Artigo Acesso aberto Revisado por pares

Paleogene dinoflagellate cysts from Punta Prat, southern Chile

2009; Taylor & Francis; Volume: 33; Issue: 1 Linguagem: Inglês

10.1080/01916122.2009.9989670

ISSN

1558-9188

Autores

Mirta E. Quattrocchio,

Tópico(s)

Marine and coastal ecosystems

Resumo

Research Article| January 01, 2009 PALEOGENE DINOFLAGELLATE CYSTS FROM PUNTA PRAT, SOUTHERN CHILE MIRTA E. QUATTROCCHIO MIRTA E. QUATTROCCHIO Departamento de Geología, Universidad Nacional del Sur, San Juan 670, 8000 Bahía Blanca, Argentina, e-mail: mquattro@criba.edu.ar Search for other works by this author on: GSW Google Scholar Palynology (2009) 33 (1): 141–156. https://doi.org/10.2113/gspalynol.33.1.141 Article history first online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation MIRTA E. QUATTROCCHIO; PALEOGENE DINOFLAGELLATE CYSTS FROM PUNTA PRAT, SOUTHERN CHILE. Palynology 2009;; 33 (1): 141–156. doi: https://doi.org/10.2113/gspalynol.33.1.141 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyPalynology Search Advanced Search Abstract Paleogene dinoflagellate cysts were recorded from the Chorrillo Chico and Agua Fresca formations at Punta Prat, southern Chile. Due to the presence of Palaeoperidinium pyrophorum, the Chorrillo Chico Formation is no younger than Late Selandian. By comparison with other basins, a Late Danian to Late Selandian age is proposed for the Chorrillo Chico Formation at Punta Prat. The Paleocene–Eocene boundary is characterized by Apectodinium-dominated assemblages in the mid and high latitudes, the Atlantic coast of Isla Grande de Tierra del Fuego in Argentina, and Chile. The absence of this event at Punta Prat suggests a regional hiatus across the Paleocene–Eocene boundary. An Early to Middle Eocene age is assigned to the lower part of the Agua Fresca Formation by comparison with dinoflagellate cyst assemblages from elsewhere in the Southern Hemisphere. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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