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© 2014 Pearson Education, Inc. Animals of the Benthic Environment Essentials of Oceanography Eleventh Edition Alan P. Trujillo Harold V. Thurman Chapter 15 Lecture

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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

  • 2014 Pearson Education, Inc.

    Chapter Overview

    Benthic communities include a variety of habitats.

    Corals need specific environmental conditions.

    Hydrothermal vents support diverse communities that rely on chemosynthesis.

  • 2014 Pearson Education, Inc.

    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

  • 2014 Pearson Education, Inc.

    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