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OceanographyTRANSCRIPT
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2014 Pearson Education, Inc.
Animals of the Benthic Environment
Chapter 1 Clickers
Essentials of Oceanography Eleventh Edition
Alan P. Trujillo Harold V. Thurman
Chapter 15 Lecture
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Chapter Overview
Benthic communities include a variety of habitats.
Corals need specific environmental conditions.
Hydrothermal vents support diverse communities that rely on chemosynthesis.
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Distribution of Benthic Organisms
More than 98% of 250,000 known marine species live in or on ocean floor
Benthic organisms live mainly on continental shelves.
Their distribution is affected by surface ocean currents.
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Distribution of Benthic Organisms
Benthic biomass matches surface chlorophyll distribution.
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Communities on Rocky Shores
Epifauna Attached to substrate (e.g., marine algae) Move over sea floor (e.g., crabs, snails)
Moderate diversity of species Greatest animal diversity at tropical latitudes Greatest algae diversity at mid-latitudes
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Intertidal Zonation
Spray zone above spring tide zone
Intertidal zone High tide zone
relatively dry Middle tide zone
covered by all high tides/exposed by all low tides
Low tide zone usually wet
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Spray Zone
Supratidal zone Organisms
Avoid drying out Many animals have
shells Few species of
marine algae
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High Tide Zone
Animals have shells to avoid drying out.
Marine algaerock weeds with thick cell walls
Rock weeds colonize first
Sessile animals establish later
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Middle Tide Zone
More types of marine algae
Soft-bodied animals Barnacles and
mussels
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Middle Tide Zone Carnivorous snails
and starfish Sea anemones
Stinging nematocysts on tentacles poison prey
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Middle Tide Mussel Bed and Sea Star
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Middle Tide Zone
Hermit crabs Sea urchins
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Low Tide Zone
Abundant algae and surf grass
Many animals hidden by seaweed and sea grass
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Low Tide Zone
Various shore crabs Scavengers
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Physical Environment of Sediment-Covered Shores Sediment size related to wave and current
strength Course boulder beaches Sand beaches Salt marshes Mud flats
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Intertidal Zonation and Common Organisms
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Sandy Beach Organisms and Adaptations
Infauna burrowing animals No stable, fixed surface Burrowing provides more stable
environment Less risk of temperature extremes and
drying out
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Sandy Beach Organisms and Adaptations
Bivalve mollusks Soft body, hard shell Example: clams and
mussels Greatest number in
low tide regions Annelid worms
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Sandy Beach Organisms and Adaptations
Crustaceans Segmented body, hard
exoskeleton, paired jointed limbs
Sand crabs common
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Sandy Beach Organisms and Adaptations
Echinoderms Spiny skin Five tapered legs Example: starfish
and heart urchin
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Meiofauna Small, feed on bacteria Polychaetes, mollusks,
arthropods, nematodes
Sandy Beach Organisms and Adaptations
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Mud Flats
Eelgrass and turtle grass common
Bivalves and other mollusks
Fiddler crabs
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Shallow Offshore Ocean Floor Communities
Subtidal zone rocky bottom
Kelp Attaches to rocky
bottoms with strong holdfast
Stipes and blades supported by pneumatocysts
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Shallow Offshore Ocean Floor Communities
Kelp forests beds of giant brown bladder kelp and bull kelp Fast growing Highly productive
ecosystems Shelter for variety of
organisms
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Kelp Distribution
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Rocky Bottom Shallow Offshore Ocean Floor Communities Lobsters
Large, spiny antennae Live in water deeper
than 20 meters (65 feet)
Scavengers Also feed on live
animals
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Rocky Bottom Shallow Offshore Ocean Floor Communities Oysters
Sessile bivalve mollusks
Thick shell Food for sea stars,
fish, crabs, and snails Oyster beds empty
shells with living generation on top
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Coral Reefs
Reefs shallow water communities restricted to tropics
Polyps individual corals
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Coral Reef Distribution
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Conditions for Coral Reef Development
Warm seawater Sunlight for zooxanthellae symbiotic
photosynthetic microscopic algae in coral tissues
Strong waves or currents Clear seawater Normal salinity Hard substrate
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Symbiosis of Coral and Algae
Coral reefs made of algae, mollusks, foraminifers as well as corals
Hermatypic coral mutualistic relationship with algae Algae provide food Corals provide nutrients
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Coral Reefs
Other reef animals with symbiotic relationships
Mixotrophs derive part of nutrition from algae Include coral,
foraminifers, sponges, and mollusks
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Coral Reef Zonation
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Coral Reef Zonation
Many fish species inhabit shallow water near reef
Reef lagoon habitat for other animals
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Importance of Coral Reefs
Largest structures created by living organisms Great Barrier Reef, Australia, more than
2000 km (1250 miles) long Great diversity of species Important tourist locales Fisheries Reefs protect shorelines
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Coral Reefs and Nutrient Levels
Fishing, tourist collecting, and sediment influx due to shore development harm coral reefs.
Sewage discharge and agricultural fertilizers increase nutrients in reef waters. Hermatypic corals thrive at low nutrient levels Phytoplankton overwhelm at high nutrient levels Bioerosion of coral reef by algae-eating organisms
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Crown of Thorns Phenomenon
Sea star eats coral polyps
Outbreaks (greatly increased numbers) decimate reef
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Coral Bleaching and Other Diseases
Coral bleaching loss of color in corals Symbiotic zooxanthallae die, leave, or
become toxic Bleached coral lacks nourishment from algae
Linked to climate changes
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Bleached Corals
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Coral Bleaching
Some causes High surface water temperatures Elevated UV levels Decrease in sunlight-blocking atmospheric
particles Pollution Salinity changes Disease
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Other Diseases
Causes still under investigation Bacteria, viruses, fungi Human population stressors Increased nutrients and turbidity Environmental stress
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Coral Reefs in Decline
30% healthy today, 41% healthy in 2000 One third of corals high risk of extinction Humans greatest threat Other threats
Hurricanes Global warming Floods Tsunami
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Deep-Ocean Floor Communities
Less known about than shallower water communities Expensive to explore the deep Limited oxygen Robotic technology for exploration
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Deep Ocean Physical Environment
Bathal, abyssal, hadal zones Light absent below 1000 meters
(3300 feet) Temperature usually between 1.8C
(28.8F) and 3C (37F)
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Deep Ocean Physical Environment
High oxygen High pressure Abyssal storms
Affect bottom currents Created by warm and cold core eddies of
surface currents Can last weeks
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Deep Ocean Food Sources and Species Diversity
No primary productivity
Only 13% of euphotic food present
Special adaptations for detecting food
Species diversity equivalent to rain forest
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Deep-Sea Hydrothermal Vent Biocommunities
Discovery Alvin in 1977 Galapagos Rift in Pacific Ocean Water temperature
812C (4654F) Chimney vents, hot acidic water
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Deep-Sea Hydrothermal Vent Communities
Hydrothermal vent biocommunities Organisms previously
unknown to science Unusually large for
depth in ocean Black smokers
underwater chimney vents emit sulfides
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Locations of Hydrothermal Vent Communities
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Hydrothermal Vent Species
Giant tubeworms Giant clams Giant mussels Crabs Microbial mats Life supported by
chemosynthesis
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Hydrothermal Vent Species
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Hydrothermal Vent Species
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Chemosynthesis
Microscopic archaea thrive on hydrogen sulfide from vents
Manufacture sugar, carbon dioxide, and dissolved oxygen Base of hydrothermal
vent food chain
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Hydrothermal Vent Communities
Vents active for years or decades Animal species similar at widely separated vents Larvae drift from site to site Dead whale hypothesis
Large carcasses may be stepping stone for larvae
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Hydrothermal Vent Communities
First Atlantic vents with biocommunities discovered in 1985
First Indian Ocean vent found in 2000
Vents differ in chemical and geological characteristics
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Life Span of Hydrothermal Vents
Vents controlled by sporadic volcanic activity Vent may be active for only years to decades Organisms die when vent is inactive Increased volcanic activity can kill organisms
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Hydrothermal Vents and the Origins of Life
Life on Earth may have originated at hydrothermal vents. Uniform conditions Presence of archaea bacteria Microbes with genes identical to those found
in humans
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Low-Temperature Seep Biocommunities
Chemosynthetically support life
Hypersaline seeps High salinity Florida Escarpment
seeping water from limestone fractures
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Low-Temperature Seep Biocommunities
Gulf of Mexico seep from limestone escarpment fractures
Sulfide rich waters support diverse biocommunitiy
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Low-Temperature Seep Biocommunities Hydrocarbon seeps
Oil and gas seeps Hydrogen sulfide
and/or methane Hydrocarbon seep
biocommunities
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Low-Temperature Seep Biocommunities
Subduction zone seeps Juan de Fuca plate Folded sedimentary
rocks Methane
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Beneath the Sea Floor
A new frontier Deep biosphere
Exists within sea floor Microbes live in pore fluids Might represent much of Earths total
biomass
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End of CHAPTER 15 Animals of the Benthic Environment
Slide Number 1Chapter OverviewDistribution of Benthic OrganismsDistribution of Benthic OrganismsCommunities on Rocky ShoresIntertidal ZonationSpray Zone High Tide ZoneMiddle Tide ZoneMiddle Tide ZoneMiddle Tide Mussel Bed and Sea StarMiddle Tide ZoneLow Tide Zone Low Tide ZonePhysical Environment of Sediment-Covered ShoresIntertidal Zonation and Common OrganismsSandy Beach Organisms and AdaptationsSandy Beach Organisms and AdaptationsSandy Beach Organisms and AdaptationsSandy Beach Organisms and AdaptationsSandy Beach Organisms and AdaptationsMud FlatsShallow Offshore Ocean Floor CommunitiesShallow Offshore Ocean Floor CommunitiesKelp DistributionRocky Bottom Shallow Offshore Ocean Floor CommunitiesRocky Bottom Shallow Offshore Ocean Floor CommunitiesCoral ReefsCoral Reef DistributionConditions for Coral Reef DevelopmentSymbiosis of Coral and AlgaeCoral Reefs Coral Reef ZonationCoral Reef ZonationImportance of Coral ReefsCoral Reefs and Nutrient LevelsCrown of Thorns PhenomenonCoral Bleaching and Other DiseasesBleached CoralsCoral Bleaching Other DiseasesCoral Reefs in DeclineDeep-Ocean Floor CommunitiesDeep Ocean Physical EnvironmentDeep Ocean Physical EnvironmentDeep Ocean Food Sources and Species DiversityDeep-Sea Hydrothermal Vent BiocommunitiesDeep-Sea Hydrothermal Vent CommunitiesLocations of Hydrothermal Vent CommunitiesHydrothermal Vent SpeciesHydrothermal Vent SpeciesHydrothermal Vent SpeciesChemosynthesis Hydrothermal Vent CommunitiesHydrothermal Vent CommunitiesLife Span of Hydrothermal VentsHydrothermal Vents and the Origins of LifeLow-Temperature Seep BiocommunitiesLow-Temperature Seep BiocommunitiesLow-Temperature Seep BiocommunitiesLow-Temperature Seep BiocommunitiesBeneath the Sea FloorEnd of CHAPTER 15Animals of the Benthic Environment