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Vocabulary flashcards covering deserts geography, abiotic factors, adaptations, soils, and species patterns.
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Global desert coverage
Deserts occupy about 20–30% of Earth's terrestrial surface.
Desert population
About 1 billion people live in deserts, roughly 1/6 of the world population.
Desert rainfall threshold
Deserts are defined by an annual rainfall of about 10 inches (25 cm) or less.
Subtropical desert
Deserts formed by Hadley cell circulation producing dry air and high pressure, leading to low precipitation.
Cold desert
Deserts at higher latitudes with cold conditions and low precipitation.
Coastal desert
Deserts near cold coastal waters; fog and humidity are high but not enough to cause significant precipitation.
Fog Oasis
A moist microhabitat where fog condensation supports plant and animal growth in coastal/desert regions.
Rainshadow desert
Desert on the leeward side of a mountain where moisture is blocked from prevailing winds.
Interior desert
Desert located far from water sources; often with endemic species and variable rainfall.
Boom cycles
Periods of variable, high-volume precipitation that allow rapid plant growth in deserts.
Liebig’s Law of the Minimum
Population growth is limited by the scarcest resource, not by the total amount of resources.
Limiting resource
The resource in shortest supply that constrains growth (e.g., water, nutrients).
Water availability
One of the primary limiting resources for desert organisms.
Soil fertility
Nutrient content of soil that affects plant growth.
Extreme temperatures
Large temperature fluctuations that can limit organism performance in deserts.
Principle of Tolerance Limits
Organisms have an optimal growth range with limits beyond which growth declines.
Stenothermal
Narrow, restricted optimal temperature range for a species.
Eurythermal
Wide tolerance to a range of temperatures.
Net Primary Productivity (NPP)
Biomass and organic matter produced by photosynthesis after accounting for respiration.
Photosynthesis
Process by which plants convert CO2 and H2O into glucose and O2 using light energy.
Xylem water transport
Movement of water up the plant via cohesion and adhesion in the xylem, driven by transpiration.
Crassulacean Acid Metabolism (CAM)
Desert photosynthesis where CO2 is fixed at night as malate and used in the day for the Calvin cycle.
Desert soils horizons
Desert soils typically have horizons such as O, A, E, B, and C reflecting weathering and deposition.
Ardisol
Desert soil order (as listed): an arid soil developed from parent material.
Alfisol
Desert soil order with ill-defined argillic/pale horizons and typically higher fertility than aridisols.
Oxisol
Highly weathered tropical soil order; in deserts may be listed among desert soil types.
Transpiration
Plant cooling via evaporation of water from stomata.
Perspiration
Animal cooling through sweating or evaporative cooling.
Nocturnal behavior
Desert animals active at night to avoid daytime heat.
Aestivation
Drought-time dormancy or hibernation-like state in hot, dry conditions.
Adaptation
Heritable trait that improves an organism's survival and reproductive success.
Escaping
Adaptive strategy of avoiding bad conditions by migrating or relocating.
Evading
Adaptive strategy of avoiding dry conditions through burrowing or deep rooting.
Resiting
Adaptive strategy of living within a stressful zone by tolerance and resource concentration.
Enduring
Traits enabling survival in harsh conditions (e.g., aestivation).
Structural adaptation
Physical changes like leaf coatings, skin, or exoskeleton to reduce water loss.
Physiological adaptation
Internal functional changes to conserve water or optimize metabolism.
Behavioral adaptation
Behavior changes such as timing activities to cooler periods.
Life History Strategies
Evolutionary trade-offs in reproduction and energy use to survive in deserts.
Desert species diversity patterns
Mammal diversity is higher along western coasts; reptiles along the south; birds along coastlines.