dc.creatorLafuente Diaz, Maiten Amalia
dc.creatordel Fueyo, Georgina Marisa
dc.creatorD`angelo, José Alejandro
dc.creatorCarrizo, Martin Alejandro
dc.date.accessioned2022-03-18T11:06:40Z
dc.date.accessioned2022-10-15T11:27:54Z
dc.date.available2022-03-18T11:06:40Z
dc.date.available2022-10-15T11:27:54Z
dc.date.created2022-03-18T11:06:40Z
dc.date.issued2021-07
dc.identifierLafuente Diaz, Maiten Amalia; del Fueyo, Georgina Marisa; D`angelo, José Alejandro; Carrizo, Martin Alejandro; Fourier transform infrared spectroscopy studies of cretaceous gymnosperms from the santa cruz province, patagonia, argentina; University of Chicago Press; International Journal of Plant Sciences; 182; 6; 7-2021; 508-522
dc.identifier1058-5893
dc.identifierhttp://hdl.handle.net/11336/153578
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4380837
dc.description.abstractPremise of research. In this contribution, the spectroscopic characterization of gymnosperm fossil remains belonging to Pteridospermophyta, Cycadophyta, Ginkgophyta, and Coniferophyta collected from the Anfiteatro de Ticó and Punta del Barco Formations (Baqueró Group; Aptian) and Springhill (Hauterivian-Barremian) and Piedra Clavada/Kachaike (Albian) Formations, outcropping in the Santa Cruz Province, Argentina, is presented. From these lithostratigraphic units, specimens of several fossil taxa showing the existence of a diverse plant assemblage during the Lower Cretaceous in Patagonia were selected. Methodology. The fossils consist of foliar compressions with very well-preserved cuticles, which are chemically characterized by Fourier transform infrared spectroscopy. Foliar remains are analyzed in two sample forms: (1) compressions (Cps; including coalified mesophyll and cuticles) and (2) cuticles (Cts). Additionally, semiquantitative data are evaluated through principal component analysis, revealing the functional groups preserved at the mesophyll and cuticle levels for all analyzed fossil taxa. Pivotal results. In general, the species fromthe Baqueró Group show similar chemical compositions between the Cp and Ct sample forms, whereas the chemistry of the foliar compressions from the Springhill and Piedra Clavada/ Kachaike Formations reveals the presence of a high contribution of aromatic structures making up the cuticles. Conclusions. The compressions of Pseudoctenis ornata, Ginkgoites tigrensis, and Squamastrobus tigrensis probably underwent, during and after diagenesis, a natural oxidation process most likely caused by the recurrent volcanic activity that occurred during the Aptian sedimentation of the Baqueró Group. In contrast, Ruflorinia orlandoi, Ptilophyllum micropapillosum, and Ginkgoites skottsbergii have cuticles presumably composed of highly aromatic structures (such as phenylpropanoids and aromatic domains) in cutins and cutans as well due to the presence of other phenolic compounds. Anew term, vitrinitic compression, is proposed here for G. skottsbergii, while P. ornata, G. tigrensis, S. tigrensis, P. micropapillosum, and R. orlandoi are called liptinitic compressions.
dc.languageeng
dc.publisherUniversity of Chicago Press
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1086/714283
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://www.journals.uchicago.edu/doi/10.1086/714283
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.rightsAtribución-NoComercial-CompartirIgual 2.5 Argentina (CC BY-NC-SA 2.5 AR)
dc.subjectCOMPRESSION
dc.subjectCUTICLE
dc.subjectFOURIER TRANSFORM INFRARED (FTIR) SPECTROSCOPY
dc.subjectGYMNOSPERMS
dc.subjectLOWER CRETACEOUS
dc.subjectPATAGONIA
dc.titleFourier transform infrared spectroscopy studies of cretaceous gymnosperms from the santa cruz province, patagonia, argentina
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:ar-repo/semantics/artículo
dc.typeinfo:eu-repo/semantics/publishedVersion


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