Reefs - Lecture 7 Flashcards

1
Q

What are organic reefs?

A

Calcareous deposits with a topographic relief created by sessile organisms. High fossilisation potential

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2
Q

How are organic reefs formed?

A

Formed from growth of corals and other organisms (e.g. algae, sponges) creating a framework for sediment to be trapped

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3
Q

What are the three main components of reef rocks?

A

Cement, Matrix and Skeletons

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4
Q

Name three types of reef.

A

Cement-supported reefs (early seafloor cementation between skeletons), Matrix-supported reefs (e.g. Cluster and Segement reefs) and skeleton-supported reefs (e.g. frame reefs)

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5
Q

What is special about an ahermatypic coral?

A

They lack photosymbiontic algae

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6
Q

Hermatypic corals have symbiotic algae, what is the algae called?

A

Dinoflagellates

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7
Q

What traits are characteristic of a basic coral body plan?

A

Skeletons always made of calcium carbonate and environmental conditions strongly influence morphology (ecophenotypy)

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8
Q

What are common features of corals living in both high energy environments and low energy environments?

A

High energy: large surface area, high polyp density and rapid regrowth following damage. Low energy would have small surface area with low polyp density due to limitations of light and nutrients

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9
Q

What were the key Palaeozoic reef formers?

A

Sponges, Bryozoans and ahermatypic corals

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10
Q

How do Modern and Palaeozoic reefs compare?

A

They contained different groups of corals and organisms, less bioerosion from fish in palaeozoic coral reefs, palaeozoic corals could not attach to hard substrate and lacked symbiotic algae

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11
Q

What are the two major polymorphs of calcium carbonate?

A

Calcite and Aragonite

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12
Q

Mg/Ca in the oceans is closely linked to ocean spreading rates. What is the Mg/Ca concentration at high and low spreading rates?

A

High spreading rates: lower Mg/Ca Lower spreading rates: Higher Mg/Ca

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