LECTURE 4: Paleozoic Era Silurian/Devonian Periods (439 mya- 360 mya)

Slides:



Advertisements
Similar presentations
Earth Science 13.2A Paleozoic Era : Life explodes
Advertisements

Paleozoic ( mya) events. Late Paleozoic-key things ・ ・ Several key things happen beginning at the end of the Silurian through the Permian - -
Biology 12.3 History Life on Earth: Life Invaded the Land
Earth History The Paleozoic Era. Paleozoic Time ( Million Years Ago) n Bracketed by the two most important biological events in Earth’s history:
Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying.
Recording natural history
Ordovician The first vertebrates - jawless fishes called ostracoderms.
Life in the Paleozoic Era Chapter 13 Section 2. The Cambrian Period The Cambrian Explosion: a span of about 15 million years when many new types of invertebrates.
End Show Slide 1 of 30 Copyright Pearson Prentice Hall Biology.
Paleozoic Era Life starts in the seas and moves onto land
8-2 Notes – Early Earth History
History of the Earth Chapter 12. How Old is the Earth?  Early Earth  4.5 Billion Years Old  Before then it was a fiery ball of molten rock.  The water.
PALEOZOIC ERA (542 Mya Mya) Andrea Villalba, Fabiola Ferrabone, Alfredo de Obaldia, Nicole Cortez.
Botany Unit Notes Part I. What is a Plant? When you are asked, “what color is life?”, the color that comes to mind is usually green! It is no wonder that.
Section 2: Precambrian Time and the Paleozoic Era
Aim: What were the first organisms to appear on Earth? HW # 8 read chapter 19 Pg.493 q.#40 due thurs Group work Go through the progression of what we think.
Earth Science 13.2B Paleozoic Era : Life explodes
PLANT NOTES Part 1 Plant Diversity  Plants are members of the Kingdom ______.  They are classified as eukaryotic organisms that have cell walls made.
Lets start 390 million years ago… During the Devonian Period, there were many creatures living in the oceans (some on their way to becoming the true.
Paleozoic Life Vertebrates & Plants.
Foothill High School Science Department The History of Life Evolution of Multicellular Life.
Agenda: 1.WarmUp 2.How It’s Made 3.Lottery 4.Timeline 5.Video.
Zach Holtslander & Steven Weber. Time Period The Devonian period took place during the Paleozoic era, and lasted from 416 to million years ago.
What is the Earth’s time scale? The Geological time scale is a record of the life forms and geological events in Earth’s history. Scientists developed.
What is fish with out an eye. FSH
II. Animal Diversity 3. Vertebrata c. Jawed Fishes - Placoderms(extinct – survived to Permian) - Cartilaginous fish (Class: Chondrichthyes) - Bony Fish.
II. Animal Diversity C. Bilateria 2. Deuterostomes – blastopore forms anus c. Chordata: 3. Vertebrata - four traits - vertebral column - trends: - increased.
Recent animal phylogenies use molecular data and result in a different looking tree Tree built using protein or gene sequences Need to use a gene(s) that.
17-3 Evolution of Multicellular Life
Geologic Time Scale Spring th Grade.
Fish Lecture 1.
The Geological Time Scale Events in Your Life ___When you started second grade ___When you were born ___ When you started kindergarten ___When you learned.
The Paleozoic Era has 6 different periods. The Permian, Carboniferous, Devonian, Silurian, Ordovician, and Cambrian.
Chapter 13 Section 2 Paleozoic Era: Life Explodes
 Evolution of life in the Ocean and Classification of the Marine Environment.
8e. Know how to analyze fossil evidence with regard to biological diversity, episodic speciation and mass extinction.
Section 6 – Eras of Earth’s History
Life and Geologic Time  Majority of life in the history of Earth, 4.6 billion years, is confined to the past 600 million years.  This life as outline.
Paleozoic Era 570,000,000 yrs ago to 225,000,000 yrs ago Life starts in the seas and moves onto land Six periods: Cambrian Ordovician Silurian Devonian.
Evolutionary History Chapter 15. What you need to know! The age of the Earth and when prokaryotic and eukaryotic life emerged. Characteristics of the.
Precambrian Time and the Paleozoic Era
Unit 1 Lesson 4 The History of Life on Earth Copyright © Houghton Mifflin Harcourt Publishing Company.
End Show Slide 1 of 62 Copyright Pearson Prentice Hall Biology.
Diversity of marine animals, and extinction events over geologic time.
Ch.14 – Geologic Time Earth Science.
Section 4: Chordate Evolution
PALEOZOIC ERA KNOWN AS THE AGE OF FISH OR TRILOBITES.
Geologic Time.
Chapter 14 Lesson 2 Early Earth History.
Section 2: Precambrian Time and the Paleozoic Era
The Fossil Record.
Paleozoic Era 540,000,000 yrs ago to 250,000,000 yrs ago
Paleozoic Era Life starts in the seas and moves onto land
Geological timeline events
Materials: Pencil Notebook Notes highlighter Bell work
Section 2: Precambrian Time and the Paleozoic Era
Section 2: Precambrian Time and the Paleozoic Era
GEOLOGIC TIME If it is in red, write it!.
A Quick Look at the History of Life on Earth Part 2
What is Mass Extinction?
Copyright Pearson Prentice Hall
And changes in organisms
Section 2: Precambrian Time and the Paleozoic Era
Vertebrate Evolution.
CHAPTER 12 LIFE OF THE PALEOZOIC.
LECTURE 5: Paleozoic Era Silurian/Devonian Periods (439 mya- 360 mya)
LECTURE 4: PALEOZOIC ERA Cambrian/Ordovician Periods
19.3 Evolution of Life I. Fishes first vertebrates
17-3 Evolution of Multicellular Life
The Geological Time Scale
Presentation transcript:

LECTURE 4: Paleozoic Era Silurian/Devonian Periods (439 mya- 360 mya) Explain how,why, what life colonized land during the Silurian Identify the oldest plant fossil- Cooksonia Explain the evolution of plants Describe the evolution of jaws Describe the evolution of fishes Explain how Sarcopterygians evolved into tetrapod ancestors Describe why and how fish transitioned onto land Identify the 1st Amphibian- Ichthyostega

To be an index fossil you must be: Lived for a long time Lived for a short time Found in limited locations

What happened at the beginning of the Cambrian Period? Mass extinction #1 Cambrian Explosion Evolution of Eukaryotes Evolution of Jaws

What evolved during the Cambrian-Ordovician? Jawless Fish Echinoderms Arthropods All of the Above

What caused the Mass Extinction at the end of the Ordovician? Volcanic Eruptions Global Cooling Meteor

What Index Fossil appears at the Beginning of the Silurian? Parakidograptus acuminatus Extinct group: graptolite (hemichordate)

What Significant Events Happened during the Silurian and Devonian? Life emerged from the water and colonized the land. Plants (green algae evolved into bryophytes(non-vascularized), then tracheophytes(vascularized) and animals (insects) KEY DEVELOPMENTS: The development of vascular plants, pollen and seeds provided plants with a way to reproduce and survive on dry land, creating new habitats The development of jaws allowed fishes and other emerging vertebrates to catch larger prey The development of tetrapods— limbed animals—would pave the way for animals that could walk on land

Why did Plants Move onto Land? The ozone layer shielded life like water once did Gave protection from the sun’s harmful radiation. Only water had provided this protection before Soils had formed that could nourish plant life Bacteria, algae, and fungi had gained an early foothold on land, secreting organic acids that broke rock down into its mineral elements. Nutrient-rich soils formed as these organisms died and their decaying matter combined with the minerals. The next Plants to evolve were vascular plants

What Adaptations are Required for Land Plants? Stand Upright (no support form water) Tolerate UV radiation Tolerate Climate Changes Be able to acquire nutrients from substrate other than water Produce gametes (seeds) that can move in the air

How did Plants Evolve? Green Algae Bryophytes (430 mya) Non- vascular Moist areas Mosses/liverworts (spores) Seedless Tracheophytes (420 mya) Vascular Ferns, horsetails (spores) Seed Producing Tracheophytes (365 mya) (Gymnosperms)

First land plants (Bryophytes)likely similar to extant leafy liverworts…….

What is the Oldest Fossil Plants? Cooksonia – 428 mya Bryophyte Small, few cm long No leaves, roots horizontal stems with hairs connecting to soil

Bryophytes

How did Plants Evolve? Green Algae Bryophytes (430 mya) Non- vascular Moist areas Mosses/liverworts (spores) Seedless Tracheophytes (420 mya) Vascular Ferns, horsetails (spores) Seed Producing Tracheophytes (365 mya) (Gymnosperms)

By the end of the Devonian: Extensive forests (club moss and horse tail ancestors) with tall trees (Seedless Tracheophytes- Lycophytes)--FERNS These plants later were out competed by seed plants and nearly all have gone extinct

Why did Jaws Evolve? The vertebrate jaw can be traced back to 440 mya Most jawless fishes went extinct, but jawed fishes became the ancestors for most modern fishes today. Jaws evolved from gill arches (Gnathostomes- jawed Fish) From Jawless fish (Agnathas) Helped fish catch food Jaws allow mouths to open wide and catch larger prey Jaws with teeth can bite, crush, and chew. Protected by bony, overlapping plates, Placoderms were among the first fishes with jaws

http://www. mhhe. com/cgi-bin/netquiz_get. pl http://www.mhhe.com/cgi-bin/netquiz_get.pl?qfooter=/usr/web/home/mhhe/biosci/genbio/animation_quizzes/animate_45fq.htm&afooter=/usr/web/home/mhhe/biosci/genbio/animation_quizzes/animate_45fa.htm&test=/usr/web/home/mhhe/biosci/genbio/animation_quizzes/animate_45q.txt&answers=/usr/web/home/mhhe/biosci/genbio/animation_quizzes/animate_45a.txt

Placoderm fish armored head Dunkleosteus terrelli Devonian (417-354 million years ago) Cleveland, Ohio Stretching up to twenty feet long and sporting powerful jaws (no teeth) equipped with tooth-like plates, Dunkleosteus was one of the world’s first large vertebrate predators.

FISH GROUP KEY FEATURE Jawless Fish (agnathas) 500 mya - no jaws - no paired fins - gave rise to placoderms, cartilaginous and bony fish Placoderms – First Jawed Fish (Gnathostome) 439 mya Jaws without teeth - Armored fish Cartilage Skeleton Paired fins Cartilaginous (Chondrichthyes) -sharks/rays 395 mya Cartilage skeletons - no swim bladder - no lungs - internal fertilization Jaws Bony (Osteichthyes) Actinopterygians (ray-finned) Sarcopterygians (lobe-finned) gills -Jaws - lungs - swim bladder - some developed fleshy lobe fins (gave rise to amphibians)

When did Tetrapods Evolve? Fish were the first animals to develop “feet” about 370 mya Sarcopterygian fishes had muscular lobes at the bases of their paired fins. Within these lobes were large bones, one of which connected the rest of the fin bones to the body, like toes on a foot Their fins were made for walking. Over time, some Sarcopterygian fishes may have begun using their muscular, lobed fins to "walk" in shallow, swampy waters, pushing their way through dense plant growth Tetrapods branched out to include many familiar animals. From one type of Sarcopterygian fish evolved the first tetrapods: vertebrates with four paired limbs and digits (fingers and toes)

What is a Coelacanth? "living fossil" – only lobe-finned fish in existence Evolved about 360 mya paired lobe fins that extend away from its body like legs and move in an alternating pattern, like a trotting horse

What is the Evidence for Tetrapod Evolution? Homologous Structures The front fins of certain sarcopterygian fishes and the front limbs of tetrapods share the same bones: humerus, ulna, and radius. The hind fins of certain sarcopterygian fishes and the hind limbs of tetrapods share the same bones: femur, tibia, and fibula. Sarcopterygian fins are paddle-like, while tetrapod limbs have digits (fingers and toes) that grip the ground

Evolution of Tetrapods From Water to Land Eusthenopteron: "Fish with Legs" Panderichthys “Fish with Fingers” Tiktaalik- 375 mya Acanthostega- 365 mya Ichthyostega – 360 mya

Eusthenopteron: "Fish with Legs"

Panderichthys (“Fish with Fingers”)

Tiktaalik- 375 mya Extinct Sarcopterygian They may have begun using their muscular, lobed fins to "walk" in shallow, swampy waters, pushing their way through dense plant growth Eventually they would move from shallow waters to land

Acanthostega- 365 mya First Fish with Digits (8 of them) on each limb Probably Stayed in shallow waters Limbs could not support weight

Ichthyostega – 360 mya First 4-legged land animal- Amphibian Stayed near water

What were the Characteristics of Early Tetrapods? It lived in the water and had a long, fishy tail But its feet had 8 digits (more than any living tetrapod has today)

Hynerpeton

What Happened at the End of the Devonian Period (360 mya)? Mass Extinction #2 Continental Movement Continents had moved over the South Pole Because of the pole’s year-round cold climate, snowfall accumulated on the continents, forming glaciers The climate became too cold for many species With much of Earth’s water frozen into glaciers, sea levels dropped. Lower sea levels would have robbed life of their habitat in the shallower oceans.

Who was Impacted by the Mass Extinction? Up to 70% of all marine species may have died out Reefs, and the life they supported, were devastated Many species of corals, brachiopods, trilobites, and mollusks disappeared The armored fishes—placoderms and ostracoderms—were completely wiped out

Sea Levels and Temp vs. Time

Explain how,why, what life colonized land during the Silurian Identify the oldest plant fossil- Cooksonia Explain the evolution of plants Describe the evolution of jaws Describe the evolution of fishes Explain how Sarcopterygians evolved into tetrapod ancestors Describe why and how fish transitioned onto land Identify the 1st Amphibian- Ichthyostega