lab/lecture 3: first reefs Flashcards

(14 cards)

1
Q

What are stromatolites?

A

Laminated organo-sedimentary structures formed by trapping, binding, or precipitation of minerals by microorganisms.

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2
Q

Where do stromatolites grow today?

A

Intertidal to supratidal zones (e.g., Hamelin Pool, Shark Bay, Australia).

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3
Q

Describe stromatolite fossils.

A

Finely laminated micrite with replaced organic seams, porous septa or sparite cement; often form cabbage-shaped heads.

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4
Q

Describe the body plan of a sponge.

A

Porous skeleton with ostia (inhalant pores), spongocoel (inner cavity), and osculum (exhalant opening), reinforced by spicules.

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5
Q

How do sponges feed?

A

They are suspension feeders; water is pumped through ostia by choanocytes with flagella, filtering food.

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6
Q

What are the main cell types in sponges?

A

Pinacocytes (outer surface)

Choanocytes (flagellated, line canals, gather food)

Archaeocytes (amoeboid, digest, transport, turn into sex cells)

Sclerocytes/spongocytes (secrete skeleton)

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7
Q

Describe sponge fossils.

A

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).

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8
Q

Describe (class) Hexactinellida fossils.

A

Siliceous skeleton with six-rayed spicules forming cubic symmetry; reef-building forms like Hydnoceras.

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9
Q

Describe (class) Calcarea fossils.

A

Calcareous spicules; examples include star-shaped spicules in Astraeospongia and coiled forms like Girtyocoelia in Permian reefs.

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10
Q

Describe (class) Demospongiae fossils.

A

Spongin skeleton or siliceous spicules (never 90°); massive globular forms like Astylospongia, boring traces (Cliona → Entobia).

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11
Q

Describe (class) Stromatoporoidea fossils.

A

Laminated calcareous skeleton, horizontal laminae, vertical pillars, surface bumps called mammelons with astrorhizae; important Silurian–Devonian reef builders.

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12
Q

Describe (class) Archaeocyatha fossils.

A

Cone-shaped, double-walled skeleton with septa and intervallum; sometimes tabulae or dissepiments; dominant Early–Middle Cambrian reefs.

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13
Q

Where are modern sponges found?

A

Shallow marine (80%) and deep-sea habitats (>500 m).

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14
Q

Why are sponges important in paleobiology?

A

Major reef-builders; fossil record includes demosponge reefs (Ordovician), stromatoporoids (Silurian–Devonian), and hexactinellids (post-Devonian).

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