Mollusca
Mollusca Mollusca
mollusks Mollusca blötdjur molluscs
- Page 2 and 3: Mollusca Mollusca One of the larges
- Page 4 and 5: What is a mollusc? Fundamental orga
- Page 6 and 7: Typical features: Shell complex st
- Page 8 and 9: Typical features: Foot Muscular st
- Page 10: Gastropoda mollusks with a head an
- Page 14 and 15: Tryblidiida (”monoplacophorans”
- Page 17: Cephalopods most highly evolved mo
- Page 20 and 21: Aplacophora (shell less, vermiform
- Page 22 and 23: Helcionellida laterally compressed
- Page 24 and 25: Stenothecoida Bivalved mollusks wi
- Page 26 and 27: origins Mollusca Mollusca
- Page 29: What is a mollusc? Fundamental orga
- Page 32 and 33: What’s the problem? D C B A
- Page 35 and 36: Mollusca
- Page 37 and 38: Ediacaran Fauna First macroscopic
- Page 39: Kimberella Impressions in fine san
- Page 42: Cambrian Mollusca Mollusca
- Page 50 and 51: More problems Mollusca Mollusca
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