ADAPTATIONS IN GRAMMYSIA OBLIQUA
Identifieur interne : 00E838 ( Main/Exploration ); précédent : 00E837; suivant : 00E839ADAPTATIONS IN GRAMMYSIA OBLIQUA
Auteurs : Richard K. Bambach [États-Unis]Source :
- Lethaia [ 0024-1164 ] ; 1971-04.
English descriptors
- KwdEn :
- Adductor, Anterior view, Appressed, Bambach, Bedding, Bedding plane, Bivalve, Byssal, Byssal gape, Byssus, Compaction, Dorsal, Dorsal margins, Flat surface, Gape, Grammysia, Grammysia obliqua, Groove, Gvammysia, Gvammysia obliqua, Length line, Life attitude, Life position, Ligament, Matrix, Mccoy, Middle devonian, Natural history, Nova, Nova scotia, Obliqua, Posterior adductor, Radial groove, Right valve, Right view, Scotia, Sediment, Single valves, Smooth periostracal sheath, Stonehouse formation, Valve, Ventral, Ventral margins, Water currents, Yale university.
- Teeft :
- Adductor, Anterior view, Appressed, Bambach, Bedding, Bedding plane, Bivalve, Byssal, Byssal gape, Byssus, Compaction, Dorsal, Dorsal margins, Flat surface, Gape, Grammysia, Grammysia obliqua, Groove, Gvammysia, Gvammysia obliqua, Length line, Life attitude, Life position, Ligament, Matrix, Mccoy, Middle devonian, Natural history, Nova, Nova scotia, Obliqua, Posterior adductor, Radial groove, Right valve, Right view, Scotia, Sediment, Single valves, Smooth periostracal sheath, Stonehouse formation, Valve, Ventral, Ventral margins, Water currents, Yale university.
Abstract
The Grammysiidae are an important but little understood family of Paleozoic bivalves. Specimens of Grammysia obliqua (McCoy) from the Stonehouse Formation (Uppermost Silurian), Nova Scotia, permit interpretation of their functional morphology and autecology. Grammysia obliqua was an immobile, semi‐infaunal, filter‐feeding bivalve. It lived fixed by a byssus, with the shell inclined about 40° to the sediment‐water interface. Though incapable of opening the shell, the animal maintained contact with the environment through byssal and dorsal‐posterior gapes. This latter gape was in a peculiar position for a bivalve and required some anatomical adaptation, but it was functionally efficient for the animal's life attitude.
Url:
DOI: 10.1111/j.1502-3931.1971.tb01287.x
Affiliations:
Links toward previous steps (curation, corpus...)
- to stream Istex, to step Corpus: 004F50
- to stream Istex, to step Curation: 004F50
- to stream Istex, to step Checkpoint: 006B93
- to stream Main, to step Merge: 00F170
- to stream Main, to step Curation: 00E838
Le document en format XML
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<series><title level="j" type="main">Lethaia</title>
<title level="j" type="alt">LETHAIA</title>
<idno type="ISSN">0024-1164</idno>
<idno type="eISSN">1502-3931</idno>
<imprint><biblScope unit="vol">4</biblScope>
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<publisher>Blackwell Publishing Ltd</publisher>
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<date type="published" when="1971-04">1971-04</date>
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<term>Anterior view</term>
<term>Appressed</term>
<term>Bambach</term>
<term>Bedding</term>
<term>Bedding plane</term>
<term>Bivalve</term>
<term>Byssal</term>
<term>Byssal gape</term>
<term>Byssus</term>
<term>Compaction</term>
<term>Dorsal</term>
<term>Dorsal margins</term>
<term>Flat surface</term>
<term>Gape</term>
<term>Grammysia</term>
<term>Grammysia obliqua</term>
<term>Groove</term>
<term>Gvammysia</term>
<term>Gvammysia obliqua</term>
<term>Length line</term>
<term>Life attitude</term>
<term>Life position</term>
<term>Ligament</term>
<term>Matrix</term>
<term>Mccoy</term>
<term>Middle devonian</term>
<term>Natural history</term>
<term>Nova</term>
<term>Nova scotia</term>
<term>Obliqua</term>
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<term>Right view</term>
<term>Scotia</term>
<term>Sediment</term>
<term>Single valves</term>
<term>Smooth periostracal sheath</term>
<term>Stonehouse formation</term>
<term>Valve</term>
<term>Ventral</term>
<term>Ventral margins</term>
<term>Water currents</term>
<term>Yale university</term>
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<term>Anterior view</term>
<term>Appressed</term>
<term>Bambach</term>
<term>Bedding</term>
<term>Bedding plane</term>
<term>Bivalve</term>
<term>Byssal</term>
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<term>Dorsal margins</term>
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<term>Grammysia obliqua</term>
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<term>Gvammysia obliqua</term>
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<term>Life position</term>
<term>Ligament</term>
<term>Matrix</term>
<term>Mccoy</term>
<term>Middle devonian</term>
<term>Natural history</term>
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<term>Nova scotia</term>
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<term>Posterior adductor</term>
<term>Radial groove</term>
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<term>Right view</term>
<term>Scotia</term>
<term>Sediment</term>
<term>Single valves</term>
<term>Smooth periostracal sheath</term>
<term>Stonehouse formation</term>
<term>Valve</term>
<term>Ventral</term>
<term>Ventral margins</term>
<term>Water currents</term>
<term>Yale university</term>
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<front><div type="abstract" xml:lang="en">The Grammysiidae are an important but little understood family of Paleozoic bivalves. Specimens of Grammysia obliqua (McCoy) from the Stonehouse Formation (Uppermost Silurian), Nova Scotia, permit interpretation of their functional morphology and autecology. Grammysia obliqua was an immobile, semi‐infaunal, filter‐feeding bivalve. It lived fixed by a byssus, with the shell inclined about 40° to the sediment‐water interface. Though incapable of opening the shell, the animal maintained contact with the environment through byssal and dorsal‐posterior gapes. This latter gape was in a peculiar position for a bivalve and required some anatomical adaptation, but it was functionally efficient for the animal's life attitude.</div>
</front>
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