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Recommandé
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lorizimmerman
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][
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Describe general features of the history of life on Earth, including generally accepted dates and sequences of the geologic time scale and characteristics of major groups of organisms present during these periods (STEM-BIO11/12-IIIC-G-8). Specific Objectives: 1. Identify the date, eon, era, period, epoch and describe the major events base on Geologic Time Scale. 2. Differentiate the types of fossils. 3. Appreciate the history of life on earth by making a personal timeline.
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Making communications land - Are they received and understood as intended? webinar Thursday 2 May 2024 A joint webinar created by the APM Enabling Change and APM People Interest Networks, this is the third of our three part series on Making Communications Land. presented by Ian Cribbes, Director, IMC&T Ltd @cribbesheet The link to the write up page and resources of this webinar: https://www.apm.org.uk/news/making-communications-land-are-they-received-and-understood-as-intended-webinar/ Content description: How do we ensure that what we have communicated was received and understood as we intended and how do we course correct if it has not.
Making communications land - Are they received and understood as intended? we...
Making communications land - Are they received and understood as intended? we...
Association for Project Management
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Basic Civil Engineering first year Notes- Chapter 4 Building.pptx
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Python Notes for mca i year students osmania university.docx
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This PowerPoint helps students to consider the concept of infinity.
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Salient Features of India constitution especially power and functions
Salient Features of India constitution especially power and functions
Making communications land - Are they received and understood as intended? we...
Making communications land - Are they received and understood as intended? we...
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How to Create and Manage Wizard in Odoo 17
Food safety_Challenges food safety laboratories_.pdf
Food safety_Challenges food safety laboratories_.pdf
Basic Civil Engineering first year Notes- Chapter 4 Building.pptx
Basic Civil Engineering first year Notes- Chapter 4 Building.pptx
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Python Notes for mca i year students osmania university.docx
SKILL OF INTRODUCING THE LESSON MICRO SKILLS.pptx
SKILL OF INTRODUCING THE LESSON MICRO SKILLS.pptx
Geologic Time
1.
Geologic Time Chapter
21-24
2.
Capitol Reef National
Park What do the layers of rock have to do with Geologic Time?
3.
What has happened
to the rock layers since they were deposited?
4.
5.
6.
Geologic Time Scale
7.
8.
9.
10.
Superposition
11.
12.
13.
14.
15.
Carbon Dating
16.
17.
18.
Radioactive Decay of
Uranium 238
19.
20.
Tree Ring Dating
21.
Seasonal Climatic Changes
22.
Distinctive Sediment Layers
Key Beds are time markers that correlate rock layers across large areas.
23.
24.
25.
26.
27.
28.
The Precambrian Earth
The first 4 billion years
29.
How old is
the Earth?
30.
31.
Formation of the
Crust and Continents
32.
33.
34.
35.
36.
37.
Supercontinents
38.
Precambrian Atmosphere
39.
Why is Oxygen
important?
40.
41.
Ocean Formation
42.
43.
44.
Proterozoic Life
45.
46.
47.
48.
Paleozoic Era
49.
50.
MYBP = millions
of years before present
51.
Characteristic Sediment
52.
53.
Early Paleozoic Life
Almost all life forms started at this time.
54.
55.
Paleozoic animals
56.
Mass extinction
57.
58.
59.
Late Paleozoic
60.
61.
62.
63.
64.
Triassic Period –
Pangaea breaks apart and new seaways formed. Jurassic – dinosaurs Cretaceous – Flowering plants
65.
66.
Flying reptiles Modern
Fauna Reef Builders
67.
Ammonite Fossils
68.
Insects Angiosperm
69.
Dinosaurs
70.
Mass Extinction
71.
72.
73.
Pleistocene Mammals
74.
Primates
75.
76.
Humans