The continental shelf is an underwater landmass which extends from a continent, resulting in an area of relatively shallow water known as a shelf sea. Much of the shelves were exposed during glacial periods and interglacial periods
3. THE CONTINENTAL SHELVESTHE CONTINENTAL SHELVES
• Average width – 75 km, narrower in
areas with strong current;
• Average slope – 0o
07’;
• Average depth flattest portion– 60 m;
• Average depth where greatest change
of slope – 130 m;
• Hills of 20 m or more and depression of
20 m or more
7. SUBTIDAL ABIOTIC FACTORSSUBTIDAL ABIOTIC FACTORS
• rich in nutrients (brought in from river
discharges), i.e., sediment runoff)
Mississippi Delta Nile River Delta
8. SUBTIDAL ABIOTIC FACTORSSUBTIDAL ABIOTIC FACTORS
• Influenced by sedimentation processes
(especially shallow areas)
- lithogenic sediments (physical and chemical
weathering of rocks (turbidities, volcanic ash,
red clay))
- biogenic sediments (shells and skeletons of
marine organisms)
9. SUBTIDAL ORGANISMSSUBTIDAL ORGANISMS
• Plankton (suspended in water column)
• Nekton (able to swim against current)
Benthic (on/in bottom sediment)
• Demersal
• Epifauna
• Infauna
Pelagic
14. CHARACTERISTICS OF SOFT-
BOTTOM SUBTIDAL
COMMUNITIES
• Type of dominant substrate i.e. sand,
mud etc.
• Mainly infauna, some epifauna and
almost no sessile organisms
15. SOFT-BOTTOM SUBTIDAL
ORGANISMS
1. infauna
– Benthic organisms that bury themselves in the
sediment
2. epifauna
– Organisms that inhabit the surface of the
bottom sediment
No. of subtidal sp. > intertidal (more stable, no desiccation)
Distribution of organisms influenced by particle size (mud or sand)
19. Infauna:
• live within the sediment, mostly soft bottom;
• mostly clams and worms (polychaetes)
• burrow tubes for food scavenging and oxygen
supply
• Primary producers: algae, mostly benthic
diatoms and dinoflagellates
• cyanobacteria mats on mudflats
• mud more productive than sand
• macro- and meiobenthos, often detrivores,
living of deposits from seagrasses and
marshes
• birds important grazers
Soft-bottom subtidal communities
28. PRODUCERS
• Most important communities -
seaweeds
• Strong competition
• Amount of light influence distribution
of seaweeds
• Seaweeds found in these areas have
higher chlorophyll concentration
29. grazers
• Invertebrates that move slowly: sea urchin,
limpets, chitons, abalone
• Algal defense against predators
- By having food that are not tasty
- Fast regeneration
- Calcification (formation of calcium)
34. Muddy shores
• Deposition of silt by tide or river
Temperate: intertidal- mud flat communities
subtidal- muddy bottom or seagrass communities
Tropic: intertidal- mangroves
subtidal- muddy bottom or seagrass communities
Sandy shores
• Deposition of sand by wave action
Temperate: intertidal- beach communities
subtidal- muddy bottom or seagrass communities
Tropic: intertidal- beach communities
subtidal- sandy bottom or seagrass communities
Rocky shores
• Little deposition
Temperate: intertidal- barnacles, seaweeds, mussels
subtidal- kelp beds or forests
Tropic: intertidal- algae and corals
subtidal- coral reefs
Recap
35. Inquiry
1. What is the sublittoral zone?
2. What is meiofauna (infauna)?
3. How do organisms survive living in a
soft bottom community?
4. What food source are soft-bottom
communities are based on?
5. Why don’t we see anemones and sea
slugs in the high tide zone?
Editor's Notes
Notice the narrow shelf by Florida
Transform faults- fractures along which the lithosphere slides horizontally past one another
Lithogenous sediments are formed by the weathering process and are made up of small particles of weathered rocks and oceanic volcanoes. They are often formed together when metal and silicate ions bond. There are two types of lithogenous sediments; terrigenous and “red clay” and they are different because of the process behind their existences. For instance, terrigenous sediments are produced as a result of the weathering process of rocks above the water. These eroded particles are carried by the wind and other natural means to the oceans and are deposited at the bottom. Although it can be easily found in river beds, not much of this finds its way to the deep ocean. Red clay lithogenous sediment, on the other hand, is plentiful in the ocean. It is reddish-brown (hence the name) and is a combination of terrigenous material and volcanic ash. It is transported to the oceans by currents and wind and it settles in deep places along the ocean floor.
Biogenous sediments are formed from the insoluble remains of past life forms and parts such as bones and teeth. In many areas where the water is shallow, a majority of these sediments are the remains of shells or fragments from shelled sea creatures as well as corals. In the deep sea where there is no such a high concentration of these life forms, biogenous sediment is made from the microscopic shells that are deposited by tiny plants, animals, and plankton that live on the water’s surface and eventually make their way down to the ocean floor.
Lithogenous sediments are formed by the weathering process and are made up of small particles of weathered rocks and oceanic volcanoes. They are often formed together when metal and silicate ions bond. There are two types of lithogenous sediments; terrigenous and “red clay” and they are different because of the process behind their existences. For instance, terrigenous sediments are produced as a result of the weathering process of rocks above the water. These eroded particles are carried by the wind and other natural means to the oceans and are deposited at the bottom. Although it can be easily found in river beds, not much of this finds its way to the deep ocean. Red clay lithogenous sediment, on the other hand, is plentiful in the ocean. It is reddish-brown (hence the name) and is a combination of terrigenous material and volcanic ash. It is transported to the oceans by currents and wind and it settles in deep places along the ocean floor.
Biogenous sediments are formed from the insoluble remains of past life forms and parts such as bones and teeth. In many areas where the water is shallow, a majority of these sediments are the remains of shells or fragments from shelled sea creatures as well as corals. In the deep sea where there is no such a high concentration of these life forms, biogenous sediment is made from the microscopic shells that are deposited by tiny plants, animals, and plankton that live on the water’s surface and eventually make their way down to the ocean floor.
Muddy shoresMuddy shores develop on places where clay and silt (particles finer than sand) are deposited by river currents or by tidal action. In places where the velocity of the water is low enough the fine particles will sink to the bottom where bottom organisms will fixate them. In temperate regions this is the place of mud-flats with saltmarshes higher up the coast. In tropics these muddy shores are mostly covered by mangroves. If the visibility is high enough there is a chance that sea-grass communities occure in deeper water.