lab/lecture 3: first reefs Flashcards
(14 cards)
What are stromatolites?
Laminated organo-sedimentary structures formed by trapping, binding, or precipitation of minerals by microorganisms.
Where do stromatolites grow today?
Intertidal to supratidal zones (e.g., Hamelin Pool, Shark Bay, Australia).
Describe stromatolite fossils.
Finely laminated micrite with replaced organic seams, porous septa or sparite cement; often form cabbage-shaped heads.
Describe the body plan of a sponge.
Porous skeleton with ostia (inhalant pores), spongocoel (inner cavity), and osculum (exhalant opening), reinforced by spicules.
How do sponges feed?
They are suspension feeders; water is pumped through ostia by choanocytes with flagella, filtering food.
What are the main cell types in sponges?
Pinacocytes (outer surface)
Choanocytes (flagellated, line canals, gather food)
Archaeocytes (amoeboid, digest, transport, turn into sex cells)
Sclerocytes/spongocytes (secrete skeleton)
Describe sponge fossils.
Typically preserved as spicules or fused skeletons; some like Astylospongia have massive globular bodies, others like Cliona bore holes in shells (trace fossils called Entobia).
Describe (class) Hexactinellida fossils.
Siliceous skeleton with six-rayed spicules forming cubic symmetry; reef-building forms like Hydnoceras.
Describe (class) Calcarea fossils.
Calcareous spicules; examples include star-shaped spicules in Astraeospongia and coiled forms like Girtyocoelia in Permian reefs.
Describe (class) Demospongiae fossils.
Spongin skeleton or siliceous spicules (never 90°); massive globular forms like Astylospongia, boring traces (Cliona → Entobia).
Describe (class) Stromatoporoidea fossils.
Laminated calcareous skeleton, horizontal laminae, vertical pillars, surface bumps called mammelons with astrorhizae; important Silurian–Devonian reef builders.
Describe (class) Archaeocyatha fossils.
Cone-shaped, double-walled skeleton with septa and intervallum; sometimes tabulae or dissepiments; dominant Early–Middle Cambrian reefs.
Where are modern sponges found?
Shallow marine (80%) and deep-sea habitats (>500 m).
Why are sponges important in paleobiology?
Major reef-builders; fossil record includes demosponge reefs (Ordovician), stromatoporoids (Silurian–Devonian), and hexactinellids (post-Devonian).