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°C0 °C, Boiling point 100°C100 °C, Range 100°C100 °C
    • Ammonia: Melting point 78°C-78 °C, Boiling point 33°C-33 °C, Range 45°C45 °C
    • Methane: Melting point 182°C-182 °C, Boiling point 164°C-164 °C, Range 18°C18 °C
    • Ethane: Melting point 183°C-183 °C, Boiling point 89°C-89 °C, Range 94°C94 °C
  • Adhesion-cohesion-tension:
    • Emergent adaptation from physics enables transpiration.
    • Osmosis: H2OH_2O enters the root.
    • Polarity: H2OH_2O attracted to polar xylem walls, allowing it to creep up.
    • H-bonding: H2OH_2O 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°C4°C.
  • The density of water and ice varies with temperature.
  • Density is measured in gcm3\frac{g}{cm^3}.

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 (NaClNa++ClNaCl → Na^+ + Cl^−).
  • It also dissolves other minerals like carbonate (CO<em>32CO<em>3^{-2}) and silicate (SiO</em>42SiO</em>4^{-2}).

pH

  • pH is measured using a log scale.
  • pH affects physiology.
  • Ocean acidification is linked to increasing seawater CO2CO_2 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.
Osmoconformers
  • 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>2CO<em>2 and HCO</em>3HCO</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.