Pluricarpellatia Temporal range: Cretaceous [1] Early | |
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Scientific classification | |
Kingdom: | Plantae |
Clade: | Tracheophytes |
Clade: | Angiosperms |
Order: | Nymphaeales |
Family: | Cabombaceae |
Genus: | † Pluricarpellatia B. Mohr, Bernardes-de-Oliveira & David W. Taylor [1] |
Species: | †P. peltata |
Binomial name | |
†Pluricarpellatia peltata B. Mohr, Bernardes-de-Oliveira & David W. Taylor [1] | |
Pluricarpellatia peltata was a species of herbaceous aquatic plant, which occurred in the early Cretaceous period of Brazil. [1]
Pluricarpellatia peltata was an aquatic, rhizomatous, herbaceous plant with 5 mm wide rhizomes and 0.3-1.3 mm wide roots. The plant could exceed 25 cm in length. The thin, petiolate leaves have a smooth margin. The petioles were 5 cm long, and 3 mm wide. [1]
The pedunculate, 2 cm wide flowers had up to 17 cm long peduncles. The gynoecium consists of 6-12 carpels. [1]
It was published by Barbara Adelheid Rosina Mohr, Mary Elizabeth Bernardes de Oliveira and David Winship Taylor in 2008. [1]
The type specimen was collected by Barbara Adelheid Rosina Mohr, Mary Elizabeth Bernardes de Oliveira and David Winship Taylor South of Nova Olinda, Brazil in the Crato Formation of the Araripe Basin. It is stored in the Natural History Museum, Berlin, Germany. [1]
It was likely a basal member of the family Cabombaceae. [1] [2]
The generic name Pluricarpellatia references the many carpels present in the flowers. The specific epithet peltata refers to the peltate leaves. [1]
The Nymphaeales are an order of flowering plants, consisting of three families of aquatic plants, the Hydatellaceae, the Cabombaceae, and the Nymphaeaceae. It is one of the three orders of basal angiosperms, an early-diverging grade of flowering plants. At least 10 morphological characters unite the Nymphaeales. One of the traits is the absence of a vascular cambium, which is required to produce both xylem (wood) and phloem, which therefore are missing. Molecular synapomorphies are also known.
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The Santana Group is a geologic group, formerly included as the middle part of the Araripe Group, in the Araripe Basin of northeastern Brazil. The group comprises the Crato, Ipubi and Romualdo Formations and is dated to the Aptian to Albian stages of the Early Cretaceous. The formations of the group were deposited in a lacustrine to subtidal shallow marine environment in the Araripe rift basin.
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