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Gas is defined as a formless fluid that expands readily to fill any containing vessel, and which can be changed to the liquid or solid state only by the combined effect of increased pressure and decreased temperature.
When the solubility of gases in liquids changes with increasing temperature, it decreases.
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Gas solubility decreases at higher temperatures;
When the solubility of gases in liquids changes with increasing temperature, it decreases.
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Gas solubility in water decreases when the temperature goes up.
When the solubility of gases in liquids changes with increasing temperature, it decreases.
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Gas solubility is exothermic, so solubility of gases decreases with increasing temperature.
When the solubility of gases in liquids changes with increasing temperature, it decreases.
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Gases, however, decrease in solubility with an increase in temperature.
When the solubility of gases in liquids changes with increasing temperature, it decreases.
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In general, the solubility of gases decreases with increasing temperature.
When the solubility of gases in liquids changes with increasing temperature, it decreases.
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The solubility of a solid in water generally increases with temperature while the solubility of a gas decreases with temperature.
When the solubility of gases in liquids changes with increasing temperature, it decreases.
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The solubility of gases in liquids decreases with an increase in temperature.
When the solubility of gases in liquids changes with increasing temperature, it decreases.
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This voltage will increase and decrease with temperature changes.
When the solubility of gases in liquids changes with increasing temperature, it decreases.
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liquid changes into solid by decrease in temperature.
When the solubility of gases in liquids changes with increasing temperature, it decreases.
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Carbon Dioxide and water vapour are excreted from the lungs by a combination of exhalation and diffusion (explained on the respiration page).
Ccarbon dioxide and water vapor that is produced by cellular respiration is released through exhalation.
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The respiratory system eliminates water vapor and carbon dioxide through exhalation (the process of breathing out).
Ccarbon dioxide and water vapor that is produced by cellular respiration is released through exhalation.
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Diffusion tests (abbreviated DL,CO or TL,CO) determine how well your lungs take in air and move the oxygen contained in this air into the bloodstream.
Oxygen is transferred into the bloodstream by simple diffusion.
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Hypoxic hypoxia occurs when not enough oxygen is in the air or when decreasing atmospheric pressures prevent the diffusion of O 2 from the lungs to the bloodstream.
Oxygen is transferred into the bloodstream by simple diffusion.
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Oxygen is transferred from the atmosphere into the surface waters by diffusion Factors Affecting Dissolved Oxygen Levels The amount of oxygen available to estuarine organisms is affected by salinity and temperature.
Oxygen is transferred into the bloodstream by simple diffusion.
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Oxygen is transferred from the atmosphere into the surface waters by diffusion and the aerating action of the wind.
Oxygen is transferred into the bloodstream by simple diffusion.
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Oxygen is transported from the alveoli to the pulmonary bloodstream by passive diffusion and is made available to tissues.
Oxygen is transferred into the bloodstream by simple diffusion.
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Oxygen molecules pass from the air space of an alveoli into its capillary bed via simple diffusion -- oxygen concentration in the air is greater than it is in the bloodstream.
Oxygen is transferred into the bloodstream by simple diffusion.
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The circulation then transfers oxygen rich blood to the tissues where it diffuses by simple concentration gradients into the tissues.
Oxygen is transferred into the bloodstream by simple diffusion.
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Theoretically, oxygen delivered by diffusion may be more available, and more readily off-loaded from the bloodstream, than hemoglobin-delivered oxygen.
Oxygen is transferred into the bloodstream by simple diffusion.
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air diffusion The transfer of air to a liquid through an oxygen-transfer device.
Oxygen is transferred into the bloodstream by simple diffusion.
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A current study in cooperation with the NRP is assessing the transport of sediment and associated trace metals.
Sediment is transported by currents.
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Sediment is transported along the coast in the direction of the prevailing current (longshore drift).
Sediment is transported by currents.
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Sediments Transported and Redeposited in Low Areas The currents generated by crustal uplift eroded the areas surrounding the Shields, transported the sediments and deposited the sediment load in deeper waters.
Sediment is transported by currents.
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Some of these instruments are pressure gauges, current meters, and sediment transport sensors.
Sediment is transported by currents.
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Such a current can transport considerable amounts of sediment along a coast.
Sediment is transported by currents.
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The focus of our current research is erosion and transport of sediment and phosphorus to the lake.
Sediment is transported by currents.
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Tidal currents are responsible for resuspension of sediment and transport of this sediment seaward (Noble and Gelfenbaum, 1990;
Sediment is transported by currents.
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Transportation of sediment, mixing current, and other phenomena.
Sediment is transported by currents.
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Water flow (current) is the driving force behind such sediment transport.
Sediment is transported by currents.
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137 Cs (half-life 30 years) became the first long-lived isotope related to nuclear fallout intensively studied in aquatic organisms.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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A large nuclear-powered ship with more than one reactor, designed for years of service without refueling, can have nearly as much long-lived radioactivity (e.g., 90Sr) on board as an operating commercial reactor (Rickover, 1980).
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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According to nuclear scientists, this can be as long as ten thousand to a hundred thousand years.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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Because cosmogenic isotopes have long half-lives (anywhere from thousands to millions of years), scientists find them useful for geologic dating.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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Because it has isotopes with very long half-lives, it is of particular concern in the context of designing confinement facilities that can last for thousands of years.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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By 60 years, the initial short-lived isotopes, including cobalt-60, will have decayed to background levels.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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For years the processes of formation and decay of the long-lived nuclear isomers were studied by A.V.Davydov et al.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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In one year of operation of a nuclear reactor, long-lived fission products that have been manufactured will not have decayed significantly.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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In the end (after three years' use), 100 kg of spent nuclear fuel from a VVER-1000 reactor will contain 740 g of long-lived plutonium isotopes (emitting alfa radiation), and some 4 kg of other long-lived trans-uranium radio nucleides.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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Isotopes with long half-lives such as uranium -238 (5 billion year halflife) decay into daughter products with shorter halflives, such as radium -226 and -228, which exhibit the higher activity levels that can be of great concern for human health.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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It decays via alpha and beta emission through a series of short-lived progeny, 218 Po, 214 Pb, 214 Bi, 214 Po to a moderately long-lived (21 years) isotope of lead;
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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Long-lived isotopes will have ample time to spread across the Earth and concentrate in food chains for thousands of years.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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Some of these isotopes have half-lives of tens of thousands of years, and therefore require long-term isolation.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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Strontium 90, with a half-life of twenty-eight years, is a long-lived isotope.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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The ages of Earth and Moon rocks and of meteorites are measured by the decay of long-lived radioactive isotopes of elements that occur naturally in rocks and minerals and that decay with half lives of 700 million to more than 100 billion years to stable isotopes of other elements.
The long-lived isotopes require thousands of years to decay to a safe level in a nuclear reactor.
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A 24-hour period during which the earth completes one rotation.
It takes 24 hours for the earth to make a complete rotation of its axis.
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A day is 86,400 seconds or 24 hours long which is the time it takes Earth to rotate once on its axis.
It takes 24 hours for the earth to make a complete rotation of its axis.
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A day, the time it takes for the Earth to rotate completely, takes 24 hours.
It takes 24 hours for the earth to make a complete rotation of its axis.
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Earth rotates once on its axis about every 24 hours.
It takes 24 hours for the earth to make a complete rotation of its axis.
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Earth's rotation on its axis makes a day at 24 hours.
It takes 24 hours for the earth to make a complete rotation of its axis.
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Every 24 hours our earth makes a complete rotation on its axis.
It takes 24 hours for the earth to make a complete rotation of its axis.
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Every 24 hours the earth makes one complete turn, or rotation .
It takes 24 hours for the earth to make a complete rotation of its axis.
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For example, the Earth completes one rotation about its axis about every 24 hours, but it completes one revolution around the Sun about every 365 days.
It takes 24 hours for the earth to make a complete rotation of its axis.
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It is the rotation of the earth on its axis that determined a 24-hour day.
It takes 24 hours for the earth to make a complete rotation of its axis.
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It takes 24 hours for our planet to rotate completely.
It takes 24 hours for the earth to make a complete rotation of its axis.
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It takes Earth 23.439 hours to complete a rotation on its axis, and roughly 365.26 days to complete an orbit around the sun.
It takes 24 hours for the earth to make a complete rotation of its axis.
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It takes approximately 24 ½ hours to complete a full rotation on its axis, making its day almost the same as Earth's.
It takes 24 hours for the earth to make a complete rotation of its axis.
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It takes the Earth 24 hours to rotate around its axis.
It takes 24 hours for the earth to make a complete rotation of its axis.
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It takes the Earth one day (answer A) or 24 hours to make one rotation on its axis.
It takes 24 hours for the earth to make a complete rotation of its axis.
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RA for the entire celestial sphere is divided into 24 hours ( 24h ), the amount of time it takes for the Earth to complete a full rotatation on it's axis.
It takes 24 hours for the earth to make a complete rotation of its axis.
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Since Homeland is older than Earth, it accordingly rotates on its axis much more slowly, which makes the day twenty-seven hours long by my wrist watch, but thirty-two hours long by Homelander reckoning.
It takes 24 hours for the earth to make a complete rotation of its axis.
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Since our planet rotates, it appears to a stationary observer on Earth that a gyroscope's axis is completing a full rotation once every 24 hours.
It takes 24 hours for the earth to make a complete rotation of its axis.
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The Earth is also rotating on its axis every 24 hours, and there are good reasons for believing that the Earth really does rotate within its gravitational field;
It takes 24 hours for the earth to make a complete rotation of its axis.
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The Earth makes one complete revolution about its axis in an average of 24 hours, so that any position on the Earth is in direct line with the Sun every 24 hours.
It takes 24 hours for the earth to make a complete rotation of its axis.
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The Earth makes one rotation around its axis in every 24-hour period, giving it a surface speed at the equator of 1,688 kilometres per hour.
It takes 24 hours for the earth to make a complete rotation of its axis.
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The earth rotates on its axis and this takes 24 hours.
It takes 24 hours for the earth to make a complete rotation of its axis.
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The earth takes 23 hours and 56 minutes of solar time to make one rotation an its axis with respect to the stars (a sidereal day).
It takes 24 hours for the earth to make a complete rotation of its axis.
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The earth's rotation is 24 hours.
It takes 24 hours for the earth to make a complete rotation of its axis.
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The earths revolution about its own axis takes 24 hours.
It takes 24 hours for the earth to make a complete rotation of its axis.
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The speed of Earth's rotation on its axis, completing one turn every 24 hours, means that the sun warms the planet evenly.
It takes 24 hours for the earth to make a complete rotation of its axis.
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This means that it takes 24 hours for the Earth to spin, or rotate, completely around one time.
It takes 24 hours for the earth to make a complete rotation of its axis.
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Use a model of Earth to demonstrate that Earth rotates on its axis once every 24 hours to produce the night and day cycle.
It takes 24 hours for the earth to make a complete rotation of its axis.
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We all experience 24-hour days because on this earth it takes that long for the earth to rotate on its axis and nobody can speed it up.
It takes 24 hours for the earth to make a complete rotation of its axis.
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All mammals suckle their young, have three middle-ear bones, and have hair.
The mammalian middle ear has three bones.
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Another basic difference is that all mammals have three bones in their middle ear (hammer, anvil, and stirrup).
The mammalian middle ear has three bones.
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In reptiles, for instance, the lower jaw consists of several bones and the three bones equivalent to the mammalian middle ear are attached to the jaw and the cranium.
The mammalian middle ear has three bones.
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Like their ancient relatives, all living mammals have three middle ear bones.
The mammalian middle ear has three bones.
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Mammal ears are relatively complex, the middle ear containing three bones, as opposed to only one bone in the middle ear of reptiles and birds.
The mammalian middle ear has three bones.
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Mammals have three bones in the middle ear and a cochlea in the inner ear.
The mammalian middle ear has three bones.
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The condition in which the middle ear has three bones linking the ear drum to the middle ear is what defines mammals.
The mammalian middle ear has three bones.
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The middle ear includes the ear drum, three middle ear bones (ossicles) and the eustachian tube.
The mammalian middle ear has three bones.
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The middle of a chain of three bones of the mammalian middle ear.
The mammalian middle ear has three bones.
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Two characteristics of mammals that are at least sometimes preserved in the fossil record are (1) the mammalian middle ear contains a chain of three bones, the malleus, incus, and stapes;
The mammalian middle ear has three bones.
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have three inner ear bones
The mammalian middle ear has three bones.
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it's those three bones in the middle ear.
The mammalian middle ear has three bones.
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1 gram of sugar provides 4 Kcal of energy.
One gram of sugar or starch provides 4 calories of energy.
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A 4-gram serving is said to have about the same sweetness as 8 grams of sugar but only one-fifth the calories.
One gram of sugar or starch provides 4 calories of energy.
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A bag of sugar in the same store states that one serving weighs 4 grams and has 15 calories.
One gram of sugar or starch provides 4 calories of energy.
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A simple way to understand the principle behind a comparison of starches, fats and protein is to realize that all carbohydrates have 4 calories per gram, whether sugar or a starch.
One gram of sugar or starch provides 4 calories of energy.
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One (food) Calorie is equal to 4.19kJ, and to give you an idea of scale, common granulated sugar has an energy content of about 4 Calories per gram or 19.76 kJ per gram.
One gram of sugar or starch provides 4 calories of energy.
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One gram of proteins provides 4 Calories of energy.
One gram of sugar or starch provides 4 calories of energy.
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Protein provides about 4 calories per gram.
One gram of sugar or starch provides 4 calories of energy.
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Remember that one gram of protein is equal to 4 calories.
One gram of sugar or starch provides 4 calories of energy.
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Since sugar carbohydrates provide 4 calories per gram, you can have up to 30 grams of total sugar based on a 1,200-calorie diet.
One gram of sugar or starch provides 4 calories of energy.
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Sugars and starches have 4 calories per gram, while fat has 9 calories per gram.
One gram of sugar or starch provides 4 calories of energy.
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Sugars and starches provide 4 calories per gram of carbohydrate.
One gram of sugar or starch provides 4 calories of energy.
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They may be surprised to know that sugar contains 4 calories to the gram while bread has only 2 calories per gram.
One gram of sugar or starch provides 4 calories of energy.
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and 33% to 66% for lipids, (taking into account that one gram of fat provides 9 kcal of energy as opposed to 4 kcal for one gram of sugar or protein).
One gram of sugar or starch provides 4 calories of energy.
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Amphibians and most living reptiles have a three-chambered heart, which has usually been regarded as inferior to the four-chambered heart of living mammals and birds.
There are three chambers in a reptiles heart.
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An amphibian's heart has three chambers.
There are three chambers in a reptiles heart.
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