Aquatic Adaptations Study Notes 2
Organism Adaptations
- Organisms adapt to water, land, and changes in climate, life history, sex, and sociality.
- Populations exhibit structure, growth, and dynamics.
- Communities show species interactions, structure, succession, and biogeography.
- Ecosystems cycle energy and nutrients.
- The biosphere undergoes anthropogenic change and requires conservation.
Adaptations to Aquatic Environments
- Properties of water influence aquatic life.
- Water and salt balance are crucial for aquatic organisms.
- Light availability affects photosynthesis in aquatic environments.
- Bioluminescence is a significant adaptation in the deep sea.
Properties of Water
- Water is liquid over a wide temperature range:
- Water: Melting point 0°C, Boiling point 100°C, Range 100°C
- Ammonia: Melting point −78°C, Boiling point −33°C, Range 45°C
- Methane: Melting point −182°C, Boiling point −164°C, Range 18°C
- Ethane: Melting point −183°C, Boiling point −89°C, Range 94°C
- Adhesion-cohesion-tension:
- Emergent adaptation from physics enables transpiration.
- Osmosis: H2O enters the root.
- Polarity: H2O attracted to polar xylem walls, allowing it to creep up.
- H-bonding: H2O molecules attract each other, pulling each other up in xylem.
- Evaporation occurs out of leaves.
- Surface tension allows pond life to thrive on top of the water.
Density and Buoyancy
- Water has high density.
- Adaptations for buoyancy include:
- Floating at or near the surface.
- Maintaining position in the water column at a specific depth.
- Examples include: Water-dispersed seeds, macro- and microalgae (e.g., Sargassum spp.), swim bladders in ray-finned fishes.
Density and Temperature
- Maximum density of water occurs at 4°C.
- The density of water and ice varies with temperature.
- Density is measured in cm3g.
Life Under Sea Ice
- Various organisms thrive under sea ice, including ice algae, Arctic cod, jellyfish, detritus, sea stars, urchins, and bowhead whales.
- Antarctic krill (Euphausia superba) feed on ice algae.
Antarctic Ice Shelf Loss
- The collapse of the Larsen B ice shelf occurred in Jan-Mar 2002.
- This ice shelf had been stable for over 10,000 years.
Water as a Polar Solvent
- Water dissolves salt (NaCl→Na++Cl−).
- It also dissolves other minerals like carbonate (CO<em>3−2) and silicate (SiO</em>4−2).
pH
- pH is measured using a log scale.
- pH affects physiology.
- Ocean acidification is linked to increasing seawater CO2 levels and decreasing seawater pH.
- Ocean acidification can lead to decalcification in plankton, coralline algae, reef corals, and mollusks.
- Buffering systems, such as bicarbonate and carbonate, are important in maintaining pH.
Water and Salt Balance
- Aquatic animals are either osmoconformers or osmoregulators.
- Marine invertebrates are typically osmoconformers.
Osmoregulators
- Marine ray-finned fishes are osmoregulators.
- Osmoregulation differs in freshwater vs. saltwater teleosts.
- Cells isolate solutes but allow water to pass through osmosis.
- Water movement is from areas of high concentration to low concentration.
- Marine teleosts are hypoosmotic, excreting salt and conserving water.
- Freshwater teleosts are hyperosmotic.
- Mangroves exhibit adaptations for water and salt balance, including salt excretion, tolerance to high sugar concentrations, salt exclusion, and salt storage.
Light and Photosynthesis
- Light penetration varies in marine waters, with less penetration in coastal waters.
- Photosynthesis action spectra differ among marine algae, such as Ulva (shallow) and Porphyra (deep benthic).
- Gas exchange is difficult underwater due to low solubility and slow diffusion.
- Seagrasses utilize both CO<em>2 and HCO</em>3− for photosynthesis.
- They transport oxygen via air tubes for root respiration.
Bioluminescence
- Bioluminescence is common in deep-sea organisms.
- Examples include anglerfish, firefly squid, lanternfish, and certain shrimp species.
- It is hypothesized that 76% of deep-sea animal species use bioluminescence.
- In summary, adaptations to aquatic environments include properties of water, water and salt balance, light and photosynthesis, and bioluminescence.
Marine Ray-Finned Fish Osmoregulation
- Marine ray-finned fishes are hypoosmotic compared to their environment, excreting salt and conserving water.
Phylogeny of Ray-Finned Fishes
- The MRCA (most recent common ancestor) of extant ray-finned fishes likely lived in freshwater.
- The transition to freshwater occurred after the first ray-finned fishes, which were marine.
- Following adaptation to freshwater, some descendants returned to the sea and became hypoosmotic.
- A mass extinction event in the ocean affected ancestral marine ray-finned fishes.
Mangrove Adaptations
- Red mangroves and black mangroves employ different strategies for water and salt balance.
- Red mangroves exclude salt and tolerate high sugar concentrations in their roots.
- Black mangroves excrete salt from their leaves.
- Some mangroves are osmoregulators, while others are not.