2017
DOI: 10.1080/08912963.2017.1313840
|View full text |Cite
|
Sign up to set email alerts
|

Small Celastraceae and Polygonaceae twigs from the Upper Cenozoic (Ituzaingó Formation) of the La Plata Basin, Argentina

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
5
0
3

Year Published

2019
2019
2023
2023

Publication Types

Select...
5

Relationship

0
5

Authors

Journals

citations
Cited by 5 publications
(8 citation statements)
references
References 38 publications
0
5
0
3
Order By: Relevance
“…Other fossil taxa that have a simple perforation plate are Lophopetalumoxylon (Mehrotra et al 1983) and Maytenoxylon (Franco 2018). The first one is characterized by the presence of diffuse porosity, solitary vessels, bordered and alternate intervascular pits, thin apotracheal bands of parenchyma, uniseriate homocellular rays, non-septate thick-walled fibers, and intercellular canals.…”
Section: Resultsmentioning
confidence: 99%
See 2 more Smart Citations
“…Other fossil taxa that have a simple perforation plate are Lophopetalumoxylon (Mehrotra et al 1983) and Maytenoxylon (Franco 2018). The first one is characterized by the presence of diffuse porosity, solitary vessels, bordered and alternate intervascular pits, thin apotracheal bands of parenchyma, uniseriate homocellular rays, non-septate thick-walled fibers, and intercellular canals.…”
Section: Resultsmentioning
confidence: 99%
“…On the other hand, Maytenoxylon is a wood with diffuse porosity, mainly solitary vessels, intervascular pits that vary from alternate to opposite, bands of fiber resembling parenchyma that alternate with ordinary fibers, both non-septate and septate ones, diffuse and scanty parenchyma, homocellular rays with some perforated cells (Franco 2018). The identification of Maytenoxylon is supported by the presence of perforated ray cells, which are restricted to Maytenus (Joffily et al 2007).…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…A partir de ellos, se elaboró una base de datos integrada por 438 especies fósiles del Mioceno-Pleistoceno provenientes de las formaciones Paraná, Ituzaingó, Anta, San José, Chiquimil, Palo Pintado, Andalhuala, del Buey, Pozo YPF.SE.x-2 Los Horcones y de la Aloformación Playa del Zorro. Ante las reiteradas mencio-nes en , Brea et al (2013); Franco y Brea (2008, 2009; Franco (2009Franco ( , 2017; y Franco et al (2013) de taxones del Mioceno-Pleistoceno del noreste argentino como posibles integrantes de los actuales Bosques Secos Estacionales Neotropicales (BSEN), y considerando la paleoflora censada por las autoras (Anzótegui, Garralla y Mautino) para el norte de Argentina, en el presente trabajo se encara la revisión de la paleoflora arbórea y arbustiva con el fin de hallar los posibles integrantes de este tipo de asociación vegetal. Por otra parte, Prado corroboró y señaló otros taxones que podrían haber formado parte de asociaciones vegetales semejantes a las actuales del Chaco (Prado, 1993a,b;Mogni et al, 2015y DRYFLOR, 2017) y Cerrado (Ratter et al, 1997(Ratter et al, , 2003, estrechamente relacionadas a los BSEN.…”
Section: Issn 2469-0228unclassified
“…(Anzótegui y Lutz, 1988), Maytenus sp. (Franco, 2017), Sebastiania sp. (Anzótegui y Lutz, 1988) y Sorocea sp.…”
Section: Materiales Y Métodosunclassified