CHAPTER 15 Animals of the Benthic Environment Distribution

CHAPTER 15 Animals of the Benthic Environment

Distribution of benthic organisms Fig. 15. 1 n n n More benthos beneath areas of high primary productivity Mainly on continental shelves Affected by surface ocean currents

Benthic organisms on rocky shores n Epifauna Attached to substrate (e. g. , marine algae) n Move over seafloor (e. g. , crabs, snails) n n Moderate diversity of species Greatest animal diversity at tropical latitudes n Greatest algae diversity at mid-latitudes n

Intertidal zonation (rocky shore) Fig. 15. 2 a

Intertidal zonation (rocky shore) n Spray zone (supratidal) n Avoid drying out n Many animals have shells n Few species of marine algae Fig. 15. 2 b

Intertidal zonation (rocky shore) n High tide zone Avoid drying out so animals have shells n Marine algae—rock weeds with thick cell walls n n Middle tide zone More types of marine algae n Soft-bodied animals n n Low tide zone Abundant algae n Many animals hidden by sea weed and sea grass n Crabs abundant in all intertidal zones n

Benthic organisms on sedimentcovered shores n n Similar intertidal zones Less species diversity Greater number of organisms Mostly infauna n n Burrow into sediment Microbial communities

Benthic organisms on sedimentcovered shores n n n Coarse boulder beaches Sand beaches Salt marshes Mud flats Energy level along shore depends on Wave strength n Longshore current strength n n Fine-grained, flat-lying tidal flat more stable than high energy sandy beach

Intertidal zonation (sandy shore) Fig. 15. 8

Sandy beaches n n n Animals burrow Bivalve mollusks Annelid worms Crustaceans Echinoderms Meiofauna Fig. 15 -9

Mud flats n n n Eelgrass and turtle grass common Bivalves and other mollusks Fiddler crabs

Shallow ocean floor n n n Continental shelf Mainly sediment covered Kelp forest associated with rocky seafloor Also lobsters n Oysters n

Coral reefs n n n Most coral polyps live in large colonies Hard calcium carbonate structures Coral reefs limited to Warm (but not hot) seawater n Sunlight (for symbiotic algae) n Strong waves or currents n Clear seawater n Normal salinity n Hard substrate n

Reef-building corals Fig. 15 -17

Symbiosis of coral and algae n n Coral reefs made of algae, mollusks, foraminifers as well as corals Hermatypic coral mutualistic relationship with algae n Algae provide food n Corals provide nutrients

Coral reef zonation n Different types of corals at different depths Fig. 15. 19

Importance of coral reefs n Largest structures created by living organisms n n n Great Barrier Reef, Australia, more than 2000 km (1250 m) long Great diversity of species Important tourist locales Fisheries Reefs protect shorelines

Humans and coral reefs n n Activities such as fishing, tourist collecting, 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 n Phytoplankton overwhelm at high nutrient levels n Bioerosion of coral reef by algae-eating organisms n

Crown-of-thorns starfish and reefs n n Sea star eats coral polyps Outbreaks (greatly increased numbers) decimate reefs Fig. 15. 21

Benthic organisms on the deep seafloor n n n n Little known habitat Bathyal, abyssal, hadal zones Little to no sunlight About the same temperature About the same salinity Oxygen content relatively high Pressure can be enormous Bottom currents usually slow

Food sources in deep seafloor n n Most food from surface waters Low supply Fig. 15. 22

Deep-sea hydrothermal vent biocommunities n n n n First discovered 1977 Chemosynthesis Archaea use sea floor chemicals to make organic matter Tube worms Giant clams and mussels Crabs Microbial mats

Global hydrothermal vent fields Fig. 15. 24

Deep-sea hydrothermal vent biocommunities n n Vents active for years or decades Animals species similar at widely separated vents Larvae drift from site to site “Dead whale hypothesis” n Large carcasses may be stepping stone for larvae

Deep-sea hydrothermal vent biocommunities n n Life may have originated at hydrothermal vents Chemosynthesis also occurs at low temperature seeps n Hypersaline seeps n Hydrocarbon seeps n Subduction zone seeps

Beneath the sea floor Deep biosphere n Microbes live in pore fluids n Might represent much of Earth’s total biomass n

End of CHAPTER 15 Animals of the Benthic Environment