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Flashcards covering marine biology zones, ecological concepts like landscape and seascape ecology, nutrient cycles, and connectivity in marine environments.
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Marine Biological Zones
Categorized by their location relative to shorelines and the ocean bottom; influenced by temperature, light, water depth, bottom substrate, and interactions with other organisms.
Pittman, 2018
Estuaries
Where rivers flow into oceans,
characterized by varying salinity, tides, and the influx of terrestrial sediments and nutrients
highly productive
Pittman, 2018
Salt Marshes
Shallow coastal wetlands dominated by grasses and rushes,
known for high productivity due to terrestrial nutrient input and the presence of salinity gradients that lead to zonation of plant species;
provide food and protection for various animals.
Pittman, 2018
Mangrove Forests
Tropical coastal zones dominated by salt-tolerant, evergreen trees and shrubs whose roots trap sediments;
provide nutrients to marine ecosystems and habitat to many animals but are threatened by human development.
Pittman, 2018
Rocky Intertidal Zones
Stable substrates for organisms that must cope with wet and dry conditions and changing salinity as tides rise and fall
dynamic zones with dramatic conditions where organisms need to resist temperature and salinity changes.
Pittman, 2018
Coral Reefs
Restricted to warm, shallow water
corals form large colonies with algal partners in symbiotic mutualism, extracting calcium carbonate to build skeleton-like structures that form large reefs providing structure for ecosystems.
grow very slowly
Pittman, 2018
Kelp Beds/Forests
Found in temperate environments
consist of large brown algae with leaf-like fronds, stems, and holdfasts, supporting a diverse marine community.
Pittman, 2018
Pelagic Zone
Open ocean beyond the continental shelves,
divided into the photic zone (up to 200m, supports high densities of organisms) and deeper zones where energy is supplied by falling detritus;
characterized by organisms adapted to avoid sinking.
Pittman, 2018
Below photic zone
temperature drops and pressure increases
hard to live here
no light here
Pittman, 2018
Climate Regulation (Ocean) - benefits of healthy ocean
Healthy oceans provide climate regulation by uptake of a quarter of CO2 emissions and through heat transport.
Pittman, 2018
Blue Economy - benefits of healthy ocean
Contribution of healthy global oceans to economy (such as EU approx. 5% GDP); including fisheries $240 billion p/a
Pittman, 2018
Human impacts
Pollutants and nutrients via rivers
Commercial fishing— overharvesting of fish and whales
Increase in UV radiation due to stratospheric ozone loss
Greenhouse gases—increasing water temperatures and ocean acidification.
Not one place in the ocean that is untouched by human impacts
Often places are touched by multiple human impacts + they interact with each other
Pittman, 2018
Landscape Ecology
Emphasizes the causes and consequences of spatial variation in surface features and biota across a range of scales.
Pittman, 2018
Seascape Ecology
An integrative, spatially explicit discipline emphasizing interactions between spatial patterns and ecological processes in marine environments.
Pittman, 2018
Challenges in applying seascape ecology
Marine realm is more heterogenous, fluid and interconnected that the terrestrial environment
Pelagic ecosystems represent 3D continuum from the surface - changing all the time
SST, salinity, productivity gradients, currents
Linnean and Wallacean shortfalls are even more pronounced in the sea than on land
Most what is out there is unknown - Linnean shortfall
Wallacean shortfall - incompleteness of our knowledge
Pittman, 2018
Nutrients in Coastal Ecosystems
In estuaries, mixing of salt and fresh water can impact nutrient chemistry;
estuarine and salt marsh sediments often have low oxygen concentrations that limit decomposition.
estuaries change in PH 0 can release nutrients bound to floor parties
Pittman, 2018
Factors limiting Aquatic Primary production
Interaction of nutrients and light structures aquatic biomes
the interaction of these two factors also regulates the rates of NPP(net primary productivity)
Nutrient limitation is far more important than in terrestrial Ecosystems
NPP in aquatic ecosystems is much more responsive to the limiting nutrient
Pittman, 2018
Colimitation in Subtropical Ocean Gyres
NPP in the subtropical gyres is very low and is co-limited by nitrogen and phosphorus
Phytoplankton contain less phosphorus than nitrogen
Relative proportions of dissolved nutrient concentrations in ocean virtually the same across the world’s oceans
Pittman, 2018
Redfield Ratio
Relative proportions of dissolved nutrient concentrations in ocean - nitrogen -phosphorus ratio.
Pittman, 2018
Upwelling of nutrient rich waters
Zones of upwelling are highly productive
Important for fishing etc..
Cold nutrient rich waters
Conversion of nutrients coming up
Net primary production as upward movement provides nutrients
Pittman, 2018
Linking pattern and process
Global positioning systems (GPS) allow ecologists in the field to document precise locations of species and other variables.
Radiotelemetry allows tracking of animal movements and migration patterns.
Data analysis and GIS continually improve with better computers and statistical methods.
Pittman, 2018
Cultural Seascape Ecology
Studies patterns of movement integrating the physical dimensions of ocean, coastal areas, and human interactions/relationships.
Ban et al., 2018
4Cs of seascape ecology
Seascape Patterns through Indigenous Worldviews
indigenous users of seascapes often create mental models of a seascape based on their observations
Mapping local knowledges can reveal a complex understanding of seascapes within TEK frameworks and unique worldviews - Dr Noelani Puniwai
Works with local communities to map their knowledge
Ban et al., 2018