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A rock formation found in southwestern Minnesota. It is one of the oldest rocks known to the world estimated to be around 3.5 million years ago. It is the oldest rock in MN It is dated to the Precambrian era when the continents were still being formed It helps scientists learn more about the formation of the earth's crust and development of landscape
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Lake Agassiz
When the Wisconsin glacier retreated for the final time about 10,000 to 12,000 years ago, the continental divide prevented the water from draining into the MN River and instead formed a huge lake called Lake Agassiz. It covers a total area around 123,500 square miles and a maximum depth of about 400 feet. The lake eventually grew high enough that it began to drain over a dam creating the glacial river warren which is now the valley of the MN River. During this, the natural drainages through lake superior, and the hudson bay opened and Lake Agassiz began to drain. Now there remains the basin of Glacial Lake Agassiz in north-central MN.
Ecosystem
A community of living organisms interacting with each other and with the nonliving environment.
Relationships through biotic factors - living elements (plants, animals)
relationships between through abiotic factors - nonliving elements (soil, light, water)
Food chains - primary consumer (bottom of the food chain, plants) secondary consumers (what consumes the primary, snails)
Watershed
Watershed as a water-land area where water drains into a lake, river etc.
Runoff, snow, rain etc all drains in - this carries minerals, nutrients, and pollution into the water bodies
3 vs 4 Biomes
Tallgrass prairie
Located mostly in southern and western MN
Dominated by grasses, flowering plants, and few trees
Lower precipitation - drought - fires
Deciduous Forest
Diagonal band stretching from southeastern to north-central MN
Dominated by trees that lose leaves seasonally - maple, basswood, elm
Northern Coniferous Forest
Northeastern MN
Dominated by evergreen trees - spruce, pine, aspen, birch
Cooler temps and shorter growing seasons
4? - Wetlands, aquatic systems
Biomass and there is no away
Biomass is the total amount of a living organic material in an organism, population, or ecosystem at a given time
Energy flow and trophic levels - plants create organic matter through photosynthesis while other organisms consume plant biomass
The amount of biomass depends on factors like sunlight, water, nutrients, climate
There is no away is a concept stating that nothing really disappears, waste we throw away remains in the environment and affects it.
Matters such as logging and other human activities deeply affects biomass
Tester’s Creation Story of MN lakes
Lakes were primarily created by glacial activity during the Ice Age, impacted significantly by the retreat of the Wisconsin Glacier - 10,000-12,000 yrs ago
As glaciers moved across MN, they scraped and made depressions in the surface, when the glaciers melted these areas filled with water creating lakes
Processes
Scouring by ice - moving glaciers created basins in the bedrock and soil
Buried ice blocks - ice chunks got trapped in sediment when they melted they left holes to be filled with water
Moraines and glacial deposits - glaciers deposited rock and sediment that created dams which helped lakes form
Glacial meltwater - rivers of meltwater reshaped valleys and created basins and wetlands
Nutrient Cycling
The continuous movement and reuse of essential nutrients - carbon, nitrogen, phosphorus, oxygen through living and nonliving organisms
Plants absorb from soil/sun/water, animals obtain them by eating plants or other animals
Organism waste, or death - decomposers like fungi, bacteria, insects break down this organic material and return the nutrients to the cycle
Types of Aquatic Systems
Wetlands
Where water stays near or above the soil for long periods of time
Prairie wetlands - shallow for ducks and amphibians
Peatlands - northern with peat, moss, tamarack, and spruce
Bogs, marshes, swamps
Lakes
Were mostly formed by glaciers
Vary in depth, nutrients, temp, and productivity
Oligotrophic lakes are deep, clear, and nutrient poor
Eutrophics lakes are nutrient rich, with more plant and algae growth
Streams and Rivers
Flowing water ecosystems formed by glacial drainage systems
Ecology is influenced by current, oxygen, temp, and sediment movement
Supports fish, insects, amphibians, and vegetation
Types of wetlands
Prairie wetlands
Shallow common in western MN
Ducks, amphibians, and aquatic plants
Bogs
Acidic, nutrient poor
Dominated by moss, spruce, and tamarack
Water comes from rain
Fens
Fed by groundwater
Contain many nutrients and plants
Marshes
Dominated by grasses, cattails, sedges, nonwoody plants
Water levels fluctuate seasonally
Swamps
Forested wetlands containing trees and shrubs
Peatland: Bogs vs Fens
Peatlands are wetlands with thick accumulations of partially decomposed organic matter called peat. Bogs and Fens
Bogs
acidic and nutrient poor wetlands
Water comes mostly from rain or snow
Moss, spruce, tamarack
Fens
Groundwater fed
Brings in dissolved minerals making less acidic, more nutrient based ecosystem
Support many grasses, and plants
Types of Prairies
Tallgrass prairie
Found in wetter regions
Dominated by tall grasses - bluestem and switchgrass
Mixed-Grass Prairie
Moderate rainfall areas
Medium and shorter grasses
Shortgrass prairie
Driest regions
Dominated by short, drought resistant grasses
Disturbance and Succession
Disturbance is an event that disrupts an ecosystem and changes its structure, resources, or species composition - natural fires, floods, or unnatural - logging, farming, pollution
Succession is the gradual process of ecological change that occurs after a disturbance. Overtime the ecosystem changes and adapts
Ex. Fires in prairies. Fires remove dead or old vegetation (grass/trees) and allows new grass to grow quicker
Fragmentation of Landscape
When large natural habitats are broken into smaller, isolated pieces by human activities. Ex: agriculture, roads, logging, urban development.
In MN fragmentation has affected tall grass prairies which are now farmland
Deciduous forest
Mainly in southeastern and central MN
Trees include Maple, Elm, Basswood, and Oak
Trees that shed leaves in the fall
Coniferous forest
Northern MN
Trees include spruce, fir, pine, tamarack, cedar
Adapted to colder temps, shorter growing seasons, and thinner soils
Two trees in the Big Woods/Deciduous forest and one ecological role
Basswood
Elm
In this forest leaves fall from trees and decompose on the forest floor returning nutrients
Two trees in Northern Hardwood forest and one ecological role
Yellow birch
Pine - balsam fir
Sugar maple
Provides shade for the animals and saplings
Two native prairie grasses, and one ecological role
Switchgrass
Bluestem
Grasses provide soil stabilization and nutrient storage
Period of time prairies were largely destroyed in MN and how
Largely destroyed during the late 1800s and early 1900s due to settlers expanded across the state and converted prairies into farming land
Invasive species and two examples from two MN biomes
Invasive species are non-native plants and animals that spread into ecosystems and disrupt
Ex 1 - Zebra mussels (aquatic biome)
Canada Thistle (Prairie Biome)