Climate, dust, and fire across the Eocene-Oligocene transition, Patagonia

The Eocene-Oligocene transition (EOT) is typically interpreted as a time of drastic global cooling and drying associated with massive growth of a glacial icecap in Antarctica and the shift to an "icehouse" climate. The effects of this transition on the terrestrial environments, floras, and...

Full description

Bibliographic Details
Published in:Geology
Main Authors: Selking, Peter A., Stromberg, Caroline, Dunn, Regan, Khon, Matthew J., Carlini, Alfredo Armando, Davies-Vollum, K. Siân, Madden, Richard H.
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of America
Subjects:
Online Access:http://hdl.handle.net/11336/78364
_version_ 1821776933880332288
author Selking, Peter A.
Stromberg, Caroline
Dunn, Regan
Khon, Matthew J.
Carlini, Alfredo Armando
Davies-Vollum, K. Siân
Madden, Richard H.
author_facet Selking, Peter A.
Stromberg, Caroline
Dunn, Regan
Khon, Matthew J.
Carlini, Alfredo Armando
Davies-Vollum, K. Siân
Madden, Richard H.
author_sort Selking, Peter A.
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 7
container_start_page 567
container_title Geology
container_volume 43
description The Eocene-Oligocene transition (EOT) is typically interpreted as a time of drastic global cooling and drying associated with massive growth of a glacial icecap in Antarctica and the shift to an "icehouse" climate. The effects of this transition on the terrestrial environments, floras, and faunas of the Southern Hemisphere, however, have been unclear. Here we document simultaneous changes in fire regime and plant community in Patagonia, Argentina. Decreases in the concentration of magnetite in loessites from the Eocene-Oligocene Vera Member of the Sarmiento Formation correlate with decreases in the fraction of burnt palm phytoliths as well as more consistently palm-dominated phytolith assemblages. Association of magnetite and burnt palm phytoliths suggests intense wildfires, which appear to have been suppressed for ~200 k.y. shortly after the EOT. The disappearance of fire-related characteristics near the EOT is possible if changes in regional wind patterns-consistent with observed changes in sediment particle sizes-caused changes in seasonal precipitation. These results imply a more important role for fire in structuring Eocene-Oligocene landscapes than previously thought. Fil: Selking, Peter A. University of Washington; Estados Unidos Fil: Stromberg, Caroline. University of Washington; Estados Unidos. Burke Museum of Natural History and Culture; Estados Unidos Fil: Dunn, Regan. University of Washington; Estados Unidos. Burke Museum of Natural History and Culture; Estados Unidos Fil: Khon, Matthew J. Boise State University; Estados Unidos Fil: Carlini, Alfredo Armando. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleontología Vertebrados; Argentina Fil: Davies-Vollum, K. Siân. Sheffield Hallam University; Estados Unidos Fil: Madden, Richard H. University of Chicago; Estados Unidos
format Article in Journal/Newspaper
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
geographic Patagonia
Argentina
Sheffield
Sarmiento
Vollum
geographic_facet Patagonia
Argentina
Sheffield
Sarmiento
Vollum
id ftconicet:oai:ri.conicet.gov.ar:11336/78364
institution Open Polar
language English
long_lat ENVELOPE(-68.000,-68.000,-72.000,-72.000)
ENVELOPE(8.530,8.530,62.771,62.771)
op_collection_id ftconicet
op_container_end_page 570
op_doi https://doi.org/10.1130/G36664.1
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1130/G36664.1
info:eu-repo/semantics/altIdentifier/url/https://pubs.geoscienceworld.org/gsa/geology/article/43/7/567/131882/Climate-dust-and-fire-across-the-EoceneOligocene
http://hdl.handle.net/11336/78364
CONICET Digital
CONICET
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
publisher Geological Society of America
record_format openpolar
spelling ftconicet:oai:ri.conicet.gov.ar:11336/78364 2025-01-16T19:42:20+00:00 Climate, dust, and fire across the Eocene-Oligocene transition, Patagonia Selking, Peter A. Stromberg, Caroline Dunn, Regan Khon, Matthew J. Carlini, Alfredo Armando Davies-Vollum, K. Siân Madden, Richard H. application/pdf http://hdl.handle.net/11336/78364 eng eng Geological Society of America info:eu-repo/semantics/altIdentifier/doi/10.1130/G36664.1 info:eu-repo/semantics/altIdentifier/url/https://pubs.geoscienceworld.org/gsa/geology/article/43/7/567/131882/Climate-dust-and-fire-across-the-EoceneOligocene http://hdl.handle.net/11336/78364 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Paleo Climate Dust Eot 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/10.1130/G36664.1 2024-10-04T09:34:03Z The Eocene-Oligocene transition (EOT) is typically interpreted as a time of drastic global cooling and drying associated with massive growth of a glacial icecap in Antarctica and the shift to an "icehouse" climate. The effects of this transition on the terrestrial environments, floras, and faunas of the Southern Hemisphere, however, have been unclear. Here we document simultaneous changes in fire regime and plant community in Patagonia, Argentina. Decreases in the concentration of magnetite in loessites from the Eocene-Oligocene Vera Member of the Sarmiento Formation correlate with decreases in the fraction of burnt palm phytoliths as well as more consistently palm-dominated phytolith assemblages. Association of magnetite and burnt palm phytoliths suggests intense wildfires, which appear to have been suppressed for ~200 k.y. shortly after the EOT. The disappearance of fire-related characteristics near the EOT is possible if changes in regional wind patterns-consistent with observed changes in sediment particle sizes-caused changes in seasonal precipitation. These results imply a more important role for fire in structuring Eocene-Oligocene landscapes than previously thought. Fil: Selking, Peter A. University of Washington; Estados Unidos Fil: Stromberg, Caroline. University of Washington; Estados Unidos. Burke Museum of Natural History and Culture; Estados Unidos Fil: Dunn, Regan. University of Washington; Estados Unidos. Burke Museum of Natural History and Culture; Estados Unidos Fil: Khon, Matthew J. Boise State University; Estados Unidos Fil: Carlini, Alfredo Armando. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleontología Vertebrados; Argentina Fil: Davies-Vollum, K. Siân. Sheffield Hallam University; Estados Unidos Fil: Madden, Richard H. University of Chicago; Estados Unidos Article in Journal/Newspaper Antarc* Antarctica CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Patagonia Argentina Sheffield Sarmiento ENVELOPE(-68.000,-68.000,-72.000,-72.000) Vollum ENVELOPE(8.530,8.530,62.771,62.771) Geology 43 7 567 570
spellingShingle Paleo Climate
Dust
Eot
Patagonia
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Selking, Peter A.
Stromberg, Caroline
Dunn, Regan
Khon, Matthew J.
Carlini, Alfredo Armando
Davies-Vollum, K. Siân
Madden, Richard H.
Climate, dust, and fire across the Eocene-Oligocene transition, Patagonia
title Climate, dust, and fire across the Eocene-Oligocene transition, Patagonia
title_full Climate, dust, and fire across the Eocene-Oligocene transition, Patagonia
title_fullStr Climate, dust, and fire across the Eocene-Oligocene transition, Patagonia
title_full_unstemmed Climate, dust, and fire across the Eocene-Oligocene transition, Patagonia
title_short Climate, dust, and fire across the Eocene-Oligocene transition, Patagonia
title_sort climate, dust, and fire across the eocene-oligocene transition, patagonia
topic Paleo Climate
Dust
Eot
Patagonia
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Paleo Climate
Dust
Eot
Patagonia
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/78364