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Is Santaniella a ranunculid? Reassessment of this enigmatic fossil angiosperm from the Lower Cretaceous (Aptian, Crato Konservat-Lagerstätte, Brazil) provides a new interpretation

dc.contributor.authorPessoa, Edlley M.
dc.contributor.authorRibeiro, Alexandre C.
dc.contributor.authorChristenhusz, Maarten J. M.
dc.contributor.authorCoan, Alessandra Ike [UNESP]
dc.contributor.authorJud, Nathan A.
dc.contributor.institutionUniversidade Federal de Mato Grosso
dc.contributor.institutionCurtin University
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)
dc.contributor.institutionWilliam Jewell College
dc.date.accessioned2023-07-29T13:12:38Z
dc.date.available2023-07-29T13:12:38Z
dc.date.issued2023-05-01
dc.description.abstractPremise: The Lower Cretaceous Crato Konservat-Lagerstätte (CKL) preserves a rich flora that includes early angiosperms from northern Gondwana. From this area, the recently described fossil genus Santaniella was interpreted as a ranunculid (presumably Ranunculaceae). However, based on our examination of an additional specimen and a new phylogenetic analysis, we offer an alternative interpretation. Methods: The new fossil was collected from an active quarry for paving stones in the state of Ceará, northeastern Brazil. We assessed support for alternative phylogenetic hypotheses using a combined analysis of morphological data and DNA sequence data using Bayesian inference. We used a consensus network to visualize the posterior distribution of trees, and we used RoguePlot to illustrate the support for alternative positions on a scaffold tree. Results: The new material includes a flower-like structure not present in the original material and also includes follicles preserved at early stages of development. The flower-like structure is a compact terminal cluster of elliptical sterile laminar organs surrounding internal filamentous structures that occur on flexuous axes. Phylogenetic analyses did not support the fossil placement among eudicots. Instead, Santaniella appears to belong in the magnoliid clade. Conclusions: The presence of seeds in a marginal-linear placentation and enclosed in a follicle supports the fossil as an angiosperm. However, even though most characters are clearly recognizable, its combination of characters does not provide strong support for a close relationship to any extant order of flowering plants. Its position in the magnoliid clade is intriguing and, based on plicate carpels, it is definitely a mesangiosperm.en
dc.description.affiliationLaboratório de Estudos Integrados de Plantas Departamento de Botânica e Ecologia Universidade Federal de Mato Grosso, Mato Grosso
dc.description.affiliationDepartamento de Biologia e Zoologia Universidade Federal de Mato Grosso, Mato Grosso
dc.description.affiliationDepartment of Environment and Agriculture Curtin University, Perth, Western Australia, Australia; Royal Botanic Gardens, Kew, Richmond
dc.description.affiliationDepartamento de Biodiversidade Universidade Estadual Paulista “Júlio de Mesquita Filho,” Instituto de Biociências, São Paulo
dc.description.affiliationDepartment of Biology William Jewell College
dc.description.affiliationUnespDepartamento de Biodiversidade Universidade Estadual Paulista “Júlio de Mesquita Filho,” Instituto de Biociências, São Paulo
dc.identifierhttp://dx.doi.org/10.1002/ajb2.16163
dc.identifier.citationAmerican Journal of Botany, v. 110, n. 5, 2023.
dc.identifier.doi10.1002/ajb2.16163
dc.identifier.issn1537-2197
dc.identifier.issn0002-9122
dc.identifier.scopus2-s2.0-85158086141
dc.identifier.urihttp://hdl.handle.net/11449/247313
dc.language.isoeng
dc.relation.ispartofAmerican Journal of Botany
dc.sourceScopus
dc.subjectangiosperm
dc.subjectCretaceous
dc.subjectGondwana
dc.subjectmacrofossil
dc.subjectpaleobotany
dc.subjectSouth America
dc.titleIs Santaniella a ranunculid? Reassessment of this enigmatic fossil angiosperm from the Lower Cretaceous (Aptian, Crato Konservat-Lagerstätte, Brazil) provides a new interpretationen
dc.typeArtigo
dspace.entity.typePublication
unesp.author.orcid0000-0003-3800-8684[1]
unesp.author.orcid0000-0001-7313-9562[2]
unesp.author.orcid0000-0003-1398-8743[3]
unesp.author.orcid0000-0002-8584-1700[4]
unesp.author.orcid0000-0001-6100-9779[5]

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