Contents of Curriculum Unit 92.05.04:

Introduction

Many people today seem to have lost hope in the future, feeling helpless and paralyzed to do anything to affect it. I believe that, in part, this comes from viewing nature and ecology at a distance, and feeling that the “important issues” are global, too distant and overwhelming for the common person to do anything about. Others I have spoken with seem to feel that the earth is so powerful and magnificent that it can take in stride anything that mere men could do to it and still manage to right itself. I am hopeful that by involving students in a study of our earth on a personal level, they will begin to realize that each person can have an impact on changing the future, for better or worse.

Objectives

Strategies

Fall Component

Ecology Defined and Explained

Living organisms are widely varied and abundant on earth and are reliant on each other; they are not totally independent, distinct entities. They may share a common ancestry, they do share a common habitat in our biosphere, and they compete for the same sources of energy and materials. Living organisms are especially organized parts of the biosphere that interact constantly with one another and also with the nonliving components of the biosphere. They are regarded as a web of life in which all of the parts are intricately interwoven. As plants and animals solve the problem of finding energy sources, they affect each other. Sometimes the way these organisms affect one another are easy to see, sometimes they are impossible to observe, but all living things do affect one another directly or indirectly.

Scientists since Darwin have been concerned with the organization of living and nonliving things, and “biological community” is a phrase they have used to describe the distinctive organization of plants and animals in a given area they are studying. This concept tended to focus on the organisms occupying a given area, rather than the processes going on there. Ecologists are now interested in understanding how biological communities function. The term ecosystem was coined for this purpose in the 1930s, but did not become widely used and understood until the 1960s.

Theoretically, there are an unlimited number of ecosystems for any situation being studied. Students will be encouraged to brainstorm names of the ecosystems of which they are a part, ranging from the earth as a whole to the United States to New Haven, Connecticut, to our school, to our class, to their family, etc. At this point they will not be asked to analyze these ecosystem as much as to recognize the many ways there are to look at our place in the environment. I intend to use activities like this to reinforce constantly the fact that every person has an impact on the environment, no matter how distanced he may feel from major problems.

Although I intend to focus my unit on the local environment, I will briefly expose students at this time to the fact that ecologists tend in general to look at a limited number of ecosystems when they are looking at the earth as a whole, and that these generally are divisions of large units of nonmarine earth space called biomes. Biomes are almost all named for the principal physical aspect of the vegetation. In general, the recognized classification of the world’s biomes includes:

Tropical Rainforest

Tropical Cloud Forest

Tropical Deciduous Forest	Tropical Scrub Forest
Tropical Savanna	Mangrove Forest
Mediterranean Woodland and Shrub	Oceans
Middle Latitude Grasslands	Lakes
Middle Latitude Marshlands	Rivers
Middle Latitude Deciduous Forest	Coniferous Forest

Tundra

Cycles in Nature

In illustrating this, students will begin their hands on experiments with ecosystems. We will go out to the area around the school and collect soil samples to be used. Back in the classroom, students will create their own bottle ecosystems by placing soil samples into clean, recycled plastic soda bottles (two or three liter) and sealing them. These will be their individual sealed ecosystems. Students will be encouraged to comment on what they found out about the environment around their school and to make notes of the components they find in their soil, including such things as rocks, bugs, glass, bits of asphalt, etc. (At this point I will remove any objects which might be dangerous to students, including glass. If a student feels that she/he wants this to be part of their ecosystem as an experiment, I will personally see if there is a way to include it.) They will be encouraged to predict what will happen within their ecosystems. Preliminary findings on soil, procedures, and students’ predictions will be charted and displayed in the classroom. Throughout this unit I will stress with the students that there are no “right” or “wrong” answers. They may find very different results at any time from the same procedures, but it will hopefully reinforce that there is no guarantee of results where so many factors of nature are involved. Our bottle ecosystems will then be placed in varying conditions around the room to be observed in future days. Students will be encouraged to experiment with conditions where they place their bottles, including putting them inside a cabinet or dark place which would simulate the low light conditions we generally experience in New Haven in winter. Bottles will be checked periodically and observations recorded on our charts.

At this point, I would like to involve students in thinking about the soil they have collected as a product of both nature and man. After telling students that soil is partly made up of rock particles, I would encourage them to think of a rocky area they know. (West Rock and East Rock are certainly good examples for students in New Haven who believe they cannot think of an individual area.) I would ask the students to think about what weather conditions the seasons bring to the area, and we would do a prediction chart: What effects do you think certain seasons might have on rocks? (For all prediction sessions to be most productive, I believe the teacher should accept and record all given answers nonjudgementally.) If possible, this would be a great time to plan a field trip to the beach, where many of the concepts about to be covered could be demonstrated.

After predicting, I will ask students to think about the bare rock, and to picture hot sun shining down on it in the summer; rain, hail, and wind pounding against it and snow covering the rocky area in winter, and ice freezing in its cracks. Then think about the rain coming again in the Spring. I would try to elicit from them the response that after many years of this treatment a rock would begin to split and crumble. At this point I would ask them to think about the possibility of seeds being deposited there by natural causes, such as wind or birds. Hopefully I will engage them in thinking about roots growing into the rock, making tiny tunnels. I will give them information on rain seeping in next to the roots and ask how this would contribute to further splitting and cracking. This discussion will continue, encompassing the fact that the rock will eventually crumble into various sized pieces, and how these contribute to our soil.

Soil is made up of more than rock particles, and my next topic with students would be humus. In the Fall, leaves fall from the trees. Birds who have been flying around a neighborhood leave their droppings, and now and then a feather. Animal droppings are also left on the soil. Bits of fur may also brush off the animals as they walk about. These are added to the multitude of other things which may be on the soil: butterfly wings, old cocoons, bits of food, garbage created by people but spread by animals, dead roots and twigs, and many other things. Students will be encouraged to add information to the discussion from their own findings in their soil samples. All of the things which have ever lived and died from insects, to plants, to animals—become part of the earth when they die. They stay in the ground year after year in all of the cycles of weather and, like the rocks we talked about, they eventually break down. In addition to the process we discussed with rocks, animals also decay. Millions of bacteria and molds exist in the soil, so small that we cannot see them, but in their daily life cycle they produce chemicals that take apart and change the materials around them. This is how humus is made in a process called decay. The process of making humus also involves many tiny plants, and insects and worms who loosen and mix the soil as they tunnel about, and by microscopic animals. Humus mixes with sand and clay that has been made by the weathering of rocks.

In looking at the season of Fall or Autumn, it would be appropriate to have students comment on the changes they see happening in their neighborhood and to take a trip to nearby Edgewood Park to observe changes and to take pictures for a display project on seasonal changes. If possible, a Park Ranger would accompany the group for this trip. In addition to walking and talking about what they observe, students will be provided with a worksheet and possibly a list for a fall scavenger hunt containing such items as dried seed pods, colorful leaves, etc. Back in the classroom, we will discuss changes in plants which occur in Fall and what effect they have on the environment. We will also look at and chart temperature and weather changes. Discussion will include the fact that the changes we are observing are a gradual preparation by nature for the onset of winter, a cold and difficult season for the environment.

Winter Component

Some Major Cycles in Nature

Everything that surrounds and touches us is composed of molecules of matter. Some of these compounds of matter may be newly produced, while others are years or centuries old. Regardless of the age of the particular compound, they are all composed of elements that have existed since the beginning of the earth. Although they may have changed form throughout that time, most of the elements exist in the same quantity they did when the earth began. Life on earth exists and flourishes because of the use and reuse of these elements. Since there is no new source of these elements, their cycling is critical to life. Plants and animals need at least thirty to forty chemical elements for their growth and development. Three elements—oxygen, carbon and hydrogen—make up ninety-three per cent of the human body, but people also need other elements.

The cycles we’ll be discussing are called “biogeochemical cycles”, “bio” meaning life, “geo” referring to rocks, soils, water and air, and “chemical” referring to the changes that occur as the elements go through these cycles. There are two main types of these cycles: gaseous and sedimentary. In a gaseous cycle, the element is mainly stored in the earth’s atmosphere where it exists as a gas. Carbon and nitrogen are gaseous biogeochemical cycles. Sedimentary cycles have the earth’s crust as the main storage area for their elements, as demonstrated by phosphorus and sulfur.²

The carbon cycle is an important gaseous cycle. Most of the carbon in our world is stored as carbon dioxide, in either the atmosphere or dissolved in the ocean. Plants need carbon dioxide to carry on photosynthesis, a process where the carbon atoms become part of molecules of simple carbohydrates (sugars) and may later be changed to fats, proteins and DNA or more complex carbohydrates. The carbon becomes part of the energy system for ecosystems, since fats and carbohydrates are forms of stored energy. The carbon atoms travel through food chains, with decomposers at any step of the way. To fuel their bodies living things take in oxygen from their environment and use it to oxidize carbohydrates to release energy, the reverse process of photosynthesis. The process in which this energy is made available for growth and other activities is called respiration, and produces carbon dioxide which must be excreted from the body, usually through lungs, gills or leaves.

The process of respiration makes carbon dioxide available for photosynthesis. Many living things build shells of calcium carbonate (a combination of carbon, calcium and oxygen) and when they shed them in growth or when they die these shells may accumulate and build up into rocks. The White Cliffs of Dover is a famous example of this. Carbon in animals might stay in its bones until the bone decays after the animal’s death, or might leave an animal’s body relatively quickly with waste matter. Some carbon in dead bodies of plants or animals becomes trapped and fossilized before decomposure is complete, and can form materials such as peat, coal or oil.³

The nitrogen cycle involves the earth’s atmosphere, which is about 78 per cent nitrogen. Nitrogen is of no use by itself to most living things, and we breathe it in and back out again. However, nitrogen is vital to life when combined with other elements. The nitrogen cycle is largely dependent on bacteria, fungi and blue-green algae which convert the nitrogen from the air into nitrogen compounds. These nitrogen-fixing organisms may live in the soil or on the roots of plants. The nitrogen compounds they generate may be given off into the soil or become available when the nitrogen-fixing organisms die, at which point the nitrogen compounds move through food chains.⁴ Nitrogen is returned to circulation when the bodies of dead plants and animals disintegrate, and when animals excrete uric acid after breaking down proteins in their food. The excreted matter is eventually converted to nitrates after complex bacterial action.⁵ Nitrogen compounds can thus cycle from the soil to plants to bacteria and back to the soil again and again without returning to the atmosphere. However, denitrifying bacteria and fungi break down nitrogen compounds and release nitrogen gas into the atmosphere.

The nitrogen cycle also has a component affected by humans. Industrialists have learned how to take nitrogen gas from the air and “fix” it in compounds that are an important part of fertilizers. It is significant to note that the amount of nitrogen treated this way has been doubling every six years. Since large amounts of these nitrogen compounds tend to wash from the lands where they are used into the waters of our streams, lakes and rivers, they are having an effect the size of which is still being studied. When these waters become highly nitrogen enriched, there is too much plant growth and a loss of oxygen which can result in the death of fish and other animals.

The water cycle is different from the other two cycles we will talk about, because of the fact that water can exist in all three forms of matter: solid, liquid and gas. It can exist naturally at all of the temperatures which occur on earth, and can easily change from one form into another. Interestingly enough, if water did not change form it would all exist today in the oceans or deep in the lithosphere since it responds to the pull of gravity pulling it downward.

When water is in contact with the atmosphere it evaporates, with the rate of evaporation depending on such things as air temperature, water temperature, wind speed and humidity of the air. The amount of water vapor in the air is called the relative humidity and for any given temperature there is a set amount of water that the air can hold. In general, the warmer the air is, the more water it can hold. Relative humidity is an expression of the percentage of water in the air at a given temperature as compared to what it could hold.

As water evaporates it moves upward on currents of warm air until it reaches a temperature where the temperature is low enough that it cannot hold any more water. At this level the water vapor condenses and form clouds. Droplets of the water in the clouds condense on dust particles until they are too large to withstand the force of gravity’s pull and they drop to earth. This precipitation may fall on a place far from the land area where the water initially evaporated, due to wind movement, and so water forms all over the earth are constantly being replenished.

Lakes or oceans are not the only sources from which water enters the air. Water evaporates from everything that is wet. Clothes drying on the line, a swimming pool, puddles after a rainshower, a steamy bathroom after your shower, all of these are sources of water for evaporation. Perhaps the easiest way to observe water evaporation is to boil water in a pan or tea kettle and watch the process. It should be stressed with students that most normal processes of evaporation are not readily observable; there may be evaporation going on in the room around them at the very moment they are talking about it, but normally they will not see anything. They will however see the results: a saucer of water which has dried up after being left out for some time, or the drying of their skin as they calm down to a cooler temperature after running around the track for gym on a hot day.

At this point I would encourage students to pay close attention to the next rain or snowfall. What happens to the water/snow after it is on the ground? This could lead to talking about the water which seeps back into the ground and eventually back to the nearest underground water flow, or to the nearest storm drain, which may take it under city streets to the ocean or another destination. At the same time, students should explore the absorption of water by plants and its expulsion into the air through respiration. And, of course, discussion should include man’s use of water and the way he returns it to his environment.

Spring Component

At this time of the year I will also have students think about some of the ways man pollutes his environment and what effect they think these have. In addition to looking at the effect of the world in general, I will again ask students to personalize the assignment. What things do they observe in their neighborhood? What have they personally done that might cause pollution? They will have a chance to take photographs of examples of the pollution they observe, at the same time that they are taking pictures of Spring for their display. I will encourage the students to get involved in the New Haven clean-up activities such as Park Friends and Clean Sweep, and perhaps we can have a school clean-up day with everyone or volunteers getting involved. Students will also be encouraged to start new bottle ecosystems and experiment with different pollutants, to observe and chart results.

Summer Component

Finally, students will be asked to do some written work for me. I will devise a form where students will : 1. answer questions on specific things they have learned, 2. generalize some of the ideas they have learned about their environment, and 3. discuss what their feelings have been in doing this unit and explain what effect (if any) it may have on the way they interact with their own environment in the future.

Lesson Plans

Lesson Plan #1 (Ongoing)

Possible Student Activities

Lesson #2

Suggested Vocabulary List

Lesson Plan #3

Upon return to the classroom, students will add the water they have taken from the Sound to the aquarium. Schooner, Inc. will attempt to provide living specimens taken from Long Island Sound upon request, but students may also wish to contribute those they have personally found in the Sound.

From here on, possibilities are enormous for classroom participation. Students can chart facts about animals in the aquarium: how they grow, how they interact with each other, what they eat, etc. They can make graphs of the water temperature (which does not need to be controlled by a heater since the Sound varies greatly in temperature). We may want to keep a classroom log of who contributes to the aquarium in any way: adding more water when needed, feeding fish, measuring water for evaporation, and so on.

Students may want to volunteer, or could be assigned, to do reports on various organisms living in the aquarium. Again, the whole idea would be to personalize this experience for the children in terms of organisms living in their environment. Charts, raps, dance,and pictures could all be examples of how students could tell about the animal they’ve studied.

Further lessons could focus on pollution which can/is happening in our area and how it affects the animals in our aquarium.

Notes

Bibliography for Students

Bibliography for Teachers