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 Introduction
 Branches needed to study
 Geochronology
 Straitigraphy
 Paleontology
 Geocronological units
 Hadean eon
 Theories for evolution
 Conclusion
Evolution from rocks is a brief research work done on
how rocks had evolved over billions of years ago and
how life originated from them. To study evolution
from rocks some branches of geology and related
sciences are very important to know about. While the
work is mainly based on different theories of
evolution by different scientists and the latest
researches of geologists which are recently trying to
explain the relation of biological life with that of
mineral basis.
Geochronology
Straitigraphy
Paleontology
Geochronology is
the science of
determining
the age of rocks
, fossils, and
sediments.
Straitigraphy is a
branch of geology
which studies
rock layers (strata)
and layering
(stratification).
Paleontology is the
scientific study of
prehistoric life. It
includes the study of
fossils to determine
organisms' evolution
and interactions with
each other and their
environments.
Units which are
used to divide
geological
time period
are called
geochronological
units.
Time spans in
geochronology
Notes to
geochronological units
Eon 4 total, half a billion
years or more
Era 10 total, several hundred
million years
Period Several hundred
million years
Epoch tens of
millions of years
Age millions of years
Chron subdivision of an age, not
used by the ICS timescale
Geochronology
 Geochronology is science
of studying about
geological time
 Geochronological units are
units which designate
periods of time
 thus it is correct to say that
Tyrannosaurus rex lived
during the
Late Cretaceous Epoch
 Straitigraphy is science of
studying rocks and its
layers
 While strait chronological
units explain the time of
formation of rock layers
 it is also correct to say that
fossils of the
genus Tyrannosaurus have
been found in the Upper
Cretaceous Series
Straitigraphy
 Hadean eon has been considered the first geologic eon
of Earth
 It lied even before the Achaean (a geologic eon before
the Proterozoic Eon2,500 million years ago.)
 So according to scientists’ Hadean eon is the one due to
which earth got its present form with the period of time
 the rocks of
hadean eon
were the ones
which contained
essential substances
for life to evolve.
Life from the rocks of Hadean eon
Life from hydrothermal vents
Life due to phosphorites
Life due to meteor or commit
Life from volcanic eruptions
Life from clay hydro gels
 Rocks formed in the time period of hadean eon gave life
to earth
 They reacted with other substances in that
environment to produce materials which gave rise to
ancient life
 So the first step in evolution was the formation of rocks
furthermore those rocks have molecules to support life
 it is thought that once earth was covered with water all
over
 And due to high temperatures water was hot so
somewhere in hydrothermal vents life originated and
multiplied
 Some archeobacteria which can resist temperature of
about 120 degree Celsius survived as the rocks beneath
or magma had basic molecules for life
 2 billion years ago Earth system was recovering from
perhaps the single-most profound modification of its
surface environments: the oxygenation of the
atmosphere and oceans.
 This also resulted in the distribution of one of life's key
elements, phosphorus.
 The formation of Earth's earliest phosphorites was
influenced strongly, if not controlled completely, by
the activity of sulfur bacteria.
 In the modern world, sulfur bacteria inhabit
upwelling vent and seep areas known as "Black
Smokers" and mediate phosphorites formation.
 The scientists therefore conclude that the formation of
the earliest worldwide phosphorites 2 billion years ago
can be linked to the establishment of sulfur bacteria
habitats, triggered by the oxygenation of Earth.
 commits and meteors which hit the surface of the
earth provided environment perfect for evolution
 Some organic molecules came to earth by sticking to a
meteorite
 Formic acid, a compound implicated in the origins of
life, has been found at record levels on a meteorite that
fell onto a frozen Canadian lake in 2000.
 the gasses emitted during volcanic eruptions contained
molecules for life
 The organic gases emitted from volcanic eruptions
reacted with water due to high temperature at that time
and made the molecules which persisted the ability to
divide and transfer the hereditary material
 clay (a silicate) has the ability to absorb liquid up to
great extent so the materials being absorbed in that
clay provided conditions and molecules for the life to
evolve.
 In simulated ancient seawater, clay forms a hydro gel -
a mass of microscopic spaces capable of soaking up
liquids like a sponge.
 Over billions of years, chemicals confined in those
spaces could have carried out the complex reactions
that formed proteins, DNA and eventually all the
machinery that makes a living cell work.
 Clay hydrogels could have confined and protected
those chemical processes until the membrane that
surrounds living cells developed.
No theory can explain totally
the origin of life on planet
earth!
All these theories might seem different
from each other but actually they all are
connected in some way. So from the
above discussion it is quite evident that
life originated after the evolution of
different types of rocks and that
geological landforms became the reason
for life to come into being!
Evolution from rocks
Evolution from rocks

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Evolution from rocks

  • 1.
  • 2.  Introduction  Branches needed to study  Geochronology  Straitigraphy  Paleontology  Geocronological units  Hadean eon  Theories for evolution  Conclusion
  • 3. Evolution from rocks is a brief research work done on how rocks had evolved over billions of years ago and how life originated from them. To study evolution from rocks some branches of geology and related sciences are very important to know about. While the work is mainly based on different theories of evolution by different scientists and the latest researches of geologists which are recently trying to explain the relation of biological life with that of mineral basis.
  • 5. Geochronology is the science of determining the age of rocks , fossils, and sediments.
  • 6. Straitigraphy is a branch of geology which studies rock layers (strata) and layering (stratification).
  • 7. Paleontology is the scientific study of prehistoric life. It includes the study of fossils to determine organisms' evolution and interactions with each other and their environments.
  • 8. Units which are used to divide geological time period are called geochronological units.
  • 9. Time spans in geochronology Notes to geochronological units Eon 4 total, half a billion years or more Era 10 total, several hundred million years Period Several hundred million years Epoch tens of millions of years Age millions of years Chron subdivision of an age, not used by the ICS timescale
  • 10. Geochronology  Geochronology is science of studying about geological time  Geochronological units are units which designate periods of time  thus it is correct to say that Tyrannosaurus rex lived during the Late Cretaceous Epoch  Straitigraphy is science of studying rocks and its layers  While strait chronological units explain the time of formation of rock layers  it is also correct to say that fossils of the genus Tyrannosaurus have been found in the Upper Cretaceous Series Straitigraphy
  • 11.  Hadean eon has been considered the first geologic eon of Earth  It lied even before the Achaean (a geologic eon before the Proterozoic Eon2,500 million years ago.)  So according to scientists’ Hadean eon is the one due to which earth got its present form with the period of time
  • 12.  the rocks of hadean eon were the ones which contained essential substances for life to evolve.
  • 13. Life from the rocks of Hadean eon Life from hydrothermal vents Life due to phosphorites Life due to meteor or commit Life from volcanic eruptions Life from clay hydro gels
  • 14.  Rocks formed in the time period of hadean eon gave life to earth  They reacted with other substances in that environment to produce materials which gave rise to ancient life  So the first step in evolution was the formation of rocks furthermore those rocks have molecules to support life
  • 15.
  • 16.  it is thought that once earth was covered with water all over  And due to high temperatures water was hot so somewhere in hydrothermal vents life originated and multiplied  Some archeobacteria which can resist temperature of about 120 degree Celsius survived as the rocks beneath or magma had basic molecules for life
  • 17.
  • 18.  2 billion years ago Earth system was recovering from perhaps the single-most profound modification of its surface environments: the oxygenation of the atmosphere and oceans.  This also resulted in the distribution of one of life's key elements, phosphorus.  The formation of Earth's earliest phosphorites was influenced strongly, if not controlled completely, by the activity of sulfur bacteria.
  • 19.  In the modern world, sulfur bacteria inhabit upwelling vent and seep areas known as "Black Smokers" and mediate phosphorites formation.  The scientists therefore conclude that the formation of the earliest worldwide phosphorites 2 billion years ago can be linked to the establishment of sulfur bacteria habitats, triggered by the oxygenation of Earth.
  • 20.
  • 21.  commits and meteors which hit the surface of the earth provided environment perfect for evolution  Some organic molecules came to earth by sticking to a meteorite  Formic acid, a compound implicated in the origins of life, has been found at record levels on a meteorite that fell onto a frozen Canadian lake in 2000.
  • 22.
  • 23.  the gasses emitted during volcanic eruptions contained molecules for life  The organic gases emitted from volcanic eruptions reacted with water due to high temperature at that time and made the molecules which persisted the ability to divide and transfer the hereditary material
  • 24.
  • 25.  clay (a silicate) has the ability to absorb liquid up to great extent so the materials being absorbed in that clay provided conditions and molecules for the life to evolve.  In simulated ancient seawater, clay forms a hydro gel - a mass of microscopic spaces capable of soaking up liquids like a sponge.
  • 26.  Over billions of years, chemicals confined in those spaces could have carried out the complex reactions that formed proteins, DNA and eventually all the machinery that makes a living cell work.  Clay hydrogels could have confined and protected those chemical processes until the membrane that surrounds living cells developed.
  • 27.
  • 28. No theory can explain totally the origin of life on planet earth!
  • 29. All these theories might seem different from each other but actually they all are connected in some way. So from the above discussion it is quite evident that life originated after the evolution of different types of rocks and that geological landforms became the reason for life to come into being!