
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dspace |
institution |
Universidad Nacional de La Plata |
institution_str |
I-19 |
repository_str |
R-120 |
collection |
SEDICI (UNLP) |
language |
Inglés |
topic |
Geología Phytolith Mesopotamia Late pleistocene Paleoenvironment |
spellingShingle |
Geología Phytolith Mesopotamia Late pleistocene Paleoenvironment Erra, Georgina Osterrieth, Margarita Luisa Zurita, Alfredo Eduardo Francia, Analía Carlini, Alfredo Armando Paleoenvironment of the Toropí Formation (Upper Pleistocene), Corrientes province (Mesopotamian region, Argentina): A phytolith approach |
topic_facet |
Geología Phytolith Mesopotamia Late pleistocene Paleoenvironment |
description |
Two Pleistocene sedimentary units are recognized in the Corrientes province, Argentina: the Toropí and Yupoí formations. These sediments have proven productive for fossil vertebrates, but few macrofossils have been recovered. To remedy this situation, plant silica (phytoliths) were extracted from the sediments, enabling a direct comparison of paleovegetation data and information based on previous study of vertebrates. The studied samples (n = 28) come from two profiles from the Toropí Stream (28°36'S; 59°02'W), near Bella Vista, Corrientes, from which two Quaternary mammals, Lestodon (Xenarthra) and Hippocamelus (Artiodactyla), have previously been excavated. All samples were productive and contained both non-plant biogenic silica (diatoms, sponge spicular, chrysophyte cysts) and phytoliths. Phytolith assemblages were dominated by morphotypes diagnostic of grasses, in particular C 3 pooids, C 4 chloridoids, and C 3 or C 4 panicoids (or related grasses in the PACMAD clade). Rare phytoliths of palms and other woody or herbaceous dicotyledonous angiosperms were also present. This combination of C 3 and C 4 grasses, and rare palms and other forest indicators, indicates grass-dominated habitats with groves with palms and other trees/shrubs along rivers, growing under a relatively warm and dry climate. This mixed plant community reflects shifting biogeographic affinity with the Chaco-Pampean plain and inter-tropical regions, respectively, linked to the frequent climatic-environmental fluctuations during the Late Pleistocene. |
format |
Articulo Preprint |
author |
Erra, Georgina Osterrieth, Margarita Luisa Zurita, Alfredo Eduardo Francia, Analía Carlini, Alfredo Armando |
author_facet |
Erra, Georgina Osterrieth, Margarita Luisa Zurita, Alfredo Eduardo Francia, Analía Carlini, Alfredo Armando |
author_sort |
Erra, Georgina |
title |
Paleoenvironment of the Toropí Formation (Upper Pleistocene), Corrientes province (Mesopotamian region, Argentina): A phytolith approach |
title_short |
Paleoenvironment of the Toropí Formation (Upper Pleistocene), Corrientes province (Mesopotamian region, Argentina): A phytolith approach |
title_full |
Paleoenvironment of the Toropí Formation (Upper Pleistocene), Corrientes province (Mesopotamian region, Argentina): A phytolith approach |
title_fullStr |
Paleoenvironment of the Toropí Formation (Upper Pleistocene), Corrientes province (Mesopotamian region, Argentina): A phytolith approach |
title_full_unstemmed |
Paleoenvironment of the Toropí Formation (Upper Pleistocene), Corrientes province (Mesopotamian region, Argentina): A phytolith approach |
title_sort |
paleoenvironment of the toropí formation (upper pleistocene), corrientes province (mesopotamian region, argentina): a phytolith approach |
publishDate |
2013 |
url |
http://sedici.unlp.edu.ar/handle/10915/96375 https://ri.conicet.gov.ar/11336/76276 |
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Repositorios |
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1764820492069371904 |