The Geology of the Paleozoic Era

Mar 30, 2013

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The Paleozoic Era. . Geologic periods in Paleozoic record 7% of Earth's history Cambrian, Ordovician, Silurian, Devonian Carboniferous (Miss., Penn.) Permian Boundaries in the major divisions originally defined by changes in the fossil recordStart of the Paleozoic used to be defined by appearance of first easily visible fossils; later lowered to include small shelly fauna; then lowered further to first appearance of complex branching trace fossils. .

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The Geology of the Paleozoic Era

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Lecture 19 Life of the Late Paleozoic Era

Lecture 19 Life of the Late Paleozoic Era. Historical Geology. Late Paleozoic Life. I Late Paleozoic Marine Communities II Late Paleozoic Land Communities A) Plants 1) Spore-bearing Plants 2) Gymnosperms B) Metazoans (Animals) 1) Reptiles 2) The Amniotic Egg

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Paleozoic Era Invertebrates

Paleozoic Era Invertebrates. Chapter 12 Part 2. Cambrian. Cambrian explosion Burgess Shale Trilobites, brachiopods, archaeocyathids Sauk Sea regression. Ordovician. Tippecanoe sequence Warm climate New environments. Ordovician sea floor. New diversity of fauna with shells.

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Early Paleozoic Geology

Early Paleozoic Geology. Chapter 10 Part 1. Early Paleozoic Cambrian Ordovician Silurian. Precambrian rocks. Precambrian: formed First crust First continents First supercontinent (broke up too) Shield: exposed Precambrian rock Craton: buried and exposed Precambrian rock

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HISTORICAL GEOLOGY LECTURE 9. EARLY PALEOZOIC GEOLOGY II.

HISTORICAL GEOLOGY LECTURE 9. EARLY PALEOZOIC GEOLOGY II. . ORDOVICIAN (488-443 MYBP) 1. Paleogeography

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North America During the Paleozoic Era

Cambrian Period. . Ordovician Period. . Clastic wedge developed NW of Taconic High-lands, tidal flat and alluvial/delta sediments in-clude Red Mountain Fm. in NW Ga. and Birmingham, AL.. 5. Silurian Period. . Devonian PeriodThe presence of widespread reefs and evaporite deposits indicate the climate was uniformly warm and mild world-wide, and generally dry. .

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Section 2: Precambrian Time and the Paleozoic Era

Section 2: Precambrian Time and the Paleozoic Era. Preview Objectives Evolution Precambrian Time The Paleozoic Era. Objectives. Summarize how evolution is related to geologic change. Identify two characteristics of Precambrian rock.

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The LATE Paleozoic Era

The LATE Paleozoic Era. One Giant Leap for Evolution Charles Roelant Nicolas Ciccone. The Devonian Period. Known as the “Age of the Fishes”

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PALEOZOIC ERA

PALEOZOIC ERA. Age of sea-life. CAMBRIAN. 542 mya Gondwanaland- mainly in S. Hemisphere “ waterworld ”. CAMBRIAN LIFE. Ocean life Trilobites- over 800 species First shells. Ordovician. 505 mya Mostly water (still) Barren land. Ordovician. Ocean life- warm reefs Mollusk

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Paleozoic Era

Paleozoic Era. By: Sade. What is The Paleozoic Era. The Paleozoic Era is time period hundreds of million years ago. The dinosaurs were alive during the Paleozoic Era. . What Animals Were Alive During The Paleozoic Era. BECAUSE...Shallow seas covered most of the continents...

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Paleozoic Era Carboniferous Period

Paleozoic Era Carboniferous Period. 359-299mya “Coal Age,” very well known for plant fossils that make up the world’s major coal seams “Age of the Amphibians,” including ancestors of modern terrestrial vertebrates Diversification of terrestrial and aquatic arthropods

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HISTORICAL GEOLOGY LECTURE 10. LATE PALEOZOIC GEOLOGY I.

HISTORICAL GEOLOGY LECTURE 10. LATE PALEOZOIC GEOLOGY I. . The Late Paleozoic (Devonian-Mississippian-Pennsylvanian-Permian) is noted for a number of geologically significant events:. - widespread COLONIZATION of the land by large plants, reptiles and amphibians.

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Life of the Paleozoic

Life of the Paleozoic. CHAPTER 10. Paleozoic Organism Innovations. Shelly fauna Land plants Amniotes Vertebrates. Precambrian Life. Precambrian life begins as: Prokaryotes (beginning at least 3.5 bya, possibly 3.8 bya or more, in the Archean)

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The Late Paleozoic Era

The Late Paleozoic Era. Geology 103. Sea level changes. Kaskasia transgression starts in Devonian, continues to the end of the Mississippian Absaroka transgression begins in Pennsylvanian, continues to Triassic. Late Paleozoic plate configuration. Basically, Pangea is assembling

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The Geology of the Cenozoic Era

The Geology of the Cenozoic Era. Introduction. The Cenozoic began ~65 mya and continues until the present Cenozoic rocks are more easily accessible and less deformed than older rocks divided into the Tertiary and Quaternary. Early Work on the Cenozoic.

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Paleozoic Era

Paleozoic Era. Continents in late Proterozoic Eon. Cratons and Mobile Belts. Rodinia began breaking apart sometime during the late Proterozoic By the beginning of the Paleozoic Era, six major continents were present Each continent can be divided into two major components a craton

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Paleozoic Era

Life starts in the seas and moves onto land. Paleozoic Era. Six periods : Cambrian Ordovician Silurian Devonian Carboniferous Permian. 570,000,000 years ago to 225,000,000 years ago. Cambrian Period (570-500 MYA).

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Section 2: Precambrian Time and the Paleozoic Era

Section 2: Precambrian Time and the Paleozoic Era. Preview Key Ideas Evolution Precambrian Time The Paleozoic Era. Key Ideas. Summarize how evolution is related to geologic change. Identify two characteristics of Precambrian rock.

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The Early Paleozoic Era

The Early Paleozoic Era. Geology 103. Precambrian Washington…doesn ’ t exist. In fact, you ’ d have to go to the Idaho-Montana border to see rocks of Precambrian age

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PALEOZOIC ERA

PALEOZOIC ERA. KNOWN AS THE AGE OF FISH OR TRILOBITES. Life starts in the seas and moves onto land. Paleozoic Era. Six periods : Cambrian Ordovician Silurian Devonian Carboniferous-2 periods included Permian. Timeframe: 544 million to 248 million years ago. IMPORTANT FACTS.

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HISTORICAL GEOLOGY LECTURE 8. EARLY PALEOZOIC GEOLOGY I.

HISTORICAL GEOLOGY LECTURE 8. EARLY PALEOZOIC GEOLOGY I. Introduction The Paleozoic is long – 7 periods covering almost 300 million years. Therefore, we divide it into an early and late period. Cambrian + Ordovician + Silurian = early paleozoic (126 m.y)

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HISTORICAL GEOLOGY LECTURE 10. LATE PALEOZOIC GEOLOGY I.

HISTORICAL GEOLOGY LECTURE 10. LATE PALEOZOIC GEOLOGY I. The Late Paleozoic (Devonian-Mississippian-Pennsylvanian-Permian) is noted for a number of geologically significant events:. - widespread COLONIZATION of the land by large plants, reptiles and amphibians.

259 views • 21 slides

Precambrian Time and the Paleozoic Era

Precambrian Time and the Paleozoic Era. 9.2. Evolution. Evolution: an inheritable change in the characteristics within a population from one generation to the next; the development of new types of organisms from preexisting types of organisms over time

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