The northern hemisphere tends to have higher plant biomass.
This is partly due to the majority of landmasses being located here.
Phytoplankton and zooplankton are also more abundant in temperate and coastal areas.
No math is required for the exam.
The format consists entirely of multiple-choice questions with no short answers.
Vertical profiles of phosphorus (phosphate) and nitrate demonstrate low levels at the surface due to uptake by phytoplankton.
As one moves away from the photic zone, residual nutrients are present since photosynthesis ceases.
Photosynthesis Equation:
Reactants: Solar energy, carbon dioxide (CO2), water (H2O).
Products: Glucose and oxygen.
Key gases in the ocean include nitrogen, oxygen, and carbon dioxide.
Carbon dioxide can dissolve in water, forming carbonic acid, which can break down into bicarbonate ions.
Excess CO2 may lead to ocean acidification, resulting in reduced carbonate ions available for shell-building organisms.
Current ocean pH is slightly above 8, but it is decreasing, which is a concern as it approaches neutrality (pH 7).
Particulate Organic Carbon (POC): Refers to larger organic particles.
Dissolved Organic Carbon: Refers to smaller, dissolved organic particles.
The photic zone (top 100 meters) is where most biological activity occurs.
Only about 5% of organic carbon makes it to the bottom as sediments.
Some organic carbon is utilized by deep-sea organisms.
Light absorption decreases with depth (attenuated).
Longer wavelengths, such as red, are absorbed first.
Color perception is predicated on the wavelengths that objects reflect (e.g., plants appear green because they reflect green light).
A notable demonstration of light attenuation can be observed through scuba diving with a color chart.
Osmotic pressure drives water movement from areas of high to low concentration.
Saltwater fish possess adaptations for high salinity, such as excreting salty urine.
Energy expenditures are greater for moving organisms; they either need to eat more or have efficient metabolisms.
Different feeding mechanisms include:
Filter Feeding: Organisms filter nutrients from water.
Deposit Feeding: Organisms consume sediments totaling organic matter.
Foraging: Directly hunting or searching for food.
Genus and Species Naming: Genus is capitalized and species is lowercase, both italicized.
Recent changes in taxonomy, e.g., stingrays reclassified from Dasyatis to Hypanus.
The three domains recognized are:
Bacteria
Archaea
Eukaryota
Within Eukaryota, classification progresses from kingdom to species.
Eukaryotes include kingdoms such as:
Animalia
Fungi
Protista
Plantae
Prokaryotes are single-celled and lack membrane-bound organelles.
Examples include:
Heterotrophic Bacteria: Require organic substances for energy.
Autotrophic Bacteria: Can produce their own food.
Important for the microbial loop—the cycling of nutrients in marine environments.
Algae Types:
Red Algae (Rhodophyta): Includes species like sea moss.
Brown Algae (Phaeophyta): Includes kelps, important for their size and habitat formation.
Green Algae (Chlorophyta): Includes chlorophyll a and b for photosynthesis.
Flowering Plants: Seagrasses are true grasses that create diverse ecosystems and stabilize shorelines.
Sponges (Porifera): Benthic, asymmetrical, and capable of filtering water for nutrients.
Cnidarians: Characterized by stinging cells (nematocysts) with classes such as hydrozoans and scyphozoans.
Ctenophores (Comb Jellies): Simple organisms that use cilia for locomotion and capturing prey.