GY 112L: Earth History Lab
|
|
- Godfrey Underwood
- 5 years ago
- Views:
Transcription
1 UNIVERSITY OF SOUTH ALABAMA GY 112L: Earth History Lab Week 11 Paleozoic Part 2 Instructor: Dr. Douglas W. Haywick
2 Today s Agenda The Paleozoic Part 2 (Lab 8 exercises) 1) Sponges & Stromatoporoids 2) Stromatolites 3) Corals 4) Bryozoans 5) Stratigraphy
3 Sponges Sponge Facts: Phylum: Porifera
4 Sponges Sponge Facts: Phylum: Porifera Range: Cambrian-Recent
5 Sponges excurrent pore incurrent pore Sponge Facts: Phylum: Porifera Range: Cambrian-Recent Mode of Life: Marine, benthic, filter feeder excurrent pore
6 Sponges Sponge Facts: Phylum: Porifera Range: Cambrian-Recent Mode of Life: Marine, benthic, filter feeder Mineral composition: spongin with spicules or calcite (calcisponges)
7 Sponges Sponge Facts: Phylum: Porifera Range: Cambrian-Recent Mode of Life: Marine, benthic, filter feeder Mineral composition: spongin with spicules or calcite (calcisponges) Fossil Pres.: mineral replacement or pristine
8 Stromatoporoids Now known to be a type of sponge. They were important paleozoic reef builders
9 Stromatoporoids Stromatoporoid Facts: Phylum: Porifera Range: Ordovician-Mississippian Cretaceous? Mode of Life: Marine, benthic, filter feeder Mineral composition: calcite Fossil Pres.: pristine
10 Stromatolites The first visible fossils
11 Stromatolites Stromatolite Facts: Kingdom: Cyanobacteria Range: Archean-Recent Mode of Life: Marine, benthic, colonial, photosynthesis Mineral composition: calcite Fossil Pres.: pristine
12 Corals One of the most important animals as far as geology is concerned. They evolved early and showed amazing diversity
13 Corals Phylum: Cnidaria Coral Facts:
14 Corals Coral Facts: Phylum: Cnidaria Class: Anthozoa
15 Corals Coral Facts: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia
16 Corals Coral Facts: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Range: Rugosa (Cambrian-P/T)
17 Corals Coral Facts: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Range: Rugosa (Cambrian-P/T) Tabulata (Ordovician-P/T)
18 Corals Coral Facts: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Range: Rugosa (Cambrian-P/T) Tabulata (Ordovician-P/T) Scleractinia (Triassic-Recent)
19 Corals Coral Facts: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Range: Rugosa (Cambrian-P/T) Tabulata (Ordovician-P/T) Scleractinia (Triassic-Recent) Mode of Life: Marine, benthic, filter feeder, colonial or solitary (stinging cells)
20 Corals Coral Facts: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Range: Rugosa (Cambrian-P/T) Tabulata (Ordovician-P/T) Scleractinia (Triassic-Recent) Mode of Life: Marine, benthic, filter feeder, colonial or solitary (stinging cells) Mineral composition: calcite or aragonite
21 Corals Coral Facts: Phylum: Cnidaria Class: Anthozoa Subclass: Rugosa Tabulata Scleractinia Range: Rugosa (Cambrian-P/T) Tabulata (Ordovician-P/T) Scleractinia (Triassic-Recent) Mode of Life: Marine, benthic, filter feeder, colonial or solitary (stinging cells) Mineral composition: calcite or aragonite Fossil Pres.: pristine, molds/chalky/replaced
22 Bryozoans (Moss Animals) Bryozoan Facts: Phylum: Bryozoa (old) Phyla: Entoprocta, Ectoprocta (new)
23 Bryozoans Bryozoan Facts: Phylum: Bryozoa (old) Phyla: Entoprocta, Ectoprocta (new) Range: Ordovician-Recent
24 Bryozoans Bryozoan Facts: Phylum: Bryozoa (old) Phyla: Entoprocta, Ectoprocta (new) Range: Ordovician-Recent Mode of Life: Marine, benthic, filter feeder, colonial
25 Bryozoans Bryozoan Facts: Phylum: Bryozoa (old) Phyla: Entoprocta, Ectoprocta (new) Range: Ordovician-Recent Mode of Life: Marine, benthic, filter feeder, colonial Mineral composition: calcite and aragonite
26 Bryozoans Bryozoan Facts: Phylum: Bryozoa (old) Phyla: Entoprocta, Ectoprocta (new) Range: Ordovician-Recent Mode of Life: Marine, benthic, filter feeder, colonial Mineral composition: calcite and aragonite Fossil Pres.: pristine
27 Bryozoan Forms Digitate Lacy
28 Bryozoan Anatomy The living chambers are called zooecia The animals are called zooids
29 Stratigraphy and Rock Suites Collections of rocks from a specific region that cover a specific time frame 1) Niagara Falls (limestone and dolostone)
30 Stratigraphy and Rock Suites Why a waterfall and not a set of rapids? Consider the stratigraphy. 1) Niagara Falls
31 Rate of retreat Stratigraphy and Rock Suites
32 Lab Time
33 GY 112L: Earth History Lab 8: Paleozoic Rocks and Fossils 2 Instructor: Dr. Doug Haywick dhaywick@southalabama.edu This is a free open access lecture, but not for commercial purposes. For personal use only.
GY 112L: Earth History Lab
UNIVERSITY OF SOUTH ALABAMA GY 112L: Earth History Lab Week 9: Paleozoic Part 3 Instructor: Dr. Douglas W. Haywick Today s Agenda The Paleozoic Part 3 (Week 9 exercises) 1) Brachiopods 2) Molluscs 3) Alabama
More informationQuiz Four (9:30-9:35 AM)
Quiz Four (9:30-9:35 AM) UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Fossils Part 1: Telling Time Instructor: Dr. Douglas W. Haywick Last Time A) Stable isotopes of use to geology (fractionation)
More informationLecture 24: Paleozoic 1:
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lecture 24: Paleozoic 1: Laurentia Instructor: Dr. Douglas W. Haywick Last Time (before the exam) The Cambrian Explosion A) Why a Cambrian explosion B)
More informationGY 112L Lab Assignment 8 Paleozoic Lab 2
Name: Grade /100 (+5 bonus) Percent: GY 112L Lab Assignment 8 Paleozoic Lab 2 Note: There are a lot of specimens to look at in this weeks lab. It is probably best for you to look at the physical specimens
More informationGY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 21: Rock Deformation Instructor: Dr. Douglas W. Haywick Last Time A) How long is long? B) Geological time divisions Web notes 20 Geological
More informationSkeletal grains. Pores. Matrix <20 m) Cement. Non-skeletal grains. 1 cm
Components of a Carbonate rock Skeletal grains Pores Matrix
More informationLab 4 Identifying metazoan phyla and plant groups
Geol G308 Paleontology and Geology of Indiana Name: Lab 4 Identifying metazoan phyla and plant groups The objective of this lab is to classify all of the fossils from your site to phylum (or to plant group)
More informationQuiz Three (9:30-9:35 AM)
Quiz Three (9:30-9:35 AM) UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lecture 7 & 8: Dating Instructor: Dr. Douglas W. Haywick Last Time 1. William Smith and Water 2. Stratigraphic Principles 3.
More informationGY 112L: Earth History
UNIVERSITY OF SOUTH ALABAMA GY 112L: Earth History Lab Lecture 1: Rock Review Instructor: Dr. Douglas W. Haywick Introductory Agenda 1. Contact info for D. Haywick 2. GY 112L Course Outline (syllabus)
More informationRadiolaria and the Rock Record
1 Radiolaria and the Rock Record Radiolarians are important constituents of chert at certain times in geologic history. Their tests accumulate on the seafloor today to form radiolarian ooze, particularly
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 22: Reefs Instructor: Dr. Douglas W. Haywick Last Time Shelves Definition and a bit of history Factors controlling shelf sedimentation
More information1. Identify this organism (it is 1mm in diameter) 2. The shell or of this organism is made of 3. How do these one-celled organism feed? 4.
Fossil Test 2 1. Identify this organism (it is 1mm in diameter) 2. The shell or of this organism is made of 3. How do these one-celled organism feed? 4. Describe the biological and geological importance
More informationQuiz Nine (9:30-9:35 AM)
Quiz Nine (9:30-9:35 AM) UNIVERSITY OF SOUTH ALAAMA GY 112: Earth History Lecture 25: Paleozoic 2: More Laurentia! Instructor: Dr. Douglas W. Haywick Last Time The Paleozoic of North America 1) Laurentian
More informationMarine Invertebrates in the Paleozoic Seas
Marine Invertebrates in the Paleozoic Seas The fossils of shell-bearing invertebrates that inhabited shallow seas are common in Paleozoic rocks. Archaeocyathids, sponges, corals, bryozoans, trilobites,
More informationQuiz 12 Bonus 2 (9:30-9:35 AM)
Quiz 12 Bonus 2 (9:30-9:35 AM) UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lectures 32 and 33: Mesozoic Sedimentation Instructor: Dr. Douglas W. Haywick Last Time Mesozoic Tectonics A) The Triassic
More informationGY 112: Earth History. Fossils Part:
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Fossils Part: Telling Time Predicting Paleoenvironments Instructor: Dr. Douglas W. Haywick Last Time 1. Chronostratigraphy versus biostratigraphy 2. Paleontological
More information2010 National Science Olympiad Fossil Test Final Qs & A s
2010 National Science Olympiad Fossil Test Final Qs & A s Note: Fossil pictures are unavailable (consider using the internet for samples) Station 1 Specimens A and B. DO NOT WRITE ON THIS SHEET USE YOUR
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 21: Shelves Instructor: Dr. Douglas W. Haywick Last Time Carbonate Petrography Beasties (know your enemy!) Corals Molluscs (gastropods
More informationGY 112 Lecture Notes Cambrian Explosion
GY 112 Lecture Notes D. Haywick (2006) 1 GY 112 Lecture Notes Cambrian Explosion Lecture Goals: A) Phanerozoic time frame (Paleozoic Era) B) Why a Cambrian explosion C) Introducing our ancestors Textbook
More informationThe Proterozoic Part 1
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History The Proterozoic Part 1 Lectures 18/19: Tectonics Instructor: Dr. Douglas W. Haywick Last Time 1) The Early Atmosphere 2) The Oceans and Hydrosphere 3)
More informationChapter 12. Life of the Paleozoic
Chapter 12 Life of the Paleozoic Paleozoic Invertebrates Representatives of most major invertebrate phyla were present during Paleozoic, including sponges, corals, bryozoans, brachiopods, mollusks, arthropods,
More informationChapter 12. Life of the Paleozoic
Chapter 12 Life of the Paleozoic Paleozoic Invertebrates Representatives of most major invertebrate phyla were present during Paleozoic, including sponges, corals, bryozoans, brachiopods, molluscs, arthropods,
More informationGY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 25: Metamorphic Facies Last Time Contact Metamorphism A) Metamorphic Aureoles B) Isograds C) Index minerals and metamorphic grade Contact Metamorphism
More informationLab 9: Fossils, paleontology and the complete reconstruction
Geology 103 Name: Lab 9: Fossils, paleontology and the complete reconstruction Objective: To classify fossil organisms and to demonstrate how fossil assemblages are constructed. Finally, to determine the
More informationSTATION 4. STATION refer to specimen in box see page 3 for pictures for online version. Can you name this fossil? Class
STATION 1 Can you name this fossil? Phylum Class STATION 2 --- refer to specimen in box see page 3 for pictures for online version Identify the Phylum of each specimen Genus When did he live? Cambrian,
More informationGY 112: Earth History
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lecture 8a: Stable Isotope Stratigraphy Instructor: Dr. Douglas W. Haywick GY 112: Lecture test preparation Thursday February 9th Word List for Lecture
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 12: Petrology of Immature Siliciclastic Sed. Rocks Instructor: Dr. Douglas W. Haywick Last Time 1. Factors promoting beach development
More informationSponge and Cnidarian Review
Name Period Date Sponge and Cnidarian Review Matching On the lines provided, write the letter of the definition that matches each term. 1. Invertebrate 2. Filter feeder 3. Asymmetry 4. Radial 5. Medusa
More informationCycles in the Phanerozoic
Cycles in the Phanerozoic Evolutionary trends: extinctions, adaptive radiations, diversity over time Glaciations Sea level change Ocean chemistry Atmospheric CO 2 biosphere Mass extinctions in the..you
More informationGY 112 Lecture Notes Proterozoic Life forms
GY 112 Lecture Notes D. Haywick (2006) 1 Lecture Goals: A) Eukaryote Life forms (Acritarchs) B) Metazoans (Ediacaran Fauna) GY 112 Lecture Notes Proterozoic Life forms Textbook reference: Levin 7 th edition
More informationGY 112: Earth History
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lectures 31: Mesozoic Tectonics Instructor: Dr. Douglas W. Haywick Last Time Mesozoic Overview A) The end of the Paleozoic B) Mesozoic time frame and evolutionary
More informationQuiz Seven (2:00 to 2:02 PM)
Quiz Seven (2:00 to 2:02 PM) UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 22: Agents of Metamorphism Instructor: Dr. Douglas W. Haywick Last Time Rock Deformation A) Confining pressure
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 9: Walther s Law Instructor: Dr. Douglas W. Haywick Today s Agenda 1. Walther s Law 2. Sequence stratigraphy 3. Markov Chain Analysis Named
More informationNeoarchean to Mesoarchean Ga
Name: Answers Geology 1023 Lab #7, Winter 2014 Shields & Precambrian life forms Lab day: Tu W Th Shields are the oldest (and most stable) parts of the continental masses. They consist of rocks of Precambrian
More information402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA 402: Sedimentary Petrology Lecture 14: Siliciclastic Diagenesis Instructor: Dr. Douglas W. Haywick Last Time (online) Immature siliciclastic sediment and sedimentary rocks Pictorial
More informationGY 302: Crystallography & Mineralogy
UNIVERSITY OF SOUTH ALABAMA GY 302: Crystallography & Mineralogy Lecture 7a: Optical Mineralogy (two day lecture) Instructor: Dr. Douglas Haywick This Week s Agenda 1. Properties of light 2. Minerals and
More informationGY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 1: Introduction to Physical Geology Instructor: Dr. Douglas W. Haywick Today s Agenda 1. Introductions and class policy 2. What do geologists
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 16: Volcaniclastic Petrography Instructor: Dr. Douglas W. Haywick Last Time (online) Moscow Landing, Alabama Photo credit: Jan Smit (http://www.geo.vu.nl/~smit/indexjansmit/jansmitindex.htm)
More informationChapter 7. Marine Animals Without a Backbone
Chapter 7 Marine Animals Without a Backbone General Characteristics of Animals Multicellular, diploid organisms with tissues, organs or organ systems in most Heterotrophic Require oxygen for aerobic
More informationGY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 3: The Rock Cycle Instructor: Dr. Douglas W. Haywick Last Time 1. Alfred Wegener and Drifting Continents 2. The Plate Tectonic Revolution 3.
More informationLecture 14/15: Evolution
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lecture 14/15: Evolution Instructor: Dr. Douglas W. Haywick Last Time 1) Linne (the Linnaean System) 2) Taxonomy ordering 3) Some examples (important beasties
More informationLecture 9 PHYLUM PROTOZOA
Lecture 9 PHYLUM PROTOZOA The Protozoa include a diversity of one-celled aquatic organisms, most of which are less than one millimetre in diameter. A shell is secreted by members of two groups, the Foraminifera
More informationChapter 8. Sponges Phylum Porifera Basic characteristics: simple asymmetric sessile
Chapter 8 Key Concepts Sponges are asymmetric, sessile animals that filter food from the water circulating through their bodies. Sponges provide habitats for other animals. Cnidarians and ctenophores exhibit
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 5: Bedform Development (Flume Studies) Instructor: Dr. Douglas W. Haywick Today s Lecture 1. What s a flume? 2. Traction induced bed forms
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 8: Sedimentary Facies Instructor: Dr. Douglas W. Haywick Last Time Sedimentary sections 1. Important sedimentary data 2. Examples of sedimentary
More informationGY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 9: Extrusive Igneous Rocks Instructor: Dr. Douglas W. Haywick Last Time 1) The chemical composition of the crust 2) Crystallization of molten
More informationEarth Science 105 Geologic Time Chapter 11
Correlation of rock layers Earth Science 105 Geologic Time Chapter 11 Earth Science 11 th ed. Tarbuck & Lutgens Matching same age rocks In local area Across wide area In different regions Grand Canyon
More informationEarth Science 105. Geologic Time Chapter 11. Earth Science 11 th ed. Tarbuck & Lutgens
Earth Science 105 Geologic Time Chapter 11 Earth Science 11 th ed. Tarbuck & Lutgens Correlation of rock layers Matching same age rocks In local area Across wide area In different regions Grand Canyon
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 17: Sandy Fluvial Depositional Environments Instructor: Dr. Douglas W. Haywick Last Time Volcaniclastic Sedimentary Rocks 1. Origin of
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 27: Introduction to Wireline Log Interpretations Instructor: Dr. Douglas W. Haywick Last Time Carbonate Diagenesis Diagenesis 0.5 mm PPL
More informationShield was above sea-level during the Cambrian and provided the sediment for the basins.
Name: Answers Geology 1023 Lab #8, Winter 2014 Platforms and Paleozoic life-forms Lab day: Tu W Th 1. Schematic geologic cross-sections A-B and C-D (shown below) cross the edge of the continental platform
More informationUNIT 8A MARINE SCIENCE: Lower Invertebrates
UNIT 8A MARINE SCIENCE: Lower Invertebrates Essential Questions: What are the characteristics of the simple body structured organisms? Unit Objectives/I Can Statements: General Invertebrates 1. List taxa
More informationZoology Name: Block: Exercise #7: The Sponges, Phylum Porifera Lab Guide
Zoology Name: Block: Exercise #7: The Sponges, Phylum Porifera Lab Guide Members of the phylum Porifera are considered the simplest metazoans, they are little more than a loose grouping of cells, with
More informationGY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 14: Sedimentary Rocks Part 2: Alluvial Fans and Rivers Instructor: Dr. Douglas W. Haywick Last Time 1) Types of Sediment 2) Sedimentary Rock
More informationModule 4: Marine Invertebrates I. Kingdom Animalia
Module 4: Marine Invertebrates I Kingdom Animalia Kingdom Animalia Contains the largest number of species We will split them into 2 large groups Invertebrates- Animals w/o a backbone Vertebrates- Animals
More informationCOMPARISON BETWEEN PORIFERA AND CNIDARIA. Colwyn Sleep
COMPARISON BETWEEN PORIFERA AND CNIDARIA Colwyn Sleep INTRODUCTION Porifera Cnidaria Porifera and Cnidaria are organisms which share similar characteristics with one another. -They are both multicellular,
More informationPh. Porifera and Ph. Cnidaria
I. Phylum Porifera (sponges; pore bearer ) A. General characteristics 1. simplest animals 2. asymmetric 3. aquatic habitats a. typically marine 4. live alone or in colonies a. often members of reef habitats
More informationAnimal Diversity I: Porifera, Cnidaria, Ctenophora, Platyhelminthes, Rotifera, Annelida
1 Animal Diversity I: Porifera, Cnidaria, Ctenophora, Platyhelminthes, Rotifera, Annelida Objectives: Be able to distinguish radial symmetry from bilateral symmetry. Be able to identify which of the phyla
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 6: Primary and Diagnostic Sedimentary Structures Instructor: Dr. Douglas W. Haywick Today s Lecture 1. Models of traction structures 2.
More informationNotes - Porifera and Cnideria
Notes - Porifera and Cnideria - Animals exist on every continent on the planet. Most people consider animals to be the most important kingdom as we are considered animals. But, what is an animal? What
More informationTHE ORDOVICIAN EXTINCTION. 444 million years ago
THE ORDOVICIAN EXTINCTION 444 million years ago TOTAL GENERA THROUGH THE PHANEROZOIC ERA The Cambrian to the Present PERMIAN TRIASSIC CRETACEOUS Holocene The Present Miocene DEVONIAN ORDOVICIAN Mississippian
More informationReefs: Rainforests of the Marine Realm. A Symbiotic World: The Significance of Symbiosis in the Fossil Record. Reefs Through Time
Reefs: Rainforests of the Marine Realm A Symbiotic World: The Significance of Symbiosis in the Fossil Record A reef, rising above the sea floor, is an entity of its own making - a sedimentary system within
More informationGY 302: Crystallography & Mineralogy
UNIVERSITY OF SOUTH ALABAMA GY 302: Crystallography & Mineralogy Lecture 7b: Optical Mineralogy Instructor: Dr. Douglas Haywick Last Time 1. Properties of light 2. Minerals and light transmission Light
More informationFossils Fossil Identification and Analysis Lab Walk Through Earth Science Essentials-Advanced by Russ Colson
Fossils Fossil Identification and Analysis Lab Walk Through Earth Science Essentials-Advanced by Russ Colson I've provided more specific guidance for this lab than for the previous ones, including giving
More informationPLANET EARTH CAMBRIDGE UNIVERSITY PRESS. Cesare Emiliani. Cosmology, Geology, and the Evolution off Life and Environment
PLANET EARTH Cosmology, Geology, and the Evolution off Life and Environment Cesare Emiliani Department of Geological Sciences, The University of Miami CAMBRIDGE UNIVERSITY PRESS Preface page xi PART I
More informationLab ( 3) Kingdom: Animalia
Lab ( 3) Kingdom: Animalia Characteristics of animals: - Multicellular - Eukaryotic organisms - Cells with out cell wall Animalia is divided in two group : A/ Invertebrate ( animals with out backbones
More informationMesozoa, Parazoa, and Metazoa. Chapter 12 pg. 239
Mesozoa, Parazoa, and Metazoa Chapter 12 pg. 239 3 Multicellular Groups: Mesozoa, Parazoa, Eumetazoa Multicellular organisms are divided into three groups: Mesozoa, Parazoa (phylum Porifera, phylum Placozoa)
More informationPALEONTOLOGY. Muhittin Görmüş Department of Geology. Lecture gov.tr/bilgipaket/jeolojik /index.htm
PALEONTOLOGY http://www.biltek.tubitak. gov.tr/bilgipaket/jeolojik /index.htm Muhittin Görmüş Department of Geology http://members.cox.net/jdmount/paleont.html 1. Hemicordata General characteristics Classification
More information12.1. Advent of Multicellularity A. Advantages 1. Nature s experiments with larger organisms without cellular differentiation are limited. 2. Increasi
Phylum: Porifera The Sponges 12.1. Advent of Multicellularity A. Advantages 1. Nature s experiments with larger organisms without cellular differentiation are limited. 2. Increasing the size of a cell
More informationGENERAL GUIDE TO FOSSIL IDENTIFICATION AND PALEOECOLOGY
EARTH HISTORY AND THE FOSSIL RECORD GEOL220 GENERAL GUIDE TO FOSSIL IDENTIFICATION AND PALEOECOLOGY Eurypteris remipes State Fossil of New York Compiled by J. R. Ebert Illustrations from Linsley (1994)
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 28: Student Choice Lecture 1: Sequence Stratigraphy Instructor: Dr. Douglas W. Haywick Today Sequence Stratigraphy The basic concept (systems
More informationQuiz Three (2:00 to 2:05 PM)
Quiz Three (2:00 to 2:05 PM) UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 6: Plate Tectonics and Volcanism Calbuco volcano (Chile) (March, 2015) https://www.reddit.com/r/photoshopbattles/comments/
More informationTIME LINE OF LIFE. Strip for Clock of Eras representing the circumference. 1. Review the eras represented on the Clock of Eras:
TIME LINE OF LIFE Material Time Line of Life Working Time Line of Life Clock of Eras Strip for Clock of Eras representing the circumference Elastic strip for Clock of Eras Presentation 1: Overview 1. Review
More informationGY 112L Lab Assignment 5 Modes of Fossil Preservation
Name: Grade /100 (+5 bonus) Percent: GY 112L Lab Assignment 5 Modes of Fossil Preservation Note: In this lab we will begin to look at fossilized animals, plants, and their traces. You will soon become
More information2 Eras of the Geologic Time Scale
CHAPTER 8 2 Eras of the Geologic Time Scale SECTION The History of Life on Earth BEFORE YOU READ After you read this section, you should be able to answer these questions: What kinds of organisms evolved
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 13: Immature Siliciclastic Sedimentary Environments Alluvial Fans, Braided Streams Instructor: Dr. Douglas W. Haywick Last Time Immature
More informationMARINE SCIENCE. Monday 9 Apr 2018
MARINE SCIENCE Monday 9 Apr 2018 Entry Task Grab your ISN from the front counter. Agenda Housekeeping Variables Graphing Techniques Housekeeping No more breaks for the remainder of the month. Variables
More informationScience B-16: The History of Life
Science B-16: The History of Life Lab 1: The Invertebrate Phyla Objectives The object of this lab is to get you familiar with the sorts of organisms that comprise the fossil record. We ll discuss how fossils
More information2009 Fossil notes Div B
The Objectives of this event are to: 2009 Fossil notes Div B 1. Create the motivation and interest in the pursuit of the earth sciences. 2. Understand the identity of fossils and the process of fossilization.
More informationQuiz Two (9:30-9:35 AM)
Quiz Two (9:30-9:35 AM) UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lecture 5: Clever Thinking 2: Plate Tectonics Instructor: Dr. Douglas W. Haywick Last time... 1. The first geologists and their
More informationField trip to Racine Reef Complex, Thornton Quarry, Illinois
Field trip to Racine Reef Complex, Thornton Quarry, Illinois Primary objectives for this fieldtrip 1) Collect and identify the fossils of the Racine Reef Complex. 2) Discuss procedures for collecting fossil
More informationFossils and Geology of Litzsinger Road Ecology Center
Fossils and Geology of Litzsinger Road Ecology Center Table of Content Key Terms 1 Key Terms 2 What you need to know Geologic Map of Missouri Geologic Time Chart More of what you need to know Digital map
More informationGY 112L Earth History
GY 112L Earth History Lab 2 Vertical Successions and Sequences of Events GY 112L Instructors: Douglas Haywick, James Connors, Mary Anne Connors Department of Earth Sciences, University of South Alabama
More informationSpring th Grade
Spring 2015 8 th Grade The geologic time scale is a record of the major events and diversity of life forms present in Earth s history. The geologic time scale began when Earth was formed and goes on until
More informationPTYS 214 Spring Announcements Midterm #4: two weeks from today!
PTYS 214 Spring 2018 Announcements Midterm #4: two weeks from today! 1 Previously Radiometric Dating Compare parent / daughter to determine # of half lives 14C, 40K, 238U, 232Th, 87Ru Evidence for Early
More informationLab 2 Phylum Porifera and phylum Cnidaria. Grantia. Phylum Porifera. Kingdom :- Animalia. Phylum:- Porifera. Class:- Calcarea. Order:- Leucosolenida
Lab 2 Phylum Porifera and phylum Cnidaria Phylum Porifera Adults sessile and attached Radial symmetry or asymmetrical Multi-cellular ; loose aggregation of cells Skeleton made of collagen and spicules
More informationbasal animalia porifera, cnidaria
basal animalia porifera, cnidaria PHYLUM PORIFERA porifera Sponges, no tissues or organs, cellular level of organization outer layer is made of cells called pinacocytes choanocytes (collar cells) Flagella
More informationQuiz Five (9:30-9:35 AM)
Quiz Five (9:30-9:35 AM) UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 10: Intrusive Igneous Rocks Instructor: Dr. Douglas W. Haywick Last Time 1) Pyro-what? (air fall volcanic rocks) 2)
More informationFossils, Environments, and Geologic Time
Fossils, Environments, and Geologic Time By Rachel Dolbier, W.M. Keck Earth Science and Mineral Engineering Museum & D.D. LaPointe, Nevada Bureau of Mines and Geology In this activity, we will evaluate
More informationEarth s s Geologic History
The Earth s s Geologic History and The Earth s s Interior Earth s s Geologic History Geologic timescale Divides Earth s s history into relative time periods Relative dating based on: (apply for entire
More informationGY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 7: Sedimentary Sections Instructor: Dr. Douglas W. Haywick Last Time (online) 1. Models of traction structures 2. Sediment transport versus
More informationHistorical Geology GEL 102 Syllabus Spring, 2015
Historical Geology GEL 102 Syllabus Spring, 2015 Dr. Jacob Sewall sewall@kutztown.edu 484-646-5864 http://faculty.kutztown.edu/sewall Boehm Bldg. 422 Office hours: M: 10 12, T: 9:30 10 W: 10 12, TH: 9:30
More informationWisconsin Science Olympiad 2015 West Regional Fossils. Team Name:
Wisconsin Science Olympiad 2015 West Regional Fossils Team Name: Team Members: There are 12 stations and you will have approximately 3-4 minutes at each one. Each page of the test corresponds to one of
More informationTeam members (First and Last Names): Fossil lab
Team members (First and Last Names): Period: Group #: Fossil lab Background: Fossils are traces of organisms that lived in the past. When fossils are found, they are carefully excavated and then analyzed.
More informationGeological Time How old is the Earth
Geological Time How old is the Earth How old is everything? Universe? Universe ~ 14 Billion Years Old Milky Way Galaxy? Milky Way Galaxy - 10 Billion Years Old Solar System? Solar System -4.6 Billion Years
More informationEarth History & the Fossil Record
Earth History & the Fossil Record The Dynamic Earth Earth s Dynamic Geology Earth is approx. 4.6 billion years old Since its formation, the surface has been unstable Crust and Core rotate as slightly different
More informationBiomineralisation. Dr. Abby Smith. Department of Marine Science University of Otago
Biomineralisation Dr. Abby Smith Department of Marine Science University of Otago Biomineralisation Biomineralisation is the process by which living organisms produce mineral products, usually skeletal
More informationBIFs. BIFs. Last time we covered. Oxygen. Oxygen
UNIVERSITY OF SOUTH ALABAMA Last time we covered Archean Oceans Discussion (Robbie) MAS 603: Geological Oceanography Banded Iron Formations (Evolution of the Earth s atmosphere and hydrosphere) Lecture
More informationRock cycle diagram. Relative dating. Placing rocks and events in proper sequence of formation Deciphering Earth s history from clues in the rocks
Geologic Time Rock cycle diagram Leaves of History Chapter 21 Modern geology Uniformitarianism Fundamental principle of geology "The present is the key to the past Relative dating Placing rocks and events
More informationGeologic Time. Geologic Events
Geologic Time Much of geology is focused on understanding Earth's history. The physical characteristics of rocks and minerals offer clues to the processes and conditions on and within Earth in the past.
More information