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Primary production of carbon compounds
production in ecosystems is the accumulation of carbon compounds in the form of biomass
gross primary productivity is the biomass or energy of carbon compounds per time and area, made in plants by photosynthesis
net primary productivity is the GPP minus the biomass lost due to respiration of the plant, it is what’s available to consumer
Secondary productivity
the accumulation of carbon compounds in biomass by heterotrophs
Nutrient cycle
nutrients enter biosphere via autotrophs, which obtain all of their nutrients from the abiotic environment
within biotic, heterotrophs obtain most nutrients from their food
nutrients pass from organisms to organism via feeding
Atoms return to the abiotic from biotic
carbon is the most abundant element of life and is continuously cycled between the biotic and abiotic components
Carbon pool
a location or system that can store or release carbon
Carbon flux
processes that exchange carbon between pools
a single carbon pool can often have several fluxes both adding and removing carbon simultaneously
Carbon sink
anything that absorbs more carbon from the atmosphere than it releases
Carbon source
anything releasing more carbon into the atmosphere than it absorbs
Carbon cycle
nutrients in an ecosystem are recycled and reused in form of chemical elements of nutrients circulating between living things and the environment
carbon is a main nutrient found in proteins, carbs, and lipids
it cycles continuously between abiotic and biotic environments
Main carbon storage sinks/pools
Carbon is stored in sinks or pools in form of organic or inorganic compound
ex: biosphere, oceans and lakes, atmosphere, sediments and soil
carbon moves between 4 pools by variety of biological or industrial processes called fluxes
Amount of carbon stored in parts of earth
atmosphere - 750 GT
Soil - 1580 GT
Terrestrial Pool - 610 GT
Aquatic pool - 3 GT
Ocean surface pool - 970 GT
Ocean deep pool - 38,000 GT
Lithosphere
largest amount of carbon on Earth is stored in sedimentary rocks within the planets crust
these rocks are produced by hardening of mud into shale or by collecting calcium carbonate particles into limestone
Pool - 1,000,000+ GT
Fossil fuels
a fossil store in organic matter (coal, oil, natural gas) which formed over millions of years
normally there would be no flux of this carbon back into the carbon cycle however through human actions, this carbon is introduced into the other carbon pools unnaturally
Pool - 1200 GT
Fluxes - Photosynthesis
carbon dioxide diffuses from the atmosphere or water into autotrophs
CO2 is removed from the atmosphere and moved to the biosphere
only process that has a net decrease on level of carbon dioxide in atmosphere
Fluxes - respiration
terrestrial organisms release carbon to the atmosphere whereas aquatic organisms release carbon to the hydrosphere
CO2 produced by respiration is diffused out of organisms into water or the atmosphere
CO2 is released from biosphere to the atmosphere during cellular respiration by decomposers
Lithification
lithification is the process in which sediments compact under pressure, expel fluids, and gradually become solid rock
moves carbon from the biosphere to the lithosphere
Combustion
forest fires and fossil fuel combustion releases carbon gases when organic hydrocarbons are burned as a fuel source
move carbon from fossil fuels and biosphere into atmosphere
Fossilization
in anaerobic conditions, dead organisms decay slowly or not at all
these organisms build up and if compressed over millions of years, can form fossil fuels
moves carbon from soil and biosphere to the geosphere
Keeling curve
past CO2 concentrations can be collected from ice cores
annual rhythm shows that the carbon dioxide concentrations is lower in the summer months and higher in the winter months
Ecosystem stability
the capacity of an ecosystem to maintain its structure, function, and biodiversity over time
able to withstand environmental changes, recover from disturbances, maintain biodiversity, preserve ecological functions
ecosystem resistance
the ability to continue functioning without significant change when stressed by disturbance
forest ecosystem with minimal damage from a minor wildfire
Ecosystem resilience
ability to recover and return to original state or function after a disturbance
grassland ecosystem that regrows quickly after a drought/fire
ecosystem stability requirements
nutrient cycling without leakages
steady supply of energy
high genetic diversity so populations can survive selection
climatic variables within tolerance (temp)
absence of disruptions with would interfere with sustainability
Disruptions to an ecosystem
erosion leads to a loss of nutrients
eutrophication is when nutrient enrichment of water causes population imbalance
harvesting and removal of materials disrupts nutrient cycles and food webs
poaching and selective removal disrupts ecosystem structure, especially if keystone species is removed
Amazon rainforest stability - water cycle
sustains itself through a tight recycling of water and nutrients
trees release huge amounts of water vapour through transpiration, helping create rainfall that falls back on forest
Amazon rainforest stability - nutrient cycling
most nutrients are stored in living plants, not soil
dead leaves and organisms decompose quickly
roots absorb the released nutrients from decomposition
Amazon rainforest stability - biodiversity balance
millions of species fill different ecological roles, keeping food webs stable and resources efficiently used
Amazon rainforest stability - climate regulation
dense vegetation moderates temp and humidity, creating conditions the forest itself depends on
tipping point of ecosystems
there is so much disturbance that a critical point is reached where a reversal might be difficult or impossible
positive feedback loops (Water cycle)
positive feedback loops have tendency to amplify the effects and drive a system to a point where new form of stability is reached
Mesocosm
completely sealed off ecosystems with only light entering as a source of energy, or open but controlled in some way
used to investigate ecosystem stability and sustainability
Keystone species
every ecosystem has certain species that are critical to the survival of other species in the ecosystem
could be a predator, like a wolf or a plant, but without them, the ecosystem may not survive
example of keystone species
the american beaver is an example of a keystone species in North america
they perform unique and crucial roles within an ecosystem
sustainability of resource harvesting
the responsible maintenance of ecological systems so that there is no reduction of conditions for future generations
ensures long term viability of a system
depends on the rate of harvesting being lower than rate of replacement
factors affecting the sustainability of agriculture
soil erosion
fertilizers
leaching
carbon footprint
monocultures
soil erosion
caused by tillage, which involves plowing, harrowing, and results in a reduction of soil quality
Fertilizers
growing crop causes nutrient depletion over time which needs fertilizers to compensate
excess fertilizers leach into water systems which can lead to eutrophication
leaching
soil exposure can lead to leaching of nutrients from the soil
when it rains, nutrients are washed away and not available for plants
carbon footprint
the use of heavy machines for tillage, harvest, and transport need a lot of energy
processes large amounts of carbon emissions (diesel engines)
Monocultures
repeated growth of the same crop results in pests and weeks to become increasingly problematic
use of pesticides can cause pollution problems and the production of the chemicals needs energy
Eutrophication
the excessive nutrient enrichment of water
nutrients like phosphates and nitrates favour the growth of algae, which multiply in big numbers and lead to algae bloom
can occur naturally through gradual drying up of pools of water
can be due to leakage of excess chemicals used in agriculture
Algae bloom
forms a thick, sunlight blocking cover on the surface of water
prevents oxygen to dissolve and prevents plants to photosynthesis and die
decomposition by bacteria further depletes oxygen supplies
Biological oxygen demand (BOD)
amount of dissolved oxygen required to break down organic material in a given volume of water
aerobic organisms use oxygen in respiration, resulting in higher BOD
BOD can indirectly measure pollution
BOD measurement technique
indirect method to determine water quality and aerobic activity by bacteria
determined by taking a measured volume of water from source and measuring the dissolved oxygen content on day 1
sample then placed in dark to prevent photosynthesis
after 5 days, the oxygen level is measured again
BOD is difference between initial and final oxygen concentration
Bioaccumulation
increase in the concentrations of a toxin in body tissues during an animal’s lifetime
usually happens with fat soluble chemicals which cannot be excreted
Biomagnification
increase in the concentration of a chemical at each successive trophic level in a food chain
predators tend to accumulate higher chemicals of a toxin than their prey because larger quantities are consumed
effects of plastic pollution of oceans
main reason plastic accumulation in oceans in a problem is due to their non-biodegradability
macroplastics (large, visible, more than 5mm in size)
microplastics (extremely small pieces of plastic debris, less than 5mm)
Ecosystem degradation
ecosystem degradation by human actions has caused severe consequences such as loss of biodiversity, species extinction and loss of ecosystem services (flood protection)
efforts are being made to encourage natural ecosystems to return
rewilding
the process of restoring an area of land to its natural uncultivated state
ex: distributing seeds of plants, re-introducing apex predators and other keystone species, control of invasive species