Palynological record of the Paleogene Río Leona Formation (southernmost South America): Stratigraphical and paleoenvironmental implications

Terrestrial palynomorph assemblages have been recovered from the Río Leona Formation, southwestern Santa Cruz Province, southern South America. Organic debris (spores, pollen grains, fresh water algae, plant tissues and fungi) are preserved in shales associated with other plant fossil remains (leave...

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Published in:Review of Palaeobotany and Palynology
Main Authors: Barreda, Viviana Dora, Palazzesi, Luis, Marenssi, Sergio Alfredo
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier Science
Subjects:
Online Access:http://hdl.handle.net/11336/102731
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author Barreda, Viviana Dora
Palazzesi, Luis
Marenssi, Sergio Alfredo
author_facet Barreda, Viviana Dora
Palazzesi, Luis
Marenssi, Sergio Alfredo
author_sort Barreda, Viviana Dora
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 1-4
container_start_page 22
container_title Review of Palaeobotany and Palynology
container_volume 154
description Terrestrial palynomorph assemblages have been recovered from the Río Leona Formation, southwestern Santa Cruz Province, southern South America. Organic debris (spores, pollen grains, fresh water algae, plant tissues and fungi) are preserved in shales associated with other plant fossil remains (leaves and wood). The Río Leona Formation is here assigned to the early Late Oligocene based on the presence of key species of the M–M palynological zone (Margocolporites tenuireticulatus Barreda, Diporites aspis Pocknall and Mildenhall, Granodiporites nebulosus Partridge, Mutisiapollis spp.) and the virtual absence of warmth-adapted taxa (abundant from the latest Late Oligocene to Middle Miocene in Patagonia). A temporal gap between the Río Leona Formation and the overlying Centinela Formation (Early Miocene) – exposed in the studied region – is suggested here based on the differences observed in their palynological assemblages. The Río Leona Formation was deposited in a continental environment, with local peat swamps and coastal plain environments. The presence of Antarctic lineages in the lower and middle sections of the Río Leona Formation is consistent with the cooling trend globally recognized during the Late Eocene and Early Oligocene times. The appearance of some Neotropical families in the upper section might indicate the beginning of the Late Oligocene warming event. Records of Asteraceae (Mutisiapollis telleriae Barreda and Palazzesi sp. nov.), Menyanthaceae (Striasyncolpites laxus Mildenhall and Pocknall), and Rosaceae (Psilatricolporites quenua Barreda and Palazzesi sp. nov., Psilatricolporites sp.) are the oldest reports in Patagonia to date, and provide significant information on the early divergence and radiation times of these major angiosperm families. Fil: Barreda, Viviana Dora. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; Argentina. Consejo Nacional de Investigaciones ...
format Article in Journal/Newspaper
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
geographic Antarctic
Patagonia
Argentino
Argentina
geographic_facet Antarctic
Patagonia
Argentino
Argentina
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op_doi https://doi.org/10.1016/j.revpalbo.2008.11.005
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info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0034666708001759
http://hdl.handle.net/11336/102731
Barreda, Viviana Dora; Palazzesi, Luis; Marenssi, Sergio Alfredo; Palynological record of the Paleogene Río Leona Formation (southernmost South America): Stratigraphical and paleoenvironmental implications; Elsevier Science; Review of Palaeobotany and Palynology; 154; 1-4; 4-2009; 22-33
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/102731 2025-01-16T19:38:47+00:00 Palynological record of the Paleogene Río Leona Formation (southernmost South America): Stratigraphical and paleoenvironmental implications Barreda, Viviana Dora Palazzesi, Luis Marenssi, Sergio Alfredo application/pdf http://hdl.handle.net/11336/102731 eng eng Elsevier Science info:eu-repo/semantics/altIdentifier/doi/10.1016/j.revpalbo.2008.11.005 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0034666708001759 http://hdl.handle.net/11336/102731 Barreda, Viviana Dora; Palazzesi, Luis; Marenssi, Sergio Alfredo; Palynological record of the Paleogene Río Leona Formation (southernmost South America): Stratigraphical and paleoenvironmental implications; Elsevier Science; Review of Palaeobotany and Palynology; 154; 1-4; 4-2009; 22-33 0034-6667 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ PALINOLOGY OLIGOCENE PATAGONIA https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1016/j.revpalbo.2008.11.005 2023-09-24T19:11:14Z Terrestrial palynomorph assemblages have been recovered from the Río Leona Formation, southwestern Santa Cruz Province, southern South America. Organic debris (spores, pollen grains, fresh water algae, plant tissues and fungi) are preserved in shales associated with other plant fossil remains (leaves and wood). The Río Leona Formation is here assigned to the early Late Oligocene based on the presence of key species of the M–M palynological zone (Margocolporites tenuireticulatus Barreda, Diporites aspis Pocknall and Mildenhall, Granodiporites nebulosus Partridge, Mutisiapollis spp.) and the virtual absence of warmth-adapted taxa (abundant from the latest Late Oligocene to Middle Miocene in Patagonia). A temporal gap between the Río Leona Formation and the overlying Centinela Formation (Early Miocene) – exposed in the studied region – is suggested here based on the differences observed in their palynological assemblages. The Río Leona Formation was deposited in a continental environment, with local peat swamps and coastal plain environments. The presence of Antarctic lineages in the lower and middle sections of the Río Leona Formation is consistent with the cooling trend globally recognized during the Late Eocene and Early Oligocene times. The appearance of some Neotropical families in the upper section might indicate the beginning of the Late Oligocene warming event. Records of Asteraceae (Mutisiapollis telleriae Barreda and Palazzesi sp. nov.), Menyanthaceae (Striasyncolpites laxus Mildenhall and Pocknall), and Rosaceae (Psilatricolporites quenua Barreda and Palazzesi sp. nov., Psilatricolporites sp.) are the oldest reports in Patagonia to date, and provide significant information on the early divergence and radiation times of these major angiosperm families. Fil: Barreda, Viviana Dora. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; Argentina. Consejo Nacional de Investigaciones ... Article in Journal/Newspaper Antarc* Antarctic CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic Patagonia Argentino Argentina Review of Palaeobotany and Palynology 154 1-4 22 33
spellingShingle PALINOLOGY
OLIGOCENE
PATAGONIA
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Barreda, Viviana Dora
Palazzesi, Luis
Marenssi, Sergio Alfredo
Palynological record of the Paleogene Río Leona Formation (southernmost South America): Stratigraphical and paleoenvironmental implications
title Palynological record of the Paleogene Río Leona Formation (southernmost South America): Stratigraphical and paleoenvironmental implications
title_full Palynological record of the Paleogene Río Leona Formation (southernmost South America): Stratigraphical and paleoenvironmental implications
title_fullStr Palynological record of the Paleogene Río Leona Formation (southernmost South America): Stratigraphical and paleoenvironmental implications
title_full_unstemmed Palynological record of the Paleogene Río Leona Formation (southernmost South America): Stratigraphical and paleoenvironmental implications
title_short Palynological record of the Paleogene Río Leona Formation (southernmost South America): Stratigraphical and paleoenvironmental implications
title_sort palynological record of the paleogene río leona formation (southernmost south america): stratigraphical and paleoenvironmental implications
topic PALINOLOGY
OLIGOCENE
PATAGONIA
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet PALINOLOGY
OLIGOCENE
PATAGONIA
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/102731