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Marine Biology Fall 2005 Oceans Bays Estuaries Tidal Salt Marshes Nekton – Swimmers Pelagic– Floaters – Carried by the currents and waves Benthic – Bottom dwellers Abiotic Factors( Marine environment) Salinity – Marine organisms sensitive to a range of salinity from 1. 018 -1.024 specific graavity. In terms of salt it is 33-37 ppt NaCl. Other key elements in sea water, Mg++, Ca++, Zn++, K+, Cu++, Fe++ or Fe+++ Organics rain in a snow from top to bottom Light Photic Zone – Critical – Photosynthetic cyanobacteria and algae live at the surface and the edges where they can utilize light Green algae lives near the surface because of the wavelength of blue and red light( particularly red) that are required for cholorophyll, the main photosynthetic pigment. Light(continued) Red and brown algaes can live in deeper water because the wave lengths of light that they use in the purple range are more energetic and can penetrate in the depths of the ocean This is the case for Kelp Forests Waves Organisms on the shore and on the surface have to have adaptations that permit survival under harsh and turbulent conditions. Storms carry pelagic organisms Organisms need a type of attachment to substrates – bottom and shore features Marine Biomes AP Biology 2005 Kelp Forests Biogeography • The larger forests extend to the Arctic and Antarctic circles for the kelp grows well in sub 20°C waters. Although they may reach the arctic circles, their dependence on photosynthesis restricts them to shallow, clear waters of about 15-40m because if any deeper sunlight would not reach. • Kelp Forests are found along the coasts of North and South America because of the nutrient-rich water swells from the seasonal winds. Kelp forests are also found along New Zealand, Australia , and ROLE PLAYERS Kelp Urchins Sea Otters The Food Cycle of The Kelp Forest Urchins enjoy a diet of kelp. Many molluscs and urchins live on and near the kelp. Sea lions swim through the kelp forest and thrive on these delightful treats. •A coral reef is an accumulation of dead corals and other organisms with a limestone skeleton. •It is an underwater biome shaped by limestone formations that resemble branching trees. Coral reefs range widely in area. They may vary from a few square yards to hundreds of square miles. Typically, they tend to grow faster in clear water. Coral reefs lie mainly in shallow tropical or subtropical seas. They’re confined to such shallow water because the corals on which the reefs rely contain small algae called zooxanthellae. These algae help to supply food to the coral and require light to survive. Also, the number of species of corals on a reef declines rapidly in deeper water. Coral reefs are generally found within 30°N and 30°S latitudes, and most can’t live in water cooler than 61-68ºF Located in the waters of: Pacific Ocean Southeast Asia (coastal waters) Indian Ocean Red Sea Brazil (tropical eastern coast) Caribbean Sea Florida and Bermuda Coast) Madagascar (Southeast African Although coral reefs do not develop in colder seas, certain corals live as far north as the Arctic Circle. Coral reefs are the home to an incredibly high diversity of organisms. They provide thriving ecosystems for numerous species of plants, fish, and other marine life. Coral reefs represent the most complex ecosystem found on Earth, which tens of thousands of living species inhabit. the “rainforest of the oceans”. There are vast numbers of colorful fish, reptiles, and invertebrates. mollusks, as well as sea urchins, jellyfish, oysters, clams, turtles, and sea anemones. Threats • Storms • Temperature increases in the ocean water Bleaching • Pollution • Man Conservation If coral reefs continue to be destroyed, in 20 years the living corals on many of the world's reefs will be dead and the ecosystems that depend on them will be severely damaged. Therefore it is extremely important to enforce proper reef management. Many governments and conservation organizations are working to preserve these important ecosystems. USGS is focusing on detailed mapping of reefs, developing monitoring techniques, studying reef geologic growth and development, and determining the effects of sedimentary and hydrologic processes and water quality on reefs. Mangrove swamps Mangrove Trees The radiating cable roots with their tangle of anchor roots provide support against the ocean's strong waves and tides Little nutritive roots grow up out from the main cable root and feed on the rich soil just below the mud's surface The third type of root collects oxygen for the plant. More facts Mangrove swamps protect the land from soil erosion and the effects of storms. They also act as a form of pollution control, naturally filtering out industrial and human waste. Mangrove swamps, like other wetlands, are important components of the water cycle, absorbing excess water flow during times of flooding. Mangrove swamps serve important functions: They provide food, nesting and nursery areas for many animals which include at least 220 fish species, 24 reptile and amphibian species, 18 mammal species and 181 bird species. The dead leaves and twigs in the water grow microorganisms that provide food for Biogeography of Mangroves Florida coast Central American coast Australia India Biota Birds – Nest in the branches/Boobies and the frigate birds Roots – Sponges,molluscs, crutaceans ( crabs and shrimp) Nursery for the ocean – baby fish Barracuda, rays, pipefish Abiotic factors Still ocean water Murky – filled with organics Shallow water Lessened effect of wind and waves Concerns Mangrove forests are lost when they are torn up, filled in and dug under for other purposes such as agriculture, aquaculture and other development activities. People often wrongly perceive Mangroves as unsightly and want them removed so as to enhance the environment. Mangroves then often become garbage dumps. Pollution adversely affects Mangrove Swamps. Pollution degrades the quality of the plantlife and the water in the swamp, which in turn adversely affects the insects and animasls that also live there. The roots of the mangroves can become easily clogged with man-made sediments and petroleum as well as from other pollution Grass Biomes Large seagrass meadows usually occur in the protected waters landward of coral reefs. Seagrasses are true flowering plants with the male and female flower capable of sexual reproduction ,although most of the reproduction is performed asexually via the rhizome system in the sediment. The two main seagrass species, the turtle grass (Thalassia testudinum) and the manatee grass (Syringodium filiforme), occur Seagrasses Turtle Grass Thalassia testudinum: Turtle Grass. Root-stalks are elongated and creeping; stems are short. Leaves ribbon-like or strap-like. Common on soft bottoms in shallow waters. Often encrusted with coralline algae. Manatees Sea Grass Meadow Biota Turtles Sea urchins Star fish Small snails Jelly fish Juveniles of many large fish( red snappers) Conchs Abiotic Roots of grasses stabilize sediment Helps to hold sediment in this area so that the water is clear near the reefs which are dependent upon the abolute clarity of the water Rocky Shore Biogeography Pacific Coast N. East Coast of N. America Scotland Norway S. America Zonation Splash Zone Intertidal Subtidal Rocky Shores Biota Splash-Chitons,snails, and limpets. Algaes Intertidal-Algaes, crabs,shrimp, snails,and small fish. Barnacles Subtidal – starfish, urchins, marine worms, crabs,and fish Sandy Shores and Beaches Zonation •High Tide - Wrack line •Intertidal •Subtidal Biogeography Carribean Islands Mexico Southeastern United States Mediterranean Zonations The intertidal zone is the area exposed between high and low tides. In the intertidal zone, part of the day is spent in open air and the rest of the day is spent covered in ocean water. High tide brings with it nutrients and food. When it goes out, the tide takes with it waste products and disperses eggs and larvae. Because of the shifting sands, organisms living in the intertidal zone on a beach have adapted to these changing conditions. Without the cover of water, many animals simply shut down during low tide. Some of the animals spend most of their life buried under the sand. Others burrow into the sand when the tide is low or when the crashing waves hit the shore. Some of the animals feed on materials that washes ashore. Others filter food from the water. Still others feed on tiny algae and bacteria among the sand grains. Abiotic Waves High and Low tides – 2X a day – require protection from heat( sun) and dessication Turbulence of the water Biota Intertidal Sand crabs, calico crabs,hermitcrabs,coquinas,s mall fish like silver sides,flounder, grass shrimp,and other molluscs Subtidal Flounder, blue crabs, starfish, sea cucumbers, clams,small fish Biota Sand dunes They represent flexible barriers, which absorb wave energy during storms by moving and adjusting their shape and position. They form a crucial natural resource as a unique habitat for rich and diverse communities of highly specialised plant and animal species. However, their proximity to the ocean has made them desirable sites for locating coastal real estate. Such alterations to the coastline, as well as beach mining and renourishment, dredging, and filling are of particular concern in coastal areas because they have considerable Sand dunes Sea weeds Tidal Salt Marshes Biogeography Salt marshes form on stable or emerging coastlines when sediment accumulates in sheltered intertidal areas in estuaries, behind spits, bars or islands, and in protected bays. Tidal Salt Marshes Commercial Fisheries - 70% of commercial fish depend upon salt marshes for all or part of their lives. Nursing, Habitat, and Breeding Grounds - 63 species of Narragansett Bay fish use salt marshes as nurseries, and many more fish and shellfish depend on them for living and breeding. Wading birds such as egrets and great blue herons feed in the productive salt marshes during the summer months. Migratory birds such as shorebirds and ducks use salt marshes as stop-over points while traveling between summer and winter habitats. Tidal Salt Marshes Flood, Storm and Shoreline Protection - Salt marshes shield and protect coastal areas from storms, and are important shoreline stabilizers due to their wave dampening effect. Established marsh grasses are also highly effective against erosion. Tidal Salt Marsh Clean and Filter Water - Salt marshes clean water by filtering sediments, nutrients, heavy metals, and other toxins from upland runoff. Grasses Biota Highly Productive Ecosystems - Salt marshes produce more basic food energy per acre than any other known ecosystem including tropical rainforests and freshwater wetlands. Commercial Fisheries - 70% of commercial fish depend upon salt marshes for all or part of their lives. Salt Marsh Grass System Threats Salt marshes are among the most productive ecosystems in the world The key plant of the salt marsh is cord grass, Spartina A river of grass swaying in the breeze where the land meets the water, salt marshes are among the most productive habitats found within the Indian River Lagoon. Because they exist in areas which man has steadily developed or altered over many years, they are also among the most threatened habitats. Hydrothermal Vents In 1977 colonies of animals were identified in areas of the ocean with volcanic activity and vents Geologists working in such an area discovered 5 foot long worms near the Galapagos Islands The basis of this biome is the bacteria that are able to produce energy by chemoautotrophy Hydrothermal Vents In many vent areas the super heated water rises quickly from the ocean bottom with so many minerals that it appears black. As it rises from the seafloor some of the minerals precipitate out and form a 'chimney' around the water vent. These chimneys may grow to over 40 feet high while venting the black mineral-rich heated water. The Origin of Vents Seawater, found in cracks in the ocean bottom, is heated by volcanic activity and it becomes less dense and rises. If this water has come into contact with newly solidified rock it will have leached many minerals from that new rock. Large vestimintiferan worms over six feet long are one of the most visible animals at the vents. These are tube worms, secreting a thick paper-like white tube along their body. The vestimintiferans do not have a mouth or gut instead they rely on mutualistic symbiotic bacteria living in their tissue to produce the 'cell food' needed to keep them alive. The discovery of the vent communities was the first time anyone had seen vestimintiferan worms - a new phylum. It is believed these worms are some of the fastest growing invertebrates known. Vent Biome Inhabitants Profundal The depths of the ocean No light in the depths High Pressure Low dissolved oxygen 2000 – 6000 m in depth 39oF Creatures of the Deep Bioluminescence Many of the organisms in the depths are capable of producing lightthis phenomenon is called bioluminescence Animals produce red, green, and blue light The spectrum of light Blue light . Most bioluminescence is blue in color Blue light of wave lengths is 470 nm. It transmits the furthest in the depths of the oceans Most organisms are sensitive to blue light they lack the visual pigments which can absorb longer (yellow, red) or shorter (indigo, ultraviolet) wavelengths. Benthopelagic These animals have high levels of TMAO TMAO enables marine organisms to retain hydration while living in salt water Live above the bottom of the ocean Giant Grenadier Fish Chilly Oceans Antarctica -2oC water in many places 100oC water from volcanic action Ice Violent storms Winter darkness Short summer Orcas Animals Antarctic fish – Antifreeze in the blood Antarctic fish have lived at between +2°C and -2°C for 5 million years (-2°C is the freezing point of sea water, below zero because of the salt). They are therefore the best cold adapted animals that there are on the planet now or ever. Adaptations to Cold