Lecture 12 - Mollusks II Flashcards
Class Pelecypoda:
Mollusks without a distinct head, radula, or any anterior sensory apparatus; foot adapted for burrowing in most forms, but is adapted for crawling in some forms, and is functionless in others; poorly developed nervous system; general bilateral symmetry (they do not undergo “torsion”); have a hinged, bivalved shell with the symmetry plane oriented between the two valves, which are mirror images of each other; the shell is usually composed entirely of calcite, but some forms have a shell composed entirely of aragonite, and a few forms have a shell that is mostly calcite with an interior lining of nacreous aragonite; 5 diverse subclasses with excellent fossil records
Class Pelecypoda Geologic Range
Early Cambrian to Recent
Five main subclasses of Class Pelecypoda
Subclass Palaeotaxodonta Subclass Isofilibranchia Subclass Heteroconchia Subclass Pteriomorpha Subclass Anomalodesmata
Subclass Palaeotaxodonta:
Pelecypods with protobranch gills; shell usually aragonite with nacreous microstructure; dentition usually taxodont, but some are actinodont; usually isomyarian; no siphons; foot adapted for burrowing or crawling
Subclass Palaeotaxodonta Geologic Range
Early Cambrian to Recent
Subclass Isofilibranchia:
Pelecypods with filibranch gills; shell either calcite + aragonite or totally aragonite with a nacreous interior; dentition usually absent or functionless; usually isomyarian; no siphons; small, functionless foot
Subclass Isofilibranchia Geologic Range
Early Cambrian to Recent
Subclass Heteroconchia:
Pelecypods with filibranch or eulamellibranch gills; shell usually aragonite with variable microstructure; dentition usually heteroodont, but some are taxodont; usually isomyarian; most have siphons; foot adapted for burrowing in most forms, crawling in some
Subclass Heteroconchia Geologic Range
Early Ordovician to Recent
Subclass Pteriomorpha:
Pelecypods with filibranch or eulamellibranch gills; shell may be aragonite, calcite or both, with variable microstructure, dentition may be heteroodont, taxodont, actinodont or absent; usually anisomyarian; most do not have siphons; small, functionless foot
Subclass Pteriomorpha Geologic Range
Early Ordovician to Recent
Subclass Anomalodesmata:
Pelecypods with eulamellibranch or septibranch gills; shell is aragonite with prismatic microstructure on the outside and nacreous microstructure on the inside; dentition usually absent; usually isomyarian; most have siphons; small, foot adapted for burrowing
Subclass Anomalodesmata Geologic Range
Middle Ordovician to Recent
Visceral Mass:
Headless mass is positioned in the hinge region of the shell interior
Foot:
Muscular organ modified mainly for burrowing
Labial Palps:
Pair of fleshy structures adjacent to the mouth; used for feeding
Mantle:
Tissue that lines the inside of the pelecypod shell
Siphon:
Folds in the mantle forming two tubes, including one inhalent and one exhalent siphon.
Gills:
Variably-shaped structures of blood-filled tissue that serve as respiratory organs.
Adductor Muscles:
Muscles that flex to close the two pelecypod valves.
Isomyarian:
Equal-sized anterior and posterior adductors
Anisomyarian:
Small anterior adductor and large psterior adductor
Monomyarian:
Only one adductor muscle (the posterior adductor)
Ligament:
Connective tissue holding the valves together at the hinge (either external or internal)
Beak (=Umbo):
Pointed end of the shell, near the hingeline
Commissure:
Site where the two valves meet opposite the beak when the shell is closed.
Right Valve vs. Left Valve
The two valves are mirror images of each other
Anterior:
end of the shell towards which the beak points
Posterior:
end away from beak
Dorsal:
hinge side of shell
Ventral:
commissure side of the shell
Ornamentation:
Radial ribs, growth rings, spines, etc., on the exterior of the shell
Adductor Scars:
Lines on the shell interior marking where the adductor muscles attach
Pallial Line:
Line on the shell interior along which the mantle attaches.
Pallial Sinus:
Indentation of the pallial line marking where the siphons are positioned.
Hinge Dentition:
Tooth and socket structure that articulates the two valves together.
Cardinal Teeth:
Short hinge teeth that are oriented roughtly perpendicular to the hingeline.
Lateral Teeth:
Long hinge teeth that are oriented roughly parallel to the hingeline.