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Piptadenioxylon paraexcelsa
Taxonomy
Piptadenioxylon paraexcelsa was named by Franco and Brea (2008). It is considered to be a form taxon. Its type specimen is PALBO 23. PALBOmic 523, a plant debris (log), and it is a 3D fossil preserving soft parts. Its type locality is Nivel Fosilifero 1, Toma Vieja, Paraná, which is in a Miocene terrestrial siltstone in the Paraná Formation of Argentina. It is the type species of Piptadenioxylon.
Synonymy list
Year | Name and author |
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2008 | Piptadenioxylon paraexcelsa Franco and Brea |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Piptadenioxylon paraexcelsa Franco and Brea 2008
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Diagnosis
Reference | Diagnosis | |
---|---|---|
M. J. Franco and M. Brea 2008 | Dicotyledonous fossil wood. Growth rings indistinct or subtle. Diffuse porosity or semi-ring-porous. Vessels solitary, some in radial multiple series of 2-3 or in clusters. Small and numerosous. Vessel elements very short. Simple perforation plates. Intervessel pits bordered and alternate. Rays homocellular, numerosous, low, biseriate and uniseriate. Fibers quadrangular in section, with an irregular arrengement are abundant. Fibers not septate. Axial parenchyma apotracheal and paratracheal; paratracheal vasicentric incomplete in wide bands and apotracheal diffuse-in-aggregates. |
Measurements
No measurements are available
No ecological data are available
Age range: Middle Miocene or 15.98000 to 11.63000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
---|---|---|---|
Middle Miocene | Argentina (Entre Ríos) | Piptadenioxylon paraexcelsa (type locality: 136133) |