Ecology Terms Starting With P

P

Ecology Glossary: P

Community EcologyClimate And EcologyEnvironmental EcologyBiogeochemistryPopulation Ecology

Parasitism

/ PAIR-uh-sih-tiz-um /  ·  Greek parasitos, one who eats at another's table; -ism, state or practice

Community EcologyIntro
Also known as:parasitic interactionhost-parasite relationship

Parasitism is a symbiotic relationship in which one organism, the parasite, benefits by obtaining resources from a host organism that is harmed but usually not immediately killed by the interaction.

Parasites are extraordinarily diverse, encompassing viruses, bacteria, fungi, protozoa, helminths, arthropods, and parasitic plants, and collectively they may represent the majority of all species on Earth when all forms are counted. Unlike predators, parasites typically do not kill their hosts immediately, instead exploiting them as living resources over extended periods, and many have coevolved diverse mechanisms to evade host immune systems. Parasitism drives much of the diversity of immune systems and life history traits across animals and plants, making it one of the most powerful selective forces in evolution.

Did you know?

Parasitism benefits the parasite while harming the host. Parasites usually do not kill hosts immediately because they often need the host to stay alive long enough to spread.

How To Become A Parasitologist? →
Common misconception

Parasites are always tiny worms. Parasites include protozoa, fungi, plants, insects, mites, and many other organisms.

Mycology →
Example in nature

Mistletoe is a parasitic plant that taps into host trees for water and minerals. Heavy infestation can weaken branches and reduce growth.

Order Santalales →

Permafrost

/ PER-mah-frost /  ·  Latin permanere, to remain; Old English forst, frost

Climate And EcologyIntermediate
Also known as:permanently frozen groundpergelisol

Permafrost is ground that stays frozen at or below 0 degrees C for at least two consecutive years, covering about a quarter of all land in the Northern Hemisphere and storing enormous amounts of frozen carbon from ancient plant material.

Permafrost underlies much of Siberia, Canada, and Alaska, as well as high-altitude mountain areas worldwide. While the surface layer thaws each summer, the ground below stays frozen year-round. Permafrost stores carbon like a giant freezer for dead plant material that has accumulated for thousands of years, when it thaws, bacteria break down this material and release carbon dioxide and methane, both greenhouse gases.

Did you know?

Permafrost stores nearly 1,700 billion tons of carbon, almost twice as much as the entire atmosphere currently holds. Scientists have found frozen plant material in Siberian permafrost that is over 400,000 years old.

Common misconception

Permafrost is always covered by snow. The surface layer can thaw in summer while deeper ground remains frozen.

Example in nature

In Arctic tundra, thawing permafrost can release carbon dioxide and methane as microbes decompose once-frozen organic matter. This can add to climate warming.

Greenhouse Gases →

Persistent Organic Pollutants

/ per-SIS-tent or-GAN-ik POL-yoo-tants /  ·  Latin persistere, to persist; Greek organikos; Latin polluere

Environmental EcologyIntermediate
Also known as:POPslegacy pollutantsbioaccumulative toxins

Persistent organic pollutants, commonly abbreviated POPs, are toxic human-made chemicals that do not break down in the environment for many years, build up in the fat of animals and humans, and become more concentrated the higher up the food chain they go.

POPs include pesticides like DDT, industrial chemicals like PCBs, and unwanted by-products like dioxins. Because they are fat-soluble and very stable, they dissolve into the fat of small animals, plankton, insects, small fish. When larger animals eat many of these smaller ones, the chemicals accumulate further in their fat.

Did you know?

Persistent organic pollutants resist breakdown and can travel long distances through air, water, and food webs. Many also accumulate in fatty tissues.

Common misconception

Pollution stays near where it was released. Persistent chemicals can reach remote regions such as the Arctic.

Example in nature

PCBs have been detected in marine mammals far from industrial sources. These pollutants can build up through food webs and affect reproduction or health.

Phosphorus Cycle

/ FOS-fer-us SY-kul /  ·  Greek phosphoros (light-bearing) + Greek kyklos (circle)

BiogeochemistryIntermediate

Phosphorus Cycle phosphorus cycle is the continuous movement of phosphorus from rocks and soil into plants and animals, through food chains, back to the soil through decomposition, and eventually into water systems and ocean sediments.

Phosphorus enters ecosystems through weathering of phosphate-rich rocks at rates of 0.1 to 10 milligrams per square meter per year depending on rock type and climate. Plants absorb dissolved phosphate ions from soil water through their root systems, and animals obtain phosphorus by consuming plants or other animals. Decomposition releases phosphorus back to soil, while water transport carries phosphate to lakes and oceans where it settles into sediments.

Unlike carbon and nitrogen, phosphorus lacks a significant atmospheric gaseous phase under normal Earth conditions.

Did you know?

Phosphorus has no stable gaseous form in Earth's atmosphere, making its cycle unique among major nutrient elements.

Common misconception

Phosphorus cycles through the atmosphere like carbon or nitrogen. It mainly enters ecosystems through rock weathering and moves with water, soil, and organisms.

Biological Weathering 101 →
Example in nature

Phosphate released from weathered granite rock gets absorbed by plant roots and incorporated into proteins and DNA. Animals consuming plants accumulate phosphorus in their tissues and bones.

Population Density

/ pop-yoo-LAY-shun DEN-sih-tee /  ·  Latin populatio + densitas (thickness)

Population EcologyIntro

Population density is the number of individuals of a species that live within a specific area or volume, such as the count of deer per square mile in a forest.

Population density measured as individuals per unit area affects resource availability, disease transmission rates, and mating opportunities for individuals in a population. High-density mussel beds experience intense competition for space with individual mussels reducing growth rates as available attachment substrate becomes limited. Disease spread increases exponentially with population density in crowded populations, allowing pathogens to transmit rapidly between nearby hosts.

Predation intensity often increases with prey density as predators locate food more efficiently in crowded populations.

Did you know?

Population density is the number of individuals per unit area or volume. It can affect competition, disease spread, mating success, and predation.

Common misconception

Population density and total population size are identical measurements. A small area containing 1000 individuals has high density while 1000 individuals spread across a vast area has low density despite identical total population size.

Example in nature

A crowded mussel bed has high population density on a rocky shore. Space for attachment becomes a major limiting resource.

Population Dynamics

/ pop-yoo-LAY-shun dy-NAM-iks /  ·  Latin populatio + Greek dynamis (power)

Population EcologyIntermediate

Population dynamics is the study of how and why the size and structure of a population change over time.

Births, deaths, immigration, and emigration directly change population size through mathematical relationships described by the equation Nt+1 equals Nt plus births plus immigration minus deaths minus emigration. Population size affects intraspecific competition for food and space, which then influences survival and reproduction rates. Density-dependent factors like disease and resource availability can cause populations to cycle, crash, or stabilize rather than grow indefinitely.

Environmental variation drives populations to fluctuate unpredictably in some species while others show stable cycles.

Did you know?

Snowshoe hare populations cycle every 8 to 11 years in northern forests, rising from about 1000 to over 40000 individuals per 100 square kilometers before crashing again.

Common misconception

Populations only grow until they fill all space. Real populations can rise, crash, cycle, or stabilize depending on conditions.

Example in nature

Snowshoe hare populations in northern forests rise and fall in cycles with peaks separated by roughly a decade. Lynx predation lags behind hare abundance by about one year because lynx numbers depend on recent prey availability.

Predator Prey

/ PRED-ah-tor PRAY /  ·  Latin praedator, hunter; praeda, prey

Population EcologyIntro
Also known as:predator-prey dynamicstrophic interaction

Predator Prey predator-prey relationship is the interaction between a predator, the hunting animal, and its prey, the animal it hunts and eats, a relationship that shapes the population sizes of both species in linked cycles over time.

Predator and prey populations cycle through predictable phases with a time lag between peaks. When prey like snowshoe hares are abundant, predator lynx have abundant food, reproduction increases, and lynx population surges after about one year. The larger lynx population then overhunts hares, causing hare numbers to crash.

With insufficient food, lynx reproduction declines and population falls, allowing hare recovery and restarting the cycle. These linked oscillations occur in many predator-prey systems including wolves and moose.

Did you know?

Predator-prey relationships can shape behavior, body defenses, and population cycles. Both predator and prey populations can influence each other over time.

Common misconception

Predators always wipe out prey if they can. Predators often depend on prey survival, and prey scarcity can reduce predator numbers.

Example in nature

Canada lynx prey heavily on snowshoe hares in northern forests. Hare population peaks are typically followed by lynx peaks one or two years later.

Primary Producer

/ PRY-mair-ee proh-DOO-ser /  ·  Latin primarius (first) + producere (to lead forward)

EcologyIntro
Also known as:autotrophphotoautotroph

Primary Producer primary producer is an organism that makes organic food from simple substances, usually by photosynthesis.

Primary producers capture light or chemical energy and convert it into organic molecules through photosynthesis or chemosynthesis. Plants fix carbon dioxide into glucose using chlorophyll and solar energy at efficiency rates between 0.5 and 3 percent. Cyanobacteria and chemosynthetic bacteria oxidize hydrogen sulfide or methane to generate energy in deep ocean vents and other anoxic environments.

These organic molecules flow up food chains as herbivores consume producers and carnivores consume herbivores.

Did you know?

Phytoplankton in oceans and lakes produce roughly 50 percent of atmospheric oxygen while forming the energy base for aquatic food webs.

Respiratory System Fun Facts →
Common misconception

Primary producers are always plants. Algae, cyanobacteria, and chemosynthetic bacteria are also primary producers.

Cyanobacteria →
Example in nature

Phytoplankton are primary producers in oceans and lakes that convert sunlight and carbon dioxide into organic molecules. They support zooplankton, fish, and larger predators that consume them or their herbivorous consumers.

Primary Production

/ PRY-mair-ee proh-DUK-shun /  ·  Latin primarius, first; producere, to bring forth

Ecosystem EcologyIntermediate
Also known as:gross primary productionnet primary productionGPPNPP

Primary production is the process by which plants, algae, and some bacteria convert sunlight or chemical energy into organic matter, forming the energetic foundation of nearly all food chains.

Gross primary production is the total amount of organic matter made by photosynthesis. Net primary production is what remains after producers use some of that energy for respiration, and it represents the energy available to animals and other consumers. On land, tropical rainforests have the highest net primary production; at sea, coastal waters and upwelling zones are among the most productive.

Did you know?

Primary production is the creation of organic matter by autotrophs. It is the entry point for much of the energy used by ecosystems.

Common misconception

Primary production happens only on land. Phytoplankton in oceans and lakes perform huge amounts of primary production.

Example in nature

In the open ocean, microscopic phytoplankton use sunlight to fix carbon dioxide. Their production supports zooplankton, fish, and marine predators.

Respiratory System Fun Facts →

Primary Succession

/ PRY-mair-ee suk-SESH-un /  ·  Latin primarius (first) + successio (following after)

EcologyIntermediate

Primary succession is the development of a community in a place where soil and an earlier community are absent.

Primary succession begins on unvegetated surfaces like new lava flows, bare rock, or sand dunes where no soil or previously established biological community exists. Lichens and mosses colonize bare substrate first because they require minimal soil and can fix nitrogen from the air. These early colonists weather rock surfaces and accumulate organic matter that gradually builds soil depth measured in millimeters per year.

Grasses and shrubs establish once soil development supports their deeper root systems, eventually allowing trees to dominate decades or centuries later.

Did you know?

Lichen and moss growth rates of 1 to 2 millimeters per year can take hundreds of years to produce soil deep enough for shrubs and trees.

Common misconception

Primary succession occurs after a forest fire or farm abandonment. These situations involve secondary succession because soil and dormant seeds already exist.

Example in nature

After a glacier retreats, pioneer lichens like Rhizocarpon geographicum colonize bare rock. Over 100 to 200 years, weathering and organic accumulation develop soil thick enough for mosses, grasses, and eventually shrubs and trees.

Explore Biological Weathering →