Test #2 Flashcards
List the major sea level cycles (Sloss cycles) of the Paleozoic and during what periods they existed.
Sauk- Precambrian - early Ordovician
Tippecanoe- Mid Ordovician - the Early Devonian
Kasaskia- Mid Devonian - Mississippian boundary
Absaroka- Pennsylvanian boundary - Jurassic periods
Explain the difference between the Flysch and Molasse phases of sedimentation during orogenies.
Flysch phases involve shales and turbidites (marine sediment) that are accumulated in foreland basins during mountain building. Molasse phases involve non-marine sediment deposited after the mountain has formed.
Explain how trilobites prove the accretion of exotic terrains to the eastern margin of North America. Name the genus of trilobite.
During the Taconic Orogeny subduction was in the opposite direction than it currently is, which caused collision of igneous arcs with Laurentia. Trilobites and other fossils known only in specific exotic terranes are included in these areas which prove the landmass accretion. Peridoxies is the Trilobite.
What type of basin formed on the eastern margin of North America during the Taconic Orogeny? Acadian Orogeny? When did these orogenies occur?
Taconic- peripheral foreland basin- Ordovician
Acadian- retroarc foreland basin- Mid/Late Devonian
What is the difference between Stromatolites and Stromatoporoids?
Stromatolites are layered accretionary structures produced by cementation of cyanobacteria that show some of the most ancient records of life on earth. Stromatoporoids are sponges that were important to reef-building during the Ordovician.
What are Sepkoski’s three evolutionary faunas?
1) Cambrian Fauna
2) Palaeozoic Fauna (Ordovician to Permian)
3) Modern Fauna (since Triassic)
Explain the hypothesized causes for the two steps of the end Ordovician Mass Extinction.
1) The onset of glaciation caused extinction of many taxa because they were adapted to warmer conditions.
2) When the climate eventually warmed back up, many taxa that had adapted to the cool conditions died out.
Explain why the Michigan Basin contains large amounts of evaporites during the Silurian.
Seas in the Michigan Basin had high saline content which flowed from North American inlets, which sank to the bottom of the seas. Sunlight and warm temperatures caused evaporation of the water and concentrated the salt. This salt was then “trapped” by reef banks around the edges of the basin.
What was the dominant predator of the Silurian?
Eurypterids.
Why do we see a wedge-shaped package of sediment thickest in the east that formed during the Devonian in New York State?
The Acadian Orogeny occured during the Devonian which formed a retroarc foreland basin. The flysch and molasse phases filled the basin with sediment. As you move westward, the basin thins out which causes its wedge-shaped appearance.
List and describe two possible reasons for widespread black shale deposits during the Devonian.
1) Deep sea deposits: dying of reefs, below photic zone and stagnant water.
2) Worldwide increase of salinity by evaporation condition- petroleum source.
What type of basin formed during the Acadian Orogeny?
The Acadian Foreland Basin is a retroarc foreland basin.
How do the White Mountains of New Hampshire relate to the Acadian Orogeny?
The White Mountains formed during the Acadian Orogeny. The orogeny was the result of the collision between current day North America and Western Europe. The collision caused the crust to deform and uplift to form the White Mountains.
What type of basin formed on the western margin of North America during the Antler Orogeny? When did this occur?
It formed an elongated peripheral foreland basin during Late Devonian and Early Mississipian times.
When was the time period on Earth with the largest reefs ever?
Devonian.
What types of brachiopods were dominant during the Ordovician? Silurian? Devonian? Carboniferous?
Ordovician- Orthids and Strophomenids
Silurian- Pentamerids, Strophomenids, Spiriferids
Devonian- Spiriferids
Carboniferous- Decline of spiriferids replaced by productides