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Mass extinction (Permian-Triassic- Extinction) - The Evolutionary Theory on Extinction
Extinction happens. But what's evolution got to do with it?
Mass extinctions. Dinosaurs and the first mammals. Saving an unspoiled forest near Bangkok. Biological invaders in the Hawaiian Islands. Using a beneficial insect to control weeds in North Dakota.
"Extinction is the termination of a species." At least 95 per cent of all species that have ever lived are now extinct. Extinction is normal,
-
Araguainha crater - Video Learning - WizScience.com
The "Araguainha Crater" or "Araguainha Dome" is an impact crater on the border of Mato Grosso and Goiás states, Brazil, between the villages of Araguainha and Ponte Branca. With a diameter of 40 km, it is the second largest known impact crater in South America, and possibly the oldest one.
The crater has most recently been dated to 254.7 ± 2.5 million years ago, when the region was probably a
-
The History of Life on Earth - Crash Course Ecology #1
With a solid understanding of biology on the small scale under our belts, it's time for the long view - for the next twelve weeks, we'll be learning how the ...
-
Timeline of the development of tectonophysics (after 1952) - Video Learning - WizScience.com
The evolution of tectonophysics is closely linked to the history of the continental drift and plate tectonics hypotheses. The continental drift/ Airy-Heiskanen isostasy hypothesis had many flaws and scarce data. The fixist/ Pratt-Hayford isostasy, the contracting Earth and the expanding Earth concepts had many flaws as well.
The idea of continents with a permanent location, the geosyncline theo
-
Scotland's geology -- a fly-through from the Solway Firth to Stirling
This movie, compiled in Virtalis GeoVisionary, begins over the Solway Firth and flies over to Carlisle. The pinks and yellow are Permo-Triassic rocks and the...
-
Earth's Natural Geographic History / Palaeogeography From Ediacaran to Quarternary / Present.
Hadean: Cryptic Basin Groups Nectarian Lower Imbrian Archaen / Archaeozoic: Eoarchaen Palaeoarchaen Mesoarchaen Neoarchaen Proterozoic: Siderian Rhyacian Oro...
-
Earth History1
Paleozoic (Silurian, Devonian, Carboniferous, Permian); Mesozoic (Triassic, Jurassic, Cretaceous), Cenozoic (Eocine, Pleistocene, Mesozoic) in 544 million ye...
-
Animal Armageddon The Great Dying - Episode 5
The Permian--Triassic extinction event, informally known as the Great Dying, was an extinction event that occurred 252 million years ago, forming the boundar...
-
How to Pronounce Permian
Learn how to say Permian correctly with EmmaSaying's "how do you pronounce" free tutorials.
Definition of Permian (oxford dictionary):
adjective
([sometimes p-]) designating or of the sixth and last geologic period of the Paleozoic Era, characterized by the formation of Pangea, glaciation in the Southern Hemisphere, development of mountains, esp. in the Appalachians, and an increase in the diver
-
Continental drift
Continental drift is the movement of the Earth's continents relative to each other by appearing to drift across the ocean bed. The speculation that continent...
-
Nelle foreste del Carbonifero
Sequenza ad uso didattico tratta dalla serie "The making of planet Earth", 2001. Tutti i diritti sono riservati a BBC.
-
Nature Documentary: Australia's First 4 Billion Years EP02 Life Explodes english subtitles
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Visit my other documentary channels english su
Mass extinction (Permian-Triassic- Extinction) - The Evolutionary Theory on Extinction
Extinction happens. But what's evolution got to do with it?
Mass extinctions. Dinosaurs and the first mammals. Saving an unspoiled forest near Bangkok. Biologic...
Extinction happens. But what's evolution got to do with it?
Mass extinctions. Dinosaurs and the first mammals. Saving an unspoiled forest near Bangkok. Biological invaders in the Hawaiian Islands. Using a beneficial insect to control weeds in North Dakota.
"Extinction is the termination of a species." At least 95 per cent of all species that have ever lived are now extinct. Extinction is normal, and is happening all the time, at the rate of a few species per year.
We watch various animals foraging for food, and a lioness bringing down her prey. "The extinction of old species that can no longer adapt or compete creates opportunities for new species that can--in an endless cycle," the narrator says. "So evolution and extinction are in balance. But what happens when a planet-wide catastrophe strikes and a great dying begins?"
The scene changes dramatically--to lightning, volcanoes, and fire. Five times in the last half-billion years, we are told, mass extinctions wiped out most species alive at the time. As the smoke clears, we see Peter Ward driving through South Africa to investigate the greatest of these mass extinctions--the one that occurred at the end of the geological period known as the Permian. He stops at an old abandoned farmhouse, and sees from the tombstones in a nearby graveyard that the family that used to live there died within a five-year period about a century ago. "So a hundred years [ago], these people were just wiped off the face of the Earth, and we have no idea what killed them," says Ward. "And if that's the case, how am I going to figure out what killed animals that lived in those hills [gesturing], the fossils of which we have from 250 million years ago?"
In the rocks of those hills, Ward finds evidence that a great catastrophe occurred at the end of the Permian. "So catastrophic was that mass extinction," says Ward, "that even the small creatures have died out. It's not just the mighty, it's the meek." An animation shows us what might--or might not--have caused the Permian extinction. "When species died, they didn't die alone," says the narrator. "The collapse of one helped bring down the others."
Ward explains: "You could almost analogize that to a house of cards. Each species props up another, in a sense." We watch as a huge house of playing-cards teeters in front of us. Ward continues: "Because the creature that you eat is that card that is sitting under you that gives you your energy. Now let's pretend that we start kicking out card after card after card--and that's what a mass extinction does, isn't it? It starts knocking out a species here, it knocks out a species there, but pretty soon lots of species are gone. And it's not just the disappearance of species now--the whole house of cards falls down."
Not everything died in the Permian extinction, however. Ward holds up the skull of a mammal-like reptile. He says that the few lineages that survived the extinction "start evolving, because the world is empty, and empty worlds really begat [a] tremendous amount of evolutionary diversifications."
But how do empty worlds beget new species, exactly? Mass extinction may be an important feature of the history of life; but the question is, how did living things diversify afterwards? That is the question Darwin's theory is supposed to answer, but the fact of extinction doesn't help us. Species go extinct, and new ones take their places. This may come as a surprise to people who believe that species never go extinct (if, in fact, there are such people); but how does it provide evidence for Darwinian evolution?
What Really
happen to the Dinosaurs?
wn.com/Mass Extinction (Permian Triassic Extinction) The Evolutionary Theory On Extinction
Extinction happens. But what's evolution got to do with it?
Mass extinctions. Dinosaurs and the first mammals. Saving an unspoiled forest near Bangkok. Biological invaders in the Hawaiian Islands. Using a beneficial insect to control weeds in North Dakota.
"Extinction is the termination of a species." At least 95 per cent of all species that have ever lived are now extinct. Extinction is normal, and is happening all the time, at the rate of a few species per year.
We watch various animals foraging for food, and a lioness bringing down her prey. "The extinction of old species that can no longer adapt or compete creates opportunities for new species that can--in an endless cycle," the narrator says. "So evolution and extinction are in balance. But what happens when a planet-wide catastrophe strikes and a great dying begins?"
The scene changes dramatically--to lightning, volcanoes, and fire. Five times in the last half-billion years, we are told, mass extinctions wiped out most species alive at the time. As the smoke clears, we see Peter Ward driving through South Africa to investigate the greatest of these mass extinctions--the one that occurred at the end of the geological period known as the Permian. He stops at an old abandoned farmhouse, and sees from the tombstones in a nearby graveyard that the family that used to live there died within a five-year period about a century ago. "So a hundred years [ago], these people were just wiped off the face of the Earth, and we have no idea what killed them," says Ward. "And if that's the case, how am I going to figure out what killed animals that lived in those hills [gesturing], the fossils of which we have from 250 million years ago?"
In the rocks of those hills, Ward finds evidence that a great catastrophe occurred at the end of the Permian. "So catastrophic was that mass extinction," says Ward, "that even the small creatures have died out. It's not just the mighty, it's the meek." An animation shows us what might--or might not--have caused the Permian extinction. "When species died, they didn't die alone," says the narrator. "The collapse of one helped bring down the others."
Ward explains: "You could almost analogize that to a house of cards. Each species props up another, in a sense." We watch as a huge house of playing-cards teeters in front of us. Ward continues: "Because the creature that you eat is that card that is sitting under you that gives you your energy. Now let's pretend that we start kicking out card after card after card--and that's what a mass extinction does, isn't it? It starts knocking out a species here, it knocks out a species there, but pretty soon lots of species are gone. And it's not just the disappearance of species now--the whole house of cards falls down."
Not everything died in the Permian extinction, however. Ward holds up the skull of a mammal-like reptile. He says that the few lineages that survived the extinction "start evolving, because the world is empty, and empty worlds really begat [a] tremendous amount of evolutionary diversifications."
But how do empty worlds beget new species, exactly? Mass extinction may be an important feature of the history of life; but the question is, how did living things diversify afterwards? That is the question Darwin's theory is supposed to answer, but the fact of extinction doesn't help us. Species go extinct, and new ones take their places. This may come as a surprise to people who believe that species never go extinct (if, in fact, there are such people); but how does it provide evidence for Darwinian evolution?
What Really
happen to the Dinosaurs?
- published: 10 May 2015
- views: 0
Araguainha crater - Video Learning - WizScience.com
The "Araguainha Crater" or "Araguainha Dome" is an impact crater on the border of Mato Grosso and Goiás states, Brazil, between the villages of Araguainha and P...
The "Araguainha Crater" or "Araguainha Dome" is an impact crater on the border of Mato Grosso and Goiás states, Brazil, between the villages of Araguainha and Ponte Branca. With a diameter of 40 km, it is the second largest known impact crater in South America, and possibly the oldest one.
The crater has most recently been dated to 254.7 ± 2.5 million years ago, when the region was probably a shallow sea. The margins of error of this date overlap the time of the Permian–Triassic extinction event, one of the largest mass extinction events in Earth's history. The impact punched through Paleozoic sedimentary units belonging to the Paraná Basin formations, and exposed the underlying Ordovician granite basement rocks. It is estimated that the crater was initially 24 km wide and 2.4 km deep, which then widened to 40 km as its walls subsided inwards.
Araguainha is a complex crater with annular and radial faults, exposed to the surface and eroded, crossed by the Araguaia River. The crater has an uplifted central core, shaped like an elliptical basin, consisting of exposed basement granite. Surrounding this core is a ring of shocked granite and overlying breccias; then another ring of ridges and mountains, 6.5 km in diameter and up to 150 m high, consisting of folded and steeply tilted Devonian sandstones. This central region is surrounded by an annular depression floored by rocks from Devonian and Carboniferous sandstone formations. The outer rim of the crater consists of remnants of semi-circular grabens in highly deformed Permo-Carboniferous sediments. Evidences of impact origin include shatter cones, impact breccias, and shocked quartz.
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Disclaimer: This video is for your information only. The author or publisher does not guarantee the accuracy of the content presented in this video. USE AT YOUR OWN RISK.
Background Music:
"The Place Inside" by Silent Partner (royalty-free) from YouTube Audio Library.
This video uses material/images from https://en.wikipedia.org/wiki/Araguainha+crater, which is released under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . This video is licensed under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . To reuse/adapt the content in your own work, you must comply with the license terms.
wn.com/Araguainha Crater Video Learning Wizscience.Com
The "Araguainha Crater" or "Araguainha Dome" is an impact crater on the border of Mato Grosso and Goiás states, Brazil, between the villages of Araguainha and Ponte Branca. With a diameter of 40 km, it is the second largest known impact crater in South America, and possibly the oldest one.
The crater has most recently been dated to 254.7 ± 2.5 million years ago, when the region was probably a shallow sea. The margins of error of this date overlap the time of the Permian–Triassic extinction event, one of the largest mass extinction events in Earth's history. The impact punched through Paleozoic sedimentary units belonging to the Paraná Basin formations, and exposed the underlying Ordovician granite basement rocks. It is estimated that the crater was initially 24 km wide and 2.4 km deep, which then widened to 40 km as its walls subsided inwards.
Araguainha is a complex crater with annular and radial faults, exposed to the surface and eroded, crossed by the Araguaia River. The crater has an uplifted central core, shaped like an elliptical basin, consisting of exposed basement granite. Surrounding this core is a ring of shocked granite and overlying breccias; then another ring of ridges and mountains, 6.5 km in diameter and up to 150 m high, consisting of folded and steeply tilted Devonian sandstones. This central region is surrounded by an annular depression floored by rocks from Devonian and Carboniferous sandstone formations. The outer rim of the crater consists of remnants of semi-circular grabens in highly deformed Permo-Carboniferous sediments. Evidences of impact origin include shatter cones, impact breccias, and shocked quartz.
Wiz Science™ is "the" learning channel for children and all ages.
SUBSCRIBE TODAY
Disclaimer: This video is for your information only. The author or publisher does not guarantee the accuracy of the content presented in this video. USE AT YOUR OWN RISK.
Background Music:
"The Place Inside" by Silent Partner (royalty-free) from YouTube Audio Library.
This video uses material/images from https://en.wikipedia.org/wiki/Araguainha+crater, which is released under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . This video is licensed under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . To reuse/adapt the content in your own work, you must comply with the license terms.
- published: 04 Sep 2015
- views: 0
The History of Life on Earth - Crash Course Ecology #1
With a solid understanding of biology on the small scale under our belts, it's time for the long view - for the next twelve weeks, we'll be learning how the ......
With a solid understanding of biology on the small scale under our belts, it's time for the long view - for the next twelve weeks, we'll be learning how the ...
wn.com/The History Of Life On Earth Crash Course Ecology 1
With a solid understanding of biology on the small scale under our belts, it's time for the long view - for the next twelve weeks, we'll be learning how the ...
- published: 05 Nov 2012
- views: 448227
-
author: CrashCourse
Timeline of the development of tectonophysics (after 1952) - Video Learning - WizScience.com
The evolution of tectonophysics is closely linked to the history of the continental drift and plate tectonics hypotheses. The continental drift/ Airy-Heiskanen ...
The evolution of tectonophysics is closely linked to the history of the continental drift and plate tectonics hypotheses. The continental drift/ Airy-Heiskanen isostasy hypothesis had many flaws and scarce data. The fixist/ Pratt-Hayford isostasy, the contracting Earth and the expanding Earth concepts had many flaws as well.
The idea of continents with a permanent location, the geosyncline theory, the Pratt-Hayford isostasy, the extrapolation of the age of the Earth by Lord Kelvin as a black body cooling down, the contracting Earth, the Earth as a solid and crystalline body, is one school of thought. A lithosphere creeping over the asthenosphere is a logical consequence of an Earth with internal heat by radioactivity decay, the Airy-Heiskanen isostasy, thrust faults and Niskanen's mantle viscosity determinations.
Many concepts had to be changed:
The shifting and evolution of knowledge and concepts, were from:
Actually, there were two main "schools of thought" that pushed plate tectonics forward:
Wegener's continental drift hypotheses is a logical consequence of: the theory of thrusting , the isostasy, the continents forms resulting from the supercontinent Gondwana break up, the past and present-day life forms on both sides of the Gondwana continent margins, and the Permo-Carboniferous moraine deposits in South Gondwana.
Wiz Science™ is "the" learning channel for children and all ages.
SUBSCRIBE TODAY
Disclaimer: This video is for your information only. The author or publisher does not guarantee the accuracy of the content presented in this video. USE AT YOUR OWN RISK.
Background Music:
"The Place Inside" by Silent Partner (royalty-free) from YouTube Audio Library.
This video uses material/images from https://en.wikipedia.org/wiki/Timeline+of+the+development+of+tectonophysics+(after+1952), which is released under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . This video is licensed under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . To reuse/adapt the content in your own work, you must comply with the license terms.
Wiz Science™ is "the" learning channel for children and all ages.
SUBSCRIBE TODAY
Disclaimer: This video is for your information only. The author or publisher does not guarantee the accuracy of the content presented in this video. USE AT YOUR OWN RISK.
Background Music:
"The Place Inside" by Silent Partner (royalty-free) from YouTube Audio Library.
This video uses material/images from https://en.wikipedia.org/wiki/Timeline+of+the+development+of+tectonophysics+(after+1952), which is released under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . This video is licensed under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . To reuse/adapt the content in your own work, you must comply with the license terms.
wn.com/Timeline Of The Development Of Tectonophysics (After 1952) Video Learning Wizscience.Com
The evolution of tectonophysics is closely linked to the history of the continental drift and plate tectonics hypotheses. The continental drift/ Airy-Heiskanen isostasy hypothesis had many flaws and scarce data. The fixist/ Pratt-Hayford isostasy, the contracting Earth and the expanding Earth concepts had many flaws as well.
The idea of continents with a permanent location, the geosyncline theory, the Pratt-Hayford isostasy, the extrapolation of the age of the Earth by Lord Kelvin as a black body cooling down, the contracting Earth, the Earth as a solid and crystalline body, is one school of thought. A lithosphere creeping over the asthenosphere is a logical consequence of an Earth with internal heat by radioactivity decay, the Airy-Heiskanen isostasy, thrust faults and Niskanen's mantle viscosity determinations.
Many concepts had to be changed:
The shifting and evolution of knowledge and concepts, were from:
Actually, there were two main "schools of thought" that pushed plate tectonics forward:
Wegener's continental drift hypotheses is a logical consequence of: the theory of thrusting , the isostasy, the continents forms resulting from the supercontinent Gondwana break up, the past and present-day life forms on both sides of the Gondwana continent margins, and the Permo-Carboniferous moraine deposits in South Gondwana.
Wiz Science™ is "the" learning channel for children and all ages.
SUBSCRIBE TODAY
Disclaimer: This video is for your information only. The author or publisher does not guarantee the accuracy of the content presented in this video. USE AT YOUR OWN RISK.
Background Music:
"The Place Inside" by Silent Partner (royalty-free) from YouTube Audio Library.
This video uses material/images from https://en.wikipedia.org/wiki/Timeline+of+the+development+of+tectonophysics+(after+1952), which is released under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . This video is licensed under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . To reuse/adapt the content in your own work, you must comply with the license terms.
Wiz Science™ is "the" learning channel for children and all ages.
SUBSCRIBE TODAY
Disclaimer: This video is for your information only. The author or publisher does not guarantee the accuracy of the content presented in this video. USE AT YOUR OWN RISK.
Background Music:
"The Place Inside" by Silent Partner (royalty-free) from YouTube Audio Library.
This video uses material/images from https://en.wikipedia.org/wiki/Timeline+of+the+development+of+tectonophysics+(after+1952), which is released under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . This video is licensed under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . To reuse/adapt the content in your own work, you must comply with the license terms.
- published: 11 Sep 2015
- views: 0
Scotland's geology -- a fly-through from the Solway Firth to Stirling
This movie, compiled in Virtalis GeoVisionary, begins over the Solway Firth and flies over to Carlisle. The pinks and yellow are Permo-Triassic rocks and the......
This movie, compiled in Virtalis GeoVisionary, begins over the Solway Firth and flies over to Carlisle. The pinks and yellow are Permo-Triassic rocks and the...
wn.com/Scotland's Geology A Fly Through From The Solway Firth To Stirling
This movie, compiled in Virtalis GeoVisionary, begins over the Solway Firth and flies over to Carlisle. The pinks and yellow are Permo-Triassic rocks and the...
- published: 23 Aug 2011
- views: 3954
-
author: bgschannel
Earth's Natural Geographic History / Palaeogeography From Ediacaran to Quarternary / Present.
Hadean: Cryptic Basin Groups Nectarian Lower Imbrian Archaen / Archaeozoic: Eoarchaen Palaeoarchaen Mesoarchaen Neoarchaen Proterozoic: Siderian Rhyacian Oro......
Hadean: Cryptic Basin Groups Nectarian Lower Imbrian Archaen / Archaeozoic: Eoarchaen Palaeoarchaen Mesoarchaen Neoarchaen Proterozoic: Siderian Rhyacian Oro...
wn.com/Earth's Natural Geographic History Palaeogeography From Ediacaran To Quarternary Present.
Hadean: Cryptic Basin Groups Nectarian Lower Imbrian Archaen / Archaeozoic: Eoarchaen Palaeoarchaen Mesoarchaen Neoarchaen Proterozoic: Siderian Rhyacian Oro...
Earth History1
Paleozoic (Silurian, Devonian, Carboniferous, Permian); Mesozoic (Triassic, Jurassic, Cretaceous), Cenozoic (Eocine, Pleistocene, Mesozoic) in 544 million ye......
Paleozoic (Silurian, Devonian, Carboniferous, Permian); Mesozoic (Triassic, Jurassic, Cretaceous), Cenozoic (Eocine, Pleistocene, Mesozoic) in 544 million ye...
wn.com/Earth History1
Paleozoic (Silurian, Devonian, Carboniferous, Permian); Mesozoic (Triassic, Jurassic, Cretaceous), Cenozoic (Eocine, Pleistocene, Mesozoic) in 544 million ye...
- published: 02 Aug 2009
- views: 370
-
author: Jegadeli
Animal Armageddon The Great Dying - Episode 5
The Permian--Triassic extinction event, informally known as the Great Dying, was an extinction event that occurred 252 million years ago, forming the boundar......
The Permian--Triassic extinction event, informally known as the Great Dying, was an extinction event that occurred 252 million years ago, forming the boundar...
wn.com/Animal Armageddon The Great Dying Episode 5
The Permian--Triassic extinction event, informally known as the Great Dying, was an extinction event that occurred 252 million years ago, forming the boundar...
How to Pronounce Permian
Learn how to say Permian correctly with EmmaSaying's "how do you pronounce" free tutorials.
Definition of Permian (oxford dictionary):
adjective
([sometimes p...
Learn how to say Permian correctly with EmmaSaying's "how do you pronounce" free tutorials.
Definition of Permian (oxford dictionary):
adjective
([sometimes p-]) designating or of the sixth and last geologic period of the Paleozoic Era, characterized by the formation of Pangea, glaciation in the Southern Hemisphere, development of mountains, esp. in the Appalachians, and an increase in the diversity of land plants and animals
http://www.emmasaying.com/
Take a look at my comparison tutorials here: https://www.youtube.com/user/EmmaSaying/videos?view=1
Subscribe to my channel here: https://www.youtube.com/user/EmmaSaying
wn.com/How To Pronounce Permian
Learn how to say Permian correctly with EmmaSaying's "how do you pronounce" free tutorials.
Definition of Permian (oxford dictionary):
adjective
([sometimes p-]) designating or of the sixth and last geologic period of the Paleozoic Era, characterized by the formation of Pangea, glaciation in the Southern Hemisphere, development of mountains, esp. in the Appalachians, and an increase in the diversity of land plants and animals
http://www.emmasaying.com/
Take a look at my comparison tutorials here: https://www.youtube.com/user/EmmaSaying/videos?view=1
Subscribe to my channel here: https://www.youtube.com/user/EmmaSaying
- published: 04 Jun 2014
- views: 0
Continental drift
Continental drift is the movement of the Earth's continents relative to each other by appearing to drift across the ocean bed. The speculation that continent......
Continental drift is the movement of the Earth's continents relative to each other by appearing to drift across the ocean bed. The speculation that continent...
wn.com/Continental Drift
Continental drift is the movement of the Earth's continents relative to each other by appearing to drift across the ocean bed. The speculation that continent...
- published: 09 Aug 2014
- views: 6
-
author: Audiopedia
Nelle foreste del Carbonifero
Sequenza ad uso didattico tratta dalla serie "The making of planet Earth", 2001. Tutti i diritti sono riservati a BBC....
Sequenza ad uso didattico tratta dalla serie "The making of planet Earth", 2001. Tutti i diritti sono riservati a BBC.
wn.com/Nelle Foreste Del Carbonifero
Sequenza ad uso didattico tratta dalla serie "The making of planet Earth", 2001. Tutti i diritti sono riservati a BBC.
Nature Documentary: Australia's First 4 Billion Years EP02 Life Explodes english subtitles
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Visit my other documentary channels english subtitles:
Documentary HD english subtitles: http://bit.ly/1HiwVHZ
Buzz Documentary english subtitles: http://bit.ly/1A1Snys
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Nature Documentary: Australia's First 4 Billion Years EP02 Life Explodes english subtitles
See full series at: https://www.youtube.com/playlist?list=PLpay8XTQ-le8hcxtxz2TKlmvfvy9H9AR_
Life Explodes
How did life storm the beaches and dominate planet Earth? Ancient Australian fossils offer clues in "Life Explodes." Half a billion years ago, Australia was still part of the super-continent Gondwana. The oceans were teeming with weird and wonderful animals, but the world above the waves remained an almost lifeless wasteland. All that was about to change, though. Host Richard Smith introduces Earth's forgotten pioneers: the scuttling arthropod armies that invaded the shores and the waves of green revolutionaries whose battle for the light pushed plant life across the face of a barren continent. Evolution continued underwater as well, with armor-plated fish experimenting with teeth, jaws, sex, and lungs. NOVA's prehistoric adventure continues with four-legged animals walking onto dry land—and the planet poised for disaster
wn.com/Nature Documentary Australia's First 4 Billion Years Ep02 Life Explodes English Subtitles
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My facebook: http://on.fb.me/1G8rf1x
My twitter: http://bit.ly/1AYp5f9
My google +: http://bit.ly/1e2Kjn7
----------------------------------------------------------------------------------
Visit my other documentary channels english subtitles:
Documentary HD english subtitles: http://bit.ly/1HiwVHZ
Buzz Documentary english subtitles: http://bit.ly/1A1Snys
----------------------------------------------------------------------------------
Nature Documentary: Australia's First 4 Billion Years EP02 Life Explodes english subtitles
See full series at: https://www.youtube.com/playlist?list=PLpay8XTQ-le8hcxtxz2TKlmvfvy9H9AR_
Life Explodes
How did life storm the beaches and dominate planet Earth? Ancient Australian fossils offer clues in "Life Explodes." Half a billion years ago, Australia was still part of the super-continent Gondwana. The oceans were teeming with weird and wonderful animals, but the world above the waves remained an almost lifeless wasteland. All that was about to change, though. Host Richard Smith introduces Earth's forgotten pioneers: the scuttling arthropod armies that invaded the shores and the waves of green revolutionaries whose battle for the light pushed plant life across the face of a barren continent. Evolution continued underwater as well, with armor-plated fish experimenting with teeth, jaws, sex, and lungs. NOVA's prehistoric adventure continues with four-legged animals walking onto dry land—and the planet poised for disaster
- published: 20 May 2015
- views: 1