Mollusca

Mollusca Mollusca

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mollusks Mollusca blötdjur molluscs

mollusks<br />

<strong>Mollusca</strong><br />

blötdjur<br />

molluscs


<strong>Mollusca</strong><br />

<strong>Mollusca</strong><br />

One of the largest and most diverse animal groups today<br />

~200 000 extant species (130 000 described)<br />

Strong shell gives exceptionally good fossil record<br />

~70 000 described fossil species<br />

Well represented from the earliest Cambrian onwards


general things<br />

<strong>Mollusca</strong><br />

<strong>Mollusca</strong>


What is a mollusc?<br />

Fundamental organization :<br />

- shell secreted by a layer of tissue called the mantle<br />

- mouth and anus at opposite end (but in gastropods both anterior)<br />

- mantle cavity bears gills (but pulmonate gastropods have no gills)<br />

- above mantle cavity is the visceral mass<br />

with gut, nervous, circulatory and muscular system<br />

- muscular foot facilitates movement<br />

- shell is of calcium carbonate (calcite or aragonite) (but may be secondaryly lost)<br />

- shell typically external (but in some groups it became internal)<br />

- grow by accretion (calcium carbonate is added to the edge of the shell by the mantle)<br />

- generally marine (but also few freshwater and terrestrial groups)<br />

<strong>Mollusca</strong>


Typical features: Shell<br />

Strongly mineralised = hard<br />

1-2 components (up to 8)<br />

Simple, compact shapes<br />

Usually coiled to some degree<br />

= Facilitates excellent fossil record<br />

No other animal group can compete!


Typical features: Shell<br />

complex structure (often important for classification)<br />

calcitic or aragonitic, or both; with organic matrix<br />

often 3 shell units<br />

- periostracum<br />

- ostracum<br />

- hypostracum<br />

6 primary structure types<br />

- simple prismatic (a)<br />

- compound prismatic (b)<br />

- sheet nacreous (c)<br />

- foliated (d)<br />

- crossed-lamellar (e)<br />

- homogeneous (f)<br />

periostracum (organic)<br />

ostracum (calcitic, aragonitic)<br />

hypostracum (nacreous)


Typical features: Radula<br />

Most molluscs have a radula (rasping<br />

tongue)<br />

The radula is ribbon-like and bears<br />

many small teeth arranged in rows<br />

Found in at least some representatives<br />

of all molluscan classes except<br />

Bivalvia<br />

Allowed early molluscs to graze on<br />

bacterial films on soft sediment?<br />

Now specialised to allow herbivory,<br />

detrivory and carniverous diets<br />

<strong>Mollusca</strong>


Typical features: Foot<br />

Muscular structure below visceral<br />

mass and mantle cavity<br />

Creeping sole in Tryblidiida,<br />

Polyplacophora, Gastropoa<br />

-Presumably primitive feature<br />

-Movement by ciliary movement or<br />

rythmic muscular contraction<br />

Modifications for burrowing in Bivalvia<br />

-Movement by hydrostatic pressure<br />

and muscular contraction<br />

Modified into tentacles and hyponome<br />

in cephalopods<br />

Reduced or abscent in some groups


Tryblidiida<br />

(”monoplacophorans”)<br />

Scaphopoda<br />

(tusk shells)<br />

Polyplacophora<br />

(chitons)<br />

Bivalvia<br />

Phylum <strong>Mollusca</strong><br />

- 8 extant Classes<br />

Gastropoda<br />

Cephalopoda<br />

Solenogastres<br />

(aplacophora)<br />

Caudofoveata<br />

(aplacophora)


Gastropoda<br />

mollusks with a head and foot (the head-foot), and a mantle covering visceral mass<br />

typically with a univalve calcareous shell (maybe reduced, or pseudo-bivalved)<br />

head-foot can be withdrawn into the shell (sealed by operculum)<br />

shell generally anisometrically coiled in some manner and external<br />

radula typically present<br />

torsion of the visceral mass is the single unique defining characteristic (synapomorphy)<br />

known since Late Cambrian<br />

<strong>Mollusca</strong> – systematics – Gastropoda


Polyplacophora (chitons)<br />

primitive molluscs with eight, articulating (overlapping) aragonitic plates<br />

(except one Palaeozoic lineage had seven)<br />

generally oval in outline with a flattened body<br />

creeping foot, a primitive feature in molluscs<br />

radula, mineralized with magnetite<br />

head is poorly developed<br />

the girdle (perinotum), a band of muscular tissue, runs along the dorsal periphery<br />

embedded in the girdle are small calcareous spines, scales or spicules<br />

known since the Late Cambrian (isolated plates)<br />

<strong>Mollusca</strong> – systematics – Polyplacophora


Tryblidiida (”monoplacophorans” sensu stricto)<br />

simple cap-shaped shells<br />

never a diverse or abundant group<br />

well-represented in the fossil record from the late Cambrian to the Devonian<br />

first appeared in the Middle Cambrian<br />

until the discovery of Neopilina in 1952, considered to be extinct<br />

coiling exogastric<br />

distinguished by the fact that virtually all organ systems are found in multiples<br />

(gills, nephridia, muscles) pseudo-segmentation or serialization<br />

common ancestry with annelids and arthropods have been suggested<br />

serialization ≠ segmentation<br />

<strong>Mollusca</strong>


Bivalvia (=Pelecypoda, Lamellibranchia)<br />

pair of valves (right and left valve)<br />

bilobed mantle<br />

valves articulate along a dorsal hinge line<br />

typically bilaterally symmetric (plane of symmetry passing between the valves,<br />

= commissural plane)<br />

no head<br />

prominent ventral foot<br />

known since the Early Cambrian, but diversify not prior to Ordovician<br />

but still not a very common faunal element during the Paleozoic<br />

<strong>Mollusca</strong> – systematics – Bivalvia


Cephalopods<br />

most highly evolved molluscs (especially eyes and brain)<br />

a high level of cephalization (concentration of sensory and neural centers in the head)<br />

group includes the modern Nautilus, argonauts, squids, octopuses, cuttlefishes<br />

as well as the fossil ammonites and belemnites<br />

2 main groups: Palcephalopoda (nautilids and endoceratids)<br />

Neocephalopoda (orthoceratids, ammonites, belemnites, most living forms)<br />

typically bilaterally symmetrical<br />

shell, if developed, subdivided in chambers by septae<br />

chambers are connected by a tube (siphuncle)<br />

hyponome and tentacles are homologue to foot of bivalves and gastropods<br />

mouth with powerful horny beaklike jaws and a radula<br />

radula less developed than in gastropods<br />

since Late Cambrian<br />

<strong>Mollusca</strong> – systematics – Cephalopoda


Scaphopoda (tusk shells)<br />

small group of mostly small, infaunal or semi-infaunal, marine mollusks<br />

shell typically a few centimeters in length<br />

(largest form found 30 cm in length)<br />

shell is a slender tapering and usually gently curved tube<br />

shell is open at both ends, the large end of the shell being anterior<br />

exterior has finely spaced growth lines and usually some<br />

type of longitudinal ornamentation or ribs.<br />

protrusible burrowing foot extends from the anterior end<br />

no gills, respiration by direct exchange with mantle tissue<br />

head is poorly-developed<br />

numerous tentacles (called captacula) and a radula<br />

animal feeds on microscopic organisms and organic detritus.<br />

Scaphopoda first appear in the Ordovician or the Devonian or even the early Carboniferous<br />

rare in fossil record<br />

Scaphopods probably evolved from a tiny, semi-infaunal helcionellid ancestor<br />

(via conocardioid rostroconches)<br />

<strong>Mollusca</strong><br />

Pinnocaris (Ordovician)<br />

not a scaphopod!


Aplacophora (shell less, vermiform molluscs)<br />

No shell = not well known from fossils<br />

Two groups, possibly not closely related<br />

Solenogastres<br />

Caudofoveata


Helcionellida<br />

(Cambrian-Ordovician)<br />

Rostroconchia<br />

(Cambrian-Permian)<br />

<strong>Mollusca</strong><br />

Phylum <strong>Mollusca</strong><br />

At least 4 extinct Classes<br />

Stenothecoida<br />

(Cambrian)<br />

Hyolitha<br />

Cambrian-Permian)


Helcionellida<br />

laterally compressed coiled shell<br />

typically 1mm to 2 cm long<br />

typically bilateral symmetrical<br />

coiling endogastric<br />

some develop a snorkle<br />

resemble gastropods, but are considered to be untorted<br />

first molluscs to develop a mineralized shell<br />

earliest Cambrian to Early Ordovician<br />

<strong>Mollusca</strong>


Rostrochonchia<br />

single, pseudobivalved shell which enclosed the mantle and muscular foot<br />

anterior, probably downwards-orientated, part of shell has a gape<br />

from which the foot could probably emerge<br />

probably sedentary semi-infaunal lifestyle<br />

no functional hinge, shell layers are continuous across the dorsal margin<br />

and some or all of the shell layers are continuous across the ventral margin (pegma)<br />

posterior of the shell is usually elongated into a flattened tube called the rostrum<br />

endo- or exogastric, or both<br />

Early Cambrian to Late Permian<br />

<strong>Mollusca</strong><br />

gape<br />

anterior<br />

rostrum<br />

posterior


Stenothecoida<br />

Bivalved mollusks with two non-equal,<br />

assymmetrical shells<br />

No articulation<br />

Only found in the Cambrian<br />

Reef environments<br />

Epibenthic filter feeders<br />

Probably not closely related to proper Bivalves


Hyolitha<br />

Probable molluscs<br />

Early Cambrian to Permian<br />

Most common in the Cambrian<br />

One deep cone-shaped shell (conch)<br />

One flat lid (operculum)<br />

Sometimes two curved rods (helens)<br />

Circular, triangular or rectangular<br />

in cross-section<br />

Two Orders:<br />

Hyolithida<br />

Triangular cross-section<br />

Have helens<br />

Lived on the sediment surface<br />

Probably filter feeders<br />

Orthothecida<br />

Circular or rectangular cross-section<br />

No helens<br />

Burried in the sediment<br />

Found with sediment filled gut<br />

Possibly related to siphunculans, not molluscs


origins<br />

<strong>Mollusca</strong><br />

<strong>Mollusca</strong>


<strong>Mollusca</strong><br />

Protostomes<br />

Part of the Lophotrochozoan<br />

branch among protostomes<br />

(sometimes called Spiralia)


What is a mollusc?<br />

Fundamental organization :<br />

- shell secreted by a layer of tissue called the mantle<br />

- mouth and anus at opposite end<br />

- mantle cavity bears gills<br />

- above mantle cavity is the visceral mass<br />

with gut, nervous, circulatory and muscular system<br />

- muscular foot facilitates movement<br />

- shell is of calcium carbonate (calcite or aragonite)<br />

- Shell is external<br />

- grow by accretion (calcium carbonate is added to the edge of the shell by the mantle)<br />

- marine<br />

<strong>Mollusca</strong><br />

Hypothetical ancestral<br />

mollusc


What’s the problem?


What’s the problem?<br />

D C B A


What’s the problem?<br />

D C B A<br />

The HAM:<br />

-A conceptual animal<br />

-Has ALL the important<br />

characters of modern<br />

molluscs<br />

-All molluscs derived from<br />

HAM independently<br />

Last common ancestor:<br />

-A real, living animal<br />

-Would NOT have all<br />

charatcers of modern<br />

molluscs<br />

-Characters and groups<br />

were acquired by steps


<strong>Mollusca</strong>


Precambrian<br />

<strong>Mollusca</strong><br />

<strong>Mollusca</strong>


Ediacaran Fauna<br />

First macroscopic ’animal’ fossils<br />

Most are difficult to place in modern<br />

groups<br />

Sponge- or Cnidarian-grade animals?<br />

Something completely different?


Ediacaran Substrate<br />

Very stable soft sediment<br />

No, or almost no burrowing activity<br />

Bacterial films covering the surface<br />

Led to enhanced preservation<br />

And a fantastic food-sourse for the<br />

first vagrant animals


Kimberella<br />

Impressions in fine sandstone<br />

Possible foot, mantle and ’soft’ shell<br />

White Sea region of Russia<br />

Associated with traces of mobility and/or<br />

feeding with a scraping radula<br />

One of the oldest convincing Metazoans<br />

But is it a mollusc?


Typical features: Radula<br />

Most molluscs have a radula (rasping<br />

tongue)<br />

The radula is ribbon-like and bears many<br />

small teeth arranged in rows<br />

Found in at least some representatives of<br />

all molluscan classes except Bivalvia<br />

Allowed early molluscs to graze on bacterial<br />

films on soft sediment?<br />

Now specialised to allow herbivory,<br />

detrivory and carniverous diets<br />

<strong>Mollusca</strong>


Cambrian<br />

<strong>Mollusca</strong><br />

<strong>Mollusca</strong>


Helcionellida<br />

laterally compressed coiled shell<br />

typically 1mm to 2 cm long<br />

typically bilateral symmetrical<br />

coiling endogastric<br />

some develop a snorkle<br />

resemble gastropods, but are considered to be untorted<br />

first molluscs to develop a mineralized shell<br />

earliest Cambrian to Early Ordovician<br />

<strong>Mollusca</strong>


More problems<br />

<strong>Mollusca</strong><br />

<strong>Mollusca</strong>


But what about the phylogeny?<br />

Molecular phylogeny suggest that Aplacophorans are the basal (most primitive) molluscs<br />

How does that fit the fossil record?


Aplacophora (shell less, vermiform molluscs)<br />

No shell = not well known from fossils<br />

Two groups, possibly not closely related<br />

Solenogastres<br />

Caudofoveata


Aplacophora (solenogastres)<br />

No shell = not well known from fossils<br />

Have a multitude of small calcareous spicules<br />

Narrow, ventral pedal groove = reduced foot<br />

Lack gills<br />

Feed on cnidarians and hydrozoans<br />

Hermaphrodites<br />

250 species


Aplacophora (Caudofoveata)<br />

No shell = not well known from fossils<br />

Have a multitude of small calcareous spicules<br />

No remains of foot<br />

Have gills at posterior end<br />

Have separate sexes<br />

Live buried in sediment, feed on microbiota (foraminifers etc.)<br />

250 species


Acaenoplax<br />

Possible caudofoveate<br />

from the Silurian<br />

Preserved as “ghosts” in<br />

volcanic ash<br />

Calcareous bristles<br />

6 shells + many small<br />

plates<br />

Has posterior gills<br />

Acaenoplax (Silurian)


Back to the Cambrian<br />

Small shelly fossils = little bits of the<br />

earliest skeltons<br />

Include helcionellid shells<br />

Include Hyolith conchs and opercula<br />

Include sponge spicules<br />

Include brachiopods<br />

Include problems:<br />

Tommotiids<br />

Chancelloriids<br />

Halkieriids<br />

= sclerites (scale-like “shells”<br />

that joined together to form a<br />

skeleton)


Chancelloriids<br />

Star shaped sclerites<br />

Hollow<br />

Form cylindrical scleritomes<br />

Similar to sponges<br />

Has been considered to be molluscs<br />

(If it looks like a sponge, it may be a<br />

sponge)


Halkieriids<br />

Blade-like or spine-like sclerites<br />

Hollow with narrow base<br />

Right- and left-hand specimens<br />

No evidence of accretionary growth


Halkieriids<br />

Articulated specimens in Greenland<br />

(Sirius Passet)<br />

about 2000 sclerites<br />

2 large accretionary shells<br />

<br />

Polyplacophoran connection?<br />

Halkieria evangelista


Odontogriphus<br />

Shell-less “worm”<br />

Burgess Shale<br />

central gut<br />

U-shaped excretionary<br />

organs suggest a mantle?<br />

Possible miniature<br />

radula with 6 teeth<br />

Scraper of bacterial<br />

films?<br />

Compare Kimberella!<br />

Odontogriphus


Odontogriphus


Kimberella<br />

Impressions in fine sandstone<br />

Possible foot, mantle and ’soft’ shell<br />

White Sea region of Russia<br />

Associated with traces of mobility and/or<br />

feeding with a scraping radula<br />

One of the oldest convincing Metazoans<br />

But is it a mollusc?


Halwaxiids<br />

Mollusc-like<br />

unmineralised sclerites/shells<br />

combines characteristics of<br />

Odontogriphus and Halkieria<br />

Intermediates?<br />

Wiwaxia Orthrozanclus


The early Evolution of the <strong>Mollusca</strong><br />

Slug‐like, creeping and grazing<br />

animals like Kimberella, Odontogriphus<br />

and Halkieria may have given rise to the<br />

<strong>Mollusca</strong><br />

Shell‐less forms and Polyplacophora<br />

diverged early (mollecular data only)<br />

Helcionellida represents the earliest<br />

Conchifera (molluscs with a single or<br />

bivalved shell)<br />

Different Helcionellids evolved into<br />

separate mollusc lineages?<br />

Conchifera<br />

Kimberella? Odontogriphus? Halkieria?<br />

Helcionellida?


Conchifera =<br />

-Bivalvia<br />

-Gastropoda<br />

-Scaphopoda<br />

-Cephalopoda<br />

Testaria =<br />

-Conchifera<br />

-Polyplacophora<br />

Possible test:<br />

Molecular phylogeny<br />

<strong>Mollusca</strong>


systematics minor groups<br />

<strong>Mollusca</strong>


Tryblidiida (”monoplacophorans” sensu stricto)<br />

simple cap-shaped shells<br />

never a diverse or abundant group<br />

well-represented in the fossil record from the late Cambrian to the Devonian<br />

first appeared in the Middle Cambrian<br />

until the discovery of Neopilina in 1952, considered to be extinct<br />

coiling exogastric<br />

distinguished by the fact that virtually all organ systems are found in multiples<br />

(gills, nephridia, muscles) pseudo-segmentation<br />

common ancestry with annelids and arthropods have been suggested<br />

serialization ≠ segmentation<br />

<strong>Mollusca</strong>


Scaphopoda (tusk shells)<br />

small group of mostly small, infaunal or semi-infaunal, marine mollusks<br />

shell typically a few centimeters in length<br />

(largest form found 30 cm in length)<br />

shell is a slender tapering and usually gently curved tube<br />

shell is open at both ends, the large end of the shell being anterior<br />

exterior has finely spaced growth lines and usually some<br />

type of longitudinal ornamentation or ribs.<br />

protrusible burrowing foot extends from the anterior end<br />

no gills, respiration by direct exchange with mantle tissue<br />

head is poorly-developed<br />

animal feeds on microscopic organisms and organic detritus.<br />

numerous tentacles (called captacula) and radula<br />

Scaphopoda first appear in the Ordovician or the Devonian or even the early Carboniferous<br />

rare in fossil record<br />

Scaphopods probably evolved from a tiny, semi-infaunal helcionellid ancestor<br />

(via conocardioid rostroconches)<br />

<strong>Mollusca</strong><br />

Pinnocaris (Ordovician)<br />

not a scaphopod!


Rostrochonchia<br />

single, pseudobivalved shell which enclosed the mantle and muscular foot<br />

anterior, probably downwards-orientated, part of shell has a gape<br />

from which the foot could probably emerge<br />

probably sedentary semi-infaunal lifestyle<br />

no functional hinge, shell layers are continuous across the dorsal margin<br />

and some or all of the shell layers are continuous across the ventral margin (pegma)<br />

posterior of the shell is usually elongated into a flattened tube called the rostrum<br />

endo- or exogastric, or both<br />

Early Cambrian to Late Permian<br />

<strong>Mollusca</strong><br />

gape<br />

anterior<br />

rostrum<br />

posterior


<strong>Mollusca</strong>


Helcionellida<br />

endogastric<br />

<strong>Mollusca</strong><br />

torsion<br />

Gastropoda<br />

Rostroconchia<br />

endogastric /<br />

exogastric<br />

separation of the valves<br />

development of hinge<br />

x<br />

Scaphopoda<br />

endogastric (larval stage)<br />

exogastric (adult)<br />

Cephalopoda<br />

endogastric<br />

Bivalvia


Stenothecoida<br />

Bivalved molluscs with two non‐equal,<br />

assymmetrical shells<br />

No articulation<br />

Only found in the Cambrian<br />

Reef environments<br />

Epibenthic filter feeders<br />

Probably not closely related to proper Bivalves


Hyolitha<br />

Probable molluscs<br />

Early Cambrian to Permian<br />

Most common in the Cambrian<br />

One deep cone‐shaped shell (conch)<br />

One flat lid (operculum)<br />

Sometimes two curved rods (helens)<br />

Circular, triangular or rectangular<br />

in cross‐section<br />

Two Orders:<br />

Hyolithida<br />

Triangular cross‐section<br />

Have helens<br />

Lived on the sediment surface<br />

Probably filter feeders<br />

Orthothecida<br />

Circular or rectangular cross‐section<br />

No helens<br />

Burried in the sediment<br />

Found with sediment filled gut<br />

Possibly related to siphunculans, not molluscs


Hyolithid (Parkula, Microcornus)


Orthothecid (Conotheca)


Ortothecid (Cupitheca)


Hyoliths in stomach of<br />

Ottoia

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