Palissya Temporal range: | |
---|---|
Scientific classification | |
Kingdom: | Plantae |
Clade: | Tracheophytes |
Clade: | Gymnospermae |
Division: | Pinophyta |
Class: | Pinopsida |
Order: | † Palissyales |
Family: | † Palissyaceae |
Genus: | † Palissya Endlicher, 1847 |
Species | |
See text |
Palissya is an extinct form genus of female (ovule-bearing) conifer cones, known from the Late Triassic (Rhaetian) to the Early Cretaceous (Aptian). The cone of Palissya is noted for its unusual catkin-like construction: Slender bracts (modified leaves) are rigidly attached in a helical pattern around a tall woody core. The adaxial (upper) surface of each bract bears two parallel rows of ovules which are encased in cup-like structures formed by scales. The seeds are thin-walled and were likely only viable for a short period of time, meaning that they were probably adapted to wind dispersal. [1] [2]
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. Palissya specimens from the Middle Jurassic of Yorkshire are associated with Elatocladus-like leaves. Several Australasian species with fragile cones were referred to the separate genus Knezourocarpon , [2] though some were later moved back into Palissya. [1] Other related cone genera include Stachyotaxus , Metridiostrobus , and Compsostrobus , all from the Late Triassic of the Northern Hemisphere. [1] [2]
True specimens of Palissya first appeared in the Northern Hemisphere during the latest Triassic (Rhaetian) and spread to Eastern Gondwana (modern Australia, New Zealand, and Antarctica) 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]
After [1]
Species | Authority | Country | Age |
---|---|---|---|
P. hunanensis | Wang 2012 | China (Hunan) | Late Triassic (Rhaetian) |
P. sphenolepis | (Braun 1843) Nathorst 1908 emend. Florin 1958 | Germany (Franconia) Sweden (Stabbarp) | Late Triassic-Early Jurassic (Rhaetian-Hettangian) |
P. harrisii | C.R. Hill ex Pattemore & Rozefelds | England (Yorkshire) | Middle Jurassic (Aalenian) |
P. bartrumii | Edwards 1934 | New Zealand | Middle Jurassic (Callovian) ?Late Jurassic (?Tithonian) |
P. elegans | Parris et al. 1995 | Australia (Victoria) | Early Cretaceous (Valanginian) |
P. tillackiorum | Pattemore & Rozefelds, 2019 | Australia (Queensland) | Early Cretaceous (Valanginian) |
Palissya sp. (Koonwarra) | N/A | Australia (Victoria) | Early Cretaceous (Aptian) |
P. antarctica | Cantrill 2000 | Antarctica (Antarctic Peninsula) | Early Cretaceous (Aptian) |
Glossopteris is the largest and best-known genus of the extinct Permian order of seed plants known as Glossopteridales. The genus Glossopteris refers only to leaves, within a framework of form genera used in paleobotany. Species of Glossopteris were the dominant trees of the middle to high-latitude lowland vegetation across the supercontinent Gondwana during the Permian Period. Glossopteris fossils were critical in recognizing former connections between the various fragments of Gondwana: South America, Africa, India, Australia, New Zealand, and Antarctica.
Bennettitales is an extinct order of seed plants that first appeared in the Permian period and became extinct in most areas toward the end of the Cretaceous. Bennettitales were amongst the most common seed plants of the Mesozoic, and had morphologies including shrub and cycad-like forms. The foliage of bennettitaleans is superficially nearly indistinguishable from that of cycads, but they are distinguished from cycads by their more complex flower-like reproductive organs, at least some of which were likely pollinated by insects.
Agathoxylon is a form genus of fossil wood, including massive tree trunks. Although identified from the late Palaeozoic to the end of the Mesozoic, Agathoxylon is common from the Carboniferous to Triassic. Agathoxylon represents the wood of multiple conifer groups, including both Araucariaceae and Cheirolepidiaceae, with late Paleozoic and Triassic forms possibly representing other conifers or other seed plant groups like "pteridosperms".
Nilssonia is a genus of fossil foliage traditionally assigned to the Cycadophyta either in Cycadales or their own order Nilssoniales, though the relationships of this genus with the Cycadales have been put into question on chemical grounds.
Brachyphyllum is a form genus of fossil coniferous plant foliage. Plants of the genus have been variously assigned to several different conifer groups including Araucariaceae and Cheirolepidiaceae. They are known from around the globe from the Late Carboniferous to the Late Cretaceous periods. B. sattlerae was named after the fictional palaebotanist Ellie Sattler from the Jurassic Park franchise.
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Corystosperms are a group of extinct seed plants belonging to the family Corystospermaceae assigned to the order Corystospermales or Umkomasiales. They were first described based on fossils collected by Hamshaw Thomas from the Burnera Waterfall locality near the Umkomaas River of South Africa. Corystosperms are typified by a group of plants that bore forked Dicroidium leaves, Umkomasia cupulate ovulate structures and Pteruchus pollen organs, which grew as trees that were widespread over Gondwana during the Middle and Late Triassic. Other fossil Mesozoic seed plants with similar leaf and/or reproductive structures have also sometimes been included within the "corystosperm" concept sensu lato, such as the "doyleoids" from the Early Cretaceous of North America and Asia. A potential corystosperm sensu lato, the leaf genus Komlopteris, is known from the Eocene of Tasmania, around 53-50 million years old, over 10 million years after the Cretaceous–Paleogene extinction event.
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Czekanowskiales, also known as Leptostrobales, are an extinct group of seed plants. Members of the family are distinguished by persistent leaves borne on deciduous short shoots, subtended by scale-like leaves. The leaves are highly dissected. They likely grew as trees and shrubs. The main ovulate structure of Czekanowskiales, Leptostrobus, consists of bivalved seed-bearing round capsule-like structures arranged along a long axis. The fossil record of Czekanowskiales is largely confined to the Northern Hemisphere, and they inhabited warm-temperate and temperate climates under humid conditions. The oldest possible records of the group are ovulate cones from the Late Permian of Italy, but the group is primarily known from the Late Triassic onwards, and were abundant during the Jurassic and Early Cretaceous. Only a handful of species are known from the Late Cretaceous, confined to the northern Russian Far East, corresponding to the decline of other seed plant groups during the explosive radiation of flowering plants. The affinites of Czekanowskiales to other seed plants are obscure. A close relationship to the Ginkgoales have been proposed, based on similar preserved molecular signatures of fossil cuticles, with some authors placing Ginkgoales and Czekanowskiales into the broader grouping Ginkgophyta.
Palissyales are an extinct order of conifers, known from the Mesozoic. They are best known from the genus Palissya, which is found in Laurasia and Eastern Gondwana dating from the Late Triassic to Early Cretaceous. The only other confirmed genus of the family, Stachyotaxus known from the Late Triassic of the Northern Hemisphere. The genus Knezourocarpon from the Jurassic of Australia has also been tentatively considered a member of the order. The cone of the best known genus Palissya is noted for its unusual construction, which is borne on a large bract, 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.
Otozamites is an extinct form genus of leaves belonging to the Bennettitales.
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