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The Earth`s Interior Structure Reading
The Earth`s Interior Structure Reading

... where m1 and m2 stand for the masses of two objects, d stands for the distance between them, and g stands for the gravitational constant (known from experiments). Because the Earth exerts a certain force on a body (like you) with a certain mass m1 on the Earth’s surface, some 6400 km from its center ...
the annelids and the
the annelids and the

... Ectoderm - The outer layer of tissue in multicellular animals Endoderm - The inner layer of tissue in multicellular animals, forming, for example, the inner epithelium of digestive and respiratory tracts Epitoky - The occurrence of a special reproductive stage in the life cycle of some annelids Gas ...
Quiz 2 - Brooklyn College
Quiz 2 - Brooklyn College

... FOCUS 25. The point on the surface directly above an earthquake occurrence is called the _______. EPICENTER 26. The process of one plate diving under another plate is known as _______. SUBDUCTION ...
April 15, 2017 How Earth Got its Moon
April 15, 2017 How Earth Got its Moon

... Discussion Questions: 1. List as many possible hypotheses as you can think of for how the moon formed and how it ended up in its current orbit around Earth. Discuss the evidence that would support or refute each hypothesis. [Students may have other ideas, or variations or combinations of the ideas ...
THE EVOLUTION OF MOUNTAIN RANGES AND THE ORIGIN AND
THE EVOLUTION OF MOUNTAIN RANGES AND THE ORIGIN AND

... What has changed through the earth's history, however, and Lyell was not aware of, is the relative abundances of different rocks. Some rocks form in much greater abundance today than in the past, others have declined in importance, while a few have ceased forming altogether. The implication is that ...
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File

... C) notochord during at least some period of their life D) glands that produce milk to nourish their offspring E) pharyngeal slits during at least some period of their life ...
Unit 11 Animal Evolution Chp 32 Introduction to
Unit 11 Animal Evolution Chp 32 Introduction to

... That ancestor was most likely a colonial flagellated protist that lived over 700 million years ago in the Precambrian era. This protist was probably related to choanoflagellates, a group that arose about a billion years ago. Modern choanoflagellates are tiny, stalked organisms inhabiting shallow pon ...
The issue is that for a long time scientists where not able
The issue is that for a long time scientists where not able

... through many studies and shows that the relationship between the number of observed species and the area of the sampling is universal and true for all organisms (3). The time hypothesis is divided to ecological and evolutionary components. The first one, states that species exist in particular habit ...
CRCT Review - Chapter 7 Plate Tectonics.
CRCT Review - Chapter 7 Plate Tectonics.

... _____ 10. What hypothesis by Alfred Wegener explains why continents seem to fit together? a. continental spreading c. Wegener’s puzzle b. plate tectonics d. continental drift _____ 11. What did Wegener hypothesize happened to the continents? a. They broke up and re-formed. b. They drifted together t ...
Continental Drift Theory
Continental Drift Theory

... and Scandinavia which are comparable in age and structure. ...
TEKS_Geology
TEKS_Geology

... time scale of these changes and their impact on human society must be understood to make wise decisions concerning the use of the land, water, air, and natural resources. Proper stewardship of Earth will prevent unnecessary degradation and destruction of Earth's subsystems and diminish detrimental i ...
Mesozoic Era - edsc127summer2012
Mesozoic Era - edsc127summer2012

... Precambrian History  Earth’s Atmosphere Evolves • Earth’s original atmosphere was made up of gases similar to those released in volcanic eruptions today—water vapor, carbon dioxide, nitrogen, and several trace gases, but no oxygen. • Later, primary plants evolved that used photosynthesis and releas ...
Biology EOC Review Packet
Biology EOC Review Packet

... Regulation - How organisms control processes - hormones, nervous system. Respiration - How organisms get oxygen from the environment and release carbon dioxide back to the environment and how plants exchange gases. Nutrition - How organisms break down and absorb foods. Synthesis - How organisms buil ...
Biology EOC Review Packet
Biology EOC Review Packet

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... ▫ Proposed that the mid-ocean ridges marked regions where hot magma rose close to the surface ▫ This extrusion pushed the ocean floor away from the ridges like a conveyor belt ▫ In deep trenches (e.g. off the coast of South America and Japan) spreading ocean floor forced down below the thick ...
Teaching Through Science Trade Books MacLaren Stephanie
Teaching Through Science Trade Books MacLaren Stephanie

... environment. The complex cell groupings had specific cells with different purposes. Some multicell organisms turned into plants that produced their own food and others turned into animals. Animals ate other plants or animals in order to survive. Animals developed outer shells for protection and move ...
Life on an Ocean Planet
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...  Phylum Bacillariophyta is made up of diatoms, the most productive phytoplankton.  These primary producers are a widely diverse group.  Between 5,000 to 50,000 species may make up this phylum.  Diatoms are larger than prokaryotes – from 20 to 80 microns across.  They have two-part silicon shell ...
Antarctic Ecology II Penguins and Seals
Antarctic Ecology II Penguins and Seals

... grows longer, the krill slow their living processes as they rise and fall through the water column. They pass through several larval stages of development until they reach maturity over a two-year period. The krill all the while are excreting ammonia into the water, which is used by the phytoplankto ...
Life Science Reveiw
Life Science Reveiw

... water. They spend their first stage of life as larvae in the water. When they become adults, they are flying, winged insects. This is an example of A. mutation. B. evolution. C. metamorphosis. D. parasitism. ...
EVOLUTION - Matrix Education
EVOLUTION - Matrix Education

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Creature Features - Dauphin Island Sea Lab
Creature Features - Dauphin Island Sea Lab

... Life Science M.C.5 Diversity and adaptations of organisms Life Science H.C.6 Behavior of organisms Ocean Literacy Standards Essential Principle 5 The ocean supports a great diversity of life and ecosystems. II. Concepts Invertebrate definition: animals without a backbone. Unfortunately this doesn’t ...
8H Quick Quiz
8H Quick Quiz

... B the high pressure and high temperature inside the Earth. C the low pressure and high temperature inside the Earth. D the low pressure and low temperature inside the Earth. 3 Which of the following statements is true? A Marble is formed from limestone. B Marble is not a metamorphic rock. C Slate is ...
Bio EOC Review Resources - Highline Public Schools
Bio EOC Review Resources - Highline Public Schools

... 5. Describe how a cell can be built from the new molecules mentioned in question 3. 6. Use a model to explain why it requires a different enzyme to break a molecule apart than it did to put the molecule together. What are the molecules that transfer energy for cell processes? ...
Biology I Curriculum Pacing Guide Week Test Chapters/ QC Units
Biology I Curriculum Pacing Guide Week Test Chapters/ QC Units

... maintain their chemical and physical organization. C.5.2 As matter and energy flow through different levels of organization of living systems and between living systems and the physical environment, chemical elements are recombined in different ways by different structures. Matter and energy are con ...
Historical Geology
Historical Geology

... – The date obtained would correspond to the time of crystallization of the mineral, – when it formed in an igneous or metamorphic rock, – and NOT the time that it was deposited as a ...
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Evolutionary history of life



The evolutionary history of life on Earth traces the processes by which living and fossil organisms have evolved since life appeared on the planet, until the present day. Earth formed about 4.5 Ga (billion years ago) and life appeared on its surface within 1 billion years. The similarities between all present-day organisms indicate the presence of a common ancestor from which all known species have diverged through the process of evolution. More than 99 percent of all species, amounting to over five billion species, that ever lived on Earth are estimated to be extinct. Estimates on the number of Earth's current species range from 10 million to 14 million, of which about 1.2 million have been documented and over 86 percent have not yet been described.
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