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Flashcards covering ecosystem components, functional properties, thermodynamics, Redfield ratio, carbon cycling pumps, and the global hydrological cycle based on lecture notes.
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Ecosystem
A system of organisms and their physical environment, composed of all organisms in an area, the physical environment, and their biotic and abiotic interactions.
Population
Organisms of the same species living in the same habitat, characterized by the fundamental property of abundance (e.g., biomass).
Community
Coexisting populations of different species, defined by the fundamental properties of species diversity and food web structure.
Autotrophs
Organisms ("self-nourishers") that synthesize organic material from solar or chemical energy and essential inorganic elements from the atmosphere (e.g., N2) and lithosphere (e.g., P, S, Ca).
Heterotrophs
Organisms ("nourished from others") that obtain energy and organic nutrients by consuming autotrophs or other heterotrophs.
Redfield Ratio
The relative atomic ratio of carbon, nitrogen, and phosphorus in living phytoplankton, defined as C:N:P=106:16:1 (with an N:P ratio of 16:1).
Liebig's Law of the Minimum
The principle stating that growth is limited by only one nutrient at any one time: the nutrient in least supply relative to what is needed.
First Law of Thermodynamics
The law of conservation of matter and energy stating that matter and energy are neither created nor destroyed in any physical or chemical process, but merely transformed.
Second Law of Thermodynamics
The law of energy degradation (entropy) stating that energy moves from an organized, useful form to a disorganized, less useful form, and cannot be recycled to its original state of usefulness.
Marine Biological Pump
The pathway in which surface phytoplankton convert atmospheric CO2 into organic carbon, which sinks into the deep ocean via sedimentation and undergoes bacterial decomposition before returning to the surface via upwelling.
Solubility Pump
The chemical exchange process where atmospheric CO2 dissolves in ocean water to form carbonic acid (H2CO3), bicarbonate (HCO3−), and carbonate (CO32−), which shelled organisms convert into calcium carbonate (CaCO3).

Foraminiferans
Protozoa (<0.5accession−idmm in size) inhabiting plankton and marine sediments that feed on bacteria and produce approximately 1×109 tons of CaCO3 per year.

Coccolithophores
Planktonic algae that produce 1.5×106 tons of CaCO3 per year and form ocean surface blooms that reflect visible light.
Short-term Carbon Cycles
Carbon exchange processes that occur rapidly between the atmosphere and biosphere, such as photosynthesis and respiration.
Long-term Carbon Cycles
Carbon processes occurring over geological timescales involving rock weathering, volcanic activity, and the formation and destruction of sediments and fossil fuels.
Evaporation
The phase transition of liquid water to water vapor, occurring at a rate dependent on liquid temperature because higher thermal energy provides the energy needed to break chemical bonds.
Condensation
The phase transition of water vapor to liquid water, occurring at a rate dependent on vapor pressure and molecule collisions in an air parcel.
Vapor Pressure
A measure of the quantity of water vapor molecules present in a specific parcel of air at any given moment.
Transpiration
The conversion and release of liquid water to water vapor into the atmosphere by plants through their leaves.
Flying River
An atmospheric movement of huge quantities of water vapor over large land areas driven by wind currents and high volumes of recycled plant transpiration.
Biological Cloud Seeding
The release of volatile organic compounds by trees and plants that act as cloud condensation nuclei to promote localized cloud formation and rainfall.
Sublimation
The direct phase transition of water from a solid state (ice or snow) to a vapor state without passing through a liquid state.
Desublimation (Deposition)
The direct phase transition of water from a vapor state to a solid state without passing through a liquid state.

Residence Time
The average amount of time water or a substance spends within a specific reservoir, calculated under steady-state conditions as reservoir volume (S) divided by inflow or outflow rate (I).
Atmospheric Water Residence Time
The characteristic residence time of water in Earth's atmospheric reservoir, calculated as 0.03years or approximately 11days.