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UNIT 4

HISTORY OF ECOLOGY

For modern ecologists, ecology can be studied at several levels: population level (individuals of the same species), biocoenosis level (or community of species), ecosystem level, and biosphere level.

The outer layer of the planet Earth can be divided into several compartments: the hydrosphere (or sphere of water), the lithosphere (or sphere of soils and rocks), and the atmosphere (or sphere of the air). The biosphere (or sphere of life), sometimes described as "the fourth envelope", is all living matter on the planet or that portion of the planet occupied by life.

It is thought that life first developed in the hydrosphere, at shallow depths, in the photic zone. (Although recently a competing theory has emerged, that life originated around hydrothermal vents in the deeper ocean.) Multicellular organisms then appeared and colonized benthic zones. Photosynthetic organisms gradually produced the chemically unstable oxygen-rich atmosphere that characterizes our planet. Terrestrial life developed later, after the ozone layer protecting living beings from UV rays formed. Biodiversity is expressed at the ecological level (ecosystem), population level (intraspecific diversity), species level (specific diversity), and genetic level.

The biosphere contains great quantities of elements such as carbon, nitrogen and oxygen. Other elements, such as phosphorus, calcium, and potassium, are also essential to life, yet are present in smaller amounts. At the ecosystem and biosphere levels, there is a continual recycling of all these elements, which alternate between the mineral and organic states.

Water is also exchanged between the hydrosphere, lithosphere, atmosphere and biosphere in regular cycles. The oceans are large tanks, which store water, ensure thermal and climatic stability, as well as the transport of chemical elements thanks to large oceanic currents.

For a better understanding of how the biosphere works, and various dysfunctions related to human activity, American scientists simulated the biosphere in a small-scale model, called Biosphere II.

Notes on the text

outer - зовнішній layer - шар

compartment - відділення portion - частина

extend – простягатися, протягуватися

shallow – обмілина, мілкий, неглубокий, поверховий

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depth - глибина

photic zone - світлова зона vent - отвір

benthic zones - придонні зони

unstable -1) нетвердий, нестійкий 2) нестабільний, мінливий 3) хім. нестійкий (про сполуку)

terrestrial life - земне життя

UV rays - ультрафіолетові промені store - накопичувати

ensure - гарантувати current - потік

tanks - резервуари

simulate - моделювати, відтворювати

alternate - 1)чергувати(ся) 2)переміжний; перемінний, змінний; що чергується

Post-text exercises

I.Answer the questions:

1.How can ecology be studied ?

2.How can the outer layer of the planet Earth can be divided ? 3.Where did the first life develope ?

4.When did terrestrial life develope? 5.What does the biosphere contain?

2.Refute statements or agree with them.

Model 1: Ecology can be studied at one level. Do you agree with me?

No, that is wrong. Ecology can be studied at several levels.

Model 2: Life first developed in the hydrosphere. Do you agree with me?

Yes, you are (quite) right. Life first developed in the hydrosphere.

1.The outer layer of the planet Earth can be divided into several compartments.

2.Photosynthetic organisms gradually produced the chemically unstable carbon-rich atmosphere that characterizes our planet.

3.The biosphere contains great quantities of elements such as carbon, nitrogen and oxygen.

4.Other elements, such as phosphorus, calcium, and potassium, are also essential to life, yet are present in larger amounts.

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