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Flowering after disaster: Early Danian buckthorn (Rhamnaceae) flowers and leaves from Patagonia

Southern-Hemisphere terrestrial communities from the early Paleocene are poorly known, but recent work on Danian plant fossils from the Salamanca Formation in Chubut Province, Argentina are providing critical data on earliest Paleocene floras. The fossils described here come from a site in the Salam...

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Autores principales: Jud, Nathan A., Gandolfo, Maria A., Iglesias, Ari, Wilf, Peter
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2017
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5425202/
https://www.ncbi.nlm.nih.gov/pubmed/28489895
http://dx.doi.org/10.1371/journal.pone.0176164
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author Jud, Nathan A.
Gandolfo, Maria A.
Iglesias, Ari
Wilf, Peter
author_facet Jud, Nathan A.
Gandolfo, Maria A.
Iglesias, Ari
Wilf, Peter
author_sort Jud, Nathan A.
collection PubMed
description Southern-Hemisphere terrestrial communities from the early Paleocene are poorly known, but recent work on Danian plant fossils from the Salamanca Formation in Chubut Province, Argentina are providing critical data on earliest Paleocene floras. The fossils described here come from a site in the Salamanca Formation dating to ca. 1 million years or less after the end-Cretaceous extinction event; they are the first fossil flowers reported from the Danian of South America, and possible the entire Southern Hemisphere. They are compressions and impressions in flat-laminated light gray shale, and they belong to the family Rhamnaceae (buckthorns). Flowers of Notiantha grandensis gen. et sp. nov. are pentamerous, with distinctly keeled calyx lobes projecting from the hypanthium, clawed and cucullate emarginate petals, antepetalous stamens, and a pentagonal floral disk that fills the hypanthium. Their phylogenetic position was evaluated using a molecular scaffold approach combined with morphological data. Results indicate that the flowers are most like those of extant ziziphoid Rhamnaceae. The associated leaves, assigned to Suessenia grandensis gen. et sp. nov. are simple and ovate, with serrate margins and three acrodromous basal veins. They conform to the distinctive leaves of some extant Rhamnaceae in the ziziphoid and ampelozizyphoid clades. These fossils provide the first unequivocal megafossil evidence of Rhamnaceae in the Southern Hemisphere, demonstrating that Rhamnaceae expanded beyond the tropics by the earliest Paleocene. Given previous reports of rhamnaceous pollen in the late Paleogene and Neogene of Antarctica and southern Australia, this new occurrence increases the possibility of high-latitude dispersal of this family between South America and Australia via Antarctica during the Cenozoic.
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spelling pubmed-54252022017-05-15 Flowering after disaster: Early Danian buckthorn (Rhamnaceae) flowers and leaves from Patagonia Jud, Nathan A. Gandolfo, Maria A. Iglesias, Ari Wilf, Peter PLoS One Research Article Southern-Hemisphere terrestrial communities from the early Paleocene are poorly known, but recent work on Danian plant fossils from the Salamanca Formation in Chubut Province, Argentina are providing critical data on earliest Paleocene floras. The fossils described here come from a site in the Salamanca Formation dating to ca. 1 million years or less after the end-Cretaceous extinction event; they are the first fossil flowers reported from the Danian of South America, and possible the entire Southern Hemisphere. They are compressions and impressions in flat-laminated light gray shale, and they belong to the family Rhamnaceae (buckthorns). Flowers of Notiantha grandensis gen. et sp. nov. are pentamerous, with distinctly keeled calyx lobes projecting from the hypanthium, clawed and cucullate emarginate petals, antepetalous stamens, and a pentagonal floral disk that fills the hypanthium. Their phylogenetic position was evaluated using a molecular scaffold approach combined with morphological data. Results indicate that the flowers are most like those of extant ziziphoid Rhamnaceae. The associated leaves, assigned to Suessenia grandensis gen. et sp. nov. are simple and ovate, with serrate margins and three acrodromous basal veins. They conform to the distinctive leaves of some extant Rhamnaceae in the ziziphoid and ampelozizyphoid clades. These fossils provide the first unequivocal megafossil evidence of Rhamnaceae in the Southern Hemisphere, demonstrating that Rhamnaceae expanded beyond the tropics by the earliest Paleocene. Given previous reports of rhamnaceous pollen in the late Paleogene and Neogene of Antarctica and southern Australia, this new occurrence increases the possibility of high-latitude dispersal of this family between South America and Australia via Antarctica during the Cenozoic. Public Library of Science 2017-05-10 /pmc/articles/PMC5425202/ /pubmed/28489895 http://dx.doi.org/10.1371/journal.pone.0176164 Text en © 2017 Jud et al http://creativecommons.org/licenses/by/4.0/ This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/) , which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
spellingShingle Research Article
Jud, Nathan A.
Gandolfo, Maria A.
Iglesias, Ari
Wilf, Peter
Flowering after disaster: Early Danian buckthorn (Rhamnaceae) flowers and leaves from Patagonia
title Flowering after disaster: Early Danian buckthorn (Rhamnaceae) flowers and leaves from Patagonia
title_full Flowering after disaster: Early Danian buckthorn (Rhamnaceae) flowers and leaves from Patagonia
title_fullStr Flowering after disaster: Early Danian buckthorn (Rhamnaceae) flowers and leaves from Patagonia
title_full_unstemmed Flowering after disaster: Early Danian buckthorn (Rhamnaceae) flowers and leaves from Patagonia
title_short Flowering after disaster: Early Danian buckthorn (Rhamnaceae) flowers and leaves from Patagonia
title_sort flowering after disaster: early danian buckthorn (rhamnaceae) flowers and leaves from patagonia
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5425202/
https://www.ncbi.nlm.nih.gov/pubmed/28489895
http://dx.doi.org/10.1371/journal.pone.0176164
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