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WHAT IS
THE
BIOSPHERE?
5
1410L
By Lorem Ipsum
Born
February 12, 1809
Shrewsbury, England
Died
April 19, 1882
Downe, England
WHAT IS
THE
BIOSPHERE?
By Big History Project
2 	3
The history of a word
Sometimes the history of a word can tell us a lot about what the word means.
The study of words even has its own name: etymology. Often, a closer look
at a word unfolds into another story, one that may connect to other people
and other scientific studies.
The word biosphere was first used by English-Austrian geologist Eduard
Suess (1831 — 1914) more than a hundred years ago in a four-volume work
entitled The Face of the Earth (1885 — 1908). Suess is also credited with
being the first person to propose the existence of the supercontinent Gond-
wanaland and the ancient Tethys Ocean, based upon his work studying
fossils in the Alps and his knowledge of the fossils of Glossopteris ferns that
were found on several different continents.
At the time, no one knew about plate tectonics. German meteorologist Alfred
Wegener didn’t put forth his theory on continental drift until 1912, a couple
of years before Suess died, and the best explanation Suess could offer
for the presence of marine fossils in the mountains was that the waters of
the Tethys Ocean had flooded the whole Earth, not that the continents had
actually drifted apart and changed. This is a great example of how limited
evidence can sometimes lead scientists to settle on incorrect conclusions.
It also demonstrates how the work of one person can build on that of
others, collectively leading to new discoveries about the world around us.
Suess combined bio, meaning “life,” and sphere, referencing the Earth’s
rounded surface, to express the portion of the Earth that supported life.
He invented the word because he felt it was important to try to understand
life as a whole rather than singling out particular organisms. He wrote in
The Face of the Earth:
The plant, whose deep roots plunge into the soil to feed, and which at
the same time rises into the air to breathe, is a good illustration of or-
ganic life in the region of interaction between the upper sphere and the
lithosphere, and on the surface of continents it is possible to single out
an independent biosphere.
BIOSPHERE
COMFORT
ZONE
RÜPPELL'S GRIFFON
Gypps rupelli
BAR-HEADED GOOSE
Anser indicus
MOST BIRDS
Fly within 2 km
of the ground
MOST LIFE ON EARTH
Lives in a thin layer on, near,
or under the surface
SPERM WHALE
Physeter macrocephalus
EXTREMOPHILE BACTERIA
Staphylothermus marinus &
Thermoproteus tenax
DEVIL WORM
Halicephalobus mephisto
GIANT SQUID
Architeuthis dux
ANGLERFISH
Cryptopsaras couesii
SNAILFISH
Liparidae
FORAMINIFERA
Single-celled protists
12
8.8
5
3
0
2
11
KILOMETERS
AIR
SEA
LAND
MOUNT EVEREST
CHALLENGER DEEP
Its summit 8,848 meters (29,029
feet) above sea level, Mount
Everest is the world’s highest
mountain. Located on the
Nepal-Tibet border, Everest is one
of many peaks taller than 8,000
meters in the massive Himalayan
range. The Himalayas were formed
40–50 million years ago when the
Indian plate collided with the
Eurasian plate. The intense cold at
this altitude makes for a rough
habitat, but birds have been seen
flying over Everest and some even
nest on its lower slopes.
At least 10,902 meters (35,768 feet)
below sea level, Challenger Deep is
the deepest depression in the western
Pacific’s Mariana Trench. The trench,
near Guam, was formed when the
Pacific plate was subducted beneath
the smaller Mariana plate. The
pressure this deep in the ocean is
more than a thousand times that at
sea level, but some organisms
thrive in these extreme conditions.
6 	7
As our knowledge of life on the planet evolves, we’ve come to use the word
biosphere as a way of explaining the entire intertwined network of life on
Earth. This concept combines an understanding of geology, knowledge of
the distinct layers that make up the Earth and its atmosphere, and an aware-
ness of the biodiversity surrounding us. We can think of the biosphere as
the habitat, or home, for all life on our planet, in all its forms, and with all its
intricate biological and geological relationships.
	 Biosphere = the network of all life on Earth
Worlds within worlds
The biosphere is incredibly small — just a thin layer around a medium-size
planet. But it’s also incredibly large, when you consider all of the different
living things and our planet’s vast expanses of water and land. As with most
things that seem large and encompassing, it’s possible to break down the bio-
sphere and to use other words to describe specific environments or habitats.
These smaller areas are called “ecosystems,” and they are characterized
by particular geologic or climatic features that accommodate certain forms
of life. Oceans, jungles, and mountain ranges can be ecosystems, but even
more specific places can be their own ecosystems. Think of a cave, a river
or river valley, a coral reef, a city, or the “vent communities” that surround
black smokers on the ocean floor. Altitude, latitude, longitude, climate,
soils, and terrain can all contribute to the distinct features of an ecosystem
— the Earth’s geologic processes have produced a multitude of diverse envi-
ronments. The biosphere boasts incredible diversity and, even in extreme
environmental conditions, astounding examples of life’s flexibility and deter-
mination.
Every organism — from baboons to bacteria — has a specialized way to make
a living as it vies for resources and energy and reproduces within its own
environment. Examining these individual ecosystems, using biology and
geology, reveals the many complex relationships between life and the planet
we all share.
8
Image credits
Earth from space
© Science Picture Co/Science Faction/CORBIS
An 1869 lithograph of Eduard Suess by Josef Kriehuber,
public domain
Illustration of the biosphere
© The Big History Project
Scuba diver looking at coral reef
© moodboard/CORBIS
Articles leveled by Newsela have been adjusted along several dimensions of text complexity including
sentence structure, vocabulary and organization. The number followed by L indicates the Lexile measure
of the article. For more information on Lexile measures and how they correspond to grade levels:
http://www.lexile.com/about-lexile/lexile-overview/
To learn more about Newsela, visit www.newsela.com/about.
The Lexile®
Framework for Reading
The Lexile®
Framework for Reading evaluates reading ability and text complexity on the same developmental
scale. Unlike other measurement systems, the Lexile Framework determines reading ability based on actual
assessments, rather than generalized age or grade levels. Recognized as the standard for matching readers
with texts, tens of millions of students worldwide receive a Lexile measure that helps them find targeted
readings from the more than 100 million articles, books and websites that have been measured. Lexile measures
connect learners of all ages with resources at the right level of challenge and monitors their progress toward
state and national proficiency standards. More information about the Lexile®
Framework can be found at
www.Lexile.com.

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Unit 5: What Is The Biosphere?

  • 2. By Lorem Ipsum Born February 12, 1809 Shrewsbury, England Died April 19, 1882 Downe, England WHAT IS THE BIOSPHERE? By Big History Project
  • 3. 2 3 The history of a word Sometimes the history of a word can tell us a lot about what the word means. The study of words even has its own name: etymology. Often, a closer look at a word unfolds into another story, one that may connect to other people and other scientific studies. The word biosphere was first used by English-Austrian geologist Eduard Suess (1831 — 1914) more than a hundred years ago in a four-volume work entitled The Face of the Earth (1885 — 1908). Suess is also credited with being the first person to propose the existence of the supercontinent Gond- wanaland and the ancient Tethys Ocean, based upon his work studying fossils in the Alps and his knowledge of the fossils of Glossopteris ferns that were found on several different continents. At the time, no one knew about plate tectonics. German meteorologist Alfred Wegener didn’t put forth his theory on continental drift until 1912, a couple of years before Suess died, and the best explanation Suess could offer for the presence of marine fossils in the mountains was that the waters of the Tethys Ocean had flooded the whole Earth, not that the continents had actually drifted apart and changed. This is a great example of how limited evidence can sometimes lead scientists to settle on incorrect conclusions. It also demonstrates how the work of one person can build on that of others, collectively leading to new discoveries about the world around us. Suess combined bio, meaning “life,” and sphere, referencing the Earth’s rounded surface, to express the portion of the Earth that supported life. He invented the word because he felt it was important to try to understand life as a whole rather than singling out particular organisms. He wrote in The Face of the Earth: The plant, whose deep roots plunge into the soil to feed, and which at the same time rises into the air to breathe, is a good illustration of or- ganic life in the region of interaction between the upper sphere and the lithosphere, and on the surface of continents it is possible to single out an independent biosphere.
  • 4. BIOSPHERE COMFORT ZONE RÜPPELL'S GRIFFON Gypps rupelli BAR-HEADED GOOSE Anser indicus MOST BIRDS Fly within 2 km of the ground MOST LIFE ON EARTH Lives in a thin layer on, near, or under the surface SPERM WHALE Physeter macrocephalus EXTREMOPHILE BACTERIA Staphylothermus marinus & Thermoproteus tenax DEVIL WORM Halicephalobus mephisto GIANT SQUID Architeuthis dux ANGLERFISH Cryptopsaras couesii SNAILFISH Liparidae FORAMINIFERA Single-celled protists 12 8.8 5 3 0 2 11 KILOMETERS AIR SEA LAND MOUNT EVEREST CHALLENGER DEEP Its summit 8,848 meters (29,029 feet) above sea level, Mount Everest is the world’s highest mountain. Located on the Nepal-Tibet border, Everest is one of many peaks taller than 8,000 meters in the massive Himalayan range. The Himalayas were formed 40–50 million years ago when the Indian plate collided with the Eurasian plate. The intense cold at this altitude makes for a rough habitat, but birds have been seen flying over Everest and some even nest on its lower slopes. At least 10,902 meters (35,768 feet) below sea level, Challenger Deep is the deepest depression in the western Pacific’s Mariana Trench. The trench, near Guam, was formed when the Pacific plate was subducted beneath the smaller Mariana plate. The pressure this deep in the ocean is more than a thousand times that at sea level, but some organisms thrive in these extreme conditions.
  • 5. 6 7 As our knowledge of life on the planet evolves, we’ve come to use the word biosphere as a way of explaining the entire intertwined network of life on Earth. This concept combines an understanding of geology, knowledge of the distinct layers that make up the Earth and its atmosphere, and an aware- ness of the biodiversity surrounding us. We can think of the biosphere as the habitat, or home, for all life on our planet, in all its forms, and with all its intricate biological and geological relationships. Biosphere = the network of all life on Earth Worlds within worlds The biosphere is incredibly small — just a thin layer around a medium-size planet. But it’s also incredibly large, when you consider all of the different living things and our planet’s vast expanses of water and land. As with most things that seem large and encompassing, it’s possible to break down the bio- sphere and to use other words to describe specific environments or habitats. These smaller areas are called “ecosystems,” and they are characterized by particular geologic or climatic features that accommodate certain forms of life. Oceans, jungles, and mountain ranges can be ecosystems, but even more specific places can be their own ecosystems. Think of a cave, a river or river valley, a coral reef, a city, or the “vent communities” that surround black smokers on the ocean floor. Altitude, latitude, longitude, climate, soils, and terrain can all contribute to the distinct features of an ecosystem — the Earth’s geologic processes have produced a multitude of diverse envi- ronments. The biosphere boasts incredible diversity and, even in extreme environmental conditions, astounding examples of life’s flexibility and deter- mination. Every organism — from baboons to bacteria — has a specialized way to make a living as it vies for resources and energy and reproduces within its own environment. Examining these individual ecosystems, using biology and geology, reveals the many complex relationships between life and the planet we all share.
  • 6. 8 Image credits Earth from space © Science Picture Co/Science Faction/CORBIS An 1869 lithograph of Eduard Suess by Josef Kriehuber, public domain Illustration of the biosphere © The Big History Project Scuba diver looking at coral reef © moodboard/CORBIS Articles leveled by Newsela have been adjusted along several dimensions of text complexity including sentence structure, vocabulary and organization. The number followed by L indicates the Lexile measure of the article. For more information on Lexile measures and how they correspond to grade levels: http://www.lexile.com/about-lexile/lexile-overview/ To learn more about Newsela, visit www.newsela.com/about. The Lexile® Framework for Reading The Lexile® Framework for Reading evaluates reading ability and text complexity on the same developmental scale. Unlike other measurement systems, the Lexile Framework determines reading ability based on actual assessments, rather than generalized age or grade levels. Recognized as the standard for matching readers with texts, tens of millions of students worldwide receive a Lexile measure that helps them find targeted readings from the more than 100 million articles, books and websites that have been measured. Lexile measures connect learners of all ages with resources at the right level of challenge and monitors their progress toward state and national proficiency standards. More information about the Lexile® Framework can be found at www.Lexile.com.