This document provides an overview of geological time scales and the evolution of Earth. It discusses the units used to measure geological time, from milliseconds to eons. It describes the key events and periods that make up the Precambrian, Paleozoic, Mesozoic, and Cenozoic eras. Methods for constructing the geological time scale are also summarized, drawing on evidence from fossils, radioactive dating, and other sources. Overall, the document serves as a reference for understanding Earth's structural and tectonic development through deep time.
The geologic time scale (GTS) is a system of chronological dating that relates geological strata (stratigraphy) to time. Geologists have divided Earth's history into a series of time intervals. These time intervals are not equal in length like the hours in a day. Instead the time intervals are variable in length. This is because geologic time is divided using significant events in the history of the Earth.
The geologic time scale (GTS) is a system of chronological dating that relates geological strata (stratigraphy) to time. Geologists have divided Earth's history into a series of time intervals. These time intervals are not equal in length like the hours in a day. Instead the time intervals are variable in length. This is because geologic time is divided using significant events in the history of the Earth.
Evolution is a developmental process from simple to complex form of life. Evolution of elephant started 60mya, from size of a pig. It spread all over world especially Africa and Asia. Today only two species Loxodonta and Elephas exist.
These slides cover all the necessary points regarding to fossilization as well as all the types of fossilization which will be beneficial for someone. Regards
Microfossils are very small remains of organisms 0.001 mm (1 micron) to 1 mm, that require magnification for study.
They are abundant, can be recovered from small samples.
Provide the main evidence for organic evolution through the time
They classified into two groups:
Organic-walled; Acritarchs, Dinoflagellate, Spores and Pollen grains … etc.
Foraminifera Each chamber interconnected by an opening (foramen) or several openings (foramina).
Known from Early Cambrian through to recent times, and has reached its acme during the Cenozoic.
Have a wide environmental range from terrestrial to deep sea and from polar to the tropical region.
Depending on the species, the shell may be made of organic compounds, sand grains and other particles cemented together, or from crystalline calcite.
Inorganic walled; Diatoms, Silicoflagellates, Ostracods, Conodonts, and Foraminifera
Evolution is a developmental process from simple to complex form of life. Evolution of elephant started 60mya, from size of a pig. It spread all over world especially Africa and Asia. Today only two species Loxodonta and Elephas exist.
These slides cover all the necessary points regarding to fossilization as well as all the types of fossilization which will be beneficial for someone. Regards
Microfossils are very small remains of organisms 0.001 mm (1 micron) to 1 mm, that require magnification for study.
They are abundant, can be recovered from small samples.
Provide the main evidence for organic evolution through the time
They classified into two groups:
Organic-walled; Acritarchs, Dinoflagellate, Spores and Pollen grains … etc.
Foraminifera Each chamber interconnected by an opening (foramen) or several openings (foramina).
Known from Early Cambrian through to recent times, and has reached its acme during the Cenozoic.
Have a wide environmental range from terrestrial to deep sea and from polar to the tropical region.
Depending on the species, the shell may be made of organic compounds, sand grains and other particles cemented together, or from crystalline calcite.
Inorganic walled; Diatoms, Silicoflagellates, Ostracods, Conodonts, and Foraminifera
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (scientific branch of geology that aims to determine the age of rocks). It is used primarily by Earth scientists (including geologists, paleontologists, geophysicists, geochemists, and paleoclimatologists) to describe the timing and relationships of events in geologic history. The time scale has been developed through the study of rock layers and the observation of their relationships and identifying features such as lithologies, paleomagnetic properties, and fossils. The definition of standardized international units of geologic time is the responsibility of the International Commission on Stratigraphy (ICS), a constituent body of the International Union of Geological Sciences (IUGS), whose primary objective[1] is to precisely define global chronostratigraphic units of the International Chronostratigraphic Chart (ICC)[2] that are used to define divisions of geologic time. The chronostratigraphic divisions are in turn used to define geochronologic units.[2]
While some regional terms are still in use,[3] the table of geologic time presented in this article conforms to the nomenclature, ages, and color codes set forth by the ICS as this is the standard, reference global geologic time scale – the International Geological Time Scale.[1][
Mechanism of Plate Tectonics and Resultant LandformsMithun Ray
Plate tectonics is a scientific theory that explains how major landforms are created as a result of Earth’s subterranean movements. The theory transformed the earth sciences by explaining many phenomena, including mountain building events, volcanoes, and earthquakes.
By going through this presentation, students will be able to understand the diversity within Geography. Introductory and comprehensive details have been given about each branch of Geography.
By going through this presentation, students will be able to understand the meaning and derivation of the word 'Geography', definition of 'Geography' as a discipline and the plurality character of Geography
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In this webinar you will learn how your organization can access TechSoup's wide variety of product discount and donation programs. From hardware to software, we'll give you a tour of the tools available to help your nonprofit with productivity, collaboration, financial management, donor tracking, security, and more.
The French Revolution, which began in 1789, was a period of radical social and political upheaval in France. It marked the decline of absolute monarchies, the rise of secular and democratic republics, and the eventual rise of Napoleon Bonaparte. This revolutionary period is crucial in understanding the transition from feudalism to modernity in Europe.
For more information, visit-www.vavaclasses.com
Embracing GenAI - A Strategic ImperativePeter Windle
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This Gasta posits a strategic approach to integrating AI into HEIs to prepare staff, students and the curriculum for an evolving world and workplace. We will highlight the advantages of working with these technologies beyond the realm of teaching, learning and assessment by considering prompt engineering skills, industry impact, curriculum changes, and the need for staff upskilling. In contrast, not engaging strategically with Generative AI poses risks, including falling behind peers, missed opportunities and failing to ensure our graduates remain employable. The rapid evolution of AI technologies necessitates a proactive and strategic approach if we are to remain relevant.
Introduction to AI for Nonprofits with Tapp NetworkTechSoup
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1. Mithun Ray
Department of Geography
Malda College (University of Gour Banga)
E-mail: mithun.ray147@gmail.com
Understanding of Earth’s Tectonic and
Structural Evolution through
Geological Time Scale
2. Units of Time
1000
milliseconds
= 1 second
60 seconds = 1 minute
60 minutes = 1 hour
24 hours = 1day
7 days = 1 week
28, 29, 30 or
31 days
= 1 month
365 or 366
days
= 1 year
12 months = 1 year
10 years = 1 decade
100 years = 1 century
1000 years = 1 millennium
4. What is Geological Time Scale
A system of chronological dating that
classifies geological strata in time
A Calendar for events in Earth History
A record of the major events and diversity
of life forms present in Earth’s history.
5. Constructing Evidences of
Geological Time Scale
Field observations
Fossil records
Stratigraphic correlations
Radioactive dating
Palaeomagnetic orientations
Orbital revolution of the Earth and
The rotation of the earth.
6. Major Incidences accounted in Geological
Time Scale
Mass extinctions,
Appearance of new species or genera of life,
Mountain-building movements
Drifting of continents
Spreading of ocean floors
Widespread glaciations
Dominance of certain species
Massive migration of life between land and water
7. From the time of Hutton, scientists were convinced that
the earth was much older than the 6000 years predicted
by the religious scholars.
The oldest rocks found so far on Earth (based on zircon
grains from Australia) have been dated at 4.1-4.2 billion
years.
Meteorites have also been dated at 4.6 billion years.
Meteorites are considered to be remnants of a plant or
asteroid that originally formed at the same time as the
Earth, so that the Earth’s age is currently estimated to be
4.6 billion years.
The oldest fossils are preserved remains of
stromatolites, which are layers of lithified blue-green
algae, dating to approximately 3.5 billion years before
present.
Age of our Planet ?
16Table of Contents
8. Units of Geological Time Scale
Duration of half a billion
years (or) more time
EON
ERA
PERIOD
EPOCH
AGE
Duration of Millions
of years
Duration of Tens of
Millions of years
Duration of hundreds of
millions of years
Duration of several hundred
millions of years
9. EON / AEON
Aeon শব্দটি গ্রীক শব্দ “Aion” থেকক একেকে যার অেথ “জীবনকাল”
PhanerozoicArchean
Greek word “Cryptos” means “Hidden”
“”Zoion” means “Living being” / “Life”
Greek word “Phaneros” means “Vissible”
“”Zoion” means “living being” / “life”
Proterozoic
CRYPTOZOIC
10. CRYPTOZOIC
[ Also known as “Pre-Cambrian” ]
Span of time between 4000 mya and 540 mya
Archean EonProterozoic Eon
### HADEAN EON ###
4600 mya to 4000 mya
As of 2016, International Commission on Stratigraphy
describes its status as “informal”. Geologist Preston
Cloud coined the term in 1972, originally to label the
earliest rocks on earth.
11. (A) ARCHEAN EON
The oldest era of the earth ( between 4000 mya and 2500 mya )
The word “archean” comes from the Greek word “arkhe” which means
“beginning” or “ origin”
The Oldest Rock Formations exposed on the surface of earth ( Canadian
Shield, Baltic Shield, Peninsular India, African Shield etc.)
Formation of Greenstone Belts
Origin of life, especially the prokaryotes, bacteria and blue-green algae
12. (B) PROTEROZOIC EON
Between 2500 mya and 540 mya
Dry and Cold climate
Origin of Eukaryotic cells and multi-cellular
life
Occurrence of
earliest known
fossils including
of soft-bodied
marine
invertebrates
15. (a) Cambrian Period
Between 540 mya and 505 mya
Age of trilobites (Marine invertebrates )
Supercontinent Gondwana forms near the South Pole
(note position of present-day Florida)
Existence
of plants was
observed
only as algae
Absence of
land plants.
16. (b) Ordovician Period
Between 505 mya and 438 mya
Age of Graptolites
First vertebrates originated as jawless fishes
All plants and animals still restricted to water
Four main
continents:
Gondwana,
Baltica, Siberia
and Laurentia
First
fungi
originated
17. (c) Silurian Period
Between 438 mya and 408 mya
First land plants appear and land animals follow
Laurentia collides with Baltica and closes Iapetus Sea
Dominance
of Sea lilies,
eurypterids
and land
scorpions
Origin of
the earliest
Vascular
Plants on
earth
18. (d) Devonian Period
Between 408 mya and 360 mya
Age of the
Fish
Pre-Pangea
forms
Extinction of primitive vascular plants happened
Origin of modern Vascular plants with true leaves, roots
and stems
Violent
volcanic
eruptions and
crustal
movements
19. (e) Carboniferous Period
Between 360 mya and 286 mya
It is known
for its coal
deposits
First land
vertebrates
First Reptiles laid eggs with shells in this period.
Highest ever atmospheric oxygen levels seen on earth
was in this period.
20. (f) Permian Period
Between 286 mya and 245 mya
Pangea
forms.
Reptiles
spread across
continents.
Widespread aridity on one side and Glaciation at the
other side.
Extinction of Palaezoic Plants and invertebrates (251
Mya).
22. (a) Triassic Period
Between 245 mya and 208 mya
Formation
of Salt,
Gypsum and
red beds
First dinosaurs, turtles, lizards appear
Pangaea
still in
existence
Climate arid
Modern
Corals
appeared
23. (b) Jurassic Period
Between 208 mya and 144 mya
Great plant eating dinosaurs were in existence-
“Golden age of dinosaurs”
Appearance
of the first
frogs,
salamanders,
crocodiles,
flying reptiles
and birds
were noticed
Breakup of Pangaea into Gondwana and Laurasia happened
during this period only
24. (c) Cretaceous Period
Between 144 and 66 Mya.
First snakes
appear
First
flowering
plants
Deciduous
trees and
grasses
common
This is the last period of the age of Dinosaurs
Breakup of Gondwana
27. (i) Paleocene
Between 65 mya and 55 mya
First horses appear
Tropical plants dominate
Climate Tropical
28. (ii) Eocene
Between 55 mya and 38 mya
Whales, rhinos, elephants and other large mammals
develop.
Reglaciation
in South Pole
First
Grasses
Appeared
29. (iii) Oligocene
Between 38 mya and 25 mya
Dogs and cats appear
Early ancestral
elephants
Warm but
cooling climate
30. (iv) Miocene
Between 25 mya and 5 mya
Extensive glaciation in Southern Hemisphere
Horses and
Mastodons
diverse
First Apes
appeared
Spread of
grasslands as
forests
contracted
31. (v) Pliocene
Between 5 mya and 2 mya
Ice Age begins
Seas restricted
The Grand Canyon Forms
Cool and dry climate
First known appearance of hominids (human like
primates)
33. (i) Pleistocene
Between 2 mya and 0.01 mya
Ice sheets are predominant- Ice age
Glacial climate
Four great ice
advances and
retreats
Modern
humans
develop
Formation of
large scale
Deserts –
Sahara was
formed
34. (ii) Holocene
Since 10,000 years ago
Rise of human civilization
Beginning of Agriculture
Copper Age
3500 BC
Bronze Age
2500 BC
Iron Age (1200
BC)
Man used iron
implements in
1350 BC
35. Holocene
Epoch
Meghalayan Age
(4200 years ago to the present)
North Grippian Age
(8200 years ago to 4200 years ago)
Greenlandian Age
(11700 years ago to 8200 years ago)
36.
37. We are living in
Meghalayan Age of
Holocene Epoch of
Quaternary Period of
Cenozoic Era of
Phanerozoic Eon
38. Now the question is
How to remember this!
To remember the sequence of ERAs you have to keep
in your mind the following sentence:
Please Pay My Children
Please
Pay
My
Children
Pre-Cambrian
Paleozoic
Mesozoic
Cenozoic
YoungerOlder
39. In case of PERIODs you have to remember
Camels Often Sit Down Carefully Perhaps Their Joints
Creak
Camels
Often
Sit
Down
Carefully
Perhaps
Their Joints
Creak
Cambrian
Silurian
Devonian
Carboniferous
Permian
Triassic
Jurassic
Cretaceous
Ordovician
PaleozoicEra
Mesozoic
Era
YoungerOlder
40. In case of EPOCHs you have to remember
Put Eggs On My Plate, Please Honey
Put
Eggs
On
My
Plate
Please
Honey
Paleocene
Oligocene
Miocene
Pliocene
Pleistocene
Holocene
Eocene
TertiaryPeriodQuaternary
Period
YoungerOlder
44. This Power Point Presentation (PPT) has
been prepared especially for Undergraduate
Students. The materials (Maps, Diagrams
and Images) used in this presentation were
collected and compiled mainly from variours
academic blogs, research papers, books etc.
The author has designed this PPT according
to his convenience to deliver the lecture.