PALEONTOLOGY: KEY QUESTIONS How do we locate, recover, and date fossil remains? What are the features of the primate skeleton, and how can our knowledge.

Slides:



Advertisements
Similar presentations
Relative and Absolute Age Law of Superposition
Advertisements

Hominid Origins Introduction
EARTH HISTORY Chapter 6 review.
PALEONTOLOGY How do we locate, recover, and date fossil remains?
Models on WHY? Why we became bipedal (6 hypotheses)6 hypotheses Efficient bipedalism as the primary form of locomotion is seen only in hominins.
Paleoanthropology: Reconstructing Early Hominid Behavior and Ecology
The Age of Earth. Classification Quick Quiz Write the letter of the correct definition below the number of the correct corresponding term. Remember to.
Earth and Space Sciences Unit 4
Digging Up the Past: Paleoanthropology and Archaeology
Analysis of Primates Comparisons of Human, Ape, and Australopithecine.
Relate Cause and Effect Why have so few organisms become fossilized
Chapter 8.  itarianism  A principle that geologic processes that occurred in the past can be explained by current geologic processes.  Volcanism and.
Determining Geologic Ages Lab # 8 pg 91
HOW OLD IS OLD? The Rock Record and Geologic Time Chapter 3
Paleoanthropology: Reconstructing Early Hominid Behavior and Ecology.
The Fossil Record Section 17–1
UNIT 2 Archaeology and Physical Anthropology – Studying the Past.
Fossils Remains of organisms (often partially or wholly replaced by “rock”) Bones, teeth, shells, hard exoskeletons Usually in sedimentary rocks (water.
How do we know the age of the Earth?
Earth and Space…7b and c (7)  Earth in space and time. The student knows that scientific dating methods of fossils and rock sequences are used to construct.
Archaeology.
Unit 2 Lesson 3 Absolute Dating
Foothill High School Science Department The History of Life The Fossil Record.
How do scientists know evolution has occurred?. Paleontologists: scientists who study fossils Geologists: scientists who study rock layers.
Biology Unit 4 – Continuity and Change Outcome 2.
IN SEARCH OF HUMAN ORIGINS. Jinsha Museum in Chengdu, southwest China's Sichuan province.
IN SEARCH OF HUMAN ORIGINS.  What are the features of the primate skeleton, and how can knowledge of them help us identify fossil remains?  Great.
DO NOW What is stratigraphy? Write a statement about the age of the various layers (and fossils that may be found in those layers) you observe in the strata.
Unit 7 Lesson 3 Absolute Dating
FOSSILS, RELATIVE & ABSOLUTE DATING
Dating Notes Donald’s 101 to Dating.
Miocene Hominoid Distribution, From Fossils Thus Far Discovered.
Modern Humans and Modern Apes Compared. EYES Modern Human Located in front of skull. Excellent binocular vision Excellent colour vision Reduced sense.
Dating 1.Radioactive Half-Lifes 2.Index Fossils 3.Tree Rings 4.Genetic.
Chapter 8 Hominid Origins.
Hominins (us) review… Defined by dental features, bipedal locomotion, large brain size, and tool making behavior Characteristics that developed at different.
Unit 1- Earth Systems and Resources Geological Time Scale.
Geologic Time.
Section 2: Determining Absolute Age
A Fossil.  Any method of measuring the age of an event or object in years.
Mountain Building Folding vs. Faulting Geologic time & dating.
Dating Rocks & Fossils. Will you go out with me NO! I’m far too old for you!
Radioactive Dating Chapter 7 Section 3.
Unit 2 Lesson 3 Absolute Dating Copyright © Houghton Mifflin Harcourt Publishing Company.
Chapter 17.1 Principle of Uniformitarianism
History of Life on Earth Evolutionary TIMELINE Ms. Herrera.
(7) Earth in space and time. The student knows that scientific dating methods of fossils and rock sequences are used to construct a chronology of Earth's.
ABSOLUTE-AGE DATING: A MEASURE OF GEOLOGIC TIME. THINK ABOUT IT… How old is the Earth? Can it be determined? What are some tools or methods that scientists.
The Rock Record Section 2 Section 2: Determining Absolute Age Preview Objectives Absolute Dating Methods Radiometric Dating Radioactive Decay and Half-Life.
Do First Actions: Turn in yesterday’s worksheet 1. List the layers from youngest to oldest.
Visualizing Earth Science By Z. Merali and B. F. Skinner Chapter 10 – How Old is Old? The Rock Record and Deep Time.
Geological Time Dating Absolute and Relative. Geologic Time B y examining layers of sedimentary rock, geologists developed a time scale for dividing up.
Fossils & History of Life Chapter 12 Biology. KEY CONCEPT Specific environmental conditions are necessary in order for fossils to form.
Rock Dating Geologists generally know the age of a rock by determining the age of the group of rocks, or formation, in which it is found.
Geological Time Dating Absolute and Relative. Geologic Time B y examining layers of sedimentary rock, geologists developed a time scale for dividing up.
Scientists have determined the age of the Earth to be about 4.6 billion years old 4,600, 000, 000 years = 4.6 x 10 9 years (scientific notations you should.
 Geographical isolation- part of the population is isolated (usually physical barrier eg. River/mountains)  Phenotypes that are advantageous in one environment.
Evidence of Evolution. 1) Fossil Record 2) Geographical Distribution 3) Homologous Body Structures 4) Similarities in Embryology.
HOW OLD IS OLD? The Rock Record and Deep Geologic Times.
Geologic Time. The Geologic Time Scale  A summary of major events in Earth’s past that are preserved in the rock record  Divisions of Geologic Time.
The Record of the Past Chapter 11.
Unit 2 Lesson 3 Absolute Dating
Chapter 8: Fossils in Geological Context
Hominid Evolution in Context
Unit 2 Lesson 3 Absolute Dating
Unit 2 Lesson 3 Absolute Dating
Unit 2 Lesson 1 Absolute Dating
NOTES: GEOLOGIC DATING
NOTES: GEOLOGIC DATING
Presentation transcript:

PALEONTOLOGY: KEY QUESTIONS How do we locate, recover, and date fossil remains? What are the features of the primate skeleton, and how can our knowledge of them help us identify fossil remains?

THE FOSSIL RECORD: PRESERVATION –Not a representative sample of all of the species that have lived on earth –Some species and body parts preserve better than others –TAPHONOMY = study of the processes that affect the remains of dead animals

THE FOSSIL RECORD: FINDING FOSSILS * More likely to be found in areas with little vegetation and lots of erosion (i.e. lake bottoms) * Due to issues regarding the preservation and discovery of fossils, the fossil record of early primates is “limited and spotty”

DATING CONCEPTS PALEONTOLOGY = study of ancient life through the fossil record Anthropology & Paleontology -- interested in establishing a chronology for primate and human evolution Much dating depends on STRATIGRAPHY = study of the sequence of geographical layers

RELATIVE DATING Uses natural layers or strata to establish a relative chronology— material from this layer is older than the material from that layer Association with known fossils, biostratigraphy = most common method of fossil dating

ABSOLUTE DATING (p.202!) Produce dates in years, so differences in age can be quantified Radiometric techniques = based on known rates of radioactive decay in elements found in or around fossils Radiocarbon (Half-life of 14C is 5,730 yrs.), dates organic remains from 100s to 40,000 ya (half life = time needed for ½ amount of 14C to decay) Potassium Argon (K/A) dates volcanic rock from 100,000 to billions ya

ABSOLUTE DATING Electron Spin Resonance (ESR) = Measures # of electrons excited to higher energy levels by natural radiation & trapped at those levels, dates teeth & cave deposits from 100s to 10 mya Luminescence = Same as ESR, but trapped energy is released using heat or light, dates pottery, bricks, burned rock up to 800,000 ya

IF Humanlike remains were found between two layers of volcanic rock, how could we date the remains? K/Ar (potassium/argon) dating Remains are younger than the volcanic deposit below and older than the one above Hypothetical Stratigraphic Sequence

Absolute Dating Techniques TechniqueAbbrev- iation Materials Dated Effective Time Range Carbon Corganic materials up to 40,000 years Potassium- Argon K/A and 40 K volcanic rock older than 500,000 years Uranium Series 238 Umineralsbetween 1,000 and 1,000,000 Thermo- luminescence TLrocks and minerals between 5,000 and 1,000,000 years Electron Spin Resonance ESRrocks and minerals between 1,000 and 1,000,000 years

Continents At End of the Mesozoic Placement of the continents at the end of the Mesozoic and beginning of the Cenozoic, about 65 mya Tethys Seaway

Cenozoic Timescale

Taphonomy Leopard + remains of early hominid in tree above entrance to cave Accumulation of bones, including hominid bones, in South African caves Bones, antlers, teeth found in the caves once thought to be early tools used by bipedal “killer apes” to hunt and forage Taphonomic research now shows that they are a natural accumulation & the “killer apes” were prey not predator!

Skeletons of: Modern Human Gorilla Domestic Cat Skeletal Anatomy

Comparative Primate Anatomy Differences in stance: Indri: Vertical clinging and leaping Macaque: Generalized quadrupedalism Gorilla: Semi-erect knuckle walking Chimp: Knuckle- walking and tree climbing Human: Fully erect bipedalism

Cranial Anatomy Hominoid primates share same overall construction of the skull Proportions of the various bones of the skull, however, vary, as do the expression of various ridge-like features on surface of the bone What do you think are some of the reasons for these differences? Sagittal crest Frontal Brow ridge

Axial Skeleton (Trunk) of OW Primates

Changes in the anatomy of the trunk

Hominoid Comparative Anatomy

Changes in Human Skeleton 1.Skull more balanced on spine 2.Smaller neck muscles 3.Spine articulates under skull 4.Multiple curves of spine 5.Narrower rib cage

Changes in Human Skeleton (cont.) 6.Shorter wider pelvis 7.Proportionately longer legs 8.Upper leg angled inward so knees closer to midline 9.Big toe in line with other toes 10.Center of gravity in pelvic basin