2019
DOI: 10.1163/22941932-40190238
|View full text |Cite
|
Sign up to set email alerts
|

An early record of a vesselless angiosperm from the middle Cenomanian of the Envigne valley (Vienne, Western France)

Abstract: Thousands of silicified wood fragments were recently collected from the middle Cenomanian of Vienne in western France at less than 10 km away from a historical locality where in 1870 the French geologist Alphonse Le Touzé de Longuemar reported silicified wood. The plant assemblage is very diverse, and includes several species of ferns, conifers, and angiosperms. We describe and discuss the systematic affinities of a new vesselless angiosperm. Many of its characters are shared by extant and fossil Winteraceae. … Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

1
1
0

Year Published

2019
2019
2021
2021

Publication Types

Select...
3

Relationship

0
3

Authors

Journals

citations
Cited by 3 publications
(2 citation statements)
references
References 71 publications
1
1
0
Order By: Relevance
“…The beds mainly consist of fine, green quartz sands, sometimes brown to yellow, glauconitic with consolidated calcareous sandstones, locally called "Grison". This facies is comparable to the "sands of Vierzon" of Alcaydé et al (1976), which correspond to the base of the Cenomanian and well exposed from Marigny Brizay to Châtellerault Boura et al (2019). The amber grains were collected from a lenticular, dark, clayey bed at the base of the section (Fig.…”
Section: Scorbé-clairvaux-la Bergeonneau (Scb)supporting
confidence: 58%
See 1 more Smart Citation
“…The beds mainly consist of fine, green quartz sands, sometimes brown to yellow, glauconitic with consolidated calcareous sandstones, locally called "Grison". This facies is comparable to the "sands of Vierzon" of Alcaydé et al (1976), which correspond to the base of the Cenomanian and well exposed from Marigny Brizay to Châtellerault Boura et al (2019). The amber grains were collected from a lenticular, dark, clayey bed at the base of the section (Fig.…”
Section: Scorbé-clairvaux-la Bergeonneau (Scb)supporting
confidence: 58%
“…1). The series continues up into green sandstones, already described by Mathieu (1960Mathieu ( , 1968, and progressively reaches up into 30 m in thickness in Colombiers; they contain rich fossil wood and oyster shells (Exogyra colomba Lamarck, 1819), which are dated as middle Cenomanian in age (Robin et al, 2018;Boura et al, 2019). They are overlaid by upper Cenomanian marlstones, locally called "Chalk tufa", which bear Calycoceras Hyatt, 1900, by lower Turonian beds with Mammites nodosoides Schlüter, 1871 and Lewesiceras peramplum Mantell 1822, and by flint breccia deposits containing a few plant megafossil inclusions (Gomez et al, 2018).…”
Section: General Overviewmentioning
confidence: 82%