Title: Ordovician
1EARLY PALEOZOIC LIFE
Ordovician
2EARLY PALEOZOIC LIFE
Silurian
3EARLY PALEOZOIC LIFE
Plants in the Paleozoic
Stromatolites Blue-green algae Abundant in
Cambrian
4EARLY PALEOZOIC LIFE
Plants in the Paleozoic
Green algae Receptaculids Chlorophytes Silurian
to Devonian
Unknown affinity Sunflower coral Not sunflower
or coral
5EARLY PALEOZOIC LIFE
Plants in the Paleozoic
Land Plants Cooksonia Silurian
6EARLY PALEOZOIC LIFE
Mass Extinctions
7EARLY PALEOZOIC LIFE
Mass Extinctions
- Extinction Processes
- Extinction strikes on the land and in the sea.
- On the land, while animals suffer repeatedly,
- plants tend to be highly resistant to mass
extinctions. - Preferential disappearance of tropical forms of
life - during mass extinctions.
- Tendency of certain groups of animals to
experience - them repeatedly (for example, trilobites and
- ammonoids).
- Alleged equal spacing, or periodicity in
geological time - (occurring about every 26 million years).
8EARLY PALEOZOIC LIFE
Mass Extinctions
9EARLY PALEOZOIC LIFE
Mass Extinctions
10EARLY PALEOZOIC LIFE
Mass Extinctions
Ordovician Mass Extinction Second most
devastating in earth history Caused by glaciation
and associated lowering of sea level
11EARLY PALEOZOIC LIFE
Mass Extinctions
Devonian Mass Extinction Caused by glaciation or
meteorite impact
12EARLY PALEOZOIC LIFE
Mass Extinctions
Permian Mass Extinction 90-95 of marine species
became extinct in the Permian Caused by formation
of Pangea, glaciation, volcanic eruptions
13EARLY PALEOZOIC LIFE
Mass Extinctions
Triassic Mass Extinction 25 of all families
became extinct at end of Triassic Caused by
climate change (increase in rainfall)?
14EARLY PALEOZOIC LIFE
Mass Extinctions
Cretaceous-Tertiary (K-T) Mass Extinction 85 of
all species died in the K-T extinction Caused by
meteorite impact and/or volcanic eruptions
15 THE DEVONIAN
The Age of Fishes Named for outcrops near
Devonshire, England Named by Sedgewick and
Murchison in 1839 prior to bitter
arguments Includes the Old Red Sandstone of
Scotland and Wales
16THE DEVONIAN
The Age of Fishes
17THE DEVONIAN
18THE DEVONIAN
Kaskaskia Sequence Began in Devonian and
continued to the end of the Mississippian Craton
again flooded
19THE DEVONIAN
Kaskaskia Sequence Began with deposition of
clean quartz sand Initial deposit of
transgressing sea Oriskany Sandstone
20THE DEVONIAN
Kaskaskia Sequence Oriskany Sandstone Some heavy
minerals Indicate source area Sandstone
followed by Limestones Salts and
gypsum Shales
21THE DEVONIAN
Acadian Orogeny
22THE DEVONIAN
Devonian Paleogeography
23THE DEVONIAN
Devonian Paleogeography
24THE DEVONIAN
Impact of Avalonian Terrane Thick folded
sequence of turbidites Intruded with rhyolites
and granites Destroyed the marine depositional
basin off eastern US coast
25THE DEVONIAN
Impact of Avalonian Terrane Nonmarine clastics
shed to west
26THE DEVONIAN
Impact of Avalonian Terrane Changes from
conglomerate to shale going east to west
27THE DEVONIAN
Impact of Avalonian Terrane
Catskill Clastic Wedge
28THE DEVONIAN
Impact of Avalonian Terrane
Catskill Clastic Wedge
29THE DEVONIAN
Impact of Avalonian Terrane
Catskill Clastic Wedge Nonmarine rocks red
color Braided or meandering streams
30THE DEVONIAN
Impact of Avalonian Terrane
Catskill Clastic Wedge
31THE DEVONIAN
Impact of Avalonian Terrane
Catskill Clastic Wedge
First forests Gilboa, NY
32THE DEVONIAN
Impact of Avalonian Terrane
Gilboa, NY Fossils
Winifred Goldring NY State Paleontologist First
woman to hold title
Aneurophyton (foliage) Eospermatopteris (tree)
33THE DEVONIAN
Impact of Avalonian Terrane
Gilboa, NY Reconstruction of Forest
34THE DEVONIAN
Europe Old Red Sandstone Equivalent to Catskill
Clastic Wedge
35THE DEVONIAN
Acadian shales Chattanooga Shale Few fossils,
stagnant anoxic water High organic content,
black, phytoplankton bloom
36THE DEVONIAN
Western US Williston Basin Reefs developed Salt
and gypsum Extensive oil reserves
37THE DEVONIAN
Western US Antler Orogeny Late Devonian to
Pennsylvanian Began with subduction on west coast
38THE DEVONIAN
Western US Antler Orogeny Late Devonian to
Pennsylvanian Convergence of volcanic island arc
39THE DEVONIAN
Western US Antler Orogeny Convergence of volcanic
island arc
40THE DEVONIAN
Devonian Paleogeography