Integrated biostratigraphical study of La Horqueta section (Aptian-Albian boundary), Cardiel lake, Patagonia, Argentina
La Horqueta at Cardiel lake is a classical section in Santa Cruz province where marine invertebrates include ammonites of the Aptian-Albian transition. New collections at this site yielded palynological remains from several horizons in both Río Mayer Formation (latest Aptian) and Piedra Clavada Form...
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todo:paper_15145158_v10_n2_p273_Medina2023-10-03T16:19:33Z Integrated biostratigraphical study of La Horqueta section (Aptian-Albian boundary), Cardiel lake, Patagonia, Argentina Medina, F. Archangelsky, S. Guler, V. Archangelsky, A. Cárdenas, O. Aptian-Albian boundary Argentina Biostratigraphy Palynology Patagonia Bacteria (microorganisms) Cheirolepidiaceae Coniferophyta Dinophyceae Invertebrata Magnoliophyta Podocarpaceae La Horqueta at Cardiel lake is a classical section in Santa Cruz province where marine invertebrates include ammonites of the Aptian-Albian transition. New collections at this site yielded palynological remains from several horizons in both Río Mayer Formation (latest Aptian) and Piedra Clavada Formation (earliest Albian). Marine dinoflagellate cysts are found in the lower part of the section; they agree with an Aptian to earliest Albian age suggested by ammonites. Statistical counts of six palynological groups show the dominance of the conifer family Cheirolepidiaceae in the Río Mayer Formation coinciding with the presence of dinoflagellate cysts and the gradual increase of pteridophitic spores and saccate pollen, mainly of the family Podocarpaceae in the upper Piedra Clavada Formation. Angiosperm pollen is present throughout the section although it is more significant in the upper Piedra Clavada Formation where several new types have their first appearance (tricolpate, tricolporoidate and other types). Most palynological taxa are found across the whole section and many are known to occur in other units cropping out in this area, as the Baqueró Group (Early Aptian) or Kachaike Formation (Mid-Late Albian). Only few selected and probably significant species have been found to be of a possible biostratigraphic value and their distribution along the section is shown in a chart. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_15145158_v10_n2_p273_Medina |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Aptian-Albian boundary Argentina Biostratigraphy Palynology Patagonia Bacteria (microorganisms) Cheirolepidiaceae Coniferophyta Dinophyceae Invertebrata Magnoliophyta Podocarpaceae |
spellingShingle |
Aptian-Albian boundary Argentina Biostratigraphy Palynology Patagonia Bacteria (microorganisms) Cheirolepidiaceae Coniferophyta Dinophyceae Invertebrata Magnoliophyta Podocarpaceae Medina, F. Archangelsky, S. Guler, V. Archangelsky, A. Cárdenas, O. Integrated biostratigraphical study of La Horqueta section (Aptian-Albian boundary), Cardiel lake, Patagonia, Argentina |
topic_facet |
Aptian-Albian boundary Argentina Biostratigraphy Palynology Patagonia Bacteria (microorganisms) Cheirolepidiaceae Coniferophyta Dinophyceae Invertebrata Magnoliophyta Podocarpaceae |
description |
La Horqueta at Cardiel lake is a classical section in Santa Cruz province where marine invertebrates include ammonites of the Aptian-Albian transition. New collections at this site yielded palynological remains from several horizons in both Río Mayer Formation (latest Aptian) and Piedra Clavada Formation (earliest Albian). Marine dinoflagellate cysts are found in the lower part of the section; they agree with an Aptian to earliest Albian age suggested by ammonites. Statistical counts of six palynological groups show the dominance of the conifer family Cheirolepidiaceae in the Río Mayer Formation coinciding with the presence of dinoflagellate cysts and the gradual increase of pteridophitic spores and saccate pollen, mainly of the family Podocarpaceae in the upper Piedra Clavada Formation. Angiosperm pollen is present throughout the section although it is more significant in the upper Piedra Clavada Formation where several new types have their first appearance (tricolpate, tricolporoidate and other types). Most palynological taxa are found across the whole section and many are known to occur in other units cropping out in this area, as the Baqueró Group (Early Aptian) or Kachaike Formation (Mid-Late Albian). Only few selected and probably significant species have been found to be of a possible biostratigraphic value and their distribution along the section is shown in a chart. |
format |
JOUR |
author |
Medina, F. Archangelsky, S. Guler, V. Archangelsky, A. Cárdenas, O. |
author_facet |
Medina, F. Archangelsky, S. Guler, V. Archangelsky, A. Cárdenas, O. |
author_sort |
Medina, F. |
title |
Integrated biostratigraphical study of La Horqueta section (Aptian-Albian boundary), Cardiel lake, Patagonia, Argentina |
title_short |
Integrated biostratigraphical study of La Horqueta section (Aptian-Albian boundary), Cardiel lake, Patagonia, Argentina |
title_full |
Integrated biostratigraphical study of La Horqueta section (Aptian-Albian boundary), Cardiel lake, Patagonia, Argentina |
title_fullStr |
Integrated biostratigraphical study of La Horqueta section (Aptian-Albian boundary), Cardiel lake, Patagonia, Argentina |
title_full_unstemmed |
Integrated biostratigraphical study of La Horqueta section (Aptian-Albian boundary), Cardiel lake, Patagonia, Argentina |
title_sort |
integrated biostratigraphical study of la horqueta section (aptian-albian boundary), cardiel lake, patagonia, argentina |
url |
http://hdl.handle.net/20.500.12110/paper_15145158_v10_n2_p273_Medina |
work_keys_str_mv |
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1807323253619818496 |