Palissya
Palissya Temporal range:
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Scientific classification ![]() | |
Kingdom: | Plantae |
Clade: | Tracheophytes |
(unranked): | Gymnosperms |
Division: | Pinophyta |
Class: | Pinopsida |
Order: | †Palissyales |
Family: | †Palissyaceae |
Genus: | †Palissya Endlicher, 1847 |
Species | |
See text |
Palissya is an extinct genus of conifer, known from the Late Triassic to the Early Cretaceous. The cone of Palissya is noted for its unusual construction, which is borne on a large bract (modified leaf), and consists of two parallel rows of ovules that run along the midline of the adaxial surface of the bract which are encased in cup-like structures formed by scales. The bracts are helically arranged around an axis, forming a compound catkin-like structure. The seeds are thin-walled were likely only viable for a short period of time, and were likely adapted to wind dispersal. Palissya has been considered in some aspects to be similar to some Paleozoic Voltziales, as well as Taxaceae and Podocarpaceae. Most leaves assigned to the genus do not belong to the same plant as the conifer cone. The specimens from the Middle Jurassic of Yorkshire are associated with Elatocladus like leaves. Several species that were formerly considered part of the genus have been moved over to the separate genus . Palissya first appeared in the Northern Hemisphere during the latest Triassic (Rhaetian) and spread to Eastern Gondwana during the Middle Jurassic. The youngest known records of Palissya in the Northern Hemisphere are from the Middle Jurassic, but Palissya persisted in Eastern Gondwana into the Early Cretaceous, with the youngest records being from the Aptian.[1]
Species[]
After[1]
Species | Authority | Country | Age |
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P. hunanensis | Wang 2012 | ![]() |
Late Triassic (Rhaetian) |
P. sphenolepis | (Braun 1843) Nathorst 1908 emend.
Florin 1958 |
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Late Triassic-Early Jurassic (Rhaetian-Hettangian) |
P. harrisii | C.R. Hill ex
Pattemore & Rozefelds |
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Middle Jurassic (Aalenian) |
P. bartrumii | Edwards 1934 | ![]() |
Middle Jurassic (Callovian) ?Late Jurassic (?Tithonian) |
P. elegans | Parris et al. 1995 | ![]() |
Early Cretaceous (Valanginian) |
P. tillackiorum | Pattemore & Rozefelds, 2019 | ![]() |
Early Cretaceous (Valanginian) |
Palissya sp. (Koonwarra) | N/A | ![]() |
Early Cretaceous (Aptian) |
P. antarctica | Cantrill 2000 | ![]() |
Early Cretaceous (Aptian) |
References[]
- ^ a b Pattemore, Gary A.; Rozefelds, Andrew C. (2019-12-01). "Palissya – absolutely incomprehensible or surprisingly interpretable: a new morphological model, affiliations and phylogenetic insights". Acta Palaeobotanica. 59 (2): 181–214. doi:10.2478/acpa-2019-0015. ISSN 2082-0259.
- ^ a b Van Konijnenburg-Van Cittert, Johanna H.A.; Pott, Christian; Schmeißner, Stefan; Dütsch, Günter; Kustatscher, Evelyn (2021-05-01). "The Rhaetian flora of Wüstenwelsberg, Bavaria, Germany: Description of selected gymnosperms (Ginkgoales, Cycadales, Coniferales) together with an ecological assessment of the locally prevailing vegetation". Review of Palaeobotany and Palynology. 288: 104398. doi:10.1016/j.revpalbo.2021.104398. ISSN 0034-6667.
- Fossil record of plants
- Extinct plants of New Zealand
- Conifers
- Prehistoric plant genera