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Talbragar Fossil Site
The Talbragar fossil site is a paleontological site of Late Jurassic (Tithonian) age in the central west of New South Wales, Australia. It lies about north-east of the town of Gulgong, and north-west of Sydney. The site has been known for over a century during which it has been extensively excavated to the point of near exhaustion. It is now registered as a Crown Land Reserve for the preservation of fossils; access is by permit, and the collection of rocks and fossil specimens is prohibited. The reserve is listed on the (now defunct) Register of the National Estate. Fossils The fossil-bearing rocks are fine-grained siltstones and mudstones that are part of the Purlawaugh Formation. They occur mainly as loose blocks and weathered shales over an area of about , with a thickness of no more than . They are thought to be the remnants of sediments from a small freshwater lake, surrounded by forest, which existed about 175 million years ago when Australia was part of Gondwana. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cavenderichthys
''Cavenderichthys talbragarensis'' is a species of prehistoric bony fish found in the Talbragar Fish beds. Recently, it has been placed as a member of Orthogonikleithridae, alongside ''Leptolepides ''Leptolepides'' is an extinct genus of prehistoric ray-finned fish that lived during the early Tithonian stage of the Late Jurassic epoch. See also * List of prehistoric bony fish genera This list of prehistoric bony fish is an attempt to c ..., Orthogonikleithrus'' and '' Waldmanichthys.'' References External links {{Taxonbar, from=Q5055005 Prehistoric fish of Australia Prehistoric bony fish genera Jurassic bony fish ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nilssonia (plant)
''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. Taxonomy The genus was erected by Brongniart under the name ''Nilsonia'' based on material from the Hettangian of Scania. The spelling of the name (a dedication to Sven Nilsson) was later corrected to ''Nilssonia''. The diagnosis of the genus, initially based on the pinnate ''Nilssonia brevis'', was later amended to include entire-margined and irregularly segmented species as well as information on the cuticle. Description ''Nilssonia'' leaves can have entire margins, irregularly dissected margins or clearly divided leaflets. The lamina or the leaflets are attached to the midrib or rachis on the 'upper' (adaxial) side of the leaf, unlike in other similar genera such as ''Taeniopteris''. Parallel veins exit the midrib, with no fusion ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seed Fern
A seed is an embryonic plant enclosed in a protective outer covering, along with a food reserve. The formation of the seed is a part of the process of reproduction in seed plants, the spermatophytes, including the gymnosperm and angiosperm plants. Seeds are the product of the ripened ovule, after the embryo sac is fertilized by sperm from pollen, forming a zygote. The embryo within a seed develops from the zygote, and grows within the mother plant to a certain size before growth is halted. The seed coat arises from the integuments of the ovule. Seeds have been an important development in the reproduction and success of vegetable gymnosperm and angiosperm plants, relative to more primitive plants such as ferns, mosses and liverworts, which do not have seeds and use water-dependent means to propagate themselves. Seed plants now dominate biological niches on land, from forests to grasslands both in hot and cold climates. The term "seed" also has a general meaning that ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pagiophyllum
''Pagiophyllum'' 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 were found around the globe during the Carboniferous to the Cretaceous period. Location of palaeontological sites *In Paleorrota geopark in Brazil. Upper Triassic period, the Santa Maria Formation The Santa Maria Formation is a sedimentary rock formation found in Rio Grande do Sul, Brazil. It is primarily Carnian in age (Late Triassic), and is notable for its fossils of cynodonts, "rauisuchian" pseudosuchians, and early dinosaurs and oth .... References Prehistoric gymnosperm genera Araucariaceae {{paleo-conifer-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brachyphyllum
''Brachyphyllum'' (meaning "short leaf") 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.''Brachyphyllum'' in the List of species * † ''B. yorkense'' * † ''B. castatum'' * † ''B. castilhoi'' * † ''B. punctatum'' * † ''B. sattlerae'' - a taxon from the of |
Elatocladus
''Elatocladus'' is an extinct form genus of Mesozoic sterile conifer Conifers are a group of conifer cone, cone-bearing Spermatophyte, seed plants, a subset of gymnosperms. Scientifically, they make up the phylum, division Pinophyta (), also known as Coniferophyta () or Coniferae. The division contains a single ... leaves, used for shoots with the morphology of "elongated, dorsiventrally flattened leaves with a single vein; divergent from stem". Conifers with leaves of ''Elatocladus'' morphology are of uncertain taxonomic position within conifers. References Conifer genera Triassic plants Jurassic plants Cretaceous plants Prehistoric gymnosperm genera {{cretaceous-plant-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Agathis Jurassica Leaves
''Agathis'', commonly known as kauri or dammara, is a genus of 22 species of evergreen tree. The genus is part of the ancient conifer family Araucariaceae, a group once widespread during the Jurassic and Cretaceous periods, but now largely restricted to the Southern Hemisphere except for a number of extant Malesian ''Agathis''.de Laubenfels, David J. 1988. Coniferales. P. 337–453 in Flora Malesiana, Series I, Vol. 10. Dordrecht: Kluwer Academic. Description Mature kauri trees have characteristically large trunks, with little or no branching below the crown. In contrast, young trees are normally conical in shape, forming a more rounded or irregularly shaped crown as they achieve maturity.Whitmore, T.C. 1977. ''A first look at Agathis''. Tropical Forestry Papers No. 11. University of Oxford Commonwealth Forestry Institute. The bark is smooth and light grey to grey-brown, usually peeling into irregular flakes that become thicker on more mature trees. The branch structure ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Podozamites
''Podozamites'' is an extinct genus of fossil conifer leaves. In its broader sense, it has been used as a morphogenus (Form classification, form taxon) to refer to any broad leaved multi-veined conifer leaves. Modern broad-leaved conifers with a similar form include ''Agathis'' in the family Araucariaceae and ''Nageia'' in Podocarpaceae, with some ''Podozamites'' ''sensu lato'' probably belonging to the same families. In a more narrow sense, ''Podozamites'' has been used to refer to the leaves of a probably Monophyly, monophyletic group of deciduous broad leafed Voltziales, voltzialean conifers which lived in the Northern Hemisphere, particularly East Asia and Siberia, during the Late Triassic to early Late Cretaceous, where it formed part of wet coal swamp communities. Description In the right conditions, ''Podozamites'' leaves ''sensu stricto'' preserve delicate cuticle and insect damage, and are thought to have been regularly shed. They are associated with conifer cones of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
