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Succession in Reefs

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Succession in Reefs. 4 stages : Pioneering or Stabilization a. Accumulation of skeletal debris b. Creation of a surface with some relief. Succession in Reefs. 2. Colonization a. Branching & encrusting organisms b. Low diversity. Succession in Reefs. Diversification - PowerPoint PPT Presentation

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Page 1: Succession in Reefs
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Succession in Reefs• 4 stages :

1. Pioneering or Stabilization

a. Accumulation of skeletal debris

b. Creation of a surface with some relief

Page 3: Succession in Reefs

Succession in Reefs

2. Colonization

a. Branching & encrusting organisms

b. Low diversity

Page 4: Succession in Reefs

Succession in Reefs

3. Diversification

a. Increased diversity of organisms

b. Takes the form of a massive structure

Page 5: Succession in Reefs

Succession in Reefs

4. Domination

a. “lamellar framestones”

b. Evidence of high water energy (rudstones)

c. Species diversity is reduced

Page 6: Succession in Reefs

Reef Evolution

Archaeocyathids (sponges?)

Lowly Pond Scum

Cambrian 500 my

12 bybp

Precambrian570 my

www.netrocks.netinyo.topcities.com

Stromatolites

Page 7: Succession in Reefs

Reef Evolution

12 bybp

Loss of “ecospace”

What happens witha sea-level fall?

Precambrian570 my

Back to “pond slime”

Page 8: Succession in Reefs

www.ammonite.free-online.co.uk

The Ordovician

Page 9: Succession in Reefs

AstrorhizaeMammelon

Stromatoporoids

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Ordovician Reefs(505-438 my)

Pratt & James (1982)

Stromatoporoid

Bryozoan

Peter Sholle

Page 11: Succession in Reefs

EarlySilurian

Extinction

Page 12: Succession in Reefs

Sea-level is back up

REEF DIVERSIFICATION

Page 13: Succession in Reefs

The Silurian World

Equator

Chris Scotese

OCEAN

20°

20°

Page 14: Succession in Reefs

Silurian Time430 mybp

Dott & Prothro (1994)Scotese (1997)

Reefs

Equator

Page 15: Succession in Reefs

New Life in the SilurianCorals Through Time

Wider = more abundant

0

200

400

600

Page 16: Succession in Reefs

Crinoids

Karla Parsons-Hubbard (Oberlin College)

Beloit College Collection

Page 17: Succession in Reefs

Opening up;Sea-level rise

40 million years later..

Shallow, clear water

Page 18: Succession in Reefs

Devonian

Stromatoporoids;Rugose Corals Crinoids

StromatolitesCambrian

Ordovician500 my

430 myStromatoporoids (sponges?)

Silurian

12 bybp

390 myStromatoporoids;Tabulate Corals Crinoids

Devonian

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Late Devonian

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280 myPermian

Sponges

Devonian

360 myCarboniferous

A time of poor reef development Major coal swamps

Reefs made of sponges…..

The Capitan Reef Complex

Just when things were looking good…..

Sea-Level DropsSea Level Back Up

Page 21: Succession in Reefs

Photo by Mark EberlePhoto by Peter Sholle

Photo by Peter Sholle

Page 22: Succession in Reefs

280 myPermian

Sponges

Reefs disappear!!!!!!!!245 my

Triassic

Extinction

• Sea level - no• Climate change - maybe• Ocean chemistry?

Why?

Page 23: Succession in Reefs

Scleractinean corals

280 myPermian

Sponges

245 myTriassic

A watershed event in reef history??

20 million yr gap

Page 24: Succession in Reefs

Watch here…

Chris Scotese

Page 25: Succession in Reefs

Cretaceous

Rudists

• The cup shaped form is back…..• but it’s a mollusk this time???

Triassic --> Jurassic

Scleractineans

140 my

A broadening tropics

An open pan-equatorial seaway

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No glaciers !

Open tropical seaway

Page 27: Succession in Reefs

Why mollusks and not corals???

• High temperatures

• “Greenhouse” climate much warmer than today

• Too warm for corals

Page 28: Succession in Reefs

Reefs Today

Cretaceous Reef Line

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Rudist Reefs

Photo by D. Schumann (from Woods, 1999)

Drawing by John Sibbick (in Woods, 1999)

They photosynthesized??the missing article……

Page 30: Succession in Reefs

Cretaceous Time

Images by Mary Parrish, NMNH

The End of theCretaceous

Irridium

ExtinctionDewey McLean

Page 31: Succession in Reefs

Cretaceous

Rudists

65 myTertiary

Major extinction95% of species disappear

Page 32: Succession in Reefs

Return tosclractinean

corals

Reefs have stayed pretty much the same ever since

65 myTertiary

Rest of the Cenozoic

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Cambrian “Explosion”Mostly non-reef forms

Page 35: Succession in Reefs

Calcification

Jaws --> BioE

Increased Calcification

Page 36: Succession in Reefs

M

ore

Com

ple

xF

aste

r G

row

thNo O2

Increased grazing

Sea Level

“Party Crashers”

Environment