Wattieza: Difference between revisions
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Belgian paleobotanist [[François Stockmans]] described ''Wattieza givetiana'' in 1968 from fossil fronds collected from Middle Devonian strata in the [[London-Brabant Massif]] in Belgium.<ref>{{cite journal |last1=Berry |first1=Chris |title=The Middle Devonian plant collections of Francois Stockmans reconsidered. |journal=Geologica Belgica |date=2009 |volume=12 |issue=1–2 |pages=25–30 |url=https://popups.uliege.be/1374-8505/index.php?id=2633&file=1}}</ref> |
Belgian paleobotanist [[François Stockmans]] described ''Wattieza givetiana'' in 1968 from fossil fronds collected from Middle Devonian strata in the [[London-Brabant Massif]] in Belgium.<ref>{{cite journal |last1=Berry |first1=Chris |title=The Middle Devonian plant collections of Francois Stockmans reconsidered. |journal=Geologica Belgica |date=2009 |volume=12 |issue=1–2 |pages=25–30 |url=https://popups.uliege.be/1374-8505/index.php?id=2633&file=1}}</ref> |
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English geologist and palaeobotanist Chris Berry described ''Wattieza casasii'' in Review of Paleobotany and Palynology (112) in 2000, based on fossil branches (13 slabs) and numerous other fragments (Berry, 2000) collected from middle Givetian-strata from the lower member of Campo Chico Formation (Casas et al, 2022). The lithology of the lower member consists in dark grey to green mudstones and shales, interbedded with medium-coarse grained sandstones close to the base of the Campo Chico Formation, in outcrops of the road to the Rio Socuy (Casas et al, 2022; pag 24), close to Cano Colorado river, Perija Range, Zulia state Venezuela (Casas et al, 2022). The fossil material of Wattieza casasii is currently in the National Museum and Gallery, Cardiff, Wales and the Palaeontological section, Museo de Biologia, Universidad del Zulia, Maracaibo, Venezuela (Berry, 2000; pag. 127). The etymology of the |
English geologist and palaeobotanist Chris Berry described ''Wattieza casasii'' in Review of Paleobotany and Palynology (112) in 2000, based on fossil branches (13 slabs) and numerous other fragments (Berry, 2000) collected from middle Givetian-strata from the lower member of Campo Chico Formation (Casas et al, 2022). The lithology of the lower member consists in dark grey to green mudstones and shales, interbedded with medium-coarse grained sandstones close to the base of the Campo Chico Formation, in outcrops of the road to the Rio Socuy (Casas et al, 2022; pag 24), close to Cano Colorado river, Perija Range, Zulia state Venezuela (Casas et al, 2022). The fossil material of Wattieza casasii is currently in the National Museum and Gallery, Cardiff, Wales and the Palaeontological section, Museo de Biologia, Universidad del Zulia, Maracaibo, Venezuela (Berry, 2000; pag. 127). The etymology of the species Wattieza casasii was assigned in honor of Jhonny Casas, one of the discoverers of the original material (Berry, 2000; pag. 144).<ref>{{Cite journal|last=Berry|first=CM|date=October 2000|title=A reconsideration of Wattieza Stockmans (here attributed to Cladoxylopsida) based on a new species from the Devonian of Venezuela|journal=Review of Palaeobotany and Palynology|volume=112|issue=1–3|pages=12 |issn=0034-6667|doi=10.1016/s0034-6667(00)00038-5}}</ref><ref>{{Cite journal|last=Casas|first1=Jhonny|date= 2022|title=Formacion Campo Chico, una increible ventana a la flora y fauna fosil del Devonico (Givetiano-Frasniano) en la Sierra de Perija, Venezuela |
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|journal=Publicación Electrónica de la Asociación Paleontológica Argentina|volume=22|issue=1|pages=20-35|url=http://doi.org/10.5710/PEAPA.08.03.2022.401}}</ref> |
|journal=Publicación Electrónica de la Asociación Paleontológica Argentina|volume=22|issue=1|pages=20-35|url=http://doi.org/10.5710/PEAPA.08.03.2022.401}}</ref> |
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Revision as of 19:10, 23 December 2023
Wattieza Temporal range: Middle Devonian
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W. givetiana | |
Scientific classification | |
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Genus: | Wattieza |
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![](http://upload.wikimedia.org/wikipedia/commons/thumb/1/1b/Wattieza_casasii.jpg/220px-Wattieza_casasii.jpg)
Wattieza was a genus of prehistoric trees that existed in the mid-Devonian that belong to the cladoxylopsids, close relatives of the modern ferns and horsetails. The 2005 (publicly revealed in 2007) discovery in Schoharie County, New York, of fossils from the Middle Devonian about 385 million years ago united the crown of Wattieza to a root and trunk known since 1870. The fossilized grove of "Gilboa stumps" discovered at Gilboa, New York, were described as Eospermatopteris, though the complete plant remained unknown. These fossils have been described as the earliest known trees, standing 8 m (26 ft) or more tall, resembling the unrelated modern tree fern.[1]
Wattieza had fronds rather than leaves,[2] and they reproduced with spores.[1]
Belgian paleobotanist François Stockmans described Wattieza givetiana in 1968 from fossil fronds collected from Middle Devonian strata in the London-Brabant Massif in Belgium.[3]
English geologist and palaeobotanist Chris Berry described Wattieza casasii in Review of Paleobotany and Palynology (112) in 2000, based on fossil branches (13 slabs) and numerous other fragments (Berry, 2000) collected from middle Givetian-strata from the lower member of Campo Chico Formation (Casas et al, 2022). The lithology of the lower member consists in dark grey to green mudstones and shales, interbedded with medium-coarse grained sandstones close to the base of the Campo Chico Formation, in outcrops of the road to the Rio Socuy (Casas et al, 2022; pag 24), close to Cano Colorado river, Perija Range, Zulia state Venezuela (Casas et al, 2022). The fossil material of Wattieza casasii is currently in the National Museum and Gallery, Cardiff, Wales and the Palaeontological section, Museo de Biologia, Universidad del Zulia, Maracaibo, Venezuela (Berry, 2000; pag. 127). The etymology of the species Wattieza casasii was assigned in honor of Jhonny Casas, one of the discoverers of the original material (Berry, 2000; pag. 144).[4][5]
![](http://upload.wikimedia.org/wikipedia/commons/thumb/8/87/Wattieza_trunk.jpg/220px-Wattieza_trunk.jpg)
References
- ^ a b Stein, W. E., F. Mannolini, L. V. Hernick, E. Landling, and C. M. Berry. 2007. "Giant cladoxylopsid trees resolve the enigma of the Earth's earliest forest stumps at Gilboa", Nature (19 April 2007) 446:904-907.
- ^ Meyer-berthaud, B.; Decombeix, A.L. (2007). "Palaeobotany: A tree without leaves". Nature. 446 (7138): 861–862. arXiv:0704.2554. Bibcode:2007Natur.446..861M. doi:10.1038/446861a. PMID 17443169. S2CID 4324196.
- ^ Berry, Chris (2009). "The Middle Devonian plant collections of Francois Stockmans reconsidered". Geologica Belgica. 12 (1–2): 25–30.
- ^ Berry, CM (October 2000). "A reconsideration of Wattieza Stockmans (here attributed to Cladoxylopsida) based on a new species from the Devonian of Venezuela". Review of Palaeobotany and Palynology. 112 (1–3): 12. doi:10.1016/s0034-6667(00)00038-5. ISSN 0034-6667.
- ^ Casas, Jhonny (2022). "Formacion Campo Chico, una increible ventana a la flora y fauna fosil del Devonico (Givetiano-Frasniano) en la Sierra de Perija, Venezuela". Publicación Electrónica de la Asociación Paleontológica Argentina. 22 (1): 20–35.
- Paleobiology Database accessed 19 April 2007
- "Oldest tree had fronds, not leaves". Article on CNN.com
- (Cosmos) Michelle Carr, "Wattieza is world's oldest tree" 19 April 2007