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Marine Ecosystems Chapter 7.2. Natural Capital Ecological Services Climate moderation CO 2 absorption Nutrient cycling Waste treatment and dilution Reduced.

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Presentation on theme: "Marine Ecosystems Chapter 7.2. Natural Capital Ecological Services Climate moderation CO 2 absorption Nutrient cycling Waste treatment and dilution Reduced."— Presentation transcript:

1 Marine Ecosystems Chapter 7.2

2 Natural Capital Ecological Services Climate moderation CO 2 absorption Nutrient cycling Waste treatment and dilution Reduced storm impact (mangrove, barrier islands, coastal wetlands) Habitats and nursery areas for marine and terrestrial species Genetic resources and biodiversity Scientific information Economic Services Food Animal and pet feed (fish meal) Pharmaceuticals Harbors and transportation routes Coastal habitats for humans Recreation Employment Offshore oil and natural gas Minerals Building materials © 2004 Brooks/Cole – Thomson Learning Marine Ecosystems

3 Categories of marine ecosystems 1. Coastal ecosystems – includes: estuaries, salt marshes, mangrove swamps, rocky and sandy shores 2. Coral reefs 3. Oceans

4 Estuaries Definition: an area in which fresh water from a river mixes with salt water from the ocean; a transition area from the land to the ocean Other names: bay, sound, lagoon, harbor, bayou River bringing freshwater to the sea The Ocean Area where fresh and salt water mix

5 Characteristics of Estuaries Water is brackish: a mixture of freshwater and saltwater There is a gradient (gradual change) in the salinity  near the input from the river: 0-5 ppt  in the middle of the estuary: 5-25ppt  at the ocean: >25 ppt (ppt = parts per thousand, a unit for salinity)

6 Mobile Bay – one of the largest estuaries in the U.S. Tensaw River Mobile River Dauphin Island Gulf of Mexico Mobile Bay What is the approximate salinity in ppt for these locations?

7 Characteristics of Estuaries Very nutrient rich ecosystems  leads to high productivity and high biodiversity Fast-moving rivers and waves carry nutrient-rich particles Sediment settles out in the estuary when the water slows down It accumulates on the bottom (benthic zone) Great place for plants to grow!

8 Important functions of estuaries: for living things 1. habitat 2. nursery 3. fisheries 4. recreation

9 Important functions of estuaries: related to water 5. Water purification 6. Flood control (from upstream) 7. Buffer land from hurricanes, absorb storm surge Loss of coastal wetlands in Louisiana made Hurricane Katrina’s effect worse than it would have been

10 Estuary plants Plants must be adapted to salty habitat cordgrass eelgrass glasswort – a succulent

11 Estuary plants Narrow leaved cattail

12 Estuary animals Huge variety! Including… horseshoe crabs Mosquito…

13 Estuary animals oysters lobster

14 Estuary animals Flounder Striped Bass

15 Estuary animals Many, many birds! Common tern Great White Egret

16 Estuary animals Manatee

17 Sea lions at Pier 39 in San Francisco Bay

18 Salt Marshes Definition: a low area that is subject to regular, but gentle, tides Dominated by grasses (Remember, marshes do not have trees or shrubs) Location: Gulf of Mexico and Atlantic coast Texas salt marsh

19 Alabama salt marsh Dauphin Island, AL

20 Mangrove Swamps Definition: coastal wetlands located in tropical and subtropical zones; characterized by salt-tolerant trees and shrubs, such as mangrove trees

21 Mangroves Different species – include red mangrove… with tangled roots that reach above the water line, form an important habitat for many animals

22 Rocky shores Also called rocky intertidal zone – many places to live in this habitat, means high biodiversity Organisms must be adapted to wave action, changing tide levels Some examples of rocky shores organisms are at the Monterey Bay Aquarium website below: http://www.montereybayaq uarium.org/efc/efc_rocky /rocky_cam.asp# http://www.montereybayaq uarium.org/efc/efc_rocky /rocky_cam.asp#

23 Rocky Shores At low tides, there are often tide pools left behind where you can see starfish, anemones, crabs, octopus

24 Rocky Shore Beach Sea starHermit crabShore crab Nudibranch Monterey flatworm KelpSea lettuce Barnacles Sea urchin Anemone Low tide Mussel Periwinkle High tide Sculpin

25 Sandy shores “The Beach!”

26 Sandy Shores Not as much biodiversity as rocky shores – Why? 1.not much habitat diversity 2.sand dries out at low tide some small things can live in the sand, food for shorebirds

27 Barrier Islands Narrow islands made of sand that provide a buffer for the mainland from the sea Constantly shifting, especially with storms Ex: Dauphin Island, Alabama

28 Barrier beach Silversides Blue crab Low tide Dwarf olive Clam Beach flea Tiger beetle High tide Ghost shrimp Mole shrimp Sandpiper Peanut worm White sand macoma Sand dollarMoon snail

29 OceanBeach Intensive recreation, no building Primary Dune No direct passage or building Trough Limited recreation and walkways Secondary Dune No direct passage or building Bay or Lagoon Intensive recreation Back Dune Most suitable for development Grasses or shrubsTaller shrubs Taller shrubs and trees Bay shore No filling Barrier Islands Think about ecological succession as you move away from the ocean. What is the “disturbance” in this ecosystem?

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31 Notice the beach erosion. Barrier islands are constantly changing.

32 This picture was taken from Dauphin Island, AL. Notice the offshore platforms for drilling natural gas in the Gulf of Mexico. Interestingly, Florida does not allow offshore drilling. Why?

33 Coral Reefs  Structures in the shallow oceans that are built by animals called corals; serve a habitat for many diverse organisms  Require two things: warm temperatures and sunlight  Found between 30°N and 30°S of the equator

34 Coral Reefs Corals are animals that belong to the phylum Cnidaria, the stinging-celled animals such as jellyfish and hydra Coral polyps resemble small sea anemones with tentacles that can sting and paralyze prey

35 Coral Reefs They build limestone houses around themselves and stay in one spot (sessile) Over many generations, the limestone builds up to form a large reef (takes a long time) Elkhorn coral Polyps in limestone skeleton

36 Coral Reefs Corals live in a symbiotic relationship with algae called ; the algae are photosynthetic and give the coral food and oxygen; the algae get carbon dioxide and nutrients from the nitrogenous wastes of the coral Corals live in a symbiotic relationship with algae called zooxanthellae; the algae are photosynthetic and give the coral food and oxygen; the algae get carbon dioxide and nutrients from the nitrogenous wastes of the coral

37 Coral Reefs There are many different kinds of corals: Soft corals Hard corals

38 Coral Reefs Growing on the reef with the corals are other animals, such as sponges, worms, shrimps, crabs, mollusks Living in and around the reef are fish, sea turtles, sea snakes, marine mammals

39 Coral Reef Destruction 1. Coral bleaching – when temperatures go above normal, the zooxanthellae (algae) in the coral can be rejected, the coral turns a whitish color and dies Natural causes: El Nino Manmade causes: Global warming

40 Coral Reef Destruction 2. Physical damage Ships, anchors, tourist divers Dynamite fishing - reefs are damaged by physical destruction that may occur when people collect fish

41 Coral Reef Destruction 3.Land development and pollution – loss of mangrove forests means more nutrients and sediments flow out to the sea; coral may die from sediment or algal blooms 4.Fish and coral trade 5.Increased exposure to UV due to ozone depletion

42 Ocean: Deep and Wide Defining characteristics: light and depth of water Varying surface of ocean floor: continental shelf, slope, trenches (deepest is Mariana Trench at about 35,000 feet below sea level), plains, geologic features (hydrothermal vents, volcanoes, fault lines that produce earthquakes and tsunamis)

43 High tide Low tide Coastal Zone Estuarine Zone Continental shelf Open Sea Sea level Sun Euphotic Zone Bathyal Zone Abyssal Zone Depth in meters 0 50 100 200 Photosynthesis 500 1,000 1,500 2,000 3,000 4,000 5,000 10,000 Darkness Twilight © 2004 Brooks/Cole – Thomson Learning Euphotic zone – full sunlight, phytoplankton (the producers), zooplankton, nekton Bathyal zone – the twilight zone Abyssal zone – cold, dark, pressure high, specialized “weird” organisms live here Benthic zone – all along the ocean bottom, benthos are organisms that live on the bottom of the ocean, filter feeders, scavengers, decomposers

44 Deep ocean Characteristics: dark, cold, high pressure How can anything live there? What is the base of the food chain? Two ways: 1. marine snow – organic particles that settle down from above 2. hydrothermal vents - cracks in the earth that allow hot gases to escape, certain bacteria can make food in these conditions (chemosynthesis) Will see both of these in the Planet Earth video….

45 Biodiversity in marine ecosystems Why do coral reefs have more biodiversity than the open ocean or the deep ocean? More sunlight and more habitat support greater diversity of species

46 Marine Ecosystems Half of coastal wetlands lost to agriculture and urban development Over one-third of mangrove forests lost since 1980 to agriculture, development, and aquaculture shrimp farms About 10% of world’s beaches eroding because of coastal development and rising sea level Ocean bottom habitats degraded by dredging and trawler fishing boats Over 25% of coral reefs severely damaged and 11% have been destroyed Natural Capital Degradation


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