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Mollusks, Fossil --- Mollusks, Fossil --- Mollusks, Fossil --- Paleontology
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The Bathonian Great Oolite Group is a fossiliferous series of calcareous and argillaceous rocks that are only rarely oolitic in composition. Based upon the collection of physician John Lycett (1804-82), made in quarries on Minchinhampton Common in the Cotswolds, this monograph, written in collaboration with the geologist John Morris (1810-86), covers only that part of the Great Oolite found in this location. However, it also includes species found on the coast of Yorkshire, near Scarborough, which would be included in the Inferior Oolite. The significance of this work is that it is one of just a handful of monographs describing and illustrating the British Jurassic gastropod and bivalve fauna. Having received no significant revision since the late 1940s, it remains a key reference point for Jurassic molluscs. Volume 2 comprises the supplement published by Lycett in 1863, covering molluscs found in geological formations besides the Great Oolite.
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The Eocene sediments of the London and Hampshire basins in southern England are rich in fossil invertebrates, plants and vertebrates; in particular, they yield a great diversity of often well-preserved fossil mollusc shells. Seeking to provide a methodical treatment of known specimens, Frederick E. Edwards (1799-1875) and Searles V. Wood (1798-1880) had divided the workload of describing the Mollusca found in the English Tertiary formations, with Edwards taking the older formations and Wood the newer. When Edwards became ill, however, Wood took on the Eocene bivalves, yet he was unable to add much to the treatment of cephalopods and gastropods. Featuring detailed illustrations, the two volumes provide for each species a synonymy, diagnosis (in Latin), full description, dimensions, occurrence, and well-informed remarks. Volume 2 comprises Wood's Monograph of the Eocene Bivalves of England, originally published in three parts between 1861 and 1871. This reissue includes the 1877 supplement.
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The Bathonian Great Oolite Group is a fossiliferous series of calcareous and argillaceous rocks that are only rarely oolitic in composition. Based upon the collection of physician John Lycett (1804-82), made in quarries on Minchinhampton Common in the Cotswolds, this monograph, written in collaboration with the geologist John Morris (1810-86), covers only that part of the Great Oolite found in this location. However, it also includes species found on the coast of Yorkshire, near Scarborough, which would be included in the Inferior Oolite. The significance of this work is that it is one of just a handful of monographs describing and illustrating the British Jurassic gastropod and bivalve fauna. Having received no significant revision since the late 1940s, it remains a key reference point for Jurassic molluscs. Volume 1 comprises three parts published between 1850 and 1854, covering cephalopods, gastropods and worms as well as bivalves.
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The Eocene sediments of the London and Hampshire basins in southern England are rich in fossil invertebrates, plants and vertebrates; in particular, they yield a great diversity of often well-preserved fossil mollusc shells. Seeking to provide a methodical treatment of known specimens, Frederick E. Edwards (1799-1875) and Searles V. Wood (1798-1880) had divided the workload of describing the Mollusca found in the English Tertiary formations, with Edwards taking the older formations and Wood the newer. When Edwards became ill, however, Wood took on the Eocene bivalves, yet he was unable to add much to the treatment of cephalopods and gastropods. Featuring detailed illustrations, the two volumes provide for each species a synonymy, diagnosis (in Latin), full description, dimensions, occurrence, and well-informed remarks. Volume 1 comprises the Monograph of the Eocene Cephalopoda and Univalves of England, originally published in several parts between 1849 and 1877.
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The Pliocene-Pleistocene Crags of East Anglia are an incredibly rich source of fossil shells, many belonging to extant Boreal and Mediterranean genera. Dominated by marine gastropods and bivalves, the deposits also contain evidence of terrestrial and non-marine gastropods and bivalves, brachiopods, and extensive epifauna including bryozoans. Published between 1848 and 1879 in four volumes, the latter two being supplements with further descriptions and geological notes, this monograph by Searles Valentine Wood (1798-1880) covers more than 650 species and varieties of fossil mollusc. For each species Wood gives a synonymy, diagnosis (in Latin), full description, dimensions, occurrence and remarks. The supplements also provide a breakdown of the species and their current distribution. The detailed plates were prepared by the conchologist George Brettingham Sowerby and his namesake son. Volume 1 (1848) covers gastropods and scaphopods, illustrated in 21 plates.
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The Pliocene-Pleistocene Crags of East Anglia are an incredibly rich source of fossil shells, many belonging to extant Boreal and Mediterranean genera. Dominated by marine gastropods and bivalves, the deposits also contain evidence of terrestrial and non-marine gastropods and bivalves, brachiopods, and extensive epifauna including bryozoans. Published between 1848 and 1879 in four volumes, the latter two being supplements with further descriptions and geological notes, this monograph by Searles Valentine Wood (1798-1880) covers more than 650 species and varieties of fossil mollusc. For each species Wood gives a synonymy, diagnosis (in Latin), full description, dimensions, occurrence and remarks. The supplements also provide a breakdown of the species and their current distribution. The detailed plates were prepared by the conchologist George Brettingham Sowerby and his namesake son. Volume 3 (1872-4) comprises the first supplement, covering univalves and bivalves, and includes an important map of the Crag district.
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The Pliocene-Pleistocene Crags of East Anglia are an incredibly rich source of fossil shells, many belonging to extant Boreal and Mediterranean genera. Dominated by marine gastropods and bivalves, the deposits also contain evidence of terrestrial and non-marine gastropods and bivalves, brachiopods, and extensive epifauna including bryozoans. Published between 1848 and 1879 in four volumes, the latter two being supplements with further descriptions and geological notes, this monograph by Searles Valentine Wood (1798-1880) covers more than 650 species and varieties of fossil mollusc. For each species Wood gives a synonymy, diagnosis (in Latin), full description, dimensions, occurrence and remarks. The supplements also provide a breakdown of the species and their current distribution. The detailed plates were prepared by the conchologist George Brettingham Sowerby and his namesake son. Volume 2 (1851-61) covers bivalves and brachiopods, illustrated in 31 plates.
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The Pliocene-Pleistocene Crags of East Anglia are an incredibly rich source of fossil shells, many belonging to extant Boreal and Mediterranean genera. Dominated by marine gastropods and bivalves, the deposits also contain evidence of terrestrial and non-marine gastropods and bivalves, brachiopods, and extensive epifauna including bryozoans. Published between 1848 and 1879 in four volumes, the latter two being supplements with further descriptions and geological notes, this monograph by Searles Valentine Wood (1798-1880) covers more than 650 species and varieties of fossil mollusc. For each species Wood gives a synonymy, diagnosis (in Latin), full description, dimensions, occurrence and remarks. The supplements also provide a breakdown of the species and their current distribution. The detailed plates were prepared by the conchologist George Brettingham Sowerby and his namesake son. Volume 4 (1879) comprises the second supplement, covering univalves and bivalves. Also included here is a third supplement, published by the late author's son in 1882.
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