1. The Marine Habitat Ecosystems and Adaptations -Biological Oceanography – Mr. Hill – CHS 2015-2016

2. The diversity of marine life The ocean is home to a wide variety of organisms Marine organisms range from microscopic bacteria and algae to the largest animal in the world (blue whale) Number of known marine species: 250,000

3. Classification of living things Organisms can be classified into one of three domains of life: Archaea Bacteria Eukarya Figure 12-1

4. Classification of living things

5. Taxonomic classification includes the following increasingly specific groupings: Domain Kingdom Phylum Class Order Family Genus Species

7. Taxonomic classification of selected organisms CategoryHumanKiller whaleGiant kelp KingdomAnimalia Protista PhylumChordata Phaeophyta Subphylum Vertebrata ClassMammalia Phaeophycae OrderPrimatesCetaceaLaminariales FamilyHominidaeDelphinidaeLessoniaceae GenusHomoOrcinusMacrocystis Speciessapiensorcapyrifera

11. Distribution of Species on Earth The land has more species because it has greater environmental variability than the ocean Most ocean species are benthic because of greater environmental variability compared to pelagic environments Figure 12-6

12. Oceanic Biodiversity… Simplified Single Cell: Prokaryotes, Achaea and Protists Marine Plants and Algae Invertebrate Animals Vertebrate Animals

13. Divisions of the marine environment Main divisions: Pelagic (open sea) Benthic (sea bottom) Figure 12-19

15. Classification of marine organisms Marine organisms can be classified into one of three groups based on habitat and mobility: 1. Plankton (floaters) Phytoplankton (drifting plants and algae) Zooplankton (drifting animals) 2. Nekton (swimmers) 3. Benthos (bottom dwellers)

16. Plankton: Examples Figure 12-2 PhytoplanktonZooplankton

17. Nekton: Examples Figure 12-4

18. Benthos: Examples Figure 12-5

19. Life cycle of a squid – gray area… Squid experience benthic, planktonic, and nektonic stages Squid are considered meroplankton (opposite = holoplankton) Figure 12-3

20. Divisions of the marine environment Main divisions: Pelagic (open sea) Benthic (sea bottom) Figure 12-19

21. Marine Ecosystems Ecosystems are divided by zones based on water depth and shoreline features. The oceanic (PELAGIC) zone is the vast open part of the ocean where animals such as whales, sharks, and tuna live. The BENTHIC zone consists of substrates below water where many invertebrates live.

22. Marine Ecosystems continued… Other near-shore (NERITIC) zone can include estuaries, salt marshes, coral reefs, lagoons and mangrove swamps. The intertidal (LITTORAL) zone is the area between high and low tides. In the deep water, hydrothermal vents may occur where chemosynthetic sulfur bacteria form the base of the food web

27. Adaptations of organisms to the marine environment The marine environment presents many challenges to organisms because seawater: Is dense enough to support organisms Has high viscosity Experiences variations in temperature and salinity Contains variable amounts of dissolved gases Has high transparency Has a dramatic change of pressure with depth Marine organisms have various adaptations for the conditions of the marine environment

28. Need for physical support Condition: Seawater is dense enough to support marine organisms Adaptations: Many marine organisms lack rigid skeletons, appendages, or vast root systems Instead, they rely on buoyancy and friction to maintain their position within the water column

29. Seawater’s viscosity controlled by temperature Condition: Seawater’s viscosity (resistance to flow) is strongly affected by temperature Cold water has higher viscosity than warm water, so is more difficult to swim through Warm water has lower viscosity, so organisms tend to sink within the water column

30. Seawater’s viscosity controlled by temperature Adaptations: Many warm- water organisms have ornate appendages to say afloat Many cold-water organisms are streamlined to swim more easily Figure 12-7 Warm-water copepod Cold-water copepod

31. Seawater’s viscosity and adaptations of phytoplankton Condition: Phytoplankton must remain in sunlit surface waters Adaptations: Small size increases surface area to volume ratio Appendages increase frictional resistance Tiny droplet of low density oil increases buoyancy Figure 12-8

32. Variations in temperature Condition: Coastal water temperatures vary more than the open ocean or at depth Adaptations: Many coastal organisms can withstand a wide temperature range (are eurythermal) Most open ocean and deep-water organisms can withstand only a small temperature range (are stenothermal)

33. Variations in salinity Condition: Coastal environments experience greater salinity variation than the open ocean or at depth Adaptations: Many shallow-water coastal organisms can withstand a wide salinity range (are euryhaline) Most open ocean and deep-water organisms can withstand only a small change in salinity (are stenohaline)

34. Osmosis Condition: Osmosis is the movement of water molecules through a semipermeable membrane from higher to lower concentrations Osmosis removes water from hypotonic organisms Osmosis adds water to hypertonic organisms Figure 12-13

35. Osmosis Adaptations: Figure 12-14

36. Dissolved gases: Oxygen Condition: Marine animals need oxygen to survive Adaptations: Many marine animals use gills to extract dissolved oxygen from seawater Marine mammals must breathe air Figure 12-15

37. Abundance of dissolved oxygen and nutrients with depth Figure 12-20

38. Seawater’s high transparency Condition: Seawater has high transparency Adaptations: Transparency Camouflage Countershading Migration (DSL) Figure 12-17 Camouflage Countershading

39. The deep scattering layer (DSL) Organisms within the deep scattering layer undertake a daily migration to hide in deep, darker waters during daytime Figure 12B

40. Increase of pressure with depth Condition: Pressure increases rapidly with depth Adaptations: Most marine organisms lack large compressible air pockets inside their bodies Water-filled bodies exert the same amount of pressure as is pushing inward, so marine organisms do not feel the high pressure at depth