historical geology lecture 11 the proterozoic eon

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Historical Geology Lecture 11 The Proterozoic Eon

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Page 1: Historical Geology Lecture 11 The Proterozoic Eon

Historical Geology

Lecture 11

The Proterozoic Eon

Page 2: Historical Geology Lecture 11 The Proterozoic Eon

Historical Geology

I Proterozoic TimelineII Tectonics Overview

A) Continental GrowthB) Wilson Cycle Tectonics

III Paleoproterozoic Laurentia (North America)A) Orogenies (Convergence)B) Rifting (Divergence)C) SedimentationD) Climate

IV Mesoproterozoic Laurentia (North America)A) Orogenies (Convergence)B) Rifting (Divergence)C) SedimentationD) Climate

V Neoproterozoic Laurentia (North America)A) Orogenies (Convergence)B) Rifting (Divergence)C) SedimentationD) Climate

VI The Proterozoic Outside Laurentia

Outline

Page 3: Historical Geology Lecture 11 The Proterozoic Eon

Historical Geology

The Proterozoic Eon

1.0 bya

2.5 bya

1.6 bya

0.545 bya

Page 4: Historical Geology Lecture 11 The Proterozoic Eon

Historical Geology

The Proterozoic EonTectonics Overview

growing cratons

lateral plate tectonic movements

rifting and sea-floor spreading

wide continental shelves

epeiric seas

Page 5: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyThe Proterozoic Eon

Aggregating Cratons

accretion - addition of crustal materials to continental margins

aggregation – bringing together and consolidation of cratonic elements

Page 6: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyThe Proterozoic Eon

Early Epeiric Seas

epeiric sea - a shallow sea flooding the continental craton

Erikkson, et al., 1998

Page 7: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyThe Proterozoic Eon

Sedimentation Overview

Carbonates appear

Banded Iron Formations peak/disappear

Red Beds

Passive Margin Sedimentation

Page 8: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyThe Proterozoic Eon

Carbonate Sedimentation

Page 9: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyThe Proterozoic EonBanded Iron Formations

Page 10: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyThe Proterozoic Eon

Red Beds

oxidation4Fe + 3O2 ---> 2Fe2O3

iron + oxygen -> iron oxide

hematite

limonite

laterite soils

Red ShaleChuar Group (Grand Canyon)

Page 11: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyPaleoproterozoic Laurentia

Orogenies

Torngat (2.1-1.75 Ga)

Taltson-Thelon (2.0-1.9 Ga)

Penokean (2.0-1.8 Ga)

Wopmay (1.97-1.84 Ga)

Cape Smith-New Quebec (1.9-18 Ga)

Trans-Hudson (1.88-1.79 Ga)

Page 12: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyPaleoproterozoic Laurentia

Slave Province

Page 13: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyPaleoproterozoic Laurentia

Slave Province Aulacogens

Athapuscow Aulacogen

Bathhurst Aulacogen

Irving, et al., in press

Page 14: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyPaleoproterozoic LaurentiaSlave Province - Wopmay Orogen

Page 15: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyPaleoproterozoic Laurentia

Superior Province

Young, 2002

Ojakangas, et al., 2001

Page 16: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyPaleoproterozoic LaurentiaSuperior Province - Huronian Supergroup

Young, 2002

2.5 - 2.2 Ga

Gowganda FormationHuronian Supergroup

Gowganda Tillite

Page 17: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyPaleoproterozoic LaurentiaGlaciation

Page 18: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyPaleoproterozoic Laurentia

Superior Province - Animikie Group2.2 - 1.8 Ga Young, 2002

Banded Iron FormationAnimikie Group

Kona DolostoneAnimikie Group

Ajubik QuartziteAnimikie Group

Page 19: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyPaleoproterozoic Laurentia

Superior Province - Penokean Orogeny

Page 20: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyPaleoproterozoic LaurentiaSuperior Province Cross Section

Page 21: Historical Geology Lecture 11 The Proterozoic Eon

Historical Geology

Paleoproterozoic LaurentiaTrans-Hudson Orogen

Schwerdtner and Cote, 2001

Page 22: Historical Geology Lecture 11 The Proterozoic Eon

Historical Geology

Mesoproterozoic LaurentiaEvents

Elsonian Orogeny

Yavapai Orogeny

Mazatzal Orogeny

Mid-Continent Rifting

Grenville OrogenyAssembly of Rodinia

Page 23: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyMesoproterozoic Laurentia

Yavapai and Mazatzal Orogenies

Series of orogenies

~1.8 - 1.6 Ga

Vishnu Schist

Page 24: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyMesoproterozoic LaurentiaGrand Canyon Region

Page 25: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyMesoproterozoic LaurentiaGrand Canyon Region

Page 26: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyMesoproterozoic Laurentia

Mid-Continent Rift~1.2-1.0 Ga

Keweenawan Supergroup

Ojakangas and Dickas, 2002

Page 27: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyMesoproterozoic Laurentia

Grenville Orogeny

Page 28: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyMesoproterozoic Era

Rodinia

S W E A T

A U S W U S

Page 29: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyMesoproterozoic Era

Rodinia – SWEAT

Page 30: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyMesoproterozoic Era

Rodinia – AUSWUS

Page 31: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyNeproterozoic Laurentia

Breakup of Rodinia

Panthalassic Ocean (proto-Pacific)

Iapetus (proto-Atlantic)

Varangian Glaciation

Eykes and Januszczak, in press

Page 32: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyNeproterozoic Laurentia

Breakup of Rodinia

Page 33: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyNeproterozoic Laurentia

Panthalassa

Page 34: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyNeproterozoic Laurentia

Late Proterozoic Rifting

Grand Canyon Supergroup

Page 35: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyNeproterozoic LaurentiaGrand Canyon Supergroup

Page 36: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyNeproterozoic Laurentia

Late Proterozoic Rifting

Breakup of Rodinia

Panthalassic Ocean (proto-Pacific)

Varangian Glaciation

Page 37: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyNeproterozoic Laurentia

Late Proterozoic Rifting

Page 38: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyNeproterozoic Laurentia

Varangian Glaciation

Page 39: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyNeproterozoic Laurentia

Varangian Glaciation

OXYGENHeavy Oxygen-18 is incorporated into minerals. More Oxygen 18 during low temperatures.

STRONTIUMIncreased Sr86/87 ratio due to increased weathering during glaciation.

CARBON 12/CARBON 13Plants use the lighter isotope Carbon 12 in photosynthesis. The lower relative abundance of Carbon 13 means the plants were worse off (dying). Evidence in “cap” carbonates

Jacobson and Kaufmann, 1999Knoll, 2000Knoll, 2000

Page 40: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyNeproterozoic Era

Snowball Earth

Page 41: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyNeproterozoic Era

Snowball Earth

Page 42: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyNeproterozoic Era

Snowball Earth

Page 43: Historical Geology Lecture 11 The Proterozoic Eon

Historical GeologyThe Precambrian Outside North America