Transcript Earth: A Living planet
Earth: A Living planet
To properly care for our planet, we must understand how the living world operates.
We study ecology, or the study of the interactions of organisms with one another and with their physical surroundings.
The part of the planet in which life exists is called the biosphere.
Where do we find life?
The part of the planet in which life exists is called the biosphere.
It includes all the areas of land, air and water on the planet as well as all the life that populates these areas.
Biosphere extends from about 8 km above the earth’s surface to as far as 8 km below the surface of the ocean.
Living organisms are not evenly distributed throughout the biosphere-why not?
Ecosystems
The biosphere is too large to study so scientists break it down into small units called ecosystems.
Ecosystems include a given area’s physical features (abiotic factors) and living organisms (biotic features) What are the abiotic and biotic factors in a pond ecosystem?
Pond ecosystem
Abiotic factors Water Sunlight Soil type Rocks Temperature Humidity Elevation rainfall Biotic factors Fishes Frogs Insects Snails Worms Amoebas Water lilies
Community
The organisms living together in an ecosystem Ex- a forest community would include trees, bird and fungi Ecosystems are not self-contained-they don’t function independently of one another.
Ecological succession
Ecosystems change with time because every organism effects environmental conditions around it.
ex- Burrowing worms change the texture of soil.
Trees shade the area beneath their branches, making it cooler Because of this, many ecosystems undergo ecological succession- a process in which an existing community of organisms is replaced by a different community over periods of time ranging from a few decades to thousands of years.
Sometimes succession occurs in places where no living community existed before.
Ex- new volcanic islands Organisms that colonize such areas are called pioneer species.
Lichen are typical pioneer species Changes in species, physical factors, natural disasters, human intervention are all things that can cause succession.
Succession often leads to a fairly stable collection of organisms called a climax community.
These are often described by the predominent species they contain Ex- temperate zone beech-maple forest
Biomes
A broad area of earth’s surface characterized by distinctive vegetation and associated animal life; for example. Broad-leaf forest biome, grassland biome, desert biome.
Land Biomes
Tundra Northernmost land biome Nearly treeless but with mosses, lichens, grasses Animals migrate there during the summer – caribou, reindeer, wolves, foxes, hordes of mosquitoes Characteristics permafrost- layer of permanently frozen subsoil; only a few centimeters thaw before its frozen again; this keeps plants small and stunted.
Taiga (Boreal Forest)
From Russian word meaning primeval forest Much of N. America/Asia- coast of N. California, Washington, Oregon –home of giant redwoods (tallest trees in the world – 60 meters) Cold summers that are mild enough and long enough to allow plants and animals to reproduce Many animals, birds
Temperate Deciduous Forests
Eastern US, most of Europe, parts of Japan, china and Australia Changing seasons and leaf fall Many animals- a lot hunted to extinction-deer, moose, gray foxes beginning to reappear An abundance of organic matter and nutrients stored in a layer called humus, making this good farmland Human activity (clearing) in New England, but much has been recovered
Grasslands
Many interior parts of continents Vast areas covered with grasses and small leafy plants Significant rainfall that falls during one season Plains and prairies of N. America, steppes of Soviet Union, veld of S. Africa and pampas of Argentina Midwest US- hot summers, cold winters Tropical grasslands- little seasonal temperature change seasons change from wet to very dry- called savannas Animal grazing keeps succession down Overfarming causes wind erosion
Tropical Rain Forest
Warm temperatures (25 C) and year round rainfall (200 400 cm) Large areas of S. America, SE Asia, Africa, Central America Home to more species of plants and animals than the rest of the land combined 70 meter tree canopy; lianas (wrapping vines) Animal life rich and varied. Many are tree dwellers-forest floor holds danger Chemicals found for diseases; destruction may be imminent
Deserts
Less than 25 cm of rainfall a year Sahara- Africa- largest desert- desolate, virtually no plant life Can be seasonal deserts- some rainfall- home to rapidly growing plants with extensive surface roots-SW US and Mexico Mountainous deserts- higher altitude-called cold deserts- brief rainy season- some grasses and shrubs Irrigation can make suitable for farming- often very fertile soil- working on it
Aquatic Biomes
Freshwater biomes Rivers, streams, lakes Provide much of our drinking water Important source of food Large rivers (Nile-Africa, Amazon-S. America) home to many species of insects, fish, amphibians,reptiles and mammals Human dumping grounds for waste
Marine Biomes
Vast habitats or the ocean Photic zone- the short distance that can be penetrated by sunlight- where photosynthesis takes place in plants May be as shallow as 30 m in N. Atlantic or as deep as 200 m in S. Pacific Ocean Layer where phytoplankton (tiny free-floating photosynthetic organisms) and algae grow Oceanographers have divided the ocean into ecologically distinct zones depending on depth and distance from shore.
Intertidal Zone
Most difficult for organisms to live in Part of the day underwater; part of the day exposed to air and sunlight; pounding surf; surging waves Some organisms burrow (clams);some attach themselves to rocks (barnacles, seaweed) still others cling by their feet or suckers (snails, sea urchins, starfish)
Neritic Zone
The part of a marine biome that extends from the low tide line to the edge of the open ocean Larger algae (seaweed) are abundant because its in the photic zone Huge numbers of marine life reside here/hunt here Fish, invertebrates, turtles, lobsters, crabs, flounder, rays
Open-sea zone
Phytoplankton responsible for 80-90% of earth’s photosynthesis Food chains are at work Fish, mammals, sea birds reside here More phytoplankton closer to shore (more nutrients), hence more fish closer to shore Unfortunately makes them more susceptible to human pollution and over-fishing
Deep-Sea Zones
Area of high pressure, cold temperatures and total darkness Until recently thought to be devoid of life Home to some of the strangest creatures- gulper eels with mouths that make up ½ of their body; giant squid with glowing side spots; huge sea cucumbers lumber on the bottom Zooplankton (free-floating microscopic animals) hide out here during the day and come to the top at night
Estuaries
Found at the boundary between fresh water and sea water Salt marshes, mangrove swamps, lagoons, and river deltas Relatively shallow, high photosynthetic areas Sheltered area for fish laying and bird nesting
Energy and Nutrients: Building the Web of Life One of the most important factors in an ecosystem is the flow of energy. Only 0.1% of the sun’s energy that reaches the surface is used by living things 1/2 of the energy absorbed by plants is used immediately- the rest is stored in plant tissue in compounds called carbohydrates
Animals that eat plants obtain this energy.
They use much of it and store very little in tissues.
Energy cannot be recycled or used again so they don’t call it an energy cycle but rather an energy flow.
Energy Flow- 1
st
step
Sunlight (solar energy) trapped by plants (and some bacteria) and changed into carbohydrates through photosynthesis.
Producers – photosynthetic organisms capable of making their own food.
Energy Flow – 2
nd
step
Directly – eat plants- primary consumers- herbivores Animals are consumers. They get their energy either directly or indirectly from producers Indirectly- eat animals that eat plants – secondary, tertiary or quaternary consumers-carnivores
Energy flow- 3
rd
step
When producers and consumers die, their remains do not build up because of
decomposers
Decomposers obtain their energy from non-living organic matter They break down dead material Include fungi and bacteria
Summary – energy flow
Each step is called a trophic level At each trophic level, energy is used and less is available to the next level As a rule, only about 10% of the energy at one level is stored to be used by the organisms at the next level.
Scientist use an ecological pyramid to represent the energy relationships among trophic levels.
Biogeochemical Cycles
Although energy moves in a one-way direction through an ecosystem, nutrients are recycled.
They are called biogeochemical cycles because nutrients, unlike energy may be used over and over again by living systems.
Water cycle
The movement of water from the atmosphere to the earth and back to the atmosphere
Nitrogen cycle
All organisms require nitrogen to build proteins Although 78% of the air is nitrogen gas, most organisms can’t use it in this form.
The nitrogen cycle shows the movement of nitrogen through the biosphere
Carbon and Oxygen cycles
Nutrient limitations
The rate at which producers can capture energy and use it to produce living tissue is controlled by several factors, one of which is the amount of available nutrients.
If the nutrients are in short supply, it is called a limiting factor Ex- adding large amounts of nitrogen to coastal water causes tremendous growth, or an algal bloom.
Adding a bit of fertilizer doesn’t usually harm an ecosystem, but adding too much can cause harm.
Feeding relationships
Simplest – food chain Usually more complex- food web
Can find more info in Ch. 17 & 18.
End of material for second test
Populations
A group of organisms that all belong to the same species and that live in a given area
Exponential Growth
Almost any organism provided with ideal conditions for growth and reproduction will experience a rapid increase in its population The larger the population gets, the faster it expands It produces a growth curve called an exponential growth curve Left unchecked, one bacteria could exponentially reproduce to cover the planet three miles thick in 72 hours.
One pair of elephants could produce in 19 million offspring in 750 years!
Logistic Growth: closer to reality
Most populations go through a number of growth phases which can be represented on a logistic growth curve.
A B C D E A- at first their numbers increase slowly B- the population soon grows rapidly (exponentially) C- speed of the growth begins to slow down- the population grows but not at as quick a rate D- from here on it grows more and more slowly until E- population growth becomes steady-the
steady state-
the birth rate is roughly equal to the death rate- population is maintained
Steady state line represents the carrying capacity of a particular environment for a particular species- certain factors keep the population from growing further.
Factors that control population growth
Density-dependent limiting factors- usually operate only when populations are large and crowded Competition Predation Parasitism Crowding and Stress
Competition- plants and animals compete for food, water, space, sunlight and other essential of life Competition between members of different yet similar species is a major force behind evolutionary change No two species occupy the same niche in the same place at the same time When two species compete, both find themselves under pressure from natural selection to change in ways that decrease their competition. This is important because it ties ecology to evolution It is an example of how all biological sciences are interrelated when you look at them from an evolutionary point of view
Predation
Predator prey relationships exist for just about every species As prey numbers increase, its easier to get. More get eaten and their numbers decrease.
As predator numbers increase, the food source gets used up and their numbers decrease.
Important to maintain both groups Ex . wolves, bobcats and deer Rabbits in Australia