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Goniophora
''Goniophora'' is an extinct genus of clams. It lived during the Ordovician to Permian The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleoz ... periods. Description ''Goniophora'' has a sharply angular, distinctive shell with a prominent ridge extending the length of the shell. The shell also has fine growth lines. References External links * * * * Bivalves described in 1848 Modiomorphida Prehistoric bivalve genera {{paleo-bivalve-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Modiomorphida
Modiomorphida is an extinct order of fossil saltwater clams, marine bivalve molluscs. Genera * †'' Ananterodonta'' * †'' Brahcylyrodesma'' * †'' Carminodonta'' * †'' Celtoconcha'' * †'' Cycloconchacea'' * †'' Dulcineaia'' * †'' Eurymya'' * †'' Fortowensia'' * †''Goniophora ''Goniophora'' is an extinct genus of clams. It lived during the Ordovician to Permian The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago ( ...'' * †'' Junjagiana'' * †'' Modiomorphoidea'' * †'' Moridunia'' * †'' Neofordilla'' * †'' Plicatomorpha'' * †'' Rimmyjmima'' * †'' Saffordia'' *†'' Tromelinodonta'' * †'' Whiteavesia'' External links * * * Bivalve orders Prehistoric bivalves {{paleo-bivalve-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Phillips (geologist)
John Phillips FRS (25 December 1800 – 24 April 1874) was an English geologist. In 1841 he published the first global geologic time scale based on the correlation of fossils in rock strata, thereby helping to standardize terminology including the term Mesozoic, which he invented. Life and work Phillips was born at Marden in Wiltshire. His father belonged to an old Welsh family, but settled in England as an officer of excise and married the sister of William Smith, a renowned English geologist. When both parents died when he was a child, Phillips's custody was assumed by Smith and Phillips was brought into Smith's London home during early 1815. During the next few years he attended various schools and helped his uncle with his geological research and writing; he also developed an interest in lithography (printing from prepared slabs of stone), and was among the earliest English practitioners of the process, experimenting with it between about 1816 and 1819. After ending sc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. The Ordovician, named after the Celtic Britons, Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same Rock (geology), rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed Stratum, strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official period of the Paleozoic Era by the International Union of Geological Sciences, Intern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian
The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the region of Perm in Russia. The Permian witnessed the diversification of the two groups of amniotes, the synapsids and the sauropsids ( reptiles). The world at the time was dominated by the supercontinent Pangaea, which had formed due to the collision of Euramerica and Gondwana during the Carboniferous. Pangaea was surrounded by the superocean Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these drier conditions, rose to dominance in place of their am ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bivalves Described In 1848
Bivalvia (), in previous centuries referred to as the Lamellibranchiata and Pelecypoda, is a class of marine and freshwater molluscs that have laterally compressed bodies enclosed by a shell consisting of two hinged parts. As a group, bivalves have no head and they lack some usual molluscan organs, like the radula and the odontophore. They include the clams, oysters, cockles, mussels, scallops, and numerous other families that live in saltwater, as well as a number of families that live in freshwater. The majority are filter feeders. The gills have evolved into ctenidia, specialised organs for feeding and breathing. Most bivalves bury themselves in sediment, where they are relatively safe from predation. Others lie on the sea floor or attach themselves to rocks or other hard surfaces. Some bivalves, such as the scallops and file shells, can swim. The shipworms bore into wood, clay, or stone and live inside these substances. The shell of a bivalve is composed of calci ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
