The Marine HabitatEcosystems and Adaptations

- Biological Oceanography –Mr. Hill – CHS 2015-2016

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

Classification of living things

Organisms can be classified into one of three domains of life:

Archaea

Bacteria

Eukarya Figure 12-1

Classification of living things

Classification of living thingsTaxonomic classification includes the following increasingly specific groupings:

DomainKingdomPhylum ClassOrderFamilyGenusSpecies

Taxonomic classification of selected organisms

Category Human Killer whale Giant kelp

Kingdom Animalia Animalia Protista

Phylum Chordata Chordata Phaeophyta

Subphylum Vertebrata Vertebrata

Class Mammalia Mammalia Phaeophycae

Order Primates Cetacea Laminariales

Family Hominidae Delphinidae Lessoniaceae

Genus Homo Orcinus Macrocystis

Species sapiens orca pyrifera

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

Oceanic Biodiversity…Simplified

Single Cell: Prokaryotes, Achaea and Protists

Marine Plants and Algae

Invertebrate Animals

Vertebrate Animals

Divisions of the marine environment

Main divisions:

Pelagic (open sea)

Benthic (sea bottom)

Figure 12-19

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)

Plankton: Examples

Figure 12-2

Phytoplankton Zooplankton

Nekton: Examples

Figure 12-4

Benthos: Examples

Figure 12-5

Life cycle of a squid – gray area…Squid experience benthic, planktonic, and nektonic stages

Squid are considered meroplankton

(opposite = holoplankton)

Figure 12-3

Divisions of the marine environment

Main divisions:

Pelagic (open sea)

Benthic (sea bottom)

Figure 12-19

Marine EcosystemsEcosystems 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.

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

Adaptations of organisms to the marine environment

The marine environment presents many challenges to organisms because seawater:

Is dense enough to support organismsHas high viscosityExperiences variations in temperature and salinityContains variable amounts of dissolved gasesHas high transparencyHas a dramatic change of pressure with depth

Marine organisms have various adaptations for the conditions of the marine environment

Need for physical support

Condition:Seawater is dense enough to support marine organisms

Adaptations:Many marine organisms lack rigid skeletons, appendages, or vast root systemsInstead, they rely on buoyancy and friction to maintain their position within the water column

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

Seawater’s viscosity controlled by temperature

Adaptations:Many warm-water organisms have ornate appendages to say afloatMany cold-water organisms are streamlined to swim more easily Figure 12-7

Warm-water copepod

Cold-water copepod

Seawater’s viscosity and adaptations of phytoplanktonCondition:

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

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)

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)

Osmosis

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

OsmosisAdaptations:

Figure 12-14

Dissolved gases: Oxygen

Condition:Marine animals need oxygen to survive

Adaptations:Many marine animals use gills to extract dissolved oxygen from seawaterMarine mammals must breathe air

Figure 12-15

Abundance of dissolved oxygen and nutrients with depth

Figure 12-20

Seawater’s high transparency

Condition:Seawater has high transparency

Adaptations:Transparency

Camouflage

Countershading

Migration (DSL)Figure 12-17

Camouflage

Countershading

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

Increase of pressure with depth

Condition:Pressure increases rapidly with depth

Adaptations:Most marine organisms lack large compressible air pockets inside their bodiesWater-filled bodies exert the same amount of pressure as is pushing inward, so marine organisms do not feel the high pressure at depth