Cambrian and Ordovician

0.0(0)
studied byStudied by 0 people
learnLearn
examPractice Test
spaced repetitionSpaced Repetition
heart puzzleMatch
flashcardsFlashcards
Card Sorting

1/29

flashcard set

Earn XP

Description and Tags

Chapter 10 of historical Geology

Study Analytics
Name
Mastery
Learn
Test
Matching
Spaced

No study sessions yet.

30 Terms

1
New cards

with the paleozoic eon brought

abundant life, dramatic change in rock types, atmosphere change from icehouse to greenhouse (oxygen started to build up)

2
New cards

how short and how many days existed in the early paleozoic

21hrs, 430 days per year

3
New cards

how can we tell that North America’s margins are passive

they have thick prisms of sediments on newly shifted margins and thin sediments over craton

4
New cards

epeiric seas

relatively shallow, geographically wide-spread bodies of water covered large parts of the continent

5
New cards

what was a change with the beaches in the cambrain

they were mature, primarily quartz sandstone beaches, as opposed to the dirty greywhackies they used to be

6
New cards

arches

topographically high areas that influenced surrounding sedimentation; areas of extremely shallow water or even islands

7
New cards

basins

topographically lows that act as receptacles for sediments; oval in plan; thickest beds in center; like michigan basin

8
New cards

transgressions

deposit sediments on cratons

9
New cards

regressions

erosion and unconformities

10
New cards

sequences

large packages bound by craton-wide unconformities

11
New cards

6 sequences on craton Paleozoic to recent

Sauk, Tippecanoe, Kaskaskia, Absaroka, Zuni, and Tejas

12
New cards

Sauk sequence started

635 myo

13
New cards

what occured during the Sauk sequence

transgression Sauk Sea flooded at least ¾ of the north american craton and left only canadian shield and transcontinental arch above sea level

14
New cards

sediment multicycle

repeated erosion, transportation, and deposition

15
New cards

the lowest rock unit during the paleozoic is usually

ripple marks, which indicate a shallow water deposit on the beach

16
New cards

why would weathering be different during the paleozoic

there were no land plants, so wind was the most common weathering fatcor

17
New cards

2 types of sandstone during the paleozoic

ripple marks and small scale cross-beds that have fossils

frosting and large scale cross-beds that lack fossils

18
New cards

frosting implies

wind transport

19
New cards

ripple marks imply

water deposition

20
New cards

Sauk sequence concludes in

Early Ordovician

21
New cards

the sauk sequence contains

limestone and is truncated by a big unconformity

22
New cards

tippecanoe transgression started in

middle ordovician

23
New cards

St. Peter sandstone is called supermature b/c

over 99% is quartz that is well-sorted and well-rounded

24
New cards

what form of tippecanoe covers Wisconsin, Illinois, Iowa, and Oklahoma

St. Peter sandstone

25
New cards

St. Peter sandstone is part of which sequence

tippecanoe

26
New cards

clastic wedge

accumulation of clastic sediment deposited next to an uplifted area

27
New cards

cambrian life includes

trilobites, archaeocyathans, primitive brachiopods, archaic mollusks, archaic echinoderms

28
New cards

what happened to all experimental groups of cambrian life

they went extinct except for lingula

29
New cards

what was the dominant fossil of the cambrian

trilobites

30
New cards