Climate

Climate influences three environmental conditions for the carbonate factory.

1. Rate of terrigenous clastic sediment input.

2. The amount and rate of evaporation/rainfall.

The evaportation and rainfall play a crucial role in keeping the water salinity in the exact range needed for optimal growth. Since most of the carbonate factories form in shallow water environments the evaporation to rainfall ratio is extremely important.

3. The storminess of the sea and it's cyclicity.

Typically high energy storms can cause damage to delicate factory organisms and errode sediment away. With a long period cyclicity the factory can restore itself but if major storm events happen rapidly it can quickly do more damage than the factories can overcome.

Index to carbonate shelf sediments below or to link back to USC website on sequence stratigraphy click here

Evolution Lag time Antecedent Topography
Biology Climatic Zone Siliclastic Influx
Temperature & Salinity Sea Level Clastic Input
Tectonism Platform Morphology Stratigraphic Succession
Water Depth & Turbidity Subsidence Lithofacies
Circulation Carbonate Growth Potential Eustatic Response

Proceed on to the carbonate platform question set.